results of 1991 exploration work wabikoba lake …...april 1992. l l l l l l l l l l l l l l l l l l...

42C13SW0092 2.14562 WABIKOBA LAKE 010

RESULTS OF 1991 EXPLORATION WORK GEOPHYSICAL SURVEY AND PROSPECTING

IHNATKO - KUSINS PROPERTY WABIKOBA LAKE AREA, NORTHWESTERN ONTARIO

N.T.S. 42 C 13 j SW

'i.

Written by: Pierre Simoneau 3-309, Catherine st. Thunder Bay, Ontario P7E 1K7 Phone: (807) 623-7496

(807) 623-1692 (messages)

April 1992

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THE IHNATKO - KUSINS OCCURENCE

ABSTRACT

The property consists of J l unpatented mining claims which include a base metal occurence known as the Kusins Showing. For the sake of this report, the showing will be called The Ihnatko-Kusins zone. in honour of the man who actually discovered the showing.

The property is located 8 kilometres due north of the famous Hemlo gold mines site on the Trans-Canada Highway 17. Access to the property is by a logging road running west ot Highway 614 at. a point about 8 km north ot the Black River and running through the western portion of the property 2-4 km south of the railroad tracks.

The property lies in a package of volcano-sedimentary rocks similar to the. Mani touwadge-Geco area which hosts several important base metaJ deposit.s. Significant. base metal mineralization obtained recently in a grab sample ran JO.7% zinc and 8 , 9-h lead with 2.5 oz . silver per ton. This mineralization is located about 1200 metres east of the logging road.

The volcanogenic mineralization is at the contact of crystal tuffs and sedi merits where the tuffaceous rocks wedge out against the sedimentary rocks-.. Ore hosts are sericite schists, siliceous sediment;; and fragmental rocks. The mineralized zone is 80 cm wide in the old trench and a vlf anomaly is following the. contact between the sediments and the crystal tuffs where the mineralization was found. The Bullring Fault, identified by the vlf survey, is a potentially significant structure in relation to the mineralization. The diabase dykes were easily identified by the magnetic survey.


Table of content;42C13SWM92 Z. 14563 WABIKOBA LAKE

Abstract. . . . . . . . .-. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . ^Table of contents . . . . . . . . . . , . . . . . . . . . . ... . . . . . . . . , . 3

1. Introduction . . . . , . . .'. . . . . .". . ... . . -. . . . . . . . . . . . . . . .' .-. 42. Location and Acces . . . .;. . . .'. ~. . . . . . . . . . . . . . . . . . . . . . . 53. Claims..............................:.............84. Regional geology.................................105. Previous work....................................126 . 1991 work program............................ . . ..13

6 . l Linecutting.............................. . . . 136.2 Prospecting............................. . ...136.3 Geophysical surveys...................... . ..15

7. Property geology.................................187.1 Volcano-sedimentary rocks................ . ..187 . 2 Intrusive rocks-. ............................187.3 Mineralization..............................20

8. Conclusion.......................................219. Recommendations..................................21

Selected References..............................22Certificate of Qualifications....................23

APPENDICES

Appendix 1. Appendix 2. Appendix 3.

LIST OF FIGURES

List of claim numbers and due dates Description of the rock samples Assay Data

Figu Figu Figu Figu Figu Figu Figu

rere re re re re re

1 . 2. 3. 4. 5. 6. 7.

General location map.. Detailed location map. Claim map.............General geology map of

. . . . . . ... .. . . . . .7

. . . . . . . . . . . . . . . .9Hern l o area. . . . . 11 and sampling...14

Compilation map of mag-vlf anomalies..17 Property Geology......................19

Sketch map of trenches

LIST OF MAPS (in pocket)

PlanPlanPlanPlanPlanPlanPlanPlanPlan

PlanPlan

1.2.3.4 .5.6.7 .B.9.

10.11.

Magnetometer survey, pMagnetometer survey, t*MAGVLFVLFVLFVLFMAGVLF

VLFVLF

survey.survey ,survey.su rvey ,survey.survey,su rvey ,

survey ,survey ,

profilesprof i lesprof i lesprofilesprofilescolored 1colored c

colored fcolored (

lStS,8,S,to20

~ r

20

010C

Plan 12. VLF survey, colored

profiles S postings total field contours

interpretation postings, Cutler station interpretation, Cutler st. postings, Jim Creek st. interpretation, Jim Creek al field contours

corrected total field contours.Cutler station

sr Filter contours, Cutler corrected total field contours.

