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TRANSCRIPT
41010NE9202 2. !5106 CUNNINGHAM 010
Ii i i iI NORANDA EXPLORATION COMPANY, UMITED
GRAND AMERICAN MINERALS LTD. J.V.
. REPORT OF EXPLORATION ACTIVITIES l ON THE
TOWER LAKE GROUP PROJECT 100/206
CUNNINGHAM TOWNSHIP NTS 41 0/10
VOLUME 1
6
li l M
!i il Timmins, Ontario Reno Pressacco, M. Sc(A) * February, 1992 Project Geologist
li
I
11111it "iiiiiiiiiibii
in Hill li ill i li li li li li li lin iiiiiiin in TADI p Op /V") 4101CNE9282 2. 15186 CUNNINGHAM
Summary
Certification
1.0 Introduction
2.0 Location, Access and Claims
3.0 Topography and Vegetation
4.0 Previous Work
5.0 Geology
5.1 Regional Geology52 Local Geology5.3 Economic Geology
6.0 Geophysics
6.1 HLEM62 VLF-EM166.3 Magnetics
7.0 Trenching
6.0 lithogeochemistry
-
10.0 Discussion of Results
11 .0 Conclusion and Recommendations
12.0 References
Appenoloes
Appendix l Detaited Uthologlcal Descriptions
III Lithogeochemical ResultsIV Assay Certificates
III010C
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SUMMARY
The results of the recent exploration activities have shown that the claim group Is underlain by a structurally complex, overturned assemblage of calc-alkaline footwall felsic volcanics and tholeiitic hanglngwall basalts. The footwall units have been subjected to widespread hydrothermal alteration consisting of co-Incident iron enrichment and soda depletion, and these signatures are similar to those observed below some Archean volcanogenic massive sulphide deposits elsewhere.
Diamond drilling has intersected widespread occurrences of strong stringer-type sulphide mineralization. The better values have been returned from holes TOW-91-3 (t.2% Zn74.96m), TOW-91 -5 (S.2% AiV6.95m) and TOW-91 -6 (1.3** Zn/21.33m). Occurrences of bedded sulphides were observed in holes TOW-91-1, 2, 5 and 7, and yielded elevated base metal values. While significant sulphide occurrences are present at all stratigraphic levels, a spatial association between better values and the top of the sequence is clearly apparent, suggesting that the upper levels may hold higher potential for hosting base metal sulphides.
The data gathered to-date all point towards a favourable environment for the formation of Archean VMS deposits. A good deal of potential remains untested in the western and southern portions of the property. Drill testing of these areas Is recommended.
11111iliiiiiiiiiiii
*(li)
CERTIFICATION
1, Reno Pressacco, residing at 181 Christine Street, Timmins, Ontario certify the following:
1) That
2) That
3) That
4) That
1 am a practising geologist,
1 hold the following degrees and diplomas:
M.Sc. (A), Mineral Exploration, 1986, McGill University B.Sc.,Geology, Lake Superior State College Diploma in GeologyEngineering Technology, 1982, Cambrian College.
l am a member in good standing of the following professional associations:
The Geological Association of CanadaPorcupine Prospectors and Developers Association
this report is base on information obtained from government publications, publicpress releases, and collected by various mining companies including Noranda ExplorationCompany, Limited.
/) t Lu~*~*f^
February, 1992 Reno Pressacco, M.Sc.(A) Timmins, Ontario Project Geologist
l l
1.0 INTRODUCTION
lm This report will describe the results of exploration activities conducted by Noranda
Exploration on the Tower Lake claim group. These claims are currently under option to Noranda
J Exploration from Grand America Minerals Ltd. located in Vancouver, B.C. A wide variety of work
j types were executed on the claims largely during the fall and early winter of 1991. These
activities were carried out under the direct field supervision of the author, with assistance being
l provided by Kim Wakeford, David MacLean, Gary Smith and Keith Green. All personnel were
u employees of Noranda Exploration.
j The goal of this exploration work was to evaluate the property's potential for hosting
significant quantities of volcanogenic massive sulphide mineralization. To that end, activities were
l conducted to 1 ) examine and explain the source of geophysical and geochemical anomalies, 2)
m refine and resolve the structural geology of the property, 3) identify the environment of
deposition, and 4) drill-test the most favourable areas Identified by the previous activities.
iil iili t
2.0 LOCATION ACCESS. AND CLAIMS
The property is located In central Cunningham Twp. approximately 130km southwest of
Timmins, Ontario and 15km northeast of Sultan, Ontario (Figure 1.). Access to the southern and
western portions of the property is by means of the gravel forestry roads as shown in Figure 1.
Additional access to northern and northwestern portions of the claims is provided by old bush
trails of 1940 vintage. The property currently consists of the seventeen (17) unpatented mining
claims as shown in Figure 2.
i i i l i11i t
PROPERTY
Figure l
mvino TOWER LAKE (10*)
LOCATION AND ACCESS
NORANDA EXPLORATION CO.LTD.I
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Beaver Tail Lake
l 1030164 'l 1030170
-^ l V*-o 1030180r—*^ ; -\ 1030182 f
\ 1030188\
l|76993
LOCATION MAP
ScaleFigure 2
l l
The village of Sultan is located on the CP Rail main line and has a population of 500-700.
l Some limited services such as gasoline, groceries, propane, and telephone are available in the
m village, but a more complete set of services are available in Chapleau, approximately 55km to the
northwest.
lg 3.0 TOPOGRAPHY AND VEGETATION
l The topography in the vicinity of the property is fairly rugged, with local relief being up
m to 50m in height. The area as a whole is very hilly with abundant rock outcroppings creating
ledges and cliffs anywhere up to a few 10's of meters in height. This rugged terrain poses some
i i
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restrictions on the movement of heavy equipment in the area, however only a few areas exist
which are not accessible.
j The vegetation in the area consists of a mixture of mature forest and cedar swamps. The
dominant tree types consist of Jack pine, black spruce and poplar. Occasional birch and rare
l amounts of maple trees are also present in the area. Both Cunningham and Blamey Townships
m have undergone forestry operations over the years. These operations have removed many of
the larger stands of jack pine and black spruce by dear cutting. Operations have largely ceased
in recent years, however, some of the smaller stands of conifers were harvested in Cunningham
Twp. in the fall of 1991. Forestry operations have extended into the southern sections of the
property, where the clear cutting has provided excellent outcrop exposure along with good road
access. The northern portions of the property, north of line 7+OOS, had not been logged as of
late 1991, and conversations with the forestry company have indicated that no further activities
are planned for the northern part of the claim group.
ll -
4.0 PREVIOUS WORK
lm * Initial exploration activity in the area dates back to the early 1900's when the Rideout
Mining Company prospected the area for iron. During that time, the Iron formations' of
l Cunningham Twp. were located but were found to be of too low a grade for Iron production.
m During 1927, lead-zinc bearing veins hosted by these "iron formations' were discovered on what
is now KIrkton Resources' Shunsby property, and since then exploration In the area continued
l in a sporadic fashion.
i ti
l
The earliest record of work on the present claim group dates back to 1953. A detailed
chronological summary of exploration activity on the property is given below.
1953: Paae-Harlev Mines Ltd.. diamond drilling of 9 holes totalling 907m.
B 1957 and 1965: Consolidated Shunsbv Mines Ltd.. diamond drilling totalling 689m.
; 1969-1970: Consolidated Shunsbv Mines Ltd.. geological mapping and soil m geochemical surveys.
i 1974: Grandora Explorations Ltd.. soil geochemical surveys,
l 1978: M.W. Resources Ltd.. diamond drilling, 5 holes totalling 377m.
m 1 960: Placer Development Ltd.. ground geophysical surveys (EM-17 and J magnetometer).
|f 1967-1988: Grand American Minerals Ltd.. linecutting, geological mapping, geophysical (HEM and magnetics) and geochemical (B-horizon soils) surveys.
i In addition to the above described work, a number of hand-dug trenches (for which there
" were no records) were encountered during the course of the 1991 program.
ij'i
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5.0 GEOLOGY
5.1 Regional Geology
While insufficient information exists to allow a thorough, detailed comprehension of the
regional geology of the area, enough information exists to allow an overview of the
geological/structural setting. Figure 3 illustrates our perception of the regional setting, and was
constructed by integration of airborne geophysical signatures (AEM, Amag) with all available
ground geological information.
Much of the area consists of variably textured mafic metavolcanics which vary in strike
from northeasterly in the western sectors, through easterly in the central sectors, and
southwesterly in the eastern sectors of the region. A number of bands or belts of dominantly
clastic and chemical sediments (an assemblage of chert-argillite-magnetite-Fe sulphides) largely
mimic the regional structural trends and are intercalated with the mafic metavolcanics on a gross
scale. Felsic metavolcanics underlie the chemical sediments In the vicinity of the Tower Lake
claim group. Figure 3 shows that these felsic metavolcanics are of only local area extent In the
area, however this is largely a function of the level of information, as additional areas of felsic
metavolcanic/pyroclastic rocks are continually being discovered with further work. An intrusive
suite ranging in composition from peridotite through gabbro to granodiorite is centred In the
southwestern sector of Cunningham Twp. The mafic and ultramafic Intrusives are interpreted to
be grossly strataform by their magnetic signatures and are believed to be older than the felsic
pluton. Granodiorite intruslves occur mostly as one large pluton, known as the Isaiah Creek
Pluton, and as numerous dikes and sills throughout the area. While no absolute age dates are
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avaflable for the area, tt is likely that the Isaiah Creek Pluton Is roughly 2675 Ma in age, similar
to many other late-stage felsic intrusions throughout the Archean sub-province. Younger diabase
dikes cross-cut all stratigraphic units with roughly north and northwesterly orientations.
From the level of information available to-date, the area Is most structurally complex in
central and southern Cunningham Twp., with the stratigraphic trends becoming simpler and more
weO-behaved as one moves eastward into Garnet Twp. and westwards Into Greenlaw-Tooms-
Ssenhower Twps. In Cunningham Twp., the structural setting can be determined by the
distribution of the cherts or "iron formations*. A broadly ellipsoidal structure centred on the Isaiah
Creek Pluton is interpreted to account for the map pattern of the chert units and likely affects the
remaining units in this area. Elsewhere to the east and west, the entire stratigraphic package
consists of a broadly homoclinal, southerly dipping assemblage of lithologies. While the cause
of the structural complexity in Cunningham Twp. is not known, it is felt to be caused by or related
to emplacement of the younger Isaiah Creek Pluton.
5.2 Local Geoloov
On a property scale, the dalm group is underlain by a complexly folded package of
lithologies composed of felsic metavolcanic flows and pyroclastics, a chert-argilltte-magnettte-Fe
sulphide assemblage, a variolitic basalt unit and mafic massive to pillowed mafic metavolcanics.
Intruding into all lithologies are dikes, sills and stocks of gabbro and granodiorite. Larger bodies
of these intruslves are located in the western extremes of the property for the most part.
The oldest units on the property (stratigraphic footwall) are the felsic metavolcanics which
-9-
consist of rhyolltic flows, felsic ash to lapilli tuffs, and a heterogenous unit which is currently
interpreted to represent some type of turbiditic sediment or debris flow. Stratlgraphically
overlying, but structurally below these felsic units is the chemical sediment assemblage. These
chemical sediments are volumetrically dominated by variably textured cherts, but also contain
significant amounts of fine clastic sediments (argillite, graphitic argillite, greywacke), minor
amounts of interbedded magnetite, massive, bedded pyrite and pyrrhotite and rare amounts of
a tuffaceous component (both felsic and chloritic-mafic). The chemical sediments are hosts to
a variolitic basalt unit which is the most important stratigraphic marker horizon in central
Cunningham Twp. This variolitic basalt has already been traced almost continuously for a strike
' length of at least 5km. In keeping with terminology applied to the type sections located on the
A Shunsby property Immediately to the southeast, those cherts stratigraphlcally below the variolitic
basalt marker are known as the Upper Cherts. Those cherts located stratigraphically above the
V marker unit are known as the Lower Cherts. The unit stratigraphically above the Lower Cherts
A consists of a basalt, which forms the ultimate hangingwall to the succession in the area. This
lithologic assemblage is illustrated in the stratigraphic column shown in Figure 4, and more
P detailed lithologic descriptions are given in Appendix l.
