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42A09NW2006 2.19806 WILKIE 010 MAGNETOMETER AND VLF REPORT COMBINED WITH GEOLOGY AND PROSPECTING REPORT WILKIE TOWNSHIP LARDER LAKE MINING DIVISION CLAIM 1225422 V L.M. DYMENT J.A. KIDSTON BOX 66 SWASTIKA, ONTARIO POK 1TO OCTOBER 21, 1999 RECEIVED prr ^ ^ f ~-n
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Page 1: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

42A09NW2006 2.19806 WILKIE 010

MAGNETOMETER AND VLF REPORT

COMBINED WITH

GEOLOGY AND PROSPECTING REPORT

WILKIE TOWNSHIP

LARDER LAKE MINING DIVISION

CLAIM 1225422

V

L.M. DYMENT J.A. KIDSTON BOX 66SWASTIKA, ONTARIO POK 1TO

OCTOBER 21, 1999

RECEIVEDprr ^ ^ f~-n

Page 2: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

42A09NW2006 2.19806

TABLE OF CONTENTS

WILKIE 010C

PAGE SUMMARY..............................................l

INTRODUCTION.........................................2

LOCATION AND ACCESS..................................3

CLAIM GROUP..........................................3

LINECUTTING..........................................3

REGIONAL GEOLOGY.....................................4

PROPERTY GEOLOGY.....................................5

PREVIOUS WORK........................................5

SURVEY PROCEDURE AND THEORY..........................6

INTERPRETATION.......................................7

CONCLUSION...........................................8

BIBLIOGRAPHY.........................................9

APPENDIX l - CERTIFICATION APPENDIX 2 - INSTRUMENT

FIGURES

1) TWP LOCATION MAP2) CLAIM LOCATION MAP3) REGIONAL GEOLOGY MAP4) PROPERTY GEOLOGY MAP5) PREVIOUS WORK6) MAG MAP7) VLF PROFILES8) VLF FRASER FILTER9) GEOLOGY AND PROSPECTING

1:1250l" TO 1/2 MILE1:12501:5000 (COMPILATION)

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SUMMARY

BETWEEN JULY 15 AND OCTOBER 21, 1999, A LINECUTTING PROGRAM COMBINED WITH MAGNETIC, VLF, GEOLOGICAL MAPPING, AND PROSPECTING WAS CONDUCTED,

THE WORK WAS CONDUCTED IN WILKIE TOWNSHIP (CLAIM MAP G3587) LARDER LAKE MINING DIVISION, FOR AND BY THE CLAIM HOLDERS L.M. DYMENT AND J.A KIDSTON (JOINT TENANTS).

THE SURVEYS DELINEATED THE FAULT-BOUNDED KIDD-MUNRO ASSEMBLAGE, SEVERAL MAFIC INTRUSIVE BODIES, AND AEM ANOMALIES AS SHOWN ON OGS MAP 80574.

THE GEOLOGICAL AND STRUCTURAL SETTING MAY PROVIDE A POSSIBLE TARGET FOR HYDROTHERMAL GOLD MINERALIZATION OR A POLYMETALLIC BODY OF ECONOMIC PROPORTION.

AN INDUCED POLARIZARION OR HORIZONTAL LOOP SURVEY IS RECOMMENDED AS THE NEXT STEP OF EXPLORATION.

PAGE l

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INTRODUCTION

RECENT TIMBER HAULAGE ROADS WITH A BRIDGE ACROSS SHALLOW RIVER HAVE MADE THIS NORTH PROPERTY MORE ACCESSIBLE FOR WORKING. THE PROPERTY HAS BEEN STAKED NUMEROUS TIMES WITH NO RECORDED WORK BEING DONE ON IT, WITH THE EXCEPTION OF A SMALL LOCATION GRID AND RECON. MAG AND HLEM IN 1965 (fig 5). A DIAMOND DRILL HOLE WAS DRILLED AT THIS TIME FROM SOUTH TO NORTH ON, PROBABLY, A PRIVATELY FLOWN AEM Se AMAG SURVEY (WORK SINCE 1965 IN THE AREA HAS SHOWN THE ROCK FORMATION DIPS TO THE NORTH.)

9 AEM ANOMALIES (OGS 80574) ARE SHOWN ON THIS PROPERTY THAT HAVE NEVER SEEN ANY EXTENSIVE WORK DONE TO PROPERLY LOCATE THEM. THEY PROBABLY REPRESENT THE CONTACT BETWEEN THE CLASTIC AND CHEMICAL METASEDIMENTARY ROCKS TO THE NORTH AND THE MAFIC VOLCANIC ROCKS TO THE SOUTH.

FROM THE 1965 DDK IT WAS KNOWN THAT THE OVERBURDEN WOULD BE DEEP BUT FROM PAST EXPERIENCE THE VLF SHOULD BE ABLE TO LOCATE THEM. THEY MAY BE SUBTLE BUT BY USING THE FRASER FILTER ONE SHOULD BE ABLE TO PINPOINT THEIR LOCATION.

