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S3B14NE0026 53BI4SE00a0 RANDALL LAKE 010
REPORT
ON
GEOLOGICAL MAPPING, LITHOGEOCHEMICAL SAMPLING,
SOIL SAMPLING, AND PROSPECTING
AGUTUA ARM PROPERTY
DISTRICT OF KENORA, PATRICIA MINING DIVISION
NORTHWESTERN ONTARIO
FOR
MOSS RESOURCES LTD.
tN 1 .1 1986
UHDS SECTION
November, 1985 Jon W. North iB.Sc.
TABLE OF CONTENTS
PageS3BHNE0028 53B14SE0e2C! RANDALL LAKE 010C ——^"~
1.0 SUMMARY....................................... l
DRAWING NO. 1: GENERAL LOCATION MAP............ 3
2.0 INTRODUCTION................... . . . . . . . . . . . . . . 4
DRAWING NO. 2:PROPERTY LOCATION MAP........... 5
3.0 PROPERTY DESCRIPTION............... . . . . . . . . . . . 6
DRAWING NO. 3: CLAIM SKETCH........... . . . . . . . . . 7
4.0 LOCATION, ACCESS, SERVICES.................... 8
5 . O PREVIOUS WORK . . . . . . . . . . . . . . . . . . . .-. . . . . . . . . . . . . 9
6.O PHYSIOGRAPHY AND VEGETATION....... . . . . . . , . . . . . 10
7.0 REGIONAL GEOLOGY.................. ............ 11
8.0 PROPERTY GEOLOGY. . . . . . . . . . . . . . ... . . . . . . . , . . . . . . 13
8.1 GENERAL DESCRIPTION...................... 13
8.2 VOLCANICS................................ - 13
8.3 SEDIMENTS................................ 14
8.4 INTRUSIVES............................... 14
8.5 METAMORPHISM............................. 15
8.6 STRUCTURE................................ 15
DRAWING NO. 4: SOIL GEOCHEMISTRY PROFILE...... 16
9.0 GEOCHEMICAL SAMPLING................... . ...... 17
9.1 LITHOGEOCHEMICAL SAMPLING................ 17
9.2 SOIL SAMPLING............... . . . . . . . . . . . . . 17
DRAWING NO. 5: TRENCHES A-K................... 18
9.3 PROSPECTING AND TRENCHING................ 19
10.0 ECONOMIC MINERALIZATION....................... 19
10.1 AGUTUA ARM SHOWING: TRENCHES A-K........ 19
DRAWING NO. 6:TRENCHES L AND M.......... 22
10.2 TRENCHES L AND M........................ 23
10.3 NORTH CARIBOU RIVER SILVER-ZINC-LEAD
OCCURRENCE........................... . . . 24
11.0 SUMMARY OF GEOPHYSICS......................... 25
12.0 CONCLUSIONS................................... 25
13.0 RECOMMENDATIONS............................... 27
13.1 PHASE I................................ 27
13.2 PHASE II..... .... . ... . .................. 27
14.0 ESTIMATED COST OF RECOMMENDED EXPLORATION
PROGRAM................................ . . . . . . . 28
14.1 PHASE I................................ 28
14.2 PHASE II........ . . . ..................... 28
15.0 REFERENCES.................................... 29 i
APPENDICES ;
A: Certificate of Qualification..............(back of report)
B: Technical Data Statement.................. " " "
C: Rock Sample Descriptions and Assays....... " " "
D: Rock and Soil Sample Analytical
Certificates.............................. " "
Drawing No. 7 Property Geology............ (map pocket) .
1.0 SUMMARY
The Agutua Arm property of Moss Resources Ltd. is under
lain principally by an east-west trending sequence of felsic
to intermediate pyroclastics and volcanoclastics. This
sequence is intercalated with minor mafic flows and intruded
by felsic to intermediate quartz-feldspar porphyry sills and
dykes. The rocks dip to the south between 20 0 and 40 0 .
Precious and base-metal mineralization occurs in two
localities on the property; the Agutua Arm gold-silver-copper
showing, and the North Caribou River silver-zinc-lead showing.
Mineralization is associated with east-west zones of shearing
and carbonate alteration which dip steeply south at the Agutua
Arm showing, and steeply north at the North Caribou River
showing.
At the Agutua Arm showing,previous surface trenching has
exposed a carbonatized shear zone three and three-quarter feet
wide along a strike length of 90 feet. Within this zone en
echelon quartz-arsu^opyrite veins carry gold-silver-copper
values. Sampling of the trenches resulted in assays up to
0.67 ounces per ton gold, and 0.71 ounces per ton silver.
Results of earlier sampling reported higher values, up to
1.92 ounces per ton gold over one Loot, and 18.80 ounces per
ton silver over 4.0 feet.
The North Caribou River showing was not located during
the present program due to unusually high water levels. This
showing was discovered by Ontario Geological Survey geologists
in 1984, and has been described as a 13 cm wide carbonatized
shear zone with silver values up to 2.9 ounces per ton. The
mineralogy, alteration and general trend of these mineralized
zones are similar to the North Caribou River fault structure,
two miles to the south.
Fifteen east-west trending VLF-EM conductors have been
delineated on the property, and are considered to have excellent
potential for shear controlled sulphide-gold-silver-copper-
lead-zinc deposits.
A two-phase exploration program is recommended. Phase I
should consist of an I.P. survey to determine which of the EM
conductors are caused by sulphide bearing shear zones, and
humus sampling to detect other bedrock zones of gold-silver mineralization. Phase II should consist of diamond drilling.
The estimated cost of these programs is $26,340 and |122,500
for a total cost of SU8,840.
- 3 -
i
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fllV THUNDER ^ ^ 8*^
r,-JJ \\ OPAPIMISKAN. LAKE
; PICKLE
K.DLAKE
MOOSONEE,
O N T A R
KENORA * *r
^ ^ t
\"^'~\\
UNITED
STATES
^ ^ s Greenstone Belts
o b
100 mi le 8
MOSS RESOURCES LTD.
AGUTUA ARM PROPERTY Patricia M.D., Ontario
LOCATION MAP
SCALE: l :!00miDWG. No: l
BY: H.H./R.T.MDATE: NOV, 1985
- 4 -
2.0 INTRODUCTION
The following report describes the results of a comprehensive
geological exploration program consisting of geological mapping,
at a scale of l inch to AGO feet, lithogeochemical sampling,
soil sampling, trenching, and prospecting on the Agutua Arm
property of Moss Resources Ltd. The property is located in
the North Caribou-Opapimiskan-Neawagank Lakes greenstone belt
in Northwestern Ontario (page 3).
The present program was carried out in August, 1985, by
Geocanex Ltd., of Toronto, subsequent to magnetic and VLF-EM
surveys which were carried out in February and March, 1985,
also by Geocanex Ltd.
All work was carried out on a cut picket line grid with
an east-west trending baseline and perpendicular cross lines
at 400-foot intervals.
The program was carried out from August 6th to August
28th, 1985.
The personnel involved in the program were:
Jon North Geologist/Party Chief Windsor, Ontario
Rob Higginson Geologist Barrie, Ontario
Brian Huston Field Assistant Pickle Lake, Ontario
Ken Wright Field Assistant Scarborough, Ontario
Grab samples of all'quartz veins and mineralized volcanics
were collected during the mapping and prospecting programs.
- 5 -900 30'
53 0 OO' MOSS RESOURCES LTD
VAN HORNE GOLD EXPLORATION INC.
NORTH CARIBOU-OPAPIMISKAN- NEAWAGANK LAKES
GREENSTONE BELTREGIONAL GEOLOGY
AND MINERALOCCURRENCES
? 6 v - H H X R T M 0*'E O ct 1 935 SCALE l - 4miGEOCANEX LTD
TORONTO. CANADA
AGUATUAARMPROPERTY
Mefavolconics
Mefosediments Staked ground
Moss Resources Ltd.
Van Horne Gold Exploration Inc
Granitic intrusive Metamorphic rocks
MUSSELWHITE DEPOSITSIron formation
Synclinal Fold axis
DOME-INCO-ESSO- L.ACANA3,000,000 tons O l/oz/ton Au
Gold occurrences
(T) Musselwhite deposit
(2) Teal prospectAgutua Arm prospect
4) Centre Lake prospect5) Eyapomikoma Lake Mo, F prospect
6) Opapimiskan Lake prospect7) N eawagank Lake prospect
8) Liberf Lake prospect9} Sage Lake prospect
, QCj) Stanley Lake prospect;:(fi) Seeseep "Lake prospect
- n i 2 "—— —-i^——j— — —L^'"T
- 6 -
In 1967, Pyrotex Mining and Exploration trenched a high
grade gold-copper-silver showing located on claim No. Pa 720082.
