dd rpt 10 moberly twp
TRANSCRIPT
42A13SEeB9B 10 MOBERLY 010
Diamond Drilling
Township O F MOBERLY Report NQ; 10
Work performed by: NORTH RANKIN NICKEL MINES LTD.
Claim N9
P.58299
P,61690
P.58292
P.58293
P.61698
Hole NO66-1
66-2
66-3
66-U
66-5
66-6
Footage511'
354'
606'
715'
497'
502'
DateApr/66
Apr/66
May/66
May/66
June/66
June/66
Note
Notes:
Formerly Report 10-13
Am. .O04Cr- 631 rev. e - TZ
42A13SE0898 10 MOBERLY020
Keport on the Diamond Drilling
Performed on the Property of
NORTH RANK1N NICKEL MINES LIMITED
situated in
Moberly Township * Porcupine Mining Division
r: ;by - - ' . - ' "'M. E, M. CONSULTANTS LIMITED
Michael Zuroweki, B.Se., P.Eng.
Toronto, September Z8. 1966
Report on the Diamond Prilling Performed on the Property of
NORTH RANKIN NICKEL MINES LIMITED Moberly Township - Province of Ontario
SUMMARY
Six hoi e t totalling 3181.0 feet of diamond drilling ware par* formed during the period April l et to July 1st 1966 On the company1 * Moberly Township property in the Province of Ontario. These holes vara drilled to investigate interesting geophysical anomalies, outlined in surveys completed earlier, in order to ascertain as to v/ he the r or not the cause of theme electrical anomalies was due to economic sulphide mineralization.
CONC. ,Non-economic sulphide mineralisation waa obtained in hole
66*3, whereas in the other five holes no conductive material was encountered to account for the anomalies. It is considered that these are probably due to conductive Overburden,
Because of the inconclusive results obtained in the better of the anomalies tested, it was considered that the anomalies of secondary import ance aid i.ot v arrant investigation. Consequently, drill operations were suspended on completion of hole 66*6. '
RE COMMENDATIONS .
It IB recommended that no further monies be expended on this property.
The assessment credits obtainable from the completed drill footage should be applied to 36 of the 64 claims, allowing 26 claims to lapse. The claims to be retained are numbered as follows j
P-58264, P-5827Z to P-58274 inclueiv* P-f82?7 to P-58279 inclusive, P-58285 to P-S8296 inclusive, P-5S299, * Pr6l682 to P-61686 incluiiva, P-61690 to P- 61694 inclusive, P-61696 to P-61699 inclusive, P-S8307 and P. 58308.
These claims encompass a major portion of the untested geophysical anomalies.
Upon recording of the assessment credits to the above claims, they would be in good standing until April 27th 1968 .
It i s also recommended that the results of the exploratory work being conducted in the area be periodically reviewed, correlated and assessed
with those obtained on the North Hankln property, Thio periodical review could well reveal valuable information ae to the possible presence of mineral deposits on the subject acreage, :
PROPERTY, LOG ATION . ACCESS f ETC .
This property of North Rankin Nickel Ml ne i Limited consists of fdxty four (64) contiguous, unsurveyed and unpatented mining claims. They are numbered P-58300 to P-58309 inclusive! Pr58264-P-56ZV9 inclusive, and P-6168Z to P-61699 inclusive, The area of the claim group is Z560 acres, more or leea. ,
The claim gioup is located almost entirely in the northeast corner of Moberly Township although part of the claim group extends into the adjoining township of Thorburn, all located in the Porcupine Mining Division, in the Province of Ontario.
Access to the property i* difficult. There are no roads within several miles of the property, nor are there any bodies of water which can be used e.s a landing field for ski or float-oquipped aircraft. The most practical means of access is by helicopter from the town of Timmins, Ontario* The distance from Tiromina to the property is about 28 air mil* a.
There are uo large streams or rivers on the property.
The property wae staked to cover a broad, high intensity , northwest Btrlklng aeromagnetic anomaly, following the announcement of the Texas Gulf Sulphur base metal deposit in Kidd Township.
During the period 1V65 to 1966, North Rankin Nickel Mints Ud. performed magnetic, horizontal and vertical loop electromagnetic surveys over the claim group.
Fox detail*, of and the results obtained in these surveys, one is referred to the reports on the above , in the company's files and dated April ^lBt 1965 and March 17th 1966.
PROPERTY GEOLXJGY
On rock outcrop i* known to be present on the property. It is located in the northwest part of claim P-58300. The rest of the property le covered by glacial deposits estimated to be in the order ol 100 feet in depth,, vertically.
Based on the pattern 0(isomagnetic lines and magnetic gradients of the ground magnetic survey, it }s interpreted that the northeast t wo-thirds of
.3-
the property is underlain by a complex of Ke o watin lavas and minor sediment*. The south one -third of the property it underlain by granite. The main contact between the two stratigraphic units it irregular and located about 1000 feet south of the baee line and more or less parallel* it.
A program of diamond drilling was conducted on the property during the period April 1st to July 1st 1966. Six diamond drill hoi e e were bored for a total footage of 3185 feet.
The object of this drilling was to investigate the cause of - geo physical anomalies outlined in the survey E completed earlier.
PISCUSfJOlj.p^T.HE RESULT? OF DIAMOND PRiLLlNO
Diamond ..Drill Hole 66-1 . This hole was drilled on claim P -58299 in order lo investigate vertical loop &.M. anomaly V*9. The hole was drilled to a depth of 51 1. 0 feet, Acid and basic volcanic e and several granitic intrueivcs were the main rock types encountered. No conductive material wasencountered to account for the anomaly,
Diam o ud D ri 1 1 Ho le 6 6j* 2 . This hole was drilled in the same plane as 66-1 but in the opposite direction. The (purpose of this hole was to obtain another t e t, t of anomaly V9 as it was considered that in hole 66-1 a granite dike occurred in the area where the conductor wae anticipated. The hole failed to intersect any conductive material to account for the anomaly.
l'?iajrypnj^D^^^Iiole^66^'S.. Thie hole was collared near the common corner of claims P~Tl684 and P.&1683 and drilled into claim P -61664, The purpose of this hole v.as to investigate coincident vertical loop anomaly V3 and a magnetic anomaly. The hole was drilled to a depth of 606.0 feet. Sulphide mineralization was inters* i c tad to account for the anomaly, but no significant value c in the base or precious metals were present.
