GEOCH SUR CAIRO TWP · Similarly, thn crooks, ponds 'i.un1 .laKni;; are oriented in a north...
Transcript of GEOCH SUR CAIRO TWP · Similarly, thn crooks, ponds 'i.un1 .laKni;; are oriented in a north...
V 42A82SE8279 63.3382 CAIRO 010
iILi'CHEMICAL bUr'tl/t. V
on the property of
.-'ii:i(;.: ?B LTO.
Cairn Tnwnohip,
T immirui, L-ntr-ria ,
IMnv^mber "lil, 197!;
H. J. Hradshaui, P. Eng,,
ConBulting GR
INTj'ICiJUCjIDPJ
A HoiJ sampling progrHimriE was undertaken on the Majestic
Wiley property in Cairn Tcminship during the ppriad August 19 ta
October ^ , 197!v. This s??mplns wars analyzed for copper, lead and
zinc and plotted nn the appropriate plans.
Purpose of t; h H survey if to detect anomalous conditions
which may reflect base or precious metal deposits in ths granitoid
JckE of tne property.
, Lf;C'-'iTK.irj aM-) ACCifciSLi
Die property consists of 60 contitjuous unpatonted claims
numbered LM'J39a tn L'*1 c)ii5?; inclusive and L^?101fJ to L^21D1U
inclusive.
About *i.r! irij IPS wuutheast of Timmins, Ontario, near the
sinHll community tif flteittichGuan, the claim group is situated in the
centre of Cairo Tuwnahip.
An all-wt?Hthcr grHvel rne-id extends northerly through the
claim group, frnni higli'Tiy 66, thereby providing excellent access.
Apparently rio significant uxploration work has been under
taken on t h t-: area oP the ulnim urou;j.
TfJf'G[iR'\f H Y
tif nf thw ganernlly uell drained terrain does not
exceed 100 feet.. Distribution uf I'ock expo;u.trs compared to the
genarfr.l HTBB i H yHnernlly y o od avBraylng about 15 per cent.
Tne major portion of thy property is ary and covered by
light brown tu rv.i.idiBh sand and sandy limm. 'ITBOU of gravel de
posits oro cordon. L.uw lying minor areas of thtjoe glacial deposits
art", covered by wet organically derive? ri soils common! y known as
muskiig. U B UK j l y these a r e a M form nartn trenriiny lensairial shaped
d B p o s i t a h e t u e e n ri d g p, 3 .
Similarly, thn crooks, ponds 'i.un1 .laKni;; are oriented in
a north direction ^ith rir^iririgE tu thy south.
Jack pine, birch, em ri poplar, in that ordnr of abunriancBt
are pressnt OD che high grDimd. l':ostlv black spruce are confined
to the l oiu suami.;y
Thu QGolugy nf the arss is ahoun on Map 2*110, Powell and
Cairo TownshipH, by t.hfj Inturiri Dtrp^rtnir-nt of Natural RssourcBB.
7hH distrihut'lor. nf lattil nn|.per Bnd total molybdenum in felsic
plutonic rocks of the; area is shown on maps I 'J 7'12 and P733 respec
tively, by thn i'lntEiriu ynvt-.-rnment. Thf Ha JBatic-'Jiley property is
located tin lha Einuthwe^t portion of the Cairn :;touk which includes
thn felsic plut-.niic ronks of thi? arHa. finally, the Cairo Stock is
the subject nf a study by u). J. Wolf Ei of thy Ontario (jeological
Branch in Open Fi IP Report 5G91. In this report, tha results of
sampling i^vnra.l felsic intrusive^ rtiloted and unrelated to gold
campa ig df.;{it:ribftd enrl inturprated.
