010 CANADIAN OCCIDENTAL PETROLEUM LTD. GEOLOGY AND GEOCHEMISTRY · 2017-01-17 · 010 canadian...
Transcript of 010 CANADIAN OCCIDENTAL PETROLEUM LTD. GEOLOGY AND GEOCHEMISTRY · 2017-01-17 · 010 canadian...
010
CANADIAN OCCIDENTAL PETROLEUM LTD.
MINERALS DIVISION
GEOLOGY AND GEOCHEMISTRY
OF THE
SANDY 'ZAHAVY 1 CLAIM TRENCHES
SANDY LAKE BELT
NORTHWESTERN ONTARIO
6 MINING CLAIMS
NO. KRL 614679-614684
CLAIM SHEET M3016 - RAHILL LAKE
RECEIVEDJAH 101983
MINING LANDS SECTION
BY:
F.W. GITTINGS, HON. B.Sc,
COVERING WORK COMPLETED DURING OCTOBER 1982
oQ
Q
TABLE OF CONTENTS PAGE
1. SUMMARY AND RECOMMENDATIONS...................... l
2. INTRODUCTION.................................. . . . 22.1 Location and Access.......................... 22.2 Previous Work................................ 4
3. WORK COMPLETED 19823.1 Trenching.................................... 63.2 Sampling and Analyses........................ 63.3 Petrography.................................. 63.4 Magnetic Susceptibility Survey............... 7
4. GEOLOGY.................... . ................ . . . . . 74.1 General Geology.............................. 74.2 Geology of the Sandy 'Zahavy 1 Claims......... 84.3 Geology of the Trenches...................... 9
4.3.1 Trench SAN-82-Z-T1 (Plan 1)........... 94.3.2 Trench SAN-82-Z-T2 (Plan 2) ...........11
4 .4 Rock Geochemistry........................... 11
5. CONCLUSIONS.............. . ..............,.. . . . . . . 12
6. REFERENCES.......... . . . . . . . . . . . . ......... . . . . . . . . 13
LIST OF TABLES
Table l Analyses on Zahavy Rocks.................... 62 Table of Rock Units......................... 7a
LIST OF FIGURES
Figure l Index Map................................... 32 Location of Zahavy Claims................... 53 Geology and Trench Locations................10
APPENDICES
Appendix I Analytical Results........................14II Thin Section Descriptions.................17
III List of Personnel......................... 28
PLANS (In Back Pocket)
Plan l Geology, Geochemistry and Magnetic SusceptibilityTrench SAN-82-Z-Tl
2 Geology, Geochemistry and Magnetic Susceptibility Trench SAN-82-Z-T2
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1. SUMMARY AND RECOMMENDATIONS
Two trenches totalling 12.0 m in length were
blasted out across a shear zone with carbonate veins and a
small otucrop of iron formation located on the northern tip
of a small island near where, in 1946, Berens River Gold
Mines discovered gold bearing quartz veins.
Trench^ SAN-82-Z-T1 exposed a shear zone with
minor quartz-carbonate veins in a diabase dyke in contact
with a dacitic dyke or sill. In trench SAN-82-Z-T2 metasediments,
including iron formation, in contact with mafic metavolcanics
are exposed. Shearing is evident in phyllite along the contact
between the metasediments and the metavolcanics.
The trenches were chip sampled at a 0.25 m inteval.
All samples were analysed for gold, silver and arsenic. One
of the 40 samples contains 450 ppb Au. Generally the results
were diappointing.
The area surrounding the trenches has not been
sufficiently mapped for the writer to make a realistic
appraisal of the potential of the claim group as a whole,
however the iron formation and quartz veins tested do not
indicate a high potential for iron formation host gold deposits.
Further mapping is recommended.
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2. INTRODUCTION
The Sandy 'Zahavy 1 Claims are part of an option
agreement with Zahavy Mines Ltd. All six claims in the claim
group are contiguous and are presently held by Canadian
Occidental Petroleum Ltd. of 180 Attwell Drive, 4th Floor,
Rexdale, Ontario, M9W 6A9.
The claims were staked by Zahavy Mines Ltd. to
cover the area in which a 1946 drill intersection containing
gold bearing quartz veins is reported.
Two trenches were blasted. One across a small
outcrop of iron formation and the other across the contact
between mafic volcanic and a dacitic sill to investigate the
gold potential of these rock types.
This report presents the results of the trenching
work and is submitted on behalf of Canadian Occidental Petroleum
Ltd., the holders of the claims.
2.1 LOGat ion and Acce s s
The Sandy 'Zahavy 1 Claims are located on Sandy Lake
225 km north of Red Lake in northwestern Ontario (N.T.S. map
sheet 53/F/3). The Zahavy claims are in the Red Lake Mining
District of Kenora (see Figures l and 2).
The native settlement of Sandy Lake is located 20 km
west of the claims. There are bi-weekly scheduled flights from
Winnipeg to Sandy Lake by Air-Dale as well as scheduled flights
from Thunder Bay and Pickle Lake.
Canadian Occidental chartered a float equipped Beaver
from Green Airways in Red Lake for transportation to the work
area from a base camp 10 km west of the claims.
"^f- Favourable Lake M one Site
Northwestern Ontario Index Map
LOCATION OFCANADIANOXY PROJECTS
SANDY CLAIMS
Figure lNTS. 528,52N,520,53A , 538, 53C.53F, 53G, 53H
O
Legend
- ' Poved road
—— Grovel roodTown
* Indian settlement
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Highway 808, a new all weather road from Pickle Lake
to Windigo Lake comes within 50 miles of the properties to the
southeast. Winter haulage roads have been used in the past to
transport heavy equipment and supplies into the area.
Getty Mines Ltd. is presently undertaking development
work at the old Favourable Lake Mine 32 km southwest of the
claims. If the mine is brought into production there is a
possibility that an all weather road will be extended into the
area and provide direct road transportation to the south
(see Figure 1).
2.2 Previous Work
In 1938 Berens River Gold Mines drilled four holes
on their "Island Prospect". One hole intersected 0.98 oz/ton
Au over 0.3 feet and another intersected 0.76 oz/ton Au over
3.1 feet. Both intersections were in quartz veins. These drill
holes are believed to be located on the northern tip of the island
trenched in 1982 but no trace was found to indicate their
original collar locations.
In January 1982 ground magnetics and VLF-EM surveys
were conducted for Canadian Occidental Petroleum Ltd. over
the Zahavy Claims. The north-south survey lines are 100 m apart
with stations picketed at 20 m intervals along the lines. Results
from this survey are reported in "Report on Ground Magnetic
and VLF-EM Surveys, Grid A and Zahavy Grid; Patricia Portion,
District of Kenora, Northwestern Ontario", by F.L. Jagodits, 1982.
KEY MAP stole : 1 inch to 200 mite*
Fimire 2
PROJECT SANDY
North Western Ontario
N.T.S 53 C B 53 F
LOCATION MAPScol*: l'250,000 Figjre
CANADIAN OCCIDENTAL PETROLEUM LT!MinefoH Diyiiion Hov 82
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3. WORK COMPLETED
3.1 Trenching
Two trenches totalling 12.0 m in length were blasted
out. The blast holes were drilled out using two pluggers,"an
Atlas Copco and a Wacker. The four-man crew spent one day,
October 10, 1982, drilling, blasting, mucking, mapping and
sampling the trenches.
3.2 Sampling and Analyses
A total of 40 channel chip samples were collected.
The sample interval was 0.25 m. All samples were analysed for
gold, silver and arsenic. Analyses were done in Ottawa by
Bondar-Clegg Ltd. The elements analysed, methods used and the
lower detection limits are listed in Table 1. Analytical
results are shown graphically on Plans l and 2, and listed by
sample number in Appendix I.
TABLE l
ANALYSES ON ZAHAVY ROCKS
Lower No. of Element Dectection Limit Extraction Method Samples
Au 5 ppb Aqua Regia Fire Assay AA 40As 2 ppm Nitric Pet- Colourimetric 40
rochloric Digestion
Ag 0.1 ppm HN0 3 -HC1 Atomic Absorption 40hot extr.
3.3 Petrographic Analysis
A total of 6 rock specimens were thin sectioned by
Geoplastech in Toronto and sent to Dr. S. Boutcher of St. Vital,
Manitoba for petrographic analyses. Her reports are in
Appendix II.
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3.4 Magnetic Susceptibility Survey
A magnetic susceptibility survey was conducted along
each trench. Readings were taken on a 0.25 ra interval. The
survey was undertaken to determine the actual magnetic strength
of the various rock types. These observations will be used
in the future be enabling a comparison between the actual
magnetic properties of known rock types to the data received
from the ground magnetic survey. The results of this comparison
will aid in the interpretation of magnetic units not exposed and
provide a better understanding of the distribution of iron
formations underlying the claim block.