PAGE 2

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COULSON

tec '"f*.

FIG. l.

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LOCATION AND ACCESS

THE WILKIE CLAIMS MAY BE REACHED BY TAKING THE CARR TWP ROAD #2 NORTH FROM MATHESON (fig 1) FOR 14km. APPROXIMATELY 200 YARDS PAST THE SHALLOW RIVER BRIDGE IS A TRAIL LEADING TO THE EAST FOR 3.5 km BY ATV OR BY FOOT TO THE PROPERTY.

CLAIM GROUP

#____________UNITS_____LOT______CON_____RECORDED 1225422 12 2,3,4 IV NOV 25, 1997

LINECUTTING

AS NOTED IN THE INTRODUCTION, SPECIAL CARE WAS TAKEN IN PLACING THE GRID TO OPTIMIZE THE BENEFIT OF THE RECENT RELEASE OF OGS MAP 3367 1999.THE GRID CONSISTED OF 22.4km, LINES BEING CUT EVERY 100m, 400m NORTH AND 400m SOUTH ACROSS A 2400m BASELINE. THE CONTRACTOR WAS MAILLET EXPLORATION SERVICES.

PAGE 3

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L- - -J - - -4

LKIE

III jg

1189926 122611 183376. J 833771 1833770

Q

! 1167637 r||67698

i- IV IL v,:u -L li.939203 I9392O2 I9B9ZOI '1939207 193920* 939209

682493 1682490 l 7OO9H 7O09I2 e i7464

L -l-——e4-—-— — —r- — — H .

FIG. 2.

Page 8: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

REGIONAL GEOLOGY

THE FOLLOWING IS QUOTED FROM BOWEN 1988:

"THE AREA IS UNDERLAIN BY ARCHEAN ROCKS OF THE ABITIBI GREENSTONE BELT. THE ABITIBI GREENSTONE BELT IS THE LARGEST GREENSTONE BELT IN THE CANADIAN SHIELD AND THE MOST PROLIFIC IN TERMS OF MINERAL PRODUCTION AND POTENTIAL.

CLASTIC METASEDIMENTARY ROCKS MAKE UP LESS THAN 20*!? OF THE ROCK TYPES AND CHEMICAL METASEDIMENTARY ROCKS LESS THAN Sir. ULTRAMAFIC INTRUSIVE PERIDOTITE AND POSSIBLE FLOWS COMPRISE ABOUT Id's? OF THE UNITS AND MAFIC INTRUSIVES PROBABLY LESS THAN 5*3?.

TWO AGES OF LATE ARCHEAN TO PROTEROZOIC DIABASE DIKES CUT ALL OLDER ROCK UNITS. THE NORTH TRENDING DIABASE DIKES ARE OLDER THAN THE NORTHEAST TRENDING DIKES. A THICK MANTLE OF PLEISTOCENE TILL, CLAY, LAKE BOTTOM DEPOSITS AND OUTWASH, COVERS OUTCROP IN THE AREA. ONLY A RELATIVELY THIN ORGANIC LAYER COVERS MOST OF THE AREA WITH THICKER DEPOSITS OCCURRING IN THE SWAMPY PORTIONS."

IN 1984 THE OGS UNDERTOOK AN INPUT AND AEM SURVEY OVER 40 TOWNSHIPS INCLUDING WILKIE TOWNSHIP.

PAGE 4

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The Western Abitibi Subprovince

SESK SkeodSL Sr. Laurent ^SR Staughfon-Roquemaure V

ST Shining TreeTO TisdaleTl TimiskamingTN Three Notions

VE VondetteWA Watabeag

WN Whitneyeag .jXy L^'\Vijl^C"/-rf^'J '{'^ J ; ., V

By .-•'V-v'-V.^ i"'H''r^^';'*- 1 '-^'^S'''^ ;'-':-"-^'\ ''

•\3Q : W\'-'i:- ^^/X^'^^^-^l V ''*"

l i i i t

Assemf i AbbreviationsAD Ado.BO BradetteBK BlakelockBL Bartlett

BM BowmanBR Bloke River

BS BostonCK Cabot-Kelvin

CP Cotharine-Pacaud

CR Carscallen

DL DeloroOR Duff-Coulson-Rond

DT DetourED EldoradoGA GauthierOK Geikie

GR GarrisonGT Garnet-ToomsHN HonrahanHE HearstHK Hong KongHL Halliday

HO HoyleHS Halcrow-Swayiei

HW Horwood

KK Kamiskotia

KM Kldd-Munro v'^'XV'^l HW/TV-KN Kinojevis ~ "*

NorthKS Klnoievis

. South 'S HS Krist (——^ , GT

LD Lower DetourLL Larder LakeME McElroyMN MarionMR Musk ego-Re e ve s

MT Midlothian

NT NatalNW NoseworthyP PeterlongPP PorcupineRO RidoutRN Raney- NewtonSA ScapaSG Sinclair

