52089SE0a68 52008NEee44 TARP LAKE 010
REPORTON THE
DIAMOND DRILLING, GEOLOGY,PROSPECTING, SOIL GEOCHEMISTRY AND
TRENCHINGON THE
CENTRAL PATRICIA PROPERTY
PICKLE LAKE, ONTARIO
FOR
GOLDEN SHADOW RESOURCES INC,
g?- z-?
JANUARY 18TH, 1984 G,B, BURTO
52009SE*068 52088NE0044 TARP LAKE
TABLE OF CONTENTS
010C
PAGE
1.0 SUMMARY . . . . . . . . . . . . . . . . . . . . l
2.0 INTRODUCTION . . . . . . . . . . . . . . . . . 2
3.0 LOCATION AND ACCESS . . . . . . . . . . . . . . 2
4.0 PROPERTY DESCRIPTION . . . . . . . . . . . . . 2
5.0 WORK PERFORMED . . . . . . . . . . . . . . . . 3
6.0 DISCUSSION OF RESULTS . . . . . . . . . . . . . 6
7.0 CONCLUSIONS AND RECOMMENDATIONS . . . . . . . . 12
APPENDICS
REFERENCES . . . . . . . . . . . . . . . . . . 15
LIST OF DRAWINGS . . . . . . . . . . . . . . . 16
DIAMOND DRILL HOLE LOGS GS-83-1 to GS-83-5 . (back of report)
DRAWINGS (back of report)
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1.0 SUMMARY
During the past year, a drilling, geological mapping, prospecting and trenching program in specific areas was carried out on the Central Patricia property of Golden Shadow Resources Inc. A geochemical soil sampling program was also conducted on the eastern most portion. The property^ is located in the Pickle Lake area within the Patricia Mining District of Northwestern Ontario. Access is either by road from Ignace or via scheduled aircraft from Thunder Bay.
A total of 1700 feet of diamond drilling was completed in 5 holes. Two holes investigated an iron formation in the west central portion of tne property. A third hole explored an EM^ and magnetic conductor in the central portion. Two holes examined the potential of the ore zone established on claim PA 627. Only trace amounts of gold were encountered in the first three holes. Low values were obtained in the ore zone on claim PA 627, the best being 0.18 oz Au over 5 feet.
Reconnaissance geology was conducted in 7 areas in the east end. Detailed mapping was done around the trenches, which were completed in 5 areas. Only low gold values were obtained.
"B" horizon soils were collected where ground permitted and analysed for gold. "A" horizon soils were taken where the "B" wasn't available. Certain areas were good sampling, whereas others were poor. The quartz veins at the Springer and the Hook Veips showed weak soil geochemistry anomalies just above background. Poor sampling ground prevented adequate testing of most of the remaining mineralized zones. A number of good geochemical anomalies were identified that require further investigation.
A comprehensive exploration program involving detailed geological mapping over the entire grid, detailed I.P., as well as detailed geochemical soil sampling is highly recommended for this property.
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2.0 INTRODUCTION
During the past year, the former Central Patricia proper
in the Pickle Lake area of Northern Ontario has been subjecte
tyd to
a mining exploration program, conducted by Geocanex Ltd. of
Toronto. The 110 claim property is held under option by
Golden Shadow Resources Inc., also of Toronto. The exploration
program conducted by Golden Shadow consisted of diamond drilling
in selected areas, geochemical soil sampling, prospecting,
geologizing and trenching over a specific area in the eastern
portion of the property. The diamond drilling was performed
by Tindale Drilling of Midland during January and February,
1983 while the. geochemical, geological and trenching were
carried out from September to October, 1983. Geologists,
Robert Burns, of Sault Ste. Marie and Kathy Gerrie of Orangeville
conducted the geological, trenching and soil sampling. Work j.'ar,
aided by Steven O'Brien, a student of Waterloo University.
Garth B. Burton supervised the program as well as conducting
geological reconnaissance sortees.
3.0 LOCATION AND ACCESS
The property is located in Connell and Ponsford townships,
in the Patricia Mining district of Northwestern Ontario. The
town of Pickle Lake lies to the west of the claim group while
the town of Central Patricia lies within the property. These
communities can be reached via scheduled air flights from
Thunder Bay, approximately 200 miles to the south. The claims
can also be accessed by Highway 599 from Ignace on Trans-
Canada Highway 'lo. 17. A good gravel road from which access
to the grid is available, traverses the property in an almost]
east-west direction.
4.0 PROPERTY DESCRIPTION- - '.---.-U - - '- L -'L -L- -J ———— ---..'.- J
The property consists of a total of 110 mining claims ir
Connell and Ponsford Townships of the Patricia Mining district.
The diamond drilling was carried out on claims PA2457 and PA80
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J
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in the northwestern portion of the property, claim PA689 in the
central section and over the known mineralized area, on claim PA627. The geochemical soil sampling was conducted on the eastern part of the property comprising the following claims:
parts of
PA
PA
PA PA PA PA
PA
625-631
634-636
647-650 653-655
2005-2010 2015 and 2016
2018 and 2019
inclusive inclusive
inclusive
inclusive
inclx'sive
The prospecting and geological work was performed on specific sections of claims PA625, PA627, PA634, PA635, PA636, PA647,
PA648, PA2005 and PA2008, all in tho eastern part of the property. Trenching was confined to claims PA627, PA635, PA648, PA655 and
PA2008.m
5.0 WORK PERFORMED
Drilling- r ' -*- j
A total of 1,700 feet of diamond drilling was completed in Janaury and February of 1983. Following is the distribution of the footage:
GS-83-1
GS-83-2
GS-83-3
GS-83-4 GS-83-5
claim PA 2457
claim PA 80 claim PA 689
claim PA 627 claim PA 627
TOTAL:
299 ft.
297 ft.
298 ft.
538 ft.268 ft.
1700 ft.
The location of these 5 drill holes are shown on the composite map of the Central Patricia Property illustrated by Drawing No, GS-17. The geological logs of the drilling are
presented in Appendix I along with geological sections showingl
assays for gold. These drill sections are designated drawings No's GS-18 to GS-22.
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Geology/Prospecting and Trenching
Seven areas for exploration were selected from the magnetic expressions obtained in a previous magnetometer
survey which are considered to be areas where gold deposition could take place, and general prospecting. These
are referred to as areas l through 7 respectively in this report.
Area l is located in claim 648 and lies between line
67+60E and 69+80E at about 6+25N to 6+75M. Soil stripping exposed "islands" of iron formation and volcanics surrounded
by muskeg and water. Six trenches were blasted and sampled. Area 2 is located in claim 655, where two backhoe trenches
were dugj One on line 54E at 1+50S and the other on line 54+50E at 2+25S. In area 3 soil stripping was done at 8+50S
to 8+80S on both sides of line 68E. This area lies in claim 2008. In area 4, located in claim 635, stripping was attempted
on the east side of line 62E between 6+25S and 6+75S. This area is muskeg and is below the water table. No trenching was done in area 5. A single backhoe trench was dug in area 6, at 4-M2N approximately 2m east of line 59E. A depth of 12-14 feet (4m) was reached, but bedrock was not exposed due to water problems. This area is located in claim 627. Area 7, located in the southeast of claim 636, was not mapped in detail). due to lack of time available, though some reconnaissance
mapping was completed.
Detailed geologic mapping was completed in areas
1,2,3 and 5 and part of area 4 and 7. Area 6 showed no significant outcrops. Bedrock trenching and rock sampling (bulk and/or chip and/or grab) were carried out in areas 1,2,3 and 4 including some sampling of old trenches on area 2.
The reconnaissance geological mapping showing locations
of the trenching, is shown at a scale of 1:5,000 on the Geology Map over selected Magnetic anomalies (Drawing No. GS-23).
Detailed geological mapping and information on the
trenches are illustrated on a sequence of small maps labelled drawing No's GS-24 to GS-32.
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Geochemlstry
A geochemical soil sampling survey was conducted ov^r
the majority of the eastern portion of the claim block. A to cal
of 3,383 soil samples were collected on the grid at 25 metre
intervals along the lines spaced at 100m. The target horizon
was B and was sampled when possible.. The A horizon was sampled
when the B horizon was not attainable. Depending on the dept
of the sample, either an auger or a grub hoe was employed, th
former being used for the majority of the survey. The averag:
depth was 3 feet (1m). To insure accurate results a sufficient
amount of soil was collected for the required 10 gram sample
size. The samples were then dried and shipped to Bell-White
Analytical Laboratories in Haileybury, Ontario, and were
assayed for gold content in parts per billion, using the fire
assaying and atomic absorption methods. Some samples were
analysed for silver.
Histograms have been plotted for both the A horizon
and the B horizon shown on the geochemical soil sampling map
(Drawing No. GS-33). The median value and the standard
deviation were calculated and used to establish a background
level and an anomalous threshold value respectively. Anomolous
values were established at two standard deviations from the
median and highly anomalous values at three standard deviations
from the median. These parameters have been summarized on
Drawing No. GS-33 along side the histograms. In order to
develop a consistent range for the results, a number of values
were isolated from the statistical array when a cutoff point
of 50 ppb was utilized. These values should not be ignored as
they are indicative of an area with very high gold mineralization.
All results for the B horizon have been plotted and
contoured on the geochemical soil survey map at a scale of
1:5,000 (Drawing No. GS-33). The values for the A horizon were
also plotted but due to the scattered nature of results and t^e
low number of anomalous values the results could not be contoured,
Line 52E and Line 54E, 0+00 to 10+OON are areas of anomalous
reading and have been profiled, shown on the contoured map
(Drawing No. GS-33).
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6.0 DISCUSSION OF RESULTS
PrillingJ-l.-.J.U-.l-T --~ ..." !