Tli e uren of the claim group is Blmoat totally underlain
by alkalic i ntrij^ive ruake, pfirt of the Cairn "itock, reprsnenteri
by H rnnynetic Inu. Alnnrj the west boundai'y of the property, over
B uiiiJth nf nhoul ^DiK.) f'e^t , coary!' tjrain'.'d svK'ii ie porphyry is
' oxpuKKfj. T h t-: rcri:1 .: rifitfr uf thrj property * '- u niJrrl :- ;)in by mudium
rjraintuj ^ycn.rtr?, ui ",h the exception rf the LTD t) tiiang the south
brunc'ary tnhinh ir. un r :;:r] fin by yrunozir coarr.? grf^ined nudiments
strikinq northern; i. !.iurth trtinrlino G' i B l.) ^ r: f clykt'9 intrude the
Cairo Stock.
ld-si iv/i^r jRpor-its have hean tninad in Powell Township
i.iif:-,t nf" Cfsiro Towntuiip. iJidftyprt-'Pc) occurrnncBS of
chalcopyrite, pyT'ite, gnlena, specular hematite, purple flunrite,
barite, iricjlybrlenltt: and touring]. inc hove bt-ien ohsnrvMri in thn Cairo
Stock. lhe c u;' mineral:"; are cciritmcn afssoRintt-H af gold in quartz,
ant] quart? nBrbon-jtB vuiria that 'jncupy fracturRf.; in' ond nunr the
syenite,
Arc-is'.; of thr-i Cairo Hj.kolir. intrusive corusidsrtjd tn bs
anomalous in noppFr ;:,nd mo] yhriantim, as-; Bhoun en trit^psi; P732 and ^733,
BTP. n ynorallv cnnf'n^rJ to thr rnarrjiny nf thr intruaivr. A relative
riBpi^tion uf .silir.ci Rxista aluno tht? m^ j." g in r, of ttie intrusive RS
co T "p::'rs! tu thf cBntrt:. ThR tiinriif icancp of copper end molybdenum
fri un i:ic?ps ('7"5k' and P733, ''.'ithin the claim group shall
fiiiBt t.fu- heodinri -''laurvny result.'; and Interpretationl
SLMULY HtSULTLi r.WJ ,
M btuciy of the mettil valuta indinateH that there are at
least three di' fan-in t pupj] r:tir;.nt of VEJlues buaf.'d on difffjring
sai j types. It, 5 1., riutsd, f' c, r example, thor, v'Jluea from muskeg
sainplBLj ,jre ,;,uoh fiigher ;,i'i,in t h us b samples from saruJs and gravela.
This fsc'turR rfitmlto frr.rn the fact that trm organic rnattHr of
swamps tend;:, to precipitate many of thp oro motalrj out, of ground
water solutions. Rather tfrbitrr-jrily, hut nevertheless baaed on
trie geology, '-soil type.1 :.;, and arithmetic averages of values together
with the ro.:;ult'.' of the rock R a m f.. 3 iny shoun on plans P732 and P733,
thi-- threshold v-'?luti ror each of tht; mstuls analyzed, namnly copper,
lead arui zinc;, was at?t -:t ^L3 part-;; par million, Although this
thrRsholr! r.^y tie: valid for tieteni'ininij wnncialous conditions in areas
of BBrir! nn;;l ^ravol, it is novioufi thnt B m uch highnr threshold is
rRquirsu1 for th:;-:-,t-- r.umplaB fro'n musiktiq. Over half the samples from
muskeg hfivu valun.'i ni-Rnt^.r than W p prn.
ilt3c:cjur,t of thfj Irarge riunib^r r-f sumplKa, huwevar, ein
adcquatB stHtisticrJ. tru^tnent of the data uuu.Td involve more
expcnditnrB then thin rRquij'r;ri for oxHmin^tion of rock exposure
adjacnnt to thrive obviously anomalous values.
fioil r.anflK'5 front the north hnj'f of the property uiera
analyzed for cooper, l r-: B d and zirr:. ;iinc:,n it, i j d B nubBBquently
dytRrmi ned f hat high .Tine value;-: alnur:t invarifjiily Rorreapondud to
hifjh co|ipor values;, tho asmpiHR frofli the south half of the; property
UJRTC anwly?f r.1 fur cor/p^r Eind IGEUJ only,
The copper, Itdiid und zinc: v^'luos for thn north half of
the property art! plotted snd cor'tuurrid on t wu plans at a ocale of
one inch to four hundred foot. [Jrie fjlon sufficfjss for displaying
results an the south h^lf of the property.