Jim Creek station Frazer Filter contours, Jim Cr

11111111

11

11

2,5002,5002.5002,5002,5002,5002,5006,000

6,0006,000

6,0006 , 000


INTRODUCTION

The following report gives the results of the exploration program carried out during winter and spring of 1991 over the Kusins Occurence. For the sake of this report, the showing will be called the Ihnatko-Kusins Zone, in honour of the man who actually discovered the showing.

Prospecting on the old trenches was carried out in January 1991 and during May 8th to May 14th 1991, limited magnetic, VLF-EM surveys were carried on the Ihnatko-Kusins property. The author of this report supervised and performed the survey work.

The claims were staked to cover the showing itself and the logging road. Detailed prospecting of the old pits was successful in relocating the base metal mineralization which was overlooked by previous operators, who were mainly interested in gold.


2. LOCATION AND ACCESS

The property is located approximately 320 kilometres east of Thunder Bay (figure 1) and 8 km due north of the famous Hemlo gold mines site on the Trans-Canada Highway 17. The property is located on a northerly extension of the same belt of rocks.

Access to the property is by a logging road which runs through the western portion of the property (figure 2). The road is the first main logging road, running west of Highway 614 at a point about 8 km north of the Black River. The property is located approximately 24 km south of the railroad tracks on the main logging road.


HUDSON BAY

Kijklond lok*

LARDE '

IHNATKO - KUSINS PROPERTY

LOCATION MAP

WABIKOBA LAKE AREA

SCHREIBER-HEMLO DISTRICT

N.W. ONTARIO

N.T.S. 42 C 13 7 SW

FIGURE 1.


' -* x-^ J A ."/i" G^i Jy""

. c"~ l

FIGURE 2.


DETAILED LOCATION MAP

WABIKOBA LAKE AREA

N.W. ONTARIO

SCALE l : 10,000

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3. CLAIMS

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The property consists of 11 unpatented mining claims which M were all covered by a geophysical survey (figure 3).

The list of claims and due dates is in appendix 1.

The claim holder of the mining property covered by the B survey is:

M. Dave Saunders

1 309, Catherine st. Thunder Bay, OntarioP7E 1K7


FIGURE 3.


CLAIM MAP

WABIKOBA LAKE AREA

N.W. ONTARIO

SCALE l : 31,680


4. REGIONAL GEOLOGY

The Ihnatko-Kusins Property lies on the northern limb of the Hemlo Synform, an east-west trending synclinorium developped within the Archean aged Heron Bay Greenstone Belt. The Syncline is flanked to the northwest by the Gowan Lake and to the south by the Bullring Lake granitic gneiss domes (figure 4).

The Bullring Lake Fault, a dextral cross fault, is interpreted by Milne (1968) to extent through the eastern portion of the property. This fault (identified by a lineament on air photos) is a potentially significant structure in relation to the mineralization.

Rocks within the syncline have locally attained an upper amphibolite grade of metamorphism. The core of the syncline has locally been intruded by several late Archean felsic complexes, including the Musher Lake Pluton. Several ages of post-Archean diabase dykes intrude the entire sequence.

The Hemlo Mining Camp, situated in the Wawa-Shebandowan subprovince, specifically occurs in a highly deformed zone flanked by intermediate to mafic volcanic rocks in the footwall and volcaniclastic rocks in the hanging wall. It has been suggested that the mineralization is at the contact of crystal tuffs and sediments, where the tuffaceous rocks wedge out against the sedimentary rocks. The mineralization is zoned both across dip and along strike.

10


(TJ7I alkalic complexgranitoid rocks, gneiss, migmatite

Intermediate to felsic metavolcanlcsmafic to Intermediate metavolcanics, amphibolitemafic and ultramafic Intrusive rocksmetasediments fault, lineament

GOWANLAKE

PLUTON

HERON BAY GROUPCEDAR LAKE PLUTON

O

HEMLO DEPOSITSHERON BAY PLUTON

PLAYTERHARBOUR

GROUP

PUKASKWA GNEISSIC COMPLEX

Lakt Superior

Map courtesy of OGS

Figure 4. Geological map of the Hemlo area by T.L. Muir, 1983. (Modified after OGS Maps 2220, 2^39* 2452, P.2701, P.2702, P.2738, P.2739).

11


5. PREVIOUS WORK

The property and W. Kusins (Milne, have suggested it was for the Ontario Paper the discovery claims.

was reported to have been discovered by T. 1968) in 1963. Sources to M. Dave Saunders discovered by Ihnatko while timber cruising Co. Ihnatko and Kusins became partners in

The showing was examined by several companies in 1963 (Milne, 1968). The mineralization was trenched by Ihnatko and Kusins following this and optioned to Cominco in 1965. Grab samples were reported to run over 20 02. silver per ton. (not published). Cominco conducted limited geophysical and geochemical work before drilling 5 X-ray drill holes.