During the present program these trenches were cleaned out and
extended, chip sampled and mapped in detail. One north-south line was run over the trenches, and humus and '3' horizon
soil samples were collected and analyzed for orientation
purposes. A mineralized shear zone was discovered on the base
line near line 28 west. Two trenches were put in over the
zone, chip sampled and mapped. Prospecting was carried out over all geophysical anomalies.
The time breakdown in man-days for the work performed
is as follows:
Mapping 41 1/2 man-days
Chip Sampling/Trenching 37 man-days
Prospecting 13 man-days
Soil Sampling 2_______man-days
Total 93 1/2 man-da.ys
A geological map of the property is included at the back of
this report (Map 1). Geologic/sample sketches of the trenches are included with the text. All rocks and soil sample descrip tions and assays are included in the Appendix.
3.0 PROPERTY DESCRIPTION
The Agutua Arm property consists of 27 contiguous unpatented mining claims recorded on Ministry of Natural Resources Randall
Lake (M-2544) and Keeyask Lake (M-2684) claim sheets (page
(* Weagamow Loke
(Agutua Arm)
MOSS RESOURCES LTD.
AGUTUA ARM PROPERTY
Patricia M. D., Ontario
CLAIM SKETCHBY: H.H.XR.T'M. DATE; NOV. 19
GEOCANEX LTD TOPONTO,
- 8 -
laim details are as follows:
Claim Nos.No. of Claims Recording Date Work Filed
Pa 720075-089 incl. 15
823397-408 incl. 12
March 5, 1985
Jan. 14, 1985
60 days
60 days
The claims are wholly owned by Moss Resources Ltd., 804-
34 King Street East, Toronto, Ontario M5C 1E5.
4.0 LOCATION, ACCESS, SERVICES
The property is located in Northwestern Ontario (Lat.52 0 53'N, Long. 91 0 li 1 W), approximately 100 miles north-northwest
of Pickle Lake, and 170 miles northeast of Red Lake. The claim group straddles the south shore of the Agutua Arm of
Weagamow (Round) Lake. The Weagamow Lake - Agutua Arm - North
Caribou River system is the main travel route for Native trappers and fishermen from the Weagamow Indian Reserve (No. 87), which is approximately nine miles northwest of the property.
Access to the property can be made by float-or ski-equiped
aircraft from Pickle Lake, Red Lake or Weagamow Lake, or via
boat from the Weagamow settlement
Highway 808, an all-weather gravel road from Pickle Lake,
ends at Windigo Lake, approximately 25 miles south-southwest
of the property. A winter road to Weagamow runs within five
miles of the property between January and April. Groceries, building materials and general mining supplies may be obtained
in Pickle Lake. Groceries and limited building materials may
be obtained from Weagamow.
- 9 -
5.O PREVIOUS WORK
The following is a chronological account of previous work
on the property.
1938 - Jack Satterly (Satterly, 1939), mapped the property
area at a scale of l inch to l mile during a reconnaisance
survey for the Ontario Department of Mines.
1959 - An airborne magnetometer survey covering the
property was flown in the area by the ODM-GSC at a scale of
l inch to l mile (ODM-GSC, Map 909G, Weagamow Lake, 1960).
1967 - Pyrotex Mining and Exploration discoverd gold-
copper-silver mineralization in quartz veins and sheared
volcanics on the south shore of Agutua Arm, and drilled four
holes totalling 940 feet. Several quartz veins up to 0.3
metres wide were sampled in trenches. The best assays from
trenching are listed below.
Au (oz/ton) Ag (oz/ton) Cu ( "L ) Length (m)
2.54 3.68 1.35 0.3
1.92 18.80 2.50 1.2
No assays were reported from the drilling.
1979 - Thurston et al (1979) mapped the area on reconn
aisance level for the Ontario Geological Survey.
1984 - In March, 428226 Ontario Ltd. staked 15 claims
covering the Agutua Arm gold-silver-copper showing.
- 10 -
1984 - In April, Moss Resources Ltd. acquired j.5 c laim
group from 428226 Ontario Ltd.
1984 - Summer mapping program by the OGS at a scale
of l inch to 0.5 mile discovered silver-zinc-lead mineralization
at the mouth of the North Caribou River in Agutua Arm.
1985 - In January, Moss Resources Ltd. staked an additional
12 tie-on claims to the original 15 claim group to cover the
North Caribou River , .Iver-zinc-lead occurrence.
1985 - In February and March,Geocanex Ltd. carried out
linecutting, and magnetic and VLF-EM surveys on the 27 claim Agutua Arm property for Moss Resources Ltd. Fifteen east-west
trending VLF-EM conductors were delineated.
1985 - In August, Moss Resources Ltd. carried out the
present geological exploration program.
6.0 PHYSIOGRAPHY AND VEGETATION
Forty to fifty percent of the property is covered by
waters of the Agutua Arm-North Caribou River sys^.am. A set of rapids, five to ten feet high, at the mouth of the North
Caribou River near line 60 west, 2800 south, empties the
westerly flowing river into Agutua Arm. The main land portion
of the property forms a penninsula trending east-west across the property, and is 3,700 feet wide at the east end.
Outcrop is exposed on 3 to 570 of the property, and usually occurs as isolated domes protruding through thick glacial cover of sand and boulders. Most of the property
- 11 -
is covered by tall pine, spruce and hardwood forest on well-
drained glacial overburden. Ten to fifteen percent of the*
property is covered by muskeg. In 1985, the water level of
the lakes and rivers in the area was unusually high, and
many islands and shoreline outcrops were submerged. The North
Caribou River silver-zinc-lead occurrence described by Bartlett
et al (1985) was under about five feet of water.
7.0 REGIONAL GEOLOGY
The Agutua Arm property is located in the southwest
portion of the North Caribou-Opapimiskan-Neawagank Lakes greenstone belt. Due to the relative remoteness of the area,
the belt has not been extensively worked by mining and ex ploration companies . Most of the available geological inform
ation on the area is from government funded geological/geophysica^ surveys. The Ontario Geological Survey is currently involved
in the second year of a three-year geological/geophysical
survey of the area, manned by staff from the Precambrian Geology, Engineering and Terrain Geology, and Mineral Deposits Sections .
The belt forms part of the Sachigo Subprovince which is
composed of several small irregularly-shaped sequences of
supracrustal rocks. The rocks in this subprovince are avolutionarily distinct and probably older than the rocks in
the Uchi and Wabigoon Subprovinces to the south (Bartlett
et al, 1985). The belt forms an arcuate, horn-shaped assemblage
of metavolcanic and metasedimentary rocks which have been
synclinally folded about an axis, approximately coincident
with Eyapimikama Lake (Satterly, 194"1.). The syncline is
- 12 -
rimmed by mafic volcanics on the north anri -outh, and filled
with trough, cross-stratified epiclastic P icumulations in
the axial portion. Two fairly continuous bands of iron form
ation and chemical sediments mark the contact between the
volcanics and sediments, (Bartlett et al, 1985). Regional geological maps indicate that the belt is bounded by paragneiss
and migmatized rocks in the north, and felsic intrusives in
he west and south (Map 2292, Big Trout Lake - North Caribou Lake).
The entire belt extends from Weagamow Lake in the north
west to Opapimiskan Lake in the southeast. South of
Opapimiskan Lake the belt bifurcates into two major lobes, one lobe extending south through Libert Lake, the other through
the Forester and Newagank Lakes areas.
Geological mapping by the O.G.S. in 1985 at a scale
of l inch to 1/2 mile, indicates that the property area is
underlain by east-west trending felsic to intermediate pyro
clastic rocks with intercalated mafic flows. The sequence
dips shallowly to the south. This sequence of rocks is the
only large felsic to intermediate pyroclastic center documented
in the belt thus far. The rocks in the property area are
underlain by felsic intrusive rocks to the west, and abut
unconformably against the north-south trending stratigraphy of the Keeyask Lake metasedimentary-metavolcanic complex, two
miles east of the property.
- 13 -
8.0 PROPERTY GEOLOGY
G.l GENERAL DESCRIPTION
The property is underlain principally by an east-
west striking sequence of felsic and intermediate pyroclastics
and volcanoclastics (Map 1). The rocks dip to the south
between 19 0 and 81 0 but more commonly around 20-40 0 . Light
green to buff weathering intermediate flows, tuffs, lapilli
tuffs, and coarse fragmental rocks with minor agglomerate,
dominate the sequence. Massive, concordant lenses of fine to
medium-grained mafic volcanics are interbedded with the
pyroclastics, and constitute approximately ID-15% of the
section. Locally lenses of rhyloite porphyry and chert are
also present, but in very minor amounts. Quartz-feldspar
porphyry sills and dyke rocks of approximately tonalitic
composition intrude all of the volcanics, but were observed
in a few outcrops only.