ID i-?
t ^ |3—
'
L l."-.
if t-
n
r* J
V-" n '-s i
aT3
t-
1a •^j
c C+ c c-1-
0
n c
g r? ct e
K
cc x
C
CJ
h
o 3 ct
c5
't; f* CJ — *j
rt ;r; M O 33 r^ - ^r *- Cj IT" n "C-
— j w w j—*
CO a C-
U3 •3 n. NJ M-
.w O
f
3 u-:
*
r*-
CT1 •^,
Ci.
r-**
M re tr V;
H'
C- ^ EC *- c-f- U* s— ** J? 10 ™j 3 E J— '
•^r C5 **^ C a •T tQ r- i-^ 3 ro tc 03
? C ICX
tn
'~* c^-
5 •i; — i ^4-
jT Q ^ C et- ci 1-5 C? "C- Ul ^ CD iX t/7 * -H U"
^ ^* VJ*
1C zr cc tu t-f o o T3 TJ l-j
n •^ c .~3 -•i .-r .i1 i — .
w/.
"j l-**
*T rt Ci.
f*-1 -i cr rj n -H 3 Q J H**
ID n O ~tn T3 *-j 1 t~*
i-W ffi Q.
*.™ Z. r"^ H-'-
-T rn f\3 JT-
iC •^ '".L
'^-4 CT
*'
Z^" o' 1-^ r * -* L
JJ r— CD 3 U3 r* 3 !D •^. cr •D ffi cu 1—
'J-
*3 to \jrf ^
w \ r—"'
±: Cz 3 r; 5 TD "V;
-O \j*t
^•^ E — r
i-" r^ 3 x -c •-i tD 1—
-0) fi- cc ea ^J r;.
3 QJ ^ — '
**C C~j
c*-
0 CD
-^ ' " ^2 C tr, TT ^ vO-
* — :
ZT •;?, CJ .•** T; CL'
i.— -
•^ O C'
•-J l-j ;3 CO ^* o 3 a 03 f- f™-
C*- — -
rc
c "T t — -
^. UJ-
L.* O Cj c^ -•*1 I-.'-
— t
m Cx
r^ ^ r- Cr. P CE 2 -ri D."
*-J rr
,Cj * ;-
(
H3 3 ^ t^.
D M H-
rt-
rr ^-** 3 'HI
,^1 IT en O"
nJ U3 tt!
*— *
t—**
~3 .T) 3"
flj r!- e ™ CO ^j ! — I--**
w CD L'rf ^ en o 3 a. iji I\3 ^ 0 H c*-
^T ™
^-1-
'-d -^j
•3 ™ H -ry L.-
J
^ct O T^ *-j
^ ^^ --J -ri ' 7. ^ Ci
-.T rf r^ ill: r2 b T2 TJ Q "i CD 3 0 3 as fvf
w^ a ^
"C*
•™ J;} r*-
— S ^ IT"
uZ 1 — 1
~*,
z* 13"
.•vv
•p -J t'j CO 3 "Tj; *— cu '™ irf ."-* ra ~^3
^ C 3 3 C M ^7 ra U3 * —
13 CO
n c C'ii
J——
'
^ rc rf- !T- i-i re "C **i rc LO ~J !7 C+ ui H'
G ^ iIT rt-
ZJ"
CD 1—*
Q c- E rB rf- 03 rr o •-j ra
ft- rr n: Lw D tt! cr "r* HI
1J.
a^
'IX i-*-
^2 r*-
IT"
;" < h*- n w*
13 j—"
d-
^^ O -ij
l— l-1' ^3 ro t^,"; en z o (•1 c*- U"
*
cu ^3 O ^r D.'
i — *
^: M-
M i — '
C n 3? c* r-j C3L
^ i^" ;4
-
c-i-
^J"
m H"
D cr
ri *^ OJ cc o c* H-
^ r) n -*5
z^ cr *"v ~ Lj" cr C
^"*C r~ 5 d c-t
- zr rc \j *^ n TJ Cw *^f r^~ "'•C'
^*"
V- ~ D C.