Diamond p rill Hotu 66 -4. This hole was drilled on claim P*i829'jt in order to investigate vertical loop anomaly V i s ituated on the flank of a strong magnetic zone. The hole was drilled to a depth of 715.0 feet. No metallic mineralization vat obtained to account for the anomaly.
Diamond Drill Hole 66 ~S. Thie hole was drilled on claim P-58Z93 in order to investigate vertical loop anomaly V14. The hole was completed at a depth of 497.0 feet. No conductive material was encountered to account for the anomaly. It is considered that the anomaly is due to conductive overburden.
.4-
Diamond Drill Hole 66-6. ThU hole was drilled on claim P-6loy8 in order to investigate vertical loop anomaly V6. It wat drilled to a depth of 502.0 loot. No metallic mineralisation was obtained to account for the anomaly.
/its the planned program of diamond drilling wat completed and results did not Justify continuing the program, operations were euapended on completion of hole 66 -6.
Respectfully submitted,
M. E. M. CONSULTANTS LIMITED
Toronto, Ontario, Michael Zuiowak^y B. Se., P.Eng. September 28, 1966
J y ^ -iA ..
1 PRO
^^3— ~~ — ~ " ~ ^
FOOTAGEPERT Y
NORTH RANKIN WJLUiJjJJL M:|wid 5"
j-
Fooiage
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189
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225
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271
To
188
L-lS2
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2 8. T
—— DJP TEST
——————— ~ ————— i
——————— - 1Xnql0 j
^ft^f^T^J
—— 52 ———Corrected
——— 55 ——
COMMENCED April l4 r lQ66
tLW( " Anr*n P7j"IQ^fi
LATrrUDE 4O c;oN of B. Lo
DEPAHTOHE jjlrie 20 00 East
DESCRIPTION
fSASTWG, O - 7^.0, C]
ANDESITE BRECCIA, C hi1ft-
ay, 7-S.O -. 95.0. Gravel. 95.0 - 150, Siltoritized and carbonatized, breccia part-^Q i /4" t,o P" in size: bandlrKT ^ few place
-,t. pe;0 -4O0 j mlnov nyrite:...... . — ———— . ————————————————
.c; RHYOLITE, alternatirr^^yjir nVio-nr
^1 7 fi- vor^y* f eV S^i."3 !"
.. .... — f, ——jo- dark c;rey and pink flow banding at b ^v-"?iri-rystfi ne^
globulesT upper ??nd lov;er contacts 2mm iof quartz. spherical in sliape,( -.oo^iv,i-,r or-intbbslite) sho*,7in,a; iridescence ( spectral colors
' o-voon strong blue and purple ) - sharp•fnvr"r' OnO- R^0 ; v^^y Vis rVJ , aphanitic. Pa]
)4.5. ANDESITE BRECCIA
contacts, upper 80u-8^.e p;reen fresh fracture
, rough banding aV 45O ———— : ———;.q PORPHORITIC ANDESITE, carbonatized. partially chloritized,
white largely oval shaped phenocrystsfeldspar* throughout, massive, homogeneous, lis;ht f^rey andpale greenish crev on freshlY broken1mm in size: soife banding"•lobules of ( oils(T,t ,,^. -[-in-ne
^•*- AC W ' ~ao 't-p t f PT* COTt.Ppt
surface; phenocrystsw JTrovfclTr ctornl 1 ot-stjpv*3 n ^ T7R-RO^ lowe-r-Ss
5.0 ANDESITE BRECCIA, PR above,4R0 ? nppp
•roiip-V. Vi?n••r rontort
^r\™ 45O J T rtwo r '"on t ac
5 PORPHORITtO^ANDESITE. aa a^ove no ^nrllr,^
f,^ A NDrr.csTTF' •R^^rrTA-
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*t Vion^nofl rt f "•bvjrdnnn' ' **
Sam;:
ELEVATION
HOH.COM. T;-,^ f^^t
VEST. COM. 40"^ "
AZIMXTTH N AO OV
LENGTH 511 feet
0*No.
o
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FOOTAGE
Front To r^agth
HOLE Ho. A^.-j^SHEET Ho. i
LOGGED BT JL.J.D'Mo-le
TOTAL HECOVEEY rj^orly 1C
ASSAYS1
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DIP TEST II COMMERCED ELEVATION__ Angl* ! FINISHED HOH. COM.
* PROPERTY * W " Heading Correct LOCATK3H VERT. COM.
