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n:?C'PHYoIC;\L REPORT
^.rAMY LIF.ITED
3C7 V i ne li. rsi ve
K-70-.;T - 307 ̂' : ----"P :, .p - 3^7.111r-ip ,'
52L07NEeei6 63.1159 REX LAKE 010
7h.; :: ; -/oiiy *: f 31 claims i;' located at the east end] '^- ^ • :'-p---c;:ir.ate J ;y n '3 mile 3 east of the Nickel Mining
.I '- -y, : , - iiyo; e: 't, y at ferrier bake j Kenora Mining Division.
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g'K- :la'r;s were staked to protect several interesting of ~ ] i-T .-/rich v ; ere located during airborne magnetic and --c i;t -',.v:a- - '--^'c r-ru-ve; ;e. Ground surveys using the same two t.hr'd.-- YK'-re cp.rried .jnt to explore the possibility that these o--; q M .e.; -'.i. ht le caiujed l:.y niaenetic sulphides -//h l c h could he of
tase lines v/ere used for control with picket ' ] Ine^ cpace!^ at intervals of 200 or 400 feet. A station v" .-rn y' 1 "1 :: 'eet along t?ie picket linee was used with a re-
r' ,o - ' ' ' .' foot intei'val where warranted.
[ !"ynet;ic i'e?dings were taken with a Jalander rnagneto-- ha/i.i: a sensjtrlvity of 30 gansnas Der scale division. 'eadliigL--. v/ere re?.at?d to a c onrnon base station located at E J - ,-f- "'ii, .vh'ch is of a permanent nature. Diurnal contro"
.'a' :'".alned ;;' veaoi rig a Sharpe A-2 magnetometer as a base-.n. Or,T-rect,ion3 were applied to all readings for diurnal .',loii-? 'M tne magnetic level. An arbitrary level of 1,500
:.- /r':.: o'-Ljcted for converting instrument readings.
An el ectronagrietic survey was also carried out using- r.ne t'-rid. The instrument used was a vertical transmitter c~r:; /en , r a l/j^o cycle motor generator and a horizontal
rersc-nne" taking part in the survey and the number of' .' n d T . r. c-prlri-.r-d are listed herev/ith.
- 2 -
"T"' . r r.-1 vi OP
J. /'c ' vo'-
"'. AVrV/u i ri
O . ' r ' ' y :;i ,
o. Onr:i :-.J
.;. i/a' co\
; . .--L?!- - '
:; I- M
riot - Pi-o.ject Supervisor
'.te Geophysicist
-.e Geophysicist - Field i'v i s or
!-!'-i.-;a^toneter Operator
[• T -v -n-toT^eter Operator
•l. M. c.nerator
; ^. M. (r; erator
Uirve;, cr - Chainman
O M, J. n:;:at!
Ax e;
30 days
27
7
30
7
7
l?
Total 363 days
'--:.-'" : u: 'l or of
''t.-:~ 111; A oo .-.r
: o,-o' .-, r -ii .-7- ..f
o':r : " o\r '"i *--r- o"'
of' surveyed lines
o/ pocket lines
: c stations read
readings
23,900 feet
175,300
2,216
1,209
l-o3ult:3 ci 1 tiie suj-vevs are shown on the accompanying ; o o; '- (•-•'l'.- c~" ^i"i- i nch equal to 200 feet. Magnetic
readii.o- p-.v-:- ; c-'.-rn ?onto\irec! at an interval of 200 gammas. ' 7 - -OY, l -'ov eri \;MO^ indicate electrorragnetic conductors. Trian-
. n"'-1 !- - i :A:-' ; -"d AC are position of transmitter set-ups during the - -~ oo too ,- no. ;- ' c .:in-/^-;; . A separate set of naps in the form of '/ or l -o o'. :o'..-.; 7"-''d:r : ; - ;;ake v ! during the electromagnetic survey.
n r:'?o shov,':ng claims and sheet layout 13
- 3 -
" r'uml '.-7' .m 1 -y-omalous magnetic readings have been•?' "••-.--'•'j mo:" b - ' vdv'eh have no associated conductors and are,, d-m-fVr':, ". v" ' .-V'-'d ':o ": e caused by local concentrations of ' --g- . - ' 1. '' - . i':; c "b- i i"-. o,^' r '--' } however, two weak electromagnetic•.•; .--••. co*nc-''-v m.ith '-larnet:' c i eak^ . Fecau^e of their : y '--r" x -^/nVj ^h*-:--'.- v;:.uln I'eqiiir-e detailed seo'-ogical -iac- ."••" '.-•"•-•''j d .:? L 1 --;., ro -n drilling could be nad e.
; ~d-- :-.g-etic survey heated severs."1 bands of narrow,,•-" : "; L -t-:-- 1 r-.nora 1 ics which occur principally on the land part•-•'"' t h-. Ualms. I genera] j these are not associated with
o relieved t D be caused by
•V' --I -c t moimagr.es le survey located a number of con ch'm ',hw: claims covered by water. Although these ..".•re . :ot interpreted as being caused by magnetic
•:; "rt.: •'"•: \, t b,-- d-; ;:' -' .-.. v.r ;s made to check them by drilling.•••y- 1;.;" -s "-..cat'.-d ...r. e"altrs 32700 and 32704 intersected raas-"v- --mv ; ^'md - Pud p. grey biotite granite or paragneiss.
"'b.' ••V--. -.. '- .-•:- ['.-.urid to be magnetic due to disseminated•- - : ' •'••- •.":-" -e'rs'ma 1 massive rtagnetite In thin n:ands.
d' . .u"shld:-r- w-i're- "ocated in the drilling. Core re-. --s ••reo-"! 1 -o.t. For the present, it is believed that
-'•-."j ' .'-A-.--'burden is responsible for the electromagnetic
;:v arums.alies cf '.-itereoi, on this sheet.
r"";r- p- - h ; lea] surveys located many- magnetic anoma•--:-., •-'•''- ~'' . dp. ;cl- a? near to be associated vn'.th conductive '..^ ' -d 1 . ""bey '-r 1 ?, i-,Vieref ore , b elieved to be caused by
-.:-'--l r---.c---utrn ' lot's cd nag.netit^ in the country rock.
' r - ;";--y v^-.rks ar-'-^ly t; o the ?-esults shown on these ;-. liT./evev, furthei- electromagnetic v.r orl; i-emains to
- -.:.--.-:c""nr-ny -ri claims 3^7n 3j 327-6 and 32 7 ' : 7.
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5000 N
3000 N
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32793
1000N
REX LAKE MAG. 9
L32707
4000NJ
3000N
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32793
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REX LAKE MAG. 9
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32770 23 32724 32725
3ZT71 32772 32773 32727
3296 328.7 1328.832764 S2765
WERNER LAKE AREA
DISTRICT OF KENORA
PATRICIA PORTION
l INCH. TO 2640 FEET
REX LAKE MAG. 7
6a-97NE*91B 63.1169 REX LAKE
REX LAKE E. M. 7
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52LC7NBMI6 63. IT99 REX LAKE 260 REX LAKE E-M. 12
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