Structurally speaking, our current interpretation suggests that the llthologles are part of
l an overturned, doubly folded, broadly synformal structure which is roughly a dome-and-basin
jm pattern as described by Ramsey (1967). The northeastern quadrant of the property is basically
upside-down and is now a flat-lying to gently plunging synform. This synform plunges gently tor i
l the southwest, and gradually broadens out westwards into a moderately dipping monoclinal
^ attitude. Figure 5 illustrates several schematic cross-sections across the synform which were
i l
constructed using drill hole and surficial data.
i i ii iii l i
•10-
Umited geological mapping of the southern half of the property was undertaken prior to
the trenching program in order to aid in the geophysical Interpretation and attempt to discover
the presence of any areas of VMS-type hydrothermal alteration. This mapping was conducted
by the author in late September, and the results are shown on Map 1 (in pocket). These results
were integrated with trenching, drilling and geophysical information to construct a surficial
geology map (Map 2, in pocket) which illustrates our current perception of the property geology.
5.3 Economic Geology
As discussed in Section 4.0, base metal mineralization had been known in the area since
1927 and Figure 3 shows locations of the more significant base metal occurrences. For the most
part, these occurrences consist of stringer-type sphalerite with associated pyrtte-galena-
chalcopyrite-(pyrrhotite). These occurrences are usually hosted within the chemical sediment
assemblage. The largest of these is the Shunsby Occurrence, where sufficient mineralization is
present to conduct mineral inventory estimates. A number of such estimates have been
conducted over the years. The most recent estimate yields a combined total of 4.0 Mt grading
D.59% Cu and 2.56*ft Zn in two zones (Main and South). Some higher grade areas are present,
and a historical estimate of one such zone yielded an inventory of 970,000 tons grading 1 tt
Cu S.0% Zn. Much of this inventory occurs as stringer-type mineralization, however workers on
the property have Identified some bedded sulphide occurrences containing significant base metal
values.
On the Tower Lake Group, a number of localities have been discovered containing
elevated zinc-(lead)-(copper) values. The more significant occurrences are tabulated below:
CUNNINGHAM AREA GENERALIZED STRATIGRAPHIC COLUMN
P*rtln*nt SlmllorltlMto
Maltobl-Typ* Envlrenmcni* (Kidd Cr**k, Horn*. Louvcn)
1) Mlxtd tholeiitic footwall fettle flows * frogmontal*
2) Thick, impcrmoabl* basaltic cap rock
3) Clastic sediments mark proximity to subartal sodlmvnt sourc*- hallow water environment-graphitic sediments act as metal scavengers In reducing environments
4) Widespread CDs alteration of host llthologles-Fe chlorite dominated pipes host strong Cu-Fe-Zn sulphide stringers-sericlte-chlorite alteration of relevant lithologles (variolitic basalt)
5) Multiple levels of bedded sulphide occurrences
6) No 20-CaO-SI02 depletion
MgO-FeTot-KjO enrichments
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INTRUSIVE SUITE
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TOW-91-f
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- - -200m
-300m
Figure 5a
REVISED
PRQJ.Mt
DWG.N?
Tower Lake (106)
Schematic Cross Section
PROJECTSURVEYED IV".. OAMMTN IV'. .. 1:2,500
NORANDA EXPLORATION CO. LTD.OFFICI: mt. ltmnt/0.
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Lower Chert
•200 m - -
-300m
tFigure 5b
Tower Lake (106)
Schematic Cross Section
SURVEYED IV'... Jan, 1992—SCALE'
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C'TOW-91-3
HanghtgwaN Basalt
REVISED
MQJ.NfNTS,DWG.Nt
Tower Lake (106)
Schematic Cross Section
PROJECT;.suavmo I
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Occurrence
TOW-9M (DD)
TOW-91 -2 (DD)
TOW-91 -3 (DD)
PH-53-21 (DD)
TOW-91 -5 (DD)
TOW-91-6 (DD)
TOW-91-7 (DD)
TOW-91-8 (DD)
TR-9-91 (trench)
Table 1:
•15-
Locaflon
12+50S/0+55W 1 .3K Zn/1.05m
Remarks
Hosted by 0.84m section of bedded massive pyrrhotite in Upper Cherts.
9+OOS/4+15W D.7% Zn. 0.1 % Cu/ Hosted by 1.73m section ofbedded massive pyrrhotite in Upper Cherts.
3+96S/1+12E
1+65S/2+52E
2+17S/2+82E
3.03m
1.2*X,ZrV4.96m
2.5% ZrV3.57m
S.2% Zn, 1 .1 % Pb/ 6.95m
Sphalerite stringers hosted in Lower Cherts.
•Ore Formation' In Page- Harley 1953 drill hole, Upper Cherts.
Strong sphalerite stringers as fracture-fillings in Upper Cherts.
21.33m Cherts.0+70N/3+OOE 1 .ra Zn, Q.4% Pb/ Sphalerite stringers in Lower
3+OOS/2+60E
0+17N/3+25E
5+OOS/2+30E
Significant Base Metal Occurrences, Tower Lake Group, Cunningham Township.
S.6% Zn, 1 .3*** Pb/ Bedded to smsv sph-cpy In 0.2m Upper Cherts.
2.^ ZrV2.0m Sphalerite stringers in UpperCherts.
Argllttte-tosted sphalerite dasts In Upper Cherts.
1 .2* Zn, 0. Cu/S.Sm
Many of the above listed occurrences are of stringer-type mineralization, however, those
occurrences intersected in drill holes 91-1,2, and 7 and uncovered in trench 91-9 are definitely
of a bedded nature. Taking both types of mineralization Into account, one can determine that
a favourable environment for the formation of VMS deposits is present both on the Tower Lake
Group and elsewhere in the region.
1111111111iii
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6.0 GEOPHYSICS (G. Hodges, Division Geophysicist)
INTRODUCTION
During 1991, the geophysical work consisted of HLEM on the east-west lines between
700S and 1600S, 1100W and the baseline. VLF and magnetic data were collected on parts of
the north-west extension of the grid, 900W to 800E, on to SOON.
6.1 HLEM
The HLEM showed a broad band of conductors between 400W and OE on most of the
lines. The conductors range from moderate to strongly conductive. The depths
conductors in the north and southeast are less than 10m, while the depths average 40
of the
to 50m
In a broad band crossing northeast through central portion. The conductors may be broken by
an east-west fault between lines 1 200S and 1 300S, and a northeast striking fault appears to cross
line1000Sat150W.
Both graphitic argillites and base metal sulphides have been detected In this anomalous
area, and tt is not possible to distinguish the best target based on HLEM alone. Either
geochemistry, if it will work, or gravity is recommended to try and prioritize the conductors.
6.2 VLF-EM16
The VLF data shows a series of west-northwest striking conductors of varying
l l l l l l l l l ll l l li i l i i
-17-
conductance and size. The variability of the overburden thickness in the area makes comparison
of the VLF to topography paramount, to assess which anomalies correlate to swamp edges, etc.
The VLF on the east part of the area covered should be reassessed with geochemistry
if possible, to highlight interesting conductors, and separate overburden from bedrock
conductors.
6.3 Magnetics
The magnetic data collected did not show significant anomalies, but they do support a
general west-northwest trend for the geology.
7.0 TRENCHING
A total of sixteen (16) trenches were excavated throughout the property in order to
examine and test selected geophysical, stratigraphic, and geochemical targets. All trenches were
dug less than 3m deep for safety reasons. This trenching was conducted during the period from
October 1-24, 1992 and used a John Deere 690 shovel contracted from Wlad and Sons of
Iroquois Falls, Ontario. All trenches were subsequently washed, and mapped with chip/channel
samples taken across any zones of interest. All samples were analyzed for Cu-Zn-Pb-Ag. A
number of rock samples for lithogeochemical analysis were collected during the course of trench
mapping. The trench locations are shown on Map 3 (in pocket) and individual trench maps are
attached (in pocket).
TRENCHING - ADDENDUM
Equipment
Hourly Rate
Dates Worked
John Deere 690 Backhoe
SSS/hr (operator included)
Oct. 2/91 - 5.0 hoursOct. 3/91 -10.5 hoursOct. 4/91 -11.0 hoursOct. 5/91 - 9.5 hoursOct. 6/91 -10.0 hoursOct. 7/91 - 7.0 hoursOct. 8/91 -10.0 hoursOct. 9/91 - 9.0 hoursOct. 10/91 - 5.0 hours
Trench
1-912-913-914-915-916-917-918-919-91
10-9111-9112-9113-9114-9115-9116-91
Length (m)
9512515380
10067
125959090
10010040
1205070
Width (m\
5555342443442343
Depth (m)
2-3 2-3 2-3 2-3 2-3 2-3 2-3 2-3 2-1 2-3 2-3 24 2-3 2-3 2-3 2-3
ll 9
A number of these trenches yielded interesting results. Trench 5-91 (5+OOS, 2+50W) was
l successful in reaching bedrock in it's western 2/3, but hit highly compacted gravel in it's eastern
M- third. To the west, several intervals of py-po-(cpy) stringers were uncovered where grab samples
consistently contained elevated copper values up to 1 "fc Cu. To the east, two zones of ferrocreter
l (compacted gravel cemented by rust) 2m and 10m wide were uncovered. These zones along
± with the intervening hardpan had a hardness approaching that of concrete so that all efforts at
™ further excavation were unsuccessful. Several boulders of massive to bedded pyrite (some
l containing traces of sph-cpy) were found to be located within the thicker ferrocrete zone. Grab
sampling of these boulders returned up to Q.7% Zn, G.6% Cu.
l Trench 1 -91 (13+OOS, 0+50E) also encountered a ferrocrete zone. This zone was located
above an HLEM conductor, was up to 20m in width, and also contained boulders of bedded
l massive pyrite. Grab samples of these boulders returned elevated base metal values to Q.3%
l Trenches 7-91 (1 -f OOE, 1+50N) and 8-91 (3+OOE, 1+50N) were excavated along the
. north limb of the synformal structure. Both trenches exposed predominantly the debris flow, with
the southern third of trench 8 exposing a massive rhyolite flow. Both trenches exposed zones
l of intense chloritic alteration which commonly contained stringer and disseminated pyrite locally
' up to 20*K abundance. These zones appear roughly conformable, display a markedly increased
tii l
foliation with Increasing alteration, and reached a thickness of 36m In trench 8-91. Despite
comprehensive chip sampling across these zones, no significant base metal values were
encountered.
-19-
Trench 13-91 (7+158,0+75W) was excavated to further examine a quartz vein occurrence
mentioned in Augsten (1989), and was successful in reaching bedrock only in it's eastern part.
Fortunately the vein zone was exposed here and was found to be at least 6m in width. The vein
zone could be wider as the western contact is covered by gravel. The vein zone contained a
good deal of disseminated and stringer py-(po)-(cpy) up to 10*fc abundance. However, no
significant gold values were returned from sampling.
Trench 14-91 (8+OOS, 2+75W) exposed two zones of moderately dipping bedded
m sulphides. The stratigraphic^ lower zone (west) contained several narrow beds of pyrrhotite.
' The upper zone, less than 10m east, contained several beds of massive sulphides across a true
l thickness of approximately 2-3m. The sulphides consisted of thin pyrrhotite beds in the
centimetre range, and one larger bed of pyrite up to 0.75m thick. Elevated Cu-Zn values were
l associated with both these occurrences, with the best value being Q.4% Zn, 0.1 *JG Cu/LOm
B (channel).
l 8.0 LJTHOGEOCHEMISTRY
A total of sixty (60) samples were taken for whole rock analysis from either outcrops,
l trenches, or diamond drill core. In ail cases a great deal of care was taken in order to obtain as
^ representative and homogenous a sample as possible. Those samples with excessive
weathering rinds, quartz-calcite veining, containing more than 0.5-1 y* pyrite or pyrrhotite, or those
l which displayed any magnetism were discarded as they would artificially affect the analytical
^ results. Due to this attention paid to sample collection, the results and conclusions presented
™ below are felt to be as accurate as possible. Sample locations are illustrated on Map 4.
i i
ll W -20-
Analytical resutts and further sample details are given In Appendix III. Representative pieces of
l selected samples were retained for future reference. All samples to X-Ray Laboratories for
m analysis and the subsequent analytical results are illustrated in Figures 6,7,8,9 and 10.