0! ^i **c *
T" -— r
C^ e C^ CD c-* o; r*-
t-'-
O Z* l':
- L .
T' C •"0 "7 *— "
mU
^J Q' 73
M-
^ G *^j C^ i—* w Q- ^* c^-
IT j^. ts
n? fC fX r;.1 c-^ C^ ^j CL O ~*^
i "
J~-
IT T* r~-. .r~"
^ 1Z M c-r
^ ** ^T I— iCJ — t-
\—^
CO D- D. n? ~2 d N H-
3 n
rjj
r"*
'". -j ra
t-"
3C
' T
X
^ci
o; i—
E
J—C"
'"C ^•
.'
~!j
~; — 'r—
V
.:
t-"
C.
( ——
——
~~
*t
r-0r-
(.i.
**
Ci.
CD ^ r1 r^ C3 1^1.
;i2 *-i
fr-1-
-tj
M- n Ci rt j~- •* Q) W l-1- Z! O.
H- n m C+ C3 C.
- b - ,
Anomaly F - A number of isolated anomalous values form this
anomalous zone butwRcn Line 2 ^ Worth at the base line and Line i*
South, station 1b L'&at. High copper and zinc values were obtained
from muskeg samples. The largest anomaly of the zone is confined
to a swamp. Here t h R metal valuer; show relative impoverishment at
the centre of the swamp which ie characteristic of the precipita-
tion effect organic matter has on ground-water. , ,
.id ~ This anomaly is situfjted along luhiskeyjcick Creek on
the we?t side of the property. High copoer values form a linear
feature partially in lou ground paralleled hy high lead values along
tha Orec-jk. This rm cima l y correr-ponrir, to a rock capper anomaly on
Map P732.
fiOSSSilLJi *" ^^Qh cnpper-lead vnlut^s crc:3siru;i Linea Q, 1?, and 16
5out f 'i junt k'Rst of tht-j ro.':d ft;rm e;nomaly H. The values are situated
in and adjacent to musk no s^nmp. ( :
L - ^ yroup of anomalies eas.;t of the lake, between Linea
20 and **8 doutfi, farm this anomalous zone. The highs along the
lake share one creak BIF, confined to low ground, in pert, muskeg.
At trie intersection of Line 3 fi South uii.th the base line, the high
values, particuliarly lead, arc in sandy iufsm. This anomaly corres
ponds to the location of a lead-copper occurrence and rock molybdenum
anomaly on Map H733.
AnomglvTi J - Korniin^ a linear narst of t(-iB base line, between Lines
20 and 3 Ei I'inuth, thl;; copper anomaly is largely situated in dry
sandy noil '. /' . . V-
Anpmaly^H - 'jsvcral isolated lead anomalies in the vicinity of
Cameron Loku form this anomalous* zonfi. The values were obtained -
from dry sandy soils adjacent to rock exposure. , '
^nSIUSl^Li; ~ This "namely crosses linea 2B, 32 and 36 South near
the west boundary, f-icst uf the high copper values are from muskeg.
Anomaly M - A rwther small feature, this copper-lead high croBBe
lines 56, 60 and 6** Sou to near the east boundary. The high values
ara confined to shallow, dry, sandy loam. . :,
sy of their close relationship to copper or molyb
denum highs, from rock samples BB shown on plans F732 end P733,
anomaliea B, C, Q and I ore cnnairifred the moat impnrtant aa poe-
aible indicBtors if bass motc'l aulphidBB. The leat! anomalous
zone K rn FI y inriicfite the pruaenne of tjold-silvsr minereilization.