The instrument used was a Scintrex SM-5. Results of the
surveys are shown graphically on each plan of the trenches.
4. GEOLOGY
4.1 Gene ral Ge ology
This belt was first mapped in 1938 at a scale of
l inch to l mile (1:63,360) by Satterly (1938), and was later
included in a regional, l inch to 2 mile reconnaissance survey
(Bennett and Riley, Operation Lingman Lake 1969). Data
collected during the Bennett et al. (1969) survey was insufficient
to modify Satterly's interpretation.
"The underlying bedrock of the area is entirely
Precambrian in age. Throughout the region a heavy drift-mantle
of Pleistocene age overlies the bedrock with a maximum thickness
of 50 feet. Much of the drift is varved clay laid down in a
post-glacial lake; towards the east end of Sandy Lake the drift
consists of sand and boulders as well as clay.
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TABLE 2
TABLE OF ROCK UNITS
Unit Description
Quartz-feldspar Porphyry Massive, light grey-green rock with sparse quartz and abundant feldspar phenocrysts set in a very fine grained groundmass.
Diabase Massive, medium grained dark green rock with an ophitic texture. Strongly altered with uralitic amphibole after pyroxene and chlorite and epidote after plagioclase laths.
Iron Formation Alternating bands rich in magnetite/ quartz and chlorite, hornblende and plagio clase.
Phyllite Light green, finely laminated with orientated flakes of chlorite biotite and sericite.
Basalt Massive, dark green, altered to tremolite and chlorite.
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The Sandy Lake Belt is about 50 miles long and has a
maximum width of about 10 to 15 miles. Mafic to intermediate
volcanics which have undergone metamorphism to greenschist and
almandine amphibolite facies make up 80 to 90% of the belt.
The remainder of the belt is felsic to intermediate metavolcanics,
metasediments, and metagabbro" (Satterly, 1938).
4.2 Geology of the Sandy 'Zahavy* Claims
The geological information over the Zahavy Grid is
taken from Satterly 1 s map (1938). Along the shore of Sandy Lake
and the inland andesite is shown to occur together with quartz
stringers near the tip of the peninsula, which is covered by the
1982 geophysical grid. Amphibolite (part of the metavolcanic
sequence) was mapped on the small island in the southern part of
the grid. Porphyry dyke f quartz veins are shown at the southeast
tip of the island and it is noted that a rhyolite dyke is
indicated at the northern tip of this small island.
The exact location of the four holes drilled in 1946
is not known, but records would imply, that they are located on
the northern tip of the small island. Two of the holes
intersected gold bearing quartz veins associated with pyrite,
little pyrrhotite and chalcopyrite. The host rocks are
described as "fine grained greenstone andesite, coarse grained
siliceous andesite, very basic greenstone and diorite".
In his 1982 report, F. Jagodits compiled a geological
map using information from Satterly's report as well as
interpretation of the ground geophysical data. Figure 3
represents this geological interpretation. It shows three
major units underlying the claims block: 1) Unit l - Iron
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Formation, characterized by large-amplitude magnetic anomalies;
2) Unit 2 - Mafic Volcanics, linear magnetic anomalies within
these units are believed to be more magnetic horizons within
the mafic volcanic stratigraphy; 3) Unit 3 - Felsic to
intermediate volcanics, characterized by gentle magnetic
gradients.
In Figure 3, a discontinuous magnetic horizon 2-1,
2-2 and 2-3 is shown. Jagodits stated that these magnetic
horizons probably represent a single unit disrupted by faulting.
This magnetic unit appears to lie immediately below the
contact between the mafic and felsic volcanic units. Trenching
done on the Zahavy grid shows that 1) the disruption in the
magnetic unit is due to the intrusion of dacitic and diabase
dykes and 2) there are at least minor amounts of iron formation
in the mafic volcanics which are reflected in the magnetic
anomalies.
4.3 Geology of Trenches
4.3.1 SAN-82-Z-T1 {Plan 1)
This 3.0 m trench was blasted across a sheared contact
between a quartz-feldspar porphyry and a diabase dyke.
The diabase dyke rock is medium grained, with an
ophitic texture. The rock has been extensively altered and
appears quite strongly strained in sample 82-SAN-4003 {see
petrographic reports in Appendix II). The rock is now composed
of uralitic amphibole, chlorite, epidote and remnant plagioclase.
The contact with the quartz-felspar porphyry is sharp.
The quartz-felspar porphyry contains sparse quartz
phenocrysts and very abundant plagioclase phenocrysts set in
an extremely fine grained groundmass. Quartz phenocrysts range
up to l mm in size and are often embayed when viewed in thin
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MAJOR UNITS1 iron formation2 mafic volcanics with magnetite rich horizons3 felsic to intermediate volcanicsSYMBOLS
postulated faull magnetic anomaly
-xx—XX— edge of flat lying conductor— -——- postulated contact
xo: o
CANADIAN OCCIDENTAL PETROLEUM LTD. Minerals Division
PROJECT SANDY ZAHAVY CLAIM GROUPNorth Western Ontario N.T.S. 53 F2
1982 Trench Locations and Major Geological UnitsSCALE- 1=5000
FIGURE 3
FWG/gv/Dec.1982
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section (see Appendix II, sample 82-SAN-4010).
Gold values are at or below the detection level of
5 ppb {see Plan l and Appendix I).
4.3.2 SAN 82-Z-T2 (Plan 2)
This 7.0 m trench was blasted to investigate the
gold potential of the iron formation located at the northern
tip of 'Zahavy Island 1 .
The iron formation exposed in the trench is
interbedded with other metasediments eg. phyllite and argillite
and appears conformable with the overlying and underlying mafic
metavolcanic rocks (see Plan 2).
The bedding strikes west-northwest and is vertical
or steeply dipping to the north. The contact with the overlying
basalt has been strongly sheared (see Plan 2 at 1.0 m). A 3 cm
wide pyrite rich bed occurs at the lower contact with the
underlying mafic metavolcanic amphibolite. Two grab samples
from this pyrite band were anlaysed and contain 60 and 15 ppb Au.
The sheared phyllite along the upper contact contains 450 ppb gold,
The irregular magnetic susceptibility profile of the
metasediment sequence reflects the interbedded nature of the
magnetic oxide facies iron formation with the non-magnetic
argillite and phyllite.
4.4 Rock Geochemistry
Forty samples were collected in the two trenches.
All samples were analysed for gold, silver and arsenic. The
results were disappointingly low.
The highest gold value is 450 ppb in a sheared phyllite
at the top of the metasedimentary sequence in trench Z-T2.
;.-J 4
l
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Silver values were all below the 0.1 ppm detection limit.
Arsenic values ranged from below the detection limit of < 2 ppr to 235 ppm in an interbedded phyllite and iron formation. Th high arsenic value was accompanied by the second highest gold value of 100 ppb. Generally, however, there is no direct correlation between arsenic and gold content of the rock.
5. CONCLUSIONS
The Sandy 'Zahavy 1 Claims where investigated offer a low potential for iron formation hosted gold deposits. No sulphide facies iron formation was located. The small outcrop of oxide iron formation that was located and trenched does not contain economic levels of gold mineralization (the highest go value is 450 ppb).
The quartz-feldspar dyke exposed in trench Z-Tl is dacitic in composition and not the rhyolite dyke reported by Satterly (see section 4.2). The breaks in the iron formation distribution shown in Figure 3 are caused, at least in the are.- investigated, by the intrusion of diabase dykes and quartz- feldspar intrusions. Geophysics proved capable of aiding in the location of the iron formation in trench SAN 82-Z-T2.
Additional mapping should be carried out over the claim group where possible. The area along the southeast tip of the island should be investigated for iron formation
Respectfully submitted,r\Toronto, Ontario
December 1982
F.W. Gittings, Hons. B.Se
AUTHOR'S QUALIFICATIONS
FRED W. GITTINGS
Fred W. Gittings graduated from Brock University, St. Catharines, Ontario, with an Honours Bachelor of Science in geology in 1975.
Since graduation he worked as a mineral exploration geologist with Uranerz Mining and Exploration until joining Canadian Occidental Petroleum Ltd. in November, 1979.
While employed with Canadian,Occidental he has carried out and supervised mineral exploration projects in Saskatchewan, Yukon, and Ontario.
He is currently a member of the Canadian Institute of Mining and Metallurgy.
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6. REFERENCES
jagodits, F.L., 1982: Ground Magnetic and VLF-EMSurveys, Grid A and Zahavy Grid, Patricia Portion, District of Kenora, Northwestern Ontario (53/F); unpublished report for Canadian Occidental Petroleum Ltd.
Leonard, K.W., 1982: Geology and Geochemistry of theSandy Claims, Sandy Lake Belt, Northwestern Ontario; internal report for Canadian Occidental Petroleum Ltd.