8.2 VOLCANICS
The pyroclastic sequence on the property was probably
deposited in large part,subaerially. The sequence strikes
east-west and has an on-property thickness of approximately
6,300 feet. The rocks are light green to buff on weathered
surface, and light to dark green on fresh surface. The rocks
are generally foliated but not highly fissile. When bedding
ir. the pyroclastics was observed it was usually quite thin,
from a few inches to a few feet. Textural variation on out
crop scale is often quite pronounced and ranged from well-
bedded tuff and lapilli tuff to marbled and very poorly sorted
fragmentals, breccias, and agglomerates. Fragments are
- 14 -
generally less than five inches in diameter, angular to sub angular, and usually non-scoriaceous. These rocks do not
exhibit much compositional variation, and are approximately
dacitic or rhyodacitic to andesitic. Blocky andesite, dacite,
and rhyolite porphyry are present in minor amounts throughout
the pyroclastic sequence.
Mafic volcanics are commonly found as conformable lenses
less than 300 feet thick. These rocks are dark green, fine-
to medium-grained, graphic textured, (hornblende-plagioclase) flows. Pillows were never observed, and although the rocks
resemble typical intrusives rather than flows, no crosscutting relationships were observed. Epidotization in late cross
cutting fractures, joints and shears with minor quartz
veins, and pyrite are common features in the mafic volcanics.
8.3 SEDIMENTS
An outcrop of chert was found at 27+00 west on the
baseline. This is the only known occurrence of sedimentary
rocks on the property, and the only indication that any of the rocks were deposited subaqueously.
8.4 INTRUSIVES
There are very few intrusive rocks on the property.
Felsic to intermediate quartz-feldspar porphyry sills were
noted in a few outcrops. These rocks are concordant to
slightly crosscutting, and are probably co-magmatic with the
pyroclastic, rocks.
- 15 -
A tonalite plug was found on line 24 west, at 2400
south. The outcrop contains mafic xendiths, numerous quartz stringers and veiniets, and crosscutting networks of quartz stringers with tourmaline, arsenopyrite and pyrite mineralization^
8.5 METAMORPHISM \
The rocks on the property for the most part, appear :
to be very fresh. The fragmental and volcanoclastic rocks i
are light green coloured due to the development c f chlorite j
during regional greenschist facies metamorphism.
Localized shearing and quartz-carbonate metasomatism
along east-west trending shear planes is present on the
property. These phenomena probably reflect the strong pene
trative fabric of the North Caribou River fault which is
located two miles south of the property.
8.6 STRUCTURE
The rocks on the property are relatively undeformed.
The volcanic sequence generally strikes east-west, and dips
shallowly at 20 to 40 0 south. No .najor crosscutting lineaments,
folds, or offsets in the stratigraphy were observed. Shear
zones are approximately concordant with the strike of the
volcanics, and dip steeply south at 52 0 to 82 0 , A prominent
joint system is present on virtually all outcrops. This
system trends at 200 0 to 210 0 and usually dips between 70 0
west to vertical. One plunge measurement was obtained from
a shear zone in trench M. This zone plunges east only at 62 0 .
- 17 -
9.0 GEOCHEMICAL SAMPLING
9.1 LITHOGEOCHEMICAL SAMPLING
A total of twelve grab samples was collected during
mapping and prospecting and analyzed for gold and silver.
Ninety-six chip samples were taken from trenches A through M. All of these samples were analyzed for gold and silver;
57 of the chip samples were analyzed for copper as well as
gold ana silver. Because many gold values from the chip
samples were greater than 1000 ppb, 15 samples were run again by assay to obtain results in ounces per ton. This is
necessary because the fire-assay atomic-obsorbtion techinque
does not resolve high gold values as well as the assay
technique. All rock analyses are listed in Appendix C.
9.2 SOIL SAMPLING
One line of orientation soil geochemistry was run
on the property over the Agutua Arm gold-silver-copper , showing. Eleven humus and eleven B horizon samples were
collected at ten-foot intervals across the showing. All samples
were analyzed for gold, silver and copper. The soil geo chemistry profiles are shown in Drawing 4. The purpose of this survey was to determine the effectiveness of soil geo
chemistry as a transducer for outlining auriferous bedrock
zones. Gold anomalies occur in both humus and B horizon samples.
A two-sample anomaly which peaks at 16 ppb gold, is present in humus samples approximately 10 to 20 feet down ice from
the main mineralization at the showing. A one-sample anomaly which peaks at 68 ppb gold is present in B horizon samples
- 19 -
approximately 10 feet down ice from the main mineralization at the showing. Silver and copper values in humus and B
horizon samples are sporadic. In this survey humus sampling
and gold give the best bedrock signature over the showing.
9.3 PROSPECTING AND TRENCHING
All geophysical anomalies, were prospected with
particular emphasis on VLF-EM conductors. The numerous low
amplitude magnetic anomalies on the property are probably
caused by increased magnetite contents in the volcanics. All
of the VLF-EM anomalies are covered by overburden and muskeg.
A total of 13 man-days was spent prospecting.
A total of 28 man-days was spent trenching (including
chip sampling and mapping) the Agutua Arm showing (trenches
A to K). Nine man-days were spent on trenches L and M.
10.0 ECONOMIC MINERALIZATION
10.1 AGUTUA ARM SHOWING: TRENCHES A-K
Economic grade gold-silver-copper mineralization
occurs on the south shore of Agutua Arm near line 32 west, in
an east-west trending carbonatized shear zone hosted in
intermediate to mafic volcanics (Drawing 5). Four holes totalling 940 feet were drilled along this zoi -. in 1967, by
Pyrotex Mining and Explorations. No assays were reported from
this drilling but it was reported that the mineralized zone
was intersected in three of the four holes. This mineralization
is confined mainly to en echelon carbonate-quartz-arsenopyrite
veins which were emplaced along shear planes and crosscutting
- 20 -
fissures in the volcanics. The main zone of mineralization
at this showing averages 3.75 feet wide, and is exposed along
strike for 90 feet in trenches C,D,E,F, and G. Two smaller
quartz-arsenopyrite veins are exposed in trenches C and D, approximately 10 feet north of the main zone. The shearing
which hosts the quartz veins dips approximately 70 0 to 80 0 south,
A subsidiary massive ankerite shear zone occurs 40 feet south of the main zone and is exposed along strike for 130
feet in trenches A,B,H,I,J and K. This zone is l-.5 to 2.1
feet wide but, where exposed, does not contain significant
precious metal values.
Economic gold and silver values were obtained in chip samples from the main shear zone. Gold, silver and minor
copper are concentrated in the quartz-arsenopyrite vein
systems which pinch and swell within the shear zone. Visible gold was not observed in the showing. It is probably contained
in the arsenopyrite crystal lattice.
The highest gold value was obtained from trench G; sample no , 3052 ran 0.67 ounces gold and 0.46 ounces silver per ton over 0.8 feet. A brief description of this sample,which is
representative for all of the veins in the main zone, is as
follows:
Approximate Modes
Arsenopyrite
Quartz
Ankerite Calcite
75 - 807o
15 - 207.
2 - 37,tr . - U
Chalcopyrite
Pyrite
Bornite? Tetrahedrite
tr. - .57,
tr .
tr. tr .
- 21 -
Veins occur in sinuous, narrow networks which are concordant
to the main shear zone which strikes roughly east-west and
dips 70-80 0 south. The veins and country rock weather
recessively to deep ochre brown from the alteration of iron
carbonate and sulphides. Fresh vein surfaces are arsenopyrite,
grey and mottled with a few quartz inclusions and fragments.
The cores of the veins are generally composed of massive, medium-to coarse-grained, euhedral arsenopyrite which has been
slightly brecciated by a late injection of quartz. Minor
amounts of pyrite and chalcopyrite are found interstitial to arsenopyrite. The vein selvage is composed of sugary, vuggy
buff-to brown-coloured quartz with minor fine-grained disseminated
arsenopyrite. The wall rock is highly sheared, silicified
and carbonitized mafic volcanic which is hydraulically fractured and contains fine-grained disseminated arsenopyrite
and crosscutting quartz-sulphide veinlets.
This mineralization is exposed for 90 feet along strike.
Gold and silver values are highest in samples of vein material
and range from 40 ppb to 22, 847 ppb, and 0.2 ppm to 22.2 ppm respectively. The average gold and silver content of vein
samples from the main zone is 4,214 ppb and 4.4 ppm respectively.