48*QO' N

m —O

CDm or~ o o

2] POJ

Huronian Supergroup (Proterozoic)

iGranitoid and metasedimentary rocks (Opatica Subprovince^

•••"::;w Granitoid rocksReverse fault

Page 10: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

PROPERTY GEOLOGY

THE PROPERTY, AS SHOWN BY OGS 1999 MAP 3367, IS MAINLY COVERED BY MAFIC METAVOLCANIC ROCKS IN CONTACT TO THE NORTH CLASTIC AND CHEMICAL METASEDIMENTARY ROCKS. THE CONTACT APPEARS TO BE DELINEATED BY A STRING OF AEM ANOMALIES (fig 4). FROM ONE DRILL HOLE ON THE PROPERTYM POSSIBLY ALONG THE VOLCANIC-SEDIMENT CONTACT, THE LOG READ QUARTZ-SERICITE SCHIST, SLATE, GREY QUARTZITE, AND GABBRO. NO KNOWN OUTCROPS HAVE BEEN FOUND TO DATE ON THE PROPERTY.

PREVIOUS WORK

THE ONLY WORK RECORDED WAS DONE BY TWIN FALLS SYNDICATE OVER A SMALL RECONNAISSANCE GRID TN 1965 AND CONSISTED OF:

1) RECON GRID2) MAG S HLEM3) l DDK (DRILLED N 30 DEGREES E)

0-186' OVB186-197' QTZ SERICITE SCHIST 197-362' GREY SLATE (DIP NORTH) 362-450' GREY QUARTZITE 450-555' GABBRO

PAGE 5

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PROPERTY GEOLOGY

u^ — ^fc^~^~^^ H' " ^".TT----^?^:.N* "^-sCT——' w w".vt""" " "- "''-' r*

,Vff*""~ T^M —M """^ -—^-v^w-v '

48 0 38' 30"

The letter "D* preceding a code refen: to data compiled from diamond j-, drill logs filed for assessment work aedrts of from unpublished diamond

drill logs made available to the author by mineral exploration compai lies. ^r*""*~ ^ The letter "G1 preceding a code refern to data interpreted from pubiisned

,J geophysical data The letter "C1 precfdlng a code refers to data compiled 2 from previously published maps.

ONTARIO GEOLOGICAL SURVEY

EXPLORATION DATA MAP

GEOLOGICAL DATA INVENTORY FOLIO 401

LOork Sec-

|9g)7 CoiMp i /a-f To

WILKIE TOWNSHII

DISTRICT OF COCHRANE

Kilometre 0.5

Scale 1:31 680

O 0.5 1 Kitome

Mile 0.5 0.5

MapP.3367OGS l *?q 9

PRECAMBRIAN GEOLOGY

5 l Clastic and Chemical Matasadlmentafy Rocft* 5a Wacke5b SiltstoneSe Mudstone5d Grapnftic and pyritfc mudstone5e Schist5f ConglomerateSg Chert

DUFF-COULSON-RAND4 l FeteJc Metavolcanlc flocks

4a Ftows - massive and flow laminated4b Autodastic flow lyeccta and/or hyalodaatfte4c Tuff and lapilli tuir4d Tufl breeds, heterolithic, pyradastic4e Schist4f SpherUfttc4g QraphltB breccia4h Quartz ±fBkJsporphanoaysttcc

Z Mafic M^avotcartc Rocks 2a Flows - massive 2b Flows-pWowed 2c Pillow breccia2d Flow top breccia f hyatodastita 2e Schist2f Tuff and lapilli tuff 2g Amygdaloidal 2h Variolitic 2j GfBphrte breccia - angular to rounded fragments in a

graphite ± chtoritn ± carbonate matrix 2k Leucmsne-beartng 2m Plagtodase-nch 2o GaDbroic-texiureo

KIDD-MUNROUltramafic and Mafic M0tavoJcanta RocKs (KomatJites)la Rows-massive1b Flows - spinifex a/id/or polysuture textured1c Schist - tate * cartxinaie-bearlng1d Basattfc komatiite - massive flows

Page 12: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

d Cor. Uorvi-

P. ModtnceA p-l Dflti7ir,(ifi*P'*'Te. .

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SURVEY PROCEDURE AND THEORY

ELECTROMAGNETIC SURVEY

THE "RADEM" UNIT IS ESSENTIALLY A SPECIALLY DESIGNED RADIO RECEIVER WHICH UTILIZES VERY LOW FREQUENCY (VLF) RADIO SIGNALS BROADCAST BY TRANSMITTERS LOCATED THROUGHOUT THE WORLD.

THE RECEIVING UNIT IS USED TO MEASURE THE DIRECTION OF THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE BODY. THE PRESENCE AND POSITION CAN THEREFORE BE DETERMINED BY MEASURING THE DIP ANGLE OF THE RESULTANT FIELD AT REGULAR INTERVALS.