Drill holes GS-83-1 and GS-83-2 were designed to test
a conductive magnetic anomaly indicative of oxide iron formation at two different locations where it appeared that the zone was interrupted by east-west striking faults as determined from magnetics and VLF EM results. The first drill hole intersected
i
a 136 ft. wide band of iron formation in mafic volcanics. A 5 foot fault zone was also intersected in this hole. Only trance amounts of gold were encountered in the drilling. The second drill hole intersected two seperate sections of iron formation, 22 feet and 53 feet, in intermediate to mafic volcanics. This hole also returned trace amounts of gold.
The third drill hole, GS-83-3 was put down to test an EM conductor with magnetic association in an area favourable for gold deposition. The hole encountered several bands of iron formation along with graphite and massive sulphides in a
mixture of intermediate tuff and mafic volcanics. Several
quartz veins were also interesected. All assays returned trace values in go]d.
Drill holes GS-83-4 and GS-83-5 were put down in the
vicinity of the gold mineralization encountered in previous drilling on claim PA627. The holes were designed to substantiate and expand the known mineralized zone in the iron formation horizon. The two holes intersected the mineralized iron formation
on target. Hole No. GS-83-4 returned the following assays across the ore zone.
Depth Length Oz Au/ton139.8 to 144.8 5.0 ft. .02144.8 to 149.3 4.5 ft. .02149.3 to 154.3 5.0 ft. .18
154.3 to 158.8 4.5 ft. .06158.8 to 163.0 4.2 ft. .05
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All remaining assays gave only trace amounts of goJ.d.
Another mineralized section from 373.5 to 398.5 had the best assay of .08 02 Au/Sft. from 388.0-393.0. Other assays in the group ranged from .01 to .04 oz Au/ton.
The second hole, GS-83-5, returned the followng assays in the same mineralized horizon:
D^jpth Length O z Au 1 1 on129.5 to 134.0 4.5 ft. .02134.0 to 139.0 5.0 ft. .04139.0 to 143.5 4.5 ft. .03143.5 to 148.0 4.5 ft. .02
All other assays gave trace gold.
Geology
Area l
Basic to intermediate volcanics with pillows and
fragmental textures and a lean cherty siderite iron formation, grading towards oxide facies with variable magnetite content
with some chlorite silicate laminae, 0.1 to 50 mm wide have tpeen exposed by soil stripping (compare trenches 4-6). Folding
within the iron formation consists of both "S" and "Z" folds formed from penecontemporaneous slumping prior to consolidation. Generally the plunge is vertical. A fault contact between andesitic greenstone with fragmental pillowed structures, approximately 100-500m long and a lean cherty siderite iron
formation with some magnetite, chlorite, pyrite and pyrrhotineis observed in the eastern part of the area. The south side ofthe volcanics appear to be moze massive. The iron formation hosts quartz veinlets with pyrite and pyrrhotite trending NN in the north end of the formation. In the mid and south are^s the quartz veins are more numerous and run both NMW and NE.
In the east central part of the stripped area (trenches 7-9) a banded cherty siderite occurs with some magnetite and
scattered quartz veinlets generally trending WNW and with some
pyrite and pyrrhotite. The veinlets are 10-50 mm wide. The
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iron formation becomes more magnetic to the west, where 1-57* pyrrhotite and pyrite are found throughout, and a greater
concentration of quartz veinlets. There is an abundance of quartz veinlets to the south (trench 4) but, become scattered
and smaller in the north and show no apparent relationship to folding in the iron formation. The quartz veinlets generally
i
trend WNW and NE with some running NNW with a thickness of less than 20 mm wide.
The outcrop area in the central portion of trench lO consists of iron formation with large blocks of andesitic
greenstone, essentially in place, north of the outcrop area.
The iron formation is a cherty siderite with minor magnetite
and some chlorite laminae, possibly silicate facies IF. The iron formation lamina is 2-50 mm wide. Pyrite and Pyrrhotite are scattered throughout with a greater abundance within the quartz veinlets. The quartz veinlets trend NNW throughout
the formation with many ENE veinlets in the north and becoming scattered to the south. The veinlets carry iron carbonate, pyrite, pyrrhotite and to the north some galena in a ENE vein. They also carry some sericite, chlorite,
late calcite and late quartz. A strong "S" fold with a vertical plunge is observed. Bedding is near north-south in the south end.
In the west portion of the area there is a fault contact between the andesitic greenstone and the iron formatioii.
Faulting occurs throughout the area displacing iron formation. Two parallel faults in the east and west ends of the area
strike approximately 80.No outstanding gold values were obtained from the
trenching. The highest assay returned 0.054 over 2 feet in
trench No. 83-5.
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Area 2
The soil trench excavated by means of a backhoe at
1+50S on line 54E exposed bedrock in which a trench was blasted
(Trench 83-2). This was sampled for gold, silver and copper. Quartz veins with pyrite, pyrrhotite, chalcopyrite, chlorite
and carbonate occur in both oxide iron formation and andesite. The iron formation is well banded and consists of mixed
chert, iron silicate, magnetite, and 5 to 107. pyrite and
some pyrrhotite. There is heavy mineralization in places.
In trench 83-3 at 54+50E just south of trench83-2, there is lamenated silicate iron formation cut by ankerit^ veinlets with some pyrite. These follow the shearing which is about 120a, same as the veins. Bedding is approximately 110?
Low gold values were encountered in both trenches.
Area 3
The stripped area revealed cherty iron formation with
minor siderite, some chlorite, a trace of magnetite and l to 370 pyrite. Locally, there is up to 107. pyrite in rows (spotty) and veinlets along bedding planes. There is also some pyrrhotite. North of the stripped area a vuggy quartz vein occurs with limonite, iron, carbonate, pyrite (10-157*) and a trace of tourmaline. Some of the rock reveals a black
argillite containing 3 to 5" fine pyrite along bedding and foliation planes.
Area A
Stripping has exposed small areas of outcrop containing andesite and iron formation. The iron formation
is a cherty, sideritic unit with magnetite, quartz veins
and pyrite. The iron formation is broken in vertical plates which are deeply weathered. Quartz veins with limonite, carbonate, pyrite and chlorite occur at the north end. Shearing
is at 355*(north end). Sheared greenstone with quartz veins
and pyrite likely indicate the presence of a fault. The proposed fault matches the displacement evident between the
central and eastern parts of area 1. Poor gold values were obtained.
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Area 5
The geology encountered in area 5 consists pie- dominantly of intermediate to andesitic volcanic rocks, mostly of the massive and pillowed variety. Foliation is at 105-110** and dipping north.
Area 6
There is no outcrop in area 6.
Area 7
Limited outcrop in this area revealed massive andesite with foliation at about 1000 dipping north at 70* to 80*! Several
quartz veins are present. These appear barren.
Folding does not appear to be important. In the iron formation folding is original sedimentary slumping. Faulting has been observed in two of the areas explored during this
phase, (l and 4). In area one a series of four parallel faults exist with two larger faults to the east and west of the area striking approximately 45 0 and dipping about 80? The
four other faults strike in a different direction with small
or no displacement of the geological units. One other large fault striking approximately 3500 displaces the central and east parts of area 4.
Geochemistry
It is difficult to assess the success of the geochemical program for several reasons. The nature of the soil deposits
are not accurately known, therefore, the proper distribution of gold in the soils from known mineralized areas is difficulty
to assess. Also the distribution of the various soil types, glacial sands and gravels with minor clays intermixed with
muskeg and swamp, did not provide a consistent sampling mediuri to co-ordinate the results. Despite these drawbacks, the geo chemical sampling did show some anomalous features that are
noteworthy.
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Prime amongst these is the low value of 20 ppb obtained
in good soils just south of the Springer Vein. (It was impossible to obtain a sample over the vein itself because
I of insufficient soils.) This value is significant in that it shows that at single,low value on the wide grid spacing used, i.e. 25m stations on 100m lines, suggest the possibility of
i good gold mineralization in quartz veins such as that mined
at the Springer. In support of this observation, a weakf geochemical anomaly of only 14 ppb was obtained in the vicinity
of the Hook Vein, (approximately 20m southeast of it). This
1 anomaly occurs in an area of good sampling. In much of the other areas where gold mineralization is
known, it was difficult to collect proper samples. Consequently f it was impossible to obtain characteristic geochemical signatures
over these mineral zones.
i Despite "he difficulties in obtaining samples, there were:a number of j-.eochemically anomalous areas defined during the
i survey. Two north-northwesterly trending zones have been out-j
lined. Extremely high values were encountered on line 68E of
g one zone that extends from 600N on line 66E to the baseline on f 70E. This value reached over 1400 ppb. A possible extension
to this zone occurs at 750S on line 74E and 825S-900S on line
l 75E. The second north-northwest striking zone runs from 950Non line 52E to 325N on line 56E. There are good high values cm
^ line 52E, but the values on the remaining lines are mediocre.These zones appear to be fault controlled.
I Another area of anomalous geochemical values occurs at the south ends of lines 64E, 65E and 66E. Multiple scattered pealjs
appear in a random fashion in a poor sampling area. i Other anomalous zones are:
between 200S and 375S, lines 78E and 79E between 675S and 825S, lines 78E and 79E
between 725N and 750N, lines 62E and 63E along the boundary.
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Individual peaks are located as follows:
Line 53E - 525N
Line 55E - 725N Line 57E - 200S
Line 5AE - 700S Line 59E - 550S
59E - SOON59E - 600!'
Line 62E - 625N Line 6AE - 225N
6AE - 125N Line 63E - 050S
63E - 175S Line 65E - AOON
Line 66E - 150S66E - 250S66E - 350N-450N
Line 70E - 200N
These areas are ideal candidates for gold quartz veins sijch as the Springer and Hook Zones especially the 33 peak value at 050S on line 63E.
7.0 CONCLUSIONS AND RECOMMENDATIONS
The 1983 drilling program was helpful in defining some of the geophysical and geological features that make up the
complexity of the Central Patricia gold property. Although low gold values were encountered, further understanding of the geology was obtained. The two holes drilled in the ore zone on claim 627 confirmed the gold mineralization occurring there. Certainly much more drilling is required on the property to properly evaluate its potential.