The gold/silver ratio in the veins is 1.15:1. Chalcopyrite
was found in quartz-arsenopyrite veins throughout the zone,
the highest copper value was 2,360 pprn (Q.2%) over 0,3 feet.
Gold, silver, and copper concentrations decrease rapidly
from the quartz-arsenopyrite veins into the wall rock.
The wall rock at the showing is mafic volcanic which
has been bleached, silicified, and carbonatized by a strong
- 22 -
ho. so
03 CSJ
Muskeg
5o
10'
LEGEND
C ! "SS'*'e^ OS
MOSS RESOURCES LTD.
Aguatua Arm Property
Trenches L and M
GEOCANEX LTD TORONTO. CANADA
BY: RDATE: Qc* 29.65 SCALE: l": O"DWG. No: 6
•/-a
- 23 -
alteration envelope which is centered on the main zone of the
showing. The altered volcanic does not contain significant
gold or silver concentrations unless it is crosscut by quartz-
sulphide veinlets in hydraulic rractures, or adjacent to the
main zone of mineralization where the hydrothermal metasomatism
in the volcanics is focused.
10.2 TRENCHES L AND M
Similar metasomatism and shearing to that of the
Agutua Arm showing occurs in intermediate to mafic volcanics
near line 28 west on the baseline. An east-west trending
limonitic shear zone with fine-grained disseminated arsenopyrite
and pyrite was exposed by trenching on the edge of a scarp
(Drawing 6). The shear zone dips 54 0 south. No economic
gold or silver values were obtained in chip samples from these trenches, however, significant values of 40 ppb gold, 1.4 ppm
silver and 771 ppm (.07/0 copper were obtained from a three-
foot sample of sheared volcanic with 1-370 disseminated pyrite
and TL arsenopyrite. The intensity of shearing and alteration
increases towards the southern edge of the scarp suggesting
that a stronger zone of alteration, mineralogically and structurally similar to the Agutua Arm showing, may be present
under the muskeg a.id spruce bog to the south of the scarp. A
strong VLF-EM conductor crosses line 28 west 80 feet south
of the baseline. It i s possible that this conductor represents a shear zone with sulphide mineralization which is only
partially exposed in trenches L and M.
- 24 -
10.3 NORTH CARIBOU RIVER SILVEK-ZINC-LEAD OCCURRENCE
Silver-zinc-lead mineralization was discovered in
a 13 cm wide shear zone at the mouth of the North Caribou River by an OGS mapping crew in 1984 (Bartlett et al, 1985).
This zone trends E 30 0 S and dips 67 0 to the northeast. Silver
values of 2.1 to 2.9 ounces per ton were obtained from the
shear zone which occurs with quartz-carbonate-chlorite alter ation at the contact of intermediate tuff and a mafic dyke.
This showing is probably located near line 72 west, 3600 south at the edge of a small island, however, the water
level of Agutua Arm was very high during the present program
and the showing was submerged under approximately five feet of water .
Numerous strong-to-moderate VLF-EM conductors are
present elsewhere throughout the property. These zones are roughly concordant to the stratigraphy and known zones of
shear-related mineralization on the property. The North
Caribou River fault is located approximately two miles south of the property, and is characterized by mineralogically similar alteration to the Agutua Arm gold-silver-copper showing.
The writer suggests that the penetrative foliation developed
along this fault extends northward onto the Agutua Arm property, where it is represented by the Agutua Arm and North Caribou
mineralized shear zones. Similar zones of alteration and
economic mineralization may be present and represented by the
VLF-EM conductors on the property which are not exposed in
outcrop.
- 25 -
11.0 SUMMARY OF GEOPHYSICS
VLF-EM and magnetic surveys were carried out on the
property in February and March, 1985.
The magnetic relief on the property is generally low.
In the central portion of the property a broad magnetic ridge
of 100 to 150 gammas is present. This feature p,robably
indicates increased magnetite content of the volcanics relative
to the rocks in the north and south portions of the property.
Several weak magnetic features are coincident with VLF-EM
responses, and may represent magnetic- sulphide mineralization.
Fifteen separate moderate-to-strong VLF-EM conductors
are present on the property. These generally trend east-west
and ara probably related to sulphide mineralization, which
may be controlled by shear zones in a number of cases.
12.0 CONCLUSIONS
The property is underlain by a thick sequence of felsic
to intermediate pyroclastics and volcaniclastics with inter
calated mafic volcanic flows. The rocks on the property strike
east-west and dip at shallow angles to the south.
Two important economic mineral showings occur on the
property. Gold-silver-copper mineralization occurs at the
Agutua Arm showing in quartz-arsenopyrite veins which have
been introduced into an east-west trending carbonatized, sili
cified shear zone. Mineralization is exposed for 90 feet in
trenches at this showing. Gold values of up to .67 ounces per
- 26 -
ton, and silver values of up to 22.2 ppm,occur in a strong
zone of mineralization which averages approximately three
and three-quarter feet in width.
At the North Caribou River showing, silver-zinc-lead mineralization occurs in a 13 cm wide southeast-northwest
trending silicified, carbonati?ed shear zone at the contact
of intermediate tuff and a mafic dyke. Silver values of 2.1
and 2.9 ounces per ton were obtained by an OGS mapping crew
in 1984. This mineral occurrence was under water in 1985
and could not be observed or sampled during the present program.
The showing is probably located on claim No. Pa 823406.
A mineralized shear zone, possibly flanking a large
unexposed zone of shearing, was found near l ine 2 8 west, on the baseline. This shear zone trends approximately east-west.
The presence of numerous, roughly concordant, east-west
trending shear zones on the property may reflect the penetrative structural fabric of the North Caribou River fault which is
located two miles south of the property. The alteration
mineralogy of the Agutua Arm showing is similar to that of the
North Caribou River fault.
Numerous east-west trending VLF-EM conductors are present
on the property but not exposed in outcrop. It is very likely
that some of these anomalies represent conductive sulphide
mineralization in shear zones similar in attitude and mineralogy
to the Agutua Arm showing and the North Caribou River fault.
- 27 -
13.0 RECOMMENDATIONS
A two-phase exploration program is recommended.
13.1 PHASE I
Since economic mineralization on the property is associated with sulphides in shear zones, all VLF-EM
conductors should be covered with Induced Polarization survey
to determine whether there are sulphides present in these
zones.
Orientation soil (hur.us) sampling carried out over known mineralized zones in trenches on the property indicates
that this method of sampling will detect gold-silvor mineral
ization. Humus sampling a d analyses for gold and silver
should be carried out ove the entire land portion of the
property.
13.2 PHASE II
Diamond drilling should be carried out to determine
the extent and grade of mineralization in the known showings ,
and to investigate geophysical and geochemical anomalies defined in Phase I.
It is estimated that a maximum of 3,500 feet of
drilling will be required.
- 28 -
14.0 ESTIMATED COST OF RECOMMENDED EXPLORATION PROGRAM
14.1 PHASE I
I.P. Surveys - 10 miles @$1,400/ mile $ 14,000.00
Humus Sampling - 530 samples @$15.00/ sample 7,950.00
Contingency 2QI 4 ,390.00
Total ? 26,340.00
14.2 PHASE II
Diamond drilling - 3,500 ft.
@ |35.00 all inclusive 3122,500.00
TOTAL PHASE I AND PHASE II $148,840.00
Respectfully Submitted,
Jon W. North B. Se. Geologist
- 29 -
15.0 REFERENCES
Bartlett, J.R., Breaks, F.W., DeKemp, E.A., and Shields, H.N., 1985. Precambrian Geology of Eyapimikama Lake Area (Opapimiskan Lake Project), Kenora District (Patricia Portion); Ontario Geological Survey, Map P. 2834, Geological Series - Preliminary Map. Scale 1:31680.
Hodge, H.J., 1985. Report on VLF-EM and Magnetic Surveys,Agutua Arm Property of Moss Resources Ltd. District of Kenora (Patricia Portion) Patricia Mining Division, Ontario for Moss Resources Ltd. - Horseshoe Resources Ltd. Joint Venture NTS 53B.
Ministry of Natural Resources Assessment Work Files; Unpublished Assessment Reports, Ontario Geological Survey, Sioux Lookout, Ontario.
Ministry of Natural Resources Map 2292, Big Trout Lake - North Caribou Lake Geological Compilation Series.
Ontario Department of Mines - GSC, 1960. Aeromagnetic, Map 909G, Weagamow Lake; l inch to l mile.
Satterly, J., 1939. Geology of the Windigo - North Caribou Lakes Area; Ontario Department of Mines, Vol. 48, Part 9, p. 1-32.
