rpt on geol mapping litho samp & pros n ......amikama lake and access was gained to the property...

53BMSE800I 010

REPORT ON

GEOLOGICAL MAPPING, LITHOGEOCHEMICAL SAMPLING,

AND PROSPECTING

ON THE

NORTH CARIBOU RIVER PROPERTY

DISTRICT OF KENORA, PATRICIA MINING DIVISION

NORTHWESTERN ONTARIO

FOR

GOLDEN TANAGER RESOURCES LTD.

RECEIVED

J'W " 5 1989

August, 1988 E.D. Timoshenko, B.Se.

TABLE OF CONTENTS

l.O SUMMARY l

2.0 INTRODUCTION 3

3.0 PROPERTY DESCRIPTION 3

4.0 LOCATION, ACCESS AND SERVICES 5

5.0 PHYSIOGRAPHY AND VEGETATION 6

6.0 PREVIOUS WORK 7

7.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION 8

7.1 Regional Geology 87.2 Economic Mineralization 10

8.0 PROPERTY GEOLOGY 12

8.1 General Geology 128.2 Structure 13

8.3 Lithologies 14

8.4 Metamorphism 169.0 SUMMARY OF GEOPHYSICS 17

9.1 Magnetics 17

9.2 VLF-EM 17

10.0 DESCRIPTION OF PROGRAM 18

11.0 DISCUSSION OF RESULTS 20

12.0 CONCLUSION 23

13.0 RECOMMENDATIONS 23

14.0 ESTIMATED COST OF RECOMMENDED PROGRAM 24

15.0 REFERENCES 25

APPENDICES

A. CERTIFICATE OF QUALIFICATION (Back of Report)

B. ROCK SAMPLE DESCRIPTIONS AND ANALYSES (Back of Report)

C. ANALYTICAL CERTIFICATES (Back of Report)

LIST OF FIGURES

NO. l - LOCATION MAP 2

NO. 2 - CLAIM SKETCH 4

NO. 3 - PROPERTY LOCATION AND REGIONAL GEOLOGY 9

NO. 4 - DETAIL AREA 1. 19

LIST OF DRAWINGS

NO. l-A GEOLOGY (In map pocket)

NO. l-B GEOLOGY (In map pocket)

l. O SUMMARY

The North Caribou River property of Golden Tanager Resources

Ltd. covers an extensive area of predominantly volcanic and

intrusive rocks belonging to a lithologic sequence known as the Agutua Arm Metavolcanics. The property is situated on

the North Caribou River east of Agutua Arm, approximately 115 miles north-northwest of Pickle Lake, Ontario.

Anomalous gold values were encountered in several areas of

the property during the surface geological exploration program. Area l yielded six values between 111-330 ppb gold

from a highly sheared iron formation as well as several

anomalous values up to 157 ppb from associated sheared

volcanics. Area 2 yielded a value of 402 ppb gold from a brecciated quartz-feldspar porphyry and mafic flow which has a matrix of iron-stained, sulphide-bearing quartz. Area 3

yielded several values from mafic and felsic volcanics ranging from 114 to 1047 ppb gold.

A two-phase exploration program is recommended to further outline gold-bearing horizons on the property. Phase I

consists of prospecting and channel sampling over favourable areas outlined in the present program. Phase II would

involve 3,000 feet of diamond drilling to test geological

targets outlined in Phase I as well as several prominent

geophysical targets. The estimated cost of the program

totals 5156,000.

- 2 -

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NORTH CARIBOU RIVERPROPERTY

Patricia M.D., Ontario

LOCATION MAP

SCALE: f* tOOmiDATE: SEPT. 68

BY: H.H./K.T.MFIG. No.. 1

- 3 -

2.0 INTRODUCTION

The North Caribou River property of Golden Tanager Resources Ltd. comprises 84 claims which straddle the North Caribou River east of Agutua Arm, approximately 115 miles north- northwest of Pickle Lake, Ontario (Figure No. 1).

The following report describes the results of a geological/ geochemical surface exploration program conducted on the property during July and August of 1988. The program consisted of geologic mapping at a scale of l inch to 400 feet, outcrop stripping, detail mapping, prospecting, and lithogeochemical sampling.

The project was conducted by Geocanex Ltd. of Toronto, Ontario. A five-man crew consisting of three geologists and two assistants were on site between July 14th and August 17th, 1988. They included the following personnel:

B. Elliott Geologist/Party Chief Oshawa, Ont.E. Timoshenko Geologist Brampton, Ont.J. Drew Geologist North Bay, Ont.K. Wright Geological Field Asst. Scarborough, Ont.S. Necan Field Assistant Osnaburgh, Ont.

3.0 PROPERTY DESCRIPTION

The North Caribou River property consists of 84 contiguous, unpatented mining claims. These are recorded on the Ontario Ministry of Natural Resources Keeyask Lake (G-2085) and Randall Lake (G-2182) claim sheets of the Patricia Mining Division, District of Kenora (Figure No. 2).

The claim numbers and recording dates are as follows:

- k -

y^rrinno mo 1 (/w

9I 0 07'

1008102'1007940 1007939 I008IIS '100811411007892 ! 1007891

--4-—4-—4- — -l—— +J.1007948 I00794|J 1007938 1008116 ' l008llsLl007893

1007947.1007942 .1007937 1006117

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I008I04 X11007945? (007944 1007935 |007897 1007896 1007867

----—h--I00804ol|00804ll 1006057 'I008058 1 1007962 '1007

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108032 j lOOBOSsl 10060361 1008039 1008042] 1006056 j 1008059 1007961 1007984 100798

^^

1008037 008038 1008043 1008085 10080601007960 1(007965 ,t0079eeL

_ —l _ _ j _ _ j _. i __ _ l __ _ j — —-

006045].OOe044J.OOe054JI00806l] 1007979 "007986 . l007987

008046 1006051 1008033 |I007977|I007978

l—————^ ———— H————— i—————l

-52 05l'

l-^n

0-5 l mile


NORTH CARIBOU RIVERPROPERTY


CLAIM SKETCH

OEOCANEX LTD TORONTO. CANADA

BY: RT. M.—— DATE SEPT. 88'

PIG. No:

- 5 -

Claim Numbers Recording Date

Pa 1007887 to 1007898 (inclusive) 12 September 29th, 1987

Pa 1007935 to 1007948 (inclusive) 14

Pa 1007977 to 1007993 (inclusive) 17 "

Pa 1008032 to 1008061 (inclusive) 30 " " "

Pa 1008102 to 1008104 (inclusive) 3

Pa 1008112 to 1008119 (inclusive) 8

84 claims

The claims are currently held by Golden Tanager Resources Ltd, Suite 1003-34 King Street East, Toronto, Ontario,M5C 1E5.

4.0 LOCATION, ACCESS AND SERVICES

The property is located in Northwestern Ontario (Latitude 52 c 53', Longitude 91" 08') approximately 115 miles north- northwest of the town of Pickle Lake and nine miles east of

the Weagamow Lake Indian Reserve. The claim block straddles a two-mile long segment of the North Caribou River east of Agutua Arm. A widening of the river extends into the northeast corner of the property and is known as Pakiagama Lake.

Given the low water conditions encountered it was evident that both the North Caribou River and Pakiagama Lake would not be able to safely accommodate float planes. Fixed wing aircraft would be able to land in these areas under higher water conditions or on the ice in the winter months. During the project the Geocanex base camp was located on Eyap- amikama Lake and access was gained to the property via a

portage into Pakiagama Lake.

- 6 -

An all-weather gravel road from Pickle Lake to Windigo Lake (Highway 808) ends approximately 25 miles south of the property. A winter road extending from Windigo Lake to Weagamow Lake is open between January and April and passes within five miles of the property.

Groceries, building materials, and general mining and exploration supplies may be obtained in Pickle Lake, a mining and transportation center with a population of approximately 350. Highway 599, a paved all-weather road, connects Pickle Lake to the CNR line at Savant Lake, 90 miles to the south, and to the Trans Canada Highway at Ignace, 180 miles to the south.

5.0 PHYSIOGRAPHY AND VEGETATION

Surficially, about 50% of the property is covered by well drained, dissected sand and boulder plain with interspersed moraine and drumlinoid deposits. Topographic lineaments trend roughly northeast-southwest. The higher ground is usually covered by mature forests of spruce, poplar, jackpine and balsam.

Low lying areas of swamp and muskeg with black spruce and tamarack forests cover approximately 301 of the property. Rivers and lakes cover an additional 151 of the total area.

Outcrop is exposed on S-5% of the property and is usually mantled by sandy overburden.

l l l l l l l l l l l l l l l l l l l

6.0 PREVIOUS WORK

The following is a chronological description of previous work on the property area.

1938 The Ontario Geological Survey mapped the area at a scale of one inch to one mile under the supervision of Dr. J. Satterly (Satterly, 1939).

1959 The Ontario Geological Survey/Geological Survey of Canada conducted airborne magnetic surveys in the area as part of a systematic aeromagnetic coverage of the province of Ontario (Map 909G., Weagamow Lake Area ODM-GSC 1960).

1967 Pyrotex Mining and Exploration discovered gold- copper-silver mineralization on the shore of Agutua Arm immediately to the west of the property.

1979 The Ontario Geological Survey re-mapped the area (Thurston, et al., 1979).

1984 Moss Resources Ltd. acquired the adjacent property covering the Pyrotex gold-copper-silver prospect. The Ontario Geological Survey conducted a multi-disciplinary program of airborne geophysical surveys, bedrock and surficial geological mapping over the area (Bartlett, et al., 1985; maps 80726, 80727) .

1985- Geocanex Ltd., on behalf of Moss Resources Ltd., and 1987 Oracle Resources Ltd., carried out ground magnetic

and VLF-EM surveys, detailed geological mapping, prospecting, lithogeochemical sampling and diamond

drilling on the adjacent Agutua Arm property to the

east and north. During the same period Moss Resources Ltd. and Power Explorations Inc. carried out a similar program on the Randall Lake property, immediately adjacent to the south and east. (North, 1985, 1987; Hodge, 1985; Elliot, 1987).

7.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION

7.l Regional Geology

The North Caribou River property is located in the

northwestern portion of the North Caribou Lake greenstone belt, located within the Sachigo Sub- province, a part of the Canadian Shield.

The North Caribou Lake belt is an arcuate, horn shaped assemblage of metavolcanic and metasedimentary rocks extending from Weagamow Lake in the northwest to

Opapimiskan Lake in the southeast. South of Opapi

miskan Lake the belt bifurcates into two major lobes; one extending south through Libert Lake, the other

east through the Porester-Neawagank Lakes area (Fig. No. 3).

The mapping of Satterly (1939) and Thurston (1971)

suggests that the volcanic-sedimentary complex has been folded into a gross synclinal or basinal structure, with dominantly clastic metasedimentary

rocks occupying the core of the syncline. The fold

axis of the syncline is approximately coincident with Eyapimikama Lake. The metasediments are underlain by

OPAPIMISKAN LAKE

Metavolcanic rocks

2 ~" Metasedimentary rocks

Iron formation

Gold occurrenceProperty

, aV^"- iGOLD, DISCOVERY

\ SNOPPY LAKE \DEPOSIT

MUSSELWHITE DEPOSITS

l TANAGER RESOURCES LTD.

!TH CARIBOU RIVER

tricia M. D, /Ontario

DPERTY LOCATION REGIONAL GEOLOGY

DATE: SEPT. 88 SCALE r*4milesGEOCANEX LTD

TORONTO. CANADA

- 10 -

the somewhat older volcanics of the system, dominantly mafic in character with lesser ultramafic components.

Two fairly continuous bands of iron formation and chemical sediments mark the contact between volcanics

and sediments throughout most of the belt.

Regional geologic maps indicate that the belt is

bounded by paragneiss and migmatized rock in the north

and by felsic intrusives in the west and south (O.G.S.

Map P. 2834, Eyapimikama Lake Area).

Metamorphic grades in the belt range from upper

greenschist to middle amphibolite facies.

7.2 Economic Mineralization

Gold is the principal metal of economic interest in the North Caribou Lake greenstone belt. Numerous gold showings have been located, generally in spatial association with iron formation.

Two closely associated gold deposits on the Musel- white property of the consortium led by Placer-Dome Inc. consist of several stratabound zones within highly folded iron formation. The deposits, known as the West Anticline and East Bay Syncline Zones, are two miles apart, located on the south shore of Opap imiskan Lake. The gold-bearing zones are concentrated in the noses of parasitic folds within garnet-horn- blende-chert-grunerite iron formation. The majority of gold occurs as stratabound zones of disseminated mineralization within pyrrhotite. A second and much smaller proportion of the mineralization is in quartz- pyrrhotite veinlets occupying dilated portions of the dominant axial planar cleavage (82) associated with the second major folding event


- 11 -

Surface drilling has delineated 6 million tons of 0.2

oz. per ton of gold in the East Bay Syncline Zone

(Northern Miner, Nov. 23, 1987). Published reserves

for the West Anticline Zone are over 3.2 million tons

grading 0.17 oz. per ton gold.

The Power Explorations' Opapimiskan Lake and Karl-

Zeemel Lake properties, which adjoin Musselwhite to

the north and southwest respectively, have encountered

numerous significant gold intersections within iron formation.

Several occurrences of gold are found in other

sections of the belt. In the northwest, a few gold showings have been partially explored. Northern

Dynasty Exploration's Arseno Lake prospect has yielded significant gold and base metal values. Power

Explorations have found several significant gold

bearing zones from a section of the North Caribou

River Fault. The Agutua Arm and Teal prospects consist of gold-silver mineralization in sulfide-

bearing quartz-carbonate veins in sheared mafic

metavolcanics.

Significant gold has also been discovered in the

southeastern section of the belt. In the Sage Lake

area, Inco Ltd. has encountered significant gold in quartz veins and iron formation. Northwest of Wesley

Lake, Tex U.S. Oil and Gas intersected gold mineral

ization in quartz-arsenopyrite-carbonate veins in sheared gabbro.

- 12 -

8.0 PROPERTY GEOLOGY

8.1 General Geology

The entire North Caribou River property is underlain by volcanic and intrusive rocks of the Agutua Arm

Volcanic Sequence which is recognized as being the

oldest lithologic package in the area (Bartlett,

et al., 1985). The sequence is unconformably overlain by the Keeyask Lake Metavolcanics and Metasediments

east of the property area; the southern boundary of

the sequence is marked by the North Caribou River

Fault, south of the property (the regionally extensive

South Rim Metavolcanics occur south of the fault).

The sequence is bounded on the north and west by the Weagamow Batholith.

The Agutua Arm Metavolcanics consist mainly of massive

mafic flows. Along with amphibolites, massive mafic

flows are the most common rock types encountered on

the property. A major intercalation of intermediate

to felsic pyroclastic/volcaniclastic rocks within the

Agutua Arm Metavolcanics is interpreted by the OGS to

cross the north property area. However, this could

not be confirmed due to a lack of outcrop exposure in that area. The intermediate volcanics that were

observed on the property are mostly massive flows,

gradational into mafic volcanics. Felsic volcanics

occur sporadically and also appear to be massive

flows. The volcanics have been intruded by numerous

small stocks, sills, and dykes of felsic to inter-

- 13 -

mediate composition (mostly diorite with less frequent trondhjemite, tonalite, grandodiorite, and quartz- feldspar porphyry). Small gabbrioc sills also occur in several areas. Intrusive activity may be responsible for the high metamorphic grade often observed in the volcanics and also for obliterating and/or over-printing any regional foliations present in the older volcanics. With the exception of shear zones and some intrusive contacts, foliated rock is relatively uncommon on the property.

Clastic sediments were not found on the property. An occurrence of oxide facies iron formation in the central property area was the only example of a chemical sediment found during the project. This is described in more detail in Section 11.0.

8.2 Structure

As mentioned, most of the rocks on the property are massive, and only rarely display primary structures, penetrative fabrics, or folding. Foliated rock is for the most part limited to shear zones and some intrusive contacts.