J Figure 6 is an alkaline-subalkaline discrimination plot, and clearly shows that all samples
g are of subalkaline affinity, with some of the basalt and variolitic basalt samples being slightly
alkaline in nature. Figure 7 is a traditional Ti02-Zn discrimination plot which is Intended to show
l the essentially bl-modal (felsic-mafic) distribution of the sample population. For the most part,
m Figure 7 illustrates a good degree of correlation between the immobile trace element ratios and
" the field name. However three samples (18120,18126,18128) which were termed rhyolite in the
l field appear to have a trace element signature similar to that of the mafic metavolcanics.
Subsequent examination of the representative samples indicated that while sample 18120 may
l be of a mafic dyke, samples 18126 and 18128 where dearly rhyolitic in appearance. A possible
m explanation for this may be that these two samples (18126, 18128) were taken in an area
containing talc-chlorite alteration observed in outcrop, and that their anomalous plotting positions
l may be a tributed to alteration. Figure 7 also dearly shows a virtually identical trace element
m signature between the rhyolites and the debris flow. This leads to the conclusion that the two
units are genetically related and that the debris flow material was likely derived from a precursor
l felsic volcanic flow. Also of interest is the similarity between the felsic volcanic signatures and
^ those of the granodiortte/feldspar porphyry samples. While an insufficient number of samples
™ is available, the limited results shown in Figure 7 suggest another genetic link between the
l - footwall felsic units and the felsic intrusive suite. This lends support to the interpretation that the
Isaiah Creek Pluton may be a sub-volcanic equivalent to the felsic volcanic units.
l l l
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Figure 8 is a discrimination diagram constructed along the same lines and similar intent
l as Figure 7, but adds a third immobile trace element for consideration. This diagram confirms
m the observations made In Figure 7 because the addition of the third element did not substantially
change the patterns of Figure 7. Of note in Figure 8 is the high degree of scatter in the variolitic
l basalt compositions. While showing some affinity with the hangingwall basalt samples, this
m variolitic basalt has a highly variable trace element signature. This may be explained by the
presence or absence of varioles in the selected sample. While attempts were made to
l consistently sample essentially massive sections of the unit, some samples may have been taken
m where a high degree of variole concentrations gave a massive appearance to the rock. Such
™ occurrences were commonly observed in drill core (eg holes TOW-91-3, 4, 5) where the unit
l would become a light beige in colour where the variole abundance approached 100**.
l Figure 9 displays the analytical results in a Jensen Cation plot. On examination, one sees
U that samples of the hangingwall basalt unit are clearly of tholeiitic affinity, but are either iron or
magnesium-tholeiites. The high degree of scatter in the variolitic basalt compositions Is again
l present, however the scatter appears to occur along a crudely linear trend along a line bisecting
m the AI203 vertex. This suggests that some process involving mostly AI203 had affected the
variolitic unit. This trend may be explained by variole abundance where a variole-free bulk
i i
composition in the Fe-tholeiite field may be shifted to that in the calc-alkaline andesite field, by
increasing tile variole contact.
l Another trend is visible in Figure 9 where both the rhyolite flows and debris flows show
. a systematic change from an initial bulk composition in the area of calc-alkaline rhyolite or dacite
•' towards a point along the Fe-Mg axis. This Is indicative of an iron enrichment (alteration) byr
i
ll •27-
some mineral (likely chlorite) containing an FeO: MgO ratio of approximately 0.85:0.15. Similar
l trends have been documented by Kranidiotis and Maclean (1987), Deptuk et al (1982), Morton
M (1984) and Osterberg (1985). The possibility that this effect can be produced by some primary
lithological variation Is reduced due to the fact that both the felsic flows and debris flows exhibit
l the same trend.
This same trend is evident to a lesser degree in the AEM diagram of Figure 10 where
l again both the rhyoiites and debris flows show a systematic variation towards the same point
B along the Fe-Mg axis as In Figure 9. This lends support to the conclusion of an iron enrichment
™ by a mineral containing and FeO:MgO ratio of approximately 0.85:0.15. The possibility that these
l trends can be caused by a systematic change in either AI203 or total alkali abundance is ruled
out by the fact that this iron enrichment trend moves towards the same point (FeO:MgO ratio)
" along the Fe-Mag axis and does not move orthogonally away from either vertex. The possibility
l that these trends may also be caused by some type of a mixing between the debris flow and an
iron-rich sediment is also ruled out due to the fact that the rhyolite samples exhibit the same
l trend in variation. This could not happen by a sediment mixing event. The most likely possibility
remains an iron enrichment alteration which affected both footwall units In an identical fashion.to
f Map 4 illustrates an attempt to identify any spatial distribution patterns of the alteration
L effects shown in Figures 9 and 1 0. Thresholds for N^O depletions and FeO* enrichments were
chosen subjectively. With respect to Na^, any samples of either rhyolite or debris flow
l containing less than 1.0* soda were considered depleted. With respect to FeO*, all samples
y of rhyolite or debris flow were considered enriched if they plotted in the tholeiitic andesite field
' or above on Figure 9. Examination of Figure 4 reveals that most of the samples of rhyolite and
ii
ll -M debris flow exhibit a co-incident soda-depletion and iron-enrichment, with almost all of the
footwall units in the northeastern quadrant being altered. The footwall unit on the western half
l of the property also shows alteration effects, but not as strongly as those units to the northeast.
In short, much of the footwall felsic volcanics on the property have been subjected to an
" alteration event whose signatures are consistent with those of a Mattabi-style alteration as
l described by Morton and Franklin (1987).
l l l l l l l l l l l l l
l i. 10.0 DISCUSSION OF RESULTS
l For the most part, the results of the recent exploration activities have contributed greatly
^ to the understanding of the geological setting on the property, as well as explaining the style of
" mineralization and alteration by the use of existing VMS models. The greatest Impact of the
l trenching program was to refine the overall geological setting from that presented by Augsten
(1969), and essentially expanded the limits of the footwall felsic volcanic units. As well, the
l trenching served to explain a good number of HEM conductors and provide some input as to
M the structural setting of the property. The diamond drilling program served to locate several
areas containing strong stringer sulphide mineralization (holes TOW-91 -3: 1 .2*fc ZiV4.96m, TOW-
| 91 -5: S.2% ZnJ6.95m, and TOW-91 -6: 1 .3*** Zn/21 .33m) as well as to resolve a good deal of the
g structural geology of the property.
J Taking all the recent results into consideration, a favourable environment for the formation
^ of Archean VMS-type deposits Is felt to exist. The overall lithologic assemblage consists of a
calc-alkalic footwall felsic volcanic pile overlain by a tholeiitic basaltic hangingwall. The footwall
l felsic units display strong signs of having been affected by a widespread alteration event whose
, . geochemical signatures are similar to a "MattaW-type" as described by Morton and Franklin
l' (1987).
iAll lithologies have been found to host Zn-Cu-Pb stringer sulphide mineralization, with a
l J crude copper to zinc zonation with stratigraphic height being apparent in some drill holes. While
I ; some Individual samples contain anomalously high lead values, the overall Zn:Cu:Pb ratios J
remain consistent with other known Archean VMS deposits. While most of the significant
ii
li * ^
mineralization encountered recently was of a stringer-type, some occurrences of bedded base
™ metal sulphides were observed, and serve to demonstrate that seawater-rock interfaces had
'fl developed at some point in time. Such interfaces have been recognized as being critical
components of other Archean VMS deposits (eg. Kidd Creek, Matagami, Noranda camps). It is
l dear that most all of the better grades returned to-date have been spatially related to either the
H Lower Cherts or the Variolitic Basalt unit, both of which are near the top of the stratigraphic
succession. This, along with the copper to zinc zonation, would suggest that the top of the
'l sequence would be most favourable for bedded sulphide mineralization.
11.0 CONCLUSIONS AND RECOMMENDATIONS
i— Based on the information presented above, the following conclusions may be made:
l 1) The overall setting of the property consists of an overturned assemblage of calc-
^ alkaline felsic volcanics overlain by tholeiitic basalts.
i l i
3) Significant occurrences of base metal sulphide mineralization show strong spatial
l Ii i
2) The footwall flows, tuffs, and debris flows all show geochemical similarities to both
the feldspar porphyry dikes and Isaiah Creek pluton. This suggests a genetic link?X.V(*\\^d
between intrusive and extensive felsic units.
relationships to units near the top of the stratigraphic sequence.
ll
5) A widespread alteration of the footwall felsic volcanic units have been recognized.
l This alteration consists dominantly of co-incident iron enrichment-soda depletion
m of all footwall units.
J On the basis of the above conclusions, it Is clear that a favourable environment for the
g formation of a classic Archean volcanogenic massive sulphide deposit is present on the property.
A good deal of the property to the west and south remains untested and should be explored.
l Further drilling at widely-spaced Intervals to test the upper portions of the stratigraphic
, succession in the western and southern portions of the property Is recommended.
fe The proposed drilling program will test the hanging wall contact by means of several
widely spaced drill holes. One drill hole will pierce the hanging wall contact at approximately the
l -200m elevation and is located such that it will test the contact in an area 500 metres away from
m hole TOW-91-5 (S.2% Zn76.95m). A second drill hole will test the hanglngwall contact at
approximately the -275m elevation, approximately -400m away from hole TOW-91 -3. In addition,
l tt will test several unexplained HEM conductors in the area of a trench which contained boulders
|| of bedded massive pyrite in a ferrocrete cement. These boulders carried elevated Cu-Zn values.
A third hole will test several unexplained HEM conductors in the vicinity of the felsic volcanic-
l chert contact and will test the hangingwall contact at approximately the -225m elevation. Hole
^ TOW-91-2 located 400m along strike to the north intersected a 1.7m thick bed of massive
"' pyrrhotite containing up to 1*fc Zn70.9m. This pyrrhotite bed may be a lateral equivalent to one
l of the 3 targeted HEM conductors in hole 3. Hole 5-X will deepen previous hole TOW-91 -5 which
intersected strong stringer-type sulphides at the variolitic basalt contact. By extending the hole
•' a short distance, the hangingwall contact will be tested at an anticipated depth of 175m.
ii
l l l
l lri'
l l l l
-42-
12.0 REFERENCES
Augsten, B.G.k, 1988, Summary Report on the Tower Claim Group: Timmins Resident Geologist l FileT-3224.
Augsten, B.G.K., 1989, Geological Report on the Tower Claim Group: Timmins Resident Geologist H File T-3224.
Deptuck, R., Squair, H., and Wierzbicki, V., 1982, Geology of the Detour Zinc-Copper Deposits: m GAC Special Paper 25, p. 319-343.
GokJich, S., 1983, Ages of Precambrian Banded Iron Formations: Econ. Geol. V. 68, P. 1126- m 1 134.
Kranidiotis, P., and Maclean, W.H., 1987, Systematics of Chlorite Alteration at the Phelps Dodge - Massive Sulphide Deposit: Econ Geol V. 82, p. 1898-1911.
™ Laird, H.C., 1935, Ontario Dept. of Mines, Vol. XUV, Pt. 7.
l Morton, R.L., 1984, Subaqueous Volcanism: {Q Volcanic Rocks, Hydrothermal Alteration and™ Associated Massive Sulphide and Gold Deposits: R.L Morton and DA Groves eds., U.m of Minnesota-Duluth Short Course Notes, p. 15-45.
" Morton, R.L., and Franklin, J.M., 1987, Two-Fold Classification of Archean Volcanic - Associated Massive Sulphide Deposits: Econ. Geol. V. 82, p. 1057-1063.
Osterberg, M.O., 1985, Stratigraphy and Hydrothermal Alteration of Archean Volcanic Rocks at the Headway-Coulee Massive Sulphide Prospect: Unpub M.Sc thesis, U of Minnesota- Duluth, p. 114.
Ramsey, J.G., 1967, Folding and Fracturing of Rocks: McGraw-Hill, 568 p.
Rye, KA, 1984, Geology of the Cunningham 42 Base Metal Prospect: Unpub B.Sc Thesis, U. of Waterloo.
Siragusa, G.M., 1977; Cunningham and Garnet Twps jn Summary of Field Work, OGS MP 75, p. 88-92.
Siragusa, G.M., 1987, Geology of the Garnet Lake Area: OGS Report 248, p. 81.