Thurston, P.L., Sage, R.P. and Siraguse, G.M., 1979. Geologyof the Winisk Lake Area; District of Kenora, Patricia Portion; OGS Report 193.
APPENDIX A
CERTIFICATE OF QUALIFICATION
r1 "
CERTIFICATE OF QUALIFICATION
THIS IS TO CERTIFY THAT:
1. I have been a resident of Ontario since 1965.
2. I ara a graduate of The University of Western Ontario,
London, Ontario, with an Honours B.Se. (1984) in geology.
3. I have been actively involved in the Canadian mining and
exploration industry in Ontario as a student from 1981
to 1983, and have been a contracting geologist since
May, 1984.
4. I have worked in the Pickle Lake area of Northwestern
Ontario since May, 1984.
5. This report is based on field observations made by the
author, and on a comprehensive study of all the available
Ministry of Natural Resources assessment work records,
and published geological maps and literature of importance
to the area described in this report.
G. In this report I have disclosed all relevant material,
descriptive and interpretive, which is to the best of
my knowledge, necessary to gain a complete understanding
of the viability of the project and the recommendations.
DATED this 15th day of November 1985, at TORONTO, Ontario.
Jon W. North B.Se. Geologist
APPENDIX B
TECHNICAL DATA STATEMENT
Ontario
Ministry of Natural Resources
GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT
File.
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.
•S)D
it. O
Type of Survey{s). Geological
Township or Ar^andall Lake (H-254A) Keeyask La|ce Claim noidcr(s) Moss Resources Ltd. 804-34 Kin"g
Street East Toronto, Ontario M5C 1E5
Survey Company-
Author of Report.
Geocanex Ltd.Jon W. North
Address of Author St. Gabriel Ct. Windsor , On t . Covering Dates of .Survey Aug. 16 -Aug. 28,1985 N9E 1P2
(linecutting lo office)
Total Miles of Line Cut -^-^^^^^^^^^^^^^^^.^^^^^.^^^.
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.
ENTER 20 days for each .additional survey using same grid.
Geophysical--Electromagnetic.
—Magnetometer—
— Radiometric——
-Other
DAYSper claim
Geological_L
Geochemical.
AIRBORNE CREDITS (Special provision credili do not apply to airborne lurvcyj)
Magnetometer. .Electromagnetic. Radiometric
DATE:.
(enter dayi per claim)
SIGNATURE:_Author of Report or Agent
Res. Gcol.. .Qualiiications.
Previous Surveys File No. Type Date Claim Holder
MINING CLAIMS TRAVERSEp List numerically
See attached list(prefix) (number) i
........................................................l
........................................................j
TfYI'AI r.I AIMS 27
LIST OF CLAIMS
Pa 720075
720076
720077
720078
720079
720080
720081
720082
720083
720084
720085
' 720086
720087
720038
Pa 720089
Pa 823397
823390
023399
323400
823401
823402
023403
823404
823405
323406
823407
823408
Total 27 claims
o
APPENDIX C
ROCK SAMPLE DESCRIPTIONS AND ASSAYS
ROCK SAMPLE DESCRIPTIONS AND ASSAYS
Assay Au Au Au No. Location Description oz/ton ppb ppm
3025 1100W, BLO sheared mafic vole., qtz., pid., 30 .237. py.
3026 450 W, 75N mafic vole., joints with qtz.,- 5 .1cc-epid. , 1-37. py.
3027 875 W, SOON rhyodacite flows, qtz.,-epid.- < 5 .1hem. stringers
3028 2780W, 25N sheared rhyolite, 1-37. po., 1-37. 15 .2fach., ser.
3029 3290W, 1880N qtz. stringers in docite?, tr.- -027 865 1.1
17. py. , tr.-.57. aspy.
3030 2500U, 2200S tonalite plug, lim., tr.py., 5 < .1fractured, 27. cc
3031 2400W, 2500S tonalite, qtz., tl. stringers, 15 < .1tr.-.57. aspy. lim.
3032 L64W, 2500N sheared int. vole., q.v.'s, tr.- 10 < .1.57. py. , lim.
3033 3950W, 1900N rhyolite, sheared, qtz. veins, cc, 5 < .1lim., tr.aspy., -57. py.
3034 3950W, 1900N rhyolite, sheared, qtz. veins, cc, 10 < .1lim., tr.aspy., -57. py.
3035 L12W, 2990N mafic flow, epidotized, tr.-57. py. 5 < .1
TRENCH A
Assay LengthNo. (Ft.)
3036 1.0
3037 2.6
3038 1.5
3039
3040
2.8
3.0
Au Description oz/ton
dac.-and flow, sil., cc
int. flow or tuff, sh., 2-37. cc.
ankerite zone,10- 157. carb, sheared 60-707. qtz. , sec.
as per 3037, tr.- .57. py.
dac. flow, 2-37. cc qtz. stringers
Au ppb
10
10
10
Agppm
c .1
.1
.1
.1
.1
Cu ppm
3041 3.0
3042 1.5
3043 0.2
as per 3040
as per 3040
q. v. , epid. on
10
10
5
< .1
< .1
< .1
selvage, chl. - cc stringers
TRENCH B
Assay Length Au An Ag Cu No. (Ft.) Description oz/ton ppb ppm
3044 1.8 int. flow, qtz. < 5 < .1 stringers,lim.
3045 2.0 as per 3044, < 5 < .1 sheared, cc-lim. rind. q.v.'s
3046 1.5 ank. zone as per 20 < .1 3038
3047 3.0 as per 3039 < 5 < .1
AssayNo.
3057
3058
3059
3068
3069
3070
3071
3072
3073
3074
3075
Length(Ft.)
3.0
3.0
3.0
2.3
3.0
1.0
0.5
2.2
3.0
2.8
0.7
TRENCH C
AuDescription oz/ton
dac. and flow
as above, minormafic material
dac. and flow,lira, rind
as per 3059
as per 3059, 1-57. aspy., py.,lim. rind
as per 3069 .070
q.v, , lim. , 1~37. py. , aspy. .028overall
sil. int. andflow, lim. rind.tr.-.57. py.
as per 3072
as per 3072
q.v., 15-507. .240
Au Ag Cuppb pptn ppm
215 .1
40 < .1
40 < .1
95 .2
145 < .1
1,630 .7
1,185 .5
380 .3
80 .1
120 .1
7,460 2.3
3076 1.3
3077 1.3
3078 0.3
aspy. , tr. - .57. py./cpy., tr.- .57. cc
int. and flow, tr. .57. aspy. , 2-37. cc. lim rind
q.v. ,3-57. aspy. , py.
q.v. , 3-57. aspy. 2-37. cc
65
325
505
.4 123
.2 142
.3 243
TRENCH D
Assay LengthNo. (Ft.)
3060 3.0
3061 2.85
3062 3.0
3063 1.5
3064 1.4
3065 0.95
3066 1.3
3067 2.6
3079 3.0
3080 2.1
3081 2.6
Description
bleached mafic vole. , lim. rind, massive
as per 3060, minor qtz.-carb. stringers
as per 3060, lim. rind, chl.stringers
as per 3062, silicified qtz. veinlets, chl. stringers
as per 3063, 0.07 1 q.v. with 17. py.
q. v. , 507. a spy. , 27. cc, 1-27. cpy. tr. py.
q.v./carb, zone, sheared, 3-57. aspy . 3-57. py.
bleached, shear ed , vein wallrock, 3-57. aspy. , 3-57. py.
bleached mafic vole.? tr. py. lim. rind.
as per 3079
as per 3079, minor qtz. str ingers
Au oz/ton
Au Ag Cu
.30
100
210
75
65
105
390
280
25
.1
.1
.1
.1
.1
13,410 22.2
4.4
7.4
.5 98
< 5 .4 69
5 .4 79
TRENCH E
Assay LengthNo. (Ft.)
3082 3.0
3083 3.0
3084 1.4
3085 2.5
3086 1.8
3087 1.7
3088 2.4
3089 3.0
3090 3.0
3091 grab
3092 2.8
3093 0.7
3094 1.5
AuDescription oz/ton
silicified blea ched and., qtz. stringers,cc-py. veinlets
as per 3082
as per 3082
as per 3082,15- 207. carb. , 4'-5' carb.,tr. py.,cpy.
as per 3085, .5- 17. py./aspy.
sheared and. dac. tr. -. V7. aspy. ,
tr . py . , qtz. cc- py. veilets.
q.v. , 2-37. aspy. l PY-
Au
.066
as per 3088, tet rahedrite?
q.v. contact zone, tr.py.aspy. bleached vole.
qtz. -aspy .veins with carb.
bleached and.- dac. qtz.-cc- epid. stringers
sheared vole . , triable, 1-37. aspy., qtz. stringers
bleached vole. , 1-37. aspy.
