geoph rpt on the squam l prop...f a bm un. n*-m ftftt fi. imb^v f^^. f^^^m tet tdmtmmi nmfmil...

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

53E185*8545 8.12385 SHOAL LAKE

101989

•l MMr j , . ,'v- f f-"- . . ... . . L .,-, i, . ^t..

GEOPHYSICAL REPORT

ON THE

SQUAW LAKE PROPERTY

FOR

TEESHIN RESOURCES INC,

Prepared by:J.C. GRANT C.E.T..F.G.A.C, Exsics Exploration Ltd. Timmins, OntarioJune 28,1988

010


52EieSW6545 2 .13385 SHOAL LAKE

TABLE OF CONTENTS

Page

INTRODUCTION. . . . . . . . . . . . . . . . . . . . . l

LOCATION AND ACCESS. . . . . . . . . . . . . . . . . . l

CLAIM GROUP. . . . . . . . . . . . . . . . . , . . . . 2

PERSONNEL. . . . . . . , . . . . . . . . . . . . . . . 2

SURVEY PROCEDURE. . . . . . . . . . . . . . . . . . . 3

SURVEY RESULTS. . . . . . . . , . . . . . . . . . . . 5

CONCLUSIONS AND RECOMMENDATIONS . . . . . . . . . . . 7

LIST OF FIGURES

Figure l Claim Location Map

Figure 2 Grid Sketch Location Map

010C

LIST OF MAPS

MAP NO. l Contoured Magnetometer Survey Map

MAP NO. 2 VLF Dip Angle

MAP NO. 3 Fraser Filtered VLF

APPENDECES

Appendix A Scintrex MP-2

Appendix B Crone Radem VLF-EM Receiver

Appendix C Technical Data Statement

l l l l

A Magnetometer and VLF--EM survey was carried out on 30

8 unpatented mining claims for Teeshin Resources Inc. The

m s urvey was carried out on a contract basis by Exsics

Exploration Ltd., Timmins, Ontario. This report deals with

l

l

l

l

l

l

l

l

l

Introduct ion

the survey procedures and results.

Location and Access

l The property is located approximately 31 km SW of the

town of Kenora, Ontario at approximately Lat. U 9 degrees 38'N,

J Long. 9 k d egrees 50'W. The property lies adjacent to the SW

shore of Squaw Lake which is part of the Lake of the Woods

water system,

l Access to the property is via water in summer and winter

roads on the lakes in winter.

l l

Claim Status

l No claim status (ownership and assessment status) has

been ascertained by the author. The current survey covered

l parts of the following 30 contiguous unpatented mining claims

B in the Shoal Lake Area, Kenora Mining Division, believed to be

held by Teeshin Resources Inc:

lClaim Number Township

g 977847-977848 incl (2) Shoal Lake Area

B 977850-977859 incl (10)

" 977865-977874 incl (10)

B 977878-977881 incl (4)

l

l

l

l

l

1055804 (1)

1064303-1064304 (2)

1064312 (l)

Total of 30 claims

l Personnel

The following personnel were directly involved with the

l project in February, 1988:

Scott Kerr Timmins, Ontario

l Paul Frederick Timmins, Ontario

- 2 -

ECHO BAY and BOYS TWP.

SQUAW

I06430X i

l—————{977869 {97786897

1 L^KE O Jl 977J4JJ 977850 {977851

97J063 1977854 j 9778/3 1977

_____l....LA-.

[|0643I2 J977856J 977857 l 9778581^859

—-Hy

OGEMA

BAY

1064303 j. — — —l. — — 971870 !

l1977866 j 977865

l

— , J97787I 977872 977873 '977874•y/r-i—.jir 977880

— —977879

977881

977878

r* H^

^G\ Ob

LABYRNTH

SHOALLAKE

AREA

BAY

W?