THE DIP ANGLE IS READ BY ALIGNING THE INTRUMENT INTO A POSITION PARALLEL TO THE FIELD DIRECTION IN A HORIZONTAL POSITION THEN RAISING IT INTO A VERTICAL POSITION AND ROTATING ABOUT A VERTICAL AXIS UNTIL A RADIO NULL IS HEARD. THE DIP ANGLE IS THEN RECORDED AS IS THE DIRECTION IN WHICH THE ARROW POINTS. THE BASE STATION SET UP WHEN THE SURVEY WAS INITIATED MUST BE REVISITED FROM TIME TO TIME IN THE COURSE OF THE SURVEY IN ORDER TO DETECT ANY DIURNAL DRIFTING IN THE HORIZONTAL FIELD STRENGTH SIMILAR TO A MAGNETIC SURVEY.

MAGNETOMETER SURVEY

THE MAGNETIC METHOD IS BASED ON MEASURING ALTETRATION IN THE SHAPE AND MAGNITUDE OF THE EARTH'S NATURALLY OCURRING MAGNETIC FIELD CAUSED BY CHANGES IN THE MAGNETISM OF THE ROCKS OF THE EARTH.

THESE CHANGES IN MAGNETISM ARE DUE MAINLY TO THE PRESENCE OF THE MAGNETIC MINERALS, OF WHICH THE MOST COMMON IS MAGNETITE, AND TO A LESSER EXTENT, ILMENITE, AND SOME LESS COMMON MINERALS.

THE MAGNETICS DATA WERE COLLECTED WITH A PROTON PRECESSION MAGNETOMETER, WHICH MEASURES THE ABSOLUTE VALUE OF THE TOTAL MAGNETIC FIELD OF THE EARTH WITH AN ACCURACY OF H- OR MINUS in TESLA. THE MAGNETOMETER IS CARRIED DOWN THE SURVEY LINE BY A SINGLE OPERATOR, WITH THE SENSOR MOUNTED ON A SHORT POLE TO REMOVE IT FROM THE SURFACE GEOLOGICAL NOISE. READINGS ARE NORMALLY TAKEN AT 25m INTERVALS, AND AT 12.5m INTERVALS WHERE THE OPERATOR OBSERVES A HIGH GRADIENT (ANOMALY).

THE READINGS ARE CORRECTED FOR CHANGES IN THE EARTH'S TOTAL FIELD (DIURNAL DRIFT) BY MEASURING AND RECORDING THE DRIFT WITH A BASE STATION.

PAGE 6

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INTERPRATION

GEOLOGY AND PROSPECTING

MAPPING AND PROSPECTING WITH A REBAR PROBE FOR NEAR SURFACE OUTCROP OR BOULDERS WAS CONDUCTED AFTER THE GEOPHYSICAL SURVEYS.THE SEARCH FOR NEAR SURFACE EVIDENCE WAS CONDUCTED MAINLY IN THE NORTH CENTRAL AND NORTH WEST QUADRANT OF THE PROPERTY, THESE AREAS BEING THE HITHERTO UNEXPLORED LOCATION OF 9 AEM ANOMALIES (OGS 1984 MAP 80574). THE REST OF THE PROPERTY WAS MAPPED FOR TOPOGRAPHY, VEGETATION AND WATER SOURCES AS WELL AS AVAILABLE ACCESS FOR FUTURE REFERENCE. UNFORTUNATELY NO OUTCROPS OR BOULDERS WERE LOCATED. A GEOLOGICAL AND PROSPECTING MAP IS IN THE BACK POCKET OF THIS REPORT.

MAGNETOMETER SURVEY

A RATHER BLAND PICTURE SHOWS UP WITH THE MAGNETOMETER SURVEY WITH THE EXCEPTION OF AN ALREADY INTERPRETED DIABASE DIKE RUNNING NORTH-SOUTH ON LINES 2W-4W (OGS MAP 1999 MAP P3367). THE POSITIONING OF THIS DIABASE DIKE AS SHOWN ON NUMEROUS OGS GEOLOGY AND GEOPHYSICAL MAPS FIVES CREDENCE TO THE PROPER LOCATION OF THE GRID IN RELATION TO THE AEM ANOMALIES.

VLF SURVEY

A PROFILE MAP AS WELL AS A FRASER FILTER CONTOUR MAP CAN BE FOUND IN THE BACK POCKET OF THIS REPORT. A CASE CAN BE MADE FOR ANOMALIES A TO D, SUBTLE AS THEY APPEAR, TO REPRESENT THE 9 AEM ANOMALIES HITHERTO UNEXPLORED BUT LOCATED IN OGS MAP 1984 MAP 80574. THE OTHER ANOMALIES REMAIN OPEN TO INTERPRETATION. ANOMALY A FROM 7W TO 24W APPEARS TO REPRESENT THE CONTACT BETWEEN THE MAFIC VOLCANICS THAT COVER THE SOUTH PART OF THE PROPERTY AND THE CLASTIC AND CHEMICAL SEDIMENTARY ROCKS TO THE NORTH (fig 4).