The closest major structures to the property are the North Caribou River Fault and the Center Lake Splay, both occurring on the adjacent Randall Lake property of Moss Resources Ltd. The most common shearing and foliation directions on the property are roughly parallel with the North Caribou Fault, and dextral fault which trends between 60-70". Other less

- 14 -

frequent shear directions are possibly related to intrusive activity. Dips are generally steep and south facing.

Numerous small shear zones are found on the property which are typically 2-5 feet wide. They display weak to moderate carbonatization and silicification and locally abundant quartz-ankerite veining. Sulphide mineralization is generally minor but typically consists of disseminated pyrite with lesser arsenopyrite and chalcopyrite. Ductile deformation, manifested by strongly foliated and crenulated rock, is most prominent although brecciated sections often occur within the shear zones.

8.3 Lithologies

The following is a description of the rock types observed on the property.

i) Volcanics

Several varieties of mafic volcanics occur on the property. The most common are massive flows

which are typically dark green, fine to medium grained, amphibole-plagioclas j chlorite ^ quartz assemblages. They are often silicified along intrusive contacts. Massive, medium grained amphibolites (amphibole-plagioclase- quartz) are also very common and may be mafic flows of higher metamorphic grade. However, they could not be reliably distinguished from coarse grained flow centers or mafic intrusives; the field classification of these rocks is

- 15 -

therefore subjective. Further stripping to determine contact relationships in conjunction with petrographic studies would aid in the clasification of these rocks. The same problem was encountered and documented by Thurston et al (1979, p.71).

Sporadic occurrences of brecciated mafic volcanics were encountered in the central property area (north of the baseline between lines 4+OOW and 24+OOW) and appear to be pyroclastic in nature.

Fine to medium grained, greyish-green intermediate flows are frequently intercalated with the mafic volcanics; contacts are often

gradational. Minor laminated tuffs and porphyritic flows were also observed.

Small lenses, pods, and dikes of massive, fine grained, felsic volcanic flows occur sporad ically on the property. These are usually light greyish-green in colour with a light grey or

buff coloured weathered surface.

i i ) Intrusive Rocks

Diorite is the most common intrusive rock on the property, occurring in dikes and sills from a

few inches to several tens of feet across. Less common are granodiorite and tonalite which occur mainly in the west end of the property (closer to the Weagamow Batholith). Thin dikelets of

trondhjemite are common throughout both

intrusive and volcanic rocks.

- 16 -

Intrusive breccias composed of highly angular blocks of mafic flows and amphiobolite within a matrix of diorite or grandiorite occur at several locations on the property (e.g. near 22+OOW, 20+OON, and 34+OOE, 19+OON).

Small bodies of dense, dark green, medium to coarse grained, magnetite bearing gabbro occur at various locations on the property (e.g. northeast property area near line 56+OOE, 40+OON). These units have strong magnetic signatures.

iii) Chemical Sediments

An oxide facies iron formation was observed in the vicinity of 4+50E, 19+50N. This is

described in detail later in the report.

8.4 Metamorphism

Metamorphic grade on the North Caribou River property varies from upper greenschist to middle amphibolite. Metamorphic isograds could not be delineated. Some areas of increased chlorite,sericite and epidote concentrations exist in sheared volcanics suggesting possible retrograde metamorphism.

- 17 -

9.0 SUMMARY OF GEOPHYSICS

9.1 Magnetics

The property is marked by numerous, relatively discontinuous magnetic anomalies up to 5000 gammas

trending generally east-northeast. These probably represent either lean iron formation (e.g. magnetic high adjacent to Detail Area #1) or magnetite-rich gabbroic intrusives (e.g. northeast property area).

The possibility exists, however, that some of the magnetic highs could be associated with pyrrhotite-

rich sulphide mineralization within recessively weathered shear zones.

In some cases the magnetic features appear to be

slightly offset possibly due to folding or en echelon patterns of the sulphide zones.

Broader areas of magnetic high readings reflect areas

of mafic to intermediate (gabbro/diorite) intrusives.

9.2 VLF-EM

There are numerous zones of conductivity which cross the property on the same trend as the magnetic

features. However, for the most part, there is poor correlation between conductive zones and magnetic features. In some cases there is a direct correlation with magnetic highs, in others conductors flank

magnetic highs.


- 18 -

An explanation for this poor correlation is that many

of the conductors are surficial and not bedrock.

However a number of those conductors which have a

broad correlation with magnetic highs are probably

caused by sulphide mineralization and possibly with

associated shearing. A number of conductors with no

magnetic correlation could be caused by non-magnetic

sulphides, also with associated shearing.

10.0 DESCRIPTION OF PROGRAM

Geologic mapping at a scale of one inch to 400 feet was

conducted along a cut picket line grid. Two principal and

five subsidiary baselines have been cut on the property, all

trending 057 6 . Perpendicular cross lines are cut at 400

foot intervals along the baselines.

Additional prospecting was caried out over geophysical

anomalies and areas of high outcrop intensity.

A total of 243 samples were obtained from outcrops during

the present program. This includes 178 grab samples, 57

channel samples and 8 chip samples. Samples were collected

to test features of potential economic interest such as

shear zones, quartz and/or carbonate veins, gossan zones,

subvolcanic intrusives, chemical sediments, and sulphide-

bearing rocks.

Detail Area No. l was stripped using a high pressure Wajax

fire pump and channel sampled using a portable Stihl rock

saw. A well exposed quartz-ankerite vein occurring at

3+50W, 10+OOS was also channel sampled.

- 19 -2E 4 c-

55

5O28-'3 !2 X 5029-13

5030-14

5026-155027-11

14897-32

r-2C M

Spruce, pop'ar, Jack Dme ; Ba'sann

on Sand 8f Bot'lders

5018-65019-10(7)5020-3305021-S8

5005- !05006-!65007-525008-635009-25

5015-75016-305017-324

Possible Fold Nose (plunge-32-HOO0 ?)

5002-815003-875004-13

14898-17 14963-1214964-57

14960- 1814961-1114962-18

14965-202 5001- 1255014-G

5013-495012-31 50H-Ml 5O'O- !54 (

14959-39 14953-26 14957-66sn,cc,onk,py ;

coy,aspy4887-25

4955-16 14954-15214885-284

'4806-45 14950-29(20)14951- 1014952-1414953-29

'4888 - 14889-'l

5024-315025-13 5023-28

5022-42

GOLDEN TANAGER RESOURCES INC

NORTH CARIBOURIVER PROPERTY


Spruce ± "~arra rack Muskea DETAIL AREA 1

GEOCANEX LTD TORONTO. CANADA

OLOGY WA, D - Shset B -. D wg. No. 1

- 20 -

l

iSamples were sent to Accurassay Laboratories of Pickle Lake (preparation) and Kirkland Lake (analysis). Samples were analyzed using standard fire assay and atomic absorption spectroscopy techniques with a lower detection limit of 5 ppb gold.

Sample descriptions and analytical results are listed in Appendix B and are shown on the property geology and detailed geology maps (Figure 4 and Drawings 1-A and 1-B respectively).

Laboratory analytical certificates listing results in ppb gold are compiled in Appendix C.

11.0 DISCUSSION OF RESULTS

The present geological program has outlined three areas of potential economic interest. The first area lies near 19+50N between lines 0+00 and 4+OOE (Detail Area No. l, refer to Figure No. 4). The area contains outcroppings of strongly sheared and gossaned oxide facies iron formation and volcanics. The iron formation is exposed over a total length of 65 feet and varies from 1-15 feet in width. Field evidence suggests the presence of a broad fold affecting the iron formation and surrounding volcancics which appears to have an axial plane striking approximately 100 0 and plunging 32-52 c towards the east. The unit is composed of recrystallized magnetite, quartz (both recrystallized chert and secondary quartz), and secondary ankerite and calcite. Irregular chlorite and sericite bands within the unit may represent sheared tuffaceous layers present in the iron formation. The unit typically contains trace to 2 % pyrite with local concentrations of up to 10% sulphide. Minor chalcopyrite and arsenopyrite also occur. Quartz-rich

- 21 -

sections of the unit tend to be the most strongly mineralized. A 0.4 to 1.2 foot wide quartz vein occurs along the hanging wall of the iron formation at its westernmost exposure adjacent to line 4+OOE. The vein is not mineralized and did not return significant gold values. Six values, however, ranging between 111 and 330 ppb gold were obtained from the iron formation unit.

Also within Area No. l are strongly sheared mafic and felsic volcanics. The mafics are highly chloritic and fissile and contain abundant quartz-ankerite veinlets and trace to 3% pyrite. A sample of this material adjacent to the iron formation returned a value of 152 ppb gold. Sheared felsic volcanic flows near 2+OOE, 20+OON contained up to 2% arsenopyrite but did not yield significant results.

Area No. l flanks a coincident magnetic high and moderately strong VLF-EM anomaly. The magnetic high rises to about 2500 gammas above background and extends to either side of the showing for a total strike length of 1200 feet. The VLF anomaly is quite extensive and may in part be topograph ically controlled. However, it may also reflect a wide spread zone of shearing in that area of the property. Several narrow to moderately wide shear zones, including those in Area No. l, occur between Line 0+00, 22+OON and Line 20+OOE, 10+OON, and may be indicative of a larger structure.

Area No. 2 is found on Line 12+OOE, 23+OON, about 1000 feet northeast of Area No. 1. A small outcrop (20 feet in diameter) of brecciated quartz-feldspar porphyry and mafic flows has provided one anomalous value of 402 ppb gold. The matrix of the breccia is clear to smokey quartz which locally has a very strong limonitic stain. The fragments are highly

- 22 -

angular and up to 2 feet in diameter. Trace - 3% pyrite occurs within small vugs in the quartz matrix. The outcrop lies within a small but moderately strong VLF-EM anomaly.

Area No. 3 has provided the highest gold values on the property. Anomalous values have been obtained from within a broad area centered on 6+OON and extending between 9+OOW and 24+OOW. The area contains numerous outcrops of predominantly mafic volcanics and diorite. Minor occurrences of felsic volcanics and quartz-feldspar porphyry were also noted. Gold values of 139 and 199 ppb were obtained from two widely separated outcrops of brecciated mafic volcanics which appear to be pyroclastic. Both samples contained disseminated pyrite. Felsic volcanics containing pyrite and arsenopyrite also provided gold values - one from a sheared flow (114 ppb Au) and another from a narrow lens of massive flow material (556 ppb Au). A three inch wide quartz-calcite-epidote vein in massive mafic flows assayed 1047 ppb gold.

Area No. 3 is flanked by several weak to moderately strong VLF-EM anomalies and displays a weak magnetic expression.

Additional anomalous gold values were discovered on the property which are worth further investigation. In particular, there are two values east of Area No. 3 which occur within 800 feet of each other - a value of 188 ppb gold from a medium grained, magnetic leucogabbro at 4+50E, 7+OOS, and a value 187 ppb gold from an arsenopyrite-rich pod within a quartz-ankerite vein at 3+70W, 5+70S.

- 23 -

12.0 CONCLUSION

The North Caribou River property is underlain by predomin antly mafic volcanic rocks with lesser intermediate to felsic volcanics and minor chemical sediments. Widespread intrusive activity has also occurred on the property.

Three areas with low but anomalous gold values were dis covered during the program. Area No. l consists of highly sheared oxide facies iron formation and volcanics which locally contain strong sulphide mineralization. Area No. 2 consists of brecciated quartz-feldspar porphyry and mafic flows with an iron-stained, sulphide-bearing quartz matrix. Area No. 3 consists of predominantly volcanic rocks within a poorly defined area measuring roughly 400 fleet wide by 1500 feet long. Anomalous gold values were obtained from brecci ated mafic volcanics, felsic volcanic flows, and quartz veins within this area.

Additional work is warranted to further delineate the nature and extent of gold mineralization on the property.

13.0 RECOMMENDATIONS

A two phase exploration program is recommended to further delineate gold-bearing horizons on the property.

Phase No. l involves additional prospecting, outcrop stripp ing and channel sampling over favourable areas outlined during the present program.

24 -

Phase No. 2 involves a limited diamond drilling program totalling 3,000 feet. Geological targets outlined in Phase No. l as well as some of the more prominent geophysical targets on the property should be tested by drilling.

14.0 ESTIMATED COST OF RECOMMENDED PROGRAM

Phase I - Four-man camp (two geologists, two assistants outfitted with supplies for 7-10 days of outcrop stripping, channel sampling, detail mapping, and prospecting

- approximate cost (supplies, wages,assay costs, contingencies) ——————— $ 12,000.00

Phase 2 - 3,000' of diamond drilling at 540 perfoot, all inclusive —————————————— $120,000.00

- Contingencies, 20% —————————————— g 24,000.00—————————————— $144,000.00

Total Estimated Cost of Phases l St 2 — $ 156,000.00

Respectfully submitted,

rf

E. D. Timoshenko GEOCANEX LTD.

- 25 -

15.0 REFERENCES

Bartlett, J.R., Breaks, F.W., DeKemp, E.A., Shields, M.N. 1985. Precambrian Geology of the Eyapamikama Lake Area (Opapimiskan Lake Project), Kenora District (Patricia Portion); Ontario Geological Survey, Map P.2834, Geological Series - Preliminary Map.

Hodge, H.J., 1988. Report on Magnetic and VLF-EM Surveys, North Caribou River property, District of Kenora, Patricia Mining Division, Ontario, for Golden Tanager Resources Ltd. (Internal Geocanex Report).

North, Jon W., 1985. Report on Geological Mapping, Litho geochemical Sampling, Soil Sampling, and Prospect ing; Agutua Arm Property, District of Kenora, Patricia Mining Division, for Moss Resources Ltd. (Internal Geocanex Report).

North, Jon W., 1985. Report on Geological Mapping, Geo chemical Sampling, Trenching and Prospecting; Randall Lake property, District of Kenora, Patricia Mining Division, for Moss Resources Ltd. (Internal Geocanex Report).

North, Jon W., 1987. Report on Prospecting, Trenching, Channel Sampling and Geological Mapping; Randall Lake property, District of Kenora, Patricia Mining Division, for Power Explorations Inc. (Internal Geocanex Report).

Thurston, P.C., Sage, R.P., Siragusa, G.M., 1979. Geology of the Winisk Lake Area, District of Kenora, Patricia Portion; Ontario Geological Survey Report 193.

APPENDIX A

CERTIFICATE OF QUALIFICATION

CERTIFICATE OF QUALIFICATION

THIS IS TO CERTIFY THAT:

I am a resident of Brampton, Ontario.

I am a graduate of the University of Waterloo, Waterloo, Ontario, with a Bachelor of Science degree (Geology).

I have worked continuously as an exploration geologist since 1985 in gold exploration in Northwestern Ontario and the Yukon.

I participated in the surface exploration program of the North Caribou property between July 14 and August 17, 1988.

The statements contained in this report, and conclusions reached, are based upon the study of all relevant assessment work records of the Ontario Geological Survey, and geological reports and maps published by the Ontario Ministry of Natural Resources.

In this report, I have disclosed all relevant descriptive and interpretative material which is, to the best of my knowledge, necessary to gain a complete understanding of the viability of the project and the recommendations.

DATED THIS Jtf DAY OF //0s, , /T//

E.D. Timoshenko, B.Se. Geologist

APPENDIX B

ROCK SAMPLE DESCRIPTIONS AND ANALYSES

APPENDIX B - SUBSECTION l

CHANNEL SAMPLE

DESCRIPTIONS

CHANNEL SAMPLE DESCRIPTIONSAwNo.

Trench Location

Length Cut True Descriptions

Assa Au pp (Check)

14950 4*64E,19-I-38N 1.5 Mafic Volcanic- weakly sheared- highly foliated- carbonatized- chloritized- weakly limonitic- rare quartz/carbonate

stringers- trace pyrite.

29 (20)

14951 4+63E,

19+36.5N 2.6 Sheared Mafic Flow- highly fissile- quartz-ankerite-calcite

stringers- carbonatized- chloritized- limonitic- trace pyrite *

arsenopyrite.

10

14952 4*61E,19*35N 2.1 Sheared Mafic Flow - as per 14951.