*ff*56

^^

EXSICS EXPLORATION LTD.f A BM UN. N*-mftftt fi. IMB^v f^^. f^^^M tet TdMtMMi NMfMil

CLIENT: TEESHIN RESOURCES INC.PROPERTY: SQUAW LAKE ORO PROPERTYTITLE:

CLAIM LOCATION MAPOar*:JUNE 1988Drawn: P.6.

Stal|M".!X2mll*Inftrp:

NTS:Job No, EE-126

- **y*chica v.t.'.v-A- •g'faX j * ~\'A*iac'! '~ ? k "-VS?

r BK-""'* ^ K •^^y^).

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z.y--ggL-fcJ* - ^ T K *--rW

EXSICS EXPLORATION LTD.PA BM MM. P4N-7X1Suit* O. (WU** BUi. ThHlM tot

J "-. f \ - : ' —~ ;"~"^ L--^--" - i -^: ' __ - j/titnr* , ^ J ___- -.~ "~ CLIENT: TEESHIN RESOURCES INC.PROPERTY: SQUAW LAKE GRID PROPERTY

GRID SKETCH LOCATIONScale: kioo.ooo NTS:

l l

Survey Pa r am e t e r s

l MaRnetometer Survey

The grid was covered on 100 m line spacing with a reading

J interval ol 25 meters. The resultant total magnetic field was

. recorded using the following parameters:

" Instrument: Scintrex MP-2 Proton Precession Magnetometer

l Parameter Measured: Earth's total Magnetic Field in

l

l

l

l

l

l

l

l

l

l

l

l

nano-teslas

Diurnal s Corrected by Base Line Looping

Accuracy: -i-/- 10 nano-teslas

Reading Interval: 25 meters

Contour Interval: 0,100,300,600,1000...nano-teslas

Datum Subtracted for Plotting: 59000 nano-teslas

Data Presentation: Plan Form Map No. l, 1:2500

VLF-EM Survey

A total of 35 km of VLF survey was conducted on the

property, covering the entire claim group. The VLF method is

a high frequency (relatively) EM technique which employs the

use of VLF transmitting stations which operate world wide, for

submarine communications. The magnetic field generated from

these vertical antennas is horizontal and concentric. This

primary field will induce a secondary field in any conductor

properly coupled with the station direction.

llM The VLF-EM method measures the vertical component of the

secondary field. Therefore a station should be chosen which is

l on strike with the expected strike of the conductor one is

searching for. This is called Maximum Coupling and in reality

f stations up to k 5 degrees off strike can be used. Because of

. the high frequency of this method, weak conductive features

* will be detected, including some overburden features,

l Therefore interpretation of VLF data should be done

discriminately and used in conjunction with other methods,

l Under some circumstances structural interpretation can be

ascertained if some knowledge of the bedrock is available.

™ Different parameters of the VLF technique can be

H measured. The "dip angle" or plane of the resultant field was

measured using the following parameters:

l Instrument: Crone radem, VLF Receiver

Transmitter Station: Cutler Maine, (NAA)

m Parameter Measured: In-phase Dip Angles

M Frequency: 24.0 KHZ

Direction to Station: 100 degrees True

l All readings taken facing 280 degrees True

Data Presentation: Dip Angle Plan Map No.2, 1:2500

l profiled

m Fraser Filterd Dip Angle Map

™ No. 3, 1:2500

l

l

l


Survey Results

The VLF was successful in outlining a number of

conductors which would appear to be legitimate bedrock

responses.

The most northerly structure extends from L100 ME to L

200 MW striking at 300 MN where it is then broken and strikes

from L kOO MW to 1. 800 MW at 300 MN to 150 MN. The western

portion of this zone has coincidental geochemical anomalies,

as indicated by the Soils Geochemistry Map, from Teeshin

Resources Inc. Only a rough copy of this map was made

available, therefore it will not be included in this report.

A structure running more or less along the base line was

also located. This zone appears to extend off the grid in the

east and as far west as L 700 MW, striking from just north of

the base line in the east and west, while dipping slightly

south of the base line in the central section.