PAGE 7

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CONCLUSION

THE PROPERTY SHOULD NOW BE SURVEYED WITH A MORE SOPHISTICATED AND DEEPER PENETRATING INSTRUMENT ie. HLEM OR I.P. PRIOR TO PICKING POSSIBLE DRILL TARGETS. SPECIAL EMPHASIS SHOULD BE PLACED ON THE VOLCANIC-SEDIMENTAARY CONTACT.

PAGE 8

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BIBLIOGRAPHY

1) TIMMINS-KIRKLAND LAKE MAP 2205 OGS 19722) MATHESON-BLACK RIVER AREA WILKIE TWP AEM-AMAG MAP 80574

OGS 1984 1:200003) GDIF 401 OGS 1987 WILKIE TWP4) OGS SPECIAL VOL 4 PT l OGS 19915) MONTEITH AREA PRECAMBRIAN GEOLOGY MAP P3367 OGS 1999

1:35000

PAGE 9

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APPENDIX l

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CERTIFICATE

l, Leslie Michael Dyment, residing in the township

of Marquis, Ontario, and having a mailing address of

Jomi Minerals and Expediting Ltd., Box 66, Swastika,

Ontario, POK 1TO, do hereby certify:

(1) That I am a Mining Technician having taken

the two year course at Haileybury School of

Mines, Haileybury, Ontario.

(2) That I have been employed in all phases of

mining exploration and developement for 40

years.

(3) That l did personally accumulate and set

forth the facts and knowledge in the

accompanying report and maps.

(4) That the accompanying report is true.

OCTOBER 21, 1999 LESLIE MICHAEL DYMENT SWASTIKA, ONTARIO

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APPENDIX 2

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,. . ^7- ^ * ,

CRONE GEOPHYSICS' LIMITED3607 WOLFEDALEJTOAD, MISSISSAUGA, ONTARIO, CANADA, L5C1V8

Phone: (416) 270-0096

Cable: CRONGEO, TORONTO

^.rA'..

f

JL -

This is a ruaaed simple to operate, ONE MAN EM unit. It can be used without line cutting te thus^M lv s^ed for GROUND LOCATION OF AIRBORNE CONDUCTORS and the CHECKING OF MiNPRAL SHOWINGS This instrument utilizes higher than normal EM frequencies and ish 3 d^^iw SMEMINATED SULPHIDE DEPOSITS and SMALL SULPHIDE BODIES itfely iso!aSs B9AN Dlb cbNDUCTORS and operates through areas of HIGH HYDRO NOISE The

is capable of deep penetration but due to the high frequency used Its penetration is lim.ted inOf rtav anrl ^-onHnative n

Page 21: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

SPECIFICATIONS

Code CM

J0URCE OF PRIMARY FIELD: VLF Communication Stations 12 to 24K hz

0UMBER OF STATIONS: 7 switch selectable

jTATlONS AVAILABLE: The seven stations my be selected from:

Station 4 Location Frequency Cutler, Maine.............................................................. .17.8 KHzSeattle, Washington........................................................ .18.6 KHz

AM Annapolis, Maryland ....................................................... .21.4 KHzH Laulualel, Hawaii .......................................................... .23.4 KHz00F Bordeaux, France .......................................................... .15.1 KHzg Rugby, England............................................................ .16.0 KHzHIS Gorki, Russia.............................................................. .17.1 KHzOD Odessa (Black Sea)......................................................... .15.6 KHz

NC Australia, N.W.C. ..........................,............................... .22.3 KHzYJ Yosamal, Japan............................................................ .17.4 KHzHN Hegaland, Norway ......................................................... .17.6 KHz

TJ Tokyo, Japan .............................................................. .20.0 KHzBA Buenos Aires .............................................................. .23.6 KHz

CHECK THAT STATION IS TRANSMITTING: Audible signal from speaker.

PARAMETERS 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 90* and an accuracy of i V4 *.

(2) FIELD STRENGTH (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 27e dependent on signal. Meter has two ranges: O 3007o and O 6007e.

(3) OUT-OF-PHASE component of the magnetic field, perpendicular in direction to the resultant field, as a percent of normal field strnegth, (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 ±27o.

OPERATING TEMPERATURE RANGE: -30*C (-20*F) to tSO'C (120*F)

DIMENSIONS AND WEIGHT:

SHIPPING:

BATTERIES:

9 x 19 x 27cm — 2.7Kg (6 Ib)

Instrument with foam lined wooden case, shipping wt. 6.0Kg (13 Ib)

2 of 9.volt Eveready 216Average life expectancy 20 hours fdrcontinuous operation

nep -

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^radTent Tolerance

Power:

Power Consumption:

Pu .ariz ing Power:

Number of Readings with l Battery Set

Frequency of Readings':

.*

Con trol s : *.