Satterly, J., 1938: Sandy Lake Area, Map No. 47F in47th Annual Report, Part 7, Ontario Deptartment of Mines.
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APPENDIX I
ANALYTICAL RESULTS
- 15 -
' BONDAB-CLEGG.^Bxm: (613)237-31 10 EK&JfiiLSa^™-''' *'^'™ -**SM**^Tf kx: 053-4455 mMuwnm* n i.n i.^^^^^^B i. .
[ REPORTS 112-1830 PROJECT? SANDY ROCKS J
1 SAMPLE ELEMENT Cu Zn Hi CoL NUHBER UNITS PPM F'PM PPM PPM
-82-SAN-3036-82-SAN-400182-SAN-400282-SAN-400382-SAN-4004
82-SAN-400582-SAN-400682-SAN-4007B2-SAN-400882-SAN-4009
82-SAN-401082-SAN-401182-SAN-4012
^2-SAN-4013^-SAN-4014
82-SAN-401582-SAN-401682-SAN-401782-SAN-401882-SAN-4019
82-SAN-402082-SAN-402162-SAN-402282-SAN-402382-SAN-4024
82-SAN-402582-SAN-402682-SAN-402782-SAN-402882-SAN-4029
82-SAN-403082-SAN-403182-SAN-403282-SAN-403382-SAN-4034
^^Bk.
WK-SAN-403582-SAH-403682-SAN-403782-SAN-403882-SAN-4039
MPPM
Vft-*——\v. i
O,l
O.IO.I0.1
O.IO.Io.i0.10.1
O.IO.IO.IO.IO.I
O.IO.IO.IO.IO.I
O.IO.IO.IO.IO.I
O.I0.1O.IO.IO.I
O.IO.IO.IO.IO.I
O.IO.IO.IO.IO.I
Asm
*M
\4
3i52
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^^
242
tfQ332
44
23235192
31731
317
33333
4442
51
ri ;*nto"Wlfi^'*ltoivfi^i(it'rt'lii'it'4'iiiJfiiil
| PAGE 7
Au ut/Au NOTESm CM
ff.\J
^o^tf
^^^0^
5^tf^^
5^40
450^
10<5
5100
10
G^^<5^
55^<5O
^<5<5^60
/r.--. - I f, -
Ud.764 Btlfut Ra OtUwi.Onurio
K K, 0/5 :(6I))2J7-JIIO
'dn: 0)34453
BDNDABrCLEGGM Geochemical Lab Report
REPORT: 112-1930 PROJECT: SANDY ROCKS PAGE B
f SAMPLEL ,!1UM?ER
ELEHENT Cu Zn Ni Co Ad As Au wl/AuPPM ™ PPM PPM PP
82-SMH040 10 15
NOTES
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APPENDIX II
THIN SECTION DESCRIPTIONS
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Specimen No. - 82-SAN-4003
Rock name - strained looking ( amphibolitised and chloritised, diabase
Mineralogy - abundant - uralitic amphibolechlorite epidote
moderate amounts - remnant plagioclasesmall amounts - sericite
leucoxene carbonate pyrite - trace
Description - This rock is a medium grained diabase, with an ophitic texture f which has been extensively altered and quite strongly strained, so that it now has a confused looking texture and is largely composed of secondary minerals. However, some of the original plagioclase remains i and enough of the original texture can be distinguished for the original rock type to be clearly established.
The original texture is mainly retained by areas of uralitic amphibole which show almost simultaneous extinction. These are up to about ^ mm across t have irregular outlines i and typically enclose lath shaped crystals of plagioclase (in varying stages of alteration) in an ophitic fashion. These presumably represent the sites of original ophitic pyroxene crystals of medium grain size. These uralitic areas often have a rather cracked appearance, so that they appear to consist of a number of adjacent but slightly disoriented fragments. The amphibole is colourless, and sometimes intermingled with a little carbonate and/or chlorite.
No phenocrysts, or phenocryst pseudomorphs, were included within the area of the thin section. However, the hand specimen contains very occasional, relatively large, compact, light green patches which have the appearance of sparse phenocrysts.
The shearing stress which has affected this rock appears to have been taken up mainly by the altered plagioclase. Therefore, apart from those plagioclase laths which are enclosed by the uralitic amphibole, the altered plagioclase in this rock shows little or no trace of its original texture. It is now composed of a variable mixture of chlorite and finely granular epidote, containing jumbled remnant 'fragments' of plagioclase, which have a typically very highly cracked appearance. Patches of fairly dense, sheaf like, chlorite appear to represent areas of particular strain. The proportion
(continued overleaf)
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82-SAN-^003 - continued
of epidote to chlorite is very variable! and a little sericite is intermingled with these minerals in some places, Small amounts of carbonate are also rather unevenly scattered through the rock. Angular masses of leucoxene, usually of the order of 0.5 mm across, are scattered through the rock probably making up about 5# of it. These probably represent original iron oxides. One irregular crystal of pyrite was also noted within the area of the thin section.
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Specimen No. - 82-SAN-4010
Rock name - strained and sericitised quartz-feldspar porphyry
Mineralogy - phenocrysts
groundmass
plagioclase quartzquartzo-feldspathic material sericite - abundant carbonate ) chlorite ) leucoxene
moderate amountsleucoxene )apatite )very small amountspyrite )
Description - This rock is a porphyry! with sparse quartz phenocrysts and very abundant plagioclase phenocrysts set in an extremely fine grained groundmass. The rock has been strained and altered, with the production of -abundant sericite accompanied by moderate amounts of carbonate and chlorite.
Quartz phenocrysts in this rock are small and sparse. They are up to about l mm in grain size, typically rounded or lobate in outline , and often embayed. They typically have a very highly strained appearance, but are not granulated. Plagioclase phenocrysts, by contrast, are extremely abundant. They range in size up to a maximum of about 3 ram, and grade down into the groundmass. They are only shadowily visible, as they are partially obscured by a finely disseminated covering of secondary sericite intermingled with a little carbonate. Some crystals have a rather cracked appearance, with quartz, sericite, or carbonate filling narrow cracks which run across the crystals. The plagioclase phenocrysts range from subhedral tabular to anhedral in outline.
The groundmass of this rock is extremely fine grained, with a rather streaky and irregular texture. It is composed predominantly of extremely fine grained quartzo-feldspathic material which is too fine grained for individual crystals to be clearly distinguished. This quartzo-feldspathic base contains abundant finely disseminated sericite which makes up around 2 0fo o f the groundmass. The sericite is rather streakily and somewhat unevenly distributed and shows a rather poorly developed preferred orientation. Intermingled rather irregularily with the sericite there is a moderate amount of tiny anhedra of carbonate. Moderate amounts of chlorite are also present, but are mainly restricted to clots and stringers of variable size and shape which are composed virtually entirely of chlorite and leucoxene. One or two of these clots have a form which is suggestive of a possible derivation from a biotite crystal, but most have very irregular outlines and tend to
(continued overleaf)
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8 2-SAN-^-010 - continued
be drawn out within the same direction as the preferred orientation of the sericite. It seems likely that the chloritic clots represent a low proportion of original ferromagnesian material. Leucoxene in this rock is mainly restricted to the chloritic clots, although a few tiny clots do occur in the main part of the groundmass. One or two tiny grains of pyrite were also noted, and there are occasional tiny euhedra and subhedra of apatite scattered through the groundmass.
The thin section is cut across by a narrow fracture zone in which the material is finely granulated. ^e^e there is a dense base of finely granulated material containing angular fragments of the host rock, finely disseminated carbonate, extremely fine grained epidote, and a little patchy chlorite. This zone is about 2 mm wide.
- 22 -
Specimen No. - 82-SAN-^013
Rock name - uralitised basalt
Mineralogy - very abundantabundant small amounts
uralitic amphibole remnant plagioclaseclinozoisitesericitemagnetitecarbonate ) mainlychloritepyriteepidote
) in fractures
Description - This rock is a fine grained i non-porphyritic, basalt which has been pervasively uralitised. The original ferromagnesian material has been completely replaced by uralitic amphibole , while the original plagioclase of the rock remains relatively unaffected by the alteration, and clearly retains the original texture of the rock.
Plagioclase appears to have made up slightly less than 50^ of the original rock. It formed randomly oriented, lath shaped, crystals of rather variable size. These average around 0.25 ram in length, with the maximum being about 0.5 mm. They are relatively fresh with respect to the associated ferromagnesian material, but are partly obscured by secondary minerals. These include marginal invasion by the surrounding uralitic amphibole, and varying proportions o f extremely fine grained clinozoisite, accompanied by some sericite. Some crystals also contain a little patchy chlorite. Some retain traces of compositional zoning, but they are too badly obscured for their composition to be determined.