This zone lies on the northern flank of a magnetic low

between L 600 ME and L 200 MW, which may be an indication of

some sort of alteration in this area.

The eastern section of this structure tends to broaden

out to the south. This may be due to stringer type material

within or extending from the main zone.

This zone also has coincidental geochemical anomalies at

various points, as indicated by the Soil Geochemistry Map.

- 5 -


A third zone runs from L 800 ME, and most likely extends

off the grid in the west, striking from 400 MS to 150 MS.

This structure appears broken in the areas of L 500 ME and

L 500 ME and L 500 MW, which may be a result of some sort of

alteration, as indicated by magnetic lows in these areas.

This area also has a number of geochemical anomalies

associated with it, as shown by the Soil Geochemistry Map.

A zone running parallel and south of this extends from L

600 ME to L 1100 MW and strikes from 700 MS to 400 MS. This

structure appears to merge with the previous zone in the east

which may be in part an overburden response, however it should

not be dismissed as such without further testing.

A zone running from L 700 MW to L 1000 MW and striking at

850 MS has coincidental geochemical anomalies as shown by the

Soil Geochemistry Map.

Conductors along the southern boundary of the grid would

appear to be overburden responses, but should not be dismissed

as such without further testing.

- 6


CPUSIjjsions and Recommendations

The surveys performed were successful in outlining a

number of areas of interest. Many of the conductors located

tend to lie along overburden horizons, however because of the

presence of strong magnetic highs and lows, and the

geochemical results for these areas, none of the zones

outlined should be dismissed as overburden responses.

Fol lowup work is recommended, particularly in the

northern portion of the grid. A number of geophysical surveys

such as Induced Polarization may give better definition of

the zones, outlined in this report.

Respectfully submitted,

J. C. Grant

- 7 -


CERTIFICATE OF QUALIFICATIONS

I, John Charles Grant do hereby certify:

1. that I am a geophysicist and reside at Lot 2Martineau Avenue, Kamiskotia Lake, Timmins, Ontario.

2. that I am a Fellow of the Geological Association of Canada.

3. that I am a member of the Certified Engineering Technologist Association.

k. t hat I graduated from Cambrian College of Applied Arts and Technology, Sudbury r *MIJMI.S in l')'/*; w i. Ui an Honour's diploma in Geology Technology.

5. that I have practised my profession continuously for 13 years.

6. that my report on SQUAW LAKE GRID PROPERTY forTEESHIN RESOURCES INC. is based on work carried out under my supervision.

k. I hold no specific or special interest in the described property. I have been retained as a Consulting Geophysicist for "the property".

Dated this 7'28th at Timmins, On

une 1988

John C. Grant

APPENDICES

APPENDIX A

l

l


SCIIMTREXearth science division

Proton Precession Magnetometer for Portable or Base Station Use

features

,*

*

*

*

fr-

MP-2

1 gamma sensitivity and accuracy over range of 20,000 to 100,000 gammas.Operates in very high gradients, to 5000 gammas per metre.Ultra small size and weight.Up to 25,000 readings from only 8 D cells.Battery pack isolated from electronics for corrosion protection.Battery pack easily extended for winter use.Light-emitting diode digital display, with complete test feature.Unique no-glare polarized reflector permits easy reading in bright sunlight.Indicator light warning of excessive gradient, ambient noise or electronic failure.Digital readout of battery voltage.Rugged all metal housing for rough field use at all temperatures.Automatic recycling or external trigger features permit ready conversion to base station use.Short reading time.Broad operating temperature range.

sciisrraex

The MP-2 is a portable one gamma proton precession magnetometer for field survey or base station use. The optimized design of sen sor and circuitry using the latest CMOS com ponents has resulted in a very light weight, low power consumption, rugged and reliable magnetometer.

Light emitting diodes coupled with an in genious optically polarized reflector combine solid state reliability with easy reading even In bright sunlight.