14

14953 4+60E,19+33N 2.0 Sheared Mafic Flow- highly chloritized- carbonatized- minor quartz-ankerite-

calcite stringers- slightly limonitic- trace pyrite.

29

Assay Ne

Trench Location


Assa Au pp (Check)

14954 4+61.5E,

l9+44N

1.7 Sheared mafic Flow - similar to 14950

152

14955 4+60.5E,

194-43N

1.6 Sheared Mafic Flow- highly fissile- highly chloritized- carbonatized- minor sericite- quartz-ankerite-

calcite stringers- trace pyrite- limonitic along

foliation planes.

16

14956 44-63E,194-47N 3.0 Sheared Iron Formation- intensely sheared- SO-40% magnetite- numerous quartz-

ankerite veinlets- carbonatized- 1-21 pyrite- highly limonitic.

19

14957 4+51E,

194-48. 5N

1.4 Sheared Flow- felsic?- sericitic- foliated- weakly limonitic- trace carbonate- trace pyrite.

66

Assay No.

Trench Location


Assa

Au pp (Check)4+52E, 19+49.5N

2.0 Quartz-Ankerite-Vein 26- dominantly vein material- minor sheared wallrock- minor calcite- trace pyrite- minor limonite

14959 4*52E,19*50N 1.8 Sheared Mafic Flow- chloritized- carbonatized- slightly limonitic- quartz-ankerite

stringers- trace pyrite- 6" band of massive

magnetite near contact with sheared iron formation.

39

14960 4+54E,19+57N 1.8 Sheared iron formation (?)- chloritic schistcontaining between ID-50% magnetite; very strongly sheared and brecciated

- local concentrations of massive, medium grained magnetite; brecciated fragments of massive magnetite also occur

- ankerite occurs in small grains and within quartz- ankerite veinlets; minor calcite veinlets

- locally silicified(possibly recrystallized chert)

- minor talc fc sericite- strongly carbonatized- trace disseminated pyrite- thick gossaned rind up

18

Assay Ne

Trench Location


Assa Au pp (Check)

14961 4+52.5E,

19+56N

2.2 Sheared iron formation(?), as per 14960- several sections of

massive magnetite- abundant quartz-ankerite

veinlets- trace pyrite and arsen

opyrite.

11

14962 4+5IE,19+53N 1.8 Sheared mafic volcanics- predominantly chlorite with lesser sericite and possibly talc

- minor quartz grains up to 1/4" wide

- numerous steeply dipping quartz-ankerite veinlets (most 1/8-1/4" wide); two large veins (4" and 6" wide) composed mostly of ankerite also occur

- trace pyrite- grades into a sericite

schist containing quartz porphyroblasts (possibly a sheared quartz-porphyry dike).

18

14963 4+56E,19+62N 1.6 Quartz-sericite ^ chlorite 12 ^ ankerite schist (possible sheared felsic volcanic)- numerous steeply dipping quartz-ankerite veinlets

- minor tourmaline in thin stringers

Assay Trench Location


Assa Au pp (Check)

14963 Cont'd ...

- trace pyrite and chal copyrite occur in several veinlets

- weakly carbonatized along fractures.

14964 4454E,19H-61N 2.2 Sheared iron formation(?), as per 14960- 15-401 magnetite- numerous steeply dipping

veinlets, mostly calcite; minor quartz-ankerite veinlets

- abundant quartz locally- trace - 2% pyrite, trace

chalcopyrite and arseno pyrite; sulphides occur mainly in silicified areas.

57

14965 4+52.5E, 19+67N

1.6 Sheared ironformation(?), as per as per 14960- strongly brecciated

and silicified locally, with up to 5% pyrite and trace chalcopyrite

- abundant ankerite as discontinuous, smeared out veinlets and fracture fillings

- S-35% magnetite.

202

Assay Ne

Trench Location


Assa Au pp (Check)

5001 4+51.5E, 19+66N

1.9 Sheared iron formation(?), 125 essentially as per 14965- several highly siliceous

intervals (recrystallized chert?)

- trace - 51 pyrite, concen- traced in siliceous areas, rare chalcopyrite

- strongly carbonatized.

5002 4*47E,19*67N 1.9 Sheared iron formation(?), 81 as per 14965- trace - 53; pyrite,

occurring in silicified sections and within ankerite veinlets; pyrite also forms in thin stringers

- strongly carbonatized.

5003 4+45E/19+65N

5004 4443E,19*64N

2.2 Sheared iron formation(?), 87 as per 14965- trace - 3% pyrite,

occurring in silicified sections and irregular ankerite veinlets;

- trace chalcopyrite.

2.5 Sheared iron formation (?), 13 as per 14965- high magnetite content

throughout interval (25-501)

- numerous quartz-calcite veinlets, minor quartz- ankerite veinlets

Assay Trench No. Location

Length

Cut True DescriptionsAssa

Au pp (Check)

5004 Cont'd ...

5005

5006

- small ankerite grains occur throughout the unit (3-71)

- trace - l% pyrite.

2.7 Sheared felsic volcanics- light green, fine

grained, strongly sheared and brecciated, predomin antly quartz and sericite

- quartz-ankerite veinlets and fracture fillings

- trace fuchsite- compact, weakly foliated- smeared out chloritic

fragments- rare disseminated pyrite.

3.0 Sheared mafic volcanics- predominantly chlorite with lesser sericite, ankerite and quartz

- numerous ankerite ^quartz veinlets infilling brecciated fragments

- trace - 3% disseminated pyrite

- rare chalcopyrite, occurring in veinlets.

10

16

Assay Ne

Trench Location


Assa Au pp (Check)

5007 2.6 Sheared mafic volcanics, 52 similar to 5006- grades into sheared iron

formation- magnetite occurs in

isolated brecciated fragments within chloritic matrix

- quartz-ankerite veining prominent throughout sample; minor calcite veinlets

- trace - 4% pyrite,occurring mainly withinchloritic material, alsoin quartz-ankerite veinlets.

5008 4+43E, 19+68.5N

1.6 Sheared iron formation(?)- predominantly chlorite

schist with isolated brecciated fragments of magnetite; small sections of massive magnetite also occur

- quartz-ankerite veining prominent throughout section; ankerite also occurs in disseminated grains

- trace - 31 pyrite, with local concentrations up to 101;.

63

AssayNe

Trench Location


Assa Au pp (Check)

5009 4+41.5E,

19+68N

2.1 Sheared iron formation, essentially as per 5008- magnetite (S-25%) occurs

in scattered, irregular patches and fragments

- up to 10% disseminated ankerite grains

- trace - 11 pyrite.

25

5010 44-03E,19*50N 1.4 Sheared Mafic Flow- chloritized- silicified- limonitic- trace calcite- few quartz ankerite

stringers- trace to Q.5% pyrite

+ chalcopyrite in stringers.

154 (177)

5011 4+02.5E,

19+51N

1.7 Sheared Iron Formation?- locally up to 301

magnetite- quartz-ankerite

stringers and flooding- l-3% pyrite- trace chalcopyrite- minor calcite- limonitic

111

5012 4+02E,19+53N 1.8 Sheared Iron Formation - as per 5011

31

Trench Location


Assa Au pp (Check)

5013 4+01E,19+54N 0.5 Quartz Vein- iron formation wallrock

as per 5011- white- trace calcite- limonitic along fracture- no visible sulphide- 2-3% pyrite in highly

fissile chloritized wallrock.

49

5014 4401E,19-f55N 1.2 Silicified Flow- possibly felsic- sericitized- Fe-carbonate- trace pyrite- trace limonite.

5015 3+96E, 19+52.5N

2.0 Quartz-Vein and Felsic Wallrock- vein as per 5013- wallrock as per 5014,

5016 3+98.5E,

19+51N2.7 Sheared Iron Formation

- as per 5011- up to 5% pyrite- traced to D.5% chal

copyrite- trace pyrrhotite- traced fuchsite.

30

5017 4+OOE,19+50N 2.0 Sheared Mafic Flow- similar to 5010- 3" wide quartz-ankerite

veinlet- veinlet limonitic with

trace pyrite.

324

Assay Trench Length Location Cut True Descriptions

Assa Au pp (Check)

5018

5019

3+98E/19+47N 1.2 Sheared Felsic Flow?- similar to 5014- chloritized- minor quartz-ankerite

veinlets- trace pyrite- weakly carbonatized.

1.4 Quartz-Ankerite Vein- l'6" wide

- slightly limonitic along fractures

- 151 ankerite- no visible sulphide- white- at contact of iron

formation and felsic flow.

10 7)

5020 3*96E,19*49N 1.6 Sheared Iron Formation 330- as per 5011- up to 21 chalcopyrite.

5021 3+94.5E, 19+50N

1.0 Sheared Mafic Flow - as per 5010.

68

5022 34-9IE, 19+43N 1.6 Sheared Iron Formation- as per 5011- 11 chalcopyrite- 2% pyrite.

42

5023 3+90.5E,

19+44N

2.0 Sheared Felsic Flow- several 2-3" quartz

veinlets- slightly limonitic

28

Assay Trench Location


Assa Au pp (Check)

5023 Cont'd ...

silicifiedchloritizedtrace chalcopyrite andpyrite in quartztrace to D.5% pyriteand chalcopyrite inwallrock.

5024 34-61E,194-33N 2.0 Quartz Ankerite Vein and Sheared Felsic Flow- flow material highly

limonitic with trace pyrite and chalcopyrite

- variably sericitized and chloritized

- trace sulphide in quartz vein

- vein up to l' wide with numerous irregular stringers.

31

5025 34-61E,194-31N

5026 24-08E,194-96N

1.6 Quartz-Ankerite Vein and Sheared Felsic Flow- as per 5024.

2.4 Sheared felsic volcanics- light to medium green,

mostly fine grained quartz and feldspar with lesser sericite and chlorite

- weakly foliated

13

15


Assay Trench

LocationNo

Length

Cut True Descriptions

Assa

Au pp (Check)

5026 Cont'd

5027

5028 1+97E/19+97N

5029 l*97E,19-f95N

5030 1+97.5E,

19+93N

- abundant carbonate along fractures

- minor quartz-ankerite veinlets

- trace - 11 disseminated pyrite, trace arsenopyrite

- weakly gossaned.

2.0 Sheared felsic volcanics, 11 as per 5026.

1.6 Sheared felsic volcanics, 13 as per 5026- abundant sericite and quartz-ankerite veinlets.

1.9 Sheared felsic volcanics, 13 as per 5026- trace pyrite and arseno pyrite

- minor quartz-ankerite veinlets.

1.9 Sheared felsic volcanics, 14 as per 5026- grades into relatively

unaltered volcanics- trace pyrite.

(20)

Assay Ne

Trench Location


Assa Au pp (Check)

5031 H-06E,194-32N 2.0 Sheared mafic volcanics 20- strongly foliated

chlorite-sericite schist- ankerite ± quartz j^

calcite veinlets occur throughout unit

- trace - 2% disseminated pyrite, rare arsenopyrite

- strongly gossaned.

5032 1+05.5E,

19+29N

3.1 Sheared felsic volcanics- predominantly quartz and

sericite with abundant ankerite veinlets

- trace chalcopyrite and pyrite occur in several veinlets

- trace fuchsite- inclusions of chloritic

material- moderately well foliated, weakly gossaned.

5033 l+05E,19+27N 2.2 Sheared mafic volcanics, as per 5031- several crosscutting quartz-ankerite veinlets up to 1/2" wide

- trace disseminated pyrite.

15


Assay Trench Length Location Cut True Descriptions

Assa

Au pp (Check)

5034 04-82E,194-82N

5035 0+82E,19+80N

5036 0+82E,19+78N

1.3 Sheared mafic volcanics, 49 as per 5031- minor intercalations

of felsic volcanics (quartz-sericite)

- trace disseminated pyrite.

2.2 Sheared felsic volcanics, 29 as per 5032- strongly foliated and gossaned

- numerous quartz-ankerite veinlets

- trace - l * pyrite, occurring mainly as thin, steeply dipping stringers.

3.3 Predominantly sheared 12 mafic volcanics (chlorite- sericite schist, as per 5031) with intercalations of felsic volcanics (quartz-sericite schist)- numerous quartz-ankerite

veinlets- trace - 1 Z d isseminated pyrite.

l l l l l l

APPENDIX B - Subsection 2

lm GRAB SAMPLE DESCRIPTIONS

l

l

l

l

l

l

l

l

l

l

GRAB SAMPLE DESCRIPTIONSKssay Location No. (North/East) Description

Assay Results ppb Au (Check)

14805 36*06E,154-OON Intermediate volcanics- fine grained, massive- minor amygdules containing

epidote, carbonate and minor pyrite

- l-2% disseminated pyrite.

8

14806 22+40W,22+35N Mafic volcanics 15- weakly brecciated,

silicified- minor quartz-carbonate

veinlets- trace pyrite in small blebs- found near gabbro contact

14807 364-35E,15*04N Mafic volcanics 8- weakly sheared, highly

carbonatized volcanics found between gabbroic intrusives

- trace - 11 pyrite- shear zone is about 2' wide, orientation 38V?5 0N.

14808 29*35E,16*40N Quartz-carbonate ^ epidote f vein in mafic volcanics amphibolite)-2" wide; very poorly exposed- small euhedral crystals of quartz and epidote

- trace pyrite along vein walls

14809 4+OON l 64+50E Fuchsitic Zone in mafic vol canics- massive volcanics with

randomly oriented 10mm long actinolite crystals

- zone trends at 082".

Assay Location No. (North/East) Description


14810 3*80N,634-90E Fine grained mafic volcanics increasingly silicified towards south- l-2% disseminated pyrite

and possible arsenopyrite- also a pyrite stringer

5mm wide.

8

14811 27*80E,18*40N Highly silicified, weakly 10carbonatized mafic volcanics in contact with diorite- possible shear zone- trace pyrite- trending roughly 92 0

14812 27+60E,19+60N Mafic volcanics; very weakly 7foliated (trending 52 C )- frequent narrow stringers

containing epidote, carb onate and minor pyrite trace - IS; disseminated pyrite.

1482.4 8(H30E,29*80N

14825 74H-OOE,31*OON

Mafic volcanic- carbonate stringers- limonitic along fractures- trace pyrite.

Intermediate Flow?- possibly silicified mafic- limonitic surface- trace carbonate- no visible sulphide- massive

10

(26)



14826 784-OOE,35H-40N Felsic intrusive- massive- trace sulphide

14827 78+0(^,35+41^ Mafic volcanic- at contact of felsic

intrusive- epidote rich- trace pyrite- trace carbonate

10

14828 77+OOE,37+80N Amphibolite- massive- limonitic along fractures- trace carbonate- trace arsenopyrite- trace chalcopyrite

17

14829 75+90E,42+20N Quartz stringers- in felsic intrusive- 0.5 to 2.0 inches wide- discontinuous- up to several feet long- orientation variable

along joints- trending 30 to 50 0 but also irregular

- dipping steeply N and S- slightly limonitic- no visible sulphides

l l l l l l l l l ll ll ll l l l l



14830 76*OOE,42*20N

14831 H-55E,49*80N

14832 H-60E,49*75N

14835

Silicified mafic flows- near contact of felsic

intrusive- trace pyrite- massive

Sheared Intermediate Lapilli Tuff- carbonatized- limonitic- trace to It; pyrite- chloritized- trending 68"- dipping steeply S.

Sheared Intermediate Lapilli Tuff- as per 14831

Sheared Intermediate Lapilli Tuff- as per 14831.

Mafic Volcanics- fine grained, chloritic- no sulphides, no

carbonate

28+45E,21+OON Mafic volcanics; very finegrained, massive, silicified- sharp, irregular contact with amphibolite

- subconchoidial fracture- numerous hairline fractures

some containing carbonate- no visible sulphides.

14833 l*70E f 49*68N

14834 10S,66E

8

16

13 (11)

Assay Location Assay Results No. (North/East)_______Description__________ppb Au (Check)

14836 26H-30E,22H-60N Mafic volcanics; silicified, 11as per 14835- trace pyrite- limonitic stain along

fracture surfaces

14837 25+40E,23+40N Shear Zone in mafic volcanics; 76' chip sample across zone- sheared material consists

mostly of chlorite and sericite with lesser quartz, ankerite and calcite.