Output:

Indicators:

600 y/ft.12-"D" eel Is

< 50 Joules (V/sec) per reading

'0.8 A g 13.5 V for 1.5 sec. (3 second cycle)

0.8 A g 13.5 V for 3 sec. (6 second cycle)

2,000 - 10,000 depending on type of batteries " "" -

l every 3 seconds : l every 6 seconds

Pushbutton switchRange Selection switch - Slide switchfor 3 and 6 sec. located on P/C Board

5 digit incandescent filament . readout

LED pointLock Indicator - last three digitsof the display blanked off whenphaselock not achievedSegment Function Indicator - allsegments light up to permit visualInspection of the display function :

in ical :

'nstru.-ent: Dimension s -7" X 3-5" ^11"(18 cm X 3 cm X 28 on)

Vefght - 3 ?bs. (3-6 kg), including .batteries

Omn ('direct fen* I .-.ofse cancelling toroidal sensing head

f men s I on s - k 7/3" 02 cm) diameter- 4 3/3" {; l -im) height

- 3 I bs (l.-'i kg)

ensor:

Vo fght

*bien t Cond i t Ions :

vi ronmcn t a l :

Operating Temperature Range -

-i.0 0 F to 13' 0 r C-^0 0 C f.o 55 0 C)

Relative Humidity - O to '00?

.- tn-s.t^umont Jnd sensor case mjde of ' ' -pr-l a s 11 c

Page 23: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

Ontario Ministry ofNorthern Developmentand Mines

Declaration of Assessment Work Performed on Mining LandMining Act, Subsection 65(2) and 66(3), R.S.O. 1990

Transaction Number (office use)

w w z o.Assessment Files Research Imaging

lority of subsections 65(2) and 66(3) of the Mining Act. Under section 8 of the sed to review the assessment work and correspond with the mining land holder, dining Recorder, Ministry of Northern Development and Mines, 6th Floor,

42A09NH2006 2.19806 WILKIE 900

Instructions: - For work performed on Crown Lands before recording a claim, use form 0240. - Please type or print in ink.

1. Recorded holder(s) (Attach a list if necessary) 2. 1980 6Name

L. iAi^iE D^IK^MTAddress

1^0* CcCp

^mJ^q-STiKA , OjUT PoK JToName

T- /V WLi'D'oTOjOAddress

"BO^ (p (0

*3otjxP^-nKA OrOT P^K l To

Client Number

/S/ *?96~Telephone Number

705^- fcya- 3ob!LFax Number

Client Number

/ass-elTelephone Number

7os~- Ce y.a- 3ot,2.Fax Number

2. Type of work performed: Check ( ^ ) and report on only ONE of the following groups for this declaration.

i-v7i Geotechnical: prospecting, surveys, i—i Physical: drilling, stripping, l—^ assays and work under section 18 (regs) '—' trenchina and associated atrenching and associated assays Rehabilitation

Work Type

Dates Work Performed From 3 o

Day

/Month j Year

Global Positioning System Data (if available)

AiDay

Township/ Area

10Month

TcO

?9Year

PM or G-Plan Number

G. 35*78

Office UseCommodity

Total S Value of Work Claimed 1 3. (o -f 9NTS Reference

Mining Division i ^ a r d e. r

Resident Geologist, District cKtrfc/A n fL

i-a.k(Ui i

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical report (Attach a list if necessary)Name

/. fYlf/ke J}yA7^~AJ7~Address

^ox 66 Scc'/jSTWx'/c^ 0AJ"77 PoAT/ToName

Address

Name

Address

4. Certification by Recorded

RE

on 25 -''i ocGEOSCIENCF ASSESS"~Nr'

bolder or Agent

CEIVEDDE h LAK.h G DiViSJON

21 19Qfi

Telephone Number

Fax Number

Telephone Number

Fax Number

Telephone Number

Fax Number

\ /u ^--

i. Z - ;_______ , do hereby certify that l have personal knowledge of the facts set(Print Name)

forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.

Date0(LT

Telephone Number Fax Number

,. O, , S /t?

Page 24: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

5. , Work to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining; to the mining land where work was performed, at the time work was performed. A map showing the contiguous Unk

Mining Claim Number. Or if work was done on other eligible mining land, show in this column the location number indicated on the claim map.

eg

eg

eg

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

TB 7827

1234567

1234568

laas+vx

Number of Claim Units. For other mining land, list hectares.

16 ha

12

2

i a

Column Totals

Value of work performed on this claim or other mining land.

S26, 825

0

S 8, 892

(3, (P! 9

1 3 cm

Value of work applied to this claim.

N/A

S24.000

S 4,000

3(*oo

——— 2

?6oo

Value of work assigned to other mining claims.

S24,000

0

0

. 198

Bank. Value of work to be distributed at a future date.