A standard automatic recycling feature allows ready use of the MP-2. with suitable (optional) Interfacing, as a base station recorder In analogue or ditlgal form. Alternatively, a remote trigger can be used.

The noise-cancelling dual-coil sensor and elec tronics have been so designed as to effectively eliminate reading problems due lo virtually all magnetic gradients which may be encountered In field survey conditions.

a world of discovery

lli;iiiiiiiiiiiiiit - j* ' ~

lil

TECHNICAL DESCRIPTION OF M P-2 MAGNETOMETER SCINTREX

RESOLUTION

TOTAL FIELD ACCURACY

RANGE

INTERNAL MEASURING PROGRAMME

EXTERNAL TRIGGER

DISPLAY

RECORDER OUTPUT (Optional)

GRADIENT TOLERANCE

POWER SOURCE

SENSOR

HARNESS

OPERATING TEMPERATURE TANGE

SIZE

WEIGHTS

1 Gamma.

± 1 Gamma over full operating range.

20,000 to 100,000 gammas in 25 overlapping steps.

Single reading — 3.7 seconds. Recyc. feature permits automatic repetitive readings 3.7 seconds intervals.

External trigger input permits use of sampling intervals longer than 3.7 seconds.

5 digit LED (Light Emitting Diode) readout dis playing total magnetic field in gammas or nor malized battery voltage.

Multiplied precession frequency and gale time outputs for Interfacing with Incremental tape recorders (eg. Increlogger) for digital recor ding. As an additional option a digital to analogue converter is available for use with analogue recorders.

Up to 5000 gammas/metre.

8 alkaline "D" cells provlce up to 25,000 readings at 25* C under reasonable signal/noise conditions (less at lower temperatures). Premium carbon-zinc cells provide about 40V* of this number.

Omnidirectional, shielded, noise-cancelling dual coil, optimized for high gradient tolerance.

Complete for operation with staff or back pack sensor.

-35eC to *600C.

Console, with batteries: 80 x 160 x 250mm. Sensor: 80 x 150mm. Staff: 30 x 1550mm. (extended)

30 x 600 mm. (collapsed)

Console, with batteries: 1.8kg. Sensor: 1.3kg. Staff: 0.6kg.

SCINTREX LIMITED222 Snidercroft Road,Concord, Ontario, Canada L4K 185

(tint tf-9-tteo. iticx i

l

APPENDIX B

i lCRONE GEOPHYSICS LIMITED

RADEM VLF EM RECEIVER

An EM receiver mea-uning the HFiLD SIMENG111.l )IP AN( ?I.H nml QUAI MATUKE components of ihe VIJcoiiiinunicfilinns slnlions

l l l l l l l

This is a tugged, simple lo opemle. ONE MAN EM unit, it can be used without line culling and is thus ideally suited forGROUND LOCATION or AIIWORNE CONDUCTORS and RECONNAISANCE SURVEYS of MINERAL SHOWINGS.This instrument utilizes hiqher than noimal EM frequencies and is capable of detecting poorly conductive sulphide deposits and fiiull ZOIIPS. It accurafply isolates BANDED CONDUCTORS and operates through areas of HIGH POWERLINE NOISE. The method is capable of deep penetration but due lo the high frequency used its penetration is limited In areas of clay and conductive overburden.

The DIP ANGLF; measutemenl detects a conductor from a considerable distance and is used primarily for location conductors. The FIELD STRENGTH measurement is used to define the shape and attitude of the conductor.

