' f: (To Accompany Maps 68-16M, 68-16E) April 2nd, KENNCO EXPLORATIONS (CANADA^ LIMITED GRANT TOWNSHIP, ONTARIO.

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1 ' ' f: 31L12SW***! Mt*AI FIBJ5 010 MAGNETOMETER AND ELECTROMAGNETIC SURVEY for KENNCO EXPLORATIONS (CANADA^ LIMITED GRANT TOWNSHIP, ONTARIO. (To Accompany Maps 68-16M, 68-16E) April 2nd, s-; f :. i'i

2 : V. GEOSEHRCH CORSUITRIITS limited MACMvTOMtnT.ll AND ELECTnOMACXnTIC SUHVEY Tor KEN7.-CO EXPLORATIONS (CAKADA.) LEOTUD GILXNT TOK?ISIUP, ONTAIttO. (To Acconpony JUipa 68-16?!, 68-l6i:) April 2nd, 1?6S. V"-'" 'ST.'- lt?:t^?s?!s?;f;ti5get^s,.a.-*.3^-ui.?.;i4.'.,

3 GEOSEARCH CONSULTANTS LIMITED SUMMARY Magnetometer and electromagnetic surveys were run in the vicinity of a reported copper showing in Grant Township. Access was from Crystal Falls, on Ontario Highway 64, a distance of five miles. No bedrock electromagnetic conductors were noted, to the depth surveyed. A series of northeasterly trending magentic features have gradients suggestive of relatively shallow over burden. METHOD OF WORK Magnetometer readings were teken at 100 foot stations along a previously established picket line grid. Readings were corrected for diurnal variation by reference to previously est ablished base stations. An ABEM, MZ-4 torsion wire magnetometer was used, with a scale constant of 10.7 gammas. Readings were estimated to the nearest fifth of a scale division. The electromagnetic survey was carried out with the "loop-frame" or "slingram" method. A battery driven oscillator was used to energize a portable transmitter coil. The alter nating electromagnetic field so generated is measured at a receiving coil connected to a compensator amplifier. By adjust ing the maglitude of the reference signal, this compensator is made to read zero over undisturbed ground at the coil separation used. Two components of the secondary field are measured and expressed as percentage of the normal field.

4 ' GE05ERRCH COnSUURIITS UmiTED - Majnotoniotor and electromagnetic surveys voro run in * the vicinity of a reported copper showing in Grant Township-. Access vs.3 fron Crystal Fall o, on Ontario Highway 6*fc* o. distance of five nilno. * No bedrock oloctronacpiotio conductors voro noted, to t:io depth surveyed, A series or northeasterly trendinn nacnctic fcaturca have pradionta cuc^ostivo or relatively oliallov over burden.?i:":'::ot^ OK VOilK, Ma/jnotonotor rcadin^o vore takon at 1OO Toot stations alon^; a previously established picket lino j;rid* llondinco voro corrected for diurnal variation by reference to previously ost I'.blinhcd bat o s tations* An ADLM, JIS-4 torsion viro nncrvotonotor vas usod, vitlx r. e crjlo constant o f 10*7 caxaaas* Koadinca vorc ootinated to tho nearest fifth of a ccalo division* t The olectroraacnotio survey vas carried out vith tlio "loep-frar.o" or "olintrasi" inothou* A battery driven oscillator v.-'.s used to cnei*ci"'0 a portable trar.cuittor coll. Tho alter i-.atint: oloctronr*; netio field so conorntod i* tioasured at a receiving coil coruicotod to a compensator onqjlifior. Oy adjust* t!:o isa^iitude of the reference signal, tliia oonixuisator la c:ado to road zero over undisturbed ground at the coil separation -- VC^'Sig:-e used* Two components of the secondary field are neaaurod and -iv^t^^ycv. i '

5 - 2 - The relative amplitudes of these in-phase and out-of-phase components may be used to estimate the approximate conductivity and depth of a conducting body. For this survey, a coil spacing of 200 feet and a frequency of 3.52 kilocycles was used. RESULTS None of the electromagnetic readings obtained indicated a significant bedrock source of conductivity. Variations in back* ground are interpreted as reflections of slightly conductive lake bottom sediments. Some positive in-phase readings (as on Line 32E) are apparently caused by magnetic fields. A series of pronounced magnetic features trend north east across the south part of the survey area. These may represent extensions or repetitions of the host rock carrying the reported copper showings. Respectfully submitted, FS/om Fenton Scott, P. Eng. ".,,; '/-. - ~ -i

6 - 2 - expressed as percentage or tlio normal field. The relative amplitudes or those in-pliase and out-of-fhaso components may bo used to estimate the approximate conductivity and depth of a conducting body, For this survey, a coil spacing of 200 foot and a frequency of 3*52 Idlocyclc? vas used* None of the electromagnetic roadincs obtained indicated a si(?iificant bedrock source of conductivity* Variations in back ground aro interpreted as reflections of slitfitly conductive lake button sediments. Some positive in-phaso roadincs (as on Lino 32E arc apparently caused by magnetic fields* A scries of pronounced nagnetio features trend northcast r.cross the south part of the survey 'area* Those nay represent extensions or repetitions of the host rode carrying the reported copper s3iowir.es. PS/oia llospectyfully subletted, - '-. ' ; :;.,, j, -",.. -. V.^/'^'U: * :--.-^..-JJL". ~

7 3tLt2SWM*1 M10A1 FIELD THE TOWNSHIP FIELD DISTRICT OF NIPISSING LARDER LAKE MINING DIVISION SCALE : 1-INCH* 40 CHAINS

8 FeW Twp. THE TOWNSHIP OF GRANT DISTRICT O NIPISSING LARDth MINING DIVISION SCALE 1-INCH^ 40 CHAINS

9 X3 Ul o O UJ \JJ a! lil O o o o UJ

10 TOMETER SURVEY ay MO RE AU, WOOD4RD g CO- LTD- KENNCO EXPLORATIONS, TtMISKfiMlNG /**A, O UT GRANT TOWNSU1P COPPER 5//OW/A/6 ^ 200 3iLi2swaeai eeteai FIELD

11 FIELDTWP GRANT TWP 2) - (90/0 -/J / M IN/GUM ELECTRQM4GNET/C SURVEY By MQREAV, WOQOARO 3 CO. LTO f OR KENNCO EXPLORATIONS, (C4MADA)LTD \. D., LEGEND IN-PHRSE COMPONENT RERDIN65...LEFT COMPONENT REAO/M&5...R/GUT FT. FREQUENCY EO GfiflWT TOU/W5A//P COPPER SHO\rJiMG SCfl i/wort - w*yz WO! 3ILI2SWM01 80I8A1 FIELD 210