The plagioclase crystal remnants are surrounded by a mass of shreddy looking uralitic amphibole which completely replaces the original ferromagnesian minerals of the rock. This amphibole is fine grained; occasional optically continuous areas are up to about 0.5 mm across, suggesting that this was probably the maximum grain size of the pre-existing pyroxene. The original rock therefore probably had a doleritic i texture. The amphibole has a pale green colour, and is probably of actinolitic composition.. It contains a moderate amount of small, scattered, inclusions of magnetite. A very little carbonate and chlorite is found scattered throughout the rock.
The thin section is criss crossed by a network of fine fractures. These are marked by a narrow zone composed mainly of a mixture of chlorite and carbonate, along with occasional scattered masses of pyrite. These fractures have rather poorly defined margins in most cases. Other fractures contain a little finely granular epidote, or fine grained feldspar.
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Specimen^No. - 82-SAN-4020
Rock name - finely laminated iron formation, with magnetite-rich, and quartz-rich laminae. The rock is cut by numerous microscopic faults.
Mineralogy - very abundant - quartzabundant - magnetitemoderate amounts - chlorite (in magnetite rich laminae)
small amounts - goetheitecarbonate
Description - This rock is a very finely laminated, and slightly metamorphosed, banded iron formation. It is composed of laminae of quartzite, intercalated with laminae rich in magnetite. The magnetite-rich laminae also contain a moderate amount of quartz and chlorite. Within the area of the thin section the rock is cut by a number of microscopic faults. These are subparallel to each other, and oriented approximately at right angles to the bedding planes of the rock. These faults result in some minor crumpling of the laminae. They typically have offsets of the order of about l mm.
The thin section contains two fairly well defined quartzitic bands 4-5 mm wide, with magnetite rich bands both between and on either side of them. The quartzitic bands are composed essentially df a very fine grained, sutured, mosaic of quartz anhedra of rather variable size, averaging around 0.05 mm. Scattered through this quartzose base there are very occasional tiny patches and crystals of carbonate and, in some places, a few tiny granules of magnetite and flakes of chlorite.
The magnetite rich bands are extremely finely laminated. The laminae are as narrow as 0.02 mm wide, and are distinguished by the varying proportions of magnetite present. All gradations from virtually monomineralic magnetite laminae to the virtually magnetite-free quartzite are present. The magnetite occurs in masses of very tiny compact crystals, usually of the order of 0,01 mm or less in grain size. It is set in a base composed of fine grained quartz, similar to that described from the quartzite band, intermingled with varying amounts of very tiny chlorite flakes. The proportion of chlorite is very variable, from virtually none to laminae in which it is abundant as the associated quartz. The chlorite is a fairly deep green penninitic variety, and forms minute flakes which show a very poorly developed preferred orientation parallel to the bedding of the rock. Where the minor faults cut the magnetite rich bands, segregations of quartz, or chlorite, tend to infill
(continued overleaf)
- 24 -
82-SAN-4020 - continued
some of the faults, while the magnetite-rich bands also contain a number of irregular quartzose and chloritic segregations. Occasional carbonate-rich stringers which run across the quartzite bands, parallel the microscopic faults and probably indicate planes of weakness parallel to them. A little goetheitic material is present in some of the fault planes, and within some of the magnetite-rich bands.
- 25 -
Specimen No. - 82-SAN-4033
Rock name - finely laminated banded iron formation, with chlorite and hornblende-rich bands
Mineralogy - abundant - chloritehornblendemagnetiteplagioclase
moderate amounts - carbonatetraces - pyrrhotite
chalcopyrite epidote
Description - This rock is a banded, magnetite-bearingt iron formation. Within the main bands, which are of the order of 0.5 - l cm thick i the bands:.are themselves very finely laminated. Within the area of the thin section there is one magnetite-rich band, a band composed predominantly of chlorite, and a relatively wide band composed of a mixture of chlorite, hornblende, and plagioclase. The latter band is characterised by a number of cross-cutting cracks and irregular segregations, usually filled by carbonate.
The magnetite-rich band is composed of very fine, rather streaky looking, laminae of magnetite, intermingled with streaks and lenses of fine grained carbonate, and with abase of extremely fine grained chlorite intermingled with some hornblende. A little extremely fine grained feldspathic material is also intermingled with the chlorite and hornblende in some parts of this band. Overall, magnetite probably makes up close to 50^ of this band, with the proportions of other minerals being rather variable.
The predominantly chloritic band makes up the other side of the thin section from the magnetite-rieh.band. It consists predominantly of extremely fine grained, pale green, chlorite which shows a very well developed preferred orientation paralleling the lamination of the rock. Intermingled with the chlorite there is a low proportion of very tiny feldspathic anhedra, and a low proportion of scattered magnetite anhedra, (about 5?0 * Occasional somewhat larger anhedra of deep blue-green hornblende are scattered through the chlorite. These tend to be elongated within the plane of schistosity established by the chlorite. The average grain size in this band, and in the magnetite-rich band, is typically less than 0.02 mm. The chlorite-rich band also contains a low proportion of tiny, scattered, epidote granules.
(continued overleaf).
- 26 -
82-SAN-4033 - continued
The central portion of the thin section is composed of a rather variable, and less clearly laminated, mixture of plagioclase, chlorite and hornblende. The plagioclase occurs in angular 'chips' which are up to about 0.3 mm in grain size and have the appearance of sand-sized detrital grains. These are usually 'pitted 1 by tiny scattered inclusions of chlorite. These grade in size down into the surrounding rock t and are intermingled with abundant irregular anhedra of deep blu-green hornblende of similar size which appear to be randomly oriented. Both minerals are embedded in a base composed of extremely fine grained chlorite and feldspathic debris. This band is characterised by the presence of numerous cracks, most of which are oriented approximately at right angles to the bedding, which are filled by a fine grained carbonate mosaic. In addition, there are a number of irregular, carbonate-filled, segregations within this band as well as spme irregularily disseminated carbonate. Magnetite is almost absent within this band.
PYRITIC METASILTSTONE*
82 SAN - 4040
Offcut :
Crudely banded grey-green to black rock with crystalline aggregates and veins of pyrite. Hard and siliceous gangue. One darker band is quite strongly magnetic.
Mineralogy :
Quite variable, depending upon position in slide.
Quartz 70 0A Av. 0.05 mm (50 micron).Opaques 15&, pyrite; includes disseminated magnetite.Carbonate 103*,Epidote 5#, granular, yellow-green.Chlorite 2 1, Fe/Mg ** 0,5, pale-green.
A carbonate - quartz breccia vein occurs at one end of the slide.
Texture, Structure, Fabric
The rock consists of weakly crenulated bands of chlorite - epidote, sulphide-carbonate and sulphide (pyrite), interbanded with fine grained mosaic quartz. In contrast to SAN 1137, the sulphide is crystalline, and rarely spongy. The nature of the quartz suggests the rock has under gone cataclasis, and this is confirmed by the appearance of the 0.5 cm wide quartz-carbonate vein. This vein is composed of broken fragments of composite quartz with undulose extinction set in a matrix of carbonate. Chlorite (blue-green-purple under X-polars) forms a selvage to the quartz carbonate breccia vein, suggesting a genetic relationship between the two.
* Meta-argillite is also applicable.
- 27 -
Specimen No. - 8 2-SAN-40 38
Rock name - tremolite amphibolite of indeterminate origin
Mineralogy - very abundant - tremolitic amphibole moderate amounts - chloritesmall amounts - plagioclase
leucoxene sericite
Description - This rock is a tremolite amphibolite! with a very confused looking texture and no trace of the original texture to indicate the original nature of the rock t It is composed of a mass of shreddy looking anhedra of tremolite* through which there i s scattered a moderate amount of very irregularily distributed fine grained chlorite. A low proportion of plagioclase is present* in small irregularily shaped anhedra , and there is also a little scattered leucoxene and sericite.
There is no regularity of texture in this rock, or traces of pseudomorphic textures. Tremolite makes up about Q Ofo of the rock. It is a virtually colourless, very fresh looking* mineral which forms irregularily shaped, shreddy looking, masses which are almost optically continuous over areas of around 0.5 mm diameter in many cases. These are intermingled with, and cut across by, patches in which the tremolite is composed of very finely matted, fibrous, crystals. Chlorite occurs, intermingled with the tremolite in a very irregular fashion. In some cases the chlorite is intimately intermingled with the tremolite; in other cases it forms irregular patches of varying size and shape, scattered through the tremolitic material. The chlorite is also virtually colourless, and is almost isotropic.
The plagioclase which is present in this rock is sparse (10-15^), occurs in small roughly equidimensional anhedra, and gives no textural indication of the original rock. The crystals are only sparsely twinned, generally very fresh looking, and are probably of metamorphic origin. They tend to be marginally invaded by needle-like fibres from the 'frayed 1 margins of the adjacent tremolite crystals.