Instrument Sales, Rental and Repair ServicesContract Survey ServicesConsulting ServicesComputer Plotting and Processing Services

l l l

l IEAD OFFICE: 3607 Wolfedale Rd.MISSISSAUGA, Ontario CANADA L5C 1V8 PHONE: (416) 270 0096 TELEX: 06-961260


OF PRIMARY FIELD: NUMBER OF STATIONS: STATIONS AVAILABLE:

SPECIFICATIONS'VLF Communications Stations l to 25 KHz7 Switch SelectableThe Seven Stations May Be Selected From:

Standard

Optional

CODECMswAMl!BOFEMSODNCUNYJTJBA

STATION A LOCATIONCutler, Maine Seattle, Washington Annapolis, Maryland Laulualei, Hawaii Bordeaux, Frace Rugby, England Moscow, Russia Odessa (Black Sea) Bernoulli. Australia l lelgelend, Norway Yosamai, Japan Tokyo, Japan

CALL SIGN FREQUENCYNAA.............. 17,8KHz 2 'hNLK. ............. 24.8KHzNSS.............. 21.4KHzNPM.............. 23.4KHzNWU.............. 15.1 KHzGBR.............. 16.0KHzUMS.............. 17.1KHzEWB.............. 15.6KHzNWC.............. 22.3KHzJXZ............... 17.6KHzNDT............... 17.4KHzJG2AR............ 20.0KHz.................. 23.6KHzBuenos Aires, Argentina

CHECK THAT STATION IS TRANSMUTING: Audible signal from speakerPARAMETERS MEASURED:(1) DIP ANGLE In degrees of the magnetic field component, from the horizontal, of the major axis of the polarization

ellipse. Detected by a minimum on the field strength meter and read from an inclinometer with a range of ± '/i0 .(2) FIELD S TRENGI 1 1 (total or horizontal) of the magnetic component of the VLF field, (amplitude of the major axis

of the polarization ellipse). Measured as a percent of normal field strength established at a base station. Accuracy dependent on signal. Meter has two ranges: 0-300^ and G-600%.

(?) QUADRATURE component of the magnetic field, perpendicular in direction to the resultant field, as a percent of the normal field strength, (amplitude of the minor axis of the polarization ellipse). This is the minimum reading of the Field Strength meter obtained when measuring the dip angle. Accuracy ±2*fc.

OPERATING TEMPERATURE RANGE: - 400C to 500C ( - 400F to 1200F) DIMENSIONS: 9cmxl9cmx27cm (3IX2 "x7l7,"xl01/,") SHIPPING DIMENSIONS: 30cmxl4cmx36cm (W x 5',*" x 14") WEIGHT: 2.7kg(6lbs) SHIPPING WEIGHT: 6.0 kg (13 Ibs)BATTERIES: 2 of 9 volt

Average Life Expectancy20 Hours for Continuous Operation

'Specifications subject lo change without notice* ,

APPENDIX C

Ministry ofNorthern Developmentand Mines

Ontario

Geophyslcal-Geologlcal-Geochemical Technical Data Statement

. : ' ; ; lS : :^ :-ai.': . : ''. : . File_

l l l l l l l l l l

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type ofTownship or Area OKexa \Claim Holder(s)^.

/ **

l l

Survey Company— Author of Report. Address of Author

E XA/\\0\ ^

Covering Dates of Survey.

Total Miles of Line Cut —(linecutting to office)

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.

DAYSper claim

y*—Radiometric.

Gejpchcmicaj

AIRBORNE CREDITS (Special provhion credit! do/Tt a,————.——————————. f ̂ silectromagnetic

(en

Res. Geol. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED , List numerically

(prefix) (number)

i

l*r 6

l

TOTAL CLAIMS.

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.S-- Ministry oi Heport o i VVOIK Northern Developmentand Mines (Geoptiv^ic. '. l~"'' logical.

Ontario -f—————————figocb?" 1 " f1 * flPM i

^cns-• '6

52E18SW8545 2.18385 SHOAL LAKE

,CI*. m Hold* Ul

900

\M

^TtC. ^ \JLP , v-

Sjtspoccjes uni fi * X ..^*f .?iv3LP.

. .Sin vcy Company O l r^ O J^-t- IO k

O^-T* of SurVty (fr

and Adclfet* of Author (o* Geo Technical report)

P.O.