- strongly gossaned locally {carbonate alteration)

- numerous quartz-ankerite ^ tourmaline veins (most

< 1/2"); majority are concordant,several contain trace chal copyrite

- trace - , l% d isseminated pyrite

- shear zone oriented 64V79 0 S.

14838 25+48E,23+40N Quartz-ankerite-tourmaline 8in sheared mafic volcanics- minor chlorite, trace pyrite- concordant vein, 1/4 - l"

wide, extends for about 8'.

14839 25+4(^,23+40^ Quartz-ankerite-tourmaline 16vein crosscutting sheared mafic volcanics- 1/2 - 3/4" wide, 3' exposed- no visible sulphides- trending 178 C .

Assay Location Assay Results No. (North/East)______Description__________ppb Au (Check)

14840 25452E,23H-40N Highly sheared, well gossaned 30mafic volcanics- essentially as per 14837,

with 1-21 disseminated pyrite.

14841 25*34E,23*38N Highly sheared mafic vol- 24canics, as per 14837, containing numerous randomly oriented veinlets composed predominantly of ankerite with minor quartztrace pyrite occurs within

veins- most veinlets between 1/4 -

1/2" wide.

14842 25+OOE,19+60N Quartz-carbonate pod in 72massive mafic volcanics (4" x l")- abundant carbonate,

inclusions of chlorite and amphibole

- trace - l * chalcopyrite, occurring in large blebs up to 1/4" wide and as fine disseminations.

14843 72*40E,39*30N Mafic volcanic 10 (11)- silicified- massive- epidote stringers- trace chalcopyrite- trace malachite- trending 105?- dip 46" NE?


14844 204-50E,154-OON Quartz porphyry; medium 11green to greenish brown colour, massive- ID-20% clear quartz porphy-

roblasts, most about 1/8"

wide

- weakly carbonatized- minor sericite- no visible sulphides.

14845 18+30E,12+20N Shear zone; strongly foliated 9and intensely carbonatized felsic to intermediate (?) volcanics- chlorite-sericite-ankerite

jj^ quartz assemblage- minor quartz-ankerite,

veinlets up to 1/4" wide- zone trends 74/75*3

-no visible sulphides.

14846 17*70E,12*30N Calcite veinlets within mafic 9

volcanics, 1/4 - 1/2" wide- concordant veinlets in

fine grained, silicified mafic volcanics

- no visible sulphides.

14847 17*50E,12*30N Quartz-ankerite vein, 1-2" 11wide, crosscutting strongly sheared mafic volcanics- heavy carbonate alteration

in area of vein- found on a 10' high scarp

face- 4 ft. exposed length- no visible sulphides.



14848 17*30E,12*OON Quartz-carbonate veinlets inmafic volcanics; mostly thin (< 1 /4"), discontinuous vein lets infilling a weakly brecciated section - no visible sulphides.

14849 5N,32-HOE 6" wide altered or sheared zone in amphibolite- zone is 5C^ quartz- moderate carbonate- trace pyrite and chalcopy-

rite(?)

11

14850 4H-90N,32E Amphibolite and felsic intrusive- amphibolite is a mafic

volcanic- minor carbonate- trace sulphides.

10

14851 10S,26E

14852 1N,24E

Boulder - Chert Beds 21- up to 51 pyrite as net

working veinlets- similar to that found

on Randall Lake property.

Massive Diorite or Plagio- 8 clase-phyric mafic volcanic flow- 50% amphibole- 50% plagioclase- trace pyrite.

5)


14853 164-30E,94-95N Quartz-carbonate vein (1-2"), 59concordant in mafic volcanics- milky quartz with abundant

chlorite inclusions, minor ankerite and calcite

- trace chalcopyrite (small blebs)

- volcanics are weakly foliated, trending 104".

14854 164-80E,12*40N Quartz-carbonate veinlets 8within silicified mafic volcanics, possibly weakly brecciated- mostly thin, discontinuous

veinlets, 1/8 - 1/4" wide, randomly oriented


14855 16*35E,13*05N Quartz-ankerite vein 138- angular float block (about

1.5' exposed, 5" wide) found 100' east of shear zone (sample 14845)

- trace - 11 chalcopyrite, occurring in blebs up to 1/4" wide

- vein also contains minor chlorite.

Assay Location Assay Results No. (North/East)_______Description__________ppb Au (Check)

14856 12+20EJ27+55N Shear zone in mafic 44volcanics, 5* exposed width- mostly chlorite with lesser

sericite, carbonate (ankerite, feldspar and quartz

- highly crenulated- weathers to a light green

colour, locally weakly gossaned

- zone contains several felsic intrusive dikes which have been highly brecciated and smeared out along foliation planes

- in contact with amphibolite (possible gabbro) to south

- orientation 70 C 768 0 S- trace very fine grained

pyrite.

14857 10+85E I 27+70N Quartz-ankerite veinlets in 54sheared mafic volcanics- narrow concordant veinlets,

most 1/8 - 1/4" wide, weakly gossaned

- shear trends 75V80 0 S- no visible sulphides.


14858 12H-10E,23*20N Brecciated mafic volcanics 15and quartz-feldspar porphyry; matrix is predominantly clear to milky quartz which is frequently strongly gossaned- large breccia fragments up

to l' long- very minor carbonate- no visible sulphides- intruded by diorite dikes.

14859 12+10E/23+24N Brecciated mafic volcanics 8with quartz matrix, as per 14858- large blebs of pyrrhotite

occur in several fragments; trace pyrite occurs in quartz matrix

- quartz has a heavy hemo- titic and limonitic stain.

14860 12*17E,23-f20N Brecciated quartz-feldspar 402porphyry, with quartz matrix, as per 14858- trace - 2% pyrite,

ocurring as small subhedral crystals within narrow vugs.

14861 20H-OOE,10*50N Highly altered volcanic 7 ( 6)- predominantly fine grained,

massive quartz and ankerite with minor calcite and fuchsite

- highly gossaned rind- no visible sulphides- possibly a large vein.

l l l l l l l l I l l l l i i l i i i



14862 11*45E,1*95N Quartz-feldspar porphyry- phenocrysts of yellow- white feldspar and clear quartz, most about 1/8" wide; around 25-301 phenocrysts

- groundmass is dark green, very fine grained, siliceous

- trace pyrite- intrudes mafic volcanics.

14863 10+4(^,0+158 Shear zone in mafic to inter- 12 mediate volcanics (^ 4 ' wide)- predominantly chlorite with

lesser sericite, ankerite, feldspar and quartz

- strongly foliated and crenulated; orientation 50V78 0 SE

- contains segregations of highly silicified, poorly foliated material (irr egular pods and lenses) which weather to a buff- white colour

- minor quartz-ankerite veinlets

- intercalations of strongly magnetic mafic material

- weakly gossaned, trace pyrite.



14864 KH44E,(H12S Quartz-ankerite vein, 2-3"wide, 3' exposed length, crosscutting sheared mafic to intermediate volcanics- minor inclusions of

chlorite- no visible sulphides

- trending 114".

14865 1(H40E,(H15S Silicified pods and lensesof intermediate to mafic volcanics within shear zone- lenses up to l' long, 4" wide

- numerous thin ankerite stringers, minor calcite


14866 10+4(^,0+148

14867 9*08E,19*35N

Thin band (~^5") of strongly magnetic mafic material within shear zone- highly crenulated, very

dense- trace disseminated pyrite

and pyrrhotite.

Shear zone in mafic volcanics, 2-3' wide- predominantly quartz-

sericite schist, highly crenulated, strongly carbonatized

- also contains minor anker ite, feldspar and quartz

- no visible sulphides- orientation 507?2 0 SE.

16

Assay Location Assay Results No. (North/East)______Description__________ppb Au (Check )

14868 9+08E,19+35N Quartz-ankerite vein, 26concordant in sheared mafic volcanics- 1/2 - l" wide, 1.5'

exposed- chloritic inclusions,

no visible sulphides

14869 8+92E,19+35N Quartz-ankerite vein in 19sheared mafic volcanics, as per above; 1/2-1" wide- trace pyrite, occurring

in small blebs.

14870 61+50E,25+OON Sheared Mafic Flows 5- chloritized- trace carbonate- trace pyrite- 6" to l' wide- 25' long exposure- trending 97"- dipping 64 C S.

14871 59+25E,32+15N Felsic Dike 5 { 6)- in gabbro- epidote rich- trace pyrite- slightly limonitic

along fractures- trending 100 0

14872 6CH40E,33H-20N Quartz-Ankerite Vein 5- in sheared mafic flows- massive


14872 cont'd ... - trace pyrite- l - 2% calcite- 1/8" limonitic rind- l' wide- 12' long exposure- trending 90 C- dipping 74 6N.

14873 6CR40E,334-20N Sheared mafic Flows < 5

- wallrock of above vein- silicified- carbonatized- well foliated- trace pyrite- limonitic- trending 90"- dipping 74 C N.

14874 60+60E/46+15N Quartz-Feldspar Porphyry <5- in gabbro- slightly limonitic along

fractures- trace sulphide- trending 190 0

14875 604-60E,46*25N Gabbro 6- l to 2% magnetite

- l% pyrite- epidote along fractures- massive.


14876 3(H50S,344-50E Fine Grained Mafic 5Volcanic

- amphibolite metamorphic grade

- l% pyrite.

14877 34*20S,25E Coarse grained Intermediate 5Rock and silicified mafic volcanics- minor carbonate.

14878 56*70E,32*05N Sheared Mafic Flows 5

- narrow band in intermediate to felsic flows

- 6" wide- quartz/ankerite

veinlets- trace pyrite- very limonitic- trending 35 C .

14879 37*95N,34-90W Mafic Volcanic - light green < 5

fresh surface- weathered surface dark

grey-brown- silicified

- carbonatized- limonite staining along

fractures- highly foliated- orientation 73'772 C S.

Assay Location Assay Results No. (North/East)______Description——--——.--.^——ppb Au (Check)

14880 39H-70N,14-80W Felsic Dike - 4' wide 7 (7)- probable trondhjemite- concordant- contains angular to sub

angular xenoliths of mafic volcanics

- xenoliths vary in size from 2-3" to 1-2'

- limonite along fractures- trace pyrite- orientation 62V90 0 .

14881 39+7013,1+801^ Quartz Vein - average width < 51/4"

- pinches and swells along contact between felsic dike and mafic volcanics

- minor limonite staining- trace pyrite.

14882 39+70N,l+80W Amphibolite - fine to medium 8grained- trace carbonate- trace limonite- few crosscutting felsic

dikes (randomly oriented)- orientation 62V90 0 .

14883 20+70N,44+OOE Quartz-Carbonate Vein: 15-1.5' wide- concordant- minor limonite staining- locally 1-31 chalcopyrite- trace pyrite- orientation 96 C 772 C N.



14884

14885

20*70N,444-OOE Quartz-Carbonate Vein:- as per 14883- trace pyrite.

Sheared iron formation (?) 284- 2-3' wide strongly

gossaned band composed of magnetite, quartz, ankerite and minor chlorite; appears to be folded (plunging 52 0 ESE)

- a 0.2 - 1.0' wide quartz j^ ankerite vein ocurs along the footwall of the ironstone

- magnetite content varies from trace-5% in highly silicified zones; upwards to 60% magnetite elsewhere

- weakly carbonatized- trace-3% pyrite, occurring predominantly in the more strongly silicified areas.

Sheared iron formation (?), 45 as per 14885- sample consists mainly of highly silicified material (essentially a chlorite - quartz j^ feldspar ^ anker ite H^ magnetite assemblage)

- 2-10% magnetite- trace-3% pyrite, occurring

as small subhedral crystals and fine disseminations

- minor calcite and ankerite veinlets.

14886 3*98E,19*50N


14887 4*04E,19*54N Sheared iron formation (?) 25as per 14886

- trace - 2% pyrite.

14888 4H-03E,19*50N Quartz ^ ankerite vein <5- predominantly milky quartz

with minor ankerite and chlorite

- 0.3 - 1.1' wide

- in contact with sheared iron formation


14889 4+03E,19+50N Quartz-ankerite vein, 11 (11)offshoot of larger vein described above (14888)- 1-2" wide

- trace pyrite in smallcubes and irregular blebs.

14890 4*70E,19*32N Quartz-ankerite vein, as < 5per 14889, in sheared mafic volcanics- 2-3" wide, 2' exposed

length- concordant, trending 105 6- no visible sulphides.

14891 20+80N,43+90E Mafic Volcanic - dark green <5- sheared, fine grained- few narrow quartz-carbonate

veinlets ( <l/B")- carbonatized U-5%)- 0.5 - l.Oi pyrite dissem

inated throughout rock or along veinlets

- minor limonite staining.

Assay Location Assay Results No. (North/East)______Description_________ppb Au (Check)

14892 36S,21*20E Fine Grained Intermediate < 5to Mafic Volcanics- trace pyrite

14893 364-70S,19E Plagioclase-phyric Flow < 5- plagioclase crystals up

to 5mm long.

14894 34*50S,16*50E Fine Grained Felsic Vol- 5canics- 2-3?; mafic- minor muscovite- weathers pink.

14895 34-72E,19*37N Quartz-ankerite vein 12crosscutting sheared mafic volcanics- l - 1.5' wide, 6' exposed- irregular trend; changes

from perpendicular to sub- concordant to the foliation

- minor inclusions of chlorite


14896 4+50E,19+55N Possible sheared iron 16formation- band of magnetite-rich

material 6-8' wide in contact with weakly sheared mafic volcanics

- appears to be a magnetite- ankerite (siderite ? ) j^ chlorite j quartz ^ calcite assemblage; minor talc and pyrite also occur

- strongly carbonatized- thick gossaned rind.




14897 2*10E,19*94N

14898 2+03E / 19+94N

14899 4*40E,0*23N

Sheared, weakly carbonatized 32 volcanics (felsic to inter mediate) containing abundant quartz-ankerite veinlets- fine grained, weakly

foliated and banded appearance; weakly brecciated sections

- trace - 2 % pyrite and arsenopyrite occurring in euhedral crystals and fine disseminations

- shear zone is 1-2' wide, strongly gossaned, trends 69" and dips steeply to the north.

Sheared felsic to inter- 17 mediate volcanics, as per 14897- trace - 2% pyrite and

arsenopyrite.

Mafic to intermediate sub- 13 volcanic; possibly a silic ified volcanic- locally contains small

grains and discontinuous veinlets of pale blue quartz

- strongly carbonatized- possibly a quartz porphyry- trace pyrite.

(17)


14900 4H-42E,0*23N Diabase dike 10- irregular shape, 8"-!' wide- dark grey, very fine

grained, weakly magnetic- strongly carbonatized- l-2% disseminated pyrite- trends 166 0 .

14901 1H-OOE,19*80N Sheared, silicified vol- 13canics (likely Mafic) containing abundant ankerite ^ quartz veinlets- weak to moderate carbon

atization- trace pyrite, rare arseno pyrite

- veinlets are mostly con cordant and between 1/16 - 1/8" wide.

14902 54*50E,254-OON Sheared Mafic Flows 21- quartz-ankerite-calcite

stringers- trace pyrite- very limonitic- 2' wide exposure- 4' long exposure- surrounding mafics highly 1

foliated- trending 85 0- dipping 60 C S.



14903 6+205,9+OOE Shear Zone in Intermediate 17Volcanics- trends at 048 0- consists of quartz/carbon

ate veins in the volcanics- up to O.S-1% pyrite and possible chalcopyrite.

14904 2*30E,32*OON Mafic volcanics (amphibolite) 9- medium grained, minor

carbonate and limonite along thin fractures

- trace - l% disseminated pyrite.

14905 0*20E,3^90N Mafic volcanics, possibly 10weakly brecciated- highly silicified; abundant

carbonate in thin veinlets- trace - IS; very fine

grained pyrite, rare arsenopyrite

- weakly gossaned.

(17)

14906 25+50E,23+40N Shear zone in maficvolcanics, as per 14837; 4' chip- predominantly chlorite-

sericite j^ ankerite ^ quartz schist; sample includes an 8" wide pod of strongly gossaned quartz-ankerite.

