dd rpt 35 joubin twp - ontario · 2017. 1. 17. · description naxinun diameter, mostly altered to...
TRANSCRIPT
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Diamond Drilling41J87NE8169 9016A1 JOUBIN
010
Township of JOUBIN (Formerly Tpt.lt3)
Work performed by: Kerr-McGee
Report N9: 35
Claim NQ
S W 3217
Hole N9
1U3-2
Footage Date Note
3509 July/67
X
Notes:
00417-69) rev 9 72
t tt?. TESTS•PROPERTY K^ttH-MrWK CORPORATION
TOTAL CSPTN 3509___ CO-ORDINATES COLLAR Twp. 143
K.LOCATION
LOGGED OY fLLJk^illL ELEVATION 1150
DATE GEGUN -L"]" . 0 ? ) ..1^7; AZIMUTH __ DAlt: FINISHED 8*!^' 20' V
LAT. 500'N PEP. POO'W of Ho. 2 PotClaim Ko. 5-14521?
Vertical
r00TAGS 0-6"
I.GTH. DESCRIPTION
Gc sing6-54___ Serpent Formation
34-476 iia^anola^ Formation -—.———.———I-.'s-anola Formation (Bruce Lirostone)
560-607 __ ____ r:rucc Foraatipn (Bruco Conglomerate) 607-2371 —__ __ Kj.s3is3p.gi Foliation (Upper MJBsissagi Qte.) 2371-3084 ?ccors F^rr^.tion (Middle Misaissqgi Argillite) '
Hr'-roy LrJco Fon^ntion ( V^igjcgyjConglqnorateX 3092^3157 3157-3466 34S6-5509
3509 LV.d of holo^ ———--
Co* f *r*az* AT Core stored at^ drill site
30-''-5.l359?.,c?J'1^torc4 {l* Kcrr-HcGo warohouoe in Algoma Milla, Ont.
Hrtl,-. firillod
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os
OATH CEGUM J .22-1- DATE
TESTS
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300' N. OEP. 200' W. No. 2 PoVAT I ON n50'MUTH
LE vertical.^ ,_ _ ^r ^ . L JU^ . . ^.M
DESCRIPTION
it
[in Serpent Formation)te: grey to light grey; fine to coarse grained; subround;stly quartz grains. Zones with no or very sparse darktorstitial argillite interbedded with zones of abundantrk interstitial argillic materialrock. SC.T.O very dark grey zones
gives banded appearancewith abundant interstitial
terial are up to 1 foot thick. Bedding planes lie at 65-70*axis of core. Sulphides sparse.a Formation ' 'Ice: dark grey; a mixture of siltstone and argillite,distinct bands, mostly with contorted laminae, with
someaomo
T! grains scattered throughout. Several zones show a con-jnoratic or brecciated texture, as might be formed by af, nud-cracked bed being re-deposited. Kuch contorted'nin.-o, as frora mud flows or turbidity currents. Lower 753 1 nhows lo s a contorted bedding than root, but some isj.-; en t throughout* Sulphide J about 1 - 1^.luo:;tonolit /jroy to lif;ht /-^:oy, with alternating dark bands fromm to /|0 pan thick. Boddin/; pl'inon vra-y frora 00* to 65*a/ifj of core* iSulphidon louu tluui I'/i*
s vi.'i-y /Ir- rk /.ropn, nlnoot blnnk.•T ——— r- — —— -
Cry M talu to about 2 mm ;f"
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PROPERTY Corporation
^^^^•T1•L FOOTAGE
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Bl 529 - 531B 531 - 560m 'mmHp560 -H&60 - 607 ;:K
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^Ko? - 746 " ;^^^•|.^^^Ei'^w^TC^^^^^^^^^HK-f- - .
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DESCRIPTION
naxinun diameter, mostly altered to chlorite.J.ir.^atone: G roy; not banded as noticeably aa interval above diabase
but laminated with finer bands 2 - 5 nu3 thick.Dinbaao: as above from 500 - 501.5*Limestone: grey, with 4" ot line-pebble conglomerate at 539* *
Pebbles to Vti" in dianeter. One foot of contorted beddingat 545'* Lisiustone grades to dark grey at 556'. Sulphidesless than \efi t
Brace FormationBiMce ConrloKorato: dark groy with pebbles of grey or pinkish-
ftrey granite 1 inch in diameter. Black jnatri* tcv~r4 top isoi'Cillic or.d grades downward to silty and quartzitic greymatrix.
