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__________________________________________________________________
2008-2009 NORTH SHORE PROJECT
DIAMOND DRILLING REPORT
J.L. BICZOK, P.GEO. and J. EDWARDS June 2010
i
TABLE OF CONTENTS
SUMMARY ............................................................................................................... 1
INTRODUCTION ..................................................................................................... 2
LOCATION AND ACCESS ...................................................................................... 3
PROPERTY DESCRIPTION .................................................................................... 5
REGIONAL GEOLOGY............................................................................................ 7
PROPERTY GEOLOGY ........................................................................................ 12
STRATIGRAPHY ........................................................................................................... 12
STRUCTURAL GEOLOGY .......................................................................................... 19
METAMORPHISM ......................................................................................................... 21
MINERALIZATION ......................................................................................................... 21
PAST WORK ......................................................................................................... 22
CURRENT PROGRAM .......................................................................................... 23
RESULTS .............................................................................................................. 26
LITHOLOGIES ................................................................................................................ 26
STRUCTURE .................................................................................................................. 28
MINERALIZATION ......................................................................................................... 29
CONCLUSIONS ..................................................................................................... 30
RECOMMENDATIONS .......................................................................................... 30
STATEMENT OF EXPENDITURES ...................................................................... 32
STATEMENT OF QUALIFICATIONS..................................................................... 34
LIST OF REFERENCES ........................................................................................ 35
ii
LIST OF FIGURES
Figure 1: General Location Map. .............................................................................. 4
Figure 2: Detailed Location Map .............................................................................. 5
Figure 3: Musselwhite Claim Map ............................................................................ 6
Figure 4: Detailed Claim map of the North Shore diamond drilling area .................. 7
Figure 5: General geology of the northwestern Superior Province (Stott and
Rayner, 2005). ......................................................................................................... 8
Figure 6: Regional geology of the North Caribou greenstone belt (OGS, 1991) ...... 9
Figure 7: General geology of the North Caribou greenstone belt. .......................... 10
Figure 8: Stratigraphy of the Musselwhite Mine area. ............................................ 15
Figure 9: Detailed stratigraphy of the Northern Iron Formation .............................. 17
Figure 10: DRILL SECTION ........................................................................ Attached
LIST OF TABLES
Table 1: Rock type codes used at musselwhite ..................................................... 12
Table 2: Summary table of 2008-9 NSD drill holes. ............................................... 26
Table 3: Significant intercepts from 2008-9 NSD drill program. ............................. 30
Table 4: Summary of major costs incurred, 2008-9 NSD drill program. ................. 33
LIST OF APPENDICES
Appendix I: Diamond Drill Logs ................................................................... Attached
Appendix II: Assay Lab Results .................................................................. Attached
Appendix III: Assay Lab Certificates ........................................................... Attached
Appendix IV: Assaying and QAQC Procedures and Results....................... Attached
Appendix V: Diamond Drilling Invoices ....................................................... Attached
Appendix VI: Chemex Invoices .................................................................. Attached
1
SUMMARY This report presents the results of the “North Shore” deep drilling program conducted
from January 3, 2008 to April 17th, 2009. The holes described herein were drilled from
the north side of Opapimiskan Lake to test for the on-strike extension of the
Musselwhite mine orebodies, primarily the PQ Deeps zones. These holes targeted the
projected location of the PQ Deeps1.6 – 2.0km below surface. They are the second
phase of the NSD program that started in 2006 and was completed in 2009. This
program consisted of two fans of drill holes collared on 14,775N (Mine Grid co-
ordinates). The second fan was collared in 2007 some 290 metres west of the first fan
which was reported on in the 2006-2007 North Shore Project Diamond Drilling Report
(Biczok, 2007). These two fans of drill holes are located 1.7km north of the
northernmost limit of previous drill testing of the PQ Deeps (which was conducted from
two barges on Opapimiskan Lake and completed in June 2006). Phase One drilling
confirmed the presence of thick sections of the target Northern and Southern Iron
Formations in the North Shore area. Phase Two drilling, however, failed to intersect
the expected position of the PQ-Deeps synformal keel due to its unexpected and
complex geometry. More drilling is recommended to fully define the potential of this
area.
2
INTRODUCTION
Drilling the down-plunge, northward extension of the Musselwhite orebodies beneath
the northern part of Opapimiskan Lake has been ongoing since 2002 with drilling both
from land and the winter ice cover of the lake. From 2003-2006 inclusive, deep drilling
was conducted from two barges on the lake with fans completed every 2-300m
between 12,100N and 13,000N. In 2006, the first phase of the North Shore Deep
Drilling Project (NSD) commenced and appears to have successfully intersected the
Northern Iron Formation (NIF) on the eastern limb of the PQ-Deeps synform several
hundred metres above the keel. Significant mineralization typical of the Musselwhite
Mine PQ Deeps orebody mine was intersected in the Northern Iron Formation and
several smaller but still appreciable intercepts were returned from “Intraformational“
silicate facies iron formations and shear zones in the adjacent metavolcanics. This
report summarizes the follow-up drilling of this 2006-7 program conducted during
2007-8
Drilling was being conducted on Musselwhite’s behalf by two contractors:
1) Boart Longyear Inc. (Boart) based in Haileybury, Ontario, using a Longyear
LY55 diamond drill.
2) Layne Christensen Canada (Layne) based in Capreol, Ontario, using a
CS4000 diamond drill.
A summary of the annual activities is presented below.
2008: Boart crews mobilized to the site January 5th and resumed drilling of hole 07-
NSD-008 on January 10th. A total of 455m was drilled from 1,747m to 2,202m before
the hole was lost on March 23rd, 2008 due to broken rods. A new daughter hole, 08-
NSD-001, was then wedged off 07-NSD-008 on March 23rd at a depth of 1,349m. It
was completed on June 28th, 2008 with a total of 1092m having been drilled from
1,349m to 2,441m. A second daughter 08-NSD-002 was then wedged off 08-NSD-001
on July 1st, 2008 at a depth of 1,514m. A total of 906m were drilled from there to end
of hole at 2,420m on September 7th, 2010. The third daughter hole 08-NSD-003, was
3
wedged off 07-NSD-008 at a depth of 950m on September 7th, 2008. Unfortunately,
only 402m was drilled to a depth of 1,352m before the drilling equipment was lost in
the hole. Attempts to retrieve it continued until October 4th, 2008 at which point the
hole was finally abandoned. The final hole of the 2008 program, 08-NSD-004, was a
wedge off of the pilot hole 07-NSD-008 beginning at a depth of 665m. As of December
2008 a total of 776m had been drilled in this hole.
2009: Boart resumed drilling of 08-NSD-004 on January 10, 2009 at a depth of 1441m
and finished the hole at a depth of 2387m on March 14th, 2009. Their drill and
associated equipment was them demobilized from the site by March 24th, 2009.
2009: Layne began mobilizing their crews to the site and making the required ice road
to the North Shore January 6th and this work continued to February 8th. The drill rig
was moved to the drill to North Shore site February 9th. On February 20th they began
drilling wedge hole 09-NSD-001 off of pilot hole 06-NSD-001 at a depth of 1446m. The
hole finished at a depth of 1978m on April 17th, 2009 and the equipment was
demobilized thereafter.
LOCATION AND ACCESS
The Musselwhite Mine property is located in the Patricia Mining District of
northwestern Ontario on NTS map sheet 53B/9. The mine is located at 52° 36’ 50” N
latitude and 90° 21’ 43” W longitude. It is 480 km NNW of Thunder Bay (Fig. 1) and
103 km north of Pickle Lake. It is serviced by an all-weather gravel road that extends
north from Pickle Lake (Fig. 2) as well as charter air service from Thunder Bay and
several local communities including Sioux Lookout, Round Lake and Cat Lake.
Access to the drill site from the mine is by boat in summer, snowmobile and/or pick-up
trucks in winter depending on the ice thickness at the time.
4
Figure 1: General Location Map.
5
º
89º90º91º
52º
53º
0 25 50
Km
Figure 2: Detailed Location Map
PROPERTY DESCRIPTION
The Musselwhite Mine property currently consists of 283 unpatented and 338 leased
claims covering an area of approximately 17,620 Ha (Fig. 3). The property is wholly
owned by Goldcorp Canada Ltd. The work described herein was conducted on the
following claims: 529778, 529785, 529786, 502219, 502220, 502221, 502222,
502223, and 502224 (see Fig. 4). Additional details are provided in the Statement of
Expenditures at the end of this report.
Exploration and mine development at Musselwhite is based upon a local mine grid
system with a grid north that is oriented at 42º 02’ 57” west of true north.
6
Figure 3: Musselwhite Claim Map
Musselwhite North Shore Drilling
7
Figure 4: Detailed Claim map of the North Shore diamond drilling area
REGIONAL GEOLOGY The Musselwhite Property covers a portion of the northwest-trending North Caribou
Lake greenstone belt which is located in the northern margin of the Archean North
Caribou Superterrane (NCS), adjacent to its internal boundary with the Island Lake
Domain (Figs. 5 & 6). The NCS is a continental block consisting of ~3.0Ga juvenile
plutonic and minor volcanic rocks which underwent two periods of rifting and related
deposition of arc sequences at 2.98-2.85 Ga and 2.85-2.71 Ga followed by extensive
reworking by continental arc magmatism at 2.75-2.70 Ga (Percival, 2007, and
references therein). The North Caribou greenstone belt is one of the earlier arc
sequences. Volcanic rocks of this belt have been dated at ~2981-2932Ma (Breaks et
8
al 2001) and, more specifically, those in the mine area at 2.98-2.97 Ga (Klipfel, 2002).
The lower portion of the volcanic pile is dominated by ultramafic to high-Mg basalts,
iron formation and lesser siliciclastic sediments, a “primitive” sequence common in
many greenstone belts of the NCS and interpreted to be products of plume-related
rifting by Hollings and Kerrich (1999).
Musselwhite
Figure 5: General geology of the northwestern Superior Province (Stott and Rayner, 2005). The North Caribou greenstone belt (NCGB) has been mapped at various times by
Satterly (1941), Emslie (1962), Sage and Siragusa (1979), Andrews et al (1981), and
most recently a 3 year, multi-disciplinary effort in the mid-1980’s by Breaks et al
(2001). These latter authors subdivided the NCGB into 8 lithotectonic supracrustal
assemblages which were then modified somewhat by Thurston et al (1991) and
9
Figure 6: Regional geology of the North Caribou greenstone belt (OGS, 1991)
Hollings and Kerrich (1999) (see Fig. 7). For the sake of this report, the combined
terminology of Thurston et al (1991) and Hollings and Kerrich (1999) will be used and
only those units occurring in the Opapimiskan Lake area will be discussed in any
detail. It is entirely possible that many of the volcanic and sedimentary assemblages
found in the northern portion of the NCGB are correlative with similar units in the
southern portion (i.e. in the vicinity of Opapimiskan Lake) as they have relatively
similar lithologies and lithogeochemical signatures. Unfortunately many of the
supposed contact areas lie beneath Opapimiskan Lake or swamps.
Musselwhite Mine
10
North Caribou Lake
Weagamow Lake
Eyapimikama Lake
Opapimiskan Lake
Forester Lake
MusselwhiteMine
NorthShoreProject
90° 30’
90° 30’
52° 30’
0 15 kmNorth CaribouAssemblages
Aguta Arm Felsic VolcanicsAguta Arm Mafic Volcanics
Keeyask Metasediments
Zeemal-Heaton MetasedimentsEyapamikama metasediments
Opapimiskan MetavolcanicsForester MetavolcanicsSouth rim Metavolcanics
North Rim Metavolcanics
McGruer Metavolcanic Rocks
N
Based upon mapping by Breaks et al (2001) in Thurston (1991)
Figure 7: General geology of the North Caribou greenstone belt.
There are 4 major dominantly volcanic rock suites observed in the Opapimiskan Lake
area and these make up the McGruer Assemblage:
North Rim Metavolcanic Suite: Dated at 2932 Ma by D. Davis (unpublished date
quoted in Thurston et al, 1991). Occurs in the northeast corner of Opapimiskan
Lake and extends northwest from there over 97km along the northern margin of
the greenstone belt. It consists largely of mafic and lesser ultramafic volcanic
rocks.
South Rim Metavolcanic Suite: Occurs on the northwestern side of Opapimiskan
Lake and extends northwest from there more than 50km along the southern
margin of the NCGB. Regionally it is dominated by fine- to medium-grained,
massive to pillowed basaltic flows with minor felsic and intermediate units and rare
ultramafic units. Drilling by the Musselwhite exploration department over the past 7
11
years has identified a thick sequence of felsic volcanic flows, tuffs and
volcaniclastic sediments beneath Opapimiskan Lake and at depth below the mafic
volcanics exposed on the northwest shore of the lake. This felsic pile varies from
coarse pyroclastics to very fine-grained, massive units (flows or welded ash tuffs?)
to biotite-rich volcaniclastic sediments. These features and the sheer volume of the
felsic units indicate that there was a major felsic volcanic edifice at this location. If
these units are part of the South Rim suite they appear to overly the Opapimiskan-
Markop suite. However, the continuation of intraformational iron formations
common in the upper Opapimiskan-Markop suite into the lower section of the felsic
volcanics of the South Rim (?) suite implies at the very least that this is largely a
conformable contact. Alternatively, the Opapimiskan-Markop volcanism may
actually include the felsic and mafic rocks on the north side of Opapimiskan Lake.
U-Pb age dating of these felsic rocks is currently underway and may shed light on
this problem.
Opapimiskan-Markop Metavolcanic Suite: Occupies the central portion of the
NCGB in the Opapimiskan Lake area and is dominated by mafic to ultramafic flows
with intercalated clastic and chemical sedimentary units, including the banded iron
formations which host the Musselwhite gold deposit. This is described in more
detail in the following section.
Forester Lake-Neawagank Metavolcanic Suite: Dominated by mafic and
ultramafic volcanics and occurs in the southeastern extremity of the belt.
Two predominantly sedimentary units occupy the central axis of the NCGB:
Eyapamikama Metasedimentary Assemblage (north of Opapimiskan
Lake): a fine-grained clastic sedimentary sequence interpreted as a submarine
turbidite fan by deKemp (1987) and Thurston et al (1991). The linear belt of
these metasediments depicted on OGS maps (Breaks et al 1987) north of
Opapimiskan Lake has been mapped and lithogeochemically sampled by
12
Musselwhite geologists and found to be less extensive than indicated. The
majority of outcrops mapped as metasediments in this area are in fact sheared
and altered basalts.
Zeemal-Heaton Assemblage (south of Opapimiskan Lake): Previously
included by Breaks et al (2001) as part of the Eyapamikama Assemblage, later
workers have assigned this belt of fine-grained clastic sediments to its own unit.
It occupies the central portion of the belt southeast of Opapimiskan Lake and
overlies the Forester Lake-Neawagank suite. Minor felsic volcanic and banded
iron formation units occur in several localities within this suite.
PROPERTY GEOLOGY
STRATIGRAPHY Rocks hosting the Musselwhite gold deposit belong to the aforementioned
Opapimiskan-Markop and have been subdivided into a detailed stratigraphy that is
relatively consistent over the property although major facies changes are locally
observed along and across strike. This “mine stratigraphy” is depicted in Fig. 8 and
rock type codes used at Musselwhite are listed in Table One.
The lowermost units observed in drilling to date are fine-grained siliciclastic sediments
with minor felsic volcanics that occur ~500m east of the mine. It is assumed that these
are underlain by mafic-ultramafic flows which crop out 2.5km southeast of the mine
along the eastern edge of the belt on the shores of Lake “282”. These are followed by
largely komatiitic basalts and ultramafic flows/intrusions with local andesite flows. This
predominantly high-Mg series of volcanic rocks is overlain by two major banded iron
formations (BIF) separated by 10-30m of mafic-ultramafic volcanics. The lowermost
BIF is locally termed the Southern Iron Formation (SIF) and is a generally monotonous
sequence of thinly laminated magnetite and chert. There is generally little or no
silicate, sulphide, or other facies within this horizon in the mine area. The SIF
commonly occurs in two principal horizons, each anywhere from 5 to 20m thick,
13
Table 1: Rock Type Codes Used at Musselwhite
ULTRAMAFIC ROCKS 1 Unsubdivided
1M Ultramafic Amphibolite 1S Serpentinized Ultramafic
MAFIC VOLCANIC & RELATED ROCKS
2 Unsubdivided
2A Massive, fine- to medium-grained flow 2B Amygdaloidal flow 2D Pillowed flow, pillow breccia, hyaloclastite 2E Flow breccia 2G Pyroclastic breccia, tuff-breccia 2H Tuff, lapilli-tuff 2K Dikes, sills, small intrusions 2T Biotite-bearing metavolcanics 2U Garnet-bearing metavolcanics
FELSIC TO INTERMEDIATE VOLCANIC & RELATED ROCKS 3 Unsubdivided
3A Intermediate flow 3B Intermediate pyroclastic breccia, tuff-breccia 3C Intermediate tuff, lapilli-tuff 3D Felsic flow 3E Felsic pyroclastic breccia, tuff-breccia 3F Felsic tuff, lapilli tuff 3G Subvolcanic rocks, unsubdivided 3H Subvolcanic quartz-plagioclase porphyry 3J Subvolcanic quartz-porphyry 3K Subvolcanic plagioclase porphyry 3M Felsic volcaniclastic rocks 3P Intermediate dikes, sills, small intrusions
IRON FORMATION 4A Chert-grunerite 4B Chert-magnetite iron formation 4C Carbonate 4B (not generally used)
4CH Chert (not generally used) 4CHP Chert with pyrite and pyrrhotite (not generally used)
4E Garnet-amphibole iron formation 4EA Garnet-amphibole-grunerite iron formation 4F Garnet-biotite schist 4H Sulphide iron formation 4I Graphitic iron formation (rarely used)
4TB Banded iron formation tectonic breccia
14
Table One continued CLASTIC SEDIMENTS
6 Unsubdivided (typically an arenite with variable biotite %) 6K Wacke 6M Arenite 6N Mudstone 6P Feldspathic wacke 6R Feldspathic arenite 6T Quartz arenite 6W Garnet-bearing mudstone/sandstone
MAFIC TO ULTRAMAFIC INTRUSIONS 7A Gabbro (C.l. = 35-90) 7B Leucogabbro (C.l. = 10-35) 7C Plagioclase-phyric gabbro
7D Mafic dikes, sills, small intrusions Unrelated to mafic volcanic rocks
7F Peridotite
7H Ultramafic rocks and altered equivalents of probable intrusive origin
7J Amphibolite GRANITOID INTRUSIONS
8A Diorite 8B Quartz diorite 8C Trondhjemite 8D Tonalite 8E Granodiorite 8F Granitic pegmatite 8H Biotite trondhjemite 8J Granite 8K Quartz monzonite 8M Gneissic granite
MISCELLANEOUS 13 Olivine Lamprophyre Dyke
No Log Upper part of mother hole, trace repeated for a wedge hole QTZ VN Quartz Vein
SHZ Shear Zone, protolith unknown
15
v v v v v v
v v v v v
v v v
v v
v v v
v v
v v v v v v v v v v v v v v v v v v v v v v v v v v
Basalt?
+ + ++ + + + + +
+ + + + + + ++ + + + + + +
+ ++++
>300m
+110
+60
0
-25-40-55-70
-200
-300
-800m
"AVOL" Massive dacite to rhyolite flows, ash & lapilli tuffs and tuff breccia
"BVOL" Tholeiitic basalt, 0-50m thick, includes ~ 4 thin IFs
2920 +/- 5
Northern Iron Formation See Figure 9 Mineralization @ 2690 Ma
Age (Ma) Unit No.
"Basement Volcanics" (2VOL) Komatiitic Basalts, Andesites, Ultramafics
Southern Iron Formation Typically 2 thinly laminated chert-mt BIFs, 5-30m thick
"Lower Basalts" Komatiitic Basalts and Ultramafic Flows
Felsic Volcanics Rhyolite tuffs, up to 30m thick
"Unit 6" Metasediments Arenite-fine grained quartzose sediments, 50-150m thick
"Lower Basalts" Basaltic and extensive Ultramafic flows; Sequence 500m thick.>
Late Granite Plutons Massive plutons intruding both older gneiss & greenstone belt
2420-2485
Older Gneissic Basement Gneissic TTG batholiths 2855-3020
?UNCONFORMITY
Musselwhite Mine StratigraphyLithostratigraphy Lithology
Opa
pim
iska
n V
olca
nics
Eya
pam
ikam
a L
ake
Sed
imen
ts
3
2
4
2
4
2
2
63
Figure 8: Stratigraphy of the Musselwhite Mine area.
separated by 5-10m of basalt. The SIF hosts a number of small ore zones including
the Ranger, Red Wing and Thunderwolves.
About 20-30m above the SIF is the Northern Iron Formation (NIF), the main ore host
at Musselwhite. This is a complexly layered horizon typically ~40m thick in total and
comprised of several different facies with locally intense overprinting alteration,
shearing and mineralization (Fig. 9). Not every facies is always present across the
drilled extent of the NIF, but where they are, the following stratigraphy is observed
from the base to the top of the formation.
16
Unit 4H: This unit is a sulphidic iron formation, typically composed of 10-30%
syngenetic pyrrhotite in a dark grey to black cherty argillite. The pyrrhotite is
commonly remobilized into cross-cutting fractures/veins accompanied by quartz veins,
however, no appreciable gold mineralization has been detected in this unit. The
continuity of the 4H is poor and where present its thickness varies from 10m in the
Esker fold area to a more common 10-50cm elsewhere.
Unit 4A: This unit is fairly ubiquitous throughout the mine area and is the most
common basal unit of the NIF. It is composed of pale grey, weak-moderately magnetic
chert, interlayered with 30-50%, diffuse bands of fine-grained, light yellow grunerite.
Minor magnetite laminae and bands, up to ~25%, are common as is a minor, fine-
grained intergrowth of calcite amongst the grunerite.
Unit 4B: Composed of thinly laminated to thick-banded (~1-2cm) chert-magnetite
oxide-facies BIF, the 4B is typically 20-30m thick and forms ~3/4 of the NIF (and
usually all of the SIF). It can be subdivided into two varieties: a lower, thick-banded,
relatively pure chert-magnetite BIF, and an upper thinly laminated, more clastic-rich
variety. The latter variety consists of 2 alternating “zones” typically <1-2cm thick, one
composed of thin, diffuse laminae of magnetic chert, the other a more homogeneous,
medium-dark green, fine-grained amphibolite. With increasing stratigraphic height
these amphibole dominant bands become garnetiferous and may contain up to 25%
pale red garnets <2mm in diameter. The amphibole+/-garnet layers are readily
affected by hydrothermal alteration and are highly altered to massive fine-grained
black biotite, with an associated coarsening of the garnets, adjacent to mineralized
shear zones and/or major quartz veins.
Unit 4EA: Although historically the 4EA has been regarded as being a mix of garnet-
grunerite and green amphibole, drilling along strike from the main ore zones has
shown that the green amphibole (hornblende or ferrotschermakite; Otto, 2002)
17
- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -
- - - - - - - - - - - - - - - - - - - -
Garnetiferous ferruginous amphibolite
Meta-arenite or siltstone
Garnet-biotite-quartz staurolite (Meta-pelite)+
Layered garnet-grunerite and chert Silicate Iron Formation. Alters to green amphibole near quartz veins. Main Ore Host.
Hydrothermal garnet-biotite alteration and quartz veining present below mineralization.
"Clastic-rich" thinly laminated Oxide-Silicate BIF. Alternating magnetite and amphibole garnet laminae, readily alters to biotite-garnet.
+
Thick banded (~1 cm) magnetite and chert BIF.
Chert with 20-40% diffuse bands of fine grained grunerite, minor carbonate.Pyrrhotite-rich meta-argillite cherty layers.+
INC
RE
AS
ING
CL
AS
TIC
S
4A
4H
4B
"Clastic 4B"
4EA
4F
64E
alteration zone
Northern Iron Formation
Figure 9: Detailed stratigraphy of the Northern Iron Formation
18
forms adjacent to quartz veins within shear zones, presumably due to calcic alteration
of the original grunerite. Consequently, “primary” 4EA is now regarded as a silicate
iron formation composed solely of massive bands of garnet-grunerite with lesser, ~20-
30%, bands of pale grey, moderately magnetic chert. The garnet-grunerite layers
typically contain ~30-55% garnets, 1-4mm across, in a fine-grained matrix of pale
yellow grunerite. The 4EA forms the main ore-host at Musselwhite and mineralization
within it is characterized by shearing, quartz flooding/veining, formation of green
amphibole adjacent to the veins, significant coarsening of the garnets due to
overgrowths, and pyrrhotite mineralization.
Unit 4F: The 4F is a garnet-biotite +/- staurolite schist with an average Fe2O3 content
of ~25-30% and thus qualifies as an iron formation itself. Typically it contains 30-55%
subhedral garnets, 1-5mm across, in a fine grained matrix of 60-70% biotite with
lesser quartz, feldspar and magnetite. Although the 4F within the NIF itself has little or
no staurolite, intraformational 4F horizons within the basaltic pile commonly contain up
to 30-40% anhedral, light yellow staurolite grains 1-2mm across. In areas of apparent
hydrothermal alteration (e.g. bordering mineralized 4EA, adjacent to quartz flooded
shear zones), the 4F matrix is commonly appears to be altered to >90% biotite. To
the west of the T-Antiform the 4F becomes more variable and commonly contains up
to 20-30% chert layers <2-3cm thick, minor 4E layers, and in some areas, abundant
thin layers of magnetite up to 3-4mm thick.
Unit 6: This is a thin but semi-continuous unit, typically <1m thick, that occurs at the
top of, or in the upper portion of, the 4F sequence in the NIF. It is a light beige-grey,
siliceous, fine-grained, equigranular, very homogeneous rock composed of 20-30%
finely dispersed biotite and 70-80% Quartz-Feldspar. It is characterized by 2-5%
quartz “sweats”, small discontinuous, locally derived veinlets. Contacts are commonly
sharp although they can be gradational over a 10-20cm into the 4F. Lithogeochemical
analyses indicate that this unit averages 63% SiO2, and 16% Al2O3. Compositionally it
19
is very similar to the local felsic volcanic rocks but has relatively elevated levels of V,
Mn and Ba. It is interpreted as a waterlain felsic ash tuff
Unit 4E: Where present, the 4E averages 25% Fe2O3 and forms the uppermost unit of
the NIF. It is generally quite thin, <1m, and often only 10-30cm, but is commonly
highly mineralized in some parts of the mine. It is a fine-grained, massive medium-
dark green amphibolite with little or no visible quartz or feldspar, studded with 15-30%
anhedral pale red garnets 2-4mm across. Overall it is similar chemically to the 4EA but
contains ~2% less silica and iron and 2-3% more calcium and alumina than the
average 4EA.
The 4H, 4A, 4E and 4F all occur as discrete, “intraformational” horizons within the
basaltic pile in addition to the NIF. These horizons are most commonly <2m thick but
can swell to ten’s of metres within fold crests or keels. They are most common in the
first 20-30m above the NIF.
Overlying the NIF is a variable thickness of basalts ranging from <2m in the Esker fold
area to 30-50m in the T-Antiform area. There are little or no komatiitic basalts or
ultramafics above the NIF. In the past, the various basalts in the mine area were
designated as “BVol” (for “basic” or “basement” volcanics) or “2Vol” for the units near
the NIF. Given the uncertainty of defining a “basement” in the mine area, these terms
have been abandoned in recent years in favour of a generic “Unit 2” and its variants
for all basalts and andesites.
STRUCTURAL GEOLOGY Three deformation events have been recognized in the NCGB by previous workers
(Hall and Rigg, 1984-5; Breaks et al, 2001). While the time between each event is
uncertain and they may be part of a continuum, there is good field evidence for these
three discrete episodes of variably oriented strain.
20
The earliest event, D1, is typically manifested only by small, local, tight to isoclinal folds
in the iron formations (Breaks et al, 2001). D2 is by far the dominant deformation event
in the area and has produced a near-vertical, moderate to strong planar north-trending
foliation throughout the area with variably developed lineations, boudinage, and
mesoscopic folds (Breaks et al, 2001). Syn-D2 shearing is commonly developed
parallel to F2. D3 is a relatively, weak and localized event evidenced by minor warping
and crenulation cleavages.
The Musselwhite property is transected by two major shear zones evident on surface
and variable high-strain zones apparent in the underground workings and drill core.
The origin of these high strain zones is still the subject of some debate. While there is
evidence for late cross-cutting shear zones (e.g.: the “Conveyor Shear”), many of the
mineralized zones in the BIF may be local structures developed during the F2
flattening/folding event. Similarly, it is now thought that many high-strain areas in the
adjacent volcanics were transposed locally as an accommodation to the folding rather
than the product of a through-going shear zone. In contrast, the Dinnick Lake Shear
Zone overprints the eastern contact of the NCGB with the adjacent granitoid batholith
beginning ~10km north of the mine and has produced a well developed mylonite in the
batholith margin. The Akow Lake Shear Zone trends northwesterly along the central
core of the NCGB beginning about 8km north of the mine. Where observed by
Musselwhite personnel, this shear zone has affected primarily basaltic rocks and
produced well foliated to banded, commonly biotitized and carbonatized rocks that
weather into a “ribbed” pattern.
Within the mine area, the strata have been folded into a broad synform, the “East Bay
Synform”, the keel of which is host to two smaller antiforms, the T-Antiform and the W-
Fold. The T-Antiform and adjacent synformal keel (known as the “PQ Deeps”) host the
bulk of gold mineralization at Musselwhite. Mineralization is hosted by sub-vertical
shear zones within the favourable iron formation units, primarily the silicate facies
(4EA) and to a lesser extent, the oxide facies (4B). Discrete mineralized shear zones
up to 10m wide occur throughout the deposit across a width of ~225m (from the
21
“Moose Zone” through the T-Antiform and into the PQ Deeps). Locally these shears
coalesce into broad zones up to 40m wide (e.g. PQ Deeps C-Block). The mineralized
shear zones tend to be quite persistent along strike, following the upper margin of the
Northern Iron Formation and/or high strain zones within second order folds (e.g. the
Jets Zone) for 2-3km. While the shear zones are primarily ductile, on both
macroscopic and microscopic scales there is evidence of associated brittle
deformation that produced dilatant zones and allowed the infiltration of gold-bearing
fluids.
METAMORPHISM Sedimentary rocks in the mine area commonly contain garnet +/- staurolite and are
therefore deemed to be of amphibolite grade. Rocks on the north side of
Opapimiskan Lake have been mapped as part of the biotite zone by Breaks et al
(2001) with the garnet isograd trending northwest along the centre of the NCGB.
MINERALIZATION Gold mineralization at Musselwhite typically occurs in sub-vertical shear zones, within
either the Northern or Southern Iron Formation. The bulk of the ore bodies occur in the
silicate facies (4EA) of the NIF, however, the mineralized shears commonly extend
into the adjacent oxide facies (4B) and a number of ore zones are found largely in the
4B (e.g.: Jets Zone, Ranger, Thunderwolves, lower portion of the PQ Deeps A-Block).
Intraformational silicate iron formations may also be sheared and mineralized well
enough to be mined economically, but due to their small widths the volume of ore is
relatively minor. Locally the mineralized shears cut mafic volcanic rocks, however, to
date these occurrences are of limited extent and uneconomic.
Gold mineralization within the 4EA is generally accompanied by substantial quartz
veining or flooding, pyrrhotite formation, green amphibole alteration of the original
grunerite-rich host, a coarsening of the garnets, and local late-stage chlorite. The
formation of pyrrhotite is thought to be a consequence of sulphidation reactions
between the original gold-bearing bi-sulphide complexes and the iron-rich minerals of
the BIF; the gold content is crudely proportional to the sulphur content of the
22
mineralization in the ratio of 5 g/t Au for each 1% of sulphur. Gold occurs as free-
milling native gold, most commonly along with pyrrhotite filling fractures in garnets with
lesser amounts in the pyrrhotite, green amphibole, and rarely in quartz veins.
PAST WORK Recorded exploration in the Opapimiskan Lake area began in 1962 when brothers
Harold and Al Musselwhite of Kenpat Mines Ltd. discovered the Kenpat gold showing
on the north side of the lake and several showings in the iron formations on the south
side. Over the next 5 years they conducted mapping, trenching and diamond drilling
(12 holes totaling 773m). The Musselwhites re-staked the ground in 1973 and were
subsequently financed by a syndicate of Dome Exploration, Canadian Nickel Co.,
Esso Minerals Canada Ltd. and Lacana Mining Corp. From 1976-1983 a major drilling
program was undertaken in the West Anticline area followed by underground
development and exploration in 1984. This zone proved to be uneconomic and work
soon shifted to the East Bay Synform area where the T-Antiform Zone was discovered
by 1986. The syndicate was eventually reduced to two partners, Placer Dome (68%)
and Kinross (32%) who put the property into commercial production in 1997. After a
series of corporate takeovers, Placer Dome’s interest became the property of
Goldcorp Canada Ltd. In 2006 who subsequently bought out Kinross’ interest in 2007
and now hold 100%. A more detailed history of early exploration in the area is given
by Piroshco et al (1989).
Beginning in 2002, the Musselwhite exploration department began a series of small
drill programs targeting the Kenpat and smaller nearby veins/shear zones on the north
shore of Opapimiskan Lake. These programs met with little success until the 2006-7
deep drilling program intersected the down-plunge extension of the PQ Deeps ore
zone 1.4km below surface. These programs are summarized below.
2002: Drilled 10 holes totaling 2,917 targeting the Kenpat vein/shear at depth and
along strike. One minor high-grade intercept in a fractured quartz vein – 1.1m @ 59.8
23
g/t Au (drilled width, uncut) - and 6.9m @ 4 g/t Au in sheared basalt. No continuity of
mineralization in adjacent holes.
2003: Drilled 4 holes totaling 778m to test the Kenpat and nearby HG vein at depth.
Intersected scattered values in the 1-3.8 g/t au range but no appreciable widths of
mineralization.
2004: Drilled two holes totaling 597m to test a prominent IP chargeability anomaly
near the Kenpat vein/shear zone. Source determined to be disseminated (primary?)
magnetite in basalts.
2006-7: Drilled 10 holes totaling 8349m to test the projected location of the PQ Deeps
orebodies 1.7km north of the northernmost past drilling (the 2003-2005 barge-drilling
program). Mineralization was intersected along the eastern (PQ) limb of the East Bay
synform.
CURRENT PROGRAM The 2008-9 drill program described herein was a follow-up to the 2006-2007 initial fan
of North Shore deep drillholes which was successful in intercepting the PQ Deeps
mineralization more than 1.7km north of the current mine development. These holes
intersected the target Northern Iron Formation (NIF), including thick intervals of the
favourable “4EA” horizon which hosts most of the gold at Musselwhite, as well as thick
sections of Southern Iron Formation. Based on these holes, it was believed that the
main PQ Deeps synformal keel was situated west of, and at greater depth than, the
mineralized intercept. The assumed position of the keel was also vertically beneath a
number of vertical mineralized shear zones encountered in the mafic volcanic and
small Intraformational BIFs overlying the NIF. The second phase of drilling covered by
this report targeted the expected PQ Deeps keel position where it would be
intersected by the aforementioned mineralized shear zones. Once again the planned
program consisted of a deep “mother hole”, 2.4 km in length, and a series of daughter
holes wedged off this at various depths.
24
Drilling of the new fan of holes was conducted on Musselwhite’s behalf by Boart
Longyear in 2008 and 2009. Layne Christensen was contracted in 2009 to drill
another daughter hole from the initial mother hole, 06-NSD-001, targeting the PQ
Limb ~50-75m above the mineralized intercept returned from DDH 07-NSD-005 in the
initial fan of holes. The program was supervised by the authors. The drill core is stored
on racks at the Musselwhite exploration camp.
The current program began January 5th 2008 with initial preparation of a >16” thick
ice road across Opapimiskan Lake to the site. This was completed by January 10th
and the drilling resumed on 07-NSD-008. Three other holes were completed during
2008. The fourth hole was started in October and continued unit March 14th, 2009.
Layne began drilling of 09-NSD-001 on February 20th 2009. The hole was completed
on April17th.
Drilling began with the continuation of the initial pilot hole, DDH 07-NSD-008, which
targeted the expected base of the PQ Deeps synform keel. This pilot hole reached a
vertical depth of 2.0km. It intersected the NIF in the West Anticline position ( a shallow
dipping, gently folded area typically ~6-900m above the PQ Deeps), mafic volcanics,
the felsic volcanic wedge, lower mafic volcanics and thin intervals of the Southern Iron
Formation (SIF). This hole was positioned well to allow 2 wedges to intersect the
Northern Iron Formation (NIF) ~300m vertically above the hole. However the hole was
lost at a depth of 2202m when the rods broke at 1400 m. DDH 08-NSD-001 was then
wedged at a depth of 1349m from 07-NSD-008. This hole passed beneath the PQ
Deeps Synform and intersected several horizons of the Southern Iron Formation. It did
not intersect the NIF in the expected fold keel position. The 2nd daughter hole, 08-
NSD-002, targeted the PQ-Deeps synform ~175m above hole 08-NSD-001. It was
wedged from 08-NSD-001 at a depth of 1514m and drilled to a depth of 2420m. The
hole intersected minor intervals of banded iron formation which may belong to the
Northern Iron Formation (NIF) but no “4EA” or significant mineralization was
intersected. The 3rd wedge in 2008 (08-NSD-003) only drilled from 950m to 1352m
before equipment was lost in the hole. Several attempts to fish the equipment out of
25
the hole were unsuccessful and consequently a fourth daughter hole was drilled from
the first pilot hole 07-NSD-008.
Drilling of this fourth daughter hole, 08-NSD-004, continued into 2009 and as of March
14th the hole was stopped at a depth of 2397m. The precise trace of this hole is
somewhat uncertain and the reported trace trends much farther to the south than the
other holes (See Fig. 4). The downhole survey of all holes on this fan were undertaken
with a Maxibor I reflex tool which is not dependent on magnetic sensors and is ideal
for usage in areas that have magnetic interference. However, this instrument was
damaged and not available when 08-NSD-004 was drilled, consequently a different
downhole survey instrument was used. International Directional Services was
contracted to perform the downhole survey using a Gyroscopic system (North seeking
Gyro). The results of this hole indicate it deviated 300m to the south or 46 degrees on
Azimuth. This apparent deviation is not considered valid because there is no evidence
in the fabric and foliations measured on the core that would indicate drilling at such an
oblique angle to this section. The hole intersected mafic volcanics and small intervals
of iron formations, however, no 4B or 4EA was interested therefore it is unknown if
these intercepts represent NIF or SIF. The vertical height below the expected position
of the PQ Deeps synform keel (and the NIF) is ~ 50 metres.
In 2009 Layne Christensen drilled DDH 09-NSD-001 on the 2006-7 fan by wedging off
07-NSD-005 to follow up on the 4m @ 15g/t reported in 2006-7. The objective was to
extent the vertical height of this intersection. Diamond drill hole 09-NSD-001
intersected 2m @ 3.5g/t ~ 40m above the aforementioned high grade intercept.
Interpretation of the lithologies and fold structures encountered in all holes suggested
that this eastern fan of holes had intersected the east (PQ) limb of the East Bay
synform, perhaps 2-300m above the keel position as now modeled. Unfortunately the
second drill fan 300m to the west was unsuccessful in intersecting the synformal keel
of the PQ Deeps. Several holes passed through the NIF but at a depth of 1,000m (at
the West Anticline level) and these did not intercept any appreciable widths of
26
mineralization. A summary of drill hole names, depths and purpose is given in Table 2
below.
Table 2: Summary table of 2006-7 NSD drill holes.
RESULTS Drill logs for this program are presented in Appendix I along with a list of the
abbreviations used in logging. A drill section with the current interpretation is enclosed
as Fig. 10. Significant assay results are summarized in Table 3 below and all values
are presented in Appendices II and III. QAQC protocols and results are presented in
Appendix IV. Results are discussed below first in terms of the lithologies encountered
and overall structure followed by a discussion of the mineralization encountered.
LITHOLOGIES The 2008-09 North Shore drilling program has expanded the known extent of the
Northern and Southern Iron Formations in this area; the Northern Iron Formation was
intersected in the West Anticline position and Southern Iron Formation was
intersected beneath the expected position of the PQ Deeps fold keel. The general
HOLE ID STARTING DEPTH (m)
FINAL DEPTH (m)
TOTAL LENGTH
PURPOSE & RESULTS
07-NSD-008
1,751 2,202 451
Pilot hole for 2nd fan 300m west of first fan, intersected NIF in the West Anticline position & SIF. Lost hole before drilling under the PQ-Deeps keel
08-NSD-001
1,343 2,441 1,092 Pilot hole restarted, wedged from 07-NSD-008. SIF intersected ~300m below the keel
08-NSD-002
1,514 2,421 906 1st daughter hole wedged from 08-NSD-001, passed ~150m below the keel.SIF intersected east of the PQ synform
08-NSD-003
950 1,352 402 Unsuccessful attempt to intersect the NIF.
08-NSD-004
665 2,387 1,722 3rd daughter hole wedged from 07-NSD-008. SIF intersected and possible NIF ~50m below keel.
09-NSD-001
1,440 1,978 538 Drilled from first fan and wedged from 07-NSD-005, intersected PQ Limb 45m above mineralization in 07-NSD-005.
TOTAL (m) 5,117
27
stratigraphy of the iron formations here is remarkably similar to that in the mine area.
The NIF varies from a basal 4A (chert-grunerite) stratigraphically upwards through a
thick sequence of 4B (chert-magnetite oxide facies BIF) into a well developed 4EA
(garnet-grunerite-chert-magnetite silicate facies BIF), followed by a typical 4F (garnet-
biotite schist) and capped by a thin horizon of 4E (garnetiferous amphibolite BIF). The
two principal horizons of the Southern Iron Formation remain the same monotonous
sequence of thinly bedded to laminated chert-magnetite BIF as observed elsewhere
on the property. The 2006-7 drilling intersected numerous intraformational iron
formations (ITFs), primarily composed of 4F and 4E, throughout the mafic volcanics
overlying the NIF in sections up to ~50m thick. During the 2008-9 program, only 09-
NSD-001 was in the proper position to intersect these ITFs above the NIF and at least
seven of these were mineralized over narrow intervals.
Both pilot holes, 07-NSD-008 and 08-NSD-001, were collared in a predominantly
mafic volcanic sequence ~750m thick overlying felsic volcanics. This sequence
includes lesser felsic and ultramafic volcanics with minor intraformational BIF
horizons. Currently it is unclear if this sequence is part of the South Rim Volcanics or
if it is a continuation of the Opapimiskan volcanism. Beneath the aforementioned
mafic volcanics is a >80m thick sequence of felsic volcanics similar to those in the
mine area. These are relatively massive siliceous units with 10-15% fine-grained
feldspar phenocrysts/crystals. Although these rocks resemble flows there is no solid
evidence of flow textures and they are assumed to be ash-crystal tuffs (similar rocks in
the mine area grade into volcaniclastic sediments). Previous drillholes in the nearby
Kenpat area intersected thick sections of coarse pyroclastic breccias, tuffs and
derived volcaniclastic sediments. Where sheared, the formerly massive, light grey,
aphanitic felsic volcanics become variably sericitized, schistose and off-white in
colour.
Between the felsic volcanic sequence and the NIF below is a mafic volcanic sequence
that is considerably greater than that in the mine area, ranging from ~250-350m in the
first (eastern) fan of drillholes to ~85m in the pilot hole of the western fan. These
28
estimates are somewhat uncertain as the fold pattern has not been completely
unraveled as yet. The great majority of the mafic volcanic sequence appears to be
basaltic in composition with a few scattered ultramafic units, commonly in the vicinity
of the ITFs. The volcanic rocks beneath both the NIF and SIF are largely basaltic as
well with no major ultramafic units present; this is in marked contrast to the abundant
ultramafics below the NIF and SIF in the mine area.
STRUCTURE As none of the holes drilled during the 2008-9 program penetrated the PQ Deeps fold
keel, this program was of little use in furthering the interpretation of the complexly
folded 300m thick interval of NIF encountered in the first phase of the program in 2006
-2007. This interpretation remains a work in progress due to a lack of information in
critical areas of the fold. At this point it is interpreted as another second-order fold
complicated by internal folds and fault repetitions.
Alteration assemblages include locally high percentages of biotite, quartz
flooding/veining, pyrrhotite, plus lesser green amphibole. The only anomalous
mineralization from the western drill setup was intersected in the NIF in the West
Anticline position and beneath this level in the SIF; none of these intercepts were of
ore grade and width. A number of appreciably mineralized shear zones within mafic
volcanic and Intraformationals were intersected during the Phase One program above
the NIF, however, no mineralized shears were discovered in Phase Two below the
NIF in the keel position. This result may not be entirely unexpected or negative if the
mineralized shears are indeed related to the flattening/folding event. Similarly, the
percentage of “2T”, the moderately strained and highly biotitized basalt, is quite low in
these holes compared to the mine area but this would be expected if the rocks above
the tightly folded NIF were transposed more than those below the fold.
29
MINERALIZATION The most significant mineralized intercepts are given below in Table 3 and depicted
on Fig. 10. As noted previously, there were only weakly anomalous levels of gold
intersected below the PQ Deeps synform. The western drill fan intersected scattered,
narrow zones of gold mineralization within the NIF in the position of the West Anticline.
DDH 08-NSD-004 returned values up to 4.4 g/t Au but the average grade of the entire
“zone” was much lower.
Above the PQ Deeps synform, DDH 09-NSD-001 intersected mineralized zones in
seven “Intraformational” horizons including values up to 38 g/t Au, however, the
overall widths of these zone is generally <1.5m. This hole also intersected scattered
low grade mineralization in the 4EA of the PQ Limb ~40m above the high-grade
intercept of DDH 07-NSD-005.
Table 3: Anomalous intercepts from 2008- 2009 NSD drill program.
Western setup at 14,775N, 7230E; UTM Coordinates NAD 83: 673670E, 583495N
Hole No.
Down Hole Depth Intersection Widths Grades
Zone Hit From (m) To (m) Drilled
Width (m) True Width
(m) Au (g/t) uncut
08-NSD-002 1816 1816.7 0.7 0.5 2.7 4E
08-NSD-002 2145.2 2124.8 0.6 0.6 2.9 SIF
08-NSD-003 1100.5 1102.2 1.7 1.5 3.5 SIF
08-NSD-004 1088.8 1098 9.2 8 1.4 West Anticline Complete
NIF
Eastern setup at 14,775N, 7521E; UTM Coordinates NAD 83: 673878E, 5835159N
Hole No.
Down Hole Depth Intersection Widths Grades
Zone Hit From (m) To (m) Drilled
Width (m) True Width
(m) Au (g/t) uncut
09-NSD-001 1703.3 1704.5 1.2 1.2 21 Intraformational
09-NSD-001 1723.5 1724.8 1.3 1.3 7.7 Intraformational
09-NSD-001 1801 1802.2 1.2 1.1 7.4 4E “Cap” to NIF
09-NSD-001 1826.8 1831 4.2 4.2 2.6 NIF 4EA 40m above DDH 07-NSD-005
30
CONCLUSIONS
The North Shore drill program has shown that the target Northern Iron Formation
extends 2km farther north than past northernmost drilling beneath Opapimiskan Lake.
The NIF has retained its overall stratigraphy along the PQ limb, including intervals of
the important 4EA facies which hosts the bulk of gold mineralization at Musselwhite.
The second fan 300m to the west failed to intersect the target keel of the PQ-Deeps
synform. The overall shape of the East Bay synform appears to be largely intact and
at least one, if not two, tight secondary antiformal folds are developed in the lower
portion of the synform. It is not possible at this point to determine if either of these is
the continuation of the T-Antiform or if that structure exists at depth to the west of the
first fan of drill holes. The only intercept (4.2m @ 2.6 g/t Au) returned from the NIF in
DDH 09-NSD-001, although low grade, has extended the known vertical extent of the
mineralized zone encountered in 07-NSD-005 by 40m. This mineralized shear zone
occurs at the stratigraphic top of the NIF on the eastern limb of the East Bay Synform,
like a number of zones in the Musselwhite Mine. This intercept is open up-dip and
along strike and remains a very high priority target for further drilling.
RECOMMENDATIONS
Recommendations for further work are quite straightforward at this time:
1. Drill at least one more daughter hole to intersect the keel of the PQ-Deeps from
the western setup on 14,775N.
2. If significant mineralization is intersected in these holes, wedge off a series of
follow up holes as needed.
3. Once the current fan of holes and any follow-ups are complete, move the drill
back to the initial set-up. Wedge another hole off 06-NSD-001 at a depth of
900m in order to intersect the NIF approximately 50m below hole 07-NSD-005.
Continue follow-up drilling of this target as warranted south toward the mine
infrastructure.
31
4. The PQ Limb should also be drill off above hole 09-NSD-001 with a separate
fan of holes to test for mineralization at higher levels (e.g.: in the A2 (?) and
Esker-Jets positions).
Respectfully submitted,
John L. Biczok, P.Geo.,
Senior Exploration Geologist
Musselwhite Mine
Jim Edwards
Senior Exploration Geologist
Musselwhite Mine
32
STATEMENT OF EXPENDITURES
The total costs for diamond drilling and assays are tabulated below in Table 4. Details
concerns in the application of these costs are discussed below.
ASSAYS: All assays were undertaken by ALS Chemex with crushing and pulverizing
at their Thunder Bay facility followed by assaying in Vancouver. Costs quoted include
crushing, splitting, pulverizing, weight charges and gold fire assay with AA finish.
Some samples were also subjected to drying charges of about $1 per sample but
these costs have not been included in the average sample costs below.
December 2007 to December 2009: $15.65 per sample. 356 core samples.
To date 1453 core samples have been assayed during the program along with a
standard or blank sample after every 9th core sample. The number of assays per claim
was then derived from these “From” and “To” depths. Detailed analyses of the QA/QC
protocols used for this program are described in detail in Appendix 6.
DRILL METRES and Down hole Surveys per claim were calculated by measuring (in
VULCAN) the co-ordinates at the point where each drill hole crossed a claim boundary
and then determining the downhole depth at that point using the calculated XYZ co-
ordinates from the Maxibor downhole orientation surveys excluding 08-NSD-004. The
contract work conducted by International Directional Services with a north seeking
Gyro was used on 08-NSD-004 and there were discrepancy between each method
that cannot be explained. Both the Maxibor and Gyro surveys have been included on
the Claim map. The number of assays per claim was then derived from these “From”
and “To” depths.
33
Table 4: Summary of major costs incurred, 2006-7 NSD drill program.
Hole # Claim # Drill Metres
Total Metres Drill Costs Assays
Assay Costs Total
From To
07‐NSD‐008 529786 1751 2123 372 $129,156 111 $869 $130,024
1/2 Jan 8th ‐ Mar. 23th,08 502223 2123 2202 79 $22,230 48 $376 $22,606
Note: Costs are reported as half the original since the hole is older than 2 years.
08‐NSD‐001 529786 1343 2108 765 $151,913 175 $1,369 $153,282
1/2 Mar. 23‐ Jun. 30th, 08 502223 2108 2441 333 $120,537 108 $845 $121,382
Note: Costs are reported as half the original since the hole is older than 2 years.
08‐NSD‐002 529786 1514.5 1994 479.5 $290,415 131 $2,050 $292,465
July 1 ‐ Sept. 7, 08 502223 1994 2421 426.5 $286,870 94 $1,471 $288,341
Note: Invoice #5023479 indicates drilling started on July 1st,2008
08‐NSD‐003 529786 950 1352 402 $171,060 159 $2,488 $173,548
Sept 7th ‐ Sept 30, 08
08‐NSD‐004 529786 665 1763 1097.9 $478,641 179 $2,801 $481,442
Oct 4th, 2008 ‐ Mar 26th,09 502224 1762.9 2320 556.6 $262,775 144 $2,254 $265,029
502221 2319.5 2387 67.5 $59,070 16 $250 $59,320
Note: Cost difference between claims is a result of Wedging and Ice Building operations
09‐NSD‐001 529786 ‐ ‐ ‐
Jan 8th ‐ April 7th, 09 502223 1440 1747 307 $152,815 161 $2,520 $155,335
502222 1747 1966 219 $109,012 121 $1,894 $110,905
502219 1966 1978 12 $5,973 6 $94 $6,067
Total 5,117 $2,240,466 1453 $18,037 $2,259,747
34
STATEMENT OF QUALIFICATIONS
I, John Biczok, of the city of Winnipeg, Manitoba, do hereby swear and affirm that:
1. I am a Professional Geologist registered in good standing with the Association of Professional Geoscientists of Ontario (since 2007) and the Association of Professional Engineers and Geoscientists of Manitoba (since 2003).
2. I have an Honours B.Sc. degree in Geology from Lakehead University in
Thunder Bay, ON.
3. I have been employed as an exploration geologist on a full-time basis since 1979 throughout central and western Canada and much of India.
4. I am currently a Senior Exploration Geologist at the Musselwhite Mine and co-
supervised the work described in this report. Signed: __John L. Biczok_________________ Date: ____June 20, 2010______
35
LIST OF REFERENCES
Breaks, F.W., Osmani, I.A., and deKemp, E.A. 1987. Precambrian Geology of the Opapimiskan-Neawagank Lakes Area, Western Part (Opapimiskan Project), Kenora district (Patricia Portion); Ontario Geological Survey, Map P.3080, Geological Series-Preliminary Map, scale 1:31,680. Geology 1986. Breaks, F.W., Osmani, I.A., and deKemp, E.A. 2001. Geology of the North Caribou Lake area, northwestern Ontario; Ontario Geological Survey, Open File report 6023, 80p. deKemp, E.A.,1987. Stratigraphy, provenance and geochronology of Archean supracrustal rocks of western Eyapamikama lake area, northwestern Ontario. Unpublished M.Sc. thesis, Carleton University, Ottawa, Ontario, 98p. Hall, R.S., and Rigg, D.M., 1986. Geology of the West Anticline Zone, Musselwhite Prospect, Opapimiskan Lake, Ontario, Canada. In: Macdonald, A. J. Gold ’86: An International Symposium of the Geology of Gold Deposits, Proceedings. p. 124-136. Hollings, P., and Kerrich, R., 1999. Trace element systematics of ultramafic and mafic volcanic rocks from the 3 Ga North Caribou greenstone belt, northwestern Superior Province. Precambrian Research, v. 93, p. 257-279. Klipfel, P., 2002. Musselwhite U-Pb Zircon and Ar-Ar Dates, Synthesis and Interpretation. Internal Placer Dome Exploration research report. Otto, A., 2002. Ore forming processes in the BIF-hosted gold deposit Musselwhite Mine, Ontario, Canada. Unpublished M.Sc. thesis, Freiberg University of Mining and Technology. 86p. Percival, J.A., 2007. Geology and Metallogeny of the Superior Province, Canada, in Goodfellow, W.D., ed., Mineral Deposits of Canada: A Synthesis of Major Deposit-Types, District Metallogeny, the Evolution of Geological Provinces, and Exploration Methods. Geol. Assoc. of Canada, Mineral Deposits Div., Spec Pub. No. 5, p. 903-928. Piroshco, D.W., Breaks, F.W., and Osmani, I.A., 1989. The Geology of Gold Prospects in the North Caribou Greenstone Belt, District of Kenora, Northwestern Ontario. Ontario Geological Survey, Open file Report 5698. Stott, G., and Rayner, N., 2005. Discrimination of Archean domains in the “Sachigo Subprovince”, northwestern Ontario. Ontario Geological Survey, poster, Ontario Exploration and Geoscience Symposium, Toronto, Ontario, December 13-14.
36
Thurston, P.C., Osmani, I.A., Stone, D., 1991. Northwestern Superior Province Review and Terrane Analysis: Geology of Ontario. Ontario Geological Survey, pp. 81–144
APPENDIX ONE:
DIAMOND DRILL LOGS AND ABBREVIATIONS USED IN LOGGING
NB: See individual PDFs for each drill log.
SHORT FORMS USED IN MUSSELWHITE DRILL LOG TEXT
MINERALS & ROCK TYPES GRAIN SIZE amph amphibole f.g. fine-grained amph'd amphibolitized m.g. medium-grained Ank ankerite c.g. coarse-grained
Asp Arsenopyrite
bio biotite TEXTURES & FEATURES bio'd biotitized alt'd altered bio'n biotitization alt'n alteration Cc calcite brx'd brecciated Dol dolomite fol'n foliation Fd feldspar fol'd foliated gar or gnt garnet frags fragments grun or gru grunerite homog homogeneous grun'd gruneritized hetero heterogeneous Metaseds metasediments mod moderate Mt magnetite phenos phenocrysts Plag plagioclase SHZ Shear Zone Po Pyrrhotite Sil'n silicification
Py pyrite Sil'd silicified Qtz quartz Str strong Seds sediments Vn vein
Staur Staurolite wk weak
VG Visible Gold
MISCELLANEOUS assoc'd associated avg average tca to core axis dca degrees to core axis
SHORT FORMS FROM LOGGING TEMPLATES
Location / Heading
Short Form
Complete Wording
` Alteration BIO Biotite Alteration CAR Carbonate Alteration HEMA Hematite Alteration CHL Chlorite Alteration SER Sericite Alteration SILI Silicification Alteration GRU Grunerite Alteration GRT Garnet Alteration GRA Green Amphibole
Colour G Grey Colour B Brown Colour BK Black Colour W White Colour BE Beige Colour DG Dark Green Colour BG Blue-grey Colour LG Light Green Colour GG Grey-Green Colour Y Yellow Colour P Pink
Fault Type KF Knife fault, very sharp fault which juxtaposes
varying units Fault Type SC Ductile shear zone developing a S-C fabric
Fault Type MY Mylonite zone, characterised by fluxion
banding and possibly rotated porphyroclasts/blasts
Fault Type GG Unconsolidated fault gouge
Fault Type BC A zone of brecciation, characterised by
irregularly shape tectonic clasts Fault Type OS Open space fill in fault zone Fault Type SZ Shear Zone Fault Type PD Plastic Deformation
Fold Type FD unclassified folding Fold Type SF S-type folds Fold Type ZF Z-type folds Fold Type MF M-type folds Fold Type IF Isoclinal folding Fold Type PT Ptygmatic
Grain Size Aph Aphanitic Grain Size Fgr Fine grained, <0.5mm grain/crystal diameter Grain Size Mgr Medium grained, 0.5-1mm grain/crystal size Grain Size Cgr Coarse grained, >1mm grain/crystal size
Grain Size Lgr Used to distinguish extremely coarse
grain/crystal size, generally greater than 5mm
Intensity Str Strong Intensity Med Medium
Intensity Wk Weak
Lower Contact S Sharp
Lower Contact D Diffuse
Lower Contact I Irregular
Lower Contact G Gradational
Lower Contact F Faulted/Sheared
Major Unit 1 Unsubdivided
Major Unit 1A Massive flow
Major Unit 1B Spinifex-textured flow
Major Unit 1C Oliphant (polysuture)-textured flow
Major Unit 1D Talc-carbonate ? magnetite ? tremolite ?
serpentine schist of probable volcanic origin
Major Unit 1E Flow top breccia
Major Unit 1F Pillowed flow
Major Unit 1H Variolitic flow Major Unit 1M Ultramafic Amphibolite Major Unit 1S Serpentinized Ultramafic Major Unit 2 Unsubdivided Major Unit 2A Massive, fine- to medium-grained flow Major Unit 2B Amygdaloidal flow Major Unit 2D Pillowed flow, pillow breccia, hyaloclastite Major Unit 2E Flow breccia Major Unit 2G Pyroclastic breccia, tuff-breccia Major Unit 2H Tuff, lapilli-tuff Major Unit 2J Medium- to coarse-grained flow centres Major Unit 2K Dikes, sills, small intrusions
Major Unit 2M Chlorite-actinolite schist of probable volcanic
origin Major Unit 2N Variolitic flow Major Unit 2P Amphibolite
Major Unit 2Q Metavolcanics containing diopside-
plagioclase-epidote ? tourmaline? garnet pods and/or layers
Major Unit 2R Hornblende-plagioclase schist characterized
by mm to cm scale layering
Major Unit 2S Hornblende-porphyroblastic Major Unit 2T Biotite-bearing metavolcanics Major Unit 2U Garnet-bearing metavolcanics Major Unit 3 Unsubdivided Major Unit 3A Intermediate flow Major Unit 3B Intermediate pyroclastic breccia, tuff-breccia Major Unit 3C Intermediate tuff, lapilli-tuff Major Unit 3D Felsic flow Major Unit 3E Felsic pyroclastic breccia, tuff-breccia Major Unit 3F Felsic tuff, lapilli tuff Major Unit 3G Subvolcanic rocks, unsubdivided Major Unit 3H Subvolcanic quartz-plagioclase porphyry Major Unit 3J Subvolcanic quartz-porphyry Major Unit 3K Subvolcanic plagioclase porphyry Major Unit 3M Felsic volcaniclastic rocks Major Unit 3P Intermediate dikes, sills, small intrusions Major Unit 4A Chert-grunerite Major Unit 4B Chert-magnetite iron formation Major Unit 4C Carbonate 4b Major Unit 4CH Chert Major Unit 4CHP Chert with pyrite and pyrrhotite Major Unit 4D Carbonate magnetite Major Unit 4E Garnet-amphibole iron formation Major Unit 4EA Garnet-amphibole-grunerite iron formation Major Unit 4F Garnet-biotite schist Major Unit 4H Sulphide iron formation Major Unit 4I Graphitic iron formation Major Unit 4TB Banded iron formation tectonic breccia Major Unit 6 Unsubdivided Major Unit 6A Clast-supported conglomerate Major Unit 6B Matrix-supported conglomerate Major Unit 6C Oligomictic conglomerate Major Unit 6D Polymictic conglomerate Major Unit 6E Boulder (>256 mm) conglomerate Major Unit 6F Cobble (64 to 256 mm) conglomerate Major Unit 6G Pebble (4 to 64 mm) conglomerate Major Unit 6H Granule (2 to 4 mm) conglomerate Major Unit 6I Andalusite-bearing metasediments
Major Unit 6J Garnet-rich layers associated with
metapelites and/or banded iron formation Major Unit 6K Wacke Major Unit 6M Arenite Major Unit 6N Mudstone Major Unit 6P Feldspathic wacke Major Unit 6R Feldspathic arenite Major Unit 6T Quartz arenite
Major Unit 6U Amphibole-bearing
mudstone/sandstone/conglomerate Major Unit 6V Biotite-bearing mudstone/sandstone
Major Unit 6W Garnet-bearing mudstone/sandstone
Major Unit 6X Chlorite-bearing mudstone/sandstone
conglomerate
Major Unit 6Y Amphibole ? biotite-bearing foliated rock of
probable sedimentary origin
Major Unit 6Z Ultramafic rock interbedded with
metasediments Major Unit 7A Gabbro (Cl = 35-90) Major Unit 7B Leucogabbro (Cl = 10-35) Major Unit 7C Plagioclase-phyric gabbro
Major Unit 7D Mafic dikes, sills, small intrusions not related
to mafic volcanic rocks Major Unit 7F Peridotite
Major Unit 7H Ultramafic rocks and altered equivalents of
probable intrusive origin Major Unit 7J Amphibolite Major Unit 7K Anorthositic gabbro Major Unit 7L Gabbroic anorthosite and anorthosite Major Unit 8 Unsubdivided Granitoid Intrusions Major Unit 8A Diorite Major Unit 8B Quartz diorite Major Unit 8C Trondhjemite Major Unit 8D Tonalite Major Unit 8E Granodiorite Major Unit 8F Granitic pegmatite Major Unit 8H Biotite trondhjemite Major Unit 8J Granite Major Unit 8K Quartz monzonite Major Unit 8M Gneissic granite
Major Unit 8N Xenolithic felsic intrusive rocks (xenolith
composition indicated in parenthesis) Major Unit 8P Mylonitized granitoid rocks
Major Unit 8Q Biotite-muscovite ? fluorite
trondhjemite/syenite Major Unit 8R Biotite-tonalite gneiss Major Unit 8S Hornblende-biotite tonalite gneiss Major Unit 8U Garnet-muscovite ? tourmaline granite Major Unit 13 Lamprophyre Dyke Major Unit No Log Not logged, upper part of wedge hole Major Unit QTZ VN Quartz Vein Major Unit SHZ Shear Zone
Mineralogy AS Arsenopyrite Mineralogy CP Chalcopyrite Mineralogy MT Magnetite Mineralogy PO Pyrrhotite Mineralogy PY Pyrite Mineralogy VG Visible Gold
Texture Tex Texture Texture LA Laminated Texture DI Distorted Texture MA Massive Texture AM Amygdaloidal Texture RG Ragged Texture MO Mottled Texture SCH Schistose Texture FOL Well Foliated Texture PORBL Porphyroblastic Texture POR Porphyritic Texture BA Banded
Vein
Assemblage CA Carbonate (Usually calcite, local dolomite)
Vein Assemblage
QZ Quartz
Vein Assemblage
QZ-CA Quartz-Carbonate
Vein Texture f fibrous
Vein Texture sy syntaxial, vein fibres are growing from the
margins of the vein inward
Vein Texture ay antitaxial, vein fibres are growing from the
centre of the vein toward the margins
Vein Texture m massive, no easily recognised internal
structure
Vein Texture l laminated, clear banding within the vein.
Either a function of shearing or alternating composition fill
Vein Texture c crustiform, "epithermal-like" veins
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT Majo1 Cont As Cp Mt p I I
Alpha! AJi;:n•I Int Typ Alph From To o/~ Py% VG Comments From To Vein :Vein iTe> Contact Comments From To Corrrnenls From To a Int Type Comments From To ::re~ Int Type Comments Unit % % % Speck, Type, % I Type deg , eg: : e dea
0.00 4.10 CASI 4.10 17.80 CA 5 I 40 distorted 4.10 29.90 2 Cc veins
9.00 10.00 40 MO S1
1.0 Po associaled
with
m.g.chlorile vein
29.90 37.60 2 55 23.10 29.90 CA 3 I distorted 18.00 19.00 40 MO S1 43.70 45.20 50 MOO BC angle probably not 37.60 50.00 2 55 Cc veins, 26.00 27.00 30 MO S1 reliable.
brecciatic 36.00 37.00 45 MO S1
texture 45.20 46.00 55 MO S1
locally
43.70 45.20 CA 8 I breccia,
no angle
10. po in veins 48.00 48.50 40 MO S1 along foliation
plans in mafic
volcanic
8.0 Po in veins in
ma!ic volcanic,
borderline UM 50.00 51.80 1
51.80 59.60 2
8.0 Po veins in 57.90 58.30 40 MO S1 mafic volcanic
25 10. Po in veins
along foliation
plans. Mafic
bordeline UM
3.0 mafic
borderline um
59.60 62.00 1 50
i i i I I
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT I 1i~~I Cont As Cp Mt~ 0 VG Vein Veintre> Contacti~ments AJ~;a Int~ Comments I From
Alph ; Alh I From To % Y Yolspeck, Comments From To From To To a Int Comments From To la eg nt Type Comments % jo/o Type % Type :
deg
62.00 77.30 2 90 1 Py associated 231.60 242.00 OZ-C 15 I vertical 65.00 66.00 40 MO 81 177.70 181.80 WEK BC slightly brecciatted 77.30 78.30 1 90 with Cc veins. hole, no 70.00 71.00 30 MO 81 78.30 100.00 2 10 0.5 minor Pyrtte in alpha 77.30 78.30 40 WE 81
100.00 107.30 2 40 mafic volcanic 274.80 275.60 oz 100 I 30 massive 84.00 85.00 45 MO 81 107.30 131. 10 2 30 0.1 minor Pyrite in qtz vein 92.00 93.00 40 MO S1 131.10 156.20 2 40 maflc volcanic. lnmafic 102.00 103.00 40 MO S1 156.20 168.60 2 0.1 traces Po in 299.00 305.00 CA 25 I 0 105.00 106.00 40 MO 81 168.60 177.70 2 slightly 305.00 329.00 QZ-C 30 I 0 Varles 119.00 120.00 40 MO S1 177.70 181.80 2 brecciatic zone from low 123.00 124.00 30 MO S1 181.80 204.00 2 0.3 pyrite angle to 128.00 129.00 40 MO S1 204.00 206.60 2T associated zero 136.00 137.00 40 MO 81 206.60 226.40 2 with Cc veins 142.00 143.00 50 MO S1 226.40 231.60 2 0.1 pyrtte 147.00 148.00 50 MO S1 231.60 242.00 2 associated 151.00 152.00 40 MO 81 242.00 248.00 2K with Cc veins 157.80 157.80 40 MO 81 248.00 256.70 2 0.1 Pyrite 162.20 162.20 40 WE 81 256.70 268.00 2 assocatted wtth 168.30 168.30 45 MO S1 268.00 269.00 3A strong Cc 169.80 169.80 35 WE S1 269.00 282.80 2T veining 175.00 175.00 50 WE 81 282.80 283.30 28 185.20 185.20 50 WE S1 283.30 290.80 2 194.30 194.30 55 WE 81 290.80 291.40 13 202.60 202.60 45 WE 81 291.40 305.00 2
305.00 329.00 2
329.00 333.00 2
333.00 337.70 2T
337.70 341.00 2
341.00 343.30 6
343.30 345.70 4F 90
345.70 349.90 6
349.90 361.80 2T
I I I I i I i . i I I
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT
1ia~r Cont As C?,f; Mt~ VG • Vein Vein Te Contact Alpha! I T~pl
Alph From To Comments From To Comments From To A:f.ha Int Comments From To a Int lfyp, Comments From To A:t Int Type Comments % % 0 speck~ : Type % Type deg eg deg a eg
361.80 365.90 2 50 1.0 disseminated 386.30 386.70 QZ 100 I Qlz vein 576.00 577.00 60 WE S1 hole 355.50 357.70 INT GG Fault, broken up 365.90 367.40 2 50 cpy with 40% started rocks, RQD<10, 367.40 406.30 2 55 5.0 of the host flatening. with calctte and 406.30 409.00 1 65 6.0 rock Start of chlorile filling locally 409.00 413.20 1 25 3.0 651.00 655.80 CA 10 I 50 foliation 652.20 652.60 45 INT sz 413.20 440.00 1 57 0.3 664.50 681.30 CA 15 I 30 again. 677.00 678.00 20 MOD sz 440.00 497.50 1 45 0.5 689.00 714.00 QZ-C 15 I various Assume 680.40 681.30 21 MOD sz 497.50 510.90 7A 33 alphas tht beta=90 684.00 684.60 30 INT sz 510.90 522.00 1 45 730.20 740.10 QZ·C 30 D irregular 583.00 584.00 60 WE $1 694.00 696.70 10 WEK 8Z 522.00 568.00 1 20 veins, no 587.00 588.00 50 MO $1 705.80 706.50 15 MOD sz 568.00 570.80 2K 22 alpha 596.00 597.00 50 MO S1 730.20 733.50 15 MOD sz 570.80 597.00 2 27 749.80 752.30 CA 25 D 18 603.90 604.90 50 MO S1 749.80 752.30 15 MOD sz 597.00 599.30 2 35 784.80 808.10 CA 7 I 20 610.00 611.00 60 MO 81 766.40 768.50 30 INT sz 599.30 613.50 6 10 617.00 618.00 50 MO S1 613.50 651.10 2 18 626.00 627.00 50 MO S1 651.10 655.80 2T 50 632.00 633.00 30 MO S1 655.80 658.00 2 641.00 642.00 50 MO S1 658.00 696.70 2T 645.00 648.00 45 WE $1 696.70 708.70 2 652.00 652.60 40 INT S1 708.70 710.50 2T 660.00 663.00 10 WE S2 710.50 710.70 3K 665.00 666.00 20 MO S1 710.70 712.50 2T 674.00 675.00 25 MO 81 712.50 730.20 2K 677.00 678.00 20 MO $1 730.20 760.90 2T 687.00 689.00 35 WE S1 760.90 761.10 3G 695.00 700.00 16 MO S1 761.10 768.50 2T 705.80 706.50 17 INT S1 768.50 791.50 2 717.00 725.00 17 MO S1 791.50 796.50 2T 726.00 729.00 20 MO S1 796.50 803.80 2 730.20 733.70 15 INT S1 803.80 808.10 2K 745.00 746.00 15 MO 81 808.10 825.00 3F 749.00 751.00 12 MO S1
752.50 758.00 12 MO S1
760.50 766.00 24 MO S1
766.00 771.40 30 MO S1
772.30 777.00 27 MO S1
782.60 787.00 25 WE S1
791.00 795.00 20 MO 81
795.00 796.50 35 MO S1
796.50 800.00 20 MO S1
804,00 806.00 34 MO S1 ! 811.00 818.00 25 jMO 82
!
I
821.00 823.00 32 WE S2
i
823.00 825.00 QZ-C 80 •mi D
i
50
I i i i i I . I i I
I MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT Majo1 Cont As ~! MtiPo VG Vein Vein rreJCont!C' Alpha' A!fe~a Typ Alt:h From To Py% Comments From To Comments From To Int Comments From To ype Comments From To Int Type Comments i Unit % % % Speck, Type % i Type deg , e ~ •!
825.00 825.70 6V 90 838.00 846.00 CA 15 I Veins are 827.00 828.00 57 WE S1 825.70 837.50 3F 90 irreg and 838.00 839.00 47 WE $1 Very weak 837.50 862.90 3F wide foliation
range of at best
angles. and
generally
erratic
and
deformed,
often
massive, 846.00 846.80 CA 95 846.80 847.70 QZ 80 I Minor
Toumaline
x'ls up to
Smm along vein
edges.
i
i I I •
I i I i I I •
I
MAJOR UNIT I MINERALS QTZVEINING FABRIC FOLD FAULT Majo; Cont As Cp ~tl~y% VG Comments From To I Vein Vein ~eJc~e!!etl Alpha Comm-Onts From To A!ftt Int Typ From To
Alph Int ITyp, Cemments From To ~~~i Int Type Comments From To Comments a Unit• % % l5peck1 Type ! % • Type deg e deg
I 847.70 848.50 CA 75 862.90 896.00 3D 848.50 852.50 CA 20 I 856.00 857.00 47 MO S1 Shear 851.00 852.00 27 WEK sz Mod bio'n and 896.00 995.20 3F 854.50 856.00 CA 65 foliation, -20% Cc veins.
856.00 862.00 CA 7 possible 654.50 862.50 50 MOD sz Local S-C 862.00 894.00 CA 5 So at 145 farbrlc. S @ 64
deg to lop dca, C@ 35 dca. of CA.
860,00 861.00 50 MO S1 Shear
foliation,
localS-C
fabric
with Sal
64 dca
and Cat
35 dca 920,00 921.00 50 WE S1 Foliation
in this
unit is
very faint
and
erratic at
best, often
just a
local
weakshea
943.00 945.00 45 WE S1
962.00 963.00 52 WE S1 Weak
shear torn
972.00 974.00 18 WE S1 Weak
shearforn
994.00 995.00 52 WE S1 weak shea
995.20 1002.40 6 0.6
0.4
1002.00 1003.00 67 MO S1 Weak
I
shearfol'n. 11002.40 1008.00 • 4E
I I I I .
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT
From To Majo( Cont As ~ Mt Po Py%lsp~~k~ Comments From I To Vein Veln~Alphal Comments From To Alpha Int Typ Comments From To !Alp:EE Comments From To A:J:h Int Type Comments Unit i % % % Type % deg I deg I a
e deg a eg, 1003.20 1004.70 QZ-C 20
0.1
1005.50 1008,00 QZ 7 1006.00 1007.00 72 so
1008.00 1016.40 4F
1012.00 1013,00 78 so
1014.00 1015.00 60 S1 Folaition
is weak
and
erratic
throughout
these seds
1016.40 1021.00 4E 45
4.0
20. 1019.00 1020.00 10 S1 8.0
1021.00 1022.50 4EA 0.2
1.0 1022.50 1024.00 4F
1024.00 1026.20 6 1025.00 1026.00 10 S1
1026.20 1027.20 4E 0.1 1027.20 1030.70 4F
1030.70 1041.00 1 43 1041.00 1042.50 1 1042.50 1046.70 4F
i I I I I i I I I I I i I i
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT
From I Majo1 Cont As Cp Mt Po p o/c-1 v\J I Vein Veinfre~ Contact Alpha A:f.ha1 Int Typj 1Arh ~Int
! To Comments From To Comments From To Comments From To Int ~yp1 Comments From Type Comments Unit % % % % Y 0 iSpeck , ! Type %: Type deg eg ! e I !deg 1046.70 1051.30 1M 46
1051.30 1064.70 4F 32
1052.00 1053.00 29 WE 81
1053.00 1054.00 44 WE 81
1054.00 ~060.00 40 MO SF Broad
folds, AP
hard to
measure,
-approx.
All appear
to be S
type
except for
oneZ 0.1
1057.00 1058.00 68 so
0.5
1061.00 1062.00 25 WE 82 x-cuttlng
forn and
cleavage.
1063.00 ~064.00 35 FD
1064.70 1071.00 48 1065.00 1066.50 33 so Core is
not
oriented
In this
NIF
section,
82 i
cleavage
assumed
to be near
vertical
and used
to orient
I I
I core.
I i I I i I i • • •
I I i I
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT Majo1 Cont As cp! Mt Po
Py%5p~~k1 Vein lveln Contact, Alpha I l••-k- Typ I Al phi I
A~h From To Unit o/o %1% % Comments From To Type· % Te) Type I deg Comments From To deg Int Comments From !
To a .Int Typ~ Comments From To a eg Int Type Comments e deg 1066.50 1067.00 34 WE S2
2.0 1066.70 1067.30 QZ 30 I 1067.00 1068.00 34 so 1067.30 1072.00 QZ 2
1068.00 1069.00 43 so 1069.00 1070.00 28 S2 Fairly
consistent
thin
cleavage
frax
throughout
the BIF at
high angle
to
bedding/for
n, used to
orient core.
1071.00 1075.00 4EA 0.1 1071.00 1072.00 78 S1
1074.00 1075.00 18 FD 1075.00 1079.95 46
1.0 VG in small 1076.00 1077.00 QZ 2 1077.00 1078.00 77 so patch of 1077.00 1077.80 QZ 30
garnets <1cm
flanking a 3cm
qtz vein
1078.00 1080.00 82 so 1078.80 1079.95 oz 7
1079.95 1083.30 1
1083.00 1083.50 65 so 1083.30 1095.80 48 3.0 1083.30 1084.00 QZ 15 D 1083.50 1084.00 45 MO S2 Shear
fol'n,
-5ocm
wide zone 1084.00 1084.50 QZ 3
5.0 1084.50 1085.20 QZ 40 1085.00 1086.00 65 so 42
i I i I I I I I I I i i I I I I
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT ~Cont As Cp
~y% VG
To Vein Vein
rre> Contact Alpha
From To AJ/eha Int Typ From To
:Afph / 1nt~yp~ Comments From To A:J:h Int Type Comments I
From To Comments From Comments Comments d:g % % Speck~ Type % Type deg eg e a eE 1085.80 1086.90 QZ-C 5 1086.00 1087.00 43 MO S2 Frax
cleavage,
thin,
some
with Po,
QtzorCc.
some
offset
bedding
slightly. 1.0 1086.90 1087.90 QZ 8
1087.90 1093.00 QZ 2 1088.00 1089.00 33 so 1089.00 1090.50 82 so 1090.50 1091.00 47 S2
1093.00 1094.00 80 so 1094.00 1095.00 23 S2
1094.50 1095.25 QZ-C 20 1095.25 1095.80 QZ 15
1095.80 1096.95 4A 4.0 1095.80 1096.95 OZ 25 D 75.
1096.95 1097.95 4B 1096.95 1100.40 QZ 5 1097.00 1098.00 83 so 1097.95 1099.40 4A 3.0 1098.00 1099.00 75 so
1099.40 1100.40 4H 15. 1100.40 1108.50 1 42 5.0 All in one velin 1100.50 1101.00 79 so
II to CA along
edge of core.
1108.50 1128.00 2 1112.00 1113.00 40 WE S1 1128.00 1146.70 2T 1119.00 1120.00 32 WE S1
1121.00 1122.00 25 WE S1 1131.00 1137.00 52 WE S1
1146.70 1164.30 1 40 1160.00 1161.80 CA 35 s Brittle 1139.00 1140.00 39 WE S1 veins up 1143.00 1144.00 60 WE S1 to 3cm. 1146.00 1147.00 69 WE S1
! 1152.00 1153.00 49 WE S1 : 1155.00 1156.00 55 WE S1
1164.30 1168.00 4B i 1164.50 1165.00 85 so
I I i I I
• I .
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT Majo1 Cont As IC?p! Mt Po
Py%1sp~~k~ Com~ Vein lveln Contact Alpha iAlpha Typ Alplll l ,J
A!f:h From To From To ifex Comments From To Int Comments From To a : Int Typ , Comments From To Int Type Comments Unit % % % % Type % Typo deg : deg e dog · : " ., 1165.00 1165.50 QZ 12 1165.10 1165.20 50 MO S2 Thin
cleavage
planes.
1165.50 1166.00 85 so 1166.00 1167.00 23 MO S2 Some are
filled
wtth
qtz-po up
to-6mm
wide. 0.1 1.0 1166.50 1167.40 QZ 5 Narrow
frax
filling
veins
<6mm
with
assoc'd Po
0.6 1167.40 1168.00 85 so 1168.00 1186.60 7A 1168.00 1169.00 80 WEK sz
1171.00 1172.00 81 WE S1 Weak 1181.00 1182.00 60 WEK sz shearfol'n.
1181.00 1182.00 60 WE S1 Weak
shearfol'n.
1186.60 1196.10 48 63 0.7 2.0 Cp conc'd in a 1186.60 1187.60 QZ 12
2-3cm wide,
slightly
strained band,
no Po orQtz
wtthtt.
1.0 1189.00 1189.40 QZ 15
1190.00 1191.00 85 so 1191.00 1194.00 74 so
0.2 1191.40 1192.20 QZ 3
1194.00 1195.00 QZ 6
1195.00 1196.00 78 so :
1196.10 ,1202.70 1 73 1196.10 1196.50 48 MO S1 Shear
foliation. 1202.70 1214.00 7A
I
1214.00 1215.00 CA 15 ! I 1200.00 1201.00 60 MO S1 Shearfol'n.
I
1214.00 1216.40 1
i I i
11214.00 • 1215.00 53 , MO S1
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MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT
From I Majo1 Cont As !cp Mt Po VG Vein Vein Contact! Alpha . I Alpha Typj !
IAlph ::re~! Int To Py% Comments From To ire) Comments From To Int Comments From To . a Int ifypE Comments From To Type Comments Unit % 1% % % ~pecki Type % Type deg ' deg e i :deg
1216.40 1225.00 48
1217.00 1218.00 74 so
1220.00 1221.00 oz 5 1.5 1221.00 1222.00 oz 2 1221.00 1221.30 30 MO FD
1222.00 1223.00 82 so 1223.00 1224.00 oz 10
6.0 1224.00 1224.50 oz 50 7.0 1224.50 1225.00 oz 50
1225.00 1292.30 2D
1292.30 1292.80 2 50 0.05 1226.00 1227.00 51 WE S1 1316.60 1320.00 45 WEK sz Strong! calcite 1292.80 1304.80 2J 65 1233.00 1234.00 72 WE S1 stringers and 1304.60 1337.50 20 50 1245.00 1246.00 24 MO S1 Weak chlorlte maybe 1337.50 1348.10 2 65 shear zone close to open 1348.10 1350.20 1 1259.00 1260.00 50 WE 81 spaced fault. 1350.20 1359.60 2 1269.00 1270.00 50 WE S1
1278.00 1279.00 33 WE S1 Poss a
weak
shear
forn but
most
selvages
are now
at-this
angle too.
1283.00 1284.00 26 WE S1 1292.80 1304.80 30 WE S1 1304.80 1316.60 40 WE S1 1321.50 1329.00 30 WE S1 1329.00 1335.00 55 WE 81 1335.00 1347.00 35 WE S1 1347.00 1348.10 30 WE 81 1348.10 1359.60 35 MO S1
1359.60 1361.00 88 40 1359.60 1361.00 QZ 100 s 40 massive 1359.60 1361.10 35 WE S1 1359.60 1361.00 INT BC qtz vein with qtz vein locally brecciated
zones 0.5 Minor Po in
massive Qtz vei1
1361.00 371.20 2 40
I 1361.10 1374.00 45
MO! S1 I i I I . I
• I i
MAJOR UNIT •
MINERALS QTZVEINING FABRIC FOLD FAULT Majo1 Cont As!cp Mt.Po~ Vein Vein Contact Alpha Alphaj Int Typl From I
Alph tryp~ Comments A~h IType
From To Comments From To rre, Comments From To Comments To a Int From To Int Comments i Unit % % % % . . Type % Type deg deg, , e , deg " eg
1371.20 1394.00 2 50 1374.00 1383.00 65 MO S1 1396.30 1396.80 50 WEK sz 1394.00 1398.80 2 55 1383.00 1398.80 50 WE S1 1398.80 1403.50 1 60 1398.80 1403.50 60 WE S1 1403.50 1418.70 2 1403.50 1409.80 35 MO S1
0.5 3.0 2 1409,80 1411.40 25 INT sz
1411.40 1424.90 40 WE S1
1418.70 1422.90 2 45 1424.90 1462.00 55 WE S1 1426.50 tt426.70 35 WE FD 1416.70 1418.40 35 WEK sz 1422.90 1424.20 2 60 1424.20 1428.70 50 WEK sz 1424.20 1467.70 2 50
1428.70 1431.90 40 WEK sz
2 1433.50 1433.70 QZ-C 80 f D 50
1440.00 1462.00 CA 95 m D 60 1443.20 1445.30 65 MOD sz
3.0 2 1453.40 1454.10 35 WEK sz
1467.70 1472.50 7A 35 0.2 0.3 0.5 1521.00 1523.00 QZ 10 may not 1462.00 1467.80 30 WE S1 1515.00 1515.40 45 MOD OS 1472.50 1485.60 2 35 be qtz, 1467.80 1472.90 35 WE S1 1485.60 1488.30 7A 40 appears 1472.90 1485.00 40 MO S1 1488.30 1511.30 2 45 like barlte. 1488.30 1494.00 40 MO S1 1511.30 1512.80 8A 30 1494.00 1510.00 55 WE S1 1512.80 1521.70 7F 30 1515.00 1522.80 40 WE S1 1521.70 1523.10 1 50
1523.10 1527.80 1 50 2% tantalum in !
1527.80 1530.60 1 22 pegmatlte
! 1530.60 1533. 10 8F 40 0.5 1.0 0.3
I I
.1533.10 1535.80 1
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•
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MAJOR UNIT • MINERALS QTZVEINING FABRIC FOLD FAULT
I Majo1 Cont Mt 1 Po
i Contact' Alpha IA:te~· Typ
1Alph From To As ~ Py% VG Comments From To Vein Vein !Te) Comments From To Int Comments From To a Int ~YPE Comments From To Int Type Comments I Unit % % % Speck, Type % Type deg e deg
1535.80 1537.30 1 34 1.0 0.3 0.2 1536.00 1537.00 24 INT S1 1537.30 1538.80 8F 15 1538.80 1539.00 33 INT S1 1538.80 1543.20 1 25
1543.20 1549.80 1 0.2
1547.00 1550.00 0 WE so 1549.80 1552.40 2 32 2.0 very fine 1550.00 1551.00 32 MO S1 1552.40 1600.70 1 45 grained 1559.00 1560.00 55 INT S1
sulphides 1562.00 1563.00 30 MO S1 throughout,
mostly Po,
ranging 0.5-5%
1572.00 1574.00 65 MO S1
1600.70 1605.10 1 55 1583.60 1584.00 45 WE so 1599.30 1600.70 55 WEK sz 1605.10 1617.50 2 90 1584.00 1599.00 45 WE S1 1620.00 1620.70 90 MOD OS 1617.50 1620.00 2 60 1624.50 1628.00 60 MO S1 1620.00 1643.00 2 65 1628.00 1630.80 50 WE S1
1634.00 1637.00 70 MO S1
1.0 Semi massive 1637.00 1638.00 55 MO S1 Po In vns 1 cm
wide local and
diss. blebs 0.5
to2%
1639.70 1643.00 45 WEK sz
1643.00 1657.40 2 1643.00 1644.80 45 MO S1 1657.40 1662.10 1 45 1649.00 1657.40 50 MO S1 1661.00 ~661.40 70 MO FD faint fold 1662.10 1682.00 2 65 1662.50 1665.90 55 MO S1 near
lower
contract
of mafic
I I and
I ultramafic
l'T' i'1 ,., I 1665.90 i 1669.00 55 MO S1
.
•
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MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT iMajo1 Cont As Cpl Mt Po
Py%1sp~~kJ Vein Vein Contact Alpha At~a In~
Alp hi A1f:h From To Unit % %:%,% Comments From To Type % tre> Type deg Comments From To Comments From To d:a Int ITYP• Comments From To a eg Int Type Comments
1669.00 1682.00 40 MO $1
1670.80 1682.00 CA 95 ay s 1682.00 1689.90 1 55 1682.00 1689.90 40 WE S1
1689.90 1697.60 2T 65 0.5 1.0 1 1689.90 1692.80 65 MOD sz
1693.80 1697.60 65 MO S1
1697.60 1727.00 2 45 0.3 0.5 Diss Suphlde 1697.60 1709.00 55 MO $1 1727.00 1729.40 2 28 2.0 Desseminated 1709.00 1718.00 40 MO S1 1729.40 1746.00 1 Po 1718.00 1721.00 40 MO $1
1721.00 1727.00 55 MO S1
1729.00 1729.40 33 MO S1
10. Dessem,m.g
1.0 1735.50 1736.00 37 MO S1
13.
3,0 f.g dessem
1741.30 1741.70 33 MO S1
15.
0.2
1746.00 1747.10 2 55 15. sheared, 1746.00 1747.00 45 INT S1 desseminated
inmafic 1747.10 1757.80 1 60 0.5 f.g
dessemlnated.
i 1757.80 1764.30 2 70 1757.80 1758.70
1QZ-C 65 s 70
11.0 weak shear
I I I I
I desseminated fine-med grainec
1 i I I I I I
MAJOR UNIT
Coot ~'it MINERALS QTZVEINING FABRIC FOLD FAULT
From~ Majo1 Mt Po • I VG J Comments From To Vein Vein~Alpha Comments From To iAr~a Int Typ Comments From To
Alph Int ITYP• Comments From T Int Type Comments Unit % % PyYospeck~ Type % deg a e deg
1760.00 1764.30 45 MO S1 1764.30 1768.40 2A 50 0.3 0.5 Trace sulphide 1768.40 1782.90 QZ-C 65 m D 55 1764.30 1768.40 50 MO S1 1768.40 1782.90 20 60 associated with 1768.40 1776.00 40 MO S1
pillow selvages. 1776.00 1782.90 45 MO S1
1782.90 1797.00 2A 55 0.01 1782.90 1783.80 55 MOD sz 1783.90 1792.00 55 MO S1
1797.00 1816.50 2 3.0 1794.40 1804.50 40 INT sz 1801.50 1804.50 CA sy
1803.00 1811.00 60 MO S1
3.0
1811.00 1816.50 CA 85
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• •
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I
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT Majo1 Cont As ~,. Mt Po~ From !
Vein Vein ~ 9Jcontact Alpha Alpha! Int ,Typ i Alph ~:re~ From To Comments To Comments From To Comments From To a Int ITYP' Comments From To Int Type Comments Unit % % % k, Type % : : Type deg , deg ! e deg 1816.50 1820.90 2 65 1816.50 1820.90 45 MO $1 1820.90 1831.50 2D 60 1 1845.50 1846.10 QZ·C 25 s 68 1820.90 1824.00 50 MO S1 1845.50 1846.10 68 MOD sz 1831.50 1842.00 2 55 0.1 veryf.g 1858.50 1876.00 CA 5 m s 43 1824.00 1831.50 45 WE St 1925.40 1928.00 58 WEK sz 1842.00 1886.10 2 30 sulphide 1878.00 1911.70 CA 7 D 50 1833.00 1842.00 50 MO S1 1886.10 1887.10 2 30 throughout 1921.20 1922.40 QZ-C 85 m s 50 1842.00 1843.50 35 WE S1 1887.10 1911.70 2 52 much of the unit 1924.00 1928.00 QZ-C 25 D 60 1851.00 1852.00 50 MO S1 1911.70 1917.20 2 55 0.7 F.g Po 1856.00 1857.00 45 MO $1 1917.20 1921.20 2 50 throughout 1862.50 1863.50 46 MO $1 1921.20 1922.40 OTZ 65 untt, some 1867.00 1868.00 44 INT S1 1922.40 1934.00 2 42 grains up lo 1876.00 1878.00 40 MO $1 1934.00 1936.30 1 1mm. 1882.00 1883.00 35 INT $1
0.5 mostly confined 1888.00 1888.50 41 INT $1 to the small 1890.00 1891.00 56 MO $1 dkgreen 1898.00 1899.00 45 MO $1 amph-gnt 1911.00 1913.00 45 INT $1
patches where 1917.00 1918.00 44 INT $1
Po is 3-7% 1926.00 1927.00 56 MO S1 0.5 concentrated in 1928.00 1929.00 40 INT $1
biotlsed dk 1932.00 1933.00 60 MO $1 green amph
patches and
lesser
throughout
matrix
0.2 0.2
0.0 0.0 locally up to
2% for Asp & Po
0.1 f.g
desseminated
in matrix
1936.30 1939.40 2 50 0.5 Patchy biol
alt'n assoc Po
locally up to 5%.
1939.40 1939.80 2T 70 5.0 1939.40 1939.80 67 INT sz 1939.80 1945.00 2 65 0.8 1940.00 1940.50 53 MO Si
7.0 weak shear 1940.70 1941.30 68 WEK sz 0.8
0.2 1942.00 1944.00 56 MO S1 12.0 5.0 qtzflooding
o.2' and sheared
I I I
!
I i i I i
1944.00 1944.70 43 : INT $1
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I MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT I i Majo, Cont As !Cpl Mt Po p •k VG Vein 'Vein Contact Alpha From I Alpha Int 'Typ Alph I From To Comments From To Te} Comments To Comments From To a Int :Typ, Comments From To Int Type Comments Unit %:%'%'% Y •r5peck, Type % Type deg deg e deg
1944.70 1945.90 QZ 15 s 60 1945.00 1948.20 2T 60 7.0 increasing 1945.00 1948.20 57 INT sz Strong Po min'zn
toward LC
0.5 confined to 1945.90 1946.50 QZ 85 m s 60 host rock
enclaves
12. ranges 6% at 1946.50 1948.00 66 INT S1 UC to 18% at LC
1948.20 1950.30 1 90 0.0 0.0 Finely
dessemina!ed
1950.30 1950.80 4H 70 20. 1950.30 1950.80 70 INT sz 1950.80 1956.00 1 60 1951.00 1952.00 45 INT S1 1956.00 1959.60 2 1952.60 1953.50 61 MO S1
1957.00 1958.00 50 WE S1
1959.60 1961.50 4H 25 12. 2% in first 1 /3,
15% in rest
2.0 1960.40 1960.80 QZ 20 I 1961.50 1975.50 4A 33.
3.0 1961.65 1962.30 QZ 20 1962.00 1963.00 50 so
1966.00 1967.00 45 so 0.1
1968.50 1969.00 CA 60
1970.00 1971.00 55 so 0.1 0.1 1971.00 1973.00 QZ 10 D 0.1
0.1 0.1 2.0
35.
I
!
i I i I I I I I I I I i
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MAJOR UNIT I MINERALS QTZVEINING FABRIC FOLD FAULT From To
Majo~ Cont As ! c,. Mt I Po Py% VG Comments From To Vein Vein !Te, Contact! Alpha Comments From To A::ai Int f!P From To Alph
lnt~YP• Comments From To :!fe~ Int Type Comments · Unit % i 00 % % Speck, Type % Type ! deg Comments ltt:n
1975.50 12009.20 2 90
1977.00 1978.00 46 WE S1
1982.00 1983.00 60 WE S1
1987.00 1988.00 46 S1
1991.00 1992.00 42 S1
1996.00 1997.00 48 WE S1
2002.00 2003.00 60 MO S1 weak
shearfol'n
2008.00 2009.00 46 MO S1
2009.20 2011.70 4H 2.0
16.
2011.70 2013.70 4H 7.0
9.0
2013.70 2014.50 2T 1.0 2014.50 2022.45 7A
2020.00 2021.00 60 MO S1
2022.45 2022.85 4H 20.
2022.85 2025.40 4A 1.0 2023.00 2024.00 52 so
0.5 0.1 2024.60 2024.70 37 ZF
2025.40 2044.60 48 10.
2026.00 2028.00 50 so
2027.60 2028.00 QZ 25 2-3cm
grun alt'n
margins.
2030.00 12031.60 50 MO SF
0.5 2031.60 2032.30 QZ 75 I Minor Po 2032.00 2036.50 40 MO S1 3.0 increase in and Chi
I mineralization patches.
down section
semi massive
pod at 2042.1 :
which Is 3 cm
I I
wide i
I I I I : i i I
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT Majo1 Cont As Cp Mt I Pol VG Vein Vein Contact Alpha AJJ:,ha Typ Alph ~ Aih From To Comments From To !Te> Comments From To Int Comments From To a Int I Comments From To Int Type Comments Unit. % % % : % Py% Speck~ Type % Type deg eg e Idea ~ eg
2033.50 ~034.00 55 MO MF
2035.40 ~036.20 50 MO SF 2036.50 2039.00 60 MO S1
2037.00 ~038.00 50 MO FD
2039.00 2043.50 3 MO S1
2043.50 2044.60 40 MO S1
2044.60 2089.00 1 48 0.3 2044.60 2057.00 45 MO S1
0.3 0.3 minor specks 2057.00 2063.00 50 MO S1 2058.00 2058.40 20 MOD OS of Pyrite and
Cp 2060-2062
2089.00 2091.10 7H 62 0.1 2063.00 2080.00 50 WE S1 very very 2091.10 2132.00 1 60 0.1 weak 2132.00 2157.50 2 40 0.1 foliation
massive
2080.00 2089.00 55 MO S1
2089.00 2091.10 55 MO S1
2091.10 2117.00 50 MO S1
2117.00 2129.00 55 MO S1
2130.00 2132.00 40 MO S1
2132.00 2140.00 40 MO S1
2140.00 2156.00 35 MO S1
I
!
I I i
i
. I i i I j I I i .
! MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT
From To IM1:1j()~ Com As 'cp Mt ~~1Py%
VG Comments From I To Vein Vein Te> Contact Alpha Comments From To Alpha Int Typ From To Alph
Int trypE From To :1~~ Comments Comments a Comments Unit % j% % Speck, Type % Type deg : deg e deg
2157.50 2167.05 1 2158.00 2159.00 CA 5 Carb-serp
frax
linings
1·3mm 2160.30 2162.50 QZ-C 6
2162.00 2163.00 45 WE 82
2167.05 2172.60 48 10. Varies from
-2% to zones
of 25% over
15cm.
2170.00 2171.00 66 MO 82
2171.00 2172.00 47 MO 82
2172.60 2173.40 13 2173.00 2174.00 45 MO 81 2173.40 2181.70 1 45 40.
10.
30.
0.1 17.
0.1 1.0
2181.70 2182.40 13
2182.40 2185.40 2
2185.40 2186.40 1
2186.40 2198.20 48 2187.30 2188.00 QZ 85
2189.00 2191.00 57 MO FD
2191.00 2192.00 63 FD Folds
appear to
: be Z's but
not certain.
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: : I I i I i I I
MAJOR UNIT MINERALS QTZVEINING FABRIC FOLD FAULT Majo Cont Aslcf Mt Po Py%~ Vein Vein Contact Alpha A1fe~a Ttp Alph I
Alfd Int From To Comments From To 'Te) Comments From To Int Comments From To a Int Typ, Comments From To Type Comments Unit % i •., % % Type % Type deg deo 1a •o.
2196.00 2197.00 64 so 2196.00 ~196.50 75 WE ZF 0.1
2198.20 2201.00 4A
45. 2201.00 2202.50 2
. I I I
• Assay MAJOR UNIT MINOR UNIT ALTERATION
Sample From AU ppm From To it Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments 0.00 4.10 CASIN M M Chlorite rich veins with 4.10 29.90 2 Fine grained to medium grained mafic volcanic. The The amph-pyrox in the maybe chloritoid.
unit is cut by 5% Cc veins ranging from 0.3-1.5cm chlorite might be
wide (locally the unit is more Cc flooded than Cc chloritoid ? -1 % Po
veined). From 4.1-19m, the unit displays strong (ternish) from
chlorite alt'n in veins with m.g-c.g amph-pyrox. 11-11.3m associated
with chlorite veins.
From 27-29.3m, the
unit Is slightly
brecciated. The lower
contact is irregular and
truncated by Cc flooding ::376461 9.00 10.00 0.01 ~376462 10.00 11.00 0.01 :376463 11.00 11.30 O.D1 _376464 11.30 12.00 0.01 _376465 12.00 13.00 0.01
29.90 37.60 2 Fine grained mafic volcanic, weakly foliated, fairly The unit is borderline w less chlorite, less Cc fresh unit with weak-mod chlorite alt'n in the last ultramafic amphibolite veins 1m only. The unit is cut by <1% Cc veins up to (1M) from 32.5m over w M M increase of Cc veins in 0.8cm wide. The matrix is mainly composed off.g. 50cm. the lower contact mafic volcanic, almost amph and 8-10% f.g. feldspars. is gradalional. brecciatic texture in
37.60 50.00 2 Fine grained to medium grained mafic volcanic, From 43.7·45.2m, the some places. fairly similar to first# 2 unit. The unit displays unit is brecciated with w Relatively fresh mafic weak-mod chlorite alt'n with f.g. planar black-dark strong Cc volcanic compared to green minerals: pyroxenes or chloritoid?. The unit veining/flooding. From previous units. is cut by 2% Cc veins ranging from 0.3-1.5cm wide. 48-50m, the unit M M weak-mod chlorite altn,
displays 10-12% Po in weak green amph alt'n veins . Increase of the in the Po rich zone. dark green amph
content in the Po rich
zone: the unit is
borderline UM. The
lower contact is
gradalional. 376466 46.00 47.00 0.01 376467 47.00 48.00 0.02
::376468 48.00 48.50 0.02 ::376469 48.50 49.20 0.01 ::376471 49.20 50.00 0.02
I i i •
i i
•
Assay MAJOR UNIT MINOR UNIT ALTERATION I Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
E376472 50.00 51.00 0.01 50.00 51.80 1 Ultramafic Amphibolite. Weakly foliated f.g.unit. The lower contact is
Dark colour and hard to break. The entire unit might gradational. be borderline 2 but displays <3% feldspars. The
matrix is mainly composed of amphiboles (acicular
shape?). Featureless & no signifveining. :376473 51.00 52.00 0.01 51.80 59.60 2 Weakly foliated fine grained unit. The unit is dark From 57.9-59m, the w weakly altered
in colour and hard to break. The entire unit might unit displays 10-15%
be borderline 2 but displays <3% Fd. The matrix is Po in veins along
mainly composed of amphiboles (acicular shape?). foliation planes with
Featureless and no significant veining. weak bio alt'n (<1%}.
The lower contact is
sharp.
'.:466001 55.90 56.90 0.02 :466002 56.90 57.90 0.02 :466003 57.90 58.30 0.06 ~466004 58.30 59.00 0.69 t:466005 59.00 59.60 0.08 t:466006 59.60 60.60 0.02 59.60 62.00 1 Ultramafic Amphibolite? The first 1 m is borderline 2, Locally, short and
the rest of the unit seems to have only acicular irregular Cc veins up
amphiboles. The unit is weakly foliated and to 0.5cm wide. The
featureless. The amph (probably pyroxenes as well) lower contact is are f.g.to m.g. gradational.
t:466007 60.60 61.60 0.03
i
I I I i
I i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
62.00 77.30 2 F.g. to m.g. mafic volcanic. The unit seems to be a The chlorite is usually w M amygdoidal texture of flow. The unit displays f.g-m.g. pyroxenes, 5% associated with a the chlorile alt'n feldspars (locally up to 10%). Mod-str chlorite alt'n. black-dark green w decrease of the chlorite The chlorite is in pockets (looks like amygdaloidal). mineral (looks like alt'n
needles): chloritoid? UM with 1 % talc Decrease of the w w w fairly fresh basalt with chlorite content in the weak bio alt'n locally. last 3.5m. The lower M s strong ch!orite alt'n in contac Decrease of the mafic (intrusive unit?) chlorite content in the w w weak chlorite locally, last 3.5m. The lower cut by 1 % Cc veins contact is fairly sharp. w w fairly fresh mafic
volcanic, less fd than 77.30 78.30 1 Ultramafic Amphibolite. F.g. to m.g. unit. The unit The entire unit is previous 2 unit
is dark in colour, wk-mod foliated and featureless. borderline 2 since the w relatively more Cc veins The matrix is mainly composed of unit displays 2-3% than previous unit but f.g-m.g.amphiboles and 1 % soft white minerals feldspar. The lower still weak (probably talc). contact is truncated by w M more chloritic unit than
chlorite alt'n with a previous unit black mineral (needle). M w slightly brecciatic zone
78.30 100.00 2 Well foliated f.g. mafic volcanic. The unit is The unit is fairly fresh, in mafic grading from weak feldspar mafic with weak mod no significant veining. w w locally mod chlorite chlorite alt'n to feldspar rich mafic volcanic with Locally, the unit alt'n but overall weak. 50% green amph. and 50% feldspar. displays weak bio all'n. Weak green amph alt'n
The lower contact is around Cc veins gradational with M M w biotite bearing increase of the chlorite metavolcanic alt'n. M w weak chlorite locally,
100.00 107.30 2 M.g. mafic volcanic. The unit looks like more The unit is cut by Cc veins can be intrusive than the other units. The unit displays 1-2% Qtz-Cc veins up discontinuous/dismembe strong chlorite alt'n, m.g. pyroxenes/amph., and f.g. to 1.5cm wide. The ed feldspar (content decreases in the lower part of the unit displays dark w section) green amph rich bands M w
(probably alt'n) around fairly fresh sill the Cc veins. The w w w locally Qtz/Cc veins. lower contact is M
! Mt alt'n
irregular. M w more biotitic unit than
others mafic units.
i I i i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
107.30 131.10 2 F.g. to m.g. mafic volcanic. Relatively finer grained Locally, the unit
than previous 2 unit (averaging 2-3% m.g. displays mod-strong w weak bio on the edges amph/pyrox). The matrix consists of f.g. amph chlorite alt'n. <1% w w (65%) and f.g-m.g. feldspar (35%). The unit ls well Pyrite. The unit is M biotitic mafic volcanic foliated. borderline UM over s M kimberliles with altered
50cm. The unit is cut olivine, Cc floods and by 1 % Cc veins ranging phlogopite from 0.5-1cm wide. The M w altered mafic lower contact is M s strongly Cc veined gradational. mafic volcanic
131.10 156.20 2 Fine grained, well foliated mafic volcanic. Fairly The unit is cut by 1 % M s M Stronlgy Cc veined similar to previous 2 unit but finer grained and with Cc veins. The unit is mafic volcanic, mod bio less feldspar. The unit displays 5-8% feldspar cul by 1 % Qtz veins alt'n locally throughout. Locally, wk-mod chlorite alt'n (+needle averaging 2cm wide. M M w w sed?mafic?inter? like black mineral, amph?). Locally, minor Pyrite. M M Jess sheared mafic
The upper part of the volcanic section looks like w fairly fresh mafic volcanic intrusive with weak w garnet bearing mafic? foliation. Or sediment
156.20 168.60 2 M.g. mafic volcanic, relatively coarser grained than The unit is cut by
previous unit. The unit does not display any chlorite 2-3% Cc veins ranging
alt'n. The relative amph/feldspars content varies from 0.5·1.5cm wide.
throughout the section. Le zones with more fd than The lower contact is
others. The foliation is weak. gradational with
increase of the chlorite
content. 168.60 177.70 2 F.g. to m.g., chlorite rich mafic unit. The unit Possibly dark green
displays mod-strong chlori!e alt'n overprinted by a amph alt'n around Cc
kind of amph (black needle, amph?). The lower part veins.
of the section is less chloritic but e.g.
177.70 181.80 2 Slightly brecciated mafic volcanic, f.g. to m.g. Traces Po
unit. The unit is cut by discontinuous Cc (disseminated} and
veins/floods. The matrix is mainly composed of probably chalco in
green amph and feldspar (55%/45%). The chlorite traces as well.
alt'n is weakly developed throughout.
•
•
i I I i I
LITHOLOGY LOG 07-NSD-008 Page 5 of 451
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
181.80 204.00 2 Well developed mafic volcanic that varies from f.g. The unit is cut by
to m.g. (small intrusive parts?). The chlorite alt'n 2-3% Cc veins up to
is locally mod-sir developed, locally in veins or 2.5cm wide. Very weak
rimming Cc veins and overprinted by m.g. amph. bio alt'n (locally) in
the lower part of the
section. The lower
contact is truncated by
a Qtz-Cc vein 5cm wide. 204.00 206.60 2T Nil-wk foliated fine grained mafic volcanic, bio
bearing unit. The unit consists of 15% f.g bio, 55%
amph, 35% feldspar. Locally strong chlorite-green
amph alt'n. Po in traces and has been
disseminated. No significant veining. 206.60 226.40 2 Fine grained mafic volcanic, locally medium From 215-221m, the
grained. Varies from fairly fresh basalt to more unit is massive
green coloured unit. Some amph are alt'd (e.g. and (grey-green) and darker in bands 1cm wide, do not look like pillow flanked with 10% selvages). dismembered/discontim
ous foliated Cc veins.
Over 1 Ocm, black hard
bands cross cut by Cc
veins: maybe a Cc
veined: tachylite?. The
lower contact is
gradational. 226.40 231.60 2 Weakly foliated unit with less Cc veins than From 226.4m over
previous unit and coarser grained (but the unit does 40cm, f.g.-m.g. Qtz-Cc
not look like a sill or dyke). The unit is weakly fol'd veins. Gradational LC. and the m.g-c.g. amph are orientated in the
direction of foliation. 231.60 242.00 2 Fine grained unit, strongly Cc veined, cut by 25% The dark green amph
m.g. Cc veins ranging from 0.3-10cm wide (-2% alt'n is weakly-mod
qtz-Cc veins). -1-2% pyrite associated with Cc. developed. The lower
Pervasive mod chlorite alt'n overprinted by a low T contact is diffuse. amph (actinolite?)
242.00 248.00 2K Intrusive unit, probably a sill, no foliation. The unit The centre/vent might
consists of m.g-c.g. amph/pyroxene and f.g. be not too far away
feldpsar. The unit is fairly fresh and cut only by 3 since the contacts are
Cc veins up to 3cm wide. The lower contact is diffuse diffuse.