The reconnaissance geological and prospecting program carried out on the extreme eastern portion of the property
also provided further insight into the potential for gold
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mineralization there. Although a more comprehenisve geologica mapping program is required to satisfactorily understand the full picture, the detailed geology gathered from the trenching has provided an insight into the localization of gold mineralization. Ore controls, according to, R. Burns, geologist who did the majority of the mapping on the property, are:
1. Post porphyry mineralization and potentially favourable structures cutting the porphyries.
2. Although folding does not appear to be a con trolling factor, ore zones appear to follow the strong regional foliation, that is about 1200, where it cuts the porphyry and older rocks.
3. Faulting is important in ore control. Ore veins trend from about WNW (120 0 ) to east- west to northwest.
4. Significant iron formation types associated with ore zones include oxide, carbonate (the most abundant), and silicate facies. Sulphide facies iron formation was not particularly recognized in the present program.
The sulphides, whether in veins or in iron formations and most of that in other rocks, appears to be conventional introduced hydrothermal mineralization.
The flat topography and poor drainage make stripping difficult in this area.
The following recommendations are proposed to further
explore the Central Patricia property:
1. Detailed geological mapping over the entire property, paying close attention to quartz porphyry intrusive distribution; iron formation facies variations as well as structures and mineralization. Faulting and fracturing patterns should also be mapped closely.
2. Detailed I.P. should be conducted over specific areas such as iron formations in low magnetic areas, under swamps where possible sulphide con centrations could exist, faults and slips which could be related to veins, particularly the north-northwest striking geochemistry anomalies.
i111 11111I111i11l\1
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3. Closer spaced geochemical soil sampling in areas where lengthy anomalies appear, particularly the north-northwest striking zones and around other high values.
4. Further sampling of old surface trenched areas along with trenching in new areas where feasible should be done concentrating on geochem. and I. P. anomalies.
Following careful analysis of the geology, I. P. and
geochemistry data, a comprehensive drill program should be devised.
Respectfully submitted,
GEOCANEX LTD./ ~~)
Garth B. Burton Geophysicist
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REFERENCES
Ferguson, Stewart A., 1966, Geology of Pickle Crow Gold Mines Limited and Central Patricia Gold Mines Limited, No. 2 Operation, ODM, Mis. Paper MP-4.
Tilsley, James E., 1983, Exploration of the Central PatriciaProperty, Pickle Lake Area, Northwestern Ontario for Golden Shadow Resources Inc. - company files.
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1
1
1
1
1
1
1
1
I
1
1
1
1
1
R11
V
LIST
GS-17
GS-18
GS-19
GS-20
GS-21
GS-22
GS-23
GS-24
GS-25
GS-26
GS-27
GS-28
GS-29
GS-30
GS-31
GS-32
GS-33
OF DRAWINGS - CENTRAL PATRICIA PROPERTY
Central Patricia Property
Vertical Section - D. D. H. GS-83-1
Vertical Section - D. D. H. GS-83-2
" - D. D. H. GS-83-3
11 - D. D. H. GS-83-4
" - D. D. H. GS-83-5
Geology Map over Selected MagneticAnomalies
Geological Mapping and SamplingArea 1 Overview
M M M
Area 1 East EndII M M
Area 1 Trenches 83-7,8,9M it ti
Area 1 Trench 83-10M tt II
Area 2 North Sectionn n MArea 2 Trench 83-2
n M MArea 2 Trench 83-3
n tt ti
Area 3n tt tt
Area 4 Stripped Section
Geochemical Soil Sampling
1:12, Of(back poc
1 ln-5C
0ket)
ft.
1 in-5CJ ft.
1 in-5q ft.
1 in-5C
1 in-ST
ft.
ft.
1:5,000(back poc :ket)
1:80C)
1:100
1:10C
l:10d
1:1,OC)0
1:50Q
1:501r
l:50Cl
l:10(j
1:5,000 (back pocket)
l
DIAMOND DRILL RECORDNAME OF PROPERTY GOLDEN SHADOW- CENTRAL PATRICIA PROP.M mr Mft GS - 83-1 , rnoTH 299 feetLOCATION Claim 2457LATITUDE 15 + 25 East nep*. ., 13 4- 25 NorthELEVATION " A7IMUTH 130* Dlp -50
STARTED January 23, 1983- 1M1 , UPn January 30th, 1983
FOOTAGE
FROM
0
125.0
130.0
|
,M|
TO
125.0
130.0
236.0
DESCRIPTION
CASING, sand, sandy clay and boulders.
FOOTAGE
299
DIP
42
MAFIC VOLCANICS, BASALT?, fine to medium grained, darkgreen, chloritic, numerous brown (limonitic)oxidized stringers, slighty porphyritic,leucoxene, strongly shepred at 40^ to C. A
minor
125.5-1^0.0 - FAULT ZONE, broken core. 2 feet of lostcore in this section.
IRON FORMATION - finely laminated to coarsely beddedwhite to grey chert and magnetite. Individualbeds up to 2 thick. Much of the magnetite ispartly oxidized to ochrous to chocolate brownlimonite. Occasional narrow (1-2 m. m) bands ofminor pyrite. Bedding at 45" to C. A. Scatteredvuggy sections suggesting leaching of ironcarbonate? Sulphides?
143.6-146.6 - heavy magnetite (and limonite), 5-87.pyrite.
146.6-159.0 - mainly light grey, well bedded chertwith fine magnetite throughout in thin (1bands and disseminations. Minor pyrite.
mm)Bedding
35 to C. A., slightly crenulated in sections.Occasional wisps of pale green chlorit . Minorreddish brown mineral in thin laminae, probablyspecularite, possibly sphalerite?
159.0-191.0 - as above with increasing chlorite,occasional sections of chert-chloritic brecciawith chert fragments in a chloritic matrixscattered sections of heavy brown, partly oxidizedmagnetite, probably representing water-bearing fracture zones, partly vugp.y with minor pyrite
AZIMUTH
-
"OOTAGE
SAM
NO,
910
911
S.fc
0
P L
FO"FROM
143.
168.
6
0
1
1
p AZIMUTHHOLE f
o GS -83- \H EET MO. -L
REM ARKS
LOGGED BV H. J. HodgC
e)TAGCTO
46
71
.C
.C
TOTAL
3.
3.
0
0
ASSAYS
t i, AUOZ/TON
T r
Tr
OZ/TON
DIAMOND DRILL RECORDM o i. r NO ....Q.S;.
rOOTAGC
f BOM
236.0
237.6
10
237.6
266.6
DESCRIPTION
from 168.0-171.0, 188.6-191.0. At 174.0 bedding30 e to C. A. Occasional cross-cutting quartz-carbonate veinlets up to 1/2" wide.
191.0-224.2 - over 502, magnetite in 2"-3" bands withinterbedded chert and occasional green chloritebands. Minor pyrite, occasional cross-cuttingstringers and veinlets of quartz 203.7-204.3 -quartz vein milky white, cataclastic texture.Bedding at 206.0 - 30'to C. A.
224.2-224.6 - Andesite, dark green (tuff)224.6-233.3 - mainly cream colored chert, finely
laminated to coarsely bedded with minor blackmagnetite bands and occasional narrow palegreen chlorite bands.PROBABLY SILICIFIED ZONE
223.0-236.0 - CHERT BRECCIA SILICIFIED, cream colouredsilicified, highly fractured and brecciated,with network of narrow bluish-white quartz vein lets, and pyrite stringers. Minor magnetitethroughout occasional chloritic stringers,generally with pyrite. Short sections showremnant fine bedding laminations. Some shortsections up to 30-40^ pyrite, probably 57,overall.
QUARTZ VEIN - bluish-white, irregular contacts, minorwispy chlorite, pyrite, 40-50* chert breccia,
IRON FORMATION, CHERT BRECCIA, as above.At 238.0-1" irregular matic dyke.
238.6-244.0, mainly laminated chert (non-brecciated) .Light grey to cream coloured beds, minorchloritic bands (beds?) with pyrite occasionalthin bands of magnetite bedding 60' to C. A.
244.0-246.0 - Silicified, cream colored, welllaminated, minor pyrite in fine bands parallelto bedding (57. overall) minor crenulations.
SAMPl
NO
912
913
914915916
917
* *UIFM
!RM r*oM
189.6
203.7
223.0228.0223.0
236.0
1TV.GQ.1.
5.3dL-.J)J5tLSHAPPW-j5MTRAl.eAmiCl/...... ___ SHE t T NO,- _ 2
eOOI*Of
TO
191.1
04.3
228.0233.0236.0
237.6
'O'Al
1.6
0.6
5.05.03.0
1.6
S, m.
ASSAYSAll
'\ *, 01 TO*
Tr
Tr
TrTrTr
T r
Of TO*
DIAMOND DRILL RECORD NAMC or
HOI. C NO. .-M?.^ SHEET NO.__i.__.
rooTAoe
f HOM
266.6
299.0
l
to
299.0
DESCRIPTION
246.0-247.4 - Magnetite plus 507. well bedded.247.4-248.4 - Grey intermediate dyke. Slightly
porphyritic iwth white feldspar phenocrysts.Minor pale green chlorite.
248.4-252.0 - as above (246.0-247.4)252.0-253.3 - Rhyolite?, pale yellowish white, highly
sericitized for first 4". Massive, minordisseminated pyrite. (Dyke?)
2.53.3-258.0 - Magnetite rich, as above with creamcolored silicified section 254.0-256.0,This section shows remant of partly silicifiedmagnetite with laminations crossing the re placement "front".
258.0-266.6 - bleached, silicified to cream color asbefore. Well laminated at 40" to C. A. Occasionscross-cutting bluish white quartz veinlets up to1". Minor pyrite.1" to 2" quartz veinlets at low angles to C, A.from 264.0-265.0
ANDESITE - medium grey green, fine to medium grained.Massive, occasional quartz-carbonate stringersto 1/2".