J-assif.nnei Formation"vartztto: light crey; very coarse (a "grit" by some definitions),
arkosic; subrounded grains; very poor sorting, with beddingplanes from 75* to 85* to axic of core. Crey to dark greyzones of greywacke or abundant interstitial argillite occur .at 694 - 702; 712 - 71/j; 734 - 736; Sulphides less than 0.555
TV.^.Vv - n nill or diko: very dark /:roy to black} lamprophyric}fi no urn.ir.iil w ith, oovoral quartz ooama 2 nsra thick cutting thsf?' b."r:A, Contacts about 65* to 70* to nxtn of core, noti.'u;)i rnoro th.-in bedding pl."noo of adjacent qunrt/ito. No
c.ii ••(•l.'/Uos .-id nVovo with //ivywacko wnon at 770 - 7'J2; 799 - 000} .'/•*t - (-/(?, filial tly con;;lomo ratio with ruvo pi^.hlixi to VO"
SAMPLE NO.
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PROIIIKIY Corporation
HOLE
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mHmV905 - 963
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^Hf?63 - 1025
^Hp25 - 1 110^^ft.•RlO - 1150
HP•:^^^Ki ^HB?0 - WQHKHHp - i5';5•k-...IHi^^HELHBHpil?'KW^' KiSisas^r...^/-?Hi?--
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Df-ISCRIPTION
in diameter 064 - 866.Zone of greywacke 876 - 879.; bedding planes at 85* to 90*to axis of core. Sulphides leas than 0.5?* trades downwardinto
Quartzite: as above but generally coarser with 1 to 10 pebblesper foot; pebbles both black and white chert, some white feld spar, up to 3/4" in diameter. Some zones of greywacke ofinterstitial argillite, but less abundant, more arkosic.Sulphides less than 0*5#.
Quartzite: as above, but only very rare pebbles. Greywackezones at 963 - 964; 987 - 989; 1006 - 1010.
Ojartzite: as above; but more zone of fine quartzite. Rare grey-wacko .
Quartzite: aa above but conglomeratic with occassional chertpebble to 3/4" in diameter* Greywacke zones at 1141 - 1143l1164 - 1166; Grades downward into
Quartzite: light grey; mostly coarse, some very coarse-grainedzones. Greywacke, etc. at 1250 - 52| 1258 - 61 j 1342 - 44l1J52 - 56; 13b9 - 90; 1400 - 02; Generally dirtier tho- above1150. fiulphideu Ions thfn 0.5/^*
Oo j ;j - /nek n ; d f. rk i , cay to troy; inoatly fine to medium quartz grninsvlth abundant dark grains ond dark interstitial material*!ior.o ll^Jit Ki'irj quax't/.ito '/otioa ut 1559 - 64 J 1572 - 74lly/y - 01 j 15^3 - HM, all with /,ivutationnl boundaries*:iiilri}ild(;.i ln:;:j tl.,-0 l'/. ^Jivtitoii (!o\;nwiird Into
' 'f r'./.i t'-: ^i'.-./ to ]1;,lit i r-ryj finn to vi?ry noaroo /.ivHnod,:i\ (.M -"V - ':!-o xoii":i K,0.| . 0'.; \ (j'') - Y';; l6fJ5 - J'M; 1754 "' ' ' " .. - - ---. .... - . -, .
SAMPLE NO.
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MRtAGE
IB2 - 2iiiB'flimL
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my^gr ai6i
BHE& 2312Ml•ft^K^n^^^^RLIBRh—BHBP750BHKIBHB'f: -
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DfiSCRIPTION
59; 1764 - 68; 1600 - O?; l?05 - .10; 1958 - 6?} 1968 - 70.(li-adoa dov.Tiward into
Cu.-irtalte: li^ht yellowish ^rey with coino light grey to freyzones; fino to very coarse, as above, Boddin/r planes 85*to 90* to axis of core. Some croso-bedding. Sulphidesloss than l'/}. Greenish-yellow color very pronounced at2066, again at 2080. No abnormal radioactivity. Argilliczone 2083 -85.
lamprophyre diabase sill: black} also 2" Beam at 2099. KLnetrained; chloritic. Contacts parallel with bedding planesof quartzite.