LATITUDE . AZIMUTH
niAMOND DRILL LOG i ' DSWUlTVafi LiJitiTH
Foolage
From
288
5O6,
7jll
"^Vi
•2,50
4Q2
To
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5-4
DESCRIPTION
RfTVOT.TTK: PORPHYRY ( '•-"n't* ^ - Of •non-pi v fl ev^l opfid .. .f el d s ri a rphenocrysts ( "StJ/o or more) in an aohanitic
crr'niji-idmoen; rmnyt.7. r.1 RO 1 n srVherl caA aTnrre^ates as describedabove but much mons abundant: littht crev , mottled white feld:par; p^le r;reen1 nh on fresh surface; an .Intrusive .porphyrv
^.q ANDESITE PORPHYRY, numerous nhenocrvsts of white feldspar iro flnr*V tyre y nnhianitic groundmass: some
c^rbo-n-'tizat.i on "nd chloritization, massive, homogeneous-j . . Q.-0 - - —— U
1.^. ANDS3ITS. as above, massive
/r r\ T? T *YOT T T1"^ PORPHYRY T ^a T ^ l T ^^^^^^P'?s f •t~An o-nVionitl c darlc s^rey ijroynflmaas; STDhGr
orro-rpo-ot.Qc. of (nu-'r'tz) 03 above ( ^ive a deex) blue or Durol*Iridescence on core surfacec) ; finer ^r^ined n SBr~' ower conta*w.M.nVi. 1 s of. 6-^ c,-f-.r-onn- olto-p^tion of intruded rock on lowercontact - iinper contact 80^
;o.O RHYOLITE , pink -ohenocrTsts feldspar snarselv scatteredthroughout, some flow banding, verv hard^
pore surface medium sxrev and Dale nink, also greenish onfrpntured surface: sBerical pT-^-^pc-ates of ou^rtz an^rselv
f V) T* ™ it? Vi 01 it. j c^vo-ral nu^rtz cprbonate stringers at Q •wit.hcoinnon r-f^ nT t.erp t.1 on s on walls.
———————————————— no contact betvreenc; R'-^YOT.TTK, ( RlTrnlpr to "^"56 - "5SO, save l^rs^er t)rot3ortion of
oink f eld soar end. s ome flow banding at 4"5U -sharp lower contact at 75? d .
;9.5 RHYOLITE, verv similar to above but in uart aooears slishtlcoarser trained wnd divided into following subsea
t,1ons bv slight ^1 ^f erenr.e in t.o-x-t.-iirp ond nnlonr*' 1 i o-ht.
throughout with accoiDpaning bright salmon red alteration of walls
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FOOTAGE
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Angl* li FIHISHEDi f WJJL.Jt.VdJU | -. . ——————————— - 1* PROPERTY BeadjD9 Conrec±~i LOCATIONj LATTTUDE
ntAMOKD DRILL LOG i ' DEyAAIUiU.
Footage
402
4^Q
46S
ToS-4 ;
c;-4#
c;- c;
•?11
DESCBXPTIOK
Q. c; PrYOT.T^TT (fon^.)ZiOO.c;-ApA (rr-oy wlt.-h .mo^t.Tar! rt In Tr t.ingeAPA.O-44R J ^or-P Rn-pfo.f.fi colour p#?.le pink and with specks off,vnTvvnacmeRlssn mineral f hornblende) altered to
chlorite4^^-E-4^4 P" mi e -rt K corbon.o.te veinlet at 30 , ^nor
ovrlteA4B - 4^Q.R. P-?.le ccrey vith winkish tin^e; few spherical QU.-AT ^ -nn -now rnn-t-.ont.n ohnerved between these subsections^. R ANDESITE BRECCIA, sharr) utJTDer contact at 8^
lower contact at 51 fr-TYOT.TTT? RlT-^lsr- t.n 4nP . c;-4c;O . t;
A^^. 1-!— AOO RfipTv Too^Tlni" OOT*'3 RijyTpfp' mol^Ty T 1 "Vi^rev vrith slirrht •ninkiRh t.lnTa
4QO - Sil r ve rv "Dale oinkEND OF EOL2
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Samp No.
ELEVATIONHOB. COM.
VERT. COM.
AZIMUTH \
HOLE Ho. ^^" - XSHEET 31o. ,3*
LOGGED BY
TOTAL. BECOVEHT
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FOOTAGE
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ASSAYS1
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,, --'
FOOTAGEPERTY
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DIAMOKD DRILL LOG i
y
Footage
From
o-j pp
152
154
P3Q
?40
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3OR
316
To
1 pp1 PP
154
p^g
P4O,
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Aagi*Beading Corrected
rjo . i.7 .iU
COMMENCED ^v* 1 PR T O/^fi! ninsHED Mnv ^th 1Q66
Z! LOC&nOH pt0?^^^ RRPQO
lATTTUDE 44-f-70N Of 3 /L
DEPAHTUHE Line 20-K)0 -S
DESCHIPTIOK
p^ ciT'^T(^.~t*vQf T^T OOP PV"V"cjY ( C5-yanl t.p )152. 0, Bh^.rp irregular contact
DIABASE, fine trained contacts ....
TUFF BRACCI A r 154 - ]187 - ?
87. fragments more)^^ fpwor- bomh^ c-L. R P110TM-.7. ^o-rbinn
abundant nnd InrT0^mr-ITpr- "Tr-^o-npri+.o^^ vo^yjlof.
20? . ^— ?O4 , r*nstv wfip thiftrp'^ -
c; tJUYOT.TTF PO^PT-TYPY ( nr^oM-l ^-.o ^2^0. 0, contact, sh^rp at 55o ,f1ow b.^n^l no- j-f-1 n^
trained margins240.5. contact 30U . no fi ow b^ nr? j n T
.R.R J VOLCANIC ^ffiCCTA,
240. S.
PAR c;
ip pTTVnTTT1^ POPPpYPY
siTillo.T' to tuff -breccia abovs but •frso--^r m on t. R TIO-TO nii-TH^rnaooears to containno-r-nbvrv ohnvp1 yT'p" c^n 1 r* r1 ^V".ar"p co
jpjjn^a o-nn-lno^ upper*
H R onrl TriT'.'ror1 * Vior)^ 1 n""YnfrasotJent of rhyolite"
ntsf-t 0 - RU
onfl lovo-n rsnj^t-ao.-tsnT 4 R
R TUFF BRF.CCI.V ( y0 T Qnn1 n Pv^^ol o ^
fi R FKT.SnPHYPT T,r,T Qvi t. Vi ssmoTT Mn-KoVioo i-i-"o
- . qpof ^. oflj l.^I-U-L\Uj
308.5 5'or, t ., ot ^o316.5 content. 4R O 1 yro
4.0. RHYOLITE PORPHYRYr _ ( (Z-^o-nl t.*O
-i- Er pph^nitlo .srroiin^Tiftss
crill •ST'
I^iNiD OF HOLE
Samf
ELEVA.TIOM
HOB. COAX. pp7 fVfz.t
VEHX. COM. 2Y7
AZIMUTH 3 4Q i,f
LENGTH 3 54 . 0 '
O*Ho.