Thurston, P.C., Siragusa, G.M., and Sage, R.P., 1977, Geology of the Chapleau Area: OGS Report 157, p. 293.
l l I l l l: APPENDIX lr M
DETAILED LTTHOLOGICAL DESCRIPTIONS
l
l
l
l
l
l
i l i i
l l l l l l l l l l l l l llll l l
-1-
FELSIC METAVOLCANICS
1) Rhyolite Flow - Colour typically medium to light grey when fresh, beige to buff when weathered. Typically very hard, massive to porphyritic texture with locally up to 10"* plagioclase phenocrysts set in an aphanitic siliceous groundmass. The phenocryst rarely exceed 2-3mm in size and are usually subhedral to anhedral. Unit may contain trace amounts of disseminated subhedral to euhedral pyrite.
2) Ash to Lapilli Tuff - Colour typically beige to light earthy brown when fresh, white to beige when weathered. Typically much softer than the rhyolite flows, and usually displays a strongly oriented fabric. This fabric appears as a distinct foliation and may represent primary bedding surfaces. Fragment abundance Is highly variable from nil to IS-20%, with fragments being usually of rhyolitic composition. In several locations (eg. 13+OOS 5+80W, 12+OOS 4+90W, 15+OOS 2+75W, etc.) rusty-weathering patches in the size and shape of the lapilli fragments were observed, and may represent sulphide fragments. The lapilli fragments are up to 10cm In size and are typically elongated parallel to the foliation. This unit has only been seen In the western portion of the claim group, south of line 8+OOS.
3) Debris Flow - Essentially a heterolithic fragmental unit with mafic/chloritic matrix. Colour dark green when weathered dark green to black when fresh, generally weakly to moderately magnetic, son to very son. Unit usually displays a fragmental texture with variable abundances of lithic fragments all matrix - to grain - supported in a massive chloritic matrix.
The matrix is foliated In some localities, and the unit was observed to be bedded (1m thick beds) in Trench 10-91. Lithic fragments are of variable sizes from 3-5mm up to 1 -2m (Trench 6-91), and are composed of either rhyolite, argillite, chert, or rare magnetite. One lithic composition may dominate In any one local (eg. rhyolite in Trench 7-91, cherts in Trench 16-91). Up to 5*K disseminated pyrite can be found in this unit. The lithic fragments are usually sub-rounded to rounded in shape, possibly indicating a sedimentary process rather than explosive volcanic process.
NOTE: Upon initial recognition of this unit in Trench 7-91, the field name "Felsic Agglomerate' (alphanumeric code: 3R agg) was applied due to the dominance of porphyritic rhyolite fragments. This field name was then uniformly applied throughout the trenching and drilling program for the sake of consistency. While fragment abundance and composition varied, the recognition that the matrix composition remained constant was used as an Identification criteria. Subsequent to completion of the exploration program, discussions with other geologists led to the interpretation of a debris flow. The initial appellation remains unchanged on trench notes, drill logs and sections.
l l l l l l l l l l l i i l l l i ii
•2-
CHEMICAL SEDIMENTS
1) Upper Chert - Colour variable from white to grey to black when fresh, same when weathered. Very hard, variably textured unit with textures varying from massive to bedded to fragmental. These textures make correlations of specific sub-units (eg. bedded chert) difficult across more than 100-200m. The fragmental-textured chert (alphanumeric code: 5 Cht-Brx) occurs in three basic formats: with a sulphide matrix, with a silica matrix, and with a magnetite matrix. In all cases, the unit is typically grain-supported with some instances of matrix-supported chert breccia being observed. The sulphide-matrix chert breccia consists typically of massive to weakly bedded pyrrhotite which may contain up to S-7% disseminated pyrite. These chert breccias usually grade into overlying Itthologles and show some preference for occurring near the lower reaches of the unit.
Interbedded throughout are clastic sediments (greywacke, argillite, graphitic argillite) which appear to occupy local basins, as correlations between dosely-spaced drill holes are difficult. These clastic sediments may represent episodes of turblditic deposition.
2) Variolitic Basalt - Colour light grey when fresh, same when weathered, typically moderately soft, non-magnetic. Characteristic of this unit is it's colour and presence of varioles. Variole abundance ranges up to IS-20% and variole size ranges up to 1-2cm. At times varioles coalesced into bands or patches of a very hard, siliceous material. Unit is weakly pillowed in places.
3) Lower Chert - Similar to Upper Cherts, but usually lacking the presence of any type of chert breccia. Unit typically much thinner than Upper Chert.
MAFIC METAVOLCANICS
Basalt - Colour medium to dark green when fresh, same when weathered, soft, non magnetic. Generally massive texture, but can be pillowed or contain pillow breccia in places.
INTRUSIVE SUITE
1) Granodlorite/Quartz Moonzonlte - Colour variable from pink to white on both fresh and weathered surfaces, massive texture, very hard. Typically feldspar-dominated and may contain up to S-5% disseminated biotite or hornblende(?). Several dikes of a (quartz)- feldspar porphyry occur throughout the property and are likely related to the larger pluton. Several dikes contain zoned plagioclase phenocrysts, possibly suggesting that they are sub-volcanic in nature.
2) Gabbro - Colour dark green when fresh and weathered, massive fine to medium grained texture. Unit is mafic-dominated, but some plagioclase can be seen In some locales.
i" APPENDIX III
ii LTTHOGEOCHEMICAL RESULTS
iiii i ii i
i
l f l l l i i
r^
{
^i
iii i i i il* i
•1-TOWER LAKE PROPERTY
TABULATION OF LITHOGEOCHEMICAL SAMPLE DETAILS
Sample No.
18114181171811818119181201812218123181241812518126181271812818129181301813118132181331813418135181361813718138
181471816118162181631816418165181781817918180181811818218197
696276964369644696456964669648
Location
8+OOS 5+50W9+75S 0+90E
11+OOSO+78E11+80S4+OOW12+OOS4+20W14+75S2+75W14+15S5+75W13+75S3+30W12+1 OS 5+75W10+10S3+80W9+40S 4+50W8+60S5+10W8+60S 5+35W8+50S 5+25W8+OOS 4+75W8+10S6+30W8+75S 6+50W9+30S9+15W
12+40S11+OOW13+90S1+10E
Trench 2-91Trench 2-91
Trench 3-91Trench 7-91
Shunsby PropertyShunsby Property
Trench 7-91Trench 7-91Trench 6-91Trench 8-91Trench 8-91Trench 8-91Trench 8-91
Trench 16-91
Trench 15-910+25S 3+25E
BL8+OOW6+OOS 3+50E1+OON2+OOE
Trench 11-91
FteldName
Massive RhyoliteVariolitic BasaltVariolitic BasaltRhyolite/Felsic TuffRhyoliteFelsic Lapilli TuffFelsic Lapilli TuffFelsic Tuff, MassivePorphyritic RhyoliteRhyoliteRhyoliteRhyoliteRhyoliteRhyoliteRhyoliteRhyoliteRhyoliteGranodioriteGranodioriteVariolitic BasaltVariolitic BasaltVariolitic Basalt
Variolitic Basalt?? Debris Flow Debris Flow Debris Flow Debris Flow Debris Flow Debris Flow (?) Debris Flow Debris Flow Rhyolite Rhyolite Debris Flow
Debris Flow Porphyritic Rhyolite Variolitic Basalt Variolitic Basalt Debris Flow Rhyolite
Remarks
Weak chloritization
Fresh-looking Chlorttized
Weak chloritization Area of chlorite fractures
Weak-mod chloritization Strong chl. alteration BJacK mod eh. alteration Black, foliated, chl att'd Fresh, weak ser att'n Fresh, weak ser att'n Weak chloritization Fresh looking Isaiah Creek Pluton Isaiah Creek Pluton Weakly foliated 4W/1+42N 4W/1+42N
Matrix only Character sample Character sample
Heavy chl. alteration
Small chert fragments Heavy chl. att'n zone Massive, fresh Moderately chloritlzed Chlorite stringer?
OC's at cabins
Old trail•Foliated basatf Strong chloritized
l l l l l l l ll i l i i i i l l l l
Sample No.
2301230223032304230523062307230823092310231123122313231423152316231723182319
Location
TOW-91-9,16mTOW-91-9,130.5mTOW-91-9,150.0m
TOW-91-8, 22.8mTOW-91-8, 34.1mTOW-91-7, 97.5m
TOW-91-7,138.7mTOW-91-8, 255.5m
TOW-91-6, 27.4mTOW-91-6,145.5mTOW-91-6,196.5mTOW-91-5,144.0m
TOW-91-4, 4.9mTOW-91-4, 97.0mTOW-91-4, 42.7m
TOW-91-3,152.5mTOW-91-2,15.1m
TOW-91-2,137.0mTOW-91-1,22.0m
-2-
FlekJName
Debris FlowVariolitic BasaltBasalt?Porphyritic DikeDebris FlowVariolitic BasaltBasaltBasaltDebris Flow?Variolitic BasaltBasalt?Variolitic BasaltVariolitic BasaltBasaltDebris FlowVariolitic BasaltRhyoliteBasaltPorphyritic Rhyolite
Matrix only
Ught brown colour
Matrix only Epldote-ser alt'n?