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From = To AU ppm From To Unit Comments Comments From ! To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
248.00 256.70 2 Well developed weakly foliated 2 unit. The unit In the last 2m, the unit looks like a flow. Varies from f.g. mafic volcanic displays weak chlorite
with 1% m.g. amph to a more feldspar rich unit alt'n and is cut by 2 (50% fd/50% amph) with 1 % Cc veins. Qtz veins up to 15cm
wide. The lower contact
is obscured by
Cc/chlorite and minor
Py. 256.70 268.00 2 Grading from Mt altered mafic unit in the first 2m
to more massive medium grey unit cut by bands of
wispy light green amph (probably actinolite). The
upper part of the section displays 15% bio slips <
1mm wide. The lower contact is gradational. 268.00 269.00 3A Intermediate (andesite?). The unit is very pale in Possible orientation of
colour and consists of 90% very f.g. plagioclase the amphiboles but
flanked by 10% m.g. amph ranging from 1-5mm most of them are in long. No significant veining. The lower contact is random position. irregular (no more m.g. amph).
269.00 282.80 2T Well developed mafic volcanic with relatively more The upper part of the
bio slips than all the other mafic units in this hole. section has a light The unit displays 10-15% bio slips locally. green planar mineral,
Heterogeneous unit regarding the bio alt'n. From probably amph
274.7-275.6m, the unit is cut by a f.g. Qtz vein. (actinolite?). Bio alt'n
increases in the lower
part of the section. The
lower contact is
gradational. 282.80 283.30 28 Small unit, fairly massive with 3-5% bio alt'n (bio Both upper and lower
slips). The matrix is mainly composed of amph and contacts are
Fd. The unit displays 5-8% amygdals up to 3mm in gradalional (diffuse?)
diameter filled with a white soft mineral (not calcite,
zeolile?) 283.30 290.80 2 Weakly foliated mafic volcanic with up to 5-8% bio
alt'n (up to 30% in the last 1 m). The unit displays
-25% feldspar throughout. No significant veining. 290.80 291.40 13 Kimberlites ranging from 1.5-5cm wide. Consists of The three kimberlites
5% altered olivine up to 5mm in diameter, the rest are intrusive in of the dyke is composed of brown micas massive mafic volcanic. {phlogopite?) and Cc (floods). Possibly ilmenite.
I I
LITHOLOGY LOG 07-NSD-008
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
291.40 305.00 2 Varies from bio alt'd mafic volcanic with bio alt'n Possibly <1 % amygdal up to 5-8%, probably wk-mod green amph alt'n, to around 301.5m. strongly Cc veined unit (from 299-305m) with 25% Disseminated Py Cc up to 1 cm wide II to CA. Mod bio alt'n is associated with Cc associated with the Cc veins. veins.
305.00 329.00 2 Strongly Qtz-Cc veined mafic volcanic, locally In the upper part of mod-sir biotitic. The matrix is mainly composed of the section is cut by 3
amph and feldspars (locally m.g.green amph). The Qtz veins 10-15cm unt is cut by 30% irregular and discontinuous Qtz wide. Locally, -Cc veins ranging from 0.3-4cm wide. weak-mod green amph
alt'n (e.g. and darker
amph). The green
amph alt'n is strongly
developed in the last
1 m with weak light
green amph alt'n
(actinolite?). 329.00 333.00 2 Intermediate? Mafic? Sediment? The unit displays It seems that the unit
much more feldspar than previous mafic volcanic. displays 3-5% f.g. -20% amph (brown-black). The unit has 5-8% f.g. sericite and f.g.
bio and is cut by 5-8% Cc veins up to 1.5cm wide. tourmaline. The lower
contact is gradational. 333.00 337.70 2T Well foliated f.g. mafic volcanic, bio bearing unit. The bio alt'n decreases
Relatively more biotitic than previous 2 unit. Bio from 336.7m down alt'n is up to 25%. The unit is cut by 10% Cc veins section. The lower ranging from 0.1-1.5cm wide. contact is gradational.
337.70 341.00 2 Weakly foliated fine grained mafic volcanic, fairly The lower contact is
fresh. Consisting off.g. amph and <10% feldspar. gradational The unit is dark grey and fairly massive
(featureless). From 339.7-341m, the unit displays
weak-mod bio alt'n (bio slips <1mm wide). 341.00 343.30 6 Mafic or sediment? The unit is fairly massive, dark Its hard to tell if the
grey and weakly foliated. The matrix seems to have matrix is composed of feldspar, Qtz and minor bio. The unit displays 3% amph or just m.g. garnets overprinting the matrix. feldspars/Qtzlbio. No
significant veining
except the lower
contact truncated by a
Qtz vein 15cm wide. A66008 341.30 342.30 0.01 466009 34230 343.30 0.01
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit I Comments Bio Car Chi Gru Hem Ser Si Comments
::466011 343.30 344.00 0.01 343.30 345.70 4F Porphyroblastic 4F. The unit consists of 15% e.g. M porphyroblastic 4F garnets averaging 1cm in diameter in a f.g.
bio/feldspars/Qtz rich matrix. The unit displays a
10% f.g. green amph rich patch with e.g. garnets:
4E bands or altered ::466012 344.00 345.00 0.01 ::466013 345.00 345.70 0.02 ::466014 345.70 346.70 0.01 345.70 349.90 6 Sed? Garnet poor 4F? The unit is weakly The lower contact is w w sediment? Or garnet
developed and distorted. The unit displays biotite gradational. The unit bearing mafic volcanic? and garnets (3-5%), and probably Qtz (too hard to has 1-2% Qtz eyes (do
be feldspar). The garnets are 0.3-0.8cm in not seem to be
diameter. The unit has 3% green amph in bands dismembered Qtz veins] overprinting the matrix.
:466015 346.70 347.70 0.08 -466016 347.70 348.50 0.01 :466017 348.50 349.00 0.01 ::466018 349.00 349.90 0.09 ::466019 349.90 350.90 0.01 349.90 361.80 2T Fine grained to medium grained mafic volcanic with From 357.7-358m, the M w
30% biotite. The unit displays feldspar and remnant unit has 5-8% remnant
amphibole. The unit is cut by 1 % Cc veins. From serpentinized olivines
355.5-357.7m, there is a fault with broken up rocks (2mm in diameter in
(RQD<10) with carbonate and weak chlorite alt'n. average). From 358m
down section, the unit
has more
m.g.amphiboles than
the upper part of the
section. -466021 350.90 351.90 0.01
361.80 365.90 2 Fine grained mafic volcanic. Relatively fresh w M w Fault gouge with weak compare to previous unit. The unit displays <5% bio chlorite alt'n and alt'n. The matrix is mainly composed of f.g.green fractures filled with Cc amph and feldspars. No significant veining. The M w lower contact is diffuse. w Failry fresh basalt
365.90 367.40 2 Fine grained to medium grained mafic volcanic The unit does not have M flecks of micas (maybe intermediate). The unit consists of f.g. any foliation {random {phlogopite) feldspars (more than 70%) and lesser amph. The orientation of the mica w w unit is overprinted by flecks of soft brown mineral, rich flecks. No M w weak-mod bio alt'n probably mica (phlogopite?}. significant veining. locally.
i i I i i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
367.40 406.30 2 Weakly foliated unit, f.g. to m.g. mafic volcanic. From 386.3-386.7m, w ultramafic? With Alternating feldspar rich zones and zones with less the unit is cut by a serpentine on fracture feldspar. Amph content varies from 30-60%. From medium grained Qtz plans. 379-390m, the unit Is finer grained and appears vein with 40% remnant w w more massive than upper part. hosted rock. Locally, w w Ultramafic with
weak chlorite alt'n and porphyroblasts of talc weak-mod bio alt'n In Ultramafic with amph the lower part of the and talc section Gabbro with minor talc
406.30 409.00 1 The unit is featureless and weakly foliated. The Both upper and lower alt'n matrix is mainly composed of amorphous contacts are Ultramafic amphibolite serpentine. The unit Is fairly hard except in some gradational. with talc alt'n. places where the unit displays 3-5% talc. The CHECKED by JB 09/7 w Ultramafic amphibolite serpentine Is seen only along fractures. with talc throughout
409.00 413.20 1 Well foliated ultramafic, with f.g. amph and less The lower contact is and weak carbonate talc. The unit displays nil bio alt'n (locally weak). gradational. alt'n in the lower part of The unit is cut by 1 % Qtz-Cc veins ranging from the section 0.5-1cm wide, surrounded by weak dark green w mafic? ultramafic? amph alt'n. w w weakly altered mafic
413.20 440.00 1 Unusual texture. The unit displays f.g serpentine. Locally. the unit is cut volcanic, weakly foliated The unit Is overprinted by elongated porphyroblasts by 1-2% irregular Cc w strong e.g. dark green of talc {give the direction of foliation, otherwise veins up to 1.5cm wide amph alt'n the unit is fairly massive) that average al 5mm in (locally slighlty M w green amph alt'n in the diameter, overprinted by a dark green amphibole brecciatlc). It is very last 70cm
hard to see any M sediment or mafic? crystals in the matrix. w sediment or mafic? The lower contact is w w weakly altered mafic gradational. The volcanic original protolith is M probably a pyroxenite M .CHECKED by JB 09/07 M
I I •
i •
I I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
440.00 497.50 1 Fairly similar to previous ultramafic. The matrix is As before, the unit w still fine grained but not as amorphous as the other displays 20% M UM. The unit has a light green colour due to the elongated M w composition of matrix (acicular amphiboles). The porphyroblasts of talc w unit is probably a 1 M. averaging 0.8cm in s
length, overprinted by w a dark mineral with a s needle shape w (amph?). M Porphyroblasts M
boundaries are not as
clear as before
(diffuse). CHECKED
by JB 09/07 497.50 510.90 7A The unit is light green in colour and displays 75% The presence of talc is
f.g-c.g. pyroxenes and 25% f.g. plagioclase. The probably due to the
crystals are intergrown. The unit does not have any high content in Mg
foliation and is fairly massive. The unit has 3% of a {the gabbro is
soft white mineral (talc?}. surrounded by two UM
units). Both upper and
lower contacts are
gradational.
501.5m=switch to NQ 510.90 522.00 1 The unit ls fairly similar to previous UM. The unit In some places, the talc
consists of f.g-m.g. acicular amphibole (not as fine is overprinted by
grained as the other UM) with light green colour. another type of
The unit displays 3-5% talc (not porphyroblasts amphibole. The unit is
anymore, overprinting the matrix). slightly foliated. 522.00 568.00 1 The unit is fairly similar to previous unit. The Talc can be
matrix is composed of f.g-m.g. amphibole acicular in porphyroblastic as
shape. The unit is weakly foliated, but on fractures before but also f.g.in
plans the amph does not have orientation. The unit the matrix. The
displays 5-8% talc throughout. porphyroblasts are
overprinted by a
black-dark green
m.g.amphibole. The
. lower part of the :
section has weak
carbonate alt'n
I
(irregular and short Cc
i i I i
. veins).
I I i I
! Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
568.00 570.80 2K C.g. mesocratic gabbro dyke/sill. The matrix is No serpentine or talc.
composed of -40-50% green amph, the rest mainly The plag matrix is fine
f.g. plagioclase. Trace cp. Minor veins <5mm wide grained, <1% short
with cores of black f.g. tourmaline? and irregular Cc veins.
The unit has a
brecciated texture at
upper contacts. Both
contacts are gradational 570.80 597.00 2 Weakly foliated maflc volcanic. The upper part of From 588m down
the section is still borderline UM, and the unit section, the unit has
displays a soft light green mineral (does not seem 5% bio slips. WEDGE
to be talc). In the rest of the unit, the matrix to the left (270) @
consists of mainly f.g.-m.g.amph and f.g. plagioclase 594m. The lower
contact is gradational.
The unit is cut by
1-2% Qtz-Cc veins up
to 1 Ocm wide. 597.00 599.30 2 The unit is weakly foliated. The unit is dark green At upper contact, the
in colour and displays pervasive strong green amph unit has 2 bio-gar rich
alt'n (coarser grained, hornblende?) and weak bio bands overprinting the
alt'n. The original matrix has been destroyed by green amph (not
alt'n. Disseminated Cpy throughout. magnetic). Strong
green amph alt'n in the
last 70cm. The lower
contact is gradational. 599.30 613.50 6 Biotitic light brown, well fol'd metaseds with Varies from well
variable textures, most has -30-40% f.g. bio & foliated, -planar, to 50-60% f.g. white qtz. Qtz varies from mainly vfg sheared and
matrix to mainly re-crsyt'd aggregates up to 3-4mm -deformed looking
that give a pseudo-porhyritic look. No signif gar or (mainly where the amph. recryst', has taken
place). Trace cp
throughout. Unusual v
bio'd UM?? at
603-603.9.
• • i I I i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
613.50 651.10 2 Mod foliated, clotty mafic volcanic. F.g. to m.g. The unit is cut by 1%
unit. The unit consists of f.g.-m.g. amphiboles and Cc veins up to 1 cm
equigranularfeldspars. Locally, the unit displays wide. Much has 5-10% 2-3% bio slips (biotitic unit from 638-640M, with bio dark green amph clots content up to 10-12%). -1-2mm wide x 5-7mm
long in the vfg pale
matrix. 651.10 655.80 2T Nil to wk foliated brown-grey homogenous 2T with Gradational LC with
10% Irregular Cc veins (0.5-20cm). 40cm sheared c.g biotised 2.
foliated section with 20cm Cc vein (652.1-652.6m). 655.80 658.00 2 M.g. homogenous green-grey, weakly to
non-foliated amphibolite consisting of 20%
plagioclase, 20% biotite, 60% green amphibole. 658.00 696.70 2T Brown-grey 2T ranging from non foliated to 671-674m is
moderately foliated. Fabric development and strain med-coarse grained
increasing towards LC. Overall 10% irrgeular Cc strongly biotised
veins (0.5-20cm). Increased feldspar content in 2Twith no fabric. lower -7m to -30%.
696.70 708.70 2 Fine grained, foliated non-schistose 2, consisting Difficult to tell but
of very f.g matrix of biotite -25%, brown possible minor quartz. amphibole -25% and 30% feldspar. 10-20% 10% of rock is
feldspar "phenocrysts" (0.5-3mm). scattered irregular
Qtz-Cc veins 1-10cm.
Grad'nl LC. 708.70 710.50 2T Very fine grained, very finely foliated wavy fabric Also the development
conisting of-10-30% Cc, -25% biotite, with the of Cc stringers 1-2mm
remainder being brown amphibole. -5% irregular in much of the unit. Qtz-Cc veins (0.5-3cm) Rare muscovite flakes
up to 10mm along
some Qtz vein margins. 710.50 710.70 3K Cross-culling plag porphyry intrusion (-13cm true Sharp brittle
thickness). -80% sub-rounded cream plag contacts. -2% brown phenocrysts ranging from 0.3-5mm in size, -10% angular 2T host rock
are> 1mm. The cream-grey f.g groundmass fragments <1.5cm. No
seems mostly plag with -15% tiny elongate dk brn visible qtz, perhaps mineral (probably biotite) some in the
groundmass though. 710.70 712.50 2T Exactly the same as previous 2T above the cross
cutting porphyry.
i
I . I I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From I To AU ppm I From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
712.50 730.20 2K Mostly well foliated but non-schistose fabric. UC to 114.4m has Fairly homogenous unit consisting of-40% mo-strong Cc alt'n,
elongate aligned green amph crystals (0.3-3mm) 114.4-116m has 5-10%
within a matrix of plagioclase and perhaps some f.g biotite. Whole pale amphibole. unit has -3% cc-Qtz
irregular veins 1-4mm. 730.20 760.90 2T F.g brown-grey 2T with -15-20% irregular Sheared with strong
pervasive Cc-Qlz veining throughout unit. Veins planar fabric from UC
are mostly m.g. (0.5-2mm g.s.). Veins contain -5% to 733.7 with -20%
green-grey amphibole where associated with Po, sheared Cc stringers. which is up to 10% Po locally. Rest of fabric is wavy
to completely
dismantled by the
pervasive Cc-qlz
veining and
deformation.
744m-LC has
consistent fol of -15deg 760.90 761.10 3G Homogeneous, equigranular green-cream coloured, Contacts display
semi-concordant aplite intrusion with true several 1-2mm
thickness of 12cm. Mineralogy is quartz and aphanitic cream
feldspar -40%/60%, with a grain size of <1 mm. irregular stringers. 761.10 768.50 2T Mod to Str foliated typical brown f.g 2T with 35% Cc 1-2% muscovite flakes
irregular stringers and a blebby matrix. The unit <2mm associated with
is weakly sheared with increasing intensity and Cc alteration.
fabric development towards LC . 2% green amph
crystals that are 1-2mm along Cc vein margins in
places 768.50 791.50 2 Well-foliated m.g. green-grey 2 with 5% planar Cc F.g brown 2T zone
stringers (1-4mm). Weak foliation from 776m-LC. from 772.3-772.8m.
Mineralogy is 5-10% biotite(locally 25%), 30%
plag, 60% green/green- grey amphibole. 791.50 796.50 2T Moderately to well fol'd brown 2T, borderline 2, due 10-15% f.g biotite,
to 10-15% green amphibole within the matrix. 25% -60% brown
of the rock consists of f.g Cc in the matrix and also amphibole, 2%
at fine stringers and veins up to 3cm wide. red-orange euhedral
gnt porphs up 13mm.
i •
I I
Assay MAJOR UNIT MINOR UNIT ALTERATION s From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
796.50 803.80 2 Weakly foliated homogeneous green-grey 2 with a -0.3% very fine matrix consisting of 25% f.g plag, 5% biotite, and grained desseminated
55% green amphibole. 5% Cc-Qtz veins (<2cm). Po. throughout unit.
10% scattered porphyroblast-like ragged oval blebs
of Cc (1-8mm). 803.80 808.10 2K Weakly foliated , m.g homogeneous, -equigranular <3% qtz sweats and
rock consisting of -25% feldspar, 20% biolite, 15% thin irregular veins
green amphibole, -30% quartz, and 10% Cc as fine intermixed with the irregular stringers and veins. Cc. -0.3% f.g
desseminated Po. 808.10 825.00 3F Fairly homogeneous unit of light grey foliated rock From 823m to LC ii is
with weak distortion and folding evident by the very intensely Cc-Qtz
fine biotite layering on the mm-cm scale. flooded (75% is Cc),
Mineralogy is -60% fd-qtz, 10-15% blot, 15% Cc only -20% of the host
blebs and stringers (<3mm}. and 0.5% local fine rock remains in this dissem'd Po section and it does not
have a strong shear
fabric. E466022 823.00 824.00 0.34 s s f':466023 824.00 825.00 0.29
825.00 825.70 6V Metapelite similar to 4F except there are no -0.5%fine w s garnets. Equigranular speckled rock of 60% biotite desseminated Po, Tr Cp
and 40% white grains of qtz and/or feldspar. Weak
foliation overall. 825.70 837.50 3F Generally a massive, med-dark grey felsic volcanic,
no phenos, could be a flow but presumed to be
welded ash luff. Composed of aphanitc qtz-fd with
minor sericite and bio.
837.50 862.90 3F Light beige-grey, weakly to mod foliated felsic vole, Although it is
still mainly aphanitic qtz-fd with minor ser-bio. Unit grey-beige and fol'd,
is much more fol'd and a lighter colour than hard to see much previous massive section. biottie,could be
discolouration caused
by shearing. Avgs
-10-15% Cc veins,
f':466152 846.00 846.80 minor qtz veins.
0.08 f':466153 846.80 847.70 0.96 ;:466154 847.70 848.50 0.09
I i i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit! Comments Bio Car Chi Gru Hem Ser Si Comments
862.90 896.00 30 Med-dark grey, massive falsie volcanic with UC unusually sharp ~52.90 854.50 1 Sheared, -mottled ultramafic -10-15% Fd phenos 1-3mm In aphanitic grey within 1-Zcm so serpentinite. 50cm margins groundmass of Qtz-Fd. No obvious possibly a flow have mod-strong dolomite alt'n bedding/banding so logged as a flow but could be contact? Scattered lenses < 2-4mm throughout. Rest welded ash-x'I luff instead. brittle Cc filled veins is -m.g. green serpentine, often
up to 6cm, -5% micaceous flakes. overall. LC gradual 912.60 913.20 1 Massive, med green UM, mix of
colour change over serpentine and amph.
1-2m 896.00 995.20 3F Light to med grey falsie vole, fresh sections contain Unit is commonly x-cut
5-10% pale Fd phenos which are obscured in the by thin frax <2-3mm, at
weakly sheared areas. Aphyric, typical aphanltlc mix high angle to fol'n,
of Qtz-Fd, minor Ser, Tr Bio, Foliation is - all due to flanked by irreg
local weak shears and is very irreg. bleached patches. No
major qtz or Cc veins,
no signif alt'n or major
shears. l::466024 994.20 995.20 0.01
:::466025 995.20 996.00 0.05 995.20 1002.40 6 Variable, highly & pervasively alt'd section. Appears Minor relict intervals M w HI % bands of pale to have been mainly f.g. biotitic elastics but now of felslc vole sects. green amph-f.g. Cc largely overprinted by irreg, -diffuse, f.g. pale Last 1 m looks like a with minor Po. green amph>Cc alt'n bands up to 5-7cm wide+/- 2/2T but all green
-2% Po. amph appears
E:466026 996.00 997.00 secondary.
0.01
E:466027 997.00 998.00 0.02
l::466028 998.00 999.00 0.07
l::466029 999.00 999.60 0.74
1::466031 999.60 1000.70 0.04
!=466032 1001.40 1002.40 0.58
!=466033 1002.40 1003.20 0.15 1002.40 1008.00 4E 70% Is -typical 4E with 30-40% garnets 1-5mm in a All units are locally
vfg green amphibolite, -massive to weakly strained. cut by -10-15% bands
20% intervals of same f.g. biotitic metased as up to 1 Ocm of pale
above and -10% intervals of 4F with 30% f.g. staur. green amph-Cc +/-
minor Po. Scattered
intervals 10-15cm are
mod magnetic l::466034 1003.20 1004.00 0.03
l::466035 1004.00 1004.70 0.04
I
l::466036 1004.70 1005.50 0.04
I i • •
i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample ! From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
=466037 1005.50 1006.30 0.03 =466038 1006.30 1006.90 0.03 466039 1006.90 1008.00 0.03 466041 1008.00 1009.00 O.D1 1008.00 1016.40 4F Fairly typical 4F with -50% garnets 1-4mm in a f.g. LC sharp @ 45dac,
matrix of-75% bio, 25% Qtz>Fd and minor staur. UC also sharp but irreg.
Several intercalated 4E layers up to 30cm wide,
e.g. 1009.9-1010.3m. 1::466042 1009.00 1009.90 0.03 1::466043 1009.90 1010.30 0.12 1009.90 1 010.30 4E Not very deformed or min'd.
466044 1010.30 1011.00 0.04 l::466045 1011.00 1012.00 0.02
466046 1012.00 1013.00 0.05 466047 1013.00 1014.00 0.05 466048 1014.00 1015.40 0.13 466049 1015.40 1016.40 0.07
=466051 1016.40 1017.00 0.33 1016.40 1021.00 4E Well mineralized, highly qtz veined and deformed Fol'n/banding is very
4E. Generally- 5-10% e.g. garnets iff.g. dark erratic, often wavy and amphibolite. Laced with -25% thin, irreg qtz veins sub-parallel to CA. LC and 7-25% Po veinlets and blebs. into 4EA ia -sharp but
deformed. UC sharp at
45 dca. =466052 1017.00 1018.00 0.18 466053 1018.00 1018.60 0.13
1::466054 1018.60 1019.00 1.34 466055 1019.00 1020.00 0.63
466056 1020.00 1021.00 12.25 l::466057 1021.00 1021.70 0.15 1021.00 1022.50 4EA Relatively f.g 4EA, mod developed bands of Green amph layers are
massive gar-grun 1-10cm thick, gently folded at conformable with 4EA
low angle to CA. -5% dark green amph bands < but appear to replace it. 1-3mmwide.
1=466058 1021.70 1022.50 0.32 l::466059 1022.50 1023.00 0.02 1022.50 1024.00 4F Upper 50cm is -good 4F, followed by 40-50cm of
weak 4E and then an intermediate unit between 4F
and 6 composed of 10% e.g. ragged garnets in a
f.g. bio-qtz metased. ::466061 1023.00 1024.00 0.02
I i i I i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
1024.00 1026.20 6 Homogeneous, med grey f.g. metased composed Local biotite rich of -40-50% bio and 50-60% qtz-(Fd). Rare garnets, "streaks"/slivers up no staur. to 3mm x 20mm that
might have been shale
clasts?? or sheared
out pelitic layers. 466062 1025.20 1026.20 0.00 466063 1026.20 1027.20 0.19 1026.20 1027.20 4E Fresh sections are -typical 4E with -30% e.g. LC is M w w w
garnets in f.g. green amphibolite. -30% is grada!ional/interbanded overprinted by weak-mod bio-amph+/- silica alt'n. with the 4F below. Little or no Po.
=466064 1027.20 1028.00 0.06 1027.20 1030.70 4F Fairly typical 4F again with -50% garnets 2-5mm in LC sharp at 43 dca.
f.g. bio dominant matrix, -30% fg Qtz. 10% thin 4E
layers, 1-3cm and -5% qtz veins. 466065 1028.00 1029.00 0.18 466066 1029.00 1030.00 0.27
l::466067 1030.00 1030.70 0.03 l::466068 1030.70 1031.70 0.02 1030.70 1041.00 1 Serpentinized UM. Upper 2m is med green UM with This unit is prob the
local e.g. garnets, bio and amph due to meta'd peridotite hydration/metamorphism reactions, followed by bottom of a light grey speckled UM, with -30-40% f.g. white differentiated
talc? Grains down to 1041m. sill/dyke. LC is -
sharp into UM
amphibolite
(meta-pyroxenite?)
below. 1041.00 1042.50 1 Ultramafic Amphlbolite. Light-med green, -massive, Composed of >90%
presumably the upper, pyroxenitic part of the same light-med green, f.g. differentiated sill as the above 1 S. -acicular amph. LC is
bio'd for 40cm due to
hydration reactions
with adjacent schist.
=466069 1042.50 1043.50 0.03 ,1042.50 1046.70 4F 4F with -20-30% garnets 3-7mm, (-coarser then 5% irreg qtz veins and previous sections) in a biotite-rich matrix(-60%), 5% 4E layers <5cm.LC but more qtz-fd than before (-40%). sharp at 60 into UM
dyke? below. l::466071 1043.50 1044.50 0.12
I
~466072 1044.50 1045.50 0.50
I I I :
•
f.---·· Assay MAJOR UNIT MINOR UNIT ALTERATION
Sample From To AU ppm From To Unit Comments Comments From I To Unit Comments Bio Car Chi Gru Hem Ser Si Comments 466073 1045.50 1046.70 0.14 466074 1046.70 1047.70 0.03 1046.70 1051.30 1M Similar to base of previous UM, composed largely of Sharp, clean contacts
f.g. short acicluar green amph. LC highly bio'd for and the position in the
20cm. middle of this
meta-pelite interval
suggest this is a dyke
or sill, not a flow.
466075 1050.50 1051.30 0.02 s w M "466076 1051.30 1052.00 0.25 1051.30 1064.70 4F Typical 4F with -30-50% garnets (2-5mm), in f.g. 4F and 4E are
matrix of -60-70% bio, 30% Qtz-(Fd). Contains commonly folded into
-30% intercalated 4E and chertyfweak 4E layers up -open S-folds up to to 1 Ocm thick. 60cm wide between
limbs (This assumes
the core is oriented
properly using the S2
clavage as approx.
vertical) =466077 1052.00 1053.00 0.11 =466078 1053.00 1054.00 0.01 =466079 1054.00 1055.00 0.03 -466081 1055.00 1056.00 0.02
466082 1056.00 1057.00 0.02 ;:466083 1057.00 1058.00 0.01 =466084 1058.00 1059.00 0.01
466085 1059.00 1059.75 0.02
r::466086 1059.75 1060.75 0.33
466087 1060.75 1061.50 0.02 1P60.75 1 062.25 6 F.g. pelitic metased lnterbedded
with the 4F. Varies from -40-70%
f.g. biotite, rest mainly qtz>fd.
little or no garnets. ::466088 1061.50 1062.25 0.02 -466089 1062.25 1063.00 0.01 =466091 1063.00 1064.00 0.02 466092 1064.00 i 1064.70 -'" l
I I ·····~···· L I i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
466093 1064.70 1065.20 0.17 1064.70 1071.00 48 Thinly laminated elastic 48 with 25% gar-bio alt'n Only a few small 1064.70 068.00 48 J.E. Clastic48 with Str. M bands up to 15cm thick replacing the more elastic intervals of weak 4EA, Bio/garn alteration From layers. Non-alt'd areas have layers <6cm thick of <30cm and no signif 1065-1065.60 Foliation II to the thinly lam'd chert-Mt separated by 40% bands Po but alteration C.A. Then weakly folded, minor of f.g. green amph laminae with 20% garnets 1-5mm. banding is relatively quartz flooding between
strong 1067.3-1068 l:466094 1065.20 1066.00 0.03 w
466095 1066.00 1066.70 1.20 s ::466096 1066.70 1067.30 2.77
466097 1067.30 1068.00 0.05
l::466098 1068.00 1069.00 0.14 1068.00 1 071.00 48 Well laminated Clastic 48 with M w with 5% grunerite altration, and
moderately quartz flooded. relic
garnets are .5-1.5 cm in
diameter with grunerite halos =466099 1069.00 1070.00 0.12 1=466101 1070.00 1071.00 0.82 1=466102 1071.00 1072.00 1.65 1071.00 1075.00 4EA Well developed 4EA wrt silicates (massive bands of Relatively straight 1071.00 1 080.00 4EA Moderately developed 4EA
gar-grunerite 5-20cm thick) but no major alt'n, banding, some gradual laminated to open folded with a shearing or qtz flooding, garnets only m.g. reversals in core angle strong S2 fabric present @ 40
and a few small open -45 degrees to C.A. (3 well folds of uncertain developed between 1074-175) type. LC and UC are
gradational over -50cm. '::466103 1072.00 1073.00 0.04 w =466104 1073.00 1074.00 0.05 =466105 1074.00 1075.00 0.04
466106 1075.00 1076.00 0.03 1075.00 1079.95 48 Thinly laminated elastic 48 as before with -50cm wide qlz veined M w mod-strong gar-bio alt'n banding especially in upper shear starting at
1 m. Straight banded with only minor changes in 1077.2 with one fleck
orientation. VG and 2% Po. LC
deformed, sheared
and qtz veined for 20cm 466107 1076.00 1077.10 0.26
t':466108 1077.10 1077.80 5.68 =466109 1077.80 1078.80 0.07 =466111 1078.80 1079.30 0.10
-4661 0.42
::466 0.02 1079.95 1 Massive to weakly sheared f.g. green ultramafic
composed of >85% f.g.green, anhedral amph (?}
i i i •
i i i ; i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
466114 1082.30 1083.30 0.03 ~466115 1083.30 1084.00 1.70 1083.30 1095.80 48 Thinly laminated 48 with local minor elastic layers 3 small qtz flooded M w s
(vfg green amph rich +/- minor garnets) shear zones with <7%
throughout. Banding flips orientation a few times, Po at 1083.3-1084, several broad folds. 1085.8-1086.5,
1086.9-1087.9m. Cut
by another small UM
dyke at 1085.2-1085.8m 466116 1084.00 1084.50 0.55 w 466117 1084.50 1085.20 5.98 w s "Sil'n" is actuially 2
~466118 1085.20 1085.80 0.08 1~85.20 1 qtz veins, 20cm and 5cm
085.80 1 Massive UM dyke composed of
>90% f.g. med green equant
amph (?) grains. LC and UC
sharp and at high angle to
banding in BIF - UC at 90 to BIF. 466119 1085.80 1086.90 0.16 w w w
=466121 1086.90 1087.90 0.15 s s 466122 1087.90 1088.90 0.12
466123 1088.90 1090.00 0.01 466124 1090.00 1091.00 0.13
466125 1091.00 1092.00 0.02 =466126 1092.00 1093.00 0.02 M ~466127 1093.00 1094.00 0.05 466128 1094.00 1094.50 0.01
,...466129 1094.50 1095.25 1.35 M ~466131 1095.25 1095.80 0.59 ~466132 1095.80 1096.50 2.35 1095.80 1096.95 4A Strongly (-30%) qtz flooded 4A, locally borderline Dissem'd Po around w M s
4B. Composed of-40% f.g. grun layers <1-2cm, the qtz floods/veins, 50% chert layers <2-3cm, and -10% Mt layers <1cm. up to 5% over 40cm.
Last 6cm is
semi-massive Po vein. ;:466133 1096.50 1096.95 0.52 _466134 1096.95 1097.95 0.04 1096.95 1097.95 48 Straight banded, homog section of alternating Mt
layers <2cm thick and light yellow grun-chert layers
<1cm. 3-4 small gar-bio alt'n layers <1cm thick.
i i I i i I i I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments I Bio Car Chi Gru8ser SI Comments
l::466135 1097.95 1098.95 0.66 1097.95 1099.40 4A Chert dominant 4A with weak-mod, -diffuse pale Highly qtz veined M s "Sil'n" mainly veins. yellow grun layers, <1-2cm wide, <5% Mt laminae. from -15% alt'n bands 2-25cm wide of green amph-m.g. 1098-6-1098.95m with Cc+/- Qtz veins, often -brecciated. 7% Po.
l::455135 1098.95 1099.40 0.04 11)98.95 1 099.40 4C The ground mass of the unit is
strongly carbonatized there are
veinlets of sugary carbonate
3-1 O cm wide associate with a
light green alteration halo
epiodote??1099 .40-1099.90 =466137 1099.40 1100.40 2.32 1099.40 1100.40 4H Classic 4H. lnterbedded dark grey-black thin LC sharp at 42dca.
argillaceous layers, <5mm, and lesser cherty and
amphibolitic laminae. Contains 15-20% net-textured
f.g. Po and -10% gar-bio alt'n bands (<6mm). l::466138 1100.40 1100.90 0.03 1100.40 1108.50 1 Pale grey, -completely serpentinized UM, locally Generally -massive,
with 10-30% white anhedral grains <2mm which weak fol'n at best. LC may be talc. No amph or other mafics visible. -gradalional and
broken up. 466139 1100.90 1101.90 0.08
1108.50 1128.00 2 Moderately fol'd, med grey basalt. Composed of Unit has no green tinge
-40% green anhedral amph, 45% plag, 10-20% in spite of the amph, x-cutting bio grains/slips. but is not a 2T. No
major shear zones or
veins. LC gradational
into 2T over 1-2m. 1128.00 1146.70 2T Continuation of grey basalt above but now there is Matrix is light grey,
no visible green amph left, just 15-35% bio flakes not beige like much of
and slips cutting -amorphous light grey matrix. 2T in mine area, but
this is still pervasively
alt'd/strained. Bio
filled bands/slips
locally up to 1cm.
Small IF at
1131.2-1131.75m,
well min'd with Po. ::455141 1130.20 1131.20 0.01 466142 1131.20 1131.75 0.06 1131.20 1131.75 48 Upper 1/2 is -clear thinly
laminated 4B with minor green
amph layers. Lower 1/2 has
-35% Po, several gar-bio alt'n
I i I bands to 1 cm and 2-3 qtz veins.
I I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
466143 1131.75 1132.30 0.01
1146.70 1164.30 1 Serpentinised Ultramafic. Varies from pale green to 1160-1161.5m is cut
light grey In 2-4m zones but all appears to be type bu 35% brittle CC
of serpentinite. Serp varies from micaceous to veins 1-3cm at high -anhedral, amorphous textures. angles to CA. UC
diffuse over -20cm.
LC - bleached but
prob was sharp. -466144 1163.30 1164.30 0.01 =466145 1164.30 1165.00 0.03 1164.30 1168.00 48 Southern Iron Fm, laminated to thinly banded LC sharp. Banding is
chert-Mt BlF, no significant grun or other minerals. at high dca, -80, weak Quite straight banded with minor reversals wrt CA. 82 cleavage used to
Scattered qtz veins to 5cm and a few Po filled frax orient core. with Tr Cpy at -1167m.
=466146 1165.00 1165.50 0.01 =466147 1165.50 1166.50 0.01
-466148 1166.50 1167.40 0.02
t::466149 1167.40 1168.00 0.10
.... 466151 1168.00 1169.00 0.01 1168.00 1186.60 7A Upper and lower 3-6m is mod strained but rest is Tr dissem'd Po in
e.g., massive gabbro composed of -85% equant weak-mod sheared
dark green-black amph grains 2-4mm with -15% area at 1172 and interstitial f.g. plag. 1181.5m. Lower 60cm
is chilled margin.
~466155 1185.60 1186.60 0.01
l::466156 1186.60 1187.60 0.15 1186.60 1196.10 48 Classic Southern Iron Fm; thinly laminated LC and UC sharp.
alternating pale grey-white chert and black Mt Several scattered qtz laminaes -1-4mm thick. Very straight bandng, only veins up to 4cm with minor small folds or distortions. minor Po blebs but no
major shears or alt'n.
Rare 82 cleavage
planes, core oriented
mainly with banding
angle. :466157 1187.60 1188.40 0.02 ;.:466158 1188.40 1189.00 0.04 :::466159 1189.00 i 1189.40 1.75
i I i I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit • Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser SI Comments
~466161 1189.40 1190.40 0.01 466162 1190.40 1191.40 0.11
l::466163 1191.40 1192.20 0.07
l::466164 1192.20 1193.00 0.07 l::466165 1193.00 1194.00 O.Q1
:466166 1194.00 1195.00 0.21 466167 1195.00 1196.10 0.03
-466168 1196.10 1197.00 0.01 1196.10 1202.70 1 Light green, soft, locally friable serpentinite,
commonly strongly sheared. Posed almost entirely
of micaceous green serpentine, flakes up to 2mm.
LC somewhat sheared and qtz veined but seems to
grade into melanocratic gabbro below. 1202.70 1214.00 7A Homogeneous, med grey, -massive melanocratic UC and LC appear
gabbro composed of - 70-90% green-black equant gradational over
amph grains, 1-3mm, and 10-30% f.g. intertsitial plag -30-50cm into UM
serpentinite, probably
a differentiated sillfdyke. 1214.00 1216.40 1 Light grey-green, mod sheared UM serpentinite with
7% Cc veins (<2cm). More hetero than previous
units with mod lcal bio'n bands and variable % of
intertsital plag remaining; plag % decreases with
depth from -15% to <2%. :::466169 1215.40 1216.40 0,01 ::;:466171 1216.40 1217.00 0.01 1216.40 1225.00 48 Southern Iron Fm as above, almost identical. A few
minor parasitic folds and lower 1 m is borderline
4A. Lower 3m has 2 qtz veins 20-30cm wide with
mod strong green amph alt'n and Po veinsfblebs . .... 466172 1217.00 1218.00 0.07 ::466173 1218.00 1219.00 0.01 l;:466174 1219.00 1220.00 0.02 :466175 1220.00 1221.00 0.01
1::466176 1221.00 1222.00 0.02 ::466177 1222.00 1223.00 0.01
l::466178 1223.00 1223.80 0.02 ::466179 1223.80 1224.50 0.61 :466181 1224.50 1225.00 0.89
I I I i I i
. Assay MAJOR UNIT MINOR UNIT ALTERATION
! Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Biol car Chi Gru Hem Ser SI Comments ~466182 1225.00 1226.00 0.02 1225.00 1292.30 20 Generally a med green-grey, f.g., weakly fol'd to Quite homg, no major
massive, pillowed basalt, minor sections of shears, alt'n or qtz
mod-strong shear fol'n and mod bio'n but no real veins. Local x-cutting
2T. Pillow selvages up to 2cm wide, composed of chi veins to 1 cm and
f.g.- m.g green amph, only a few with garnets. local chi in the
selvages. LC diffuse
over 10cm. 1292.30 1292.80 2 Intensely bleached due to strong carbonate within s
the ground mass and amp and chlorite are present w M as small 2-3 cm blebs which are elongated II to the M foliation. An over of chlorite which is spotted looking. s M
1292.80 1304.80 2J Medium to coarse grained mafic volcanic with 45% Moderately fol'd, med M w plag and 40% green tabular amphibole. Close to an grey basalt. w fairly fresh mafic volcanic amphibolite. 10% X cutting calcite vienlets rimmed Composed of -40% UM with serpentine and with chlorite. green anhedral amph, talc
45% plag, 10-20% w massive mafic volcanic, x-cutting bio grains/slips no biotite slips
1304.80 1337.50 2D A medium grained grey-green massive pillowed There is an moderate
basalt with minor section of mod biotite alteration. shear between
Selvages have strong chlorite halos and are 1-3 cm 1316.60-1321.50 wide. Occassiona! garnets. consisting of moderate
carbonate x culling
vnlets and weak to
moderate chlorite may
be close to open
spaced fault ??Down
section localized areas
of strong calcite viening. 1337.50 1348.10 2 Fine grained mafic volcanic, weakly foliated and The lower contact is
green in colour. The unit consists of mainly f.g. gradational over 1m.
green amph and 10-15% f.g. fedspars. The unit is
fairly fresh, no biotite slips. The unit is cut by <1 % Qtz-Cc veins up to 1cm wide.
i
I •
i ; •
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si I Comments
1348.10 1350.20 1 UM? Unusual looking. The unit is pale in coulour, The unit displays
softer than previous unit. The matrix seems to have dismembered Qtz
f.g. greenish micaceous serpentine (becoming veins, almost a breccia
amorphous serpentine down section) and 3-5% f.g. looking in some talc. places. One big white
clast (or mineral)
10cm wide, too soft to
be qtz: maybe porphy.
talc or remnant plagio?. 1350.20 1359.60 2 Fairly massive mafic volcanic, green In colour. fine
grained unit. The unit is weakly foliated in some
places. No significant veining. The lower contact Is
sharp@40 dca. E:466183 1357.60 1358.60 0.00 l::466184 1358.60 1359.60 0.01 l::466185 1359.60 1360.30 0.01 1359.60 1361.00 88 Felsic intrustion Quartz Diorite?? Both the U.C and Locally brecciated and massive Qtz vein,
L.C are sharp like a quartz vein however, there is fractured with 5% f.g. white micas locally weak biolile and sericite alteration with several white micas. The unit
micro fractures and relic albitized sub-rounded displays <1 % Po In
phenocrysts. No remnant hosted rock. short veins. The lower
contact is sharp
@40dca. ~466186 1360.30 1361.00 0.02 l::466187 1361.00 1362.00 0.01 1361.00 1371.20 2 Weakly foliated mafic volcanic. Grading from fine The unit is cut by 1 % fairly fresh mafic volcani<
grained fairly massive basalt to darker unit with m.g Qtz-Cc veins up to
amph-pyroxenes and 5-10% interstitial feldspars 1 cm wide. The lower (almost looks like a gabbro). contact is gradational.
E:466188 1362.00 1363.00 0.00
1371.20 1394.00 2 Weakly foliated mafic volcanic, varies form fine Locally, the unit w chlorite alt'n? grained to medium grained. The unit consists off.g. contains a pale green w w M amph and feldspars mainly (relative % varies soft mineral w M w throughout). The amph are coarser grained and the overpinting the matrix M talc feldspars are interstitial, down section. and overprinted by a w M M
type pf amph: might be
chlorite (maybe too
deep to be chlorite,
retrograde
metamorphism? mod.
szbetween
1388.1-1389 strong
calcite vning
i I i ! i i i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From I To Unit Comments Comments From To i Unit Comments Bio Car Chi Gru Hem Ser Si Comments !
. 1394.00 1398.80 2 Fine to medium grained mafic volcaninc The U.C. is Down section of the
cut by 10 cm qtz/calcite vn greenish - grey in Qz vn the unit is
colour and fine grained to 1396.3. A 50 cm wide medium grained and
tz/carb vn is present with 5% sulphides, 2% Po, 3% 60% mafics an 40 % Py & 0.5% Cpy. feldspar with minor
carbonate vning.
minor mm scale
ptgmatic vning
between between
1398-1398.20 1398.80 1403.50 1 Serpentinite. Amorphous and featureless ultramafic
volcanic. Dark grey-blue in colour and very soft
weakly magnetic at the L.C. with moderate
carbonate viening . 1403.50 1418.70 2 Fine grained mafic volcanic dark green in colour There is a wek to
with overprinted chi. & biol alt. assocaited with 2 moderate shear
discrete shear zones(1409.60-1411.40) where the between
unit strongly distorted mod. sz. with 30% QzVCarb 1416.70-1418.40
veining and 7-10% Po concentrated in Qtz/carb vns. where the unit is less
distorted and Oz/Car
vns are 2-3 cm wide
with 2% Po. Minor UM
1418.4-1418.7m. E466189 1406.00 1407.00 0.00 E466191 1407.00 1408.00 O.D1 l::466192 1408.00 1409.00 0.00 l,:466193 1409.00 1409.60 0.00 E466194 1409.60 1410.70 O.D1 w s w M E466195 1410.70 1411.40 0.01 t:466196 1411.40 1412.30 0.00 w M w l::466197 1412.30 1413.00 0.00
1418.70 1422.90 2 Fine to medium grained mafic volcanic with 11418.40 1418.70 1S Minor Ultramafic at the lower w M w moderate carbonate veining and finger print swirling contract soft and greasy and w M bitotie rimming carb veininng. 55% mafic 35% weakly magnetic. M M M feldspar. M w
1422.90 1424.20 2 A bleached maflc volcanic which is fine grained
with tabular mafic phenocrysts 0.5-0.8 cm in
diameter and weak carbonate veining.
I I I i i I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To • AU ppm From To Unit I Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
1424.20 1467.70 2 Fine grained biotitic mafic volcanic with 3 SZ is present beteen moderate shear zones. -1-1.5 metre moderate sz. 1428.7-1431.90
45% feldspar. 45% mafics and 10% carbonate distorted mafic vning within shear zones that are sub II to the core volcanic with carb. axis. vning and overprinted
with bio. 50 cm Qtz/vn
@ 1433.50 illminate.
f.g with wk sz from
1443.20-1445.30
Mineralized sz from
1453.4-1454.1 3% Po
%2% Py.
466198 1428.00 1428.70 0.01 "466199 1428.70 1429.70 0.01 "466201 1429.70 1430.70 0.01 ::466202 1430.70 1431.20 0.01 ::466203 1431.20 1431.90 0.01 466204 1431.90 1432.90 0.01
=466205 1432.90 1433.70 0.04 466206 1433.70 1434.70 0.01
::466207 1450.00 1451.00 0.00 466208 1451.00 1452.00 0.01
=466209 1452.00 1452.70 0.01 =466211 1452.70 1453.40 0.00 466212 1453.40 1454.10 0.01 466213 1454.10 1455.00 0.01 466214 1455.00 1456.00 0.01
1467.70 1472.50 7A The U.C and L.C. are gradational and moderately The lower contract is w strained with a medium to coarse grained centre Intercalated with the w with equigranular dark green and black amphibole lower Ultramafics and w M and a light pinkish feldspar ground mass salt and pepper texture w M
gabbro. w M M
i i I I i
I Assay MAJOR UNIT MINOR UNIT ALTERATION .
Sample From To AU ppm From To Unit Comments Comments From To Unit• Comments Bio Car Chi Gru Hem Ser Si Comments 1472.50 1485.60 2 Fine to medium grained mafic volcanic with 1 % Almost looks like w s
carbonate vning 1-3 cm wide. There is a section spinifex texture. Laths
from 1474.3-1474.7, which is Intensely strained with of mafic are 3-4 cm long needle like actlnolite In a random orientation wide. Down section
there Is an increase in
Calcite vnlng. The unit
is greyish green in
colour. 1485.60 1488.30 7A Weakly magnetic igneous intrusion. Gabbro is a
medium to coarse grained dense unit. Consisting of
translucent plagioclase, amphibole and pyroxene.
The unit is igneous textured. Fractures have intense
slickenslides. 1488.30 1511.30 2 Fine to medium grained biolitic mafic with weak
carbonate vning eiand several sections with 1-2 cm
wide biotite slips.
1511.30 1512.80 BA Massive looking Diorite with well foliated mafic micro fractures appear
minerals laths and tabular dark amphibole. There is to have sericite. Lime a wispy fracture fabric that is II to the folitation. green to yellow.
Intercalated with lower
ultramafic unit
between
1512.60-1512.80. 1512.80 1521.70 7F Again an igneous intrusive with translusent
plagioclase and a salt&pepper texture. The unit is
dense and moderately magnetic. There appears to
be minor amounts of magnetite. 1521.70 1523.10 1 Ullramafic Amphibolite. F.g massive dark green 0.5-2% very f.g
rock consisting of a fine matrix of 100% green disseminated Cpy Asp
amph. 10% blebs and irregular veins, 1-3cm off.g and Po.
very white hard mineral (dol/ank/magnesite?),
seems too white to be qtz. {Did not fizz). E:466215 1522.00 1523.00 0.00
1523.10 1527.80 1 UltramaficAmphibolite. -100% massive green Up to 15% Plag in !
amphibole matrix with 2% scattered 1-3mm Cc 30cm section around stringers. Variable grainsize but same mineralogy 1526.7m. throughout. C.g (1-2mm: UC-1524.5m). M.g.
1524.5-1525m, f.g 1525m-LC.
•
I I I i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From I To Unit Comments Comments Fr 0 Unit Comments Bio Car Chi Gru Hem Ser Si Comments I
•
1527.80 1530.60 1 Ultramafic Amphibolite. Massive c.g dark green
rock consisting of -100% equigranular amphibole
1-2mm from UC to 1530m. 1530-LC is moderately
foliated with 30% biotite, 70% green amph; this may
be due to contact with pegmatite at LC. 1530.60 1533.10 8F Granitic pegmatite consisting of -25% qtz crystals 4% elongate, light
(1-8mm) and 5% small (3-7mm) qtz veinlets, 3% green-white
black tantalum (JB), 63% f.g white feldspar matrix. phenocrysts 3-10mm
No blolite. Non-foliated. Sharp contacts. of unknown soft
mineral, could be
alteration of
feldspar. Chilled 1cm
margins consisting of
100% feldspar. 1533.10 1535.80 1 Ultramafic Amphibolite. Massive, equigranular Two 1.5cm hard, white
igneous textured rock consisting of 92% green barite-like veins with amphibole crystals (1-3mm), 5% plag (<1mm), and no fizz. One Qtz-fsp
patchy f.g disseminated sulphides. Probably vein 5mm.
recrystallised pyroxenite. -466216 1534.50 1535.50 0.01
1535.80 1537.30 1 Ultramafic Amphibolite. Moderately foliated medium 25% med-c.g biolite In
to fine grained green rock with matrix consisting lower 40cm probably
of 85% dark green amphibole & 15% f.g Cc. UC is due to pegmatite
a 2cm qtz-fsp pegmalite offshoot. intrusive below. Cc In
foliated rock may be
due to weak shear. 1537.30 1538.80 8F Exactly the same as previous 8F, but with only -1 %
tantalum crystals. 1538.80 1543.20 1 Ultramafic Amphibollte. Massive, equigranular
igneous textured rock consisting -99% green
amphibole crystals (1-3mm), & -1% aspy (UC-
-1542m). Also, 0.2% cpy, 0.3% Po, as very fine
desseminated grains throughout unit. 466217 1541.00 1542.00 0.01
. •
i i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit ! Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
1543.20 1549.80 1 Dark green m.g rock with a mottled core-parallel ' Broken core ends have
fabric defined by wavy 1-3cm small folds in 1-5mm the typical ultramafic
wispy laminations of dark green amphibole granular texture.
(50-60%), lighter green amph (20-40%) & Small patches of weak
semi-translucent greyish mineral ranging 10-40%- serpentisation
interpreted as olivine. between
1544-1548m.
Desseminated f.g
sulphides -0.7% Asp,
plus lesser cpy & Po. _466218 1547.00 1548.00 0.01
1549.80 1552.40 2 Very fine grained matrix consisting of -87% dark Upper contact is w M green amphibole and -10% f.g feldspar. -3% small gradational with upper
scattered wisps of Cc (1-3mm). No sulphides. 30cm have same wavy
Weak planar foliation in centre of unit. fabric as previous unit
but with no "olivine". 1552.40 1600.70 1 Ullramafic Amphibolite. Fairly homog unit consisting Very f.g sulphides
of 70-98% dark & light green amph. [-60% light throughout unit, most
green I 40% dk green amph]. 70% displays a seem to be cpy and
mottled texture containing -20-30% very f.g 0.2-1% abundance.
interstitial Cc, and -10% irregular Cc stringers & Weak planar fabric in
blebs. <1m patches, most
has a distorted fabric
with weak 82. No
significant fsp visible. 466219 1566.00 1567.00 0.01
466221 1576.50 1577.50 0.00
1600.70 1605.10 1 Ultramafic Amphibolile. Equigranular, massive light The U.C is sharp with w M green amphibole with a mottled (texture minor an irregular L.C. w M sections are magnetic). Cc stringers 1 to 2cm wide. M Consists of 80% dark green amph. and scattered M wispy Cc veins.
1605.10 1617.50 2 Fine to medium grained mafic volcanic with
15-20% Cc veining with biotite slips present. Unit
is weakly distorted and weakly sheared. Light
green amphibole.
1617.50 1620.00 2 Medium to coarse grained flow. Weakly foliated
with minor CC veining.
I
!
I i I I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
1620.00 1643.00 2 The upper contact is brittle faulted. Down section The unit is medium the unit is med. to fine grained. A wedge is present grained with patchy
at 1623.50 where 1.5 m of core had been ground. section between
Mod. fol. Cc stringers from .5 to 2 cm in width. Fr. 1637-1643 .25-1% Po 1630.8 to 1634.10 f.g. with strong bio. alt'n. associated with Quartz
carbonate veining.
Weak shear zone
between
1639.40-1643. 85%
green amph. and 5%
biotite alteration and
1=466222 1636.00 1637.00 10% Cc vning.
0.01 -466223 1637.00 1638.00 0.01 M t:466224 1638.00 1639.00 0.01 466225 1639.00 1640.00 0.01 466226 1640.00 1640.55 0.01
1=466227 1640.55 1641.10 0.01 466228 1641.10 1642.00 0.02 466229 1642.00 1643.00 0.01 466231 1643.00 1644.00 0.02 1643.00 1657.40 2 Moderately fol'd, med grey basalt. Composed of Both the Upper and
50% green anhedral amph, 45% plag, and 5% X lower contracts are cutting Cc veining . gradational.
1657.40 1662.10 1 Ultramafic Amphibolite. Dark green m.g rock with Trace sulphides M a mottled texture. Faint wispy wavy folds exist thought out the unit. between 1661-1662m and are 2-3 cm wide. Wispy
dark green amphlbole (55%) with a lighter green
amph (15%) 1662.10 1682.00 2 Fine to medium grained mafic volcaninc with 55% Intensely bleached due
amp and 40% plag. 5% Cc veining. Bleached to strong carbonate
section has more Cc and from 1670.80. 10-15% Cc within the ground veinlets 1-3 cm wide. mass and light green
amp. Po and Aspy is
disseminated. There
is a moderate chlorite
overprint between
1665.9-1670.8 "466232 1665.00 1665.90 0.02 "466233 1665.90 1666.90 0.01 s w ::466234 1666.90 1667.90 0.01
'Jt"" .... """ ... 1667.90 1668.90 0.01
I I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To ' Unit Comments Bio Car Chi Gru Hem Ser Si Comments
466236 1668.90 1669.90 O.D1 ::466237 1669.90 1670.80 0.01 l':466238 1670.80 1671.80 0.01 M
1682.00 1689.90 1 Ultramafic Amphibolite. Medium to coarse grained
ultramafic with a mottled texture and composed of
75% dark green and light green amphibole. E:466239 1688.00 1689.00 0.01 E:466241 1689.00 1689.90 0.02 t:466242 1689.90 1690.90 0.01 1689.90 1697.60 2T Fine to medium grained mafic volcanic. The upper The shearing is
section from 1689.9-1693.80m is sheared and moderate with strong
strong Cc veining up to 20%. Down section of the amph. alteration. From unit is light brown. 1693.8-1697.60 is light
brown 2T. t:466243 1690.90 1691.90 0.01
l':.466244 1691.90 1692.80 0.02 E:466245 1692.80 1693.30 0.01
E:466246 1693.30 1694.00 0.01 s w l::466247 1694.00 1695.00 0.02
1697.60 1727.00 2 The unit is a medium grained mafic volcanic with have a sepentinized M localized sections of 1-2% diss. sulphides and greasy feel. With M minor chalco associated with Cc vning. The unit minor intercalated consists of 70% dark green amph and 15% Cc ultramafics between
vning ranging btw .5 to 2 cm with some fracture 1715-1721m planes
1727.00 1729.40 2 Same as above. Borderline 2-1 M weakly foliated The sulphides are to massive mafic consisting of 88% m.g darkish often more
amphibole, 1-3% disseminated sulphides and -7% concentrated around irregular Cc veinlets and minor patchy the Cc veinlets. desseminated Cc.
1729.40 1746.00 1 Ultramafic Amphibolite. M.g.-f.g. matrix of 3cm wide plag-qtz amphibole, often granular looking, with -1-4% pegmatite at
m.g.-c.g. Cc irregular veinlets (<1cm). Moderate 1731.9m. Undulating
foliation in places. Several sections with very weak SO amphibole high m.g dissem'd Po: 1734.2-1735.4m, layering 2-5mm scale
1740-1740.4, 1745.2-1745.4m visible
fr.17 42.6-17 43m. No
biotite or serp alt'n.
Common equigranular
1-2mm cumulate texture t:466248 1733.50 1734.20 0.01 E:466249 11734.20 11734.80 i 0.01
i
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To ! Unit Comments Bio Car Chi Gru Hem Ser Si Comments
E466251 1734.80 1735.40 0.02 :::466252 1735.40 1736.00 0.01
t:466253 1739.00 1740.00 O.Q1
l:466254 1740.00 1740.40 0.01 ;::466255 1740.40 1741.00 O.D1
~466256 i743.00 1744.00 0.01 ~466257 1744.00 1745.00 0.04 l:466258 1745.00 1746.00 0.01 E466259 1746.00 1747.10 0.01 1746.00 1747.10 2 Sheared, well foliated amphibolilic rock with
10-15% disseminated and coarse Po throughout
the m.g matrix. 5-10% biotite. l:466261 1747.10 1748.00 0.01 1747.10 1757.80 1 Ultramafic Amphibolite. Massive, non to weakly
foliated unit. Consists of -98% amphibole, 2% Cc
stringers, equigranular texture. -0.5% fine
disseminated Po. l:466262 1748.00 1749.00 0.01
i':466263 1756.00 1757.00 0.01 :::466264 1757.00 1757.80 0.02 :::466265 1757.80 1758.70 0.02 1757.80 1764.30 2 Upper 90cm contains 40% thick Cc veining and Rest of unit is w s s
25% qtz veins amongst thin bands and wisps of amphibollte with
mafic host rock No mineralisation. increasing fabric
development and grey
colour towards LC.
Weakly gradalional
LC. 5% Cc veinlets.
-1 % f.g disseminated
Po. E466266 1758.70 1759.70 0.10
E:466267 1759.70 1760.70 0.01 mod grey bleaching of
green amphibole 1764.30 1768.40 2A Medium to coarse grained mafic volcanic with w M
strong salt and pepper texture 55% plagiclose and M M 40% mafic with 5% anhedral green amphibole.
Minor disseminated sulphide (-1%). The unit grades
into a medium grained flow along the L.C.
• i i i . I :
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments I Comments From I To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
1768.40 1782.90 2D Medium grained pillowed flow. Selvages consist of Massive looking from
biotite and garnets with trace sulphides. They are 1779-1782m.
cuspate and range in width from 0.5 to 5 cm wide. Generally 3-7 selvages
Garnets are euhedral. Minor hyaloclastite present per metre. There are between 1771.5-1772.20m. minor biotite slips and
strong green
amphibole present
around the rims of
pillowed selvages.
Qtz/Cc vnining is II to
a weak to moderate
foliation. f::466268 1782.00 1782.90 0.02 1=466269 1782.90 1783.80 0.02 1782.90 1797.00 2A Fine to medium grained mafic volcanic. The U.C. of Between M M
the unit is strongly sheared and strongly bleached 1794.20-1795.6m there
from 1782.90-1783.80m. -Strong biotite, green is another bleached
amphibole alteration with Cc minor calcite veining. section of mafic
Down hole there is an increase In blotite. volcanics associated
with Cc veining and
strong green
amphibole alteration.
Ptygmatic veining on
mm scale between
1796.5. Intense Cc
veining between
1797-1806 with strong
green amph f::466271 1783.80 1784.80 0.02
f::466272 1784.80 1785.80 0.01
1797.00 1816.50 2 M.g. mafic volcanic with massive calcite veins
between 1801.50-1804.Sm and 1811-1816.50m. In
these two sections, 75-86% calcite. From
1804.50-1811 m the unit has a mottled texture with
light green amphibole alteration. No visible
sulphides present S466273 1801.00 1802.00 0.01 s f::466274 1802.00 1803.00 0.01 !
1=466275 1803.00 1804.00 0.03
1=466276 1804.00 1805.00 0.03
l::466277 1805.00 1806.00 0.04
l::466278 1806.00 1807.00 0.03
I I I I
• Assay MAJOR UNIT MINOR UNIT ALTERATION
Sample From To AU ppm From To Unit Comments Comments From To Unit i Comments Bio Car Chi Gru He SI Comments -466279 1807.00 1808.00 0.01 t:466281 1808.00 1809.00 0.01
t:466282 1809.00 1810.00 0.02 l::466283 1810.00 1811.00 0.04
-466284 1811.00 1812.00 0.02 s M 466285 1812.00 1813.00 0.01
._466286 1813.00 1814.00 0.05 466287 1814.00 1815.00 0.01 1~14.40 1 818.60 4E Weak 4E with strong light green
arnphibole alteration and
moderate garnet alteration t:466288 1815.00 1816.00 0.14
466289 1816.00 1816.50 0.01 =466291 1816.50 1817.50 0.01 1816.50 1820.90 2 Fine to medium grained biotitic mafic basalt with M
moderate green arnphibole alteration and a minor
weak 4E btw 1818.4-1818.SOm. The unit consists
of several biotite slips (1-3 cm wide) with some
consisting of weak garnet alteration. 1820.90 1831.50 20 Fresh looking pillowed basalt with selvages Small mm scale calcite s
between 2-4 cm wide trending between 20 to 50 veinlets (20 -30 per M M M degrees TCA. Selvages consist of moderate biotite metre). A 20cm calcite w /garnet alteration and are rimmed with green vein is present at the M M amphibole. LC .. w M
1831.50 1842.00 2 Fine grained mafic volcanic with the first 0. 70m M amph bleaching having strong biotite slips. The unit is 45% plag and M M 55% mafic. Again, mm scale calcite veining (20 - 30 M s s per metre) are all trending the same direction as the w M foliation. M s M
1842.00 1886.10 2 M.g green-grey mafic wlth fabric ranging from poorly Most of unit is fresh w w weak only patchy Bio to well foliated. Most of the unit is well foliated. with non to very little and Car 15-20% f.g biotite in matrix from 1855-1859m. bio!ite. Strong shear
Scattered Cc veins (5-20mm). Several bands of fr. 1845.5-1856.im,
grey bleached sheared amphibolite. containing two 13cm
qtz veins with one
containing pink fsp
and brown vug
suggesting Pegmalite
related.
I I I i I I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From ! To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
1886.10 1887.10 2 Unusual mafic unit with planar fabric. The unit Between these
consists of semi planar partially dismembered irregular bands/wisps
bands, 0.5-3cm of f.g grey-green amph with light is m.g green amph
greenish amph along the -3mm wispy margins. with minor biotite
alt'n, where bio is
stronger there are
gnts (1-3mm). No Po. 1887.10 1911.70 2 Green grey mostly fresh amphibolite of 25% f.g Scattered throughout
plag, 75% amph matrix. 5-10% of the rock is the unit are distorted
numerous thin 1-5mm irregular Cc stringers. fragments & elongate
Irregular wisps (1-5cm)
of f.g dk green amph
(4E type amph)
containing -15% gnts
(1-6mm) with -5%
bio. No significant
pervasive Biot'n
overall- only that
assoc'd with the
gnt-amph patches. 1911.70 1917.20 2 Light grey, bleached, moderately to well foliated, 1 %
irregular Cc stringers. Most foliated In lower 2m.
Minor bio'n in some patches, 3% overall.
1917.20 1921.20 2 Well foliated green grey amphibolite with -10% Small patches of dk
intense bio alt'n as discrete irregular wisps and green amph as before,
slips 3-10mm wide. 5% Cc stringers and pervasive but without the gnts.
Cc alt'n 5mm from veinlets. The bio alt'n is not very
pervasive.
1921.20 1922.40 QTZ Large Cc-qtz vein consisting of a mixture of qtz and 15% of the rock is
Cc roughly 50-50 with massive Cc being irregular, moderately
concentrated within 40cm of the vein margins. Qtz aligned sheared
mostly in centre of vein. fragments of
amphibolitic host
rock. These fragments
of moderately biotised
and often contain
moderate amounts of
Asp and Po on broken
surfaces.
i i I I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
1922.40 1934.00 2 Moderately to well foliated green grey amphibolite 1925.4-1928m is
with 10% pervasive Cc vein lets and alt'n. Scattered mod-str sheared mafic
(-2%) irregular folded bands of dark green m.g with pervasive Cc alt'n amph with bio. and silicifcation with
mod biotite alt'n.
Still inlcudes 15-25%
green amphibole. 1934.00 1936.30 1 Ultramafic Amphibolite. Massive coarse grained Could be gabbroic as It
(1-5mm g.s} amphlboles, moderate foliation in looks like there might
patches. Generally massive with crystalline texture. be -5% f.g plag with
95% amphiboles. l::466292 1936.30 1937.40 0.01 1936.30 1939.40 2 Well foliated grey green f.g mafic with 15% patches M w
1-30cm of moderate biotile ait'n associated with
weak shearing. These biotised sheared patches
have 1-5% Po within them. =466293 1937.40 1938.40 0.01 =466294 1938.40 1939.40 0.01 ::466295 1939.40 1939.80 0.01 1939.40 1939.80 2T Well foliated sheared mafic with intense Overall composition s s
silicification and strong biotite al'tn. 5% Po, and a 40% biotite, 55% qtz, couple qtz veins 1-2cm wide. 5% Po. Could have
some minor fsp or
some minor bleached
amph in there
somewhere. ::466296 1939.80 1940.70 0.03 1939.80 1945.00 2 Same as previous 2. Well foliated green grey mafic 1940.7-1941.3m is a
unit. Amphibole matrix is greyer that the usual 2 weakly sheared green
and has dark amph alt'n halos around thin Cc mafic with patchy stringers in places. pervasive Cc alt'n and
7% Po. Po is
desseminated and
forms blebs up to
15mm. 0.2% in rest of
unit. 1 Ocm qtz veined
band at 1943.4
containing 12% Asp
and 5% Po. Qtz veining
in lower 30cm. 2466297 1940.70 1941.30 0.03 w w :466298 1941.30 1942.00 0.02 w ;::466299 1942.00 1943.00 0.01
I ~466301 11943.00 • 1944.00 0.10
I I I
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit ! Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
-466302 1944.00 1944.60 0.02 466303 1944.60 1945.00 0.01 466304 1945.00 1945.90 0.06 1945.00 1948.20 2T Strongly sheared mafic with strong biotisation, The rest is generally s w s
silicification and mod Cc alt'n. The upper 40cm is well foliated
distorted and turbulent with swirls of biot alt'n, biotite+qtz+f.g+Cc+Po
green amph and qtz veins. Overall mineralogy 20% with strong Po min'zn
green amph, 30% biotite, 30% qtz, 10% Po, 10% Cc. increasing towards LC
where it's -18%. Po
is both finely
desseminated and
coarse and blebby.
Massive white qtz vein
1945.9-1946.5m with
15% min'zd host rock
enclaves. No vg. :466305 1945.90 1946.50 0.02 1S45.90 1 946.50 QTZ Massive while qtz vein with 15% s
wisps of min'zd host rock. l::466306 1946.50 1947.00 0.04 s M s ::466307 1947.00 1947.60 0.05 ;:466308 1947.60 1948.20 0.02 :466309 1948.20 1949.00 0.01 1948.20 1950.30 1 Ultramafic Amphibolite. Fine grained homogeneous 30cm section
light green fresh rx with fine to m.g granular and 1949.7-1950m is acicular amphibole texture on core ends. The unit moderately silicified
has the classic fresh ultramafic texture. Unusually with patchy Cc alt'n sharp upper contact. and -25% biotite al'tn;
inward pointing fol'n
suggests this could be
::466311 1949.00 1949.70 a fold hinge.
0.01 l::466312 1949.70 1950.30 0.01 M M M
w M l::466313 1950.30 1950.80 0.07 1950.30 1950.80 4H Typical Po-rich dark grey to black 4H with a local s w s
overprint of pale green f.g. amph-Cc alt'n. -25% Po
stringers, laminae, & blebs in an argillic matrix.
-25% brecciated qtz vein frags <2cm . . :466314 1950.80 1951.40 0.01 1950.80 1956.00 1 Ultramafic Amphibolite. Composed largely of -fresh
f.g. green amph, little serp'n or talc visible.
Cross-cut by -10% discrete bio'd shear bands up to
1-2cm wide.
I I i
LITHOLOGY LOG 07-NSD-008 Page 39 of 4t
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
1956.00 1959.60 2 Generally fresh , weakly fol 'd basalt becoming mod Composed of f.g .
sheared in lower 1 m approaching the 4H below. relatively fresh green
-1 % thin Cc vein lets, little or no bio alt'n. amph and lesser Fd.
Probably a high-Mg
variety of basalt. Lower
contact is strained
over 1 m and hard to
be precise. :::455315 1958.60 1959.60 0.01
~466316 1959.60 1960.40 0.09 1959.60 1961.50 4H Another classic 4H with -25-35% f .g. Po as irreg Lower 85cm has - 15%
network, blebs, minor veins to 2cm, and sheared, dismembered qtz vein
distorted laminae -all in a dark grey-black argillite frags <1 cm across.
matrix. Trace Cp. Minor unit
of 4A from
1960.4-1960.8m,
same as following unit. 466317 1960.40 1960.80 0.07 11360.40 1 960.80 4A lrreg distorted 4A, Most grun has M M
been replaced by green
actinolite with fg assoc'd Cc and
- 2% Po. Mod-strong qtz
flooding/veins. =466318 1960.80 1961 .65 0.03 1961 .50 1975.50 4A Fresh sections are thinly banded white to grey chert Below - 1966.5m the
with variable amount, 5-20 %, of dissem'd Mt, and O unit becomes more
to >50% f.g. acicular yellow grunerite, giving an distorted with
overall thinly striped grey-yellow-white look. Only a moderate qtz flood ing
few minor, unreliable parasitic folds. & veining, local Cc
veins to 20cm, and up
to 40% irreg
veins/patches to 6cm of
f.g. actinolite +/-
2-5% Po & Tr Asp
replacement. LC
marked by 1 Ocm of 4H. ~466319 1961 .65 1962.30 0.04 w w
466321 1962.30 1963.00 0.01
466322 1963.00 1964.00 0.01
466323 1964.00 1965.00 0.01
466324 1965.00 1966.00 0.01
=466325 1966.00 1967.00 0.03 Local Cc veins, much
more distorted than
above 4A.
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit i Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
l::466326 1967.00 1968.00 0.06
E:466327 1968.00 1969.00 0.05
::466328 1969.00 1970.00 0.01
466329 1970.00 1971.00 0.04 ::466331 1971.00 1972.00 0.04 w M ::466332 1972.00 1973.00 0.05 E:466333 1973.00 1973.50 0.02
466334 1973.50 1974.50 0.10
466335 1974.50 1975.50 0.09 =466336 1975.50 1976.50 0.01 1975.50 2009.20 2 Relatively fresh, unaltered basalt with -3-5% Composed of -60%
scattered Cc veins <1cm. No significant bio'n, qtz f.g. -fresh looking
veins or shears. Overall, has a weak fol'n with green amph, rest
local, minor weak shears, becoming mod-strongly presumably plag. LC is
sheared and bio'd in lower 2m nearing contact with sheared and possibly 4H. grada!ional from mafic
vole luff (?) into the
4H over 40cm.
M
E:466337 2008.20 2009.20 0.00 ::466338 2009.20 2010.00 0.02 2009.20 2011.70 4H From UC to 2011.1 it is a weak 4H, prob mixed From 20111.1-2011. 7m M
with mafic luff and then overprinted by mod-strong is well developed
Cc-pale green amph-(Po) alt'n, only -2% Po but black, Po-rich 4H with
matrix is often black argillite in thin, sheared out -20% Po. Followed by
streaks. a prob mix of 4H-tuff. l':466339 2010.00 2011.10 0.01 ::466341 2011.10 2011.70 0.01
l:466342 2011.70 2012.40 0.01 2011.70 2013.70 4H Po-poor type of mixed 4H with mafic vole tuff, only Still has a strong,
-2-3% Po but matrix is streaky banded from black diffuse overprint of
argillite slivers to more common mod-strongly bio'd f.g. Cc-green amph-(Po) maficvolc.
!:466343 2012.40 2013.20 0.02
~466344 2013.20 2013.70 0.01 !
I I I I I i I I I -
LITHOLOGY LOG 07-NSD-008 Page 41 of 4}
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser SI Comments
466345 2013.70 2014.50 0.01 2013.70 2014.50 2T Light brown, well fol'd, varies from f.g. M w homogeneous 2T to banded highly bio'd bands up
to 2cm separated by off-white bands of fg
Cc-(amph) replacement. 466346 2014.50 2015.00 0.00 2014.50 2022.45 7A Unit has 1-2m wide f.g. margins that look like
hi-Mg basalts (composed of -acicular green amph
with only minor visible plag). These grade quickly
into core section of - massive gabbro with -80-90%
stubby amph grains 1-3mm in f.g. groundmass of
plag-amph.
466347 2021.45 2022.45 0.00 466348 2022.45 2022.85 0.06 2022.45 2022.85 4H Typical black, Po-rich argillite type of 4H with
-25-30% net-textured and laminae Po.Sharp
contact with 4A facies below 466349 2022.85 2024.00 0.16 2022.85 2025.40 4A Mod magnetic, thinly banded chert-grun 4A with - 10% alt'n bands up to w Con'c in a few bands
<5-10% Mt laminae -2-4mm wide. Grun bands are 2cm wide and II to <2-3cm wide with relatively thin, usually < few mm. fol'n, composed of minor Po.
m.g. green amph with
minor Cc and 2%
dissem'd po. From
2024.6-2025m is irreg
folding cut by 3-4 Asp
veinlets -2-5mm wide
with minor Po. 466351 2024.00 2024.60 0.09
!=466352 2024.60 2025.00 0.07 l::455353 2025.00 2025.40 0.00
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit Comments Comments From To ! Unit! Comments Bio Car Chi Gru Hem Ser Si Comments
E:466354 2025.40 2026.00 0.02 2025.40 2044.60 48 Southern Iron Formation SIF 48, thinly laminated Moderate folding with alternating layers of black Mt and off-white to though out the unit- cm
pale yellow fg grunerite with minor chert A to deci S folds and M
greater% of grunerite than anything. -75% folds between 2033 to
Grunerite, -15% chert and 10% magnetite. 2035m. The lower 2
metres has a foliation
which tends to flip flop
from O to 180 degrees
with a foliation
parallel to the Core
Axis. Last 10 cm has
7%Po. t:466355 2026.00 2027.00 0.00
E:466356 2027.00 2027.60 0.00 t::466357 2027.60 2028.00 0.01 s Flanks it\rreg qtz vein
for 2-4cm. E:466358 2028.00 2028.80 0.00 w s E:466359 2028.80 2029.50 0.01
E:466361 2029.50 2030.00 0.01
E:466362 2030.00 2031.00 0.04
E:466363 2031.00 2031.60 0.02
E466364 2031.60 2032.40 0.08 1::466365 2032.40 2033.40 0.84 =466366 2033.40 2034.00 0.02
l::466367 2034.00 2035.00 0.04
E:466368 2035.00 2036.00 0.25
E:466369 2036.00 2037.00 O.o1 E:466371 2037.00 2038.00 0.01 1::466372 2038.00 2039.00 0.09
=466373 2039.00 2040.00 0.11
"'466374 2040.00 2041.00 0.04
466375 2041.00 2042.00 0.05 t:466376 2042.00 2043.00 0.03
l::466377 2043.00 2044.00 0.00
E:466378 2044.00 2044.60 0.02
i i
•
i
•
i i
•
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample ! From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
;:,455379 2044.60 2045.60 0.01 2044.60 2089.00 1 Amorphous looking with minor phenocrysts of green The unit is massive w w Talc and sepentine very amphibole. The first 2 metres are intercalated with with 2-3% sub anhedral soft unit minor mafic volcanics. However downhole there is a light green amphibole.
strong increase in sepentine and talc along From 2069 to 2081m, fractured surfaces. the unit is buff
coloured due to an
increase in talc and
carboante. A minor
open spaced fault
between 2058-2058.6m. =466381 2045.60 2046.60 0.01
466382 2059.00 2060.00 0.01
466383 2060.00 2061.00 0.01 466384 2061.00 2062.00 0.01
=466385 2062.00 2063.00 0.00
12089.00 2091.10 7H Course grained intrusive with porphyritic texture w M where strong green amphibole is present in a M w anhedral lo subhedral form. The unit has up to 30%
green amphibole.
2091.10 2132.00 1 Ultramafic Amphibolite. F.g. to m.g. UM with minor 2 and minor carbonate
intercalated mafic volcanic- 2098-2101 section with within the ground
mod bio. alt. . However, green amph is pervasive & mass. 2117 to 2132m
fractures are serpentintized. there is intercalated
volcanics with 40%
plag and 50% mafic
with 10% green amph. 2132.00 2157.50 2 Fine to medium grained biotmc mafic volcanic with From 2147 to 2152m,
40% feldspar and 45% mafic minerals; there is a calcite veining is
decrease in green amphibole alteration and an associated with rare
increase in biotite laths. Calcite stringers 1 to 3 cm grains of Po and Cpy
wide are also present. mineralization -466386 2146.00 2147.00 0.00
-466387 2147.00 2148.00 0.00 _466388 2148.00 2149.00 0.00
=466389 2149.00 2150.00 0.00
=466391 2150.00 2151.00 0.01
-466392 2151.00 2152.00 0.00
-466393 2152.00 2153.00 0.00
-466394 2153.00 2154.00 0.01
I 466395 2154.00 2155.00 0.00
I I I
•
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample I From To AU ppm From To Unit Comments Comments From To Unit Comments Bio Car Chi Gru Hem Ser Si Comments
2157.50 2167.05 1 Serpentinised Ultramafic. Light-med grey-green UM From 2160.3m to composed largely of fg serpentine, only minor light 2162.m there are 3-4 green f.g. amphibolite sections. Upper 4m is highly carb-qtz veins up to
fractured along a -1-3mm thick Joint set lined with 5cm. serp-carb
;::466396 2160.30 2161.00 0.00 ;:466397 2161.00 2161.70 0.01 _466398 2161.70 2162.50 0.17
..,.466399 2166.05 2167.05 0.05 "466401 2167.05 2168.00 1.62 2167.05 2172.60 4B Unusual type of green-black SIF 4B, similar to that Unit has discrete to
in parts of Trench 5. Composed of -50-60% f.g. Mt diffuse bands <10cm and 40-50% light yellow-green amph. Banding is thick with 30-100% Mt lrreg contorted throughout. plus broad zones of
disseminated Mt in the
amph matrix. Avg
5-10% Po in first 1.8m
as veins and networks. 466402 2168.00 2168.90 0.32
::466403 2168.90 2169.40 0.14 -466404 2169.40 2169.70 8.47 ::466405 2169.70 2170.50 0.52 =466406 2170.50 2171. 10 0.33 466407 2171.10 2172.00 0.06
::466408 2172.00 2172.60 0.01
2172.60 2173.40 13 Typical "klmberlite" (olivine lamprophyre) for here,
composed largely of oval serp'd olivine grains up
to 5mm, black to med green, with -20% phlogopite
flakes (3-4mm), and minor Cc In matrix. Mod
magnetic. No visible garnets or diopside. ~466409 2173.40 2174.00 0.29 2173.40 2181.70 1 Unusual Serpentinised Ultramafic. Most is Unit is locally rich in
-massive, light green serp'd UM but several Po, up to 30-50% sections have Mt layers 1-5mm thick conc'd in net-textured type over
bands up to 1 Ocm wide + local high % of dissm'd 1-2m zones, some of
Mt. Some bands may be assimiliated 4B?? others these are near the Mt are far from the margins. layers.- barren below
2178.3m. Analyzed for
Ni, Cu, PGE's.
0466411 12174.00 : 2174.65 0.18
I
l::466412 2174.90 '2175.50 0.32
.... . ....
07-NSD-008
Assay MAJOR UNIT MINOR UNIT ALTERATION Sample From To AU ppm From To Unit ! Comments Comments From To Unit Comments I Bio !Car Chi Gru Hem Ser Si Comments
:=455413 2175.50 2176.10 0.69 466414 2176.10 2177.00 0.75
i::466415 2177.00 2177.85 0.36 466416 2177.85 2178.30 0.14
466417 2178.30 2179.30 0.02
2181.70 2182.40 13 "Kimberlite" or an o!ivine-phlog lamprophyre as
before. 2182.40 2185.40 2 Homogenous, light grey basalt, pronounced hi-Mg
type bordering on an UM. Composed ofvfg
amph-plag?, no obvious serpentine, bio. =466418 2185.40 2186.40 0.00 2185.40 2186.40 1 Serpentinlsed Ultramafic.Vfg, mod strained
producing mottled to striped look and mod fracture
network. 466419 2186.40 2187.40 0.00 12186.40 2198.20 4B More typical SIF 4B now. -50:50 thinly laminated
black Mt and off-white chert-(grun) layers. Unit is
highly open-folded throughout but no major shears,
veins or Po. 466421 2187.40 2188.00 0.01
i::466422 2188.00 2189.00 0.00 i::466423 2189.00 2190.00 0.00 =466424 2190.00 2190.60 0.01 =455425 2190.60 2191.60 0.00
466426 2191.60 2192.60 0.00 =466427 2192.60 2193.80 0.00 466428 2193.80 2194.90 0.00
=466429 2194.90 2195.40 0.00
l::466431 2195.40 2196.40 0.01 466432 2196.40 2197.40 0.00 466433 2197.40 2198.20 0.00
E:466434 2198.20 2199.00 0.04 2198.20 2201.00 4A Fairly well banded 4A with alternating 60% white Lower 10cm is a good chert bands to 1-2cm and 40% light yellow, 4H with 55% Po. in somewhat diffuse grunerite layers <1 cm. Locally black f.g. argillite matrix.
up lo 5% bands of mg green amph +/- minor Po
and -15cm of dark amph-c.g. gar. l:466435 2199.00 2200.00 0.08 l:466436 2200.00 2200.70 0.01
466437 2200.70 2201.00 0.07 2200.90 ~ 201.00 4H 40-50% Po network in a black
argillite matrix. l:466438 ! 2201.00 2202.00 0.00 2201.00 2202.50 2 Med grey green basalt, -1/2 has mod bio alt'n
along fol'n planes bordering on a weak 2T, rest is
I i -fresh. Cut by -15% Cc veins (2-6cm wide). EOH
! due to broken rods and Jammed wireline in hole. i Backed up to 1350m and started 08-NSD-001.
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A ~~~~~~~~
Target2:'--~~~~~~__J Target3:L-~~~~~~__J
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
exploration compound
Survev Depth Azimuth Dip SurveyType
0 84.169 -85.729 SURV 3 84.29 -85.71 MAXI
6 85.23 -85.73 MAXI
9 86.15 -85.73 MAXI
12 87.27 -85.66 MAXI
15 88.17 -85.54 MAXI
18 89.27 -85.49 MAXI
21 89.21 -85.48 MAXI
24 89.44 -85.49 MAXI
27 89.66 -85.48 MAXI
30 89.72 -85.46 MAXI
33 89.54 -85.45 MAXI
36 90.26 -85.47 MAXI
39 89.49 -85.43 MAXI
42 90.21 -85.4 MAXI
45 90.83 -85.41 MAXI
48 91.45 -85.42 MAXI
51 91.67 -85.45 MAXI
54 91.5 -85.41 MAXI
57 91.03 -85.39 MAXI
60 91.84 -85.35 MAXI
63 91.98 -85.42 MAXI
66 92.19 -85.39 MAXI
69 91.85 -85.38 MAXI
72 91.64 -85.37 MAXI
75 91.85 -85.36 MAXI
78 92.09 -85.32 MAXI
81 92.3 -85.33 MAXI
84 91.83 -85.33 MAXI
87 91.84 -85.34 MAXI
90 92.02 -85.32 MAXI
93 91.76 -85.29 MAXI
96 91.89 -85.27 MAXI
99 92.32 -85.28 MAXI
102 92.79 -85.26 MAXI
105 92.62 -85.24 MAXI
108 92.64 -85.23 MAXI
111 92.25 -85.2 MAXI
114 92.33 -85.15 MAXI
117 92.67 -85.08 MAXI
120 92.95 -85.05 MAXI
123 93.21 -85.09 MAXI
126 92.93 -85.08 MAXI
129 92.73 -85.01 MAXI
132 92.18 -85.02 MAXI
135 92.09 -85.02 MAXI
138 92.09 -84.99 MAXI
141 92.3 -84.98 MAXI
144 92.44 -84.96 MAXI
147 91.99 -84.95 MAXI
150 92.28 -84.92 MAXI
153 92.53 -84.95 MAXI
156 92.17 -84.96 MAXI
159 92.36 -84.96 MAXI
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A ~~~~~~~~
Target 2: ~==========~ Target3:'--~~~~~~--'
omments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Depth Azimuth SurveyType 162 92.75 -84.97 MAXI
165 92.56 -84.95 MAXI
168 92.65 -84.91 MAXI
171 92.58 -84.93 MAXI
174 92.97 -84.93 MAXI
177 93.11 -84.89 MAXI
180 93.26 -84.9 MAXI
183 93.48 -84.86 MAXI
186 93.78 -84.82 MAXI
189 93.76 -84.85 MAXI
192 93.8 -84.84 MAXI
195 93.82 -84.78 MAXI
198 94.08 -84.8 MAXI
201 93.66 -84.75 MAXI
204 93.89 -84.73 MAXI
207 94.12 -84.67 MAXI
210 93.97 -84.67 MAXI
213 93.76 -84.61 MAXI
216 93.71 -84.57 MAXI
219 93.93 -84.47 MAXI
222 94.55 -84.45 MAXI
225 94.96 -84.47 MAXI
228 95.09 -84.42 MAXI
231 95.26 -84.37 MAXI
234 95.29 -84.37 MAXI
237 95.28 -84.35 MAXI
240 95.25 -84.3 MAXI
243 95.3 -84.27 MAXI
246 95.41 -84.24 MAXI
249 95.61 -84.22 MAXI
252 95.56 -84.21 MAXI
255 95.37 -84.18 MAXI
258 95.04 -84.14 MAXI
261 94.92 -84.11 MAXI
264 95.34 -84.1 MAXI
267 95.39 -84.13 MAXI
270 95 -84.19 MAXI
273 94.86 -84.2 MAXI
276 95.4 -84.2 MAXI
279 95.28 -84.23 MAXI
282 95.29 -84.16 MAXI
285 95.65 -84.21 MAXI
288 95.5 -84.25 MAXI
291 95.48 -84.19 MAXI
294 95.38 -84.22 MAXI
297 95.12 -84.25 MAXI
300 95.09 -84.2 MAXI
303 95.49 -84.23 MAXI
306 95.49 -84.22 MAXI
309 96 -84.2 MAXI
312 95.69 -84.2 MAXI
315 95.24 -84.2 MAXI
318 94.82 -84.15 MAXI
321 95.01 -84.15 MAXI
Mine Grid Easting: 7230. 1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A ~------~
Target 2: ~------~
Target3:~--------'
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Survev Depth Azimuth Dip SurveyType
324 95.65 ·84.15 MAXI
327 95.49 -84.14 MAXI
330 95.33 -84.12 MAXI
333 95.69 -84.16 MAXI
336 96.05 -84.11 MAXI
339 96.06 -84.09 MAXI
342 96.11 -84.06 MAXI
345 96.03 -84.06 MAXI
348 96.5 -84.06 MAXI
351 97.24 -84.06 MAXI
354 97.54 -84.02 MAXI
357 98.05 -84.05 MAXI
360 98.43 -84.12 MAXI
363 99.63 -84.13 MAXI
366 100.1 -84.11 MAXI
369 99.95 -84.11 MAXI
372 100.4 -84.06 MAXI
375 100.83 -84.04 MAXI
378 100.96 -84.03 MAXI
381 100.93 -83.99 MAXI
384 100.81 -83.96 MAXI
387 100.88 -83.96 MAXI
390 101.1 -83.95 MAXI
393 101.46 -83.96 MAXI
396 101.17 -83.96 MAXI
399 101.11 -84 MAXI
402 101.09 -83.96 MAXI
405 101.71 -83.92 MAXI
408 101.36 -83.91 MAXI
411 100.93 -83.92 MAXI
414 100.94 -83.88 MAXI
417 101.81 -83.87 MAXI
420 101.74 -83.9 MAXI
423 101.98 -83.87 MAXI
426 102.08 -83.82 MAXI
429 102.07 -83.8 MAXI
432 101.83 -83.83 MAXI
435 101.85 -83.82 MAXI
438 102.18 -83.79 MAXI
441 101.8 -83.79 MAXI
444 101.9 -83.74 MAXI
447 102.44 -83.75 MAXI
450 102.41 -83.79 MAXI
453 102.15 -83.74 MAXI
456 102.03 -83.73 MAXI
459 102.47 -83.73 MAXI
462 102.53 -83.7 MAXI
465 101.6 -83.7 MAXI
468 102.91 -83.7 MAXI
471 102.9 -83.67 MAXI
474 103.47 -83.66 MAXI
477 103.01 -83.57 MAXI
480 103.58 -83.58 MAXI
483 103.45 -83.55 MAXI
: :
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A ...---------~
Target 2: ~==========~ Target 3: ~------_J
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
exploration compound
Survev Depth Azimuth Dip SurveyType
486 103.91 -83.5 MAXI
489 103.85 -83.48 MAXI
492 103.87 -83.41 MAXI
495 104.68 -83.39 MAXI
498 105.18 -83.37 MAXI
501 105.44 -83.4 MAXI
504 106.16 -83.39 MAXI
507 106.73 -83.35 MAXI
510 107.45 -83.33 MAXI
513 108.18 -83.31 MAXI
516 109.08 -83.25 MAXI
519 109.21 -83.22 MAXI
522 109.89 -83.24 MAXI
525 111.23 -83.17 MAXI
528 111.58 -83.11 MAXI
531 112.69 -83.02 MAXI
534 114.11 -82.96 MAXI
537 114.65 -82.81 MAXI
540 114.65 -82.74 MAXI
543 114.73 -82.6 MAXI
546 115.22 -82.47 MAXI
549 115.52 -82.39 MAXI
552 116.32 -82.33 MAXI
555 116.49 -82.25 MAXI
558 116.83 -82.16 MAXI
561 117.48 -82.06 MAXI
564 117.86 -82 MAXI
567 118 -81.89 MAXI
570 118.29 -81.83 MAXI
573 118.88 -81.75 MAXI
576 119.26 -81.65 MAXI
579 119.48 -81.6 MAXI
582 119.85 -81.56 MAXI
585 120.1 -81.46 MAXI
588 120.24 -81.39 MAXI
591 120.33 -81.35 MAXI
594 120.81 -81.29 MAXI
597 119.67 -81.16 MAXI
600 116.02 -80.83 MAXI
603 113.62 -80.53 MAXI
606 113.63 -80.41 MAXI
609 114.13 -80.36 MAXI
612 113.94 -80.3 MAXI
615 113.96 -80.2 MAXI
618 113.98 -80.15 MAXI
621 114.4 -80.11 MAXI
624 114.17 -80.03 MAXI
627 114.31 -80 MAXI
630 114.44 -80.01 MAXI
633 114.59 -79.93 MAXI
636 114.67 -79.88 MAXI
639 113.54 -79.81 MAXI
642 110.81 -79.59 MAXI
645 109.66 -79.45 MAXI
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07 -NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A .----------,
Target 2: '---------__)
Target 3: '--------__,
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Depth
Survev Azimuth =Dip SurveyType
648 109.8 -79.39 MAXI
651 110.15 -79.22 MAXI
654 110.2 -78.9 EZS
654 110.34 -79.03 MAXI
657 110.48 -78.82 MAXI
660 110.49 -78.7 MAXI
663 110.6 -78.49 MAXI
666 110.86 -78.3 MAXI
669 110.78 -78.15 MAXI
672 110.79 -78.01 MAXI
675 110.96 -77.86 MAXI
678 111.3 -77.73 MAXI
681 111.59 -77.6 MAXI
684 111.7 -77.51 MAXI
687 112.03 -77.45 MAXI
690 112.32 -77.37 MAXI
693 112.7 -77.29 MAXI
696 113.36 -77.32 MAXI
699 113.23 -77.26 MAXI
702 111.86 -77.15 MAXI
705 109.18 -76.96 MAXI
708 107.49 -76.79 MAXI
711 107.43 -76.79 MAXI
714 107.57 -76.76 MAXI
717 107.65 -76.68 MAXI
720 107.67 -76.65 MAXI
723 107.81 -76.6 MAXI
726 107.96 -76.54 MAXI
729 107.82 -76.49 MAXI
732 107.83 -76.47 MAXI
735 107.99 -76.43 MAXI
738 107.92 -76.34 MAXI
741 108.18 -76.31 MAXI
744 108.08 -76.28 MAXI
747 108.25 -76.26 MAXI
750 108.4 -76.24 MAXI
753 108.26 -76.2 MAXI
756 108.36 -76.24 MAXI
759 108.42 -76.19 MAXI
762 108.3 -76.15 MAXI
765 108.12 -76.11 MAXI
768 108.18 -76.07 MAXI
771 108.28 -76.04 MAXI
774 108.08 -75.97 MAXI
777 108.19 -75.95 MAXI
780 108.23 -75.94 MAXI
783 108.05 -75.93 MAXI
786 108.23 -75.9 MAXI
789 108.19 -75.88 MAXI
792 108.33 -75.84 MAXI
795 108.51 -75.82 MAXI
798 108.24 -75.77 MAXI
801 108.26 -75.8 MAXI
804 108.48 -75.72 MAXI
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A ,---------,
Target 2: ::===========~ Target 3: '---------_J
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Surve Depth Azimuth
807 108.5 MAXI
810 108.6 MAXI
813 108.65 -75.6 MAXI
816 108.81 -75.53 MAXI
819 108.74 -75.51 MAXI
822 108.82 -75.44 MAXI
825 109 -75.39 MAXI
828 109.14 -75.33 MAXI
831 109.19 -75.31 MAXI
834 109.12 -75.31 MAXI
837 109.02 -75.29 MAXI
840 109.01 -75.24 MAXI
843 109.12 -75.24 MAXI
846 109.09 -75.21 MAXI
849 109.14 -75.17 MAXI
852 109.27 -75.15 MAXI
855 109.06 -75.16 MAXI
858 109.13 -75.05 MAXI
861 109.4 -74.97 MAXI
864 109.38 -74.87 MAXI
867 109.25 -74.79 MAXI
870 109.5 -74.67 MAXI
873 109.62 -74.61 MAXI
876 109.52 -74.58 MAXI
879 109.54 -74.51 MAXI
882 109.7 -74.47 MAXI
885 109.91 -74.45 MAXI
888 109.95 .74.43 MAXI
891 109.95 -74.37 MAXI
894 109.97 -74.31 MAXI
897 110.12 -74.25 MAXI
900 110.11 -74.17 MAXI
903 110.3 -74.07 MAXI
906 110.36 -73.98 MAXI
909 110.23 -73.9 MAXI
912 110.46 -73.88 MAXI
915 111.05 -73.96 MAXI
918 111.69 -74.2 MAXI
921 112.04 -74.31 MAXI
924 111.99 -74.24 MAXI
927 112.25 -74.23 MAXI
930 112.32 -74.29 MAXI
933 112.46 -74.3 MAXI
936 112.66 -74.26 MAXI
939 112.89 -74.2 MAXI
942 112.99 -74.15 MAXI
945 112.9 -74.09 MAXI
948 112.99 -74.02 MAXI
951 112.87 -73.85 MAXI
954 112.59 -73.68 MAXI
957 109.77 -73.04 MAXI
960 109.09 -72.83 MAXI
963 109.18 -72.68 MAXI
966 109.39 -72.45 MAXI
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A .--~~~~~~~
Target2:~~~~~~~__J
Target3:~~~~~~~__J
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Survev Depth Azimuth Dip SurveyType
969 109.5 -72.16 MAXI
972 109.15 -71.9 MAXI
975 109.1 -71.64 MAXI
978 109.03 -71.4 MAXI
981 109.23 -71.38 MAXI
984 109.64 -71.28 MAXI
987 109.9 -71.14 MAXI
990 109.8 -71.06 MAXI
993 109.8 -71.01 MAXI
996 109.92 -70.96 MAXI
999 109.92 -70.98 MAXI
1002 109.94 -71 MAXI
1005 110.15 -70.99 MAXI
1008 110.12 -70.97 MAXI
1011 110.13 -70.93 MAXI
1014 110.15 -70.88 MAXI
1017 110.15 -70.83 MAXI
1020 110 -70.75 MAXI
1023 110.1 -70.68 MAXI
1026 110.15 -70.57 MAXI
1029 110.09 -70.55 MAXI
1032 110.22 -70.53 MAXI
1035 110.41 -70.52 MAXI
1038 110.49 -70.47 MAXI
1041 110.56 -70.4 MAXI
1044 110.62 -70.34 MAXI
1047 110.79 -70.32 MAXI
1050 110.82 -70.26 MAXI
1053 110.94 -70.2 MAXI
1056 111.03 -70.15 MAXI
1059 110.94 -70.12 MAXI
1062 111.01 -70.08 MAXI
1065 111.14 -70.05 MAXI
1068 111.15 -69.98 MAXI
1071 111.17 -69.92 MAXI
1074 111.16 -69.89 MAXI
1077 111.24 -69.85 MAXI
1080 111.25 -69.8 MAXI
1083 111.5 -69.75 MAXI
1086 111.04 -69.76 MAXI
1089 111.73 -69.61 MAXI
1092 111.7 -69.58 MAXI
1095 111.82 -69.55 MAXI
1098 111.9 -69.51 MAXI
1101 111.95 -69.45 MAXI
1104 111.94 -69.43 MAXI
1107 111.93 -69.35 MAXI
1110 112.13 -69.32 MAXI
1113 111.97 -69.3 MAXI
1116 112.02 -69.24 MAXI
1119 112.08 -69.21 MAXI
1122 112.09 -69.2 MAXI
1125 112.1 -69.12 MAXI
1128 112.22 -69.04 MAXI
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD·A .---------
Target 2: c__ ______ _
Target3:...._ ______ ~
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by
Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Survev Depth Azimuth Dip Survey Type
1131 112.38 -68.95 MAXI
1134 112.23 -68.81 MAXI
1137 112.02 -68.66 MAXI
1140 112 -68.56 MAXI
1143 112.03 -68.51 MAXI
1146 111.97 -68.37 MAXI
1149 112 -68.27 MAXI
1152 111.92 ·68.19 MAXI
1155 111.82 -68.07 MAXI
1158 111.8 -67.95 MAXI
1161 111.77 -67.78 MAXI
1164 111.79 ·67.64 MAXI
1167 111.73 -67.52 MAXI
1170 111.78 -67.43 MAXI
1173 111.88 -67.37 MAXI
1176 111.85 -67.29 MAXI
1179 111.82 -67.28 MAXI
1182 111.93 -67.22 MAXI
1185 112.1 -67.19 MAXI
1188 112.02 ·67.2 MAXI
1191 112.11 -67.22 MAXI
1194 112.16 -67.17 MAXI
1197 112.23 -67.23 MAXI
1200 112.3 ·67.17 MAXI
1203 111 -67 EZS 1203 112.33 ·67.13 MAXI
1206 112.28 ·67.07 MAXI
1209 112.33 -67.02 MAXI
1212 112.35 ·66.91 MAXI
1215 112.37 ·66.88 MAXI
1218 112.25 -66.9 MAXI
1221 112.34 -66.89 MAXI
1224 112.32 ·66.87 MAXI
1227 112.37 -66.86 MAXI
1230 112.42 -66.8 MAXI
1233 112.53 ·66.76 MAXI
1236 112.6 -66.7 MAXI
1239 112.64 ·66.7 MAXI
1242 112.74 -66.64 MAXI
1245 112.67 -66.63 MAXI
1248 112.68 -66.59 MAXI
1251 112.77 -66.59 MAXI
1254 112.86 -66.59 MAXI
1257 112.82 -66.55 MAXI
1260 112.94 -66.53 MAXI
1263 113.05 -66.5 MAXI
1269 113.11 -66.47 MAXI
1272 112.99 -66.47 MAXI
1275 i 112.99 -66.47 MAXI
1278 113.05 -66.4 MAXI
1281 112.96 -66.37 MAXI
1284 112.9 -66.34 MAXI
1287 112.99 ·66.31 MAXI
1290 112.83 -66.29 MAXI
•
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A .--------~
Target 2: c__ ______ _
Target 3: '----------'
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Survev Azimuth Dip !surveyType
1293 112.9 -66.21 MAXI
1296 112.89 -66.19 MAXI
1299 112.91 -66.2 MAXI
1302 112.91 -66.14 MAXI
1305 112.95 -66.13 MAXI
1308 112.83 -66.09 MAXI
1311 112.86 -66.08 MAXI
1314 112.86 -66.04 MAXI
1317 112.77 -65.99 MAXI
1320 112.77 -65.95 MAXI
1323 112.74 -65.86 MAXI
1326 112.68 -65.79 MAXI
1329 112.62 -65.72 MAXI
1332 112.6 -65.66 MAXI
1335 112.47 -65.67 MAXI
1338 112.6 -65.69 MAXI
1341 112.59 -65.65 MAXI
1344 112.55 -65.6 MAXI
1347 112.48 -65.57 MAXI
1350 112.29 -65.53 MAXI
1353 112.33 -65.49 MAXI
1356 112.32 -65.47 MAXI
1359 112.16 -65.44 MAXI
1362 112.09 -65.44 MAXI
1365 112.25 -65.44 MAXI
1368 112.2 -65.44 MAXI
1371 112.21 -65.4 MAXI
1374 112.19 -65.37 MAXI
1377 112.12 -65.35 MAXI
1380 112.07 -65.34 MAXI
1383 112.13 -65.35 MAXI
1386 112.11 -65.33 MAXI
1389 112.03 -65.32 MAXI
1392 111.87 -65.31 MAXI
1395 111.95 -65.26 MAXI
1398 111.93 -65.2 MAXI
1401 111.77 -65.14 MAXI
1404 111.78 -65.09 MAXI
1407 111.66 -65.03 MAXI
1410 111.51 -65 MAXI
1413 111.53 -64.95 MAXI
1416 111.39 -64.89 MAXI
1419 111.36 -64.84 MAXI
1422 111.32 -64.78 MAXI
1425 111.26 -64.76 MAXI
1428 111.41 -64.8 MAXI
1431 111.49 -64.8 MAXI
1434 111.46 -64.73 MAXI
1437 111.36 -64.7 MAXI
1440 111.39 -64.66 MAXI
1443 111.27 -64.66 MAXI
1446 111.1 -64.73 MAXI
1449 111.08 -64.84 MAXI
1452 111.16 -64.88 MAXI
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A
Target 2: ....._ ______ _j
Target 3: L._ ______ .....;
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Survev Depth Azimuth Dip SurveyType
1455 111.21 -64.86 MAXI
1458 111.25 -64.85 MAXI
1461 111.3 -64.85 MAXI
1464 111.4 -64.79 MAXI
1467 111.39 -64.74 MAXI
1470 111.38 -64.71 MAXI
1473 111.43 -64.67 MAXI
1476 111.49 -64.67 MAXI
1479 111.46 -64.64 MAXI
1482 111.45 -64.57 MAXI
1485 111.53 -64.49 MAXI
1488 111.63 -64.41 MAXI
1491 111.72 -64.32 MAXI
1494 111.7 -64.47 MAXI
1497 111.64 -64.43 MAXI
1500 111.68 -64.44 MAXI
1503 111.72 -64.4 MAXI
1506 111.63 -64.38 MAXI
1509 111.61 -64.38 MAXI
1512 111.62 -64.36 MAXI
1515 111.62 -64.35 MAXI
1518 111.78 -64.38 MAXI
1521 111.81 -64.39 MAXI
1524 111.77 -64.34 MAXI
1527 111.77 -64.32 MAXI
1530 111.85 -64.36 MAXI
1533 111.84 -64.38 MAXI
1536 111.86 -64.39 MAXI
1539 111.85 -64.35 MAXI
1542 111.92 -64.31 MAXI
1545 111.93 -64.28 MAXI
1548 111.89 -64.26 MAXI
1551 111.79 -64.24 MAXI
1554 111.77 -64.21 MAXI
1557 111.9 -64.17 MAXI
1560 111.94 -64.11 MAXI
1563 111.77 -64.08 MAXI
1566 111.81 -64.11 MAXI
1569 111.91 -64.07 MAXI
1572 111.83 -64.03 MAXI
1575 111.8 -64 MAXI
1578 111.77 -63.96 MAXI
1581 111.65 -63.92 MAXI
1587 111.65 -63.83 MAXI
1590 111.66 -63.81 MAXI
1593 111.59 -63.77 MAXI
1596 111.58 -63.73 MAXI
1599 111.58 -63.68 MAXI
1602 111.47 -63.65 MAXI
1605 111.48 -63.62 MAXI
1608 112.22 -63.86 MAXI
1611 113.29 -64.23 MAXI
1614 113.84 -64.34 MAXI
1617 114.02 -64.17 MAXI
;
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A ~~~~~~~~
Target2:.__~~~~~~--'
Target3:.__~~~~~~--'
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by
Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Survev i Depth Azimuth Dip SurveyType i 1620 113.84 -63.43 MAXI
1623 -64 EZS
1623 113.43 -62.69 MAXI
1626 112.93 -62.29 MAXI
1629 112.74 -62.12 MAXI
1632 112.51 -61.91 MAXI
1635 112.22 -61.63 MAXI
1638 111.95 -61.32 MAXI
1641 111.83 -61.09 MAXI
1644 111.79 -60.96 MAXI
1647 111.61 -60.87 MAXI
1650 111.48 -60.78 MAXI
1653 111.51 -60.65 MAXI
1656 111.32 -60.57 MAXI
1659 111.31 -60.53 MAXI
1662 111.27 -60.5 MAXI
1665 111.04 -60.4 MAXI
1668 111.07 -60.29 MAXI
1671 111.02 -60.22 MAXI
1674 111.09 -60.23 MAXI
1677 111.01 -60.15 MAXI
1680 111.04 -60.07 MAXI
1683 111.05 -60.05 MAXI
1686 111.07 -59.98 MAXI
1689 111.1 -59.89 MAXI
1692 111.22 -59.85 MAXI
1695 111.25 -59.82 MAXI
1698 111.3 -59.76 MAXI
1701 111.4 -59.79 MAXI
1704 111.59 -59.8 MAXI
1707 111.75 -59.77 MAXI
1710 111.86 -59.73 MAXI
1713 111.95 -59.67 MAXI
1716 112.17 -59.57 MAXI
1719 112.18 -59.45 MAXI
1722 112.17 -59.36 MAXI
1725 112.28 -59.18 MAXI
1728 112.5 -59.11 MAXI
1731 112.44 -58.97 MAXI
1734 112.57 -58.85 MAXI
1737 112.7 -58.81 MAXI
1740 112.77 -58.74 MAXI
i 1743 112.89 -58.67 MAXI
1746 112.88 -58.63 MAXI
1749 113.03 -58.53 MAXI
1752 113.04 -58.44 MAXI
1755 113.12 -58.23 MAXI
1758 113.16 -58.04 MAXI
1761 113.07 -57.92 MAXI
1764 111.2 -57.8 EZS
1764 113.14 -57.89 MAXI
1767 113.02 -57.9 MAXI
1770 112.99 -57.82 MAXI
1773 113.08 -57.74 i MAXI
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A ,--~~~~~~~
Target2=~~~~~~~--'
Target3:L....-.~~~~~~--'
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Survev Depth Azimuth Dip SurveyType
1776 113 -57.66 MAXI
1779 112.84 -57.64 MAXI
1782 112.79 -57.54 MAXI
1785 112.88 -57.53 MAXI
1788 112.82 -57.52 MAXI
1791 112.77 -57.48 MAXI
1794 112.73 -57.45 MAXI
1797 112.77 -57.41 MAXI
1800 112.72 -57.41 MAXI
1803 112.74 -57.42 MAXI
1806 112.76 -57.43 MAXI
1809 111.81 -56.77 MAXI
1812 111.11 -56.31 MAXI
1815 110.86 -56.07 MAXI
1818 110.85 -55.91 MAXI
1821 110.91 -55.84 MAXI
1824 110.93 -55.8 MAXI
1827 110.82 -55.77 MAXI
1830 110.86 -55.73 MAXI
1833 110.73 -55.68 MAXI
1836 110.56 -55.64 MAXI
1839 110.67 -55.56 MAXI
1842 110.69 -55.52 MAXI
1845 110.53 -55.47 MAXI
1848 110.56 -55.38 MAXI
1851 110.58 -55.27 MAXI
1854 110.46 -55.19 MAXI
1857 110.41 -55.12 MAXI
1860 110.25 -55.12 MAXI
1863 110.23 -55.08 MAXI
1866 110.24 -55.08 MAXI
1869 110.17 -54.99 MAXI
1872 110.14 -54.91 MAXI
1875 110.04 -54.87 MAXI
1878 110 -54.78 MAXI
1881 110.13 -54.71 MAXI
1884 110.1 -54.63 MAXI
1887 110.08 -54.58 MAXI
1890 110.23 -54.58 MAXI
1893 110.21 -54.52 MAXI
1896 110.24 -54.45 MAXI
1899 110.27 -54.38 MAXI
1902 110.31 -54.3 MAXI
1905 110.37 -54.22 MAXI
1908 110.32 -54.17 MAXI
1911 110.45 -54.11 MAXI
1914 110.57 -54.06 MAXI
1917 110.69 -54.02 MAXI
1920 110.66 -53.98 MAXI
1923 110.65 -53.89 MAXI
1926 110.74 -53.88 MAXI
1929 110.84 -53.75 MAXI
1932 110.96 -53.61 MAXI
1935 110.82 -53.61 MAXI
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.7839
Elevation: 5296.6106
UTM East 673666.8
UTM North: 583495.1
Planned Depth: 2600
Actual Depth: 2202.5
MUSSELWHITE MINE - GEOLOGY
Hole ID: 07-NSD-008
Project Code: 9320_NSD
Drill Start Date: 9/06/07
Drill End Date: 3/24/08
Core Diameter: NQ2
Plugged: UNKNOWN
Target 1: PQD-A -------~
Target 2: '------------'
Target 3: '-------------'
Comments: Hole in progress as of Dec '07. Logged by or supervised by John Biczok and Jim Edwards. Drilled by Boart Longyear. Drilled on claims 529778, 529785, 529786. Core stored in racks at Musselwhite
Survev Depth Azimuth Dip SurveyType
1938 110.96 -53.47 MAXI
1941 110.98 -53.44 MAXI
1944 111.01 -53.52 MAXI
1947 110.98 -53.64 MAXI
1950 111.08 -53.72 MAXI
1953 111.14 -53.71 MAXI
1956 111.03 -53.7 MAXI
1959 111.04 -53.65 MAXI
1962 111.02 -53.58 MAXI
1965 111.07 -53.53 MAXI
1968 110.96 -53.51 MAXI
1971 111.05 -53.48 MAXI
1974 111 -53.44 MAXI
1977 111.05 -53.39 MAXI
1980 111.11 -53.43 MAXI
1983 111.09 -53.38 MAXI
1986 111.03 -53.34 MAXI
1989 111.01 -53.29 MAXI
1992 111.09 -53.24 MAXI
1995 111.16 -53.19 MAXI
2030 111.5 -51.5 EZS
2096 111.5 -49 EZS
2146 111.5 -48.2 EZS
2198 111.5 -47.4 EZS
08-NSD-001
MAJOR UNIT
From
0.00
1349.00
1349.80
1359.40
1360.60
1393.70
1400.90
1409.00
1411.90
1437.60
To
1349.00
1349.80
1359.40
1360.60
1393.70
1400.90
1409.00
1411.90
1437.60
1453.70
MINERALS
As%Cp%
Mt%
Po%
3.0
0.1
5.0
3.0
3.0
3.0
1.0
Py% Comments
banded
amphibolite,
cummulate?