'
-
FOOTAGE
Front To rjftngth
HOLE Ho. 66-2SHEET Ka. -^
LOGGED BT L^ 0 t M ^
TOTAL. BECOVEBY n ea3j*^^
ASSAYS
A^tage.
.
.Ofco.\XO -
lL
rJcc. ,uo
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/c?0 PROPERTY
::ORTK H*UT KT\T \T ICK5L MIKES
Fooiag*
From
n
TOO
10^
10^
.11.
PQ.
148
162
16"5
178
18"^
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-12
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JJS2.
VI
1 8"^
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FOOTAGE
Col 1 ar.
i fioo1
DIP T!r2jT————————————— 1 Angl* l
Beading1 ——— p-^u ———————— i® ———
fiO-S-~
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———— ————
?3 u ...,
1 "' - " " ' ' —— ' "
COMMENCED Me. y 6,1Q66FINISHED jffov 17 . 1966Locaxjou pll"1™!1 '^690LATrrCTDE 7. pc; N of g/L
DEPARTURE j |1po 4 00 T.V
DESCRIPTION
RHYOT.TTM:
DIABASE, f 1 0.+, contacts with li ttle nyrite.oyrrhotite
^ RHYOT.TT3 BRECCIA, minor nvrrhotitemo - no,
'.5 DIABASE,
Diabase, flat contacts
minor disseminated pyrrhotite a pyritem. c;, sham contact 80~
1PQ-R1 l^.^-lic
" 80";. ci. Ou s* r t z- Carbon at e Vein , contacts Of. 80"
* VOT.CAVTC T3HXGCIA f Tuff ft Rhvolite) heterogeneous
TUFF, verv fine straJi-tyrl
*5 DIORITE fa'
t.o p T ov-i n- -n-
Gr an od i or iter- s t.uff
ined ( du st. ash) few1-mi-hc. fr-or
f rac-ment.R . nvrrnot.1 t.ot.nT-oaj tllU*3 rrvo-ir
te?) lower contacton lower contact to
at 3O0 ii^^or QO?Dale olive green
8 TUFF, light blue ^rev r ^ine strained. plt.e-rot.1 ons onnpor -holoo•anfl r*'n1 or-1 t,1 o. onr? .Q-TO -p
17P.. 177.
o3-e ol 1 ve D-ree-n 1n ool oy0-1 7^ -O r ALTERED TUFF nod of ovrrhot.1 t.e onri nbolconv0-178.0, P ,,-rt.l 0^-] v ^
COARSE TUFF fraffment of this
n on "h o f* t. ^T yo.q-iyr
JD0 T O'.TOT*
C! -f*^ via r*
, .^no 9- no^' , i ; -
Itered tuff
formation
4^ -W^^^rt^* ^ v\/^** *^
conts Inert 1n nTnove t.u
eont^ct f 1 at^" " ~
TUFFTTT^~O-1 8^, o ATT'-rqvn TTTTTT? ^ nvr,y,-hrit1 f o ^^^-.v^T * r,^---^ ^v.1Q6^O 1 07 n AT .'i'u'S'tjip flr-rv ^•n'Trhc-'- * J-pi . 7 ^ j i i u t, uj. i,e
Samf NOL
ELEVATION
HOB- COM. V ZL , t
VEBT. COM. ^Qg i
AZIMUTH JT ^Q -p
LEKGTH 606
0*
0
It.e
f
6621
FOOTAGE.
From
241
To
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/^ —\
24"^^
Length
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ASSAYS
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^ PROFOOTAGE
PERTY
DIAMOND DRILL LOG '
Foolage
From
2SQ
267
291,
501^Oft
J
To
267
,
291
5-3C
^S f™\'J\J C,
^2?
DEP TKSrAnglo '
Beading
——————————— l
Cozrected
l ——— —— —— ——
DESCRIPTION
COMMENCED ELEVATION
FINISHED HOB. COM..
LOCATIOH VEST. COM.
LATITUDE AZIMUTH
DEPARTURE j LENGTH
9Al, O-OP^ o M.TH-;~-7:n TUFF, f a l, .r- . amount, nvrrhotite 5: rsvritealon^ minute fractures
??7- o^o n ,\T,TK:RT-:D
P^O, nuar-t.7. ve i9-Vj t;-OA-5; . t; ALT^R^DpqO ^-^^2,^ AT.T'C^s'.Doc;p t c;.^co fn ^-"V" "bon
TUFF - ?-3C ha
nlR-t at ^o
v', pvrrhotite. pyrite and minorIcoDYriteo
TUFF j 2 C' TrrrViotite-'Dvrite .minor chalcopyrPUFF, mLrJo^S Df ^It.C!