The only other minerals identified in this rock were sericite and leucoxene. Sericite occurs extremely sparsely, in tiny flakes which are irregularily scattered through the tremolite. Leucoxene is somewhat more abundant, forming small compact masses, usually of the order of 0.1 mm across, which are rather irregularily scattered through the tremolite. They often tend to occur in loose aggregates of several masses.
Late stage carbonate veinlets are also present, which are generally oriented perpendicular to the banding.
Alteration :
The crudely banded nature of the euhedral sulphide suggests this sediment contained a primary sulphide component. There is an intimate association of pyrite with carbonate, however, which could imply that the pyrite has formed through re-actions involving ferroan-dolomite and/or siderite during a sulphidation event. Some of the larger non-banded segregations of pyrite certainly suggest this possibility.
Opaques :
White to creamy pyrite is the dominant sulphide present. Some of the sulphide grains are embayed, suggesting the original sulphide was euhedral. At high power magnification numerous small (5-10 micron) inclusions of pale yellow-white chalcopyrite are resolved. Minor grey magnetite is disseminated throughout the slide. No visible arsenopyrite. The Cu assay should be moderate ^100 ppm). One large (l mm) grain of pyrite is observed in a non-pyrite-bearing portion of the slide.
Assay :
15 ppb Au, 10 ppm As.
Interpretation :
A siliceous metasiltstone which has been affected by a dynamic event and flooded by pyrite and carbonate. It is difficult to tell if the pyrite is entirely introduced or has formed through sulphidation of a pre-existing iron-bearing phase.
- 28 -
APPENDIX III
LIST OF PERSONNEL
- 29 -
APPENDIX III
FIELD WORK
Name Title
LIST OF PERSONNEL
Address Dates
Mike Henrick Project Supervisor
Fred Gittings Project Geologist
Art Murdy Project Geologist
John Allard Prospector
FFICE WORK
Sue Allen
S. Annett
F. Gittings
Draftsperson
Typist
Project Geologist
Canadian Occidental Petroleum Ltd. 180 Attwell Drive 4th Floor Rexdale, Ontario M9W 6A9
Same as above
530 John Street Espanola, Ontario POP ICO
Canadian Occidental Petroleum Ltd. 180 Attwell Drive 4th Floor Rexdale, Ontario M9W 6A9
Oct. 10, 1982 (l day)
Same as above
Dec. 9 , 101982(1.5 days)
Dec. 22, 1982 (1.0 day)
Dec. 15, 161982(2 days)
900
100
1983 10 19 2.5336
Mr. Albert Scott RivettMining RecorderMinistry of Natural ResourcesOntario Government BuildingBox 324Red Lake, OntarioPOV 2MO
Dear Sir:
RE: Geological Survey and Assaying Survey on mining claims KRL 614681 it the Area of Rahill Lake
The Geological Survey and Assaying Survey assessment work credits as listed with my Notice of Intent dated September 14, 1983 have been approved as of the above date.
Please Inform the recorded holder of these mining claims and so 1nd1date on your records.
Yours very truly,
E.F. AndersonDirectorLand Management Branch
Whitney Block, Room 6643 Queen's Park Toronto, Ontario Phone:(416)965-1380
D. K1nv1g:mc
End.
cc: Canadian Occidental Petroleum Limited 180 Attwell Drive 4th Floor Rexdale, Ontario M9H 6A9
cc: Resident Geologist Red Lake, Ontario
© Ministry of Technical Assessi Natural .
Resources Work CreditsOntario ^p
men! w*2,5336
Biite Winino Recorder'1 Report of1983 09 14 WQrk ^0' 100
Recorded HolderCANADIAN OCCIDENTAL PETROLEUM LIMITED
Township or AreaRAHILL LAKE AREA
Type of survey and number of Assessment days credit per claim
Geophysical
Ei*ctromeonftic day*
|nrt"C"d pollination ,, , days
nther flays
Section 77 (19) See "Mining Claims Aliened" column
ttpnlngirpl days
fienrhpnrvral days
Man days CI Airborne D
Special provision d Ground CD
G Credits have been reduced because of partial coverage of claims.
O Credits have been reduced because of corrections to work dates and figures of applicant.
Mining Clilmt Atsewed
S736.00 spent on petrographic studies and on assaying samples taken from mining claims KRL 614680, KRL 614683
49 days credit allowed which may be grouped in accordance with Section 76(6) of The Mining Act.
For Mining Recorder use: The work assignment
for each of the above listed two claims is 24.5 days per claim.
Special credits under section 77 (16) for the following mining claims
No credits have been allowed for the following mining claims
l — j not sufficiently covered by the survey l — l Insufficient technical data filed
The Mining Recorder may reduce the above credits if necessary In order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 77(19)—60:
828 (83/6)
/^z\ Ministry ot Technical Assess iVr 1 Natural t i , , ^ . u \Vj Resources Work Credit*Ontario ^B
ment f*'* 2.5336
Dete Mining Recorder'! Report of
1983 09 14 work W 100
Recorded HolderCANADIAN OCCIDENTAL PETROLEUM LIMITED
Township or AreaRAHILL LAKE AREA
'Type of survey and number of
Assessment days credit per claim
Geophysical
Dthor .days
Section 77 (19) Sac "Mining Claims Assessed" column
14Geological . dayi
Geochemical f*ayi
Man days S Airborne tU
Special provision D Ground G)
j~l Credits have been reduced because of partial coverage of claims.
(~1 Credits have been reduced because of corrections to work dates and figures of applicant.
Mining Clelms Attested
KRL 614680 614683
k
Special credits under section 77 (16) for the following mining claims
No credits have been allowed for the following mining claims
I^J not sufficiently covered by the survey l — l Insufficient technical data filed
KRL 614681-82
The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on
each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 77(19)—60:
826 {83/6)
Ministry of NaturalResources
ftario
Yourfile:#100
1983 09 14 Our file: 2.5336
Mr. Albert Scott RivettMining RecorderMinistry of Natural ResourcesOntario Government BuildingBox 324Red Lake, OntarioPOV 2MODear 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 the 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, y^u may then change the work entries on the claim record sheets.
For further information, if required, please contact Mr. F.W. Matthews at 416/965-1380.
Yours very truly,
**\ XXXAnderson Director Land Management Branch
Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1316
^. D. Kinvig:mc
Ends:cc: Canadian Occidental Petroleum Limited
180 Attwell Drive, 4th Floor Rexdale, Ontario M9W 6A9
cc: Mr. G.H. FergusonMining S Lands.Commissioner
845 Toronto, Ontario
Ministryof Notice of Intent NaturalResources for Technical Reports
Ontario
1983 09 14
2.5336/100
An examination of your survey report indicates that the 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 his 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 direct to the Lands Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked will be issued.
846 (82/5)
•Mimstryof Report of WorkNatural ,~ , . , r- , . ,R.. SO , ,r s (Geophysical, Geological,
Geochemicel arid Expenditures)
The Mining
Instructions: Please type or print.— If number of mining claims travers
exceeds space on this form, attach a.li Note: — Only days credits calculated in t
i " Expenditures" section may be enter \tif i n the "Expend. Days Cr." colum
{O — Do not use shaded areas below.Township or Area
, pf o* Sur veyis)
Geological and Chemical Report. . , ...,.Ci?-: m Holder's)
.Canadian. Occidental Petroleum Ltd.. ,. .. , . . . .Address
180 Attwell Drdve, 4th Floor, Rexdale, Ontario M9W 6A9Survey Company 'Date of Survey (~from ^ to)
Day J Mo.J Yr. Day J Mo. ± Y r.
- . .Prospector's Licence No.
T644
Total Miles of line Cut
Ni!r-,t arid Address of Author (of Geo Technical re-port)
-Er.e.d .Gl.t.^ing^,-JL8JI..At.tMaU ..Driv.e^.,JLth Floor, Rexdale,, Ontario M9.W 6A9Credits Requested per^ Each Claim in Columns at r ight M ining^Claims Traversed (List in numerical sequence)Special Provisions
For first survey:
E nter A O d ays. (This includes line cutting)
For e:och additional survey: using the same grid:
Enter ?0 days (for each)
Geophysical
- E lecjromaonetic
- Magrieiometer
- Rediomelric
- Other
Geological
Geochemicel
Days per Claim
a^ Days
Cornpirie reverse side fins' tntet totBl(s) here
Days per Cltim
- r.'c or,f tO'r.t U'
- Radiometric
- Other
Geological
Geocherriicaf
14
Airborne Credits
K'ole: Spt'Cta! precisions Elecirorrt&oneticcredits do not apply ito Ai'borne Surveys, i Magnetometer
Rodiornetric
Days per Claimr —-- —~
Expenditures (excludes power stripping)Type of work Performed Analyses of rock
Eetrographijc _ studies. ^^^ ___ ... ....Performed On Clairn(s)
KRI, 614683 and KRL 614680
iCulalion o~f Expenditure D&ys Credits
l oial T xpt'fto'hures7o;a!