VGSpecks
FABRIC
From
1360.90
1382.30
1390.50
1405.30
1425.50
1437.60
To
1361.40
1382.70
1391.00
1414.00
1437.60
1442.00
Alphadeg
42
68
37
50
40
35
CommentsInt
MO
MO
WE
MO
MO
MO
Type
S1
S1
S1
S0
S1
S1
FOLD
To
150.20
151.10
152.30
185.20
188.00
188.50
191.60
1357.50
Alpha
deg
70
60
65
40
50
55
55
32
CommentsInt
MO
MO
MO
MO
MO
MO
MO
Type
IF
MF
IF
ZF
ZF
MF
MF
FD
From
150.10
151.00
152.20
185.10
187.90
188.40
191.50
1356.60
QTZ VEINING
VeinType
QZ
QZ
QZ
Vein% Tex Contact
TypeAlphadeg
CommentsFrom
1427.00
1448.00
1451.60
To
1427.50
1449.30
1452.50
FAULT
From
33.30
33.80
34.40
174.50
1404.50
1414.40
1424.00
1437.60
To
33.50
34.00
34.70
175.90
1405.30
1415.70
1425.50
1442.00
Alphadeg
78
75
74
50
50
65
50
CommentsInt
INT
INT
INT
MOD
WEK
WEK
WEK
WEK
Type
SZ
SZ
SZ
SZ
SZ
SZ
SZ
SZ
MajorUnit
No
3K
2
8F
2
2
2
1M
2
2
Cont
55
61
29
19
83
77
60
50
35
40
50
50
STRUCTURAL LOG Page 1 of 10
08-NSD-001
MAJOR UNIT
From
1453.70
1508.30
1509.70
1510.40
1511.60
1527.00
1528.60
1567.80
1574.00
1594.90
1596.45
1600.10
1602.30
1603.30
1606.90
1614.70
1615.30
1617.40
To
1508.30
1509.70
1510.40
1511.60
1527.00
1528.60
1567.80
1574.00
1594.90
1596.45
1600.10
1602.30
1603.30
1606.90
1614.70
1615.30
1617.40
1625.20
MINERALS
As%Cp%
0.1
0.1
0.2
Mt%
Po%
0.0
3.0
4.0
2.0
0.5
0.1
1.5
2.5
3.0
4.0
25.
2.5
1.5
10.
1.0
Py% CommentsVGSpecks
FABRIC
From
1470.00
1483.00
1496.00
1507.00
1520.00
1530.00
1540.00
1550.00
1571.00
1580.00
1587.00
1599.00
1607.00
1610.40
1616.00
To
1471.00
1484.00
1496.50
1507.50
1522.00
1531.00
1541.00
1552.00
1573.00
1582.00
1588.00
1600.00
1608.00
1611.00
1617.00
Alphadeg
35
47
57
51
42
0
25
35
42
37
58
51
40
35
50
Comments
Shear fol'n.
Shear fol'n
Shear
foliation.
Int
MO
MO
MO
MO
WE
WE
WE
WE
WE
WE
WE
MO
MO
MO
Type
S1
S1
S1
S1
S1
S2
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ
CA
CA
Vein%
100
7
3
Tex ContactType
Alphadeg
CommentsFrom
1517.60
1542.00
1583.00
To
1518.00
1557.00
1592.00
FAULT
From
1529.30
To
1536.00
Alphadeg Comments
Highly irreg,
contorted shear
zone.
Int
WEK
Type
SZ
MajorUnit
2
8F
2
8F
2
8F
2
2D
2
4E
1M
6M
4E
2
4E
1S
4E
2
Cont
55
45
55
35
30
30
45
50
STRUCTURAL LOG Page 2 of 10
08-NSD-001
MAJOR UNIT
From
1625.20
1626.00
1632.10
1632.90
1633.30
1634.80
1638.10
1638.60
1642.40
1664.30
1664.70
1669.20
1672.90
To
1626.00
1632.10
1632.90
1633.30
1634.80
1638.10
1638.60
1642.40
1664.30
1664.70
1669.20
1672.90
1775.00
MINERALS
As%Cp%
0.1
Mt%
Po%
17.
4.0
4.0
3.0
2.0
2.0
20.
0.2
8.0
2.0
0.1
4.0
2.0
5.0
Py% CommentsVGSpecks
FABRIC
From
1630.00
1673.00
1682.00
1693.00
1700.00
1704.00
To
1631.00
1674.00
1683.00
1694.00
1701.00
1706.00
Alphadeg
20
45
37
40
55
30
Comments
Shearing
Int
MO
WE
WE
WE
Type
S1
S1
S1
S1
S1
S2
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
CA
QZ
Vein%
15
100
Tex ContactType
Alphadeg
CommentsFrom
1654.00
1757.00
To
1656.00
1757.70
FAULT
From
1629.20
To
1631.00
Alphadeg
20
CommentsInt
WEK
Type
SZ
MajorUnit
4H
4E
6M
4H
6M
2
4H
4E
2
4E
2
4E
2D
Cont
STRUCTURAL LOG Page 3 of 10
08-NSD-001
MAJOR UNIT
From
1775.00
1802.00
1860.00
1866.55
1880.00
1882.00
1884.40
1886.70
1887.00
1901.00
1903.00
To
1802.00
1860.00
1866.55
1880.00
1882.00
1884.40
1886.70
1887.00
1901.00
1903.00
1903.40
MINERALS
As%
1.0
0.1
0.1
2.0
0.1
0.1
Cp%
0.1
0.1
Mt%
Po%
5.0
0.1
15.
15.
1.0
0.1
0.1
2.0
2.0
3.0
3.0
10.
Py% CommentsVGSpecks
FABRIC
From
1769.00
1771.00
1782.00
1786.00
1798.00
1806.00
1814.00
1826.00
1830.00
1838.00
1856.00
1868.00
1886.00
1893.00
1898.00
To
1770.00
1773.00
1784.00
1787.00
1799.00
1808.00
1816.00
1828.00
1832.00
1840.00
1859.00
1870.00
1888.00
1895.00
1901.00
Alphadeg
45
70
70
60
47
39
45
57
40
41
50
47
57
55
53
Comments
Foliation
is very
weak and
changes
~substantia
lly due to
local
weak
shears.
Int
MO
WE
MO
MO
MO
WE
WE
WE
WE
WE
WE
WE
WE
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1887.00
Alpha
deg
55
CommentsInt
MO
Type
ZF
From
1886.70
QTZ VEINING
VeinType
QZ
CA
QZ
Vein%
100
15
12
Tex ContactType
Alphadeg
CommentsFrom
1758.20
1882.00
1903.00
To
1758.60
1886.70
1903.40
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
2
2
2
2
2T
QTZ
4A
4B
2
2T
4H
Cont
45
STRUCTURAL LOG Page 4 of 10
08-NSD-001
MAJOR UNIT
From
1903.40
1908.20
1919.10
1920.10
1937.50
1947.50
To
1908.20
1919.10
1920.10
1937.50
1947.50
1955.30
MINERALS
As%
2.5
0.8
0.5
0.1
0.4
Cp%
Mt%
Po%
1.0
4.0
0.3
0.1
0.1
0.1
12.
7.0
0.2
5.0
Py% Comments
al,ost all Po
is in one
massive vein
~5-7cm wide.
VGSpecks
FABRIC
From
1907.00
1908.00
1917.00
1924.00
1928.00
1937.00
1943.00
1944.00
To
1907.50
1909.00
1918.00
1926.00
1932.00
1940.00
1944.00
1950.00
Alphadeg
27
39
50
55
53
60
47
50
Comments
Fracture
cleavage
with
Asp-Po
filings.
Int
MO
WE
WE
MO
MO
MO
Type
S2
S0
S0
S1
S1
S1
S1
S2
FOLD
To
1912.00
Alpha
deg
59
Comments
Range
from
50-63
deg AP
Int
MO
Type
ZF
From
1910.00
QTZ VEINING
VeinType
QZ
QZ
QZ
QZ
Vein%
7
20
7
50
Tex ContactType
I
I
Alphadeg
Comments
10% Po
amd 1%
Asp
From
1903.40
1905.00
1905.60
1915.90
To
1904.40
1905.60
1908.00
1916.10
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
4A
4B
4B
2
2
4B
Cont
45
50
STRUCTURAL LOG Page 5 of 10
08-NSD-001
MAJOR UNIT
From
1955.30
1969.50
1980.30
1991.10
1995.50
2013.20
2021.20
2045.20
2054.75
To
1969.50
1980.30
1991.10
1995.50
2013.20
2021.20
2045.20
2054.75
2066.90
MINERALS
As%Cp%
0.1
Mt%
Po%
5.0
1.5
2.5
4.0
0.1
0.5
Py% CommentsVGSpecks
FABRIC
From
1952.00
1958.00
1962.00
1969.00
1972.00
1982.00
1988.00
1994.00
2005.00
2013.50
2024.00
2036.00
2040.00
2045.20
2054.75
To
1953.00
1959.00
1963.00
1970.00
1974.00
1983.00
1990.00
1996.00
2010.00
2014.00
2028.00
2040.00
2045.20
2054.75
2066.60
Alphadeg
63
55
45
70
52
32
40
50
47
55
56
45
40
35
60
CommentsInt
MO
WE
MO
WE
MO
WE
MO
MO
MO
MO
WE
Type
S2
S1
S1
S1
S1
S0
S0
S0
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ
QZ
QZ
QZ
Vein%
35
100
15
6
Tex ContactType
Alphadeg
CommentsFrom
1955.30
1983.50
1985.30
1994.00
To
1955.80
1983.60
1987.00
1997.00
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
2
1
4B
4A
2
1
2
1
2
Cont
60
70
STRUCTURAL LOG Page 6 of 10
08-NSD-001
MAJOR UNIT
From
2066.90
2074.20
2085.10
2086.00
2088.10
2114.90
2119.60
2124.00
To
2074.20
2085.10
2086.00
2088.10
2114.90
2119.60
2124.00
2164.40
MINERALS
As%Cp%
Mt%
Po%
0.5
0.0
0.1
Py% Comments
Note Po is
associated with
light green
amphibole
Very f.g
dessem Po.
VGSpecks
FABRIC
From
2066.60
2069.50
2070.00
2070.20
2071.00
2074.20
2085.00
2087.00
2093.00
2103.00
2106.00
2114.00
2117.00
2120.00
2130.00
2142.00
2147.00
2158.00
To
2069.00
2069.55
2070.20
2071.00
2074.20
2082.00
2087.00
2088.00
2094.00
2104.00
2107.00
2114.50
2117.50
2120.70
2131.00
2146.00
2149.00
2160.00
Alphadeg
35
90
30
0
50
40
45
30
60
62
42
42
59
53
66
50
53
50
CommentsInt
MO
MO
MO
MO
MO
INT
INT
MO
MO
MO
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S0
S1
S1
S1
S1
S1
FOLD
To
2070.00
2116.60
Alpha
deg
90
47
Comments
2cm wide
Z in 1cm
thick
chert band
Int
MO
MO
Type
FD
ZF
From
2069.00
2116.40
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From
2086.00
To
2088.10
Alphadeg
47
CommentsInt
MOD
Type
SZ
MajorUnit
4A
2
1
2T
1
4A
13
1
Cont
70
70
58
40
55
60
55
65
STRUCTURAL LOG Page 7 of 10
08-NSD-001
MAJOR UNIT
From
2164.40
2165.90
2183.00
To
2165.90
2183.00
2220.30
MINERALS
As%Cp%
Mt%
Po%
1.0
1.0
1.0
3.0
0.5
Py% Comments
qtz veined 4A
VGSpecks
FABRIC
From
2165.00
2169.00
2177.00
2180.00
2184.00
2187.00
2190.00
2192.00
2194.20
2197.00
2201.00
To
2166.00
2170.00
2179.00
2183.00
2184.80
2188.00
2191.00
2193.00
2194.80
2198.00
2202.00
Alphadeg
50
40
50
55
40
40
0
70
40
40
20
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S2
S1
S1
S0
S1
S1
S1
S1
FOLD
To
2184.00
Alpha
deg
50
CommentsInt
WE
Type
FD
From
2183.00
QTZ VEINING
VeinType
QZ
QZ
Vein%
40
2
Tex ContactType
Alphadeg
Comments
qtz
flooding/vei
ning
From
2164.40
2193.70
To
2165.20
2194.20
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
4B
4A
4A
Cont
50
STRUCTURAL LOG Page 8 of 10
08-NSD-001
MAJOR UNIT
From
2220.30
2225.10
2239.50
2242.70
2243.00
2244.00
2246.60
2247.90
2248.60
To
2225.10
2239.50
2242.70
2243.00
2244.00
2246.60
2247.90
2248.60
2250.30
MINERALS
As%
0.0
Cp%
Mt%
Po%
3.0
0.5
2.0
1.0
0.1
0.1
3.0
Py% Comments
qtz veined 4A
qtz veined 4A
small 4E itf
VGSpecks
FABRIC
From
2206.00
2208.00
2212.00
2214.00
2219.70
2223.80
2231.00
2237.50
2242.00
2243.00
2248.60
To
2207.00
2209.00
2213.00
2215.00
2220.30
2224.80
2232.00
2238.50
2242.70
2244.00
2249.20
Alphadeg
60
0
0
75
60
60
70
70
70
80
70
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
Type
S1
S0
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ
QZ
Vein%
5
8
Tex ContactType
Alphadeg
Comments
qtz
flooding/vei
ning
qtz
flooding/vei
ning
From
2209.00
2218.00
To
2210.00
2220.30
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
1
2
4A
4E
4A
2
4E
4A
4B
Cont
80
60
80
75
STRUCTURAL LOG Page 9 of 10
08-NSD-001
MAJOR UNIT
From
2250.30
2250.70
2261.00
2301.40
2311.80
2313.60
2321.20
2334.10
2336.00
2393.40
2393.70
2403.00
To
2250.70
2261.00
2301.40
2311.80
2313.60
2321.20
2334.10
2336.00
2393.40
2393.70
2403.00
2441.00
MINERALS
As%Cp%
Mt%
Po%
20.
11.
0.5
Py% Comments
well
mineralised 4A
VGSpecks
FABRIC
From
2251.70
2257.00
2267.00
2275.00
2284.00
2293.00
2300.00
2320.00
2333.00
2343.00
2351.00
2360.00
2376.00
2385.00
2396.00
2408.00
2420.00
2432.00
2440.00
To
2252.70
2258.00
2268.00
2276.00
2285.00
2294.00
2301.00
2321.00
2334.00
2344.00
2352.00
2361.00
2377.00
2386.00
2397.00
2409.00
2421.00
2433.00
2441.00
Alphadeg
50
70
60
60
50
50
60
46
50
44
50
45
45
35
50
37
40
44
39
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
INT
INT
INT
MO
MO
MO
MO
MO
INT
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
2314.50
Alpha
deg
50
CommentsInt
MO
Type
FD
From
2314.20
QTZ VEINING
VeinType
CA
Vein%
2
Tex ContactType
I
Alphadeg
60
Comments
in mafic
volcanic
From
2261.00
To
2301.40
FAULT
From
2319.30
To
2319.60
Alphadeg
50
CommentsInt
MOD
Type
SZ
MajorUnit
4A
2
2
2
4H
2
7A
2
2
13
2
2
Cont
55
80
62
46
47
STRUCTURAL LOG Page 10 of 10
08-NSD-001
Assay
Sample
E466439
E466441
AU ppm
0.01
0.01
MAJOR UNIT
From
0.00
1349.00
1349.80
1359.40
1360.60
1393.70
1400.90
To
1349.00
1349.80
1359.40
1360.60
1393.70
1400.90
1409.00
From
1403.00
1404.50
To
1404.50
1405.30
MINOR UNIT
From To CommentsComments
Wedged off of DDH 07-NSD-008
Light to medium grey unusual rock with ~15%
irregular m.g qtz veins and distorted fabric.
Logged as 1 in 07-NSD-008, termed a plagioclase
porphyry due to presence of phenocrysts.
Very fine grained medium green rock consisting of
amphibole with irrgeular patches of matrix containing
25% f.g Cc.
Very coarse grained massive granite pegmatite
consisting of ~50% qtz groundmass and ~50% large
plagioclase crystals 5-30mm, minor biotite and
muscovite up to 5%.
Weakly foliated corase grained amphibolite. 80% of
the unit of the unit consists of amphibolite with
1-4mm grain size. 85% amphibole, 15% f.g
plagioclase.
Fine grained matrix of 95-100% green amphibole with
0-5% f.g plagioclase. 7ft/1.9m ground at wedge
between 1397 and 1398.9m. Weak to no foliation.
Fine grained mafic volcanic dark green in colour with
overprinted chl. & bio alt'n. associated with 2
discrete shear zones, 1404.5-1405.30 where the unit
strongly distorted mod. sz. with 20% Qzt/Carb veins
and 1-2% Po concentrated in Qtz/carb veins.
Comments
The matrix is soft with
a greenish tint and
maybe serpentine (or
other
phyllosilicate/clay)
with finer grained
patches containing
5-10% euhedral soft
meta-plag equant
porphyblasts 1-3mm.
1356.5-1357.6m
displays abundant tight
folding, parts show
fine banding 1-5mm
and 3% Po overall as
large wisps and blebs
and thin 1mm
conformable layers.
Foliated ~10cm at
contacts which are
conformable with
foliation.
F.g sparsely scattered
visible Po grains, ~0.1%.
1389.9-1399.3m is
finely banded
amphibolite containing
layers with high Po
content. 5% Po overall
in this section.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 1 of 22
Unit
No
3K
2
8F
2
2
2
Unit
08-NSD-001
Assay
Sample
E466442
E466443
E466444
E466445
E466446
E466447
E466448
E466449
E466451
E466452
E466453
E466454
E466455
E466456
E466457
E466458
E466459
E466461
AU ppm
0.01
0.01
0.01
0.01
0.01
0.01
0.01
0.02
0.01
0.00
0.01
0.01
0.01
0.02
0.00
0.01
0.01
0.00
MAJOR UNIT
From
1409.00
1411.90
1437.60
To
1411.90
1437.60
1453.70
From
1405.30
1411.90
1413.00
1413.70
1414.40
1415.00
1422.00
1423.00
1424.00
1425.00
1425.50
1436.00
1437.00
1437.60
1438.20
1439.00
1440.00
1441.00
To
1406.00
1413.00
1413.70
1414.40
1415.00
1415.70
1423.00
1424.00
1425.00
1425.50
1426.50
1437.00
1437.60
1438.20
1439.00
1440.00
1441.00
1442.00
MINOR UNIT
From To CommentsComments
UM? Unusual looking. The unit is pale in colour. The
matrix seems to have f.g. greenish micaceous
serpentine (becoming amorphous serpentine down
section) and 3-5% f.g. talc.
Meduim to Corase grained mafic volcanic with wispy
weak to moderate shear zones. 1414.4-1415.7m
contorted banding associated with weak shear zone
3-5% Po and 5-15% Carbonate
Fine grained mafic volcanic with 2 discrete shear
zones. SZ between 1437.6-1442 and
1452.5-1453.70. Both display contorted bands of
light green amphibole and qtz carbonate vns.
Comments
The unit has a mottled
texture with 20% patch
light green amphibole
alteration. 1424-1425.5
weak shear zone of
wispy contorted bands
of light green
amphibole and 30%
carbonate vning 2-3%
Po. Bull Qtz vein at
1427-1427.5.
The unit itself is fine
to medium grained with
2 bull quartz vns
between 1448.7-1449.3
and 1451.6-1452.50
Fresh looking mafic
volcanic.
ALTERATION
Bio Car
M
M
W
M
W
W
Chl Gru Hem Ser Si
W
Comments
LITHOLOGY LOG Page 2 of 22
Unit
1M
2
2
Unit
08-NSD-001
Assay
Sample
E466462
E466463
E466464
E466465
E466466
E466467
E466468
AU ppm
0.01
0.00
0.01
0.01
0.01
0.00
0.01
MAJOR UNIT
From ToFrom
1448.00
1448.70
1449.50
1450.00
1450.80
1451.60
1452.50
To
1448.70
1449.50
1450.00
1450.80
1451.60
1452.50
1453.50
MINOR UNIT
From To CommentsComments Comments
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 3 of 22
Unit Unit
08-NSD-001
Assay
Sample
E466469
E466471
AU ppm
0.01
0.02
MAJOR UNIT
From
1453.70
1508.30
1509.70
1510.40
1511.60
1527.00
1528.60
1567.80
1574.00
To
1508.30
1509.70
1510.40
1511.60
1527.00
1528.60
1567.80
1574.00
1594.90
From
1453.50
1594.00
To
1454.50
1594.90
MINOR UNIT
From
1529.00
1574.10
1591.00
To
1529.30
1577.10
1592.00
Comments
Spodumene rich pegamatite as
per 1527-1528.6m.
Massive gabbro; ~50:50
amph-plag giving a salt & pepper
texture.
Gabbro composed of ~50-50
Amph-Plag, cut by 5% thin CC
veinlets.
Comments
Grain size varies from medium to medium -coarse
grained, homogeneous fresh mafic rock with no
areas of biotisation. ~1-3% scattered 1-7mm
irregular Cc stringers
Massive non-foliated granite pegmatite with grain
size 1-5mm. Roughly 50-50 qtz and feldspar
Homogeneous moderately foliated darkish green
grey mafic rock.
Same as previous except weakly to moderately foliated.
Basalt, f.g., quite homog, foliation very weak but
often highly contorted due to weak shearing. No signif
bio'n or other alt'n. One 30cm qtz vein & Tr Cc veins,
otherwise no appreciable veins,
Spodumene rich pegamtite, ~20-30% Spod x'ls up to
5cm x 5mm in f.g.quartz-(spod) groundmass. No
visible Tantalite. Minor light yellow m.g.
muscovite/lepid and rare dark red garnets 1-3mm
throughout.
Similar to previous basalt but commonly more
pervasively weakly sheared and contorted; still no
signif bio'n. Approx 7% irreg Cc veins up to 5cm
between 1541-1567and a few minor qtz veins.
Variable section of bleached white to grey-green
basalt with 5-10% irreg dark green amph bands <1cm
thick that are probably pillow selavges.
Med grey green basalt, weak fol'n, no signif bio'n or
other alt'n. Only ~1% minor Cc veinlets and rare qtz
veins. M.g. gabbro feeder dykes/sills at 1594-1597m
and 1591-1592m with ~gradational contacts.
Comments
Fabric ranges form
massive to well
foliated, generally
weakly foliated
overall. Very minor
very f.g Po
desseminated within
the amphibole, ~0.1%.
Composed largely of
f.g. acicular green amph
(Actinolite?) and could
easily be taken for an
UM but no sign of
serp'n so logged as
basalt, prob hi-Mg or
komatiitic.
As before, it is
composed largely of
~acicular dark green
amph and much less
Fd, prob hi-Mg or
komatiitic basalt.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 4 of 22
Unit
2
8F
2
8F
2
8F
2
2D
2
Unit
8F
2K
2K
08-NSD-001
Assay
Sample
E466472
E466473
E466474
E466475
E466476
E466477
E466478
E466479
E466481
E466482
AU ppm
0.01
0.02
0.02
0.00
0.01
0.03
0.01
0.03
0.01
0.02
MAJOR UNIT
From
1594.90
1596.45
1600.10
1602.30
1603.30
To
1596.45
1600.10
1602.30
1603.30
1606.90
From
1594.90
1595.80
1596.45
1599.10
1600.10
1601.00
1601.90
1602.30
1603.30
1605.90
To
1595.80
1596.45
1597.40
1600.10
1601.00
1601.90
1602.30
1603.30
1604.30
1606.90
MINOR UNIT
From To CommentsComments
Interflow sediment, mainly a pale green-pink variety
of 4E composed of f.g.grun, minor garnets, ~5% Mt
laminae and 5-10% dark green amph laminae. Highly,
irreg folded with 1-15% Po throughout.
Ultramafic, very homog, equigranualr, composed of
~90% acic to tabular, green to black amph-pyx? and
~10% Fd. Tr Cp throughout.
Unusual unit. ~60% is off-white, siliceous metased
composed mainly of f.g. qtz, prob some vfg Fd, no
bio, plus 1-2% f.g. garnets. 30% is c.g. bands
3-10cm wide of 60% black amph and 40% garnets
with variable % interspersed relic? qtz.
Most is med to pale green banded amphibolite with
20% Mt layers up to 7mm; only minor garnets. Lesser
areas of more typical pale 4E, bleached volcanics,
possible arenite.
~massive, hi-Mg basalt as before composed largely
of m.g. acicular green amph; borderline UM but no
obvious serpentine
Comments
From ~1595.8-1596.1m
is mainly basalt with
few slivers of 4E.
Contacts with adjacent
volc are ~diffuse.
Contacts do not show
hydration reaction;
~sharp.
Gar-Amph bands have
2-5% Po veinlets and
dissem'd grains/blebs.
May be alt'n zones
(based on c.g size of
minerals and contrast
with arenite).
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 5 of 22
Unit
4E
1M
6M
4E
2
Unit
08-NSD-001
Assay
Sample
E466483
E466484
E466485
E466486
E466487
E466488
E466489
E466491
E466492
E466493
E466494
E466495
E466496
E466497
E466498
AU ppm
0.05
0.03
0.07
0.03
0.10
0.16
0.23
0.16
0.04
0.06
0.03
0.01
0.00
0.02
0.03
MAJOR UNIT
From
1606.90
1614.70
1615.30
To
1614.70
1615.30
1617.40
From
1606.90
1607.30
1607.80
1608.80
1609.50
1610.10
1610.40
1611.40
1612.00
1612.70
1613.30
1613.90
1614.70
1615.30
1616.40
To
1607.30
1607.80
1608.80
1609.50
1610.10
1610.40
1611.40
1612.00
1612.70
1613.30
1613.90
1614.70
1615.30
1616.40
1617.40
MINOR UNIT
From To CommentsComments
Unusual mix of mainly green amphibolitic IF with no
garnets and ~5% local garnet-rich patches. ~1/3 has
high % of MT in deformed layers up to 2cm thick,
most 1-3mm.
Pale grey UM composed almost entirely of f.g. to m.g.
pale green serpentine and cut by diffuse, pale green
bands of c.g. amph alt'n.
Same unusual variety of 4E as above. Mainly irreg
banded, pale to med green f.g. amphibolite with
10-25% Mt layers up to 2cm thick, no garnets in
most, one 50cm zone with 15% gar patches.
Comments
Amphibolite sections
vary from f.g. med green
to areas with hi %
overprinted pale green,
c.g. amph, incl minor
zones of possible
amph'd basalt. Several
sections up to 30 cm of
white arenite +/- gar-Po
as before.
20cm patch of ~4A like
rock, mix of chert and
yellow-green amph
bands.2-15% Po
throughout as dissem'd
grains and small
veinlets but conc'd in
bands and within prob
green amph alt'n zones.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
C.g. patches of pale
green amph throughout,
often with the Po.
LITHOLOGY LOG Page 6 of 22
Unit
4E
1S
4E
Unit
08-NSD-001
Assay
Sample
E466499
E466501
E466502
E466503
E466504
E466505
E466506
E466507
E466508
E466509
AU ppm
0.03
0.01
0.01
0.01
0.00
0.00
0.01
0.01
0.00
0.00
MAJOR UNIT
From
1617.40
1625.20
1626.00
To
1625.20
1626.00
1632.10
From
1617.40
1624.20
1625.20
1626.00
1626.80
1627.50
1628.30
1629.20
1630.00
1631.00
To
1618.40
1625.20
1626.00
1626.80
1627.50
1628.30
1629.20
1630.00
1631.00
1632.10
MINOR UNIT
From
1626.80
1628.30
To
1627.50
1629.20
Comments
Appears to be sheared 4EA.
MAinly ~f.g., massive layers of
intergrown pale pink garnets and
fg grunerite, no chert, minor Mt
laminae.
Appears to be weakly sheared
4EA. MAinly ~f.g., massive layers
of intergrown pale pink garnets
and fg grunerite, no chert, minor
Mt laminae.
Comments
Hi-Mg basalt/borderline UM as per previous Unit 2.
Composed of >90% acic med green amph, only
minor plag visible, no serpentine visible. ~1/3 has
~20% patches of 2ndary pale green c.g. amph,
Dark grey to black but still quite hard and siliceous
4H. Po conc'd in central 5-10cm, up to 20%. UC
sharp, LC gradational.
Irreg mix of ~3/4 garnet poor 4E and 1/4 4EA as
before. 4E commonly has discrete Mt laminae to
3-4mm and is sheared/banded in shades of pale and
dark green amph.
Comments
>3/4 bleached white in
lower 1m.
4EA in 2 bands <
70cm, consists of a
massive mix of pale
garnets & grunerite,
hard to distinguish
them; little on no chert
but 5% Mt laminae. Po
varies from <1% to
7%, mainly in small
veinlets or as dissem'd
grains in f.g. amph alt'n
zones or shears.
ALTERATION
Bio
W
Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 7 of 22
Unit
2
4H
4E
Unit
4EA
4EA
08-NSD-001
Assay
Sample
E466511
E466512
E466513
E466514
E466515
E466516
E466517
E466518
E466519
E466521
E466522
E466523
E466524
AU ppm
0.05
0.10
0.08
0.02
0.16
0.03
0.01
0.02
0.03
0.02
0.01
0.01
0.01
MAJOR UNIT
From
1632.10
1632.90
1633.30
1634.80
1638.10
1638.60
1642.40
To
1632.90
1633.30
1634.80
1638.10
1638.60
1642.40
1664.30
From
1632.10
1632.90
1633.30
1637.00
1638.10
1638.60
1639.10
1640.00
1641.00
1641.40
1642.40
1643.40
1644.10
To
1632.90
1633.30
1634.00
1638.10
1638.60
1639.10
1640.00
1641.00
1641.40
1642.40
1643.40
1644.10
1645.00
MINOR UNIT
From
1643.40
To
1644.10
Comments
Garnet-poor 4, a few garnet-rich
bands 1-2cm but mosy is tinly
banded green amphibole BIF.
Minor grunerite-rich layers but
less than "4E" above. 7% Po over
last 10cm.
Comments
Similar quartzose metased as before. Off-white,
f.g., eqigran, composed mainly of qtz, minor Fd,
Gar, prob ~10-20% white acicular amph 1-2mm. No
major gar-amph alt'n bands ike previous section.
Well developed 4H with 30-40% white chert layers
<7mm and 60-70% graphitic argillite laminae. ~20%
Po throughout as dissem'd grains, broken veinlets, etc.
Same siliceous metased - arenite - as before,
composed largely of f.g. Qtz, leser Fd, minor
Sericite. A few minor, <few mm thick, alt'n veins of
amph-bio with flanking Po-(Cp) veinlets <2-3mm thick.
Either a ~f.g. gabbro or a c.g. basalt; consists of
~50:50 dark green amph and plag. First 1/2 is
massive, rest becomes sheared and rubbly from
1637-1637.6m.
Well developed Po-rich meta- cherty argillite. Dark
grey-black, thinly lam'd with ~20% thin cherty layers,
7-10% Po throughout.
As before, not a true 4E due to lack of garnets but
consists of thinly banded green amphibole and ~
equal green-yellow grunerite (?) so is a related
amphibolitic BIF.
Fairly massive, m.g. basalt, very fresh looking
other than local Cc veins. Composed of 70-80%
green amph, 20-30% f.g. plag. Prob Hi-Mg basalt,
borderline UM.
Comments
20cm Qtz vein in
sheared part at
~1637.2m.
Only a few small
bands, 1-3cm, with
garnets (>50%). Cut by
a 5cm qtz-po vein at
1641.2m and 2cm Po
vein at LC.
No discernible foliation
except in one minor
shear zone.
ALTERATION
Bio
W
Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 8 of 22
Unit
6M
4H
6M
2
4H
4E
2
Unit
4E
08-NSD-001
Assay
Sample
E466616
E466617
E466618
E466525
E466526
E466527
AU ppm
0.01
0.05
0.02
0.00
0.00
0.00
MAJOR UNIT
From
1664.30
1664.70
1669.20
1672.90
1775.00
1802.00
To
1664.70
1669.20
1672.90
1775.00
1802.00
1860.00
From
1663.30
1664.30
1664.70
1757.00
1757.70
1758.20
To
1664.30
1664.70
1665.70
1757.70
1758.20
1758.80
MINOR UNIT
From
1676.30
To
1678.00
Comments
Lightgrey,~mottled serpentinite
composed almost entirely of f.g.
to m.g. micaceous to acicular plae
green to white serpentine.
Comments
Highly contorted garnet-poor 4E as before, only rare
garnets in this thinly banded, pale to dark green
amphibolite. Mod qtz veins/floods with up to 10%
Po and minor Cc/10cm.
Very f.g. dark grey to black pillowed basalt with ~5%
irreg selvages 0.5-2cm wide.
Another unusual type of chem sed, mainly m.g. pale
to dark green acicular amph, prob actinolite?, and no
garnets. Contains a 30cm serpentinite.
Massive to weakly foliated pillowed basalt. Approx
3% pillow selvages up to 1cm composed of dark
amph-bio+/-pale green amph & rare garnets.
Well folaited basalt, varies from f.g., homog,
sections to somewhat bleached sections with 35%
green amph clots 2-4mm long in an off-white matrix
of plag>amph (separation of minerals due to weak
shearing, giving a ~mottled, spotted look).
Massive to weakly foliated, very homogeneous, med
grey basalt. A few scattered pillow selvages (?) and
a great pillow brx / hyaloclastite from
1804.5-1805.5m. No signif shearing,bio alt'n or veins.
Comments
Could be logged as UM
itself except for thin
Mt laminae, lack of
serp'n and similarity to
previous more obvious
chem seds. Only rare
grains of Po and Cp.
Basalt is composed of
~60% f.g. ~equant dark
green amph, 40% vfg
plag. Only local small
areas of weak bio'n,
rest is quite fresh.
Only weak local
shears. 2 qtz veins @
~1757-8m.
Several intervals 1-2m
wide have weak-mod
bio alt'n in 1-3mm clots
aligned with fol'n;
locally almost a 2T.
Great intervals of
pillow brx /
hyaloclastite from
1796-1797m. A few Cc
veins to 30cm but no qtz.
Still ~60:40 to 50:50
Amph:Plag,
equigranualar.
ALTERATION
Bio Car Chl Gru Hem Ser Si
S
Comments
LITHOLOGY LOG Page 9 of 22
Unit
4E
2
4E
2D
2
2
Unit
1S
08-NSD-001
Assay
Sample
E466528
E466529
E466531
E466532
E466533
E466534
E466535
E466536
E466537
E466538
E466539
E466541
E466542
E466543
E466544
E466545
AU ppm
0.00
0.01
0.01
0.01
0.03
0.01
0.00
0.02
0.54
0.29
0.36
0.69
0.36
0.86
0.07
0.01
MAJOR UNIT
From
1860.00
1866.55
1880.00
1882.00
1884.40
1886.70
1887.00
To
1866.55
1880.00
1882.00
1884.40
1886.70
1887.00
1901.00
From
1859.00
1860.00
1860.70
1864.00
1864.95
1865.95
1866.55
1881.00
1882.00
1883.00
1884.00
1884.40
1885.40
1886.25
1886.70
1887.00
To
1860.00
1860.70
1861.70
1864.95
1865.95
1866.55
1867.55
1882.00
1883.00
1884.00
1884.40
1885.40
1886.25
1886.70
1887.00
1888.00
MINOR UNIT
From
1880.80
To
1889.80
Comments
Off-white to light grey, very
siliceous unit with <5% vfg biotite,
no visible Fd. Either a clastic or
chemical sed quartzite.
Comments
Continuation of basalt from above but now has
multiple zones of Po mineral'n. Possibly these are
4H-type (with only minor argillite though) but most are
either assoc'd with green amph +/- Cc "Veins" or frax
fillings in basalt, do not appear syngenetic.
Massive to mod foliated basalt as before. Med grey,
very homogeneous, equigranular, little or no bio'n.
Unusually balck and f.g. homog looking unit,
composed of ~30-40% f.g. bio flakes in a vfg pale
green groundmass (bleached, sheared basaltic?)
Solid qtz vein with minor Cc filled frax cutiing it,
prob no original Cc in the vein. Unusually hi % of
Asp scattered throughout + minor Po. Up to 2% m.g.
to c.g. Asp over 30cm as veinelts and dissem grains.
~60% white chert with 20% pale green to yellow amph
/ grun diffuse layers <1cm. Unit is mod sheared and
laced with ~15% Cc veinlets, 2-3% each Asp and Po
veinlets.
Typical thinly laminated chert-Mt 4B of the Southern
IF. LC ~obscured by rubbly core, prob sheared.
Well foliated basalt, often with streaked out clots of
green amph <3-4mm long in the ~bleached matrix.
Only minor, local bio'n so far.
Comments
One zone has ~15%
qtz veins up to 5cm
but most min'd areas
do not have any qv. Po
appears to be
secondary and
~cross-cutting.
Mod magnetic
throughout. Alt'n and
veining obscures much
of typical 4A textures.
No major alt'n, veins or
sulphides. Prob a weak
shear zone.
ALTERATION
Bio
S
Car
S
Chl Gru Hem Ser Si Comments
~15% Cc frax fillings
and veinlets.
LITHOLOGY LOG Page 10 of 22
Unit
2
2
2T
QTZ
4A
4B
2
Unit
4CH
08-NSD-001
Assay
Sample
E466546
E466547
E466548
E466549
E466551
E466552
E466553
E466554
E466555
E466556
E466557
E466558
E466559
E466561
E466562
E466563
E466564
E466565
E466566
E466567
E466568
E466569
E466571
AU ppm
0.01
0.01
0.01
0.09
0.24
0.12
0.17
0.05
0.05
0.04
0.01
0.01
0.07
0.04
0.00
0.00
0.00
0.00
0.00
0.10
0.01
0.01
0.00
MAJOR UNIT
From
1901.00
1903.00
1903.40
1908.20
1919.10
To
1903.00
1903.40
1908.20
1919.10
1920.10
From
1901.00
1901.80
1902.20
1903.00
1903.40
1904.40
1905.00
1905.60
1906.60
1907.70
1908.20
1909.00
1910.00
1910.70
1911.20
1912.00
1913.00
1914.00
1915.00
1915.90
1916.70
1917.70
1918.70
To
1901.80
1902.20
1903.00
1903.40
1904.40
1905.00
1905.60
1906.60
1907.70
1908.20
1909.00
1910.00
1910.70
1911.20
1912.00
1913.00
1914.00
1915.00
1915.90
1916.70
1917.70
1918.70
1919.70
MINOR UNIT
From To CommentsComments
Med - darkgreen, f.g., very homog, equigranular unit
composed of ~40% f.g. bio flakes in a vfg pale green
matrix. Probably a 2T but much more f.g. and
equigranular than normal.
Typical well developed black Po-rich argillte. Cut by
10cm qv // to fol'n. ~15% Po overall.
Well developed 4A composed of 60-70% white chert.
30-40% pale green-yellow grunerite in diffuse bands
up to 3-4cm wide. LC gradational over 1.5m into 4B
with increasing, dissem'd Mt, sharp break into
banded 4B though.
Typical thinly laminated 4B of the Southern IF,
composed of alternating MT layers and pale
yello-white layers of mixed vfg chert.and lesser
grunerite.
Unusual, very uncertain unit. ~60% is bands of ~15%
ragged garnets 5-10nn in f.g. micaceous matrix of
pale green chlorite (?) and/or acicular pale
amphiboles; this is prob intense hydrothermal alt'n.
Comments
Upper 2m has ~1-2%
Asp and 1-5% Po in
frax fillings / veinlets
~2-5mm wide. A few
scattered qtz veins up
to 20cm also contain
blebs of Asp-Po, up to
5%.
Generally barren, no
major shears, only 2
noteworthy Qtz-Po
veins, both <15cm wide
though. LC ~sharp.
~10% bands <1cm of
solid Mt; rest is ~cherty
BIF, more like a 4A.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 11 of 22
Unit
2T
4H
4A
4B
4B
Unit
08-NSD-001
Assay
Sample
E466572
E466573
E466574
E466575
E466576
E466577
E466578
E466579
E466581
E466582
E466583
E466584
E466585
E466586
E466587
E466588
E466589
AU ppm
0.01
0.01
0.01
0.02
0.00
0.07
0.00
0.00
0.00
0.00
0.00
0.00
0.06
0.01
0.00
0.06
0.01
MAJOR UNIT
From
1920.10
1937.50
1947.50
1955.30
1969.50
To
1937.50
1947.50
1955.30
1969.50
1980.30
From
1919.70
1920.10
1946.50
1947.50
1948.00
1949.00
1950.00
1951.00
1952.00
1953.00
1954.00
1954.90
1955.30
1955.80
1977.80
1978.80
1979.30
To
1920.10
1921.10
1947.50
1948.00
1949.00
1950.00
1951.00
1952.00
1953.00
1954.00
1954.90
1955.30
1955.80
1956.80
1978.80
1979.30
1979.80
MINOR UNIT
From To CommentsComments
Generally med dark grey, f.g.,equigranular, very
homog basalt. Massive to weakly foliated with a few
pillow selavages <1cm wide. No appreciable bio'n
except weak amount in upper 1-2m.
Light to med grey basalt, weak-mod foliation
throughout with mod bleaching to off-white colour in
central 3m. Weak-mod bio'n in lower 4.5m, almost a
2T locally.
Southern IF 4B composed of black Mt layers and
pale beige-yellow chert-(grun) layers. Mt % higher
than most, often ~70%. Unit has ~common shear
induced transpostion/intrafolial folds as well as many
parasitic folds.
Variable section of light grey to grey-green basalts
but generally fresh with only minor local bio'n. Upper
50cm is highly qtz veined with flanking c.g.
garnet-green amph alt'n.
Typical light grey serpentinite, ~mottled in shades of
grey, no obvious talc, non-magnetic. Composed
~entirely of pale green to white serpentine.
Comments
Composed of f.g.
amph-plag mix, prob
tholeiite, not hi-Mg.
Only one small zone,
10cm, with minor Po
min'n. Lower 40cm
similar to base of
previous 4B: cut by
gar-amph c.g. alt'n
bands and some pale
green cg amph bands.
LC ~sharp, within
~1-2cm.
No major veins. A
sinlge 1-2cm thick
vein/frax filling of
Po-Cp in lower 50cm.
ALTERATION
Bio
M
Car Chl Gru Hem Ser Si
S
Comments
LITHOLOGY LOG Page 12 of 22
Unit
2
2
4B
2
1
Unit
08-NSD-001
Assay
Sample
E466591
E466592
E466593
E466594
E466595
E466596
E466597
E466598
E466599
E466601
E466602
E466603
E466604
E466605
E466606
E466607
E466608
E466609
E466611
E466612
E466613
E466614
AU ppm
0.01
0.03
0.02
0.01
0.45
0.04
0.03
0.03
0.02
0.00
0.05
0.00
0.03
0.00
0.01
0.01
0.01
0.01
0.02
0.01
0.02
0.03
MAJOR UNIT
From
1980.30
1991.10
1995.50
To
1991.10
1995.50
2013.20
From
1979.80
1980.80
1981.80
1983.00
1983.50
1984.30
1985.30
1986.00
1987.00
1988.00
1989.00
1989.60
1990.60
1991.10
1992.00
1993.00
1994.00
1995.00
1996.00
1997.00
1998.00
1999.00
To
1980.80
1981.80
1983.00
1983.50
1984.30
1985.30
1986.00
1987.00
1988.00
1989.00
1989.60
1990.60
1991.10
1992.00
1993.00
1994.00
1995.00
1996.00
1997.00
1998.00
1999.00
1999.50
MINOR UNIT
From To CommentsComments
Typical SIF 4B as above, alternating black Mt layers
up to 1-2cm thick and pale yellow-beige chert-(grun)
laminae. Moderate intrafolial folding (shear-induced
transposition).
White to light grey 4A, varies from 90% chert to more
typical diffusely banded sections of ~50:50 chert and
green-yellow amphibole (grun?).
Mod to well foliated basalt with weak-mod bio alt'n.
Locally borders on being a 2T. A few short sections
<30cm that may be hi-Mg type but most is typical
~50:50 Amph-plag basalt.
Comments
A few minor qtz veins
with minor Po, <7cm
wide though. LC
gradational over 2-3m
into 4A.
Mod magnetic due to
f.g. dissem'd and/or
thin laminae of Mt.
Several zones 1-2m
with ~10% small qtz
veins and minor Po.
No significant veins or
other alt'n.
ALTERATION
Bio
W
Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 13 of 22
Unit
4B
4A
2
Unit
08-NSD-001
Assay
Sample
E466615
E466619
E466621
E466622
E466623
E466624
E466625
E466626
E466627
E466628
E466629
E466631
E466632
AU ppm
0.01
0.01
0.01
0.11
0.07
0.05
0.02
0.03
0.13
0.00
0.05
0.16
0.01
MAJOR UNIT
From
2013.20
2021.20
2045.20
2054.75
2066.90
2074.20
To
2021.20
2045.20
2054.75
2066.90
2074.20
2085.10
From
1999.50
2065.00
2066.00
2066.90
2067.80
2068.50
2069.00
2070.00
2071.00
2072.00
2073.00
2073.60
2074.20
To
2000.50
2066.00
2066.90
2067.80
2068.50
2069.00
2070.00
2071.00
2072.00
2073.00
2073.60
2074.20
2075.00
MINOR UNIT
From To CommentsComments
As before, ~massive serpentinized UM composed
almost entirely of pale green serpentine. LC hard to
discern, +/- 50cm. Some portions weakly magnetic.
Well foliated, mod bio'd basalt bordering on 2T. Bio'n
varies from weak to strong and gives a hetero look to
the rock. Matrix is still greenish.
Serpentinized ultramafic; light green to greyish blue
and medium to coarse grained. Strong Calcite
veining which is fibrous. The matrix of the unit has a
pittted texture.
Biotite rich mafic volcanic with weak to moderate
calcite veining. From 2060 appear to have been a
mislatch and the core is ground for 1.2 m There is an
increase in biotite slips down section and a decrease
in the amount of calcite stringers.
Grey to light green in colour. Moderately magnetic ,
heterogeneous 4A, that varies from 80% chert to
60% chert and 40% grunerite with minor green
amphibole. Minor Decimetre scale fold between
2069-2070
Biotite rich mafic volcanic with minor biotite slips and
weak calcite veining.
Comments
Foliation is often
contorted, local minor
amph alt'n. Biotite
increases down section
and the unit is light
brown with an increase
in Calcite veining .
Fracture surface have
talc present. Down hole
the unit becomes more
fine grained.
~30 laminated
magnetic wispy bands
of magnetite though out
the unit. Mineralization
consists of Po
associated with light
green amphibole
alteration
ALTERATION
Bio
M
M
M
W
M
Car
M
M
M
W
Chl
W
Gru
W
Hem Ser Si Comments
LITHOLOGY LOG Page 14 of 22
Unit
1
2
1
2
4A
2
Unit
08-NSD-001
Assay
Sample
E466633
E466634
E466635
E466636
E466637
E466638
E466639
AU ppm
0.00
0.00
0.01
0.02
0.02
0.01
0.01
MAJOR UNIT
From
2085.10
2086.00
2088.10
2114.90
To
2086.00
2088.10
2114.90
2119.60
From
2075.00
2112.90
2113.90
2114.90
2115.50
2116.20
2116.90
To
2076.00
2113.90
2114.90
2115.50
2116.20
2116.90
2117.90
MINOR UNIT
From To CommentsComments
Very soft coarse grained serpentinised ultramafic with
remnant m.g to c.g (1-3mm) texture still visible.
Moderately foliated and very easy to scratch.
Moderately biotised brown mafic rock with 10-35% f.g
biotite alt'n within a sheared matrix. The matrix is
variable and contains bands 1mm-10cm varying from
light green soft chlorite alt'd biotised rock to a brown
biotised harder amphibole rock.
Pale green-grey, f.g and weakly to moderately
foliated. Biotite is completely absent and numerous
sections of the unit up to 3m long a weakly to
moderately serpentised with abundant serpentine on
many joint surfaces.
Homog', weakly magnetic unit consisting of
alternating bands 1-3cm of (slightly orange) chert
(~35%), with thin 10% Mt-grun bands 3-20mm, and
55% greenish-light brown bands 5-30mm of grun &
green amph. Lower 50cm is sheared & mod
magnetic, could be 4B.
Comments
Biotite content is higher
in the softer light
green-grey alt'd
bands/patches. 10%
elongate wisps of qtz
1-10cm long. It is
possible the chlorite
alt'n is actually
serpentine. No
carbonate.
1-3% patchy irregular
carbonate alt'n as small
patches or veinlets
<1cm. Sharp contact
with the sheared brown
biotised 2 at the UC.
Lower 2m is hard, f.g
and not as strongly UM.
Some of the chert
bands are finely
laminated. No shears,
no qtz/Cc veins/alt'n
or min'zn just
scattered specks of Po
throughout much of the
unit, 0.1% Po. Higher
abundance of 40-50%
Mt bands
2119.6-2120.5m
borderline 4B.
Lamporphyre offshoot
2122-2122.1m
ALTERATION
Bio
S
Car
W
W
Chl
S
Gru Hem Ser
S
W
S
W
Si
W
Comments
LITHOLOGY LOG Page 15 of 22
Unit
1
2T
1
4A
Unit
08-NSD-001
Assay
Sample
E466641
E466642
E466643
E466644
E466645
E466646
E466647
E466648
E466649
E466651
AU ppm
0.00
0.00
0.00
0.01
0.01
0.02
0.00
0.01
0.01
0.01
MAJOR UNIT
From
2119.60
2124.00
To
2124.00
2164.40
From
2117.90
2119.00
2119.60
2120.70
2121.70
2122.50
2123.30
2124.00
2162.40
2163.40
To
2119.00
2119.60
2120.70
2121.70
2122.50
2123.30
2124.00
2125.00
2163.40
2164.40
MINOR UNIT
From To CommentsComments
Homogeneous, black, crosscutting dyke, fairly
equigranular.Grains are mainly ~ 0.3-1mm and
consist of phlogopite, a white soft mineral, and black
rounded grains (serp/olivine) with a very fine dark
brown to black groundmass (~30% of the rock).
Completely serpentinised ultramafic unit with serp'd
frax every 20-50cm, especially from UC-2126m.
Moderately foliated to massive non-foliated texture,
generally light grey or off-white to locally light green
or med grey.
Comments
Phlogopite is the most
abundant mineral and
may make up ~30-35%
of the rock. The rock
contains about 5-10%
Cc distributed as tiny
<1mm stringers and
also desseminated
throughout the matrix.
10cm inclusion of 4A
at 2122.9-2123m.
~2/3 is non-magnetic
but 1/3 has dissem'd
clots of Mt ~1-4mm in
zones 2-5m wide; no
obvious laminae/layers
of Mt or any sulphides.
No obvious change in
comp from top to
bottom. LC sharp with
~1/2 cm reaction zone
of dark green amph?
ALTERATION
Bio Car Chl Gru Hem Ser
S
Si Comments
LITHOLOGY LOG Page 16 of 22
Unit
13
1
Unit
08-NSD-001
Assay
Sample
E466652
E466653
E466654
E466655
E466656
E466657
E466658
E466659
E466661
E466662
E466663
E466664
E466665
E466666
E466667
E466668
E466669
E466671
E466672
E466673
E466674
AU ppm
0.38
0.17
0.01
0.01
0.01
0.00
0.02
0.12
0.02
0.01
0.01
0.05
0.03
0.01
0.01
0.01
0.01
0.01
0.05
0.02
0.04
MAJOR UNIT
From
2164.40
2165.90
2183.00
To
2165.90
2183.00
2220.30
From
2164.40
2165.20
2165.90
2166.90
2168.00
2169.00
2170.00
2171.00
2172.00
2173.00
2174.00
2175.00
2176.00
2177.00
2178.00
2179.00
2180.00
2181.00
2182.00
2183.00
2184.00
To
2165.20
2165.90
2166.90
2168.00
2169.00
2170.00
2171.00
2172.00
2173.00
2174.00
2175.00
2176.00
2177.00
2178.00
2179.00
2180.00
2181.00
2182.00
2183.00
2184.00
2184.80
MINOR UNIT
From To CommentsComments
Mod sheared Chert-Grun-Mt BIF, only diffuse remnant
layering, the vfg spotted Mt grains in chert-grun
matrix resembles SIF more than NIF. Consists of
~50% f.g. Mt as dissem'd grains <2mm or as
streaked out laminae in a matrix of f.g. grun > chert.
Light grey, quite distorted 4A composed of light grey
weakly magnetic chert and light yellow mod magnetic
grunerite. No major qtz veins or Po. ~5 serpentine
veins <7mm wide cutting the 4A; rare green amph-Po
alt'n patches.
Distorted 4A (folded), locally foliated. fairly similar
to previous 4A unit. Consists of alternating pale
yellow grunerite rich bands averaging 0.5cm wide and
chert bands up to 1cm wide. Locally, the unit is
weakly Qtz flooded/veined (up to 2-3%)
Comments
First 60 cm has 3 qtz
veins 2-10cm wide with
~2% Po, LC is
gradational over 20cm
into 4A
Grunerite occurs as
~discrete layers
<2-3cm, wispy streaks,
and ~pervasive bands
up to 20-30cm; varies
from ~50-80%, rest is
chert.
The unit is folded in
several places (changes
in the foliation). S2
cleavages locally well
developed (perp. to
fol). 3-5% Cc flooded in
some places. Po
scattered throughout in
veins or within
fractures (increases in
Qtz flooded zones).
ALTERATION
Bio Car Chl Gru Hem Ser Si
W
Comments
locally, qtz veined 4A
LITHOLOGY LOG Page 17 of 22
Unit
4B
4A
4A
Unit
08-NSD-001
Assay
Sample
E466675
E466676
E466677
E466678
E466679
E466681
E466682
E466683
E466684
E466685
E466686
E466687
E466688
E466689
E466691
E466692
E466693
E466694
E466695
E466696
E466697
E466698
E466699
E466701
E466702
E466703
E466704
E466705
E466706
E466707
E466708
E466709
E466711
E466712
E466713
E466714
E466715
E466716
E466717
E466718
AU ppm
0.02
0.01
0.01
0.00
0.00
0.01
0.01
0.01
0.03
0.07
0.63
0.29
0.66
0.07
0.04
0.88
0.03
0.03
0.03
0.02
0.03
0.09
0.02
0.01
0.02
0.01
0.04
0.00
0.09
0.06
0.02
0.01
0.00
0.00
0.00
0.00
0.01
0.30
0.08
1.12
MAJOR UNIT
From ToFrom
2184.80
2185.80
2186.50
2187.00
2188.00
2189.00
2190.00
2191.00
2192.00
2193.00
2193.70
2194.20
2194.80
2195.40
2196.00
2197.00
2198.00
2199.00
2200.00
2201.00
2202.00
2202.70
2203.70
2204.50
2205.00
2206.00
2207.00
2208.00
2209.00
2210.00
2211.00
2212.00
2213.00
2214.00
2215.00
2216.00
2217.00
2218.00
2218.80
2219.70
To
2185.80
2186.50
2187.00
2188.00
2189.00
2190.00
2191.00
2192.00
2193.00
2193.70
2194.20
2194.80
2195.40
2196.00
2197.00
2198.00
2199.00
2200.00
2201.00
2202.00
2202.70
2203.70
2204.50
2205.00
2206.00
2207.00
2208.00
2209.00
2210.00
2211.00
2212.00
2213.00
2214.00
2215.00
2216.00
2217.00
2218.00
2218.80
2219.70
2220.30
MINOR UNIT
From To CommentsComments Comments
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 18 of 22
Unit Unit
08-NSD-001
Assay
Sample
E466719
E466721
E466722
E466723
E466724
E466725
E466726
E466727
E466728
E466729
E466731
E466732
E466733
AU ppm
0.02
0.01
0.21
0.20
0.04
0.00
0.01
0.14
0.02
0.15
0.02
0.01
0.01
MAJOR UNIT
From
2220.30
2225.10
2239.50
2242.70
2243.00
2244.00
To
2225.10
2239.50
2242.70
2243.00
2244.00
2246.60
From
2220.30
2221.30
2237.50
2238.50
2239.50
2240.00
2241.00
2242.00
2242.70
2243.00
2244.00
2245.00
2246.00
To
2221.30
2222.30
2238.50
2239.50
2240.00
2241.00
2242.00
2242.70
2243.00
2244.00
2245.00
2246.00
2246.60
MINOR UNIT
From To CommentsComments
Varies from massive ultramafic in the first 4m to
foliated unit in the lower part of the section. The
matrix in mainly composed of fibrous planar
serpentine. The lower part displays black soft
elongated mineral. Might be another serpentine
(isomorph?).
2?2T?UM? The unit is different from previous unit by
the content of bio slips up to 10% (1mm wide). The
matrix seems to be coarser grained than usual 2 and
seems to be more fibrous. The unit is cut by 5% Cc
veins ranging from 0.3-0.5cm wide.
Well foliated, well developed 4A. The unit is
slightly magnetic and displays 80% pale yellow
f.g.-m.g.grunerite rich bands averaging 1cm wide and
chert/Qtz bands/veins up to 1cm wide. Weak green
amph alt'n locally.
4E? small unit within the 4A package. The unit does
not have any grunerite and consists of 80% dark
green amph and 20% pale green amph. The unit
displays also 2% f.g. garnets. unit is slightly
magnetic. No mineralisation.
Well developed 4A. The unit is weakly Qtz flooded
and displays 70-80% pale-medium yellow grunerite
rich bands. ~1% dark grey Mt rich bands up to
0.5cm wide. The unit contains 2-3% Qtz flooding in
the last 50cm.
Fairly fresh grey-green mafic volcanic with 60-70%
f.g.green amphiboles. The unit displays nil-weak
biotite alt'n throughout up to 25 locally. The unit
contains a 10 cm ITF 4E with1% Po (@2246.2m).
Comments
No significant veining.
The lower contact is
diffuse.
In some places, it is
possible to identify
amphiboles. The lower
contact is sharp
@60dca.
The unit contains
2-3% Mt grains
overprinting the gru
(alt'n?). The unit is cut
by 1% Qtz veins. No
significant
mineralisation. The
lower contact is diffuse.
Probably not a real 4E
but different from 4A
above and below. The
lower contact is sharp
~ 80dca.
The lower contact is
sharp @ 75dca.
The unit is cut by 1%
Qtz-Cc veins up to
1cm wide. The lower
contact is diffuse.
ALTERATION
Bio
M
Car Chl Gru Hem Ser Si
W
Comments
UM with serpentine
mafic volcanic, few Cc
veins
4A
pale green amph alt'n
weakly qtz flooded in the
last 50cm
fairly fresh mafic volcanic
LITHOLOGY LOG Page 19 of 22
Unit
1
2
4A
4E
4A
2
Unit
08-NSD-001
Assay
Sample
E466734
E466735
E466736
E466737
E466738
E466739
E466741
E466742
AU ppm
0.01
0.01
0.01
0.01
0.67
0.03
0.06
0.03
MAJOR UNIT
From
2246.60
2247.90
2248.60
2250.30
2250.70
To
2247.90
2248.60
2250.30
2250.70
2261.00
From
2246.60
2247.00
2247.90
2248.60
2249.20
2249.70
2250.30
2250.70
To
2247.00
2247.90
2248.60
2249.20
2249.70
2250.30
2250.70
2251.70
MINOR UNIT
From To CommentsComments
Weakly developed 4E, seems to be a mix with mafic
volcanic (<5%). the unit is a garnet poor 4E and
displays well foliated and distorted dark green amph
rich bands up to 3cm wide. Strong pale green amph
alt'n throughout.
Weakly-mod developed 4A, consisting of dark yellow
grunerite rich bands up to 1.5cm wide. The unit
contains 5-10% Mt throughout. locally, the unit
displays pale green amph and not grunerite. The unit
contains minor Po and traces As.
Mix 4B/4A. The unit consists of alternating dark
yellow grunerite rich bands averaging 0.5cm wide and
dark grey/black Mt rich bands up to 0.8cm wide
(50/50). The unit looks like 4B SIF type
intercalated with 4A bands. 1Po vein 3cm wide @
2249.7m
4A? The unit is not magnetic and displays 20%
grunerite overall. Presence of carbonate as well. The
unit contains black bands, (might be 4H?) up to
0.5cm wide. The unit is well mineralised and
contains ~20-25% Po stringers.
Fine grained to medium grained mafic volcanic. The
unit consists of 50% green amph (locally m.g) and
50% plagioclases. Nil-weak biotite alt'n throughout
(<2%). no significant veining.
Comments
From 2247m over
50cm, the unit contains
only 2% 4E bands and
the rest is light and
seems to be composed
of amph and biotite
slips. The unit
contains <1% scattered
po throughout.
The lower contact is
gradational.
one minor 4E unit over
10cm. The unit
displays 1-2%
disseminated Po
throughout. Locally, the
unit is weakly sheared
over 20cm (tight folds
present). The lower
contact is diffuse.
The lower contact is
sharp @ 65dca.
ALTERATION
Bio
W
Car
W
Chl Gru
M
Hem Ser Si Comments
pale green amph alt'n
LITHOLOGY LOG Page 20 of 22
Unit
4E
4A
4B
4A
2
Unit
08-NSD-001
Assay
Sample
E466743
E466744
E466745
E466746
E466747
E466748
E466749
E466751
E466752
E466753
AU ppm
0.01
0.02
0.14
0.01
0.00
0.00
0.04
0.02
0.01
0.00
MAJOR UNIT
From
2261.00
2301.40
2311.80
2313.60
2321.20
2334.10
To
2301.40
2311.80
2313.60
2321.20
2334.10
2336.00
From
2251.70
2266.00
2267.00
2267.40
2309.80
2310.80
2311.80
2312.80
2313.60
2314.60
To
2252.70
2267.00
2267.40
2268.40
2310.80
2311.80
2312.80
2313.60
2314.60
2315.60
MINOR UNIT
From To CommentsComments
Fine grained to medium grained mafic volcanic.
Alternating foliated mafic volcanic to more massive
unit with m.g.amph and plagioclases (gabbro
texture). Overall, the unit consists of 60%
plagioclase and 40% green amph (might be
pyroxenes?).
Massive medium-dark grey mafic volcanic, fairly
fresh unit. Hard to see any minerals (v.f.g). The
matrix seems to be composed of 60% amph and 40%
plagioclase.
Fine grained, dark grey, hard metapelite matrix of qtz
with very f.g biotite + possible graphite. 10-15%
wispy Po throughout the unit.
Fine to medium grained green grey mafic rock with
3% patches of Cc alt'n and small irregular Cc
veinlets. 2% patchy biotite alt'n. Couple patches of
Po min'zn in upper 2m.
Massive to mdoerately foliated m.g to very coarse
grained amphibole 2-7mm with a 5-15% interstitial
matrix of plagioclase. Finer grained patches are more
foliated.
Moderately to very well foliated green-grey mafic
with ~5% Cc sub-planar veinlets 1-5mm and a
couple Cc veins up to 15cm.
Comments
Weak chlorite (?) alt'n
locally overprinted by
another amphibole.
The unit is cut by 2%
Cc veins averaging
0.5cm wide. From
2267-2267.4m, 10% Po
in veins (some black
bands, might be 4H?).
LC is gradational.
No significant alt'n.
2319.3-2319.6m has
30% qtz veining with
two 2cm bands of light
green chlorite with
1-2mm Mt grains, and
a 3cm Cc vein.
In the very coarse
patches the amphibole
is greenish- brown.
2339-2346m is
extremely well foliated
and much finer grained
than the rest due to the
high strain. Not really
a shear zone though.
ALTERATION
Bio
W
W
Car
W
W
Chl Gru Hem Ser Si Comments
no significant alt'n
fresh mafic volcanic,
massive
weak alt'n around veinlets.
LITHOLOGY LOG Page 21 of 22
Unit
2
2
4H
2
7A
2
Unit
08-NSD-001
Assay
Sample AU ppm
MAJOR UNIT
From
2336.00
2393.40
2393.70
2403.00
To
2393.40
2393.70
2403.00
2441.00
From To
MINOR UNIT
From To CommentsComments
Moderately to well foliated, homogeneous green grey
fresh f.g to m.g mafic rock with 5-8% Cc veinlets.
2375-2386m has ~1-2% scattered bands and wisps
3-7mm wide consiting of biotite & gnts 3-5mm.
M.g brown dyke consisting of abundant phlogopite
(>50%) with ~25-30% white crystalline minerals
(some appear rounded, some are soft white alt'd -
serp'd olivine grains)
Moderately to well foliated green grey fresh mafic
rock. 3% Cc veinlets.
Moderately to well foliated green grey mafic rock with
1% scattered small patches of weak biotite. The rock
is very fresh and contains ~3-5% Cc veinlets and
weak alt'n patches.
Comments
5% qtz veins <5cm
2354-2360m.
Rare bands 5-20mm of
biotite-garnet, 3-5mm
euhedral garnets.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 22 of 22
Unit
2
13
2
2
Unit
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
0
3
6
9
12
15
18
21
24
27
30
33
36
39
42
45
48
51
54
57
60
63
66
69
72
75
78
81
84
87
90
93
96
99
102
105
108
111
114
117
120
123
126
129
132
135
138
141
144
147
150
153
156
159
Azimuth
84.169
84.3
85.2
86.2
87.3
88.2
89.3
89.2
89.4
89.7
89.7
89.5
90.3
89.5
90.2
90.8
91.5
91.7
91.5
91
91.8
92
92.2
91.9
91.6
91.9
92.1
92.3
91.8
91.8
92
91.8
91.9
92.3
92.8
92.6
92.6
92.3
92.3
92.7
93
93.2
92.9
92.7
92.2
92.1
92.1
92.3
92.4
92
92.3
92.5
92.2
92.4
Dip
-85.729
-85.7
-85.7
-85.7
-85.7
-85.5
-85.5
-85.5
-85.5
-85.5
-85.5
-85.5
-85.5
-85.4
-85.4
-85.4
-85.4
-85.5
-85.4
-85.4
-85.4
-85.4
-85.4
-85.4
-85.4
-85.4
-85.3
-85.3
-85.3
-85.3
-85.3
-85.3
-85.3
-85.3
-85.3
-85.2
-85.2
-85.2
-85.2
-85.1
-85.1
-85.1
-85.1
-85
-85
-85
-85
-85
-85
-85
-84.9
-85
-85
-85
SurveyType
SURV
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
162
165
168
171
174
177
180
183
186
189
192
195
198
201
204
207
210
213
216
219
222
225
228
231
234
237
240
243
246
249
252
255
258
261
264
267
270
273
276
279
282
285
288
291
294
297
300
303
306
309
312
315
318
321
Azimuth
92.8
92.6
92.7
92.6
93
93.1
93.3
93.5
93.8
93.8
93.8
93.8
94.1
93.7
93.9
94.1
94
93.8
93.7
93.9
94.6
95
95.1
95.3
95.3
95.3
95.3
95.3
95.4
95.6
95.6
95.4
95
94.9
95.3
95.4
95
94.9
95.4
95.3
95.3
95.7
95.5
95.5
95.4
95.1
95.1
95.5
95.5
96
95.7
95.2
94.8
95
Dip
-85
-85
-84.9
-84.9
-84.9
-84.9
-84.9
-84.9
-84.8
-84.9
-84.8
-84.8
-84.8
-84.8
-84.7
-84.7
-84.7
-84.6
-84.6
-84.5
-84.5
-84.5
-84.4
-84.4
-84.4
-84.4
-84.3
-84.3
-84.2
-84.2
-84.2
-84.2
-84.1
-84.1
-84.1
-84.1
-84.2
-84.2
-84.2
-84.2
-84.2
-84.2
-84.3
-84.2
-84.2
-84.3
-84.2
-84.2
-84.2
-84.2
-84.2
-84.2
-84.2
-84.2
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
324
327
330
333
336
339
342
345
348
351
354
357
360
363
366
369
372
375
378
381
384
387
390
393
396
399
402
405
408
411
414
417
420
423
426
429
432
435
438
441
444
447
450
453
456
459
462
465
468
471
474
477
480
483
Azimuth
95.7
95.5
95.3
95.7
96.1
96.1
96.1
96
96.5
97.2
97.5
98.1
98.4
99.6
100.1
100
100.4
100.8
101
100.9
100.8
100.9
101.1
101.5
101.2
101.1
101.1
101.7
101.4
100.9
100.9
101.8
101.7
102
102.1
102.1
101.8
101.9
102.2
101.8
101.9
102.4
102.4
102.2
102
102.5
102.5
101.6
102.9
102.9
103.5
103
103.6
103.5
Dip
-84.2
-84.1
-84.1
-84.2
-84.1
-84.1
-84.1
-84.1
-84.1
-84.1
-84
-84.1
-84.1
-84.1
-84.1
-84.1
-84.1
-84
-84
-84
-84
-84
-84
-84
-84
-84
-84
-83.9
-83.9
-83.9
-83.9
-83.9
-83.9
-83.9
-83.8
-83.8
-83.8
-83.8
-83.8
-83.8
-83.7
-83.8
-83.8
-83.7
-83.7
-83.7
-83.7
-83.7
-83.7
-83.7
-83.7
-83.6
-83.6
-83.6
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
486
489
492
495
498
501
504
507
510
513
516
519
522
525
528
531
534
537
540
543
546
549
552
555
558
561
564
567
570
573
576
579
582
585
588
591
594
597
600
603
606
609
612
615
618
621
624
627
630
633
636
639
642
645
Azimuth
103.9
103.9
103.9
104.7
105.2
105.4
106.2
106.7
107.5
108.2
109.1
109.2
109.9
111.2
111.6
112.7
114.1
114.7
114.7
114.7
115.2
115.5
116.3
116.5
116.8
117.5
117.9
118
118.3
118.9
119.3
119.5
119.9
120.1
120.2
120.3
120.8
119.7
116
113.6
113.6
114.1
113.9
114
114
114.4
114.2
114.3
114.4
114.6
114.7
113.5
110.8
109.7
Dip
-83.5
-83.5
-83.4
-83.4
-83.4
-83.4
-83.4
-83.4
-83.3
-83.3
-83.3
-83.2
-83.2
-83.2
-83.1
-83
-83
-82.8
-82.7
-82.6
-82.5
-82.4
-82.3
-82.3
-82.2
-82.1
-82
-81.9
-81.8
-81.8
-81.7
-81.6
-81.6
-81.5
-81.4
-81.4
-81.3
-81.2
-80.8
-80.5
-80.4
-80.4
-80.3
-80.2
-80.2
-80.1
-80
-80
-80
-79.9
-79.9
-79.8
-79.6
-79.5
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
648
651
654
657
660
663
666
669
672
675
678
681
684
687
690
693
696
699
702
705
708
711
714
717
720
723
726
729
732
735
738
741
744
747
750
753
756
759
762
765
768
771
774
777
780
783
786
789
792
795
798
801
804
807
Azimuth
109.8
110.2
110.3
110.5
110.5
110.6
110.9
110.8
110.8
111
111.3
111.6
111.7
112
112.3
112.7
113.4
113.2
111.9
109.2
107.5
107.4
107.6
107.7
107.7
107.8
108
107.8
107.8
108
107.9
108.2
108.1
108.3
108.4
108.3
108.4
108.4
108.3
108.1
108.2
108.3
108.1
108.2
108.2
108.1
108.2
108.2
108.3
108.5
108.2
108.3
108.5
108.5
Dip
-79.4
-79.2
-79
-78.8
-78.7
-78.5
-78.3
-78.2
-78
-77.9
-77.7
-77.6
-77.5
-77.5
-77.4
-77.3
-77.3
-77.3
-77.2
-77
-76.8
-76.8
-76.8
-76.7
-76.7
-76.6
-76.5
-76.5
-76.5
-76.4
-76.3
-76.3
-76.3
-76.3
-76.2
-76.2
-76.2
-76.2
-76.2
-76.1
-76.1
-76
-76
-76
-75.9
-75.9
-75.9
-75.9
-75.8
-75.8
-75.8
-75.8
-75.7
-75.7
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
810
813
816
819
822
825
828
831
834
837
840
843
846
849
852
855
858
861
864
867
870
873
876
879
882
885
888
891
894
897
900
903
906
909
912
915
918
921
924
927
930
933
936
939
942
945
948
951
954
957
960
963
966
969
Azimuth
108.6
108.7
108.8
108.7
108.8
109
109.1
109.2
109.1
109
109
109.1
109.1
109.1
109.3
109.1
109.1
109.4
109.4
109.3
109.5
109.6
109.5
109.5
109.7
109.9
110
110
110
110.1
110.1
110.3
110.4
110.2
110.5
111.1
111.2
111.3
111.4
111.2
111.1
111.1
111.2
111.3
111.4
111.5
111.6
111.6
111.1
109.8
109.1
109.2
109.4
109.5
Dip
-75.7
-75.6
-75.5
-75.5
-75.4
-75.4
-75.3
-75.3
-75.3
-75.3
-75.2
-75.2
-75.2
-75.2
-75.2
-75.2
-75.1
-75
-74.9
-74.8
-74.7
-74.6
-74.6
-74.5
-74.5
-74.5
-74.4
-74.4
-74.3
-74.3
-74.2
-74.1
-74
-73.9
-73.9
-74
-73.9
-73.8
-73.8
-73.6
-73.5
-73.4
-73.4
-73.4
-73.3
-73.2
-73.1
-73.2
-73.2
-73
-72.8
-72.7
-72.5
-72.2
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
972
975
978
981
984
987
990
993
996
999
1002
1005
1008
1011
1014
1017
1020
1023
1026
1029
1032
1035
1038
1041
1044
1047
1050
1053
1056
1059
1062
1065
1068
1071
1074
1077
1080
1083
1086
1089
1092
1095
1098
1101
1104
1107
1110
1113
1116
1119
1122
1125
1128
1131
Azimuth
109.2
109.1
109
109.2
109.6
109.9
109.8
109.8
109.9
109.9
109.9
110.2
110.1
110.1
110.2
110.2
110
110.1
110.2
110.1
110.2
110.4
110.5
110.6
110.6
110.8
110.8
110.9
111
110.9
111
111.1
111.2
111.2
111.2
111.4
111.5
111.5
111.7
111.7
111.7
111.8
111.9
112
111.9
111.9
112.1
112
112
112.1
112.1
112.1
112.2
112.4
Dip
-71.9
-71.6
-71.4
-71.4
-71.3
-71.1
-71.1
-71
-71
-71
-71
-71
-71
-70.9
-70.9
-70.8
-70.8
-70.7
-70.6
-70.6
-70.5
-70.5
-70.5
-70.4
-70.3
-70.3
-70.3
-70.2
-70.2
-70.1
-70.1
-70.1
-70
-69.9
-69.9
-69.8
-69.7
-69.8
-69.7
-69.6
-69.6
-69.6
-69.5
-69.5
-69.4
-69.4
-69.3
-69.3
-69.2
-69.2
-69.2
-69.1
-69
-69
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
1134
1137
1140
1143
1146
1149
1152
1155
1158
1161
1164
1167
1170
1173
1176
1179
1182
1185
1188
1191
1194
1197
1200
1203
1206
1209
1212
1215
1218
1221
1224
1227
1230
1233
1236
1239
1242
1245
1248
1251
1254
1257
1260
1263
1266
1269
1272
1275
1278
1281
1284
1287
1290
1293
Azimuth
112.2
112
112
112
112
112
111.9
111.8
111.8
111.8
111.8
111.7
111.8
111.9
111.9
111.8
111.9
112.1
112
112.1
112.2
112.2
112.3
112.3
112.3
112.3
112.4
112.4
112.3
112.3
112.3
112.4
112.4
112.5
112.6
112.6
112.7
112.7
112.7
112.8
112.9
112.8
112.9
112.9
112.9
113.1
113
113
113.1
113
112.9
113
112.8
112.9
Dip
-68.8
-68.7
-68.6
-68.5
-68.4
-68.3
-68.2
-68.1
-68
-67.8
-67.6
-67.5
-67.4
-67.4
-67.3
-67.3
-67.2
-67.2
-67.2
-67.2
-67.2
-67.2
-67.2
-67.1
-67.1
-67
-66.9
-66.9
-66.9
-66.9
-66.9
-66.9
-66.8
-66.8
-66.7
-66.7
-66.6
-66.6
-66.6
-66.6
-66.6
-66.6
-66.5
-66.6
-66.5
-66.5
-66.5
-66.5
-66.4
-66.4
-66.3
-66.3
-66.3
-66.2
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
1296
1299
1302
1305
1308
1311
1314
1317
1320
1323
1326
1329
1332
1335
1338
1341
1344
1347
1350
1353
1356
1359
1362
1365
1368
1371
1374
1377
1380
1383
1386
1389
1392
1395
1398
1401
1404
1407
1410
1413
1416
1419
1422
1425
1428
1431
1434
1437
1440
1443
1446
1449
1452
1455
Azimuth
112.9
112.9
112.9
113
112.8
112.9
112.9
112.8
112.8
112.7
112.7
112.6
112.6
112.5
112.6
112.6
112.7
112.7
112.5
112.2
111.9
111.6
111.5
111.4
111.2
111.1
111
110.9
110.9
110.7
110.6
110.3
109.8
109.7
109.8
109.8
109.7
109.6
109.6
109.7
109.7
109.6
109.6
109.7
109.9
110.1
110.1
110.2
110.2
110.1
110.2
110.2
110.2
110.3
Dip
-66.2
-66.2
-66.1
-66.1
-66.1
-66.1
-66
-66
-66
-65.9
-65.8
-65.7
-65.7
-65.7
-65.7
-65
-64.4
-64.1
-64
-63.9
-63.8
-63.8
-63.7
-63.6
-63.5
-63.4
-63.3
-63.2
-63.2
-63.2
-63.1
-62.7
-62.3
-62.1
-62.2
-62.2
-62.2
-62.2
-62.2
-62.2
-62.2
-62.2
-62.1
-62.1
-62.1
-62.1
-62
-62
-61.8
-61.7
-61.6
-61.5
-61.4
-61.3
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
1458
1461
1464
1467
1470
1473
1476
1479
1482
1485
1488
1491
1494
1497
1500
1503
1506
1509
1512
1515
1518
1521
1524
1527
1530
1533
1536
1539
1542
1545
1548
1551
1554
1557
1560
1563
1566
1569
1572
1575
1578
1581
1584
1587
1590
1593
1596
1599
1602
1605
1608
1611
1614
1617
Azimuth
110.3
110.1
110.1
110.2
110.1
110.1
110.1
110.1
110.1
110.2
110.2
110.3
110.2
110.3
110.3
110.3
110.4
110.5
110.5
110.6
110.7
110.7
110.7
110.7
110.7
110.8
110.8
110.6
110.5
110.5
110.4
110.3
110.3
110.3
110.4
110.4
110.2
110.1
110
109.8
109.7
109.4
109.1
108.7
108.3
108.1
107.9
107.8
107.8
107.6
107.4
107.3
107.2
107.2
Dip
-61.2
-61.1
-61
-61
-60.9
-60.8
-60.8
-60.7
-60.6
-60.5
-60.4
-60.3
-60.2
-60.1
-60
-60
-60
-59.9
-59.9
-59.8
-59.8
-59.8
-59.8
-59.8
-59.7
-59.6
-59.6
-59.5
-59.5
-59.4
-59.3
-59.3
-59.2
-59.1
-59.1
-59.1
-59
-58.9
-58.9
-58.9
-58.8
-58.8
-58.6
-58.5
-58.3
-58.2
-58.1
-58
-58
-58
-57.9
-57.9
-57.8
-57.7
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
1620
1623
1626
1629
1632
1635
1638
1641
1644
1647
1650
1653
1656
1659
1662
1665
1668
1671
1674
1677
1680
1683
1686
1689
1692
1695
1698
1701
1704
1707
1710
1713
1716
1719
1722
1725
1728
1731
1734
1737
1740
1743
1746
1749
1752
1755
1758
1761
1764
1767
1770
1773
1776
1779
Azimuth
107.1
107
107.1
107.1
107
107
106.9
106.8
106.7
106.6
106.6
106.4
106.4
106.3
106.3
106.1
106.1
106.1
106
106
106
106.1
106
106
105.9
105.9
105.8
105.8
105.7
105.5
105.2
104.8
104.5
104.2
104.1
103.8
103.6
103.4
103.2
103.1
102.9
102.6
102.5
102.2
102
101.8
101.6
101.3
101.1
100.9
100.8
100.8
100.7
100.6
Dip
-57.7
-57.6
-57.6
-57.6
-57.5
-57.4
-57.4
-57.3
-57.3
-57.3
-57.2
-57.2
-57.1
-57
-57
-57
-56.9
-57
-56.9
-56.9
-56.9
-56.9
-56.8
-56.8
-56.7
-56.7
-56.6
-56.6
-56.7
-56.7
-56.8
-56.8
-56.9
-56.9
-56.9
-56.9
-56.9
-56.9
-56.9
-57
-57
-57
-57
-57
-57
-57
-57
-57.1
-57.1
-57.1
-57.1
-57.1
-57
-57
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
Hole ID: 08-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: 9320_NSD
Target 2:
Target 3:
Drill Start Date: 07/06/2008
Drill End Date: 24/08/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor June 06/08 @ 2100
Core Diameter: NQ2
UTM North: 583495.1
Survey
Depth
1782
1785
1788
1791
1794
1797
1800
1803
1806
1809
1812
1830
1881
1932
1980
2034
2085
2135
2186
2237
2285
2339
2387
2441
Azimuth
100.4
100.3
100.3
100.2
100
100
99.9
99.9
99.9
99.8
99.6
99.23
98.43
96.03
94.71
92.53
92.3
92
92
91
91
91
90
90
Dip
-57
-57
-57
-56.9
-56.9
-56.9
-56.8
-56.8
-56.8
-56.8
-56.8
-54.9
-53.9
-53.1
-52.5
-50.6
-48.1
-46
-43.7
-41.7
-40.4
-39.5
-37.9
-37.9
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
EZS
EZS
EZS
EZS
EZS
EZS
EZS
EZS
EZS
EZS
EZS
EZS
acid
Actual Depth: 2441
Planned Depth: 2250
UTM East 673666.8
08-NSD-002
MAJOR UNIT
From
0.00
1514.50
1525.60
1527.40
1541.00
1556.00
1570.70
1584.50
1588.30
1591.40
1593.50
1596.00
1596.40
1597.20
1597.90
1604.90
1609.60
1616.90
1619.50
1624.90
1648.50
1653.10
1669.90
1699.50
1700.30
1710.10
To
1514.50
1525.60
1527.40
1541.00
1556.00
1570.70
1584.50
1588.30
1591.40
1593.50
1596.00
1596.40
1597.20
1597.90
1604.90
1609.60
1616.90
1619.50
1624.90
1648.50
1653.10
1669.90
1699.50
1700.30
1710.10
1713.30
MINERALS
As%Cp%
3.0
Mt%
Po%
2.0
7.0
3.0
1.0
0.2
1.0
0.5
0.5
0.3
Py% Comments
Semi massave
section of Po
between
1573-1573.2
VGSpecks
FABRIC
From
1522.00
1523.00
1538.00
1550.00
1556.00
1570.70
1577.00
1593.50
1596.00
1604.90
1619.60
1625.10
1630.80
1646.00
1653.90
1661.50
1664.50
1665.80
1667.80
1687.70
1700.30
1705.00
1712.50
To
1523.00
1538.00
1550.00
1556.00
1570.70
1577.00
1593.50
1596.00
1604.90
1619.60
1625.10
1630.80
1646.00
1653.90
1661.00
1664.50
1665.80
1667.80
1684.00
1687.80
1701.30
1706.00
1713.00
Alphadeg
35
35
40
45
35
40
50
60
50
35
35
35
40
60
50
45
50
35
45
55
51
55
55
Comments
mostly
irregular
fabric.
Int
WE
WE
WE
MO
WE
WE
MO
MO
MO
MO
MO
WE
WE
WE
WE
WE
WE
WE
WE
WE
WE
WE
WE
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1570.00
Alpha
deg
40
CommentsInt
INT
Type
PT
From
1568.00
QTZ VEINING
VeinType
QZ-C
Vein%
60
Tex
m
ContactType
D
Alphadeg
65
CommentsFrom
1636.10
To
1638.30
FAULT
From
1540.50
1591.40
1596.40
1630.80
1636.10
To
1541.00
1593.50
1597.20
1633.60
1638.30
Alphadeg
25
65
75
65
55
Comments
intense fault
gouge crumbly
chlorite and calcite.
Int
WEK
MOD
MOD
INT
MOD
Type
SZ
SZ
SZ
GG
SZ
MajorUnit
No
2
8F
2
2
2D
2
7A
2
4E
2
3A
4E
6
2
2
1
2D
2
2D
2
2D
2
2D
2
2D
Cont
15
22
40
35
70
65
65
70
70
75
50
60
45
80
40
40
35
60
55
50
STRUCTURAL LOG Page 1 of 9
08-NSD-002
MAJOR UNIT
From
1713.30
1730.30
1769.70
1783.60
1805.40
To
1730.30
1769.70
1783.60
1805.40
1816.70
MINERALS
As%
3.0
Cp%
0.0
Mt%
Po%
0.1
0.2
0.0
0.0
3.0
0.5
0.5
Py% Comments
qtz
flooded/veined
4A
VGSpecks
FABRIC
From
1726.50
1730.60
1736.00
1749.00
1762.00
1775.00
1784.00
1792.00
1806.20
To
1727.00
1731.30
1737.00
1750.00
1763.00
1776.00
1785.00
1793.00
1807.00
Alphadeg
41
47
35
45
60
50
60
60
50
CommentsInt
WE
WE
MO
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1809.00
Alpha
deg
40
CommentsInt
MO
Type
SF
From
1808.00
QTZ VEINING
VeinType
QZ-C
QZ-C
QZ
Vein%
5
8
85
Tex ContactType
I
S
I
Alphadeg
60
Comments
No angle
recorded.
alpha
angle
varies.
strongly
qtz
flooded/vein
ed 4A
From
1724.50
1786.00
1805.40
To
1727.00
1792.00
1806.20
FAULT
From
1794.90
1805.40
To
1795.60
1806.20
Alphadeg
60
Comments
70cm fracture //
to CA.
qtz flooded/veined
4A
Int
INT
Type
BC
SZ
MajorUnit
2
2
2D
2T
4A
Cont
60
STRUCTURAL LOG Page 2 of 9
08-NSD-002
MAJOR UNIT
From
1816.70
1831.10
1831.90
1840.00
To
1831.10
1831.90
1840.00
1879.00
MINERALS
As%
0.1
Cp%
Mt%
Po%
0.8
2.0
0.5
1.0
1.0
3.0
3.0
20.
0.1
Py% Comments
4H type band
over 15cm
one Po vein
0.8cm wide
mix 4B/4A/4H
at the contact
with the mafic
volcanic
VGSpecks
FABRIC
From
1811.00
1813.00
1815.00
1816.00
1818.00
1825.00
1832.00
1833.50
To
1812.00
1814.00
1816.00
1817.00
1819.00
1826.00
1833.00
1834.40
Alphadeg
0
30
0
50
50
40
80
80
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
Type
S0
S1
S0
S1
S1
S1
S1
S1
FOLD
To
1814.00
1815.00
Alpha
deg
90
80
CommentsInt
MO
MO
Type
FD
MF
From
1813.00
1814.00
QTZ VEINING
VeinType
QZ-C
Vein%
3
Tex ContactType
I
Alphadeg
80
Comments
angle
varies
slightly
locally
From
1840.00
To
1874.00
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
4B
2T
4B
2
Cont
40
90
STRUCTURAL LOG Page 3 of 9
08-NSD-002
MAJOR UNIT
From
1879.00
1887.80
1904.50
1906.40
1911.50
1913.00
1914.00
1917.30
To
1887.80
1904.50
1906.40
1911.50
1913.00
1914.00
1917.30
1929.30
MINERALS
As%Cp%
Mt%
Po%
2.0
0.5
2.0
2.0
3.0
1.0
Py% Comments
over 15cm in
short veins
associated
with minor
shear zones
and quartz
flooding
section 10 - 10
-30 cm wide
VGSpecks
FABRIC
From
1844.00
1850.00
1865.00
1883.00
1892.00
1904.50
1907.00
1911.00
1912.50
1915.00
1917.00
1922.00
1925.40
1927.00
To
1845.00
1851.00
1866.00
1884.00
1893.00
1905.50
1907.40
1911.50
1913.00
1916.00
1922.00
1925.00
1927.00
1928.00
Alphadeg
50
50
80
75
80
70
5
70
80
90
55
40
50
85
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1909.00
1910.50
1917.20
1923.00
Alpha
deg
90
90
70
65
CommentsInt
MO
MO
MO
MO
Type
FD
ZF
FD
SF
From
1908.00
1909.50
1916.70
1920.00
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From
1921.80
To
1925.40
Alphadeg
35
Comments
series of minor
shear zone
ranging from
35-50 degrees
Int
WEK
Type
SZ
MajorUnit
2T
1
4B
4A
4B
1
4B
4B
Cont
90
70
75
75
STRUCTURAL LOG Page 4 of 9
08-NSD-002
MAJOR UNIT
From
1929.30
1932.50
1933.60
1937.20
1951.00
1955.00
1979.00
1985.40
1990.00
2003.00
2009.00
2024.00
2028.40
2028.80
2045.50
2047.10
2052.00
2053.00
To
1932.50
1933.60
1937.20
1951.00
1955.00
1979.00
1985.40
1990.00
2003.00
2009.00
2024.00
2028.40
2028.80
2045.50
2047.10
2052.00
2053.00
2090.40
MINERALS
As%Cp%
Mt%
Po%
0.5
2.0
1.0
0.1
Py% Comments
associated
with semi
massive vein
at
1931.18-1931.20
VGSpecks
FABRIC
From
1932.00
1933.20
1946.00
1951.00
1958.00
1964.00
1970.00
1979.00
1985.10
1997.00
2009.00
2012.00
2021.00
2024.00
2028.40
2032.00
2043.40
2044.90
2048.00
2048.80
2051.10
2053.40
To
1933.20
1937.20
1951.00
1958.00
1963.00
1970.00
1979.00
1985.10
1997.00
2003.00
2012.00
2021.00
2024.00
2028.40
2032.00
2042.00
2043.40
2044.90
2048.00
2048.80
2051.10
2053.40
Alphadeg
70
65
60
70
60
45
50
60
70
80
55
65
60
70
65
70
65
55
70
75
60
90
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
INT
MO
MO
MO
WE
WE
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From
1985.10
2003.00
2014.40
2024.00
To
1986.40
2009.00
2015.50
2028.20
Alphadeg
50
60
60
Comments
poor RQD 5
pieces of core
larger than 10 cm
Int
INT
MOD
MOD
INT
Type
SZ
OS
SZ
OS
MajorUnit
4A
4B
2
1
2
2
2T
1
2T
1
2
2
13
2T
4B
2
4B
2
Cont
50
65
70
85
45
70
60
87
45
60
75
90
70
70
60
STRUCTURAL LOG Page 5 of 9
08-NSD-002
MAJOR UNIT
From
2090.40
2092.10
2106.50
2130.70
2137.90
2139.40
2140.40
2141.30
2145.20
2145.80
2158.80
2168.60
2169.80
2177.70
2188.70
2194.70
2206.70
To
2092.10
2106.50
2130.70
2137.90
2139.40
2140.40
2141.30
2145.20
2145.80
2158.80
2168.60
2169.80
2177.70
2188.70
2194.70
2206.70
2211.10
MINERALS
As%Cp%
Mt%
Po%
15.
5.0
15.
3.0
Py% CommentsVGSpecks
FABRIC
From
2055.00
2059.00
2061.00
2062.50
2065.50
2067.00
2068.30
2071.10
2072.40
2072.40
2081.00
2090.40
2106.30
2117.00
2132.80
2137.90
2139.30
2140.30
2143.50
2146.10
2148.35
2152.45
2153.90
2158.50
2160.00
2163.00
2164.40
2166.10
2170.40
2172.60
2174.40
2180.50
2189.00
2193.20
2195.30
2205.00
To
2055.00
2059.00
2061.00
2062.50
2065.50
2067.00
2068.30
2071.10
2072.40
2081.00
2090.40
2092.10
2117.00
2132.80
2137.90
2139.30
2140.30
2141.30
2143.50
2146.10
2148.35
2152.45
2153.90
2158.50
2160.00
2163.00
2164.40
2166.10
2170.40
2172.60
2174.40
2180.50
2189.00
2193.20
2195.30
2206.00
Alphadeg
55
65
65
90
70
60
65
70
89
55
65
70
65
70
65
70
75
65
80
75
75
65
75
70
50
60
65
75
50
35
60
40
65
50
50
53
CommentsInt
WE
MO
WE
WE
WE
WE
WE
WE
WE
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
WE
MO
MO
MO
MO
MO
MO
MO
MO
INT
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
2140.25
Alpha
deg
50
CommentsInt
MO
Type
FD
From
2140.20
QTZ VEINING
VeinType
QZ-C
CA
Vein%
85
85
Tex ContactType
Alphadeg
55
60
CommentsFrom
2114.40
2132.80
To
2115.50
2133.60
FAULT
From
2058.40
2098.20
2132.80
2145.00
2196.50
2202.40
To
2058.70
2099.90
2142.50
2146.50
2197.50
2203.00
Alphadeg
30
60
60
50
Comments
Not really an open
space fault but a
strongly fractured
zone (core still
pieces together)
Int
WEK
MOD
MOD
MOD
MOD
MOD
Type
OS
SZ
SZ
SZ
SZ
SZ
MajorUnit
2T
1
2
2T
4E
4B
4E
2
4E
2
1
2T
2
1
1
2
1
Cont
60
60
65
70
45
60
55
60
70
80
60
60
65
60
65
70
50
55
STRUCTURAL LOG Page 6 of 9
08-NSD-002
MAJOR UNIT
From
2211.10
2211.80
2213.60
2218.30
2222.70
2224.50
2234.80
2238.90
2253.90
2257.70
2265.00
2272.70
2275.10
2278.30
2287.40
2287.80
2329.90
2331.80
2333.10
2336.10
2351.50
2353.60
To
2211.80
2213.60
2218.30
2222.70
2224.50
2234.80
2238.90
2253.90
2257.70
2265.00
2272.70
2275.10
2278.30
2287.40
2287.80
2329.90
2331.80
2333.10
2336.10
2351.50
2353.60
2355.10
MINERALS
As%Cp%
Mt%
Po%
1.0
0.2
0.2
4.0
0.2
Py%
0.5
Comments
Cpy in a 5mm
wide serp alt'n
band.
VGSpecks
FABRIC
From
2224.00
2232.00
2242.00
2250.00
2258.00
2264.00
2270.00
2281.00
2293.00
2297.00
2306.00
2318.00
2325.00
2329.50
2335.00
2342.00
2346.60
2350.00
2354.00
To
2224.50
2233.00
2243.00
2251.00
2259.00
2265.00
2271.00
2282.00
2294.00
2298.00
2307.00
2319.00
2326.00
2330.00
2336.00
2343.00
2347.30
2351.00
2355.00
Alphadeg
66
56
35
43
48
57
55
51
55
58
40
53
45
62
54
48
54
43
57
CommentsInt
MO
WE
MO
MO
INT
INT
INT
INT
INT
INT
INT
MO
MO
MO
MO
MO
INT
INT
Type
S0
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
2212.50
2219.00
2222.70
Alpha
deg
50
45
52
CommentsInt
WE
WE
MO
Type
FD
FD
ZF
From
2211.80
2218.30
2222.60
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
2
4B
4B
4A
4B
1
1
2
1
2
1
2
2
13
2
1
2
1
2
1
2
Cont
55
90
90
40
90
60
62
40
40
50
46
56
60
61
60
73
62
65
61
67
80
52
STRUCTURAL LOG Page 7 of 9
08-NSD-002
MAJOR UNIT
From
2355.10
2355.80
2363.80
2364.30
2365.90
2378.70
2382.10
2404.10
To
2355.80
2363.80
2364.30
2365.90
2378.70
2382.10
2404.10
2420.50
MINERALS
As%Cp%
Mt%
Po%
0.1
5.0
0.1
1.0
30.
0.5
18.
8.0
Py% Comments
sparsely
scattered
blebs/specks.
proximal to 4H
4H
VGSpecks
FABRIC
From
2359.00
2360.50
2362.00
2364.50
2373.00
2378.00
2392.00
2406.00
2411.00
To
2360.00
2361.00
2363.00
2365.00
2374.00
2378.50
2393.00
2406.80
2411.50
Alphadeg
80
55
70
68
43
50
50
39
34
CommentsInt
MO
INT
MO
MO
MO
INT
INT
Type
S0
S2
S0
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
CA
CA
Vein%
30
20
Tex ContactType
I
I
Alphadeg
60
50
CommentsFrom
2369.00
2385.30
To
2371.20
2389.80
FAULT
From
2363.80
2370.70
2385.30
2388.90
2404.10
To
2364.30
2371.20
2385.90
2389.80
2418.00
Alphadeg
90
47
45
35
38
CommentsInt
MOD
MOD
INT
MOD
INT
Type
SZ
SZ
SZ
SZ
SZ
MajorUnit
2T
4A
4H
2T
2
7A
2
4H
Cont
55
65
90
80
63
70
60
43
STRUCTURAL LOG Page 8 of 9
08-NSD-002
MAJOR UNIT
From To
MINERALS
As%Cp%
Mt%
Po%
15.
Py% CommentsVGSpecks
FABRIC
From
2416.30
2419.00
To
2416.80
2420.00
Alphadeg
30
30
CommentsInt
INT
MO
Type
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From
2418.00
To
2420.50
Alphadeg Comments
core highly
broken, RQD <20%
Int
INT
Type
BC
MajorUnit
Cont
STRUCTURAL LOG Page 9 of 9
08-NSD-002
Assay
Sample AU ppm
MAJOR UNIT
From
0.00
1514.50
1525.60
1527.40
1541.00
1556.00
1570.70
1584.50
1588.30
To
1514.50
1525.60
1527.40
1541.00
1556.00
1570.70
1584.50
1588.30
1591.40
From To
MINOR UNIT
From To CommentsComments
Wedged off of DDH 08-NSD-001.
Weakly foliated to massive homogneous green
amphibolite, folded,foliated, distorted and a few
patches of Cc alt'n UC-1519m.
C.g granite pegmatite consisting of ~60% qtz, 20%
pinkish kspar and 20% creamy white to yellowish
plagioclase.
Exactly the same as the previous unit, massive green
amphibole rock, 95-100% amphibole. Minor patches
of soft alt'n with green streak = chlorite (?).
Fresh looking Basalt, f.g., homog, with a weak
foliation with mod. cgr. sugary textured Cc. The unit
is distorted between 1539.6-1541, wk shear with 3-5
cm Cc veins.
heterogenous mafic volcanin varying between a
bleached grey-green basalt with 5-10% irreg dark
green amph bands and biotite slips to 1 -3 cm cm
thick pillow selvages. 10% c.g. Cc veining.
Fresh looking massive looking basalt with minor
calcite veining. A steel wedge was installed 1585 with
.5 metres of core missing and a graphite plug marks
the top of the wedge.
Medium grey to dark green gabbro / Coarse grained
mafic basalt with minor calcite veining. The unit is
massive with a mottled.. The unit is fesh looking with
no type of alteration
medium grained to coarse grained mafic basalt with
minor calcite veining. The unit is massive with
gradational upper and lower contracts
Comments
The unit is the massive
m.g amphibolite texture
that is borderline
ultramafic.
1518-1519m has weak
serp alt'n.
There is a 10cm
biotite-rich mafic
black/brown enclave in
the middle of the
pegmatite
2% scattered irregular
Cc and qtz
veins/patches.
There is an increase in
boitite slips down section.
There is one quartz
-ourmaline vein
between
1567.2-1567.35m;
minor ptygmatic
veining is also
present between
1569-1569.20 and
1569.10-1570.3m.
The unit is composed
of 65-70% dark green
amphibole and
Pyroxene with 10 -15%
feldspar/calcite
bordering on ultramafic.
60 % mafic 30%
feldspar and 10%
green amphibole.
ALTERATION
Bio
W
W
Car
M
M
Chl
W
Gru Hem Ser Si Comments
LITHOLOGY LOG Page 1 of 22
Unit
No
2
8F
2
2
2D
2
7A
2
Unit
08-NSD-002
Assay
Sample
E446754
E446755
E446756
E446757
E446758
E446759
E446761
E446762
E446763
E446764
E446765
E446766
E446767
AU ppm
0.01
0.01
0.01
0.01
0.05
0.02
0.01
0.01
0.01
0.01
0.01
0.01
0.01
MAJOR UNIT
From
1591.40
1593.50
1596.00
1596.40
1597.20
1597.90
1604.90
1609.60
1616.90
To
1593.50
1596.00
1596.40
1597.20
1597.90
1604.90
1609.60
1616.90
1619.50
From
1589.00
1590.00
1590.70
1591.40
1592.40
1592.90
1593.50
1594.20
1595.00
1596.00
1596.40
1597.20
1597.90
To
1590.00
1590.70
1591.40
1592.40
1592.90
1593.50
1594.20
1595.00
1596.00
1596.40
1597.20
1597.90
1598.90
MINOR UNIT
From To CommentsComments
A 4E composed of f.g.grun, minor garnets
intercalated with sediment looking material, 35%
green amphibole and extermely distorted
mineralization ranges between 3-15% locally and
there is~ 3% Cpy throughout the unit.
Medium grained massive mafic basalt with intense
chlorite alteration. Locally bands massive chlorite
are present. The unit consists of 50% mafics, 20%
feldspar, and 30% green amphibole.
The unit is a massive grey-buff coloured rhyolite.
A 4E/Interflow metased with hi % of green amphibole
and bands between 2-5 cm wide. There is a lack of
garnets thoughout the unit 2-;3% Po is associated
along the margins of calcite veins that are rimmed
with chlorite.
The unit consists of equigranular biotitic and 30%
quartz. There are three quartz sweats and the unit is
extremely hard.
Medium grained massive basalt with intenrse chlorite
alteration. There are sections 2-5 cm wide of
complete chlorite alteration
Medium grained mafic basalt with up to 10% bioitite
within the marix and as biotite slips.
The upper contract is brecciated; the unit is very
soft & amorphous; all fracture planes display
moderate talc alteration with moderate green
amphibole.
Fine to medium grained pillowed basalt with selvages
between 2-5 cm wide. The selvages are composed of
biotite and garnet.
Comments
Down section garnets
become diffuse and and
the unit is light grey
in colour with minor
green amphibole bands
2-3 cm wide with a
grunerite rim 1-3mm in
width.
Down hole the unit has
a wavy overprint from
1615-1616.90
ALTERATION
Bio
W
W
M
W
W
Car
W
W
W
M
M
W
W
Chl
M
W
M
M
S
Gru Hem Ser
M
Si
W
W
W
Comments
Qartz veins present, bio
is localized.
LITHOLOGY LOG Page 2 of 22
Unit
4E
2
3A
4E
6
2
2
1
2D
Unit
08-NSD-002
Assay
Sample
E468001
E468002
AU ppm
0.00
0.01
MAJOR UNIT
From
1619.50
1624.90
1648.50
1653.10
1669.90
To
1624.90
1648.50
1653.10
1669.90
1699.50
From
1697.50
1698.50
To
1698.50
1699.50
MINOR UNIT
From To CommentsComments
Fresh looking medim to coarse grained mafic
volcanic with minor calcite veining. The unit is
composed of 60% green amphibole and 30%
medium grained plag.
The uppper 3 metres of the unit appear to have a net/
polysutured texture where mm scale chlorite veinlets
and calcite form a stock work . Down hole the unit is
massive with distinct pillow selvages. There is intense
fault gouge from
Medium grey coloured, somewhat fresh looking,
weakly foliated, f.g-m.g mafic volcanic unit with
moderate f.g. homogeneous bio alt'n and is cut by
~3-5% Cc veinlets (~1-3mm thick). From
1649.5-1649.9m there are a few distorted Cc veins
(3mm-1.2cm thick)
Med grey coloured, f.g. massive to mod foliated mafic
volcanic unit with weak amph alt'n, ~10-15% pillow
selvages (consisting of f.g. dark green amph with few
1-2mm diam garnets as well as weak bio alt'n is
some cases), minor qtz veinlets (mostly
Light to medium grey coloured, massive-weakly
foliated, fresh looking mafic volcanic unit with weak
dark green amph (within matrix) and cut by ~3-7%
(varies) Cc veinlets (~1-3mm thick and few distorted).
Locally, weak-mod bio alt'n.
Comments
1630.80 - 1633.6m.
The unit is fairly
competent in spots and
there is 15-20% calcite
veining associated with
the gouge. Mod shear
between 136.1 - 1638.30
with mod adjacent dark
green amph alt'n,
moderate f.g. chlorite
with surrounding area
appearing weakly
bleached.
associated with
pillows?) and few Cc
veinlets. There is a 5cm
thick qtz vein @
1660m. From
164.3-1666.2m and
1666.4-1666.6m the unit
is strongly alt'd and
distorted with intense
m.g-c.g. bio alt'n and
intense (localized) Cc
alteration.
@ 1678.9m there is a
1.5-2cm thick Cc vein
with open cavities and
fairly large crystals.
1679.8-1679.9m
contains mod qtz veins
with moderate
associated dark green
amph , few garnets and
1 bleb of Po.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 3 of 22
Unit
2
2D
2
2D
2
Unit
08-NSD-002
Assay
Sample
E468003
E468004
E468005
E468006
E468007
E468008
E468009
E468011
E468012
E468013
E468014
E468015
E468016
E468017
E468018
E468019
AU ppm
0.01
0.01
0.04
0.00
0.01
0.00
0.01
0.01
0.01
0.01
0.01
0.09
0.01
0.01
0.00
0.01
MAJOR UNIT
From
1699.50
1700.30
1710.10
1713.30
To
1700.30
1710.10
1713.30
1730.30
From
1699.50
1700.30
1701.30
1710.10
1711.10
1712.10
1712.50
1713.00
1713.30
1714.30
1715.30
1725.50
1726.50
1727.50
1728.50
1729.50
To
1700.30
1701.30
1702.30
1711.10
1712.10
1712.50
1713.00
1713.30
1714.30
1715.30
1715.80
1726.50
1727.50
1728.50
1729.50
1730.30
MINOR UNIT
From To CommentsComments
Fine to medium grained mafic volcanic, 70% dark
green amph 30% plag, 40-50% pillow selvages
containing bio, amph, euhedral porphyroblastic
garnets. Selvages range frrom 0.3-1.0 cm wide.
Fine - Medium grained mafic volcanic, cut by qtz -
Cc veins <5 % 5mm - 1 cm in width. Amph varies,
approx. 50-70%, plag 20%, biotite <10%, 2% pillow
selvages, 2% alteration bands consist of dark green
amph and pale green mineral.
Fine grained mafic volcanic with coarser grained
pillow selvages. Qtz - Cc veins range from 0.5 mm -
3 cm (<5%).. Pillow selvages consist of garnet
porphyroblasts ( 0.2mm - 1cm), green amphibole,
and biotite.
Fine to coarser grained mafic volcanic rock with
60-70% green amph, <5% bio, 25-30% plag. Qtz
and Cc veins ranging in thickness from 2 mm -
11cm. Veins dominant from 1723-1726m. A pale
green mineral occurs locally.
Comments
Po <1% scattered
throughout, gradational
lower and upper
contact. The unit might
be a kind of sediment
(4E type) not magnetic.
No significant
mineralization.
Po is scattered
throughout 1712.1 -
1713.3 m. No Po up
section.
Po is scattered
thorughout the mafic
volcanic rock at
1729m. Pillow selvages
occur at 1730.3-1730.6
with gar porphyblasts
(2mm-1.5cm), bio, and
green amph.
ALTERATION
Bio
M
W
M
W
Car Chl Gru Hem Ser Si
W
Comments
All present in pillow
selvages.
Pale green mineral
overprinting.
All present in pillow
selvages.
Bio, grt, gra present in
pillow selvages. quartz
veins present.
LITHOLOGY LOG Page 4 of 22
Unit
2D
2
2D
2
Unit
08-NSD-002
Assay
Sample
E468021
E468022
E468023
E468024
E468025
E468026
E468027
E468028
E468029
E468031
E468032
E468033
E468034
E468035
E468036
AU ppm
0.00
0.01
0.00
0.00
0.00
0.00
0.00
0.01
0.01
0.01
0.00
0.01
0.01
0.01
0.01
MAJOR UNIT
From
1730.30
1769.70
1783.60
To
1769.70
1783.60
1805.40
From
1730.30
1730.60
1781.50
1782.50
1783.50
1784.00
1785.00
1786.00
1787.00
1788.00
1789.00
1789.50
1790.00
1791.00
1792.00
To
1730.60
1731.30
1782.50
1783.50
1784.00
1785.00
1786.00
1787.00
1788.00
1789.00
1789.50
1790.00
1791.00
1792.00
1793.00
MINOR UNIT
From To CommentsComments
Well foliated green-grey m.g mafic rock with 1-5% f.g
biotite in the matrix. 5-20% plagioclase in the matrix.
Fine grained mod foliated mafic volcanic consisting
of equigranular f.g. plagioclase (60%) and green
amphibole (40%). The unit contains 8-10% pillow
selvages ranging from 0.3-1cm wide.
Selvagesconsist of c.g.garnets, biotite, green amph.
Grading from weakly foliated to more massive mafic
volcanic. The unit is mainly composed of
f.g-mg.amphiboles and plagioclase, locally <3%
f.g.biotite. From 1786-1792m, the unit is cut by
5-10% Qtz-[Cc] veins ranging from 0.5-15cm wide.
Comments
1732.5-1734.5m has
~5-10% planar bands
of biotite <3cm
containing garntes
1-3mm in size.
Locally, the unit
displays a soft pale
green mineral (amph?)
overprinting the dark
green amph. The unit is
cut by 3% Qtz-Cc veins
up to 3cm wide.