Drill logs submitted by Cominco for assessment work were incomplete, and no assays were reported. Several sections in the drilling reported disseminated galena and sphalerite.

The property fell idle until it was staked during the Hemlo rush by Pryme Energy. In 1982, the ground covered by this property was optioned to Noranda. A large grid was established over the entire Prime Energy Option property and was mapped in 1983 and 1984. Some IP -and conventional geophysics were conducted followed by limited drilling, which did not include the Ihriatko-Kusins zone.

The property was restaked by Dolphin Exploration and work was undertaken by Corona Corporation on behalf of Dolphin Exploration Ltd. in 1987. Soil sampling and geological mapping were performed in selected areas, including the present property.

12


,. 1991 WORK PROGRAM

6.1 Linecutting

LInecutting was undertaken using the remnant of an existing grid which had been established by Noranda in 1982. The Grid was inspected in May 1990 and the baseline recut and chained. Deadfall is abundant due to budworm damage.

Remnant of the early grid were only followable in areas of jackpine bush which is prevalent near the road (an old burn), and this grid was 200 m. spaced lines. The recutting of old lines and the cutting of new fill in lines totalling 22.5 km began in mid-January 1991, concurrent with the restaking and prospecting of the showing itself.

6.2 Prospecting

The location of the trenches was established by research and located before staking began. The trenches are deep and rock exposures were adequate, even in the winter. Snow was shovelled away from the edges and from the muck.

The old trenches as described by Milne (1968) were relocated and prospected (figure 5). These were Trenches l, 2 and 3. Trench #4 was not found. Four samples were taken from these pits and their muck, three of which came from Trench 2.

Approximately 40 metres west of the deeper documented pits, two longer, shallower pits were located and sampled with a total of seven samples. Four grab samples were taken at otherlocations.

Base metal mineralization was first located by Dave Saunders in the muck of Trench 2. This was traced to the NE face of the pit which shows a 0.80 m. thick mudstone unit with disseminated and semi-massive pyrite, sphalerite and galena mineralization. Sample 8626 ran 10.7*. zinc and S.9% lead with 2.5 oz. silver per ton in a grab sample. Sample 8624, a chip sample across 0.75m ran 0.84^ Zn and Q.13% Pb with 1.8 oz/ton silver. Description of samples in appendix 2 and the Assay data in appendix 3.

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Figure 5. Sketch Map of Trenches and Sampling - l cm s 12*5


.3 Geophysical surveys

A geophysical program was initiated on the Ihnatko-Kusins property to evaluate the economic potential of the claim block.

A grid of northwest - southeast lines spaced 100 metres apart was established as reference stations for the geophysical surveys. A total of 22.5 km of lines including the base line was completed. The ground geophysical surveys including a magnetometer and an electromagnetic VLF-Em 16 survey, were carried out by the author of this report.

The geophysical survey was conducted with a Scintrex QMNI- PLUS. The OMNI-PLUS Magnetometer/VLF System is a ruggedized compact, portable instrument designed specifically for field operation. It allows for quick surveying capability without, sacrificing accurancy and quality data. It contains several microprocessors and associated circuitry for monitoring, processing and storing data. The OMNI-PLUS has two memories: the tie-line points arid field measurements of the survey.

The magnetometer system measures the value of the total magnetic field with a precision of 0.1 gamma with a statistical error alarm flashing over 0.2 gamma. If the error is larger than 2.0 gammas, another reading must be taken. The OMNI-PLUS contains high technology circuits which allow for automatic fine tracking (tuning) over the entire field strength from 18,000 to 110,000 gammas, under cumputer control. The readings were taken systematically every 12.5 metres along the cut and chained lines. The base station is located east of the logging road near the base line. The magnetic readings have been automatically corrected for diurnal variations when the data was dumped.

The magnetic results are presented on a profile map (Plan .1) and a contour map (Plan 2) and interpreted in Plan 3 at the metric scale of 1-2,500 in pocket. An extra couloured contour map (Plan 8) was added to the report at the metric scale of 1=6,000. The major higher magnetic anomalies are oriented at about 300 and 010 degrees and correspond to the diabase dykes- Some other smaller anomalies follow the local geological trend.