An nxiiminstian of the rock exposuro in the vicinity of
these anomalies and thR nthara herein df?9cribr;d might well bs,
aufficinnt in most instancRB to determine whether 'or not base or
precious mRtfil mineralization is related to the sail anomaliee,
Those anomalies, houiRver, having a lunnuidal shape, oriented
northuards, may reflect mineralized faults in topographic lows \ :'
Thest! type of onomnlien, in pBrticular, inclurJa t, G, H and J, and'
may require Berth trenching.
a
A [;rrjgrariiTiF; of detailed rnnk examination is recommended
at the locutions of the individual anomalies u)ith anomalies B,- C,
G and l meriting special attention. A minimum amount of S30QQ ;
shnuid he allac^tfid for this programme including same earth : :
trenching at Iocs t i on;.- to be* determined during the investigation.
Any detailed assaying of rock SHHin3.ini:; that fiay be TGquired would' " : (' " "
an additional Bxperiditurs.
ly submitted, -' -,'
\ SJ, SHIELD GtUPHYSICS LIMITED,:Vi ',-.\ l :""\ ' . - '
4 c-*- -j * f-\ y y f i V "* "
V /~*";i"**i4t*B ,t, "O J ''
TimmiriB, Untariin, \'^\. ^^ /"- *-'* Bradshew, F. Eng,,\?h^""^ 0Jr
cr 1 C, 197!:.. X^eopo^^ ConnuHing Geologist.
x
s.~*' Jc:.
•-lf4O0)3}r*-*Jf-,0)^0uCDf-.04
^
"a^LO^toIE32^af-S3CT.
f-:nf.3G"'
3CO
a: c
P-ti-4.
—b
,^r^-
•ji —
in.~sCD
-V-.c•MQ-
GJT3ra
' Ba{Hti-C•xyf3Ci
f.,0)3KCI'^-ia.H(Cao;~-!Ja^-iJ^
,
Q'' — J
^~eeax:i —*0)r-HC3P
t5!0
- c"DN-^(WCjrf-*-r-i
^ea^jOJ^4Jenc.r*4
-^-i
iHCDy*Crff-*Q
.eafno'.^b3H-
3J3r-—'
mf~*Vcf;a;cD•^^
1^
a-C3c
CT
Q]
0313SQJ
f^EDJ^303C-O^-*-v-iH3-fj
tt
-fi
-T*•+JC.GJ"^•iir-f
D,
•j!'i~*L;"-^
'—i
T" 'i
5~-'gr**
"OQJE~t
^UfiSTr" ,3
CF-(a0
!a!D^^nC2
*r—
t
a.e.-jaiCs^j;o-oQJCi
a-i-2CL?~Ij^c:-J^~ciil
,'JS
^-5
t\Jdrr^•H•^^irmU3?~
i
O-
C3-•H
(00)(HenG3Rj3CP
Xy033g^
V-^^juL!lj
TJttJC-^c^*—
i*3C-r-^t^CK.KG;-t-5w
ir^3p-i
C^.
:T;t-idn
cc-J^-l-J
w
CDa cT-t
E m
T3C. a•a o33a. n. c•rHS
i
T5C
KCi
f-!
co r:
T3 C-J-*Co-j.
t
O8}cK—r
T3C
K
O!
gl"St^j
f-.
r-l
3JH-s-3^?r^C3C^x
en"J
-r-i13
"C-
^
C*
C,
•ri *r-H
"C
W-9
C"
r "*^
5t-.*-loCj
EC!