K-'oyrrhoti te— ovriter-ftfl tuff
DTCRTTE , chilled conr*nV)t. n f. t. pt.
tacts with700 1 owor-
wall rockfiO0"- rrood
both contacts ( not as basic asv^.,,^.,,..^ t.iC- t.^xtu re wiInrr p. fi f. t. 5 on R — rjOSSib]
2^9.^. A-11 ouartz carbonate vein
inclusions at uppermineralization on
common diorite alsoth acconinn.rjvinK quartz in succeec•r ouartz granodiorite porphjTy)v/ith i" nod massive suluhldes
in j-.r-or.or-t.ion 8^ ovrrhotite.lO^2^.7-26^.0, QUARTZ CARBOKATJS V
massive sul t)hides( 9926^^^^ quart.7. ocr-bortate ve^nlet
ilHat 70"^sf -nvvr^otiat" 650
pyrite, 5ft chalcopyritCont.'a 1 riin.T j.2. —j.T.th norl
^P 1'^ pVmTpnrivr'l tpj
c; TUFF267.0-278.0. ALTERED TUFF, ?^.t* e,,.-) ^^j fipcj
... .bunrMr,"- bv aTterffa'tion at 4^0?^7 O-P(^R O ^^i qulnhides . rrvrr* ovrite. chalcorjvr^ te
278.0-2QT.S. only narrow ba.nds of alteration- several2 0 o A onn 5 RbT^TL^tit " n o -n-n Q or- c •fr-^TTiont V'^ 1
norif CL Q-P -f-Ti^P-PUDDer and lower contacts st Bo
TUFF ( VOLCANIC BR
RHYOLITE, norno V O TT3OS3iblV
ECCIA) f bOTnbs Tower contact.? 1^0
r*on1 r fr-orr8 C5 U '
Ls .. ond ..t.V^.f T, ..lower i? on t ne t
Sampl.No.
t
—
i 66?2
--
FOOTAGE
front
267
To
274
L^glb
,
7. f
HOLE Ho. ^fi.3
SHEET Hot 2
LOGGED ST
TOTAL. HECOVEBY
ASSATS
cu
0.02
NIAU '
0.01
A^gc*
CO.
\S8
•'0:0.\ UIO\XO
/O)-; ea. \uo \xo
* PROFOOTAGE
PERTY
D1AMOXD PRn.T. LOG '
Foolage
-op.
71. '
383
387,
38'
453 ,
487
491
494
R4l
561.
To"W
38'
3P7
5-3?
45"
5-45
'R-4f
0-4
0-5^
O-R
^ f O
DIP Tiil"
AngI*Beading Conode
li COMMENCED
' FINISHED
* LOCATTOH
LATITUDE
DEPAHTOBE
DESCRIPTION
c^ r-.Ti^oTT7 T^T nt^J Ti*r f n iiov+j "roT5 o^ i ovi-^ t. o r-iriY""i}"iy vy JYl ""' — Ears' s i ve . homogeneous ir.inbr disseminated sulphic
DTA^^S^ r. h 111 e. ri pont.opt.s nnp^-r 8'7 ,IOWRT- ^O
R CTIART7. DT OR T ffi, PR qhovo
9.0 r FELSI6 BXTiS
.c; r,T!\RTZ niORTTS^-r5 s -S "5 T\ i\ ra "P O^.o-r-^c-— fto /?O
7. S. TU?F J (M.TT^m46o . o-Ji^7 . o p ^ RA^7.n-4Ri .o 4' i
n T nVi 1 r? o H tnolnlv Dvrrbotiteit 'i n
4^T.n-4R7.c; 1^ " QO'% pyrr"*"hotite487. R 5 noritdCt ft R0
1.0, RHYOLITE,Aoo. 0-4 01 -O. 10-1."ovrrhotite and some magnetite
4Q1.O. contact 4SU4.0 r TUFF, v-rv little
1.0. RHYOLITE, n-^flnolsectl on
p.or.t.ont. of mainly
alteration or mineralization
increase in magnetite content throughoutfrom 5 to 30 percent; pnd variable sulohicnvr*rhotite. rsvrite and little chalcoDvrit
————— fjio-n P^t.o PO p^-rcsnt.. yhvol 1 t.p- wit.CT4 n c]^ n ].r^3s
' oXr-,0
l.O r QUARTZ DIORITE, o
TTT7" ^[IT P^TTn™^ Pi
~ t.
s... above . RI 1 1 nh 1 r? o
h black and sjreen luster5^' T ov.-pyViftt.1 t.o j nv-T-1 1.^
^"
c on eon t r P 1. 1 on n on bnt.Vi
utyoer and lowej? no-nt.ont. s .of. OQ0
0. RHYOLITE f IRON V~\ -nVi Irloa m^^nQtlfr j v-j--—— "."
" *^
^ x^^j;- -* "n t-o
5aflni
ELEVATION
HOB. COM.
VEKT-COM,
AZIMUTH
HOLE Ka. 66-3
SHEET He. -z
LOGGED BT
TOTAL. HECQVEHY
LENGTH j!
J*Ka.
es
662^6624
662566266627o 6^?Q
6629663O6631663?66336634
^rr6636^
6637
6635
FOOTAGE
Front
A8T48 R
493
ROD
RI ^
^?o"qpq
R^OC;XR
537.
561 n
570
To
4^5A P, y "c
4OR5^0c-inRI "^t^l ^R?Oe-pc-R^nc;"3; c;
; RAi
1 565575
Length
4 r2 c
o nc ric^ n
^ o3.0
5.05,05. 0^'^
4.05.0
ASSAYS^
cu
0.030.06
0.060.020.030.030.030.070.030.020.020^.010 020.06
0.03
NT
NoneJiJone
NonNoneNoneNoneNoneNone
None
None
None
Averages
.
01-EO.
i UO \XO
- a a \ wo\xo
-to* i a c. two\XO
* PROPERTY
DIAMOKD DRILL LOG
Foolage
RYft
R8"3!
RO7
To
RR^
RQ7
R-^(
^nfi
DIP TiiiT
FOOTAGE
1
Angl* !Rearfing Cocrectod
l
COMMENCED
FINISHEO
LocATioarLATITUDE
DEPARTURE
DESCHIPTION
niA^Ao", TI^^ oontor,n x^ r, t[, ^^
r* t. RO lo ne, r-ol 1 7,,-^d
trp.-r 4O 0- pyrrhotite oyrite, chalco.