The electromagnetic VLF-EM16 survey was carried out with the OMNI-PLUS using Cutler, Maine station (frequency 24.0 kHz.) and Jim Creek, Washington station (frequency 24.8 kHz). The vertical components (in phase and quadrature) of the secondary field are measured with a precision of * or -G.2%. The OMNI-PLUS has been designed whereby, if a weak station is selected, the instrument will automatically increase the measurement period to produce higher quality results. The readings were taken systematically every 12.5 metres along the grid lines.

15


The results of the electromagnetic survey are plotted for the Cutler station on Plan 4 and the interpretation on Plan 5 and for the Jim Creek station an Plan 6 and the interpretation on Plan 7 at the metric scale of 1=2,500 in pocket. Profiles at the scale of l cm=20% have been drawn for the in phase and quadrature readings. The possible conductors have been interpreted and marked by a bolder line. Extra coloured contour maps (Plan 9, 1Q, 11 and 12) representing the corrected total field and the Fraser for each stations were added to this report at the metric scale of 1-6,000.

Figure 6 presents a compilation of the geophysical anomalies resulting from the ground surveys. The VLF Em-lei anomalies have been numbered and their characteristic are as follows:

Anomaly Length No. (metres)

ttl

#2

^100

Centre

L25+OOE 0+62N

H4

tt6

#7

ttS

#9

100 L29+OOE 0 + 45S

500 L28+OOE 1+65N

200 L27+OOE 2+OON

500 L27+OOE 2+65N

100 L29+OOE 4+OON

500 L21+OOE H-60N

500 L19+OOE 3425N

400 L19-I-OOE 4445N

Remarks

Deep valley, topographic feature representing a cross fault known as the Bullring fault.Weak one line anomaly close to the surface.Moderate anomaly, small valley, po sitive Beep Mat readings, probable conductor close to the surface. Weak bedrock anomaly following the Ihnatko-Kusins showing direction. Cut across magnetic anomaly. Moderate anomaly, deep valley with cliffs which may represent a fault. Cut across magnetic anomalies which stop in that area. Parallel to #3. Moderate one line anomaly open east 25 m north of the granitic contact. Weak bedrock anomaly, close to the surface. Possible extension of 4(2. Moderate to strong bedrock anomaly. Possible extension of # 3. Strong bedrock anomaly, flat topo graphy, possible extension of tt5.

The general orientation of the VLF anomalies corresponds to the local geological trend of the sedimentary bedding. The Bullring Lake fault cut across the area and the dextral displacement is spectacularly shown by the VLF survey.

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IHNATKO-KUSINS PROPERTY

GEOPHYSICAL COMPILATION

Wabikoba Lake Area Schreiber-Hemlo District

N.W. Ontario

Scale l : 13,333 goo Voo

N.T.S. 42 C 13 7 SW


PROPERTY GEOLOGY

7.1 Volcano-sedimentary .rocks

Reconnaissance geological mapping was conducted in 1964 and 1965 (Milne, 1968) at 1:31680. The only other work recorded is in 1984 (Kemp, 1984) at 1:5000 and in 1988 (Hamilton, 1989) at 1:5000. The most recent work was conducted with helicopter- support.

From compiling assessment work data, the property can be shown to be underlain by a package of volcanic and sedimentary rocks (figure 7). From the granite contact southward, a thin ^50 m. section of foliated mafic volcanics is in sharp contact with mudstones which are in contact with a thin felsic pyroclastic unit which grades into laminated sediments and conglomerates. The Ihnatko-Kusins Zone occurs at the contact of the mudstones and the felsic tuffs.

The three main rock types disclosed by other mapping were, however, observed: felsic tuffs south of the mineralized pits, grading into laminated sediments further to the south, and foliated mafic volcanics between the mineralized zone and the Monzonite. A possible agglomerate (conglomerate) was observed at the baseline near L24E.

7.2 Intrusive rocks

The Ihnatko-Kusins Zone occurs approximately 150 metres south of the regional contact of the monzonitic Gowan Lake Pluton with the greenstone belt. The monzonite is typically a light coloured, medium grained, hornblende monzonite. A faint foliation parallel with the schistosity of the volcanics can be observed in places.

Recent prospecting on a cliff near the contact at L27E 3-I-75N shows a brecciated intrusive texture at the contact with the foliated mafic rocks. This may be a widespread feature and could be significant.

The property is crosscutted by diabase dykes and theBullring Lake Fault.