Consistent foliation @
50dca. Lower contact is
gradational.
Scattered Po from
1786-1792m, <1%.
Traces Cpy. From
1794.9-1795.6m, the
unit is fractured
(fractures // to CA +
conjugate fractures).
The lower part is
darker and contains
10% bio.
ALTERATION
Bio
M
M
Car Chl Gru Hem Ser Si
W
M
Comments
alt'n mainly present in
pillow selvages.
5-10% Qtz-[Cc veins]
fairly massive fresh
mafic volcanic
LITHOLOGY LOG Page 5 of 22
Unit
2
2D
2T
Unit
08-NSD-002
Assay
Sample
E468037
E468038
E468039
E468041
E468042
E468043
E468044
E468045
E468046
E468047
E468048
E468049
E468051
E468052
E468053
E468054
E468055
E468056
E468057
AU ppm
0.02
0.02
1.15
0.07
0.01
0.02
0.05
0.02
0.02
0.08
0.03
0.03
0.02
2.74
0.10
0.73
0.02
0.01
0.00
MAJOR UNIT
From
1805.40
1816.70
To
1816.70
1831.10
From
1803.40
1804.40
1805.40
1806.20
1807.00
1808.00
1809.00
1810.00
1811.00
1812.00
1813.00
1814.00
1815.00
1816.00
1816.70
1817.20
1817.80
1818.80
1819.80
To
1804.40
1805.40
1806.20
1807.00
1808.00
1809.00
1810.00
1811.00
1812.00
1813.00
1814.00
1815.00
1816.00
1816.70
1817.20
1817.80
1818.80
1819.80
1820.50
MINOR UNIT
From To CommentsComments
Grunerite rich iron formation. The unit consists of
yellow/pale green grunerite rich bands up to 1cm
wide and chert bands up to 3cm wide. Mt content up
to 20% (more magnetic than usual 4A). The unit is
folded (foliation/bedding // to CA).
4B zebra rock, SIF type. Alternating dark grey Mt
rich bands averaging 0.8cm wide and chert bands up
to 0.5cm wide. Unusual high wispy grunerite content
( between two Mt rich bands) up to 50% (but too
much Mt to be 4A?).
Comments
From 1805.4-1806.2m,
the unit is strongly qtz
flooded (almost a Qtz
vein) with 3-5% Asp
and Po. Presence of
dark bands (argilite?) in
the first 20cm. The unit
is weakly qtz veined
overall. Po is scattered
(1-2% throughout) and
in fracture filling.
The unit seems weakly
sheared but also
displays tight folds
(plastic deformation?).
From 1830-1830.6m,
the unit contains
m.g.fractured garnets
and pale/medium green
amph. Disseminated
Po up to 2% overall.
The LC has
m.g-c.g.garnets and a
0.8cm Po vein.
ALTERATION
Bio Car Chl Gru
S
Hem Ser Si
S
W
Comments
strongly qtz flooded
veined 4A
4B sif with high
grunerite content: alt'n?
LITHOLOGY LOG Page 6 of 22
Unit
4A
4B
Unit
08-NSD-002
Assay
Sample
E468058
E468059
E468061
E468062
E468063
E468064
E468065
E468066
E468067
E468068
E468069
E468071
E468072
E468073
E468074
E468075
E468076
E468077
E468078
E468079
E468081
E468082
E468083
E468084
E468085
AU ppm
0.01
0.01
0.00
0.01
0.01
0.01
0.01
0.01
0.02
0.01
0.01
0.02
0.04
0.04
0.03
0.13
0.03
0.07
0.11
0.01
0.75
0.03
0.02
0.02
0.08
MAJOR UNIT
From
1831.10
1831.90
To
1831.90
1840.00
From
1820.50
1821.00
1822.00
1823.00
1824.00
1825.00
1826.00
1826.60
1827.30
1828.10
1829.00
1830.00
1830.60
1831.10
1831.90
1832.70
1833.50
1834.40
1834.90
1835.40
1836.10
1836.70
1837.70
1838.50
1839.10
To
1821.00
1822.00
1823.00
1824.00
1825.00
1826.00
1826.60
1827.30
1828.10
1829.00
1830.00
1830.60
1831.10
1831.90
1832.70
1833.50
1834.40
1834.90
1835.40
1836.10
1836.70
1837.70
1838.50
1839.10
1840.00
MINOR UNIT
From To CommentsComments
Fine grained mafic volcanic, consisting of
equigranular f.g. amphiboles and plagioclases
(60/40). The unit displays 10-15% biotite slips <1mm
wide. Minor Po in a a Qtz-Cc vein (0.3cm wide). No
significant veining.
Fairly similar to previous 4B unit. SIF Mt-chert banded
iron formation with high grunerite (yellow/pale green)
content. The unit is foliated and locally distorted
(weakly sheared?) From 1836.1-1836.7m, the unit is
4Aish with a 4H bands.
Comments
Weak dark green amph
alt'n. The lower
contact is sharp
@90dca.
From 1839.1-1840m,
the unit contains
dark/light green
amphibole rich bands
and Po/Asp at the lower
contact.
ALTERATION
Bio
M
Car Chl Gru
M
Hem Ser Si
W
Comments
biotitic mafic volcanci
4B with high gru content
green amph=alt'n? or is
it primary
LITHOLOGY LOG Page 7 of 22
Unit
2T
4B
Unit
08-NSD-002
Assay
Sample
E468086
E468087
E468088
E468089
E468091
E468092
E468093
E468094
E468095
E468096
E468097
E468098
E468099
AU ppm
0.02
0.07
0.01
0.02
0.01
0.01
0.00
0.08
0.01
0.01
0.01
0.02
0.01
MAJOR UNIT
From
1840.00
1879.00
1887.80
1904.50
1906.40
To
1879.00
1887.80
1904.50
1906.40
1911.50
From
1840.00
1841.00
1902.50
1903.50
1904.50
1905.50
1906.40
1907.00
1907.40
1908.00
1909.00
1909.50
1910.20
To
1841.00
1842.00
1903.50
1904.50
1905.50
1906.40
1907.00
1907.40
1908.00
1909.00
1909.50
1910.20
1911.00
MINOR UNIT
From To CommentsComments
The upper part contains 70% f.g.dark green amph
and f.g.feldspars, 5-8% biotite slips. The unit is cut
by 2% Qtz-Cc veins up to 1cm wide. Dark almost
black in the first 15cm.
Fine grained mafic volcanic consisting of 40%
light/medium green amph, 50% plagioclase and 10%
bio slips/wisps <1mm wide. The unit is cut by 1%
Qtz/Cc veins up to 1cm wide.
Serpentinised Ultramafic. Massive to weakly foliated
ultramafic, varies from f.g. to porphyroblastic locally
(talc). The unit is mainly composed of white-pale
green serpentine (70%) and f.g.-c.g. talc (30%). No
significant veining.
Well developed 4B SIF type. Consisting of alternating
dark grey Mt rich bands up to 2cm wide, yellow/light
green grunerite (higher gru content than usual 4B)
and chert bands up to 2cm wide. S2 cleavages well
developed locally.
Well developed 4A, grunerite rich iron formation,
with 8-10% 4B bands throughout (increase from
1909.5-1910.2m). The unit displays 80% pale yellow
wispy grunerite rich bands averaging 2cm wide and
10% chert bands up to 3cm wide.
Comments
The lower part of the
unit is coarser grained
and consists of
equigranular
amph/plagio (25/75).
Almost gabbro texture.
Weak bio alt'n locally.
The lower contact is
sharp @ 90dca.
Decrease of the talc
content in the lower
part of the section. The
lower contact is sharp
@ 70 dca.
No significant veining,
no mineralisation. The
lower contact is
gradational. presence
of light green amph
with 1% garnets over
20cm @ 1905.3.
The unit is folded and
locally seems weakly
sheared (tight folding).
The unit contains 3%
Po over 15cm in short
and irregular veins. The
lower contact is
gradational.
ALTERATION
Bio
W
M
Car Chl Gru
S
Hem Ser Si
W
Comments
5-8% bio slips
c.g.mafic volcanic
(almost gabbro)
biotitic mafic volcanic
UM with serpentine and
talc
grunerite alt'n?
4A with no significant alt'n
LITHOLOGY LOG Page 8 of 22
Unit
2
2T
1
4B
4A
Unit
08-NSD-002
Assay
Sample
E468101
E468102
E468103
E468104
E468105
E468106
E468107
E468108
E468109
E468111
E468112
E468113
E468114
E468115
E468116
E468117
E468118
E468119
E468121
E468122
E468123
AU ppm
0.01
0.07
0.01
0.01
0.02
0.10
0.01
0.01
0.07
0.05
0.13
0.01
0.30
0.29
0.15
0.16
0.30
0.05
0.05
0.05
0.06
MAJOR UNIT
From
1911.50
1913.00
1914.00
1917.30
To
1913.00
1914.00
1917.30
1929.30
From
1911.00
1911.50
1912.50
1913.00
1914.00
1915.00
1916.00
1916.70
1917.30
1918.00
1919.00
1920.00
1921.00
1921.80
1922.80
1923.80
1924.80
1925.80
1926.80
1927.80
1928.50
To
1911.50
1912.50
1913.00
1914.00
1915.00
1916.00
1916.70
1917.30
1918.00
1919.00
1920.00
1921.00
1921.80
1922.80
1923.80
1924.80
1925.80
1926.80
1927.80
1928.50
1929.30
MINOR UNIT
From To CommentsComments
Fairly similar to previous 4B unit. Contains 70% Mt
rich bands and 30% grunerite rich bands. The unit
contains <1% chert. Weak pale green amphibole alt'n
(?). The unit displays <2% Po throughout.
Massive ultramafic, featureless. The unit is mainly
composed of f.g. serpentine, no significant talc. Light
green in colour. Both contacts are sharp (biotite slips
at the contacts): dyke?.
Alternating Mt rich bands averaging 0.8cm wide and
light green/pale yellow grunerite rich bands up to
2cm wide. 4B SIF type, tightly folded locally in the
upper part of the section.
SIF with moderate ligh green amphibole alteration.
The unit has minor shear zones up to 15 cm wide
with wispy green amphibole. Locally there is 3 - 5%
Po associated with these shear zones
1921.8-1922.2, 1922.8-1923.2, 1925.20-1925.40
Comments
The unit is folded. The
lower contact is sharp
@ 75dca.
Appear to be along the
eastern limb. Minor
isoclinal folding
between 1916.7-19.17.2.
From 1925.40 down
section there is a
decrease in green
amphibole and an
increase in grunerite
alteration.
ALTERATION
Bio Car Chl Gru
M
M
S
Hem Ser Si Comments
gru alt'n?
UM with serpentine
is gru alt'n?
LITHOLOGY LOG Page 9 of 22
Unit
4B
1
4B
4B
Unit
08-NSD-002
Assay
Sample
E468124
E468125
E468126
E468127
E468128
E468129
E468131
AU ppm
0.01
0.00
0.01
0.05
0.02
0.00
0.01
MAJOR UNIT
From
1929.30
1932.50
1933.60
1937.20
1951.00
1955.00
1979.00
To
1932.50
1933.60
1937.20
1951.00
1955.00
1979.00
1985.40
From
1929.30
1929.70
1930.70
1931.50
1932.60
1933.60
1934.60
To
1929.70
1930.70
1931.50
1932.60
1933.60
1934.60
1935.60
MINOR UNIT
From
1990.50
1991.10
To
1990.70
1991.40
Comments
see major description
Comments
Alternating bands of chert (10-20 cm wide ) and
grunerite layers ( 3-5 cm wide). There is very weak
green amphibole alteration and only trace
mineralization.
Fine grained 4B (SIF) with alternating bands of
magnetite (1-3cm wide) and chert bands 3-5cm wide
rimmed with moderate green amphibole alteration.
Fine to medium grained biotitic mafic basalt with 20%
green amphibole and 5% coarse calcite veining. with
5% biotite slips also present.
Serpentinised Ultramafic. Amorphous looking ultra-
mafic with strong serpentine. The lower part of the
section has elongated mafic mineral Pyroxene??
Medium to coarse grained mafic volcanic with with a
strongly bleached section between 1951.70-1952.
The unit becomes medium grained and with strong
green amphibole and calcite veining.
Fine to medium grained biotitic mafic basalt with
minor brown section of 2T between (1963-19655).
There is an increase in biotite down section local
biotite slips between 1-2 cm wide.
Fine to mediun grained 2T the unit has moderate
green amphibole alteration and then this is an
increase in biotite down section from 1982 to
1985.1m. The unit is a typical 2T.
Comments
Minor section of
strong magnite
between 1931.20 to
1931.70. Massive Po
vein between 2 cm
wide between
1931.18-1931.20
Varies from massive
ultramafic. Minor calcite
veining. The lower
contact is gradational.
There is an intense
shear zone from
1985.10-1986.40 where
the unit is sheared
between 1985.1 -
1985.5 and then
brecciated with strong
green amphibole to
1986.40.
ALTERATION
Bio
W
W
W
M
S
W
S
S
M
M
Car
M
W
M
Chl Gru Hem Ser Si Comments
biotitic mafic volcanic.
LITHOLOGY LOG Page 10 of 22
Unit
4A
4B
2
1
2
2
2T
Unit
13
13
08-NSD-002
Assay
Sample
E468132
E468133
AU ppm
0.00
0.01
MAJOR UNIT
From
1985.40
1990.00
2003.00
2009.00
2024.00
2028.40
2028.80
To
1990.00
2003.00
2009.00
2024.00
2028.40
2028.80
2045.50
From
2043.50
2044.50
To
2044.50
2045.50
MINOR UNIT
From To CommentsComments
Serpentinised Ultramafic.Typical light grey
serpentinite, mottled and greyish blue. No obvious
talc and the unit is non-magnetic. The unit is pale
green with salt and pepper textured white serpentine.
Fine to Medium grained biotitic mafic basalt in the
upper section and hosts 2 minor lamprophyre dykes
between 1990.5 -1990.7 and the second between
1991.10-1991.4
Unusual UM, strongly fractured . Appears to be an
intrusive. The unit is medium grained and
equigranular. Composed of of white mineral, not soft
enough to be serpentine or talc. May be an Amphibole?
Medim grained brown 2T with weak green amphibole
ateration. The unit has local biotite slips and is
moderately sheared between 2014.4-2015.5
Fine grained mafic volcanic that is intensly fractured
with a poor RQD 5 sections greater than 10 cm wide.
The remainder of unit is poker chip like between .1
to 5cm wide
Olivine lamprophyre dyke with sharp contacts;
bt-carb groundmass with carbonate and subrounded
mineral fragments very similar to the unit between
1991.1 -1991.4
Fine to medium grained brown to 2T with local biotite
slips .5 to 2 cm wide. The unit has weak calcite
veining. associated with biotite slips making giving a
pitted appreance .
Comments
local sections are very
soft and pitted.
olivine lamprophyre
dyke with sharp
contacts; bt-carb
groundmass with minor
olivine. Downhole the
unit is a strongly
developed 2T. The unit
is moderately
fractured between
1999-2000m.
Although not soft the
unit is still pitted in a
light grey to buff matrix.
Moderate chlorite along
fracture surfaces and
no strong slickenslides
are present.
The last 1.3m of the
unit appear to be
weakly bleached (more
beige than
greyish/brown).
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 11 of 22
Unit
1
2T
1
2
2
13
2T
Unit
08-NSD-002
Assay
Sample
E468134
E468135
E468136
E468137
E468138
E468139
E468141
AU ppm
0.14
0.13
0.01
0.01
0.00
0.00
0.16
MAJOR UNIT
From
2045.50
2047.10
2052.00
To
2047.10
2052.00
2053.00
From
2045.50
2046.50
2047.10
2048.10
2050.20
2051.20
2052.20
To
2046.50
2047.10
2048.10
2049.10
2051.20
2052.20
2053.00
MINOR UNIT
From To CommentsComments
Strongly distorted and folded 4B (appears to have
been SIF) unit consists of ~thin laminations and
wisps of Mt (2045.5-2045.7m there is weak adjacent
grun), ~3mm-1.2cm thick bands of chert (dist),
~10-15% qtz blebs and veins, with weak associated
light-
Fine grained, massive-weakly foliated, mafic volcanic
unit. From 2047.1-2048.4m, unit is
weakly-moderately bleached and from 2048-2048.5
there are 10% bio slips, (1-0.4mm thick). Remainder
of unit is f.g.-aphanitic, with few random 1mm qtz/Cc
veinlets,
Similar to above described 4B/4C unit, moderately
distorted and consisting of thin Mt bands (~1-4mm
thick), hi % Cc veinlets, weak qtz vein/blebs (mostly
between2052.7-2052.9m) with moderate associated
dark green amph alt'n. There is distorted
Comments
medium green amph
alt'n and ~10-25% Cc
veins (4C?) and within
strongly dist sections
of the unit, . There is
~2% disseminated Po
(few blebs). From
2046.5-2046.6m there
is a small intercalated
section of mafics.
weakly biotized
(homogeneous). It
becomes more c.g.
from 2051.5-2052.2m.
Moderately fractured
throughout. Upper
contact is irregular,
and lower contact is
sharp.(Jemma.C)
vein of Po @ 2052.45m
(Po covering fracture
surfaces) as well as a
smaller vein @ 2052.8
and a large bleb (~2 by
5cm) @ 2052.95m.
There is a weak amount
of chl/grt alt @
2052.75m. U.C is
sharp and L.C is
gradational.
ALTERATION
Bio
M
W
Car
M
S
Chl Gru Hem Ser Si
W
W
W
W
Comments
LITHOLOGY LOG Page 12 of 22
Unit
4B
2
4B
Unit
08-NSD-002
Assay
Sample
E468142
E468143
E468144
E468145
AU ppm
0.01
0.01
0.00
0.01
MAJOR UNIT
From
2053.00
2090.40
2092.10
2106.50
2130.70
To
2090.40
2092.10
2106.50
2130.70
2137.90
From
2053.00
2054.00
2136.00
2137.00
To
2054.00
2055.00
2137.00
2137.90
MINOR UNIT
From
2137.00
To
2137.90
Comments
K feldspar see major description
Comments
Biotitic mafic basalt with weak to moderate foliation.
From 2053-2054.3m and 2057-2060m mod bio slips
exist (weak bio slips are present throughout), the rest
of the unit is aphanitic and weakly biotized with 4%
qtz/Cc veinlets, and veins
Light green, fine to medium grained 2T . The unit is
strongly pitted with a light green matrix incl
moderate green amphibole (20%) and calcite (15%)
Varies from massive homogenous ultramafic and is
strongly distorted with strongly calcite veining from
2098.2-2099.9m; weakly sheared.
Fresh looking biotitic mafic basalt with 5% calcite
veining 1-2 cm wide. Strong quartz calcite veing is
present between 2114.4-2115.5 with wispy green
amphibole present and more mineralization is present.
The unit is 2T/2 , greyish brwon and best developed
down hole. There is a Calcite-quartz vein between
2132.8-2132.6 T
Comments
(qtz veins are
0.2-10mm wide
throughout).Cc vein
from
2066.95-2067.05m.
Core is strong open
space faullting between
from
2056.4-2056.65m.
There is an increase in
biotite down hole.
Wispy calcite veins are
also presnt that range
between 4 - 7 cm in
width. The lower contact
is along a 10 cm calcite
vein.
Talc and fibrous
serpentine are both
present within the
matrix and along
fracture planes of the
unit; patchy light green
amphibole alteration
The matrix of the unit
becomes coarser down
hole between 2126.5 -
2130.70
The lower 80 cm of the
unit may have strong K
feldspar alteration as it
takes on a ligh pink
colour. Moderate light
green amphibole
alteration.
ALTERATION
Bio
W
S
W
S
Car
W
W
M
M
W
Chl Gru Hem Ser Si Comments
talc serpentine
LITHOLOGY LOG Page 13 of 22
Unit
2
2T
1
2
2T
Unit
2T
08-NSD-002
Assay
Sample
E468146
E468147
E468148
E468149
E468151
E468152
E468153
E468154
AU ppm
0.01
0.00
0.08
0.01
0.01
0.01
0.01
2.91
MAJOR UNIT
From
2137.90
2139.40
2140.40
2141.30
2145.20
To
2139.40
2140.40
2141.30
2145.20
2145.80
From
2137.90
2138.80
2139.40
2140.00
2140.40
2141.30
2144.20
2145.20
To
2138.80
2139.40
2140.00
2140.40
2141.30
2142.30
2145.20
2145.80
MINOR UNIT
From To CommentsComments
Not a typical 4E, the unit has a strongly magnetic
section between 2138.2 - 2138.8m with minor
bands of clustered garnets elongated parallel to the
foliation. One well developed garnet 1cm in diameter
at the U.C.
NIF Northern Iron Formation (?) with strong green
amphibole alteration and well banded with magnetite
bands that vary in size from a mm to 3 cm wide.
Chert bands are .5 to 2 cm and less abundant.
Intensely sheared 4E with section of coalescing
garnets; 15% Po mineralization surrounding clusters
of garnet aggregates.
Biotitic mafic volcanic grey green in colour with 30 -
40% f.g.green amphiboles. With up to 25% biotite
down section there is increase in quartz calcite
veining. with a moderate shear zone consisting of
quartz flooding with trace Po.
Small 4E with banded green amphibole and and
garnet layers 2- 5 cm wide. 2% Po disseminated
between 2145.4- 2145.5. The unit is moderately
sheared with associated quartz calcite veining.
Comments
The unit displays 15%
Po mineralization
between strong
magnetite bands
(Bordering on a 4H).
From 2138.8-2137.3m
there is strong pale
green amphibole
alteration.
Bands of magnetite are
altered to green
amphibole. Mm scale
folding between 2140 -
2140.. Strong garnet
alteration between
2140.20 - 2140.25.The
unit is weakly sheared
with 4-5% Po.
There is moderate light
green alteration.
ALTERATION
Bio
M
M
Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 14 of 22
Unit
4E
4B
4E
2
4E
Unit
08-NSD-002
Assay
Sample
E468155
AU ppm
0.00
MAJOR UNIT
From
2145.80
2158.80
2168.60
2169.80
2177.70
2188.70
2194.70
To
2158.80
2168.60
2169.80
2177.70
2188.70
2194.70
2206.70
From
2145.80
To
2147.00
MINOR UNIT
From To CommentsComments
Fine to medium grained fresh looking basalt with up
to 15% biotite and 40-50% f.g. green amphibole. 40%
plagioclase with 5-10% biotite alteration throughout
the unit. Diffuse scattered calcite veins 1 -2 cm wide.
Strongly serpentinized ultramafic with greasy feeling
fracture planes. The U.C. is strongly distorted then
grading into a weakly foliated amorphous texture. The
unit is blue - grey to off white.
Strongly bleached mafic volcanic with light green
amphibole alteration. and biotite laths 4 mm in length.
Fine grained biotitic mafic volcanic (10-15% biotite).
The unit has strong alternating zonation of rich green
amphibole and more bleached looking bands; difuse
calcite veining is also present.
Serpentinised Ultramafic. Light grey green, mottled
looking with porphyroblasts of white talc. The unit is
locally weakly magnetic. Composed of pale green to
white serpentine and is serp'd along fracture planes.
Intercalated section of mafic and Ultramafics with
strong calcite alteration.
Well foliated f.g mafic with ~5-10% Cc stringers and
patchy alt'n. Joint surfaces are biotised and f.g
biotite in the matrix ranges from 0-10%.
Comments
There is a descrease in
biotie alteration down
hole. The unit bleached
looking from 2158-2158.8
Minor intercalated
section of mafic
volcanics which display
local biotite
slips.Minor blocky
section between
2162-2162.30. The L.C
is also strongly distorted.
Fine fiberous actinolite
present down hole.
2196.5-2197.5m is
distorted weakly
sheared section with
mottled strongly
biotised and light grey
bleached patchy
texture. 2202.4-2203m
is mod sheared and well
foliated with pervasive
Cc alt'n and is grey
brown 2T ish in colour.
ALTERATION
Bio
W
M
W
M
M
Car
M
M
W
S
M
M
Chl Gru Hem Ser
M
Si Comments
LITHOLOGY LOG Page 15 of 22
Unit
2
1
2T
2
1
1
2
Unit
08-NSD-002
Assay
Sample
E468156
E468157
E468158
E468159
E468161
E468162
E468163
E468164
E468165
E468166
E468167
AU ppm
0.00
0.00
0.01
0.13
0.01
0.04
0.05
0.01
0.02
0.33
0.13
MAJOR UNIT
From
2206.70
2211.10
2211.80
2213.60
To
2211.10
2211.80
2213.60
2218.30
From
2210.10
2211.10
2211.80
2212.50
2213.00
2213.60
2214.30
2215.00
2216.00
2217.00
2217.50
To
2211.10
2211.80
2212.50
2213.00
2213.60
2214.30
2215.00
2216.00
2217.00
2217.50
2218.30
MINOR UNIT
From To CommentsComments
Poorly to moderately foliated light green grey unit with
joint surfaces ranging from weakly to strongly
serpentinised. No biotite.
Fine grained, foliated, hard, fresh, medium green,
mafic rock without the light green serp' ultramafic
appearance. No biotite.
Chert, poorly to strongly magnetic SIF consisting of
laminated dark grey laminae and bands of Mt and
straw yellow grunerite.
Mostly thick massive bands 3-25cm of f.g matrix of
grunerite and Mt, alternating with patches of finely
banded Mt and grun.
Comments
Fresh surfaces exhibit
m.g, equigranular, light
to medium amphiboles
with the usual
hard-to-describe
ultramafic texture about
them .
The unit has open
folding and moderately
developed S2 foliation
in places. Several
crosscutting irregular
qtz veins 1-2cm wide.
1% thin chert
laminations. ~50%
grun/~50% Mt.
2212.5-2213m has 1%
scattered blebs of Po.
Only ~5% scattered
chert bands 2-10mm
hence not a 4A. The
banding is generally
folded and weakly
distorted. 2% patchy
irregular qtz veins.
Few patches with very
minor Po grains.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 16 of 22
Unit
1
2
4B
4B
Unit
08-NSD-002
Assay
Sample
E468168
E468169
E468171
E468172
E468173
E468174
E468175
E466776
E466777
E466778
AU ppm
0.01
0.01
0.01
0.01
0.05
0.02
0.38
0.01
0.00
0.01
MAJOR UNIT
From
2218.30
2222.70
2224.50
2234.80
To
2222.70
2224.50
2234.80
2238.90
From
2218.30
2219.40
2220.40
2221.30
2221.80
2222.70
2223.20
2223.70
2224.50
2225.50
To
2219.40
2220.40
2221.30
2221.80
2222.70
2223.20
2223.70
2224.50
2225.50
2226.40
MINOR UNIT
From To CommentsComments
Well banded (to laminated in places) straw yellow
grunerite (~40%) and chert (~55%) with ~5% Mt
bands. Very gradational in lower 70cm. Folded in
places, planar in others. No mineralisation.
Finely banded to laminated Mt (~50%) and grunerite
(~40%) layers with about 10% chert. The unit is
tightly folded in the upper 1m with moderately to well
developed S2 fabric.
Fine to medium grained light grey-green ultramafic
unit consisting of softer serpentinised amphibole
mixed with fresher amphibole in the matrix.
UC-2236.4m is well foliated light green grey rock but
fresher than above unit with much less serpentine
and 1-3% biotite in parts. The rock here is soft, very
light in colour and weakly serp'd especially on joint
surfaces.
Comments
2221.4-2221.7m is an
unusual very c.g
mixture of coarse
purplish garnets
5-10mm with matrix of
green amph and
grunerite, very unusual
looking, no Po.
One Z-fold and
scattered specks of Po
at UC. The lower 1m is
planar and laminated on
the 1-3mm scale.
Parts of the unit are
coarse grained and
serp'd with g.s 2-4mm,
other parts of the unit
are very well foliated
and f.g. A few (~5% of
the unit) patches also
have 1-5% biotite in
the matrix.
The contact at 2236.4m
grades evenly in to
weakly foliated c.g
crystalline ultramafic
unit with grains size
1-4mm. Could be
logged as gabbro but
there is zero plag and
the several joints are
sepr'd rather than
biotised.
ALTERATION
Bio
W
M
Car Chl Gru Hem Ser
M
W
M
W
Si Comments
LITHOLOGY LOG Page 17 of 22
Unit
4A
4B
1
1
Unit
08-NSD-002
Assay
Sample AU ppm
MAJOR UNIT
From
2238.90
2253.90
2257.70
2265.00
2272.70
2275.10
2278.30
2287.40
To
2253.90
2257.70
2265.00
2272.70
2275.10
2278.30
2287.40
2287.80
From To
MINOR UNIT
From To CommentsComments
Well to moderately foliated medium to darker green
f.g mafic unit with a few parts up to 10% biotite. The
rock is very fresh and hard with no joints.
Light grey to light greenish fine grained homogeneous
unit with zero biotite. The rock is fairly fresh and
generally poorly serpentinised but some joint surface
display soft serpentine. At UC is a long 7mm wide
vein filled with soft serpentine.
Well foliated, medium green mafic rock with close to
zero biotite in the matrix. The matrix contains
approx 15-20% white plagioclase with ~75% darker
to medium green amphibole.
Serpentinised Ultramafic. Fine grained light greenish
ultramafic, moderately to strongly serpentinised. Zero
biotite. Patches with 100% intense serp'n
scratchable with finger nail.
Well foliated medium green mafic with ~30% bands
of grey bleaching of the amphibole. Hard and fresh
with no biotite alt'n.
Serpentinised Ultramafic. Fine grained light green
pale ultramafic, easily scratched with a tool and well
serpentinised joint surfaces. No biotite.
Well foliated typical mafic rock with very abundant
bands & sections of moderate grey bleaching of the
amphibole. 15-25% plagioclase in the matrix.
UC is conformable, LC cross cuts the foliation. The
unit is intrusive grey-black lamprophyre consisting of
about ~80% f.g shiny phlogopite matrix with ~20%
rounded soft light-grey grains.
Comments
The rock does not look
ultramafic based largely
on the slight differences
in crystalline texture
and darker green colour.
The ultramafic is
largely distinguished
from mafic by the f.g
homogeneous much
lighter colour of the
rock and total lack of
biotite with minor serp.
The crystalline texture
is a lot more apparent in
this 2 than in the 1
ultramafic above.
Some irregular qtz
veining at around
2269m, and a 20cm qtz
vein at 2270.6m. Fairly
sharp and well defined
contacts.
The matrix consists of
~75% amphibole and
25% plagioclase.
No biotite, no serp.
~1-3% scattered Cc
veinlets.
One of these rounded
grains is ~13mm
across and is glassy
grey-green in colour-
possibly a piece of
olivine/peridotite.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 18 of 22
Unit
2
1
2
1
2
2
13
Unit
08-NSD-002
Assay
Sample
E466779
E466781
E466782
E466783
E466784
E466785
AU ppm
0.00
0.00
0.00
0.00
0.01
0.00
MAJOR UNIT
From
2287.80
2329.90
2331.80
2333.10
2336.10
2351.50
2353.60
To
2329.90
2331.80
2333.10
2336.10
2351.50
2353.60
2355.10
From
2332.10
2333.10
2333.90
2334.70
2335.40
2354.10
To
2333.10
2333.90
2334.70
2335.40
2336.10
2355.10
MINOR UNIT
From To CommentsComments
Well foliated typical mafic rock with numerous
sections of grey bleaching of the amphibole. The rock
is fresh and unaltered and is not semi-ultramafic.
High mag on reflex at 2315m, unexplained, perhaps
proximal to an iron formation not intersected (?).
Well foliated, fine grained, homogeneous ultramafic
with borderline interbanded 1 & 2 in the lower 1m.
No biotite.
Well foliated green grey mafic. Medium green in
colour with 15% patches of borderline light green
ultramafic.
Light pale green grey, appears reasonably fresh and
unaltered but some joints are evidently serpentised
and the rock is easily scratched with a nail.
Well foliated, medium green, m.g mafic rock with few
patches of very weak biotite alt'n. The rock is hard,
unaltered and impossible to scratch with a nail.
Fine to medium grained moderately foliated
ultramafic. Light green in colour and only weakly
serpentinised. No biotite.
Medium green, well foliated elongate amphibole
grains and ~15% plagioclase. No biotite alt'n.
Couple patches of grey bleaching.
Comments
2294-2296m has biotite
in the matrix ranging
from 1-10%.
Plagioclase makes up
~10-20% of the
matrix. Weak to mod
biotite alt'n
2307.5-2309.9m with
~5-10% biotite.
Very weakly
serpentinised
80cm in the centre of
the unit is brittle
fracture with
anastomising angular
networks of c.g
crystalline qtz and
light brown mineral -
cummingtonite?- c.g
grunerite?
ALTERATION
Bio Car Chl Gru
M
Hem Ser
W
W
Si Comments
brittle fracture networks
with c.g crystalline qtz
and light medium brown
mineral- possibly
cummingtonite?
LITHOLOGY LOG Page 19 of 22
Unit
2
1
2
1
2
1
2
Unit
08-NSD-002
Assay
Sample
E466786
E466787
E466788
E466789
E466791
E466792
E466793
E466794
E466795
E466796
E466797
E466798
E466799
AU ppm
0.02
0.01
0.09
0.05
0.01
0.01
0.02
0.01
0.03
0.15
0.33
0.01
0.00
MAJOR UNIT
From
2355.10
2355.80
2363.80
2364.30
2365.90
To
2355.80
2363.80
2364.30
2365.90
2378.70
From
2355.10
2355.80
2356.80
2357.30
2358.00
2359.00
2360.00
2361.00
2362.10
2363.20
2363.80
2364.30
2368.90
To
2355.80
2356.80
2357.30
2358.00
2359.00
2360.00
2361.00
2362.10
2363.20
2363.80
2364.30
2365.30
2369.90
MINOR UNIT
From To CommentsComments
Well foliated moderately soft rock consisting of
~35% m.g biotite in a matrix with grey amphibole.
Fairly jointed, with very soft joint surfaces that display
serpentine.
The unit is a fairly homog' unit of planar chert (50%)
and bands of f.g qtz-grun +/- green amph. The grun
is very pale in colour and gives many bands an
orange colour when wet; ~30% of the unit has
grey-green grunerite instead.
Classic 4H, well foliated and consists of ~30% Po
throughout the dark brown unit consisting
predominatly of f.g argillitic matrix. Moderately sheared.
Well foliated biotised mafic rock consisting of ~35%
m.g biotite in matrix of green-grey biotite. A few
scattered Cc veinlets 5-10mm wide.
Well foliated, fine to medium grained mafic unit with
fairly abundant irregular patches and blotchy veins
of Cc alt'n associated with nearby moderate shearing
at 2370.7-2371.2m, the shear also contains some qtz
veining. No min'zn.
Comments
The rock may be a
strongly biotised
ultramafic, or biotised
borderline ultramafic.
Dark green blotchy
amph alt'n and no
biotite in the 15cm at LC.
2356.8-2357.3m is
well min'zd (~5% Po) of
poorly sheared (just
high strain really) f.g
green grunerite and qtz;
2363.3-LC is similar
and has only 1% Po.
The rest of the unit is
totally unmin'zd and
undeformed. Banding
is of the 1-10cm scale.
~7% Cc alt'n throughout
the unit. No biotite, no
garnets.
No serpentine at all.
Patches of weak biotite
alt'n are also seen
around the Cc alt'n and
deformation, along with
penetrative light green
amphibole alt'n around
Cc veining.
ALTERATION
Bio
M
W
Car
M
S
Chl Gru Hem Ser
S
Si
W
Comments
LITHOLOGY LOG Page 20 of 22
Unit
2T
4A
4H
2T
2
Unit
08-NSD-002
Assay
Sample
E466801
E466802
E466803
E466804
E466805
E466806
E466807
E466808
E466809
E466811
E466812
E466813
E466814
E466815
E466816
AU ppm
0.00
0.00
0.00
0.01
0.00
0.01
0.01
0.00
0.01
0.01
0.00
0.01
0.00
0.01
0.03
MAJOR UNIT
From
2378.70
2382.10
2404.10
To
2382.10
2404.10
2420.50
From
2369.90
2370.70
2371.20
2384.30
2385.30
2385.90
2386.90
2387.90
2388.90
2389.80
2390.90
2391.90
2392.40
2403.10
2404.10
To
2370.70
2371.20
2372.20
2385.30
2385.90
2386.90
2387.90
2388.90
2389.80
2390.90
2391.90
2392.40
2393.40
2404.10
2405.00
MINOR UNIT
From To CommentsComments
The unit is fairly homogeneous crystalline mafic rock
with equigranular equant grain size of 2-4mm. The
unit must be very mafic gabbro due to near complete
lack of any interstitial plagioclase.
Well foliated fine grained homogeneous, fresh,
green-grey mafic rock with 0-1% biotite in some
places. There is a patch of Po min'zn at 2392m
associated with Cc and green amph alt'n.
With the exception of 2413.2-2416.6m the whole unit
is very homogeneous and consists of intensely
sheared, vey well foliated dark brown, very f.g,
argillitic (and biotitic & graphitic?) matrix.
Couple patches of Cc alt'n in 2407-2409m.
EOH=2420.5m
Comments
Overall the rock
consists of 2-3% biotite
alt'n in scattered thin
<1mm seams and 99%
c.g green amphibole
grains. There is a
25cm band of f.g well
foliated rock with grad'
contacts at 2380.7m
which may be a shear.
Two significant shears
at 2385.3-2385.9m and
2388.9-2389.8m
consist of irregular
Cc-Qtz veins, Cc alt'n
minor biotite alt'n, and
some patches of light
green amph alt'n
around Cc veinlets.
Intense pervasive Cc
alt'n 2396.7-2398.9m.
~15% semi-angular
sheared qtz fragments
are distributed
throughout along with
~18% Po min'zn.
2413.2-2416.6m is
different by the
medium-f.g matrix
ALTERATION
Bio
W
Car
S
M
S
Chl Gru Hem Ser Si
W
Comments
seems to be associated
with crosscutting
structure.
LITHOLOGY LOG Page 21 of 22
Unit
7A
2
4H
Unit
08-NSD-002
Assay
Sample
E466817
E466818
E466819
E466821
E466822
E466823
E466824
E466825
E466826
E466827
E466828
E466829
E466831
E466832
E466833
E466834
E466835
AU ppm
0.09
0.04
0.08
0.05
0.16
0.10
0.58
0.06
0.11
0.03
0.06
0.05
0.05
0.44
0.04
0.21
0.10
MAJOR UNIT
From ToFrom
2405.00
2406.00
2407.00
2408.00
2409.00
2410.00
2411.00
2412.10
2413.20
2414.00
2415.00
2416.00
2416.60
2417.50
2418.00
2419.00
2420.00
To
2406.00
2407.00
2408.00
2409.00
2410.00
2411.00
2412.10
2413.20
2414.00
2415.00
2416.00
2416.60
2417.50
2418.00
2419.00
2420.00
2420.50
MINOR UNIT
From To CommentsComments Comments
ALTERATION
Bio
S
Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 22 of 22
Unit Unit
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
0
3
6
9
12
15
18
21
24
27
30
33
36
39
42
45
48
51
54
57
60
63
66
69
72
75
78
81
84
87
90
93
96
99
102
105
108
111
114
117
120
123
126
129
132
135
138
141
144
147
150
153
156
159
Azimuth
84.169
84.29
85.23
86.15
87.27
88.17
89.27
89.21
89.44
89.66
89.72
89.54
90.26
89.49
90.21
90.83
91.45
91.67
91.5
91.03
91.84
91.98
92.19
91.85
91.64
91.85
92.09
92.3
91.83
91.84
92.02
91.76
91.89
92.32
92.79
92.62
92.64
92.25
92.33
92.67
92.95
93.21
92.93
92.73
92.18
92.09
92.09
92.3
92.44
91.99
92.28
92.53
92.17
92.36
Dip
-85.729
-85.71
-85.73
-85.73
-85.66
-85.54
-85.49
-85.48
-85.49
-85.48
-85.46
-85.45
-85.47
-85.43
-85.4
-85.41
-85.42
-85.45
-85.41
-85.39
-85.35
-85.42
-85.39
-85.38
-85.37
-85.36
-85.32
-85.33
-85.33
-85.34
-85.32
-85.29
-85.27
-85.28
-85.26
-85.24
-85.23
-85.2
-85.15
-85.08
-85.05
-85.09
-85.08
-85.01
-85.02
-85.02
-84.99
-84.98
-84.96
-84.95
-84.92
-84.95
-84.96
-84.96
SurveyType
Surv
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
162
165
168
171
174
177
180
183
186
189
192
195
198
201
204
207
210
213
216
219
222
225
228
231
234
237
240
243
246
249
252
255
258
261
264
267
270
273
276
279
282
285
288
291
294
297
300
303
306
309
312
315
318
321
Azimuth
92.75
92.56
92.65
92.58
92.97
93.11
93.26
93.48
93.78
93.76
93.8
93.82
94.08
93.66
93.89
94.12
93.97
93.76
93.71
93.93
94.55
94.96
95.09
95.26
95.29
95.28
95.25
95.3
95.41
95.61
95.56
95.37
95.04
94.92
95.34
95.39
95
94.86
95.4
95.28
95.29
95.65
95.5
95.48
95.38
95.12
95.09
95.49
95.49
96
95.69
95.24
94.82
95.01
Dip
-84.97
-84.95
-84.91
-84.93
-84.93
-84.89
-84.9
-84.86
-84.82
-84.85
-84.84
-84.78
-84.8
-84.75
-84.73
-84.67
-84.67
-84.61
-84.57
-84.47
-84.45
-84.47
-84.42
-84.37
-84.37
-84.35
-84.3
-84.27
-84.24
-84.22
-84.21
-84.18
-84.14
-84.11
-84.1
-84.13
-84.19
-84.2
-84.2
-84.23
-84.16
-84.21
-84.25
-84.19
-84.22
-84.25
-84.2
-84.23
-84.22
-84.2
-84.2
-84.2
-84.15
-84.15
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
324
327
330
333
336
339
342
345
348
351
354
357
360
363
366
369
372
375
378
381
384
387
390
393
396
399
402
405
408
411
414
417
420
423
426
429
432
435
438
441
444
447
450
453
456
459
462
465
468
471
474
477
480
483
Azimuth
95.65
95.49
95.33
95.69
96.05
96.06
96.11
96.03
96.5
97.24
97.54
98.05
98.43
99.63
100.1
99.95
100.4
100.83
100.96
100.93
100.81
100.88
101.1
101.46
101.17
101.11
101.09
101.71
101.36
100.93
100.94
101.81
101.74
101.98
102.08
102.07
101.83
101.85
102.18
101.8
101.9
102.44
102.41
102.15
102.03
102.47
102.53
101.6
102.91
102.9
103.47
103.01
103.58
103.45
Dip
-84.15
-84.14
-84.12
-84.16
-84.11
-84.09
-84.06
-84.06
-84.06
-84.06
-84.02
-84.05
-84.12
-84.13
-84.11
-84.11
-84.06
-84.04
-84.03
-83.99
-83.96
-83.96
-83.95
-83.96
-83.96
-84
-83.96
-83.92
-83.91
-83.92
-83.88
-83.87
-83.9
-83.87
-83.82
-83.8
-83.83
-83.82
-83.79
-83.79
-83.74
-83.75
-83.79
-83.74
-83.73
-83.73
-83.7
-83.7
-83.7
-83.67
-83.66
-83.57
-83.58
-83.55
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
486
489
492
495
498
501
504
507
510
513
516
519
522
525
528
531
534
537
540
543
546
549
552
555
558
561
564
567
570
573
576
579
582
585
588
591
594
597
603
606
609
612
615
618
621
624
627
630
633
636
639
642
645
648
Azimuth
103.91
103.85
103.87
104.68
105.18
105.44
106.16
106.73
107.45
108.18
109.08
109.21
109.89
111.23
111.58
112.69
114.11
114.65
114.65
114.73
115.22
115.52
116.32
116.49
116.83
117.48
117.86
118
118.29
118.88
119.26
119.48
119.85
120.1
120.24
120.33
120.81
119.67
113.62
113.63
114.13
113.94
113.96
113.98
114.4
114.17
114.31
114.44
114.59
114.67
113.54
110.81
109.66
109.8
Dip
-83.5
-83.48
-83.41
-83.39
-83.37
-83.4
-83.39
-83.35
-83.33
-83.31
-83.25
-83.22
-83.24
-83.17
-83.11
-83.02
-82.96
-82.81
-82.74
-82.6
-82.47
-82.39
-82.33
-82.25
-82.16
-82.06
-82
-81.89
-81.83
-81.75
-81.65
-81.6
-81.56
-81.46
-81.39
-81.35
-81.29
-81.16
-80.53
-80.41
-80.36
-80.3
-80.2
-80.15
-80.11
-80.03
-80
-80.01
-79.93
-79.88
-79.81
-79.59
-79.45
-79.39
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
651
654
657
660
663
666
669
672
675
678
681
684
687
690
693
696
699
702
705
708
711
714
717
720
723
726
729
732
735
738
741
744
747
750
753
756
759
762
765
768
771
774
777
780
783
786
789
792
795
798
801
804
807
810
Azimuth
110.15
110.34
110.48
110.49
110.6
110.86
110.78
110.79
110.96
111.3
111.59
111.7
112.03
112.32
112.7
113.36
113.23
111.86
109.18
107.49
107.43
107.57
107.65
107.67
107.81
107.96
107.82
107.83
107.99
107.92
108.18
108.08
108.25
108.4
108.26
108.36
108.42
108.3
108.12
108.18
108.28
108.08
108.19
108.23
108.05
108.23
108.19
108.33
108.51
108.24
108.26
108.48
108.5
108.6
Dip
-79.22
-79.03
-78.82
-78.7
-78.49
-78.3
-78.15
-78.01
-77.86
-77.73
-77.6
-77.51
-77.45
-77.37
-77.29
-77.32
-77.26
-77.15
-76.96
-76.79
-76.79
-76.76
-76.68
-76.65
-76.6
-76.54
-76.49
-76.47
-76.43
-76.34
-76.31
-76.28
-76.26
-76.24
-76.2
-76.24
-76.19
-76.15
-76.11
-76.07
-76.04
-75.97
-75.95
-75.94
-75.93
-75.9
-75.88
-75.84
-75.82
-75.77
-75.8
-75.72
-75.72
-75.68
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
813
816
819
822
825
828
831
834
837
840
843
846
849
852
855
858
861
864
867
870
873
876
879
882
885
888
891
894
897
900
903
906
909
912
915
918
921
924
927
930
933
936
939
942
945
948
951
954
957
960
963
966
969
972
Azimuth
108.65
108.81
108.74
108.82
109
109.14
109.19
109.12
109.02
109.01
109.12
109.09
109.14
109.27
109.06
109.13
109.4
109.38
109.25
109.5
109.62
109.52
109.54
109.7
109.91
109.95
109.95
109.97
110.12
110.11
110.3
110.36
110.23
110.46
111.05
111.15
111.29
111.38
111.18
111.12
111.05
111.17
111.31
111.42
111.51
111.64
111.61
111.08
109.77
109.09
109.18
109.39
109.5
109.15
Dip
-75.6
-75.53
-75.51
-75.44
-75.39
-75.33
-75.31
-75.31
-75.29
-75.24
-75.24
-75.21
-75.17
-75.15
-75.16
-75.05
-74.97
-74.87
-74.79
-74.67
-74.61
-74.58
-74.51
-74.47
-74.45
-74.43
-74.37
-74.31
-74.25
-74.17
-74.07
-73.98
-73.9
-73.88
-73.96
-73.9
-73.81
-73.76
-73.63
-73.49
-73.4
-73.38
-73.36
-73.34
-73.2
-73.13
-73.17
-73.19
-73.04
-72.83
-72.68
-72.45
-72.16
-71.9
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
975
978
981
984
987
990
993
996
999
1002
1005
1008
1011
1014
1017
1020
1023
1026
1029
1032
1035
1038
1041
1044
1047
1050
1053
1056
1059
1062
1065
1068
1071
1074
1077
1080
1083
1086
1089
1092
1095
1098
1101
1104
1107
1110
1113
1116
1119
1122
1125
1128
1131
1134
Azimuth
109.1
109.03
109.23
109.64
109.9
109.8
109.8
109.92
109.92
109.94
110.15
110.12
110.13
110.15
110.15
110
110.1
110.15
110.09
110.22
110.41
110.49
110.56
110.62
110.79
110.82
110.94
111.03
110.94
111.01
111.14
111.15
111.17
111.16
111.37
111.45
111.5
111.73
111.73
111.7
111.82
111.9
111.95
111.94
111.93
112.13
111.97
112.02
112.08
112.09
112.1
112.22
112.38
112.23
Dip
-71.64
-71.4
-71.38
-71.28
-71.14
-71.06
-71.01
-70.96
-70.98
-71
-70.99
-70.97
-70.93
-70.88
-70.83
-70.75
-70.68
-70.57
-70.55
-70.53
-70.52
-70.47
-70.4
-70.34
-70.32
-70.26
-70.2
-70.15
-70.12
-70.08
-70.05
-69.98
-69.92
-69.89
-69.79
-69.74
-69.75
-69.7
-69.61
-69.58
-69.55
-69.51
-69.45
-69.43
-69.35
-69.32
-69.3
-69.24
-69.21
-69.2
-69.12
-69.04
-68.95
-68.81
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1137
1140
1143
1146
1149
1152
1155
1158
1161
1164
1167
1170
1173
1176
1179
1182
1185
1188
1191
1194
1197
1200
1203
1206
1209
1212
1215
1218
1221
1224
1227
1230
1233
1236
1239
1242
1245
1248
1251
1254
1257
1260
1263
1266
1269
1272
1275
1278
1281
1284
1287
1290
1293
1296
Azimuth
112.02
112
112.03
111.97
112
111.92
111.82
111.8
111.77
111.79
111.73
111.78
111.88
111.85
111.82
111.93
112.1
112.02
112.11
112.16
112.23
112.3
112.33
112.28
112.33
112.35
112.37
112.25
112.34
112.32
112.37
112.42
112.53
112.6
112.64
112.74
112.67
112.68
112.77
112.86
112.82
112.94
112.89
112.89
113.08
112.99
112.99
113.05
112.96
112.9
112.99
112.83
112.9
112.89
Dip
-68.66
-68.56
-68.51
-68.37
-68.27
-68.19
-68.07
-67.95
-67.78
-67.64
-67.52
-67.43
-67.37
-67.29
-67.28
-67.22
-67.19
-67.2
-67.22
-67.17
-67.23
-67.17
-67.13
-67.07
-67.02
-66.91
-66.88
-66.9
-66.89
-66.87
-66.86
-66.8
-66.76
-66.7
-66.7
-66.64
-66.63
-66.59
-66.59
-66.59
-66.55
-66.53
-66.57
-66.52
-66.5
-66.47
-66.47
-66.4
-66.37
-66.34
-66.31
-66.29
-66.21
-66.19
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1299
1302
1305
1308
1311
1314
1317
1320
1323
1326
1329
1332
1335
1338
1341
1344
1347
1350
1353
1356
1359
1362
1365
1368
1371
1374
1377
1380
1383
1386
1389
1392
1395
1398
1401
1404
1407
1410
1413
1416
1419
1422
1425
1428
1431
1434
1437
1440
1443
1446
1449
1452
1455
1458
Azimuth
112.91
112.91
112.95
112.83
112.86
112.86
112.77
112.77
112.74
112.68
112.62
112.6
112.47
112.6
112.57
112.66
112.69
112.47
112.2
111.88
111.55
111.47
111.38
111.2
111.06
111
110.9
110.89
110.72
110.62
110.26
109.84
109.74
109.83
109.77
109.66
109.6
109.59
109.66
109.66
109.59
109.63
109.7
109.86
110.07
110.09
110.15
110.16
110.12
110.17
110.22
110.23
110.3
110.25
Dip
-66.2
-66.14
-66.13
-66.09
-66.08
-66.04
-65.99
-65.95
-65.86
-65.79
-65.72
-65.66
-65.67
-65.69
-65.03
-64.36
-64.07
-63.97
-63.92
-63.83
-63.75
-63.69
-63.6
-63.5
-63.4
-63.31
-63.22
-63.19
-63.19
-63.09
-62.69
-62.26
-62.11
-62.15
-62.18
-62.19
-62.2
-62.2
-62.19
-62.17
-62.16
-62.13
-62.13
-62.14
-62.08
-62.01
-61.97
-61.84
-61.74
-61.62
-61.53
-61.4
-61.27
-61.16
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1461
1464
1467
1470
1473
1476
1479
1482
1485
1488
1491
1494
1497
1500
1503
1509
1512
1515
1518
1521
1524
1527
1530
1533
1536
1539
1542
1545
1548
1551
1554
1557
1558.5
1560
1561.5
1563
1564.5
1566
1567.5
1569
1570.5
1572
1573.5
1575
1576.5
1578
1579.5
1581
1582.5
1584
1585.5
1587
1588.5
1590
Azimuth
110.07
110.13
110.16
110.12
110.09
110.14
110.11
110.14
110.2
110.24
110.25
110.2
110.29
110.26
110.27
110.55
110.66
110.58
110.29
110.15
110.17
110.19
110.19
110.08
109.86
109.61
109.4
109.08
108.6
107.91
107.72
107.76
107.75
107.66
107.59
107.6
107.59
107.63
107.6
107.5
107.46
107.56
107.55
107.35
107.02
106.38
105.45
104.48
103.72
103.18
102.82
102.67
102.66
102.69
Dip
-61.07
-61.01
-60.95
-60.89
-60.82
-60.77
-60.69
-60.62
-60.53
-60.41
-60.33
-60.23
-60.13
-60.04
-59.99
-59.93
-59.77
-59.24
-58.78
-58.55
-58.49
-58.51
-58.43
-58.37
-58.27
-58.19
-58.02
-58.06
-58.45
-58.68
-58.49
-58.33
-58.3
-58.27
-58.24
-58.25
-58.22
-58.16
-58.14
-58.17
-58.18
-58.06
-57.72
-57.28
-56.77
-56.11
-55.39
-54.72
-54.2
-53.76
-53.47
-53.37
-53.33
-53.33
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1591.5
1593
1594.5
1596
1597.5
1599
1600.5
1602
1603.5
1605
1608
1611
1614
1617
1620
1623
1626
1629
1632
1635
1638
1641
1644
1647
1650
1653
1656
1659
1662
1665
1668
1671
1674
1677
1680
1683
1686
1689
1692
1695
1698
1701
1704
1707
1710
1713
1716
1719
1722
1725
1728
1731
1734
1737
Azimuth
102.68
102.62
102.52
102.45
102.38
102.28
102.22
102.22
102.17
102.13
102.25
102.29
102.41
102.48
102.52
102.55
102.64
102.77
102.81
102.92
102.95
103
103.16
103.16
103.13
103.09
103.03
103.03
103.14
103.14
103.13
103.12
103.15
103.17
103.18
103.2
103.22
103.19
103.16
103.12
103.16
103.15
103.18
103.24
103.21
103.26
103.31
103.29
103.31
103.37
103.36
103.38
103.42
103.35
Dip
-53.28
-53.18
-53.1
-53.02
-52.96
-52.88
-52.81
-52.75
-52.7
-52.67
-52.56
-52.46
-52.32
-52.14
-52.08
-51.95
-51.87
-51.79
-51.71
-51.61
-51.51
-51.4
-51.27
-51.17
-51.1
-50.99
-50.93
-50.79
-50.69
-50.53
-50.39
-50.3
-50.2
-50.08
-49.96
-49.84
-49.75
-49.67
-49.58
-49.48
-49.41
-49.31
-49.25
-49.17
-49.11
-49.02
-48.93
-48.87
-48.81
-48.74
-48.68
-48.61
-48.57
-48.51
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1740
1743
1746
1749
1752
1755
1758
1761
1764
1767
1770
1773
1776
1779
1782
1785
1788
1791
1794
1797
1800
1803
1806
1809
1812
1815
1818
1821
1824
1827
1830
1833
1836
1839
1842
1845
1848
1851
1854
1857
1860
1863
1866
1869
1872
1875
1878
1881
1884
1887
1890
1893
1896
1899
Azimuth
103.25
103.21
103.13
103.12
103.13
103.19
103.17
103.07
102.95
102.84
102.78
102.72
102.62
102.58
102.5
102.45
102.47
102.46
102.48
101.88
101.96
102.03
102.03
102.01
102.07
102.1
102.11
102.03
102.16
102.18
102.34
102.34
102.39
102.49
102.51
102.67
102.76
102.9
103.02
103.14
103.28
103.39
103.51
103.66
103.76
103.9
104.07
104.17
104.31
104.42
104.52
104.61
104.71
104.85
Dip
-48.44
-48.38
-48.3
-48.21
-48.14
-48.09
-47.99
-47.88
-47.78
-47.68
-47.56
-47.46
-47.34
-47.22
-47.09
-47
-46.9
-46.84
-46.78
-46.28
-46.21
-46.12
-46.04
-45.94
-45.81
-45.66
-45.47
-45.28
-45.07
-44.91
-44.72
-44.54
-44.39
-44.27
-44.17
-44.05
-43.91
-43.77
-43.64
-43.51
-43.39
-43.28
-43.14
-43.01
-42.86
-42.75
-42.62
-42.5
-42.42
-42.36
-42.33
-42.32
-42.27
-42.16
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-002
Project Code: 9320_NSD
Mine Grid Easting: 7230.1737
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A/B-N
Target 2:
Target 3:
Drill Start Date: 12/07/2008
Drill End Date: 08/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1902
1905
1908
1911
1914
1917
1920
1923
1926
1929
1932
1935
1938
1941
1944
1947
1950
1953
1956
1959
1962
1965
1968
2009
2057
2117
2164
2213
2267
2315
2361
2411
Azimuth
104.98
105.07
105.04
105.09
105.06
104.99
105.01
104.98
104.97
105.01
105.1
105.15
105.16
105.24
105.35
105.34
105.22
105.17
104.94
104.66
104.38
104.06
103.71
102.5
100
100
100
100
100
99
99
108.3
Dip
-42.06
-41.94
-41.84
-41.71
-41.6
-41.48
-41.3
-41.15
-41.05
-40.95
-40.85
-40.77
-40.77
-40.74
-40.8
-40.84
-40.83
-40.76
-40.64
-40.51
-40.4
-40.28
-40.15
-35.4
-33.8
-33.7
-33.1
-30.8
-28.6
-27.8
-27.3
-27
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
EZS
EZS
EZS
EZS
EZS
EZS
EZS
EZS
EZS
Actual Depth: 2420.5
Planned Depth: 2100
UTM East
Hole ID: 08-NSD-003
Project Code: 9320_NSD
Mine Grid Easting: 7230.173
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A
Target 2:
Target 3:
Drill Start Date: 13/09/2008
Drill End Date: 29/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ
UTM North:
Survey
Depth
0
3
6
9
12
15
18
21
24
27
30
33
36
39
42
45
48
51
54
57
60
63
66
69
72
75
78
81
84
87
90
93
96
99
102
105
108
111
114
117
120
123
126
129
132
135
138
141
144
147
150
153
156
159
Azimuth
84.169
84.29
85.23
86.15
87.27
88.17
89.27
89.21
89.44
89.66
89.72
89.54
90.26
89.49
90.21
90.83
91.45
91.67
91.5
91.03
91.84
91.98
92.19
91.85
91.64
91.85
92.09
92.3
91.83
91.84
92.02
91.76
91.89
92.32
92.79
92.62
92.64
92.25
92.33
92.67
92.95
93.21
92.93
92.73
92.18
92.09
92.09
92.3
92.44
91.99
92.28
92.53
92.17
92.36
Dip
-84.169
-85.71
-85.73
-85.73
-85.66
-85.54
-85.49
-85.48
-85.49
-85.48
-85.46
-85.45
-85.47
-85.43
-85.4
-85.41
-85.42
-85.45
-85.41
-85.39
-85.35
-85.42
-85.39
-85.38
-85.37
-85.36
-85.32
-85.33
-85.33
-85.34
-85.32
-85.29
-85.27
-85.28
-85.26
-85.24
-85.23
-85.2
-85.15
-85.08
-85.05
-85.09
-85.08
-85.01
-85.02
-85.02
-84.99
-84.98
-84.96
-84.95
-84.92
-84.95
-84.96
-84.96
SurveyType
SURV
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1352
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-003
Project Code: 9320_NSD
Mine Grid Easting: 7230.173
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A
Target 2:
Target 3:
Drill Start Date: 13/09/2008
Drill End Date: 29/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ
UTM North:
Survey
Depth
162
165
168
171
174
177
180
183
186
189
192
195
198
201
204
207
210
213
216
219
222
225
228
231
234
237
240
243
246
249
252
255
258
261
264
267
270
273
276
279
282
285
288
291
294
297
300
303
306
309
312
315
318
321
Azimuth
92.75
92.56
92.65
92.58
92.97
93.11
93.26
93.48
93.78
93.76
93.8
93.82
94.08
93.66
93.89
94.12
93.97
93.76
93.71
93.93
94.55
94.96
95.09
95.26
95.29
95.28
95.25
95.3
95.41
95.61
95.56
95.37
95.04
94.92
95.34
95.39
95
94.86
95.4
95.28
95.29
95.65
95.5
95.48
95.38
95.12
95.09
95.49
95.49
96
95.69
95.24
94.82
95.01
Dip
-84.97
-84.95
-84.91
-84.93
-84.93
-84.89
-84.9
-84.86
-84.82
-84.85
-84.84
-84.78
-84.8
-84.75
-84.73
-84.67
-84.67
-84.61
-84.57
-84.47
-84.45
-84.47
-84.42
-84.37
-84.37
-84.35
-84.3
-84.27
-84.24
-84.22
-84.21
-84.18
-84.14
-84.11
-84.1
-84.13
-84.19
-84.2
-84.2
-84.23
-84.16
-84.21
-84.25
-84.19
-84.22
-84.25
-84.2
-84.23
-84.22
-84.2
-84.2
-84.2
-84.15
-84.15
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1352
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-003
Project Code: 9320_NSD
Mine Grid Easting: 7230.173
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A
Target 2:
Target 3:
Drill Start Date: 13/09/2008
Drill End Date: 29/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ
UTM North:
Survey
Depth
324
327
330
333
336
339
342
345
348
351
354
357
360
363
366
369
372
375
378
381
384
387
390
393
396
399
402
405
408
411
414
417
420
423
426
429
432
435
438
441
444
447
450
453
456
459
462
465
468
471
474
477
480
483
Azimuth
95.65
95.49
95.33
95.69
96.05
96.06
96.11
96.03
96.5
97.24
97.54
98.05
98.43
99.63
100.1
99.95
100.4
100.83
100.96
100.93
100.81
100.88
101.1
101.46
101.17
101.11
101.09
101.71
101.36
100.93
100.94
101.81
101.74
101.98
102.08
102.07
101.83
101.85
102.18
101.8
101.9
102.44
102.41
102.15
102.03
102.47
102.53
101.6
102.91
102.9
103.47
103.01
103.58
103.45
Dip
-84.15
-84.14
-84.12
-84.16
-84.11
-84.09
-84.06
-84.06
-84.06
-84.06
-84.02
-84.05
-84.12
-84.13
-84.11
-84.11
-84.06
-84.04
-84.03
-83.99
-83.96
-83.96
-83.95
-83.96
-83.96
-84
-83.96
-83.92
-83.91
-83.92
-83.88
-83.87
-83.9
-83.87
-83.82
-83.8
-83.83
-83.82
-83.79
-83.79
-83.74
-83.75
-83.79
-83.74
-83.73
-83.73
-83.7
-83.7
-83.7
-83.67
-83.66
-83.57
-83.58
-83.55
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1352
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-003
Project Code: 9320_NSD
Mine Grid Easting: 7230.173
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A
Target 2:
Target 3:
Drill Start Date: 13/09/2008
Drill End Date: 29/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ
UTM North:
Survey
Depth
486
489
492
495
498
501
504
507
510
513
516
519
522
525
528
531
534
537
540
543
546
549
552
555
558
561
564
567
570
573
576
579
582
585
588
591
594
597
600
603
606
609
612
615
618
621
624
627
630
633
636
639
642
645
Azimuth
103.91
103.85
103.87
104.68
105.18
105.44
106.16
106.73
107.45
108.18
109.08
109.21
109.89
111.23
111.58
112.69
114.11
114.65
114.65
114.73
115.22
115.52
116.32
116.49
116.83
117.48
117.86
118
118.29
118.88
119.26
119.48
119.85
120.1
120.24
120.33
120.81
119.67
116.02
113.62
113.63
114.13
113.94
113.96
113.98
114.4
114.17
114.31
114.44
114.59
114.67
113.54
110.81
109.66
Dip
-83.5
-83.48
-83.41
-83.39
-83.37
-83.4
-83.39
-83.35
-83.33
-83.31
-83.25
-83.22
-83.24
-83.17
-83.11
-83.02
-82.96
-82.81
-82.74
-82.6
-82.47
-82.39
-82.33
-82.25
-82.16
-82.06
-82
-81.89
-81.83
-81.75
-81.65
-81.6
-81.56
-81.46
-81.39
-81.35
-81.29
-81.16
-80.83
-80.53
-80.41
-80.36
-80.3
-80.2
-80.15
-80.11
-80.03
-80
-80.01
-79.93
-79.88
-79.81
-79.59
-79.45
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1352
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-003
Project Code: 9320_NSD
Mine Grid Easting: 7230.173
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A
Target 2:
Target 3:
Drill Start Date: 13/09/2008
Drill End Date: 29/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ
UTM North:
Survey
Depth
648
651
654
657
660
663
666
669
672
675
678
681
684
687
690
693
696
699
702
705
708
711
714
717
720
723
726
729
732
735
738
741
744
747
750
753
756
759
762
765
768
771
774
777
780
783
786
789
792
795
798
801
804
807
Azimuth
109.8
110.15
110.34
110.48
110.49
110.6
110.86
110.78
110.79
110.96
111.3
111.59
111.7
112.03
112.32
112.7
113.36
113.23
111.86
109.18
107.49
107.43
107.57
107.65
107.67
107.81
107.96
107.82
107.83
107.99
107.92
108.18
108.08
108.25
108.4
108.26
108.36
108.42
108.3
108.12
108.18
108.28
108.08
108.19
108.23
108.05
108.23
108.19
108.33
108.51
108.24
108.26
108.48
108.5
Dip
-79.39
-79.22
-79.03
-78.82
-78.7
-78.49
-78.3
-78.15
-78.01
-77.86
-77.73
-77.6
-77.51
-77.45
-77.37
-77.29
-77.32
-77.26
-77.15
-76.96
-76.79
-76.79
-76.76
-76.68
-76.65
-76.6
-76.54
-76.49
-76.47
-76.43
-76.34
-76.31
-76.28
-76.26
-76.24
-76.2
-76.24
-76.19
-76.15
-76.11
-76.07
-76.04
-75.97
-75.95
-75.94
-75.93
-75.9
-75.88
-75.84
-75.82
-75.77
-75.8
-75.72
-75.72
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1352
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-003
Project Code: 9320_NSD
Mine Grid Easting: 7230.173
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A
Target 2:
Target 3:
Drill Start Date: 13/09/2008
Drill End Date: 29/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ
UTM North:
Survey
Depth
810
813
816
819
822
825
828
831
834
837
840
843
846
849
852
855
858
861
864
867
870
873
876
879
882
885
888
891
894
897
900
903
906
909
912
915
918
921
924
927
930
933
936
939
942
943.5
945
946.5
948
949.5
951
952.5
954
955.5
Azimuth
108.6
108.65
108.81
108.74
108.82
109
109.14
109.19
109.12
109.02
109.01
109.12
109.09
109.14
109.27
109.06
109.13
109.4
109.38
109.25
109.5
109.62
109.52
109.54
109.7
109.91
109.95
109.95
109.97
110.12
110.11
110.3
110.36
110.23
110.46
111.05
111.15
111.29
111.38
111.18
111.12
111.05
111.17
111.31
111.42
111.26
111.24
111.42
111.58
111.77
112.01
112.26
112.49
112.62
Dip
-75.68
-75.6
-75.53
-75.51
-75.44
-75.39
-75.33
-75.31
-75.31
-75.29
-75.24
-75.24
-75.21
-75.17
-75.15
-75.16
-75.05
-74.97
-74.87
-74.79
-74.67
-74.61
-74.58
-74.51
-74.47
-74.45
-74.43
-74.37
-74.31
-74.25
-74.17
-74.07
-73.98
-73.9
-73.88
-73.96
-73.9
-73.81
-73.76
-73.63
-73.49
-73.4
-73.38
-73.36
-73.34
-73.28
-73.09
-72.67
-72.14
-71.65
-71.29
-71.02
-70.82
-70.72
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1352
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-003
Project Code: 9320_NSD
Mine Grid Easting: 7230.173
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A
Target 2:
Target 3:
Drill Start Date: 13/09/2008
Drill End Date: 29/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ
UTM North:
Survey
Depth
957
958.5
960
961.5
963
964.5
966
967.5
969
970.5
972
973.5
975
976.5
978
979.5
981
982.5
984
985.5
987
988.5
990
991.5
993
994.5
996
997.5
999
1000.5
1002
1003.5
1005
1006.5
1008
1009.5
1011
1012.5
1014
1015.5
1017
1018.5
1020
1023
1026
1029
1032
1035
1038
1041
1044
1047
1050
1053
Azimuth
112.69
112.9
113.07
113.11
113.1
112.95
112.9
112.99
112.91
112.83
112.91
112.89
112.98
113
113.02
113.04
112.87
112.71
112.74
112.69
112.65
112.59
112.5
112.51
112.61
112.57
112.61
112.64
112.64
112.63
112.58
112.47
112.43
112.49
112.48
112.51
112.48
112.41
112.54
112.71
112.93
113.19
113.33
113.55
113.6
113.78
113.91
114.03
114.04
114.08
113.93
113.77
113.68
113.73
Dip
-70.65
-70.5
-70.34
-70.21
-70.09
-69.96
-69.82
-69.68
-69.54
-69.46
-69.4
-69.34
-69.31
-69.28
-69.2
-69.11
-69.03
-68.89
-68.67
-68.44
-68.17
-67.88
-67.66
-67.49
-67.34
-67.3
-67.26
-67.17
-67.08
-67.05
-67.01
-66.96
-66.89
-66.78
-66.72
-66.72
-66.68
-66.58
-66.32
-65.8
-65.08
-64.53
-64.28
-64.16
-64.07
-63.97
-63.85
-63.78
-63.71
-63.61
-63.56
-63.52
-63.52
-63.46
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1352
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-003
Project Code: 9320_NSD
Mine Grid Easting: 7230.173
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A
Target 2:
Target 3:
Drill Start Date: 13/09/2008
Drill End Date: 29/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ
UTM North:
Survey
Depth
1056
1059
1062
1065
1068
1071
1074
1077
1080
1083
1086
1089
1092
1095
1098
1101
1104
1107
1110
1113
1116
1119
1122
1125
1128
1131
1134
1137
1140
1143
1146
1149
1152
1155
1158
1161
1164
1167
1170
1173
1176
1179
1182
1185
1188
1191
1194
1197
1200
1203
1206
1209
1212
1215
Azimuth
113.71
113.81
113.84
113.85
113.84
113.82
113.81
113.73
113.75
113.63
113.62
113.61
113.64
113.73
113.69
113.85
113.99
114.05
113.93
113.8
113.66
113.53
113.41
113.27
113.17
113.01
112.84
112.7
112.57
112.43
112.29
112.23
112.17
112.12
112.07
112
112.04
111.94
112.04
112.23
112.12
112.19
112.22
112.15
112.25
112.35
112.37
112.54
112.45
112.4
112.35
112.26
112.1
112.12
Dip
-63.38
-63.29
-63.15
-63.06
-62.98
-62.93
-62.84
-62.77
-62.75
-62.7
-62.68
-62.66
-62.64
-62.6
-62.61
-62.64
-62.62
-62.63
-62.64
-62.61
-62.53
-62.52
-62.5
-62.51
-62.47
-62.42
-62.36
-62.32
-62.3
-62.28
-62.21
-62.09
-62.01
-61.96
-61.93
-61.91
-61.86
-61.91
-61.9
-61.9
-61.89
-61.88
-61.8
-61.7
-61.6
-61.49
-61.43
-61.43
-61.47
-61.45
-61.43
-61.35
-61.27
-61.19
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1352
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-003
Project Code: 9320_NSD
Mine Grid Easting: 7230.173
Mine Grid Northing: 14779.783
Elevation: 5296.61
Target 1: PQD-A
Target 2:
Target 3:
Drill Start Date: 13/09/2008
Drill End Date: 29/09/2008
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ
UTM North:
Survey
Depth
1262
1310
Azimuth
112
112
Dip
-60.1
-60
SurveyType
EZS
EZS
Actual Depth: 1352
Planned Depth: 2200
UTM East
08-NSD-003
MAJOR UNIT
From
0.00
950.00
967.10
969.90
992.90
998.20
999.70
1002.40
1012.30
1012.90
To
950.00
967.10
969.90
992.90
998.20
999.70
1002.40
1012.30
1012.90
1021.70
MINERALS
As%Cp%
0.1
0.5
Mt%
Po%
1.0
1.0
1.5
0.0
0.1
1.0
0.8
Py%
2
Comments
po stringers in
sed
VGSpecks
FABRIC
From
955.00
982.00
995.90
999.70
1003.70
1006.00
To
956.00
983.00
996.90
1000.70
1004.00
1007.00
Alphadeg
30
30
60
50
80
70
Comments
very weak
fabric
weak
fabric in
felsic
Int
WE
WE
MO
WE
WE
WE
Type
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ-C
QZ
Vein%
5
1
Tex ContactType
I
Alphadeg
70
Comments
irregular
qtz-cc
veins in
sediment/4
E
irregular
veins/veinlet
s in 4F
From
992.90
1004.50
To
998.20
1011.00
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
No
3D
6
3D
6
4E
2
4F
4E
4F
Cont
90
55
38
STRUCTURAL LOG Page 1 of 6
08-NSD-003
MAJOR UNIT
From
1021.70
1022.60
1036.70
1038.30
1044.70
1047.30
1056.80
1058.60
1063.10
1069.00
1072.20
To
1022.60
1036.70
1038.30
1044.70
1047.30
1056.80
1058.60
1063.10
1069.00
1072.20
1083.00
MINERALS
As%Cp%
Mt%
Po%
4.0
2.0
0.0
0.2
Py% CommentsVGSpecks
FABRIC
From
1046.00
1064.00
1080.00
To
1047.00
1065.00
1081.00
Alphadeg
52
90
58
CommentsInt
INT
Type
S2
S0
S0
FOLD
To
1021.00
1030.00
1061.00
1072.30
Alpha
deg
50
90
45
54
CommentsInt
WE
WE
MO
WE
Type
FD
FD
FD
FD
From
1020.00
1029.50
1060.00
1071.50
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From
1067.30
To
1067.80
Alphadeg
45
CommentsInt
MOD
Type
SZ
MajorUnit
4E
4F
4E
1
1
1
1
4F
4B
4EA
4B
Cont
50
75
10
50
55
50
90
40
90
80
70
STRUCTURAL LOG Page 2 of 6
08-NSD-003
MAJOR UNIT
From
1083.00
1086.20
1087.70
1099.20
1102.20
1111.30
1131.20
1131.60
1141.90
1155.70
1158.60
1159.90
1162.80
1166.20
To
1086.20
1087.70
1099.20
1102.20
1111.30
1131.20
1131.60
1141.90
1155.70
1158.60
1159.90
1162.80
1166.20
1182.80
MINERALS
As%Cp%
Mt%
Po%
0.2
0.5
1.0
4.0
1.5
0.1
Py% CommentsVGSpecks
FABRIC
From
1088.00
1094.00
1116.00
1126.00
1131.20
1134.00
1150.00
1160.00
To
1089.00
1095.00
1117.00
1127.00
1131.60
1135.00
1151.00
1161.00
Alphadeg
46
70
50
38
75
53
65
72
CommentsInt
WE
MO
MO
MO
Type
S0
S0
S1
S1
S0
S2
S1
S0
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
CA
Vein%
50
Tex
m
ContactType
S
Alphadeg
75
CommentsFrom
1156.10
To
1158.00
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
2T
1
4B
4A
1
2T
4B
2T
1
2T
1
4B
2
7A
Cont
63
70
50
90
60
90
90
80
73
60
77
78
56
90
STRUCTURAL LOG Page 3 of 6
08-NSD-003
MAJOR UNIT
From
1182.80
1193.70
1198.00
1204.50
1208.20
1218.30
To
1193.70
1198.00
1204.50
1208.20
1218.30
1220.40
MINERALS
As%Cp%
Mt%
Po%
Py% CommentsVGSpecks
FABRIC
From
1183.50
1185.50
1188.50
1191.50
1193.20
1206.10
1209.10
1212.10
1214.60
1218.10
1218.60
To
1184.00
1186.00
1188.50
1191.50
1193.20
1206.10
1209.10
1212.10
1214.60
1218.10
1218.60
Alphadeg
90
82
80
65
80
50
65
65
60
70
85
CommentsInt
INT
INT
MO
INT
WE
INT
MO
MO
INT
MO
Type
S2
S0
S0
S0
S0
S1
S0
S0
S0
S0
S0
FOLD
To
1182.90
1184.00
1193.40
1211.60
1215.30
1215.50
1216.20
1217.50
Alpha
deg
90
90
40
25
65
40
25
50
Comments
Z-FOLD
WITH
FOLIATIO
N
DIPPING
DOWN
FROM
LEFT
TO RIGHT
Int
MO
INT
WE
WE
INT
MO
INT
MO
Type
ZF
FD
FD
ZF
ZF
ZF
ZF
ZF
From
1182.80
1183.50
1193.40
1211.60
1215.30
1215.50
1216.00
1217.50
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From
1210.50
1212.00
To
1210.50
1212.00
Alphadeg
15
35
Comments
West side up and
East side down
west side up and
right side down.
Int
MOD
INT
Type
KF
KF
MajorUnit
4B
1
7A
2
4B
4A
Cont
65
65
70
STRUCTURAL LOG Page 4 of 6
08-NSD-003
MAJOR UNIT
From
1220.40
1223.30
1225.00
1229.80
1230.10
1231.10
1235.10
1239.00
1249.40
1252.00
1265.05
1265.70
1266.20
1292.50
1301.80
1313.90
To
1223.30
1225.00
1229.80
1230.10
1231.10
1235.10
1239.00
1249.40
1252.00
1265.05
1265.70
1266.20
1292.50
1301.80
1313.90
1352.00
MINERALS
As%Cp%
Mt%
Po%
35.
7.0
3.0
7.0
98.
10.
7.0
Py% CommentsVGSpecks
FABRIC
From
1219.40
1220.10
1225.80
1228.50
1230.40
1232.00
1232.50
1233.50
1233.90
1244.40
1274.80
1295.40
1318.80
1321.90
1336.80
To
1219.40
1220.10
1225.80
1228.50
1230.40
1232.00
1232.50
1233.50
1233.90
1244.40
1274.80
1295.40
1318.80
1321.90
1336.80
Alphadeg
60
90
75
40
50
85
30
50
35
60
60
50
50
65
25
CommentsInt
WE
MO
MO
WE
MO
MO
INT
INT
MO
WE
WE
WE
WE
MO
MO
Type
S1
S0
S1
S1
S1
S1
S1
S0
S0
S1
S1
S1
S1
S1
S1
FOLD
To
1219.40
1219.50
1219.70
1220.10
1226.10
1226.60
1231.40
Alpha
deg
85
70
75
90
90
45
90
Comments
Crenulation
s
Crenulation
s
Int
MO
MO
MO
MO
INT
INT
INT
Type
FD
FD
FD
FD
FD
FD
FD
From
1219.40
1219.50
1219.70
1220.10
1226.10
1226.60
1231.20
QTZ VEINING
VeinType
QZ
QZ-C
QZ
Vein%
95
85
100
Tex
m
m
m
ContactType
S
I
S
Alphadeg
30
35
CommentsFrom
1240.05
1342.05
1349.60
To
1240.40
1342.20
1349.90
FAULT
From
1276.40
To
1276.80
Alphadeg
55
Comments
Uncertain of angle
Int
MOD
Type
SZ
MajorUnit
2
4H
2
4H
4CH
4H
2
2P
2
2
4H
QTZ
2D
7A
2D
2D
Cont
70
60
30
40
60
STRUCTURAL LOG Page 5 of 6
08-NSD-003
MAJOR UNIT
From To
MINERALS
As%Cp%
Mt%
Po%
Py% CommentsVGSpecks
FABRIC
From
1345.20
To
1345.20
Alphadeg
45
CommentsInt
WE
Type
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
Cont
STRUCTURAL LOG Page 6 of 6
08-NSD-003
Assay
Sample
E466836
E466837
E466838
E466839
E466841
E466842
E466843
E466844
E466845
E466846
AU ppm
0.01
0.02
0.02
0.02
0.01
0.02
0.02
0.06
0.02
0.04
MAJOR UNIT
From
0.00
950.00
967.10
969.90
992.90
998.20
To
950.00
967.10
969.90
992.90
998.20
999.70
From
990.90
991.90
992.90
993.90
994.70
995.60
996.60
997.60
998.20
998.80
To
991.90
992.90
993.90
994.70
995.60
996.60
997.60
998.20
998.80
999.70
MINOR UNIT
From To CommentsComments
Wedge off of DDH 07-NSD-008
Weakly foliated (flow?), fairly massive
felsic-intermediate unit. Consisting of very fine
grained 85 % Qtz-feldspar and 10% f.g.biotite. Weak
sericite alt'n throughout, up to 5%. The unit is
distorted , the foliation is local and irregular.
Biotite rich sediment with similar composition as
intermediate-felsic before. The matrix is mainly
composed of equigranulqr Qtz-feldspar with 15-20%
f.g.biotite. The unit contains 3-5% m.g.garnets
(irregular shape) throughout.
Fairly similar to previous flow. Felsic-intermediate
unit, consisting of f.g.Qtz-feldspars (no phenocrysts)
with 5% biotite overall. Weak sericite alt'n throughout.
Presence of one "vein" with biotite filling.
6? The unit consists of pale green amph (probably
secondary, alt'n?), feldspars and qtz. Locally, bands
of felsic (equigranular Qtz-feldspars). The unit
contains 5% biotite throughout. No garnets present.
Can be a garnet-poor 4E?
Weakly-mod developed 4E. The unit displays 50%
typical 4E bands consisting of m.g.garnets in
f.g.green amph rich matrix (bands are irregular and
distorted). Only 2% m.g.garnets are present (=garnet
poor 4E).
Comments
The unit is cut by 1%
Qtz veins (local) up to
2cm wide.
Mineralization occurs
only in traces. The
lower contact is
gradational.
The unit displays <1%
Qtz veins, locally
dismembered. No
sericite alt'n. The lower
contact is gradational.
The unit is cut by 1%
Qtz veins up to 2cm
wide, // to CA. Traces
pyrite.
The unit is cut by 2-3%
irregular Qtz-Cc veins
up to 1cm wide. Po
occurs throughout in
stringers or veinlets
(up to 5-8% over
15cm). The lower
contact is gradational.
The rest of the unit is
more a sediment with
bio-qtz-feld. The unit
contains scattered Po
throughout, up to 2%.
The lower contact is
gradational.
ALTERATION
Bio
W
W
W
Car Chl Gru Hem Ser
W
W
Si
W
W
Comments
intermediate-felsic flow
sediment
inter-felsic flow
secondary (?) pale
green amph
weakly-mod developed 4E
LITHOLOGY LOG Page 1 of 11
Unit
No
3D
6
3D
6
4E
Unit
08-NSD-003
Assay
Sample
E466847
E466848
E466849
E466851
E466852
E466853
E466854
E466855
E466856
E466857
E466858
E466859
E466861
E466862
E466863
E466864
E466865
E466866
E466867
E466868
E466869
E466871
E466872
AU ppm
0.05
0.05
0.03
0.01
0.46
0.08
0.17
0.07
0.03
0.02
0.03
0.03
0.03
0.03
0.02
0.07
0.07
0.02
0.11
0.06
0.07
0.03
0.03
MAJOR UNIT
From
999.70
1002.40
1012.30
1012.90
To
1002.40
1012.30
1012.90
1021.70
From
999.70
1000.70
1001.70
1002.40
1003.00
1003.70
1004.50
1005.50
1006.50
1007.00
1008.00
1009.00
1010.00
1011.00
1012.30
1012.90
1014.00
1015.00
1016.00
1016.70
1019.00
1020.00
1021.00
To
1000.70
1001.70
1002.40
1003.00
1003.70
1004.50
1005.50
1006.50
1007.00
1008.00
1009.00
1010.00
1011.00
1012.30
1012.90
1014.00
1015.00
1016.00
1016.70
1017.50
1020.00
1021.00
1021.70
MINOR UNIT
From To CommentsComments
Fine grained massive equigranular unit, consisting
of 40% biotite, 40% plagioclase and 20%
pale/medium green amph (does not seem to be alt'n).
The upper part contains 2% Qtz veins ranging from
1-5cm wide rimmed by c.g.biotite alt'n.
Well developed 4F, consisting of a f.g. biotite rich
matrix (~10% Qtz) studded by 25% garnets (ranging
from 0.3-1.5cm in diameter). Unit contains 5%
f.g.staurolite where the garnets are porphyroblastic.
Weak c.g.biotite alt'n throughout.
F.g green matrix of amphibole with a scattering of
~3% garnets surrounded by patchey halos of light
green amph alteration.
Poorly to non-foliated gnt-biotite rock with patches
of folding defined by the S0 fabric- which consists
of varying thickness and abundance of gnts and
amount of green amphibole.
Comments
Po and Cpy are
scattered in veins (<1%
throughout). The lower
contact is gradational
(grades into a sediment).
The unit is cut by 2%
Qtz veinlets up to
0.5cm wide. The unit
displays mineralised
small 4E bands up to
20cm (Py and Cpy up
to 1%): @1003m, @
1003.6m,@1003.9m.
ALTERATION
Bio
W
W
W
Car Chl Gru Hem Ser Si
W
Comments
sediment or mafic volcanic
4F with 4E bands
weak hydrothermal alt'n
in 4F
LITHOLOGY LOG Page 2 of 11
Unit
2
4F
4E
4F
Unit
08-NSD-003
Assay
Sample
E466873
E466874
E466875
E466876
E466877
E466878
E466879
E466881
E466882
E466883
E466884
E466885
E466886
E466887
E466888
E466889
E466891
AU ppm
1.37
0.02
0.08
0.03
0.02
0.02
0.02
0.03
0.04
0.04
0.03
0.03
0.18
0.03
0.04
0.18
0.19
MAJOR UNIT
From
1021.70
1022.60
1036.70
1038.30
1044.70
1047.30
1056.80
1058.60
1063.10
To
1022.60
1036.70
1038.30
1044.70
1047.30
1056.80
1058.60
1063.10
1069.00
From
1021.70
1022.60
1023.30
1024.00
1025.00
1033.70
1034.70
1035.70
1036.70
1037.70
1038.30
1058.60
1059.40
1060.50
1061.50
1062.10
1063.10
To
1022.60
1023.30
1024.00
1025.00
1026.00
1034.70
1035.70
1036.70
1037.70
1038.30
1039.30
1059.40
1060.50
1061.50
1062.10
1063.10
1064.20
MINOR UNIT
From To CommentsComments
Distorted folded bands of light and dark green
amphibole with minor chert and 5% large scattered
gnts. 4% Po min'zn.
Poorly to non-foliated gnt-biotite rock with weak
banding in places. Sections of the rock are
porphyritic with gnts 1-5mm scattered within a f.g
biotite-rich matrix.
Very poorly developed 4E consisting of weakly defined
thick banding of green amphibole with bands of 6-like
f.g biotite and qtz. A few scattered garnets.
Homogeneous light grey m.g highly serpentinised
ultramafic rock.
1M Amphibolitic Ultramafic. Fine grained dark green
ultramafic rock with patches of intense chlorite alt'n
suggesting this rock may not be as UM as it looks.
Weakly foliated, exactly the same as the previous
serpentinized ultramafic above at 1038-1044m.
1M Amphibolitic Ultramafic. Exactly the same as
previous 1M except without any CHL alt'n.
Fine grained biotite-qtz matrix with ~20%
equigranular gnt porphs 3-6mm with scattered bands
1-3cm of chert and grunerite.
60% chert bands 5-30mm alternating with laminated
Mt-grun bands and biotite-gnt bands with minor green
amphibole.
Comments
1034m-1036m is light
grey porphyritic rock
similar to a 4F except
the matrix contains a lot
of qtz and only minor
biotite, and with ~10%
grunerite (but its not a
4EA).
Patches of the rock are
weakly serpentinised
however.
Bands become more
closely spaced towards
LC.
Mostly planar banding
with minor undulation.
No min'zn.
ALTERATION
Bio
M
W
Car Chl
M
Gru Hem Ser
S
W
S
Si Comments
LITHOLOGY LOG Page 3 of 11
Unit
4E
4F
4E
1
1
1
1
4F
4B
Unit
08-NSD-003
Assay
Sample
E466892
E466893
E466894
E466895
E466896
E466897
E466898
E466899
E466901
E466902
E466903
E466904
E466905
E466906
E466907
E466908
E466909
E466911
E466912
E466913
E466914
E466915
E466916
E466917
E466918
E466919
E466921
AU ppm
0.37
0.56
0.16
0.25
1.22
0.47
0.02
0.15
0.02
0.01
0.02
0.01
0.01
0.01
0.01
0.01
0.03
0.52
0.02
0.80
0.54
0.02
0.03
0.64
0.59
0.38
0.68
MAJOR UNIT
From
1069.00
1072.20
1083.00
1086.20
1087.70
To
1072.20
1083.00
1086.20
1087.70
1099.20
From
1064.20
1065.30
1066.30
1067.30
1068.00
1069.00
1069.70
1070.40
1071.00
1071.60
1072.20
1073.00
1073.80
1075.00
1076.00
1076.60
1077.60
1078.60
1079.70
1080.70
1081.80
1083.00
1086.70
1087.70
1088.80
1089.80
1090.80
To
1065.30
1066.30
1067.30
1068.00
1069.00
1069.70
1070.40
1071.00
1071.60
1072.20
1073.00
1073.80
1075.00
1076.00
1076.60
1077.60
1078.60
1079.70
1080.70
1081.80
1083.00
1084.00
1087.70
1088.80
1089.80
1090.80
1091.70
MINOR UNIT
From To CommentsComments
Moderately folded grunerite-gnt bands, with 15%
gnt-biotite bands, 15% chert, and 15% dark coloured
biot-green amph bands with minor gnts.
Planar banded Mt and chert with alternating sections
2-4m long of banded chert (45%) with mt and biotite
gnt alt'n, with ssection of laminated bands of Mt with
f.g desseminated grunerite.
Green grey mafic rock with 20-30% m.g biotite
desseminated thoughout the mafic unit. The unit has
a "crinkled" fine (1-5mm scale) S0 fabric defined by
irregular biotite layers.
Very serpentinised, soft ultramafic rock.
Alternating bands of chert and laminated Mt with
grunerite, Scattered qtz veins up to 20cm. No
min'zn. No shears.
Comments
No min'zn, no shears.
Scattered blebs of Po
here and there.
Fairly planar fabric.
ALTERATION
Bio
M
M
M
S
Car Chl Gru Hem Ser
S
Si Comments
LITHOLOGY LOG Page 4 of 11
Unit
4EA
4B
2T
1
4B
Unit
08-NSD-003
Assay
Sample
E466922
E466923
E466924
E466925
E466926
E466927
E466928
E466929
E466931
E466932
E466933
E466934
E466935
E466936
E466937
E466938
E466939
E466941
E466942
E466943
E466944
E466945
AU ppm
0.38
0.43
0.04
0.36
1.28
0.38
0.63
0.17
0.08
0.07
4.61
2.21
0.04
0.08
0.00
0.03
0.00
0.01
0.01
0.01
0.00
0.01
MAJOR UNIT
From
1099.20
1102.20
1111.30
1131.20
1131.60
1141.90
1155.70
To
1102.20
1111.30
1131.20
1131.60
1141.90
1155.70
1158.60
From
1091.70
1092.60
1093.70
1094.70
1095.80
1096.50
1097.50
1098.20
1099.20
1100.00
1100.50
1101.40
1102.20
1103.20
1130.20
1131.20
1131.60
1154.80
1155.70
1156.10
1157.00
1158.00
To
1092.60
1093.70
1094.70
1095.80
1096.50
1097.50
1098.20
1099.20
1100.00
1100.50
1101.40
1102.20
1103.20
1104.10
1131.20
1131.60
1132.60
1155.70
1156.10
1157.00
1158.00
1158.60
MINOR UNIT
From To CommentsComments
Poorly magnetic banded unit consisting of thick
(1-2cm) bands of chert and light straw brown
grunerite with patches of minor green amph alt'n.
Poorly to non-foliated massive light grey soft
serpentinite ultramafic.
Poorly foliated to massive, strongly biotised m.g
mafic consisting of a matrix ~35-40% biotite,~15%
plag, 40-55% green amphibole. The amphibole is
bleached grey in lower 3m with less biotite.
Unusual unit seems to be a cross between 4B & 4E.
Thinly banded to laminated grey Mt with chert 1-5mm
thick, with a few 5-10mm bands of pink gnt-grun,
and some (15%) dark green amphibole rich bands.
Weakly to moderately foliated partly bleached Mafic
rock with m.g biotite alt'n throughout. 20-30% biotite.
Fine grained homogeneous ultramafic with varying
degrees of serpentinsation ranging from weak to
intense. No biotite.
40cm at the UC and 60cm at the LC is poorly to
moderately biotised green grey mafic. The central
part of the unit consists of 45% c.g Cc veins 5-20mm
and 55% brown-grey moderately biotised mafic rock.
Comments
Well sheared in lower
~70cm with abundant
4% Po min'zn. 15%
scattered qtz veins up
to 30cm wide.
1.5% Po overall.
ALTERATION
Bio
S
M
M
Car
S
Chl Gru Hem Ser
S
M
Si Comments
LITHOLOGY LOG Page 5 of 11
Unit
4A
1
2T
4B
2T
1
2T
Unit
08-NSD-003
Assay
Sample
E466946
E466947
E466948
E466949
E466951
E466952
E466953
E466954
E466955
E466956
E466957
E466958
E466959
E466961
E466962
E466963
E466964
E466965
E466966
AU ppm
0.02
0.01
0.01
0.01
0.01
0.00
0.00
0.01
0.01
0.00
0.03
0.34
0.04
0.00
0.01
0.00
0.00
0.01
0.00
MAJOR UNIT
From
1158.60
1159.90
1162.80
1166.20
1182.80
To
1159.90
1162.80
1166.20
1182.80
1193.70
From
1158.60
1159.30
1159.90
1160.90
1161.90
1162.80
1181.80
1182.80
1183.30
1184.00
1185.00
1186.00
1187.00
1188.00
1189.00
1190.00
1191.00
1192.00
1193.00
To
1159.30
1159.90
1160.90
1161.90
1162.80
1163.80
1182.80
1183.30
1184.00
1185.00
1186.00
1187.00
1188.00
1189.00
1190.00
1191.00
1192.00
1193.00
1193.70
MINOR UNIT
From To CommentsComments
Reasonable soft moderately serpentinsed
homogeneous f.g ultramafic rock. No biotite.
Finely banded to laminated clean dark Mt bands
1-6mm with straw coloured grunerite bands/laminae
1-10mm. Planar fabric.
Poorly to moderately foliated mafic rock with 5-10%
m.g patchy biotite alt'n. Grain size is 2-4mm. 5-10%
plagioclase.
Gradational UC and has a consistent grainsize of
2-4mm from UC to 1169.3m. From there to 1182.4m
is very coarse grain sub-equigranular amphiboles
3-7mm with ~10-15% interstitial plagioclase.`
Fine grained, very finely banded to laminated 4B
conistsing of 40% clean dark grey Mt layers 1-5mm,
and 60% straw coloured grunerite layers 1-10mm.
Comments
Looks very much like
the zebra SIF.
40cm at the lower
contact is finer grained
(2-3mm) typical 2-
mafic rock. Weakly
foliated in places.
Tight
foldes1183.5-1184m
with strong 90deg S2
fabric.
ALTERATION
Bio
M
Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 6 of 11
Unit
1
4B
2
7A
4B
Unit
08-NSD-003
Assay
Sample
E466967
E466968
E466969
E466971
E466972
E466973
E466974
AU ppm
0.01
0.01
0.00
0.02
0.08
0.00
0.00
MAJOR UNIT
From
1193.70
1198.00
1204.50
1208.20
To
1198.00
1204.50
1208.20
1218.30
From
1193.70
1194.60
1206.20
1207.20
1208.20
1209.00
1210.00
To
1194.60
1195.60
1207.20
1208.20
1209.00
1210.00
1211.00
MINOR UNIT
From To CommentsComments
1M. Light grey/greenish coloured, massive to weakly
foliated ultramafic with an intense amount of f.g.
medium green coloured amphibole and few distorted
qtz/Cc blebs and veinlets (few with weak associated
dark green amph alt'n). There are a few fracture
Medium grey to greenish coloured gabbro with
intense c.g. amph throughout. Unit is cut by few Cc
veinlets. From 202m-1204.5m the unit becomes
increasingly more f.g. with depth. Both U.C and L.C's
are gradational .
Light grey coloured (green tint to sections), massive
to weakly foliated amfic volcanic unit with Moderate
Cc veins and stringers from 1205.5-1207m with
moderate medium-dark green amph alt'n. O.S. fault or
fractured zone from 1207.5-1207.6m (fracture
Thinly banded tolaminated 4B (SIF) unit consisting of
~ 50% mt bands, ~20% grayish/white chert bands,
~25% chert bands partially-completely overprinted by
grun & ~5% Cc veinlets. Fr 1212.9-1213m unit is
weak-mod distorted & is alt'd with
Comments
surfaces from
1193.8-1194m which
are moderately
serpentinized with weak
talc. From
1196.8-1197.4m there
is an intense amount of
talc (this section is
very soft).The L.C is
gradational. U.C is sharp.
surface seems to be
serpentinized but
surrounding unit seems
to be too hard to be
ultramafic
(uncertain)The last
10cm of the unit
contain amph and
~0.5% Po.
grun overprinting ~75%
of the mt & chert
bands. Fr
2115.2-1215.5m there
is a broad & open fold.
There is an good z fold
fr 1216-1216.2m. The
unit contains a few
minor folds and weakly
distorted patches fr
1216.2 to the end of the
unit.
ALTERATION
Bio Car
W
M
Chl Gru
W
Hem Ser Si Comments
LITHOLOGY LOG Page 7 of 11
Unit
1
7A
2
4B
Unit
08-NSD-003
Assay
Sample
E466975
E466976
E466977
E466978
E466979
E466981
E466982
E466983
E466984
E466985
E466986
E466987
E466988
E466989
E466991
E466992
E466993
E466994
E466995
E466996
AU ppm
0.00
0.00
0.00
0.00
0.02
0.01
0.03
0.25
0.06
0.02
0.01
0.01
0.01
0.05
0.03
0.02
0.01
0.01
0.01
0.09
MAJOR UNIT
From
1218.30
1220.40
1223.30
1225.00
1229.80
To
1220.40
1223.30
1225.00
1229.80
1230.10
From
1211.00
1212.00
1213.00
1214.00
1215.00
1216.00
1217.00
1217.50
1218.30
1219.30
1220.40
1221.40
1222.40
1223.30
1224.00
1225.00
1226.00
1227.80
1228.80
1229.80
To
1212.00
1213.00
1214.00
1215.00
1216.00
1217.00
1217.50
1218.30
1219.30
1220.40
1221.40
1222.40
1223.30
1224.00
1225.00
1226.00
1227.00
1228.80
1229.80
1230.10
MINOR UNIT
From To CommentsComments
Thinly banded unit consisting of ~60% chert bands,
~30% grunerite bands and 5-10% magnetite
laminations. There is the odd qtz veinlet or bleb.
Appears to be a 2cm thick (possibly iron stained)qtz
vein @ 1218.8m Unit is weakly distorted in patches
Light to medium grey coloured, massive to weakly
foliated mafic volcanic unit cut by ~5-10% distorted
Cc veins and veinlets with weak to moderate
associated bio alt'n. U.C is sharp and L.C is diffuse.
Well developed and distorted 4H unit. Consisting of
~60-70% dark grey-black material (seems to be a
mixture of magnetite and graphite) with 30-40% Po
(occurs as distorted veinlets/stringers as well as
semi massive-massive blebs).
Med grey coloured massive-weakly foliated mafic
volcanic unit. Fr 1225.5-1227m there is a mod
amount of Cc & qtz veinlets/stringers with
mod-intense m.g-c.g.bio alt'n (few bands & distorted
slips) with more bio alt'n Fr 1227.6-1228m Few folds
fr 1226-
Similar to 4H above. Moderately developed and
moderate to intensely distorted, dark grey/black
coloured unit (graphite and magnetite), with ~10% Po
stringers throughout) U.C is irregular and L.C is sharp.
Comments
throughout with weak
to moderate folding .
Small Po veinlet in last
5cm of the unit. L.C is
sharp.
Appears to be few minor
folds (M fold from
1224.41224.5m. There
is also ~1-3% qtz
blebs. L.C is irregular
but abrupt.
1226.8m.
ALTERATION
Bio
W
W
M
M
Car
M
W
M
W
Chl Gru
M
S
W
M
Hem Ser Si
W
M
Comments
LITHOLOGY LOG Page 8 of 11
Unit
4A
2
4H
2
4H
Unit
08-NSD-003
Assay
Sample
E466997
E466998
E466999
E467001
E467002
E467003
E467004
AU ppm
0.02
0.01
0.01
0.01
0.02
0.10
0.01
MAJOR UNIT
From
1230.10
1231.10
1235.10
To
1231.10
1235.10
1239.00
From
1230.10
1230.60
1231.10
1232.00
1233.00
1234.10
1235.10
To
1230.60
1231.10
1232.00
1233.00
1234.10
1235.10
1236.10
MINOR UNIT
From To CommentsComments
4CH or 4A. Consists mainly of chert bands separated
by ~0-10% grun laminae (varies) and/or 0-5% light
(little dark) green amph alt'n. Fr 1230.6-1230.7m
has ~3% Po. Fr 1230.7-1231m there is a 3cm thick
massive Po vein as well as a few chert bands
Well developed and distorted 4H unit, dark
grayish/black (graphite and magnetite mixture/weak
to mod magnetic) with ~5-10% qtz blebs (2mm-3cm
in diam) as well ~5-30% Po (% varies and occurs as
wisps/veinlets to an interconnected network
Light greenish/grey coloured, massive mafic
volcanic. Unit is cut by <5% Cc and qtz veins. From
1255.1-1236.2m the unit is moderately to well biotized
(small section of 2t) and massive to weakly foliated.
L.C is gradational.
Comments
separated by 1mm
thick mt lam's. Fr
1231-1231.1m there is
a bio/grt alt'n band
(grts are ~3mm in diam
& anhedral). The
remainder of the unit
contains trace-2% Po
with one massive 3-5cm
thick Po vein @
1231.9m. Broad open
space fault fr
1231.4-1221.7m.
of wisps and veinlets).
Sharp U.C and
irregular L.C.
ALTERATION
Bio
S
Car Chl Gru Hem Ser Si
M
Comments
LITHOLOGY LOG Page 9 of 11
Unit
4CH
4H
2
Unit
08-NSD-003
Assay
Sample
E467005
E467006
E467007
E467008
E467009
AU ppm
0.00
0.00
0.00
0.02
0.00
MAJOR UNIT
From
1239.00
1249.40
1252.00
1265.05
1265.70
To
1249.40
1252.00
1265.05
1265.70
1266.20
From
1236.10
1263.00
1264.00
1265.05
1265.70
To
1237.10
1264.00
1265.05
1265.70
1266.20
MINOR UNIT
From To CommentsComments
Uncertain of unit type. Possibly an amphibolite or a
f.g. gabbro. The unit is massive and made up of
mostly f.g.-m.g. (<1-1mm in diam) amphibole grains
with `1015% pyroxene.. Fr 1240.05m-1240.4m there
is a massive white qtz vein with a sharp U.C and
Massive grayish/greenish coloured mafic volcanic.
Unit is weakly bleached throughout. ~20-25% of the
unit is qtz veined. At 1249.9m there is a 1.2cm in
diam qtz bleb containing couple blebs of cpy.
Massive mafic volcanic unit varying from medium grey
to grey/greenish in colour. Fr1252-1259m the unit is
relatively fresh looking mafics with weak amph and
few qtz or Cc veinlet with the exception of a mod
patch of qtz/Cc veining fr 1252.4-1252.6m
Strongly distorted 4H unit (weakly developed). From
1265.05-1265.35m ~1/2 the core is still mafic due to
the irregular U.C. The unit is made up of a dark
grayish/black matrix with ~15-2-0% qtz (veining and
blebs)
Massive light grey coloured qtz vein (seems to be
some host rock within) with sharp upper and lower
contact. ~3-5% m.g. dark brown bio alt'n. There is ~
3% Po (specks and small blebs).
Comments
irregular L.C.
@1246.2m there is a
small qtz bleb/dist
veinlet with dark
grayish coloured needle
shaped minerals.
Contacts are gradational.
in which there are
several veins containing
a moderate to large
amount of light green
chlorite(very soft). The
remainder of the unit
contains mod-hi % of
amph and is cut by
many qtz veins as well
as Cc veins and veinlets.
with ~5% Po (occurs
as massive blebs and
stringers). The last
0.5cm appear to be
mafic volcanic.
ALTERATION
Bio Car
W
W
W
Chl
M
Gru Hem Ser Si
S
M
S
M
M
S
Comments
LITHOLOGY LOG Page 10 of 11
Unit
2P
2
2
4H
QTZ
Unit
08-NSD-003
Assay
Sample
E467011
E467012
AU ppm
0.00
0.01
MAJOR UNIT
From
1266.20
1292.50
1301.80
1313.90
To
1292.50
1301.80
1313.90
1352.00
From
1266.20
1267.20
To
1267.20
1268.20
MINOR UNIT
From To CommentsComments
Massive, light-medium greenish/grey coloured mafic
volcanic unit with ~ 5-10% pillow selvages
consisting of mostly c.g. amph (some seem to
contain weak-mod chl alt'n & @ 1292.1m the amph is
studded with garnets 2-4mm in diam). The unit is
cut by ~5-10%Cc
Massive gabbro unit consisting m.g-c.g amph with
~20-30% f.g. pyroxene. The unit is cut by the odd
1mm thick Cc veinlets. There are also a few Cc
veins. From 1294.2-1294.5 there is a patch with
strong Cc veining surrounding or including moderate
chl.
Massive, aphanitic-f.g. mafic volcanic, grayish/green
in colour. ~Unit contains ~15% pillow selvages
concentrated in lower portion of the unit, selvages
are made up of m.g. amph and or bio/grt (grts
~1-3mm in diam and anhedral to subhedral).
Continuation of above unit. From Fr 1342.4-1345m
the unit is very fresh with several other 0.4-1m
fresh patches throughout. Fr 1349.6-1349.9m there
is a massive qtz vein with sharp upper and lower
contacts. From 1319-1323m the unit is more c.g. than
Comments
veining and stringers
(~3-5% seems to be
associated with pillows)
& the odd qtz vein. Fr
1276-1276.9m there is
~20% Cc veins and
stringers with mod-
ntense m.g-c.g. bio
alt'n (sheared fr
1276.4-1276.8.
Patches of the unit are
very fresh looking.
Fr 1295.4-1295.6m the
unit is weakly foliated
and f.g. L.C is
gradational.
~30% of the unit is cut
by a network of cross
cutting Cc veinlets with
moderate associated
dark green amph alt'n.
Moderate qtz from
1311.7-1312.1m with
strong bio/grt alt'n.
surrounding unit with
weak to moderate bio
alt'n moderate qtz
blebs/veins and selvages.
ALTERATION
Bio Car
M
W
M
Chl
W
Gru Hem Ser Si
W
W
Comments
LITHOLOGY LOG Page 11 of 11
Unit
2D
7A
2D
2D
Unit
08-NSD-004
MAJOR UNIT
From
0.00
665.00
711.50
712.00
721.40
746.00
788.00
805.00
839.00
855.70
857.80
869.00
988.90
To
665.00
711.50
712.00
721.40
746.00
788.00
805.00
839.00
855.70
857.80
869.00
988.90
997.90
MINERALS
As%Cp%
0.0
Mt%
Po%
2.0
1.0
2.0
Py%
0.01
Comments
traces
chalcopyrite
Po at the
bottom of UM
unit.
f.g Po in the
matrix.
VGSpecks
FABRIC
From
668.00
689.00
707.00
711.50
720.40
764.00
770.00
792.00
806.00
830.00
847.00
854.60
863.00
874.00
879.00
884.00
887.00
893.00
895.20
897.00
898.00
901.00
944.00
952.00
966.00
985.00
992.00
To
689.00
695.00
711.50
720.40
744.00
770.00
782.00
793.00
807.00
831.00
848.00
855.70
864.00
875.00
880.00
885.00
888.00
894.00
896.00
897.50
899.00
902.00
945.00
953.00
967.00
985.30
992.50
Alphadeg
35
40
35
30
45
35
30
25
40
30
30
30
50
50
41
42
40
35
45
50
45
40
35
40
10
65
50
CommentsInt
MO
MO
MO
MO
WE
MO
WE
WE
WE
WE
MO
WE
WE
WE
WE
WE
WE
WE
WE
WE
WE
WE
WE
MO
WE
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S2
S1
S0
S1
S0
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ-C
QZ-C
QZ-C
QZ-C
QZ-C
QZ-C
QZ-C
QZ-C
Vein%
65
80
10
10
30
30
5
15
Tex
m
ContactType
I
I
I
I
D
Alphadeg
40
50
30
40
30
65
Comments
mafic
volcanic
cut by
Cc-[Qtz]
irregular
veins.
irregular
stringers,
hard to
find an
angle.
alpha is
approximate
, the zone
is slightly
brecciatic
irregula
veining
From
695.00
764.00
788.00
805.00
852.00
869.00
874.20
989.00
To
707.00
770.00
805.00
819.00
855.70
874.20
904.50
993.80
FAULT
From
852.00
869.00
To
855.70
874.20
Alphadeg Comments
no quite a
breccia, but strong
irregular veining
not quite a
breccia, but
irregular veining
Int Type
BC
BC
MajorUnit
No
2T
3K
2
2
2
2
3D
3D
1
3D
3D
3M
Cont
35
35
40
30
50
55
STRUCTURAL LOG Page 1 of 13
08-NSD-004
MAJOR UNIT
From
997.90
1000.10
1001.80
1011.90
1013.00
1016.30
1017.80
1019.90
1030.80
1031.90
1032.70
1055.00
To
1000.10
1001.80
1011.90
1013.00
1016.30
1017.80
1019.90
1030.80
1031.90
1032.70
1055.00
1058.70
MINERALS
As%Cp%
Mt%
Po%
0.5
0.3
0.1
0.5
5.0
0.1
0.7
0.5
Py% CommentsVGSpecks
FABRIC
From
997.00
1007.50
1010.40
1019.30
1023.90
1028.30
1031.00
1032.00
1048.00
To
998.00
1007.90
1010.70
1019.70
1024.50
1028.80
1032.00
1039.00
1049.00
Alphadeg
39
40
56
42
25
17
25
70
55
CommentsInt
WE
MO
MO
MO
WE
MO
Type
S2
S0
S1
S0
S1
S1
S0
S2
S1
FOLD
To
1018.50
Alpha
deg
60
CommentsInt
MO
Type
FD
From
1018.30
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
2T
4E
4F
4E
4F
6
4E
4F
6
2U
1
4F
Cont
77
70
73
67
40
40
55
57
45
30
30
50
STRUCTURAL LOG Page 2 of 13
08-NSD-004
MAJOR UNIT
From
1058.70
1061.00
1062.40
1065.60
1069.70
1079.00
1083.00
To
1061.00
1062.40
1065.60
1069.70
1079.00
1083.00
1096.00
MINERALS
As%Cp%
Mt%
Po%
0.1
0.1
0.1
2.0
1.0
Py% Comments
Po in traces in
4E
weakly qtz
veined 4B/4EA
Po in veins
near Qtz veins
VGSpecks
FABRIC
From
1056.00
1060.50
1061.70
1063.40
1064.00
1065.00
1068.00
1070.50
1072.60
1073.00
1076.00
1084.00
To
1057.00
1061.00
1062.40
1064.00
1065.00
1065.60
1069.00
1071.00
1073.00
1074.00
1077.00
1085.00
Alphadeg
50
75
80
40
60
80
70
70
70
70
70
40
CommentsInt
MO
MO
MO
WE
MO
MO
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S2
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1059.70
1069.00
1076.00
Alpha
deg
60
50
70
CommentsInt
MO
MO
MO
Type
ZF
ZF
FD
From
1058.70
1068.00
1075.00
QTZ VEINING
VeinType
QZ
Vein%
3
Tex ContactType
I
Alphadeg
70
Comments
weakly qtz
veined
4EA/4b
From
1062.40
To
1065.60
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
4E
4B
4EA
4EA
4B
1
4B
Cont
60
STRUCTURAL LOG Page 3 of 13
08-NSD-004
MAJOR UNIT
From
1096.00
1100.00
1111.90
1138.30
1153.90
1160.10
1160.90
1163.40
To
1100.00
1111.90
1138.30
1153.90
1160.10
1160.90
1163.40
1181.50
MINERALS
As%Cp%
Mt%
Po%
1.0
1.0
0.5
8.0
15.