CO
4-'
DJT3M"cc^4^ca;V'
druuc•r-tM
e'•^•r:C? '
a*enO)r- 1L3Ji-i(C-accCQ
42A02SEfc279 63.3383 CAIRO 900
CC~ - ^fc
l L ) L
'4I89\48 418949
T9X448 4 13 4491 419450
4210.141 419440 j 41 9439ez 676419435
419430 '419431 .419432
uogKlO 19415 1l '41
1447 4 19408 4 l9f409 1419410419411
419406 1 419405 409966
L |L \ L
I 4I9342 I 4I9\338| 4H
401425 380689,4I93\54 4I ?.S4
380690|4I 9356 L"
"-40I33I 380693; 580692
Tt. O O l* t*1 SI ' M ' f ~~ - ~
LEGEND
Meosurement station along picket line
Parts per million of copper and lead in soil
Copper Isograd in ppm
Lead anomaly I.e. over 40 ppm
Low wet ground generally covered by muskeg
Muskeg sample
Area of rock exposure
Claim post
B.L. O
(South S heet)
GEOCHEMICAL SURVEYON THE PROPERTY OF
MAJESTIC WILEY CONTRACTORS LTD.CAIRO TOWNSHIP ONTARIO
BYSHIELD GEOPHYSICS LIMITED
CAIRO TOWNSHIPt;-
SCALE400 800J ^ ^
IZOO
-nth
FEET
NOVEMBER
SOUTH SHEET1975
42A82SE0279 63.3382 CAIRO200
^ 3 C/
LEGEND
Measurement station along picket line
Parts per million of copper, zinc and leod in soil
Copper isograd In p p m
Lead anomaly i.e. over 40 ppm
Low wet ground generally covered by muskeg
Muskeg sample
Area of rock exposure
Claim post
(North Sheet)
r' 1"). - - _- '^ T -
~ - i t: a
Whiskeyjack Lake
CAIRO TOWNSHIP
KEY MAP one inch to one half m ile
Beaver Pond
o -^ V ^ ^w o ffl. rf" 10 *;.z——i——i-i—i:——i——t-
s ir s a
3-
O-
•a
•v
Ul
o- a o- o. "\
v C * \Vl 'T\ ^ ^S /? 1 i* *\ "e *- r ?\Ae^ * * S \^
\4X
(\
**
(M)r - 2 i*\^ T -s o-
~ 7^ v-v (M NO- - V
t S?
tf 2
S
~r5" "f?
- *
"^ ^3
iD !0
y t
*?- ffi \Q -fO ™ W -n vj ^ -^ ^
* 2 ^ 2
T OB O 0(
iO o.•y^ ^i
a-
o-
^* oo r- ^1
tO O" ^c 1Q— ofi Of
oOf
o A
Lfl S
S ? a(^ Ul
B.L.O
42A02SE0279 63.3382 CAIRO 210
GEOCHEMICAL SURVEYON THE PROPERTY OF
MAJESTIC WILEY CONTRACTORS LTD.
H
CAIRO TOWNSHIP ONTARIO
BYSHIELD GEOPHYSICS LIMITED
SCALE400 800
FEET
1200—j
OCTOBER 1975
NORTH SHEET
LEGEND
Measurement station along picket line
Parts per million of lead and zinc in soil
Zinc isograd in ppm
Lead isograd in pprn
J Low wet ground generally covered by muskeg
Muskeg sample
Area of rock exposure
Claim post
o-
/L4Z.IOI1 4194.4.1
(North Sheet)4ZI014. A I9440
Wh/s/reytoc* Lo*e
CAIRO TOWNSHIP
KEY MAP one inch to one ha f mile
Beaver Pond
~ \ *r rJ — - r- s \ "* "'r-
B.L.O
42A02SE0279 63.3382 CAIRO 220
GEOCHEMICAL SURVEYON THE PROPERTY OF
MAJESTIC WILEY CONTRACTORS LTD.CAIRO TOWNSHIP ONTARIO
BYSHIELD GEOPHYSICS LIMITED
SCALE4OO 8OO 1200
FEETOCTOBER 1975
NORTH SHEET