18

VD

3D


PROPERTY GEOLOGY

Wabikoba Lake Area Schrelber-Hemlo District

N.W. Ontario

Scale l : 13,333800 KPO

-J *nc5ec

N.T.S. 42 C 13 7 SW


'.3 Mineralization

Sulphide mineralization was observed at the contact of a sedimentary unit (mudstone) and a felsic crystal tuff unit. The main type of mineralized rock is a well layered pyrite sericite schist. The extent of this rock type was impossible to determine, but was present in all trenches.

In Trench 2, a 0.80 m. thick mudstone unit with disseminated and semi-massive sphalerite and galena was located. The best material ran 10.7% zinc and B.9% lead with 2.5 oz silver per ton in a grab sample. A chip sample across 0.80 m. ran Q.84% Zn and O.13% Pb with 1.8 oz/ton silver.

With the proximity of this mineralization to the Bullring Lake Fault, there may be excellent potential for a Manitouwadge- type of deposit.

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J5. CONCLUSIONS

A survey grid at 100 m. . spacing has been established over the property. Road access to the property will reduce the cost of exploration which has hampered the development "of the property in the past.

The base metal occurence known as the Ihnatko-Kusins Showing has been relocated and sampled. The presence of significant base metal mineralization has been documented. A Vlf anomaly coincide with the volcanogenic mineralized zone.

The host rocks and structural feature shares similarities with economic deposits in the area. Further ground work should evaluate the potential for an economic zone.

RECOMMENDATIONS

Theprospected instrument conductive overbu rden showing. Further s performed

property should be mapped at 1=2,500 scale andwith a Beep Mat (a miniaturized electromagnetic survey

used for surface prospecting in detection ofmineralized outcrops hidden under up to 1.5 metres of

). Prospecting was limited to an area around the mainFurther- prospecting should cover the other claims.tripping, sampling and detailed mapping should bein the vicinity of the old trenches.

The planning of more advanced work, including drilling, would be based upon the ground survey results.

diamond

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.SELECTED REFERENCES

Hami-1-ton , W . S

Kemp, R.,

Milne, V.G.,

Mui r, T.L.,

1989, Report on Geological and Geochemical -(Soil) Surveys on the Black River Property. .Company report for Dolphin Exploration Ltd; MNDM assessment file No. 2.12347, Thunder Bay.

1984, Geological Assessment Report, Joint Venture, Wabikoba Lake Area, District. Company report for Noranda Company Ltd. MNDM assessment file Thunder Bay.

1968, Geology of the Black River Area.pp. 61-63, Map 2144.

Pryme North Thunder BayExploration

No. 2.7108,

ODM GR 72,

1983, Geology of the Hemlo-Heron Bay Area: pp. 230- 239, in The Geology of Gold in Ontario; edited by A. Colvine, Ontario Geological Survey, Miscellaneous Paper 110, 278p.

22


CERTIFICATE OF QUALIFICATIONS

THIS IS TO CERTIFY THAT:

I am a resident of Thunder Bay, province of Ontario, Canada (2-309 Catherine st, Thunder Bay, Ontario, P7E 1K7).

I have been engaged in base and precious metal exploration as a geologist since 1987 and as geophysicist since 1991.

I am a graduate of University of Quebec at Chicoutimi, Chicoutimi, Quebec (M.Se. Earth Sciences, 1987), and University of Montreal, Montreal, Quebec (B.Se. Geology, 1982).

I am a member of the Professional Association of Geologists and Geophysicists of Quebec (APGGQ).

Signed in Thunder Bay, April 16 1992

APGGQ ^\

SIMONEAU

Pierre Simoneau Geologist, M.Se.

23


APPENDIX 1.

List of Claim Numbers and Due Dates

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APPENDIX 1.

LIST OF CLAIMS AND DUE DATES

l 1. TB 1142843.................... . . . . . .....February 18, 1993

2. TB 1142844. . . . . . . . . . . . . . . . . . . . . . . . . . . . ..February 18, 1993

l 3. TB 1142845.. . . . . . . . . . . . . . . . . . . . . . . . . . . . .February 18, 1993

m A. TB 1142846..............................February 18, 1993

5. TB 1142847.. . . . . . . . . . . . . . . . . . . . . . . . .....February 18, 1993

l 6. TB 1147781.......:......................May 7, 1992

7. TB 1147783. . .. . . . . . . . . . . . . . .............May 7, 1992

l 8. TB 1147784........ . . . . . . . . . . . ...........May 7, 1992

m 9. TB 1147785. . . . . . . . . . . . . . . . ..............May 7, 1992

10. TB 1147791..............................May 7, 1992

l 11. TB 1147792....... . . . . . . . . . . . . . . . . . . . ....May 7, 1992

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APPENDIX 2.