END OF HOLE
SAMPL
MD
918919
1 tut PH tors
rf ROM
258.0262,3
OtAO'.to
262.266.
rut*l
4.34.3
ASSAYS
^ ^AU or 'f**
TrTr
b r TOM
DIAMOND DRILL RECORDGS-
NAME OF PROPERTY cni.nRN RHA^nu- CENTRAL PATRICIAnmr NB. GS-83-2 LrN 0 T H 297 feetLOCATION Claim No. 80LATITUDE 13 * 70 East DrPA*Ti..r 11 * QQ NorthELEVATION " ' A'/IMUTM 130 Dlf -50*
STARTED Jan. 31st. 198JiMi*um Feb. ?nrf, 1981
FOOTAGE
FROM
0
24.0'
55.5
60.3
61.8
l
TO
24.0
55.5'
60.3
61.8
69 0
DESCRIPTION
FOOTAGE
297
DIP
45"
CASINO, sand, sandy clay, boulders near bedrock.
INTERMEDIATE VOLCANIC, (ANDESITE, SILICIFIED?)medium to light grey color, fine grained,massive to slightly banded (sheared?) at 50"to C. A.
QUARTZ VEIN. Approximately 507. bluish white and 507. cream colored(in part laminated) quartz(silicified chert?). Fractured. Minorin narrow veinlets up to 1 mm.
pyrite
55.5-56.0 - 257. pyrite and minor chlorite in irregularreinlets .
58.5-59 0 - several bands of chloritic mafic rocks.tuff?), with 15 to 207. pyrite.
59.0-60.3 - bluish white quartz, massive.
MASSIVE SULPHIDES. 607. banded pyrite, 407. chloritictiff? Banding 40" to C. A. Out contacti -regular at 20" to C. A.
CHERT (ir part TUFF?) LEAN IRON FORMATION
banded
Silicified cream to light grey, well laminated.Minor pale greenish chloritic bands withpytite "seams up to 3 mm. Bedding 50" to C. AMinor MAGNETITE in fine laminae probably 5-87.ovt-rall. Occasional fine bluish white quartzveinlet .
AZIMUTH OOTAOE DI* AZIMUTHHOLE MO. ~" "-'.. ~*HEfT MO, . * , , ,
RFMARK3 , ,.
LOPGED BY " - J - Hodge
S * M P 1 E
NO.
920
921
922
923
SULPH' Juts
FFROM
55.5
60.3
61.8
66.8
OOTAOETO
60. 3
61. f
66.
69.
ft
0
TOTAL
4.8
1 . 7
5.0
2.2
ASSAYS
* Vnu
OZ/TON
.02
T r
Tr
Tr
O7/TON
DIAMOND DRILL RECORD NAMt OF PROPER
GS-33HOLt NO. -.--....
T GOLDEN SHADOW-CENTRAL PATRICIA---- -- -- -
NO.____. .
FOOTAGE
rnoM
69.0
82.0
244.6
297.0
.
TO
82.0
244.6
297.0
DESCRIPTION
IRON FORMATION, transitional from above. Fine blackmagnetite bands with interbedded light greychert and occasional green chlorite. Occasionalnarrow bands of pyrite up to 1/8" with minorbrown limonite? or specularite?Bedding at 35 0 -40" to C. A.
MAFIC VOLCANIC, BASALT? Transitional from above.blackish grey, fine grained, well banded (tuff?)for one footfrom contact, then lighter greenishgrey and finally deep green at 85.6
85.6-106.0, mottled texture (porphyritic?) with darkgreenish black chlorite 'spots', Massivenumerous fine quartz-carbonate veinlets to 1/8",slightly magnetic.4" quartz-carbonate vein at 97.0.
106.0-110.0 - Bruken, highly chloritic (FAULT?)110.0-165.0, - as above (85.6-106.0) becomes slightly
lighter greenish grey color with bleachedsilicified section at 153.0-154,6.
165.0-244.6, darker green and mottled as before.More quartz-carbonate veinlets. Becomesfine grained at out contact.
IRON FORMATION, transitional from above. Wellbedded black variable magnetite bands andcream colored and light grey chert withoccasional green chlorite bands with minorpyrites and brown jigularite , Magnetite 257..Chert appears silicifiedT bleached.Bedding consistent at 30"-35" to C. A.
END OF HOLE
SAMPLE
HO t f III PH
1DC}
nMOM
otAoeTO 101*1
Asyyrs
-. * 0' tOM tit TOM
MUM fifi**l ta^tl^Eg^^
DIAMOND DRILL RECORDNAME or PROPERTY pOLDEh} SHADOV-r.F.NTRAl. PATRICIA PROPMOLE NO GS-83-3 LENGTH 298.0
, OCAT.ON Claim 689LATITUDE L28 4 50 E DrPA.Tn.r 4 4- 08 S
START Feb. 7. 1983 r,*,. Hm Feb. 19R1
r o o T A c E
FROM
0.0
50.0
72.0
110.0
111.3
i*
TO
50.0
72.0
110.0
111.3
167. S
OVERBURDEN
INTERMEDIATE TUFF
rOOTACr DIP AZIMUTH t
298.0 43*
OOTACe
Light to dark grey fine grained moderately to well bedded rock. Light grey chert beds noted,Sections of broken fractured core (fault zones?)at 52.5-53.0, 57.0-59.5, and 67.5-68.0.Core angles: Bedding 60-65* to C. A.
IRON FORMATION72.0-87.0 A lean Iron formation, in part oxidized.
Mainly chert and intermediate tuffs, minormagnetite oxidized to hemotite.Fault zone (?) at 76,5-78.0, with quartzstringers.
87.0-110.0 As above, with occasional graphitesections with 5*4 pyrite, increasing tolower In section.
QUARTZ VEIN
101
A greyish white quartz with 1574 tuff (wall-rock) and a 51 pyrite content.
INTERMEDIATE TUFF BRECCIAA bluish grey rock with fragmental and brecciatezones. Occasional secondary quartz(?) or chert(?) throughout the zone.Moderately bedded 141.0 is 60* to C. A.sulphide content increases down hole, averaging10-25X.
SAM
NO.
942943944945946947
924
948949950
s.fe"
DIP
PL!
FOOFROM
85.090.095.0100.104.108.
Cc0
110.0
111.3116.0120.5
T
9095
AZIMUTHHOLE MOVjS-oj-j snrrr MO. ^J. .- -
REMARKS
LOGGED BV R. T. Chstaway
AGEO
00
.06 .104.108,110.
li
IK120.12 i.
0
0
00
3
050
TOTAL
5.0
5.05.04.04.02.0
1.3'
4. 74.54.5
A SS A v S
V V O7/1OH
TrTrTrT rTrTr
Tr
TrT rTr
OI/TON
si
1C
l
i
PI AMOND DRILL RICORDHOI. E NO jLJJ?.^i?..
FOOTAGE
rHOM
111.3
167.5
171.5
178.0
.
to
167.5
171.5
178.0
180.2
DESCRIPTION
122.0-144.5 Narrow pyrite lenses (1 tnm-5 mm) thatare partly weathered (vuggy). Pyrite to 107. Quartz-magnetite bands (i74"-W2 r') with chert(?)(quartz?) bands (1") from 122.0-128.0Minor pyrrhotite associated with occasionalchloritic sections. Minor creamy-buff quartz
CONI 'D INTERMEDIATE TUFF BRECCIA144.5-150.3
Pyrrhotite averages 15-207. with only minorpyrite and occasional chalcopyrite on thincross fractures.
150.3-162.0Pyrite-f illed fractures, creamy-buff quartzfractures 'vuggy) .
162.0-167.5Sections of heavy chlorite with pyrrhotite. Afew thin fractures with chalcopyrite, i.e.(162.2').
IRON FORMATIONInterbedded grey chert (tuff?) and magnetite(25H) Occasional massive chloritic sectionswith S-8% pyrrhotite.
INTERMEDIATE TUFF BRECCIAAs before (111.3-167.5). with sections of heavychlorite (5-107. pyrrhotite) and grey chert.
QUARTZ VEIN ZONEA milky white to greyish-white quartz vein withwallrock (tuff). Minor sulphides-pyrl te andpyrrhotite.
SAMPL
NO
951952 953954
955
956957958
959
960
961962
925
, SULP*
rOCS
L J
5-3 _
;OLDEN SHADOW- CENTRAL PATRICRo
__ ,- . __ SHCET NO. __ ~ - . .
E
fOOTAOe
f MOM
125.0129.0 134.0139.0
144.0
149.0154.0158.0
163.0
167.5
171.5176.5
178.0
TO
129.1134.1 139.1144.1
149.'
154.'158.'163.
167,
171.
176.178.
180.?.
10UI
4.05.0 5.03.0
5.0
5.04.05.0
4.5
4.0
. 5. 0 1l 1.5
. 2.25
ASSAYS ill
;7TU
or TOD
TrTr TrTr
Tr
TrTrTr
Tr
Tr
TrT r
Tr
01 TO*
fcv-;-
DIAMOND DRILL RECORD GOLDEN SHADOW-CENTRAL PATRICIA
MOLE NO -:l.., SHEET NO.—--
FOOTAGE
r BOM
180.2'
225.0
231.5
233.5
242.7
l.
TO
225. (
231.5
233.5
242.7
247.5
DESCRIPTION
INTERMEDIATE TUFF BRECCIA180.25-200.0
As before, with increasing sulphide content.Strong chloritic sections, with pyrrhotite, pyrite and minor chalcopyrite. Overall average sulphide content is 201.. Numerous chert (1) orquartz(?) zones.
200.0-225.0Tuff breccia with sulphides.Sulphides occur as stringers, lenses and amatrix to the breccia. Secondary pyrite inlater fractures. Average pyrite content is 257..only minor pyrrhotite.
MASSIVE SULPHIDESPyrite to 60Z or more from 225.0-228.0Bedded 9 60" to C. A. with some vuggy andsecondary pyrite in fractures, Chert (?) orquartz(?) zones in section. Minor graphiticargillite. Minor chalcopyrite in quartz veins.