0.5
Py% Comments
distorted/qtz
veined 4b
po vein 2cm
wide
well
mineralised 4A
well
mineralised 4A
slightly
magnetic Po in
4b SIF
VGSpecks
FABRIC
From
1089.50
1092.50
1095.00
1113.00
1120.00
1123.00
1127.00
1136.00
1147.00
1161.50
1178.00
To
1090.50
1093.50
1096.00
1114.00
1121.00
1124.00
1128.00
1137.00
1148.00
1162.50
1179.00
Alphadeg
60
50
90
40
45
50
50
50
55
90
60
CommentsInt
MO
MO
MO
MO
WE
MO
MO
MO
WE
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ
QZ
QZ-C
Vein%
5
5
30
Tex ContactType
I
Alphadeg
90
Comments
distorted/qtz
flooded
zone in 4b
distorted,
qtz
flooded
zone in 4b
approx
angle
From
1087.30
1088.80
1153.90
To
1088.30
1089.50
1160.10
FAULT
From
1087.30
1088.80
1098.70
1106.40
To
1088.30
1089.50
1099.10
1106.50
Alphadeg
55
70
Comments
more distorted
than sheared in 4B
more distorted
than sheared
chlorite, pieces
are wet
small fault gouge
with small pieces
and chlorite
Int
WEK
WEK
MOD
MOD
Type
SZ
SZ
GG
GG
MajorUnit
4A
1
2T
1
2
1
4B
7A
Cont
90
90
STRUCTURAL LOG Page 4 of 13
08-NSD-004
MAJOR UNIT
From
1181.50
1192.40
1197.10
1210.00
1212.60
1213.30
1219.40
1222.20
1230.40
1253.40
To
1192.40
1197.10
1210.00
1212.60
1213.30
1219.40
1222.20
1230.40
1253.40
1283.00
MINERALS
As%Cp%
Mt%
Po%
0.1
1.0
0.5
1.0
1.0
1.0
Py% Comments
distorted 4B
SIF at contact
with UM
po in veins in
4B SIF type
Po in fractrues
filling or along
foliation plans
in 4B SIF
mineralised 4A
Qtz veined
and
mineralised 4A
VGSpecks
FABRIC
From
1181.50
1186.50
1190.50
1204.00
1213.70
1218.00
1225.00
1253.00
1262.00
To
1182.50
1187.50
1191.40
1205.00
1214.00
1219.00
1226.00
1253.40
1263.00
Alphadeg
80
90
65
85
80
85
65
45
50
CommentsInt
MO
MO
MO
WE
MO
MO
WE
WE
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ
Vein%
3
Tex ContactType
Alphadeg
Comments
locally qtz
flooded 4A
From
1219.40
To
1222.20
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
4B
1
7A
2
1
4B
4A
2
7A
2
Cont
90
90
90
75
85
STRUCTURAL LOG Page 5 of 13
08-NSD-004
MAJOR UNIT
From
1283.00
1309.80
1314.60
1329.70
1333.90
1344.40
To
1309.80
1314.60
1329.70
1333.90
1344.40
1397.00
MINERALS
As%Cp%
Mt%
Po%
15.
0.8
0.5
1.0
0.0
Py% Comments
minor 4H unit
Scattered Po
near alt'n bands
in mafic volcanic
Po in veined
mafic volcanic
Po in veined
mafic volcanic
VGSpecks
FABRIC
From
1273.00
1279.00
1286.00
1291.00
1297.00
1310.00
1312.00
1319.00
1338.00
1344.00
1360.00
To
1274.00
1280.00
1287.00
1292.00
1298.00
1311.00
1313.00
1320.00
1339.00
1345.00
1361.00
Alphadeg
75
50
55
50
50
50
45
60
60
60
30
CommentsInt
MO
MO
WE
MO
MO
MO
MO
WE
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1337.10
Alpha
deg
90
CommentsInt
WE
Type
FD
From
1337.00
QTZ VEINING
VeinType
QZ-C
QZ-C
QZ-C
Vein%
3
40
5
Tex ContactType
I
I
Alphadeg
70
60
Comments
angle
varies,
different
sets of
veins
+tension
gashes
angle varies
From
1314.60
1344.40
1360.40
To
1329.70
1350.60
1364.00
FAULT
From
1344.40
1360.40
To
1350.60
1364.00
Alphadeg Comments
not really a shear
zone, a strongly
Qtz- Cc veined
mafic volcanic
not really a shear
zone, a strongly
Qtz- Cc veined
mafic volcanic
Int
MOD
WEK
Type
SZ
SZ
MajorUnit
2
2D
2
7A
2
2
Cont
STRUCTURAL LOG Page 6 of 13
08-NSD-004
MAJOR UNIT
From
1397.00
1407.50
1409.10
1411.30
1412.50
1417.00
1429.00
1430.90
1432.40
1434.40
1438.80
1441.80
1486.80
1492.40
1494.20
1499.00
1515.20
1525.70
1533.80
1547.30
1552.70
1566.80
1578.80
1587.30
1588.00
To
1407.50
1409.10
1411.30
1412.50
1417.00
1429.00
1430.90
1432.40
1434.40
1438.80
1441.80
1486.80
1492.40
1494.20
1499.00
1515.20
1525.70
1533.80
1547.30
1552.70
1566.80
1578.80
1587.30
1588.00
1608.50
MINERALS
As%Cp%
2.0
Mt%
Po%
0.5
5.0
0.0
10.
1.0
1.0
Py%
3
7
3
5
Comments
Diss. Po
though out the
unit
concentrated
along Qtz Cc
veins
Py fractue
filling mm scale
fractures
breciated in
spots
Cp allong
quatz Cc veins
Po with
fractues mm
scale
within fractures
One 2cm wide
isolated bleb
of Po.
VGSpecks
FABRIC
From
1369.00
1376.00
1377.00
1384.00
1402.00
1407.50
1415.50
1431.50
1438.80
1442.00
1456.00
1479.00
1485.00
1494.00
1502.00
1504.00
1510.00
1518.00
1526.00
1535.00
1544.00
1552.00
1570.00
1576.00
1583.00
1590.00
1599.10
1601.00
1607.00
To
1370.00
1377.00
1384.00
1402.00
1407.50
1415.50
1431.40
1438.80
1442.00
1456.00
1469.00
1480.00
1486.00
1495.00
1503.00
1505.00
1511.00
1518.50
1527.00
1536.00
1545.00
1553.00
1571.00
1577.00
1584.00
1590.10
1599.10
1601.00
1607.00
Alphadeg
40
60
40
45
35
50
40
25
40
50
30
35
43
42
45
51
50
38
60
60
45
35
52
54
33
35
60
45
45
Comments
brittle
fractue
along
folition
between
1435.80 -
1438.80
Int
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
WE
WE
MO
INT
MO
MO
MO
WE
WE
MO
WE
INT
INT
INT
WE
WE
WE
WE
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1434.40
Alpha
deg
45
CommentsInt
MO
Type
FD
From
1434.20
QTZ VEINING
VeinType
QZ-C
QZ-C
QZ
Vein%
3
10
85
Tex
l
ContactType
I
S
Alphadeg
30
40
45
Comments
angle is
approximate
due to
variation
From
1373.00
1460.00
1566.80
To
1377.00
1469.00
1567.40
FAULT
From
1373.00
1412.50
1435.80
1566.80
To
1377.00
1414.10
1438.80
1567.40
Alphadeg
30
45
Comments
not really a shear
zone, Qtz- Cc
veined mafic
volcanic
Bad ground with
an RQD of 40%
chlorite slips
along fracture faces
85-90% qtz
flooding.
Int
WEK
MOD
INT
Type
SZ
SZ
GG
SZ
MajorUnit
2
6
2
6
2
2
6
2
6
2
8F
2
1
2
1
2
1
2
1
2
1
1
2
4E
2
Cont
50
40
35
40
30
25
20
40
90
90
55
40
35
58
60
63
68
32
45
45
42
STRUCTURAL LOG Page 7 of 13
08-NSD-004
MAJOR UNIT
From
1608.50
1610.50
1661.00
1718.00
1736.00
1746.80
1749.40
1778.60
1780.20
1799.00
To
1610.50
1661.00
1718.00
1736.00
1746.80
1749.40
1778.60
1780.20
1799.00
1818.10
MINERALS
As%Cp%
Mt%
Po%
3.0
0.0
Py% Comments
Traces Po in
mafic volcanic
VGSpecks
FABRIC
From
1619.80
1619.90
1621.50
1630.10
1634.50
1640.00
1649.00
1656.00
1662.00
1670.00
1688.00
1699.00
1711.00
1719.00
1727.00
1728.00
1749.40
1763.00
1790.00
1800.00
1811.00
1816.00
To
1619.80
1619.90
1621.50
1630.10
1634.50
1641.00
1650.00
1657.00
1663.00
1671.00
1689.00
1700.00
1712.00
1720.00
1728.00
1746.00
1763.00
1778.20
1799.00
1801.00
1812.00
1817.00
Alphadeg
55
60
45
35
50
46
40
20
45
50
60
32
40
33
42
70
60
65
70
53
49
55
CommentsInt
WE
WE
MO
WE
WE
INT
INT
MO
MO
MO
INT
INT
INT
INT
INT
MO
MO
MO
MO
INT
INT
INT
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1784.00
1787.00
Alpha
deg
85
90
CommentsInt
MO
INT
Type
MF
MF
From
1781.00
1784.00
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From
1746.80
1778.60
To
1749.40
1780.20
Alphadeg
50
55
CommentsInt
MOD
MOD
Type
SZ
SZ
MajorUnit
1
2
2D
2
2D
2
2D
2
2
2
Cont
60
50
60
55
STRUCTURAL LOG Page 8 of 13
08-NSD-004
MAJOR UNIT
From
1818.10
1820.30
1831.60
1860.10
1862.20
1889.10
1913.20
1915.50
1931.70
To
1820.30
1831.60
1860.10
1862.20
1889.10
1913.20
1915.50
1931.70
1939.20
MINERALS
As%Cp%
Mt%
Po%
4.0
0.1
10.
0.5
2.0
8.0
1.0
Py% Comments
mineralised 4A
mineralised 4A
VGSpecks
FABRIC
From
1824.00
1829.30
1836.00
1844.00
1845.00
1856.00
1860.10
1862.50
1874.00
1881.00
1906.00
1931.70
1934.50
1938.00
To
1825.00
1830.00
1837.00
1845.00
1856.00
1860.10
1862.20
1874.00
1881.00
1889.00
1907.00
1932.00
1935.20
1938.80
Alphadeg
29
53
48
62
65
70
70
50
60
70
70
60
60
60
CommentsInt
INT
INT
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
Type
S0
S2
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1823.00
1829.00
1831.00
1867.00
1938.00
Alpha
deg
40
45
37
70
90
Comments
10s of
tiny Ss
1-3cm in
size.
mm to
cm scale
folds
Int
MO
INT
INT
INT
MO
Type
SF
MF
FD
ZF
FD
From
1821.00
1826.00
1830.70
1866.70
1937.00
QTZ VEINING
VeinType
QZ-C
Vein%
85
Tex
f
ContactType
S
Alphadeg
60
CommentsFrom
1862.10
To
1886.00
FAULT
From
1828.40
1830.00
To
1828.80
1830.40
Alphadeg
47
40
Comments
Sheared/disorted
with ~35%
pervasive Cc alt'n.
Int
INT
MOD
Type
SZ
SZ
MajorUnit
4A
4B
2
7A
2
1
13
1
4A
Cont
45
32
66
50
70
60
50
90
90
STRUCTURAL LOG Page 9 of 13
08-NSD-004
MAJOR UNIT
From
1939.20
1942.00
1952.40
1976.00
1982.40
2009.50
2011.50
2020.00
2031.00
To
1942.00
1952.40
1976.00
1982.40
2009.50
2011.50
2020.00
2031.00
2055.00
MINERALS
As%Cp%
Mt%
Po%
0.0
0.5
Py% CommentsVGSpecks
FABRIC
From
1943.00
1945.00
1946.00
1949.00
1954.00
1961.00
1970.00
1971.00
2011.50
2031.00
To
1944.00
1946.00
1947.00
1950.00
1955.00
1962.00
1971.00
2009.00
2020.00
2045.00
Alphadeg
50
0
5
50
55
60
40
50
50
65
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
Type
S1
S0
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1943.00
1945.00
1948.00
2003.70
Alpha
deg
90
65
90
30
CommentsInt
MO
WE
MO
MO
Type
FD
SF
FD
FD
From
1942.00
1944.00
1947.00
2003.50
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
2
4A
2T
1
2
2
2
2T
2
Cont
90
70
60
57
50
60
STRUCTURAL LOG Page 10 of 13
08-NSD-004
MAJOR UNIT
From
2055.00
2079.20
2105.90
2108.00
2118.10
2122.40
2144.00
2146.30
2173.00
2179.00
2181.00
2193.10
2194.10
2200.30
2201.20
2203.30
2211.40
2217.50
To
2079.20
2105.90
2108.00
2118.10
2122.40
2144.00
2146.30
2173.00
2179.00
2181.00
2193.10
2194.10
2200.30
2201.20
2203.30
2211.40
2217.50
2230.80
MINERALS
As%Cp%
Mt%
Po%
2.0
Py% CommentsVGSpecks
FABRIC
From
2045.00
2055.00
2072.00
2079.20
2087.00
2100.00
2105.90
2108.00
2113.00
2118.10
2122.40
2144.00
2152.00
2162.00
2173.00
2175.00
2177.00
2181.00
2192.00
2195.00
2200.30
2211.40
2215.00
To
2055.00
2072.00
2079.20
2087.00
2100.00
2105.90
2108.00
2113.00
2118.10
2122.40
2141.00
2146.00
2162.00
2173.00
2175.00
2177.00
2179.00
2192.00
2195.00
2200.30
2211.40
2215.00
2230.80
Alphadeg
60
50
55
50
40
20
15
30
45
40
35
40
40
35
30
25
30
40
25
30
40
45
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
2211.40
Alpha
deg
60
CommentsInt
MO
Type
FD
From
2210.00
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From
2173.00
2193.10
To
2179.00
2203.30
Alphadeg
40
25
CommentsInt
MOD
MOD
Type
SZ
SZ
MajorUnit
1
2
4A
2
1
2
6V
2
2T
2
2
4E
2
4E
2
1
2
4A
Cont
70
50
90
30
55
70
35
40
30
50
35
40
25
40
50
45
50
STRUCTURAL LOG Page 11 of 13
08-NSD-004
MAJOR UNIT
From
2230.80
2232.80
2237.10
2256.30
2257.30
2260.20
2263.90
2272.40
2275.00
2280.00
2281.40
2312.00
To
2232.80
2237.10
2256.30
2257.30
2260.20
2263.90
2272.40
2275.00
2280.00
2281.40
2312.00
2330.20
MINERALS
As%Cp%
Mt%
Po%
1.0
0.5
1.0
3.0
5.0
0.3
7.0
Py% CommentsVGSpecks
FABRIC
From
2232.80
2237.10
2249.00
2255.00
2263.90
2268.00
2280.00
2281.40
2295.00
2312.00
2327.00
To
2237.10
2249.00
2255.00
2263.90
2268.00
2280.00
2281.40
2288.00
2296.00
2313.00
2328.00
Alphadeg
50
50
50
45
50
40
45
40
50
50
55
CommentsInt
WE
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ-C
Vein%
10
Tex ContactType
Alphadeg
Comments
qtz
veining/floo
ding
From
2327.00
To
2330.70
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
4B
1
2
4B
2
4B
4A
4I
2
4I
2
2
Cont
60
50
60
45
55
50
40
55
50
STRUCTURAL LOG Page 12 of 13
08-NSD-004
MAJOR UNIT
From
2330.20
2330.70
To
2330.70
2387.00
MINERALS
As%Cp%
Mt%
Po%
0.2
4.0
Py% Comments
4E/mafic
volcanic
Po in veins in
mafic volcanic
VGSpecks
FABRIC
From
2333.00
2341.00
2349.00
2363.00
2375.00
To
2334.00
2342.00
2350.00
2364.00
2376.00
Alphadeg
40
40
45
45
50
CommentsInt
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ-C
Vein%
15
Tex ContactType
Alphadeg
45
CommentsFrom
2344.50
To
2351.00
FAULT
From
2330.20
2344.50
To
2330.70
2351.00
Alphadeg
50
45
CommentsInt
MOD
WEK
Type
SZ
SZ
MajorUnit
4E
2
Cont
STRUCTURAL LOG Page 13 of 13
08-NSD-004
Assay
Sample AU ppm
MAJOR UNIT
From
0.00
665.00
711.50
712.00
721.40
746.00
788.00
To
665.00
711.50
712.00
721.40
746.00
788.00
805.00
From To
MINOR UNIT
From To CommentsComments
Wedged off of DDH 07-NSD-008
Steel Wedge installed at 665 in 07-NSD-008. The unit
is bioititic mafic volcanic with brownish - grey 2T
ranging from moderately foliated with an average
orientation of between 40-50 degrees from 668 -
686. Down section the unit is less foliated.
A plagoclase porphyry intrusion (~50cm thick). There
is 65% sub-rounded, buff coloured plag phenocrysts
ranging from 0.3-.7cm in size. Within the matrix is hi
% of biotite.
Moderately to well fol'd biotitic mafic volcanic
grading into borderline 2, up to 10-15% green
amphibole within the matrix with 5% cm scale calcite
veining.
Fine grained fresh looking basalt with 15% calcite
veiining. The unit is massive looking. brittle
fractured between 741.30 -741.60
A strongly developed foliated biotitic mafic volcanic
with 40% Cc irregular stringers (intense between
764-767.50) and a blebby matrix. The unit is weakly
sheared . 3-5% light green amph crystals that are
1-2mm along Cc vein margins
2 grading into 2T in the lower part of the section. Mod
foliated mafic volcanic with relatively less biotite
than previous unit. The unit consists of 60-70%
f.g.feldspars and 30% f.g. light/medium green
amphiboles.
Comments
There is 60% brittle
bull quartz calcite
veining between
695-707, moderate
biotite alt'n.The
veining is highly
irregular and no
visible sulphides. This
zone was sampled in
07-NSD-008..The
lower 3m is strongly
bleached.
The lower part contains
less Cc stringers. Very
black from 784-786m.
Bio alt'n increases from
793m down section
(from 1-8/10%). The
unit is cut by 10%
Cc-[Qtz] irregular
stringers averaging
2mm wide. Weak green
amph alt'n locally. No
mineralisation. The
lower contact is
gradational.
ALTERATION
Bio
M
M
S
M
W
M
M
W
Car
M
M
M
M
M
S
Chl Gru Hem Ser
W
W
Si
M
M
M
Comments
minor epidote rimming
bull quartz veins
2T, biotite slips.
weakly foliated mafic
volcanic, nil-weak bio alt'n.
increase of biotite alt'n
and Cc-[Qtz] stringers
felsic with qtz-fd and
biotite
minor sericite conten
minor sericite conten,
relatively more than
previous unit
Slightly brecciatic zone
with irregular wide
Qtz-Cc veins
LITHOLOGY LOG Page 1 of 29
Unit
No
2T
3K
2
2
2
2
Unit
08-NSD-004
Assay
Sample
E467024
E467025
E467026
E467027
AU ppm
0.07
0.06
0.91
0.03
MAJOR UNIT
From
805.00
839.00
855.70
857.80
To
839.00
855.70
857.80
869.00
From
855.70
856.70
857.50
857.80
To
856.70
857.50
857.80
858.80
MINOR UNIT
From To CommentsComments
Weakly foliated felsic/intermediate flow (or tuff?).
Consisting of f.g.equigranular feldspars-[Qtz] and
biotite (biotite content increases in the first 1.5m=
sediment?). The unit is cut by 10-15% Cc-[Qtz] veins
ranging from 1-5cm wide.
Fairly similar to previous unit, increase of biotite
and sericite content. The matrix is very
f.g./aphanatic and consists of 90% Qtz-feldspar and
10% biotite. Sericite is scattered and up to 3%. A
minor 2 unit is present from 854.2-854.6m.
Light green, fine grained to medium grained
serpentinized ultramafic. Consisting of mainly
serpentine (acicular/micaceous locally) and minor
talc. Strong Qtz-Cc veining at both contact (10-15cm
wide). Minor Po at the lower contact.
Fine grained to medium grained felsic flow. The unit
displays a f.g. Qtz-feldspars rich matrix and 5-10%
feldspars phenocrysts as well. The unit displays
nil-weak biotite and sericite content. Presence of
Qtz-Cc veins/stringers from 866m down section..
Comments
No sericite content
from 805-819m. Minor
sercicite from 819m
down section.No
mineralisation. 1% m.g.
tourmaline within Qtz
veins. Foliation is weak
and varies from
20-50dca. LC is
gradational.
From 852m dowm
section, the unit is cut
by 30% Qtz-Cc
irregular m.g ("sugary")
veins up to 3-5cm wide,
increase of biotite
content, increase of
sericite alt'n up to 10%:
the texture is slightly
brecciated. The lower
contact is sharp @
30dca.
LC is sharp @ 50dca.
903.5 - 906.5 has
intense veining and
sericite alt'n. Minor
tourmaline associated
with intense shearing.
ALTERATION
Bio Car Chl Gru Hem Ser Si
W
Comments
UM with serpentine
Felsic flow with fd
phenocysts, weak
Qtz-cc veining
LITHOLOGY LOG Page 2 of 29
Unit
3D
3D
1
3D
Unit
08-NSD-004
Assay
Sample
E467028
E467029
E467031
E467032
E467033
E467034
E467035
E467036
E467037
E467038
E467039
AU ppm
0.03
0.05
0.02
0.02
0.02
2.93
0.31
0.19
0.01
0.03
0.03
MAJOR UNIT
From
869.00
988.90
997.90
1000.10
To
988.90
997.90
1000.10
1001.80
From
987.90
988.90
990.00
991.00
992.00
993.00
993.80
994.80
999.10
1000.10
1001.00
To
988.90
990.00
991.00
992.00
993.00
993.80
994.80
995.90
1000.10
1001.00
1001.80
MINOR UNIT
From To CommentsComments
Fairly homogeneous, aphanitic to f.g felsic unit
consisting of a medium grey coloured matrix with
~5% scattered blebs and small patches of Cc alt'n.
Parts of the unit display irregular thick banding
defined by cream coloured and grey coloured rock.
Brown-green poorly foliated and distorted rocks with
intense Cc alt'n, pervasive light green amphibole alt'n
and 7% scattered qtz veins up to 10cm thick. Alt'n
completely replaces the f.g matrix in many places.
Distorted folded, brown biotised mafic rock with
moderate Cc alt'n in places and light green amph alt'n
in many places also.
30% thick bands 3-8cm of f.g to m.g biotitegnt 4F
rock. The rest of the unit is irregular and distorted
banding consisting of a fine grain green amph
matrix with 25% c.g ragged gnts 2-10mm.
Comments
Generally the unit is
weakly foliated but in
places up to 5m wide
the fol'n is moderately
to weakly developed.
953-962m displays
irregular & semi-banded
intense Cc, light green
amph & weak biotite
alt'n with irregular S0
folding. No
mineralization.
UC-993.8m has 2%
Po min'zn distriniuted
mainly has coarse
blebs associated with
qtz veins and
distortion. ~40% of the
Po is disseminated
throughout the matrix.
Distorted 10cm qtz vein
at 999.2m seems to be
the source for much of
the green amph and Cc
alt'n in this unit.
ALTERATION
Bio
W
W
W
M
W
S
Car
W
S
W
W
S
M
M
Chl Gru Hem Ser
S
Si Comments
Scattered blebs and
small patches <5cm of
Cc alt'n.
Very light coloured
green amph, assoc'd
with Cc.
LITHOLOGY LOG Page 3 of 29
Unit
3D
3M
2T
4E
Unit
08-NSD-004
Assay
Sample
E467041
E467042
E467043
E467044
E467045
E467046
E467047
E467048
E467049
E467051
E467052
E467053
E467054
E467055
E467056
E467057
E467058
E467059
E467061
E467062
E467063
AU ppm
0.99
0.03
0.10
0.90
0.02
0.09
0.08
0.23
0.44
0.03
0.71
1.32
1.18
0.01
0.01
0.02
0.03
0.01
0.00
0.16
0.07
MAJOR UNIT
From
1001.80
1011.90
1013.00
1016.30
1017.80
To
1011.90
1013.00
1016.30
1017.80
1019.90
From
1001.80
1002.80
1003.80
1004.80
1005.80
1006.40
1007.00
1008.20
1009.40
1010.40
1011.00
1011.90
1012.70
1013.00
1014.00
1015.00
1015.80
1016.30
1017.00
1017.80
1018.90
To
1002.80
1003.80
1004.80
1005.80
1006.40
1007.00
1008.20
1009.40
1010.40
1011.00
1011.90
1012.70
1013.00
1014.00
1015.00
1015.80
1016.30
1017.00
1017.80
1018.90
1019.90
MINOR UNIT
From To CommentsComments
Non-foliated 4F unit consisting predominantly of c.g
gnts (40%) and a f.g biotite-rich matrix. The rock is
moderately heterogeneous in gnt-biotite composition
which defines bands 10-50cm thick.
Openly folded bands 1-3cm thick of chert (20%) and,
c.g gnt-grun bands (30%) and bands of f.g green
amphibole +/- the c.g gnts porphs 2-10mm.
UC-1014.4m is typical 4F, f.g biotite-qtz matrix
with 30% Gnt porphs 1-3mm. The rest of the unit is
borderline 4E-4F, has more qtz in the matrix and
numerous bands 1-10cm containing more green
amph in the matrix.
Massive non- to poorly foliated rock consisting of f.g
qtz and biotite with a few gnt porphs 2-4mm
scattered near the contacts.
Banded typical 4E unit with open folds and planar
sections. 10% chert 2cm. The rest of the unit is
think bands 1-5cm of c.g gnt, gnt+grunerite, and
40% green amphibole +gnt porphs.
Comments
No sig'nt min'zn except
1010.4-1011.9m which
has numerous 4E bands
in it. ~5-10% of the
unit is narrow green
amph-gnt-Po 4E bands
up to 30cm thick.
Recystallisation of
some chert bands in to
qtz veins. Well min'zd
with 5% Po. Weakly
distorted.
30% of the rock is gnts
2-4mm.
Scattered Po grains,
0.7% overall. No biotite
alt'n, no shearing.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 4 of 29
Unit
4F
4E
4F
6
4E
Unit
08-NSD-004
Assay
Sample
E467064
E467065
E467066
E467067
E467068
E467069
E467071
E467072
E467073
E467074
E467075
E467076
E467077
E467078
AU ppm
0.03
0.07
0.11
0.02
0.02
0.02
0.02
0.02
0.02
0.34
0.08
0.02
0.02
0.02
MAJOR UNIT
From
1019.90
1030.80
1031.90
1032.70
To
1030.80
1031.90
1032.70
1055.00
From
1019.90
1021.10
1022.30
1023.30
1023.90
1025.00
1026.00
1027.00
1028.00
1029.10
1029.90
1030.80
1053.00
1054.00
To
1021.10
1022.30
1023.30
1023.90
1025.00
1026.00
1027.00
1028.00
1029.10
1029.90
1030.80
1031.90
1054.00
1055.00
MINOR UNIT
From To CommentsComments
Heteregeneous 4F consisting of non to poorly foliated
brown biotite-rich matrix with gnt porph content
ranging 10-40% and 1-5mm in size.
The entire unit seems to be a homogeneous light
grey matrix of f.g (<1mm) qtz+grunerite and biotite
with 3% gnts porph 2-3mm and 3% thin planar chert
bands 3-5mm.
Intense biotite and moderate gnt alt'n of a rock that
was probably mafic volcanic to begin with. Gnts are
large and euhedral 5-20mm. Biotite alt'n is pervasive.
1S. Homogeneous light grey and m.g intensely
serpentinised, non foliated ultramafic unit. The
upper 1.3m is greenish in colour and has more CHL
alt'n in matrix suggesting a gradational UC with
borderline mafic/UM rocks.
Comments
A couple qtz veins
1-12cm exist. And <4%
4E lithology which
exists as a few bands
less than 25cm in
thickness.
1029.1-1029.9m has
0.5% Po due to weak
distorting and qtz
veinlets and 4E bands.
Less biotite than a
typical 6, and grunerite
appears to form much
of the f.g matrix.
Weak to moderate S1
fabric in places.
ALTERATION
Bio
S
Car Chl Gru Hem Ser
S
Si Comments
LITHOLOGY LOG Page 5 of 29
Unit
4F
6
2U
1
Unit
08-NSD-004
Assay
Sample
E467079
E467081
E467082
E467083
E467084
E467085
E467086
E467087
E467088
E467089
E467091
E467092
E467093
AU ppm
0.01
0.01
0.01
0.01
0.01
0.01
0.01
0.03
0.02
0.15
0.09
0.05
0.21
MAJOR UNIT
From
1055.00
1058.70
1061.00
1062.40
To
1058.70
1061.00
1062.40
1065.60
From
1055.00
1056.00
1057.00
1058.00
1058.70
1059.70
1060.50
1061.00
1061.70
1062.40
1063.40
1064.00
1065.00
To
1056.00
1057.00
1058.00
1058.70
1059.70
1060.50
1061.00
1061.70
1062.40
1063.40
1064.00
1065.00
1065.60
MINOR UNIT
From To CommentsComments
Varies from massive to distorted 4F (mixed with 4E).
The unit contains massive biotite rich bands up to
15cm wide, studded by 15% c.g.euhedral garnets.
No mineralisation
Farily similar to previous unit. Mix 4E/4F but
relatively more 4E than before. The unit displays 85%
typical 4E bands (massive dark green amph rich
bands with 30% m.g.garnets). The rest of the unit is
biotite-garnet rich bands and chert. Two Z folds are
Mod developed 4B, borderline 4EA. The unit consists
of alternating Mt rich laminae (20), green amph-gar
rich bands (40) and chert bands (40). Grunerite
content is up to 5-8% (but no massive 4EA bands).
Scattered Po throughout (<1%).
Weakly developed 4EA, borderline clastic 4B. As
before, the unit is a mix gar-green amph rich
bands-[grunerite] rich bands and chert. No typical
4EA bands but grunerite content higher than in usual
4B. Hard to say if green amph is alt'n of gru or not
Comments
The unit displays 15%
4E bands ranging from
0.5-5cm wide (10%
f.g/m.g.garnets in
f.g.green amph rich
matrix). Presence of
3-5% distorted chert
bands up to 3cm wide.
present. Po in traces
(scattered). Possible
very weak 4EA in the
last 5cm.
Too magnetic to be 4EA?
The unit is cut by 3%
Qtz veins up to 3cm
wide. Weak biotite alt'n
locally. Disseminated
Po, <1%
overall.Cleavages
locally well developed.
The lower contact is
gradational.
ALTERATION
Bio
W
W
W
W
Car Chl Gru
W
Hem Ser Si
W
Comments
mix 4E/4F
mix 4E/4F
4B, borderline 4EA
weakly developed 4EA,
borderline clastic 4B
LITHOLOGY LOG Page 6 of 29
Unit
4F
4E
4B
4EA
Unit
08-NSD-004
Assay
Sample
E467094
E467095
E467096
E467097
E467098
E467099
E467101
E467102
E467103
E467104
E467105
E467106
E467107
E467108
E467109
E467111
E467112
AU ppm
0.47
0.27
0.03
0.45
0.02
0.01
0.01
0.02
1.70
0.10
0.11
0.52
0.01
0.04
0.07
0.03
0.33
MAJOR UNIT
From
1065.60
1069.70
To
1069.70
1079.00
From
1065.60
1066.60
1067.50
1068.00
1069.00
1069.70
1070.50
1071.00
1072.00
1072.50
1073.30
1073.60
1074.50
1075.00
1076.00
1077.00
1078.00
To
1066.60
1067.50
1068.00
1069.00
1069.70
1070.50
1071.00
1072.00
1072.50
1073.30
1073.60
1074.50
1075.00
1076.00
1077.00
1078.00
1079.00
MINOR UNIT
From To CommentsComments
More developed 4EA in terms of grunerite than
previous unit. Varies from well foliated to more
distorted unit. The unit displays alternating bands
of grunerite-garn-bio rich bands averaging 0.5cm
wide (70%) and chert bands (10%) up to 1cm wide.
Clastic 4B, consisting of 75% green
amph-f.g/m.g.garnets rich bands ranging from
0.2-0.8cm wide, 15% chert bands and 10% bio alt'd
bands with m.g. garnets. From 1073.3-1073.6m, a
dyke (mafic or Um) is present (sharp contacts , cross
cuts the banding).
Comments
The rest of the unit
consists of thin
f.g.gar-green amph rich
bands. One Z fold is
present @ 1068.5m
C.g euhedral gar at the
lower contact. No
significant
mineralisation. The
lower contact is
gradational over 50cm.
Cut by <1% Qtz veins.
From 1076m, down
section, the unit is
strongly borderline
weak 4EA with increase
of the gru content up to
10-15%. Po is scattered
(1% overall) and
occurs mainly near Qtz
veins in short and
distorted veins.
ALTERATION
Bio
W
M
Car Chl Gru
W
Hem Ser Si
W
Comments
weak 4EA
LITHOLOGY LOG Page 7 of 29
Unit
4EA
4B
Unit
08-NSD-004
Assay
Sample
E467113
E467114
E467115
E467116
E467117
E467118
E467119
E467121
E467122
E467123
E467124
E467125
E467126
E467127
E467128
E467129
E467131
E467132
E467133
AU ppm
0.04
0.03
0.02
0.36
4.41
0.18
2.44
0.03
0.01
0.02
0.02
1.53
0.44
1.64
0.12
4.04
3.04
0.60
2.00
MAJOR UNIT
From
1079.00
1083.00
To
1083.00
1096.00
From
1079.00
1080.00
1081.00
1082.00
1083.00
1084.00
1085.00
1086.00
1086.60
1087.30
1088.30
1088.80
1089.50
1090.50
1091.50
1092.50
1093.50
1094.00
1095.00
To
1080.00
1081.00
1082.00
1083.00
1084.00
1085.00
1086.00
1086.60
1087.30
1088.30
1088.80
1089.50
1090.50
1091.50
1092.50
1093.50
1094.00
1095.00
1096.00
MINOR UNIT
From To CommentsComments
Featureless, massive to weakly foliated ultramafic.
The matrix seems to be mainly composed of acicular
amph (but might be serpentine). Presence of 15-20%
f.g/m.g.talc throughout. No significant veining. The
lower contact is irregular.
Mainly banded Mt-chert unit. The unit consists of
alternating dark grey Mt rich bands/laminaes
averaging 0.5cm wide and chert bands up to 1cm
wide. The unit contains 3-5% distorted Qtz veins
(distorted/weakly sheared zones are 20-50cm wide).
Comments
Weak biotite-gar alt'n
locally. Weak grunerite
alt'n around Mt rich
bands in some places.
Disseminated Po
throughout, increases
in distorted/Qtz veined
zones, up to 3% (1%
overall). The lower
contact is gradational.
ALTERATION
Bio
W
Car Chl Gru Hem Ser Si
M
Comments
UM
presence of small
distorted / qtz veined
zones up to 50cm
LITHOLOGY LOG Page 8 of 29
Unit
1
4B
Unit
08-NSD-004
Assay
Sample
E467134
E467135
E467136
E467137
E467138
E467139
E467141
AU ppm
0.62
1.20
0.75
1.41
0.62
0.03
0.01
MAJOR UNIT
From
1096.00
1100.00
1111.90
1138.30
To
1100.00
1111.90
1138.30
1153.90
From
1096.00
1097.00
1098.00
1098.70
1099.70
1100.00
1101.00
To
1097.00
1098.00
1098.70
1099.70
1100.00
1101.00
1102.00
MINOR UNIT
From To CommentsComments
Well developed grunerite rich iron formation. The
unit displays 70% pale yellow/green grunerite rich
bands up to 1.5cm wide and slightly magnetic chert
bands averaging 1cm wide. The lower contact is
sharp @ 90dca
1S. Massive, featureless, soft Ultramafic. Fine
grained to medium grained. The unit consists mainly
of serpentine and talc. No significant veining.
Weakly-mod foliated mafic volcanic, dark grey in
colour, mainly fine grained unit. The matrix is mainly
composed of plagioclase and dark green/grey
amphibole. Biotite slips throughout: strong alt'n from
1113.1-1114.3m, weak-mod in the rest of the unit
1S. Massive to weakly foliated UM. Serpentinization
varies from weak-strong. The unit consists of
f.g/m.g.serpentine and f.g.talc. Where
serpentinization is weak, the matrix displays acicular
amphiboles.
Comments
From 1098m down
section, the unit is
well mineralised and
displays 10% Po
stringers. In the last
30cm, borderline 4H.
From 1098.7-1099.1m
is a small fault zone
with broken pieces,
chlorite (fractures seem
to be wet).
The lower part of the
section contains less
talc and is light green
in colour. The lower
contact is gradational
over 50cm.
The unit is cut by 1%
white/non-transparent
distorted Qtz veins up
to 2cm wide. From
1127m down section,
the unit is getting
pervasively bleached
(beige/white).
WEDGE @1127m.
Weak biotite alt'n
locally (increases in the
lower part of the
section).No significant
veining. The lower
contact is gradational
over 30cm.
ALTERATION
Bio
S
M
M
Car Chl Gru Hem Ser Si
W
S
Comments
4A, fairly fresh
UM with serpentine and
talc
UM
2T, 1% qtz veins (white
non translucide)
2T
UM with different
degrees of
serpentinization
Cut by 30% Qtz-Cc veins
LITHOLOGY LOG Page 9 of 29
Unit
4A
1
2T
1
Unit
08-NSD-004
Assay
Sample
E467142
E467143
E467144
E467145
E467146
E467147
E467148
E467149
E467151
E467152
E467153
E467154
AU ppm
0.01
0.07
0.00
0.01
0.01
0.01
0.01
0.00
0.01
0.00
0.01
0.00
MAJOR UNIT
From
1153.90
1160.10
1160.90
1163.40
1181.50
To
1160.10
1160.90
1163.40
1181.50
1192.40
From
1159.10
1160.10
1160.90
1161.50
1162.50
1163.40
1164.40
1179.10
1179.50
1180.50
1181.50
1182.50
To
1160.10
1160.90
1161.50
1162.50
1163.40
1164.40
1165.40
1179.50
1180.50
1181.50
1182.50
1183.50
MINOR UNIT
From To CommentsComments
Fine grained mod foliated mafic volcanic. The unit
consists of 60% green/grey amph and 40%
plagioclases. Nil-weak biotite alt'n. The unit is cut
by 30% irregular Qtz-Cc veins up to 5cm wide.
1S. Massive to weakly foliated Ultramafic,
mod-strongly serpentinized. The unit is mod soft
(contains ~10% f.g.talc). No significant veining or
mineralisation.
Well banded Mt-chert unit, SIF type 4B. The unit
consists of alternating 55% dark grey Mt rich bands
up to 1cm wide and 45% chert/grunerite rich bands
up to 1.5cm wide.
Massive grabbro. The unit displays 50% m.g. green
amp/pyrox and 50% interstitial f.g.-m.g.feldspars.
locally, weak chlorite alt'n. No biotite. From
1176.7-1178.6m, the unit is finer grained and more
foliated (2 unit)
Well developed Mt-chert banded unit (SIF type). The
unit displays 70% Mt rich bands up to 0.8cm wide,
20% chert bands up to 0.5cm wide, 10% f.g.-m/g/
grunerite rich bands on the edges of the Mt bands.
Minor Po locally.
Comments
2 sets of veins are
present: one +/- parallel
to foliation, one
extensional between 2
other veins. No visible
mineralisation. The
lower contact is
gradational.
The lower contact is
diffuse.
From 1160.9-1161.5m,
the unit contains
0.5-1% slightly
magnetic Po. The lower
contact is sharp
@90dca.
Po occurs in traces
over 3cm @ 1179.4m.
The lower contact is
sharp @90dca.
WEDGE @ 1169m
In the last 40cm, the
unit is distorted (small
tight folds) and
displays 1% Po. The
unit is cut by <1%
dismembered qtz
veins. The lower
contact is sharp
@90dca.
ALTERATION
Bio Car Chl Gru Hem Ser Si
W
Comments
UM with serpentine
grunerite
fairly fresh gabbro
LITHOLOGY LOG Page 10 of 29
Unit
2
1
4B
7A
4B
Unit
08-NSD-004
Assay
Sample
E467155
E467156
E467157
E467158
E467159
E467161
E467162
E467163
E467164
E467165
E467166
E467167
E467168
E467169
E467171
E467172
E467173
E467174
E467175
E467176
E467177
AU ppm
0.01
0.72
0.01
0.01
0.01
0.04
0.06
0.04
0.00
0.01
0.01
0.01
0.01
0.01
0.01
0.01
0.01
0.00
0.05
0.03
0.57
MAJOR UNIT
From
1192.40
1197.10
1210.00
1212.60
1213.30
To
1197.10
1210.00
1212.60
1213.30
1219.40
From
1183.50
1184.50
1185.50
1186.50
1187.50
1188.50
1189.50
1190.50
1191.40
1192.00
1192.40
1193.40
1211.60
1212.60
1213.30
1214.00
1215.00
1216.00
1217.00
1218.00
1219.00
To
1184.50
1185.50
1186.50
1187.50
1188.50
1189.50
1190.50
1191.40
1192.00
1192.40
1193.40
1194.40
1212.60
1213.30
1214.00
1215.00
1216.00
1217.00
1218.00
1219.00
1219.40
MINOR UNIT
From To CommentsComments
1S. Light-medium green Ultramafic. The unit
contains 85% m.g. serpentine and 15% f.g.-m.g. talc.
The unit is cut by 1% Cc veinlets. No mineralisation.
Grading from m.g.-c.g. gabbro consisting of
intergrown 60% green amph and 40% plagioclase to
finer grained mafic unit but still massive (no foliation).
No biotite present. No significant veining.
Fine grained to medium grained weakly foliated mafic
volcanic. The unit consists of equigranular
light/medium green amph and plagioclase. Coarser
grained than usual mafic flow but finer grained than
gabbro. No significant veining.
1S. Massive, soft, featureless, serpentinized
Ultramafic. The matrix is mainly composed of f.g.-m.g.
light green serpentine and f.g.talc. The lower contact
is sharp @75dca.
Well developed 4B SIF type. Consisting of 50% Mt
rich bands ranging from 0.3-1cm wide, 30% chert
bands up to 1.5cm wide and 20% grunerite between
Mt and chert bands. The unit is cut by <1% Qtz veins
throughout.
Comments
A brown/black mineral
is present @ 1196.9m.
The lower contact is
gradational.
The lower contact is
gradational.
The lower contact is
fairly sharp with UM
below (90dca).
Scattered Po (1%
overall) in veins up to
3mm wide. A few shear
bands are present. The
lower contact is
gradational.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
UM with serpentine and
talc
fresh gabbro
mod foliated mafic
volcanic
UM with serp
grunerite
LITHOLOGY LOG Page 11 of 29
Unit
1
7A
2
1
4B
Unit
08-NSD-004
Assay
Sample
E467178
E467179
E467181
E467182
E467183
E467184
E467185
E467186
E467187
AU ppm
0.06
0.10
0.50
0.36
0.35
0.01
0.01
0.37
0.01
MAJOR UNIT
From
1219.40
1222.20
1230.40
1253.40
To
1222.20
1230.40
1253.40
1283.00
From
1219.40
1220.00
1221.00
1221.50
1222.20
1223.20
1268.10
1269.10
1269.40
To
1220.00
1221.00
1221.50
1222.20
1223.20
1224.20
1269.10
1269.40
1270.40
MINOR UNIT
From To CommentsComments
Well foliated grunerite iron formation. The unit
consists of alternating yellow massive (locally
wispy) grunerite rich bands averaging 1cm wide and
chert bands up to 1cm wide. Contains ~2% dark
grey Mt rich bands.
Mod-well foliated mafic volcanic. The unit contains
50-60% plagiolcases and 40-50% medium green
amph. The unit is cut by a few (<1%) distorted
Qtz-Cc veins up to 1.5cm wide.
Relatively finer grained than previous gabbro. The unit
is massive (weak foliation locally) and consists of
70% m.g.green amph and 30% f.g. interstitial
plagioclases. Weak chlorite alt'n associated with Cc
veins (<1% overall).
Weakly-mod foliated unit. The unit is a mafic volcanic
consisting of f.g. equigranular plagioclases and
grey/green amph. Locally, weak chlorite alt'n
overprinted by black amph. Weak biotite throughout.
Comments
The unit is cut by 1%
Qtz veins up to 15cm
wide. Disseminated Po
in veins (2% overall)
near Qtz veins. One
band 10cm with m.g.
garnets alt'n is
present. The lower
contact is sharp @
85dca.
No biotite alt'n. The
lower contact is
gradational.
The unit is locally fine
grained mafic voclanic
flow (over 10-15cm).
No visible
mineralisation. The
lower contact is
gradational.
From 1269.1m over
15cm, minor 4H unit
(15% Po in black
argilite). Bands with
c.g. amph and weak
chlorite are present but
no garnet or biotite
alt'n (not selvages).
From 1265m over 1m,
the unit is massive &
has 95% actinolite and
5% plag (borderline UM).
ALTERATION
Bio
W
Car Chl
W
W
Gru Hem Ser Si
M
W
Comments
locally qtz veined 4A
fairly fresh mafic volcanic
fresh gabbro. Very weak
chlorite locally.
LITHOLOGY LOG Page 12 of 29
Unit
4A
2
7A
2
Unit
08-NSD-004
Assay
Sample
E467188
E467189
E467191
E467192
E467193
E467194
AU ppm
0.01
0.01
0.01
0.00
0.00
0.00
MAJOR UNIT
From
1283.00
1309.80
1314.60
1329.70
1333.90
To
1309.80
1314.60
1329.70
1333.90
1344.40
From
1289.50
1290.50
1290.90
1291.90
1292.50
1293.00
To
1290.50
1290.90
1291.90
1292.50
1293.00
1294.00
MINOR UNIT
From To CommentsComments
Weakly-mod foliated fine grained mafic volcanic.
Fairly similar to previous unit. Consisting of
f.g.equigranular plagioclase and amph. In the last
1.5m, the unit becomes m.g.. Nil-weak biotite alt'n
locally.
Fine grained mafic volcanic with 3% pillow selvages.
Consists of f.g.dark green amph and
f.g.plagioclases. Pillow selvages are 0.5-1.5cm wide
and consist of green amph-chlorite-[gar]-[bio]. No
significant veining. No visible mineralisation.
Nil-weakly foliated mafic volcanic, fine grained
overall. The unit contains 60% medium/dark green
amph and 40% plagioclases. The unit is cut by 3%
Qtz-Cc veins (one massive Qtz vein occurs @
1316.8m over 50cm). Nil-weak biotite alt'n throughout.
Medium grained massive unit (fairly finer grained than
gabbro units before). The unit is composed of 70%
f.g.m.g green amph and 30% interstitial plagioclase.
No veining or mineralisation.
Mod foliated green mafic volcanic. Nil-weak alt'n
throughout. The unit might be folded around 1337m.
The unit is cut by 1-2% distorted Cc veins.
Comments
Bands with chlorite and
dark green amph alt'n
are present up to
1.5cm wide. Po occurs
disseminated near alt'n
bands from
1290.5-1293m (<1%).
The unit is cut by 1-2%
Cc-[Qtz] veins (2 sets,
one seems to be more
extensional type of veins).
The lower contact is
gradational.
Local, patchy
chlorite-black amph
alt'n. The lower contact
is gradational.
The lower contact is
gradational.
ALTERATION
Bio
W
W
W
Car Chl
W
M
W
W
M
Gru Hem Ser Si
W
W
W
S
W
S
Comments
alt'n bands are present
(chlorite and dark green
amph)
alt'n present in pillow
selvages
gabbro, nil-weak alt'n
1% Qtz-Cc veins
strongly qtz-cc veined
mafic volcanic
strongly qtz-cc veined
mafic volcanic
LITHOLOGY LOG Page 13 of 29
Unit
2
2D
2
7A
2
Unit
08-NSD-004
Assay
Sample
E467195
E467196
E467197
E467198
E467199
AU ppm
0.01
0.00
0.00
0.00
0.00
MAJOR UNIT
From
1344.40
1397.00
1407.50
1409.10
1411.30
1412.50
1417.00
To
1397.00
1407.50
1409.10
1411.30
1412.50
1417.00
1429.00
From
1360.60
1361.40
1361.80
1362.30
1362.90
To
1361.40
1361.80
1362.30
1362.90
1363.90
MINOR UNIT
From To CommentsComments
The unit displays strongly Qtz-Cc veined zones
(almost brecciated) with veins // to foliation, veins
// to CA and small tension gashes (or extensional
fractures) filled with Cc: from 1344.4-1350.6m,
from 1360.6-1364m, from 1373-1377m.
Coarse grained fresh looking mafic volcanic 50%
feldspar and 10% calcite with in the matrix, strong
green light green amphibole. 0.5 to 1 cm wide chlorite
bands. Minor quartz -calcite veins.
A light grey looking homogeneous, well foliated
metased. Down hole there is increasing zones of 40%
fine grained biotite within a fine grained quartz,
feldspar matrix
Fine grained, dark green mafic volcanic intercalated
with minor metaseds; minor quartz calcite veining
Fine grained metasediment with mm scale fractures
containing pyrite and from 1412-1412.30 the unit is
strongly brecciated and infilled with 10% pyrite
Medium grained boititic, moderately sheared mafic
volcanic with strong green amphibole alteration.
Medium to coarse grained with 25% plagioclase and
40% green amphibole with minor Cc veinlets 1-3
mm wide and fine grained chlorite alteration; from
1427 to 1429 is an intercalated section of
metasediments.
Comments
The rest of the unit is
cut by 5%
Qtz-Ccveins. A
chlorite-m.g.black amph
is present throughout
(5% overall) and
increases in the
strongly Qtz-Cc veined
zones. 2 specks of
Cpy, up to 1% Po in the
second zone.
The U.C is 180 degrees
to CA. Appears to be
Skipping along a mafic-
sedment contact with
sections of core having
half Sed and 1/2
volcanics. L.W @ 90
degrees to Ca
This unit could be a
gabbroic still since we
have the same
sediments above and
below.
ALTERATION
Bio
W
M
W
W
W
W
W
W
Car
M
W
M
Chl
W
W
W
W
W
W
S
W
Gru Hem Ser
W
S
W
Si
M
M
M
W
S
Comments
strongly qtz-cc veined
mafic volcanic
Along brittle fractues
UM with serpentine
mafic volcanic
UM with serpentine and
talc
LITHOLOGY LOG Page 14 of 29
Unit
2
2
6
2
6
2
2
Unit
08-NSD-004
Assay
Sample AU ppm
MAJOR UNIT
From
1429.00
1430.90
1432.40
1434.40
1438.80
1441.80
1486.80
1492.40
1494.20
1499.00
To
1430.90
1432.40
1434.40
1438.80
1441.80
1486.80
1492.40
1494.20
1499.00
1515.20
From To
MINOR UNIT
From To CommentsComments
Light grey in colour composed of 20% boitite, 65%
qtz and feldspar, numerous infilled fractures of pyrite
~.5 to 2mm wide. Fractures are parallel to the C.A.
Fine to medium grained 2T volcanic consisting of
40% amphibole and 60% plagioclase. The unit
displays 10% biotite slips <1 mm wide . Minor quartz
/Cc veining.
Fine grained medasediment with 20% in a quartz
feldspar matrix. Less fractures than the last 2 unit.
Pyrite 3% and concentrated along a mm scaled
fracture network which is pervasive thoughou the unit.
Fine grained mafic volcanic with a strong brittle fault
between 1435.70 - 1438.80. RQD of 40% and
strongly fractued along the foliation. strong chlorite
along slips.
A coarse grained granitic pegmatite consisiting of
65% quartz and 10% pink kspar and 25% cream
coloured plagioclase.
Medium to coase grained mafic volcanic with 40%
green amphibole and 55% feldspar.
Very f.g homogeneous UM rock consisting of 95%
green amphibole, 5% f.g serp in the matrix in places-
giving a greyish colour.
Well foliated green grey, m.g mafic rock with
~35-45% plagiocalse in the matrix, the rest is m.g
green-grey amphibole. Fairly sharp contacts.
Identical to the previous UM unit except this unit
contains a light grey moderately serp alt'd 70cm
section at 1497.7-1498.4m, this section consists of
90-100% serpentine.
Well foliated green-grey mafic rock with plagioclase
content ranging from 15-50%. The rock is m.g in
texture with grain size ranging up to 3mm but
generally 0.5-2mm
Comments
2% iregular Cc veinlets
1-10mm. The rock
maybe be fresh
unaltered UM or high
MG basalt.
Fairly sharp contacts.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 15 of 29
Unit
6
2
6
2
8F
2
1
2
1
2
Unit
08-NSD-004
Assay
Sample AU ppm
MAJOR UNIT
From
1515.20
1525.70
1533.80
1547.30
1552.70
To
1525.70
1533.80
1547.30
1552.70
1566.80
From To
MINOR UNIT
From To CommentsComments
Very f.g green-green , homogeneous ultramafic unit
with f.g serpentine content varying from 5-35% in the
different parts of the unit. Rest of the matrix is very
f.g green amphibole.
Fine grained mod foliated mafic volcanic. The unit
consists of 60% f.g.plagioclase and 40% grey-[green]
amphibole. At 1532.5m and 1533.6m, presence of
massive black tourmaline. No significant veining.
1S.Serpentinised ultramafic. The unit varies from
light green ultramafic mainly composed of
f.g.serpentine (with green amphibole) to soft almost
white unit consisting of serpentine and talc. Locally,
talc is c.g. No significant veining or mineralisation.
Moderately foliated green mafic consisting of 30-45%
plagioclase and 55-70% m.g green amphibole. Four
planar qtz veins <10cm thick.
Light grey highly serpentinised ultramafic. The
upper 3m is pale green in colour with minor 10-30%
green amphiboles in the matrix, the rest of the unit is
~100% light grey serpentine.
Comments
The degree of serp
alt'n is very variable
and has very grading
contacts. 1% Cc
veinlets <5mm.
Gradational LC.
Borderline 2/UM from
1521-1523.4m.
The lower contact is
gradational over 1.5m.
Decreasing serpentite
towards LC with rock
consisting of ~75-85%
green amphibole with
25-15% m.g serpentine
in the matrix, the rock
is light to medium green
in colour.
The upper contact is
sharp but the LC is very
gradational over a
distance of ~1.5m with
decreasing plag and
changing texture to the
lighter green coloured
"high Mg basalt" texture.
Two sections
1557.5-1558.6m &
1560.9-1561.9m
contains 25-30% c.g
irregularly shaped
black/dark grey
porphyroblasts and
connecting stringers.
Most grains are elongate
in colour- possibly
tourmaline.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 16 of 29
Unit
1
2
1
2
1
Unit
08-NSD-004
Assay
Sample
E529459
E529461
E529462
E529463
E529464
E529465
E529466
E529467
E529468
E529469
E529471
E529472
E529473
AU ppm
0.01
0.01
0.00
0.00
0.00
0.01
0.01
0.01
0.08
0.49
0.13
0.36
0.19
MAJOR UNIT
From
1566.80
1578.80
1587.30
1588.00
1608.50
To
1578.80
1587.30
1588.00
1608.50
1610.50
From
1586.30
1587.30
1588.00
1589.00
1598.00
1599.00
1600.00
1606.00
1607.00
1608.00
1608.50
1609.20
1609.90
To
1587.30
1588.00
1589.00
1589.70
1599.00
1600.00
1601.00
1607.00
1608.00
1608.50
1609.20
1609.90
1610.50
MINOR UNIT
From To CommentsComments
Well foliated medium to pale grey rock, appears fairly
fresh but is weakly alt'd with 5-25% f.g pale green
soft serp within the matrix.
Moderately to well foliated mafic rock consisting of
1-10% plag (variable) 3% cc veinlets, and grey-green
mafic amphiboles.
Weakly developed 4E non magnetic. The unit displays
f.g.dark green amph rich bands overprinted by
chlorite and m.g.acicular black amph. The unit
contains <1% c.g.garnets. The unit is cut by 1%
Qtz-Cc veins.
2?1?Varies from well foliated to massive mafic
volcanic. The unit seems to be an Ultramafic or a
high-Mg basalt: Plagioclase content <5%. The unit is
cut by 2-3% Cc veinlets displaying scattered Po veins.
Serpentinised ultramafic, soft and featureless. The
unit contains also amph rich parts. Po occurs from
1609.2-1609.9m associated with chlorite. The lower
contact is gradational.
Comments
No biotite. Varying
~0-5% f.g plagioclase.
The unit does not seem
strongly UM but it is
more ultramafic than a
high Mg 2. 60cm at UC
is sheared qtz flooded
SZ consisting of
~80-90% qtz.
1580.7-1582.1m is
moderately biotised
with ~25% biotite.
Po occurs in blebs or in
veins: 0.5% overall. The
lower contact is diffuse.
Local tourmaline.
Breccia around 1590m
(15cm wide) with Cc,
Qtz and fragments of 2
. Serpentine is
occasionnaly present.
The lower contact is
irregular.
ALTERATION
Bio Car Chl
M
W
Gru Hem Ser Si
W
W
Comments
weakly developed 4E
local serpentine
UM with serpentine
LITHOLOGY LOG Page 17 of 29
Unit
1
2
4E
2
1
Unit
08-NSD-004
Assay
Sample
E529474
E529475
E529476
E529477
AU ppm
0.06
0.00
0.01
0.01
MAJOR UNIT
From
1610.50
1661.00
1718.00
1736.00
1746.80
To
1661.00
1718.00
1736.00
1746.80
1749.40
From
1610.50
1746.00
1746.80
1747.80
To
1611.50
1746.80
1747.80
1748.80
MINOR UNIT
From
1652.00
To
1679.00
Comments
Rods Snapped at 1679 and we
pulled up to 1655 and Wedged off.
Comments
2?High Mg basalt? Fairly similar to previous unit.
The unit is plagioclase poor and contains mainly
medium-light green amphiboles. Presence of patches
of serpentine throughout, increasing from
1618.3-1620m.
Weakly to mod foliated pillow basalt. The unit
displays 50% plagioclases and 50% light-medium
green amph. No significant veining. The unit contains
2% pillow selvages up to 1cm wide.
Well foliated f.g fresh mafic rock consisting of
15-50% (variable) and green amphibole, on average
~70% amphibole.
Fresh looking pillowed mafic volcanic. Selvages arre
1-3 cm wide with biotie, garnet and minor chlorite.
Frequency of calcite veining is mm scale to 1 cm
wide wispy and // to the foliation.
May be the shearing however the unit is medium to
coarse grained and strong distorted with bands of
green amphibole dismembered.
Comments
Nil-weak biotite alt'n
throughout. The unit is
cut by <1% Cc veins.
1638-LC is fairly
typical fresh mafic
volcanic with 5-12% f.g
plag and 3% Cc
veinlets <10mm
throughout. Black amph
alt'n around Qtz veins in
the last 3m.
Pillow selvages display
green amph, biotite,
garnets and local
chlorite. Snapped Rods
need to go back up the
hole and Wedge past
( Wedge set at 1652)
2% scattered Cc
veinlets <1cm, 2%
scattered qtz veins up
to 20cm thick. No
green amph-gnt pillow
selvedges. 2% planar
bands <1cm containing
~20-40% m.g biotite.
The band of green
amphibole are 1-3 cm
wide cross cutting
medium graind bleached
looking mafic
volcanics. A needle like
random or oriented
black mineral.
Actinolite??
ALTERATION
Bio
W
M
W
W
W
Car
W
W
Chl
W
W
Gru Hem Ser Si
W
W
Comments
local serpentine
alt'n in the pillow selvages
LITHOLOGY LOG Page 18 of 29
Unit
2
2D
2
2D
2
Unit
2D
08-NSD-004
Assay
Sample
E529478
E529479
E529481
E529482
E529483
E529484
E529485
E529486
E529487
E529488
E529489
E529491
E529492
E529493
E529494
E529495
E529496
E529497
AU ppm
0.01
0.01
0.01
0.01
0.01
0.01
0.02
0.01
0.01
0.02
0.02
0.02
0.01
0.01
0.01
0.01
0.11
0.11
MAJOR UNIT
From
1749.40
1778.60
1780.20
1799.00
1818.10
To
1778.60
1780.20
1799.00
1818.10
1820.30
From
1748.80
1749.40
1750.00
1778.00
1778.60
1779.60
1780.20
1781.00
1782.00
1783.00
1784.00
1785.00
1786.00
1787.00
1816.10
1817.10
1818.10
1819.20
To
1749.40
1750.00
1751.00
1778.60
1779.60
1780.20
1781.00
1782.00
1783.00
1784.00
1785.00
1786.00
1787.00
1788.00
1817.10
1818.10
1819.20
1820.30
MINOR UNIT
From
1818.10
To
1818.20
Comments
Dark brown sheared graphitic
layer containing 5% Po wisps nd
10% broken chert fragments.
Comments
Biotitic mafic volcanic with pillow selvages that are
spead out, ~1-2 metres apart with minor calcite
veining. Down section there is an increase in the
amount of biotite. Calcite veining is cross cutting.
The upper contract is moderately sheared and the unit
is a bleached mafic volcanic very simiilar to what is
present below the PQ Deeps deposit to the south.
The unit is a biotitic mafic volcaninc with moderate
open folds between 1784-1787. The folds consist of
boitite and garnet and are "M" shaped. May be below
the NIF.
Homogeneous, well foliated mafic rock with minor
biotite alt'n. About half of the unit in sections
contains between 5 & 15% biotite in the matrix,
sometimes as slips 1-5mm wide.
Weakly to non-magnetic, planar unit consisting of
70% chert layers, mostly 1-7mm, alternating with
thin laminations, 1-5mm, of 50/50% straw-brown
amph and light green amphibole. 7cm dark brown
graphitic 4H layer at the UC.
Comments
Biotite slips are
present. 1-3 cm wide.
The unit has a net
texture stock work of
green looking biotite
thought the unit 0.5 to
1 mm wide .
some areas where there
is a strong brown biotie
1792.4-1796.
Scattered planar Cc
viens 5-20mm.
10cm massive
Po-breccia band 30cm
from the LC. Po is also
distributed as scattered
blebs in semibrittle
fractures, and as
disseminated grains.
4% Po overall. No qtz
veining.
ALTERATION
Bio
M
M
M
M
Car
W
S
Chl Gru Hem Ser Si Comments
Strongly bleached
LITHOLOGY LOG Page 19 of 29
Unit
2D
2
2
2
4A
Unit
4H
08-NSD-004
Assay
Sample
E529498
E529499
E530501
E530502
E530503
E530504
E530505
E530506
E530507
E530508
E530509
E530511
E530512
E530513
E530514
E530515
AU ppm
0.05
0.02
0.01
0.01
0.01
0.01
0.01
0.00
0.04
0.49
0.07
0.80
0.04
0.06
0.01
0.07
MAJOR UNIT
From
1820.30
1831.60
To
1831.60
1860.10
From
1820.30
1821.00
1822.00
1823.00
1824.00
1825.00
1826.00
1827.00
1827.60
1828.40
1828.80
1829.90
1830.50
1830.90
1831.60
1832.60
To
1821.00
1822.00
1823.00
1824.00
1825.00
1826.00
1827.00
1827.60
1828.40
1828.80
1829.90
1830.50
1830.90
1831.60
1832.60
1833.60
MINOR UNIT
From To CommentsComments
Entire unit is typical zebra rock consisting of 45%
dark grey clean Mt laminations 1-10mm & 40%
cream coloured grun-qtz layers 1-5mm. 15% of the
chert. Lower 2m has ~2% Po min'zn. 4cm lamp'yre
at 1830.9m
UC-1835m is well foliated with ~5-7% biotite in the
matrix- more closer to the UC. 1835-~1839m is c.g
(2-3mm) amphibolite with plag ranging 5-35%.
Comments
UC-1825 is planar
laminated with tiny Ss in
the layers. 1825-LC is
tightly folded &
distorted with a well
devel'd S2 foliation in
many places.Tight
folding has partially
destroyed the thin
lamin'ns in places.
Semi-brittle intense
shear @
1828.4-1828.8m.
1839-LC is well foliated
fresh mafic rock with
15-30% f.g plagioclase
in the matrix. 3%
scattered irregular Cc
veinlets. Minor biotite
alt'n ranging 1-7% in
areas.
ALTERATION
Bio
M
Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 20 of 29
Unit
4B
2
Unit
08-NSD-004
Assay
Sample
E530526
E530527
E530528
AU ppm
0.01
0.01
0.09
MAJOR UNIT
From
1860.10
1862.20
1889.10
1913.20
1915.50
1931.70
To
1862.20
1889.10
1913.20
1915.50
1931.70
1939.20
From
1929.70
1930.70
1931.70
To
1930.70
1931.70
1932.70
MINOR UNIT
From To CommentsComments
Medium grey to dark green gabbro / Very Coarse
grained mafic strong dark green mineral amphibole
/pyroxene. The unit is massive with a mottled texture.
The unit is fesh looking with no type of alteration
Fine to medium grained biotitic mafic volcanic with
minor calcite viening and wispy green amphibole.
Minor 4B SIF strongly magnetic with z folds between
1867.80-1868.00. mm to cm scale Z folds
1S. UC-1889.1 Amorphous looking blue grey.
Serpentine along fractue surfaces and light blue grey
in colour. Wispy dark mineral though out the unit 1mm
to 3 mm wide. In some sections the unit look like a
bleached mafic volcanic
Lamprophyre dyke. The unit consists of a phlogopite/
Cc rich matrix with f.g-m.g.altered olivine with
f.g.serpentine. No garnets. The unit is cut by <1% Cc
veins.
Fine grained, locally medium grained Ultramafic,
massive locally weakly foliated unit. The unit displays
f.g. light green acicular serpentine and f.g.talc.
Featureless, no significant veining. The lower
contact is sharp @ 90dca.
Well developed grunerite rich Iron Formation. From
1931.7-1935.2m, the unit displays m.g.grunerite
(darker than usual) studded by 20% f.g.Mt grains.
Fairly massive. From 1935.2-1939.2m, the unit is
similar to usual 4A and consists of wispy pale yellow
Comments
The unit is composed
of 65-70% dark green
amphibole and
Pyroxene with 5 -10%
feldspar/calcite
bordering on ultramafic/
lamp. dyke.
Down section there is a
decrease in biotite and
the unit is fresher
looking 1881.50 bull
quartz veining witn
minor calcite veining
.moderate biotite
alteration from 1886-
1889
Lower contact is sharp
@ 50dca.
The lower contact is
sharp @ 90dca.
grunerite rich bands
averaging 1cm wide
and chert bands up to
0.8cm wide. Po occurs
locally in blebs or
short veins, overall
1% (8% from
1935.2-1935.6m) LC
sharp @ 90dca).
ALTERATION
Bio
W
M
W
S
Car
M
W
S
Chl
W
Gru Hem Ser
S
Si
W
Comments
UM with serpentine and
talc
phlogopite in kimberlite
UM with serpentine and
talc
4A
LITHOLOGY LOG Page 21 of 29
Unit
7A
2
1
13
1
4A
Unit
08-NSD-004
Assay
Sample
E530529
E530531
E530532
E530533
E530534
E530535
E530536
E530537
E530538
E530539
E530541
E530542
E530543
E530544
E530545
E530546
E530547
E530548
E530549
E530551
E530552
E530553
E530554
E530555
E530556
AU ppm
0.04
0.01
0.02
0.07
0.06
0.03
0.01
0.02
0.03
0.01
0.01
0.01
0.47
0.27
0.14
0.03
0.03
0.02
0.02
0.04
0.34
0.04
0.05
0.02
0.01
MAJOR UNIT
From
1939.20
1942.00
1952.40
1976.00
To
1942.00
1952.40
1976.00
1982.40
From
1932.70
1933.70
1934.50
1935.20
1935.60
1936.60
1937.00
1938.00
1938.80
1939.20
1940.00
1941.00
1942.00
1943.00
1944.00
1945.00
1946.00
1947.00
1948.00
1949.00
1950.00
1951.00
1951.60
1952.10
1953.10
To
1933.70
1934.50
1935.20
1935.60
1936.60
1937.00
1938.00
1938.80
1939.20
1940.00
1941.00
1942.00
1943.00
1944.00
1945.00
1946.00
1947.00
1948.00
1949.00
1950.00
1951.00
1951.60
1952.10
1953.10
1954.10
MINOR UNIT
From To CommentsComments
Grey-green mafic volcanic. The unit consists of
equigranular grey-green amphibole and 50%
f.g.plagioclase. The unit is cut by 1% Qtz-Cc veins up
to 0.3cm wide. No visible mineralisation.
Well foliated well developed 4A. The unit consists of
alternating f.g.-m.g.grunerite rich bands averaging
1cm wide 40% chert bands up to 1.5cm wide. The
unit is locally folded and the foliation is locally // to CA.
Well foliated fine grained mafic volcanic. The unit
displays 50% green amph, 35% plagioclase and 15%
f.g.biotite. The unit is cut by 1% Qtz veins
1S. Massive featureless Ultramafic consisting of
equigranular serpentine and talc. No significant
veining, no mineralisation. The lower contact is
gradational.
Comments
The lower contact is
sharp @ 70dca.
Po occurs in traces.
Weak bio alt'n locally.
The lower contact is
irregular.
No visible
mineralisation. The
lower contact is
gradational.
ALTERATION
Bio
M
W
Car Chl Gru
W
Hem Ser Si
W
W
Comments
mafic volcanic fairly fresh
2T
UM with serpentine and
talc
LITHOLOGY LOG Page 22 of 29
Unit
2
4A
2T
1
Unit
08-NSD-004
Assay
Sample
E530557
E530558
E530559
E530561
E530562
E530563
E530564
E530565
E530566
E530567
E530568
E530569
E530571
E530572
E530573
E530574
E530575
E530576
E530577
E530578
E530579
E530581
E530582
AU ppm
0.01
0.00
0.00
0.01
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.01
0.01
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.00
MAJOR UNIT
From
1982.40
2009.50
2011.50
2020.00
To
2009.50
2011.50
2020.00
2031.00
From
2008.50
2009.50
2010.50
2011.50
2012.50
2013.50
2014.50
2015.50
2016.50
2017.50
2018.50
2019.00
2020.00
2021.00
2022.00
2023.00
2024.00
2025.00
2026.00
2027.00
2028.00
2029.00
2030.00
To
2009.50
2010.50
2011.50
2012.50
2013.50
2014.50
2015.50
2016.50
2017.50
2018.50
2019.00
2020.00
2021.00
2022.00
2023.00
2024.00
2025.00
2026.00
2027.00
2028.00
2029.00
2030.00
2031.00
MINOR UNIT
From To CommentsComments
Well to moderately foliated medium to darker green
f.g mafic unit with 10% - 15% dissem'd biotite and
biotite slips. The unit is a 2 with moderate biotite
alteration.
The unit is a intensely sheared mafic volcanic. The
unit as strong biotite, green amphibole and with
moderate calcite veining.
Fine grained, massive-weakly foliated, mafic volcanic.
The unit is strongly bleach with up to 10% bio slips,
(1-0.4mm thick). F.g. green amphibole is also
present with few random 1mm qtz/Cc veinlets,
Intensely sheared 2T with strong hydrothermal
alteration. The unit displays mm scale fracture
network that have be infilled with biotite.
Comments
A section from 2000 -
2009 is extemely
bleached with strong
green amphibole. Minor
folds exist with in this
section on a mm to cm
scale
There is an increase in
in calcite and quartz
veining down section.
with moderate shearing
present.
The unit is strongly
bleached with fine
green amphibole
alteration.
ALTERATION
Bio
S
M
M
Car
W
Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 23 of 29
Unit
2
2
2
2T
Unit
08-NSD-004
Assay
Sample
E530583
E530584
E530585
AU ppm
0.00
0.00
0.00
MAJOR UNIT
From
2031.00
2055.00
2079.20
2105.90
2108.00
2118.10
2122.40
2144.00
2146.30
2173.00
To
2055.00
2079.20
2105.90
2108.00
2118.10
2122.40
2144.00
2146.30
2173.00
2179.00
From
2031.00
2032.00
2033.00
To
2032.00
2033.00
2034.00
MINOR UNIT
From To CommentsComments
Fresh looking mafic volcanic with the odd biotite slips
2-4 cm wide. There is strong calcite veining and
Strong green amphibole alteration.
Strongly serpentinized ultramafic with greasy fracture
planes. The U.C. is strongly distorted then grading
into a weakly foliated amorphous texture. The unit is
blue - grey to off white.
Medium green, well foliated elongate amphibole
grains and ~15% plagioclase with strong biotite
alteration. Between 2096-2103m the core is brown
coloured with intense calcite veining. The unit is
blocky between 2100-2102m and is healed fault gouge.
The unit is a fairly homog' unit of planar chert (50%)
and bands of grunerite and magnetite along the U.C
is higly magnetic and decreases down section. The
grun is very pale green in colour.
Well foliated green grey mafic. Medium green in
colour with intercalated light green ultramafics 10 -15
cm wide.
Massive ultramafic, amorphous. The unit is mainly
composed of f.g. serpentine, no significant talc. Light
green in colour. Both contacts are sharp, There is
biotite slips and calcite veining are present at the
contacts
The unit is a fresh looking 2 with minor biotie slips.
Looks like thinnly lamainted, composed of 40-50%
bio, rest Fd-Qtz, all f.g. and equigranular. A very
weak foliation at a high angle to bedding planes. Both
the U.C and L.c are extermely sharp.
The unit has alternating bands of fresh looking mafic
volcanic with strong green amphibole and minor
patches of 2T.
Strongly sheared and bio'd 2T. Minor green amph in
matrix at both the L.C and L.C. but distinct from 2 on
either side.
Comments
Minor intercalated
section of mafic
volcanics which display
local biotite slips. The
L.C is also strongly
distorted.
Well foliated, medium
green, m.g mafic rock
with intense biotite
alt'n from 2096- 2099.7.
ALTERATION
Bio
W
M
M
W
W
W
S
S
Car
M
W
M
M
W
M
W
Chl
M
M
Gru
S
Hem Ser Si Comments
talc serpentine
talc and sepentine
LITHOLOGY LOG Page 24 of 29
Unit
2
1
2
4A
2
1
2
6V
2
2T
Unit
08-NSD-004
Assay
Sample
E530586
E530587
E530588
E530589
E530591
E530592
E530593
E530594
E530595
E530596
E530597
E530598
E530599
AU ppm
0.02
0.02
0.02
0.03
0.02
0.01
0.01
0.01
0.01
0.01
0.00
0.00
0.03
MAJOR UNIT
From
2179.00
2181.00
2193.10
2194.10
2200.30
2201.20
2203.30
2211.40
To
2181.00
2193.10
2194.10
2200.30
2201.20
2203.30
2211.40
2217.50
From
2192.10
2193.10
2194.10
2195.10
2196.10
2197.10
2198.10
2199.10
2199.80
2200.30
2201.20
2202.20
2216.50
To
2193.10
2194.10
2195.10
2196.10
2197.10
2198.10
2199.10
2199.80
2200.30
2201.20
2202.20
2203.30
2217.50
MINOR UNIT
From To CommentsComments
Strongly alterated 2 with strong green amphibole
alteration and there is a patch work network or
fragments of small 10 cm wide lamprophyric dykes
Biotitic mafic volcanic with calcite veining from 2192
to 2193.1 tere is strong green amphibole alteration.
Moderately foliated 4E with intense bio/gar alteration.
Garnets between .7 to 1.2 cm in diameter and \\ to the
foliation. No mineralization present.
Medium green, well foliated elongate amphibole
grains and ~15% plagioclase. Moderate
biotite-garnet alteration at 2195-2196.5m. Large slips
3- 5 xcm wide with garnets .7 to 1.5 cm wide. There
is a decrease in biotite down section.
Not a typical 4E intense biotite \ garnet alteration
with strong green pale amphibole alteration 2% Po.
Well foliated, fine to medium grained mafic unit with
irregular patches and veins of Cc alteration.
1M, Fine to medium grained moderately foliated
ultramafic amphibolite. Light green in colour and
only weakly serpentinised. Minor folding present
between 2211-2213m.
Well foliated 2T consisting of ~35% m.g biotite in a
matrix with grey/green amphibole and moderate
calcite veining.
Comments
ALTERATION
Bio
S
S
S
S
W
Car
W
M
M
W
Chl Gru Hem Ser Si Comments
sepentine
LITHOLOGY LOG Page 25 of 29
Unit
2
2
4E
2
4E
2
1
2
Unit
08-NSD-004
Assay
Sample
E530601
E530602
E530603
E530604
E530605
E530606
E530607
E530608
E530609
E530611
E530612
E530613
E530614
E530615
E530616
E530617
E530618
AU ppm
0.05
0.02
0.02
0.07
0.01
0.01
0.01
0.01
0.03
0.01
0.01
0.01
0.00
0.00
0.00
0.04
0.01
MAJOR UNIT
From
2217.50
2230.80
2232.80
2237.10
To
2230.80
2232.80
2237.10
2256.30
From
2217.50
2218.50
2219.50
2220.50
2221.50
2222.50
2223.50
2224.50
2225.50
2226.50
2227.50
2228.50
2229.50
2230.00
2230.80
2231.80
2232.80
To
2218.50
2219.50
2220.50
2221.50
2222.50
2223.50
2224.50
2225.50
2226.50
2227.50
2228.50
2229.50
2230.00
2230.80
2231.80
2232.80
2233.80
MINOR UNIT
From To CommentsComments
The unit is a fairly homogeneous with 50% chert
bands along with f.g qtz-grun +/- green amph bands.
The grunerite is very pale green to buff coloured. The
unit is thickly banded from 2217.50 grading into
thinly banded at ~2225.
Granular looking texture similar to that of a 4CH
however no calcite present. wispy green amphobiloe
is pervasive
1M. Fine to medium grained moderately foliated
ultramafic amphibolite. Light green in colour.
Well foliated boititic mafic volcanic , fine to medium
grained with irregular patches and patches and veins
of Cc alteration.
Comments
Downhole there is an
increase in magnetite
and descrease in
gunerite and an
increase in green
amphibole alteration
The unit is extemely
magnetic between 2228
- 2229.5. There is
between 1-3% Po
associated with the
green amphibole
alteration.
4B SIF. Extermely
magnetic however
bands of magnetite are
thin and looks like
individual crystals of
magnetite are
seperated by thin wispy
green amphibole minor
grunrite.
ALTERATION
Bio
W
M
M
Car
W
W
Chl Gru
M
M
Hem Ser Si Comments
LITHOLOGY LOG Page 26 of 29
Unit
4A
4B
1
2
Unit
08-NSD-004
Assay
Sample
E530619
E530621
E530622
E530623
E530624
E530625
E467751
E467752
E467753
E467754
E467755
E467756
E467757
E467758
E467759
E467761
E467762
E467763
E467764
E467765
E467766
E467767
AU ppm
0.01
0.01
0.01
0.01
0.01
0.01
0.02
0.08
0.20
1.04
0.18
0.35
0.23
0.10
0.12
0.01
0.01
0.03
0.21
0.06
0.06
0.04
MAJOR UNIT
From
2256.30
2257.30
2260.20
2263.90
2272.40
To
2257.30
2260.20
2263.90
2272.40
2275.00
From
2254.30
2255.30
2256.30
2257.30
2258.30
2259.30
2260.20
2261.00
2262.00
2263.00
2263.90
2264.90
2265.90
2266.90
2267.90
2268.90
2269.90
2270.90
2271.60
2272.40
2273.40
2274.40
To
2255.30
2256.30
2257.30
2258.30
2259.30
2260.20
2261.00
2262.00
2263.00
2263.90
2264.90
2265.90
2266.90
2267.90
2268.90
2269.90
2270.90
2271.60
2272.40
2273.40
2274.40
2275.00
MINOR UNIT
From To CommentsComments
Thinly laminated SIF with Zebra texture and
extremely magnetic. Thinly banded to thinly laminated
0.25 - 1 cm in width. Mostly thick massive bands
3-25cm of f.g grunerite, chert and Mt, alternating
with patches of finely banded Mt and grun.
Highly distorted mafic volcanic with both pale and
dark green ampibole alteration and minor biotite slips.
The unit is a thickly laminated to thinly banded
heterogeneous 4B with strong overprint of pale green
amphibole alteration. Note that there is minor garnet
alteration which is amalgamated together (2261.8 -
2262.2)
The unit is a fairly homog' unit of planar chert
(65%) bands and 35% of f.g qtz-grun +/- green
amph with minor biotie. The chert bands are extemely
large and appear to be the protolith with wispy green
amphibole and grunerite thoughout.
A graphitic - argillaceous Iron Fm. which is thinly
laminated. The unit is heterogeneous and minor chert
and magnetite Po mineralization consists of 5-7% \\
to the laminations, and fracture filling.
Comments
The unit is extemely
magnetic and down hole
there is an increase in
grunerite alteration.
Note that magnetite
bands tend to be more
dismembered. ~1-2%
Po present
Minor section of
strong magnetite
between 2267-2269,
2271.5-2272.40 Po
and Aspy 3%.
ALTERATION
Bio
M
Car
W
W
W
Chl Gru
M
W
Hem Ser Si Comments
LITHOLOGY LOG Page 27 of 29
Unit
4B
2
4B
4A
4I
Unit
08-NSD-004
Assay
Sample
E467768
E467769
E467771
E467772
E467773
E467774
E531001
E531002
E531003
E531004
E531005
AU ppm
0.21
0.01
0.03
0.04
0.01
0.01
0.01
0.01
0.01
0.01
0.00
MAJOR UNIT
From
2275.00
2280.00
2281.40
2312.00
2330.20
2330.70
To
2280.00
2281.40
2312.00
2330.20
2330.70
2387.00
From
2275.00
2279.00
2280.00
2280.70
2281.40
2282.40
2328.20
2329.20
2330.20
2330.70
2331.70
To
2276.00
2280.00
2280.70
2281.40
2282.40
2283.40
2329.20
2330.20
2330.70
2331.70
2332.70
MINOR UNIT
From To CommentsComments
Fine grained mafic volcainc with 2-4mm biotite laths.
greyish green with minor calcite veining.
A graphitic - agillaceous Iron Fm. which is thinly
lamininated and heterogeneous. Po mineralization
consists of 7% \\ to the laminations, and fracture
filling. Minor calcite nodules present .5 to 1 cm in
diameter.
Well foliated medium grained flow, fairly fresh mafic
volcanic. The unit consists of 65% light-medium
green acicluar amph and 35% plagioclase. Amph
grains are 0.1-0.4cm in diameter. No significant
veining.
Fine grained mafic volcanic with nil-weak biotite
alt'n. The unit displays 55% light green amph and
45% plagioclase. 2% disseminated biotite alt'n
throughout. From 2327-2330.2m, the unit is cut by
8% Qtz- Cc veins.
4E? The unit has 2 or 3 garnets and is magnetic.
Otherwise, the unit looks like mafic volcanic. The
unit is Cc flooded and contains 90% medium-dark
green amph. Minor Po throughout in short veins.
Fine grained light green mafic volcanic. The unit
consists of 55% green amph and 45% plagioclase.
From 2344.5-2351m, the unit is Qtz-Cc flooded and
contains weak biotite alt'n. Po occurs in short veins
up to 1mm wide (5% throughout).
Comments
The lower contact is
gradational.
Presence of alt'n
composed of chlorite
overprinted by black
amph in the last part of
the section. The lower
contact is sharp @
50dca.
The lower contact is
sharp @ 60dca.
In the last part of the
section, the unit
displays several small
4F bands up to 1cm
wide. Kimberlite dyke
@ 2379.8m over
10cm. Entire unit is
cut by 5% Cc veins up
to 1cm wide.
EOH=2387m
ALTERATION
Bio
W
Car
W
M
M
Chl
W
Gru Hem Ser Si
W
W
Comments
fresh mafic volcanic
4E/mafic volcanic
fresh mafic volcanic
LITHOLOGY LOG Page 28 of 29
Unit
2
4I
2
2
4E
2
Unit
08-NSD-004
Assay
Sample
E531006
E531007
E531008
E531009
E531011
E531012
E531013
E531014
E531015
E531016
E531017
E531018
AU ppm
0.00
0.00
0.01
0.01
0.01
0.00
0.00
0.00
0.00
0.00
0.00
0.00
MAJOR UNIT
From ToFrom
2342.50
2343.50
2344.50
2345.00
2346.00
2347.00
2347.60
2348.00
2349.00
2350.00
2351.00
2352.00
To
2343.50
2344.50
2345.00
2346.00
2347.00
2347.60
2348.00
2349.00
2350.00
2351.00
2352.00
2353.00
MINOR UNIT
From To CommentsComments Comments
ALTERATION
Bio
W
W
Car
M
Chl Gru Hem Ser Si
W
W
Comments
mafic with Po and flooding
LITHOLOGY LOG Page 29 of 29
Unit Unit
Hole ID: 08-NSD-004
Project Code: 9320_NSD
Mine Grid Easting: 7230.174
Mine Grid Northing: 14779.784
Elevation: 5296.61
Target 1: PQ
Target 2:
Target 3:
Drill Start Date: 05/10/2008
Drill End Date: 16/03/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor@1260 Nov. 01/08
Core Diameter: NQ
UTM North:
Survey
Depth
0
10
20
30
40
50
60
70
80
90
100
110
120
130
140
150
160
170
180
190
200
210
220
230
240
250
260
270
280
290
300
310
320
330
340
350
360
370
380
390
400
410
420
430
440
450
460
470
480
490
500
510
520
530
Azimuth
94.73
92.97
91.21
91.22
94.65
98.08
92.66
94.62
96.59
94.67
97.19
99.71
99.81
98.6
97.38
97.14
96.66
96.18
102.51
99.86
97.21
102.93
100.3
97.67
101.38
101.19
101.01
102.22
103.44
102.81
102.18
103.37
104.57
105.1
105.63
105.75
105.87
107.35
108.84
109.12
109.41
110.04
110.67
109.1
107.53
109.2
110.88
109.86
108.83
111.76
114.68
117.26
118.76
120.27
Dip
-86.24
-86.05
-85.86
-85.44
-85.47
-85.5
-85.28
-85.41
-85.54
-85.14
-85.24
-85.35
-85.17
-85.11
-85.06
-84.61
-84.68
-84.75
-84.7
-84.6
-84.49
-84.47
-84.29
-84.1
-84.18
-84.12
-84.06
-84.03
-84
-83.83
-83.66
-83.65
-83.64
-83.67
-83.71
-83.8
-83.89
-83.69
-83.49
-83.53
-83.56
-83.51
-83.47
-83.5
-83.54
-83.45
-83.35
-83.16
-82.97
-82.98
-83
-82.83
-82.65
-82.48
SurveyType
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
Actual Depth: 2387
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-004
Project Code: 9320_NSD
Mine Grid Easting: 7230.174
Mine Grid Northing: 14779.784
Elevation: 5296.61
Target 1: PQ
Target 2:
Target 3:
Drill Start Date: 05/10/2008
Drill End Date: 16/03/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor@1260 Nov. 01/08
Core Diameter: NQ
UTM North:
Survey
Depth
540
550
560
570
580
590
600
610
620
630
640
650
660
670
680
690
700
710
720
730
740
750
760
770
780
790
800
810
820
830
840
850
860
870
880
890
900
910
920
930
940
950
960
970
980
990
1000
1010
1020
1030
1040
1050
1060
1070
Azimuth
119.59
120.66
121.74
122.64
122.33
122.01
117.82
119.35
120.89
117.57
116.23
114.9
114.98
116.76
118.54
121.12
119.87
118.61
118.94
118.92
118.91
122.05
121.62
121.19
118.48
118.6
118.72
118.83
120.29
121.75
122.44
121.54
120.64
121.14
121.52
121.9
124.69
123.55
122.42
123.18
123.5
123.82
124.91
125.07
125.23
125.91
126.19
126.47
127.39
127.74
128.09
128.37
129.68
130.98
Dip
-82.18
-81.97
-81.76
-81.24
-80.98
-80.73
-79.93
-79.68
-79.43
-79.26
-78.95
-78.65
-78.77
-78.55
-78.33
-77.98
-77.85
-77.72
-77.73
-77.64
-77.56
-76.99
-75.76
-74.54
-74.27
-74.17
-74.08
-74.08
-73.66
-73.23
-71.34
-71.23
-71.12
-70.95
-70.98
-71
-70.72
-69.54
-68.36
-68.24
-68
-67.75
-67.58
-67.4
-67.21
-67.06
-66.91
-66.76
-66.48
-66.37
-66.26
-65.99
-65.73
-65.46
SurveyType
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
Actual Depth: 2387
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-004
Project Code: 9320_NSD
Mine Grid Easting: 7230.174
Mine Grid Northing: 14779.784
Elevation: 5296.61
Target 1: PQ
Target 2:
Target 3:
Drill Start Date: 05/10/2008
Drill End Date: 16/03/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor@1260 Nov. 01/08
Core Diameter: NQ
UTM North:
Survey
Depth
1080
1090
1100
1110
1120
1130
1140
1150
1160
1170
1180
1190
1200
1210
1220
1230
1240
1250
1260
1270
1280
1290
1300
1310
1320
1330
1340
1350
1360
1370
1380
1390
1400
1410
1420
1430
1440
1450
1460
1470
1480
1490
1500
1510
1520
1530
1540
1550
1560
1570
1580
1590
1600
1610
Azimuth
129.26
129.51
129.76
130.87
130.97
131.07
128.21
128.8
129.4
125.85
126.17
126.49
126.22
125.66
125.1
124.78
124.97
125.16
125.23
125.25
125.28
124.92
125.31
125.71
125.58
125.54
125.5
126.22
126.62
127.02
128.03
127.96
127.89
128.3
128.25
128.19
128.78
128.88
128.99
129.1
128.75
128.41
128.73
128.94
129.15
129.03
128.9
128.78
128.81
129.04
129.26
129.99
130.21
130.44
Dip
-65.41
-65.31
-65.21
-64.92
-63.67
-62.43
-61.48
-61.28
-61.09
-58.91
-58.44
-57.98
-57.42
-57.2
-56.99
-56.36
-56.18
-56
-55.74
-55.65
-55.56
-55.14
-55.11
-55.08
-54.72
-54.44
-54.16
-53.67
-53.3
-52.94
-52.39
-52.04
-51.69
-51.53
-51.36
-51.2
-50.94
-50.8
-50.66
-50.35
-50.25
-50.15
-50.01
-49.98
-49.94
-49.88
-49.85
-49.83
-49.77
-49.72
-49.68
-49.59
-49.5
-49.42
SurveyType
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
Actual Depth: 2387
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-004
Project Code: 9320_NSD
Mine Grid Easting: 7230.174
Mine Grid Northing: 14779.784
Elevation: 5296.61
Target 1: PQ
Target 2:
Target 3:
Drill Start Date: 05/10/2008
Drill End Date: 16/03/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor@1260 Nov. 01/08
Core Diameter: NQ
UTM North:
Survey
Depth
1620
1630
1638
1640
1641
1644
1647
1650
1653
1656
1659
1662
1665
1668
1671
1674
1677
1680
1683
1686
1689
1692
1695
1698
1701
1704
1707
1710
1713
1716
1719
1722
1725
1728
1731
1734
1737
1740
1743
1746
1749
1752
1755
1758
1761
1764
1767
1770
1773
1776
1779
1782
1785
1788
Azimuth
130
129.95
129.85
129.89
130.03
130.03
130.11
130.25
130.36
130.37
130.32
130.32
130.28
130.23
130.11
129.84
129.55
129.4
129.29
129.27
129.31
129.35
129.37
129.39
129.25
129.21
129.11
128.97
128.85
128.87
128.87
128.84
128.87
128.9
128.91
128.91
128.89
128.82
128.66
128.68
128.69
128.77
128.82
128.83
128.87
128.85
128.91
128.85
128.95
129.08
129.06
129.02
129.04
129.06
Dip
-49.37
-49.3
-49.2
-49.22
-49.18
-49.17
-49.13
-49.11
-49.11
-49.38
-49.59
-49.47
-49.38
-49.4
-49.3
-49.3
-49.36
-49.47
-49.41
-49.32
-49.25
-49.11
-48.96
-48.82
-48.71
-48.58
-48.5
-48.39
-48.3
-48.28
-48.29
-48.23
-48.17
-48.12
-48.05
-47.98
-47.86
-47.72
-47.57
-47.48
-47.39
-47.31
-47.26
-47.19
-47.06
-46.95
-46.82
-46.68
-46.55
-46.46
-46.33
-46.18
-46.06
-45.93
SurveyType
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
GYRO
Actual Depth: 2387
Planned Depth: 2200
UTM East
Hole ID: 08-NSD-004
Project Code: 9320_NSD
Mine Grid Easting: 7230.174
Mine Grid Northing: 14779.784
Elevation: 5296.61
Target 1: PQ
Target 2:
Target 3:
Drill Start Date: 05/10/2008
Drill End Date: 16/03/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments: Maxibor@1260 Nov. 01/08
Core Diameter: NQ
UTM North:
Survey
Depth
1791
1794
1800
1832
1836
1880
1931
Azimuth
129.12
129.15
129.42
129
129
129
129
Dip
-45.88
-45.8
-45.65
-42.7
-42
-40.9
-39.1
SurveyType
GYRO
GYRO
GYRO
EZS
EZS
EZS
EZS
Actual Depth: 2387
Planned Depth: 2200
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
0
3
6
9
12
15
18
21
24
27
30
33
36
39
42
45
48
51
54
57
60
63
66
69
72
75
78
81
84
87
90
93
96
99
102
105
108
111
114
117
120
123
126
129
132
135
138
141
144
147
150
153
156
159
Azimuth
84.6
84.74
84.84
84.9
84.99
85.29
85.47
85.72
85.94
86.16
86.33
86.46
86.67
86.8
86.93
86.99
86.93
86.89
86.87
86.88
87.01
87.17
87.28
87.26
87.5
87.51
87.52
87.54
87.57
87.51
87.49
87.51
87.46
87.49
87.56
87.7
87.92
88.07
88.06
88.17
88.34
88.37
88.43
88.44
88.41
88.44
88.58
89.19
88.87
88.78
89.22
89.25
89.15
89.5
Dip
-82.1
-82.16
-82.2
-82.18
-82.14
-82.09
-82.06
-82.02
-81.97
-81.92
-81.88
-81.87
-81.85
-81.84
-81.82
-81.79
-81.79
-81.78
-81.78
-81.77
-81.75
-81.73
-81.71
-81.7
-81.68
-81.65
-81.64
-81.62
-81.63
-81.61
-81.59
-81.59
-81.52
-81.49
-81.45
-81.42
-81.39
-81.39
-81.37
-81.33
-81.33
-81.3
-81.29
-81.27
-81.24
-81.21
-81.13
-81.11
-81.14
-81.1
-81.08
-81.12
-81.07
-81.09
SurveyType
SURV
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
162
165
168
171
174
177
180
183
186
189
192
195
198
201
204
207
210
213
216
219
222
225
228
231
234
237
240
243
246
249
252
255
258
261
264
267
270
273
276
279
282
285
288
291
294
297
300
303
306
309
312
315
318
321
Azimuth
89.6
89.57
90.01
89.82
89.78
89.98
90.14
89.93
90.25
90.48
90.17
90.56
90.56
90.55
90.54
90.92
90.7
90.79
90.67
90.8
90.88
90.85
91.03
90.9
90.77
91.07
91.13
91.09
91.01
91.42
91.34
91.64
91.67
91.58
91.59
91.58
91.59
91.61
91.66
91.71
91.86
92.06
92.06
92.06
92.23
92.32
92.29
92.46
92.62
92.66
92.8
92.88
93.07
93.23
Dip
-81.07
-81.03
-80.99
-80.94
-80.93
-80.89
-80.88
-80.83
-80.78
-80.82
-80.77
-80.75
-80.69
-80.72
-80.66
-80.7
-80.69
-80.67
-80.71
-80.68
-80.68
-80.65
-80.64
-80.63
-80.63
-80.63
-80.66
-80.63
-80.61
-80.59
-80.56
-80.56
-80.56
-80.54
-80.55
-80.56
-80.56
-80.55
-80.54
-80.54
-80.53
-80.54
-80.54
-80.55
-80.54
-80.54
-80.55
-80.56
-80.56
-80.57
-80.57
-80.54
-80.53
-80.53
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
324
327
330
333
336
339
342
345
348
351
354
357
360
363
366
369
372
375
378
381
384
387
390
393
396
399
402
405
408
411
414
417
420
423
426
429
432
435
438
441
444
447
450
453
456
459
462
465
468
471
474
477
480
483
Azimuth
93.36
93.39
93.57
93.62
93.8
93.96
94
94.08
94.17
94.32
94.78
94.4
94.49
95.01
94.96
94.93
95.25
95.32
95.31
95.71
95.67
95.83
96.12
96.29
96.07
96.36
96.54
96.2
96.49
96.47
96.41
96.3
96.52
96.25
96.23
96.11
96.23
96.35
96.31
96.37
96.24
96.12
96.36
96.45
96.37
96.32
96.64
96.49
96.62
96.58
96.48
96.48
96.48
96.57
Dip
-80.53
-80.52
-80.51
-80.53
-80.54
-80.53
-80.49
-80.45
-80.45
-80.43
-80.45
-80.46
-80.37
-80.32
-80.34
-80.3
-80.32
-80.32
-80.28
-80.23
-80.19
-80.19
-80.16
-80.17
-80.14
-80.11
-80.15
-80.12
-80.11
-80.07
-80.08
-80.03
-80.05
-80.03
-79.99
-80.03
-80
-80
-79.99
-79.97
-79.95
-79.94
-79.9
-79.91
-79.88
-79.88
-79.86
-79.83
-79.81
-79.82
-79.79
-79.78
-79.75
-79.68
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
486
489
492
495
498
501
504
507
510
513
516
519
522
525
528
531
534
537
540
543
546
549
552
555
558
561
564
567
570
573
576
579
582
585
588
591
594
597
600
603
606
609
612
615
618
621
624
627
630
633
636
639
642
645
Azimuth
96.69
96.78
96.87
97.07
97.11
97.16
97.47
98.05
98.67
99.47
99.85
100.26
100.69
101.14
101.28
101.52
101.69
101.84
102.06
102.15
102.36
102.31
102.55
102.68
102.77
103.12
103.23
103.44
103.48
103.56
103.62
103.78
103.98
104.01
104.12
104.2
104.23
104.2
104.17
104.08
104.08
103.98
104.17
104.26
104.6
104.66
105.04
105.12
105.42
105.43
105.45
105.45
105.54
105.68
Dip
-79.64
-79.61
-79.62
-79.55
-79.54
-79.46
-79.38
-79.14
-78.84
-78.55
-78.31
-78.17
-78.01
-77.89
-77.8
-77.77
-77.71
-77.72
-77.66
-77.67
-77.59
-77.57
-77.51
-77.47
-77.4
-77.36
-77.35
-77.31
-77.21
-77.16
-77.07
-77
-76.89
-76.82
-76.68
-76.57
-76.47
-76.39
-76.33
-76.29
-76.26
-76.13
-76.05
-75.94
-75.79
-75.64
-75.53
-75.48
-75.39
-75.3
-75.11
-74.94
-74.72
-74.52
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
648
651
654
657
660
663
666
669
672
675
678
681
684
687
690
693
696
699
702
705
708
711
714
717
720
723
726
729
732
735
738
741
744
747
750
753
756
759
762
765
768
771
772.5
774
775.5
777
778.5
780
781.5
783
784.5
786
787.5
789
Azimuth
105.64
105.79
105.83
106
105.99
106.06
106.03
105.9
105.73
105.76
105.76
105.77
105.79
105.77
105.84
105.81
105.84
105.89
105.9
105.99
105.98
105.98
105.96
106.07
106.13
106.33
106.42
106.55
106.46
106.53
106.58
106.72
106.93
106.93
107.07
107.14
107.31
107.7
108.04
108.15
108.22
108.25
108.3
108.23
108.17
108.16
108.14
108.18
108.26
108.3
108.28
108.23
108.19
108.21
Dip
-74.26
-74.11
-74.01
-73.95
-73.94
-73.88
-73.79
-73.65
-73.52
-73.4
-73.33
-73.27
-73.22
-73.17
-73.11
-73.05
-72.99
-72.96
-72.93
-72.91
-72.85
-72.84
-72.81
-72.76
-72.71
-72.66
-72.63
-72.59
-72.54
-72.47
-72.4
-72.33
-72.24
-72.17
-72.09
-72.09
-72.31
-72.35
-72.12
-71.94
-71.81
-71.71
-71.67
-71.66
-71.64
-71.59
-71.52
-71.47
-71.43
-71.4
-71.36
-71.32
-71.3
-71.25
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
790.5
792
793.5
795
796.5
798
799.5
801
802.5
804
805.5
807
808.5
810
811.5
813
814.5
816
817.5
819
820.5
822
823.5
825
826.5
828
829.5
831
832.5
834
835.5
837
838.5
840
841.5
843
844.5
846
847.5
849
852
855
858
861
864
867
870
873
876
879
882
885
888
891
Azimuth
108.28
108.35
108.29
108.34
108.52
108.61
108.61
108.58
108.57
108.65
108.79
108.8
108.75
108.78
108.79
108.78
108.86
108.89
108.84
108.78
108.87
108.95
108.98
108.95
108.94
108.99
109.06
109.06
108.64
107.37
106.23
105.84
105.78
105.86
105.99
106.02
105.94
105.91
105.95
106.01
105.98
106.05
106.1
106.21
106.34
106.45
106.48
106.6
105.87
104.74
104.47
104.93
105.06
105.23
Dip
-71.16
-71.09
-71.04
-70.97
-70.89
-70.85
-70.79
-70.72
-70.67
-70.62
-70.53
-70.47
-70.44
-70.42
-70.39
-70.33
-70.31
-70.32
-70.28
-70.25
-70.25
-70.23
-70.19
-70.16
-70.12
-70.1
-70.08
-70.06
-70.02
-69.89
-69.79
-69.68
-69.57
-69.5
-69.49
-69.47
-69.46
-69.46
-69.44
-69.44
-69.43
-69.38
-69.36
-69.33
-69.33
-69.31
-69.33
-69.3
-69.22
-69.03
-68.88
-68.87
-68.86
-68.83
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
894
897
900
903
906
909
912
915
918
921
924
927
930
933
936
939
942
945
948
951
954
957
960
963
966
969
972
975
978
981
984
987
990
993
996
999
1002
1005
1008
1009.5
1011
1012.5
1014
1015.5
1017
1018.5
1020
1021.5
1023
1024.5
1026
1027.5
1029
1030.5
Azimuth
105.38
105.63
105.58
105.72
105.91
105.93
106.03
106.03
106.38
107.35
108.38
108.43
108.65
108.64
108.7
108.65
108.82
108.96
108.92
108.95
108.96
108.96
108.92
109.09
109.06
108.56
107.23
107.37
108.04
108.24
108.25
108.54
108.51
108.55
108.73
108.74
108.77
109.02
109.1
109.16
109.25
109.41
109.63
109.76
109.91
110.12
110.21
110.22
110.21
110.39
110.61
110.79
110.92
110.91
Dip
-68.82
-68.82
-68.8
-68.77
-68.79
-68.79
-68.79
-68.78
-68.79
-68.59
-68.26
-67.93
-67.79
-67.72
-67.7
-67.7
-67.69
-67.64
-67.63
-67.56
-67.52
-67.49
-67.41
-67.41
-67.33
-67.3
-66.91
-66.27
-65.93
-65.76
-65.63
-65.51
-65.4
-65.24
-65.14
-65.01
-64.89
-64.76
-64.62
-64.58
-64.53
-64.48
-64.45
-64.4
-64.34
-64.32
-64.32
-64.36
-64.37
-64.31
-64.27
-64.29
-64.17
-63.86
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1032
1033.5
1035
1036.5
1038
1039.5
1041
1042.5
1044
1047
1050
1053
1056
1059
1062
1065
1068
1071
1074
1077
1080
1083
1086
1089
1092
1095
1098
1101
1104
1107
1110
1113
1116
1119
1122
1125
1128
1131
1134
1137
1140
1143
1146
1149
1152
1155
1158
1161
1164
1167
1170
1173
1176
1179
Azimuth
110.84
110.95
111.14
111.26
111.43
111.57
111.68
111.74
111.8
111.82
111.89
111.88
111.82
111.82
111.83
111.83
111.94
112.05
112.04
112.13
112.22
112.25
112.37
112.52
112.7
112.92
112.88
112.83
112.73
112.49
112.23
111.98
111.77
111.6
111.5
111.48
111.45
111.35
111.31
111.12
110.91
110.66
110.4
110.17
109.99
109.87
109.83
109.72
109.7
109.75
109.73
109.63
109.5
109.37
Dip
-63.51
-63.21
-62.92
-62.66
-62.52
-62.47
-62.47
-62.45
-62.4
-62.17
-61.34
-60.17
-59.08
-58.36
-58.02
-57.84
-57.66
-57.56
-57.51
-57.43
-57.35
-57.25
-57.09
-56.69
-56.05
-55.67
-55.52
-55.25
-54.89
-54.51
-54.18
-53.84
-53.55
-53.2
-52.86
-52.58
-52.28
-51.95
-51.55
-51.2
-50.78
-50.39
-49.98
-49.61
-49.32
-49.03
-48.8
-48.51
-48.23
-47.97
-47.76
-47.53
-47.28
-46.98
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1182
1185
1188
1191
1194
1197
1200
1203
1206
1209
1212
1215
1218
1221
1224
1227
1230
1233
1236
1239
1242
1245
1248
1251
1254
1257
1260
1263
1266
1269
1272
1275
1278
1281
1284
1287
1290
1293
1296
1299
1302
1305
1308
1311
1314
1317
1320
1323
1326
1329
1332
1335
1338
1341
Azimuth
109.23
109.21
109.2
109.08
108.87
108.72
108.62
108.57
108.51
108.5
108.5
108.45
108.47
108.57
108.59
108.64
108.72
108.7
108.68
108.65
108.62
108.62
108.53
108.46
108.35
108.25
108.19
108.18
108.19
108.14
108.08
108.09
108.14
108.13
108.12
108.04
107.91
107.85
107.69
107.59
107.55
107.53
107.52
107.56
107.52
107.5
107.55
107.53
107.51
107.53
107.59
107.6
107.63
107.59
Dip
-46.68
-46.46
-46.22
-45.94
-45.63
-45.3
-45.04
-44.84
-44.66
-44.4
-44.14
-43.97
-43.75
-43.48
-43.28
-43.14
-43.01
-42.87
-42.72
-42.49
-42.31
-42.1
-41.87
-41.64
-41.31
-40.89
-40.57
-40.2
-39.82
-39.53
-39.23
-38.97
-38.73
-38.45
-38.14
-37.74
-37.33
-37.05
-36.82
-36.71
-36.62
-36.51
-36.38
-36.28
-36.17
-36.09
-35.95
-35.83
-35.73
-35.59
-35.49
-35.43
-35.29
-35.19
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1344
1347
1350
1353
1356
1359
1362
1365
1368
1371
1374
1377
1380
1383
1386
1389
1392
1395
1398
1401
1404
1407
1410
1413
1416
1419
1422
1424
1427
1430
1433
1436
1439
1442
1445
1448
1451
1454
1457
1460
1463
1466
1469
1473
1474.5
1476
1477.5
1479
1480.5
1482
1483.5
1485
1486.5
1488
Azimuth
107.65
107.66
107.57
107.55
107.62
107.64
107.62
107.65
107.6
107.67
107.69
107.69
107.68
107.73
107.67
107.44
107.02
106.65
106.4
106.28
106.22
106.19
106.06
105.71
105.44
105.23
105.16
105.03
104.77
104.53
104.38
104.28
104
103.19
102.27
101.91
101.69
101.44
101.18
100.96
100.84
100.65
100.46
100.27
100.16
100.04
99.93
99.83
99.74
99.63
99.5
99.53
99.86
99.53
Dip
-35.06
-34.94
-34.82
-34.67
-34.54
-34.5
-34.4
-34.29
-34.21
-34.13
-34.03
-33.97
-33.9
-33.88
-33.7
-33
-32.23
-31.61
-31.16
-30.88
-30.69
-30.53
-30.3
-29.94
-29.57
-29.26
-28.99
-28.8
-28.67
-28.47
-28.26
-28.05
-27.96
-28.27
-28.61
-28.5
-28.26
-28.01
-27.69
-27.4
-27.21
-26.97
-26.67
-26.4
-26.27
-26.15
-26.02
-25.86
-25.68
-25.52
-25.28
-25.01
-24.77
-23.44
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1489.5
1491
1492.5
1494
1495.5
1497
1498
1501
1504
1507
1510
1513
1516
1519
1522
1525
1528
1531
1534
1537
1540
1543
1546
1549
1552
1555
1558
1561
1564
1567
1570
1573
1576
1579
1582
1585
1588
1591
1594
1597
1600
1603
1606
1609
1612
1615
1618
1621
1624
1627
1630
1633
1636
1639
Azimuth
99.17
98.89
98.74
98.63
98.54
98.42
98.3
98.1
98
97.8
97.7
97.7
97.6
97.6
97.6
97.6
97.6
97.6
97.6
97.6
97.5
97.4
97.4
97.4
97.4
97.3
97.2
97.1
97
96.9
96.7
96.6
96.4
96.2
96.1
95.9
95.7
95.6
95.5
95.2
94.9
94.6
94.5
94.3
94.2
94
93.8
93.7
93.6
93.5
93.4
93.2
93
93.1
Dip
-22.51
-22.19
-22.02
-21.87
-21.74
-21.62
-21.7
-21.4
-21.2
-20.9
-20.7
-20.5
-20.4
-20.2
-20.1
-19.9
-19.8
-19.7
-19.6
-19.5
-19.3
-19.1
-18.9
-18.7
-18.5
-18.5
-18.5
-18.4
-18.4
-18.3
-18.3
-18.3
-18.3
-18.3
-18.3
-18.1
-18
-17.9
-18
-18.1
-18.2
-18.3
-18.3
-18.3
-18.2
-18.2
-18.1
-18.1
-18.1
-18.3
-18.6
-18.9
-18.9
-18.9
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1642
1645
1648
1651
1654
1657
1660
1663
1666
1669
1672
1675
1678
1681
1684
1687
1690
1693
1696
1699
1702
1705
1708
1711
1714
1717
1720
1723
1726
1729
1732
1735
1738
1741
1744
1747
1750
1753
1756
1759
1762
1765
1768
1771
1774
1777
1780
1783
1786
1789
1792
1795
1798
1801
Azimuth
93
92.9
92.9
92.8
92.8
92.7
92.7
92.6
92.6
92.5
92.6
92.6
92.6
92.6
92.5
92.3
92.2
92.2
92.1
92
91.9
91.8
91.8
91.7
91.7
91.6
91.6
91.5
91.5
91.5
91.5
91.5
91.5
91.5
91.4
91.4
91.4
91.5
91.4
91.4
91.3
91.3
91.3
91.2
91.1
91
90.9
90.9
90.8
90.8
90.7
90.6
90.4
90.4
Dip
-18.9
-18.8
-18.7
-18.6
-18.6
-18.5
-18.5
-18.5
-18.5
-18.4
-18.4
-18.3
-18.1
-18.1
-18.3
-18.4
-18.4
-18.4
-18.4
-18.4
-18.5
-18.5
-18.4
-18.4
-18.3
-18.3
-18.2
-18.1
-18
-17.8
-17.6
-17.5
-17.3
-17.2
-17
-16.9
-16.8
-16.7
-16.6
-16.4
-16.2
-16.1
-15.9
-15.9
-15.7
-15.6
-15.5
-15.4
-15.3
-15.2
-15.1
-15.1
-15
-14.7
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1804
1807
1810
1813
1816
1819
1822
1825
1828
1831
1834
1837
1840
1843
1846
1849
1852
1855
1858
1861
1864
1867
1870
1873
1876
1879
1882
1885
1888
1891
1894
1897
1900
1903
1906
1909
1912
1915
1918
1921
1924
1927
1930
1933
1936
1939
1942
1945
1948
1951
1954
1957
1960
1963
Azimuth
90.4
90.4
90.4
90.4
90.5
90.5
90.4
90.4
90.4
90.4
90.4
90.4
90.5
90.5
90.6
90.6
90.7
90.8
90.8
90.9
91
91.1
91.1
91.2
91.3
91.4
91.4
91.5
91.5
91.6
91.7
91.8
91.9
92
92
92.1
92.2
92.3
92.3
92.4
92.5
92.6
92.6
92.7
92.8
92.9
92.9
92.9
92.99
93.04
93.09
93.14
93.19
93.24
Dip
-14.5
-14.3
-14.1
-14
-13.8
-13.6
-13.4
-13.3
-13.1
-13
-12.8
-12.6
-12.4
-12.3
-12.1
-12
-11.9
-11.7
-11.6
-11.4
-11.3
-11.1
-11
-10.9
-10.7
-10.6
-10.5
-10.4
-10.2
-10
-9.9
-9.8
-9.8
-9.7
-9.6
-9.5
-9.4
-9.3
-9.2
-9.2
-9
-8.9
-8.8
-8.6
-8.4
-8.3
-8.1
-8
-7.83
-7.68
-7.53
-7.38
-7.23
-7.08
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
Hole ID: 09-NSD-001
Project Code: 9320_NSD
Mine Grid Easting: 7521.6
Mine Grid Northing: 14776.8
Elevation: 5298.4
Target 1: PQE
Target 2:
Target 3:
Drill Start Date: 06/03/2009
Drill End Date: 17/04/2009
Plugged: YES
MUSSELWHITE MINE - GEOLOGY
Comments:
Core Diameter: NQ2
UTM North:
Survey
Depth
1966
1969
1972
1975
1977
1978
Azimuth
93.29
93.34
93.39
93.44
93.49
93.49
Dip
-6.93
-6.78
-6.63
-6.48
-6.33
-6.33
SurveyType
MAXI
MAXI
MAXI
MAXI
MAXI
MAXI
Actual Depth: 1978
Planned Depth: 2075
UTM East
09-NSD-001
MAJOR UNIT
From
0.00
1440.00
1442.00
1444.80
1452.50
1465.90
1476.10
1478.10
1487.80
1520.40
1522.00
1529.50
1535.50
1536.40
1537.50
1539.10
1539.80
To
1440.00
1442.00
1444.80
1452.50
1465.90
1476.10
1478.10
1487.80
1520.40
1522.00
1529.50
1535.50
1536.40
1537.50
1539.10
1539.80
1542.50
MINERALS
As%Cp%
Mt%
Po%
2.0
4.0
2.0
2.0
2.0
3.0
0.0
0.0
2.0
Py%
1
2
3
CommentsVGSpecks
FABRIC
From
1446.10
1453.50
1457.40
1462.10
1466.20
1468.60
1474.60
1477.20
1479.50
1482.80
1485.50
1487.30
1487.30
1505.00
1519.00
1529.50
1536.40
1539.80
To
1446.10
1453.50
1457.40
1462.10
1466.20
1468.60
1474.60
1477.20
1479.50
1482.80
1485.50
1487.30
1505.00
1519.00
1529.50
1535.50
1537.50
1542.50
Alphadeg
65
65
90
60
55
85
85
75
60
45
65
65
70
75
70
85
80
75
CommentsInt
MO
MO
MO
WE
MO
MO
MO
MO
WE
MO
WE
WE
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1546.00
Alpha
deg
75
Comments
Series of
M, S
folds cm
scale
Int
MO
Type
FD
From
1543.00
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
No
2
2T
4F
2
4F
2
3F
3A
2
2T
3F
QTZ
2
4E
6
4F
Cont
70
65
60
75
55
75
75
75
70
70
75
70
STRUCTURAL LOG Page 1 of 8
09-NSD-001
MAJOR UNIT
From
1547.00
1548.00
1552.40
1562.30
1570.80
1574.80
1584.30
1585.40
1592.20
1597.30
To
1548.00
1552.40
1562.30
1570.80
1574.80
1584.30
1585.40
1592.20
1597.30
1603.90
MINERALS
As%Cp%
Mt%
Po%
0.0
Py% CommentsVGSpecks
FABRIC
From
1547.00
1555.00
1561.00
1566.00
1570.80
1576.80
1585.00
1594.00
1600.00
To
1550.50
1556.00
1561.70
1567.00
1571.80
1577.50
1586.00
1594.30
1600.80
Alphadeg
75
80
80
80
75
78
80
80
80
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From
1544.50
1600.80
To
1549.00
1603.90
Alphadeg
70
Comments
broken core
Int
MOD
MOD
Type
SZ
BC
MajorUnit
4E
1
4F
2
4F
2
4F
2
6
2
Cont
75
90
70
80
70
80
STRUCTURAL LOG Page 2 of 8
09-NSD-001
MAJOR UNIT
From
1603.90
1608.00
1621.80
1640.80
1662.70
To
1608.00
1621.80
1640.80
1662.70
1666.70
MINERALS
As%Cp%
Mt%
Po%
2.0
2.0
2.0
Py% Comments
Po in veins
along foliation
Po in 4F
VGSpecks
FABRIC
From
1609.00
1627.00
1636.00
To
1610.00
1628.00
1637.00
Alphadeg
70
80
80
CommentsInt
MO
MO
WE
Type
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From To Alphadeg CommentsInt Type
MajorUnit
4F
2
4F
2
4F
Cont
90
90
90
90
STRUCTURAL LOG Page 3 of 8
09-NSD-001
MAJOR UNIT
From
1666.70
1668.70
1677.00
1687.30
1690.40
1694.70
1699.40
1701.00
1702.30
To
1668.70
1677.00
1687.30
1690.40
1694.70
1699.40
1701.00
1702.30
1704.50
MINERALS
As%Cp%
Mt%
Po%
0.0
1.0
0.5
0.3
1.0
Py%
0.01
Comments
intermediate
two Po vein
3cm wide and
0.5cm wide
sheared 4E
VGSpecks
FABRIC
From
1666.50
1671.00
1674.00
1678.40
1683.00
1687.30
1697.00
To
1666.70
1672.00
1675.00
1679.00
1684.00
1688.30
1698.00
Alphadeg
80
90
85
85
65
80
80
CommentsInt
MO
MO
MO
MO
WE
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ
Vein%
10
Tex ContactType
Alphadeg
Comments
qtz flooded
From
1703.30
To
1703.80
FAULT
From
1703.30
To
1703.80
Alphadeg
60
CommentsInt
INT
Type
SZ
MajorUnit
2
3A
4F
2
4F
2
4F
2
4E
Cont
85
80
90
80
90
90
90
STRUCTURAL LOG Page 4 of 8
09-NSD-001
MAJOR UNIT
From
1704.50
1706.00
1706.60
1723.50
1724.80
1750.30
1754.00
1771.60
1774.10
1775.50
1780.60
To
1706.00
1706.60
1723.50
1724.80
1750.30
1754.00
1771.60
1774.10
1775.50
1780.60
1796.60
MINERALS
As%Cp%
Mt%
Po%
8.0
10.