12,825

0

S4.892

•4071

0 6

•40-71

l, L. , do hereby certify that the above work credits are eligible under(Print Full Name)

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim where the work was done.Signature of Holder/or Agent Authorized in Writing Date

ocr•y6. Instructions for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check ( s ) in the boxes below to show how you wish to prioritize the deletion of credits:

E 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.D 2. Credits are to be cut back starting with the claims listed last, working backwards; orS 3. Credits are to be cut back equally over all claims listed in this declaration; orQ 4. Credits are to be cut back as prioritized on 01 as follows (describe):

OCT 2 5 1999GEOSCIENCE ASSESSMENT

______OFFICE ^..^

Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.

For Office Use Only.-. * . . r' :"\

Received Stamp

0241 (02/96)

Ir'iti*-'— "' .LARDER l AKt

nci S11W9W*** , i

Deemed Approved Date

Date Approved

Date Notification Sent

Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

Page 25: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

Ontario Ministry otNorthern Developmentand Mines

Statement of Costs for Assessment Credit

l ransactioo

8(3

Personal information collected on this form is obtained under the authority of subsection 6(1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Act, the information is a public record. This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to the Chief Mining Recorder, Ministry of Northern Development and Mines, 6th Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.

Work Type

X X fiJE C.UTT//O Cy

fiJ)f:\(jtOlZ7~OMZ7~zl2.

ULF

(ofetsL. Kft?P)lJG. t "ptfoV?.

^LXP&^.vJ IS l o^

Ifep.f-f-usr'.-lW r^Ac.

^proOjiLS,* i ^ c f ri foPf. ne.

Units of WorkDepending on the type of work, list the number of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.

22.4 K^c2o k™cAO K fv) .

O^c^ -T K fY^ -

3 dc-^s

4 ^^

Associated Costs (e.g. supplies, mobilization and demobilization).

I^Ko-t-o -Cop^, n ri

J 2-

Transportation Costs

li do.^ y )ko K rv^ . X . 3o

Food and Lodging Costs

1 5 IMS al^ * 1 O ""

Cost Per Unit of work

^7tT-10?"

IOo VJi

loo a-•j *S-

3.00'-*

1980 6

X 7

^V^ty —

Total Value of Assessment Work

Total Cost

(0 f ^ O

3il oo c-

c^Oo o

teiv 0-00

(000

^ f-

bl*'-

I3.o *-

\S.Gn*t

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at 10007o of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 500Xo of the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0.50 Total S value of worked claimed.

Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditure; request for verification and/or correction/clarification. If ver Minister may reject all or part of the assessment work sub ni

claimed in this statement of costs within 45 days of a in clarification is not made, the

OCT 2 5 1999GEOSCIENCE ASSESSMENT

*- . OFFICE t _ , do hereby cer!ifyTtKS'the^aTrio"Onl5™s lown are as accurate as may

(please print lull name)

reasonably be determined and the costs were incurred while conducting assessment work on the lands indicated on

Lo- no,

Certification verifying costs:

i r

the accompanying Declaration of W(prk- forrflSB

to make this certification. VH^'r-Tr Vv iS'Oholder, agent, or slate company position with signing authority)

l am authorized

0212(02/96)

Page 26: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

Ministry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road

November 18, 1999 6th FloorSudbury, Ontario

JOCELYNE ANNE KIDSTON P3E 6B5BOX 66SWASTIKA, Ontario Telephone: (888) 415-9845POK-1TO Fax: (877)670-1555

Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

Dear Sir or Madam: Submission Number: 2.19806

Status Subject: Transaction Number(s): W9980.00559 Deemed Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the' response date on the summary.

If you have any questions regarding this correspondence, please contact STEVE BENETEAU by e-mail at [email protected] or by telephone at (705) 670-5855.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 14319

Copy for: Assessment Library

Page 27: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

Work Report Assessment Results

Submission Number: 2.19806

Date Correspondence Sent: November 18, 1999 Assessor:STEVE BENETEAU

Transaction NumberW9980.00559

Section:12 Geological GEOL 14 Geophysical VLF 14 Geophysical MAG

First Claim Number

1225422

Township(s) l Area(s)

WILKIE

Status

Deemed Approval

Approval Date

November 15, 1999

Correspondence to:Resident Geologist Kirkland Lake, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):JOCELYNE ANNE KIDSTON SWASTIKA, Ontario

LESLIE MICHAEL DYMENT Swastika, Ontario

Page:1Correspondence ID: 14319

Page 28: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

REFERENCESAREAS WITHDRAWN FROM DISPOSITION

M.R.O. -MINING RIGHTS ONLY

S H.O - SURFACE RIGHTS ONLY

M.+ S. - MINING AND SURFACE RIGHTS

DMcrlpiion Ordtr No. DM* DwpMlikui Ufa

DsEc.ae/ao w es/ej la/n/Bi u ft s mang

NOTES

NOTICE OF

THIS TnWNSMlfYa&Fi fill l WITHIN "Hf WATAOCAG MANAGEMfNT

UNIT AND MAT er SUBJECT TO FORCSTRV oprflAnoNS

MNR UWr FORESTER FOfl THIS AREA CAN BC COHTAfTFP AT

PO Bf l* 129

SWASTIKA ,DNT

POW - IOT

TML INt'IHMAIiON l HAT API T All!] ON IVti 1 MAP HAS ULLH CUMHlUtP FHOM VARIOUS SOURCfS, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER. MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION AM Toe CT*TI ic ne TUC