GRAPHITIC TUFFAn argillaceous tuff with 10-12* pyrite.Bedding planes 9 50" to C. A.
INTERMEDIATE TUFFAs before, with 5-8* sulphides (pyrite).Sharp contacts at 50* to C. A.
235.0-242.7Pyrite (25-40X) in narrow massive sections.
GRAPHITIC TUFFA graphitic tuff with some short breccia zones.Pyrite to 15-20*
SAMPU
WO
926927 928 929
930931932933934
935936
937
938939
940
941
. tlUfH
totsf
r*ou
80.25185.0 190.0 195.0
200.0205,0210.0215.0220.0
225.0228.0
.31,5
233.5235,5
240.3
*1 y *1 **24? . 7
ioTActTO
185.1190.i 195.i 200.
205.210.215.220.225.
!28.0!31.5
?33. 5
235.5240.3* t f\ *i242 . r
r i -j r247 . 5
TOTM
4.7'5.0 5.0 5.0
5.05.05.05.05.0
3.03.5
2.0
2.0'4.8'
f\ it- . 4
j Q l4 . 8
ASSAYS All
-, -. Ton
TrTr Tr Tr
TrTrTrTrTr
TrTr
Tr
TrTr
Tr
Tr
01 Ton
h**M0
ta'i
DIAMOND DRILL RECORDHOLE Nf
FOOTAGE
r MOM
2*7.5
298.0
i*
'O
298.0
DESCRIPTION
ANDESITEA grey-green fine to medium grained rock with minor pyrrhotite. Many c'osfl-cutting quartz- carbonate stringers (l-5mnO schistosity P 55* to C. A.
275.0-280.0A cherty sedimentary section with banded pyrrhotite and minor chalcopyrite.
END OF HOLEN. B. CASING PULLED.
" PnOl'EHTT.
j GS-S3-5
SAMPLE
NO1 *Ul'X
I0t J
toof *OM
G.QLDE.N..5.HADQW;
-. , ., SHE
Ant101*1
JCEliGC.ilCT NO
AL.1AIRICIA 4
ASSAYSAll
\ ^ 01 '(K 61 'On
!f-f '
DIAMOND DRILL RECORDNAMI or mott
GS-um r un. "" ,, . M. -- .--..WTV GOLDEN SHADOW- CENTRAL PATRICIA83-4 , . UKVU 538 Feet
~- 4T , nN Claim No. 627LATituor 4 + 13 North ^....,,... 54 4- 60 EastlUCVATIC
T ANTED , .-..~-,- u
)N .. ^.MUTM ,,'J V.-'^lo'ln.P -50'Feb. 11, 1983 , 101 . _ Feb. 1!, 1983
r o o T / o t
r*OM TO
0.0
12.0
13.0
17,5
22.5
25.5
P
12.0
13.0
17.5
22.5
25.5
36,5
ocacftiprioN
CASING
INTERMEDIATE VOLCANIC (ANDESITE?)Fine grained, dark green, massive, minorveinlets
TUFF (BRECCIA?)
roorwi300'538'
DIP
44*41*
quartz
Felsic to intermediate, white to ligth grey(bleached?) Well bedded ( lamina r.* -1) withlocally fragmental sections. Highly oxidized.3-57. pyrite principally as crosscutting veinlets.Bedding at out contact 50* to C. A.
16.0-16.4 -intermediate volcanic, ae above (12.0-13
INTERMEDIATE VOLCANIC
0)
Fine to medium grained, medium green-grey color,massive to slightly banded. Finely porphyritic?with bluish-grey feldspar? phenocrysts in a "tan"colored sericitic? ground mass.
TUFF (CHERT?)White to light grey, finely laminated nt 30 s toC. A. Minor cross-cutting quartz veinlets * idpyrite stringers.
29.0-29.8 - white to light grey (bleached?) cherty,3" irregular quartz vein at upper contact.
IRON FORMATIONPoorly to well banded, Heavy magnetite withinterbedded grey chert. Occasional chloriticintermediate tuff. Minor pyrite and quartzveinlets.
34.5-35.5 - 307.-40Z pyrite, minor pyrrhotite
A7MUTM 1 ooTAoe
SAM
NO.
963
964
965
966
siPtsV
on
f L 1
fOOrnoM
13.0
22.5
27,5
52.0
1
2
3
3
AZIMUTH
ktf^ t MO UO**DJ ̂4 ^tifff ttf\ 1
LOOOED .y H. J. Hodge
rAoe0
r
J
1
3.
5
5
0
5
TOTAL
4.5
5.0
4.5
4.5
ASSAYS
* ir.
1
nvO7/TON
Tr
Tr
Tr
Tr
07/TON
DIAMOND DRILL RECORD MAMF or PROPER'Y. yGOLDEN SHADOW-CENTRAL PATRICIA
MOLE NO GS-^3-4.._ &HEFT NO __....
FOOTAGE
rnoM
36.5
102.0
103.0
106.3
'
TO
102.0
103.0
106.3
163.0
DESCRIPTION
INTERMEDIATE VOLCANIC (ANDESITE)Medium greenish-grey, fine grained, slip,hr.lybanded at 45" to C. A.5" quartz vein - milky white at 92.5-93.0 withquartz veinlets in walls.
INTERMEDIATE TUFFWell banded 40* to C. A,, meJium green, finegrained, minor pyrrhotite (57.)
INTERMEDIATE VOLCANIC (ANDESITE)Medium green, fine grained, massive to slightlybanded.2-1" to 2" irregular quartz veins at 105.5
IRON FORMATIONCoarsely bedded, light grey chert with subordinatemagnetite, minor chloritic tuff bands. Occasionalblue-grey quartz veinlet, minor sulphides- pyrrhotite less pyrite, both as bands parallel to bedding and in cross-cutting fractures.(probably 57, overall).
113.0-163.0 - finely bedded chert and magnetite withminor chloritic tuff. Minor pyrite and pyrrhotiteNumerous interlacing blue-grey quartz filledfractures with rusty brown iron oxide.Bedding 65* to C. A.Sulphides increase down the hole to 10-127, withsections up to 257, to 307..At 134.0, A to 5" of quartz-chert breccia-fragmentof laminated chert in white quartz matrix withrusty red iron oxide.At approximately 150.0, banding becomes indistinct and changes to 35* to C. A. more irregular quartzveinlets. Sulphides increase to 457. to 507. insections, 15-207. overall .
SAMP
*IO
967
993
968969970 971 972973
974975976977 978979
^ V't PH
rpM rnou
92.5
IDS.:
106.:in.:115. f 120. f 125.6130.]
134. f"139. f144. {149.: 154.:158. i
E
rooi*ot'0
93.5
106.:
in.:115. f120.? 125Jno.:134.1
139,1144.149.154. 158.163.
lOfM
1.0
1.0
5.04. S5.0 5.0 4.54.5
5.05.04.55.0 4.5
l 4.2
ASSAYSAll ........
'. -. 01 ra*
Tr
Tr
TrTrTr Tr TrTr
Tr.02.02, 18 .06.06
fjj TOK
DIAMOND DRILL RECORD NAME Of GOl'-EN SHADOW-CENTRAL PATRICIA
SHEET NO..
FOOTAGE
mot*
163.0
165.6
199.5
'ti
i
to
165.6
199.5
368.5
DESCRIPTION
INTERMEDIATE TO MAFIC VOLCANICDark green, fine grained, highly chloritic, minorlight grey chert fragments?.
IRON FORMATIONAs above, poorly bedded chert and magnetite withminor chloritic tuff. More chert, less magnetiteBedding at 55' to C. A.Sections brecciated. Less sulphides, probably2-3* with narrow sections to 107.-15H. (pyrrhotite,minor pyrite) .
176.5-183.5 - 15-201 pyrrhotite, minor pyrite, 151Irregular quartz veins, numerous quartz and sulphide filled fractures with minor displacement
183.5-190.5 - as above but 3-51 pyrrhotite, minorpyrite occasional laminated section with bedding45* to C. A,
190.5-199.5 - becomes more banded, still with quartzstringers, minor pyrite, pyrrhotite (1-21 overall)
INTERMEDIATE TUFF? (BRECCIATED?)Dark green, chloritic, fine grained, moderately towell banded at 40* to C. A. Numerous quartzstringers up to 1". Minor pyrite, pyrrhotite(1-21)
199.5-201.3 - 501 Irregular quartz vein 223.0-233.0 - graded change to medium grey, massively
banded (bedded?) at 45* to C. A. Occasional quartzstringer to 1 to 2 mm. No sulphides
233.0-248.0 - Dark green, heavily chloritized, shearedand broken (FAULT ZONE)
248.0-318.6 - medium green as above (223.0-233.0)with interbanded section of blackish greenchloritic material. Occasional oxidized section(water bearing fault zones?) Hazy fragmentssuggest brecla.
318.6-319.0 - FAULT ZONE327.5-328.0 - "
aAMPL
NO
980
931982
983984 985 986
987
988989
990 991992
\4lllfM
lOt!
r' DU |
163.0
165.6170.0
175.0180.0 185.0 189.5
194.5
199.0199.5
201.3 206.3211.3
OOf A6E10
165. (
170.1175.1
180.'185.1 189. 194,:
199.
199.201.
206. 211.216.
rotAi
2.6
4.65.0
5.05.0 4.5 5.0
5.0
0.51.8
l 5.0 5.0
l 5.0
mrs i V 01 tot
Tr
.03Tr
Tr.01 Tr Tr
Tr
Tr.02
Tr T rTr
01 TON
DIAMOND DRILL RECORD NAME Of
HOLE NO 5.5.iiyL~A-.FOOT AGE
rao*
368.5
398.5
478.2
.