Moderate ser. alteration
Ught brown colour
ICRALXRF - WHOLE ROCK ANALYSIS 25-NOV-91 REPORT 17495 REFERENCE FILE 11259 PAGE 1 Of 2i
i i i i i i i i i i i i i i iP i
SAMPLE \ X SI02 AL203 GAO HGO NA20 K20 FE203 HNO T102 P205 CR203 LOI
XRF W.R.A. SUMS INCLUDE ALL ELEMENTS DETERMINED. FOR SUMMATION, ELEMENTS ARE CALCULATED AS OXIDES
SUM
181 H18117181181811918120
1812118122181231812418125
1812618127181281812918130
1813118132181331813418135
1813618137181381814718161
1816218163181641816518178
1817918180181811818218197
6962769643696446964569646
6964769648
66.351.349.566.647.9
SMPMISS66.860.471.961.5
51.170.160.563.869.4
70.170.364.370.074.2
46.566.150.851.447.5
34.953.761.449.664.0
44;236.165.060.055.7
71.567.754.147.362.0
50.041.6
14.914.715.616.315.7
SMPMISS16.813.411.916.5
13.67.8314.416.616.5
16.013.717.815.213.8
17.014.723.915.111.4
5.6712.517.411.516.1
1.438.4115.912.411.4
9.8516.322.612.518.8
15.012.7
2.374.999.451.779.81
SMPMISS3.372.41.87
2.63
9.127.424.043.453.63
1.384.152.381.531.11
2.814.123.845.505.13
1.993.212.212.781.03
1.00.21
2.06.88
1.20
.924.83.22
12.73.26
10.55.05
2.136.184.682.014.91
SMPMISS1.843.532.253.01
9.164.863.131.882.07
2.111.331.801.16.29
4.612.402.536.133.43
4.002.662.453.722.50
3.144.972.612.782.69
2.271.522,933.342.04
6.524.57
1.03.69
2.282.98.55
SMPMISS1.072.68.38
3.77
1.87.52
1.28.53.69
1.012.67.34
6.455.22
.353.99.45
1.39.44
.05
.741.86.07.95
.09
.05
.91
.38
.06
.592.34.56
2.682.86
1.17.06
1.96.56.75
2.191.27
SMPMISS2.941.142.171.77
.27
.90
.813.392.30
2.881.076.742.323.47
.68
.52
.83
.47
.39
^01.59
2.78.05
2.67
.06^012.15.51.09
.642.134,091.112.46
.13^01
9.1013.49.075.1215.1
SMPMISS2.92
13.16.087.16
11.85.6711.97.192.71
3.445.203.052.241.06
20.95.4511.014.526.6
37.419.37.12
25.17.84
44.234.37.4617.624.0
10.82.429.638.595.39
12.226.2
.18
.28
.34
.10
.41
SMPMISS.10.17.14.18
.22
.19
.31
.21
.13
.15
.15
.14
.05
.02
1.16.08.14.24
1.22
1.97.56.65
1.08.28
1.631.58.37.82.96
.21
.11
.14
.31
.24
.221.12
.387
.845
.874
.4691.16
SMPMISS.433.341.259.658
.757
.1031.29.414.458
.379
.335
.427
.273
.114
1.01.863
1.44.989.324
.176
.385
.559
.417
.488
.056
.189
.435
.356
.152
.240
.4161,27.686.510
.864
.411
.10
.08
.10
.13
.11
SMPMISS.08.09.07.14
.07
.04
.17
.12
.11
.08
.08
.10
.09
.04
.07
.08
.08
.09
.10
.06
.11
.14
.13
.11
.05
.05
.13
.11
.05
.07
.09
.13
.07
.14
.09
.11
.02
.07
.08*.01.02
SMPMISS*.01^01*.01•c. 01
.05•c. 01^01t. 01<.0^
^01^01•c.OI.03.04
.10
.08
.12
.03<.0^
t. 01t. 01^01^01i.01
01^01^01.01.01
t. 01^01.11.06^01
.08t.01
1.936.627.772.772.62
SMPMISS3.772.932.772.93
2.231.772.702.471.93
2.541.232.16.70.39
4.541.545.004.393.39
13.96.233.395.543.93
3.3913.43.084.003.93
2.542.394.4710.22.62
3.088.31
100.599.8100.6100.599.6
...100.2100.398.9100.4
100.399.4100.6100.2100.0
100.2100.399.4100.299.9
99.8100.0100.2100.3100.0
100.1100.0100.1100.0100.0
99.399.3100.299.9100.3
99.7100.4100.699.6100.4
99.9100.2
X-RAY ASSAY LABORATORIES 1885 LesEe Street Don Mis Ontario M3B 3J4 (416)445-5766 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Society Ginerale de Surveillance)
IKRALSAMPLE
1 18114 1811718118
m 1 8119M 1 8120
18121u 1 8122M 18123 M 1 8124
18125
1 181261812718128
1 1812918130
18131
1 18132181331813418135
1 181361813718138
1 1814718161
18162
1 18163181641816518178
1 18179" 18180
18181
1 18182 18197
69627
1 69643 696446964569646
| 6964769648
1
1
1
XRF - WHOLE ROCK ANALYSIS
\ PPM RB SR Y
82 74 47 7450 14681 17758 61
15 00272216
25-NOV-91 REPORT
ZR NB BA
128 7691
13973
SMPMISS SMPMISS SMPMISS SMPMISS130 5254 166
109 2680 293
26 8948 5252 82
104 9181 64
135 6625 201
128 5180 358
113 342
44 10936 20759 4342 11932 00
OO OO37 23
138 113OO 13134 43
26 00OO OO99 12633 4722 OO
45 1680 295
142 10649 77
111 253
20 7721 OO
1 X-RAY ASSAY LABORATORIES 1885 Leslie MemHor nf t
OO16 18
OO
0029221217
OO1824
OOOO
11OO
1514
OO
OOOO3315
00
OOOO
1811
00
OOOO 301616
16OO
StreetIB 8RS
170155 123125
4972
13287
126
13711210612362
11574
12568
105
81106154113108
2155
124107 126
11498
13964
126
83111
Donirrmn
OO 28161417
513
220
244486203
SMPMISS SMPMISS18
OO 2615
27163024
00
2313221222
2717
OO00
23
3224131028
14281015 19
1319
OO3519
1634
Mills OntariofSru-i*t* RAr
270314 400681
107123201776286
544292958861658
150229185227103
133292482
85474
154127428116 118
212614 627135438
7799
walApAl
REPORT 17495 REFERENCE FILE 11259 PAGE 2 of
l l l l l l l l l l l l l l l l l l
XRF - WHOLE ROCK ANALYSIS 27-JAN-92 REPORT 18060 REFERENCE FILE 11597 PAGE 1 Of
SAMPLE \ X SI02 AL203 CAO MGO NA20 K20 FE203 HNO TI02 P205 CR203 LOI
XRF W.R.A. SUMS INCLUDE ALL ELEMENTS DETERMINED. FOR SUMMATION, ELEMENTS ARE CALCULATED AS OXIDES
SUM
23012302230323042305
23062307230823092310
23112312231323U2315
2316231723182319
32.948.845.168.262.1
57.847.149.165.847.1
45.054.351.544.965.4
62.664.346.967.4
11.314.713.215.213.6
20.415.614.018.211.8
14.916.518.113.310.4
14.615.815.514.9
5.056.449.901.98.89
1.497.3510.43.299.23
9.228.164.219.791.76
3.832.0111.93.22
5.046.115.961.113.01
2.199.067.912.265.72
5.711.974.447.512.16
2.722.486.021.13
.02
.501.437.23.08
.292.191.49.30
2.77
3.564.884.491.70.25
5.353.70.48
6.40
.021.85.33.59
1.66
3.611.30.70.54.14
.081.511.47.33.90
.671.651.561.00
36.312.012.12.6013.8
7.8112.312.34.5911.7
10.45.827.3911.314.5
4.376.2012.12.37
1.80.25.19.05.52
.22
.23
.20
.13
.21
.17
.18
.19
.19
.18
.10
.21
.15
.05
.312
.809
.832
.302
.378
1.12.811.691.423.971
.767
.899
.995
.669
.288
.833
.444
.806
.328
.07
.08
.07
.11
.10
.06
.07
.06
.09
.35
.07
.10
.10
.06
.07
.08
.11
.08
.12
K.01
.06
.02
.01•e. 01
.09
.02
.04^01.06
.04
.08
.08
.03^01
.08O1.03^01
7.398.9311.41.624.16
3.853.002.083.238.85
9.774.775.1610.23.00
3.002.703.932.62
100.2100.6100.699.1100.4
99.099.199.098.999.0
99.799.398.2100.099.0
98.399.799.599.7
X-RAY ASSAY LABORATORIES 1886 Leslie Street Don Mils Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Socltte G6n*rale de Surveillance)
IWii/vL
SAMPLE
1 2301 23022303
— 23041 2305
2306m 2307M 2308M 2309
2310
1 2311 23122313
1 2314 2315
2316
1 2317 2318 2319
1
1
1
1
1
1
1
1
1
1
| X-RAY ASSA1
XRF - WHOLE ROCK ANALYSIS 27- J AN -92 REPORT
\ PPM RB SR Y ZR NB BA
OO OO 12 227 21 99 84 44 00 120 27 29619 53 33 83 15 66
OO 694 11 119 OO 37654 OO OO 137 OO 485
144 26 30 127 14 44372 142 25 65 17 28932 121 23 48 OO 13441 100 00 133 OO 124
OO 232 23 128 15 109
OO 70 12 59 14 77 53 284 30 80 16 39058 188 OO 113 16 24214 76 23 50 26 145 63 22 OO 127 OO 167
27 173 15 79 23 15653 148 16 132 16 398 55 86 21 54 21 15040 609 OO 122 OO 484
r LABORATORIES 1885 Leslie Street Don Mils Ontario M3IMomhor nf the Sfifi firm in (Knrlttt, fit,ntrm\
REPORT 18060 REFERENCE FILE 11597 PAGE 2 of
l l l l i i i l
i i l l l i i l i l
FeO* -f TI02
•f RhyoHt* X Dtbrit Flow* WrtoStlc BasaltO Hanglngwal BattK A Quartz Monzonitt
/Quartz-Ftldspar Porphyry
A12O3 MgO
after Jensen, 1976Nl
TOWER (10ft)
Jent*n Cation Plot
NORANDA EXPLORATION CO LTD
l l l l l l l l l i l l ll i i i l l
FeO*
4. Rhyolitt X Dtbri* Flow 9 tortoltlc Batatt O HangingwaU Batalt 4 Quartz Monzonftt
/Quartz-Feldspar Porphyry
Na2O -l- K2O
•fur Irvine -l- Baragw, 1971 .Mt
MgO
TOWER (106)
AFM Plot
MUMM W-_.—.__..NORANDA EXPLORATION CO LTD
l lr
i
lf -i i i i i k i i i i l i li i
APPENDIX IV
ASSAY CEHTFICATES
1111
x^tfcK Swastika Laboratories ocr tim^^^KjJ^Sl A i/ A Division of Assayers Corporation Ltd. | ^o^-riftN
^^^^P^^^^ i, i ORAvNDA EXPtOnM 1WNEstablished 1928 ^ Assaying - Consulting - Representation \ N T,SS5oN^^
Geochemical Analvsis Certificate
Company: NORANDA EXPLORATION CO. LTD.Project: 206
1W-4167-RG1
Date: OCT-17-91Copy 1. P.O.BOX 1205, TIMMINS. ONT.P4N7J5
Ann: ROGER DAHN/JOHN WAKEFORD
111
111111111
i
1t i1
We hereby certify the following Geochemical Analysis of 9 ROCK
2. FAX TO 268-9572
samplessubmitted OCT- 10-91 by ROGER DAHN.
SampleNumber18401 ———184021840318404 -y.18405 "**18406184071840818409 ~fffa
l 0
Au Ag Cuppb Ppm PP"^
1 34 50^01 1.8 22801 3.0 1230
l r- d\ l 0 - 4 442^ 5 -7* 1 1.8 806
1 0.2 9291 1.2 13201 0.7 1490
,M-f| 55/69 3.0 344
-z^
Certified by Ljtaf\
Pb Znppm ppm
36 40528 77996 73
8 11017 80
3 12238 76810 91
312 2740
K/'WX c^i-JTL'\^y^JL**~**c.^-
l P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244, FAX (705)642-3300
l111
•' ^
^^B^MR
^ -t T t - REGEiVED^ Swastika Laboratories3 1 A Division of Assayers Corporation Ltd. jfjV A 1 QQ1— * i* 7 * r . : N V,/ V ** lv V*
Established 1928 ^ Assaying - Consulting - Representation ^^ E:. pLORAT , crj
i CO. LVO.T.r.'r.-.:^v-.owT.Assay Certificate 1W-4293-RA1
comply: NORANDA EXPLORATION CO LTD. Date: OCT-30-91Project: Copy 1. P.O. BOX 1205 TIMMINS, ONT. P4N 7J5Attn: R.DAHNU.WAKEFORD Z.OQ, 2. FAX TO 268-9572
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
We hereby certify the following Assay of 9 ROCK samples submitted OCT-28-91 by .
SampleNumber69604 ——— 696056960669607 ^69608 ( ft*696096961069611 69612
^/^ f (T? Au Au Au check Au check /-ex^c ycg/tonne oz/ton g/tonne oz/ton -**'1'
i —— 0.03 .0010.05 .001 0.04 .0010.04 .0010.10 .003
Ox 13-5 f 0.06 .0020.04 .0010.08 .0020.14 .004 0.14 .004 0 .OS 001
1^ f/Certified by K^J^VV^NCK (TT^ir^L^Q/^-
P.O. Box 10, Swastika, Ontario POK 1TOTelephone (705) 642-3244 , FAX (705)642-3300
111111111111111111
^gtH e. w—-. '-- - — - i
^ Swastika Laboratories w B w 1fl A Division of Assayers Corporation Ltd. S ^ ;
Established^ ^ Assaying - Consulting - Representation i ^^'^^•Pagfel of '3"~
Geochemical Analvsis Certificate 1W-4297-RG1Company: NORANDA EXPLORATION CO LTD. Date: OCT-31-91Project: l/ ^ n f Copy 1 . P.O. BOX 1205.TIMMINS, ONT. P4N 7J5 Am: R. DAHN \J. WAKEFORD T ^Q 2. FAX TO 268-9572
We hereby certify the following Geochemical Analysis of 76 ROCK samples submitted OCT-28-91 by .
SampleNumber
Ag Cu Pb Znppm ppm ppm PP01
18115 ? wes &L 0 .5 155 34 ' 32618116 7/tvs c18121 MfKS18139 |18140 118141 -r-/18142 "^1814318154181551815618157 ^18158 ft*18159181601816618167181681816918170 -{jr,,.181711817218173181741817518176 f?6YA*1817718183 118184 -7^' t18185 l
V
f^w 0.8 625 62 199i/Tffvv 0.1 207 11 44
3.0 421 275 17403.4 332 1170 5850
,, 5, 2.1 424 535 2390' 0.9 97 4570 1900
1.4 132 235 10002.2 9680 27 1791.1 1210 38 10100.3 406 12 69
. 1.1 767 151 56tKpJ 1 1.6 2590 38 1090
3.2 532 82 577.8 5840 38 68800.2 106 1 1270.6 53 2 550.4 43 1 550.6 51 1 54
^1J( 0 .3 56 2 530.3 56 1 700.1 37 1 710.2 49 8 620.2 45 8 61
[ 0.1 14 1 14',-H 0 .1 11 1 13
0.1 16 1 110.4 48 10 62
fl.3( 0.4 46 14 740.2 24 12 134
ft )JCertified bv L^A^V^^C?^CLv?t^Jl^
lP.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244 FAX (705)642-3300
l l l l l l l l l l l l l l l l l l l
Established 1928
Swastika LaboratoriesA Division of Assayers Corporation Ltd.