30.
0.5
20.
3.0
3.0
10.
10.
Py% Comments
sheared 4E
sheared
altered 4E
sheared qtz
flooded 4E
sheared qtz
flooded 4E
4e
sheared 4E
VGSpecks
FABRIC
From
1706.00
1711.00
1719.00
1726.00
1735.00
1741.00
1744.00
1752.00
1767.00
1771.60
1775.50
1780.00
To
1706.60
1712.00
1720.00
1727.00
1736.00
1742.00
1745.00
1753.00
1768.00
1772.20
1776.20
1780.20
Alphadeg
80
70
70
65
50
60
70
50
75
75
70
65
Comments
shear
foliation
Int
MO
MO
MO
MO
MO
MO
MO
WE
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ
QZ
QZ
QZ
Vein%
3
30
25
10
Tex ContactType
Alphadeg
Comments
qtz flooded
qtz
flooded 4E
qtz
flooded 4E
qtz
flooded 4E
From
1706.00
1723.50
1771.60
1776.20
To
1706.60
1724.20
1774.10
1780.20
FAULT
From
1706.00
1723.50
1771.60
1778.50
To
1706.60
1724.20
1773.20
1780.20
Alphadeg
80
60
75
65
CommentsInt
MOD
INT
INT
INT
Type
SZ
SZ
SZ
SZ
MajorUnit
2
4E
2
4E
2
1
2
4E
2
4E
2
Cont
50
90
70
80
75
75
65
90
STRUCTURAL LOG Page 5 of 8
09-NSD-001
MAJOR UNIT
From
1796.60
1799.20
1801.00
1804.70
1806.70
1825.20
1826.80
1837.50
1840.30
To
1799.20
1801.00
1804.70
1806.70
1825.20
1826.80
1837.50
1840.30
1844.50
MINERALS
As%Cp%
Mt%
Po%
8.0
4.0
3.0
2.0
3.0
2.0
3.0
1.0
Py% Comments
sheared 4E
VGSpecks
FABRIC
From
1783.00
1791.00
1796.60
1802.00
1808.00
1816.00
1817.00
1825.20
1831.00
1833.70
1837.00
1840.30
To
1784.00
1792.00
1797.60
1803.00
1809.00
1817.00
1825.20
1831.00
1832.30
1837.00
1840.30
1844.50
Alphadeg
70
75
70
70
70
70
70
80
75
75
70
80
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1801.70
1840.00
Alpha
deg
90
70
CommentsInt
WE
MO
Type
FD
FD
From
1801.00
1839.00
QTZ VEINING
VeinType
QZ
Vein%
8
Tex ContactType
Alphadeg
Comments
qtz
flooded 4E
From
1801.00
To
1802.20
FAULT
From
1801.00
1807.70
1826.80
1832.30
1840.00
To
1802.20
1813.00
1827.50
1833.70
1840.30
Alphadeg
80
70
75
80
80
Comments
2t
Int
MOD
MOD
MOD
INT
MOD
Type
SZ
SZ
SZ
SZ
SZ
MajorUnit
3F
2
4E
6
2T
4F
4EA
4B
4B
Cont
90
80
65
75
70
90
STRUCTURAL LOG Page 6 of 8
09-NSD-001
MAJOR UNIT
From
1844.50
1856.00
1876.80
1878.00
1879.00
1881.90
1907.90
1911.90
1915.90
1921.10
1928.90
To
1856.00
1876.80
1878.00
1879.00
1881.90
1907.90
1911.90
1915.90
1921.10
1928.90
1934.30
MINERALS
As%Cp%
Mt%
Po%
5.0
0.3
10.
10.
Py% CommentsVGSpecks
FABRIC
From
1844.50
1870.00
1876.00
1877.40
1882.80
1888.00
1897.00
1903.00
1907.00
1911.90
1915.90
1923.00
1928.90
1931.50
To
1870.00
1876.00
1877.40
1882.80
1888.00
1897.00
1903.00
1907.00
1911.90
1915.90
1923.00
1928.90
1930.20
1933.90
Alphadeg
85
80
70
80
70
60
65
55
60
55
75
70
70
70
CommentsInt
MO
MO
MO
MO
MO
MO
MO
MO
WE
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
ToAlph
adeg
CommentsInt TypeFrom
QTZ VEINING
VeinType
QZ-C
Vein%
85
Tex
sy
ContactType
S
Alphadeg
75
CommentsFrom
1921.00
To
1923.00
FAULT
From
1929.20
To
1930.00
Alphadeg
60
CommentsInt
MOD
Type
SZ
MajorUnit
4B
2T
4H
4A
4B
2T
1
2
1
2T
4B
Cont
85
70
80
90
70
70
60
60
70
85
70
STRUCTURAL LOG Page 7 of 8
09-NSD-001
MAJOR UNIT
From
1934.30
1939.50
1947.60
1950.70
1958.80
1960.20
1969.30
1969.70
To
1939.50
1947.60
1950.70
1958.80
1960.20
1969.30
1969.70
1978.00
MINERALS
As%Cp%
Mt%
Po%
0.1
40.
Py% Comments
traces Po in 4A
4H
VGSpecks
FABRIC
From
1934.30
1937.50
1939.00
1941.60
1943.40
1958.80
1963.00
1971.00
To
1936.90
1939.00
1941.60
1943.00
1946.00
1959.70
1964.00
1972.00
Alphadeg
70
80
85
85
85
80
80
80
CommentsInt
INT
MO
MO
MO
MO
MO
MO
MO
Type
S1
S1
S1
S1
S1
S1
S1
S1
FOLD
To
1936.70
Alpha
deg
40
CommentsInt
MO
Type
ZF
From
1934.00
QTZ VEINING
VeinType
Vein% Tex Contact
TypeAlphadeg
CommentsFrom To
FAULT
From
1933.90
1943.00
To
1934.30
1943.40
Alphadeg
75
65
CommentsInt
MOD
MOD
Type
BC
SZ
MajorUnit
4B
4B
1
2
4B
4A
4H
2
Cont
60
70
85
85
80
90
STRUCTURAL LOG Page 8 of 8
09-NSD-001
Assay
Sample
E531251
E531252
AU ppm
0.00
0.00
MAJOR UNIT
From
0.00
1440.00
1442.00
1444.80
1452.50
To
1440.00
1442.00
1444.80
1452.50
1465.90
From
1463.90
1464.90
To
1464.90
1465.90
MINOR UNIT
From To CommentsComments
Hole is wedged off of 06-NSD-001
Light to medium grey coloured mafic volcanic unit
with weak to moderate biotization throughout
(m.g-c.g) and weak Cc veinlets. Hole was wedged
between 1447-1448m (core is halved).
Unit is a moderately to strongly foliated, grayish
brownish coloured mafic volcanic unit with intense
m.g.-c.g. bio alt'n throughout(dark brown) and cut by
~ 5-10% Cc veins and veinlets with weak to mod dark
green amph alt'n.
First meter appears to be gradational between 2 & 4F
(mafics with bands of bio alt'n with grts). Remainder
consists of a f.g. bio matrix studded with 1-2mm in
diam & anhedral grts (~ 20-40%), there is mod grun
alt'n (with grts) and minor staurolite
Light grey (greenish tint) mafic volcanic unit with
mod biotized patches throughout (light brown & c.g.
bio), unit is cut by minor Cc veining. There are
several minor 4F units (fr 1456.5-1456.2 there is
intercalated 4F)
Comments
L.C is gradational over
~1m.
in a few patches. Unit
appears to be altered or
bleached (pale beige)
throughout the unit,
there are several
patches with m.g.-c.g.
dark brown biotite.
There is some weak to
moderate qtz veining
and weak amph alt'n
within a few patches.
From 1456.9-1457.4,
1459-1459.6m &
1460-1461.1m there
are patches of 4F as
well. 4F patches
consist of mod light
brown bio , with wk
dark brown c.g. bio
alt'n & studded with
wk-mod grts (grts are
1-3mm in diam &
anhedral).
ALTERATION
Bio
W
S
M
M
W
S
W
S
W
Car
W
M
W
W
W
W
M
W
W
Chl Gru
M
W
W
Hem Ser Si
W
W
Comments
LITHOLOGY LOG Page 1 of 19
Unit
No
2
2T
4F
2
Unit
09-NSD-001
Assay
Sample
E531253
E531254
E531255
E531256
E531257
E531258
E531259
E531261
E531262
E531263
E531264
E531265
AU ppm
0.07
0.06
0.02
0.10
0.02
0.01
0.02
0.03
0.01
0.01
0.01
0.03
MAJOR UNIT
From
1465.90
1476.10
To
1476.10
1478.10
From
1465.90
1466.50
1467.00
1468.00
1469.00
1470.00
1471.00
1472.00
1473.00
1474.00
1475.00
1476.10
To
1466.50
1467.00
1468.00
1469.00
1470.00
1471.00
1472.00
1473.00
1474.00
1475.00
1476.10
1477.10
MINOR UNIT
From To CommentsComments
Majority of the unit consists of f.g-m.g. bio matrix
studded with varying amounts of grts (<1-6 mm in
diam, anhedral & range fr ~5-20%) as well as wk
staurolite patches. There are several 10-30cm
sections of mafic volcanic.
Light greenish/grey coloured, weakly foliated mafic
volcanic unit with few patches with moderate bio alt'n
(m.g-c.g. and med to drk brown). The unit is also cut
by several Cc veinlets. U.C and lower contacts are
gradational.
Comments
~10-15% 4E patches
consisting of f.g.,
dark green amph
studded with ~2-3mm
in diam & anhedral grts
with mod assoc'd qtz
veining & weak-mod Cc
veinlets/stringers.
Trace to 1% Po (within
4E patches).
ALTERATION
Bio
W
Car
W
W
Chl Gru Hem Ser Si
M
Comments
LITHOLOGY LOG Page 2 of 19
Unit
4F
2
Unit
09-NSD-001
Assay
Sample
E531266
E531267
E531268
E531269
E531271
E531272
E531273
E531274
AU ppm
0.01
0.01
0.01
0.20
0.01
0.02
0.03
0.50
MAJOR UNIT
From
1478.10
1487.80
1520.40
1522.00
1529.50
1535.50
1536.40
1537.50
To
1487.80
1520.40
1522.00
1529.50
1535.50
1536.40
1537.50
1539.10
From
1477.10
1534.00
1534.50
1535.50
1536.40
1537.00
1537.50
1538.50
To
1478.10
1534.50
1535.50
1536.40
1537.00
1537.50
1538.50
1539.10
MINOR UNIT
From To CommentsComments
Gradational upper contact (first 40cm of the unit
contains moderate bio. Remainder of the unit
consists of a qtz/feld matrix with patches with
moderate to strong sericite banding. Unit is cut by
weak qtz veins and weak to moderate Cc veining.
Strong sericite alteration bands with minor fine
grained biotite. There are several 1-2 cm wide
sericite slips. Minor section of pale green amphibole
and garnet alteration.
Fine to Medium grained dark green mafic volcanic
with Cc Veins \\ to the foliation. 35% plagioclase and
65% med-dark green amphibole The unit is weakly
foliated to massive..
Mafic volcanic, borderline andesitie. A biotitic mafic
volcanic with wispy strong pale green amphibole
alteration. The lower section consists of intercalated
sections of quartz Cc veining and sericite .
The unit is Buff to light grey in colour with moderate
green amphibole and 3% biotite bands. 2% Py
mineralization as fracture filling and \\ to the foliation.
Distorted quartz Cc vein with strong green amphibole
and garnet alteration. Garnets are dark pink ~ .5 to 1
cm in diameter with no mineralization.
Biotitic mafic volcanic with 35% plagiclase and wispy
mm scale Cc veining.
Strong biotite garnet alteration at the L.C. grading
in to strong green amphibole and quartz flooding
between 1538.5 - 1539..10. There is 3% Po
associated with green amphibole and garnet
alteration between 1538.5-1538.9.
Comments
Po and Py varies from ~
trace to ~5% (occurs
as stringers, veins,
disseminated patches
and few blebs). There
are some sections that
appear to be massive
and some that are
weakly foliated.
Between 1515.80-
1516.2m 10% Pyrite.
Minor sections were
there is local garnet &
green amphibole
alteration.
From the U.C. to 1522
the unit dispays strong
chlorite alteration.
The foliation is ~70
degrees t.c.a.
ALTERATION
Bio
W
W
W
W
W
M
Car
W
W
M
Chl
S
Gru Hem Ser
M
M
S
W
Si
M
M
Comments
LITHOLOGY LOG Page 3 of 19
Unit
3F
3A
2
2T
3F
QTZ
2
4E
Unit
09-NSD-001
Assay
Sample
E531275
E531276
E531277
E531278
E531279
E531281
E531282
E531283
E531284
E531285
E531286
E531287
E531288
E531289
E531291
E531292
E531293
E531294
E531295
E531296
E531297
AU ppm
0.02
0.62
0.02
0.01
0.16
0.02
0.86
0.16
0.08
0.35
0.23
0.09
0.03
0.02
0.03
0.04
0.04
0.06
0.03
0.34
0.22
MAJOR UNIT
From
1539.10
1539.80
1547.00
1548.00
1552.40
To
1539.80
1542.50
1548.00
1552.40
1562.30
From
1539.10
1539.80
1540.80
1541.80
1542.50
1543.50
1544.50
1545.50
1545.90
1546.30
1547.00
1548.00
1549.00
1550.00
1550.70
1551.70
1552.40
1553.40
1554.10
1555.00
1556.00
To
1539.80
1540.80
1541.80
1542.50
1543.50
1544.50
1545.50
1545.90
1546.30
1547.00
1548.00
1549.00
1550.00
1550.70
1551.70
1552.40
1553.40
1554.10
1555.00
1556.00
1557.00
MINOR UNIT
From To CommentsComments
Mostly grey - brown, fine grained sediment; the unit
is equigranular and evenly distributed. <1mm wide
garnets present near the L.C.
Fine grained homogeneous 4f with pinhead size
garnets. There is yellow staurolite present though out
the unit
Typical porphyroblastic 4E with moderate
biotite/garnet alteration. Primary garnets 0.4 to 0.7 cm
in diameter. Alteration garnets are up to 1.2 cm in
diameter at the lower contact
4E? Bleached?UM? The unit is magnetic and fairly
soft. Might be an ultramafic consisting of talc and
f.g.light green mineral (hard to see if it is green amph
or serpentine). Overall, the unit is white to very light
green.
Well developed 4F bio-schist The unit consists of a
f.g.biotite rich matrix studded by 25%
f.g.-m.g.garnets up to 0.5cm in diameter (more
porphyroblastic 4F in the last 30cm). The unit is cut
by 3% Qtz veins averaging 1cm wide.
Comments
Locally, the unit
contains very
f.g.garnets. From
1550.7-1552.4m, the
unit is medium green
(borderline mafic volc)
and contains less talc
and 30-40%
amorphous serpentine.
Minor 4F over 5cm.
Po in traces in massive
Qtz vein in the first
50cm. The lower
contact is sharp
@90dca.
ALTERATION
Bio
M
S
W
Car Chl Gru Hem Ser Si
W
Comments
UM
UM with less talc
LITHOLOGY LOG Page 4 of 19
Unit
6
4F
4E
1
4F
Unit
09-NSD-001
Assay
Sample
E531298
E531299
E513501
E513502
E513503
E513504
E513505
E513506
E513507
E513508
E513509
E513511
E513512
E513513
E513514
E513515
E513516
E513517
E513518
E513519
AU ppm
0.03
0.04
0.06
0.20
0.66
0.07
0.01
0.02
0.03
0.04
0.05
0.02
0.00
0.03
0.01
0.01
0.02
0.01
0.01
0.01
MAJOR UNIT
From
1562.30
1570.80
1574.80
1584.30
To
1570.80
1574.80
1584.30
1585.40
From
1557.00
1558.00
1559.00
1560.00
1561.00
1561.70
1562.30
1563.30
1568.80
1569.80
1570.80
1571.80
1572.80
1573.80
1574.80
1575.80
1582.30
1583.30
1584.30
1585.00
To
1558.00
1559.00
1560.00
1561.00
1561.70
1562.30
1563.30
1564.30
1569.80
1570.80
1571.80
1572.80
1573.80
1574.80
1575.80
1576.80
1583.30
1584.30
1585.00
1585.40
MINOR UNIT
From To CommentsComments
Well foliated fine grained to medium grained mafic
volcanic. The unit conists of 60% f.g.-m.g green
amph, 30% f.g.plagioclase and 10% biotite
(scattered). No significant veining, no visible
mineralisation.
Well developed 4F meta-pelite. Fairly similar to
previous 4F unit. The unit consists of 25-30%
f.g.-m.g.garnets in f.g.biotite rich matrix. Locally, c.g.
biotite alt'n around Qtz veins, overprinting the original
matrix.
Well foliated fine grained mafic volcanic. Borderline
2T overall, real 2T from 1577.5-1579m (40% biotite
slips). The unit consists of equigranular green amph
and plagioclases, with 5-10% biotite. The unit is cut
by <1% Qtz veins.
Bio-schist consisting of 20% f.g.-m.g.garnets
(0.2-0.5cm in diameter) in f.g.-m.g. biotite rich
matrix. The unit contains 1% pale green amph. The
unit is cut by 2% Qtz veins up to 1cm wide. No
visible mineralisation.
Comments
The lower contact is
sharp @ 70dca.
The unit is cut by <1%
Qtz veins up to 0.8cm
wide. The lower contact
is sharp @ 80dca.
No visible
mineralisation. The
lower contact is sharp
@ 70dca.
The lower contact is
sharp @ 80dca.
ALTERATION
Bio
W
W
W
S
W
W
Car Chl Gru Hem Ser Si
W
M
Comments
2t
LITHOLOGY LOG Page 5 of 19
Unit
2
4F
2
4F
Unit
09-NSD-001
Assay
Sample
E513521
E513522
E513523
E513524
E513525
E513526
E513527
E513528
E513529
E513531
E513532
E513533
E513534
E513535
E513536
E513537
AU ppm
0.05
0.39
0.02
0.00
0.00
0.01
0.02
0.02
0.01
0.01
0.01
0.02
0.67
0.16
0.29
0.37
MAJOR UNIT
From
1585.40
1592.20
1597.30
1603.90
1608.00
To
1592.20
1597.30
1603.90
1608.00
1621.80
From
1585.40
1586.40
1586.80
1587.20
1588.20
1601.90
1602.90
1603.90
1604.50
1605.00
1606.00
1607.00
1608.00
1609.00
1619.80
1620.80
To
1586.40
1586.80
1587.20
1588.20
1589.20
1602.90
1603.90
1604.50
1605.00
1606.00
1607.00
1608.00
1609.00
1610.00
1620.80
1621.80
MINOR UNIT
From To CommentsComments
Fine grained well foliated green mafic volcanic. The
unit contains 50% light-medium green amph and
45% plagioclase. The unit displays up to 5% biotite.
The lower contact is gradational.
Massive weakly foliated locally, light brown. The unit
is fine grained and displays Qtz-feldspar and very
f.g. biotite (?). The unit contains 3% Qtz sweats up
to 0.3cm in diameter. There is a minor mafic volcanic
unit from 1594.7-1595.3m.
Fine grained weakly foliated mafic volcanic. The unit
contains 70% green amph and 30% plagioclases.
Nil-weak biotite alt'n throughout. The unit is broken
from 1600.8-1602.3m
Well developed bio-schist 4F. The unit consists of
f.g.-m.g.biotite studded by 30% f.g.garnets. The unit
contains minor sericite. The unit contains 5%
c.g.garnets throughout. 3% Qtz veins throughout.
Pervasive weak-mod bio alt'n.
Fine grained well foliated mafic volcanic. The unit
consists of 50% medium green amph, 40%
plagioclase and 10% f.g.biotite. No significant
veining. No visible mineralisation.
Comments
No significant veining
except at the lower
contact (Qtz veined).
The lower contact is
Qtz veined.
Po occurs locally in
short veins along
foliation planes, up to
1%. The lower contact
is sharp @ 90dca.
The lower contact is
truncated by Qtz vein
3cm wide.
ALTERATION
Bio
W
W
W
W
Car Chl Gru Hem Ser
W
Si
W
W
W
Comments
LITHOLOGY LOG Page 6 of 19
Unit
2
6
2
4F
2
Unit
09-NSD-001
Assay
Sample
E513538
E513539
E513541
E513542
E513543
E513544
E513545
E513546
E513547
E513548
E513549
E513551
E513552
E513553
E513554
E513555
E513556
E513557
E513558
E513559
E513561
E513562
E513563
E513564
E513565
E513566
E513567
AU ppm
2.28
0.03
0.01
0.01
0.02
0.01
0.06
0.19
0.66
3.39
0.06
0.08
0.13
0.38
0.05
0.01
0.00
0.00
0.01
0.03
0.01
0.02
0.01
0.01
0.02
0.03
0.03
MAJOR UNIT
From
1621.80
1640.80
To
1640.80
1662.70
From
1621.80
1622.20
1623.00
1624.00
1625.00
1625.60
1626.20
1626.70
1627.70
1628.70
1629.40
1630.00
1631.00
1632.00
1632.60
1633.00
1634.00
1635.00
1636.00
1637.00
1638.00
1639.00
1640.00
1640.80
1641.80
1660.70
1661.70
To
1622.20
1623.00
1624.00
1625.00
1625.60
1626.20
1626.70
1627.70
1628.70
1629.40
1630.00
1631.00
1632.00
1632.60
1633.00
1634.00
1635.00
1636.00
1637.00
1638.00
1639.00
1640.00
1640.80
1641.80
1642.80
1661.70
1662.70
MINOR UNIT
From To CommentsComments
Well developed 4F. Varies from bio-schist with 30%
f.g.garnets to porphyroblastic 4f with c.g.garnets up
to 1.5cm in diameter. The unit contains 10-15%
f.g.staurolite in the porphyroblastic parts. The unit
contains weak-mod c.g.biotite alt'n
Well foliated fairly fresh mafic volcanic. The unit is
f.g.-m.g.. Consisting of 70% grey amph and 30%
plagioclase.
Comments
overprinting the
original matrix. The
unit is cut by several
small Bvol dykes (?) up
to 40cm wide. Po
occurs locally in short
veins up to 3%. The
lower contact is sharp
@ 90dca.
ALTERATION
Bio
M
Car Chl Gru Hem Ser Si
W
Comments
LITHOLOGY LOG Page 7 of 19
Unit
4F
2
Unit
09-NSD-001
Assay
Sample
E513568
E513569
E513571
E513572
E513573
E513574
E513575
E513576
E513577
E513578
E513579
E513581
E513582
E513583
E513584
E513585
E513586
E513587
E513588
E513589
E513591
AU ppm
0.02
0.02
0.03
0.01
0.96
0.03
0.02
0.01
0.00
0.05
0.02
0.12
0.02
0.16
0.01
0.01
0.01
0.01
0.01
0.02
0.01
MAJOR UNIT
From
1662.70
1666.70
1668.70
1677.00
To
1666.70
1668.70
1677.00
1687.30
From
1662.70
1663.50
1664.00
1665.00
1666.00
1666.70
1667.70
1675.00
1676.00
1677.00
1677.60
1678.40
1679.00
1680.00
1681.00
1682.00
1683.00
1684.00
1684.40
1685.00
1686.00
To
1663.50
1664.00
1665.00
1666.00
1666.70
1667.70
1668.70
1676.00
1677.00
1677.60
1678.40
1679.00
1680.00
1681.00
1682.00
1683.00
1684.00
1684.40
1685.00
1686.00
1686.60
MINOR UNIT
From To CommentsComments
Porphyroblastic 4F, well developed bio-schist. The
unit consists of a f.g.biotite rich matrix studded by
15% m.g.-c.g.garnets (up to 2cm in diameter) and
25-30% f.g.staurolite. Weak c.g.biotite alt'n
overprinting the original matrix.
Fine grained well foliated mafic volcanic. The unit
consists of 50% green amph and 50% plagioclase.
The lower part of the unit is borderline UM with
possible amorphous serpentine on surface planes. A
minor 4F unit is present in the last 15cm.
Well foliated fine grained intermediate. The unit
displays 50% Qtz-feldspar, 25% biotite and 15%
brown/green amph. The unit contains 10%
f.g.sericite. No significant veining. Traces Po and
minor scattered Po.
Well developed 4F bio-schist. The unit consists of
30% f.g.-m.g. garnets in a f.g.biotite rich matrix.
Weak bio alt'n overprinting the original matrix. Minor
intermediate unit from 1677.2-1677.4m.
Comments
No significant veining.
The lower contact is
sharp @90dca.
The lower contact is
gradational.
The lower contact is
truncated by a Po rich
vein 3cm wide (80dca).
A minor Qtz flooded 4E
is present @ 1678.4m
over 15cm. The unit
contains 3% green
amph rich bands
throughout. The lower
contact is sharp @
90dca.
ALTERATION
Bio
W
W
W
Car Chl Gru Hem Ser
M
Si
W
W
W
Comments
mafic
intermediate
4F bio-schist
LITHOLOGY LOG Page 8 of 19
Unit
4F
2
3A
4F
Unit
09-NSD-001
Assay
Sample
E513592
E513593
E513594
E513595
E513596
E513597
E513598
E513599
E513601
E513602
E513603
E513604
E513605
E513606
E513607
E513608
E513609
E513611
E513612
E513613
AU ppm
0.39
0.03
0.02
0.03
0.01
0.01
0.01
3.80
0.28
0.01
0.03
0.01
0.01
0.01
0.01
0.00
0.01
0.01
0.01
0.01
MAJOR UNIT
From
1687.30
1690.40
1694.70
1699.40
1701.00
To
1690.40
1694.70
1699.40
1701.00
1702.30
From
1686.60
1687.30
1688.30
1689.30
1689.80
1690.40
1691.00
1692.00
1693.00
1694.00
1694.70
1695.70
1696.50
1697.00
1698.00
1698.70
1699.40
1700.00
1701.00
1701.70
To
1687.30
1688.30
1689.30
1689.80
1690.40
1691.00
1692.00
1693.00
1694.00
1694.70
1695.70
1696.50
1697.00
1698.00
1698.70
1699.40
1700.00
1701.00
1701.70
1702.30
MINOR UNIT
From To CommentsComments
Fine grained well foliated mafic volcanic. Consisting
of equigranular 50% green amph and 50%
plagioclase. Nil-weak biotite alt'n throughout. The
unit is cut by 3% Qtz veins up to 3cm wide.
Well developed 4F meta-pelite. The unit varies from
4F with biotite studded by 25-30% f.g.-m.g.garnets to
4F with staurolite and garnets porphyroblasts.
Well foliated fine grained mafic volcanic. The unit
contains 70% green amph, 20% plagioclase and 10%
short biotite slips. The lower contact is sharp @ 90dca.
Fairly similar to previous 4F unit. The unit consists
of 30% f.g.-m.g.garnets (from 0.2-1cm in diameter) in
a f.g.biotite rich matrix. Weak c.g.biotite alt'n
throughout. The unit contains 1%
hornblende-grunerite rich bands with minor Po in
short veins.
2/2T. The unit is well foliated and displays up to
10-12% biotite locally, 70% green amph and 20%
interstitial plagioclases. No significant veining. The
lower contact is sharp @ 90dca.
Comments
The lower contact is
sharp@80dca.
No sginificant alt'n.
The lower contact is
sharp @ 90dca.
The lower contact is
gradational.
ALTERATION
Bio
W
W
W
M
Car Chl Gru Hem Ser Si Comments
mafic volcanic
fresh mafic
2/2T
LITHOLOGY LOG Page 9 of 19
Unit
2
4F
2
4F
2
Unit
09-NSD-001
Assay
Sample
E513614
E513615
E513616
E513617
E513618
E513619
E513621
E513622
E513623
E513624
E513625
E531126
AU ppm
0.02
8.30
38.30
0.05
0.09
7.73
0.04
0.01
0.03
0.02
11.85
2.83
MAJOR UNIT
From
1702.30
1704.50
1706.00
1706.60
1723.50
To
1704.50
1706.00
1706.60
1723.50
1724.80
From
1702.30
1703.30
1703.80
1704.50
1705.00
1706.00
1706.60
1707.60
1721.50
1722.50
1723.50
1724.20
To
1703.30
1703.80
1704.50
1705.00
1706.00
1706.60
1707.60
1708.60
1722.50
1723.50
1724.20
1724.80
MINOR UNIT
From To CommentsComments
Well developed 4E/4EA. The unit consists of 55%
green amph and 45% grunerite. the unit contains 20%
f.g.-c.g.garnets. Weak biotite alt'n locally. The unit
is sheared and Qtz flooded from 1703.3-1703.8m (Po
in traces).
Fairly fresh mafic volcanic. The unit is fine grained
and consists of equigranular amph and plagioclases.
No significant veining. The lower contact is sharp @
90dca.
Sheared Qtz flooded 4E. The unit is a garnet poor 4E
(removed by shearing?) and consists mainly of f.g.
hornblende. Pervasisve mod chlorite alt'n. The unit
contains 3% Qtz flooding.
Well foliated fine grained mafic volcanic. The unit
consists of 80% green amph and 20% plagioclase.
The unit is cut by 3% Qtz veins up to 5cm wide.
Nil-weak biotite alt'n.
Sheared and Qtz flooded garnet poor 4E from
1723.5-1724.2m. The unit displays dark green amph
rich bands averaging 0.5cm wide. Weak pale green
amph alt'n. Po occurs in veins up to 30%.
Comments
In the last 20cm, the
grunerite content
decreases, no garnets
anymore, and 10% Po
in short veins.The
lower contact is sharp
@ 50dca.
Mod pale green amph
alt'n. The unit
contains 8-10% Po
stringers. The lower
contact is sharp @
90dca.
The lower contact is
sharp @ 70dca.
From 1724.2-1728.8,
the unit is less sheared
and contains typical 4E
bands consisting of
green amph and
streched garnets (with
25% grunerite). No Po
in this part. The lower
contact is sharp @
80dca.
ALTERATION
Bio
W
W
W
Car Chl
W
M
Gru
M
Hem Ser Si
M
W
S
Comments
sheared qtz flooded 4E
altered 4E, no garnets.
farily fresh mafic volcanic
qtz flooded 4E
LITHOLOGY LOG Page 10 of 19
Unit
4E
2
4E
2
4E
Unit
09-NSD-001
Assay
Sample
E531127
E531128
E531129
E531131
E531132
E531133
E531134
E531135
E531136
E531137
E531138
E531139
E531141
E531142
AU ppm
0.02
3.32
0.02
0.01
6.70
0.01
0.02
0.02
0.01
10.95
6.02
0.11
0.00
0.01
MAJOR UNIT
From
1724.80
1750.30
1754.00
1771.60
1774.10
To
1750.30
1754.00
1771.60
1774.10
1775.50
From
1724.80
1725.80
1757.00
1758.00
1759.00
1759.50
1760.50
1769.60
1770.60
1771.60
1772.20
1773.20
1774.10
1774.80
To
1725.80
1726.80
1758.00
1759.00
1759.50
1760.50
1761.50
1770.60
1771.60
1772.20
1773.20
1774.10
1774.80
1775.50
MINOR UNIT
From To CommentsComments
Well foliated fine grained mafic volcanic with nil-weak
biotite alt'n. The unit conists of 65% green amph and
35% plagioclase. Bio alt'n occurs only around Qtz
veins. Locally, the unit is coarser grained.
Massive to weakly foliated ultramafic. The matrix
seems to be mainly composed of light green
serpentine and lesser talc No significant veining.
Well foliated fine grained mafic volcanic. The unit
consists of 50-70% green amph and 50-30%
plagioclase. Biotite content varies from 0-10%. From
1759-1759.5m, there is a minor garnet poor 4E with
minor Po.
Sheared and Qtz flooded 4E. The unit contains 30%
dark green amph rich bands averaging 0.8cm wide
with 3% f.g-m.g.garnets. Weak chlorite alt'n
throughout around garnets.
Fine grained well foliated mafic volcanic. Consists
of 60% green amph and 40% plagioclase. Nil-weak
biotite throughout.No significant veining.The lower
contact is sharp @65dca.
Comments
From 1747.7-1748.1m,
the unit contains 1%
garnets and seems to
be sheared (not
magnetic). The lower
contact is gradational.
The lower part of the
section is borderline
mafic.
The lower contact is
sharp @ 75dca.
The unit contains 5-8%
grunerite. Po occurs in
veins throughout, 10%
overall. Weak-mod pale
green amph alt'n.
ALTERATION
Bio
W
W
W
W
Car Chl
M
Gru Hem Ser Si
W
S
Comments
UM?
mafic volcanic
sheared qtz flooded 4E
LITHOLOGY LOG Page 11 of 19
Unit
2
1
2
4E
2
Unit
09-NSD-001
Assay
Sample
E531143
E531144
E531145
E531146
E531147
E531148
E531149
E531151
E531152
E531153
E531154
E531155
E531156
E531157
AU ppm
0.01
0.07
0.02
0.34
7.24
2.15
0.80
0.10
0.01
0.03
0.03
0.08
0.09
0.11
MAJOR UNIT
From
1775.50
1780.60
1796.60
1799.20
To
1780.60
1796.60
1799.20
1801.00
From
1775.50
1776.20
1777.00
1778.00
1778.50
1779.30
1780.00
1780.60
1781.60
1796.60
1797.60
1798.60
1799.20
1800.20
To
1776.20
1777.00
1778.00
1778.50
1779.30
1780.00
1780.60
1781.60
1782.60
1797.60
1798.60
1799.20
1800.20
1801.00
MINOR UNIT
From To CommentsComments
Strongly sheared and Qtz flooded 4E. The unit
displays 30% typical 4E bands consisting of green
amph rich matrix with 5% f.g.-m.g.garnets, 40% dark
green amph with no garnets, 15% grunerite-gar,
15% Qtz flooding.
Weakly biotitic mafic volcanic. The unit contains
equigranular medium-dark green amph and
plagioclase. Biotite content up to 5%. The unit is cut
by 1% Qtz veins up to 5cm wide.
Weakly to mod foliated unit, white and hard. The
matrix is fine grained and seems to be composed of
Qtz/feldspars and 30% sericite. Rare biotite. No
significant veining. A minor 4E ocurs from
1798.6-1799.2m.
Well foliated mafic volcanic. No significant alt'n, the
unit is mainly composed green amph and
plagioclase.No significant veining.
Comments
Po throughout,
increases from
1779.3-1780.6m (in
veins or fractures
filling within the
garnets, up to 20%).
Weak biotite alt'n
locally. The lower
contact is sharp @
90dca.
The lower contact is
gradational.
The lower contact is
sharp @ 65dca.
ALTERATION
Bio
W
W
W
Car Chl Gru Hem Ser
S
Si
M
Comments
sheared altered 4E
LITHOLOGY LOG Page 12 of 19
Unit
4E
2
3F
2
Unit
09-NSD-001
Assay
Sample
E531158
E531159
E531161
E531162
E531163
E531164
E531165
E531166
E531167
E531168
E531169
AU ppm
2.95
13.55
0.07
0.19
0.07
0.18
0.02
0.01
0.23
0.01
0.03
MAJOR UNIT
From
1801.00
1804.70
1806.70
1825.20
To
1804.70
1806.70
1825.20
1826.80
From
1801.00
1801.70
1802.20
1803.00
1804.00
1804.70
1805.70
1824.10
1824.60
1825.20
1826.00
To
1801.70
1802.20
1803.00
1804.00
1804.70
1805.70
1806.70
1824.60
1825.20
1826.00
1826.80
MINOR UNIT
From To CommentsComments
Well developed 4E, locally sheared and Qtz
flooded.The unit consists of 60% dark green amph
rih bansd p o wide with no garnets, 30%
grunerite-gar rich bands and 10% green amph-gar
rich bands (distorted bands).
Weakly foliated homogeneous sediment. The unit
contains Qtz-feldspar and 30% f.g.biotite. The unit
displays 1% Qtz sweats up to 0.5cm in diameter. No
significant veining. The lower contact is gradational.
Biotitic mafic volcanic, locally sheared. The unit
consists of 50% brown-[green] amph and 20%
plagioclase. The unit displays 30% bio slips. The
unit contains 1% garnets (from shearing) throughout.
Hetergenous 4F with 60% fine grained biotite. 15%
green amphibole and 10% quartz/fd bands
associated quartz. with minor staurolite. ~5% Minor
Py and Po near qtz veins and green amphibole at
1826 - 1826.8m.
Comments
The unit is sheared
from 1801-1802.2m
and contains 10% Po in
short veins. Po is
rmming the garnets in
the lower part of the
section <1%). Mod pale
green amph alt'n. The
lower contact is sharp
@ 80dca.
The unit is cut by
broken and distorted
Qtz veins 2-3%. Down
section there is an
increase in coarse laths
of biotite (.5 to .7 cm
long, needle like) and
green amphibole
alteration. A small
section between
1826.4-1826.8 where
there is a small 4E
present.
Garnets are between
0.3 to 0.6 cm in
diameter and sub
rounded and have a
pale /dull red
appearence.
ALTERATION
Bio
W
W
S
M
M
Car
W
Chl Gru Hem Ser Si
W
W
W
W
Comments
6
2T
LITHOLOGY LOG Page 13 of 19
Unit
4E
6
2T
4F
Unit
09-NSD-001
Assay
Sample
E531171
E531172
E531173
E531174
E531175
E531176
E531177
E531178
E531179
E531181
E531182
E531183
E531184
E531185
E531186
E531187
E531188
E531189
E531191
E531192
AU ppm
3.44
3.46
1.04
2.09
1.83
0.59
0.24
0.82
1.28
0.38
0.28
7.29
0.38
0.38
0.17
0.02
0.01
0.01
0.01
0.01
MAJOR UNIT
From
1826.80
1837.50
1840.30
To
1837.50
1840.30
1844.50
From
1826.80
1827.80
1828.80
1829.30
1830.00
1831.00
1831.60
1832.30
1833.00
1833.50
1834.50
1835.50
1836.50
1837.50
1838.50
1839.50
1840.00
1840.30
1841.00
1841.50
To
1827.80
1828.80
1829.30
1830.00
1831.00
1831.60
1832.30
1833.00
1833.50
1834.50
1835.50
1836.50
1837.50
1838.50
1839.50
1840.00
1840.30
1841.00
1841.50
1842.50
MINOR UNIT
From
1831.50
To
1831.60
Comments
Mafic Dyke within the 4ea not
common in the PQ-Deeps ???
Comments
Moderate to Well developed 4EA with a banded
planar fabric. It consists of garnets that are .5 to
.7 cm wide the remaining 50% consists of med grey
magnetic chert bands1-3 cm wide. The U.C is mod
sheared with for 70cm however no visible
mineralization.
Clastic 4B, Banded and weakly folded; composed of
grey Mt-chert with ragged looking grey-green
amph-gar bands. becomes thinly laminated Clastic
4B with depth. Minor shear zone between
1840-1840.30.
Thinly laminated Clastic 4B. with strong green
amphibole alteration. Chert bands vary between 0.2
to 1 cm wide however the Magnetite bands are
1-5mm of alternating thinly laminated grey-green
amph-gar layers.
Comments
Intensely sheared from
1832.3-1833.5 with
strong qtz flooding and
amph alt'n. 3% Po
between 1834 to 1837.
There is a small 10cm
mafic dike at 1831.5m.
These are rarely
observed in the
PQ-Deeps, common in
the T-Aniform). 6 m
core barrel started at
1834
Amph bands are typical
very f.g. green amph
with ~10-20% m.g.
ragged garnets.
ALTERATION
Bio
S
M
S
M
Car Chl Gru
M
Hem Ser Si
S
M
M
S
Comments
LITHOLOGY LOG Page 14 of 19
Unit
4EA
4B
4B
Unit
2K
09-NSD-001
Assay
Sample
E531193
E531194
E531195
E531196
E531197
E531198
E531199
E531201
E531202
E531203
E531204
E531205
E531206
E531207
E531208
E531209
E531211
E531212
E531213
E531214
E531215
AU ppm
0.10
0.06
0.01
0.03
0.49
0.26
0.06
1.02
0.47
1.81
0.25
0.06
0.17
0.04
0.04
0.01
0.01
0.01
0.06
0.28
0.07
MAJOR UNIT
From
1844.50
1856.00
1876.80
1878.00
To
1856.00
1876.80
1878.00
1879.00
From
1842.50
1843.50
1844.50
1845.50
1846.50
1847.50
1848.50
1849.50
1850.50
1851.50
1852.50
1853.50
1854.50
1855.00
1856.00
1857.00
1875.00
1876.00
1876.80
1877.40
1878.00
To
1843.50
1844.50
1845.50
1846.50
1847.50
1848.50
1849.50
1850.50
1851.50
1852.50
1853.50
1854.50
1855.00
1856.00
1857.00
1858.00
1876.00
1876.80
1877.40
1878.00
1879.00
MINOR UNIT
From To CommentsComments
Thickly banded Heterogeneous 4B with bands
between 2-4 cm wide with minor biotite-garnet
alteration. The unit is more ragged looking with
boudinaged chert bands
Moderatly sheared 2t. The U.C is strongly bleached
and there is weak to moderate calcite veining
present. Biotite varies from fine grained to prominent
biotite laths along with clusters of biotite slips 3-7mm
wide.
Intercalated 60% 4H/ 30% 4A/ 2T 10%. The U.C has
10-15% Po for the first 30 cm and then an
intercalated section of 2T, 30 cm wide and back into
10 -15% Po with green -yellow grun alt and quartz
calcite vein.
4A with alternating bands of chert and grunerite. The
chert bands are 13-5cm wide and mask thinly
laminated wispy grunerite layers with biotite and
minor amphibole alteration. Again there is strong
quartz-calcite veining that masks the the protolith.
Comments
Minor quartz-calcite
vein between
1851.70-1852.0 with
strong pale green amph
alteration. The lower 3
metres has 3% Po and
trace Aspy.
Srtong
Po-calcite-quartz
veining with 5%Po.
ALTERATION
Bio
M
S
S
M
Car
M
Chl Gru
M
S
Hem Ser Si
W
M
S
Comments
LITHOLOGY LOG Page 15 of 19
Unit
4B
2T
4H
4A
Unit
09-NSD-001
Assay
Sample
E531216
E531217
E531218
E531219
E531221
E531222
E531223
E531224
E531225
AU ppm
0.07
0.02
0.08
0.12
0.05
0.01
0.00
0.00
0.01
MAJOR UNIT
From
1879.00
1881.90
1907.90
1911.90
1915.90
1921.10
To
1881.90
1907.90
1911.90
1915.90
1921.10
1928.90
From
1879.00
1879.60
1880.60
1881.20
1881.90
1882.90
1883.90
1927.00
1928.00
To
1879.60
1880.60
1881.20
1881.90
1882.90
1883.90
1885.00
1928.00
1928.90
MINOR UNIT
From To CommentsComments
The unit is thinly laminated and strongly distorted
and ragged looking with15% green amphibole wisps.
3% light green /yellow grunerite. The unit is
moderately Qtz Veined; 3-5 cm wide and 5 per
metre. Qtz Vns host 5% Po.
Fine to medium grained. Patches where the unit has
strong green amph alteration bordering on a 1M;
these sections are light green with tabular pyroxenes
within the matrix.
Serpentinised Ultramafic. Amorporus looking matrix
which is light green in colur Massive to 1910 -
1911.9m; wisps of seperntine /talc are present,
2-3mm in length.
Biotitc mafic volcanic with minor biotite slips with
minor Cc veining.
A medium to coarse grained Ultramafic. The first part
appears to be chilled with a coarse grained core from
1971-1973.8 then again a chill margin with strong
calcite Veining.
Biotitic mafic volcanic, weakly sheared. Fgr brown Bt
as 1-2 cm lenses/bands; talc and minor chert bands;
light-green transparent serpentine on fractures.
Comments
Interesting brx zone
along the U.C. The
magnetite is banded
increasing in width
down section to 2-4 cm
wide & up to 30%. 40
% of the unit consists
of boudinaged chert
bands 1-2 cm wide,
often fractured with
wispy green amphibole
and grunerite.
Thers is a descrease in
biotite down section
grading in to biotitic
mafic volcanic with an
incresae in Cc veining.
The matrix is weakly
porphyroblastic with
soft talc? grains 2mm
length throughout.
Cc veins have been
deformed. No
mineralization. Sharp
L.C. at 70 dca.
ALTERATION
Bio
W
M
W
W
Car
M
Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 16 of 19
Unit
4B
2T
1
2
1
2T
Unit
09-NSD-001
Assay
Sample
E531226
E531227
E531228
E531229
E531231
E531232
E531233
E531234
E531235
E531236
E531237
E531238
E531239
E531241
AU ppm
0.03
0.04
0.03
0.01
0.04
0.08
0.20
0.07
0.01
0.02
0.02
0.08
0.05
0.08
MAJOR UNIT
From
1928.90
1934.30
1939.50
To
1934.30
1939.50
1947.60
From
1928.90
1929.20
1930.10
1931.00
1932.00
1933.00
1933.90
1934.30
1935.00
1936.00
1937.00
1938.00
1939.00
1939.50
To
1929.20
1930.10
1931.00
1932.00
1933.00
1933.90
1934.30
1935.00
1936.00
1937.00
1938.00
1939.00
1939.50
1940.50
MINOR UNIT
From To CommentsComments
The U.C. is typical SIF "zebra rock" 4B with15% fgr
yellow-green grun (in the 0.1-0.2cm chert layers in
upper 30cm with 50% black Mt (0.2-1.5cm layers),
35% chert (0.1-0.7cm layers).
Intensely folded section of thickly laminated SIF
with 40% chert bands 2-4 cm wide and 60%
magnetite bands. from 1935 - 1936 there is a well
developed S2 foliation @ 65 d.c.a.
Typical lamainted 4B similar to above;
weakly-moderately distorted from 1943- 1943.4.
~35-40% Mt (black fgr, 1-8mm bands), ~30%
thinly-laminated chert bands (2-15mm). Minor,
~10-15% light-green Cgr Amph and~10-15% Grunerite
Comments
The unit is strongly
sheared and quartz
flooded and is ragged
looking with 3% Po
between 1929.2 -
1930. Both chert and Mt
layers become thickly
laminated. The L.C is
intensely brecciated
with 20% Po .
Minor slivers of
sheared amphibole and
light-green cgr amph,
~30% grunerite, ~20%
magnetite (brown,
hematite alt'n). All
folded, dispays
crenulated cleveage
along the edges chert
bands. Z folds are 4 -
5 cm wide and can be
traced from 1937.5-1938
Light-green Cgr amph
(rimmed by Mt),
grunerite (alt'n)
laminations become
thicker down section
from alternating mm
scale to .5 to 1 cm
scale from 1943.4m.
ALTERATION
Bio Car Chl Gru Hem Ser Si Comments
LITHOLOGY LOG Page 17 of 19
Unit
4B
4B
4B
Unit
09-NSD-001
Assay
Sample
E531242
E531243
E531244
E531245
E531246
E531247
E513451
E513452
E513453
E513454
E513455
E513456
E513457
E513458
E513459
E513461
E513462
E513463
E513464
E513465
E513466
E513467
E513468
E513469
E513471
AU ppm
0.10
0.01
0.02
0.04
0.02
0.02
0.00
0.00
0.00
0.00
0.00
0.00
0.00
0.21
0.09
0.75
0.03
0.01
0.02
0.85
0.51
1.80
0.47
0.86
0.36
MAJOR UNIT
From
1947.60
1950.70
1958.80
1960.20
To
1950.70
1958.80
1960.20
1969.30
From
1940.50
1941.60
1942.40
1943.00
1943.40
1944.00
1945.00
1946.00
1947.00
1947.60
1948.60
1956.80
1957.80
1958.80
1959.70
1960.20
1961.00
1962.00
1963.00
1964.00
1965.00
1966.00
1967.00
1968.00
1968.70
To
1941.60
1942.40
1943.00
1943.40
1944.00
1945.00
1946.00
1947.00
1947.60
1948.60
1949.60
1957.80
1958.80
1959.70
1960.20
1961.00
1962.00
1963.00
1964.00
1965.00
1966.00
1967.00
1968.00
1968.70
1969.30
MINOR UNIT
From To CommentsComments
Serpentinized fine grained weakly foliated ultramafic.
The unit consists of f.g.micaceous serpentine and
lesser talc. Featureless. No significant veining.
Fairly fresh, fine-grained mafic volcanic. The unit
consists of 60% grey-green amph and 40%
plagioclase. The unit is cut by 2% Qtz-cc veins up to
0.8cm wide.
Well laminated 4B, zebra rock, SIF type. The unit
consists of alternating dark grey Mt rich laminae and
chert laminae. The unit contains 20% grunerite rich
bands (4A type).
Well developed 4A, grunerite iron formation. The
unit displays 65% grunerite rich bands averaging
0.5cm wide and 35% chert bands up to 0.5cm wide.
Weak pale green amph content.
Comments
The lower contact is
gradational.
No visible
mineralisation. The
lower contact is
gradational.
No significant veining
or mineralisation.
Po occurs in traces and
scattered throughout
the unit. The lower
contact is irregular
(90dca).
ALTERATION
Bio
W
Car Chl Gru Hem Ser Si
W
Comments
UM with serpentine
fresh @
LITHOLOGY LOG Page 18 of 19
Unit
1
2
4B
4A
Unit
09-NSD-001
Assay
Sample
E513472
E513473
E513474
AU ppm
0.13
0.01
0.01
MAJOR UNIT
From
1969.30
1969.70
To
1969.70
1978.00
From
1969.30
1969.70
1970.70
To
1969.70
1970.70
1971.70
MINOR UNIT
From To CommentsComments
Po-rich mudstone. The unit contains black argillite
bands with 3% clasts of Qtz up to 3cm in diameter.
Po occurs in stringers or blebs up to 40% overall.
The lower contact is sharp @ 90dca.
Well foliated fine grained mafic volcanic with nil-weak
biotite alt'n. The unit contains equigranular green
amph-plagioclase (55/45). Locally, the unit displays
biotite slips (up to 2% overall). The unit is cut by <1%
veining.
Comments
EOH=1978m
ALTERATION
Bio
W
Car Chl Gru Hem Ser Si Comments
H
weak bio locally
LITHOLOGY LOG Page 19 of 19
Unit
4H
2
Unit
Assay Certificate Sample# Hole Number From To Assay (g/t) Analysis Date Sample Date TB07105231 E376461 07-NSD-008 9 10 0.009 19-Sep-07 06-Sep-07 TB07105231 E376462 07-NSD-008 10 11 0.006 19-Sep-07 06-Sep-07 TB07105231 E376463 07-NSD-008 11 11.3 0.005 19-Sep-07 06-Sep-07 TB07105231 E376464 07-NSD-008 11.3 12 0.007 19-Sep-07 06-Sep-07 TB07105231 E376465 07-NSD-008 12 13 0.005 19-Sep-07 06-Sep-07 TB07105231 E376466 07-NSD-008 46 47 0.01 19-Sep-07 06-Sep-07 TB07105231 E376467 07-NSD-008 47 48 0.019 19-Sep-07 06-Sep-07 TB07105231 E376468 07-NSD-008 48 48.5 0.017 19-Sep-07 06-Sep-07 TB07105231 E376469 07-NSD-008 48.5 49.2 0.011 19-Sep-07 06-Sep-07 TB07105231 E376471 07-NSD-008 49.2 so 0.02 19-Sep-07 06-Sep-07 TB07105231 E376472 07-NSD-008 so 51 0.011 19-Sep-07 06-Sep-07 TB07105231 E376473 07-NSD-008 51 52 0.008 19-Sep-07 06-Sep-07 TB07105231 E466001 07-NSD-008 55.9 56.9 0.024 19-Sep-07 06-Sep-07 TB07105231 E466002 07-NSD-008 56.9 57.9 0.019 19-Sep-07 06-Sep-07 TB07105231 E466003 07-NSD-008 57.9 58.3 0.064 19-Sep-07 06-Sep-07 TB07105231 E466004 07-NSD-008 58.3 59 0.689 19-Sep-07 06-Sep-07 TB07105231 E466005 07-NSD-008 59 59.6 0.075 19-Sep-07 06-Sep-07 TB07105231 E466006 07-NSD-008 59.6 60.6 0.022 19-Sep-07 06-Sep-07 TB07105231 E466007 07-NSD-008 60.6 61.6 0.026 19-Sep-07 06-Sep-07 TB07105231 E466008 07-NSD-008 341.3 342.3 0.007 19-Sep-07 12-Sep-07 TB07105231 E466009 07-NSD-008 342.3 343.3 0.01 19-Sep-07 12-Sep-07 TB07105231 E466011 07-NSD-008 343.3 344 0.011 19-Sep-07 12-Sep-07 TB07105231 E466012 07-NSD-008 344 345 0.014 19-Sep-07 12-Sep-07 TB07105231 E466013 07-NSD-008 345 345.7 0.023 19-Sep-07 12-Sep-07 TB07105231 E466014 07-NSD-008 345.7 346.7 0.009 19-Sep-07 12-Sep-07 TB07105231 E466015 07-NSD-008 346.7 347.7 0.078 19-Sep-07 12-Sep-07 TB07105231 E466016 07-NSD-008 347.7 348.5 0.014 19-Sep-07 12-Sep-07 TB07105231 E466017 07-NSD-008 348.5 349 0.013 19-Sep-07 12-Sep-07 TB07105231 E466018 07-NSD-008 349 349.9 0.089 19-Sep-07 12-Sep-07 TB07105231 E466019 07-NSD-008 349.9 350.9 0.008 19-Sep-07 13-Sep-07 TB07105231 E466021 07-NSD-008 350.9 351.9 0.005 19-Sep-07 13-Sep-07 TB07119021 E466022 07-NSD-008 823 824 0.342 07-0ct-15 04-0ct-07 TB07119021 E466023 07-NSD-008 824 825 0.291 07-0ct-15 04-0ct-07 TB07119021 E466024 07-NSD-008 994.2 995.2 0.014 07-0ct-15 04-0ct-07 TB07119021 E466025 07-NSD-008 995.2 996 0.05 07-0ct-15 04-0ct-07 TB07119021 E466026 07-NSD-008 996 997 0.008 07-0ct-15 04-0ct-07 TB07119021 E466027 07-1\JSD-008 997 998 0.021 07-0ct-15 04-0ct-07 TB07119021 E466028 07-1\JSD-008 998 999 0.073 07-0ct-15 04-0ct-07 TB07119021 E466029 07-1\JSD-008 999 999.6 0.737 07-0ct-15 04-0ct-07 TB07119021 E466031 07-1\JSD-008 999.6 1000.7 0.037 07-0ct-15 04-0ct-07 TB07119021 E466032 07-1\JSD-008 1001.4 1002.4 0.581 07-0ct-15 04-0ct-07 TB07119021 E466033 07-I\JSD-008 1002.4 1003.2 0.146 07-0ct-15 04-0ct-07 TB07119021 E466034 07-1\JSD-008 1003.2 1004 0.027 07-0ct-15 04-0ct-07 TB07119021 E466035 07-1\JSD-008 1004 1004.7 0.037 07-0ct-15 04-0ct-07 TB07119021 E466036 07-1\JSD-008 1004.7 1005.S 0.041 07-0ct-15 04-0ct-07 TB07119021 E466037 07-NSD-008 1005.5 1006.3 0.026 07-0ct-15 04-0ct-07 TB07119021 E466038 07-NSD-008 1006.3 1006.9 0.031 07-0ct-15 04-0ct-07 TB07119021 E466039 07-NSD-008 1006.9 1008 0.028 07-0ct-15 04-0ct-07 TB07119021 E466041 07-NSD-008 1008 1009 0.01 07-0ct-15 04-0ct-07
TB07119021 E466042 07-NSD-008 1009 1009.9 0.025 07-0ct-15 04-0ct-07 TB07119021 E466043 07-NSD-008 1009.9 1010.3 0.116 07-0ct-15 04-0ct-07 TB07119021 E466044 07-NSD-008 1010.3 1011 0.04 07-0ct-15 04-0ct-07 TB07119021 E466045 07-NSD-008 1011 1012 0.022 07-0ct-15 04-0ct-07 TB07119021 E466046 07-NSD-008 1012 1013 0.047 07-0ct-15 04-0ct-07 TB07119021 E466047 07-NSD-008 1013 1014 0.052 07-0ct-15 04-0ct-07 TB07119021 E466048 07-NSD-008 1014 1015.4 0.127 07-0ct-15 04-0ct-07 TB07119021 E466049 07-NSD-008 1015.4 1016.4 0.07 07-0ct-15 04-0ct-07 TB07119021 E466051 07-NSD-008 1016.4 1017 0.331 07-0ct-15 04-0ct-07 TB07119021 E466052 07-NSD-008 1017 1018 0.179 07-0ct-15 04-0ct-07 TB07119021 E466053 07-NSD-008 1018 1018.6 0.127 07-0ct-15 04-0ct-07 TB07119021 E466054 07-NSD-008 1018.6 1019 1.335 07-0ct-15 04-0ct-07 TB07119021 E466055 07-NSD-008 1019 1020 0.63 07-0ct-15 04-0ct-07 TB07119021 E466056 07-NSD-008 1020 1021 12.25 07-0ct-15 04-0ct-07 TB07119021 E466057 07-1\JSD-008 1021 1021.7 0.145 07-0ct-15 04-0ct-07 TB07119021 E466058 07-1\JSD-008 1021.7 1022.5 0.321 07-0ct-15 04-0ct-07 TB07119021 E466059 07-NSD-008 1022.5 1023 0.015 07-0ct-15 04-0ct-07 TB07119021 E466061 07-1\JSD-008 1023 1024 0.015 07-0ct-15 04-0ct-07 TB07119021 E466062 07-1\JSD-008 1025.2 1026.2 0.0025 07-0ct-15 04-0ct-07 TB07119021 E466063 07-1\JSD-008 1026.2 1027.2 0.191 07-0ct-15 04-0ct-07 TB07119021 E466064 07-NSD-008 1027.2 1028 0.062 07-0ct-15 04-0ct-07 TB07119021 E466065 07-NSD-008 1028 1029 0.177 07-0ct-15 04-0ct-07 TB07119021 E466066 07-NSD-008 1029 1030 0.272 07-0ct-15 04-0ct-07 TB07119021 E466067 07-NSD-008 1030 1030.7 0.031 07-0ct-15 04-0ct-07 TB07119021 E466068 07-NSD-008 1030.7 1031.7 0.024 07-0ct-15 04-0ct-07 TB07119021 E466069 07-NSD-008 1042.5 1043.5 0.029 07-0ct-15 04-0ct-07 TB07119021 E466071 07-NSD-008 1043.5 1044.5 0.117 07-0ct-15 06-0ct-07 TB07119021 E466072 07-NSD-008 1044.5 1045.5 0.495 07-0ct-15 06-0ct-07 TB07119021 E466073 07-NSD-008 1045.5 1046.7 0.135 07-0ct-15 06-0ct-07 TB07119021 E466074 07-NSD-008 1046.7 1047.7 0.03 07-0ct-15 06-0ct-07 TB07119021 E466075 07-NSD-008 1050.5 1051.3 0.016 07-0ct-15 06-0ct-07 TB07119021 E466076 07-NSD-008 1051.3 1052 0.253 07-0ct-15 06-0ct-07 TB07119021 E466077 07-NSD-008 1052 1053 0.114 07-0ct-15 06-0ct-07 TB07119021 E466078 07-NSD-008 1053 1054 0.013 07-0ct-15 06-0ct-07 TB07119021 E466079 07-NSD-008 1054 1055 0.03 07-0ct-15 06-0ct-07 TB07119021 E466081 07-NSD-008 1055 1056 0.02 07-0ct-15 06-0ct-07 TB07119021 E466082 07-NSD-008 1056 1057 0.023 07-0ct-15 06-0ct-07 TB07119021 E466083 07-NSD-008 1057 1058 0.012 07-0ct-15 06-0ct-07 TB07119021 E466084 07-NSD-008 1058 1059 0.014 07-0ct-15 06-0ct-07 TB07119021 E466085 07-NSD-008 1059 1059.8 0.016 07-0ct-15 06-0ct-07 TB07119021 E466086 07-NSD-008 1059.8 1060.8 0.328 07-0ct-15 06-0ct-07 TB07119021 E466087 07-NSD-008 1060.8 1061.5 0.016 07-0ct-15 06-0ct-07 TB07119021 E466088 07-NSD-008 1061.5 1062.3 0.016 07-0ct-15 06-0ct-07 TB07119021 E466089 07-NSD-008 1062.3 1063 0.012 07-0ct-15 06-0ct-07 TB07119021 E466091 07-NSD-008 1063 1064 0.019 07-0ct-15 06-0ct-07 TB07119021 E466092 07-NSD-008 1064 1064.7 0.027 07-0ct-15 06-0ct-07 TB07119021 E466093 07-NSD-008 1064.7 1065.2 0.168 07-0ct-15 06-0ct-07 TB07119021 E466094 07-NSD-008 1065.2 1066 0.028 07-0ct-15 06-0ct-07 TB07119021 E466095 07-NSD-008 1066 1066.7 1.195 07-0ct-15 06-0ct-07 TB07119021 E466096 07-NSD-008 1066.7 1067.3 2.77 07-0ct-15 06-0ct-07
TB07119021 E466097 07-NSD-008 1067.3 1068 0.05 07-0ct-15 06-0ct-07 TB07119021 E466098 07-NSD-008 1068 1069 0.139 07-0ct-15 06-0ct-07 TB07119021 E466099 07-NSD-008 1069 1070 0.123 07-0ct-15 06-0ct-07 TB07119021 E466101 07-NSD-008 1070 1071 0.819 07-0ct-15 06-0ct-07 TB07119021 E466102 07-NSD-008 1071 1072 1.645 07-0ct-15 06-0ct-07 TB07119021 E466103 07-NSD-008 1072 1073 0.035 07-0ct-15 06-0ct-07 TB07119021 E466104 07-NSD-008 1073 1074 0.05 07-0ct-15 06-0ct-07 TB07119021 E466105 07-NSD-008 1074 1075 0.036 07-0ct-15 06-0ct-07 TB07119021 E466106 07-NSD-008 1075 1076 0.029 07-0ct-15 06-0ct-07 TB07119021 E466107 07-NSD-008 1076 1077.1 0.264 07-0ct-15 06-0ct-07 TB07119021 E466108 07-NSD-008 1077.1 1077.8 5.68 07-0ct-15 06-0ct-07 TB07119021 E466109 07-NSD-008 1077.8 1078.8 0.07 07-0ct-15 06-0ct-07 TB07119021 E466111 07-NSD-008 1078.8 1079.3 0.096 07-0ct-15 06-0ct-07 TB07119021 E466112 07-NSD-008 1079.3 1080 0.421 07-0ct-15 06-0ct-07 TB07119021 E466113 07-NSD-008 1080 1081 0.018 07-0ct-15 06-0ct-07 TB07119021 E466114 07-NSD-008 1082.3 1083.3 0.033 07-0ct-15 06-0ct-07 TB07119021 E466115 07-NSD-008 1083.3 1084 1.695 07-0ct-15 06-0ct-07 TB07119021 E466116 07-NSD-008 1084 1084.5 0.551 07-0ct-15 06-0ct-07 TB07119021 E466117 07-NSD-008 1084.5 1085.2 5.98 07-0ct-15 06-0ct-07 TB07119021 E466118 07-1\JSD-008 1085.2 1085.8 0.077 07-0ct-15 06-0ct-07 TB07119021 E466119 07-1\JSD-008 1085.8 1086.9 0.162 07-0ct-15 06-0ct-07 TB07119021 E466121 07-1\JSD-008 1086.9 1087.9 0.153 07-0ct-15 07-0ct-07 TB07119021 E466122 07-1\JSD-008 1087.9 1088.9 0.115 07-0ct-15 07-0ct-07 TB07119021 E466123 07-1\JSD-008 1088.9 1090 0.014 07-0ct-15 07-0ct-07 TB07119021 E466124 07-1\JSD-008 1090 1091 0.126 07-0ct-15 07-0ct-07 TB07119021 E466125 07-NSD-008 1091 1092 0.022 07-0ct-15 07-0ct-07 TB07119021 E466126 07-NSD-008 1092 1093 0.02 07-0ct-15 07-0ct-07 TB07119021 E466127 07-NSD-008 1093 1094 0.051 07-0ct-15 07-0ct-07 TB07119021 E466128 07-NSD-008 1094 1094.5 0.01 07-0ct-15 07-0ct-07 TB07119021 E466129 07-NSD-008 1094.5 1095.3 1.35 07-0ct-15 07-0ct-07 TB07119021 E466131 07-NSD-008 1095.3 1095.8 0.589 07-0ct-15 07-0ct-07 TB07119021 E466132 07-NSD-008 1095.8 1096.5 2.35 07-0ct-15 07-0ct-07 TB07119021 E466133 07-NSD-008 1096.5 1097 0.521 07-0ct-15 07-0ct-07 TB07119021 E466134 07-NSD-008 1097 1098 0.042 07-0ct-15 07-0ct-07 TB07119021 E466135 07-NSD-008 1098 1099 0.657 07-0ct-15 07-0ct-07 TB07119021 E466136 07-NSD-008 1099 1099.4 0.035 07-0ct-15 07-0ct-07 TB07119021 E466137 07-NSD-008 1099.4 1100.4 2.32 07-0ct-15 07-0ct-07 TB07119021 E466138 07-NSD-008 1100.4 1100.9 0.031 07-0ct-15 07-0ct-07 TB07119021 E466139 07-NSD-008 1100.9 1101.9 0.084 07-0ct-15 07-0ct-07 TB07119021 E466141 07-NSD-008 1130.2 1131.2 0.006 07-0ct-15 07-0ct-07 TB07119021 E466142 07-NSD-008 1131.2 1131.8 0.055 07-0ct-15 07-0ct-07 TB07119021 E466143 07-NSD-008 1131.8 1132.3 0.007 07-0ct-15 07-0ct-07 TB07119021 E466144 07-NSD-008 1163.3 1164.3 0.012 07-0ct-15 07-0ct-07 TB07119021 E466145 07-NSD-008 1164.3 1165 0.03 07-0ct-15 07-0ct-07 TB07119021 E466146 07-NSD-008 1165 1165.5 0.011 07-0ct-15 07-0ct-07 TB07119021 E466147 07-NSD-008 1165.5 1166.5 0.009 07-0ct-15 07-0ct-07 TB07119021 E466148 07-NSD-008 1166.5 1167.4 0.019 07-0ct-15 07-0ct-07 TB07119021 E466149 07-NSD-008 1167.4 1168 0.103 07-0ct-15 07-0ct-07 TB07119021 E466151 07-NSD-008 1168 1169 0.008 07-0ct-15 07-0ct-07 TB07119021 E466152 07-NSD-008 846 846.8 0.078 07-0ct-15 09-0ct-07
TB07119021 E466153 07-NSD-008 846.8 847.7 0.961 07-0ct-15 09-0ct-07 TB07119021 E466154 07-NSD-008 847.7 848.5 0.094 07-0ct-15 09-0ct-07 TB07119021 E466155 07-NSD-008 1185.6 1186.6 0.009 07-0ct-15 10-0ct-07 TB07119021 E466156 07-NSD-008 1186.6 1187.6 0.147 07-0ct-15 10-0ct-07 TB07119021 E466157 07-NSD-008 1187.6 1188.4 0.024 07-0ct-15 10-0ct-07 TB07119021 E466158 07-NSD-008 1188.4 1189 0.04 07-0ct-15 10-0ct-07 TB07119021 E466159 07-NSD-008 1189 1189.4 1.75 07-0ct-15 10-0ct-07 TB07119021 E466161 07-NSD-008 1189.4 1190.4 0.009 07-0ct-15 10-0ct-07 TB07119021 E466162 07-NSD-008 1190.4 1191.4 0.107 07-0ct-15 10-0ct-07 TB07119021 E466163 07-NSD-008 1191.4 1192.2 0.068 07-0ct-15 10-0ct-07 TB07119021 E466164 07-NSD-008 1192.2 1193 0.074 07-0ct-15 10-0ct-07 TB07119021 E466165 07-NSD-008 1193 1194 0.006 07-0ct-15 10-0ct-07 TB07119021 E466166 07-NSD-008 1194 1195 0.208 07-0ct-15 10-0ct-07 TB07119021 E466167 07-NSD-008 1195 1196.1 0.03 07-0ct-15 10-0ct-07 TB07119021 E466168 07-NSD-008 1196.1 1197 0.006 07-0ct-15 10-0ct-07 TB07119021 E466169 07-NSD-008 1215.4 1216.4 0.007 07-0ct-15 10-0ct-07 TB07119021 E466171 07-NSD-008 1216.4 1217 0.008 07-0ct-15 10-0ct-07 TB07119021 E466172 07-1\ISD-008 1217 1218 0.065 07-0ct-15 10-0ct-07 TB07119021 E466173 07-1\ISD-008 1218 1219 0.01 07-0ct-15 10-0ct-07 TB07119021 E466174 07-1\150-008 1219 1220 0.016 07-0ct-15 10-0ct-07 TB07119021 E466175 07-I\ISD-008 1220 1221 0.01 07-0ct-15 10-0ct-07 TB07119021 E466176 07-NSD-008 1221 1222 0.02 07-0ct-15 10-0ct-07 TB07119021 E466177 07-NSD-008 1222 1223 0.013 07-0ct-15 10-0ct-07 TB07119021 E466178 07-NSD-008 1223 1223.8 0.024 07-0ct-15 10-0ct-07 TB07119021 E466179 07-NSD-008 1223.8 1224.5 0.611 07-0ct-15 10-0ct-07 TB07119021 E466181 07-NSD-008 1224.5 1225 0.888 07-0ct-15 10-0ct-07 TB07119021 E466182 07-NSD-008 1225 1226 0.021 07-0ct-15 10-0ct-07 TB07129303 E466183 07-NSD-008 1357.6 1358.6 0.0025 06-Jan-07 17-0ct-07 TB07129303 E466184 07-NSD-008 1358.6 1359.6 0.007 06-Jan-07 17-0ct-07 TB07129303 E466185 07-NSD-008 1359.6 1360.3 0.012 06-Jan-07 17-0ct-07 TB07129303 E466186 07-NSD-008 1360.3 1361 0.016 06-Jan-07 17-0ct-07 TB07129303 E466187 07-NSD-008 1361 1362 0.007 06-Jan-07 17-0ct-07 TB07129303 E466188 07-NSD-008 1362 1363 0.0025 06-Jan-07 17-0ct-07 TB07129303 E466189 07-NSD-008 1406 1407 0.0025 06-Jan-07 20-0ct-07 TB07129303 E466191 07-NSD-008 1407 1408 0.006 06-Jan-07 20-0ct-07 TB07129303 E466192 07-NSD-008 1408 1409 0.0025 06-Jan-07 20-0ct-07 TB07129303 E466193 07-NSD-008 1409 1409.6 0.0025 06-Jan-07 20-0ct-07 TB07129303 E466194 07-NSD-008 1409.6 1410.7 0.007 06-Jan-07 20-0ct-07 TB07129303 E466195 07-NSD-008 1410.7 1411.4 0.006 06-Jan-07 20-0ct-07 TB07129303 E466196 07-NSD-008 1411.4 1412.3 0.0025 06-Jan-07 20-0ct-07 TB07129303 E466197 07-NSD-008 1412.3 1413 0.0025 06-Jan-07 20-0ct-07 TB07129303 E466198 07-NSD-008 1428 1428.7 0.006 06-Jan-07 20-0ct-07 TB07129303 E466199 07-NSD-008 1428.7 1429.7 0.006 06-Jan-07 20-0ct-07 TB07129303 E466201 07-NSD-008 1429.7 1430.7 0.014 06-Jan-07 20-0ct-07 TB07129303 E466202 07-NSD-008 1430.7 1431.2 0.011 06-Jan-07 20-0ct-07 TB07129303 E466203 07-NSD-008 1431.2 1431.9 0.008 06-Jan-07 20-0ct-07 TB07129303 E466204 07-NSD-008 1431.9 1432.9 0.005 06-Jan-07 20-0ct-07 TB07129303 E466205 07-NSD-008 1432.9 1433.7 0.04 06-Jan-07 20-0ct-07 TB07129303 E466206 07-NSD-008 1433.7 1434.7 0.006 06-Jan-07 20-0ct-07 TB07129303 E466207 07-NSD-008 1450 1451 0.0025 06-Jan-07 20-0ct-07
TB07129303 E466208 07-NSD-008 1451 1452 0.007 06-Jan-07 20-0ct-07 TB07129303 E466209 07-NSD-008 1452 1452.7 0.009 06-Jan-07 20-0ct-07 TB07129303 E466211 07-NSD-008 1452.7 1453.4 0.0025 06-Jan-07 20-0ct-07 TB07129303 E466212 07-NSD-008 1453.4 1454.1 0.006 06-Jan-07 20-0ct-07 TB07129303 E466213 07-NSD-008 1454.1 1455 0.006 06-Jan-07 20-0ct-07 TB07129303 E466214 07-NSD-008 1455 1456 0.007 06-Jan-07 20-0ct-07 TB07129303 E466215 07-NSD-008 1522 1523 0.0025 06-Jan-07 29-0ct-07 TB07129303 E466216 07-NSD-008 1534.5 1535.5 0.005 06-Jan-07 29-0ct-07 TB07129303 E466217 07-NSD-008 1541 1542 0.008 06-Jan-07 29-0ct-07 TB07129303 E466218 07-NSD-008 1547 1548 0.01 06-Jan-07 29-0ct-07 TB07129303 E466219 07-NSD-008 1566 1567 0.008 06-Jan-07 29-0ct-07 TB07129303 E466221 07-NSD-008 1576.5 1577.5 0.0025 06-Jan-07 29-0ct-07 TB08013500 E466222 07-NSD-008 1636 1637 0.012 04-Feb-08 15-Dec-07 TB08013500 E466223 07-NSD-008 1637 1638 0.01 04-Feb-08 15-Dec-07 TB08013500 E466224 07-NSD-008 1638 1639 0.014 04-Feb-08 15-Dec-07 TB08013500 E466225 07-NSD-008 1639 1640 0.01 04-Feb-08 15-Dec-07 TB08013500 E466226 07-NSD-008 1640 1640.6 0.009 04-Feb-08 15-Dec-07 TB08013500 E466227 07-1\ISD-008 1640.6 1641.1 0.008 04-Feb-08 15-Dec-07 TB08013500 E466228 07-1\ISD-008 1641.1 1642 0.021 04-Feb-08 15-Dec-07 TB08013500 E466229 07-1\ISD-008 1642 1643 0.013 04-Feb-08 15-Dec-07 TB08013500 E466231 07-NSD-008 1643 1644 0.023 04-Feb-08 15-Dec-07 TB08013500 E466232 07-1\ISD-008 1665 1665.9 0.02 04-Feb-08 17-Dec-07 TB08013500 E466233 07-NSD-008 1665.9 1666.9 0.009 04-Feb-08 17-Dec-07 TB08013500 E466234 07-NSD-008 1666.9 1667.9 0.008 04-Feb-08 17-Dec-07 TB08013500 E466235 07-NSD-008 1667.9 1668.9 0.007 04-Feb-08 17-Dec-07 TB08013500 E466236 07-NSD-008 1668.9 1669.9 0.009 04-Feb-08 17-Dec-07 TB08013500 E466237 07-NSD-008 1669.9 1670.8 0.013 04-Feb-08 17-Dec-07 TB08013500 E466238 07-NSD-008 1670.8 1671.8 0.007 04-Feb-08 17-Dec-07 TB08013500 E466239 07-NSD-008 1688 1689 0.01 04-Feb-08 19-Dec-07 TB08013500 E466241 07-NSD-008 1689 1689.9 0.02 04-Feb-08 19-Dec-07 TB08013500 E466242 07-NSD-008 1689.9 1690.9 0.014 04-Feb-08 19-Dec-07 TB08013500 E466243 07-NSD-008 1690.9 1691.9 0.014 04-Feb-08 19-Dec-07 TB08013500 E466244 07-NSD-008 1691.9 1692.8 0.016 04-Feb-08 19-Dec-07 TB08013500 E466245 07-NSD-008 1692.8 1693.3 0.013 04-Feb-08 19-Dec-07 TB08013500 E466246 07-NSD-008 1693.3 1694 0.014 04-Feb-08 19-Dec-07 TB08013500 E466247 07-NSD-008 1694 1695 0.021 04-Feb-08 19-Dec-07 TB08013500 E466248 07-NSD-008 1733.5 1734.2 0.009 04-Feb-08 22-Dec-07 TB08013500 E466249 07-NSD-008 1734.2 1734.8 0.011 04-Feb-08 22-Dec-07 TB08013500 E466251 07-NSD-008 1734.8 1735.4 0.015 04-Feb-08 22-Dec-07 TB08013500 E466252 07-NSD-008 1735.4 1736 0.011 04-Feb-08 22-Dec-07 TB08013500 E466253 07-NSD-008 1739 1740 0.012 04-Feb-08 22-Dec-07 TB08013500 E466254 07-NSD-008 1740 1740.4 0.01 04-Feb-08 22-Dec-07 TB08013500 E466255 07-NSD-008 1740.4 1741 0.012 04-Feb-08 22-Dec-07 TB08013500 E466256 07-NSD-008 1743 1744 0.011 04-Feb-08 10-Jan-08 TB08013500 E466257 07-NSD-008 1744 1745 0.038 04-Feb-08 10-Jan-08 TB08013500 E466258 07-NSD-008 1745 1746 0.011 04-Feb-08 10-Jan-08 TB08013500 E466259 07-NSD-008 1746 1747.1 0.012 04-Feb-08 10-Jan-08 TB08013500 E466261 07-NSD-008 1747.1 1748 0.009 04-Feb-08 10-Jan-08 TB08013500 E466262 07-NSD-008 1748 1749 0.011 04-Feb-08 10-Jan-08 TB08013500 E466263 07-NSD-008 1756 1757 0.012 04-Feb-08 10-Jan-08
TB08013500 E466264 07-NSD-008 1757 1757.8 0.022 04-Feb-08 10-Jan-08 TB08013500 E466265 07-NSD-008 1757.8 1758.7 0.023 04-Feb-08 10-Jan-08 TB08013500 E466266 07-NSD-008 1758.7 1759.7 0.103 04-Feb-08 10-Jan-08 TB08013500 E466267 07-NSD-008 1759.7 1760.7 0.014 04-Feb-08 10-Jan-08 TB08013500 E466268 07-NSD-008 1782 1782.9 0.018 04-Feb-08 10-Jan-08 TB08013500 E466269 07-NSD-008 1782.9 1783.8 0.017 04-Feb-08 10-Jan-08 TB08013500 E466271 07-NSD-008 1783.8 1784.8 0.017 04-Feb-08 10-Jan-08 TB08013500 E466272 07-NSD-008 1784.8 1785.8 0.01 04-Feb-08 10-Jan-08 TB08019381 E466273 07-NSD-008 1801 1802 0.007 15-Feb-08 02-Feb-08 TB08019381 E466274 07-NSD-008 1802 1803 0.01 15-Feb-08 02-Feb-08 TB08019381 E466275 07-NSD-008 1803 1804 0.028 15-Feb-08 02-Feb-08 TB08019381 E466276 07-NSD-008 1804 1805 0.029 15-Feb-08 02-Feb-08 TB08019381 E466277 07-NSD-008 1805 1806 0.036 15-Feb-08 02-Feb-08 TB08019381 E466278 07-NSD-008 1806 1807 0.025 15-Feb-08 02-Feb-08 TB08019381 E466279 07-NSD-008 1807 1808 0.009 15-Feb-08 02-Feb-08 TB08019381 E466281 07-NSD-008 1808 1809 0.014 15-Feb-08 02-Feb-08 TB08019381 E466282 07-NSD-008 1809 1810 0.018 15-Feb-08 02-Feb-08 TB08019381 E466283 07-NSD-008 1810 1811 0.039 15-Feb-08 02-Feb-08 TB08019381 E466284 07-NSD-008 1811 1812 0.017 15-Feb-08 02-Feb-08 TB08019381 E466285 07-1\JSD-008 1812 1813 0.013 15-Feb-08 02-Feb-08 TB08019381 E466286 07-NSD-008 1813 1814 0.045 15-Feb-08 02-Feb-08 TB08019381 E466287 07-NSD-008 1814 1815 0.005 15-Feb-08 02-Feb-08 TB08019381 E466288 07-NSD-008 1815 1816 0.142 15-Feb-08 02-Feb-08 TB08019381 E466289 07-NSD-008 1816 1816.5 0.008 15-Feb-08 02-Feb-08 TB08019381 E466291 07-NSD-008 1816.5 1817.5 0.011 15-Feb-08 02-Feb-08 TB08033801 E466292 07-NSD-008 1936.3 1937.4 0.01 19-Mar-08 13-Feb-08 TB08033801 E466293 07-NSD-008 1937.4 1938.4 0.008 19-Mar-08 13-Feb-08 TB08033801 E466294 07-NSD-008 1938.4 1939.4 0.006 19-Mar-08 13-Feb-08 TB08033801 E466295 07-NSD-008 1939.4 1939.8 0.012 19-Mar-08 13-Feb-08 TB08033801 E466296 07-NSD-008 1939.8 1940.7 0.034 19-Mar-08 13-Feb-08 TB08033801 E466297 07-NSD-008 1940.7 1941.3 0.032 19-Mar-08 13-Feb-08 TB08033801 E466298 07-NSD-008 1941.3 1942 0.022 19-Mar-08 13-Feb-08 TB08033801 E466299 07-NSD-008 1942 1943 0.011 19-Mar-08 13-Feb-08 TB08033801 E466301 07-NSD-008 1943 1944 0.095 19-Mar-08 13-Feb-08 TB08033801 E466302 07-NSD-008 1944 1944.6 0.021 19-Mar-08 13-Feb-08 TB08033801 E466303 07-NSD-008 1944.6 1945 0.01 19-Mar-08 13-Feb-08 TB08033801 E466304 07-NSD-008 1945 1945.9 0.058 19-Mar-08 13-Feb-08 TB08033801 E466305 07-NSD-008 1945.9 1946.5 0.024 19-Mar-08 13-Feb-08 TB08033801 E466306 07-NSD-008 1946.5 1947 0.044 19-Mar-08 13-Feb-08 TB08033801 E466307 07-NSD-008 1947 1947.6 0.048 19-Mar-08 13-Feb-08 TB08033801 E466308 07-NSD-008 1947.6 1948.2 0.015 19-Mar-08 13-Feb-08 TB08033801 E466309 07-NSD-008 1948.2 1949 0.01 19-Mar-08 13-Feb-08 TB08033801 E466311 07-NSD-008 1949 1949.7 0.009 19-Mar-08 13-Feb-08 TB08033801 E466312 07-NSD-008 1949.7 1950.3 0.005 19-Mar-08 13-Feb-08 TB08033801 E466313 07-NSD-008 1950.3 1950.8 0.07 19-Mar-08 13-Feb-08 TB08033801 E466314 07-NSD-008 1950.8 1951.4 0.006 19-Mar-08 13-Feb-08 TB08033801 E466315 07-NSD-008 1958.6 1959.6 0.009 19-Mar-08 25-Feb-08 TB08033801 E466316 07-NSD-008 1959.6 1960.4 0.094 19-Mar-08 25-Feb-08 TB08033801 E466317 07-NSD-008 1960.4 1960.8 0.071 19-Mar-08 25-Feb-08 TB08033801 E466318 07-NSD-008 1960.8 1961.7 0.029 19-Mar-08 25-Feb-08
TB08033801 E466319 07-NSD-008 1961.7 1962.3 0.043 19-Mar-08 25-Feb-08 TB08033801 E466321 07-NSD-008 1962.3 1963 0.005 19-Mar-08 25-Feb-08 TB08033801 E466322 07-NSD-008 1963 1964 0.007 19-Mar-08 25-Feb-08 TB08033801 E466323 07-NSD-008 1964 1965 0.007 19-Mar-08 25-Feb-08 TB08033801 E466324 07-NSD-008 1965 1966 0.008 19-Mar-08 25-Feb-08 TB08033801 E466325 07-NSD-008 1966 1967 0.028 19-Mar-08 25-Feb-08 TB08033801 E466326 07-NSD-008 1967 1968 0.063 19-Mar-08 25-Feb-08 TB08033801 E466327 07-NSD-008 1968 1969 0.049 19-Mar-08 25-Feb-08 TB08033801 E466328 07-NSD-008 1969 1970 0.014 19-Mar-08 25-Feb-08 TB08033801 E466329 07-NSD-008 1970 1971 0.036 19-Mar-08 25-Feb-08 TB08033801 E466331 07-NSD-008 1971 1972 0.036 19-Mar-08 25-Feb-08 TB08033801 E466332 07-NSD-008 1972 1973 0.053 19-Mar-08 25-Feb-08 TB08033801 E466333 07-NSD-008 1973 1973.5 0.023 19-Mar-08 25-Feb-08 TB08033801 E466334 07-NSD-008 1973.5 1974.5 0.102 19-Mar-08 25-Feb-08 TB08033801 E466335 07-NSD-008 1974.5 1975.5 0.089 19-Mar-08 25-Feb-08 TB08033801 E466336 07-NSD-008 1975.5 1976.5 0.006 19-Mar-08 25-Feb-08 TB08033801 E466337 07-NSD-008 2008.2 2009.2 0.0025 19-Mar-08 26-Feb-08 TB08033801 E466338 07-NSD-008 2009.2 2010 0.017 19-Mar-08 26-Feb-08 TB08033801 E466339 07-NSD-008 2010 2011.1 0.01 19-Mar-08 26-Feb-08 TB08033801 E466341 07-NSD-008 2011.1 2011.7 0.012 19-Mar-08 26-Feb-08 TB08033801 E466342 07-NSD-008 2011.7 2012.4 0.014 19-Mar-08 26-Feb-08 TB08033801 E466343 07-NSD-008 2012.4 2013.2 0.016 19-Mar-08 26-Feb-08 TB08033801 E466344 07-NSD-008 2013.2 2013.7 0.014 19-Mar-08 26-Feb-08 TB08033801 E466345 07-NSD-008 2013.7 2014.5 0.006 19-Mar-08 26-Feb-08 TB08033801 E466346 07-NSD-008 2014.5 2015 0.0025 19-Mar-08 26-Feb-08 TB08033801 E466347 07-NSD-008 2021.5 2022.5 0.0025 19-Mar-08 26-Feb-08 TB08033801 E466348 07-NSD-008 2022.5 2022.9 0.057 19-Mar-08 26-Feb-08 TB08033801 E466349 07-NSD-008 2022.9 2024 0.161 19-Mar-08 26-Feb-08 TB08033801 E466351 07-NSD-008 2024 2024.6 0.089 19-Mar-08 26-Feb-08 TB08033801 E466352 07-NSD-008 2024.6 2025 0.071 19-Mar-08 26-Feb-08 TB08033801 E466353 07-NSD-008 2025 2025.4 0.0025 19-Mar-08 26-Feb-08 TB08033801 E466354 07-NSD-008 2025.4 2026 0.02 19-Mar-08 26-Feb-08 TB08033801 E466355 07-NSD-008 2026 2027 0.0025 19-Mar-08 26-Feb-08 TB08033801 E466356 07-NSD-008 2027 2027.6 0.0025 19-Mar-08 26-Feb-08 TB08033801 E466357 07-NSD-008 2027.6 2028 0.007 19-Mar-08 26-Feb-08 TB08045641 E466358 07-NSD-008 2028 2028.8 0.0025 14-Apr-08 26-Feb-08 TB08045641 E466359 07-NSD-008 2028.8 2029.5 0.005 14-Apr-08 26-Feb-08 TB08045641 E466361 07-NSD-008 2029.5 2030 0.008 14-Apr-08 26-Feb-08 TB08045641 E466362 07-NSD-008 2030 2031 0.04 14-Apr-08 26-Feb-08 TB08045641 E466363 07-NSD-008 2031 2031.6 0.02 14-Apr-08 26-Feb-08 TB08045641 E466364 07-NSD-008 2031.6 2032.4 0.075 14-Apr-08 26-Feb-08 TB08045641 E466365 07-NSD-008 2032.4 2033.4 0.838 14-Apr-08 11-Mar-08 TB08045641 E466366 07-NSD-008 2033.4 2034 0.019 14-Apr-08 11-Mar-08 TB08045641 E466367 07-NSD-008 2034 2035 0.042 14-Apr-08 11-Mar-08 TB08045641 E466368 07-1\JSD-008 2035 2036 0.247 14-Apr-08 11-Mar-08 TB08045641 E466369 07-1\JSD-008 2036 2037 0.007 14-Apr-08 11-Mar-08 TB08045641 E466371 07-1\JSD-008 2037 2038 0.01 14-Apr-08 11-Mar-08 TB08045641 E466372 07-1\JSD-008 2038 2039 0.088 14-Apr-08 11-Mar-08 TB08045641 E466373 07-1\JSD-008 2039 2040 0.113 14-Apr-08 11-Mar-08 TB08045641 E466374 07-NSD-008 2040 2041 0.037 14-Apr-08 11-Mar-08
TB08045641 E466375 07-NSD-008 2041 2042 0.048 14-Apr-08 11-Mar-08 TB08045641 E466376 07-NSD-008 2042 2043 0.033 14-Apr-08 11-Mar-08 TB08045641 E466377 07-NSD-008 2043 2044 0.0025 14-Apr-08 11-Mar-08 TB08045641 E466378 07-NSD-008 2044 2044.6 0.019 14-Apr-08 11-Mar-08 TB08045641 E466379 07-NSD-008 2044.6 2045.6 0.005 14-Apr-08 11-Mar-08 TB08045641 E466381 07-NSD-008 2045.6 2046.6 0.01 14-Apr-08 11-Mar-08 TB08045641 E466382 07-NSD-008 2059 2060 0.007 14-Apr-08 11-Mar-08 TB08045641 E466383 07-NSD-008 2060 2061 0.005 14-Apr-08 11-Mar-08 TB08045641 E466384 07-NSD-008 2061 2062 0.006 14-Apr-08 11-Mar-08 TB08045641 E466385 07-1\JSD-008 2062 2063 0.0025 14-Apr-08 11-Mar-08 TB08045641 E466386 07-1\JSD-008 2146 2147 0.0025 14-Apr-08 11-Mar-08 TB08045641 E466387 07-1\JSD-008 2147 2148 0.0025 14-Apr-08 11-Mar-08 TB08045641 E466388 07-1\JSD-008 2148 2149 0.0025 14-Apr-08 11-Mar-08 TB08045641 E466389 07-1\JSD-008 2149 2150 0.0025 14-Apr-08 11-Mar-08 TB08045641 E466391 07-1\JSD-008 2150 2151 0.007 14-Apr-08 11-Mar-08 TB08045641 E466392 07-1\JSD-008 2151 2152 0.0025 14-Apr-08 11-Mar-08 TB08045641 E466393 07-1\JSD-008 2152 2153 0.0025 14-Apr-08 11-Mar-08 TB08045641 E466394 07-NSD-008 2153 2154 0.005 14-Apr-08 11-Mar-08 TB08045641 E466395 07-NSD-008 2154 2155 0.0025 14-Apr-08 11-Mar-08 TB08045641 E466396 07-NSD-008 2160.3 2161 0.0025 14-Apr-08 24-Mar-08 TB08045641 E466397 07-NSD-008 2161 2161.7 0.014 14-Apr-08 24-Mar-08 TB08045641 E466398 07-NSD-008 2161.7 2162.5 0.168 14-Apr-08 24-Mar-08 TB08045641 E466399 07-NSD-008 2166.1 2167.1 0.052 14-Apr-08 24-Mar-08 TB08045641 E466401 07-NSD-008 2167.1 2168 1.62 14-Apr-08 24-Mar-08 TB08045641 E466402 07-NSD-008 2168 2168.9 0.319 14-Apr-08 24-Mar-08 TB08045641 E466403 07-NSD-008 2168.9 2169.4 0.139 14-Apr-08 24-Mar-08 TB08045641 E466404 07-NSD-008 2169.4 2169.7 8.47 14-Apr-08 24-Mar-08 TB08045641 E466405 07-NSD-008 2169.7 2170.5 0.521 14-Apr-08 24-Mar-08 TB08045641 E466406 07-NSD-008 2170.5 2171.1 0.325 14-Apr-08 24-Mar-08 TB08045641 E466407 07-NSD-008 2171.1 2172 0.055 14-Apr-08 24-Mar-08 TB08045641 E466408 07-NSD-008 2172 2172.6 0.009 14-Apr-08 24-Mar-08 TB08045641 E466409 07-NSD-008 2173.4 2174 0.287 14-Apr-08 24-Mar-08 TB08045641 E466411 07-NSD-008 2174 2174.7 0.18 14-Apr-08 24-Mar-08 TB08045641 E466412 07-NSD-008 2174.9 2175.5 0.322 14-Apr-08 24-Mar-08 TB08045641 E466413 07-NSD-008 2175.5 2176.1 0.693 14-Apr-08 24-Mar-08 TB08045641 E466414 07-NSD-008 2176.1 2177 0.75 14-Apr-08 24-Mar-08 TB08045641 E466415 07-NSD-008 2177 2177.9 0.362 14-Apr-08 24-Mar-08 TB08045641 E466416 07-NSD-008 2177.9 2178.3 0.136 14-Apr-08 24-Mar-08 TB08045641 E466417 07-NSD-008 2178.3 2179.3 0.022 14-Apr-08 24-Mar-08 TB08045641 E466418 07-NSD-008 2185.4 2186.4 0.0025 14-Apr-08 24-Mar-08 TB08045641 E466419 07-NSD-008 2186.4 2187.4 0.0025 14-Apr-08 24-Mar-08 TB08045641 E466421 07-NSD-008 2187.4 2188 0.006 14-Apr-08 24-Mar-08 TB08045641 E466422 07-NSD-008 2188 2189 0.0025 14-Apr-08 24-Mar-08 TB08045641 E466423 07-NSD-008 2189 2190 0.0025 14-Apr-08 24-Mar-08 TB08045641 E466424 07-NSD-008 2190 2190.6 0.006 14-Apr-08 24-Mar-08 TB08045641 E466425 07-NSD-008 2190.6 2191.6 0.0025 14-Apr-08 24-Mar-08 TB08045641 E466426 07-NSD-008 2191.6 2192.6 0.0025 14-Apr-08 24-Mar-08 TB08045641 E466427 07-NSD-008 2192.6 2193.8 0.0025 14-Apr-08 24-Mar-08 TB08045641 E466428 07-NSD-008 2193.8 2194.9 0.0025 14-Apr-08 24-Mar-08 TB08045641 E466429 07-NSD-008 2194.9 2195.4 0.0025 14-Apr-08 24-Mar-08
TB08045641 E466431 07-NSD-008 2195.4 2196.4 0.005 14-Apr-08 24-Mar-08
TB08045641 E466432 07-NSD-008 2196.4 2197.4 0.0025 14-Apr-08 24-Mar-08
TB08045641 E466433 07-NSD-008 2197.4 2198.2 0.0025 14-Apr-08 24-Mar-08
TB08045641 E466434 07-NSD-008 2198.2 2199 0.038 14-Apr-08 24-Mar-08
TB08045641 E466435 07-NSD-008 2199 2200 0.081 14-Apr-08 24-Mar-08
TB08045641 E466436 07-NSD-008 2200 2200.7 0.008 14-Apr-08 24-Mar-08
TB08045641 E466437 07-NSD-008 2200.7 2201 0.074 14-Apr-08 24-Mar-08
TB08045641 E466438 07-NSD-008 2201 2202 0.0025 14-Apr-08 24-Mar-08
Assay Certificate Sample# Hole Number From To Assay {g/t} Analysis Date Sample Date TB08052738 E466439 08-NSD-001 1403 1404.5 0.014 28-Apr-08 06-Apr-08 TB08052738 E466441 08-NSD-001 1404.5 1405.3 0.013 28-Apr-08 06-Apr-08 TB08052738 E466442 08-NSD-001 1405.3 1406 0.007 28-Apr-08 06-Apr-08 TB08052738 E466443 08-NSD-001 1411.9 1413 0.005 28-Apr-08 06-Apr-08 TB08052738 E466444 08-NSD-001 1413 1413.7 0.01 28-Apr-08 06-Apr-08 TB08052738 E466445 08-NSD-001 1413.7 1414.4 0.01 28-Apr-08 06-Apr-08 TB08052738 E466446 08-NSD-001 1414.4 1415 0.008 28-Apr-08 06-Apr-08 TB08052738 E466447 08-NSD-001 1415 1415.7 0.006 28-Apr-08 06-Apr-08 TB08052738 E466448 08-NSD-001 1422 1423 0.005 28-Apr-08 06-Apr-08 TB08052738 E466449 08-NSD-001 1423 1424 0.02 28-Apr-08 06-Apr-08 TB08052738 E466451 08-NSD-001 1424 1425 0.013 28-Apr-08 06-Apr-08 TB08052738 E466452 08-NSD-001 1425 1425.5 0.0025 28-Apr-08 06-Apr-08 TB08052738 E466453 08-NSD-001 1425.5 1426.5 0.008 28-Apr-08 06-Apr-08 TB08052738 E466454 08-NSD-001 1436 1437 0.008 28-Apr-08 06-Apr-08 TB08052738 E466455 08-NSD-001 1437 1437.6 0.005 28-Apr-08 06-Apr-08 TB08052738 E466456 08-NSD-001 1437.6 1438.2 0.016 28-Apr-08 06-Apr-08 TB08052738 E466457 08-NSD-001 1438.2 1439 0.0025 28-Apr-08 06-Apr-08 TB08052738 E466458 08-NSD-001 1439 1440 0.006 28-Apr-08 06-Apr-08 TB08052738 E466459 08-NSD-001 1440 1441 0.007 28-Apr-08 06-Apr-08 TB08052738 E466461 08-NSD-001 1441 1442 0.0025 28-Apr-08 06-Apr-08 TB08052738 E466462 08-NSD-001 1448 1448.7 0.006 28-Apr-08 06-Apr-08 TB08052738 E466463 08-NSD-001 1448.7 1449.5 0.0025 28-Apr-08 06-Apr-08 TB08052738 E466464 08-NSD-001 1449.5 1450 0.005 28-Apr-08 06-Apr-08 TB08052738 E466465 08-NSD-001 1450 1450.8 0.009 28-Apr-08 06-Apr-08 TB08052738 E466466 08-NSD-001 1450.8 1451.6 0.007 28-Apr-08 06-Apr-08 TB08052738 E466467 08-NSD-001 1451.6 1452.5 0.0025 28-Apr-08 06-Apr-08 TB08052738 E466468 08-NSD-001 1452.5 1453.5 0.005 28-Apr-08 06-Apr-08 TB08052738 E466469 08-NSD-001 1453.5 1454.5 0.007 28-Apr-08 06-Apr-08 TB08052738 E466471 08-NSD-001 1594 1594.9 0.019 28-Apr-08 13-Apr-08 TB08052738 E466472 08-NSD-001 1594.9 1595.8 0.012 28-Apr-08 13-Apr-08 TB08052738 E466473 08-NSD-001 1595.8 1596.5 0.02 28-Apr-08 13-Apr-08 TB08052738 E466474 08-NSD-001 1596.45 1597.4 0.017 28-Apr-08 13-Apr-08 TB08052738 E466475 08-NSD-001 1599.1 1600.1 0.0025 28-Apr-08 13-Apr-08 TB08052738 E466476 08-NSD-001 1600.1 1601 0.01 28-Apr-08 13-Apr-08 TB08052738 E466477 08-NSD-001 1601 1601.9 0.028 28-Apr-08 13-Apr-08 TB08052738 E466478 08-NSD-001 1601.9 1602.3 0.008 28-Apr-08 13-Apr-08 TB08052738 E466479 08-NSD-001 1602.3 1603.3 0.03 28-Apr-08 13-Apr-08 TB08052738 E466481 08-NSD-001 1603.3 1604.3 0.006 28-Apr-08 13-Apr-08 TB08052738 E466482 08-NSD-001 1605.9 1606.9 0.02 28-Apr-08 13-Apr-08 TB08052738 E466483 08-NSD-001 1606.9 1607.3 0.051 28-Apr-08 13-Apr-08 TB08052738 E466484 08-NSD-001 1607.3 1607.8 0.029 28-Apr-08 13-Apr-08 TB08052738 E466485 08-NSD-001 1607.8 1608.8 0.074 28-Apr-08 13-Apr-08 TB08052738 E466486 08-NSD-001 1608.8 1609.5 0.034 28-Apr-08 13-Apr-08 TB08052738 E466487 08-NSD-001 1609.5 1610.1 0.101 28-Apr-08 13-Apr-08 TB08052738 E466488 08-NSD-001 1610.1 1610.4 0.162 28-Apr-08 13-Apr-08 TB08052738 E466489 08-NSD-001 1610.4 1611.4 0.228 28-Apr-08 13-Apr-08 TB08052738 E466491 08-NSD-001 1611.4 1612 0.157 28-Apr-08 13-Apr-08 TB08052738 E466492 08-NSD-001 1612 1612.7 0.041 28-Apr-08 13-Apr-08 TB08052738 E466493 08-NSD-001 1612.7 1613.3 0.062 28-Apr-08 13-Apr-08
TB08052738 E466494 08-NSD-001 1613.3 1613.9 0.034 28-Apr-08 13-Apr-08 TB08052738 E466495 08-NSD-001 1613.9 1614.7 0.013 28-Apr-08 13-Apr-08 TB08052738 E466496 08-NSD-001 1614.7 1615.3 0.0025 28-Apr-08 13-Apr-08 TB08052738 E466497 08-NSD-001 1615.3 1616.4 0.021 28-Apr-08 13-Apr-08 TB08052738 E466498 08-NSD-001 1616.4 1617.4 0.028 28-Apr-08 13-Apr-08 TB08052738 E466499 08-NSD-001 1617.4 1618.4 0.027 28-Apr-08 13-Apr-08 TB08052738 E466501 08-NSD-001 1624.2 1625.2 0.006 28-Apr-08 16-Apr-08 TB08052738 E466502 08-NSD-001 1625.2 1626 0.009 28-Apr-08 16-Apr-08 TB08052738 E466503 08-NSD-001 1626 1626.8 0.005 28-Apr-08 16-Apr-08 TB08052738 E466504 08-NSD-001 1626.8 1627.5 0.0025 28-Apr-08 16-Apr-08 TB08052738 E466505 08-NSD-001 1627.5 1628.3 0.0025 28-Apr-08 16-Apr-08 TB08052738 E466506 08-NSD-001 1628.3 1629.2 0.014 28-Apr-08 16-Apr-08 TB08052738 E466507 08-NSD-001 1629.2 1630 0.01 28-Apr-08 16-Apr-08 TB08052738 E466508 08-NSD-001 1630 1631 0.0025 28-Apr-08 16-Apr-08 TB08052738 E466509 08-NSD-001 1631 1632.1 0.0025 28-Apr-08 16-Apr-08 TB08052738 E466511 08-NSD-001 1632.1 1632.9 0.047 28-Apr-08 16-Apr-08 TB08052738 E466512 08-NSD-001 1632.9 1633.3 0.096 28-Apr-08 16-Apr-08 TB08052738 E466513 08-NSD-001 1633.3 1634 0.078 28-Apr-08 16-Apr-08 TB08052738 E466514 08-NSD-001 1637 1638.1 0.016 28-Apr-08 16-Apr-08 TB08052738 E466515 08-NSD-001 1638.1 1638.6 0.159 28-Apr-08 16-Apr-08 TB08052738 E466516 08-NSD-001 1638.6 1639.1 0.032 28-Apr-08 16-Apr-08 TB08052738 E466517 08-NSD-001 1639.1 1640 0.007 28-Apr-08 16-Apr-08 TB08052738 E466518 08-NSD-001 1640 1641 0.017 28-Apr-08 16-Apr-08 TB08052738 E466519 08-NSD-001 1641 1641.4 0.026 28-Apr-08 16-Apr-08 TB08052738 E466521 08-NSD-001 1641.4 1642.4 0.017 28-Apr-08 16-Apr-08 TB08052738 E466522 08-NSD-001 1642.4 1643.4 0.01 28-Apr-08 16-Apr-08 TB08052738 E466523 08-NSD-001 1643.4 1644.1 0.014 28-Apr-08 16-Apr-08 TB08052738 E466524 08-NSD-001 1644.1 1645 0.014 28-Apr-08 16-Apr-08 TB08052738 E466525 08-NSD-001 1757 1757.7 0.0025 28-Apr-08 18-Apr-08 TB08052738 E466526 08-NSD-001 1757.7 1758.2 0.0025 28-Apr-08 18-Apr-08 TB08052738 E466527 08-NSD-001 1758.2 1758.8 0.0025 28-Apr-08 18-Apr-08 TB08052738 E466528 08-NSD-001 1859 1860 0.0025 28-Apr-08 18-Apr-08 TB08052738 E466529 08-NSD-001 1860 1860.7 0.013 28-Apr-08 18-Apr-08 TB08052738 E466531 08-NSD-001 1860.7 1861.7 0.007 28-Apr-08 18-Apr-08 TB08052738 E466532 08-NSD-001 1864 1865 0.007 28-Apr-08 18-Apr-08 TB08052738 E466533 08-NSD-001 1864.95 1866 0.025 28-Apr-08 18-Apr-08 TB08052738 E466534 08-NSD-001 1865.95 1866.6 0.009 28-Apr-08 18-Apr-08 TB08052738 E466535 08-NSD-001 1866.55 1867.6 0.0025 28-Apr-08 18-Apr-08 TB08052738 E466536 08-NSD-001 1881 1882 0.023 28-Apr-08 18-Apr-08 TB08052738 E466537 08-NSD-001 1882 1883 0.544 28-Apr-08 18-Apr-08 TB08052738 E466538 08-NSD-001 1883 1884 0.285 28-Apr-08 18-Apr-08 TB08052739 E466539 08-NSD-001 1884 1884.4 0.359 28-Apr-08 18-Apr-08 TB08052739 E466541 08-NSD-001 1884.4 1885.4 0.69 28-Apr-08 18-Apr-08 TB08052739 E466542 08-NSD-001 1885.4 1886.3 0.358 28-Apr-08 18-Apr-08 TB08052739 E466543 08-NSD-001 1886.25 1886.7 0.857 28-Apr-08 18-Apr-08 TB08052739 E466544 08-NSD-001 1886.7 1887 0.066 28-Apr-08 18-Apr-08 TB08052739 E466545 08-NSD-001 1887 1888 0.013 28-Apr-08 18-Apr-08 TB08052739 E466546 08-NSD-001 1901 1901.8 0.005 28-Apr-08 19-Apr-08 TB08052739 E466547 08-NSD-001 1901.8 1902.2 0.011 28-Apr-08 19-Apr-08 TB08052739 E466548 08-NSD-001 1902.2 1903 0.005 28-Apr-08 19-Apr-08
TB08052739 E466549 08-NSD-001 1903 1903.4 0.086 28-Apr-08 19-Apr-08 TB08052739 E466551 08-NSD-001 1903.4 1904.4 0.238 28-Apr-08 19-Apr-08 TB08052739 E466552 08-NSD-001 1904.4 1905 0.115 28-Apr-08 19-Apr-08 TB08052739 E466553 08-NSD-001 1905 1905.6 0.167 28-Apr-08 19-Apr-08 TB08052739 E466554 08-NSD-001 1905.6 1906.6 0.046 28-Apr-08 19-Apr-08 TB08052739 E466555 08-NSD-001 1906.6 1907.7 0.046 28-Apr-08 19-Apr-08 TB08052739 E466556 08-NSD-001 1907.7 1908.2 0.044 28-Apr-08 19-Apr-08 TB08052739 E466557 08-NSD-001 1908.2 1909 0.01 28-Apr-08 19-Apr-08 TB08052739 E466558 08-NSD-001 1909 1910 0.008 28-Apr-08 19-Apr-08 TB08052739 E466559 08-NSD-001 1910 1910.7 0.071 28-Apr-08 19-Apr-08 TB08052739 E466561 08-NSD-001 1910.7 1911.2 0.037 28-Apr-08 19-Apr-08 TB08052739 E466562 08-NSD-001 1911.2 1912 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466563 08-NSD-001 1912 1913 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466564 08-NSD-001 1913 1914 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466565 08-NSD-001 1914 1915 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466566 08-NSD-001 1915 1915.9 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466567 08-NSD-001 1915.9 1916.7 0.095 28-Apr-08 19-Apr-08 TB08052739 E466568 08-NSD-001 1916.7 1917.7 0.01 28-Apr-08 19-Apr-08 TB08052739 E466569 08-NSD-001 1917.7 1918.7 0.008 28-Apr-08 19-Apr-08 TB08052739 E466571 08-NSD-001 1918.7 1919.7 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466572 08-NSD-001 1919.7 1920.1 0.005 28-Apr-08 19-Apr-08 TB08052739 E466573 08-NSD-001 1920.1 1921.1 0.008 28-Apr-08 19-Apr-08 TB08052739 E466574 08-NSD-001 1946.5 1947.5 0.01 28-Apr-08 19-Apr-08 TB08052739 E466575 08-NSD-001 1947.5 1948 0.019 28-Apr-08 19-Apr-08 TB08052739 E466576 08-NSD-001 1948 1949 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466577 08-NSD-001 1949 1950 0.07 28-Apr-08 19-Apr-08 TB08052739 E466578 08-NSD-001 1950 1951 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466579 08-NSD-001 1951 1952 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466581 08-NSD-001 1952 1953 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466582 08-NSD-001 1953 1954 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466583 08-NSD-001 1954 1954.9 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466584 08-NSD-001 1954.9 1955.3 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466585 08-NSD-001 1955.3 1955.8 0.058 28-Apr-08 19-Apr-08 TB08052739 E466586 08-NSD-001 1955.8 1956.8 0.006 28-Apr-08 19-Apr-08 TB08052739 E466587 08-NSD-001 1977.8 1978.8 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466588 08-NSD-001 1978.8 1979.3 0.056 28-Apr-08 19-Apr-08 TB08052739 E466589 08-NSD-001 1979.3 1979.8 0.012 28-Apr-08 19-Apr-08 TB08052739 E466591 08-NSD-001 1979.8 1980.8 0.012 28-Apr-08 19-Apr-08 TB08052739 E466592 08-NSD-001 1980.8 1981.8 0.025 28-Apr-08 19-Apr-08 TB08052739 E466593 08-NSD-001 1981.8 1983 0.016 28-Apr-08 19-Apr-08 TB08052739 E466594 08-NSD-001 1983 1983.5 0.007 28-Apr-08 19-Apr-08 TB08052739 E466595 08-NSD-001 1983.5 1984.3 0.449 28-Apr-08 19-Apr-08 TB08052739 E466596 08-NSD-001 1984.3 1985.3 0.039 28-Apr-08 19-Apr-08 TB08052739 E466597 08-NSD-001 1985.3 1986 0.031 28-Apr-08 19-Apr-08 TB08052739 E466598 08-NSD-001 1986 1987 0.031 28-Apr-08 19-Apr-08 TB08052739 E466599 08-NSD-001 1987 1988 0.018 28-Apr-08 19-Apr-08 TB08052739 E466601 08-NSD-001 1988 1989 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466602 08-NSD-001 1989 1989.6 0.046 28-Apr-08 19-Apr-08 TB08052739 E466603 08-NSD-001 1989.6 1990.6 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466604 08-NSD-001 1990.6 1991.1 0.027 28-Apr-08 19-Apr-08