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Description of the rocks samples

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APPENDIX 2.

DESCRIPTION OF THE ROCK SAMPLES

8613. Light grey medium grained acid tuff with thin millimetric bands of pyrite (10& of the rock).

8614. Light greenish grey, fine grained acid tuff with fine laminations of amphiboles and a few millimetric bands of quartz, reddish garnets and 2% pyrite.

8615. Light grey medium grained acid tuff with lS-25% pyrite in massive bands and trace of sphalerite.

8616. Dark grey pyritic argillite (mudstone).

8617. Light grey medium grained acid crystal tuff with 2\ pyrite.

8618. White bleached foliated quar tz-serici te tuff with S-15% thin laminations of pyrite, and J.% magnetite.

8619. Medium grey cherty tuff with S-5% layers of pyrite.

8620. Light grey pyritic bedded cherty tuff with 15% pyrite and 2* magnetite.

8621. Light grey pyritic bedded cherty tuff with 25% pyrite bands.

8622. Light grey medium grained pyritic bedded cherty tuff with 25?o laminations of pyrite.

8623. Light grey medium grained pyritic bedded cherty tuff with 1-3 mrn thick bands of pyrite (2C^) and T.% Chalcopyrite.

8624. Dark grey mudstone unit with disseminated sphalerite and Galena. Chip sample 0.80m long.

8625. Dark grey pyritic mudstone with 40?6 pyrite, 20?s sphalerite and 5% Galena.

8626. Massive sphalerite sample from a float but found in situ as part of sample 8624. Represent 3 cm bed of massive sphalerite and Galena Zone.

8627.

8628.

Light grey medium grained tuff with massive pyrite

Medium grey, sericitic intermediate tuff with 3% pyrite.

APPENDIX 3.

ASSAY DATA

COMP; CAVE SAUNDERS PROJ:^

SAUNDERS

MIN-EN LABS —— ICP REPORT705 WEST 15TK ST., NORTH VANCOUVER, B.C. V7M 1T2

(604)980-5814 OR (604)988-4524

FILE NO: 1B-0163-RJ1DATE: 91/01/30

* ROCK * (ACT:f31)

SAMPLE NUMBER

TB-1442 8613 T8-1442 6614 TB-1442 B615 TB-1442 8616 TB-1442 8617

T8-1442 B618 TB-1442 8619 TB-1442 8620 TB-1442 8621 TB-1442 8622

T6-1442 8623 TB-1442 8624 TB-1442 8625 TB-1442 8626 TB-1442 8627

TB-1442 8628

AG CU PB ZN GA SN AU PPM PPM PPM PPM PPM PPM PPB.8 22 48 80 3 1 2 ^^.,— — --*-~ -~ ..^

1.1 26 29 51 1 1 1 -'"- " .3 58 90 130 1 1 26

1.7 100 22 86 1 1 2 1.8 57 18 6! 1 1 lJ H 14 21 1 1 8 .9 12 19 52 5 1 Z

1.5 75 13 19 1 1 25 .9 132 13 41 1 1 1 .1 65 3 18 1 1 3

.3 739 49 85 1 92 6,4 69 1298 8435 1 1 18 3.0 43 1181 2749 1 1 2 8.7 907 S9527 107369 1 2 340 .1 9 107 270 1 1 17

.5 15 159 181 5 1 2

:

Ministry ofNorthern Developmentand Mines

Ontario

Report of Work Conducted After Recording Claim

Mining Act

Transaction Number

./71//I//AJ6rilfbruBe(ffor corresponcPersonal Ink Jtlon collected on this form Is obtained under the authority of the Mining Act. This Information wiUrb/JsAf f5r Correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street, Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264.

Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for ree

Recorder.- A separate copy of this form must be complete- Technical reports and maps must accompany ti- A sketch, showing the claims the work is assigi ^ciaswee^'a.'Msea'wABiKoeA LAKE 900

Recorded Holder(s)

DflVlU

Client No.

Address _ CrfTWlJJ, ID/

Telephone No.807

Mining Division

RAM or Q Plan No,

G-Dates ttmed

Ff0m: To: MfVy i?Work Performed (Check One Work Group Only)

Work Group

Geotechnical SurveyPhysical Work, Including Drilling

RehabilitationOther Authorized Work

AssaysAssignment from Reserve

Type

M/k^c&fomJtfU /r/OcL \JLF- ^ /6

ô.SpfcTb/06

/L\ fftrTotal Assessment Work Claimed on the Attached Statement of Costs S

""

Note: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address

RtflRL. S/mo/^Vu 2-309 O^w*RE0EW:^R /ky (^r?*te\tfi"

———— m 1 1 1992 ————————————

MINING LANDS BRANCH

(attach a schedule if necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse sidel certify that at the time the work was performed, the claims covered in this report were recorded in the current holder's name or held under a beneficial Int by the current recorded holder.

work 7\ate Recorded Holder or Agent (Signature)arest TORlLf?7^ "X^ ,

' 13? D dâftAÂ^-^

Certification of Work Reportl certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after Its completion and annexed report is true.