.058
.047
350
2,010
40
4,685
50
1,060
100
Ag PP"1
.1
.2
.5
.1
.2
CuPPm
22
5 < .1 32
5 < .1 26
5 .1 23
44
.9 417
1.4 106
70
50
1.5 105
79
.7 120
.8 156
TRENCH F
Assay LengthNo. (Ft.)
3095 3.0
3096 0.15
3097 2.6
3098 0.3
3099 1.7
3100 2.0
3301 3.0
Description
bleached vole., mafic?, tr.-.57. cpy., qtz. stringers
q.v., x-cutting, tr. py.
carb, shear zone 0.3' q.v. with tet.? 3-57. aspy. py., tr. cpy.
q.v. offsett from 3097
bleached vole., 0.4' q.v. with 2-37. aspy. , 3-57.py.
triable, limon- itic, sheared vole., 0.3' q.v. with 3-57. aspy./py.
bleached vole, contact with q.v.
Au oz/ton
.132
.100
.053
Au ppb
115
270
2,865
?.,725
1,200
50
Ag ppm
.4
Cu ppm
69
1.2 520
2.5 189
4.4 2360
2.9 508
2.8 2270
1.2 142
3302 1.3 as per 3301 25 .2 82
TRENCH G
Assay LengthNo. (Ft.)
3048 2.4
3049 0.7
3050 0.2
3051 1.3
Description
massive and flow, 2-37. cc
as per 3048, fractured, lim. rind.
q.v., ochre, 10- 257. aspy. , py., tr.-.57. cpy.
silicified and?, 1-107. aspy. ,tr. cc
Au oz/ton
49
.023
Au Ag Cuppb ppm ppm
5 .2
15
12,070
6,050
.1
5.6
1.9
3052 0.8
3053 0.7
3054 0.2
3055 O.i
q.v. 15-507. .670 aspy., massive aspy. , tr. - .57. py./cpy.
bleached int. .024 flow, 1-37. aspy. 707. qtz. , lim. rind.
bleached vole., .111 tr.-57. cpy. , 1-37. py. , aspy. q.v.'s
sheared, bleached vole. , lim. rind.
22,847 15.6
765
3,510
180
2.0
9.4
.6
3056 0.15 q.v. tr.-.57. cc 235 .9
TRENCH H
Assay Length Au Au Ag Cu No. (Ft.) Description oz/ton ppb ppm ppm
3325 3.4 chl.-ser.-qtz. 10 < .1 23 schist (bleached mafic vole.?) cc
3326 2.0 sheared carb. .050 1,)AO .2 23 zone, friable, qtz.-cc vein- lets
3327 2.8 bleached vole., 145 .2 41 5-17. aspy.
TRENCH I
Assay Length Au Au Ag Cu No. (Ft.) Description oz/ton ppb ppm ppm
3312 3.0 massive silic- < 5 .2 29 eous int. vole. -0.1' q.v.
3313 1.1 shear zone, ser.- 195 .2 30 chl. qtz. schist
3314 2.1 massive ank. < 5 .2 24 zone, 17. py., cpy.? ser. schist
3315 3.1 0.2' chl. schist, 45 .3 44 int. vole.
3316 3.0 massive It. green 5 .1 36 vole. V' q-v., 0.2' shear, 27. cpy. , 57. aspy.
TRENCH J
AssayNo.
3306
3307
3308
3309
3310
3311
Length (Ft. )
3.3
1.7
1,7
3.1
2.1
2.1
Au Description oz/ton
bleached mafic vole. , ank. , chl. stringers
sheared ank. zone ser., chl., 0,1' q.v.
ser. schist, 0.4' q. v. , ank. , +1.
massive bleached vole. , tr . py. , lim. rind.
as per 3309, tr. .57. py. , chl. stringers, v.f.g. red mineral
as per 3310, 0.2' shear, 0.21' qtz.- carb. , .57. aspy .
Au ppb
AS Cu
10
30
.1
.2
37
15
25
30
18
15
TRENCH K
AssayNo.
Length (Ft.)
Au Description oz/ton
Au Ag ppb PPm
Cu ppm
3303 2.5 siliceous int.- 5 .1 30 mafic vole., shearing, tr. sulphide
3304 2.0 ser. schist, ank- 55 .1 10 erite, sheared
3305 2.6 as per 3304 10 < .1 25 possibly sheared mafic vole.
TRENCH L
Assay Length AM Au Ag Cu No. (Ft.) Desc ciption oz/tot: ppb ppm
85-90 0 qtz., tr.- .57. py./aspy.
3328 2.5 ser.-chl.-qtz. 40 .3 71 schist qtz.-chl. sulph. veinlets
3329 3,0 sheared vo]-.., 40 1.4 771 fissile, limon- itic, 1-37. py. , 27. a spy.
3330
3331
3332
3.0
1.3
2.1
as per 3329
as per 3329
bleached mafic?
10
10
< 5
.2
.1
.2
160
56
70
TRENCH M
AssayNo.
3317
3318
3319
3320
Length(Ft.)
3.2
3.15
2.25
2.9
AuDescription oz/ton
grey chert, 17.py. , minor vole.interbeds
as per 3317, tr.py.
as per 3318
carbonatized
Au Ag Cuppb ppm ppm
< 5 .2 81
< 5 .2 53
< 5 .1 84
10 .1 62vole. , tr. aspy. cc, py.
3321 2.5 as per 3320, ma fic? tr. epid. , chl.
3322 2.0 silicic ank. zone in mafics, shear -ed tr. py. l a spy.
3323 2.2 as per 3322, buff schist
3324 2.3 as per 3323, v. limoni tic
10
10
.2
.2
.2
54
88
55
61
APPENDIX D
ASSAY CERTIFICATES
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REPORT: 015-3074 ( COMPLETE ) ] | REFERENCE wo;CLIENT: MISS RESOURCES SUIIUTKD UT: JOH XDKTHPROJECT: AGUTUA ARH DATE PRINTED: 3o-SEP-es, . . .. ... . .. ... . . . . . . . ..... i. .. ......
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ORDER
1 2
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SARPLE
SOIL
mm O F LOVERELEHENT ANALYSES DETECTIOH LIBIT EXTRACTIOI flETHOD
[B Copper 11 1 PPR HC1-HH03, (1:3) Atoiic Absorption A 9 Silver H 0.1 FPB HCI-HH03, (1:3) Aloiic Absorption
. . . . - . . jAu Sold 11 I PFI AfiOA IEBIA FTreAssajiACarbohKDo'
Testyt Au Test Ueight 1 0.01 gi
TYPES Mm S IZE FRACTIOUS UMBER SAHPLE PREPARATIOHS UMBER
H —— " " -B5 ' II " URTTSTIVl -BO 11
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j
SEPORT COPIES TO: H.J. HODBE JOX NOKTH
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REPORT: 015-307i
SARPIE ElEflENT NURBER yXITS
AA L33y-00 AA L33y-lS AA L33y-2S AA L33M-3S AA L33U-4S
AAL33y-5S AAL33y-lM AAL33V-2K AA L33U'3M AA L33IHH
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Certificafe of Analysis
[ _ J^i^j^jjl™''CLIENT: HGSS RESOURCESPROJECT: A6UTUA ARfl
SUs.lITTED BY: JON fiflRIH DATE PRINTED: 27-SEP-E5
ORDER ELEfltHT
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mm O FANALYSES DETECTION LlfUT EXTRACTION J1ETHOD
7 0.001 0/T
SARPLE TYPES
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H'JURER
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SIZE FRACTIOUS
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KURBER
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SAMPLE PREPARATIONS NUMER
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REPORT COPIES TO: H.J. HODGE JOH XORTH
INVOICE TO: H,J. HODBE
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Certificate of Analysis
REPORT; 415-2722 1 COBPLET U H REFERENCE INFO;CLIENT: BOSS RESOURCES ROJECT! AllTUUR
SU&HITTED 6T: JOH HDRTH DATE PRINTED: 2t-SEP-85
ORDER ELE/IEHTOF LOiER
ANALYSES DETECTION UdlT EXTRACTION /IETHOD
Au Gold -Assay 8 0.001 0/T 0.01 0/T
SAHPLE TYPES
OTHER
KURBER
B
SIZE FRACTIONS
-200
NUMBER
B
SAMPLE PREPARATIONS BUBBER
PULVERIZIHB 3
REMARKS: OTHER SAKPLE TTPE REFERS TO REJECT.