CO

tr LU

i

RICKARD TOWNSHIP

L IL i Til4M jrH4*4J

JtJ .'J

L Ll4ilTQ MH7|

122542

1-1 { 122 2 494 r"1

X/V ~~" — - -J

L L LW •014*1 Ml 4*0 * POW\s IZJ l jJMea**^*'

' tt ffi H t W", B jr- |r.~i |L"~ "^""^I ^^ 11865.04 [MIT.; |*"TTl *MT70

1236045 ;1189926i l ,T"?* ----L" ~ L7M2M

- jii*iti ItiBiai --- J^L "E jC t "*~

|*l*p*-|TlttIt

" .L -JVan H [Wit 1 1 l•1*11* 71*210 7B*ltB

I8630652459 1682458 1682457 1632454 l

c ~ ~ "lu™ " " r ~ ~ HL~ ~ ~ l ___™U, —— ^..^

737489 j7374IB 737485 j 737484

1219878 r

1214349

oo

COo

CO

876

CARR TOWNSHIPCOPY OF Tl US MYI..AH ARCHIVKU ON Ft:0 04 /S^

F.rrT.29, 190 l

ARCHIVED AUGUST 21/96.

LEGENDHIGHWAY AND ROUTF Nn OTHER ROADS TRAILSSURVEYED LINES:

TOWNSHIPS. BASF LINES. ETC. LOTS, MINING CLAIMS. PARCELS. ETC

UNSUHVEYEP LINESLUT LINESPARCEL BOUNDARYMINING CLAIMS ETC

RAILWAY AND RIGHT OF WAY UTILITY LINES NON-PFRENNIAL STREAM FLOODING OR F l OODING RIGHTS SUBDIVISION OR COMPOSITE PLAN R E SF R VAT IONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT

•f t

DISPOSITION OF CROWN LANDS

SYMBOL

e6

TYPE DF DOCUMENTPATENT, SUBFACE tt MINING RIGHTS ....

" .SURFACE RIGHTS ONLY....,..,,.," . MINING HIGHTSONLY--.-^.^.

LEASE. SURFACE A MINING RIGHTS—————.-— H" .SURFACE RlfiHTSONLY.. —.. ....—....—— B" . MINING HItiHTSONLY— -..-^— -————— li

LICENCE OF OCCUPATION ———.——_............—.. TORDER IN COUNCIL ————. ——————,,......—. OCRESERVATION .__.— .......,.^...,^^....,,..._. (J)CANCELLED ,.......... ............. ................. 4)SAND ft GRAVEL ,...,..........—..^...,—............ O

SCALE: 1 INCH ~ 40 CHAINS

Fit TQ 1QOO 3000 4000 WOO

3000- -r-. T- . v - , , ,, , - r-, n , i^nn^j tjJ^J l nid)

* MAP HAS BEEN COMPl L S;~:.; i-SQM VARIOUS

O 300 1000E5 THE !NFORNI*Tit(BM THAI

-

GUARANTEED

10 SUKE MININGTO W NSH |fHOULD CONSULT WITH THE MINIMO RE

MINISTRY OF NORTHERN DEVELOPMENT NAl- WWaMATlON ON

LANDS

M. N. Ft ADMINISTRATIVE DISTRICT

COCHRANEMINING DIVISION

LARDER LAKELAND TITLES/ REGISTRY DIVISION

COCHRANE

Ontario

Ministry ofNaturalResources

Ministry ofNorthern Developmentand Mines

0*1*

. ("D

Nunikir

G-358742A09NW2006 2.19806 WILKIE 200

Page 29: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

2 aw 16 W I5W I3W ilw low /\V

LM DYMENTMAGNETOMETER SURVEY

WILKIE TWP.ADD 57000 GAMMAS

F G6

Page 30: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

22.W 15W I3W low 71A/

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LM DYMENT VLF PROFILE MAP

WILKIE TWP.\

y

42A09NW2006 2.19B06 WILKIE 220

-lM.

4S

Page 31: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

23\v 2 aw I5w 13W 12W ilw low 4W 3w/

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Page 32: MAGNETOMETER AND VLF REPORT COMBINED …...THE MAGNETIC COMPONENT OF THE TRANSMITTED FIELD. THE NORMAL VLF FIELD IS HORIZONTAL BUT BECOMES DISTORTED IN THE PRESENCE OF A CONDUCTIVE

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OL-^e^ ci

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F G. 942A09NW2006 2.19806 WILKIE 240


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