R TROW FORMATION f RHYOLITE). 753 mayenite f i lax. oanaj.n 5 ,nvr-rhot.lt.fi, nvrite p.nd chalco. on lower contauL
c^f 1 1 on *? o OTI t. 1 n s verv littleR07 r R can t.?.(?t. pt ?
sulohides
^ P WOT .ITS, nq.le green r^nl 01-Rd p Iteration verv little sulphide s
.. KWD OF HOLS;—————— . . . . . .. -. .
L,
ELEVATION
HOB. COM.
VERT. COM.
AZIMUTH
LENGTH
SansO.No.
^(^^Q
FOOTAGE
FromJ To
ROD RQR
Length
R.O
HOLE Ra. 6^.3
SHEET Ea. ^
LOGGED BT
TOTAL. HECOVESY
ASSAYS
A^rag^ '
.DO \XO
/o'aa ' v uo \xo
IOi-'eo. \uo
T
^ PROPERTYNORTH RANKIN NICKEL MINES
DIAMOKD DRILL LOG
C
1
)2.6
f
3
Footage
From
125
t
^o 5
73.5
98.0
L2.5
Top,-
3,59.
-273
298.
312.
W,
FOOTAGE
UCollar
i
DIP TEST1
Headingg-*0
Corrected
R40
1
COJSCMENCED Way T7 y 1Q66
FnnSHE:D Moy ^11 T 066rxxaoio. 21^0^58293LATITUDE 6 50 N Of B/L
DEPAHTC7HE 24 00 W
DESCSIPTIOK
rA^TNfi
5 TUFF ( Sll±125 - 129.12Q - 136.136 - 139.
139,139 - 146,146 - 151,
151,
l elf led & Partially Chloritized)li^ht strey tuff .few fragments, fine grainedSilicified tuff ( rhyolite 1 )medium grey fine grained tuffsharp irregular contact 20OGRANITESilicified Tuff ^sharp contact 2O
151 - 152.5,. Basic completely chloritized band with few fragmen152.5. sharp contact 3OW
152. 5-159. 5 P Silicified Tuff159.5. Sharp contact 45
.S.^ANTTK. imedium fffalned. tvPlcal1RQ.R-.1Q7. l Silicified Tuff.)IRQ.197
R, Indefinite contact 45"e on tan t. -^-45U f?)
261 - 271.5. Basin Mnre-lnal Facies of Granite271.5-273. 5 t Feldspathized altered zone
) BASIC TUFF, dark orey to black, aphanitic, small rounded white, fragments, hard, massive
273 .5, irregular contact 10 - 2O"PQft.O. nnarn contact 45"
5 PORPHYRITIC GRANITE.312
white feldspar & blue Quartz phenocrvsts.5, basic marginal facies, contact 45U
) TUFF, liffht A mediumspindal shaped
grey , few •frasr'a malnlv TP aa ?mm oovo-nolbombs, alteration increasen 1n 1nt.ens1t.v
towards lower contact,-j t pir.at1 ori
u
**
EUEVATION
HOH.COM. 4-1 c; 1
VEHT. COM. c^ i
AZIMUTH w ^O V
LENGTH 715 '
Sainpi*KOL
ps
i
r-.
FOOTAGE
From l To Leagih
HOIX Ko. 66-4SHEET So. ^
LOGGED BT L^T ^ p ' A1 p-1 P
TOTAL, KECOVEHY gQfg
ASSAYS'
^
i.'—'•-
Ar^r,^
o-ea mo
' COL
V UO\XO
J/o/CO
-j.'Oy-' a a
"
' PROPERTY
DIAMOND DRILL LOG
Fooiage
L2 5
1-04
(.4-^
48^
too
R24
560
To
404
443
y 48
,S 4
R?4
RfiO
680
FOOTAGE
- ————————— — ' l
Heading ! Correc±*d j——————————— j ———————————
t
1
DESCRIPTION
COMMENCED 1
FINISHED
LOCATIOK
LATITUDE |
DEPARTURE
T n f TTTFF (Con t., )^56-0-^67- ( Cont..) appear to be amygdule s.. ,367 ^..^825. q. Hire '^l?- ci-356.O,382.5-404.0, Intensely SilicifJLecLA-Shloritized Tuff
appear rhyolitlc, little sulphide mineralizationmainly pyrite
404.0, Sharp contact 65
5 PORPHORITIC ( DIORITE; creamy white phenocrysts feldspar,dark grey aphanitic groundmass
443.5, sharp contact 85U
;.R AT.TERTTO TITPT?. fllllRl-Med. chloritized.H\^c; t c;, cont.act shart) at 4R0
)Q PORPRQBlIJS-OnORITE). 70# phenocryst s
epidotized
(porphyry)4QQ.O. contact sharp at 45V
AT.TfP.RED TUFF, r.VH oritized r silicified.c;P4-0. Indistinct contact 45U
DIORITE PORPHYRY .
•550. 0. con-;33-535. A,
same as 485.5-499, 5act 30"
li^ht & med. Krey-
Wfc phenocrysts
TERED BASIC DYES ( DlCftlTS)( . .
TUFF, -1 /-x. -^
560.0-574.0, Altered Tun1 , silicified chloritized574.0-590.O, darK grey to DiacK, imm rrag's r ounaea, angular590.0-601.0, light601.0-619.0, s6me"
grey, little ^alterationbanding 200 C^-TU ^i.
619.0-631.5, same as 574-590,M' ?^
631.5-642.0, silicified, pale grey aphanitic642.0-660.5, like ^74-^00
fJv3 .O j rnr(t.~*.n AL+^.VIJ
nr.t. ^n j fifir),c; } r*ont.a^/i Tir-P.f. ci 1 J pi -f Ipd eh
nt "^c;01 OT-1 t.1 7.Afl
670672, DIORITE, upper & lower contact 75O
ELEVATION
HOB. COM.