REPORT COPIES TO: H. J. HODtE JOHIORTH
INVOICE TO: HJ. HODGE
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REPORT: 015-28^3 i COMPLETE ) j RTFlRTNCTlNfor~
CLIENT: KDSS RESOURCES PROJECT: AGUTUA m
ORDER
i2
ELEMENT
Cu CopperAg Silver
mm O FANALTSES
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LOyERDETECTION LISIT
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SUP.fllfiED i r- R . HI66!iifiOil DATE PRINTED: 17-SEP-85
EXTRACTION
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Atoiic AbsorptionAtonic Absorption
3 Au Bold 57 5 PPB ABUA RE6IA FA-AA e 10 31 veight————
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K',..iir,ityolNnturalFlcsources
Ontario
Report of Work(Geophysical, Geological, Geochemical and Expenditures)
The Mining Act
Imlructioiu: -- rlc;i',o lyp" nr print,— !f number of mining c!aim^ linvr-rsiMl
excopd? sp.ico on this form, aijtnch n l'5t.l Noio: — Only days credits calculate^ In th*
"Expenditures" section may iff c riierrtdIn !ho "Expend. Dnys Cr."! columns.
— Do not use shaded areas below.]Typa of Survay(i)
GeologicalClaim Holdorli)
Moss Resources Ltd.Address
JTownihlp or Arm
Randall ^b PV'oVi"ictor'TiTic" encTRa--
804-34 King Street East Toronto, Ontario M5C 1E5__|6ate o? Si/rvev Ifrom A to)
06 08 85 28 08Day Mo. l Yr.
Company
Geocanex Ltd.Nam* And Addrtu of Author {of Qto-Tachnlca! rtport)
Jon W. North 1669 St. Gabriel Ct. Windsor, Ontario N9E 1P24—
Credits Requested per Each Claim in Columns at rightSpccijl Provisions
For first survey:Enter 40 days. (This includes lin* cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
Man Oayt
Complete reverse side and enter total(s) here
*
Airborne Credits
Note: Special provisions credits do not apply to Airborne Surveys.
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Geophyi leal
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Electromagnetic
Magnetometer
Radiometric
Days per Claim
-
~40
Doyi per Claim
Days per Claim
Mining Claims Traveiscd (List in numerical sequence)
Expenditures (excludes power stripping)Type of Work Performed
Performed On Claim(s)
Calculation of Expenditure Days Credits
Total Expenditures
S 4- 15
Total Days Credits
s:
Instruction! Total Days Credits mey be apportioned at the claim holder^o choice. Enter number of deyi credits par claim telected/'y' In columns at right. S X
Mining C'fl'mPrefix
'•i j ;.\..V:: 5OVV
Number
See at list
E xpend. Roys Cr,
ied
.W-i-8-t-!W"
..s r/
1986
v.
'.f:'
?r
Mining Claim Prefix Number
^Expend. Cr.
1.
Total number of mining clnimt couersd by this report of work.
Recorded^olde/or AgerrjKignature)
Certification Verifying Report ofWofl?
For Office Use OnlyTotel Days Cr rtecoided
HB co r d ad
as Hecordoo Branch Oirlctor
1 hereby certify that 1 have t personal and intimate knowledge of the fact? set forth in the deport of Work annexed hereto, having performed the i|vork or witnessed same during and/or alter its completion and the annexed report is true. i
Name ond Postal Address of Person Certifying s?
H. J. Hodge fi'
804-34 King St. Easttare IB i/o),- -.r,*.^,, wi*.'^ ; i; ".'"••; T " [ '^J?jTt 'JT5'"^T , *^"V WJ
J Oite Certified Certified by
Toronto, On t. M5C 1E5J f?n. f^/^ ( -
i ; '
(Signature)/
r?^
AGUTUA ARMS PROPERTY
LIST OF CLAIMS
Pa 720075720076720077
720078
720079
720080
720081
720082
. 720083
720084720085720086720087720088
Pa 720089
Pa 823397
823390823399823400823401823402023403823404823405823406823407823408
Total 27 claims
^E'cEs'tf fejjjiJAN-6 ^6
P.I t
\F*^*Wmml
-t-'
Onlnrlo
Ministry ofNorthern Developmentand Minesu
Technical Assessment Work Credits
Fllo
c.198.6-02.02..
.___^I Mining Recorder! R eport of Work No. l
Recorded Holder
MOSS RESOURCES LTDTownihlp or Arei
RANDALL LAKE AND KEEYASK LAKE AREAS
Type of survey and number of Assessment dayi credit per claim
Geophysical
|nrlnr*d Pol*rl'*t'O" , Hayt
Section 77 (19) See "Mining Claims Assessed" column
Geological . lo ,1ay,
Opochoniical , , riayi
Man days [~] Airborne L]
Special provision [X] Ground [3
[X] Credits have been reduced because ol partial coverage of clairm.
*
L~U Credits have been reduced because of corrections to work dates end figures of applicant,
Mining Claims Assessed
PA 720075 : 720077 to 089 inclusive; 823397 to 404 inclusive. 823406-07-08
Special credits under tection 77 (16) for the following mining claims :
No credit! have been allowed for the following mining claims[X] not jufficienlfy covered by the survey
PA 720076 823405
( ] insufficient technical dels filed
Linecutting credits previously granted on Report of Work #85-68.
The Mining Recorder may reduce the above credits if necessary in order that the total number o( approved assessment days recorded on each claim cjoes not exceed the maximum allowed as follows: Geophysical - 80; Gcologocal - 40; Geochemical - 40; Section 77(19)-60.
828 (85/1?)
801-34 KING ST. EAST TORONTO, ONTARIO M5C 1F.5
(416)862-9078 ^MOSS RESOURCES LTD.
January 13th, 1986
Mr. S.E. YundtDirectorLand Management BranchRoom 6643, Whitney BlockQueen's ParkToronto, OntarioM7A 1W3
RE: Geological Reports- Randall.Lake and Agutua Arm Properties
Dear Mr. Yundt,
I am enclosing two (2) copies each of Geological Reports on our Randall Lake and Agutua Arm Properties.
I hope everything is in order.
Yours very truly,
MOSS RESOURCES
i.J. Hodge, P. Eng. President
HJH/sw Encls .
RECEIVED
MINING LANDS SF.CllOfl
mn
' ~WW*•- jlfH;t :;' ' p A t? t.'. .^ Ui3. :V
\
( i Ontario^~-*
Ministry ofNorthern Development and Mines
1986 02 07 Your File: 86-5 Our File: 2.8798
Mining RecorderMinistry of Northern Development and MinesP.O. Box 309Sioux Lookout, OntarioPOV 2TO
Dear Sir:
Enclosed are two copies of a Notice of Intent with statements listing a reduced rate of assessment work credits to be allowed for a technical survey. Please forward one copy to the recorded holder of the claims and retain in? other. In approximately fifteen days from the above date, a final letter of approval of these credits will be sent to you. On receipt of the approval letter, you may then change the work entries on the claim record sheets.For further information, if required, please contact Mr. R.J. Pichette at (416) 965-4888.
Yours sincerely,
f-i
S.E. Yundt, Director Land Management Branch
Mining Lands Section Whitney Block, 6th Floor Queen's Park Toronto, Ontario H7A 1W3
.SH/mc Ends.
cc: Moss Resources Ltd Suite 80434 King Street East Toronto, Ontario M5C 1E5 Attention: H.J. Hodge
Jon W. North 1669 St. Gabriel Ct. Windsor, Ontario N9E 1P2
G.H. FergusonMining S Lands Commissioner Toronto, Ontario
•v rv w•ip:'M-i-- 'Hie*;j^! i•f4.. j;:-i' H rf. 1 :! ; i ;'i s#:•••*\w ff^m•m^fi i;:i P:
Ontario
Ministry ofNorthern Developmentand Mines
Notice of Intc-ntfor Technical Reports
1986 02 07 2.8798-86-5
An examination of your survey report indicates that th: requirements of The Ontario Mining Act have not been fully met to warrant maximum assessment work credits. This notice is merely a warning that you will not be allowed the number of assessment work days credits that you expected and also that in approximately 15 days from the above date, the mining recorder will be authorized to change the entries on the record sheets to agree with the enclosed statement. Please note that until such time as the recorder actually changes the entry on the record sheet, the status of the claim remains unchanged.
If you are of the opinion that these changes by the mining recorder will jeopardize your claims, you may during the next fifteen days apply to the Mining and Lands Commissioner for an extension of time. Abstracts should be sent with your application.
If the reduced rate of credits does not jeopardize the status of the claims then you need not seek relief from the Mining and Lands Commissioner and this Notice of Intent may be disregarded.