- trace pyrite.

Assay Location Assay Results No. (North/East)-——-—-——Description__________ppb Au (Check)

14907 25*57E,23*40N Shear zone in mafic volcanics 12as per 14837- 5' chip across zone

14908 25+62E,23+40N Strongly brecciated, highly < 5gossaned section (4" - 2' wide) within sheared mafic volcanics- fragments composed of quartz-ankerite material and chlorite sericite schist within a matrix of tourmaline and quartz

- breccia grades into massive quartz-ankerite

- no visible sulphides

14909 254-57E,23*40N Quartz-ankerite vein trend- < 5ing along shear fracture- 1-2" wide, 4' exposed,

discontinuous- no visible sulphides- trending 049 e .

14910 26+35E,23+75N Shear zone in mafic volcanics 5as per 14837- crude 5' chip across zone- folded locally- trace pyrite- shear trends roughly 55".

14911 264-31E,23*75N Quartz-ankerite veinlets in < 5sheared mafic volcanics- 1-2" wide discontinuous

veinlets and pods, most concordant




14912 364-20S,174-70E Dirty Quartz Vein orSilicified Intermediate Volcanics- outcrop is intermediate

volcanics and felsic intrusives.

14913 40S,12E Brecciated IntermediateVolcanics with FelsicIntrusives- trending at 033 0 .

14914 7S,8*60E Intermediate to Mafic l Volcanics with Felsic Dikelets- rock is of amphibolite facies- trace carbonate and pyrite.

14915 7+808,8+80^ Intermediate Pyroclastic Breccia- clasts are quartz-rich,

subrounded to angular with average length 3cm

- matrix is fine grained and mafic

- trace pyrite.

14916 7+508,9+lOE Silicified Zone in Inter mediate Volcanics- quartz is recrystallized- trace to Q.5% pyrite.

40




14917 S+SOS^+SOE Shear Zone in IntermediateVolcanics

- the main shear zone is 1.5' wide and consists of chlorite schist and a 3" wide quartz/carbonate vein

- trace - 11 pyrite.

14918 1+20^43+81^ Mafic Volcanic - weathered 31 surface is buff to light

green- fine grained

- carbonatized

- limonite staining along fractures

- 0.5 - 1.01 pyrite.

14919 20+40S,88+50W Felsic Intrusive 9- weathered surface buff to

white

- medium to coarse grained- carbonatized

- sharp contact with mafics- limonite staining along

fractures- 0.5 - 1^ pyrite- trace magnetite.

14920 20+405,88+50*^ Mafic Volcanic 5- weathered surface dark green

- fine grained- pervasive epidotization along

fractures and to a lesser extent throughout rock

- trace carbonate in stringers- limonite staining along

fractures- trace pyrite.


14921 20+505,88+30;^ Intermediate Volcanic 5

- medium grained- buff coloured- within 14919

- contact is sharp but no preferred orientation

- locally contain fragments of felsic intrusives

- local epidote-rich sections.

14922 38+OOS,75+60W Felsic Volcanic <5 (35)

- fine grained- highly foliated- weak-moderate carbonatization- minor limonite staining- trace pyrite- narrow interflow.

14923 38+OOS,75+60W Mafic Volcanic: 22- fine grained

- weakly sheared- strongly carbonatized- limonite staining along


14924 36+605,75+301* Shear Zone: 5- in mafic volcanics- 1.5' wide- intense shearing- highly fissile- heavy limonite staining

along cleavage- strongly carbonatized- trace pyrite.



14925 36460S,75*20W Quartz Vein - 2" wide- concordant- trace carbonate- minor limonite staining- trace pyrite.

14926 6+25S,7+90E Quartz Vein in Felsic In trusive in Mafic Volcanics- trace pyrite.

<5

14927 6*70S,7*75E

14928 7*70E,8S

Quartz Feldspar Porphyry 36- phenocrysts 0.5 - 4mm long- fresh surface is grey- weathers buff coloured. Epidotized Diorite 30- area is 1.5m long by 3"

wide- weathers lime green- trace pyrite.

14929 78,4+SOE Leucogabbro 188- slightly higher percentage

of amphibole than in the diorite

- grains are up to 2-3mm long

- magnetic.

14930 0+Q0.21+89N Quartz 4 ankerite vein in weakly sheared intermediate to mafic volcanics- 4" - 12" wide, 20' exposed

length; concordant to sub- concordant

- somewhat anastomosing



14930 Cont'd ... - mostly barren, milky quartz with local concentrations of ankerite; minor muscovite

- no visible sulphides- trending around 60 0 , steep

dip to north.

14931 Quartz ^ ankerite vein, as per 14930.

(16)

14932 CHOO,2^89N Wallrock along quartz^ ankerite vein- weakly foliated chlorite

quartz ^ sericite schist- minor grains and small

veinlets of ankerite- no visible sulphides.

10

14933 1*30E,19H-75N Sheared mafic volcanics 29 containing abundant ankerite ^ quartz veinlets- weakly carbonatized- trace - 11 pyrite, dissem

inated and in thin stringers- down strike from sample 14901.

14934 29+OOW / 12+OON Intermediate Volcanic- trace pyrite- numerous randomly oriented quartz-feldspar epidote veinlets.

8


14935 41+255,8+OOE Highly Foliated Intermediate 7Volcanics- minor carbonate- weathers rusty brown.

14936 41+608,9+50^ Highly Foliated Mafic 11Volcanics- strongly carbonatized- fine grained- also minor felsic intrusive

14937 6+5QE.41S Carbonatized Highly Foliated 8Mafic Rock- possibly a gabbro- moderately magnetic

14938 SS+SOS^E Shear Zone with 3" Quartz 11Siderite Vein- trace pyrite- very fine grained- weathers rusty orange- trending 118 C .

14939 35+80W,0+25N Intermediate Volcanic 13- sheared- quartz stringers- trace carbonate- slightly limonitic- trace pyrite- at contact of flow and quartz-feldspar porphyry

- striking 62"- dipping 82 0 to S.



14940 35+2(^,0+20^ Intermediate Flow- massive- slightly limonitic- trace pyrite- several carbonate stringers.

8 9)

14941 (H90E,29*30N Quartz-carbonate-epidote vein (1-2" wide) in mafic volcanics- trace - l% pyrite, minor chalcopyrite and pyrrhotite

- euhedral quartz and epidote crystals

- weak limonitic stain.

8

14942 S+OOW^+SON

14943 5-HOW,9*30N

Intermediate volcanics, 21 porphyritic- quartz porphyroblasts (5%)- minor quartz-ankerite

veinlets, minor calcite- trace arsenopyrite.

Porphyritic intermediate 50 volcanics, as per 14942- numerous quartz-ankerite

veinlets up to 1/2" wide- trace chalcopyrite and

arsenopyrite.

14944 0+40E,8+20S Shear Zone in Intermediate Volcanics- quartz/carbonate vein is

1-3" wide- trace pyrite.

12

l l l l lll l l I l l llll ll l

Assay Location Assay Results No. (North/East)————--Description__________ppb Au (Check)

14945 4W,10S Milky Quartz - Boulder 30- includes some chlorite- trace - .5% arsenopyrite- boulder had broken apart

making it difficult to determine angularity.

14946 42H-50W,3H-60N Quartz-Feldspar-Epidote Vein 37- in coarse grained mafic

flows- slightly limonitic- trace sulphide- trending 80"

14947 42+70W,31+75N Mafic Dike 13- massive- trace magnetite.

14948 48+15W/13+35N Mafic Flows 13- weakly sheared- weakly limonitic- mildly carbonatized- trace pyrite- 6" wide- 3' long exposure- trending 172".

14949 10S,3*60W Quartz Carbonate Vein 10 (15)- weathers rusty- 2' wide at maximum- no sulphides seen- carbonate is calcite

and ankerite.



14966 105,3+SOW

14967 10S,3W

14968 10S,3W

Quartz Carbonate Vein 10- 10' east of 14949

along same vein- shear zone is in quartz porphyry

- orientation: 076/83S- trace pyrite.

Quartz Carbonate Vein 8- continuation of vein

of 14949- vein is l' in width- trace sulphides.

Shear Zone Related Quartz 11 (9) Flooding of Volcanics- l' south of 14967- limonite staining on

fractures and foliation planes

- minor carbonate

14969 10S,3W Quartz Porphyry- country rock of shear

zone- clear, .5-3mm wide quartz phenocrysts ( 5% o f rock) in yellow/green quartz/ sericite fine grained matrix

- iron staining along fractures

10



14970 5*70S,3*70W Sulphide-Rich Bleb in Quartz Vein- bleb is 2' x 6"- S-5% pyrite and arseno

pyrite.

187

14971 5+70S,3+70W

14972 5*75S,3*60W

14973 5+85S,3+45W

Quartz Flooded Shear Zone 54- Strike: 078 Dip: variable

but near vertical- zone is about 4' wide- minor carbonate- trace sulphides.

Sheared Volcanics with Quartz 55- 10' down strike from 14971- minor carbonate- trace - Q.5% pyrite

and arsenopyrite.

Sheared Volcanics with Quartz 16 Sericite Schist- continuation of 14972.

14974 5+85S,3+25W Epidote Altered Intermediate to Mafic Volcanics- transected by networking

quartz veinlets- moderate carbonate- .S-1% pyrite- possible trace malachite.

37

1 1

Assay Location ^k No. (North/East) Description


14975 7+008, 53+40W Quartz Vein - 2" wide 10

1

1

I

1

1

f1

11

t

1

1

1

1

1

1

1

- in 1 ' x 15' localof mafic volcanics

- limonite stainingcontact

- no visible mineral

shear

along

ization- orientation 14/76^.

14976 6+608, 49+80W Shear Zone - 1' wide- in mafic volcanics- carbonatized- limonite staining

fractures- trace pyrite- orientation 80/60 0

<5

along

S.

14977 19+008, 52+20W Diorite - coarse-grained 10 (11)- feldspar rich- limonite staining

fractures- trace pyrite- trace carbonate

along

14978 19+808, 53+OOW Tonalite - medium-grained 18- minor limonite staining

along fractures.

14979 21+405,53+201^ Quartz-Feldspar Porphyry: 12- eo-70% angular to sub-

angular feldspar phenocrystsaveraging - 1/8" diameter

- quartz phenocrystsrounded averagingdiameter

are1/8" in

- trace pyrite along 1/16"wide carbonate veinlet.


14980 21+60S,53+20W Quartz-Feldspar Porphyry: 10- as per 14979- extensive silicification

near contact with Diorite.

14981 23*OOS,524-70W Mafic Volcanic: 37- fine-grained, light green- silicified- trace pyrite.

14982 23+808,53+OOW Intermediate Volcanic: 8- fine-grained, light green- foliated- minor limonite staining

along fractures- orientation 114764 0 N.

14983 10+705,46+OOW Quartz-Carbonate Vein: 15- 2" wide- in l 1 wide zone of

sheared mafic volcanics- trace pyrite- trace chalcopyrite.

14984 10+708,46+OOW Mafic Volcanics: 17 (55)- medium to coarse grained- sheared- carbonatized- silicified- limonite staining along




14985 Intermediate Tuff?- trace carbonate- weakly limonitic- trace sulphide.

12

14986 76+OOW/23+10N Sheared mafic volcanics 11-l" wide zone- quartz-ankerite veining- minor calcite- limonitic- no visible sulphides.

14987 1H-10S,27H-90W 2" Quartz Vein in Foliated 19Mafic Volcanics- prevalent iron oxide

staining- minor carbonate- .5% pyrite.

14988 7S,25*40W 6" Quartz Vein within Felsic Intrusive in Amphibolite- quartz is glassy- within a tonalite dike.

11

14989 3+608,261^ 18" x 6" Quartz Pod in Diorite- prevalent iron oxide

staining- glassy quartztrace to . 5% pyrite and pyrrhotite.

17



14990 23+82W,8+35N Brecciated mafic to inter mediate volcanics; narrow strongly gossaned section adjacent to a diorite dike or sill- trace - l % pyrite- numerous small vugs

infilled with limonite.

139

14991 314-95W,H-OOS Mafic Volcanics - amphi bolite- fine to medium grained- trace carbonate- trace pyrite- trace pyrrhotite along

fractures.

18 (24)

14992 15*70W,3*90N Felsic volcanics- weakly gossaned, highly

fractured with carbonate coatings

- several small, irregular quartz-ankerite veinlets

- trace disseminated pyrite,

556

14993 15H-45W,3*90N Mafic volcanics, highly silicified- found adjacent to an

irregular diorite dike- trace - l % pyrite and chalcopyrite, occurring as fine disseminations and in small quartz- epidote veinlets.

35



14994 13*60W,7*50N Sheared intermediate to felsic volcanics- predominantly quartz-

sericite schist (weakly foliated) with minor chlorite

- numerous ankerite j quartz veinlets (most barren)

- weakly carbonatized- trace - l% disseminated pyrite and arsenopyrite

- strongly gossaned- orientation 112/82'N.

114

14995 13*OOW,74-30N Sheared intermediate to felsic volcanics, as per 14994.

44

14996 164-30W,26*50N Sheared felsic to inter mediate volcanics- gossaned volcanics found between irregular sub volcanic dikes

- weakly foliated, trending 108 0

- minor quartz-ankerite veining near contacts

- trace - 3?; arsenopyrite, occurring as euhedral to subeuhedral crystals up to 1/8" wide

- weakly carbonatized- minor intercalations of

mafic volcanics.

56

l l l l l l l l ll l ll l l l l l l



14997 16*30W,26*50N Subvolcanic intrusive dikes 29intruding felsic to inter mediate volcanics- medium grained, massive; predominantly quartz (SO-70%) and feldspar (20-301;) with lesser ankerite (S-10%)

- trace pyrrhotite and arsen opyrite

- weakly carbonatized.

14998 le+SOW^e+SON Subvolcanic dikes as per 3414997- 1-51 arsenopyrite, trace

pyrite, occurring in euhedral crystals or small blebs.

14999 1H-OOW,4*65N

15000 29+60W,6+20S

Quartz-carbonate-epidote 1047 vein in mafic volcanics- 1-3" wide, irregular

trend- coarsely crystalline

sections- trace pyrite.

Intermediate Volcanic: 108- weathered surface - light

green- highly fractures- numerous random quartz

veinlets- no visible mineralization.



5037 7*50S,6*50W Plagioclase/Amphibole Phyric Intermediate Rock- possibly altered

intermediate volcanics- weathers medium green

to light brown- trace pyrite.

73 (17)

5038 7+50S.6+50W Quartz Vein Related to Diorite Intrusive- maximum of 18" wide- dips 46* to the north- quartz is glassy- trace pyrite.

11

5039 6*50W,7H-50S Quartz Vein:- varies from 0.6 1 - 2.5'

wide- randomly oriented? follows

contact between intermediate volcanics and Diorite intrusive


- trace pyrite

5040 6*50W,7*50S Quartz Vein:- as per 5039- few sulphide stringers, ^ 1/8" wide

- 0.5 - 1.01 pyrite- trace - Q.5% pyrrhotite- heavy limonite staining

along fractures

16



5041 6 +50*1, Intermediate Volcanic: 29- fine-grained, silicified,

light green- heavy limonite staining

along fractures- Q.5% - l.OS; pyrite in -

1/8" wide stringer, trace - D.5% pyrrhotite.

5042 59-i-50W,20*50N Intermediate Flow- mildly carbonatized

- slightly limonitic- trace pyrite- massive

5043 32*OOW,22*15N Mafic Flow- slightly limonitic- up to l% pyrrhotite.

8

5044 10S.3+50W

5045 108,3+SOW

Siliceous Host Rock of 10

Quartz Carbonate Vein

- described in 14966- channel is 1.4' long- crosscut by numerous

quartz carbonate veinlets- trace pyrite.

Quartz/Carbonate Vein < 5- rock sawed channel

sample of vein described in 14966

- very clean quartz, ankerite and calcite

- trace pyrite.