Dt ys Cfediis
. J ^ Q5] ^ f l?-!]Insfuctions
Total Dtys C'triits rriay t-e apjportioned at the claim holder's choice Enter number of (leys credits per claim selected in coljr-iris n \ r ight.
Mining Claim "Pr efix"T Nu mber
.61.4 fi a 2..
Expend. Days Cr.
X-^S
/^NINCjiANDSSEGl
.orDfc..Ho'-ei O' Acem (S'onstu'c) j f'^JyJjydC. J v
ia! number o* rriining ci&ims cc^'Cfed by this
•For'tmice U se Only ] __J'__"
Mining Claim Prefix | Number
RfiCEJVEPOtClB1982
•xpend Days Cr
ON
Nov. ^4/82^ CtJ-tificaticM"! ^''j; | i"'yinQ^Report^c)f Work
l he:eby Certify that l h?v? i personal and intim:-.:e J.noivledge of the f^cts set forth in the Report of VVoik annexed hereto, having performed the work or v . i trif-f.sed sane djririr, ar-.d/or tfler its completion and the annexed report is true.Vsfn.:- and Festal A:ioreT.s of Pt'&on Ce'ti*yirip
Fred Gittings, 180 Attwell Drive, 4th ̂ F
3 se? (si '9)
pete CertNov.
Canadian Occidental Petroleum Ltd.
August 4, 1983
Mr. E.F. AndersonDirector, Land Management BranchMinistry of Natural ResourcesWhitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3
Dear Mr. Anderson:
RECEIVEDAU8 3 i tgf-j
M1N.NG LANDS SECT.ow
Re: Your File 2.5336Mining Claims KRL 614681
____in the Area of Rahill Lake
I enclose the following as requested in your letter of August 4, 1983:
(1) Geological maps, in duplicate, entitled "Project Sandy Zahavy Option" signed and dated by F.W. Gittings*
(2) Resume of F.W. Gittings, (3) Verification of Expenditures.
I trust the above is satisfactory.
Thank you.
i Yours truly,;' \ ' ' ( '
CANADIAN OCCIDENTAL PETROLEUM LTD.
RJE/sa
Enclosure
R.J. Evans Administration Manager
Minerals Division — 1BO Attwell Drive, 4th Floor, Rexdale, Ontario M9W BA9 [416] B75-S31S Telex O6-9B9493
BDNDAR-CLEGG S. COMPANY LTD,
764 BELFAST ROAD. O^TTA,Yy.A1 ONTARiO, K1G OZ5
/y:'~ Fr-fH";..*-.!^fa -^".J/^D -
PHONE: S37-311O
August 16, 1983
Canadian Occidental Petroleum Limited 180 Attwell Drive 4th Floor Rexdale, Ontario M9W 6A9
Attention: Mr. R. Evans
Dear Mr. Evans
In a recent telephone discussion with Mr. Art Murdy of your firm, he had requested that we provide written confirmation that the invoices submitted with the Bondar-Clegg reports 112-1795, 112-1830 and 112-1872 had been paid.
We are confirming that full payment has been received for the following invoices, which correspond to the reports mentioned above
Invoice No.
101378
101429
101430
101464
101474
101536
Copies of these invoices are attached.
Report No.
112-1795
112-1795
112-1830
112-1830
112-1872
112-1872
Amount
959.09
660.00
1,420.95
2,599.25
1,392.99
882.00
Yours truly
WHITEHORSE VANCOUVER OTTAWA CAMPBELLTON
. ff , , u - -Jf*
i M D AFt .- C L b Gi G SL C CD NC *-V\ NY LTD .
BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455
U*HHl)lttHl .H. 01l H') M! IWKl.l MR,1IH H.OUKkhXMMt.br
UHITK.I)
Hw t 112-
SnHOY KOCKS
l 3 'j
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110
u(
t.*t-bub 1 1." 1. 1.1 1
fct
tfl
wf C KUBHrPULVtKnE -200 Hublolfal
Hi VCfc* J l eJllt'UUi t'lltf Ci']
IflYUJlCl'
u'.? * w* \
vo.ov vo f ov
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f y y v, o 9
THIS IS A PROFESSIONAL SERVICE
y. CLEGG "&L UUfV^HANY LTD.BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455
PKTKUU.UMr , H, on mm*1 HO H! M4bU lib., H H KLMOR
.r UHIAK10J1VU
l O H 30
U-1 Huv(-*liibttf O'j?
Hoi 312-1830
KOCKii
tin t.* j v* vi ul fei l'/orM11 e* i V li v le O l t. u L* tt l t
. V l . l .mil/'Jl yv-'-.'i w| t ui'f*-'r HI i tit l y s t? is o|' Hit'f.ul
frU'V uf 3! i l H: ir'lblul ail
u P ffi -* r* t ion ii*iHrlt,'fe wf C
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fivt
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321'10
6-1 y, 20
*t 2. 7li 772.73
TH/S IS A PROFESSIONAL SERVICEFM 1C U/LJCM DB
BDNDAT^CLEGG S. CDf\PANY LTD.ROAD, OTTAWA, ONTARIO, K1G 025 PHONE: 237-3110 TELEX: 053-4455
H OlTIDEMIVit PETROLEUM DMITEJJF. w, aimJ80 AnNELL liH FLOUR
P* Iff t Hov^wbcT JO r
Rtipoi'l Mot 112-1830
ProJvcl* SAHDY ROCKS
ut
Ahflwt't
l. o*, w l
Atf**v
)iivoice*
00
THIS IS A PROFESSIONAL SERVICE
^ J3Lji\lDAt:'-LJLbGG fc* CJUTCHANY LID.
BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455
PETKOUUH L J II] Tt:. J)F. w, nrm now160 MllMfLt OK, 41 H r LO UK
Tuvoic^J 101
UatoJ MovofcUer 12r
t Hot 112-1072
J J) 7 A n a l ve w* of Si lv'12 I'll l tf Jl V ft V* t til l .'ut'di t
•J '^ An 41 y* w tt o f' Oui'py rl'2 fiMfrlufci'fc el HlcKi*!
• t. l, VOvi O * VO*l OtVOtt 0,90
27V*30 3X, BO 37 )8037,80
I-?'1 *iiij*Jvwei wl' Ai-itMii' •J* 23477.7 1/.
117 Swl i UMut CKUSHrPUU'EKIZC
Sub lo l s? l*l 2175
Total
118 ( 2f 118,29 11B i 29
H3V2.VV
THfS (S A PROFESSIONAL SERVICEniiP u/uPM
BDNOA1( /CLEGG Su LJLJh("PANY LID.
ELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455
InvoKtft
CAHAU1AH OCCII'E.HTAl f'ETROLEUli 11 MI IE f*
l ,W, CUTTINGS ISO ATIHEU TiRi '1TH FLOOF'
3f J 902
Wot
1 'T'' of Ool'J - Fire A .00 PR.** .00
Total
THIS IS A PROFESSIONAL SERVICEtlJLJCh.1
CDIX3RAN "Y LTD ,H- Ja
BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455
101 -12ViiH ULTJDkMlHt
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11 H H.UMK
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lift 4 l
THfS IS A PROFESSIONAL SERVICE Af!f;nnMT.Q mie VA/UCKJ
Ministryof GeotechnicalSees Report
Ontario Approval
File
Mining Lands Comments
MC ((.f t (i -"'.r'
To: Geophysics
Comments
l | Approved | | Wish to see again with correctionsDate Signature
To: Geology - Expenditures A'ff,Comments
Dj Approved [ | Wish to see again with corrections
one t
Tim W ?I ' 3Signature
To: Geochemistry
Comments
[^Approved Q Wish to see again with correctionsDate Signature
To: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)
1593 (81/10)
August 4, 1803 2.5336
Canadian Occidental Petroleum United 180 Attwell Drive, 4th Floor Rexdale, Ontario H9U 6A9Attention: Fred GUtlngs
Dear Sirs:RE: Data submitted for Assaying and Sampling credits
on Mining Claims KRL 614681 1n the Area of Rahill Lake.
Returned herein are two geological plans (1n duplicate) lor the above mentioned survey. Please sign all copies of the maps.
Also, please submit signed receipts or cancelled cheques (1n duplicate) as verification of expenditures claimed.
When submitting this Information, please quote File No.2.5336.
For further Information please contact Mr. F.W. Matthews at 416/965-1380.