Name and Address of Person Certifying

Tetepone No.

For Office Use OnlyTotal Value Gr. Recorded

Date^ /i^L. tt/fz-.Date Recorded Mjrafo,

1 G n J&**(Jsps\ 3,11 7 2- *ci

Deem/d Approval Date Date A

Dale/Notice Mr Amendments Sent

——— nr ——— . i-n . ————————— i ———— T—— - fcP

Certified ^Signature) ro

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8 iits

Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (^) one of the following:

1. D Credits are to be cut back starting with the claim listed last, working backwards.2. B'Credits are to be cut back equally over all claims contained In this report of work.3. D Credits are to be cu.t back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one will be Implemented.

Note 1: Examples of beneficial interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.

Note 2: If work has been performed on patented or leased land, please complete the following:

i certify that the recorded holder had a beneficial Interest In the patented or leased land fi foe lime 'he work was performed.

Signature Date

Ministry ofNorthern Development

——, andsMlnes OntarkJ fl|

Mi^re du Dewoppement du Nord et de* mines

Statement of Costs for Assessment CreditIztat des coQts aux fins du credit devaluation

Mining Act/Loi sur les mines

Transaction NO./N* de transaction

Personal Information collected on this form Is obtained under the authority of the Mining Act, This information will be used to maintain a record and ongoing status of the mining clalm(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands. Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5, telephone (705) 670-7264.

Les renseignements personnels contenus dans la presente formula sont recueillis en vertu de la Lol sur let mines et servlront li tenir a jour un registre des concessions mlnieres. Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains mlnlers, ministere du Developpement du Nord et des Mines, 159, rue Cedar, 4* etage. Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/Gouts directs

Type

Wages Salalras

Contractor's •nd Consultant's FeesDrolts de ('entrepreneur •t de I'expert- consell

Supplies Used Fournltures utlllsees

Equipment Rental Location de materiel

Description

Labour ^ /kj^vcTT^- Main-d'oeuvre ^ /st ^Field Supervision Supervision sur le terrain

Type

/•)sSAyS

i. i h t ûttiu c

DftA-^tiiOoType

'i.OOî t fij Cl '

Type C^c^K^/c/JL-

IMSlTvOrYxA/OT

Amount Montant

CO3.S50

a^L

W*So**

I3e. oy

f w'0M9,80

Total Direct Costs Total des couts directs

Totals Total global

3W"

ty3?fc

\^

—— *®WSTW950

2. Indirect Costs/CoOts Indlrects* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les coOts indirects ne sont pas admisslbles en tant que travaux devaluation.

Type

Transportation Transport

Food and Lodging Nourrlture et hebergementMobilization and Demobilization Mobilisation et demobilisation

DescriptionType

Amount Montant

HSO*

^

Sub Total of Indirect Costs Total partial des coOts Indlrects

Amount Allowable (not greater than 20H of Direct Costs) Montant admissible (n'excedant pas 20 H des coots directs)Total Value of Assessment Credit Valeur totale du credit (Total of Direct and Allowable devaluation Indirect eoittl (Toll! del eedti direct*

Totals Total global

HZQ*\t/ f ^

88^

loe&V•t Indirect! admlttlblei

Note: The recorded holder will be required to verify expenditures claimed in Note : Le titulaire e'nregistre sera tenu de verifier les depenses demandees dans this statement of costs within 30 days of a request for verification. If le present etat des coOts dans les 30 jours suivant une demande a cet verification is not made, the Minister may reject for assessment work effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout all or part of the assessment work submitted. R F" O F" Tl '^T^18 Partie des 'rav*ux devaluation presented.

Filing Discounts MAY l pe1Q8^pourdep6t

1. Work filed within two years of completion is claimed at 10007o of j. Les Xavauiutyposes dans les deux ans suivant leur achievement sontl^NDSethe above Total Value of Assessment Credit. e^ÔVUJôoc^delavaleurtotalesusmentionneeducredild'evaluation.