5046 2*40S,6W

5047

5048 JLO+OOSfS+SOW

5049 lO+OOSjS+SOW

Shear Zone with Quartz and < 5 Carbonate Flooding- in intermediate rock

(sheared)- trend is 056/61W.

Felsic Volcanic: 33- channel sample - 1.7'

long- sheared fine-grained,

light green- silicified near contact with quartz-carbonate vein

- weak to moderate carbon- itization

- few quartz-ankerite veinlets - 1/8" wide near contact


- no visible mineralization.

Quartz-Carbonate Vein: 8- calcite and ankerite present

- 1/16" - 1/8" red-brown rind on surface

- no visible mineralization- as per 14966- sample length - 1.7' long.

Felsic Volcanic:- as per 5047- no visible mineralization- sample length - 0.9' long

<5



5050 Quartz-feldspar-calcite pod or vein within brecciated mafic volcanics- irregular trend, up to

3" wide- trace pyrite- strongly carbonatized.

5051 Gossan zone in brecciated 199 mafic volcanics- 2' exposed width- up to 51 pyrite ^ pyrrhotite, with trace chalcopyrite and malachite

- sulphides occur in small blebs and stringers up to 1/8" wide

- irregular carbonate veinlets- heavily limonitic, numerous

small vugs.

5052 94-05W,24-90N Gossan zone in brecciated mafic volcanics, as per 5051.

35

5053 Quartz vein or pod in massive mafic volcanics- 2-6" wide, 1.5' exposed

length- coarsely crystalline milky

quartz; barren; limonitic stain locally.

<5


Assay Resulpp ppb Au (Check)

5054

5055 12+17E,23+20N

Mafic volcanics (amphi

bolite)

- weakly gossaned section about 2' wide, possibly weakly sheared (trending roughly 020 0 )

- trace - l S pyrite - strongly carbonatized.

Brecciated quartz-feldspar porphyry with a quartz matrix, as per 14860- large fragments up to

6" wide, highly angular- quartz matrix is strongly

gossaned; contains trace - 21 pyrite in small vugs.

46 (39)

5056 12*17E,23*20N Quartz-feldspar porphyry < 5 fragments from the breccia described in 14860- ID-15% phenocrysts (mostly

feldspar) in a fine grained, greenish-grey matrix

- trace - l * disseminated pyrrhotite.

5057 Mafic volcanics containing small blebs of pyrite and pyrrhotite (trace - ^ total sulphide)- several small carbonate

stringers also contain trace sulphide

- weakly gossaned.


5058 63*50E,394-50N Gabbro 14 ^5)

- slightly silicified- minor epidote- magnetic, massive- trace pyrite.

APPENDIX C

ROCK SAMPLE ASSAY CERTIFICATES

ACCURASSAY UBORATORIES LTD.P.O. BOX 604

KIRKLAND LAKE, ONTARIO, CANADA P2N 3J5 TEL.: (705) 567-6343

President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Chem (Ont.), c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of Analysis19395

Kr. K.J. HodgeGeocanex Ltd.1003 - 34 King Street EastToronto, OntarioK5C-1E5

SAMPLE NUMBERSAccurassay

439180 439lSI439182439183439184439185439180439187439188439189439189439190439191439192439193439194439195439196439197439198439198439199439200439201439202439203439204439205439206439207439207

Customer

14805146061480714808148091481014811148121482414625148251482614827148281482914830148311483214833148341483414835148361483714838148391484014841148421484314843

Gold ppb

6158678

107

107

267

10179668

1613117

1178

163024721011

Date: July 29

Check

Vork Order Project

Gold Oz/T

'. 0 .002 ^.002 ^.002 ^.002 ^.002 ^.002 ^.002 ^.002 ^.002 ^.002 ^ . 002 ^.002 ^.002 O), 002 ^.002 ^.002 ^.002 ^.002 ^.002 <0.002 < 0.002 <0.002 ^.002 <0.002 <0.002 <0.002 <0.002 ^.002 0.002 <0.002 x'0.002

: P080211: NORTH CARIBOU

Check

Check

Per:

ORIGINAL

ACCURASSAY LABORATORIES LTD.P.O. BOX 604


President: Dr. GEORGE DUNCAN, M.SC., PH. o., c. Chem (Om.i, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of flnalysis19396

Mr. H.J. HodgeGeocanex Ltd.1003 - 34 King Street EastToronto, OntarioK5C-1E5

SAMPLE Accurassay

439206439209439210439211439212439213439214439215439216439216439217439218439219439220439221439222439223439224439225439225

NUMBERS GoldCustomer ppb

14844 1114845 914846 914847 1114848 614849 1114850 1014851 2114852 814852 514853 5914854 814855 13814856 4414857 5414858 1514859 814860 40214861 714861 6

Date: J uly 29

Page: 2

_____1988.

Work Order # : P080211 Project : NORTH CARIBOU

Gold Oz/T

(0.002 (0.002 (0.002 (0.002 (0.002 (0.002 (0.002 (0.002 (0.002 (0.002 Check0.002 (0.0020.004 (0.0020.002 (0.002 (0.0020.012 (0.002 (0.002 Check

Per:

ORIGINAL



President: Dr. GEORGE DUNCAN, M .SC., ph. D., c . Chem (Ont.i, c. Chem (U.K.), M.C.I.c., M.R.S.C., A.R.C.S.T.

Certificate of AnalysisMr. K.J, Hodge1 7 J T *i vfc-5; "i: /T Tt fc-J V l . T ;"!s.*"-v."fc-* t^ li c-yk j.,* t- ^* *

K5C-3E5

SAKPLE NUKBERS Accurassay Ci

439430439431439432439433439434439435439436439437439438439439439439439440439441439442439443439444439445439446439447439448439446439449439450439451

jt c-i i--, f C' f-,4oyf5^ 439453439454439455439456439457 43945?

.J -r .dgt.-"*

ing Streettar lo

omer

148621486314864148651486614867148681 48691487014871148711487214873148741487514876148771487814879148801488014881148821488314884

East

Goldppb

6126f,

167

261955G5

\T*X1 5

6555

^i77^e

15PJ14885 Result to be1488614887148881488914889

4525•\ 51111

Page : 1Date: August 3 1 9 88

Work Order # : P080222Project ; North Caribou

GoldOz/T

a) . 002< 0.002< 0.002^.002\' 0.002< 0.002< 0.002vO.002^.002< 0.002< 0.002 Checkv 0.002a*. 002< 0.002<0.002< 0.002\' 0.002^.002<0 . 002^.002< 0.002 Check^.002< 0.002< 0.002s' 0.002forwarded^.002< 0.002\0 . 002^.002< 0.002 Check

J /lPfl, y * UAA^CC^

ORIGINAL



President: Dr. GEORGE DUNCAN, M .SC., PH. D., c. Chem (Onu, c. Chem IU.K.I, M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of AnalysisKr. H.J. Hodge Page #1Geocanex Ltd.

1QCn7 1003 ' 34 K ing Street East Date:06/05/68_________19 ——— l d DU i Toronto, OntarioK5C-1E5 Work Order F080222

Project: Korth CaribouAssay results are as follows:

SAMPLE NUMBER Original Gold Gold GoldAccurassay Customer ppb ppb Oz/T439453 14885 Result to follow 284 0,008

f± ^ rw * m ^\ f \~^^*\r - **^VX*^^^.Per:

ORIGINAL



President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Chem (Om.i, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of AnalysisPage.;

Mr. H.J. Hodge Geoosnex Ltd.1003 - 34 King Street East

19451 Toronto, Ontario K5C-1E5

SAKPLE NUMBERS issav Customer

•1 '.'•Ci '"' K C t*-'S H vJU

439459439460439461439462439463

439466439466439467439468439469439470

71439471

14890148911489214893148941489514896148971489814898148991490014901149021490314903

Gold ppb

AugustDate: 19

Vork Order # Project

Gold Oz/T

P080222Korth Caribou

C5C5C5C55

1216321717131013211717

CO. 002CO. 002CO. 002CO. 002CO . 002CO. 002CO. 002CO. 002CO. 0020 . 002CO. 002CO. 002CO. 002CO. 002CO. 002CO. 002

Check

Check

Per:

ORIGINAL



President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Chem (Onu, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of AnalysisKr. H, J. Kods-fcGeocarifcx Ltd.1003 -- 34 King Street EastToront o, Ontar i oK5C-1E5

Date: August 9

SAMPLE IWKBEES Ac-cur&.sss.y Customer'

14904149051490614907 J 4 90614909149101491114912149131491314914149151491614917 1491 d 34919 14920 349I-!! 14922 14922 34923 j 49241492514926149271492814929 l 4930 14931 14933

439636439637 43963S 439639 439040439641439642439643439643439644439645439646 43964?'

439643 439640 439650,'. r,' f i .": r-, ',

439653

439657439653439659439666439661439663

Work Order Project

P080232 North Caribou

Goldppb

9106

12^*C55

<5<55

<556

406

31955

•(535225r.

xT*3630188

65

16

GoldOs /T

^.002\' 0.002(0.002(0.002^.002x" 0.002^.002(0.002(0.002< 0,002^.002(0.002•(0.002'(0.002^' 0.002^.002< 0.002< 0.002^' 0.002< 0.002C 0.002•(0.002'(0.002(0.002(0.002^.002v' 0.0020 . 005(0.002'(0.002x' 0.002

Check

Check

Check

Per:

ORIGINAL



President: Dr. GEORGE DUNCAN, M.SC., Ph. o., c. chem (Om.i, c. Chem (U.K.), M.C.I.c., M.R.S.C., A.R.C.S.T.

Certificate of Rnolysis19530

Mr. H.J. HodgeGtocaijfex Ltd .1003 - 34 King Street Ea&tToronto, OntarioKJJC-1E5

H c c u r 6. s s f j. v

439662439663439664439665439666439667439666439669439670439670439671 4396^2 4396"' 4396^4

'6439677 439675 439679 439679

Customer

1493214933149341493514936149371493814939149401494014941149421494314944149451494614947149481494914949

Gold ppb

Page :

Date: Angu&t 9

Work Order # Project

Gold Oz/T

P0602S2 Nortli Caribou

102987

118

111389S

215012303713131015

(0 . 002(0.002(0.002(0.002(0.002(0.002(0.002(0.002(0.002(0.002(0.002(0.002(0.002(0.002(0.002(0.002^.002(0.002(0.002(0.002

Check

Check

Per:

ORIGINAL



President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Chem (Om.i, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of AnalysisMr. H.J. Hodge Geocanex Ltd.

19659 1003 - 34 King Street East Toronto, Ontario M5C-1E5

SAKPLE NUMBERS Accurassay Customer

439776439777439778439779439780439781439782439783439784439785439785439786439787439788439789439790439791439792439793439794439794439795439796439797439798439799439800439801439802439803439803

5001500250035004500550065007500850095010501050115012501350145015501650175018501950195020502150225023502450255026502750285028

Page: l

Date: August 18 1988

Work Order * : P080236 Project : NORTH CARIBOU

Goldppb

1258187131016526325154177111314967

30324

6107

330684228311315111320

GoldOz/T

0.0040.0020.003^.002tt. 002^.0020.0020.002^.0020.0040.0050.003

*C0.002^.002^.002^.002^.0020,009^.002^.002^.0020.0100.002^.002^.002^.002^.002^.002*CO . 002^.002^.002

Check

Check

Per:

Check

ORIGINAL



President: Dr. GEORGE DUNCAN, M .SC., Ph. D., c . Chem lom.), c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of flnalysisMr, H.J. Hodge Geocanex Ltd.

19660 1003 - 34 King Street EastToronto, M5C-1E5

Ontario

SAMPLE NUMBERS Accurassay Customer

439804439805439806439807439808439809439810439811439812439812439813439814439815439816439817439818439819439820439821439821439822439823439824439825439826439827439828439829439830439830439831

502950305031503250335034503550361495014950149511495214953149541495514956149571495814959149591496014961149621496314964149651496614967149681496814969

Page; 2

Date: August 18 19 88

Work Order * : P080236 Project : NORTH CARIBOU

Goldppb

1314209

1549291229201014291521619662643391811181257

202108

119

10

GoldOz/T

^.002^.002^.002^.002^.002^.002^.0024.Q , 002^.002^.002<0,002<0,002<0.0020.004^.002<0,0020,002^.002^.002<0.002<0.002<0.002<0,002^.0020,0020,006<0.002^.002^.002<0.002<0,002

Check

Check

Check

Per:

i Dr. G. Dunca Q

ORIGINAL



President: Dr. GEORGE DUNCAN, M.SC., PH. D., c. Chem (Ont.i, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of AnalysisMr. H.J. Hodge Geocanex Ltd.


SAMPLE NUMBERS Accurassay Ci

439832439833439834439835439836439837439838439839439839439840439841439842439843439844439845439846439846

Page: 3

Date: August 18 1988

Work Order # : P080236 Project s NORTH CARIBOU

omer

1497014971149721497314974149751497614977149771497814979149801498114982149831498414984

Goldppb

1875455163710(.51011181210378151755

GoldOz/T

0.0050.0020.002^.002^.002^.002^.002^.002^ . 002O). 002^.002^.002^.002^.002^.002^.0020,002

Check

Check

Per:

ORIGINAL



President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Chem (Ont.i, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of flnalysisMr. H.J. Hodge Geocanex Ltd.



439975439976439977439978439979439980439981439981

1498514986149871498814989149901499114991

Gold ppb

1211191117

1391824

Page:

Date: August 19

l

198JL

Work Order Project

Gold Oz/T

^ . 002 ^.002 ^.002 ^.002 <0.002 0.004

<0.002 < 0.002

P080243 North Caribou

Check

Per:

ORIGINAL



President: Dr. GEORGE DUNCAN, M.SC., PH. D., c. Chem (Ont.i, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of AnalysisMr. H.J. Hodge

•1 Q 71 1 Geocanex Ltd^L. \s t •L- iJl* M f* f* f-, f** /t v *1003 - 34 King Street East

Toronto, Ontario M5C-1E5


429161429161429162429163429164429165429166429167429168429169429170429170429171429172429173429174429175429176429177429178429179429179429180429181429182429182429152429153429154429155429156

503750375038503950405041504250435044504550465046504750485049505050515052505350545055505550565057505850581499214993149941499514996

Gold ppb

73 17 117

16 2968

10 C5 C5 C5 338

C56

199 35 C5 C5 46 39C56

C5 14

556 35114 44 56

Page : lDate: August 28 8S ——

Work Order Project

Gold Oz/T

P080247 Worth Caribou

0 CO CO ("OCO COW CO

CO

0 CO CO CO CO CO CO COco co0co0co0

.002

.002

.002

.002

.002

.002

.002

.002

.002

.002

.002

.002

.002

.002

.002

.002

.006

.002

.002

.002

.002

.002

.002

.002

.002

.002

.016

.002

.003

.002

.002

Check

Check

Check

Check

Per:

ORIGINAL



President: Dr. GEORGE DUNCAN, M.SC., ph. D., c. Chem (Ont.l, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of AnalysisMr. H.J. Hodge

1Q71p Geocanex Ltd, A ^ •Lt 1003 - 34 King Street East

Toronto, OntarioK5C-1E5


429157429158429159429160

14997149981499915000

Gold ppb

2934

1047108

Date: August 28

Page i 2

————— 1 986——

Work Order 4t i P080247 Project : North CaribouGold Oz/T

^.002 ^.0020.0300.003

Per:

ORIGINAL

Ministry of.Northern Development

Report of Work |(Geophysical, Geological,! Geochemical and Expenditures)—"u

Mining Act

'Instructions: — Please type or print. ; — If number of mining claims traversed

exceeds space on this form, attach a list. Note: — Only days credits calculated in the

"Expenditures" section may be entered in the "Expend. Days Cr." columns.