Yours very truly,
E.F. AndersonDirectorLand Management Branch
Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1380
S. Hurst:sc
Ends:cc: Mining Recorder
Red Lake, Ontario
10019830204 2.5336
Mining RecorderMinistry of Natural ResourcesOntario Government BuildingBox 324Red Lake, OntarioPOV 2MO
Dear Sir:
We have received data for Assaying and Sampling Credits submitted under Section 77(19) of the Mining Act R.S.O. 1980 for Mining Claims KRL 614681 et al 1n the Area of Rahill Lake.
This material will be examined and assessed and a statement of assessment work credits will be Issued.Yours very truly,
E.F. AndersonDirectorLand Management Branch
Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1380
DU: se
cc: Canadian Occidental Petroleum Limited Rexdale, Ontario
Assessment Work Breakdown
f/irri Days arc based on eight (8) hour Techmcal or Line-cutting days. Technical days include work performed by consultants, draftsmen, etc..
Geological and Geocjiemical ReportL
r ••~"""""| f-'—i - f—————i r- L...4..__l X LZJ ~ L .28__l * L
1 (.cS-.ic Days
Ttc^r^Crt' Days Line- cutting C'td.ts D?yi Tote 1 Credits
No. o) Cis irm
Days per- r 14
^"ic-al D?ys C.-ec-i is
Line-cuttingDpys Totalcivil x IID * E
r::::Da yshnical Days Credits
Line-cutlinp Days
x CUD
No. ofClaims
_
Days per C'eim
No. of DP.vs per Claims C'aim
Techr.lcal t.-^.'rcsl Deys
IV I'D x H^ i:;;::;]Line-culting
Days Total CreditsNo. of Claims
Days per C.a'm
- czi
t^J J'—— -ri'-———'
S3NIW
O3)isnwsawn y
l^r ^^^ca^L^^0^of Work ~*--v*-*^^j ,-'- '.-''J"- C S.
Instructions — Supply required date on a separate form for each type o' work u be recorded (see table below).Fei- GecMsthr.ir.;. 1 nn-r us* 'o-m no. "36? "Report of Work (Geolop.c* 1 Gf c .physics', Geoci-.emicBl and Expenditures)".
Canadian Occidental Petroleum Ltd,180 Attvell Drive, 4th Floor, Rexdale, Ontario M9VJ 6A9 i-~ —— ..-.....--- . —-_..--___ ,,- __ --... -_ _._,___._ ..,™.--—._________Sumniary di IVo'k F'erio: rr.ance fcnd Distr iS.iution of Credits
; Prosriecio' s Licence No.
. -T6 4 4 . . . ...
Requited Infoirnation eg: type of equipment, Names, Addresses, etc. (See Table below)
Tele 1 Work Days C '. r :s rned
12
*-.c -K. :C'.f-:k or. f only)
Q f.'aruEi Work
other L felt ' s \\'C*r k
[^Ccm.f.r fir.;-:: Air, o 1 , herF'cnvf cinttT or r 1 -t : Li- rncf f ::L' ip-
L J DioriiDrio c.' ether Core drilling
M:nir.p ClaimF'l f f i > i K' j rnt .fr
i
KRL ' 614681
614682i
Work DE ys. C'.
6
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—
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D? v-s Cr.
-- -- -
Work Performed on Claims: KRL 614683 -^.G.^. c
KRL 614680 — ̂,. SKr . -̂ C, .rquipment: l Atlas Copco Plugger
l hocker Plugcer
Men: Fred Gittings ) Canadian Occidental Petroleum Ltd.Mike Henrick ) 180 Attv.'ell Drive, 4th FloorArt Murdy ) Rexdale, Ontario M9W 6A9
^ RECElVtU
1 6 IQfi?
MINING LANDS SECTION
John Allard, John Street, Espanola, Ontario
Date: 9 hours on October 10/82
1A-^ x A ^ul"b"iT\T"" l
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Certification Verifying Rt-|.)Oit of Workl htreby ct-rtif^ tritl i h;; ve c f e -t. c-rife! end intiniaU Kno-.vlt'Cipe of the "f 6 cis s e-1 forth in the Rtpyrt o"f \Vork a nnexed hereto, h aving p e'"f orrned thf- wor or vv i t n e:-. E. e. d sa-Tit1 ouririp s^sd/or t f K" ilb conip'eiior, and the annexed report i s true.
't-."iE fcrid PC-RI&! AddrpE.t of Person CeMtlytripFred Gittj--- "i sn Rtt- Drive, 4th Floor, Rexdale, Ontario M9W 6A9id b y ( Sipr,
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SAN-Z-T1
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RED L A K ':f;.!NIS'o DiV.El K CP P ~ '
FOV 101382A.M.
K O Z
CANADIAN OCCIDENTAL PETROLEUM LTD. Minerols Division
PROJECT SANDY ZAHAVY CLAIM GROUPNorth Western Ontario N.T.S. 53 F2
I982 TRENCH LOCATIONSSCALE- );5000
FWG/gv/Nov. I982
Sand
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Area
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Canadian Occidental Petroleum Ltd.
January 7, 1983
Mr . Fred Matthews Mining Administrator Ministry of Natural Resources Mining Land Section Whitney Block, Room 6452 Queen's Park Toronto , Ontario M7A 1A2
1 f) ^983
,^ r INNING LANDS
Dear Mr. Matthews:
Please find enclosed duplicate copies of geology and geochemical reports for five separate claim groups in the Sandy Lake area (Sandy A, B, C West, C East and Zahavy).
Attached to each set of reports is a copy of the report of work forms sent to Scott Rivett, Mining Recorder in Red Lake, Along with report of work forms I have included a breakdown of costs for each claim block and proof of payment for the lapidary and petrographic work. Repeated requests to Bondar-Clegg for a statement of payment has failed to generate one, although they have promised a statement in the mail. In lieu of this statement I have used a copy of the original invoices.
I hope this will suffice. If there are any problems please call me immediately.
Yours truly,
CANADIAN OCCIDENTAL PETROLEUM LTD.
RJErer
Enclosures
Via McLean Courier
R. J. Evans Administration Manager
Minerals Division — 1BO Attwell Drive, 4th Floor, Rexdale, Ontario M9W 6A9 [41 B] 675-2312 Telex O6-9B9493
SANDY 'ZAHAVY' CLAIMS
STATEMENT OF EXPENDITURES
Petrology: Dr. Boutcher $ 120.00Geoplastech 50.00 (invoice 204)
Thin sectioning: Geoplastech 86.22
Analyses: Bondar-Clegg Ltd.40 Ag, As, Au 556.00
TOTAL EXPENDITURES S 8 12.22
Natural Resources
f W,' k,^r -31-f O f Instructions Supply itiqunt-ci detff on a separate form for t ncti
type of work to be recorded (see table below). 1 ' For Geo-iechnita' work use form no. 13G?"Rfpon
of Work (Geological. Geophysical, Geochtrrrncai ond Expenditures)".
180 Attwell Drive, 4th Floor, Rexdale, Ontario M9W 6A9Summary of Work Performance and Distribution of Qea'itsTotal Work Days C', claimed
121or Performance of the following
[ J Manual Work
QShaft Sinking Drifting orother Lateral Work.
[2 Compressed Air, otherPower driven or mechanical equip.
[ _ |PoAer Stripping
J _ | Diamond or other Core drilling
[ _ J Land Survey
NPrefix
LKBL...
lining ClaimNumber
6146816.14682
WorkDays Cr.
6-6.. .
r.Prefix
ining ClaimNumber
WorkDays Cr,
r.Prefix
lining ClaimNumber
,
W or rDays Cr.
Required Information eg: type of equipment, Names, Addiesses, etc. (See Table below)
Work Performed on Claims: KRL 614683
KRL 614680 Equipment: l Atlas Copco Plugger
-q . G G CW/.S
Men: Fred Gittings ) Canadian Occidental Petroleum Ltd.Mike Henrick ) 180 Attwell Drive,Art Murdy ) Rexdale
John Allard, John Street
Date: 9 hours on October 10/82a fi v A i^ ,i^fVct** A Hr k^vAvN i -^ . 1 ^ ^......—— - f^) Jflti—— r,. ————— ,..., —— \ d. CT.C**1
•^ i
4th Floor, Ontario M9W 6A9
, Espanola,ifFrT'T*
;.'.ijj!NG r.r|"x r. r it ( i [v L: (u L M
Ontario l
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j6ete "oT'Rep'brt
Nov. 4/82R-
__ . __ _ . . ———— —'jT^Tr^ t A K Ev "'i*' c ;V; f r*-'..^..V,-'^ J
1 - ^ L * 1 1
' - i - i ' -' ' O ',0 10-11 i- - ' "
A
^E corde6 Ho!rier*6r ^Apeni jE ^niu.ft)
-vuf UJ Jbt/Jox"l tiereby certify that l have t personal and intimate knowledge of the facts set forth in me Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.