2. Work filed three, four or five years after completion is claimed at 50"M) of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimedx 0.50 -

2. Les travaux deposes trols, quatre ou cinq ans apres leur achievement sont rembourses a 50 •ft de la valeur totale du credit devaluation susmentionne. Voir les calculs ci-dessous.

Valeur totale du credit devaluationx 0,50 -

Evaluation totale demandee

Certification Verifying Statement of Costs

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that as(Recorded Holder, Agent, Position in Company)

to make this certification

Attestation de I'etat des coOts

J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont ete engagers pour effectuer les travaux devaluation sur les terrains indiqu6s dans la formule de rapport de travail ci-joint.

, l am authorized Et qu'a litre de je suls autoris6(titulaire enreglttre, representant, po*te occupe dans la oompagnie)

a faire cette attestation.

Date

0212 (04/91) Nola : Dans cette tormule. lorsqu'il designe des personnes. le masculin est utilise au sens neutre.

OntarioMinistry of Ministere duNorthern Development D6veloppement du Nordand Mines et des Mines

Mining Lands Branch Geoscience Approvals Section 159 Cedar Street, 4th Floor Sudbury, Ontario P3E 6A5

Telephone: Fax:

(705) 670-7267 (705) 670-7262

July 17, 1992

Mining RecorderMinistry of Nothern Develojand Mines435 James Street SouthP. O. Box 5000Thunder Bay, OntarioP7C 5G6

Dear Sir/Madam:

Our File: 2. 14562 Transaction #W9240. 085

GEOLOGICAL SURVEY GIS - ASSESSMENT FILES

AUG O 7 1992

RECEIVEDSubject: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMS

TB1142843 et al, IN WABIKOBA LAKE AREA

The assessment work credits for the Geophysical surveys and Prospecting filed under Sections 14 and 9 of the Mining Act Regulations have been approved as originally filed.

The approval date is July 17, 1992.

Please indicate this approval on your claim record sheets.

Yours sincerely,

Ron C. GashinskiSenior Manager, Mining Lands BranchMines and Minerals Division

LJ/jl Enclosures:

cc: Resident GeologistThunder Bay, Ontario

Assessment Files Office Toronto, Ontario

REFERENCESHRFA.S WITHDRAWN FROM

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APPROXIMATE HKAH l)KCU,NAT]ON 1992

Annual chance Increasing 1.5*

MAGNETOMETER JSURVEYCOLORlP TOTAl FlElD CONTOURS

fftOPEftTVs 5WABIKOBA tAKf "AREA

Scale: t/Cooo t

r 4. ( -j p\

y.

SURVEY VLF SURVEYCOLORED CORRECTED TOTAL FIELD CONTOURS

CUTLER MAINE US A, N AA FRi24.0KHi

FOR

BY

P. SIMONEAU 05/91

P. MMONFAU OS/91


WABIKOBA LAKE AREA

NW. ONTARIO

230

SURVEY VLF SURVEYCOLORED FRAZER FILTER CONTOURS CUTIER MAINE USA.NAA FR:24.0KHx

DAVE:

tiP. SIMONEAU 05/91

P. SIMONEAU 05/91

P. SIMONEAU

l"**OHCi *1

OJ/91

CI*N NO /Q

P*OJF( i Ne

IHNATKO-KUSIN5 PROPERTY

WABIKOBA LAKE AREA

N.W. ONTARIO

IOMG H'51'1*

?. l 4562 WABIKOBA, l AKE 300

SURVEY VLF SURVEYCOLORED CORRECTED TOTAL FIELD CONTOURS

JIM CREEK WASHINGTON USA. NIK FR:24.8KHt

FOR DAVE S

BY

EHICUTED (l

P. SIMONEAUIHIM'XTFD II

f. SIMONEAU

05/91

05/91

DRAWN lv

P, SIMONEAU 05/91

IHNATKO- KUSINS PROPERTY

WABIKOBA LAKE AREA

N.W. ONTARIO

M' tftr'n i OJO IJ'JI'W

WABIKOBA LAKC 310

SURVEY VLF SURVEYCOLORED FRAZER FILTER CONTOURS

JIM CREEK WASHINGTON USA.NIK FR:24.8KHi

FOR DAVE SAUNDERS

BY

IKECUtFD BY

f. SIMONEAU 05/91

P. SIMONEAU 05/91

f. SIMONEAU OS/91

IHNATKO- KUSINS PROPERTY

WABIKOBA LAKE AREA

N.W. ONTARIO

3SW8092 P-M562 WABIKOBA LAKE

results of 1991 exploration work wabikoba lake …...april 1992. l l l l l l l l l l l l l l l l l l...

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