TO
398.5
478.2
484.5
DESCRIPTION
IRON FORMATION BRECCIATEDMainly cream colored laminated chert with minor(3-5*) magnetite, minor chlorite chaotic mixtureof well-bedded sections with variable beddingdirections (generally out 55" to 60* to C. A.)and brecciated sections. Numerous roultidirectional minute fractures with displacementalong.Numerous veins, veinlets and stringers of blue-grey quart*.. Variable sulphides-pyrite andpyrrhotite, probably 5-87. overall with sectionsup to 30*.
371.6-372.6 - irregular quartz, minor pyrite380.5-381.0 - "4" quartz (blue) at 385.03" blue quartz veins at 379.5, 392.0 and 398,0
INTERMEDIATE VOLCANIC (ANDESITE)Dark green, fine grained, moderately chloritic,possibly fragmental near 'in' contact with palebrown fragments, Numerous fine quartz-carbonatefilled fractures, Moderately banded at 50* to C. A.near in contact, becomes massive
433.5-435.5 - interbedded magnetite (20*) in severalbands to 1" at 70* to C. A.
475.0-475,6 - CHERTY IRON FORMATION
IRON FORMATIONPale brownish grey chert with occasional narrowbands of magnetite. Chaotically brecciated. Minorquartz veining. Mino:' pyrite, pyrrhotite mainlyin cross-cutting stringers
480.5-481.5 - INTERMEDIATE VOLCANIC, as above
SAMPL
HO
994
995996997998900100C
701702
'Ot I MOM
368.5
373.5378.5383.5388.0393.0397.5
478.0483.0
E
r OOTAOtto
373.!
378.:383.:388.'393. f397.!398.:
483. f485.
101*1
5.0
5.05.04.55.04.51.0
5.02.2
ASSAYSAll
; o; 'o*
.01
.04
.03Tr.08.02.01
TrTr
01 100
DIAMOND DRILL RECORDnot r NC
root ABC
f MOM
ASA. 5
525.3
538.0
.
TO
525.3
538.0
DESCRIPTION
INTERMEDIATE TUFF (ANDESITIC?)as above (398.5-478.2)3" quartz vein at 485.0
487.0-487.7 - CHERT BRECCIA - fine fragmental textureminor pyrrhotite, pyrite.
494.7-496 0, quartz- sulphide zone. Tuffaceous.Crudely banded at 50', Dark greenish grey,chloritic. 257.-307, pyrrhotite, minor pyrite.2" white quartz at in contact.
496.0-530.3, as above (484.5-487.0)
IRON FORMATION, CHERT hINOR MAGNETITEPartly brecciated as beforePale brownish grey. Humorous fine fractures withdisplacement along. Numerous fine quartz veinletn. Minor pyrrhotite, pyrite, probably 3-57, overall.
533.0-535.0 - ANDESITE TUFF, as above
END OF HOLE
j GS-8
SAMPL
MO
703
'04'05'06
till *N
r*ou
A94.7
525.3530.3535.3
(Tv GOLDEN SHADOW- CENTRAL PATRICIA3-4
root'or
TO
i96.0
530.3535.3538.0
tot/
1.3
5.05.02.7
suet T NO. .-. . .?
ASSAYSAU
-.
Tr
TrTrTr
IKmggl n^ I^^^JM^^^^^^
DIAMOND DRILL RECORDNAMI or pnopciirv GOLDEN SHADOW- CENTRAL PATRICIAHOLt NOLOC ATIOI.
GS-83-5 LiNfltn 268 feetclaim 627
L.T.Tunr 3 -r 91 N nr-A.Tn.r 54 4 60 EELEVATION . AZIMUTH "^O DIP 45"
Feb. 16, 1983 Feb. 17 1983• T A D ———————————————————— r IN IBM EO ——————————————————————————————————
r o o T A o e
r* 0 M
0
14.0
125.0
W^
TO
15.0
125.0
211.0
DESCRIPTION
CASING
INTERMEDIATE VOLCANIC
r OOTAOt
268OIP
43"
Medium grey, massive to slightly banded finegrained. Numerous quartz veins to 1". Bandingand veins at variable angles to C. A. generallyapproximately 20*. Numerous water bearingfractures with iron oxide. At 53.0 2" quartzvein.
40.0-109.0, gradual change to darker green, mediumgrained with mottled texture probably representingpartial chloritic alteration (dark green clots)3"-4" quartz veins at 89.6 and 98.0
109.0-125.0, - TUFF? fine grained, grey green. slightlybanded at 10* to C. A. Heavly cnloritized nearlower contact.
IRON FORMATION, mainly cream colored chert withmagnetite. Alternating sections of well
minor
laminated beds at 55'-60" to core and chaotic brecciated sections with chert fragments interlacedby blue grey quartz and sulphides veinlets andstringers. Probably 107. pyrrhotite and pyriteoverall with sections to 3Q7.
152.0-170.0 - well laminated, more magnetite(probably 257.) S-8% pyrrhotite and pyriteshort sections to 307.
with
170.0-178.6, CHERT BRECCIA, as before, less sulphides3-57. overall.
A/IMUTM OOTAOt DIP
NO.
'07
'08'09'10'11'12'13'14'15'16'17'18'19
W' FOOT/FROM
122.0
125.0129.5134.0139.0143.5148.0153.0158,0163.0168.0172.5177.0
fd
125
f — — — — Mn r MO. "-; "T ' -'tnttt no, ... *A JIM UTM
*rM AUKS
T .onoeo BY K. J. Hodge
Gt
.0
129.5134.0139.0143.5148.0153.0158.0163.0168172177181
.0
.5
.0
.5
TOTAL
3.0
4.54.55.04.54.55.05.05.05.04.54.54.5
Au\ t or/ TON
Tr
T r.02.04.03.02T rT rTrT rT rTrT r
07/TON
mmmmmmwmmmmmmmmu
DIAMOND DRILL RECORD NAME Or PWO^EPTY GOLDEN SHADOW-CENTRAL PATRICIA
HOI- f NO ..GS-TJ
FOOTAGE
f ROM
211.0
268.0
)
*,
i-
to
268.0
DESCRIPTION
178.6-211.0 - Well bedded in thin chert-magnetitelaminae, at 60" to C. A. Dragfold at 189.0Scattered sections of heavy chlorite withheavy pyrite and pyrrhotite, up to 3" to 4" in core length.
183.0-184.0 - Quartz rubble, FAULT ZONE in quartzvein.
200.4-200.8 - heavy chlorite with 507. pyrite.
INTERMEDIATE VOLCANIC (ANDESITE)Medium green fine grained, numerous quartz-carbonate veinlets up to 1", generally at lowC. A. (approximately 20')
260-268.0 - Highly sheared and chloritized shearing20" to C. A. Mottled texture due to greenchlorite clots in grey matrix.
END OF HOLE
SAMPL
'JO
720721722723 724725726
Ipf S
f
r*0u
181.5186.0191.0196.0 200.0201.0206.0
h.-5..^
OO . AGE'D
.86.091.096.0100. 0 101.0!06.0111.0
TO f* l
4.55.05.04.0 1.05.05.0
SHEET NO .......r. .
A K\t vst o, ra.
Tr.02T rT r Tr.03T r
[i J TO*
5J Sedimentory Rocks o-Argillite, b-Greywocke
4 J iron Formation o-Magnetite, b-Chert
T"j Mafic Vblcanlcs a- Flows, b- Fragmented
Intermediate Volcanics
o-Flows, b- Frogmentals
l J Felsic Volcanics a-Flows, b-Fragmenfals
Sulphides
Pyrite. . . . . . . . . .Pyrrhotite . Magnetite . . Sphalerite. . . .Chalcopyrite .
Quartz Vein. . . .
Fault . . Intersecting Drill Hole. .
PyPoMagSpCp
Ov
GOLDEN SHADOW RESOURCES INC.
CENTRAL PATRICIA PROPERTY VERTICAL SECTION
D.D.H. GS-83-1Looking Northeast
GEOCANEX LTDTORONTO. CANADA
BY:DATE: NOV. 1963SCALE: L-COODWG. No: GS-18
W *S|
-iivxl
Z
8
GS-83-2
-100*
-200
297'
-300'
-400'
.. 'fe LEGEND- -^ r
f~j Sedimentary Rocks o-Argillite, b-Greywacke
Iron Formationa-Magnetite, b-Chert
T] Mafic \toteanlcs a-Rows, b-Fragmentals
2 j Intermediate Volcanics
o-Flows, b-Fragmentals
T~] Felsic Volcanics o-Flows, b-Fragmentals
Sulphides
Pyrite. . . Pyrrhotite . Magnetite Sphalerite. Chalcopyrite
PyPoMag
SpCp
OvQuartz Vein. . Fault . . . . -V/V Infersecting Drill Hole. . -0-
Au (0Xo) a ijFeet "*
5O IOO fe*t
GOLDEN SHADOW RESOURCES INC.
CENTRAL PATRICIA PROPERTY VERTICAL SECTION
D.D.H. GS-83-2Looking Northeast
GEOCANEX LTD TORONTO. CANADA
BY:DATE: NOV. 1903SCALE: I'SOO
No: G S-19
if
I
-- --05-7^:^5fe I
V) OD O
GS-83-3
Overburden
Py-5-10% Ov
-100'
-200
L28+5OC
2b-10-25 0Xo
4o-250XoMog ' 2b-l00Xo Po
Ov
2 b -Py 25- 4007o C-50
-300'
-400'
'•AV^Mr. :
^:^y^^^^^W^^^
LEGEND
5 l Sedimentary Rocks o-Argillite , b-Grevwacke
4 j Iron Formation o-Magnetite, b-Chert
3 ) Mafic volcanics a-Flows, b- Fragmenrols
2 [ Intermediate Volcanics
o-Flows, b-Frogmentals
Felsic Volcanics o-Flows, b-Fragmentals
Sulphides
Pyrite Pyrrhotite Magnetite . Sphalerite . . . Chalcopyrite
Quartz Vein
FaultIntersecting Drill Hole. .
Au (07o) Feet
PyPoMag
SpCp
Ov
50 IOO
GOLDEN SHADOW RESOURCES INC.