Assaying - Consulting - Representation
Geochemical Analysis Certificate
Page 2 of 3
1W-4297-RG1
comply: NORANDA EXPLORATIONProject:
CO LTD.
Attn: R. DAMN \J. WAKEFORD
We hereby certify the following Geochemical Analysis submitted OCT-28-91 by .
SampleNumber18186181871818818189181901819118192 -T-O18193 ' ^1819418195181961819818199 -y-.18200 "^696016960269603696136961469615 -^.^69616696176961869619696206962169622 -r,*69623 |6962469625 y
Agppm0.30.30.40.10.20.1
i h a ( 0.6^-^ 0.4
0.50.20.30.1
kit, V 0 ' 1Mfc-* 1 o.i0.10.32.20.20.6
UJL — — — ?:?-..-1.93.10.91.71.41.7
A j d-vl 0.5^n 1.3
2.72.1
Cuppm
22312817242147302220232932
10632
198330522422817597758
109010805320
330767
1120554535
of 76
Pbppm
332111242231131
141600
128
36111195
673
10510719468
Date: OCT-31-91Copy 1. P.O. BOX 1205.TIMMINS, ONT. P4N7J5
2. FAX TO 268-9572
ROCK samples
Znppm
21716390839546624958472332
151123322
6280668
1940183031402040
8256
1632720
293439029603400
Certified by
P.O. Box 10, Swastika, Ontario POK1TO Telephone (70S) 642-3244, FAX (705)642-3300
l l l l l l l l l l l l l l ll
i
lll
Established 1928
Swastika LaboratoriesA Division of Assayers Corporation Ltd.
Assaying - Consulting - Representation
Geochemical Analysis Certificate
Page 3 of 3
1W-4297-RG1
Company: NORANDA EXPLORATIONProject:Attn: R. DAHN \J. WAKEFORD
CO LTD.
We hereby certify the following Geochemical Analysissubmitted OCT-28-91 by .
Sample AgNumber ppm69626 ^ftrik ik-'9( 6 .969628 2.269629 1.769630 2.069631 1.969632 3.369633 1.769634 ^ , 1.769635 f/iWAV-? 1 2.069636 7.269637 8.769638 4.669639 9.669640 0.469641 -TVCfccA 1 -^ 1 0 - 769642 0.9
Cuppm
113052601740777747
1050985905623792
1630647789
383749
Date: OCT-31-91Copy 1. P.O. BOX 1205.TIMMINS, ONT. P4N 7J5
2. FAX TO 268-9572
of 76 ROCK samples
Pbppm
381231279198
13618114492
248438289
9980651019
Znppm
1410259902
183047805640354023302630443047803620
40500214
6681
Certified bv dy&vL^S^
P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244. FAX (705)642-3300
1111111111111111ii111
^.*^W Swastika Laboratories^3(^^JB?5 A Division of Assayers Corporation Ltd.
Established 1928 Assaying - Consulting - RepresentationPage 2 of 2
Assay Certificate 1W-3531-RA1Company: NORANDA EXPLORATION (TIMMINS) Date: AUG-01-91Project: Copy 1. P.O. BOX 1205 TIMMINS ONT.Attn: 2. FAX TO 268-9572
We hereby certify the following Assay of 33 ROCK samples L 7 ^^ submitted JUL-28-91 by . - ^
Sample Au Au Au check Au check Ag Cu PbNumber g/tonne oz/ton g/tonne oz/ton ppm ppm ppm80860 0.01 .001 4.6 812 896080861 0.01 .001 0.01 .001 1.9 245 182080862 0.01 .001 5.1 124 212
ft -HCertified by\^6V\*^A ^T&yjL^Q*^
P.O. Box 10, Swastika, Ontario POK 1TO Telephone (705) 642-3244 , FAX (705)642-3300
Znppm
2100062801540
111111111111111
w
c^Bis^a ^Established 1928 AR
Swastika LaboratorA Division of Assayers Corpoi alton W^O E
Assaying - Consulting - R( presentatiokiic *!•M.JVJ
Assay Certificate NO*ANDAEco.company: NORANDA EXPLORATION (TIMMINS) ^^j^*Project:Attn: OR-IC* |A
Vie hereby certify the submitted JUL-28-91
Sample Number
8085180852808538085480855
i\i'P f\
njg^ Pag j 1 of 2
riORATioiW 3531-RA1LTD..^. ONT Tiiin iV JG-01-91
Copy 1 . P.O. BOX 1205 TIMMINS ONT.j-Av __ I/O -**- "Z-O \ 2 - FAX TO 268-9572
following Assay of 33 ROCK samples by.
Au Au Au check Au check Ag g/ tonne oz/ton g/ tonne oz/ton ppm
~o~3T !ooi 0.30.01 .001 .f ^ r 3 .90.01 .001 i ^.Cs {C- 4 .70.01 .001 V 2.8
Cu Pb Zn ppm ppm ppm
18 6 22525 172 492671 159 459
1310 20200 62500__ Q..54 .001 4.0 954 68 3960
l l Certified by
P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244. FAX (705)642-3300
MAXMIIVI MEM
Five frequencies: 222, aa*, BBS, 1777 and 3555 Hz. Maximum coupled C horizontal-loop J operation with reference cable.Minimum coupled operation with reference cable. Vertical-loop operation without reference cable.CollBeDarations: 25, 5O, 1OO , ISO , 2OO and 25Om CwltTTcSble J or lbo,2Oa,3Da,aaO,6OOand BOO ft.Reliable data from depths of up to ISO m C GOO ft). Built-in voice communication circuitry with cable. Tilt meters to control coil orientation.
•'
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SPECIFICATIONS :
Frequencies: 222,444,BBS, 1777 and 3555Hz. Repeatability:
Modes of Operation: MAX:
Coil Separations:
Parameters Read:
Readouts:
Scale Ranges :
NOW ALSO ±4* QUADRATURE FULL SCALE.
Readability:
Transmitter coil plane and re ceiver coil plane horizontal (Max-coupled ; Horizontal-loop model Used with refer, cable .
IV! l N: Transmitter coil plane horizon tal and receiver coil plane ver tical CMin- coupled mode). Used with reference cable.
V. L. Transmitter coil plane verti cal and receiver coil plane hori zontal (Vertical-loop mode]. Used without reference cable , in parallel lines.
25,50,1(30,150.200 S25Omor 1OO, 2OO, 3OO, 4OO,6OOandBOO ft. (MMHF).Coil separations in VL.mode not re stricted to fixed values .
- In-Phase and Quadrature compo nents of the secondary field i n MAX and M IN modes.
- Tilt-angle of the total field in V.L. mode .
- Automatic, direct readout on 9Qmm (3.5") edgewise meters in MAX and MIN modes. No null ing or compensation necessary .
- Tilt angle and null in 9Omm edge wise meters in VL.mode .
In-F'hase: ±2OV.,t1OOV. by push button switch .
Quadrature: *2O -/., fOOV. by push button switch .
Tilt: ±75 '/o s lope .NullCVLJ: Sensitivity adjustable
by separation switch.
In-Phsse and Quadrature : O.25 */. to 0. 5 V. ; Tilt: 1 '/. .
±O.25 0Xoto±1 0Xo normally, depending on conditions, frequencies and coil separation used .
Transmitter Output: - 222Hz : 22OAtme- 444HZ : SCO Atme- BSBHz : 12OAtms- 1777 Hz : BOAtme-3555 Hz : 3OAtme
Receiver Batteries: 9V trans radio type batteries (4). Life: approx. 35hrs. continuous du ty (alkaline , O.5 Ah), less in cold weather.
Transmitter Batt e r le s :
Reference Cable :
Voice Link:
12V 6 Ah Gel-type rechargeable battery. (Charger supplied).
Light weight 2-conductor teflon cable for minimum friction. Unshield ed. All reference cables optional at extra cost. Please specify.
Built-in intercom system for voice communication between re ceiver and transmitter operators in MAX and MIN modes, via re ference cable .
Indicator Lights: Built-in signal and reference warn ing lights to indicate erroneous readings .
Temperature Range: - 4O0Cto*6O"C (-4O"Fto*14O0F).
Receiver Weight: B kg ( 13lbs.)
Transmitter Weight: 1 3kg (29lbs.)
Shipping Weight: Typically BOkg (135 Ibs.), depend ing on quantities of reference cable and batteries included. Shipped in two field/shipping cases.
Specifications subject to criange without notification.
APEX PARAMETRICS LIMITED2OO STEELCASE RD. E., MARKHAM, ONT, CANADA, L3R 1G2
Phone: (416) 495-1612 Cables: APEXPARA TORONTO : aeasearoaD6-966775 APEXPARA MKHM
Page l
EMl6 SPECIFICATIONS
MEASURED QUANTITY
SENSITIVITY
RESOLUTION
OUTPUT
OPERATING FREQUENCY
OPERATOR CONTROLS
POWER SUPPLY
DIMENSIONS
WEIGHT
In-phase and quad-phase components of vertical magnetic field as a percentage of horizontal primary field, (i.e. tangent of the tilt angle and ellipticity) .
In-phase : Quad-phase :± 401
Nulling by audio tone. In-phase indication from mechanical inclino meter and quad-phase from a graduated dial.
15-25 kHz VLF Radio Band. Station selection done by means of plug-in units.
On/Off switch, battery test push button, station selector switch, audio volume control, quadrature dial, inclinometer.
6 disposable 'AA' cells.
42 x 14 x 9cm
Instrument: 1.6 kg Shipping : 4.5 kg
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ntario410ieiNE92a2 a. 15106 CUNNINGHAM 900
Ministry ofNorthern Developmentand Mines
Ministere duDeveloppement du Nord et des Mines
November 19, 1993
Geoscience Approvals section Willet Green Miller Centre 933 Ramsey Lake Rd 6th Floor Sudbury, Ontar io P3E 6B5
Telephone: (705) 670-5853 Fax: (705) 670-5863
Our File: 2.15106 Transaction #: W9360.00120
: W9360.00122
Mining Recorder Ministry of Northern Development and Mines 60 Wilson Avenue 1st Floor Timmins, Ontario P4N 2S7
Dear Sir:
RE: APPROVAL OF ASSESSMENT WORK ON MINING CLAIMS P 1030179 ET AL. IN CUNNINGHAM TOWNSHIP.
The Assessment Credits for GEOLOGY, GEOPHYSICS and ASSAYS, sections 12, 14 and 17 of the Mining Act Regulations, as listed on the above reports of work, have been approved.
The approval date for report of work W9360.00120 is October 29, 1993, and for report of work W9360.00122, is September 16, 1993.
Please indicate these approvals on the claim record sheets.
If you have any questions please call Clive Stephenson at (705) 670-5856.
Yours sincerely
Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division
CDS/ls
v/ cc: Assessment Files Office Toronto, Ontario
Resident Geologist Timmins, Ontario
Transaction NumberReport of Work ConductedAfter Recording Claim __ __ _
Mining ActPersonal Inf^Btlon collected on this form Is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street, Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264.
Ministry otNorthern Development w)rt M ines
Ontario (
2. 1 5 106MfHlng assessment work or coni
Instructions: - Please type or print and submit in duplicate. ^- Refer to the Mining Act and Regulations for requirements of filing
Recorder.- A separate copy of this form must be completed for each Work Qroup.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.
consult the Mining
Recorded Hdder(t)- ....*r?m Vv\.X*roll
Address
. .fUOT/W*
Mining DMslonAJJft fc fl******-*
Township/AreaUi
Client No.
W, (W To:
Work Performed (Check One Work Group Only)WorkGroup
Geotechnical SurveyPhysical Work, Including Drilling
RehabilitationOther Authorized Work
AssaysAssignment fromReserve
Typef \ f -ft t . \ \ Jl* |J i i? Art l/l C*.Q^jvo*i*1 1 M lki^tockf"^ , MK# C u a^'j i n *- V. 1 'i i *- r ttf
RECORDED
JUN 2 1 1993
Receipt
Total Assessment Work Claimed on the Attached Statement of Costs 3SNote: The Minister may reject for assessment work credit all or part of the assessment work submitted If the recorded
holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.
Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address
W fu HH. MLCi. (YLF-fr'i
R. fcfllft.LilL}
(attach a schedule 11 necessary)
Certification of Beneficial Interest * See Note No. 1 on reverse side(holder or Agent (Signature)l certify that at the time the work was performed, the claims covered In this work
report were recorded In the current holder's name or held under a beneficial interest by the current recorded holder.
Date
Certification of Work Reportl certify that l have a personal knowledge of the facts set forth In this Work report, having performed the work or witnessed same during and/or after Its completion and annexed report Is true.
Name and Address of Penon Certifying
No* Oats Certified f3y (Signature)
r -~ -^For Office Use Only
rotal Value cr. Hecoroea oats Recorded
OC41(OM1)
Details^ lork Report l NEONT93.018 Page l
York Report! for Applying
ReserveClaii (see
P 1P 1P 1P 1P 1
P 1P 1P 1P 1P 1P 1P 1P lP tP tP lP l
Nuiber note 2)
.176,988
.176,989
.176,990
.176,991
.178,992
.176,993
.030,179
.030,180
.030,181
.030,182
.030,183
.030,184
.030,165
.030,186
.030,187
.030,188
.030,189
17
t Of Claii Units
11111111111111111
Total Nuiber of Claiis
Total Value Hork Done
Value of Assesient Vork Done
on this Claii2,569.002,350.00
2,527.00
2,901.00
2,325.00
2,325.00
1,128.00
466.00
347.00
347.00
438.00
635.00
853.00
425.00
347.00
2,834.00
2,723.00
25,540.00
Value Applied to this Claii
—— RECOt
—— JIWJL
Receipt ,— basa*""———
0.00
Db
n. 13
Values Assigned froi this Claii
3 —— ———
QT3*1 ——— ——————
0.00
Reserve:Kork to be ClaiMd at
a future Date2,569.002,350.002,521.002,901.00
2,325.00
2,325.00
t, 128.00
461.00
347.00
347.00
438.00
835,00
853.00
425.00
347.00
2,834.00
2,723.00
25,540.00
Total Value Hork Applied
Total Assigned Froi
Total Reserve
Credits you are claiiing in this report lay be cut back. In order to linilize the adverse affects of such deletions, please indicate froi which claiis you wish to priorize the deletion of credits. Please lark (x) one of the following:1.!) Credits are to be cut back starting with the claiis listed last, working backwards. - ---- r - --T~-~j —LJ i ..., - ,
2.F] Credits are to be cut back equally over all claiis contained in this report of
3.M Credits are to be cut back as priorized on the attatched appendix.
," -- .. .,~*: -. . - ' ' ' ~*-'" ' i\; • '••i* '': " v i ;f' : , -..'A : • -•- J \:^. j
JUN 2 11983j4.1x1 Credits are to be cut back starting with the claiis that have reserve credits.
In the event that you have not specified your choice of priority, option one will be iipleiented.Note 1: Exaiples of beneficial Interest are unrecorded transfers, option payients, leiorandui of agreeients, etc.,
with respect to the lining claiis. Note 2: If work has been perforied on patented or leased land, please coiplete the following:I certify that the recorded holder had a beneficial interest in the patented or leased land at the tiie the work was perforied.
Signature Date
Ontario
Ministry of•Northern Developmentt Jines
^feitere du B^loppement et des mines
duNord
Statement of Costs for Assessment CreditEtat des coQts aux fins du credit devaluationMining Act/Lol sur tot mines
Transaction HoM* d* transaction
Personal Information collected on this form Is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines, 4th Boor, 159 Cedar Street, Sudbury, Ontario P3E 6AS. telephone (70S) 670-7264.
Let renselgnements personnels contenus dans la presente formule sent recuelllis en vertu de la lo! sur lea mines et serviront a tenir 4 Jour un registre des concessions mlnieres. Adresser toute question sur la collece de ces renselgnements au chef provincial des terrains mlnters, ministers du Devetoppement du Nord et des Mines, 159. rue Cedar, 4* etage, Sudbury (Ontario) P3E 6A5, telephone (70S) 670-7264.
1. Direct Costs/CoOts directs
Type
Wag** SalatnM
Contractor's and Consultant's Fees Drottsde ('entrepreneur et de ('expert-
flupptles Used PountHufM
Equipment Rental
material
Description
Supervision sur le terrainTyp*
Type
Typt
Amount Montant
Total Direct Costs Totsl des eoQts directs
Totals Total global
2. Indirect Costs/Gouts Indirect** * Note: When claiming Rehabilitation work Indirect costs arc not
allowable as assessment work. Pour le remboursement des travaux de rehabilitation, lea coOts Indlrects ne sort pas admissible* en tant que travaux d'evaluatlon.
Type
Transportation Transport
Food andLodging Noumtureet rtebtrcementMobflteatlon and Demobilization MoMHeatlonet demobilisation
Description
UN 2 1
Amount Montant
Sub Totsl of Indirect Costs Totsl partial des coOts Indlrects
Amount Allowable (not greater than tt* of Direct Costs) Montant admissible (n'cxoMant pas 20 H des coots directs)Total Value of Assessment Credit (Totalof Direct and AKowaMeIffMlfMI C09t9|
Valeur total* du cnWH4i*4kJ*k*ttU*AO wVmMUUn(TetstdttteMta^ttki etkMRneltaMtsMis
Totals Total global
Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. H verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.
Note: Le titulalre enregMre sera tenu de verifier lesdepensesdemandees dans le present etat des coOts dans lee 30 Jours survant une demande a eel effet. SI la verification n'est pas effectuee, le mlntotre peut rejeter tout ou une partie des travaux d'evaluatlon presentee.
Filing Discounts
1 . Work filed within two years of completion Is claimed at 10Wfe of the above Total Value of Assessment Credit.
Remises pour depot
1. Les travaux deposes dans tos deux ans survant tour achevement sont
2. Work filed three, four or five years after completion Is claimed at 504fc of the above Total Value of Assessment Credit. See
' calculations below:
Total Value of Assessment Credit x 0.50 -
Total Assessment Claimed
2 . Les travaux deposes trois. quatre ou cinq ans apres tour achevement sont rembourses a 60 "to de la valeur totale du credit d'evaluatlon susmentlonn*. Volr tos calculs d-dessous.
Valeur totale du credit d'evaluatlonx 0,50
Evaluation totale demandee
Certification Verifying Statement of Cost*
l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.
thatss
Attestation de I'etat des coOts
J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont ete engagees pour effectuer les travaux devaluation sur tos terrains Indiques dans la formule de rapport de travail cl-jolnt.
Et qu'a tltre de je suls aulorise(UtulAlr* •nr*glstr*. rapreMntant, pott* occup* dant to eomp^nl.)(Rtcoritod HohJ*r. Agtpt,
to make this certification
0312 (04*1) Nota : Dani cett* formule. kxsqu'll design* des partonnes, le masculln est utlllt* au sens neutre.
Ministry of. Northern Development
a 1 " MinesOntario
informal!
Report of Work Conducted After Recording Claim
Mining Act
Transaction Number
Personal information collected on this form Is obtained under the authority of the Mining Act. This information will be used for correspondence, Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street, Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264. ^
9 1 c: 1 Q 6Instructions: - Please type or print and submit in duplicate. *w * J. t/ J. vr v- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining
Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.
From: A^usV i,miWork Performed (Check One Work Group Only)
Work Group
Geotechnical Survey
Physical Work, Including Drilling
Rehabilitation
Other Authorized Work
Assays
Assignment from Reserve
Type
WUjfocU, ^fVUUffim *frQ*)
^ —— —— *-RECORDED
JUN 2 1 1993
- —— -^ —— —— ""
Total Assessment Work Claimed on the Attached Statement of CostsNot*: The Minister may reject for assessment work credit all or part of the assessment work submitted If the recorded
holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.
Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address
ViW lt\M r aL rTtl lo . ITZ)ftttaii
(attach a schedule If necessary)
Certification of Beneficial Interest * See Note No. 1 on reverse side1 certify that at the time the work was performed, the claims covered In this work report were recorded In the current holder's name or held under a beneficial interest by the current recorded holder.
Date
Su* l&.lW
RecordaAWblder or Agent (Signature)
Certification of Work Reportl certify that l have a personal knowledge of the facts set forth In this Work report, having performed the work or witnessed same during and/or after Ks completion and annexed report Is true. ____________ ___ ^^
Name and Address of Pereon Certifying
Tetopone No. Date Certified By (signature)
For Office Use OnlyTotal Value Gr. Recorded Date Recorded
0941 (OS/91)
Details^ fork Report t NEONT93.020 Page \
York Report! for Applying
ReserveClaii (see
P 1P 1P 1P 1P 1P 1P 1P 1P 1P 1P 1P 1P 1
Nuiber note 2)
, 030, 180.030,181
.030,182
.030,183
.030,184
.030,181
.030,187
.030,188
.030,189
.176,988
.176,989
.178,990
.176,991
t of Clan Units
1111111111111
13
Total Nuiber of Claiis
Total Value Hork Done
Value of Assesient work Done
on this Claii
97.0049.00
380.00365.00333.00124.00
319.00
313.00
154.00
24.00
194.00
148.00
24.00
Value Applied to this Claii
———— —— ft
J
Daroir
" f\f— ^"^
IN:t.-
Values Assigned froi this Claii
IRDED ^
i 1 1993
.nr
Will f,.
Reserve:Hork to be Claiied at
a Future Date97.0049.00
360.00365.00333.00
124.00
319.00
313.00
154.00
24.00
194.00
146.00
24.00
2,502.00 0.00 0.00 2,502.00Total Value Vork Applied
Total Assigned Froi
Total Reserve
Credits you are claiiing in this report nay be cut back. In order to liniiize the adverse affects of such deletions, please indicate fron which clam you irish to pnorize the deletion of credits. Please lark (x) one of the following:1.n Credits are to be cut back starting with the claiis listed last, working backwards.
2.j~j Credits are to be cut back equally over all claiis contained in this report of work.
3. j] Credits are to be cut back as priorized on the attatched appendix.
4. [x] Credits are to be cut back starting with the claiis that have reserve credits.In the event that you have not specified your choice of priority, option one will be iipleiented.Note 1: Examples of beneficial Interest are unrecorded transfers, option payients, leiorandui of agreements, etc.,
with respect to the fining claiis. , . Note 2: If work has been perforned on patented or leased land, please coiplete the following:I certify that the recorded holder had a beneficial interest in the patented or leased land at the tile the work was perfoned.
Signature Date
Ontario
- Ministry of f*'"ih*rn Development ^^ Minet
iMlttere du Developpement du Nord et det mines
Statement of Costs for Assessment Creditttat des coQts aux fins du credit d'evaluationMining Act/Loi tur let mines
Transaction NO./N* de transaction
* oo l fa
Personal Information collected on this form Is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining clalm(s). Questions about this collection should be directed to the Provincial Manager. Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5. telephone (70S) 670-7264.
Les renseignements personnels contenus dans la presente formule sont recueillis en vertu de la Lot sur toe mines et serviront a tenlr a Jour un registre des concessions minleres. Adresser tout* queslton sur la collece de ces renseignements au chef provincial des terrains minlers, minister* du Developpement du Nord et des Mines, 159, rue Cedar, 4* etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.
1. Direct Costs/CoQts direct*
Type
Wage* SalaJres
Contractor's end Consultant's Fees Drone def 0lttrOpitfMUret de ('expert- ooneeN
SuppMee Used FowiHtunM utfttoeee
Equipment Rental LoeaDondeflMtvfWl
Description
Labour Maln-d'oeuvreField Supervision Supervision sur to terrain
Type AAL^IW 6rA*4t.li)
fou^ (U1U)
Type
Type
Amount Montant
1HH40
i^ift-od
Total Direct Costs Total des coOts directs
Totals Total global
Xda-co
PfA?^0
2. Indirect Costs/Couts Indirect** ' Note: When claiming Rehabilitation work Indirect costs are not
allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les coots Indlrects ne sont pas admlsslWes en tant que travaux d'evaluatlon.