- Do not use shaded areas below.Type of Sufvdy(s)

Claim Holder(s)

Address

Survey Company

Name and Address

Geological

see attached

c/o 1003-34 King Street

Geocanex Ltd.of Author (of Geo-Technical report)

E. Timoshenko R. R. #

[Township or Area S)g a/Si-* t* *2O6f

\ Randa!!* KeeyaskProspector's Licence No.

see attached

East, Toronto Ontario M5C 1E5iDate of Survey (from A to) total Miles of line Cut

9 Bramptom, Ontario L6T 3Z8Credits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:

Enter 4 0 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here *

Airborne Credits

Note: Special provisionscredits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days perClaim

- —— ——

40

Days perClaim

Days per Claim

Mining Claims Traversed (List in numerical sequence)

Expenditures (excludes power stripping)Type of Work Performed

Performed on ClaimU)

Calculation of Expenditure Days Credits

Total Expenditures

InstructionsTotal Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

Total number of mining claims covered by this report of work.

Certification Verifying Report of Woril hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of WorR ajfiexcd hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person Certifying

H.J. Hodge 1003-34 King Street East Toronto, Ontario M5C 1E5Date Certified

May 25/89Certified by (Signa

CFnT36? 165/lgl

POWER EXPLORATIONS

\ OWNER

10078871-O07888

r 100788910078901007891100789210078931007894

; 1007895100789610078971007898100811210081131OO811410081151008116100811710081181008119100797710079781007979100798O10079811007982100798310079841OO79861OO79871O07988100798910079901O079911007992100799310080321008033100803410080351008036100803710080381008039100804010080411O080421008043100804410080451O080461008O4710080481008049

C.C.C.C.C.C.C.C.C.C.C.C.C.C.C.C.C.C.C.C.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.

Darveau # K 20388DarveauDarveau *DarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauRobert # E 29771RobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobert # E 29771RobertRobertRobertRobertRobert

CLAIM OWNER

100805010080511O0805210080531008054100805510O80561008057100805810080591008060100806110079351007936100793710079381007939100794010079411007942100794310079441007945100794610079471O07948100810210081031008104

J.J.J.J.J.J.J.J.J.J.J.J.R.R.R.R.R.R.R.R.R.R.R.R.R.R.R.R.R.

*. ~ -Robert -- (T ^Ci ,;' J \RobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertDarveau # S 6095DarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveau

Ministry ofNorthern Developmentand Mines

Geophysical-Geologlcal-Geochemical Technical Data Statement

Ontario

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

i(dB

Type of Survey(s). Township or Area. Claim Holder(s).—

Geological

Keeyask Randall

Please see attached

Survey Company Geocanex Ltd.Author of Report E.D. Timoshenko

Address of Author R.R. 3 9 Brampton, Ontario L6T 3Z8

Covering Dates of Survey July 14th to August 17th. 1988(linecutting to office)

Total Miles of Line Cut 5 4 - 8————————————^—————

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical—Electromagnetic.—Magnetometer——Radiometric———Other——————

DAYS per claim

Geological. 40

Geochemical.

AIRBQRNE CREDITS (Special provision credits do not apply to airborne lurveyi)

Magnetometer. .Electromagnetic(enter days per clai

DATR- May 25th. 1989 SIGNATURE:Authol

Res. Geol.. . Qualifications CX-

Previous Surveys File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

t PJL e a s et t s e et i a ttaehedt t tttti (prefix) (number)

i

TOTAL CLAIMS.

837 (65/12)

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

Number of Stations —————————————————————————Number of Readings — Station interval -....-..———---.—-—..—-—————-——-——-Line spacing,—————Profile scale——————-—-^—.—-.———-——-^——^-,—————.———^—-———^.—.—.Contour interval.

Instrument ————————Accuracy — Scale constant. Diurnal correction method.

o

2N H

HI-H

*-HS&BM i—(w:w q *D

Base Station check-in interval (hours). Base Station location and value —-—-

ELECTROMAGNETIC

Instrument .

Coil configuration Toil separation

Accuracy.Method:Fr^qiicnry

D Fixed transmitter D Shoot back D In line D Parallel line

(specify V.L.F. station)Parameters measured.

Instrument.Scale constant.Corrections made.

Base station value and location.

Elevation accuracy-

Instrument ———————————————————————————————————————————————— Method D Time Domain D Frequency Domain Parameters - On time __________________________ Frequency —————

—Off time——-——,—————————————— Range.— Delay time ——————————————————————————— Integration time ——————————————————.

Power.Electrode array _ Electrode spacing . Type of electrode .

SELF POTENTIAL Instrument________________________________________ Range.Survey Method .—————————-————-————-—..—.—^-..——.—-^—.—-^.—-.-^..—

Corrections made.

RADIOMETRIC

Instrument.Values measuredEnergy windows (levels)——^————-..-——————^-———.———^——^^————Height of instrument____________________________Background Count, Size of detector———————^—————.———————————.—^^...^.^^....-^—.Overburden ——.-^———^—————^—^-^-^——^^——^——^-——.^——.^-——^

(type, depth - include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.)Type of survey—————————————————————————Instrument -——————————————-.-^^——^—Accuracy.———————————-—————^—————Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYS Type of survey(s)————. Instrument(s) ——————

{specify for each type of survey) Accuracy,————————————^^

(specify for each type of survey)Aircraft used.———^——^———————————^—.————^——-.—Sensor altitude.Navigation and flight path recovery method.

Aircraft altitude______________________________Line Sparing Miles flown over total area———————^-—————.^-——^—-—Over claims only.

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.

Total Number of Samples. Type of Sample.

243 samplesrock

(Nature of Material) Average Sample Weight________

Method of Collection.———. channel, grab

Soil Horizon Sampled. Horizon Development. Sample Depth——^-. Terrain————————

Drainage Development———————————— Estimated Range of Overburden Thickness.

ANALYTICAL METHODSValues expressed in: per cent

p. p. m. p. p. b.

D Q O

Cu, Pb,

Others—

Zn, Ni,

Au

Co, Ag, Mo, As.-(circle)

Field Analysis (. .tests)Extraction Method. Analytical Method- Reagents Used——

Field Laboratory AnalysisNo. ———————— .tests)

SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)

Mesh size of fraction used for analysis -150

Extraction Method. Analytical Method . Reagents Used.——

Commercial Laboratory (—————————————tests) Name of Laboratory^. Extraction Method—— Analytical MpthnH fire assay,atomic absobtion

Reagents Used_______aqua regia—————

Accurassay Ltd.

pulverize_____

GeneraL General.

4 s l*'

^' i :.CLAIM *^:

'; vr^07887 Y'

rvl'O07889 /"''" UO07890 '..,/'Ht)0789if i-*O~O7892/l 007893 "^1x1*607894 x -

rV4r007895 ^Ix4u078961x1007897 xVxl007898 Xv 10081 12vi"b08113VXD08H4vfodsiis•11D08116^08117^0081181/10081191^007977td'0079781^007979t.4 007980vi 007981i i007982^10079831x1007984•10079851x10079861^0079871^007988t^.0079891/1007990/l 007991i 1007992u-l'O07993^1008032t/1008033V4'OPS034txl008035^1^)08036tl^p08037H008038tlp08039vi 0080 40Vl'0080410.^08042V1008043L/1008044Jo'008045^0080461^608047J/008048/1O08049

*'' ! '' \ \- , r.- X-.

OWNER M.-. . , ^

C.C.c.c.c.c.c.c.c.c.c.c.c.c.c.c.c.c.c.c.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.

DarveaulX # K 20388 X Darveaui/ ix-""Darveau^ ** .Jil—^.Darveau/ x tS—Zj!-Darveaui/ tyDarveauu/ ,'-^Darveau i/ . - ~-DarveauiX^^ .- Q ~~Darveaui/ , ,^L^~Darveau i/ yDarveaut^ x /^4Darveau Xx fc tyDarveau ^ V'*-Darveau. x l^-'/'^Darveau L iiXDarveau x iXDarveau -/^ uX/Darveau,/ s 1^Darveau' p^.Darveau v/ ^y^Robert , f "E 29771 \X?Robert., j 1^'Roberti -x - /^Robert- '" v SRobert 1 x \ yRobert 'iX^Robert' ;^ u'Robert/ l ix^/Robert' iXRobert, jjXRobert, **^xRobert f^Robert!/' ffy-Robert^x" ^1~-Roberti/^ \SRobertu/^ ^ 7Roberts/^ vXRobertiX ^^Robert.Xx ^Robert/ X,Robert- -x y Xx"/Robert 1X VyvRobert x y r 'Robert^/7/ tX/'Roberf.//' ^ ^ .i.vX ...Robert ,X X^xRobert x ixy.Robert 1-'// ^X .RobertiX/ 5^-X^Robert'/ # E 29771 ^XRobert. U-^xRobert t// X;Robert1 ' y iXxXRobert-" 7 iXXRobert i// IX'^

POWER EXPLORATIONS

3o

lo

89 r

CLAIM

100805O/1 00805 1-7 /1008052//1008053/ 10080541/1008055//1008056'X1008057V/1008058//1008059/-lOOSdSO'V10080611-'1007935V/vlb07936/1007937i1007938/1007939 x1007940100794 1/1007942^1007943/1007944-i 007945 /^1007946V/1007947/1007948:1008102' 1008103/1008104 1/

OWNER "': f J-

J.J.J.J. J.J.J.J.J.J.J.J.R.R,R.R.R.R.R.R.R.R.R.R.R.R.R.R.R.

Robert/ ^ ( (T T^V;Robert/,Robert t/Robertv/ Robert t/Robert Robert Robert fRobert i/'Robert '••yRobert VRobert i/yDarveau^/ # S 6095Darveauvx/7Darveau i/

''"Irx/l/V t/i/'i^-L^- w/^)Kn"

i ^^

Darveauv/T /^Darveaux/ ^^*"Darveau i/ x ix*Darveau i/ x ; 'A..Darveau^// j j.^^Darveau lxxX ' U,Darveau t,^ ,^-Darveau* x

v^1 ^-

Darveaur/ /^Darveau,// ; ^^Darveau/ x i/^Darveau/ i/Darveau.,/^ '^aDarveau t/ K,

POWER EXPLORATII19

CLAIM

1O07887100788810O78891O078901OO78911OO789210078931OO78941O07895100789610078971007898100811210081131008114100811510081161OO81171OO81181OO811910079771O079781O079791O07980100798110079821O07983100798410079851O079861OO79871007988100798910O79901OO799110079921O07993100803210O8O3310080341008035100803610080371O08O381008O3910080401OO804110080421008043100804410080451008046100804710080481OO8O49

OWNER

C.C.C.C.C.C.C.C.C.C.C.C.C.C.C.C.C.C.c.c.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.J.

Darveau # K 20388DarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauDarveauRobert # E 29771RobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobertRobert # E 29771RobertRobertRobertRobertRobert

Ministry otNorthern Developmentand Mines

Ontario

Technical Assessment Work Credits

AMENDED

Oil*

August 21. 1989Minln WorkW8S

File

2.12537o Recorder'* Report of

fe-104

Recorded Holder

"Township or AreaR. DARVEAU

RANDALL LAKE AND KEEYASK LAKE AREASType of survey and number of

Assessment days credit per claim Mining Claims AssessedGeophysical

Electromagnetic .

Magnetometer,

Radiometric —.

Induced polarization .

Other ———————-

.days

.days

.days

-days

.days

Section 77 (19) See "Mining Claims Assessed" column

Geological .——————-———————————days

Geochemical ———^————-——-———.-——..days

Man days [~]

Special provision SB

Airborne f"!

Ground

f~i Credits have been reduced because of partial coverage of claims.

f~| Credits have been reduced because of corrections to work dates and figures of applicant.

Special credits u nder s ection 77 (16) for the following mining claims20 days PA 1007935, 1007937, 1007939-40, 1007944-45, 1007947-48, 1008102,1007942

PA 1007936, 1007941, 1007943, 100810410 days PA 1007938, 1007946 5 days PA 1008103

No credits have been allowed for the following mining claimsnot sufficiently covered by the survey 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; Geologocal - 40; Geochemical - 40; Section 77(19) -60.

(28 (8S/12)

Ministry ofNorthern Developmentand Mines


AMENDED

Oat*

August 21 ,

Pila

2.12537Winino Reorder'. R.pon ol

1989^903-104

Recorded Holder

J. ROBERTTownship of Area

RANDALL LAKE AND KEEYASK LAKE AREAS.Typ* of survey and number of

Assessment days credit per claim Mining Claims AssonadGeophysical

Electromagnetic.

Magnetometer.

Radiometric —

Induced polarization.

Other —.-———-———

-days

.days

.dayt

.days

.days


Geological ___________________ dayj

Geochemical ————————————————— days

Man days Q

Special provision ffi

Airborne

Ground

Q] Credits have be*n reduced because of partial coverage of claims.

l O Credits have been reduced because of corrections to work dates and figures of applicant.

Special credits under section 77 (16) for the following mining claims

20 days PA 1007977 to 988 incl., 1007991, 1008032, 1008034 to 042 Incl1008044 to 061 incU 1007993

15 days PA 1007989, 1007992 10 days PA1007990, 1008043 5 days PA 1008033

No credits have been allowed for the following mining cJalmsnot sufficiently covered by Ihe survey Q insufficient technical data filed

The Mining Recorder may reduce Ihe 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; Geologocal. *0; Geochemical -40; Section 77(19) -60.

(28 (8V12)

Ministry otNorthern Development


Ontario Dm

August 11,2.12537

Minlno Recorder's Report o)198!)Worfeo3-104

Recorded Holder

C. DARVEAUTownship or Area

RANDALL LAKE AND KEEYASK LAKE AREAS.Type of survey and number of

Assessment days credit per claimGeophysical


iO fieolngical HVJ days

Man days Q Airborne [~j

Special provision ^ Ground ^^

f~) Credits have been reduced because of partial coverage of claims.

l l Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

PA 1007895

Special credits under section 77 (16) for the following mining claims

30 days PA 100788920 days PA 1007887-88, 1007892,15 days PA 1007891, 1007893, 100 10 days PA 1007890, 1007898, 10C 5 days PA 1008119

1007896, 1008113 to 117 incl.7897 8112, 1008118

Mo credits have been allowed for the following mining claimsfkj) not sufficiently covered by the survey Q insufficient technical data filed

PA 1007894

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; Geologocal -40; Geochemical - 40; Section 77(19) -60.

628 (85/12)

CLAIM OWNER

1008050100805110080521008053100805410080551008056100805710080581008059100806010080611007935100793610079371007938100793910079401007941100794210079431007944100794510079461007947 1OO7948100810210081031008104

J- Robert J. Robert J. Robert J. Robert J. Robert J. Robert J. Robert J. Robert J. Robert J. Robert J. Robert J. Robert R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau R. Darveau

# S 6O95

Mining Lands Section 680 Bay Street, 3rd Floor Toronto, Ontario MSS 1Z8

Telephone: (416) 965-4888

Your File: Our File:

W8903-104 2.12537

September 26, 1989

Mining RecorderMinistry of Northern Development and MinesCourt HouseP.O. Box 3000Sioux Lookout, OntarioPOV 2TO

Dear Sir:

Re: Notice of Intent dated August 21, 1989 for Geological Survey submitted on Mining Claims PA 1007895 et al In Randall Lake and Keeyask Lake Areas.

The assessment work credits, as listed with the above-mentioned Notice of Intent have been approved as of the above date.

SEP 2 8 1989

Please Inform the recorded holder of these mining claims and so Indicate on your records.