CENTRAL PATRICIA PROPERTY VERTICAL SECTION
D.D.H. GS-83-3Looking East
GEOCANEX LTD TORONTO. CANADA
Bf:DATE: NOV. i*9JSCALE: l'COOOWO. No: 65^20
i.**- ',- ir.-v^-.-
-100
-200'
GS-83-4
S-I35O 33 S. of sect.
4b
-300
4b 3-507oPy,Po
2o
4bPo-25-30%
2b
538 O
-400
LEGEND
Sedimentory Rocks o-Argillite , b-Greywocke
Iron Formationo-Magnetite, b-Chert
j j Mafic \tolconfcs a-Flows, b- Fragmentats
2 [ Intermediate Volcanics
o-Flows, b-Frogmentals
l Felsic Volcanics o-Flows, b-Fragmentals
Sulphides
Pyrite. Pyrrhotite . Magnetite Sphalerite. Chalcopyrite .
Py
Po
Mog
Sp
Cp
OvQuartz Vem
Fault .
Intersecting Drill Hole. . - -
Au (0Xo) c *, Feet
5O
GOLDEN SHADOW RESOURCES INC.
CENTRAL PATRICIA PROPERTY VERTICAL SECTION
D.D.H. GS-83-4Looking North
GEOCANEX LTD TORONTO. CANADA
BY:
DATE: NOV. 11*63SCALE i'6OCOWQ. No. GS^Zl
5j Sedimentary Rocks o-Argillire , b-Greywacke
^ Iron Formation o - Magne tile, b - Cher t
Mafic \tolcanics a-Flows, b- Frogmenfals
[ 2 j Intermediate Volcanics
o-Flows, b-Fragmentals
TJ Felsic Volcanics o-Flows, b-Fragmentals
Sulphides
Pyrite. . F/rrhotite Magnetite . Sphalerite . Chalcopyrite .
PyPoMag
SpCp
OvQuartz VeinKOUlt . . . . -v/v
Intersectmg Drill Hole. . -0-
Au (70) ** Feet
50 IOO
GOUJMM SHAUOV: RESOURCES INC.
CENTRAL PATRICIA PROPERTY VERTICAL SECTION
D.D.H. GS-83-5Looking Northeast
GEOCANEX LTD TORONTO, CANADA
BY:DATE: MOV 1985SCALE: i 600iDwo. NO: GS-22
li
^
-too
-200
-300
-400'
^-::::r"vv
. u r- u
6. SON
6. DON
C
A c
: '-- -y :- '. ,-'-; - -. .'-.---r .'-- "' - - : . - - ' -. . - ' ' - - -
J u
5 st f
T*
1
ss
~- ^ ^
r*,-- -" —r-
r-* r* f
i~- i—
^^- f^****^ r-*
-"-"""^ r* r-'
LEGEND Sutpnidp5
-4j Quortz Porphyry pyr|fe
3 j Volcanics - mafic to intermed- Pyrrhotite . . . .'ate Chalcopyrite . . . .
pi2 Argillite ( in port silicate Iron VJUICMU . . ..
—— l - ,. v Carbonate . . . . . . . .Formation ;
Chlorite . . . . . .1 Iron Formation- oxide and car
- bonote facies and some silicate facies
)uortz Vein . . . . . . . . . . . . . . Qv
-
———— .- , ..-...--••e.^^.sl^gi...... ....,, ,... .^iMii^^^^^HBrtaa^^^^^-^^i^^^V' '--- ;V^--. -.^, ,;.,,- -.--•.••:,,.
S : ^-fS^-;- •v;: ^r^P^;.- : - -. -••^; . : j3 - - ,Vv- - - - - -- -.- ;"' "10. . . : rJ '\ - ,-.. : .':: - ' - ,' : "r -t- /' -
. - - f-"r*
t-"
' rX'
\ S " ^~"-^ cr^"^\ ' -' \ '^^ T'^'
r Tr 83-9^4 — V^^it- -^^.oposed jj^^ f ̂ ^ ..^^\ ̂ S3-e
L 4*r \ .- - .....y jL^vi^r-^ ^-^T ^Wr' ^r\':' - ^--~~~7 ^^-83-4
Proposed -^^j pfe /JflK \"^ ^ 7 ^- :^..l^' /--7 r Tr83-8 ^
^-/" " ** ^-Tr83-7 ^. ^^^^ T* ^ *- ^ "t ' ^ ~k\V v^, , . :, \^, ^ '^ ' lt^^
^^^^ ^ 'i^-V^^^I^X ^ L-Tr 83-10 Y^-\\^v^ ^ lt
\l l
4
,i li— — -
/'/^3^y/"1 ; v/
J~~^~) 10* | —————— —--———- ———— —— ———————————————— ——Trench . . . . . . . . . . . . . f^~s Foliation (inclined, vertical) y^*' .j^ ,~-r^t nPN qwAnow RF^niiRPFc: IMP
Dy ^™* — *-^^ ' ^^ ' VJ V^ L. Lx i- 1 V Ori/^L/V-/ VH (l LO V/ wli V^CO UNO.
. . Po Swamo . . . . . . . . -i- AssuTiec Contact . — ? — OPMTRAI PATRICIA PPOPPDTVJ " r - . - . - - - - - - - - . - - — " V^LN 1 rirtU rM 1 Ml^ir\ r Mvjrt-li 1 Y
Cp pillows ^ AU- AO Geological Mappingriuows. . . . . . . . . . . . . . ^o.. AU Mg ^ ]f. Nn a ,., -, ,, * r f am *. "" and Sampling
C Fault Direction --^ r 0
Cl Fracturing ............XX AREA 1C^vorx/ioxA/Bedding (inclined , tops \y v ̂ i v ITS W
unknown) X X ——————— ————————————
IT i, f i ^r M ? IO 20 30 40 50 crfjSfi DATE NOV. IMS'Fuull (turned, defined) . . ^ " - "KWu GEQCANEX LTD SCALE ,-eoo
^•^ mwl... - - TORONTO, CANADA DWG. No: GS-24
••-•••'•'-•'.•' . i .
'"-ff't-- tt -j-'~^- -f..*•••••••i
3h.
J
*v^
.-;v-
;- ,^-:. V V^*|
LU
8•*-
o to
tu oCO
'K
Z928
293O
t
Trench 83-6—-" -- Proposed Trench
S"
-T -Trench 83-5
y l- 6. 5O N
Trench 83-4•' T- ' -a~ 3
: 3
LEGENDQuartz Porphyry
Volcanics - mafic Jo intermed iate
Argillite (in port silicate Iron Formation )
Iron Formation- oxide and car - boiiofe facies and some silicate facies
Quartz Vein . . . . . . . . . . . . . . Qv
Sulphides
PynTe .Pyrrhotite .ChalcopyriteGalenaCarbonateChlorite
Py PO Cp Gn C
CI
Trench . . . . .
Swamp. . . . . .
Pillows. . . . . .
Fault Direction
Fracturing . . .
so*Foliation (inclined, vertical)
Assumed Contact . . .—7
Au ' Ag Sample No.. "** ' '"
Bedding (inclined, tops unknown). . .
S
s 8 O
metres
Faulf (assumed, defined)
GOLDEN SHADOW RESOURCES INC.
CENTRAL PATRICIA PROPERTYGeological Mapping
and Sampling
AREA 1 East End
GEOCANEX LTD TORONTO, CANADA
QV
DATE NOV. iSCALE iDWG. NO. G ry-2"5
•.V- - .'y —— .-..-^-^ '^m^^^\
00 ID
2925
Trench 83-8
/;M
LEGEND
Quortz Porphyry
Volconics - mofic to intermed iate
Argillite (in part silicate Iron Formation )
Iron Formation- oxide and cor -Donate facies and some silicate facies
. Quartz Vein . . . . . . . . . . . . . . Qv
Sulphides
Pyrite . . . . Pyrrhotite . . Chalcopyrite Galena . Carbonate . Chlorite .
PyPo Cp Gn.C C!
Trench. . . . . .
Swamp. . . . . .
Pillows.
Fault Direction
Fracturing . . .
80*
Foliation (inclined, vertical).
Assumed Contact . . . . . —?
mSample No.
S
Bedding (inclined, tops unknown). . .
O l
metre*
Fault (assumed, defined)
GOLDEN SHADOW RESOURCES INC.
CENTRAL PATRICIA PROPERTYGeological Mapping
and Sampling
AREA 1 Trenches 83-7 -8 -9
GEOCANEX LTD .TORONTO. CANADA
DATE NOV. 1983SCALE:owa No GS-26
|f,:,-
-:^:/
;ii i i i i i i i i i ii i i iiliS-v,:,:.. '-•i^w,1 - -•
••KR?•- •••3'*-^', -,/ ui -;^;--"--... - -.-vaf-.V;
9 ? '1^' s1 ' — — 6. SON
.-••••""" - ^"""^ li"" ~
~~"~ ~~?l '\/''''?'- ^ s ' S - '
^^ py ^ /' ^ j"^. —^ -^ ^- /x , -. o x x- ^ /" -X x X ~/ ' S s . -^ S \ ' s ' i 's' X - ^X / ,—— -. - 7 /OD^ V4^'//saV// 7 M^^
/^ :^-TPO //( U77^/; ) /x -y•-•--.-.........//////^ •- ••....... ..../././^
LEGEND CiilphiH..
3 Volcanics - mafic to intermed- Pyrrhotite . . . . . . . . . Po Swamp. . . . . . . . . . .ia ' e Chalcopyrite . . . . . . . . . . . Cp7 Pillows. . . . . . . . , . .
2 Argillite ( in port silicate Iron a ^n r- c -. n- ,- y . Carbonate . . . .C Fault Direction . . . . .Formation J
Chlorite . . . . . . . . CI Froeturmg . . . . . . . .[ 1 j Iron Formation - oxide and cor
-bonote facies and Bedding (inclined, tops some silicate facies unknown). . .