VEKT. COM,
AZIMUTH
HOLE Kow ^ ^ - 4gHv.v.r Hot ^2,
LOGGED BT
TOTAL HECOVEST
LENGTH l!
SamploNo.
--
^
FOOTAGE
From J To
-
-.
^
Length
ASSAYS(
-~-
i
•~
-~, — -
-
l
ca uo"l
,: aa - •: uo \xo~r
(ra \uo \xo
--
^ PROPERTY
DIAMOND DRILL LOG
FooJage
From
-QO
To
715
715
,
. .-. — ———————————— -! —— ' ————————————————————— ——— r
DIP TEST J
FOOTAGE
t ———————————
•— ' 1 Angla
Heading Corrected j
11
COMMENCED |FINISHED j
LOCATIOH
LATITUDE
DEPARTURE !
DESCRIPTION
*RO ri r-rtrrt-Qot 45O
fi-RATTTTTr ^Imtlpr to 15O^5-P7^- ei
END OP HOT.K
—
.
ELEVATION !HOB. COM.
VERT. COM. |
AZIMUTH
HOLENOL 6 6 - 4
SHEET Ea. 3^
LOGGED BT
TOTAL. BECOVEEY
LENGTH i
Samjil*No.
i - -
FOOTAGE
From l To
i--
LengDb
ASSATS
Av^g*. J
O"ten.i DO IXO"t
'o-' CC. ' \ UO \XO
PROPERTYTO R&WTTTW WTCXELJIINE!.
DIP TEST
i FOOTAGE
1 collar !3 pcin 1
DIAMOND DRILL LOG i'
FoaJage
f)
.30U,
173
1 ffX:Lo2-
206.
i±y
300
300
y^-
To
130
J-JLZ
1P3
20^
b 21
5OO
30b
•^) 3
? ^
AngleHeading
c COCozrec±*d
______ 7*^ O — ———————— ft —— rR44-0 j 470————————— ! ————————
f— * ——————————————— rCOMMENCED .Tlwft P r 1 Q66
ro"32™ June r5 r 1966 jLocATios Claim NoP58286 \LOCS.TIOH Wn-hor.1 Py Twp. jLATITUDE 25+5O N !
DEPAH.TUBE . 16 00 W S
DESCRIPTION
—CASINO- ———————————————————————————————— : ——————————————————AT.TVR^n 'ANDESITE, f eldspathized . carbonatizea, ftvi ovi t.i *e*1^4.0-157.'T loas nil •.^•p^fl ba-nd1 AI , R..1 *? . c; , ...3 ^...pyrlt.p ———————————— , .**i.T7^.rwiR^(")- bleachec L andesite C&&5&&3& .carbonitized)
BLEACHED ANDESITE. (183.0, 1nd Igt-lnnt. COT
c: RHYOT.TTTT PORPHYRY (a* 0 0* AK0
carbonitized fc Sericitlzed andesite}it ac t 806 ('
GRANITE)onri ^0U- ,
?)
vit-b T^ar-hz-carbonate s^rinsersilt.ecration banding at 45 — pvrltemineralization scattered throughout oiLfractures and stringers
195 5-2oni,6 T V
Q*1 — opT*b . velnlet at 50U•hand containing 20^ pyrite at ^45
202-0-PO?.c; j T1art7j r- rb stringer s at 45W T 1O^ pyrite206.5, indistinct contact
? ALTERED ANDESITE, mainly feldspathization, chloritized.minor pyrite
219 contact ( possibly 501"?)
ANDESITE.^Suu.u, c^q
.5 Feldspar
bleached.ntact 1RW
Felsophyre
or alteration banding
contains few fracgnents
phenocrysts become more abundant towardslower contact ( last 1^'}305.5, sharp contact at 'dy
'•2*5 FELDSAPR FELSOPHYRE from ^")8.R to w . f?-O few Bna-ht.eTeflphenocryst s - become more abundant toward lower- eon-tact
323.5. contact 5-10"
'.5 ANDESITE32^*5
, aphanitic f massivesharp contact 4^"
Sarnp Kb.
ELEVATIOH
HDH. COM. ,,j0 *—————————— y d. — j ———————— . VEHT. COM. 33Q
AZIMUTH N 40 E 'LEKGTH 497 ft. - ~
la FOOTAGE.
From To Length
HOLE No. 6fi-5
SHEET 3Sot \
^OGS^^L.J. D'Ai^le
TOTAL. BSCQVEHT 99^
|
ASSAYS1
A.VOTS^S3
OfKB.
\lilO \XO
V UJO \XO
rj
/ft
f - ' "
* PROPERTY
•z-
•z
r
Fooiage
7 ,-
39 5
353
394.
4-21
432
1-37.
442
•56.'
72. '
To339*
353
394
5 4?
432
.5 4
b 44
456
i 47^i 491
4yi ^y49'
DIP TEST
FOOTAGE
'
Angl*Reading Corrected
11'
——————————————————— ! ——— —— - ——— - —————————— ! ———— ~ ——— j]
COMMENCED
FINISHED
LOCATIOH
LATrnjDE ' ,
DEPAKTOTE
DESCBIPTION
c; FET nq'PA.R JEELSJ2PJECSE: f sparse number of phenocrysts'^^0 c —— vTo-pr, ^rvYi+aft. at. 4t^0
FELDSPAR FELSOPHYRE, the odd phenocrysi-353.0, sharp contact 45"
. ^ FLEDSPAR FELSOPHYRE, 405S phenocrysts tnrougnouii394. 5. "basic, silicified obscured oouuaou
ANDESITE , chloritized, carbonatizea, lew ju-agujeiJOB4Pl,n, contact 30"
.5 ALTERED42Q.O, J
PORPHYRITIC ANDESITE (?;*-3" nuartz-carbonate veinlet at 30W with massivepods pyrrhotite and pyrite 30^
A. 9 , J2 pViarir* oont.of't 7R
B7 ANDESITE^ medium grained,, few phenocry432. "S, contact ( siliceous alteration"^437.0. contact 700 (?)