TB08052739 E466605 08-NSD-001 1991.1 1992 0.0025 28-Apr-08 19-Apr-08 TB08052739 E466606 08-NSD-001 1992 1993 0.008 28-Apr-08 19-Apr-08 TB08052739 E466607 08-NSD-001 1993 1994 0.008 28-Apr-08 19-Apr-08 TB08052739 E466608 08-NSD-001 1994 1995 0.007 28-Apr-08 19-Apr-08 TB08052739 E466609 08-NSD-001 1995 1996 0.007 28-Apr-08 19-Apr-08 TB08052739 E466611 08-NSD-001 1996 1997 0.017 28-Apr-08 19-Apr-08 TB08052739 E466612 08-NSD-001 1997 1998 0.006 28-Apr-08 19-Apr-08 TB08052739 E466613 08-NSD-001 1998 1999 0.022 28-Apr-08 19-Apr-08 TB08052739 E466614 08-NSD-001 1999 1999.5 0.025 28-Apr-08 19-Apr-08 TB08052739 E466615 08-NSD-001 1999.5 2000.5 0.005 28-Apr-08 19-Apr-08 TB08052739 E466616 08-NSD-001 1663.3 1664.3 0.01 28-Apr-08 20-Apr-08 TB08052739 E466617 08-NSD-001 1664.3 1664.7 0.047 28-Apr-08 20-Apr-08 TB08052739 E466618 08-NSD-001 1664.7 1665.7 0.015 28-Apr-08 20-Apr-08 TB08068690 E466619 08-NSD-001 2065 2066 0.007 28-May-08 05-May-08 TB08068690 E466621 08-NSD-001 2066 2066.9 0.012 28-May-08 05-May-08 TB08068690 E466622 08-NSD-001 2066.9 2067.8 0.108 28-May-08 05-May-08 TB08068690 E466623 08-NSD-001 2067.8 2068.5 0.067 28-May-08 05-May-08 TB08068690 E466624 08-NSD-001 2068.5 2069 0.049 28-May-08 05-May-08 TB08068690 E466625 08-NSD-001 2069 2070 0.017 28-May-08 05-May-08 TB08068690 E466626 08-NSD-001 2070 2071 0.029 28-May-08 05-May-08 TB08068690 E466627 08-NSD-001 2071 2072 0.126 28-May-08 05-May-08 TB08068690 E466628 08-NSD-001 2072 2073 0.0025 28-May-08 05-May-08 TB08068690 E466629 08-NSD-001 2073 2073.6 0.053 28-May-08 05-May-08 TB08068690 E466631 08-NSD-001 2073.6 2074.2 0.157 28-May-08 05-May-08 TB08068690 E466632 08-NSD-001 2074.2 2075 0.009 28-May-08 05-May-08 TB08068690 E466633 08-NSD-001 2075 2076 0.0025 28-May-08 05-May-08 TB08096495 E466634 08-NSD-001 2112.9 2113.9 0.0025 15-Jul-08 10-Jun-08 TB08096495 E466635 08-NSD-001 2113.9 2114.9 0.005 15-Jul-08 10-Jun-08 TB08096495 E466636 08-NSD-001 2114.9 2115.5 0.021 15-Jul-08 10-Jun-08 TB08096495 E466637 08-NSD-001 2115.5 2116.2 0.018 15-Jul-08 10-Jun-08 TB08096495 E466638 08-NSD-001 2116.2 2116.9 0.005 15-Jul-08 10-Jun-08 TB08096495 E466639 08-NSD-001 2116.9 2117.9 0.007 15-Jul-08 10-Jun-08 TB08096495 E466641 08-NSD-001 2117.9 2119 0.0025 15-Jul-08 10-Jun-08 TB08096495 E466642 08-NSD-001 2119 2119.6 0.0025 15-Jul-08 10-Jun-08 TB08096495 E466643 08-NSD-001 2119.6 2120.7 0.0025 15-Jul-08 11-Jun-08 TB08096495 E466644 08-NSD-001 2120.7 2121.7 0.011 15-Jul-08 11-Jun-08 TB08096495 E466645 08-NSD-001 2121.7 2122.5 0.006 15-Jul-08 11-Jun-08 TB08096495 E466646 08-NSD-001 2122.5 2123.3 0.017 15-Jul-08 11-Jun-08 TB08096495 E466647 08-NSD-001 2123.3 2124 0.0025 15-Jul-08 11-Jun-08 TB08096495 E466648 08-NSD-001 2124 2125 0.009 15-Jul-08 11-Jun-08 TB08096495 E466649 08-NSD-001 2162.4 2163.4 0.0125 20-Apr-10 15-Jun-08 TB08096495 E466651 08-NSD-001 2163.4 2164.4 0.005 15-Jul-08 15-Jun-08 TB08096495 E466652 08-NSD-001 2164.4 2165.2 0.375 15-Jul-08 15-Jun-08 TB08096495 E466653 08-NSD-001 2165.2 2165.9 0.166 15-Jul-08 15-Jun-08 TB08096495 E466654 08-NSD-001 2165.9 2166.9 0.005 15-Jul-08 15-Jun-08 TB08096495 E466655 08-NSD-001 2166.9 2168 0.007 15-Jul-08 15-Jun-08 TB08096495 E466656 08-NSD-001 2168 2169 0.006 15-Jul-08 15-Jun-08 TB08096495 E466657 08-NSD-001 2169 2170 0.0025 15-Jul-08 15-Jun-08 TB08096495 E466658 08-NSD-001 2170 2171 0.024 15-Jul-08 15-Jun-08 TB08096495 E466659 08-NSD-001 2171 2172 0.115 15-Jul-08 15-Jun-08
TB08096495 E466661 08-NSD-001 2172 2173 0.017 15-Jul-08 15-Jun-08 TB08096495 E466662 08-NSD-001 2173 2174 0.009 15-Jul-08 15-Jun-08 TB08096495 E466663 08-NSD-001 2174 2175 0.006 15-Jul-08 15-Jun-08 TB08096495 E466664 08-NSD-001 2175 2176 0.05 15-Jul-08 15-Jun-08 TB08096495 E466665 08-NSD-001 2176 2177 0.032 15-Jul-08 15-Jun-08 TB08096495 E466666 08-NSD-001 2177 2178 0.012 15-Jul-08 15-Jun-08 TB08096495 E466667 08-NSD-001 2178 2179 0.005 15-Jul-08 15-Jun-08 TB08096495 E466668 08-NSD-001 2179 2180 0.007 15-Jul-08 15-Jun-08 TB08096495 E466669 08-NSD-001 2180 2181 0.006 15-Jul-08 15-Jun-08 TB08096495 E466671 08-NSD-001 2181 2182 0.012 15-Jul-08 15-Jun-08 TB08096495 E466672 08-NSD-001 2182 2183 0.047 15-Jul-08 15-Jun-08 TB08096495 E466673 08-NSD-001 2183 2184 0.024 15-Jul-08 22-Jun-08 TB08096495 E466674 08-NSD-001 2184 2184.8 0.039 15-Jul-08 22-Jun-08 TB08096495 E466675 08-NSD-001 2184.8 2185.8 0.019 15-Jul-08 22-Jun-08 TB08096495 E466676 08-NSD-001 2185.8 2186.5 0.014 15-Jul-08 22-Jun-08 TB08096495 E466677 08-NSD-001 2186.5 2187 0.012 15-Jul-08 22-Jun-08 TB08096495 E466678 08-NSD-001 2187 2188 0.0025 15-Jul-08 22-Jun-08 TB08096495 E466679 08-NSD-001 2188 2189 0.0025 15-Jul-08 22-Jun-08 TB08096495 E466681 08-NSD-001 2189 2190 0.007 15-Jul-08 22-Jun-08 TB08096495 E466682 08-NSD-001 2190 2191 0.009 15-Jul-08 22-Jun-08 TB08096495 E466683 08-NSD-001 2191 2192 0.007 15-Jul-08 22-Jun-08 TB08096495 E466684 08-NSD-001 2192 2193 0.027 15-Jul-08 22-Jun-08 TB08096495 E466685 08-NSD-001 2193 2193.7 0.065 15-Jul-08 22-Jun-08 TB08096495 E466686 08-NSD-001 2193.7 2194.2 0.628 15-Jul-08 22-Jun-08 TB08096495 E466687 08-NSD-001 2194.2 2194.8 0.293 15-Jul-08 22-Jun-08 TB08096495 E466688 08-NSD-001 2194.8 2195.4 0.655 15-Jul-08 22-Jun-08 TB08096495 E466689 08-NSD-001 2195.4 2196 0.069 15-Jul-08 22-Jun-08 TB08096495 E466691 08-NSD-001 2196 2197 0.035 15-Jul-08 22-Jun-08 TB08096495 E466692 08-NSD-001 2197 2198 0.881 15-Jul-08 22-Jun-08 TB08096495 E466693 08-NSD-001 2198 2199 0.03 15-Jul-08 22-Jun-08 TB08096496 E466694 08-NSD-001 2199 2200 0.025 15-Jul-08 22-Jun-08 TB08096496 E466695 08-NSD-001 2200 2201 0.029 15-Jul-08 22-Jun-08 TB08096496 E466696 08-NSD-001 2201 2202 0.018 15-Jul-08 22-Jun-08 TB08096496 E466697 08-NSD-001 2202 2202.7 0.031 15-Jul-08 22-Jun-08 TB08096496 E466698 08-NSD-001 2202.7 2203.7 0.093 15-Jul-08 22-Jun-08 TB08096496 E466699 08-NSD-001 2203.7 2204.5 0.024 15-Jul-08 22-Jun-08 TB08096496 E466701 08-NSD-001 2204.5 2205 0.007 15-Jul-08 22-Jun-08 TB08096496 E466702 08-NSD-001 2205 2206 0.019 15-Jul-08 22-Jun-08 TB08096496 E466703 08-NSD-001 2206 2207 0.01 15-Jul-08 22-Jun-08 TB08096496 E466704 08-NSD-001 2207 2208 0.037 15-Jul-08 22-Jun-08 TB08096496 E466705 08-NSD-001 2208 2209 0.0025 15-Jul-08 22-Jun-08 TB08096496 E466706 08-NSD-001 2209 2210 0.09 15-Jul-08 22-Jun-08 TB08096496 E466707 08-NSD-001 2210 2211 0.061 15-Jul-08 22-Jun-08 TB08096496 E466708 08-NSD-001 2211 2212 0.019 15-Jul-08 22-Jun-08 TB08096496 E466709 08-NSD-001 2212 2213 0.008 15-Jul-08 22-Jun-08 TB08096496 E466711 08-NSD-001 2213 2214 0.0025 15-Jul-08 22-Jun-08 TB08096496 E466712 08-NSD-001 2214 2215 0.0025 15-Jul-08 22-Jun-08 TB08096496 E466713 08-NSD-001 2215 2216 0.0025 15-Jul-08 22-Jun-08 TB08096496 E466714 08-NSD-001 2216 2217 0.0025 15-Jul-08 22-Jun-08 TB08096496 E466715 08-NSD-001 2217 2218 0.009 15-Jul-08 22-Jun-08
TB08096496 E466716 08-NSD-001 2218 2218.8 0.304 15-Jul-08 22-Jun-08 TB08096496 E466717 08-NSD-001 2218.8 2219.7 0.082 15-Jul-08 22-Jun-08 TB08096496 E466718 08-NSD-001 2219.7 2220.3 1.115 15-Jul-08 22-Jun-08 TB08096496 E466719 08-NSD-001 2220.3 2221.3 0.018 15-Jul-08 22-Jun-08 TB08096496 E466721 08-NSD-001 2221.3 2222.3 0.011 15-Jul-08 22-Jun-08 TB08096496 E466722 08-NSD-001 2237.5 2238.5 0.208 15-Jul-08 22-Jun-08 TB08096496 E466723 08-NSD-001 2238.5 2239.5 0.198 15-Jul-08 22-Jun-08 TB08096496 E466724 08-NSD-001 2239.5 2240 0.038 15-Jul-08 22-Jun-08 TB08096496 E466725 08-NSD-001 2240 2241 0.0025 15-Jul-08 22-Jun-08 TB08096496 E466726 08-NSD-001 2241 2242 0.011 15-Jul-08 22-Jun-08 TB08096496 E466727 08-NSD-001 2242 2242.7 0.141 15-Jul-08 22-Jun-08 TB08096496 E466728 08-NSD-001 2242.7 2243 0.017 15-Jul-08 22-Jun-08 TB08096496 E466729 08-NSD-001 2243 2244 0.149 15-Jul-08 22-Jun-08 TB08096496 E466731 08-NSD-001 2244 2245 0.019 15-Jul-08 22-Jun-08 TB08096496 E466732 08-NSD-001 2245 2246 0.009 15-Jul-08 22-Jun-08 TB08096496 E466733 08-NSD-001 2246 2246.6 0.011 15-Jul-08 22-Jun-08 TB08096496 E466734 08-NSD-001 2246.6 2247 0.012 15-Jul-08 22-Jun-08 TB08096496 E466735 08-NSD-001 2247 2247.9 0.005 15-Jul-08 22-Jun-08 TB08096496 E466736 08-NSD-001 2247.9 2248.6 0.014 15-Jul-08 22-Jun-08 TB08096496 E466737 08-NSD-001 2248.6 2249.2 0.009 15-Jul-08 22-Jun-08 TB08096496 E466738 08-NSD-001 2249.2 2249.7 0.669 15-Jul-08 22-Jun-08 TB08096496 E466739 08-NSD-001 2249.7 2250.3 0.027 15-Jul-08 22-Jun-08 TB08096496 E466741 08-NSD-001 2250.3 2250.7 0.057 15-Jul-08 22-Jun-08 TB08096496 E466742 08-NSD-001 2250.7 2251.7 0.025 15-Jul-08 22-Jun-08 TB08096496 E466743 08-NSD-001 2251.7 2252.7 0.008 15-Jul-08 22-Jun-08 TB08096496 E466744 08-NSD-001 2266 2267 0.021 15-Jul-08 24-Jun-08 TB08096496 E466745 08-NSD-001 2267 2267.4 0.14 15-Jul-08 24-Jun-08 TB08096496 E466746 08-NSD-001 2267.4 2268.4 0.011 15-Jul-08 24-Jun-08 TB08096496 E466747 08-NSD-001 2309.8 2310.8 0.0025 15-Jul-08 28-Jun-08 TB08096496 E466748 08-NSD-001 2310.8 2311.8 0.0025 15-Jul-08 28-Jun-08 TB08096496 E466749 08-NSD-001 2311.8 2312.8 0.037 15-Jul-08 28-Jun-08 TB08096496 E466751 08-NSD-001 2312.8 2313.6 0.02 15-Jul-08 28-Jun-08 TB08096496 E466752 08-NSD-001 2313.6 2314.6 0.006 15-Jul-08 28-Jun-08 TB08096496 E466753 08-NSD-001 2314.6 2315.6 0.0025 15-Jul-08 09-Jul-08
Assay Certificate Sample# Hole Number From To Assay (g/t) Analysis Date Sample Date TB08119994 E446754 08-NSD-002 1589 1590 0.009 22-Jul-08 TB08119994 E446755 08-NSD-002 1590 1590.7 0.009 22-Jul-08 TB08119994 E446756 08-NSD-002 1590.7 1591.4 0.012 22-Jul-08 TB08119994 E446757 08-NSD-002 1591.4 1592.4 0.011 22-Jul-08 TB08119994 E446758 08-NSD-002 1592.4 1592.9 0.046 22-Jul-08 TB08119994 E446759 08-NSD-002 1592.9 1593.5 0.015 22-Jul-08 TB08119994 E446761 08-NSD-002 1593.5 1594.2 0.005 22-Jul-08 TB08119994 E446762 08-NSD-002 1594.2 1595 0.006 22-Jul-08 TB08119994 E446763 08-NSD-002 1595 1596 0.008 22-Jul-08 TB08119994 E446764 08-NSD-002 1596 1596.4 0.006 22-Jul-08 TB08119994 E446765 08-NSD-002 1596.4 1597.2 0.007 22-Jul-08 TB08119994 E446766 08-NSD-002 1597.2 1597.9 0.005 22-Jul-08 TB08119994 E446767 08-NSD-002 1597.9 1598.9 0.007 22-Jul-08 TB08119994 E466776 08-NSD-002 2223.7 2224.5 0.007 22-Sep-08 12-Sep-08 TB08119994 E466777 08-NSD-002 2224.5 2225.5 0.0025 22-Sep-08 12-Sep-08 TB08119994 E466778 08-NSD-002 2225.S 2226.4 0.008 22-Sep-08 12-Sep-08 TB08119994 E466779 08-NSD-002 2332.1 2333.1 0.0025 22-Sep-08 01-Sep-08 TB08119994 E466781 08-NSD-002 2333.1 2333.9 0.0025 22-Sep-08 01-Sep-08 TB08119994 E466782 08-NSD-002 2333.9 2334.7 0.0025 22-Sep-08 01-Sep-08 TB08119994 E466783 08-NSD-002 2334.7 2335.4 0.0025 22-Sep-08 01-Sep-08 TB08119994 E466784 08-NSD-002 2335.4 2336.1 0.007 22-Sep-08 01-Sep-08 TB08119994 E466785 08-NSD-002 2354.1 2355.1 0.0025 22-Sep-08 01-Sep-08 TB08119994 E466786 08-NSD-002 2355.1 2355.8 0.015 22-Sep-08 01-Sep-08 TB08119994 E466787 08-NSD-002 2355.8 2356.8 0.008 22-Sep-08 01-Sep-08 TB08119994 E466788 08-NSD-002 2356.8 2357.3 0.09 22-Sep-08 01-Sep-08 TB08119994 E466789 08-NSD-002 2357.3 2358 0.045 22-Sep-08 01-Sep-08 TB08119994 E466791 08-NSD-002 2358 2359 0.009 22-Sep-08 Ol-Sep-08 TB08119994 E466792 08-NSD-002 2359 2360 0.006 22-Sep-08 01-Sep-08 TB08119994 E466793 08-NSD-002 2360 2361 0.017 22-Sep-08 01-Sep-08 TB08119994 E466794 08-NSD-002 2361 2362.1 0.007 22-Sep-08 01-Sep-08 TB08119994 E466795 08-NSD-002 2362.1 2363.2 0.027 22-Sep-08 01-Sep-08 TB08119994 E466796 08-NSD-002 2363.2 2363.8 0.152 22-Sep-08 01-Sep-08 TB08119994 E466797 08-NSD-002 2363.8 2364.3 0.329 22-Sep-08 01-Sep-08 TB08119994 E466798 08-NSD-002 2364.3 2365.3 0.012 22-Sep-08 01-Sep-08 TB08119994 E466799 08-NSD-002 2368.9 2369.9 0.0025 22-Sep-08 01-Sep-08 TB08119994 E466801 08-NSD-002 2369.9 2370.7 0.0025 22-Sep-08 Ol-Sep-08 TB08119994 E466802 08-NSD-002 2370.7 2371.2 0.0025 22-Sep-08 Ol-Sep-08 TB08119994 E466803 08-NSD-002 2371.2 2372.2 0.0025 22-Sep-08 01-Sep-08 TB08119994 E466804 08-NSD-002 2384.3 2385.3 0.011 22-Sep-08 01-Sep-08 TB08119994 E466805 08-NSD-002 2385.3 2385.9 0.0025 22-Sep-08 01-Sep-08 TB08119994 E466806 08-NSD-002 2385.9 2386.9 0.011 22-Sep-08 01-Sep-08 TB08119994 E466807 08-NSD-002 2386.9 2387.9 0.005 22-Sep-08 01-Sep-08 TB08119994 E466808 08-NSD-002 2387.9 2388.9 0.0025 22-Sep-08 01-Sep-08 TB08119994 E466809 08-NSD-002 2388.9 2389.8 0.005 22-Sep-08 01-Sep-08 TB08119994 E466811 08-NSD-002 2389.8 2390.9 0.005 22-Sep-08 01-Sep-08 TB08119994 E466812 08-NSD-002 2390.9 2391.9 0.0025 22-Sep-08 Ol-Sep-08 TB08119994 E466813 08-NSD-002 2391.9 2392.4 0.011 22-Sep-08 Ol-Sep-08 TB08119994 E466814 08-NSD-002 2392.4 2393.4 0.0025 22-Sep-08 01-Sep-08 TB08119994 E466815 08-NSD-002 2403.1 2404.1 0.007 22-Sep-08 02-Sep-08
TB08119994 E466816 08-1\JSD-002 2404.1 2405 0.03 22-Sep-08 02-Sep-08 TB08119994 E466817 08-NSD-002 2405 2406 0.09 22-Sep-08 02-Sep-08 TB08119994 E466818 08-NSD-002 2406 2407 0.04 22-Sep-08 02-Sep-08 TB08119994 E466819 08-NSD-002 2407 2408 0.083 22-Sep-08 02-Sep-08 TB08119994 E466821 08-NSD-002 2408 2409 0.049 22-Sep-08 02-Sep-08 TB08119994 E466822 08-NSD-002 2409 2410 0.156 22-Sep-08 02-Sep-08 TB08119994 E466823 08-NSD-002 2410 2411 0.097 22-Sep-08 02-Sep-08 TB08119994 E466824 08-NSD-002 2411 2412.1 0.578 22-Sep-08 02-Sep-08 TB08119994 E466825 08-NSD-002 2412.1 2413.2 0.064 22-Sep-08 02-Sep-08 TB08119994 E466826 08-NSD-002 2413.2 2414 0.114 22-Sep-08 02-Sep-08 TB08119994 E466827 08-NSD-002 2414 2415 0.027 22-Sep-08 02-Sep-08 TB08119994 E466828 08-NSD-002 2415 2416 0.056 22-Sep-08 02-Sep-08 TB08119994 E466829 08-NSD-002 2416 2416.6 0.047 22-Sep-08 02-Sep-08 TB08119994 E466831 08-NSD-002 2416.6 2417.5 0.048 22-Sep-08 08-Sep-08 TB08119994 E466832 08-NSD-002 2417.5 2418 0.438 22-Sep-08 08-Sep-08 TB08119994 E466833 08-NSD-002 2418 2419 0.042 22-Sep-08 08-Sep-08 TB08119994 E466834 08-NSD-002 2419 2420 0.206 22-Sep-08 08-Sep-08 TB08119994 E466835 08-NSD-002 2420 2420.5 0.099 22-Sep-08 08-Sep-08 TB08119994 E468001 08-NSD-002 1697.5 1698.5 0.0025 25-Aug-08 01-Aug-08 TB08119994 E468002 08-NSD-002 1698.5 1699.5 0.007 25-Aug-08 01-Aug-08 TB08119994 E468003 08-NSD-002 1699.5 1700.3 0.005 25-Aug-08 01-Aug-08 TB08119994 E468004 08-NSD-002 1700.3 1701.3 0.008 25-Aug-08 01-Aug-08 TB08119994 E468005 08-NSD-002 1701.3 1702.3 0.039 25-Aug-08 01-Aug-08 TB08119994 E468006 08-NSD-002 1710.1 1711.1 0.0025 25-Aug-08 01-Aug-08 TB08119994 E468007 08-NSD-002 1711.1 1712.1 0.006 25-Aug-08 01-Aug-08 TB08119994 E468008 08-NSD-002 1712.1 1712.5 0.0025 25-Aug-08 01-Aug-08 TB08119994 E468009 08-NSD-002 1712.5 1713 0.005 25-Aug-08 01-Aug-08 TB08119994 E468011 08-NSD-002 1713 1713.3 0.006 25-Aug-08 01-Aug-08 TB08119994 E468012 08-NSD-002 1713.3 1714.3 0.007 25-Aug-08 01-Aug-08 TB08119994 E468013 08-NSD-002 1714.3 1715.3 0.005 25-Aug-08 01-Aug-08 TB08119994 E468014 08-NSD-002 1715.3 1715.8 0.005 25-Aug-08 01-Aug-08 TB08119994 E468015 08-NSD-002 1725.5 1726.5 0.092 25-Aug-08 01-Aug-08 TB08119994 E468016 08-NSD-002 1726.5 1727.5 0.005 25-Aug-08 01-Aug-08 TB08119994 E468017 08-NSD-002 1727.5 1728.5 0.006 25-Aug-08 01-Aug-08 TB08119994 E468018 08-NSD-002 1728.5 1729.5 0.0025 25-Aug-08 01-Aug-08 TB08119994 E468019 08-NSD-002 1729.5 1730.3 0.005 25-Aug-08 01-Aug-08 TB08119994 E468021 08-NSD-002 1730.3 1730.6 0.0025 25-Aug-08 01-Aug-08 TB08119994 E468022 08-NSD-002 1730.6 1731.3 0.005 25-Aug-08 01-Aug-08 TB08119994 E468023 08-NSD-002 1781.5 1782.5 0.0025 25-Aug-08 08-Aug-08 TB08119994 E468024 08-NSD-002 1782.5 1783.5 0.0025 25-Aug-08 08-Aug-08 TB08119994 E468025 08-NSD-002 1783.5 1784 0.0025 25-Aug-08 08-Aug-08 TB08119994 E468026 08-NSD-002 1784 1785 0.0025 25-Aug-08 08-Aug-08 TB08119994 E468027 08-NSD-002 1785 1786 0.0025 25-Aug-08 08-Aug-08 TB08119994 E468028 08-NSD-002 1786 1787 0.007 25-Aug-08 08-Aug-08 TB08119994 E468029 08-NSD-002 1787 1788 0.007 25-Aug-08 08-Aug-08 TB08119994 E468031 08-NSD-002 1788 1789 0.008 25-Aug-08 08-Aug-08 TB08119994 E468032 08-NSD-002 1789 1789.5 0.0025 25-Aug-08 08-Aug-08 TB08119994 E468033 08-NSD-002 1789.5 1790 0.006 25-Aug-08 08-Aug-08 TB08119994 E468034 08-NSD-002 1790 1791 0.006 25-Aug-08 08-Aug-08 TB08119994 E468035 08-NSD-002 1791 1792 0.005 25-Aug-08 08-Aug-08
TB08119994 E468036 08-NSD-002 1792 1793 0.005 25-Aug-08 08-Aug-08 TB08119994 E468037 08-NSD-002 1803.4 1804.4 0.02 25-Aug-08 10-Aug-08 TB08119994 E468038 08-NSD-002 1804.4 1805.4 0.016 25-Aug-08 10-Aug-08 TB08119994 E468039 08-NSD-002 1805.4 1806.2 1.15 25-Aug-08 10-Aug-08 TB08119994 E468041 08-NSD-002 1806.2 1807 0.065 25-Aug-08 10-Aug-08 TB08119994 E468042 08-NSD-002 1807 1808 0.012 25-Aug-08 10-Aug-08 TB08119994 E468043 08-NSD-002 1808 1809 0.015 25-Aug-08 10-Aug-08 TB08119994 E468044 08-NSD-002 1809 1810 0.05 25-Aug-08 10-Aug-08 TB08119994 E468045 08-NSD-002 1810 1811 0.015 25-Aug-08 10-Aug-08 TB08119994 E468046 08-NSD-002 1811 1812 0.02 25-Aug-08 10-Aug-08 TB08119994 E468047 08-NSD-002 1812 1813 0.082 25-Aug-08 10-Aug-08 TB08119994 E468048 08-NSD-002 1813 1814 0.031 25-Aug-08 10-Aug-08 TB08119994 E468049 08-NSD-002 1814 1815 0.031 25-Aug-08 10-Aug-08 TB08119994 E468051 08-NSD-002 1815 1816 0.019 25-Aug-08 10-Aug-08 TB08119994 E468052 08-NSD-002 1816 1816.7 2.74 25-Aug-08 10-Aug-08 TB08119994 E468053 08-NSD-002 1816.7 1817.2 0.099 25-Aug-08 10-Aug-08 TB08119994 E468054 08-NSD-002 1817.2 1817.8 0.734 25-Aug-08 10-Aug-08 TB08119994 E468055 08-NSD-002 1817.8 1818.8 0.023 25-Aug-08 10-Aug-08 TB08119994 E468056 08-NSD-002 1818.8 1819.8 0.006 25-Aug-08 10-Aug-08 TB08119994 E468057 08-NSD-002 1819.8 1820.5 0.0025 25-Aug-08 10-Aug-08 TB08119994 E468058 08-NSD-002 1820.5 1821 0.011 25-Aug-08 10-Aug-08 TB08119994 E468059 08-NSD-002 1821 1822 0.007 25-Aug-08 10-Aug-08 TB08119994 E468061 08-NSD-002 1822 1823 0.0025 25-Aug-08 10-Aug-08 TB08119994 E468062 08-NSD-002 1823 1824 0.005 25-Aug-08 10-Aug-08 TB08119994 E468063 08-NSD-002 1824 1825 0.007 25-Aug-08 10-Aug-08 TB08119994 E468064 08-NSD-002 1825 1826 0.011 25-Aug-08 10-Aug-08 TB08119994 E468065 08-NSD-002 1826 1826.6 0.012 25-Aug-08 10-Aug-08 TB08119994 E468066 08-NSD-002 1826.6 1827.3 0.01 25-Aug-08 10-Aug-08 TB08119994 E468067 08-NSD-002 1827.3 1828.1 0.022 25-Aug-08 10-Aug-08 TB08119994 E468068 08-NSD-002 1828.1 1829 0.012 25-Aug-08 10-Aug-08 TB08119994 E468069 08-NSD-002 1829 1830 0.01 25-Aug-08 10-Aug-08 TB08119994 E468071 08-NSD-002 1830 1830.6 0.015 25-Aug-08 10-Aug-08 TB08119994 E468072 08-NSD-002 1830.6 1831.1 0.036 25-Aug-08 10-Aug-08 TB08119994 E468073 08-NSD-002 1831.1 1831.9 0.035 25-Aug-08 10-Aug-08 TB08119994 E468074 08-NSD-002 1831.9 1832.7 0.026 25-Aug-08 10-Aug-08 TB08119994 E468075 08-NSD-002 1832.7 1833.5 0.134 25-Aug-08 10-Aug-08 TB08119994 E468076 08-NSD-002 1833.5 1834.4 0.034 25-Aug-08 10-Aug-08 TB08119994 E468077 08-NSD-002 1834.4 1834.9 0.07 25-Aug-08 10-Aug-08 TB08119994 E468078 08-NSD-002 1834.9 1835.4 0.113 25-Aug-08 10-Aug-08 TB08119994 E468079 08-NSD-002 1835.4 1836.1 0.011 25-Aug-08 10-Aug-08 TB08119994 E468081 08-NSD-002 1836.1 1836.7 0.75 25-Aug-08 10-Aug-08 TB08119994 E468082 08-NSD-002 1836.7 1837.7 0.028 25-Aug-08 10-Aug-08 TB08119994 E468083 08-NSD-002 1837.7 1838.5 0.015 25-Aug-08 10-Aug-08 TB08119994 E468084 08-NSD-002 1838.5 1839.1 0.021 25-Aug-08 10-Aug-08 TB08119994 E468085 08-NSD-002 1839.1 1840 0.079 25-Aug-08 11-Aug-08 TB08120968 E468086 08-NSD-002 1840 1841 0.02 25-Aug-08 11-Aug-08 TB08120968 E468087 08-NSD-002 1841 1842 0.065 25-Aug-08 11-Aug-08 TB08120968 E468088 08-NSD-002 1902.S 1903.5 0.009 25-Aug-08 13-Aug-08 TB08120968 E468089 08-NSD-002 1903.5 1904.S 0.015 25-Aug-08 13-Aug-08 TB08120968 E468091 08-NSD-002 1904.5 1905.5 0.006 25-Aug-08 13-Aug-08
TB08120968 E468092 08-NSD-002 1905.5 1906.4 0.006 25-Aug-08 13-Aug-08 TB08120968 E468093 08-NSD-002 1906.4 1907 0.0025 25-Aug-08 13-Aug-08 TB08120968 E468094 08-NSD-002 1907 1907.4 0.082 25-Aug-08 13-Aug-08 TB08120968 E468095 08-NSD-002 1907.4 1908 0.006 25-Aug-08 13-Aug-08 TB08120968 E468096 08-NSD-002 1908 1909 0.007 25-Aug-08 13-Aug-08 TB08120968 E468097 08-NSD-002 1909 1909.5 0.007 25-Aug-08 13-Aug-08 TB08120968 E468098 08-NSD-002 1909.5 1910.2 0.023 25-Aug-08 13-Aug-08 TB08120968 E468099 08-NSD-002 1910.2 1911 0.01 25-Aug-08 13-Aug-08 TB08120968 E468101 08-NSD-002 1911 1911.5 0.008 25-Aug-08 13-Aug-08 TB08120968 E468102 08-NSD-002 1911.5 1912.5 0.071 25-Aug-08 13-Aug-08 TB08120968 E468103 08-NSD-002 1912.5 1913 0.008 25-Aug-08 13-Aug-08 TB08120968 E468104 08-NSD-002 1913 1914 0.005 25-Aug-08 13-Aug-08 TB08120968 E468105 08-NSD-002 1914 1915 0.017 25-Aug-08 13-Aug-08 TB08123787 E468106 08-NSD-002 1915 1916 0.103 02-Sep-08 13-Aug-08 TB08123787 E468107 08-NSD-002 1916 1916.7 0.014 02-Sep-08 21-Aug-08 TB08123787 E468108 08-NSD-002 1916.7 1917.3 0.006 02-Sep-08 21-Aug-08 TB08123787 E468109 08-NSD-002 1917.3 1918 0.074 02-Sep-08 21-Aug-08 TB08123787 E468111 08-NSD-002 1918 1919 0.048 02-Sep-08 21-Aug-08 TB08123787 E468112 08-NSD-002 1919 1920 0.134 02-Sep-08 21-Aug-08 TB08123787 E468113 08-NSD-002 1920 1921 0.01 02-Sep-08 21-Aug-08 TB08123787 E468114 08-NSD-002 1921 1921.8 0.296 02-Sep-08 21-Aug-08 TB08123787 E468115 08-NSD-002 1921.8 1922.8 0.285 02-Sep-08 21-Aug-08 TB08123787 E468116 08-NSD-002 1922.8 1923.8 0.154 02-Sep-08 21-Aug-08 TB08123787 E468117 08-NSD-002 1923.8 1924.8 0.159 02-Sep-08 21-Aug-08 TB08123787 E468118 08-NSD-002 1924.8 1925.8 0.295 02-Sep-08 21-Aug-08 TB08123787 E468119 08-NSD-002 1925.8 1926.8 0.049 02-Sep-08 21-Aug-08 TB08123787 E468121 08-NSD-002 1926.8 1927.8 0.048 02-Sep-08 21-Aug-08 TB08123787 E468122 08-NSD-002 1927.8 1928.5 0.048 02-Sep-08 21-Aug-08 TB08123787 E468123 08-NSD-002 1928.5 1929.3 0.061 02-Sep-08 21-Aug-08 TB08123787 E468124 08-NSD-002 1929.3 1929.7 0.009 02-Sep-08 21-Aug-08 TB08123787 E468125 08-NSD-002 1929.7 1930.7 0.0025 02-Sep-08 21-Aug-08 TB08123787 E468126 08-NSD-002 1930.7 1931.5 0.014 02-Sep-08 21-Aug-08 TB08123787 E468127 08-NSD-002 1931.5 1932.6 0.053 02-Sep-08 21-Aug-08 TB08123787 E468128 08-NSD-002 1932.6 1933.6 0.022 02-Sep-08 21-Aug-08 TB08123787 E468129 08-NSD-002 1933.6 1934.6 0.0025 02-Sep-08 21-Aug-08 TB08123787 E468131 08-NSD-002 1934.6 1935.6 0.01 02-Sep-08 28-Aug-08 TB08123787 E468132 08-NSD-002 2043.5 2044.5 0.0025 02-Sep-08 24-Aug-08 TB08123787 E468133 08-NSD-002 2044.5 2045.5 0.005 02-Sep-08 24-Aug-08 TB08123787 E468134 08-NSD-002 2045.5 2046.5 0.137 02-Sep-08 24-Aug-08 TB08123787 E468135 08-NSD-002 2046.5 2047.1 0.127 02-Sep-08 24-Aug-08 TB08123787 E468136 08-NSD-002 2047.1 2048.1 0.008 02-Sep-08 24-Aug-08 TB08123787 E468137 08-NSD-002 2048.1 2049.1 0.005 02-Sep-08 24-Aug-08 TB08123787 E468138 08-NSD-002 2050.2 2051.2 0.0025 02-Sep-08 24-Aug-08 TB08123787 E468139 08-NSD-002 2051.2 2052.2 0.0025 02-Sep-08 24-Aug-08 TB08123787 E468141 08-NSD-002 2052.2 2053 0.155 02-Sep-08 24-Aug-08 TB08123787 E468142 08-NSD-002 2053 2054 0.005 02-Sep-08 24-Aug-08 TB08123787 E468143 08-NSD-002 2054 2055 0.005 02-Sep-08 24-Aug-08 TB08123787 E468144 08-NSD-002 2136 2137 0.0025 02-Sep-08 24-Aug-08 TB08123786 E468145 08-NSD-002 2137 2137.9 0.008 02-Sep-08 24-Aug-08 TB08123786 E468146 08-NSD-002 2137.9 2138.8 0.01 02-Sep-08 24-Aug-08
TB08123786 E468147 08-I\JSD-002 2138.8 2139.4 0.0025 02-Sep-08 24-Aug-08 TB08123786 E468148 08-NSD-002 2139.4 2140 0.081 02-Sep-08 24-Aug-08 TB08123786 E468149 08-NSD-002 2140 2140.4 0.008 02-Sep-08 24-Aug-08 TB08123786 E468151 08-NSD-002 2140.4 2141.3 0.013 02-Sep-08 24-Aug-08 TB08123786 E468152 08-NSD-002 2141.3 2142.3 0.008 02-Sep-08 24-Aug-08 TB08123787 E468153 08-NSD-002 2144.2 2145.2 0.008 02-Sep-08 26-Aug-08 TB08123787 E468154 08-NSD-002 2145.2 2145.8 2.91 02-Sep-08 26-Aug-08 TB08123787 E468155 08-NSD-002 2145.8 2147 0.0025 02-Sep-08 26-Aug-08 TB08133367 E468156 08-NSD-002 2210.1 2211.1 0.0025 22-Sep-08 28-Aug-08 TB08133367 E468157 08-NSD-002 2211.1 2211.8 0.0025 22-Sep-08 28-Aug-08 TB08133367 E468158 08-NSD-002 2211.8 2212.5 0.013 22-Sep-08 28-Aug-08 TB08133367 E468159 08-NSD-002 2212.5 2213 0.134 22-Sep-08 28-Aug-08 TB08133367 E468161 08-NSD-002 2213 2213.6 0.01 22-Sep-08 28-Aug-08 TB08133367 E468162 08-NSD-002 2213.6 2214.3 0.038 22-Sep-08 28-Aug-08 TB08133367 E468163 08-NSD-002 2214.3 2215 0.046 22-Sep-08 28-Aug-08 TB08133367 E468164 08-NSD-002 2215 2216 0.012 22-Sep-08 28-Aug-08 TB08133367 E468165 08-NSD-002 2216 2217 0.022 22-Sep-08 28-Aug-08 TB08133367 E468166 08-NSD-002 2217 2217.5 0.333 22-Sep-08 28-Aug-08 TB08133367 E468167 08-NSD-002 2217.5 2218.3 0.125 22-Sep-08 28-Aug-08 TB08133367 E468168 08-NSD-002 2218.3 2219.4 0.01 22-Sep-08 28-Aug-08 TB08133367 E468169 08-NSD-002 2219.4 2220.4 0.006 22-Sep-08 28-Aug-08 TB08133367 E468171 08-NSD-002 2220.4 2221.3 0.008 22-Sep-08 28-Aug-08 TB08133367 E468172 08-NSD-002 2221.3 2221.8 0.013 22-Sep-08 28-Aug-08 TB08133367 E468173 08-NSD-002 2221.8 2222.7 0.052 22-Sep-08 28-Aug-08 TB08133367 E468174 08-NSD-002 2222.7 2223.2 0.018 22-Sep-08 28-Aug-08 TB08133367 E468175 08-NSD-002 2223.2 2223.7 0.375 22-Sep-08 28-Aug-08
Assay Certificate Sample# Hole Number From To Assay (g/t) Analysis Date Sample Date TB08138859 E466863 08-NSD-003 1012.3 1012.9 0.01 29-Sep-08 16-Sep-08 TB08138859 E466864 08-NSD-003 1012.9 1014 0.023 29-Sep-08 16-Sep-08 TB08138859 E466865 08-NSD-003 1014 1015 0.023 29-Sep-08 16-Sep-08 TB08138859 E466866 08-NSD-003 1015 1016 0.022 29-Sep-08 16-Sep-08 TB08138859 E466867 08-NSD-003 1016 1016.7 0.012 29-Sep-08 16-Sep-08 TB08138859 E466868 08-NSD-003 1016.7 1017.5 0.016 29-Sep-08 16-Sep-08 TB08138859 E466869 08-NSD-003 1019 1020 0.019 29-Sep-08 16-Sep-08 TB08138859 E466871 08-NSD-003 1020 1021 0.063 29-Sep-08 16-Sep-08 TB08138859 E466872 08-NSD-003 1021 1021.7 0.015 29-Sep-08 16-Sep-08 TB08138859 E466873 08-NSD-003 1021.7 1022.6 0.041 29-Sep-08 16-Sep-08 TB08138859 E466874 08-NSD-003 1022.6 1023.3 0.05 29-Sep-08 17-Sep-08 TB08138859 E466875 08-NSD-003 1023.3 1024 0.046 29-Sep-08 17-Sep-08 TB08138859 E466876 08-NSD-003 1024 1025 0.028 29-Sep-08 17-Sep-08 TB08138859 E466877 08-NSD-003 1025 1026 0.014 29-Sep-08 17-Sep-08 TB08138859 E466878 08-NSD-003 1033.7 1034.7 0.46 29-Sep-08 17-Sep-08 TB08138859 E466879 08-NSD-003 1034.7 1035.7 0.079 29-Sep-08 17-Sep-08 TB08138859 E466881 08-NSD-003 1035.7 1036.7 0.17 29-Sep-08 17-Sep-08 TB08138859 E466882 08-NSD-003 1036.7 1037.7 0.068 29-Sep-08 17-Sep-08 TB08138859 E466883 08-NSD-003 1037.7 1038.3 0.025 29-Sep-08 17-Sep-08 TB08138859 E466884 08-NSD-003 1038.3 1039.3 0.023 29-Sep-08 17-Sep-08 TB08138859 E466885 08-NSD-003 1058.6 1059.4 0.034 29-Sep-08 17-Sep-08 TB08138859 E466886 08-NSD-003 1059.4 1060.5 0.032 29-Sep-08 17-Sep-08 TB08138859 E466887 08-NSD-003 1060.5 1061.5 0.029 29-Sep-08 17-Sep-08 TB08138859 E466888 08-NSD-003 1061.5 1062.1 0.032 29-Sep-08 19-Sep-08 TB08138859 E466889 08-NSD-003 1062.1 1063.1 0.024 29-Sep-08 19-Sep-08 TB08138859 E466891 08-NSD-003 1063.1 1064.2 0.07 29-Sep-08 19-Sep-08 TB08138859 E466892 08-NSD-003 1064.2 1065.3 0.074 29-Sep-08 19-Sep-08 TB08138859 E466893 08-NSD-003 1065.3 1066.3 0.023 29-Sep-08 19-Sep-08 TB08138859 E466894 08-NSD-003 1066.3 1067.3 0.113 29-Sep-08 19-Sep-08 TB08138859 E466895 08-NSD-003 1067.3 1068 0.055 29-Sep-08 19-Sep-08 TB08138859 E466862 08-NSD-003 1011 1012.3 0.07 29-Sep-08 19-Sep-08 TB08138859 E466861 08-NSD-003 1010 1011 0.03 29-Sep-08 19-Sep-08 TB08138859 E466859 08-NSD-003 1009 1010 0.025 29-Sep-08 19-Sep-08 TB08138859 E466858 08-NSD-003 1008 1009 1.365 29-Sep-08 19-Sep-08 TB08138859 E466857 08-NSD-003 1007 1008 0.015 29-Sep-08 19-Sep-08 TB08138859 E466856 08-NSD-003 1006.5 1007 0.083 29-Sep-08 19-Sep-08 TB08138859 E466855 08-NSD-003 1005.5 1006.5 0.028 29-Sep-08 19-Sep-08 TB08138859 E466854 08-NSD-003 1004.5 1005.5 0.022 29-Sep-08 19-Sep-08 TB08138859 E466853 08-NSD-003 1003.7 1004.5 0.016 29-Sep-08 19-Sep-08 TB08138859 E466852 08-NSD-003 1003 1003.7 0.017 29-Sep-08 19-Sep-08 TB08138859 E466851 08-NSD-003 1002.4 1003 0.025 29-Sep-08 19-Sep-08 TB08138859 E466849 08-NSD-003 1001.7 1002.4 0.037 29-Sep-08 19-Sep-08 TB08138859 E466848 08-NSD-003 1000.7 1001.7 0.041 29-Sep-08 19-Sep-08 TB08138859 E466847 08-NSD-003 999.7 1000.7 0.029 29-Sep-08 19-Sep-08 TB08138859 E466846 08-NSD-003 998.8 999.7 0.033 29-Sep-08 19-Sep-08 TB08138859 E466845 08-NSD-003 998.2 998.8 0.176 29-Sep-08 19-Sep-08 TB08138859 E466844 08-NSD-003 997.6 998.2 0.027 29-Sep-08 19-Sep-08 TB08138859 E466843 08-NSD-003 996.6 997.6 0.038 29-Sep-08 19-Sep-08 TB08138859 E466842 08-NSD-003 995.6 996.6 0.177 29-Sep-08 19-Sep-08
TB08138859 E466841 08-NSD-003 994.7 995.6 0.194 29-Sep-08 19-Sep-08 TB08138859 E466839 08-NSD-003 993.9 994.7 0.366 29-Sep-08 19-Sep-08 TB08138859 E466838 08-NSD-003 992.9 993.9 0.562 29-Sep-08 19-Sep-08 TB08138859 E466837 08-NSD-003 991.9 992.9 0.159 29-Sep-08 19-Sep-08 TB08138859 E466836 08-NSD-003 990.9 991.9 0.252 29-Sep-08 19-Sep-08 TB08138859 E466896 08-NSD-003 1068 1069 1.215 29-Sep-08 19-Sep-08 TB08138859 E466924 08-NSD-003 1093.7 1094.7 0.47 29-Sep-08 21-Sep-08 TB08138859 E466925 08-NSD-003 1094.7 1095.8 0.023 29-Sep-08 21-Sep-08 TB08138859 E466926 08-NSD-003 1095.8 1096.5 0.146 29-Sep-08 21-Sep-08 TB08138859 E466927 08-NSD-003 1096.5 1097.5 0.017 29-Sep-08 21-Sep-08 TB08138859 E466928 08-NSD-003 1097.5 1098.2 0.011 29-Sep-08 21-Sep-08 TB08138859 E466929 08-NSD-003 1098.2 1099.2 0.016 29-Sep-08 21-Sep-08 TB08138859 E466931 08-NSD-003 1099.2 1100 0.013 29-Sep-08 21-Sep-08 TB08138859 E466932 08-NSD-003 1100 1100.5 0.007 29-Sep-08 21-Sep-08 TB08138859 E466933 08-NSD-003 1100.5 1101.4 0.012 29-Sep-08 21-Sep-08 TB08138859 E466934 08-NSD-003 1101.4 1102.2 0.011 29-Sep-08 21-Sep-08 TB08138859 E466935 08-NSD-003 1102.2 1103.2 0.005 29-Sep-08 21-Sep-08 TB08138859 E466936 08-NSD-003 1103.2 1104.1 0.034 29-Sep-08 21-Sep-08 TB08138859 E466937 08-NSD-003 1130.2 1131.2 0.52 29-Sep-08 21-Sep-08 TB08138859 E466938 08-NSD-003 1131.2 1131.6 0.019 29-Sep-08 21-Sep-08 TB08138859 E466939 08-NSD-003 1131.6 1132.6 0.803 29-Sep-08 21-Sep-08 TB08138859 E466941 08-NSD-003 1154.8 1155.7 0.538 29-Sep-08 21-Sep-08 TB08138859 E466942 08-NSD-003 1155.7 1156.1 0.016 29-Sep-08 21-Sep-08 TB08138859 E466943 08-NSD-003 1156.1 1157 0.033 29-Sep-08 21-Sep-08 TB08138859 E466944 08-NSD-003 1157 1158 0.635 29-Sep-08 21-Sep-08 TB08138859 E466945 08-NSD-003 1158 1158.6 0.589 29-Sep-08 21-Sep-08 TB08138859 E466946 08-NSD-003 1158.6 1159.3 0.378 29-Sep-08 21-Sep-08 TB08138859 E466947 08-NSD-003 1159.3 1159.9 0.683 29-Sep-08 21-Sep-08 TB08138859 E466948 08-NSD-003 1159.9 1160.9 0.375 29-Sep-08 21-Sep-08 TB08138859 E466949 08-NSD-003 1160.9 1161.9 0.43 29-Sep-08 21-Sep-08 TB08141162 E466951 08-NSD-003 1161.9 1162.8 0.042 29-Sep-08 21-Sep-08 TB08141162 E466952 08-NSD-003 1162.8 1163.8 0.363 29-Sep-08 21-Sep-08 TB08141162 E466953 08-NSD-003 1181.8 1182.8 1.28 29-Sep-08 21-Sep-08 TB08141162 E466954 08-NSD-003 1182.8 1183.3 0.377 29-Sep-08 21-Sep-08 TB08141162 E466955 08-NSD-003 1183.3 1184 0.63 29-Sep-08 21-Sep-08 TB08141162 E466956 08-NSD-003 1184 1185 0.169 29-Sep-08 21-Sep-08 TB08141162 E466957 08-NSD-003 1185 1186 0.082 29-Sep-08 21-Sep-08 TB08141162 E466958 08-NSD-003 1186 1187 0.071 29-Sep-08 21-Sep-08 TB08141162 E466897 08-NSD-003 1069 1069.7 4.61 29-Sep-08 21-Sep-08 TB08141162 E466898 08-NSD-003 1069.7 1070.4 2.21 29-Sep-08 21-Sep-08 TB08141162 E466899 08-NSD-003 1070.4 1071 0.035 29-Sep-08 21-Sep-08 TB08141162 E466901 08-NSD-003 1071 1071.6 0.08 29-Sep-08 21-Sep-08 TB08141162 E466902 08-NSD-003 1071.6 1072.2 0.0025 29-Sep-08 21-Sep-08 TB08141162 E466903 08-NSD-003 1072.2 1073 0.029 29-Sep-08 21-Sep-08 TB08141162 E466904 08-NSD-003 1073 1073.8 0.0025 29-Sep-08 21-Sep-08 TB08141162 E466905 08-NSD-003 1073.8 1075 0.012 29-Sep-08 22-Sep-08 TB08141162 E466906 08-NSD-003 1075 1076 0.009 29-Sep-08 22-Sep-08 TB08141162 E466907 08-NSD-003 1076 1076.6 0.005 29-Sep-08 22-Sep-08 TB08141162 E466908 08-NSD-003 1076.6 1077.6 0.0025 29-Sep-08 22-Sep-08 TB08141162 E466909 08-NSD-003 1077.6 1078.6 0.01 29-Sep-08 22-Sep-08
TB08141162 E466911 08-NSD-003 1078.6 1079.7 0.018 29-Sep-08 22-Sep-08 TB08141162 E466912 08-NSD-003 1079.7 1080.7 0.009 29-Sep-08 22-Sep-08 TB08141162 E466913 08-NSD-003 1080.7 1081.8 0.006 29-Sep-08 22-Sep-08 TB08141162 E466914 08-NSD-003 1081.8 1083 0.008 29-Sep-08 22-Sep-08 TB08141162 E466915 08-NSD-003 1083 1084 0.012 02-0ct-08 22-Sep-08 TB08141162 E466916 08-NSD-003 1086.7 1087.7 0.0025 02-0ct-08 22-Sep-08 TB08141162 E466917 08-NSD-003 1087.7 1088.8 0.0025 02-0ct-08 22-Sep-08 TB08141162 E466918 08-NSD-003 1088.8 1089.8 0.007 02-0ct-08 22-Sep-08 TB08141162 E466919 08-NSD-003 1089.8 1090.8 0.013 02-0ct-08 22-Sep-08 TB08141162 E466921 08-NSD-003 1090.8 1091.7 0.0025 02-0ct-08 22-Sep-08 TB08141162 E466922 08-NSD-003 1091.7 1092.6 0.03 02-0ct-08 22-Sep-08 TB08141162 E466923 08-NSD-003 1092.6 1093.7 0.343 02-0ct-08 22-Sep-08 TB08141162 E466959 08-NSD-003 1187 1188 0.042 02-0ct-08 24-Sep-08 TB08141162 E466961 08-NSD-003 1188 1189 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466962 08-1\JSD-003 1189 1190 0.006 02-0ct-08 24-Sep-08 TB08141162 E466963 08-NSD-003 1190 1191 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466964 08-NSD-003 1191 1192 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466965 08-1\JSD-003 1192 1193 0.007 02-0ct-08 24-Sep-08 TB08141162 E466966 08-NSD-003 1193 1193.7 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466967 08-NSD-003 1193.7 1194.6 0.007 02-0ct-08 24-Sep-08 TB08141162 E466968 08-NSD-003 1194.6 1195.6 0.013 02-0ct-08 24-Sep-08 TB08141162 E466969 08-NSD-003 1206.2 1207.2 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466971 08-NSD-003 1207.2 1208.2 0.018 02-0ct-08 24-Sep-08 TB08141162 E466972 08-NSD-003 1208.2 1209 0.078 02-0ct-08 24-Sep-08 TB08141162 E466973 08-NSD-003 1209 1210 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466974 08-NSD-003 1210 1211 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466975 08-NSD-003 1211 1212 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466976 08-NSD-003 1212 1213 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466977 08-NSD-003 1213 1214 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466978 08-NSD-003 1214 1215 0.0025 02-0ct-08 24-Sep-08 TB08141162 E466979 08-NSD-003 1215 1216 0.02 24-Apr-10 24-Sep-08 TB08141162 E466981 08-NSD-003 1216 1217 0.005 02-0ct-08 24-Sep-08 TB08141162 E466982 08-NSD-003 1217 1217.5 0.028 02-0ct-08 24-Sep-08 TB08141162 E466983 08-NSD-003 1217.5 1218.3 0.247 02-0ct-08 24-Sep-08 TB08141162 E466984 08-NSD-003 1218.3 1219.3 0.06 02-0ct-08 24-Sep-08 TB08141162 E466985 08-NSD-003 1219.3 1220.4 0.023 02-0ct-08 24-Sep-08 TB08141162 E466986 08-NSD-003 1220.4 1221.4 0.006 02-0ct-08 24-Sep-08 TB08141162 E466987 08-NSD-003 1221.4 1222.4 0.005 02-0ct-08 24-Sep-08 TB08141162 E466988 08-NSD-003 1222.4 1223.3 0.009 02-0ct-08 24-Sep-08 TB08141162 E466989 08-NSD-003 1223.3 1224 0.046 02-0ct-08 24-Sep-08 TB08141162 E466991 08-NSD-003 1224 1225 0.029 02-0ct-08 24-Sep-08 TB08141162 E466992 08-NSD-003 1225 1226 0.016 02-0ct-08 24-Sep-08 TB08141162 E466993 08-NSD-003 1226 1227 0.013 02-0ct-08 24-Sep-08 TB08141162 E466994 08-NSD-003 1227.8 1228.8 0.009 02-0ct-08 24-Sep-08 TB08141162 E466995 08-NSD-003 1228.8 1229.8 0.011 02-0ct-08 24-Sep-08 TB08141162 E466996 08-NSD-003 1229.8 1230.1 0.087 02-0ct-08 24-Sep-08 TB08141162 E466997 08-NSD-003 1230.1 1230.6 0.021 02-0ct-08 24-Sep-08 TB08141162 E466998 08-NSD-003 1230.6 1231.1 0.009 02-0ct-08 24-Sep-08 TB08141162 E466999 08-NSD-003 1231.1 1232 0.01 02-0ct-08 24-Sep-08 TB08141162 E467001 08-NSD-003 1232 1233 0.014 02-0ct-08 24-Sep-08
TB08141162 E467002 08-NSD-003 1233 1234.1 0.016 02-0ct-08 24-Sep-08
TB08141162 E467003 08-NSD-003 1234.1 1235.1 0.096 02-0ct-08 24-Sep-08
TB08141162 E467004 08-NSD-003 1235.1 1236.1 0.007 02-0ct-08 25-Sep-08
TB08141162 E467005 08-NSD-003 1236.1 1237.1 0.0025 02-0ct-08 25-Sep-08
TB08141162 E467006 08-NSD-003 1263 1264 0.0025 02-0ct-08 26-Sep-08
TB08141162 E467007 08-NSD-003 1264 1265.05 0.0025 02-0ct-08 26-Sep-08 TB08141162 E467008 08-NSD-003 1265.05 1265.7 0.016 02-0ct-08 26-Sep-08
TB08141162 E467009 08-NSD-003 1265.7 1266.2 0.0025 02-0ct-08 26-Sep-08
TB08155438 E467011 08-NSD-003 1266.2 1267.2 0.0025 10-Aug-30 26-Sep-08
TB08155438 E467012 08-NSD-003 1267.2 1268.2 0.005 10-Aug-30 26-Sep-08
Assay Certificate Sample# Hole Number From To Assay (g/t) Analysis Date Sample Date TB08155438 E467024 08-NSD-004 855.7 856.7 0.072 06-Nov-08 14-0ct-08 TB08155438 E467025 08-1\JSD-004 856.7 857.5 0.055 06-Nov-08 14-0ct-08 TB08155438 E467026 08-NSD-004 857.5 857.8 0.912 06-Nov-08 14-0ct-08 TB08155438 E467027 08-NSD-004 857.8 858.8 0.03 06-Nov-08 14-0ct-08 TB08155438 E467028 08-1\JSD-004 987.9 988.9 0.026 06-Nov-08 22-0ct-08 TB08155438 E467029 08-NSD-004 988.9 990 0.046 06-Nov-08 22-0ct-08 TB08155438 E467031 08-NSD-004 990 991 0.016 06-Nov-08 22-0ct-08 TB08155438 E467032 08-NSD-004 991 992 0.015 06-Nov-08 22-0ct-08 TB08155438 E467033 08-NSD-004 992 993 0.02 06-Nov-08 22-0ct-08 TB08155438 E467034 08-NSD-004 993 993.8 2.93 06-Nov-08 22-0ct-08 TB08155438 E467035 08-NSD-004 993.8 994.8 0.314 06-Nov-08 22-0ct-08 TB08155438 E467036 08-NSD-004 994.8 995.9 0.194 06-Nov-08 22-0ct-08 TB08155438 E467037 08-NSD-004 999.1 1000.1 0.014 06-Nov-08 22-0ct-08 TB08155438 E467038 08-NSD-004 1000.1 1001 0.025 06-Nov-08 22-0ct-08 TB08155438 E467039 08-NSD-004 1001 1001.8 0.031 06-Nov-08 22-0ct-08 TB08155438 E467041 08-NSD-004 1001.8 1002.8 0.989 06-Nov-08 22-0ct-08 TB08155438 E467042 08-NSD-004 1002.8 1003.8 0.034 06-Nov-08 22-0ct-08 TB08155438 E467043 08-NSD-004 1003.8 1004.8 0.097 06-Nov-08 22-0ct-08 TB08155438 E467044 08-NSD-004 1004.8 1005.8 0.898 06-Nov-08 22-0ct-08 TB08155438 E467045 08-NSD-004 1005.8 1006.4 0.021 06-Nov-08 22-0ct-08 TB08155438 E467046 08-NSD-004 1006.4 1007 0.089 06-Nov-08 22-0ct-08 TB08155438 E467047 08-NSD-004 1007 1008.2 0.076 06-Nov-08 22-0ct-08 TB08155438 E467048 08-NSD-004 1008.2 1009.4 0.233 06-Nov-08 22-0ct-08 TB08155438 E467049 08-NSD-004 1009.4 1010.4 0.437 06-Nov-08 22-0ct-08 TB08155438 E467051 08-NSD-004 1010.4 1011 0.028 06-Nov-08 22-0ct-08 TB08155438 E467052 08-NSD-004 1011 1011.9 0.705 06-Nov-08 22-0ct-08 TB08155438 E467053 08-NSD-004 1011.9 1012.7 1.315 06-Nov-08 22-0ct-08 TB08155438 E467054 08-NSD-004 1012.7 1013 1.175 06-Nov-08 22-0ct-08 TB08155438 E467055 08-NSD-004 1013 1014 0.014 06-Nov-08 22-0ct-08 TB08155438 E467056 08-NSD-004 1014 1015 0.011 06-Nov-08 22-0ct-08 TB08155438 E467057 08-NSD-004 1015 1015.8 0.02 06-Nov-08 22-0ct-08 TB08155438 E467058 08-NSD-004 1015.8 1016.3 0.032 06-Nov-08 22-0ct-08 TB08155438 E467059 08-NSD-004 1016.3 1017 0.008 06-Nov-08 22-0ct-08 TB08155438 E467061 08-NSD-004 1017 1017.8 0.0025 06-Nov-08 22-0ct-08 TB08155438 E467062 08-NSD-004 1017.8 1018.9 0.161 06-Nov-08 22-0ct-08 TB08155438 E467063 08-NSD-004 1018.9 1019.9 0.072 06-Nov-08 22-0ct-08 TB08155438 E467064 08-NSD-004 1019.9 1021.1 0.028 06-Nov-08 22-0ct-08 TB08155438 E467065 08-NSD-004 1021.1 1022.3 0.066 06-Nov-08 22-0ct-08 TB08155438 E467066 08-NSD-004 1022.3 1023.3 0.108 06-Nov-08 22-0ct-08 TB08155438 E467067 08-NSD-004 1023.3 1023.9 0.022 06-Nov-08 22-0ct-08 TB08155438 E467068 08-NSD-004 1023.9 1025 0.017 06-Nov-08 22-0ct-08 TB08155438 E467069 08-NSD-004 1025 1026 0.021 06-Nov-08 22-0ct-08 TB08155438 E467071 08-NSD-004 1026 1027 0.02 06-Nov-08 22-0ct-08 TB08155438 E467072 08-NSD-004 1027 1028 0.021 06-Nov-08 22-0ct-08 TB08155438 E467073 08-NSD-004 1028 1029.1 0.016 06-Nov-08 22-0ct-08 TB08166930 E467074 08-NSD-004 1029.1 1029.9 0.344 26-Jan-09 22-0ct-08 TB08166930 E467075 08-NSD-004 1029.9 1030.8 0.079 26-Jan-09 22-0ct-08 TB08166930 E467076 08-NSD-004 1030.8 1031.9 0.019 26-Jan-09 22-0ct-08 TB08166930 E467077 08-NSD-004 1053 1054 0.024 26-Jan-09 24-0ct-08
TB08166930 E467078 08-NSD-004 1054 1055 0.023 26-Jan-09 24-0ct-08 TB08166930 E467079 08-NSD-004 1055 1056 0.01 26-Jan-09 24-0ct-08 TB08166930 E467081 08-NSD-004 1056 1057 0.009 26-Jan-09 24-0ct-08 TB08166930 E467082 08-NSD-004 1057 1058 0.012 26-Jan-09 24-0ct-08 TB08166930 E467083 08-NSD-004 1058 1058.7 0.012 26-Jan-09 24-0ct-08 TB08166930 E467084 08-NSD-004 1058.7 1059.7 0.01 26-Jan-09 24-0ct-08 TB08166930 E467085 08-NSD-004 1059.7 1060.5 0.014 26-Jan-09 24-0ct-08 TB08166930 E467086 08-NSD-004 1060.5 1061 0.009 26-Jan-09 24-0ct-08 TB08166930 E467087 08-NSD-004 1061 1061.7 0.029 26-Jan-09 24-0ct-08 TB08166930 E467088 08-NSD-004 1061.7 1062.4 0.016 26-Jan-09 24-0ct-08 TB08166930 E467089 08-NSD-004 1062.4 1063.4 0.152 26-Jan-09 24-0ct-08 TB08166930 E467091 08-NSD-004 1063.4 1064 0.094 26-Jan-09 24-0ct-08 TB08166930 E467092 08-NSD-004 1064 1065 0.045 26-Jan-09 24-0ct-08 TB08166930 E467093 08-NSD-004 1065 1065.6 0.206 26-Jan-09 24-0ct-08 TB08166930 E467094 08-NSD-004 1065.6 1066.6 0.473 26-Jan-09 25-0ct-08 TB08166930 E467095 08-NSD-004 1066.6 1067.5 0.271 26-Jan-09 25-0ct-08 TB08166930 E467096 08-NSD-004 1067.5 1068 0.031 26-Jan-09 25-0ct-08 TB08166930 E467097 08-NSD-004 1068 1069 0.451 26-Jan-09 25-0ct-08 TB08166930 E467098 08-NSD-004 1069 1069.7 0.019 26-Jan-09 25-0ct-08 TB08166930 E467099 08-NSD-004 1069.7 1070.5 0.01 26-Jan-09 25-0ct-08 TB08166930 E467101 08-NSD-004 1070.5 1071 0.008 26-Jan-09 25-0ct-08 TB08166930 E467102 08-NSD-004 1071 1072 0.023 26-Jan-09 25-0ct-08 TB08166930 E467103 08-NSD-004 1072 1072.5 1.695 26-Jan-09 25-0ct-08 TB08166930 E467104 08-NSD-004 1072.5 1073.3 0.101 26-Jan-09 25-0ct-08 TB08166930 E467105 08-NSD-004 1073.3 1073.6 0.107 26-Jan-09 25-0ct-08 TB08166930 E467106 08-NSD-004 1073.6 1074.5 0.517 26-Jan-09 25-0ct-08 TB08166930 E467107 08-NSD-004 1074.5 1075 0.014 26-Jan-09 25-0ct-08 TB08166930 E467108 08-NSD-004 1075 1076 0.036 26-Jan-09 25-0ct-08 TB08166930 E467109 08-NSD-004 1076 1077 0.071 26-Jan-09 25-0ct-08 TB08166930 E467111 08-NSD-004 1077 1078 0.034 26-Jan-09 25-0ct-08 TB08166930 E467112 08-NSD-004 1078 1079 0.33 26-Jan-09 25-0ct-08 TB08166930 E467113 08-NSD-004 1079 1080 0.037 26-Jan-09 25-0ct-08 TB08166930 E467114 08-NSD-004 1080 1081 0.025 26-Jan-09 25-0ct-08 TB08166930 E467115 08-NSD-004 1081 1082 0.022 26-Jan-09 25-0ct-08 TB08166930 E467116 08-NSD-004 1082 1083 0.359 26-Jan-09 25-0ct-08 TB08166930 E467117 08-NSD-004 1083 1084 4.41 26-Jan-09 25-0ct-08 TB08166930 E467118 08-NSD-004 1084 1085 0.179 26-Jan-09 25-0ct-08 TB08166930 E467119 08-NSD-004 1085 1086 2.44 26-Jan-09 25-0ct-08 TB08166930 E467121 08-NSD-004 1086 1086.6 0.029 26-Jan-09 25-0ct-08 TB08166930 E467122 08-NSD-004 1086.6 1087.3 0.011 26-Jan-09 25-0ct-08 TB08166930 E467123 08-NSD-004 1087.3 1088.3 0.023 26-Jan-09 25-0ct-08 TB08166930 E467124 08-NSD-004 1088.3 1088.8 0.019 26-Jan-09 25-0ct-08 TB08166930 E467125 08-NSD-004 1088.8 1089.5 1.53 26-Jan-09 25-0ct-08 TB08166930 E467126 08-NSD-004 1089.5 1090.5 0.44 26-Jan-09 25-0ct-08 TB08166930 E467127 08-NSD-004 1090.5 1091.5 1.64 26-Jan-09 25-0ct-08 TB08166930 E467128 08-NSD-004 1091.5 1092.5 0.119 26-Jan-09 25-0ct-08 TB08166930 E467129 08-NSD-004 1092.5 1093.5 4.04 26-Jan-09 25-0ct-08 TB08166930 E467131 08-NSD-004 1093.5 1094 3.04 26-Jan-09 25-0ct-08 TB08166930 E467132 08-NSD-004 1094 1095 0.596 26-Jan-09 25-0ct-08 TB08166930 E467133 08-NSD-004 1095 1096 2 26-Jan-09 25-0ct-08
TB08166930 E467134 08-NSD-004 1096 1097 0.615 26-Jan-09 25-0ct-08 TB08166930 E467135 08-NSD-004 1097 1098 1.2 26-Jan-09 25-0ct-08 TB08166930 E467136 08-1\JSD-004 1098 1098.7 0.748 26-Jan-09 25-0ct-08 TB08166930 E467137 08-1\JS D-004 1098.7 1099.7 1.41 26-Jan-09 25-0ct-08 TB08166930 E467138 08-NSD-004 1099.7 1100 0.622 26-Jan-09 25-0ct-08 TB08166930 E467139 08-NSD-004 1100 1101 0.031 26-Jan-09 25-0ct-08 TB08166930 E467141 08-NSD-004 1101 1102 0.012 26-Jan-09 25-0ct-08 TB08166930 E467142 08-NSD-004 1159.1 1160.1 0.012 26-Jan-09 31-0ct-08 TB08166930 E467143 08-NSD-004 1160.1 1160.9 0.066 26-Jan-09 31-0ct-08 TB08166930 E467144 08-NSD-004 1160.9 1161.5 0.0025 26-Jan-09 31-0ct-08 TB08166930 E467145 08-NSD-004 1161.5 1162.5 0.006 26-Jan-09 31-0ct-08 TB08166930 E467146 08-NSD-004 1162.5 1163.4 0.008 26-Jan-09 31-0ct-08 TB08166930 E467147 08-NSD-004 1163.4 1164.4 0.006 26-Jan-09 31-0ct-08 TB08166930 E467148 08-NSD-004 1164.4 1165.4 0.007 26-Jan-09 31-0ct-08 TB08166930 E467149 08-NSD-004 1179.1 1179.5 0.0025 26-Jan-09 31-0ct-08 TB08166930 E467151 08-NSD-004 1179.5 1180.5 0.008 26-Jan-09 31-0ct-08 TB08166930 E467152 08-NSD-004 1180.5 1181.5 0.0025 26-Jan-09 31-0ct-08 TB08166930 E467153 08-NSD-004 1181.5 1182.5 0.005 26-Jan-09 31-0ct-08 TB08166930 E467154 08-NSD-004 1182.5 1183.5 0.0025 26-Jan-09 31-0ct-08 TB08166930 E467155 08-NSD-004 1183.5 1184.5 0.006 26-Jan-09 31-0ct-08 TB08166930 E467156 08-NSD-004 1184.5 1185.5 0.723 26-Jan-09 31-0ct-08 TB08166930 E467157 08-NSD-004 1185.5 1186.5 0.006 26-Jan-09 31-0ct-08 TB08166930 E467158 08-NSD-004 1186.5 1187.5 0.007 26-Jan-09 31-0ct-08 TB08166930 E467159 08-NSD-004 1187.5 1188.5 0.008 26-Jan-09 31-0ct-08 TB08166930 E467161 08-NSD-004 1188.5 1189.5 0.036 26-Jan-09 31-0ct-08 TB08166930 E467162 08-NSD-004 1189.5 1190.5 0.06 26-Jan-09 31-0ct-08 TB08166930 E467163 08-NSD-004 1190.5 1191.4 0.039 26-Jan-09 31-0ct-08 TB08166930 E467164 08-NSD-004 1191.4 1192 0.0025 26-Jan-09 31-0ct-08 TB08166930 E467165 08-NSD-004 1192 1192.4 0.007 26-Jan-09 31-0ct-08 TB08166930 E467166 08-NSD-004 1192.4 1193.4 0.005 26-Jan-09 31-0ct-08 TB08166930 E467167 08-NSD-004 1193.4 1194.4 0.01 26-Jan-09 31-0ct-08 TB08166930 E467168 08-NSD-004 1211.6 1212.6 0.006 26-Jan-09 01-Nov-08 TB08166930 E467169 08-NSD-004 1212.6 1213.3 0.009 26-Jan-09 Ol-Nov-08 TB08166930 E467171 08-NSD-004 1213.3 1214 0.013 26-Jan-09 01-Nov-08 TB08166930 E467172 08-NSD-004 1214 1215 0.006 26-Jan-09 01-Nov-08 TB08166930 E467173 08-NSD-004 1215 1216 0.005 26-Jan-09 01-Nov-08 TB08166930 E467174 08-NSD-004 1216 1217 0.0025 26-Jan-09 01-Nov-08 TB08166930 E467175 08-NSD-004 1217 1218 0.052 26-Jan-09 01-Nov-08 TB08166930 E467176 08-NSD-004 1218 1219 0.031 26-Jan-09 01-Nov-08 TB08166930 E467177 08-NSD-004 1219 1219.4 0.573 26-Jan-09 01-Nov-08 TB08166930 E467178 08-NSD-004 1219.4 1220 0.056 26-Jan-09 01-Nov-08 TB08166930 E467179 08-NSD-004 1220 1221 0.103 26-Jan-09 01-Nov-08 TB08166930 E467181 08-NSD-004 1221 1221.5 0.503 26-Jan-09 01-Nov-08 TB08166930 E467182 08-NSD-004 1221.5 1222.2 0.364 26-Jan-09 01-Nov-08 TB08166930 E467183 08-NSD-004 1222.2 1223.2 0.354 26-Jan-09 01-Nov-08 TB08166930 E467184 08-NSD-004 1223.2 1224.2 0.005 26-Jan-09 01-Nov-08 TB08166930 E467185 08-NSD-004 1268.1 1269.1 0.007 26-Jan-09 02-Nov-08 TB08166930 E467186 08-NSD-004 1269.1 1269.4 0.368 26-Jan-09 02-Nov-08 TB08166930 E467187 08-NSD-004 1269.4 1270.4 0.006 26-Jan-09 02-Nov-08 TB08166930 E467188 08-NSD-004 1289.5 1290.5 0.005 26-Jan-09 03-Nov-08
TB08166930 E467189 08-NSD-004 1290.5 1290.9 0.005 26-Jan-09 03-Nov-08 TB08166930 E467191 08-NSD-004 1290.9 1291.9 0.006 26-Jan-09 03-Nov-08 TB08166930 E467192 08-NSD-004 1291.9 1292.5 0.0025 26-Jan-09 03-Nov-08 TB08166930 E467193 08-NSD-004 1292.5 1293 0.0025 26-Jan-09 03-Nov-08 TB08166930 E467194 08-NSD-004 1293 1294 0.0025 26-Jan-09 03-Nov-08 TB08166930 E467195 08-NSD-004 1360.6 1361.4 0.006 26-Jan-09 05-Nov-08 TB08166930 E467196 08-NSD-004 1361.4 1361.8 0.0025 26-Jan-09 05-Nov-08 TB08166930 E467197 08-NSD-004 1361.8 1362.3 0.0025 26-Jan-09 05-Nov-08 TB08166930 E467198 08-NSD-004 1362.3 1362.9 0.0025 26-Jan-09 05-Nov-08 TB08166930 E467199 08-NSD-004 1362.9 1363.9 0.0025 26-Jan-09 05-Nov-08 TB09032095 E467751 08-NSD-004 2260.2 2261 0.017 02-Apr-09 08-Mar-09 TB09032095 E467752 08-NSD-004 2261 2262 0.077 02-Apr-09 08-Mar-09 TB09032095 E467753 08-NSD-004 2262 2263 0.196 02-Apr-09 08-Mar-09 TB09032095 E467754 08-NSD-004 2263 2263.9 1.04 02-Apr-09 08-Mar-09 TB09032095 E467755 08-NSD-004 2263.9 2264.9 0.178 02-Apr-09 08-Mar-09 TB09032095 E467756 08-NSD-004 2264.9 2265.9 0.353 02-Apr-09 08-Mar-09 TB09032095 E467757 08-NSD-004 2265.9 2266.9 0.228 02-Apr-09 08-Mar-09 TB09032095 E467758 08-NSD-004 2266.9 2267.9 0.103 02-Apr-09 08-Mar-09 TB09032095 E467759 08-NSD-004 2267.9 2268.9 0.122 02-Apr-09 08-Mar-09 TB09032095 E467761 08-NSD-004 2268.9 2269.9 0.008 02-Apr-09 08-Mar-09 TB09032095 E467762 08-NSD-004 2269.9 2270.9 0.013 02-Apr-09 08-Mar-09 TB09032095 E467763 08-NSD-004 2270.9 2271.6 0.03 02-Apr-09 08-Mar-09 TB09032095 E467764 08-NSD-004 2271.6 2272.4 0.21 02-Apr-09 08-Mar-09 TB09032095 E467765 08-NSD-004 2272.4 2273.4 0.056 02-Apr-09 08-Mar-09 TB09032095 E467766 08-NSD-004 2273.4 2274.4 0.056 02-Apr-09 08-Mar-09 TB09032095 E467767 08-NSD-004 2274.4 2275 0.035 02-Apr-09 08-Mar-09 TB09032095 E467768 08-NSD-004 2275 2276 0.206 02-Apr-09 08-Mar-09 TB09032095 E467769 08-NSD-004 2279 2280 0.007 02-Apr-09 08-Mar-09 TB09032095 E467771 08-NSD-004 2280 2280.7 0.029 02-Apr-09 08-Mar-09 TB09032095 E467772 08-NSD-004 2280.7 2281.4 0.042 02-Apr-09 08-Mar-09 TB09032095 E467773 08-NSD-004 2281.4 2282.4 0.011 02-Apr-09 08-Mar-09 TB09032095 E467774 08-NSD-004 2282.4 2283.4 0.008 02-Apr-09 08-Mar-09 TB09022320 E529459 08-NSD-004 1586.3 1587.3 0.014 17-Jan-09 TB09022320 E529461 08-NSD-004 1587.3 1588 0.006 17-Jan-09 TB09022320 E529462 08-NSD-004 1588 1589 0.0025 17-Jan-09 TB09022320 E529463 08-NSD-004 1589 1589.7 0.0025 17-Jan-09 TB09022320 E529464 08-NSD-004 1598 1599 0.0025 17-Jan-09 TB09022320 E529465 08-NSD-004 1599 1600 0.012 17-Jan-09 TB09022320 E529466 08-NSD-004 1600 1601 0.005 17-Jan-09 TB09022320 E529467 08-NSD-004 1606 1607 0.007 17-Jan-09 TB09022320 E529468 08-NSD-004 1607 1608 0.078 17-Jan-09 TB09022320 E529469 08-NSD-004 1608 1608.5 0.488 17-Jan-09 TB09022320 E529471 08-NSD-004 1608.5 1609.2 0.132 17-Jan-09 TB09022320 E529472 08-NSD-004 1609.2 1609.9 0.36 17-Jan-09 TB09022320 E529473 08-NSD-004 1609.9 1610.5 0.187 17-Jan-09 TB09022320 E529474 08-NSD-004 1610.5 1611.5 0.058 17-Jan-09 TB09022320 E529475 08-NSD-004 1746 1746.8 0.0025 10-Feb-09 TB09022320 E529476 08-NSD-004 1746.8 1747.8 0.012 10-Feb-09 TB09022320 E529477 08-NSD-004 1747.8 1748.8 0.011 10-Feb-09 TB09022320 E529478 08-NSD-004 1748.8 1749.4 0.006 10-Feb-09
TB09022320 E529479 08-NSD-004 1749.4 1750 0.005 10-Feb-09 TB09022320 E529481 08-NSD-004 1750 1751 0.006 10-Feb-09 TB09022320 E529482 08-NSD-004 1778 1778.6 0.008 10-Feb-09 TB09022320 E529483 08-NSD-004 1778.6 1779.6 0.014 10-Feb-09 TB09022320 E529484 08-NSD-004 1779.6 1780.2 0.014 10-Feb-09 TB09022320 E529485 08-NSD-004 1780.2 1781 0.015 10-Feb-09 TB09022320 E529486 08-NSD-004 1781 1782 0.011 10-Feb-09 TB09022320 E529487 08-NSD-004 1782 1783 0.012 10-Feb-09 TB09022320 E529488 08-NSD-004 1783 1784 0.017 10-Feb-09 TB09022320 E529489 08-NSD-004 1784 1785 0.023 10-Feb-09 TB09022320 E529491 08-NSD-004 1785 1786 0.02 10-Feb-09 TB09022320 E529492 08-NSD-004 1786 1787 0.011 10-Feb-09 TB09022320 E529493 08-NSD-004 1787 1788 0.01 10-Feb-09 TB09022320 E529494 08-NSD-004 1816.1 1817.1 0.006 12-Feb-09 TB09022320 E529495 08-NSD-004 1817.1 1818.1 0.011 12-Feb-09 TB09022320 E529496 08-NSD-004 1818.1 1819.2 0.11 12-Feb-09 TB09022320 E529497 08-NSD-004 1819.2 1820.3 0.112 12-Feb-09 TB09022320 E529498 08-NSD-004 1820.3 1821 0.052 12-Feb-09 TB09022320 E529499 08-NSD-004 1821 1822 0.021 12-Feb-09 TB09022320 E530501 08-NSD-004 1822 1823 0.006 12-Feb-09 TB09022320 E530502 08-NSD-004 1823 1824 0.005 12-Feb-09 TB09022320 E530503 08-NSD-004 1824 1825 0.005 12-Feb-09 TB09022320 E530504 08-NSD-004 1825 1826 0.005 12-Feb-09 TB09022320 E530505 08-NSD-004 1826 1827 0.006 12-Feb-09 TB09022320 E530506 08-NSD-004 1827 1827.6 0.0025 12-Feb-09 TB09022320 E530507 08-NSD-004 1827.6 1828.4 0.044 12-Feb-09 TB09022320 E530508 08-NSD-004 1828.4 1828.8 0.487 12-Feb-09 TB09022320 E530509 08-NSD-004 1828.8 1829.9 0.073 12-Feb-09 TB09022320 E530511 08-NSD-004 1829.9 1830.5 0.8 12-Feb-09 TB09022320 E530512 08-NSD-004 1830.5 1830.9 0.041 12-Feb-09 TB09022320 E530513 08-NSD-004 1830.9 1831.6 0.058 12-Feb-09 TB09022320 ES30514 08-NSD-004 1831.6 1832.6 0.012 12-Feb-09 TB09022320 E530515 08-NSD-004 1832.6 1833.6 0.068 12-Feb-09 TB09022320 E530526 08-NSD-004 1929.7 1930.7 0.01 21-Feb-09 TB09022320 E530527 08-NSD-004 1930.7 1931.7 0.009 21-Feb-09 TB09022320 E530528 08-NSD-004 1931.7 1932.7 0.093 21-Feb-09 TB09022320 E530529 08-NSD-004 1932.7 1933.7 0.038 21-Feb-09 TB09022320 E530531 08-NSD-004 1933.7 1934.5 0.009 21-Feb-09 TB09022320 E530532 08-NSD-004 1934.5 1935.2 0.018 21-Feb-09 TB09022320 E530533 08-NSD-004 1935.2 1935.6 0.072 21-Feb-09 TB09022320 E530534 08-NSD-004 1935.6 1936.6 0.062 21-Feb-09 TB09022320 E530535 08-NSD-004 1936.6 1937 0.026 21-Feb-09 TB09022320 E530536 08-NSD-004 1937 1938 0.013 21-Feb-09 TB09022320 E530537 08-NSD-004 1938 1938.8 0.023 21-Feb-09 TB09022320 E530538 08-NSD-004 1938.8 1939.2 0.034 21-Feb-09 TB09022320 E530539 08-NSD-004 1939.2 1940 0.014 21-Feb-09 TB09022320 E530541 08-NSD-004 1940 1941 0.009 21-Feb-09 TB09022320 E530542 08-NSD-004 1941 1942 0.007 21-Feb-09 TB09022320 E530543 08-NSD-004 1942 1943 0.469 21-Feb-09 TB09022320 E530544 08-NSD-004 1943 1944 0.273 21-Feb-09
TB09022320 E530545 08-NSD-004 1944 1945 0.137 21-Feb-09 TB09022320 E530546 08-NSD-004 1945 1946 0.028 21-Feb-09 TB09022320 E530547 08-NSD-004 1946 1947 0.033 21-Feb-09 TB09022320 E530548 08-NSD-004 1947 1948 0.016 21-Feb-09 TB09022320 E530549 08-NSD-004 1948 1949 0.024 21-Feb-09 TB09022320 E530551 08-NSD-004 1949 1950 0.035 21-Feb-09 TB09022320 E530552 08-NSD-004 1950 1951 0.338 21-Feb-09 TB09022320 E530553 08-NSD-004 1951 1951.6 0.043 21-Feb-09 TB09022320 E530554 08-NSD-004 1951.6 1952.1 0.045 21-Feb-09 TB09022320 E530555 08-NSD-004 1952.1 1953.1 0.015 21-Feb-09 TB09022320 E530556 08-NSD-004 1953.1 1954.1 0.008 21-Feb-09 TB09032097 E530557 08-NSD-004 2008.5 2009.5 0.014 02-Apr-09 07-Mar-09 TB09032097 E530558 08-NSD-004 2009.5 2010.5 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530559 08-NSD-004 2010.5 2011.5 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530561 08-NSD-004 2011.5 2012.5 0.006 02-Apr-09 07-Mar-09 TB09032097 E530562 08-NSD-004 2012.5 2013.5 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530563 08-NSD-004 2013.5 2014.5 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530564 08-NSD-004 2014.5 2015.5 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530565 08-NSD-004 2015.5 2016.5 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530566 08-NSD-004 2016.5 2017.5 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530567 08-NSD-004 2017.5 2018.5 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530568 08-NSD-004 2018.5 2019 0.0025 02-Apr-09 07-IVlar-09 TB09032097 E530569 08-NSD-004 2019 2020 0.006 02-Apr-09 07-Mar-09 T809032097 E530571 08-NSD-004 2020 2021 0.012 02-Apr-09 07-Mar-09 TB09032097 E530572 08-NSD-004 2021 2022 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530573 08-NSD-004 2022 2023 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530574 08-NSD-004 2023 2024 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530575 08-NSD-004 2024 2025 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530576 08-NSD-004 2025 2026 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530577 08-NSD-004 2026 2027 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530578 08-NSD-004 2027 2028 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530579 08-NSD-004 2028 2029 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530581 08-NSD-004 2029 2030 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530582 08-NSD-004 2030 2031 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530583 08-NSD-004 2031 2032 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530584 08-NSD-004 2032 2033 0.0025 02-Apr-09 07-Mar-09 TB09032097 E530585 08-NSD-004 2033 2034 0.0025 02-Apr-09 07-Mar-09 TB09044021 E530586 08-NSD-004 2192.1 2193.1 0.019 18-May-09 08-Mar-09 TB09044021 E530587 08-NSD-004 2193.1 2194.1 0.022 18-May-09 08-Mar-09 TB09044021 E530588 08-NSD-004 2194.1 2195.1 0.021 18-May-09 08-Mar-09 TB09044021 E530589 08-NSD-004 2195.1 2196.1 0.025 18-May-09 08-Mar-09 TB09044021 E530591 08-NSD-004 2196.1 2197.1 0.017 18-May-09 08-Mar-09 TB09044021 E530592 08-NSD-004 2197.1 2198.1 0.008 18-May-09 08-Mar-09 TB09044021 E530593 08-1\JSD-004 2198.1 2199.1 0.008 18-May-09 08-Mar-09 TB09044021 E530594 08-NSD-004 2199.1 2199.8 0.008 18-May-09 08-Mar-09 TB09044021 E530595 08-1\JSD-004 2199.8 2200.3 0.006 18-May-09 08-Mar-09 TB09044021 E530596 08-NSD-004 2200.3 2201.2 0.011 18-May-09 08-Mar-09 TB09044021 E530597 08-NSD-004 2201.2 2202.2 0.0025 18-May-09 08-Mar-09 TB09044021 E530598 08-NSD-004 2202.2 2203.3 0.0025 18-May-09 08-Mar-09 TB09032096 E530599 08-NSD-004 2216.5 2217.5 0.031 02-Apr-09 08-Mar-09
TB09032096 E530601 08-1\ISD-004 2217.5 2218.5 0.054 02-Apr-09 08-Mar-09 TB09032096 E530602 08-1\ISD-004 2218.5 2219.5 0.017 02-Apr-09 08-Mar-09 TB09032096 E530603 08-NSD-004 2219.5 2220.5 0.019 02-Apr-09 08-Mar-09 TB09032096 E530604 08-1\ISD-004 2220.5 2221.5 0.072 02-Apr-09 08-Mar-09 TB09032096 E530605 08-NSD-004 2221.5 2222.5 0.01 02-Apr-09 08-Mar-09 TB09032096 E530606 08-NSD-004 2222.5 2223.5 0.011 02-Apr-09 08-Mar-09 TB09032096 E530607 08-1\ISD-004 2223.5 2224.5 0.005 02-Apr-09 08-Mar-09 TB09032096 E530608 08-NSD-004 2224.5 2225.5 0.006 02-Apr-09 08-Mar-09 TB09032096 E530609 08-NSD-004 2225.5 2226.5 0.03 02-Apr-09 08-Mar-09 TB09032096 E530611 08-NSD-004 2226.5 2227.5 0.006 02-Apr-09 08-Mar-09 TB09032096 E530612 08-NSD-004 2227.5 2228.5 0.01 02-Apr-09 08-Mar-09 TB09032096 E530613 08-NSD-004 2228.5 2229.5 0.009 02-Apr-09 08-Mar-09 TB09032096 E530614 08-NSD-004 2229.5 2230 0.0025 02-Apr-09 08-Mar-09 TB09032096 E530615 08-NSD-004 2230 2230.8 0.0025 02-Apr-09 08-Mar-09 TB09032096 E530616 08-NSD-004 2230.8 2231.8 0.0025 02-Apr-09 08-Mar-09 TB09032096 E530617 08-NSD-004 2231.8 2232.8 0.035 02-Apr-09 08-Mar-09 TB09032096 E530618 08-NSD-004 2232.8 2233.8 0.009 02-Apr-09 08-Mar-09 TB09032096 E530619 08-NSD-004 2254.3 2255.3 0.005 02-Apr-09 08-Mar-09 TB09032096 E530621 08-NSD-004 2255.3 2256.3 0.008 02-Apr-09 08-Mar-09 TB09032096 E530622 08-NSD-004 2256.3 2257.3 0.011 02-Apr-09 08-Mar-09 TB09032096 E530623 08-NSD-004 2257.3 2258.3 0.006 02-Apr-09 08-Mar-09 TB09032096 E530624 08-NSD-004 2258.3 2259.3 0.013 02-Apr-09 08-Mar-09 TB09032096 E530625 08-NSD-004 2259.3 2260.2 0.006 02-Apr-09 08-Mar-09 TB09044021 E531001 08-NSD-004 2328.2 2329.2 0.008 18-May-09 16-Mar-09 TB09044021 E531002 08-NSD-004 2329.2 2330.2 0.007 18-May-09 16-Mar-09 TB09044021 E531003 08-NSD-004 2330.2 2330.7 0.006 18-May-09 16-Mar-09 TB09044021 E531004 08-NSD-004 2330.7 2331.7 0.005 18-May-09 16-Mar-09 TB09044021 E531005 08-NSD-004 2331.7 2332.7 0.0025 18-May-09 16-Mar-09 TB09044021 E531006 08-NSD-004 2342.5 2343.5 0.0025 18-May-09 16-Mar-09 TB09044021 E531007 08-NSD-004 2343.5 2344.5 0.0025 18-May-09 16-Mar-09 TB09044021 E531008 08-NSD-004 2344.5 2345 0.005 18-May-09 16-Mar-09 TB09044021 E531009 08-NSD-004 2345 2346 0.005 18-May-09 16-Mar-09 TB09044021 E531011 08-NSD-004 2346 2347 0.009 18-May-09 16-Mar-09 TB09044021 E531012 08-NSD-004 2347 2347.6 0.0025 18-May-09 16-Mar-09 TB09044021 E531013 08-NSD-004 2347.6 2348 0.0025 18-May-09 16-Mar-09 TB09044021 E531014 08-NSD-004 2348 2349 0.0025 18-May-09 16-Mar-09 TB09044021 E531015 08-NSD-004 2349 2350 0.0025 18-May-09 16-Mar-09 TB09044021 E531016 08-NSD-004 2350 2351 0.0025 18-May-09 16-Mar-09 TB09044021 E531017 08-NSD-004 2351 2352 0.0025 18-May-09 16-Mar-09 TB09044021 E531018 08-NSD-004 2352 2353 0.0025 18-May-09 16-Mar-09
Assay Certificate Sample# Hole Number From To Assay (g/t) Analysis Date Sample Date TB09044021 E513451 09-NSD-001 1945 1946 0.0025 18-May-09 17-Apr-09 TB09044021 E513452 09-NSD-001 1946 1947 0.0025 18-May-09 17-Apr-09 TB09044021 E513453 09-NSD-001 1947 1947.6 0.0025 18-May-09 17-Apr-09 TB09044021 E513454 09-NSD-001 1947.6 1948.6 0.0025 18-May-09 17-Apr-09 TB09044021 E513455 09-NSD-001 1948.6 1949.6 0.0025 18-May-09 17-Apr-09 TB09044021 E513456 09-NSD-001 1956.8 1957.8 0.0025 18-May-09 17-Apr-09 TB09044021 E513457 09-NSD-001 1957.8 1958.8 0.0025 18-May-09 17-Apr-09 TB09044021 E513458 09-NSD-001 1958.8 1959.7 0.205 18-May-09 17-Apr-09 TB09044021 E513459 09-NSD-001 1959.7 1960.2 0.09 18-May-09 17-Apr-09 TB09044021 E513461 09-NSD-001 1960.2 1961 0.749 18-May-09 17-Apr-09 TB09044021 E513462 09-NSD-001 1961 1962 0.034 18-May-09 17-Apr-09 TB09044021 E513463 09-NSD-001 1962 1963 0.009 18-May-09 17-Apr-09 TB09044021 E513464 09-NSD-001 1963 1964 0.018 18-May-09 17-Apr-09 TB09044021 E513465 09-NSD-001 1964 1965 0.851 18-May-09 17-Apr-09 TB09044021 E513466 09-NSD-001 1965 1966 0.514 18-May-09 17-Apr-09 TB09044021 E513467 09-NSD-001 1966 1967 1.795 18-May-09 17-Apr-09 TB09044021 E513468 09-NSD-001 1967 1968 0.472 18-May-09 17-Apr-09 TB09044021 E513469 09-NSD-001 1968 1968.7 0.863 18-May-09 17-Apr-09 TB09044021 E513471 09-NSD-001 1968.7 1969.3 0.36 18-May-09 17-Apr-09 TB09044021 E513472 09-NSD-001 1969.3 1969.7 0.126 18-May-09 17-Apr-09 TB09044021 E513473 09-NSD-001 1969.7 1970.7 0.007 18-May-09 17-Apr-09 TB09044021 E513474 09-NSD-001 1970.7 1971.7 0.009 18-May-09 17-Apr-09 TB09032093 E513501 09-NSD-001 1559 1560 0.06 02-Apr-09 12-Mar-09 TB09032093 E513502 09-NSD-001 1560 1561 0.195 02-Apr-09 12-Mar-09 TB09032093 E513503 09-NSD-001 1561 1561.7 0.661 02-Apr-09 12-Mar-09 TB09032093 E513504 09-NSD-001 1561.7 1562.3 0.074 02-Apr-09 12-Mar-09 TB09032093 E513505 09-NSD-001 1562.3 1563.3 0.011 02-Apr-09 12-Mar-09 TB09032093 E513506 09-NSD-001 1563.3 1564.3 0.022 02-Apr-09 12-Mar-09 TB09032093 E513507 09-NSD-001 1568.8 1569.8 0.027 02-Apr-09 12-Mar-09 TB09032093 E513508 09-NSD-001 1569.8 1570.8 0.038 02-Apr-09 12-Mar-09 TB09032093 E513509 09-NSD-001 1570.8 1571.8 0.048 02-Apr-09 12-Mar-09 TB09032093 E513511 09-NSD-001 1571.8 1572.8 0.016 02-Apr-09 12-Mar-09 TB09032093 E513512 09-NSD-001 1572.8 1573.8 0.0025 02-Apr-09 12-Mar-09 TB09032093 E513513 09-NSD-001 1573.8 1574.8 0.034 02-Apr-09 12-Mar-09 TB09032093 E513514 09-NSD-001 1574.8 1575.8 0.014 02-Apr-09 12-Mar-09 TB09032093 E513515 09-NSD-001 1575.8 1576.8 0.005 02-Apr-09 12-Mar-09 TB09032093 E513516 09-NSD-001 1582.3 1583.3 0.015 02-Apr-09 12-Mar-09 TB09032093 E513517 09-NSD-001 1583.3 1584.3 0.01 02-Apr-09 12-Mar-09 TB09032093 E513518 09-NSD-001 1584.3 1585 0.01 02-Apr-09 12-Mar-09 TB09032093 E513519 09-NSD-001 1585 1585.4 0.008 02-Apr-09 12-Mar-09 TB09032093 E513521 09-NSD-001 1585.4 1586.4 0.051 02-Apr-09 12-Mar-09 TB09032093 E513522 09-NSD-001 1586.4 1586.8 0.392 02-Apr-09 12-Mar-09 TB09032093 E513523 09-NSD-001 1586.8 1587.2 0.019 02-Apr-09 12-Mar-09 TB09032093 E513524 09-NSD-001 1587.2 1588.2 0.0025 02-Apr-09 12-Mar-09 TB09032093 E513525 09-NSD-001 1588.2 1589.2 0.0025 02-Apr-09 12-Mar-09 TB09032093 E513526 09-NSD-001 1601.9 1602.9 0.009 02-Apr-09 13-Mar-09 TB09032093 E513527 09-NSD-001 1602.9 1603.9 0.016 02-Apr-09 13-Mar-09 TB09032093 E513528 09-NSD-001 1603.9 1604.5 0.02 02-Apr-09 13-Mar-09 TB09032093 E513529 09-NSD-001 1604.5 1605 0.005 02-Apr-09 13-Mar-09
TB09032093 E513531 09-NSD-001 1605 1606 0.007 02-Apr-09 13-Mar-09 TB09032093 E513532 09-NSD-001 1606 1607 0.009 02-Apr-09 13-Mar-09 TB09032093 E513533 09-NSD-001 1607 1608 0.023 02-Apr-09 13-Mar-09 TB09032093 E513534 09-NSD-001 1608 1609 0.672 02-Apr-09 13-Mar-09 TB09032093 E513535 09-NSD-001 1609 1610 0.159 02-Apr-09 13-Mar-09 TB09032093 E513536 09-NSD-001 1619.8 1620.8 0.292 02-Apr-09 13-Mar-09 TB09032093 E513537 09-NSD-001 1620.8 1621.8 0.372 02-Apr-09 13-Mar-09 TB09032093 E513538 09-NSD-001 1621.8 1622.2 2.28 02-Apr-09 13-Mar-09 TB09032093 E513539 09-NSD-001 1622.2 1623 0.027 08-May-09 13-Mar-09 TB09032093 E513541 09-NSD-001 1623 1624 0.009 02-Apr-09 13-Mar-09 TB09032093 E513542 09-NSD-001 1624 1625 0.011 02-Apr-09 13-Mar-09 TB09032093 E513543 09-NSD-001 1625 1625.6 0.015 02-Apr-09 13-Mar-09 TB09032093 E513544 09-NSD-001 1625.6 1626.2 0.014 02-Apr-09 13-Mar-09 TB09032093 E513545 09-NSD-001 1626.2 1626.7 0.059 02-Apr-09 13-Mar-09 TB09032093 E513546 09-NSD-001 1626.7 1627.7 0.188 02-Apr-09 13-Mar-09 TB09032093 E513547 09-NSD-001 1627.7 1628.7 0.655 02-Apr-09 13-Mar-09 TB09032093 E513548 09-NSD-001 1628.7 1629.4 3.39 02-Apr-09 13-Mar-09 TB09032093 E513549 09-NSD-001 1629.4 1630 0.064 02-Apr-09 13-Mar-09 TB09032093 E513551 09-NSD-001 1630 1631 0.076 02-Apr-09 13-Mar-09 TB09032093 E513552 09-NSD-001 1631 1632 0.125 02-Apr-09 13-Mar-09 TB09032093 E513553 09-NSD-001 1632 1632.6 0.384 02-Apr-09 13-Mar-09 TB09032093 E513554 09-NSD-001 1632.6 1633 0.047 02-Apr-09 13-Mar-09 TB09032093 E513555 09-NSD-001 1633 1634 0.01 02-Apr-09 13-Mar-09 TB09032093 E513556 09-NSD-001 1634 1635 0.0025 02-Apr-09 13-Mar-09 TB09032093 E513557 09-NSD-001 1635 1636 0.0025 02-Apr-09 13-Mar-09 TB09032093 E513558 09-NSD-001 1636 1637 0.01 02-Apr-09 13-Mar-09 TB09032093 E513559 09-NSD-001 1637 1638 0.025 02-Apr-09 13-Mar-09 TB09044021 E513561 09-NSD-001 1638 1639 0.014 18-May-09 13-Mar-09 TB09044021 E513562 09-NSD-001 1639 1640 0.016 18-May-09 13-Mar-09 TB09044021 E513563 09-NSD-001 1640 1640.8 0.012 18-May-09 13-Mar-09 TB09044021 E513564 09-NSD-001 1640.8 1641.8 0.008 18-May-09 19-Mar-09 TB09044021 E513565 09-1\JSD-001 1641.8 1642.8 0.018 18-May-09 19-Mar-09 TB09044021 ES13566 09-1\JSD-001 1660.7 1661.7 0.025 18-May-09 19-Mar-09 TB09044021 E513567 09-NSD-001 1661.7 1662.7 0.032 18-May-09 19-Mar-09 TB09044021 E513568 09-NSD-001 1662.7 1663.5 0.02 18-May-09 19-Mar-09 TB09044021 E513569 09-NSD-001 1663.S 1664 0.015 18-May-09 19-Mar-09 TB09044021 E513571 09-NSD-001 1664 1665 0.032 18-May-09 19-Mar-09 TB09044021 E513572 09-NSD-001 1665 1666 0.012 18-May-09 19-Mar-09 TB09044021 E513573 09-NSD-001 1666 1666.7 0.956 18-May-09 19-Mar-09 TB09044021 E513574 09-1\JSD-001 1666.7 1667.7 0.031 18-May-09 19-Mar-09 TB09044021 E513575 09-NSD-001 1667.7 1668.7 0.024 18-May-09 19-Mar-09 TB09044021 E513576 09-NSD-001 1675 1676 0.007 18-May-09 19-Mar-09 TB09044021 E513577 09-NSD-001 1676 1677 0.0025 18-May-09 19-Mar-09 TB09044021 E513578 09-NSD-001 1677 1677.6 0.046 18-May-09 19-Mar-09 TB09044021 E513579 09-NSD-001 1677.6 1678.4 0.018 18-May-09 19-Mar-09 TB09044021 E513581 09-NSD-001 1678.4 1679 0.117 18-May-09 19-Mar-09 TB09044021 E513582 09-NSD-001 1679 1680 0.024 18-May-09 19-Mar-09 TB09044021 E513583 09-NSD-001 1680 1681 0.162 18-May-09 19-Mar-09 TB09044021 E513584 09-NSD-001 1681 1682 0.01 18-May-09 19-Mar-09 TB09044021 E513585 09-NSD-001 1682 1683 0.008 18-May-09 19-Mar-09
TB09044021 E513586 09-NSD-001 1683 1684 0.01 18-May-09 19-IVlar-09 TB09044021 E513587 09-NSD-001 1684 1684.4 0.007 18-May-09 19-Mar-09 TB09044021 E513588 09-NSD-001 1684.4 1685 0.01 18-May-09 19-Mar-09 TB09044021 E513589 09-NSD-001 1685 1686 0.015 18-May-09 19-Mar-09 TB09044021 E513591 09-NSD-001 1686 1686.6 0.007 18-May-09 19-Mar-09 TB09044021 E513592 09-NSD-001 1686.6 1687.3 0.385 18-May-09 19-Mar-09 TB09044021 E513593 09-NSD-001 1687.3 1688.3 0.033 18-May-09 19-Mar-09 TB09044021 E513594 09-NSD-001 1688.3 1689.3 0.016 18-May-09 19-Mar-09 TB09044021 E513595 09-NSD-001 1689.3 1689.8 0.033 18-May-09 19-Mar-09 TB09044021 E513596 09-NSD-001 1689.8 1690.4 0.014 18-May-09 19-Mar-09 TB09044021 E513597 09-NSD-001 1690.4 1691 0.01 18-May-09 19-Mar-09 TB09044021 E513598 09-NSD-001 1691 1692 0.009 18-May-09 19-Mar-09 TB09044021 E513599 09-NSD-001 1692 1693 3.8 18-May-09 19-Mar-09 TB09044021 E513601 09-NSD-001 1693 1694 0.277 18-May-09 19-Mar-09 TB09044021 E513602 09-NSD-001 1694 1694.7 0.01 18-May-09 19-Mar-09 TB09044021 E513603 09-NSD-001 1694.7 1695.7 0.03 18-May-09 19-Mar-09 TB09044021 E513604 09-NSD-001 1695.7 1696.5 0.013 18-May-09 19-Mar-09 TB09044021 E513605 09-NSD-001 1696.5 1697 0.011 18-May-09 19-Mar-09 TB09044021 E513606 09-NSD-001 1697 1698 0.012 18-May-09 19-Mar-09 TB09044021 E513607 09-NSD-001 1698 1698.7 0.011 18-May-09 19-Mar-09 TB09044021 E513608 09-NSD-001 1698.7 1699.4 0.0025 18-May-09 19-Mar-09 TB09044021 E513609 09-NSD-001 1699.4 1700 0.005 18-May-09 19-Mar-09 TB09044021 E513611 09-NSD-001 1700 1701 0.01 18-May-09 19-Mar-09 TB09044021 E513612 09-NSD-001 1701 1701.7 0.005 18-May-09 19-Mar-09 TB09044021 E513613 09-NSD-001 1701.7 1702.3 0.006 18-May-09 19-Mar-09 TB09044021 E513614 09-NSD-001 1702.3 1703.3 0.017 18-May-09 19-Mar-09 TB09044021 E513615 09-NSD-001 1703.3 1703.8 8.3 18-May-09 19-Mar-09 TB09044021 E513616 09-NSD-001 1703.8 1704.5 38.3 18-May-09 19-Mar-09 TB09044021 E513617 09-NSD-001 1704.5 1705 0.045 18-May-09 19-Mar-09 TB09044021 E513618 09-NSD-001 1705 1706 0.092 18-May-09 19-Mar-09 TB09044021 E513619 09-NSD-001 1706 1706.6 7.73 18-May-09 19-Mar-09 TB09044021 E513621 09-NSD-001 1706.6 1707.6 0.044 18-May-09 19-Mar-09 TB09044021 E513622 09-NSD-001 1707.6 1708.6 0.01 18-May-09 19-Mar-09 TB09044021 E513623 09-1\JSD-001 1721.5 1722.5 0.031 18-May-09 20-Mar-09 TB09044021 E513624 09-NSD-001 1722.5 1723.5 0.017 18-May-09 20-Mar-09 TB09044021 E513625 09-1\JSD-001 1723.5 1724.2 11.85 18-May-09 20-Mar-09 TB09044021 E531126 09-NSD-001 1724.2 1724.8 2.83 18-May-09 20-Mar-09 TB09044021 E531127 09-NSD-001 1724.8 1725.8 0.017 18-May-09 20-Mar-09 TB09044021 E531128 09-NSD-001 1725.8 1726.8 3.32 18-May-09 20-Mar-09 TB09044021 E531129 09-NSD-001 1757 1758 0.017 18-May-09 23-Mar-09 TB09044021 E531131 09-NSD-001 1758 1759 0.012 18-May-09 23-Mar-09 TB09044021 E531132 09-NSD-001 1759 1759.5 6.7 18-May-09 23-Mar-09 TB09044021 E531133 09-NSD-001 1759.5 1760.5 0.012 18-May-09 23-Mar-09 TB09044021 E531134 09-NSD-001 1760.5 1761.5 0.022 18-May-09 23-Mar-09 TB09044021 E531135 09-NSD-001 1769.6 1770.6 0.017 18-May-09 23-Mar-09 TB09044021 E531136 09-NSD-001 1770.6 1771.6 0.014 18-May-09 23-Mar-09 TB09044021 E531137 09-NSD-001 1771.6 1772.2 10.95 18-May-09 23-Mar-09 TB09044021 E531138 09-NSD-001 1772.2 1773.2 6.02 18-May-09 23-Mar-09 TB09044021 E531139 09-NSD-001 1773.2 1774.1 0.106 18-May-09 23-Mar-09 TB09044021 E531141 09-NSD-001 1774.1 1774.8 0.0025 18-May-09 23-Mar-09
TB09044021 E531142 09-NSD-001 1774.8 1775.5 0.011 18-May-09 23-Mar-09 TB09044021 E531143 09-NSD-001 1775.5 1776.2 0.007 18-May-09 23-Mar-09 TB09044021 E531144 09-NSD-001 1776.2 1777 0.066 18-May-09 23-Mar-09 TB09044021 E531145 09-NSD-001 1777 1778 0.019 18-May-09 23-Mar-09 TB09044021 E531146 09-NSD-001 1778 1778.5 0.339 18-May-09 23-Mar-09 TB09044021 E531147 09-NSD-001 1778.5 1779.3 7.24 18-May-09 23-Mar-09 TB09044021 E531148 09-NSD-001 1779.3 1780 2.15 18-May-09 23-Mar-09 TB09044021 E531149 09-NSD-001 1780 1780.6 0.795 18-May-09 23-Mar-09 TB09044021 E531151 09-NSD-001 1780.6 1781.6 0.1 18-May-09 23-Mar-09 TB09044021 E531152 09-NSD-001 1781.6 1782.6 0.012 18-May-09 23-Mar-09 TB09044021 E531153 09-NSD-001 1796.6 1797.6 0.03 18-May-09 23-Mar-09 TB09044021 E531154 09-NSD-001 1797.6 1798.6 0.028 18-May-09 23-Mar-09 TB09044021 E531155 09-NSD-001 1798.6 1799.2 0.083 18-May-09 23-Mar-09 TB09044021 E531156 09-NSD-001 1799.2 1800.2 0.092 18-May-09 23-Mar-09 TB09044021 E531157 09-NSD-001 1800.2 1801 0.108 18-IVlay-09 23-Mar-09 TB09044021 E531158 09-NSD-001 1801 1801.7 2.95 18-May-09 23-Mar-09 TB09044021 E531159 09-NSD-001 1801.7 1802.2 13.55 18-May-09 23-Mar-09 TB09044021 E531161 09-NSD-001 1802.2 1803 0.066 18-May-09 23-Mar-09 TB09044021 E531162 09-NSD-001 1803 1804 0.19 18-IVlay-09 23-Mar-09 TB09044021 E531163 09-NSD-001 1804 1804.7 0.071 18-May-09 23-Mar-09 TB09044021 E531164 09-NSD-001 1804.7 1805.7 0.182 18-May-09 23-Mar-09 TB09044021 E531165 09-NSD-001 1805.7 1806.7 0.019 18-May-09 23-Mar-09 TB09032091 E531166 09-NSD-001 1824.1 1824.6 0.011 02-Apr-09 28-Mar-09 TB09032091 E531167 09-NSD-001 1824.6 1825.2 0.225 02-Apr-09 28-Mar-09 TB09032091 E531168 09-NSD-001 1825.2 1826 0.013 02-Apr-09 28-Mar-09 TB09032091 E531169 09-NSD-001 1826 1826.8 0.029 02-Apr-09 28-Mar-09 TB09032091 E531171 09-NSD-001 1826.8 1827.8 3.44 02-Apr-09 28-Mar-09 TB09032091 E531172 09-NSD-001 1827.8 1828.8 3.46 02-Apr-09 28-Mar-09 TB09032091 E531173 09-NSD-001 1828.8 1829.3 1.04 02-Apr-09 28-Mar-09 TB09032091 E531174 09-NSD-001 1829.3 1830 2.09 02-Apr-09 28-Mar-09 TB09032091 E531175 09-NSD-001 1830 1831 1.83 02-Apr-09 28-Mar-09 TB09032091 E531176 09-NSD-001 1831 1831.6 0.589 02-Apr-09 28-Mar-09 TB09032091 E531177 09-NSD-001 1831.6 1832.3 0.241 02-Apr-09 28-Mar-09 TB09032091 E531178 09-NSD-001 1832.3 1833 0.823 02-Apr-09 28-Mar-09 TB09032091 E531179 09-NSD-001 1833 1833.5 1.28 02-Apr-09 28-Mar-09 TB09032091 E531181 09-NSD-001 1833.5 1834.5 0.384 02-Apr-09 28-Mar-09 TB09032091 E531182 09-NSD-001 1834.5 1835.5 0.278 02-Apr-09 28-Mar-09 TB09032091 E531183 09-NSD-001 1835.5 1836.5 7.29 02-Apr-09 28-Mar-09 TB09032091 E531184 09-NSD-001 1836.5 1837.5 0.377 02-Apr-09 28-Mar-09 TB09032091 E531185 09-NSD-001 1837.5 1838.5 0.381 02-Apr-09 28-Mar-09 TB09032091 E531186 09-NSD-001 1838.5 1839.5 0.165 02-Apr-09 28-Mar-09 TB09032091 E531187 09-NSD-001 1839.5 1840 0.021 02-Apr-09 28-Mar-09 TB09032091 E531188 09-NSD-001 1840 1840.3 0.01 02-Apr-09 28-Mar-09 TB09032091 E531189 09-NSD-001 1840.3 1841 0.011 02-Apr-09 28-Mar-09 TB09032092 E531191 09-NSD-001 1841 1841.5 0.006 22-Apr-09 28-Mar-09 TB09032092 E531192 09-NSD-001 1841.5 1842.S 0.009 22-Apr-09 28-Mar-09 TB09032092 E531193 09-NSD-001 1842.5 1843.5 0.1 22-Apr-09 28-Mar-09 TB09032092 E531194 09-NSD-001 1843.5 1844.5 0.057 22-Apr-09 28-Mar-09 TB09032092 E531195 09-NSD-001 1844.5 1845.5 0.01 22-Apr-09 28-Mar-09 TB09032092 E531196 09-NSD-001 1845.5 1846.5 0.033 22-Apr-09 28-Mar-09
TB09032092 E531197 09-NSD-001 1846.5 1847.5 0.49 22-Apr-09 28-Mar-09 TB09032092 E531198 09-NSD-001 1847.5 1848.5 0.259 22-Apr-09 28-Mar-09 TB09032092 E531199 09-NSD-001 1848.5 1849.5 0.061 22-Apr-09 28-Mar-09 TB09032092 E531201 09-NSD-001 1849.5 1850.5 1.015 22-Apr-09 28-Mar-09 TB09032092 E531202 09-NSD-001 1850.5 1851.5 0.467 22-Apr-09 28-Mar-09 TB09032092 E531203 09-NSD-001 1851.5 1852.5 1.81 22-Apr-09 28-Mar-09 TB09032092 E531204 09-NSD-001 1852.5 1853.5 0.251 22-Apr-09 28-Mar-09 TB09032092 E531205 09-NSD-001 1853.5 1854.5 0.056 22-Apr-09 28-Mar-09 TB09032092 E531206 09-NSD-001 1854.5 1855 0.173 22-Apr-09 28-Mar-09 TB09032092 ES31207 09-NSD-001 1855 1856 0.039 22-Apr-09 28-Mar-09 TB09032092 E531208 09-NSD-001 1856 1857 0.042 22-Apr-09 28-Mar-09 TB09032092 ES31209 09-NSD-001 1857 1858 0.006 22-Apr-09 28-Mar-09 TB09032092 E531211 09-NSD-001 1875 1876 0.005 22-Apr-09 28-Mar-09 TB09032092 E531212 09-NSD-001 1876 1876.8 0.008 22-Apr-09 28-Mar-09 TB09032092 E531213 09-NSD-001 1876.8 1877.4 0.061 22-Apr-09 28-Mar-09 TB09032092 ES31214 09-NSD-001 1877.4 1878 0.278 22-Apr-09 28-Mar-09 TB09032092 E531215 09-NSD-001 1878 1879 0.067 22-Apr-09 28-Mar-09 TB09032092 E531216 09-NSD-001 1879 1879.6 0.065 22-Apr-09 28-Mar-09 TB09044021 E531217 09-NSD-001 1879.6 1880.6 0.016 18-May-09 28-Mar-09 TB09044021 E531218 09-NSD-001 1880.6 1881.2 0.076 18-May-09 28-Mar-09 TB09044021 E531219 09-NSD-001 1881.2 1881.9 0.116 18-May-09 28-Mar-09 TB09044021 E531221 09-NSD-001 1881.9 1882.9 0.051 18-May-09 30-Mar-09 TB09044021 E531222 09-NSD-001 1882.9 1883.9 0.006 18-May-09 30-Mar-09 TB09044021 ES31223 09-NSD-001 1883.9 1885 0.0025 18-May-09 30-Mar-09 TB09044021 E531224 09-NSD-001 1927 1928 0.0025 18-May-09 30-Mar-09 TB09044021 E531225 09-NSD-001 1928 1928.9 0.005 18-May-09 30-Mar-09 TB09044021 E531226 09-NSD-001 1928.9 1929.2 0.025 18-May-09 30-Mar-09 TB09044021 E531227 09-NSD-001 1929.2 1930.1 0.035 18-May-09 30-Mar-09 TB09044021 E531228 09-NSD-001 1930.1 1931 0.029 18-May-09 30-Mar-09 TB09044021 E531229 09-NSD-001 1931 1932 0.014 18-May-09 30-Mar-09 TB09044021 E531231 09-NSD-001 1932 1933 0.039 18-May-09 30-Mar-09 TB09044021 E531232 09-NSD-001 1933 1933.9 0.076 18-May-09 30-Mar-09 TB09044021 E531233 09-NSD-001 1933.9 1934.3 0.201 18-May-09 30-Mar-09 TB09044021 E531234 09-NSD-001 1934.3 1935 0.072 18-May-09 30-Mar-09 TB09044021 E531235 09-NSD-001 1935 1936 0.012 18-May-09 30-Mar-09 TB09044021 E531236 09-NSD-001 1936 1937 0.023 18-May-09 30-Mar-09 TB09044021 E531237 09-1\ISD-001 1937 1938 0.023 18-May-09 30-Mar-09 TB09044021 E531238 09-1\ISD-001 1938 1939 0.08 18-May-09 30-Mar-09 TB09044021 E531239 09-NSD-001 1939 1939.5 0.05 18-May-09 30-Mar-09 TB09044021 E531241 09-1\ISD-001 1939.5 1940.5 0.076 18-May-09 30-Mar-09 TB09044021 E531242 09-NSD-001 1940.5 1941.6 0.1 18-May-09 30-Mar-09 TB09044021 E531243 09-NSD-001 1941.6 1942.4 0.011 18-May-09 30-Mar-09 TB09044021 E531244 09-1\ISD-001 1942.4 1943 0.016 18-May-09 30-Mar-09 TB09044021 E531245 09-1\ISD-001 1943 1943.4 0.04 18-May-09 30-Mar-09 TB09044021 E531246 09-NSD-001 1943.4 1944 0.017 18-May-09 30-Mar-09 TB09044021 E531247 09-NSD-001 1944 1945 0.015 18-May-09 30-Mar-09 TB09032094 E531251 09-NSD-001 1463.9 1464.9 0.0025 02-Apr-09 06-Mar-09 TB09032094 ES31252 09-NSD-001 1464.9 1465.9 0.0025 02-Apr-09 06-Mar-09 TB09032094 E531253 09-NSD-001 1465.9 1466.5 0.074 02-Apr-09 06-Mar-09 TB09032094 E531254 09-NSD-001 1466.5 1467 0.061 02-Apr-09 06-Mar-09
TB09032094 E531255 09-NSD-001 1467 1468 0.02 02-Apr-09 06-Mar-09 TB09032094 E531256 09-NSD-001 1468 1469 0.103 02-Apr-09 06-Mar-09 TB09032094 E531257 09-NSD-001 1469 1470 0.022 02-Apr-09 06-Mar-09 TB09032094 E531258 09-NSD-001 1470 1471 0.014 02-Apr-09 06-Mar-09 TB09032094 E531259 09-NSD-001 1471 1472 0.016 02-Apr-09 06-Mar-09 TB09032094 E531261 09-NSD-001 1472 1473 0.027 02-Apr-09 06-Mar-09 TB09032094 E531262 09-NSD-001 1473 1474 0.012 02-Apr-09 06-Mar-09 TB09032094 E531263 09-NSD-001 1474 1475 0.013 02-Apr-09 06-Mar-09 TB09032094 E531264 09-NSD-001 1475 1476.1 0.013 02-Apr-09 06-Mar-09 TB09032094 E531265 09-NSD-001 1476.1 1477.1 0.028 02-Apr-09 06-Mar-09 TB09032094 E531266 09-NSD-001 1477.1 1478.1 0.006 02-Apr-09 06-Mar-09 TB09032094 E531267 09-NSD-001 1534 1534.5 0.006 02-Apr-09 09-Mar-09 TB09032094 E531268 09-NSD-001 1534.5 1535.5 0.007 02-Apr-09 09-Mar-09 TB09032094 E531269 09-NSD-001 1535.5 1536.4 0.196 02-Apr-09 09-Mar-09 TB09032094 E531271 09-NSD-001 1536.4 1537 0.011 02-Apr-09 09-Mar-09 TB09032094 E531272 09-NSD-001 1537 1537.5 0.016 02-Apr-09 09-Mar-09 TB09032094 E531273 09-NSD-001 1537.5 1538.5 0.027 02-Apr-09 09-Mar-09 TB09032094 E531274 09-I\JSD-001 1538.5 1539.1 0.495 02-Apr-09 09-Mar-09 TB09032094 E531275 09-1\JSD-001 1539.1 1539.8 0.024 02-Apr-09 09-Mar-09 TB09032094 E531276 09-NSD-001 1539.8 1540.8 0.62 02-Apr-09 09-Mar-09 TB09032094 E531277 09-1\JSD-001 1540.8 1541.8 0.021 02-Apr-09 09-Mar-09 TB09032094 E531278 09-1\JSD-001 1541.8 1542.5 0.009 02-Apr-09 09-Mar-09 TB09032094 E531279 09-NSD-001 1542.5 1543.5 0.157 02-Apr-09 09-Mar-09 TB09032094 E531281 09-NSD-001 1543.5 1544.5 0.02 02-Apr-09 09-Mar-09 TB09032094 E531282 09-NSD-001 1544.5 1545.5 0.858 02-Apr-09 09-Mar-09 TB09032094 E531283 09-NSD-001 1545.5 1545.9 0.158 02-Apr-09 09-Mar-09 TB09032094 E531284 09-NSD-001 1545.9 1546.3 0.084 02-Apr-09 09-Mar-09 TB09032094 E531285 09-NSD-001 1546.3 1547 0.346 02-Apr-09 09-Mar-09 TB09032094 E531286 09-NSD-001 1547 1548 0.234 02-Apr-09 09-Mar-09 TB09032094 E531287 09-NSD-001 1548 1549 0.093 02-Apr-09 12-Mar-09 TB09032094 E531288 09-NSD-001 1549 1550 0.028 02-Apr-09 12-Mar-09 TB09032094 E531289 09-NSD-001 1550 1550.7 0.017 02-Apr-09 12-Mar-09 TB09032094 E531291 09-NSD-001 1550.7 1551.7 0.034 02-Apr-09 12-Mar-09 TB09032094 E531292 09-NSD-001 1551.7 1552.4 0.041 02-Apr-09 12-Mar-09 TB09032094 E531293 09-NSD-001 1552.4 1553.4 0.044 02-Apr-09 12-Mar-09 TB09032094 E531294 09-NSD-001 1553.4 1554.1 0.06 02-Apr-09 12-Mar-09 TB09032094 E531295 09-NSD-001 1554.1 1555 0.027 02-Apr-09 12-Mar-09 TB09032094 E531296 09-NSD-001 1555 1556 0.343 02-Apr-09 12-Mar-09 TB09032094 E531297 09-NSD-001 1556 1557 0.223 02-Apr-09 12-Mar-09 TB09032094 E531298 09-NSD-001 1557 1558 0.03 02-Apr-09 12-Mar-09 TB09032094 E531299 09-NSD-001 1558 1559 0.043 02-Apr-09 12-Mar-09
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample Weight
LOG-22 Sample login - Rcd w/o BarCode
CRU-31 Fine crushing - 70% <2mm
CRU-QC Crushing QC Test
PUL-QC Pulverizing QC Test
SPL-21 Split sample - riffle splitter
PUL-31 Pulverize split to 85% <75 um
LOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08052738
This report is for 100 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 28-APR-2008.