If your survey was submitted and assessed under the "Special Provision-Performance and Coverage" method and you are of the opinion that a re-appraisal under the "Man-days," method would result in the approval of a greater number of days credit per claim, you may, within the said fifteen day period, submit assessment work breakdowns listing the employees names, addresses and the dates and hours they worked. The new work breakdowns should be submitted directly to the Land Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked ^ill be issued.
.ii;- !- mrnf'';;;,:---^Iii
March 4, 1986 Your File: 86-5 Our File: 2.8798
Mining RecorderMinistry of Northern Davelopwant and MinesP.O. Box 309Sioux Lookout, OntarioPOV 2TO
Dear Sir:
RE: Notice of Intent dated February 7, 19fl6 Geological Survey on Mining Claims PA 720075, et al, 1n the Randall Lake and Keeyask Lake Areas
The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.
Please Inform the recorded holder of these mining claims and so indicate on your records.
Yours sincerely,
J.C. Smith, Supervisor Mining Lands Section
Whitney Block, 6th Floor Queen's Park Toronto, Ontf/Mo M7A 1H3
Telephone: (416) 965-4888
SH/mccc: Moss Resources Ltd
Suit* 80434 King Street EastToronto, OntarioM5C 1E5Attention: H.J. Hodge
Resident Geologist Sioux Lookout, Ontario
Oon W. North 1669 St. Gabriel Ct. Windsor, Ontario N9E 1P2
Mr. G.H. FergusonMining A Lands CommissionerToronto, Ontario
End.
'MM'!-''gmk
LEGEND
QUATERNARY
30 N
20N
ION
B.L.00-90
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AGUTUA ARM
2a
BL.2IS
30 S
405
PINE AND HARDWOOD
GLACIAL OVERBURDEN
720076 -__
l___130,30^.___ i___^\. i-)*. V ^ ~- -~
Hardwood foresl Agutua Arm Cu-Au-Ag showing,Trenches A-Karea enlarged onDwg. No. 5 )
glacial overburden
720 .083
DEADFALL ON HUMMOCKY OVERBURDEN
., - 'q.v.epidt —^t
720 -- 089 :*
, DEADFALL ON OVERBURDEN
720
086 '3028 po,.fu
sh.py.q.v.
2o epid.py ::.--r-^ sK 4 -
Trenches L a see Dwg. No. 6
3c,3d,4b Ai
**zr--J*—r399D E A D FA L L
ON GLACIAL
OVERBURDEN
DEADFALL '
OVERBURDEN..-l-:-3c,3d,5b.....
3031 qtz tl.aspy
HARDWOODGLACIAL OVERBURDEN
PROBABLE SUBMERGEDLOCATION OF
THE N.CARIBOU •RIVER Ag-Zn-Pb ~
OCCURRENCE
-—— — -~ ,;;.v2a
NORTH CARIBOU RIVER
500t^
53B14NEW28 53et4SEM28 RANDALL LAKE
1000 t
1500 t -
2000 i - t T
ddhqvSh9" sil ser ccpypo a spycpy ga spa l bn9f"mt litn tl mo
Stream, lake, bog deposits Glacial, glociofluvial lacustrine sediments
LATE PRECAMBRIAN (Keeweenawan?)
Ma Diabase
EARLY PRECAMBRIAN
Intermediate and Felsic Intrusives!0a Granite pegmatitelOb AplitelOc Granitel Od Syenite10* Quartz monzonitelOf GranodioritelOg TrondjemitelOh Quartz diorite(Oj Diorite10k Unsubdivided gneiss10 l Granite gneiss
Mafic Intrusives9a Unsubdivided9b Gabbro9c Leucogabbro9d Plagioclase-phyric gabbro9e Peridotite9f Pyroxenite
Iron Formation8a Oxide facies8b Carbonale facies8c Silicate facies6d Sulphide facies
Chemical Metasediments 7a Chert 7b Calcitic marble 7c Dolomitic marble
Clastic Metasediments6a Clast supported conglomerate6b Matrix supported conglomerate6c Oligomictic conglomerate6d Polymictic conglomerate6e Sandstone , Unsubdivided6f Wacke6g Arenite6h Mudstone, argilliteSj Feldspathic wacke6k Feldspathic arenite61 Quartz arenite6m Schistose rock i omphibole,± biotite,
± garnet, ± chlorite of probablesedimentary origin
Felsic and Intermediate Subvolcanic Rocks5a Unsubdivided5b Quartz-feldspar porphyry5c Quartz porphyry5d Feldspar porphyry
Felsic Metavolcanics
4o Massive fine-medium grained flow4b Pyroclastic breccia , tuff breccia
j 4c Tuff, lapilli tuff
Intermediate Metavolcanics3o Massive fine-medium groined flow 3b Flow breccia3c Pyroclastic breccia, tuff breccia 3d Tuff , lapilli tuff
Mafic Metavolcanics2a Massive fine-medium groined flow2b Amygdaloidal flow2c Variolitic flow2d Pillowed flow, pillow breccia2e Flow breccia2f Medium-coarse grained flow centres2g Plagioclase-phyric flow2h Amphibolite2t Co-magmatic sills, dikes2j Pyroclastic breccia, tuff breccia2k Tuff, lapilli tuff21 Chorite ± amphibole schist
Ultramafic Metavolcanicsla Massive fine-medium grained flow Ib Spinifex textured flow le Talc-carbonate i magnetite ± amphibole
± s erpentine ± chlorite schist
SVI1BOL5 l ABBREVIATIONS
xxxxxxXx
diamond drill holequartz veinshearinggneisssil icificationsericitizationcarbonatizedpyritepyrrhotitearsenopyritechalcopyritenalenasphaleritebornitegraphitemagnetitelimonitetourmalinemolybdenite
beaver damscarpwatercreek with flow direction, intermittentwet groundclaim post, claim l inetownship line
trenchdiamond drill holebedding strike, dip, top directionfoliation strike, dipgneissosity strike, dippillowed flow, top directiongeologic contact, inferredqeoloqic contact inferred fron geophysics
fault, inferredslope, steep slope pointing downhill
bush road, winter road
MOSS RESOURCES LTD -- TORONTO
AGUTUA ARM PROPERTYNORTH CARIBOU LAKE AREA Patricia Mining Division, Ontario
GEOLOGY
GEOCANE.X LTDTORONTO. CANADA
BY:DATE: NOV. 1965SCALE: l":400'DWG. No:
- 16 -
68ppb
E E SQ. g- Q.Q. d Q.
oC*
30 -i 3 .0 T 30 n
25 -
20-
15 -
10-
5-
O J
2.5 -
2.0-
1.5-
1.0 -
0.5 -
O J
25 -
20-
Gold, Silver, Copper in Humus
6 EQ. Q. Q.^ -
o30 -, 3,0 i
25 H 25 -
20 -
15 -
10 -
5 -
O J
2.0-
.5 -
1.0 - l
0.5 -
O J
30 i
25 -
20 -
15 -
10 -
5 -
O J
Gold, Silver, Copper in B Horizon Soils
5 N 4N 3N 2N 00 IS fe 3S 43 5S
Main shear zone with quartz-arsenopyrite veins
Subsidiary ankerite zone
ICE DIRECTION
5N 4N 3N 2N 00 2S \
3S—i—
4S 55
Main shear zone withquartz-arsenopyrite veins
^ Subsidiary ankerite zone
ICE DIRECTION
MOSS RESOURCES LTD.
Aguatua Arm Property
Aguatua Arm Au-Ag-CuShowing Orientation Soil
Geochemistry Profile
QEOCANEX LTD TORONTO. CANADA
BY; R T. M.DATE; AUG 1985SCALE: l :lOft.DWG. No: 4
PART
Aguatua Arm of Weagamow Lake
332? n-r o-i l tiJlltS, /fit, ' l t) IStf, to 'f ' , J!
Sheared ankerite zone
Silica-carbonate alteration zone ishearing ± quartz stringers
V'5 Quartz vein ± carbonotized volcanic
Geologic contact , inferred
Foliation , dip indicated
Joint , dip indicated
3641 1 /f .,, . , Chip sample , classified os such ' number, Au ppb , Ag ppm , Cu ppm
- iw r*i f ) M G rab sample
i ..J— c Soil sample station, showing - ' v^ ""Au in B Horizon (ppb)
--— ---™Au in humus (ppb)
*~-t~—*' S carp
Outcrop, trench
- - T. L. 18 t 27 N
Main Shear Zone
f Subsidiary Ankerite Zone
Trench ATrench K
2 + 5'
53B14NEM28 53814SEM20 RANDALL LAKE aio l
MOSS RESOURCES LTD.
Aguatua Arm Property
Trenches A-K
QEOCANEX LTD TORONTO. CANADA
BY: R T. M DATE: Aug. 36. 85SCALE: T i IQft. DWG. No: /3
top related