! ANDESITE
— :
•st s
. fine grained, some flow banding at 45~fc 55"440.6-442.0, core
5 ANDESITE
( 449.O,452.0.
in small pieces
, medium grained, few, phenocrysts, few gragments, someflow banding
possible contact at 800 )contact (?) at 35?
456. 5 r sharp contact 70W
.5 ANDESITIC VOLCANIC BRECCIA.471.O-474.O. core in fine pi
20-30^ fragmentseces
ANDESITE, medium grained, bleached491.0. sharp contact 5O O| ——— FfiLJJbJ'AI ——— —— ——— ————————————————————————————————"^FELSOPHYREj
Samj No.
ELEVATIOM
HOB. COM.
VEHT- COM. j
AZIMUTH 1
UMKV"T Ua, ^7
LOGGED BY
TOTAL SECOVEET
LEJTGTH i!
J* FOOTAGE
From To LeagSii
.
ASSATS
i Araac^
i i,Wb OF HOLE
o-O.H.
aa 'i WO
'tt C.\uo
"V
.|| DIP Tt-jsT I) coMMEKCEDjxjn e Jl)nel6 ELEVATION0 ————————————— ~- "" ' 1 ^ _ , ^8^ Angle ! FINISHED -r\mp ? R 1066 HDH. COM. 290^^^B u x i/u i A.VU.C. — .. i ,. . , —— ' /*n—4™ "li" C -i C. o !-!
W PROPERTY , Bea^ 1 COI"Cted LOCATIO^^l^E^1^ VEHT.C014- Zn fi ,i Collar ^ o j ™ —————— ri±-±d 1 UJ-JJ- "- ———— t ——— t.i.v.,..TJnwrmj WAWTfTTxT T.TTI-TVT MTTra"S 2R0 1 ^8*" ^"3- LATTTUDS 20; 00 N j AZIMUTH S 40 W
DIAMOND DRILL LOG i 1 1 1 OSPAHTWHS 28 UCL K
Fooiage
From
0
151
263
295
393
471
To
L51
263
295
393
471
o b502
DESCEIPTION
CASING
FELSPAR FELSOPHYRE,, massive , hard, rneduim srey. porphyriticmi - It^l.n rtnmrvlo+.^ly •r^1dnr.a,fh1 zed and chloritizedT^, lg-" band nmsnlvfi chlorite with 2R^ coarse, crystal pyrite' t-1 J - at., &00174.0, 3" quartz veinlet at 70O - feldspath! zed mar^^ns217. S, 2" quarts veinlet a,t. pcio , tourmaline, no Ri}lph1r^F .248.^-24Q.6 r completely -feldnrtathl zed r26 3.0, Sharp contact at 45^, trtmcptes bedding n^prT y ofr onv-TUFF . bedding at 45". carbonatized throughout r quartzitlc-
greywacke like layers, few samll rounded and angularfraOTients r locally massive with no banding, locally 5 to lO1^
massive chloritized sections, pyrite'Cvrr'T T\ QTD A TD L'lt'T C! r\'OTTVT5Tri m t . .r JSJUL'DJrArt^^r JMjOUJriliru!* . rnpaftlye, nOTnocren.eniia tVirox^Viryt^"SQ^^O, Sharp r.ontaott at ^Oo ' - ^ w .
0 VOLCANIC BRECCIA. TUFF BRECCIA, TUFF. ( no distinct contactsbetween ) mainly well, bedded but . with massive sections nobanding, rounded and angular fragments throughout. lOcallvaKclomerltic393.0-402.0. cosjse, basic, chloritized, volcanic breccia-
no banding402.0-407.0. basic tuff breccia-, banding 35 to4o ( bedding)407.0-434.0. coarse banded tuff breccia, bedding at 45W428.0-447.0, bedding at 75 - 80O434.O-471.0, mainly massive fine grained tuff with few small
fragments^.71.0, Sharp contact at 20"
2 FELDSPAR- FELSOPHYRE, as above '
END OF HOLE
ij LENGTH ^02 ft.
Sarnpl*No.
66406641
FOOTAGE
From
433.0418.0
To
434.5419.5
Length
1.51.5
HOLE Ha. 66- 6
SHEET JSe. li.
t^acEDBY L. J. D 'AideTOTAL HSCOVESY .^Pl 1 en t
ASSAYS
Aa.
NilNil
1
Pyr tizedi
1
A^r*.^ ;
j
Tuffit
, aa.- IdO \XO'L
' ac. . wo \xo
'eaVUO
-/o v J ac."i-
iJM
jL3
&O
H-L
WILHLL Mi *1 A
MOtJERL v'
TOWNSHIP
TOWNSHIP
GEAR f TOWNSHIP^
THORBURN TOWNSHIP
t O T 4 LOT UO'T SL L. O T l
l UMCi-M l N R Tu/P.
V l
p. p
j oft2-J?
P ' V
.t rt t, 6.1 f-
e ae i
* p, -t
4 -..
l2tfoftOfo I
KEY MAPi " - i .^
O
NORTH RANKIN NICKEL MINES LIMITEDMOBERLY TOWNSHIP PORCUPINE M NING DIVISION ONTARIO
DAT Y 7, I9GG SCALE i INCH s 400 FEET DRAWN BY
M.E.M. CONSULTANTS LTD.42AI3SE0898 1* MOBERLY 200