Name end Postal Address of Person CertifyingFred Gittings, 180 Attwell Drive, 4th Floor, Rexdale, Ontario M9W 6A9
Date Certified
Nov. 4/82(Signature)
Table of Information/Attachments Required by the Mining Recorder
Type of Work Specific information per type Other information (Common to 2 or more Types) Attachments
l.'onua! Work
Stiaft Sinking, Drifting or O'.r.fcr Lbttral V^ork
NilNames and addresses of men who performed manual work/opereied equipment, together with cates and hours of employment.
Coi-.prcivtrf t'.r, o'her power C'uen or n i; '.tnicd! equip.
Type of equipment
Fo.'.er SlippingTyf'e of equipment ancf amount expenc^ecf. Note: Pioof of actual COM mutt be submitted
Work Sketch: tKtse are required 10 ^^.c>^^ the locetior, a r. o txttnl of work in relation to the neatest clfc'iro pt)S\.
CANADIAN OCCIDENTAL PETROLEUM LTD. Minerals DivisionPROJECT SANDY ZAHAVY CLAIM GROUPNorth Western Ontario N.T.S. 53 F2
1982 TRENCH LOCATIONSSCALE- 1'5000
Sw rf!
^ St. Germain Street, Winnipeg,
Mani toba R2M 4N3
20^-255-17^1 December 30th 1982
To Whom It May Concern -
This is to certify that, during the fall of 1982, I produced petrographic descriptions of 16 rock samples from the Horseshoe claim property and ^-9 rock samples from the Sandy claim property. These were delivered to Canadian Occidental Petroleum Ltd., Minerals Division. I received payment of $320,00 for the Horseshoe reports i and $980.00 for the Sandy reports, from Canadian Occidental Petroleum Ltd.
Sheila M.A. Boutcher Ph.D.
SHEILA M.A. BOUTCHER, Ph.D. Petrologist
Phone:(204)255-174134 St. Germain Street,
Winnipeg, ManitobaR2M 4N3
ins.
COPY
212 King St. West Suite 100 Toronto, Ontario M5H 1K6 596-0381/82
INVOICENo. 1 72Terms:Payable upon receipt
SERVICES RENDERED TO:Canadian Occidental Petroleum Limited 4th Floor 180 Attwell Drive Rexdale, Ontario
.'tsr.v-r^i ,','i.-r i -.i--:--'tv^'^^.-.4--^.-^: .•v-: ;; :.:.- ;,'v-vi;^i;::':;v/
'^'^tft^VJf --55^-:*?,--••V 'iiXli'^V''-'-''-.'-'':-.';
f^ Date: Nov 19/82- ,.' : Quan.
;tfr; Ordered
fi "
p 2
H 46Ipi
^
H|lg] ————
Shipped Via:Description
Your Order No.: Gittings J
thin sections (could not section 82-SAN-2086)
polished thin sections
minimum charge cuts
shipping to Dr.
8MM paid to ^ Geoplastech Inc.
^jJJjoujtcher . St. Vital Man.
fvtn, Ckd. By ____ . ————— 1
p. ,'- rM. r-- - _ 1
1.-'.
receivfr -' 0 V S t i r' ' A' 1 '^' J
' ———— . (^\J^\ red with thanks. KJv \———— \
Total
Quan. Shipped
52
2
54
Unit Price
7.75
18.00
2.00
tAmount (
iftP
403.00 f L
36.00 Ii
96.00 i
112.85 t
1
S547.85
1
COPY
212 King St. West Suite 100 Toronto, Ontario M5H 1K5 596-0381/82
INVOICENo. 204Terms:Payable upon receipt
'^•^•,:'',-''^'':'^^SERVICES RENDERED TO
Canadian Occidental Petroleum Limited 4th floor - 180 Attwell Drive Rexdale, Ontario
•-f.' 1-.-'
-/•v^:- ;s-;-^.i-. - f. i'.'^Vi ̂ ,i ^•^••^•'^3
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^ D ate: Jan 3/ 83Ouan.
;. Ordered
3
J 24i
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Shipped Via:Description
Your Order No.: Sittings ^
polished thin section interpretations
im nairl to Rpnnlastprh Inr.
—
Exfn. Ckd. By
Rec'g. Ckd. D-—— D AT r: — Rr;c'D. ——
JAN -5 1983* -
PfiEEi ft Terms Ghd. ryj ..^^^ -
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rprp-iupri with thanlcc /^iTotal
Ouan. Shipped
2
2
Unit Price
50.00
Amount'f'. '.' '
100.00
Sioo.oo——————————
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BONDAR-CLEGG S. COMPANY LTD.
BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: 053-4455
CANADIAN OCCIDENTAL PETROLEUM LIMITEDF.w, SITTINGS180 'ATTWELL DR.4TH FLOORREXDALEf ONTARIO,H9W 6A9
Invoice:
Patei Moveu.ber lOr 1982
Report Not 112-1630
Pi-oJectJ SANDY ROCKSi ^ c ^,-^Uc.
281 Analyses of Gold - Fire Astaw &1 Subtotal
281 An*lwtt6fc of Arfc&nic m i
Invoice? Total.
of Subtotal
6.00 1686.00 1A86.00 1686.00
913,23
THIS IS A PROFESSIONAL SERVICE ACCOUNTS DUE WHEN RENDERED
BQNDAR-CLEGG S COMPANY LTD.BELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-3110 TELEX: Q53-4455
CANADIAN OCCIDENTAL PETROLEUM LIMITEDP.W* CUTTINGS180 ATTUELL DR,4TH FLUORRfc'XDALEi ONTARIO iM9W AA?
Invoice} 101430
Date} November 05* 1982
Report No J U2-1830
P coJoe t J SANDY ROCKS)
28132363623
281
Art*? 1 wiitffcAnalysesAn* lute*Analv&esAna? lyses
Le PreporSamples
of Silverof Cobaltof Copperof Nickelof Zinc -iBut' total
, iat ionof CRUSHfPULVERIZE -200Subtotal
Invoice Total
atatatsteft
oft
10000
2
,vo.90t 90.90,90
,75
S3328323220
A4t*
772772
,90.80*40,40.70.20
.73,7S
648,20
772*73
11420,95
THIS IS A PROFESSIONAL SERVICE ACCOUNTS DUE WHEN RENDERED
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rROCK GEOCHEMISTRY PROFILES
i Ag As Au . ppm ppm ppb
i ; "JO -i "lOOO -, 500-1
7 -
4 -
3 -
900 -
600 -
700 -
600 -
500 -
400 -
300 ~
EOO-
100 -
O O J
400-
300-
200-
100 -
MAGNETIC SUSCEPTIBILITY PROFILE;
"310 cgs units
SAMPLE NUMBERSCO Nl l
QUARTZ FELDSPAR PORPHYRY
SAN 82-Z-T1
FWO/sa/Nov. 1082
eio
i L12GENDl , ' l r l . : - -
It* i Iron formationpo ; pyrrhotitePY ; pyrite \cp i chalcopyriteqv : quartz vein
Outline of outcrop in trench
Told with plunge direction 4* -t- Anticlinal* Synclinal axis " i^ with plunge direction
Bedding (vertical, inclined showing dip)
S ̂ Schistosity (vertical, r Y inclined showing dip)
*w Shear Zone
Geological Contact f i (defined, assumed)
CANADIAN OCCIDENTAL PETROLEUM LTD minerals division
l PROJECT SANDYZahavy Option
! North Western Ontario N.T.S. 53 F/2
ROCK GEOCHEMISTRY PROFILES
Ag As ppm
10 i 1000 -i 500 -
MAGNETIC SUSCEPTIBILITY PROFILE
•PH*3
10 cgs units
SAMPLE NUMBERS s 8 eo o o o o
(RONFORMATION
SANQY
LAKE:Quartz-calcite
veinlels in PHYLLITE with minor Iron Formation
AMPHIBOLITE
Grab Sample 4039 Au - 60 ppb Ag-O.lppm As - 51 ppm
3cm wide py rich bedfractured Iron Format ion
Grab Sample 4040 Au-15ppb Ag-O.I ppm As- 10 ppm
IFpopy cp qv
i
S*9 X/
y?r /
'j LEGEND
Iron Formationpyrrhotitepyritechalcopyritequartz vein
Outline of outcrop in trench
Fold with plunge direction Anticlinal, Synclinal axis with plunge direction
Bedding (vertical, inclined showing dip)
Schistosity (vertical , inclined showing dip)
shear Zone
l Geological Contact j (defined, assumed)
CANADIAN OCCIDENTAL PETROLEUM LTD.
{minerals division PROJECT SANDYi Zahavy Option
North Western OntarioN.T.S. 53 F/2i
SAN 82-Z-T2
cale 1:
50 100 15pm
PLAN 2 FWG/sa/Nov. 1 982