Yours slncerelyi

W.R. CowanProvincial Manager, Mining LandsMines fi Minerals Division

LJS:eb Enclosure

cc: Mr. G.H. FergusonMining and Lands Commissioner Toronto, Ontario

C. Darveau l J . Robert c/o 1003 King street E. Toronto, Ontario M5C 1E5

E. Tfmoshenko R R 19Brampton, Ontario L6T 3Z8

Resident Geologist Sioux Lookout, Ontario

9i 0 00'

52 0 52'30"—

100803511006036' 1008039 11008042. IOO8056 |10080;S9 IQ079BI 11007984

'—U4--1008037 JlOOB03B|lOOB043Jiooe055 jlOOB06jTo07980 "fl007985 j 1007988)1007.993

' ' ' .-l————-J———————J- ———

^..-. _,_ .10080461008051 fioOBOS3 i007977 IO07978

)I008047JI008050|I008052 Po

l i/ 720021 ! 720022 l

l j- - -^ j

720O3I ! 7Z0030 J 7 2002S

. - — -~

14 13- 12'

53B14SE088) 200

LEGEND

HIGHWAY AND ROUTE No

OTHER ROADS

TRAILS

SURVEYED LINES:TOWNSHIPS, BASE LINES, ETC., LOTS. MINING CLAIMS. PARCELS; ETC

UNSURVEYED LINESLOT LINES

PARCEL BOUNDARYMINING CLAIMS ETC

RAILWAY AND RIGHT OF WAY

UTILITY LINES

NON PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS

SUBDIVISION OR COMPOSITE PLAN

RESERVATIONS

ORIGINAL SHORELINE

MARSH O R MUSKEG

MINES

TRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

E OF DOCUMENT

PATENT. SURFACE 8. MINING RIGHTS

. SURFACE RIGHTS ONLY.....

. MINING RIGHTS ONLY .....

LEASE, SURFACE t, M INING RIGHTS-.

" .SURFACE RIGHTS ONLY......

" .MINING RIGHTS ONLY........

LICENCE OF OCCUPATION ............

SYMBOL

.. ...., O

. .... . . B

....,......... O

................ B

............ - . T

ORDER IN-COUNClL .................. . . .. ..... ...... OC

RESERVATION ,,,,.,.,,. ...,. ......... ............ (J)

CANCELLED __............. ... , ..... . .. . ®

SAND&GRAVEL .......:...,...\...... ....-. . 0

NOTE: M INING RIGHTS IN fABCBLS *-AT(NTED*WiQK TO MA* 6 1913. VESTED IN ORIGINAL PATENTEE B' THE PUBLIC LANDS ACT. *SO 1B7Q CHAP 380, S6C 6 3 S uBSEC l

REFERENCESAREAS WITHDRAWN F ROM DISPOSITION

M.R.O. - MINING RIGHTS ONLY

S.R.O. - SURFACE RIGHTS ONLY

M.+ S. -MINING AND SURFACE RIGHTSP- ft P?g/ ' O-""JW-v

Description Order No. O at* D opowiion * Fit*

/s 1 1 1 ft

/'F-JI./^'" J-~- x

\

SCALE: 1 INCH * 40 CHAINS

i OOO 2OOQ 60OO 8OOO

O JOG METRES

1DOOi l KM

7 OOO (2 KM

AREA

RANDALL LAKEi

M.N.R. ADMINISTRATIVE DISTRICT

SIOUX LOOKOUTMINING DIVISION

PATRICIALAND TITLES/ REGISTRY DIVISION

KENORA ( PATRICIA. PORTION)

B.Ch.

Ministryof. LandNatural .' Management

.. Resources- BranchOntario

Dm FEBRUARY, 1984.

G-2I82

Spruce, Muskeg

Property' Thick!

Tamarack,/ Muskeg i

Spruce, Birch, *t- Alder ± Tamarack , x

Spruce,Birch j

BalsamSpruce, ForestSpruce

Ta ala rae k uskeg LOCATION MAP

Birch, Alder/Spruce

-C-

Open 0 -v , Spruce \o on boulders^

Spruce ± Birch on

81 Bouk ers o

Spruce, ± Birch

ylv Sprucef Spruce t ~

i ^ Spruce 'T.L.5200N

5000N - 14831-6 l 2a/Spruce,x'Ql^^k-

Spruce,± Birch ± Poplar

± Sand ± Boulderst M us teg s

Spruce/ t

Spruce t t Tamarack

Spruce \

Spruced

BalsamSpruce, Balsam, Birch

± Poplar on Sand S

SpruceISandSpruce,.

Birch Q 2a,ep,3il " 2oSpruce, Birch± fDoplar, Balsam on Sand t

Spruce f Birch *Alderpruce Balsam, Birch 2a x- 2

4 x 2a x

\ \ \ Spruce

xSpruce

Balsam i BirchSpruce i Birch

MuskegSpruce

Balsamy Spruce

Birch t Balsam

tAlder

l l Spruce /'n ' ).:Balsam, Birch

Poplars S pruce, i [ - ± .

' M uskeg 'Balsam, Birch 'Poplar

14871-5(6) Spruce ,. \

Spruce/ .alsam i/

/#lder s "Spruce "X ' ^ r- ^ \ Poplai^Balsam Spruce -t- Balsam

t Aldery I4ISI"^ W837-7 Marsh/ 14908--* W838-8

I4909-C5fc Spruce

Birch14841-24 ,

14910-5 ,l49ll-<5 /

' Poplar, . f.. ' Balsam, I0f -

2a,5bJ tOj,py,po

t Spruce, ± Jack Pine

Balsam\ Balsam Aider

T. L. 2000 N

DETAIL AREA l2o,(8a?)5b,4a C30I4883-15

014884-5 014891^5

Spruce /x//'2a,IOf 2h,lOf.(intbx) Caribou River ,* Jack Pine,

Poplar, Balsam

x 2h,IOf? d!kes

2h,f

14867-714868-26 414869-19

14890-*5

x 14885-28414886-4514887-23 14 868-* 5 14869-

Open SpruceTamarack Muskeg

Spruce Tamarack x Muskeg

I4B46-9 14845-9 l

sh. 2a,3o ? 5c

cc,ank/7 Poplar. "

Spruce,Jack Pine, lolic/

X ' Drtnlnr r\nPopla r, Birch,Spruce, Alders

Poplar on , Sand a Boulders pug (Of,2h

' B . L. 000Birch,a Alders Poplar,Birch.Spruce a14863-12

14864-6I48O5-5

, 14866-16.. 2o,ft?),IOo Poplar,\Birch, Spruce a,Elders

sPoplar, Spruce,

Birch, Alders j on Boulders-

Poplar, CD pineAlder Bo Spruce

os f Spruce ± Birch ± Aiderss l4927-36

x f ±Tamarack M929-i8i N \L l ; 14914-5 .49,5-6 I0j2,.ll O4i.j - S^\49\6-4Q

Boulder-^Ridge

LEGENDPoplar, Birch,Poplar, Spruce,Spruce a Alders s.on' Birch , Alders

Grid line with 100 foot stations

Claim post and line

Stream , swamp , lakeshore

Bush road

i / Boulders-N \/

Poplar, Spruce, Birch a Alders

Small Spruce

/and Jack Pine/ \x ; ^jack;Spruce a Bin?h Sparse f

Spruce a Tamarack

Roplar, Birch, Sp.ruc BouldersSmall Spruce a JackPine S-^" to

Tall Poplars

on Boulders ' Spruce, Jack Alders, Birch — Poplar

Boulders/^Poplar, Birch

Spruce]l/'Tall Poplar Spruce

TO,, SP™, 8i Birch

Tall Spruce \

T. L, 2800S s

Hall Birch,Spruce SHEET INDEX^ " Tall Spruce, " 7 and Jack Pine

For Geology Legend see SHEETS - Dwg. No. 1-B

Spruce ± Birch ± Poplar ± Jock Pine l Poplar on

2.12537GOLDEN TANAGER RESOURCES INC.

NORTH CARIBOURIVER PROPERTY.

Patricia M.D., Ontario.X 2a,l0g Spruce

3a,2a,IOg"i 14913-

.. ± SprucePoplar Forest

GEOLOGYPoplar Forest \

SCALE ; i* 4c?oDATE: OCT 1988-- 2a,3a,10g OSCALE: 1:4800GEOCANEX LTD

TORONTO, CANADA DWG. No: l - A

500

LEGEND

QUATERNARY

Stream (lake , bog deposits Glacial, glaciofluvial lacustrine sediments

LATE PRECAMBRIAN (Keeweenawan?)

Ma Diabase

EARLY PRECAMBRIAN

Intermediate and Felsic IntmsivesI0a Granite pegmatitelOb AplitelOc GranitelOd SyenitelOe Quartz monzonitelOf GranodioritelOg TrondjemitelOh Quartz dioritelOi Diorite10k Unsubdivided gneiss10 l Granite gneiss

5000N

T. L. 4400 N

Mafic Intrusives 9a Unsubdivided 9b Gabbro 9c Leucogabbro9d Plagioclase-phyric gabbro > 9e Peridotite x 9f Pyroxenite s

fIron Formation x

8a Oxide facies /8b Carbonate facies '8c Silicate facies 3^8d Sulphide facies ^ ^

x x

Chemical Metasediments x x7a Chert7b Calcitic marble7c Dolomitic marble

Clastic Metasediments6a CLosl supported conglomerate6b Matrix supported conglomerate6c Oligomictic conglomerate6d Polymictic conglomerate6e Sandstone, unsubdivided6 f Wacke6g Arenite6h Mudstone, argillite *6j Feldspathic wacke6k Feldspathic arenite61 Quartz arenite6.m Schistose rock ± amphibole^ biotitB,

± garnet, ± chlorite of probablesedimentary origin

Felsic and Intermediate Subvolcanic Rocks5o Unsubdivided5b Quartz-feldspar porphyry5c Qudrtz porphyry5d Feldspar porphyry

Felsic Metovolcanics

4o Massive fine-medium grained flow4b Pyroclastic breccia, tuff breccia4c Tuff, lapilli tuff

Intermediate Metavolcanics3a Massive fine-medium grained flow3b Flow breccia3c Pyroclastic breccia," tuff breccia3d Tuff , lapilli tuff

Mafic Metavolcanics2a Massive fine-medium grained flow2b Amygdaloidal flow2c Variolitic flow2d Pillowed flow, pillow breccia2e Flow breccia2f Medium-coarse groined flow centres2g Plagioclase-phyric flow2h Amphibolite2i Co-magmatic sills, dikes2j Pyroclastic breccia, tuff breccia2k Tuff, lapilli tuff21 (Jhorite ± amphibole schist

Ultramafic Metavolcanicsla Massive fine-medium grained flow Ib Spinifex textured flow le Talc-carbonate ± magnetite t amphibole

± serpentine ± chlorite schist

53B14SE0001 220

SHEET INDEX

B

•-" ^ ^

. 12500 1000

SCALE : 400

GOLDEN TANAGER RESOURCES INC.

NORTH CARIBOURIVER PROPERTY.


GEOCANEX LTD TORONTO. CANADA

BY: / R .T.M.DATE: OCr 1988SCALE: l :4800DWG. No: l-B

Birch -^

± Balsam ± Birch

Tall Spruce

±Birch*. Sandt Boulder^

/' Caribou** River o o14880-7 -14881- 5

__. Alder, Birch, S pruc?; \ Balsam

Spruce4-

MuskegAlder, Birch

x Spruce v ii/ Spruce, Birch/Alder ± BalsamSp-uce, Muskeg

Tall Spruce ± BalsamX x Tt Birch ± Poplar

Tall Spruce/T

on Sand 'S Boulders s Hummocky Ground Moraine (Sand 9 Boulders)-•X2a,10g

Tall Spruce ± B irch on Sand a Boulders

x14996-5614997-2914998-34

Tall Spruce, Jack Pine Minor Poplar -t- Alder LO

X 2a,i0g ,-.;; 2a 3 'Og

7\4a,5o,2a

sh 7 aspy,ppSpruce ,

Tamarack, Muskeg

2o,IOg V--. coo o

pruce, Birch ^Rjolar 2a 39,21,10 Spruce, Jack Pine, Poplar

±N Bolsom , BirchCO

I 20jf,lOg;O

10806-15

•!*^f""2h ? IOf{inlbx)

on Sand ,a BouldersSpruce,x± Balsam

14931-5(16) 2a x 14932-IOABBREVIATIONS

3a' t0f ^ l Spruce *

± Jack PineSilicification.......,. SIL , si!Sericitization........SER.serCarbonatization . . .CAR , carChloritization..... ..CHL, chl

l l strong weak

Pyrite.. .... .. . . . ,.. . ... . . .,. .. pyPyrrhotite ..,...,. . . .. . poChalcopyrite... .,.......... cpArsenopyrite .. ... . ,. ,,. aspSphalerite - ... ... . -.,..,. .sphGalena . ........ .... .. . gaBornite . ..... ...... ...... brMalachite ............. . . malGraphite . . .. .. . . . . .grChrysocollo . .... ..... .. .chryMagnetite ..,............... mtLimonite ..... -.. ........ MmHematite . ... ...... ... hemMolybdenite .......,. ..... moGrunerite ................. grunSiderite.. ,.......,........ sidDolomite . .... . ........ .... dolAnkerite . ... .....,..... .ankGarnet . ... .. ... gntEpidote . . ... . . ... ...,. epTourmaline .. .............. . tlXenolithMylonite . ...... ........... .mylShearing ..................... shCarbonatized . ,...... .. ... cc

VTamarack)— — '

Spruce, Poplar

Jack Pine on Sand a -x, : x 2o

Boulders / ' 2 a,lOjSpruce, T^hfa/

Spruce, Tamarack/Alder,2hf,IOf (intbx) Spruce

Jack Pine Sand

Boulder± Spruce

X"TL. I300N - 7 SpruceSpruce -i- Tamarack

^ Muskegg ,. Jock Pine X..3o,2ag 7 lg Jack Pine

RidgeO 14934-8 i " ircri0 .--^ c*

Alder ^ Birch

± Tamarack N.

^ 14994-114 ~- 14995-442oh,iOb,9b? ep""'

X 2ahf\ ^ 2ah,IOiAlder, Birch

± Spruce 14942-2114943-50

2f Jack Pine lPoplarv5b,2ac^x,2jah andafetdrs ^ ' XH. Jr;..2hf7iOjgon

Alder "**

Birch ± Tamarack

Sand a Boulders 3a,2a.Di; ^A

Spruce a Tamarack

Spruce Birch ^Spruce, Alder

tBirch! Muskeg

•7*14939-1314940-8(9)

Spruce, Tamarack, Muskeg

r^vffi^o\,^Z0'^{Spruce, Jack Pine,. Spruce"! Birch ± AldeT r ^/-^ -'

14970-IS?Birch Poplar ± Balsamon Sand 9 Boulders

2a,2f

I0j J4976 - jy

X 2a,l0j. Spruce t Birch ±VX!ders

i Tamarack Muskeg2a,IOh 'f'.:-, v /I4983-I5 V-J/./ 14984-17(55) •--....-*' v

fW949-IO(l5) 14966-10

5047-5048-8 "4969-10S x5b,IOj

*pruce^.Rne\

x lOh Spruce l

-r l ,Tamarack y Spruce Muskeg

Poplar S Birch

Spruce, Jack Pin Birch a Poplar

on BouldersSpruce, Jack Pine, Birch a Poplar on Sand 8 Boulders

//Open h Muskegy1 X *

Spruce and Poplar o:i Boulderspruce,

:: MuskegSpruce,Poplar, Jack Pine t Birch , Balsam

on Sand t

To 11 Spruce± Jack Pine iBirc

14922^5(35) 14923 - 22

See SHEET A for LOCATION MAP

Shoreline

Creek , showing flow

Swamp

Beaver Dam.

Break in slope

Claim post, line,witness post

Township line.

Trench, pitDiamond drill hole

Highway, bush road

Power transmission line

Outcrop, outcrop area

Geological boundary, observed

Inferred, inferred from geophysics.—— —— — G — G^

Surficial feature boundaryRock sample location S number.. * 17501

Assay for Au (ppb), Ag(ppm)

Pillow; tops known , unknown

Bedding ; inclined, vertical.

Foliation, cleavage; 6 0

Inclined, vertical, unknown .

Gneissosity ; incl., vert, unknown.

Lineation , plunge...,....---... . - -- 6 0

Fracture ; inclined , vertical

Shear zone ; dip Shear fracture; inclined,vertical.

Fault zone ; dextral .sinistral-. . yy

Anticline , syncline, plunge

Drag folds with plunge

Dyke ; width , dip Vein; width, d ip, quartz , carbonate

Glacial striae

T. L. 2400 S

/^ s

f

**. •^.

10 ^"

i-uj'vj \ n

^

•x

xx

^

o oC\J

ooCO CO

4000S

rpt on geol mapping litho samp & pros n ......amikama lake and access was gained to the property...

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