Date of Survey (from 8. lol

Day l Wo l Tr j Day l Mo. l V

hotel Miles of line Cut

2. Jo

Credits Requesled pet EacnClaim in Columns at right\3,

Special Provisions

For first survey:

Entet 40 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

RECEIVE

WAR 8

MINING LANDS SEAirborne Credits

Note: Special provisions

Geophysical Oayt P* rClaim

- Electromagnetic j

- Magnetometer r^- Radiometric |

- Other

Geological j

Geochemical

GeophysicalDays per

Claim

- Electromagnetic j

L/ - Magnetometer

- Radiometric |U

- Other i

rGeochemical

l Days per i Claim

Electromagneticcredits do not applyto Airborne Surveys Magnetometer

i Radiometric

Expenditures {excludes power stripping)t VP* O* Work

, ICalculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

^ 15 ^

Total D* y i Crcdm may be apportioned at (he claim holder'! - choice Enter number of days.ered.u pef claim selected m columns at right. i

Of A0cnj (Siynature)

Certification Verifying Report of Work

Mining Claims T raversed ( List in n umeiical sequence!Mining Clair

Prefix Number

ST1S-.-- - q, ——-

":"yj.._...

rv-

654

•857

80

^R

Expend. Days C',

40

60

O40^LC4-Q

40

-— ^.^Mininj Claim _ —^ —- Prefix T Number

M KENORAinlAM

-19

E xppnd Dnv* C'

flSJ9PM

3456

177*3*Total number of rnmmg claims covered by this report Of work.

For Office Use OnlyTotal Days C' Recorded

litoDate Recorded

Q fie. Z(Da* Approved as R

l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the wo* or witnessed same during and/or after its completion and the annexed report is true

Name and Postal Address,ot Person Certifying

s, AO Hfav\Date Certified gee lifted bylSigottural ^

y^T^^/^-^—

Ministry oiNorthern Developmentand Mines

Technical Assessment Work Credits

OntarioMay 5. 1989

2.12385Report ol

Recorded Holder

TEESHIN RESOURCES LTD.Township or Ara

SHOAL LAKE AREAType of survey and number of

Assessment days credit per claim Mining Claims Aneoad

Geophysical

Electromagnetic . 31

Magnetometer.

Radiometric _

16

Induced polarization .

Other.-^^———^

.days

.days

.days

-days

.days

K 977847-48 977850 to 859 1ncl. 977865 to 874 1ncl. 977878 to 881 Incl.

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

Geological

Geochemical.

-days

-days

Man days

Special provision

Airborne LJ

Ground

j j 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.

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

No credits have been allowed for the following mining claims

j | not sufficiently covered by the survey [~| iniufficient technical data filed

The Mining Recorder may reduce (he above crediti if necessary in order Ihat the total number of approved assessment days recorded on etch claim does not exceed the maximum allowed as follows: Geophysical-80; Geologoeal - 40; Geochemical - 40; Section 77(191 -60.

128 (8VI 2)

Mining Lands Section 3rd Floor, 880 Bay Street Toronto, Ontario MSS 1Z8

Telephone: (416) 965-4888

June S, 1989 Your file: W8901-61 Our file: 2.12385

Mining RecorderMinistry of Northern Oevelopnent and Nines808 Robertson StreetP.O. Box 5200Kenora, OntarioP8N 3X9

Dear Sir:

Re: Notice of Intent dated May 5, 1989 Geophysical (Electromagnetic and Magnetometer) Survey submitted on Mining Claims K 977847 et al in Shoal Lake Area.

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

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

Yours sincerely.

M.R. CowanProvincial Manager, Mining LandsMines A Minerals Division

RM:eb Enclosure

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

Teeshin Resources Ltd. Oakville, Ontario

John Grant Tinmns, Ontario

Resident Geologist Kenora, Ontario

Mel de Quadros Toronto, Ontario

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