^ Quart/ Vein . . . . . . . . . Qv Fault (assumed, defmec
, - : : ^;-;^' r ^ •....-•. -:/-- . :- - .- :.' - - . - - ---.v--: .••-:-..'..- -•;'-:-;v:"^^^'
•' - " . ' ' --.
^•^LL— "29^--......_ ̂ '9 * * - - - . . . ^
1- V--..^-a- 3932 PO |^— ".j".
x ~~ U---T j,--...X ' -*- " X , W- ?Q^ f --~ 1 i?X /r *^ , 1-04-' l
t- x \i^S"\^ -'
X *- 2934 f 1-7,' ^"-'"— " PV ^ I| -^ .••\ i..- i.--'N ) r* " 2935 t ' -J/ r?^ C.-33J . - - - - . ,.. - - - . . .....\.. . -
/
~Ti — .-' 2936 1
•"•-"" '-'V, If- / if! W)-A-(//yt^i '1J
. . . C-^s Foliotion {inclined, verticol) *** ^ GOLDEN SHADOW RESOURCES INC.
. .. ^ Assumed Contoct .— ? — CENTRAL PATRICIA PROPERTY
AU AQ Geological Mapping. . . ^ Ay Ag sompte No * *. - . ,, ** r' 1"m *. and Sampling
' ' J^ AREA 1o , , , . . Trench 83-1O
^ x . ————————————————— -' ' ' ' ' m*trt* ~?)Xr~ BV:
n eifri^u DATE NOV "MU . . -v.-w W"^ GEOCANEX LTD SCALE i- IOO
'vv" *" " TORONTO. CANADA DWG. NO; 9S-27
: " - ^. - .-^-.
i:\*-*-'SyJ-
"•' V ---i-*^..:-^ ,-jjf, ^ ^
*^..^^,,-y.,,, . -,.,- .,.,. r v..;.-,-:,--:--,:-- , :-^:—— -.v----^--: ? , ^i^.^^-vS-^^ --.*-v: ••^^••-.^^;•^*.^r^^-W,?^A^^r^^^.^^^^
aSgHiM'IB^VK?* -~ ' ''gs^Bifejs-vV'.'-
Pli-:.
II
fi
1
I
1
1
1
1
1t '
P
6'Urn---
ijv'./
K
i^^^jS^^^S^^v*:^' : ;-"-7:^*'^f^jt^^'^%— ': ': ' ; ; - : "' . "\-T'-' ^D-^~^- -- " ' ; .. . - •."•':"
- . ^ ^ - ' ~- - . .
- : .: ''."
LEGENDf~4 | Quartz Porphyry
|3 | Volcanics - mafic to iniate
2 Argillite ( in part silicotFormation )
| 1 Iron Formation - oxide- bonate facsome silicate
• Quartz Vein- - ; v ; " ; :-.'" '- - - 'l'- ' -'•' .-••-'-, ,- -' --••-•" .\ . ,1*'- ' -
" ' . ' ' -' ' - ' " " " ' -^ * - . * -' V " . - ' ^ k ' -- - '-. ' ~ v -- - . -
•iui
Z955
/*: 2956
2954 - .Ol oz/too Au
Bose Line 00
Sulphides
Pyrite . . . . . . . . . . . . . . . . PyPyrrhotite . . . . . . . . . . . . . . . . PoCholcopyrite . . . . . . . . . . . . . CpGolena . . . . . . . . . . . . . . . GnCarbonate. . . . . . . . . . . . . . .CChlorite . . . . . , . . . . . . CI
Trench. . . . . . . . . ^ . . . . .
Swamp. . . .. . .;;:i:.
Pillows. ........ .. .
Fault Direction . ®i. . . . .
Fracturing . . ^.^'^-. . . .' ',!tt---~-' ."- "
Bedding (inclined^ops
Foliation (inclined, vertical).
Assumed Contact . . . . — 7 —
Au " Ag Sample No.. . " -* '' " ,...
f
Fault {assume^?cjeiRned)^vv -V.W, ,.......... -p^,^. ;; - ::vv.
sfeH^'Sls; :..-^pfei^il^SSi!Zl''-'--'
m
o 10 20 3 s
GOLDEN SHADOW RESOURCES INC.
CENTRAL PATRICIA PROPERTYGeological Mapping
and Sampling
AREA 2 North Section
61GEOCANEXLTO
TORONTO. CANADA
BY;DATE: NOV. 19*3SCALE- I'lOOO
•i&N?l-'-'OVt^Vi ^ . v\* i^E, V.-
f^i^^x^^&^i^
^^'^'^^-•'^•.•••'''••^''•^''^^•'^A'^.^'^^-f^^
^Sia^d&^t^^^S^eEif^U^^iHKSiJMi^i'fiW'i^^^
DWG. No: 6 S -28
mm-^3&Zm
-S&asfiiss-
i if*.
i is l l l
2941
2942
2943
Qv,C,CI,Py, Po
^//
-l.50 S
Excovoted oreo
l m:-*t:l
l
l
l
i lssr
^
ste?^;v\-|g^^
LEGEND
4 l Quartz Porphyry
Volcanics - mafic to intermed iate
Argillite (in part silicate Iron Formation )
Sulphides
Pyrite . . . . . . . . . . . . . . . PyPyrrhotite . . . . . . . . . . . . . . . . PoChalcopyrite . . . . . . . . . . . CpGalena . . . . . . . . . . . . . GnCarbonate . . . . . . . . . . . . . . .CChlorite . . . . . . . . . . . . CI
l l iron Formation- oxide and car -bonate facies and some silicate facies
Quartz Vein . . . . . . . . . . . . . . Qv
Trench. . . . . . . . . . . . . .
Swamp. . . . . . . .. .. .. . . j^.
Pillows. . . . . .. . . . . . .. . ^
Fault Direction . . . . . . . . . ±z^
Fracturing . . . . . . , . .. . . /^ S
Foliation (inclined, vertical).
Assumed Contact . . . . . . — \
Au " A9 Sample No.. . f-** - '-y
Bedding (inclined, tops unknown). .. XX
m
O 5 IO 15 2O 25
Fault (assumedt defined) ;.; -;- :.-.^ri^W;c:; v
GOLDEN SHADOW RESOURCES INC.
CiJJTRAL PATRICIA PROPERTYGeological Mapping
and Sampling
AREA 2 Trench 83-2
GEOCANEXLTD TORONTO. CANADA
BY:DATE: MOV.SCALE: K500DWQ. 6S-29
- , j-"*^rv ';" ."""VtV
®tf^*^@)t^^
MAGNETIC READINGS'I 1
7O69
5984
6O7O
2951
295O 25^-
2949 ^-,
2948 *-
Z42I
1164
957
Bockhoe trench
.2947
LEGENDQuortz Porphyry
Volconics - mafic to intermed iate
Argillite (in part silicate Iron Formation )
Iron Formation- oxide and car - bonate facies and some silicate facies
Quortz Vein . . . . . . . . . . . . . . Qv
Sulphides
Pyrite . . . . . . . . . . . . . . PyPyrrhotite . . . . . . . . . . . . . . . PoChalcopyrite . . . . . . . . . . . CpGalena . . . . . . . . . . . . . . GnCarbonate . . . . . . .. . . . . . .CChlorite . . . . . . . . . . . . . CI
Trench. . . . . . . . . . . . .
Swamp. . . . . . . . . .. . .
Pillows. . . . . . . . . . . . .
Fault Direction . .. . . . .
Fracturing . . . . . . . . . .
(C?SO*
Foliation (inclined, vertical).
Assumed Contact . . . — 7
Au-im
Sample No. .
Bedding (inclined,tops unknown):..;.
S
s O 5 10 15 2O 25 m*tr**.•"..v-'-.;'
Fault (assumed, defined) .
GOLDEN SHADOW RESOURCES INC.
CENTRAL PATRICIA PROPERTY Geological Mapping
and Sampling i
AREA 2 Trench 83-3
DATE NOV. 1989
GEOCANEX LTD TORONTO. CANADA Dwa No: GS-3O
•C^g&g^^;^^^
l l l l
fiV'V, -
ElfIK
LEGENDQuartz Porphyry
Volcanics - mafic to intermed iate
Argillite (in port silicate Iron Formation )
Iron Formation- oxide and cor - bonote facies and some silicate facies
Quartz Vein . . . . . . . . . . . . . . Qv
Sulphides
Pyrite . . . . . . . . . . . . . . . . . . PyPyrrhotite . . . . . . . . . . . . . . . . FoChalcopyrite . . . . . . . . . . . . CpGalena . . . . . . . . . . . . . GnCarbonate . . . . . . . . . . . . .CChlorite . . . . . . . . . . . . . . CI
Trench. . . . . .
Swamp. . . . . .
Pillows.
Fault Direction
Froc luring . . .
Foliotion (inclined, vertical).
Assumed Contact . . . . . . .
Au " Ag Sample No.. . L
—?—
m
S
Bedding (inclined,tops unknown)...
O 5 10 15 2O 25
Fault (assumed, defined) ..
GOLDEN SHADOW RESOURCES INC.
CENTRAL PATRICIA PROPERTYGeological Mapping
and Sampling
AREA 3
GEOCANEX LTD TORONTO. CANADA
___
DATE: MOV. I98J SCALE: I-5OO
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LEGEND
Quartz Porphyry
Volconics - mofic to intermed iate
Argillite (in port silicate Iron Formation )
Sulphides
Pyrite . Pyrrhotite Chalcopyrite Galena . , Carbonate. . Chlorite . .
PyPoCpGn-CCI
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Quartz Vein . . . . . . . . . . . - . - Qv
Trench.
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Fault Direction
Fracturing . . .
Foliation (inclined, vertical).
Assumed Contact . . . . . .—7 —
AU " AQ Sample No.. . * -* ' "* ^,,m
Bedding (inclined,tops unknown)^, . XX
012345
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Fault
GOLDEN SHADOW RESOURCES INC.
CENTRAL PATRICIA PROPERTYGeological Mapping
and Sampling
AREA 4 Stripped Section
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