Type
Transportation Transport
Food andLodging Nowriture et hebergementMobmzatlon and Demobilization
demobilisation
DescriptionType
RECORD
JJJN 2 1 1
Receipt — ——
Sub Total of Indli Total partlel des coOti
Amount Allowable (not greater than 20* of Dlr Montant admissible (n'excedant pas 20 H desTotal Value of Assessment Credit Valeur toti (Total of Mrsct and AltowaW* d'evakiatto Indirect eottt) (Tottl d** M
Amount Montant
— •••"•n :.D
393
reet Costs i Indlrectsect Costs)
feducredN nlOttamdt
Totals Total global
%-v~ t ;\ '
•f-''' '.
cW'A)
Note: The recorded holder will be required to verify expenditures claimed In this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.
Note: Le Utulalre enregistr* sera tenu de verifier tea depensee demandees dans le present etat des coOts dans les 30 Jours auhvant une demand* a cet effet. Si la verification n'est pas effecluee, le mlnlstre peut rejeter tout ou une partie des travaux d'evaluatlon present**.
Filing Discounts
1. Work filed within two years of completion is claimed at KXttfc of the above Total Value of Assessment Credit.
2. Work filed three, four or five years after completion is claimed at SOW of the above Total Value of Assessment Credit. See calculations below:
Total Value of Assessment Credit Total Assessment Claimedx 0.50
Remises pour depot
1. Les travaux deposes dans les deux ans suhvant tour achievement sont rembourses 4100 9b de la valeur totale susmentionnee du credit (revaluation.
2. Les travaux deposes trois, quatre ou cinq ans apres tour achevement sont rembourses 4 50 H de la valeur totale du credit d'evaluatlon susmenttonne. Voir tos calculs ci-dessous.
Valeur total* du cr*dtt d'evaluatlonx 0,60
Evaluation totale demand**
Certification Verifying Statement of Coste
l hereby certify:that the amounts shown are as accurate as possible and these costs were Incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.
that as ~(R*eord*d HoM*r. Ag*nt. Position In Company)
to make this certification
Attestation de I'etat des coOte
J'atteste par la presente :que les montants Indiques sont le plus exact possible et que ces depenses ont et6 engagees pour effectuer les travaux devaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.
l am authorized Et qu'ajitre de je suls autoris*(titulalr* *nr*glstnt, r*pnto*ntant, pott* occupe dan* la dompagnl*)
a faire cette attestation.
Signature Dal*
i0212 (04/91) Nota : Dans cette formule, loriqu'H design* des p*rsonn*s. l* masculln *st utilise au sent neutre.
f?- ] 'f'
LEGENDAREAS WITHDRAWN FROM DISPOSITION
M.R.O. - MINING RIGHTS ONLY
S.R.O. SURFACE RIGHTS ONLY
M.+S. M INING AND SURFACE RIGHTS
Description Order No. Date Disposition Fil
l) CHOWN R ESERVE
SWAYZE TWP.f '/-NL-i'IPS B *W l IN!- S l- Tt.
L f?^- - Lffg'jj--- — i^i'i L —;."; - ; NtsV '. -'. ,- ' 'j\i At b
M. i ''. ' V , ', ;H M ( KUJiM, '•no H r
S; Ri ' 'v'^'ON r. (J (.OMPUSI M ^l AN
RI St H
i')HK,iNAL SHORt L INt
MAHSH OR Ml ISK t l.
Ml-NrS
M( JNI iME N T
p rM/ ' 740052 l 7-30065 l U " ^ l v..-, /' f L '- f ' '- ,''.' l 740066 j 740C(7)9/ l
i'
IQiaiBD l 9GH3a118280
DISPOSITION OF CROWN LANDS
TYPt OF DOCUMENT
SURFACE ^ MINING RIC,HTS . Act SIGHTS OML YMINING RIGH'S ONL v
LtASF SUHf-AC.f S MINING H IGHTS
ACF MIGHTS ONLjiir*jr^nIIILV^^J
II55T08 '
LH;tNCFC)f OCCUPATION
ORCH" R 'N COuNCii
Rt Sf. RVATiON
CANCf L l t O
SAND ft GRAVtL ...
C-AP 3HO SEC 63 SU8&EC 1
— J.\t'(J V t [r t 'li! l \.""" t&t-
1030184
— — — -J — - J, - -
1158594 J pgii^j j P64WW- \ l t ||5ft593 JI1S85M
t f- " ! ; ^20 30 40 S O 60 'O
SCALE 1:20 OOO
.^-— - — - ——
TWPJS-SUMECT TO FOREST ACTIVITY IN FURTHER WFOWIATION OH FILE.
—-l—————-———t 1 1*466 \||6469
H32OO4 l M32OO5
__i J.__^ ^ *S IP L-H770I7 J
1182489(2 UNI
*ii*?,i r-- 4-6^ toe
r^™---!_---
IOI3!25 \-iJI0-I?'3? 1 i ~ {\~*
118663^ i*^ _^-w ___il 1013)42 l
TOWNSHIP190034(4 UNITS) CUNNINGHAM, (OI3WO
189916(4 UNITS)
M N R ADMINISTRATIVE DISTRICT
CHAPLEAUoivrstoN
IQJBI66 i lOI 31 •fit
PORCUPINELAND TITLES/ REGISTRY DlVfSIOW
SUDBURY1189871
UNITS)— -| i —-^. AJi—--^, ~^^2— ~L,——— ———.THE INFORMATION THAT
APPEARS ON THIS MAP HAS BEEN COMPILED FftOM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON.
(9 UNITS)(182.85? V1
^' ( 9 UNITS)l
13 UNIT Mnistry of MWstiy of. . MaturdJ Northern-Devetoprnent
aid MinesP l J82824- os UNITS)
Bat * AUGUST, 1986
41010NE9202 2.15106 CUNNINGHAM
/1030180*~ o
117698*
falconbridge
LOCATION MAP
Scale 1:20,000Shunsby
7+OOS7+OOS - Soht/olUoriUc
Oobt/maf wlc oh t brat
8+OOS
ficht/maf vk 4Argmod-fi at weet dip
F 1030188welJ bedded Soht/maf
30 9-fOOSO ^ axx ^ Tow-91-2
med-itrou aHtVtronf ohl alteration obi alteration v alon* fracture*. TVaoe-
IX diee+etrlotfer
old (ranch bedded flofat
MoaUy Clear
P-1176988 Cedar Swamp
- 1 0+OOSJO+00S
Om. oontofnt&c O pebble*
Mostly Clear
Cut11+OOS1J+00S
161*0.oBJ. alt (O 12+OOS12+OOS
raJpfaMe/llmoaftfe patch* Soht/bri/Arf
p-117699l 5ohtbedded
top dirfouon from load oaata
- 1 3+OOS13-f-OOS
mod. chJXvN
bouldere XI
3t-xtl)/ 16124/J
14+OOS
31, Mb ^ UpbvcMiu 330/7W
llmonitio patches
- 15+OOS
ISAIAH CREEK
PLUTON P-1176993
P-1176992
14+OOS
15+OOS ^
16+OOS 16+OOS
• Mn
Sample #181141811518116
181171811818119
181201812118122
181231812418125
181261812718128
181291813018131
181321813318134
1813518136
ANALYTICAL RESULTS Location Zn(ppm) Cu(ppm) Pb(ppm)
8+OOS 5+50W Whole Rock7-*-OOS BL 326 155 347+OOS 0+70W l99 625 62
Ag(ppm)
0.8
Tt TOO X* OuWtrF*Mpir*
Iff
VMM**
9+75S 0+90W11+OOS 0+78E11+80S 4+OOW
12+OOS 4+20JT14+75S 2+75W14+75S 2+75W
14+15S 5+75W13+75S 3+30W12+10S 5+75F
10+10S 3 +80W9+40S 4+50W8+80S 5+10F
Whole Rock*
44 207 11 TfhoJe Rock
0.1
t GhHrtnf IMaMCfenvurY RocM t CM Owl t F tan FoniWMm
VoOricto
1 01
4V VatowK •*n
8+60S 8+50S 8+OOS
8+10S 8+75S 9+30S
12+40S 13+90S
5+35W 5+25W 4+75W
6+30W 6+50W 9+15W
11+OOF 1 + lOE
1 N
tU
Mpfc For MiMMlMrtC AodM
|4 MWW yHncd poMUy v*MBt*V t t*ndMa lsu*
' Nah v*di mot
t
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gvotogim corucf ertnvri f)
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l400
1
•nttcirMl toU wucbn **i ptap
tyndn* takJ Mruekn *
METERS
•Mnopyita
T ^, . -jRevise d
*
Geological Mapam Twp
Dwg //:
PROJECT: TOWER' - - ' - -
Proj. #: -206Surveyed by: REP Drawn by: A. B.-^
N.T.S.: 41 0/10 Date: O CT/91 Scale: 1 :2500
NORANDA EXPLORATION co. LTD
7005.D —
8005.
9005.
10005.
O
11005.
12005.
13005.
14005.
15005.
D
16005.
LO CD OD OO CD r^
CN O4 CN
*-t 01 (TJ
in m in
in ta
P-1176992
LU
UJin CLCQ
2.1510B CUNNINGHAM
Instrument
Co 11 Spec lng
MflX-MIN II
150m
Vart lcol Scale: l on - 1 BX
Frequency
In Phase
Quadra"turo
444 Hz
50m 25m l l l
50m l
LBEU l
T OVER L RK EHLEM SURVEY
FREQ. 444 HERTZ PROJECT; CUNNINGHflM PROJECT *
BflSELINE flZIMUTH : 0 Deg.
SCflLE * SURVEY
•- 1 : 2500 DflTE i BY : HU5SEY NTS :
FILE: H206TOWNORflNDR EXPLORflTION
: 206
7/30/91 410/10
g De* IWl .-t Ili31 feral Prof 11. C-n*r. of p l .rt rt 3T7B.H f 1 11
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P-1030188
700:
800S.
900S.
1000S.
110OS.
1200S.
1300S.
1400S.
1500S.
1600S.
2.15136 CUNNINGHAM
oJ to 10l l
CN O (O O O O
oo oo at to
j?*--—..a) ift 10 (D ,..
L. - -- -l- ——--L——- -,-l——————
,,.
f'•f
InPh
Quad
Instrument : MAX-MIN II
Coil Spacing : 150m Vertical Scale: l cm - 10X Frequency : 1777 Hz
In Phase : M M . Quadrature : . .*...A ......
SOn tfni Onl__II__LI™
60ml
100mt
TOWER LAKEHLEM SURVEY
FREQ. 1777 HERTZ PROJECT: CUNNINGHAM PROJECT #
BASELINE AZIMUTH : O Deg.206
SCALE = 1: 2500 DATE : 7/30/91 SURVEY BY : HUSSEY NTS : 410/10
FILE: H206TOW NORANDA EXPLORATION
230
jfere. 5.00 KM B Oet im at I liM Nonnal Proflto Cwrin of plat at 375.0W i 1 1BO.OS Swtd f HM14O Rlj|hlli*d UMr l NORAHOA EXPUMWDN
600N.
500N.
400N.
300N.
200N.
100N.
ON BASELINE 90*
41010NE92C2 2,15106 CUNNINGHAM
o oLO
o o o o00
o oCM
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317.0
x x x1
D
2. 1510 6
CONDUCTIVITY - T HICK ME 8 S
Strong
Moderate
r\ Weak
E S
Interpretaion By: G. Hodges, Division Geophysicist
Instrument : EM—16
Vertical Scale Inphooe/Quad : 1 cm
Tx Location : NAA Cutler, Maine
Contour Interval :
In-phase : ——————
Quadrature : ...............
20. OX
50m 26m On l l l i l
50mi 100m J
TOWERVLF-EM SURVEY
PROJECT : TOWER GROUP PROJECT # : 106 BASELINE AZIMUTH : 90 Deg.
SCALE - 1: 2500 DATE : 1/15/91 SURVEY BY : DM NTS : 41 0/15 RLE: VTOWEXT FREQ.: 24.0 KHz.
NORANDA EXPLORATION
jtera. 5.02 Thu 13 P* 19*2 rt tiSI Normol Prefll* Cwitn *T plot at 150.0C / 300. ON 5*14 f VTM4O MgMwwd Ua*r : NOTWOA EXPUXWION
UJo o*tO
UJo o
5+QQN
10301
wer
— — -
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1 A1 i o i
313
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79
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y
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—
69644
——————— E
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11
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^ 0+00 B. L
11
11 1 +OOSJ
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