Project: MUSSELWHITE
P.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JIM EDWARDSMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 21-MAY-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 4 (A)
Finalized Date: 21-MAY-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08052738
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E466439 2.65 0.014E466440 1.34 <0.005E466441 2.20 0.013E466442 2.79 0.007E466443 2.86 0.005
E466444 1.96 0.010E466445 1.80 0.010E466446 1.69 0.008E466447 1.63 0.006E466448 2.45 0.005
E466449 2.44 0.020E466450 0.08 3.20E466451 2.61 0.013E466452 1.17 <0.005E466453 2.55 0.008
E466454 2.63 0.008E466455 1.47 0.005E466456 1.66 0.016E466457 2.20 <0.005E466458 2.74 0.006
E466459 2.32 0.007E466460 1.69 <0.005E466461 2.55 <0.005E466462 1.68 0.006E466463 1.23 <0.005
E466464 1.95 0.005E466465 2.24 0.009E466466 2.00 0.007E466467 1.57 <0.005E466468 2.78 0.005
E466469 2.74 0.007E466470 0.08 7.08E466471 2.29 0.019E466472 2.35 0.012E466473 1.90 0.020
E466474 2.38 0.017E466475 2.34 <0.005E466476 2.23 0.010E466477 2.38 0.028E466478 0.81 0.008
Page: 3 - ATotal # Pages: 4 (A)
Finalized Date: 21-MAY-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08052738
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E466479 2.95 0.030E466480 1.45 <0.005E466481 2.54 0.006E466482 2.56 0.020E466483 1.27 0.051
E466484 1.25 0.029E466485 2.97 0.074E466486 1.98 0.034E466487 1.64 0.101E466488 1.05 0.162
E466489 2.72 0.228E466490 0.08 3.20E466491 1.81 0.157E466492 2.05 0.041E466493 1.44 0.062
E466494 1.59 0.034E466495 2.17 0.013E466496 1.60 <0.005E466497 3.05 0.021E466498 2.78 0.028
E466499 2.83 0.027E466500 1.56 <0.005E466501 2.79 0.006E466502 2.37 0.009E466503 2.25 0.005
E466504 2.07 <0.005E466505 2.26 <0.005E466506 2.63 0.014E466507 2.25 0.010E466508 2.91 <0.005
E466509 2.92 <0.005E466510 0.08 3.01E466511 2.11 0.047E466512 1.17 0.096E466513 1.77 0.078
E466514 2.31 0.016E466515 1.09 0.159E466516 1.47 0.032E466517 2.24 0.007E466518 2.81 0.017
Page: 4 - ATotal # Pages: 4 (A)
Finalized Date: 21-MAY-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08052738
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E466519 1.12 0.026E466520 1.32 <0.005E466521 2.97 0.017E466522 2.67 0.010E466523 1.87 0.014
E466524 2.51 0.014E466525 1.64 <0.005E466526 1.32 <0.005E466527 1.58 <0.005E466528 2.43 <0.005
E466529 1.89 0.013E466530 0.08 7.14E466531 2.62 0.007E466532 2.10 0.007E466533 2.79 0.025
E466534 1.60 0.009E466535 2.64 <0.005E466536 2.47 0.023E466537 2.31 0.544E466538 2.28 0.285
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08096496
This report is for 60 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 15-JUL-2008.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 2-AUG-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 2-AUG-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08096496
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466694 2.90 0.025E466695 3.18 0.029E466696 2.59 0.018E466697 1.82 0.031E466698 2.89 0.093
E466699 1.88 0.024E466700 1.45 <0.005E466701 1.31 0.007E466702 2.66 0.019E466703 2.47 0.010
E466704 2.71 0.037E466705 2.47 <0.005E466706 2.65 0.090E466707 2.69 0.061E466708 2.79 0.019
E466709 2.32 0.008E466710 0.08 3.27E466711 2.32 <0.005E466712 2.43 <0.005E466713 2.78 <0.005
E466714 2.53 <0.005E466715 2.90 0.009E466716 2.52 0.304E466717 2.49 0.082E466718 1.65 1.115
E466719 2.11 0.018E466720 1.50 0.005E466721 2.92 0.011E466722 2.45 0.208E466723 2.37 0.198
E466724 1.36 0.038E466725 2.51 <0.005E466726 2.58 0.011E466727 1.87 0.141E466728 1.23 0.017
E466729 2.94 0.149E466730 0.08 7.21E466731 2.29 0.019E466732 2.22 0.009E466733 1.47 0.011
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 2-AUG-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08096496
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466734 1.01 0.012E466735 1.98 0.005E466736 1.70 0.014E466737 2.44 0.009E466738 1.31 0.669
E466739 1.55 0.027E466740 1.65 0.007E466741 1.12 0.057E466742 2.07 0.025E466743 2.40 0.008
E466744 2.22 0.021E466745 0.97 0.140E466746 2.49 0.011E466747 2.53 <0.005E466748 2.69 <0.005
E466749 2.59 0.037E466750 0.10 3.09E466751 1.89 0.020E466752 2.68 0.006E466753 2.50 <0.005
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08096495
This report is for 60 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 15-JUL-2008.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 29-JUL-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 29-JUL-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08096495
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466634 2.19 <0.005E466635 2.31 0.005E466636 1.64 0.021E466637 1.76 0.018E466638 1.55 0.005
E466639 2.26 0.007E466640 1.55 <0.005E466641 2.47 <0.005E466642 1.30 <0.005E466643 2.92 <0.005
E466644 2.39 0.011E466645 2.04 0.006E466646 1.87 0.017E466647 1.48 <0.005E466648 2.27 0.009
E466549 2.59 <0.005E466650 0.08 3.09E466651 2.38 0.005E466652 2.12 0.375E466653 1.98 0.166
E466654 2.57 0.005E466655 2.41 0.007E466656 2.44 0.006E466657 2.44 <0.005E466658 2.28 0.024
E466659 2.53 0.115E466660 1.50 <0.005E466661 2.36 0.017E466662 2.29 0.009E466663 2.36 0.006
E466664 2.65 0.050E466665 2.37 0.032E466666 2.48 0.012E466667 2.50 0.005E466668 2.24 0.007
E466669 2.27 0.006E466670 0.08 7.68E466671 2.17 0.012E466672 2.49 0.047E466673 2.35 0.024
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 29-JUL-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08096495
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466674 1.80 0.039E466675 2.68 0.019E466676 2.10 0.014E466677 1.22 0.012E466678 2.47 <0.005
E466679 2.60 <0.005E466680 1.48 <0.005E466681 2.46 0.007E466682 2.41 0.009E466683 2.63 0.007
E466684 2.34 0.027E466685 1.53 0.065E466686 1.44 0.628E466687 1.26 0.293E466688 1.54 0.655
E466689 1.42 0.069E466690 0.08 3.16E466691 2.68 0.035E466692 2.88 0.881E466693 2.75 0.030
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with BarcodeDRY-21 High Temperature Drying
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08068690
This report is for 15 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 28-MAY-2008.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 5-JUN-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 2 (A)
Finalized Date: 5-JUN-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08068690
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466619 2.94 0.007E466620 1.85 <0.005E466621 1.97 0.012E466622 1.89 0.108E466623 1.92 0.067
E466624 1.96 0.049E466625 2.55 0.017E466626 2.92 0.029E466627 2.94 0.126E466628 2.86 <0.005
E466629 1.82 0.053E466630 0.08 7.09E466631 1.63 0.157E466632 2.17 0.009E466633 2.49 <0.005
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample Weight
CRU-QC Crushing QC Test
LOG-22 Sample login - Rcd w/o BarCode
PUL-QC Pulverizing QC Test
CRU-31 Fine crushing - 70% <2mm
SPL-21 Split sample - riffle splitter
PUL-31 Pulverize split to 85% <75 um
LOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08133367
This report is for 80 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 22-SEP-2008.
Project: MUSSELWHITE
P.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 20-OCT-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 20-OCT-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08133367
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E466776 2.72 0.007E466777 2.66 <0.005E466778 2.47 0.008E466779 2.41 <0.005E466780 0.42 <0.005
E466781 2.21 <0.005E466782 1.67 <0.005E466783 1.49 <0.005E466784 1.64 0.007E466785 2.55 <0.005
E466786 1.85 0.015E466787 2.42 0.008E466788 1.41 0.090E466789 1.75 0.045E466790 0.08 3.22
E466791 2.32 0.009E466792 2.59 0.006E466793 2.58 0.017E466794 2.67 0.007E466795 2.86 0.027
E466796 1.30 0.152E466797 1.31 0.329E466798 2.42 0.012E466799 2.35 <0.005E466800 0.46 <0.005
E466801 2.16 <0.005E466802 1.10 <0.005E466803 2.36 <0.005E466804 2.27 0.011E466805 1.50 <0.005
E466806 2.41 0.011E466807 2.44 0.005E466808 2.62 <0.005E466809 2.00 0.005E466810 0.08 3.25
E466811 2.80 0.005E466812 2.38 <0.005E466813 1.35 0.011E466814 2.79 <0.005E466815 2.65 0.007
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 20-OCT-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08133367
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E466816 2.32 0.030E466817 2.45 0.090E466818 2.52 0.040E466819 2.45 0.083E466820 0.61 <0.005
E466821 2.55 0.049E466822 2.38 0.156E466823 2.39 0.097E466824 2.71 0.578E466825 2.89 0.064
E466826 2.01 0.114E466827 2.29 0.027E466828 2.25 0.056E466829 1.58 0.047E466830 0.08 7.27
E466831 1.97 0.048E466832 1.22 0.438E466833 1.89 0.042E466834 3.10 0.206E466835 1.52 0.099
E468156 2.78 <0.005E468157 1.63 <0.005E468158 2.00 0.013E468159 1.66 0.134E468160 1.80 <0.005
E468161 2.05 0.010E468162 2.21 0.038E468163 2.24 0.046E468164 3.06 0.012E468165 3.20 0.022
E468166 1.52 0.333E468167 2.46 0.125E468168 3.24 0.010E468169 2.97 0.006E468170 0.08 7.54
E468171 2.58 0.008E468172 1.39 0.013E468173 2.46 0.052E468174 2.17 0.018E468175 1.79 0.375
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08123787
This report is for 42 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 2-SEP-2008.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 12-SEP-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 12-SEP-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08123787
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E468106 3.21 0.103E468107 1.95 0.014E468108 2.00 0.006E468109 1.56 0.074E468110 0.07 3.17
E468111 2.80 0.048E468112 2.66 0.134E468113 2.78 0.010E468114 2.58 0.296E468115 2.55 0.285
E468116 2.72 0.154E468117 2.90 0.159E468118 2.85 0.295E468119 2.75 0.049E468120 1.70 0.017
E468121 3.01 0.048E468122 1.76 0.048E468123 2.52 0.061E468124 1.81 0.009E468125 1.67 <0.005
E468126 2.50 0.014E468127 2.00 0.053E468128 3.24 0.022E468129 2.49 <0.005E468130 0.07 7.20
E468131 2.42 0.010E468132 2.36 <0.005E468133 2.05 0.005E468134 2.66 0.137E468135 1.35 0.127
E468136 2.37 0.008E468137 2.20 0.005E468138 2.25 <0.005E468139 2.17 <0.005E468140 1.44 <0.005
E468141 1.99 0.155E468142 2.63 0.005E468143 2.23 0.005E468144 2.67 <0.005E468153 2.60 0.008
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 12-SEP-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08123787
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E468154 1.79 2.91E468155 2.73 <0.005
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08123786
This report is for 8 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 2-SEP-2008.
Project: MESSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JIM EDWARDSMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 9-SEP-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 2 (A)
Finalized Date: 9-SEP-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MESSELWHITE
CERTIFICATE OF ANALYSIS TB08123786
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E468145 2.86 0.008E468146 2.11 0.010E468147 1.74 <0.005E468148 1.82 0.081E468149 1.67 0.008
E468150 0.08 3.35E468151 2.48 0.013E468152 2.35 0.008
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08120968
This report is for 20 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 25-AUG-2008.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JIM EDWARDSMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 10-SEP-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 2 (A)
Finalized Date: 10-SEP-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08120968
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E468086 2.81 0.020E468087 2.53 0.065E468088 2.31 0.009E468089 2.46 0.015E468090 0.08 3.30
E468091 2.64 0.006E468092 2.17 0.006E468093 1.85 <0.005E468094 1.13 0.082E468095 1.60 0.006
E468096 2.66 0.007E468097 1.19 0.007E468098 2.19 0.023E468099 2.08 0.010E468100 1.68 <0.005
E468101 1.60 0.008E468102 2.80 0.071E468103 1.27 0.008E468104 2.14 0.005E468105 2.78 0.017
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08119994
This report is for 99 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 25-AUG-2008.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 12-SEP-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 4 (A)
Finalized Date: 12-SEP-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08119994
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466754 2.48 0.009E466755 1.77 0.009E466756 1.59 0.012E466757 2.76 0.011E466758 1.30 0.046
E466759 1.38 0.015E466760 1.38 <0.005E466761 1.81 0.005E466762 1.83 0.006E466763 2.24 0.008
E466764 0.83 0.006E466765 1.97 0.007E466766 1.44 0.005E466767 2.20 0.007E468001 2.56 <0.005
E468002 2.37 0.007E468003 1.95 0.005E468004 2.44 0.008E468005 2.15 0.039E468006 2.08 <0.005
E468007 2.41 0.006E468008 0.99 <0.005E468009 1.14 0.005E468010 0.07 3.17E468011 0.86 0.006
E468012 2.43 0.007E468013 2.51 0.005E468014 1.16 0.005E468015 2.42 0.092E468016 2.82 0.005
E468017 2.70 0.006E468018 2.54 <0.005E468019 2.75 0.005E468020 0.84 <0.005E468021 0.83 <0.005
E468022 2.71 0.005E468023 2.74 <0.005E468024 2.71 <0.005E468025 1.39 <0.005E468026 2.65 <0.005
Page: 3 - ATotal # Pages: 4 (A)
Finalized Date: 12-SEP-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08119994
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E468027 2.57 <0.005E468028 3.02 0.007E468029 2.71 0.007E468030 0.08 6.93E468031 2.47 0.008
E468032 1.29 <0.005E468033 1.41 0.006E468034 2.61 0.006E468035 2.52 0.005E468036 2.80 0.005
E468037 2.30 0.020E468038 2.23 0.016E468039 1.71 1.150E468040 1.99 <0.005E468041 1.77 0.065
E468042 2.33 0.012E468043 2.20 0.015E468044 2.40 0.050E468045 2.75 0.015E468046 2.33 0.020
E468047 2.31 0.082E468048 2.63 0.031E468049 2.20 0.031E468050 0.08 3.02E468051 2.46 0.019
E468052 2.23 2.74E468053 1.65 0.099E468054 1.65 0.734E468055 2.85 0.023E468056 3.03 0.006
E468057 2.02 <0.005E468058 1.55 0.011E468059 2.65 0.007E468060 1.88 <0.005E468061 2.98 <0.005
E468062 3.10 0.005E468063 2.79 0.007E468064 3.19 0.011E468065 1.87 0.012E468066 1.83 0.010
Page: 4 - ATotal # Pages: 4 (A)
Finalized Date: 12-SEP-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08119994
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E468067 2.62 0.022E468068 2.60 0.012E468069 2.63 0.010E468070 0.08 7.12E468071 1.51 0.015
E468072 1.63 0.036E468073 2.16 0.035E468074 2.35 0.026E468075 2.24 0.134E468076 2.33 0.034
E468077 1.54 0.070E468078 1.68 0.113E468079 1.93 0.011E468080 1.47 <0.005E468081 1.75 0.750
E468082 2.96 0.028E468083 2.42 0.015E468084 1.82 0.021E468085 1.93 0.079
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with BarcodeDRY-21 High Temperature Drying
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Co-AA61 AASTrace Co - four-acid digestionCu-AA61 AASTrace Cu - four-acid digestionNi-AA61 AASTrace Ni - four-acid digestionPGM-ICP23 ICP-AESPt, Pd, Au 30g FA ICPAu-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08045641
This report is for 81 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 14-APR-2008.
Project: MusselwhiteP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JIM EDWARDSMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 6-MAY-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 4 (A)
Finalized Date: 6-MAY-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: Musselwhite
CERTIFICATE OF ANALYSIS TB08045641
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23 Co-AA61 Cu-AA61 Ni-AA61 PGM-ICP23 PGM-ICP23 PGM-ICP23Recvd Wt. Au Co Cu Ni Au Pt Pd
kg ppm ppm ppm ppm ppm ppm ppm0.02 0.005 5 2 5 0.001 0.005 0.001
E466358 2.28 <0.005E466359 2.00 0.005E466360 1.10 <0.005E466361 1.30 0.008E466362 2.88 0.040
E466363 1.65 0.020E466364 1.59 0.075E466365 1.91 0.838E466366 1.63 0.019E466367 3.36 0.042
E466368 2.62 0.247E466369 2.85 0.007E466370 0.08 6.95E466371 3.13 0.010E466372 2.80 0.088
E466373 3.11 0.113E466374 3.64 0.037E466375 2.81 0.048E466376 2.99 0.033E466377 2.95 <0.005
E466378 1.87 0.019E466379 2.31 0.005E466380 1.29 <0.005E466381 2.29 0.010E466382 2.37 0.007
E466383 2.36 0.005E466384 2.85 0.006E466385 2.41 <0.005E466386 2.32 <0.005E466387 2.21 <0.005
E466388 2.62 <0.005E466389 2.04 <0.005E466390 0.08 3.09E466391 2.57 0.007E466392 3.00 <0.005
E466393 2.51 <0.005E466394 2.57 0.005E466395 2.44 <0.005E466396 1.44 <0.005E466397 1.72 0.014
Page: 3 - ATotal # Pages: 4 (A)
Finalized Date: 6-MAY-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: Musselwhite
CERTIFICATE OF ANALYSIS TB08045641
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23 Co-AA61 Cu-AA61 Ni-AA61 PGM-ICP23 PGM-ICP23 PGM-ICP23Recvd Wt. Au Co Cu Ni Au Pt Pd
kg ppm ppm ppm ppm ppm ppm ppm0.02 0.005 5 2 5 0.001 0.005 0.001
E466398 1.78 0.168E466399 2.53 0.052E466400 1.42 <0.005E466401 2.74 17 157 9 1.620 <0.005 0.001E466402 2.81 9 114 <5 0.319 <0.005 <0.001
E466403 1.72 5 26 <5 0.139 <0.005 <0.001E466404 1.05 8.47E466405 2.63 0.521E466406 1.89 0.325E466407 3.00 0.055
E466408 1.73 0.009E466409 1.81 8 94 <5 0.287 <0.005 <0.001E466410 0.08 16 35 22 2.97 <0.005 <0.001E466411 1.89 22 76 5 0.180 <0.005 <0.001E466412 1.60 10 12 <5 0.322 <0.005 <0.001
E466413 1.68 9 4 <5 0.693 <0.005 <0.001E466414 2.84 63 369 40 0.750 <0.005 <0.001E466415 2.34 35 169 19 0.362 <0.005 0.001E466416 1.13 28 38 138 0.136 0.007 0.008E466417 3.06 0.022
E466418 2.21 <0.005E466419 2.95 <0.005E466420 1.62 <0.005E466421 1.70 0.006E466422 2.83 <0.005
E466423 3.05 <0.005E466424 1.76 0.006E466425 3.04 <0.005E466426 2.46 <0.005E466427 3.96 <0.005
E466428 3.39 <0.005E466429 1.25 <0.005E466430 0.08 7.11E466431 3.12 0.005E466432 3.14 <0.005
E466433 2.50 <0.005E466434 2.22 0.038E466435 2.58 0.081E466436 1.66 0.008E466437 0.79 0.074
Page: 4 - ATotal # Pages: 4 (A)
Finalized Date: 6-MAY-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: Musselwhite
CERTIFICATE OF ANALYSIS TB08045641
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23 Co-AA61 Cu-AA61 Ni-AA61 PGM-ICP23 PGM-ICP23 PGM-ICP23Recvd Wt. Au Co Cu Ni Au Pt Pd
kg ppm ppm ppm ppm ppm ppm ppm0.02 0.005 5 2 5 0.001 0.005 0.001
E466438 2.38 <0.005
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample Weight
CRU-QC Crushing QC Test
LOG-22 Sample login - Rcd w/o BarCode
PUL-QC Pulverizing QC Test
CRU-31 Fine crushing - 70% <2mm
SPL-21 Split sample - riffle splitter
PUL-31 Pulverize split to 85% <75 um
LOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08133367
This report is for 80 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 22-SEP-2008.
Project: MUSSELWHITE
P.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 20-OCT-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 20-OCT-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08133367
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E466776 2.72 0.007E466777 2.66 <0.005E466778 2.47 0.008E466779 2.41 <0.005E466780 0.42 <0.005
E466781 2.21 <0.005E466782 1.67 <0.005E466783 1.49 <0.005E466784 1.64 0.007E466785 2.55 <0.005
E466786 1.85 0.015E466787 2.42 0.008E466788 1.41 0.090E466789 1.75 0.045E466790 0.08 3.22
E466791 2.32 0.009E466792 2.59 0.006E466793 2.58 0.017E466794 2.67 0.007E466795 2.86 0.027
E466796 1.30 0.152E466797 1.31 0.329E466798 2.42 0.012E466799 2.35 <0.005E466800 0.46 <0.005
E466801 2.16 <0.005E466802 1.10 <0.005E466803 2.36 <0.005E466804 2.27 0.011E466805 1.50 <0.005
E466806 2.41 0.011E466807 2.44 0.005E466808 2.62 <0.005E466809 2.00 0.005E466810 0.08 3.25
E466811 2.80 0.005E466812 2.38 <0.005E466813 1.35 0.011E466814 2.79 <0.005E466815 2.65 0.007
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 20-OCT-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08133367
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E466816 2.32 0.030E466817 2.45 0.090E466818 2.52 0.040E466819 2.45 0.083E466820 0.61 <0.005
E466821 2.55 0.049E466822 2.38 0.156E466823 2.39 0.097E466824 2.71 0.578E466825 2.89 0.064
E466826 2.01 0.114E466827 2.29 0.027E466828 2.25 0.056E466829 1.58 0.047E466830 0.08 7.27
E466831 1.97 0.048E466832 1.22 0.438E466833 1.89 0.042E466834 3.10 0.206E466835 1.52 0.099
E468156 2.78 <0.005E468157 1.63 <0.005E468158 2.00 0.013E468159 1.66 0.134E468160 1.80 <0.005
E468161 2.05 0.010E468162 2.21 0.038E468163 2.24 0.046E468164 3.06 0.012E468165 3.20 0.022
E468166 1.52 0.333E468167 2.46 0.125E468168 3.24 0.010E468169 2.97 0.006E468170 0.08 7.54
E468171 2.58 0.008E468172 1.39 0.013E468173 2.46 0.052E468174 2.17 0.018E468175 1.79 0.375
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08155438
This report is for 52 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 30-OCT-2008.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JIM EDWARDSMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 6-NOV-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 6-NOV-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08155438
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E467011 2.55 <0.005E467012 2.67 0.005E467024 2.52 0.072E467025 2.14 0.055E467026 0.78 0.912
E467027 1.96 0.030E467028 2.19 0.026E467029 2.62 0.046E467030 0.07 7.15E467031 2.30 0.016
E467032 2.39 0.015E467033 2.30 0.020E467034 1.89 2.93E467035 2.54 0.314E467036 2.88 0.194
E467037 2.60 0.014E467038 2.21 0.025E467039 1.95 0.031E467040 0.61 <0.005E467041 2.62 0.989
E467042 2.50 0.034E467043 2.48 0.097E467044 2.68 0.898E467045 1.57 0.021E467046 1.41 0.089
E467047 3.14 0.076E467048 2.96 0.233E467049 2.51 0.437E467050 0.07 3.14E467051 1.43 0.028
E467052 2.06 0.705E467053 2.04 1.315E467054 0.71 1.175E467055 2.31 0.014E467056 2.25 0.011
E467057 1.89 0.020E467058 1.20 0.032E467059 1.47 0.008E467060 0.43 <0.005E467061 1.57 <0.005
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 6-NOV-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08155438
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E467062 3.00 0.161E467063 2.76 0.072E467064 3.07 0.028E467065 2.79 0.066E467066 2.41 0.108
E467067 1.38 0.022E467068 2.70 0.017E467069 2.67 0.021E467070 0.07 6.86E467071 2.63 0.020
E467072 2.28 0.021E467073 2.57 0.016
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08141162
This report is for 60 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 2-OCT-2008.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 21-OCT-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 21-OCT-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08141162
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466951 2.99 0.012E466952 2.59 <0.005E466953 2.60 <0.005E466954 1.63 0.007E466955 1.55 0.013
E466956 2.94 <0.005E466957 2.88 0.030E466958 2.80 0.343E466959 3.01 0.042E466960 0.49 <0.005
E466961 3.28 <0.005E466962 2.70 0.006E466963 2.86 <0.005E466964 2.92 <0.005E466965 2.74 0.007
E466966 2.03 <0.005E466967 2.39 0.007E466968 2.42 0.013E466969 2.16 <0.005E466970 0.08 7.15
E466971 2.70 0.018E466972 2.35 0.078E466973 3.36 <0.005E466974 2.72 <0.005E466975 2.95 <0.005
E466976 3.09 <0.005E466977 3.15 <0.005E466978 3.53 <0.005E466P79 3.14 0.009E466980 0.85 <0.005
E466981 2.23 0.005E466982 1.93 0.028E466983 1.60 0.247E466984 2.89 0.060E466985 3.42 0.023
E466986 2.60 0.006E466987 2.43 0.005E466988 2.22 0.009E466989 1.76 0.046E466990 0.08 3.02
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 21-OCT-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08141162
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466991 2.69 0.029E466992 2.46 0.016E466993 2.50 0.013E466994 2.40 0.009E466995 2.51 0.011
E466996 0.89 0.087E466997 1.00 0.021E466998 1.28 0.009E466999 2.09 0.010E467000 1.22 <0.005
E467001 2.36 0.014E467002 2.40 0.016E467003 2.53 0.096E467004 2.54 0.007E467005 2.33 <0.005
E467006 2.36 <0.005E467007 2.45 <0.005E467008 1.55 0.016E467009 0.96 <0.005E467010 0.08 3.07
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with BarcodeDRY-21 High Temperature Drying
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08138859
This report is for 115 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 29-SEP-2008.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 22-OCT-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 4 (A)
Finalized Date: 22-OCT-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08138859
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466836 2.33 0.010E466837 2.01 0.023E466838 2.29 0.023E466839 2.23 0.022E466840 1.02 <0.005
E466841 1.84 0.012E466842 2.29 0.016E466843 2.08 0.019E466844 0.93 0.063E466845 1.68 0.015
E466846 2.45 0.041E466847 2.47 0.050E466848 2.29 0.046E466849 1.61 0.028E466850 0.08 3.19
E466851 1.48 0.014E466852 1.62 0.460E466853 2.48 0.079E466854 2.32 0.170E466855 2.59 0.068
E466856 1.78 0.025E466857 2.48 0.023E466858 2.49 0.034E466859 2.42 0.032E466860 0.85 <0.005
E466861 2.60 0.029E466862 3.09 0.032E466863 1.45 0.024E466864 3.28 0.070E466865 2.46 0.074
E466866 3.12 0.023E466867 1.87 0.113E466868 1.93 0.055E466869 2.33 0.070E466870 0.08 7.17
E466871 2.34 0.030E466872 1.24 0.025E466873 2.14 1.365E466874 1.96 0.015E466875 1.93 0.083
Page: 3 - ATotal # Pages: 4 (A)
Finalized Date: 22-OCT-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08138859
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466876 2.08 0.028E466877 2.57 0.022E466878 2.53 0.016E466879 2.51 0.017E466880 0.85 <0.005
E466881 2.50 0.025E466882 2.51 0.037E466883 1.46 0.041E466884 2.62 0.029E466885 1.80 0.033
E466886 2.78 0.176E466887 2.42 0.027E466888 1.54 0.038E466889 2.70 0.177E466890 0.08 3.32
E466891 2.92 0.194E466892 3.00 0.366E466893 2.62 0.562E466894 2.77 0.159E466895 1.75 0.252
E466896 2.85 1.215E466897 1.74 0.470E466898 1.68 0.023E466899 1.73 0.146E466900 0.62 0.006
E466901 1.96 0.017F466902 1.75 0.011E466903 1.92 0.016E466904 2.18 0.013E466905 3.39 0.007
E466906 2.67 0.012E466907 1.53 0.011E466908 2.52 0.005E466909 2.34 0.034E466910 0.08 3.16
E466911 2.86 0.520E466912 2.61 0.019E466913 2.46 0.803E466914 3.63 0.538E466915 2.54 0.016
Page: 4 - ATotal # Pages: 4 (A)
Finalized Date: 22-OCT-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08138859
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E466916 2.49 0.033E466917 2.80 0.635E466918 2.58 0.589E466919 2.69 0.378E466920 0.82 0.009
E466921 2.30 0.683E466922 2.42 0.375E466923 2.92 0.430E466924 2.55 0.042E466925 2.66 0.363
E466926 1.66 1.280E466927 2.34 0.377E466928 2.05 0.630E466929 2.48 0.169E466930 0.08 6.90
E466931 2.03 0.082E466932 1.28 0.071E466933 2.25 4.61E466934 1.80 2.21E466935 2.36 0.035
E466936 2.03 0.080E466937 2.26 <0.005E466938 1.12 0.029E466939 2.99 <0.005E466940 0.89 <0.005
E466941 2.63 0.012E466942 0.91 0.009E466943 1.92 0.005E466944 2.35 <0.005E466945 1.41 0.010
E466946 2.00 0.018E466947 1.55 0.009E466948 3.62 0.006E466949 2.60 0.008E466950 0.08 3.22
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08155438
This report is for 52 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 30-OCT-2008.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JIM EDWARDSMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 6-NOV-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 6-NOV-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08155438
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E467011 2.55 <0.005E467012 2.67 0.005E467024 2.52 0.072E467025 2.14 0.055E467026 0.78 0.912
E467027 1.96 0.030E467028 2.19 0.026E467029 2.62 0.046E467030 0.07 7.15E467031 2.30 0.016
E467032 2.39 0.015E467033 2.30 0.020E467034 1.89 2.93E467035 2.54 0.314E467036 2.88 0.194
E467037 2.60 0.014E467038 2.21 0.025E467039 1.95 0.031E467040 0.61 <0.005E467041 2.62 0.989
E467042 2.50 0.034E467043 2.48 0.097E467044 2.68 0.898E467045 1.57 0.021E467046 1.41 0.089
E467047 3.14 0.076E467048 2.96 0.233E467049 2.51 0.437E467050 0.07 3.14E467051 1.43 0.028
E467052 2.06 0.705E467053 2.04 1.315E467054 0.71 1.175E467055 2.31 0.014E467056 2.25 0.011
E467057 1.89 0.020E467058 1.20 0.032E467059 1.47 0.008E467060 0.43 <0.005E467061 1.57 <0.005
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 6-NOV-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08155438
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E467062 3.00 0.161E467063 2.76 0.072E467064 3.07 0.028E467065 2.79 0.066E467066 2.41 0.108
E467067 1.38 0.022E467068 2.70 0.017E467069 2.67 0.021E467070 0.07 6.86E467071 2.63 0.020
E467072 2.28 0.021E467073 2.57 0.016
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample Weight
CRU-QC Crushing QC Test
PUL-QC Pulverizing QC Test
LOG-22 Sample login - Rcd w/o BarCode
CRU-31 Fine crushing - 70% <2mm
SPL-21 Split sample - riffle splitter
PUL-31 Pulverize split to 85% <75 um
LOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB08166930
This report is for 127 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 26-NOV-2008.
Project: MUSSELWHITE
P.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK JIM EDWARDS MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 9-DEC-2008
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 5 (A)
Finalized Date: 9-DEC-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08166930
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E467074 2.50 0.344E467075 2.30 0.079E467076 2.56 0.019E467077 2.41 0.024E467078 2.28 0.023
E467079 2.37 0.010E467080 0.97 <0.005E467081 2.27 0.009E467082 2.21 0.012E467083 1.69 0.012
E467084 2.32 0.010E467085 1.77 0.014E467086 1.37 0.009E467087 1.87 0.029E467088 1.77 0.016
E467089 2.54 0.152E467090 0.10 3.07E467091 1.53 0.094E467092 2.66 0.045E467093 1.55 0.206
E467094 2.91 0.473E467095 2.30 0.271E467096 1.44 0.031E467097 2.88 0.451E467098 1.91 0.019
E4Y7099 2.11 0.010E467100 1.03 0.008E467101 1.41 0.008E467102 2.59 0.023E467103 1.58 1.695
E467104 2.11 0.101E467105 0.82 0.107E467106 2.46 0.517E467107 1.44 0.014E467108 2.67 0.036
E467109 2.58 0.071E467110 0.07 3.13E467111 2.74 0.034E467112 2.98 0.330E467113 2.28 0.037
Page: 3 - ATotal # Pages: 5 (A)
Finalized Date: 9-DEC-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08166930
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E467114 2.36 0.025E467115 2.36 0.022E467116 2.70 0.359E467117 2.42 4.41E467118 2.62 0.179
E467119 2.57 2.44E467120 0.93 0.013E467121 1.48 0.029E467122 1.99 0.011E467123 2.63 0.023
E467124 1.26 0.019E467125 1.83 1.530E467126 2.83 0.440E467127 2.71 1.640E467128 2.89 0.119
E467129 2.68 4.04E467130 0.08 6.61E467131 1.12 3.04E467132 2.98 0.596E467133 2.51 2.000
E467134 2.50 0.615E467135 2.25 1.200E467136 1.47 0.748E467137 2.23 1.410E467138 1.47 0.622
E467139 2.18 0.031E467140 0.73 0.006E467141 2.72 0.012E467142 2.48 0.012E467143 2.44 0.066
E467144 1.76 <0.005E467145 3.29 0.006E467146 2.82 0.008E467147 2.57 0.006E467148 2.65 0.007
E467149 1.01 <0.005E467150 0.08 3.30E467151 2.55 0.008E467152 2.28 <0.005E467153 2.97 0.005
Page: 4 - ATotal # Pages: 5 (A)
Finalized Date: 9-DEC-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08166930
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E467154 3.35 <0.005E467155 3.36 0.006E467156 3.10 0.723E467157 3.27 0.006E467158 3.52 0.007
E467159 2.98 0.008E467160 1.04 <0.005E467161 3.21 0.036E467162 3.37 0.060E467163 2.89 0.039
E467164 1.92 <0.005E467165 1.36 0.007E467166 2.92 0.005E467167 2.66 0.010E467168 2.96 0.006
E467169 1.62 0.009E467170 0.07 7.16E467171 2.19 0.013E467172 3.16 0.006E467173 3.37 0.005
E467174 3.77 <0.005E467175 3.19 0.052E467176 3.27 0.031E467177 1.20 0.573E467178 1.91 0.056
E467179 2.69 0.103E467180 0.85 <0.005E467181 1.29 0.503E467182 1.84 0.364E467183 2.60 0.354
E467184 2.71 0.005E467185 2.47 0.007E467186 0.81 0.368E467187 2.49 0.006E467188 2.33 0.005
E467189 1.03 0.005E467190 0.07 3.19E467191 2.74 0.006E467192 1.73 <0.005E467193 1.23 <0.005
Page: 5 - ATotal # Pages: 5 (A)
Finalized Date: 9-DEC-2008Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB08166930
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E467194 2.11 <0.005E467195 1.86 0.006E467196 0.91 <0.005E467197 1.22 <0.005E467198 1.28 <0.005
E467199 2.72 <0.005E467200 1.55 <0.005
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB09032093
This report is for 60 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 2-APR-2009.
Project: P.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK ANNE CARRAUD JIM EDWARDS
MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JOHN BICZOKMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 14-APR-2009
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 14-APR-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
CERTIFICATE OF ANALYSIS TB09032093
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E513501 2.04 0.060E513502 2.34 0.195E513503 1.56 0.661E513504 1.06 0.074E513505 2.21 0.011
E513506 2.39 0.022E513507 2.03 0.027E513508 2.13 0.038E513509 2.28 0.048E513510 0.07 3.28
E513511 2.31 0.016E513512 2.23 <0.005E513513 2.28 0.034E513514 2.28 0.014E513515 2.04 0.005
E513516 2.03 0.015E513517 2.05 0.010E513518 1.36 0.010E513519 0.95 0.008E513520 1.07 <0.005
E513521 2.03 0.051E513522 0.80 0.392E513523 0.87 0.019E513524 2.23 <0.005E513525 2.01 <0.005
E513526 1.37 0.009E513527 1.96 0.016E513528 1.15 0.020E513529 1.18 0.005E513530 0.08 7.52
E513531 2.29 0.007E513532 2.27 0.009E513533 2.24 0.023E513534 2.00 0.672E513535 1.97 0.159
E513536 1.96 0.292E513537 2.41 0.372E513538 1.00 2.28H513539 2.26 0.027E513540 0.91 0.009
Comments: SAMPLES SPLIT UP BY LINE FROM SAMPLE SUBMITTAL FORMS
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 14-APR-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
CERTIFICATE OF ANALYSIS TB09032093
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E513541 2.47 0.009E513542 2.56 0.011E513543 1.25 0.015E513544 1.67 0.014E513545 1.49 0.059
E513546 2.19 0.188E513547 2.47 0.655E513548 1.70 3.39E513549 1.80 0.064E513550 0.07 3.38
E513551 2.25 0.076E513552 2.43 0.125E513553 1.37 0.384E513554 1.41 0.047E513555 2.66 0.010
E513556 2.62 <0.005E513557 2.96 <0.005E513558 2.70 0.010E513559 2.56 0.025E513560 0.92 <0.005
Comments: SAMPLES SPLIT UP BY LINE FROM SAMPLE SUBMITTAL FORMS
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB09032092
This report is for 27 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 2-APR-2009.
Project: P.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK ANNE CARRAUD JIM EDWARDS
MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: ANNE CARRAUDMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 9-APR-2009
This copy reported on 14-APR-2009Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 2 (A)
Finalized Date: 9-APR-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
CERTIFICATE OF ANALYSIS TB09032092
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E531190 0.08 3.16E531191 1.16 0.006E531192 2.10 0.009E531193 2.63 0.100E531194 2.22 0.057
E531195 3.00 0.010E531196 2.71 0.033E531197 2.54 0.490E531198 3.00 0.259E531199 2.60 0.061
E531200 0.49 <0.005E531201 2.65 1.015E531202 2.55 0.467E531203 2.65 1.810E531204 2.75 0.251
E531205 3.05 0.056E531206 1.33 0.173E531207 2.63 0.039E531208 1.96 0.042E531209 2.42 0.006
E531210 0.08 3.08E531211 2.26 0.005E531212 1.72 0.008E531213 1.38 0.061E531214 1.72 0.278
E531215 2.60 0.067E531216 1.56 0.065
Comments: SAMPLES SPLIT UP BY LINE FROM SAMPLE SUBMITTAL FORMS
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umDRY-21 High Temperature Drying
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB09032091
This report is for 24 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 2-APR-2009.
Project: MUSSELWHITE (NSD-001)P.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK ANNE CARRAUD JIM EDWARDS
MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: ANNE CARRAUDMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 6-APR-2009
This copy reported on 14-APR-2009Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 2 (A)
Finalized Date: 6-APR-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE (NSD-001)
CERTIFICATE OF ANALYSIS TB09032091
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E531166 1.01 0.011E531167 1.54 0.225E531168 1.90 0.013E531169 1.98 0.029E531170 0.08 6.92
E531171 2.88 3.44E531172 2.76 3.46E531173 1.46 1.040E531174 1.64 2.09E531175 2.58 1.830
E531176 1.63 0.589E531177 1.68 0.241E531178 1.87 0.823E531179 1.41 1.280E531180 0.69 <0.005
E531181 2.63 0.384E531182 2.82 0.278E531183 2.75 7.29E531184 2.49 0.377E531185 2.81 0.381
E531186 2.89 0.165E531187 2.13 0.021E531188 0.85 0.010E531189 1.83 0.011
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finishAu-GRA21 WST-SIMAu 30g FA-GRAV finish
CERTIFICATE TB09044021
This report is for 191 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 5-MAY-2009.
Project: MUSSELWHITEP.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK ANNE CARRAUD JIM EDWARDS
MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: ANNE CARRAUDMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 17-MAY-2009
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 6 (A)
Finalized Date: 17-MAY-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB09044021
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23 Au-GRA21Recvd Wt. Au Au
kg ppm ppm0.02 0.005 0.05
E513451 2.43 <0.005E513452 2.43 <0.005E513453 1.87 <0.005E513454 1.93 <0.005E513455 2.11 <0.005
E513456 2.17 <0.005E513457 2.07 <0.005E513458 2.14 0.205E513459 1.18 0.090E513460 1.46 <0.005
E513461 1.87 0.749E513462 2.00 0.034E513463 2.38 0.009E513464 2.05 0.018E513465 1.99 0.851
E513466 2.41 0.514E513467 1.86 1.795E513468 1.84 0.472E513469 1.66 0.863E513470 0.08 7.10
E513471 1.13 0.360E513472 0.98 0.126E513473 1.75 0.007E513474 1.37 0.009E513561 2.21 0.014
E513562 2.56 0.016E513563 1.75 0.012E513564 2.16 0.008E513565 2.42 0.018E513566 2.19 0.025
E513567 2.00 0.032E513568 1.41 0.020E513569 1.10 0.015E513570 0.08 7.01E513571 2.18 0.032
E513572 2.49 0.012E513573 1.57 0.956E513574 2.23 0.031E513575 2.20 0.024E513576 1.87 0.007
Page: 3 - ATotal # Pages: 6 (A)
Finalized Date: 17-MAY-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB09044021
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23 Au-GRA21Recvd Wt. Au Au
kg ppm ppm0.02 0.005 0.05
E513577 1.88 <0.005E513578 1.29 0.046E513579 1.89 0.018E513580 1.37 <0.005E513581 1.29 0.117
E513582 2.33 0.024E513583 2.60 0.162E513584 2.30 0.010E513585 2.20 0.008E513586 2.40 0.010
E513587 0.75 0.007E513588 1.31 0.010E513589 2.12 0.015E513590 0.08 3.19E513591 1.12 0.007
E513592 1.77 0.385E513593 2.11 0.033E513594 2.17 0.016E513595 1.27 0.033E513596 1.13 0.014
E513597 1.50 0.010E513598 1.94 0.009E513599 2.47 3.80E513600 1.70 0.016E513601 2.19 0.277
E513602 1.60 0.010E513603 2.13 0.030E513604 1.89 0.013E513605 1.12 0.011E513606 2.11 0.012
E513607 1.67 0.011E513608 1.49 <0.005E513609 1.29 0.005E513610 0.08 3.49E513611 2.39 0.010
E513612 1.11 0.005E513613 1.19 0.006E513614 2.54 0.017E513615 1.12 8.30E513616 1.44 >10.0 38.3
Page: 4 - ATotal # Pages: 6 (A)
Finalized Date: 17-MAY-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB09044021
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23 Au-GRA21Recvd Wt. Au Au
kg ppm ppm0.02 0.005 0.05
E513617 1.04 0.045E513618 1.97 0.092E513619 1.33 7.73E513620 0.95 0.009E513621 2.11 0.044
E513622 2.61 0.010E513623 1.95 0.031E513624 2.24 0.017E513625 1.48 >10.0 11.85E530586 2.36 0.019
E530587 2.77 0.022E530588 2.21 0.021E530589 2.37 0.025E530590 0.08 3.25E530591 2.16 0.017
E530592 2.15 0.008E530593 2.34 0.008E530594 1.36 0.008E530595 1.48 0.006E530596 1.99 0.011
E530597 2.13 <0.005E530598 2.78 <0.005E531001 2.41 0.008E531002 2.27 0.007E531003 1.14 0.006
E531004 2.33 0.005E531005 2.35 <0.005E531006 2.30 <0.005E531007 2.13 <0.005E531008 1.19 0.005
E531009 2.41 0.005E531010 0.08 3.29E531011 2.45 0.009E531012 1.40 <0.005E531013 1.00 <0.005
E531014 2.37 <0.005E531015 2.67 <0.005E531016 2.83 <0.005E531017 2.28 <0.005E531018 2.37 <0.005
Page: 5 - ATotal # Pages: 6 (A)
Finalized Date: 17-MAY-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB09044021
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23 Au-GRA21Recvd Wt. Au Au
kg ppm ppm0.02 0.005 0.05
E531126 1.26 2.83E531127 2.24 0.017E531128 2.35 3.32E531129 1.84 0.017E531130 0.08 7.35
E531131 2.38 0.012E531132 1.27 6.70E531133 2.07 0.012E531134 1.86 0.022E531135 2.08 0.017
E531136 2.00 0.014E531137 1.03 >10.0 10.95E531138 2.92 6.02E531139 1.70 0.106E531140 1.10 0.005
E531141 1.48 <0.005E531142 1.37 0.011E531143 1.45 0.007E531144 2.18 0.066E531145 2.40 0.019
E531146 1.04 0.339E531147 2.05 7.24E531148 1.85 2.15E531149 1.40 0.795E531150 0.08 3.26
E531151 1.81 0.100E531152 1.96 0.012E531153 2.02 0.030E531154 1.76 0.028E531155 1.39 0.083
E531156 2.06 0.092E531157 1.83 0.108E531158 1.82 2.95E531159 1.12 >10.0 13.55E531160 1.80 0.009
E531161 2.16 0.066E531162 1.24 0.190E531163 2.13 0.071E531164 1.75 0.182E531165 1.93 0.019
Page: 6 - ATotal # Pages: 6 (A)
Finalized Date: 17-MAY-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Project: MUSSELWHITE
CERTIFICATE OF ANALYSIS TB09044021
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23 Au-GRA21Recvd Wt. Au Au
kg ppm ppm0.02 0.005 0.05
E531217 1.83 0.016E531218 2.62 0.076E531219 1.68 0.116E531220 1.50 <0.005E531221 1.83 0.051
E531222 2.17 0.006E531223 1.92 <0.005E531224 2.28 <0.005E531225 1.65 0.005E531226 0.97 0.025
E531227 2.50 0.035E531228 2.69 0.029E531229 2.84 0.014E531230 0.08 7.39E531231 2.67 0.039
E531232 2.24 0.076E531233 1.39 0.201E531234 1.72 0.072E531235 2.67 0.012E531236 2.53 0.023
E531237 2.70 0.023E531238 2.75 0.080E531239 1.41 0.050E531240 1.24 <0.005E531241 2.65 0.076
E531242 1.97 0.100E531243 1.92 0.011E531244 1.54 0.016E531245 1.15 0.040E531246 1.46 0.017
E531247 2.73 0.015
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample Weight
CRU-QC Crushing QC Test
PUL-QC Pulverizing QC Test
LOG-22 Sample login - Rcd w/o BarCode
CRU-31 Fine crushing - 70% <2mm
SPL-21 Split sample - riffle splitter
PUL-31 Pulverize split to 85% <75 um
LOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB09032094
This report is for 50 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 2-APR-2009.
Project:
P.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK ANNE CARRAUD JIM EDWARDS
MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: ANNE CARRAUDMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 11-APR-2009
This copy reported on 14-APR-2009Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 11-APR-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
CERTIFICATE OF ANALYSIS TB09032094
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E531251 2.31 <0.005E531252 2.20 <0.005E531253 1.72 0.074E531254 1.19 0.061E531255 2.25 0.020
E531256 2.41 0.103E531257 2.45 0.022E531258 2.40 0.014E531259 2.43 0.016E531260 1.55 <0.005
E531261 2.41 0.027E531262 2.31 0.012E531263 2.27 0.013E531264 2.76 0.013E531265 2.26 0.028
E531266 2.39 0.006E531267 1.21 0.006E531268 2.08 0.007E531269 2.11 0.196E531270 0.07 7.14
E531271 1.50 0.011E531272 1.35 0.016E531273 2.34 0.027E531274 1.60 0.495E531275 1.74 0.024
E531276 2.36 0.620E531277 2.36 0.021E531278 1.83 0.009E531279 2.64 0.157E531280 1.59 <0.005
E531281 2.16 0.020E531282 2.41 0.858E531283 1.10 0.158E531284 0.94 0.084E531285 1.50 0.346
E531286 2.69 0.234E531287 2.36 0.093E531288 2.04 0.028E531289 1.79 0.017E531290 0.08 3.27
Comments: SAMPLES SPLIT UP BY LINE FROM SAMPLE SUBMITTAL FORMS
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 11-APR-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
CERTIFICATE OF ANALYSIS TB09032094
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23
Recvd Wt. Au
kg ppm
0.02 0.005
E531291 2.40 0.034E531292 1.60 0.041E531293 2.59 0.044E531294 1.58 0.060E531295 2.08 0.027
E531296 2.31 0.343E531297 2.23 0.223E531298 2.14 0.030E531299 2.17 0.043E531300 1.02 <0.005
Comments: SAMPLES SPLIT UP BY LINE FROM SAMPLE SUBMITTAL FORMS
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB09032093
This report is for 60 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 2-APR-2009.
Project: P.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK ANNE CARRAUD JIM EDWARDS
MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: ANNE CARRAUDMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 14-APR-2009
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 14-APR-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
CERTIFICATE OF ANALYSIS TB09032093
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E513501 2.04 0.060E513502 2.34 0.195E513503 1.56 0.661E513504 1.06 0.074E513505 2.21 0.011
E513506 2.39 0.022E513507 2.03 0.027E513508 2.13 0.038E513509 2.28 0.048E513510 0.07 3.28
E513511 2.31 0.016E513512 2.23 <0.005E513513 2.28 0.034E513514 2.28 0.014E513515 2.04 0.005
E513516 2.03 0.015E513517 2.05 0.010E513518 1.36 0.010E513519 0.95 0.008E513520 1.07 <0.005
E513521 2.03 0.051E513522 0.80 0.392E513523 0.87 0.019E513524 2.23 <0.005E513525 2.01 <0.005
E513526 1.37 0.009E513527 1.96 0.016E513528 1.15 0.020E513529 1.18 0.005E513530 0.08 7.52
E513531 2.29 0.007E513532 2.27 0.009E513533 2.24 0.023E513534 2.00 0.672E513535 1.97 0.159
E513536 1.96 0.292E513537 2.41 0.372E513538 1.00 2.28H513539 2.26 0.027E513540 0.91 0.009
Comments: SAMPLES SPLIT UP BY LINE FROM SAMPLE SUBMITTAL FORMS
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 14-APR-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
CERTIFICATE OF ANALYSIS TB09032093
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E513541 2.47 0.009E513542 2.56 0.011E513543 1.25 0.015E513544 1.67 0.014E513545 1.49 0.059
E513546 2.19 0.188E513547 2.47 0.655E513548 1.70 3.39E513549 1.80 0.064E513550 0.07 3.38
E513551 2.25 0.076E513552 2.43 0.125E513553 1.37 0.384E513554 1.41 0.047E513555 2.66 0.010
E513556 2.62 <0.005E513557 2.96 <0.005E513558 2.70 0.010E513559 2.56 0.025E513560 0.92 <0.005
Comments: SAMPLES SPLIT UP BY LINE FROM SAMPLE SUBMITTAL FORMS
ALS CODE DESCRIPTION
SAMPLE PREPARATION
WEI-21 Received Sample WeightCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-31 Pulverize split to 85% <75 umLOG-23 Pulp Login - Rcvd with Barcode
ALS CODE DESCRIPTION INSTRUMENT
ANALYTICAL PROCEDURES
Au-AA23 AASAu 30g FA-AA finish
CERTIFICATE TB09032093
This report is for 60 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 2-APR-2009.
Project: P.O. No.: WA9F00124
The following have access to data associated with this certificate:JOHN BICZOK ANNE CARRAUD JIM EDWARDS
MUSSELWHITE WEB ACCOUNT
GOLDCORP INC. - MUSSELWHITEATTN: JIM EDWARDSMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
Page: 1Finalized Date: 14-APR-2009
Account: OPB
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature:
Colin Ramshaw, Vancouver Laboratory Manager
ALS Chemex
Page: 2 - ATotal # Pages: 3 (A)
Finalized Date: 14-APR-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
CERTIFICATE OF ANALYSIS TB09032093
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E513501 2.04 0.060E513502 2.34 0.195E513503 1.56 0.661E513504 1.06 0.074E513505 2.21 0.011
E513506 2.39 0.022E513507 2.03 0.027E513508 2.13 0.038E513509 2.28 0.048E513510 0.07 3.28
E513511 2.31 0.016E513512 2.23 <0.005E513513 2.28 0.034E513514 2.28 0.014E513515 2.04 0.005
E513516 2.03 0.015E513517 2.05 0.010E513518 1.36 0.010E513519 0.95 0.008E513520 1.07 <0.005
E513521 2.03 0.051E513522 0.80 0.392E513523 0.87 0.019E513524 2.23 <0.005E513525 2.01 <0.005
E513526 1.37 0.009E513527 1.96 0.016E513528 1.15 0.020E513529 1.18 0.005E513530 0.08 7.52
E513531 2.29 0.007E513532 2.27 0.009E513533 2.24 0.023E513534 2.00 0.672E513535 1.97 0.159
E513536 1.96 0.292E513537 2.41 0.372E513538 1.00 2.28H513539 2.26 0.027E513540 0.91 0.009
Comments: SAMPLES SPLIT UP BY LINE FROM SAMPLE SUBMITTAL FORMS
Page: 3 - ATotal # Pages: 3 (A)
Finalized Date: 14-APR-2009Account: OPB
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.
212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com
GOLDCORP INC. - MUSSELWHITEMUSSELWHITE MINEPO BOX 7500THUNDER BAY ON P7B 6S8
To:
CERTIFICATE OF ANALYSIS TB09032093
ALS Chemex
Sample Description
MethodAnalyteUnitsLOR
WEI-21 Au-AA23Recvd Wt. Au
kg ppm0.02 0.005
E513541 2.47 0.009E513542 2.56 0.011E513543 1.25 0.015E513544 1.67 0.014E513545 1.49 0.059
E513546 2.19 0.188E513547 2.47 0.655E513548 1.70 3.39E513549 1.80 0.064E513550 0.07 3.38
E513551 2.25 0.076E513552 2.43 0.125E513553 1.37 0.384E513554 1.41 0.047E513555 2.66 0.010
E513556 2.62 <0.005E513557 2.96 <0.005E513558 2.70 0.010E513559 2.56 0.025E513560 0.92 <0.005
Comments: SAMPLES SPLIT UP BY LINE FROM SAMPLE SUBMITTAL FORMS
DDH # Check Sample # TYPE Au g/t Analyis Date
07‐NSD‐008 E466260 GRBLANK 0.006 4‐Feb‐08
07‐NSD‐008 E466280 GRBLANK 0.0025 15‐Feb‐08
07‐NSD‐008 E466300 GRBLANK 0.0025 19‐Mar‐08
07‐NSD‐008 E466320 GRBLANK 0.0025 19‐Mar‐08
07‐NSD‐008 E466340 GRBLANK 0.0025 19‐Mar‐08
07‐NSD‐008 E466360 GRBLANK 0.0025 14‐Apr‐08
07‐NSD‐008 E466380 GRBLANK 0.0025 14‐Apr‐08
07‐NSD‐008 E466400 GRBLANK 0.0025 14‐Apr‐08
07‐NSD‐008 E466420 GRBLANK 0.0025 14‐Apr‐08
07‐NSD‐008 E466290 STD900 3.08 15‐Feb‐08
07‐NSD‐008 E466310 STD900 3.14 19‐Mar‐08
07‐NSD‐008 E466350 STD900 3.22 19‐Mar‐08
07‐NSD‐008 E466390 STD900 3.09 14‐Apr‐08
07‐NSD‐008 E466410 STD900 N/A 14‐Apr‐08
07‐NSD‐008 E466270 STD999 7.31 4‐Feb‐08
07‐NSD‐008 E466330 STD999 7.29 19‐Mar‐08
07‐NSD‐008 E466370 STD999 6.95 14‐Apr‐08
07‐NSD‐008 E466430 STD999 7.11 14‐Apr‐08
08‐NSD‐001 E466440 GRBLANK 0.0025 28‐Apr‐08
08‐NSD‐001 E466460 GRBLANK 0.0025 28‐Apr‐08
08‐NSD‐001 E466480 GRBLANK 0.0025 28‐Apr‐08
08‐NSD‐001 E466500 GRBLANK 0.0025 28‐Apr‐08
08‐NSD‐001 E466520 GRBLANK 0.0025 28‐Apr‐08
08‐NSD‐001 E466540 GRBLANK 0.0025 28‐Apr‐08
08‐NSD‐001 E466560 GRBLANK 0.0025 28‐Apr‐08
08‐NSD‐001 E466580 GRBLANK 0.0025 28‐Apr‐08
08‐NSD‐001 E466600 GRBLANK 0.009 28‐Apr‐08
08‐NSD‐001 E466620 GRBLANK 0.0025 28‐May‐08
08‐NSD‐001 E466640 GRBLANK 0.0025 15‐Jul‐08
08‐NSD‐001 E466660 GRBLANK 0.0025 15‐Jul‐08
08‐NSD‐001 E466680 GRBLANK 0.0025 15‐Jul‐08
08‐NSD‐001 E466700 GRBLANK 0.0025 15‐Jul‐08
08‐NSD‐001 E466720 GRBLANK 0.005 15‐Jul‐08
08‐NSD‐001 E466740 GRBLANK 0.007 15‐Jul‐08
08‐NSD‐001 E466450 STD900 3.2 28‐Apr‐08
08‐NSD‐001 E466490 STD900 3.2 28‐Apr‐08
08‐NSD‐001 E466510 STD900 3.01 28‐Apr‐08
08‐NSD‐001 E466550 STD900 3.3 28‐Apr‐08
08‐NSD‐001 E466590 STD900 2.68 28‐Apr‐08
08‐NSD‐001 E466610 STD900 2.81 28‐Apr‐08
QAQC SAMPLES SORTED BY HOLE #
08‐NSD‐001 E466650 STD900 3.09 15‐Jul‐08
08‐NSD‐001 E466690 STD900 3.16 15‐Jul‐08
08‐NSD‐001 E466710 STD900 3.27 15‐Jul‐08
08‐NSD‐001 E466750 STD900 3.09 15‐Jul‐08
08‐NSD‐001 E466470 STD999 7.08 28‐Apr‐08
08‐NSD‐001 E466530 STD999 7.14 28‐Apr‐08
08‐NSD‐001 E466570 STD999 6.64 28‐Apr‐08
08‐NSD‐001 E466630 STD999 7.09 28‐May‐08
08‐NSD‐001 E466670 STD999 7.68 15‐Jul‐08
08‐NSD‐001 E466730 STD999 7.21 15‐Jul‐08
08‐NSD‐002 E466760 GRBLANK 0.0025 25‐Aug‐08
08‐NSD‐002 E468020 GRBLANK 0.0025 25‐Aug‐08
08‐NSD‐002 E468040 GRBLANK 0.0025 25‐Aug‐08
08‐NSD‐002 E468060 GRBLANK 0.0025 25‐Aug‐08
08‐NSD‐002 E468080 GRBLANK 0.0025 25‐Aug‐08
08‐NSD‐002 E468100 GRBLANK 0.0025 25‐Aug‐08
08‐NSD‐002 E468120 GRBLANK 0.017 2‐Sep‐08
08‐NSD‐002 E468140 GRBLANK 0.0025 2‐Sep‐08
08‐NSD‐002 E466780 GRBLANK 0.0025 22‐Sep‐08
08‐NSD‐002 E466800 GRBLANK 0.0025 22‐Sep‐08
08‐NSD‐002 E466820 GRBLANK 0.0025 22‐Sep‐08
08‐NSD‐002 E468160 GRBLANK 0.0025 22‐Sep‐08
08‐NSD‐002 E468010 STD900 3.17 25‐Aug‐08
08‐NSD‐002 E468050 STD900 3.02 25‐Aug‐08
08‐NSD‐002 E468090 STD900 3.3 25‐Aug‐08
08‐NSD‐002 E468110 STD900 3.17 2‐Sep‐08
08‐NSD‐002 E468150 STD900 3.35 2‐Sep‐08
08‐NSD‐002 E466790 STD900 3.22 22‐Sep‐08
08‐NSD‐002 E466810 STD900 3.25 22‐Sep‐08
08‐NSD‐002 E468030 STD999 6.93 25‐Aug‐08
08‐NSD‐002 E468070 STD999 7.12 25‐Aug‐08
08‐NSD‐002 E468130 STD999 7.2 2‐Sep‐08
08‐NSD‐002 E466830 STD999 7.27 22‐Sep‐08
08‐NSD‐002 E468170 STD999 7.54 22‐Sep‐08
08‐NSD‐003 E466960 GRBLANK 0.0025 10‐Aug‐02
08‐NSD‐003 E466980 GRBLANK 0.0025 10‐Aug‐02
08‐NSD‐003 E467000 GRBLANK 0.0025 10‐Aug‐02
08‐NSD‐003 E466840 GRBLANK 0.0025 29‐Sep‐08
08‐NSD‐003 E466860 GRBLANK 0.0025 29‐Sep‐08
08‐NSD‐003 E466880 GRBLANK 0.0025 29‐Sep‐08
08‐NSD‐003 E466900 GRBLANK 0.006 29‐Sep‐08
08‐NSD‐003 E466920 GRBLANK 0.009 29‐Sep‐08
08‐NSD‐003 E466940 GRBLANK 0.0025 29‐Sep‐08
08‐NSD‐003 E466990 STD900 3.02 10‐Aug‐02
08‐NSD‐003 E467010 STD900 3.07 10‐Aug‐02
08‐NSD‐003 E466850 STD900 3.19 29‐Sep‐08
08‐NSD‐003 E466890 STD900 3.32 29‐Sep‐08
08‐NSD‐003 E466910 STD900 3.16 29‐Sep‐08
08‐NSD‐003 E466950 STD900 3.22 29‐Sep‐08
08‐NSD‐003 E466970 STD999 7.15 10‐Aug‐02
08‐NSD‐003 E466870 STD999 7.17 29‐Sep‐08
08‐NSD‐003 E466930 STD999 6.9 29‐Sep‐08
08‐NSD‐004 E467040 GRBLANK 0.0025 10‐Aug‐30
08‐NSD‐004 E467060 GRBLANK 0.0025 10‐Aug‐30
08‐NSD‐004 E467080 GRBLANK 0.0025 26‐Jan‐08
08‐NSD‐004 E467100 GRBLANK 0.008 26‐Jan‐08
08‐NSD‐004 E467120 GRBLANK 0.013 26‐Jan‐08
08‐NSD‐004 E467140 GRBLANK 0.006 26‐Jan‐08
08‐NSD‐004 E467160 GRBLANK 0.0025 26‐Jan‐08
08‐NSD‐004 E467180 GRBLANK 0.0025 26‐Jan‐08
08‐NSD‐004 E529460 GRBLANK 0.42 17‐Jan‐09
08‐NSD‐004 E529480 GRBLANK 0.0025 10‐Feb‐09
08‐NSD‐004 E467760 GRBLANK 0.0025 2‐Apr‐09
08‐NSD‐004 E467050 STD900 3.14 10‐Aug‐30
08‐NSD‐004 E467090 STD900 3.07 26‐Jan‐08
08‐NSD‐004 E467110 STD900 3.13 26‐Jan‐08
08‐NSD‐004 E467150 STD900 3.3 26‐Jan‐08
08‐NSD‐004 E467190 STD900 3.19 26‐Jan‐08
08‐NSD‐004 E529490 STD900 3.4 10‐Feb‐09
08‐NSD‐004 E467030 STD999 7.15 10‐Aug‐30
08‐NSD‐004 E467070 STD999 6.86 10‐Aug‐30
08‐NSD‐004 E467130 STD999 6.61 26‐Jan‐08
08‐NSD‐004 E467170 STD999 7.16 26‐Jan‐08
08‐NSD‐004 E529470 STD999 6.67 17‐Jan‐09
08‐NSD‐004 E467770 STD999 7.28 2‐Apr‐09
09‐NSD‐001 E513120 GRBLANK 0.01 26‐Feb‐09
09‐NSD‐001 E513140 GRBLANK 0.0247 24‐Mar‐09
09‐NSD‐001 E513160 GRBLANK 0.01 24‐Mar‐09
09‐NSD‐001 E513180 GRBLANK 0.0315 25‐Mar‐09
09‐NSD‐001 E513200 GRBLANK 0.0106 26‐Mar‐09
09‐NSD‐001 E513220 GRBLANK 0.0261 26‐Mar‐09
09‐NSD‐001 E513240 GRBLANK 0.0117 26‐Mar‐09
09‐NSD‐001 E513260 GRBLANK 0.0265 1‐Apr‐09
09‐NSD‐001 E513280 GRBLANK 0.0112 3‐Apr‐09
09‐NSD‐001 E513460 GRBLANK 0.0025 18‐May‐09
09‐NSD‐001 E513520 GRBLANK 0.0025 2‐Apr‐09
09‐NSD‐001 E513540 GRBLANK 0.009 2‐Apr‐09
09‐NSD‐001 E513560 GRBLANK 0.0025 2‐Apr‐09
09‐NSD‐001 E513580 GRBLANK 0.0025 18‐May‐09
09‐NSD‐001 E513600 GRBLANK 0.016 18‐May‐09
09‐NSD‐001 E513620 GRBLANK 0.009 18‐May‐09
09‐NSD‐001 E513150 STD900 3.3491 24‐Mar‐09
09‐NSD‐001 E513190 STD900 3.2435 26‐Mar‐09
09‐NSD‐001 E513210 STD900 3.2846 26‐Mar‐09
09‐NSD‐001 E513250 STD900 3.3218 26‐Mar‐09
09‐NSD‐001 E513290 STD900 3.4103 4‐Apr‐09
09‐NSD‐001 E513510 STD900 3.28 2‐Apr‐09
09‐NSD‐001 E513550 STD900 3.38 2‐Apr‐09
09‐NSD‐001 E513590 STD900 3.19 18‐May‐09
09‐NSD‐001 E513610 STD900 3.49 18‐May‐09
09‐NSD‐001 E513130 STD999 7.3565 20‐Mar‐09
09‐NSD‐001 E513170 STD999 7.3292 25‐Mar‐09
09‐NSD‐001 E513230 STD999 7.3121 26‐Mar‐09
09‐NSD‐001 E513270 STD999 7.2615 2‐Apr‐09
09‐NSD‐001 E513470 STD999 7.1 18‐May‐09
09‐NSD‐001 E513530 STD999 7.52 2‐Apr‐09
09‐NSD‐001 E513570 STD999 7.01 18‐May‐09
Check Sample # DDH # Au g/t Analyis Date Check Sample #
E466260 07‐NSD‐008 0.006 4‐Feb‐08 E466290
E466280 07‐NSD‐008 0.0025 15‐Feb‐08 E466310
E466300 07‐NSD‐008 0.0025 19‐Mar‐08 E466350
E466320 07‐NSD‐008 0.0025 19‐Mar‐08 E466390
E466340 07‐NSD‐008 0.0025 19‐Mar‐08 E466450
E466360 07‐NSD‐008 0.0025 14‐Apr‐08 E466490
E466380 07‐NSD‐008 0.0025 14‐Apr‐08 E466510
E466400 07‐NSD‐008 0.0025 14‐Apr‐08 E466550
E466420 07‐NSD‐008 0.0025 14‐Apr‐08 E466590
E466440 08‐NSD‐001 0.0025 28‐Apr‐08 E466610
E466460 08‐NSD‐001 0.0025 28‐Apr‐08 E466650
E466480 08‐NSD‐001 0.0025 28‐Apr‐08 E466690
E466500 08‐NSD‐001 0.0025 28‐Apr‐08 E466710
E466520 08‐NSD‐001 0.0025 28‐Apr‐08 E466750
E466540 08‐NSD‐001 0.0025 28‐Apr‐08 E468010
E466560 08‐NSD‐001 0.0025 28‐Apr‐08 E468050
E466580 08‐NSD‐001 0.0025 28‐Apr‐08 E468090
E466600 08‐NSD‐001 0.009 28‐Apr‐08 E468110
E466620 08‐NSD‐001 0.0025 28‐May‐08 E468150
E466640 08‐NSD‐001 0.0025 15‐Jul‐08 E466790
E466660 08‐NSD‐001 0.0025 15‐Jul‐08 E466810
E466680 08‐NSD‐001 0.0025 15‐Jul‐08 E466990
E466700 08‐NSD‐001 0.0025 15‐Jul‐08 E467010
E466720 08‐NSD‐001 0.005 15‐Jul‐08 E466850
E466740 08‐NSD‐001 0.007 15‐Jul‐08 E466890
E466760 08‐NSD‐002 0.0025 25‐Aug‐08 E466910
E468020 08‐NSD‐002 0.0025 25‐Aug‐08 E466950
E468040 08‐NSD‐002 0.0025 25‐Aug‐08 E467050
E468060 08‐NSD‐002 0.0025 25‐Aug‐08 E467090
E468080 08‐NSD‐002 0.0025 25‐Aug‐08 E467110
E468100 08‐NSD‐002 0.0025 25‐Aug‐08 E467150
E468120 08‐NSD‐002 0.017 2‐Sep‐08 E467190
E468140 08‐NSD‐002 0.0025 2‐Sep‐08 E529490
E466780 08‐NSD‐002 0.0025 22‐Sep‐08 E513150
E466800 08‐NSD‐002 0.0025 22‐Sep‐08 E513190
E466820 08‐NSD‐002 0.0025 22‐Sep‐08 E513210
E468160 08‐NSD‐002 0.0025 22‐Sep‐08 E513250
E466960 08‐NSD‐003 0.0025 10‐Aug‐02 E513290
E466980 08‐NSD‐003 0.0025 10‐Aug‐02 E513510
E467000 08‐NSD‐003 0.0025 10‐Aug‐02 E513550
E466840 08‐NSD‐003 0.0025 29‐Sep‐08 E513590
GRANITE BLANKS
E466860 08‐NSD‐003 0.0025 29‐Sep‐08 E513610
E466880 08‐NSD‐003 0.0025 29‐Sep‐08
E466900 08‐NSD‐003 0.006 29‐Sep‐08
E466920 08‐NSD‐003 0.009 29‐Sep‐08
E466940 08‐NSD‐003 0.0025 29‐Sep‐08
E467040 08‐NSD‐004 0.0025 10‐Aug‐30
E467060 08‐NSD‐004 0.0025 10‐Aug‐30
E467080 08‐NSD‐004 0.0025 26‐Jan‐08
E467100 08‐NSD‐004 0.008 26‐Jan‐08
E467120 08‐NSD‐004 0.013 26‐Jan‐08
E467140 08‐NSD‐004 0.006 26‐Jan‐08
E467160 08‐NSD‐004 0.0025 26‐Jan‐08
E467180 08‐NSD‐004 0.0025 26‐Jan‐08
E529460 08‐NSD‐004 0.42 17‐Jan‐09
E529480 08‐NSD‐004 0.0025 10‐Feb‐09
E467760 08‐NSD‐004 0.0025 2‐Apr‐09
E513120 09‐NSD‐001 0.01 26‐Feb‐09
E513140 09‐NSD‐001 0.0247 24‐Mar‐09
E513160 09‐NSD‐001 0.01 24‐Mar‐09
E513180 09‐NSD‐001 0.0315 25‐Mar‐09
E513200 09‐NSD‐001 0.0106 26‐Mar‐09
E513220 09‐NSD‐001 0.0261 26‐Mar‐09
E513240 09‐NSD‐001 0.0117 26‐Mar‐09
E513260 09‐NSD‐001 0.0265 1‐Apr‐09
E513280 09‐NSD‐001 0.0112 3‐Apr‐09
E513460 09‐NSD‐001 0.0025 18‐May‐09
E513520 09‐NSD‐001 0.0025 2‐Apr‐09
E513540 09‐NSD‐001 0.009 2‐Apr‐09
E513560 09‐NSD‐001 0.0025 2‐Apr‐09
E513580 09‐NSD‐001 0.0025 18‐May‐09
E513600 09‐NSD‐001 0.016 18‐May‐09
E513620 09‐NSD‐001 0.009 18‐May‐09
DDH # Au g/t Analyis Date Check Sample # DDH # Au g/t
07‐NSD‐008 3.08 15‐Feb‐08 E466270 07‐NSD‐008 7.31
07‐NSD‐008 3.14 19‐Mar‐08 E466330 07‐NSD‐008 7.29
07‐NSD‐008 3.22 19‐Mar‐08 E466370 07‐NSD‐008 6.95
07‐NSD‐008 3.09 14‐Apr‐08 E466430 07‐NSD‐008 7.11
08‐NSD‐001 3.2 28‐Apr‐08 E466470 08‐NSD‐001 7.08
08‐NSD‐001 3.2 28‐Apr‐08 E466530 08‐NSD‐001 7.14
08‐NSD‐001 3.01 28‐Apr‐08 E466570 08‐NSD‐001 6.64
08‐NSD‐001 3.3 28‐Apr‐08 E466630 08‐NSD‐001 7.09
08‐NSD‐001 2.68 28‐Apr‐08 E466670 08‐NSD‐001 7.68
08‐NSD‐001 2.81 28‐Apr‐08 E466730 08‐NSD‐001 7.21
08‐NSD‐001 3.09 15‐Jul‐08 E468030 08‐NSD‐002 6.93
08‐NSD‐001 3.16 15‐Jul‐08 E468070 08‐NSD‐002 7.12
08‐NSD‐001 3.27 15‐Jul‐08 E468130 08‐NSD‐002 7.2
08‐NSD‐001 3.09 15‐Jul‐08 E466830 08‐NSD‐002 7.27
08‐NSD‐002 3.17 25‐Aug‐08 E468170 08‐NSD‐002 7.54
08‐NSD‐002 3.02 25‐Aug‐08 E466970 08‐NSD‐003 7.15
08‐NSD‐002 3.3 25‐Aug‐08 E466870 08‐NSD‐003 7.17
08‐NSD‐002 3.17 2‐Sep‐08 E466930 08‐NSD‐003 6.9
08‐NSD‐002 3.35 2‐Sep‐08 E467030 08‐NSD‐004 7.15
08‐NSD‐002 3.22 22‐Sep‐08 E467070 08‐NSD‐004 6.86
08‐NSD‐002 3.25 22‐Sep‐08 E467130 08‐NSD‐004 6.61
08‐NSD‐003 3.02 10‐Aug‐02 E467170 08‐NSD‐004 7.16
08‐NSD‐003 3.07 10‐Aug‐02 E529470 08‐NSD‐004 6.67
08‐NSD‐003 3.19 29‐Sep‐08 E467770 08‐NSD‐004 7.28
08‐NSD‐003 3.32 29‐Sep‐08 E513130 09‐NSD‐001 7.3565
08‐NSD‐003 3.16 29‐Sep‐08 E513170 09‐NSD‐001 7.3292
08‐NSD‐003 3.22 29‐Sep‐08 E513230 09‐NSD‐001 7.3121
08‐NSD‐004 3.14 10‐Aug‐30 E513270 09‐NSD‐001 7.2615
08‐NSD‐004 3.07 26‐Jan‐08 E513470 09‐NSD‐001 7.1
08‐NSD‐004 3.13 26‐Jan‐08 E513530 09‐NSD‐001 7.52
08‐NSD‐004 3.3 26‐Jan‐08 E513570 09‐NSD‐001 7.01
08‐NSD‐004 3.19 26‐Jan‐08
08‐NSD‐004 3.4 10‐Feb‐09
09‐NSD‐001 3.3491 24‐Mar‐09
09‐NSD‐001 3.2435 26‐Mar‐09
09‐NSD‐001 3.2846 26‐Mar‐09
09‐NSD‐001 3.3218 26‐Mar‐09
09‐NSD‐001 3.4103 4‐Apr‐09
09‐NSD‐001 3.28 2‐Apr‐09
09‐NSD‐001 3.38 2‐Apr‐09
09‐NSD‐001 3.19 18‐May‐09
STANDARD 900 STANDARD 999
09‐NSD‐001 3.49 18‐May‐09
Analyis Date
4‐Feb‐08
19‐Mar‐08
14‐Apr‐08
14‐Apr‐08
28‐Apr‐08
28‐Apr‐08
28‐Apr‐08
28‐May‐08
15‐Jul‐08
15‐Jul‐08
25‐Aug‐08
25‐Aug‐08
2‐Sep‐08
22‐Sep‐08
22‐Sep‐08
10‐Aug‐02
29‐Sep‐08
29‐Sep‐08
10‐Aug‐30
10‐Aug‐30
26‐Jan‐08
26‐Jan‐08
17‐Jan‐09
2‐Apr‐09
20‐Mar‐09
25‐Mar‐09
26‐Mar‐09
2‐Apr‐09
18‐May‐09
2‐Apr‐09
18‐May‐09
APPENDIX IV:
QUALITY CONTROL PROCEDURES
AND RESULTS
CORE SAMPLING QAQC & PROCEDURES
All drill core sampled was sawn in half lengthwise along the long axis of the foliation
ellipse. The accuracy of the cutting is checked on a regular basis by the field supervisor.
Samples are typically between 0.4 and 1.0m in length except in rare exceptions where
discrete narrow mineralized zones are encountered. The great majority of samples were
sent to the ALS Chemex laboratory in Thunder Bay for crushing and pulverizing
followed by a fire assay with AA finish at their facility in Vancouver, B.C. To ensure
proper “chain of custody”, most samples, and particularly any mineralized samples,
were shipped in locked security boxes. A small number of samples were assayed at the
Musselwhite laboratory but these did not include any mineralized samples.
To ensure the analyses are accurate and not affected by contamination, a granite blank
or one of two standards is inserted in place of every 10th sample. The two pre-
packaged standards, STD 900 and 999, are products of Geostats Pty Ltd of Australia.
The acceptable range of values for each standard is provided by Geostats and is based
on a 2 x Standard Deviation from a series of repeat analyses (see Table below). These
ranges and the upper acceptable limit for the granite blank, are programmed into the
mine’s acQuire assay handling software such that any values outside these limits is
flagged and data entry halted. If the standard has failed badly, and/or it is located in a
series of mineralized samples, it is typically re-assayed along with the adjacent 4-5
samples. Should it be a trivial failure, e.g. ~0.1 g/t too low, in a non-mineralized interval,
the assay file may be passed and imported at the discretion of the senior geologists.
Any table of assay results imported into the mine’s database with a failed standard or
blank is documented and a written record of the rationale is maintained.
Identifier
Standard
Mean
Standard
Deviation
Lower Acceptable
Limit (g/t Au)
Upper Acceptable
Limit (g/t Au)
Granite Blank - - 0.0 0.0768
STD 900 3.21 0.13 2.95 3.47
STD 999 7.18 0.31 6.56 7.8
Failed standards or blanks are typically due to one of the following reasons: 1) a mix-up
in the standard used, 2) a lack of sufficient flux used in the assaying leading to a low
result (this problem applies to standards and not core samples), or 3) a trivial and
unavoidable contamination of a sample following a series of high-grade samples.
Tables of the QAQC data are presented in the attached “QAQC Data” spreadsheet and
graphs of assay results for each standard and blank are presented below.
It is evident from these graphs that there has been no appreciable variation over time in
the average values for the standards or blanks and no significant issue with values
falling outside the accepted range. Two Standard 900 samples returned slightly low
values but as they were from a non-mineralized section and are of little consequence.
The sole failure of note was granite blank sample E529460 which assayed 0.42 g/t Au.
There are no mineralized samples for a considerable interval before or after this blank
sample and no obvious reason for the high value. Values from the standards and blanks
above and below this sample were well within the accepted limits and the adjacent core
samples are not from a mineralized section. Therefore, the reason for this spurious high
value remains unknown but inconsequential.
0
0.05
0.1
0.15
0.2
0.25
0.3
0.35
0.4
0.45Au g/t
Drill Hole #
QAQC GRANITE BLANKS: NSD 2008‐9 DRILL PROGRAM
0.0768 Upper Limit
# E529460: Reasonfor high value unknown
0
1
2
3
4
5
6
Au g/t
Drill Hole #
QAQC STANDARD 900: NSD 2008‐9 DRILL PROGRAM
2.95 Lower Limit
3.47 Upper Limit
ALS CHEMEX LABORATORY PROCEDURES
Sample Preparation Package – PREP-31 Standard Sample Preparation: Dry, Crush, Split and Pulverize
Sample preparation is the most critical step in the entire laboratory operation. The purpose of preparation is to produce a homogeneous analytical sub-sample that is fully representative of the material submitted to the laboratory. The sample is logged in the tracking system, weighed, dried and finely crushed to better than 70% passing a 2mm (Tyler 10 mesh) screen. A split of up to 250 grams is taken and pulverized to better than 85% passing a 75 micron (Tyler 200 mesh) screen. This method is appropriate for rock chip or drill core samples.
5
5.5
6
6.5
7
7.5
8
8.5
9Au g/t
Drill Hole #
QAQC STANDARD 999: NSD 2008‐9 DRILL PROGRAM
6.5 g/t Lower Limit6.5 g/t Lower Limit6.5 g/t Lower Limit
7.8 g/t Upper Limit
Fire Assay Procedure - Au-AA23 & Au-AA24 Fire Assay Fusion, AAS Finish
Sample Decomposition: Analytical Method:
Fire Assay Fusion (FA-FUS01 & FA-FUS02) Atomic Absorption Spectroscopy (AAS)
A prepared sample is fused with a mixture of lead oxide, sodium carbonate, borax, silica and other reagents as required, inquarted vnth 6 mg of gold-free silver and then cupelled to yield a precious metal bead.
The bead is digested in 0.5 rrl dilute nitric acid in the microwave oven, 0.5 ml concentrated hydrochloric acid is fhen a(!tled and the bead is further digested in the microwave at a lower power setting. The digested solution is cooled, diluted to a total volume of 4 ml with de-minerafized water, and analyzed by atomic absorption spectroscopy againsl matrix-matched slandards.
Metho<I sample Lower Upper Default
Code Element Symbol Units Weight Limit Limit Overlimit
(Cll Method Au-AX23 GOid Au Mm 30 0.005 10.0 Au-ORA21 Au-AX24 Gold Au nnm 50 0.005 10.0 Au-ORA22
Fire Assay Procedure - Ag-GRA21 , Ag-GRA22, Au-GRA21 and Au-GRA22
Precious Metals Gravimetric Analysis Methods
Sample Decomposition:
Analytical Method:
Fire Assay Fusion (FA-FUSAG1, FA-FUSAG2, FA-FUSGV1 and FA-FUSGV2) Gravimetric
A prepared sample is fused with a mixture of lead oxide, sodium carbOllate, borax, silica and other reagents in order to pioduce a lead button. The lead button containing the precious metals Is cupelled to remove the lead. The remaining gold and silver bead is parted in dilute nilric acid, annealed and weighed as gold. Silver, if requested, is then detennined by the (ifference in weights.
Sample Detection Upper Method Code Element Symbol Units Weight
In\ Limit Limit
AQ-GRA21 Silver "" com 30 5 10,000 Ao-GRA22 Silver NJ nnm 50 5 10,000 Au-GRA21 Gotd Au com 30 0.05 1000 Au-GRA22 Gotd Au com 50 0.05 1000
Musselwhite Mine Assay Lab
Gold Determination in Geological Samples
Sample Preparation Drill core is dried if necessary (if wet from the saw, rain, snow) in a propane-fired oven for a minimum of 4 hours. Samples are fed one at a time into the Rocklabs automated sampling system. Muck samples are crushed in the Big Boyd crusher to approximately ½”, and then crushed to a minimum 90% passing 6-mesh in the Boyd crusher. The sample is then split to 3000g (if the original sample was at least 3000g) and the split portion is pulverized to a minimum 90% passing 10-mesh. The sample is split again to 600g and this portion is pulverized to a minimum 90% passing 150-mesh. To minimize the chances of cross-contamination, 100-150 grams of material are allowed to pass through the pulverizer before collection begins. Reject material is not saved for these samples. Drill core samples are prepared the same way as the mucks, however virtually all of the sample continues through the process (no material is sent to waste from the crushers) until the second-stage pulverizer, where the 10-mesh reject is bagged and stored. Fire Assay The samples are weighed at 30g and mixed with a pre-mixed flux. They are inquarted with AgNO3 and fused at 1920°F for 50 to 60 minutes. The buttons are then cupelled and the resulting Doré beads are placed in 10ml test tubes. Analysis The beads are parted with 1ml of 33% HNO3 in a hot water bath, and then the gold is digested with 1ml of concentrated HCl in the same bath. The solution is cooled, diluted with DI water to 10ml and mixed. The solutions are run on a Varian AA240 using an autosampler. The results are sent to the LIMS database for approval by the technicians. Quality Control Several QC methods are employed in this analysis. In sample preparation, each batch of drill core samples includes a granite blank and reference material submitted by geology and a granite grit blank inserted by the lab. Run-of-mine sample batches include a granite blank and grit blank, but no reference material is inserted at the preparation stage. In fire assay, a pulp duplicate and reference material are added to each batch (core and mucks/chips) received from sample prep. At the analysis stage, a spike standard is analyzed before every 12 samples, and a calibration or re-slope is performed at the same rate.
TrueNorth
07‐NSD‐008collar
09‐NSD‐00108‐NSD‐001
NSD‐4 GYRO trace, to be Replaced by Maxibor
Note: Tick marks at beginning and end of hole trace is colour coded todrill hole numberdrill hole number.
74
00
E7
40
0E
75
00
E7
50
0E
76
00
E7
60
0E
77
00
E7
70
0E
78
00
E7
80
0E
79
00
E7
90
0E
80
00
E8
00
0E
81
00
E8
10
0E
82
00
E8
20
0E
83
00
E8
30
0E
84
00
E8
40
0E
85
00
E8
50
0E
86
00
E8
60
0E
87
00
E8
70
0E
3000 Z 3000 Z
3050 Z 3050 Z
3100 Z 3100 Z
3150 Z 3150 Z
3200 Z 3200 Z
3250 Z 3250 Z
3300 Z 3300 Z
3350 Z 3350 Z
3400 Z 3400 Z
3450 Z 3450 Z
3500 Z 3500 Z
3550 Z 3550 Z
3600 Z 3600 Z
3650 Z 3650 Z
3700 Z 3700 Z
3750 Z 3750 Z
3800 Z 3800 Z
3850 Z 3850 Z
3900 Z 3900 Z
3950 Z 3950 Z
4000 Z 4000 Z
4050 Z 4050 Z
4100 Z 4100 Z
4150 Z 4150 Z
4200 Z 4200 Z
4250 Z 4250 Z
4300 Z 4300 Z
4350 Z 4350 Z
4400 Z 4400 Z
4450 Z 4450 Z
4500 Z 4500 Z
4550 Z 4550 Z
4600 Z 4600 Z
4650 Z 4650 Z
4700 Z 4700 Z
4750 Z 4750 Z
4800 Z 4800 Z
4850 Z 4850 Z
4900 Z 4900 Z
4950 Z 4950 Z
5000 Z 5000 Z
5050 Z 5050 Z
5100 Z 5100 Z
5150 Z 5150 Z
5200 Z 5200 Z
5250 Z 5250 Z
5300 Z 5300 Z
5350 Z 5350 Z
5400 Z 5400 Z
5450 Z 5450 Z
14400 N 14400 N
14500 N 14500 N
14600 N 14600 N
14700 N 14700 N
14800 N 14800 N
14900 N 14900 N
15000 N 15000 N
15100 N 15100 N
2980 Z14775 N7305 E
8745 E14775 N
5480 Z
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