Quartzite: licht yellowish grey, as above, with yellow colorfading dovnv;ard gradually to light grey at 2181. Noreal ^rey wacke zones, but some zones with moderateinterstitial argillite. Sulphides less than IfS.
Quartiiitcs grey to dark grey; very coarse; mostly quartz grains.Sulphides less than 1& Core badly shattered 2228 - 22J8.A few light grey quartzite zones 2255 - 58} 2274 - ?6f^292 - 2J01;
Oi-'.-y./ncke and .jiltatonco: dni-k /ji'ey; come rare argillic laminae.t):io ia tho .tjiv-njij^tlcm ^.ojTfJ.
Pocora Formation.' r/ji 111 L'.-: *J.".rk ^roy, with oillatonoa, utroakcd with altornating
l;jiin-.o 2 - 5 rja thick; *3urk and vory dark ijrcy. . A few/..•oyv/r.c'^ ; /-/nl ;i 1 1 t,:i tonrt ))'-(J:j with no vintblo l.fMliliii; ( ^Inmm. 'i .': . f:',f,:,oH,'."t *)'vj'l?n,"- i n .-ir^mi' -. I'OMt b-.i.Hn^ tilnnoa
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PROPERTY Xorr-McGee Corporation
FOOTAGE
S750 - 3067
3067 - 3084
3084
3084 - 3098-
-30983098 - 3157
-
31573157 ~ MG6
LG! H. DESCRIPTION
at 750 to 800 to axiq^pf w*o* ^o liflht /rrey quartzite zonesin this interval. Sulnhidea l-lifi, mostly pyrrhotite, stmapyrite, rare chalcopyrite, trace of molybdenite at 2727'.Streaked laminae not as abundant toward base of unit. Gradesdownward to the argillite below.
Argillite: dark trey, with abundant siltstones and greywacke,massive.
Argillite with abundant irregular quartz veins: up to ytfi of the *unit.
Ransey Lake Formation (Whiskey Conglomerate)
Conglomerate, polymictic, with grey granite, white quartz, and darkme ta- volcanic pebbles in a dark grey greywacke matrix. Pebbleup to 3/4 inches in diameter, sub-angular to sub-round, poorl:packed. Trace of sulphides present, mostly pyrite*
KcKim Formation (Nordic)Interbedded argillite, greywacke, ^iltstones, and fine-grained
quartzites, dark grey. Argillite is darker grey and exhibitsvarvod-like laminations. In places, the fine grained quartz-itoo show traces of cross-bedding (sort of a mottled effect)Trace of sulphide:} present, mostly pyrite. JVora 3154 to baseof unit, noatly argillite and oil to tone.
Katinondiv Formation, Stinoon MemberQu.-trUito: li^ht /jroy to vory li^lit groy; vox-y conrae with rare
pobblcs of riuart'% and chort up to -y" in diiunotor; smallerliTiiJn.-j "r': noutly (luart1/., but tjo'iuo ocattoroil foldopfrb. Somey.f/Morj with Jntoratitiul oorioito have a lijjlit yellouinh-croy
*•;oloj*, though tViln'."r t-h/m Uio ytilloi/lnh wo ynnna of tho
SAMPLE NO.
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FOOTAGEv t- 1 "- \- . v .
34863486-3509
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LG1H. DESCRIPTION
region, Sulohidcs about l*', mostly pyrite which, occurs inclusters uo to v " in dinjsejkpiv 5QceJ3ona.t.l.tft. grains .1 mm. in..di;unoter are probably osucdoElorphic JifteP pyrit** grains, Tlmsft
-. ar.Q lp.s.s.jl.vTn 0..55Lro5kji....Harro.w.zones...(l.to,3-.inche,a)..with ,. -.abundant disseminated, pyjritsjlji a. dLiji-ty^ Argillic^ matrix aremoderately rndiorxctive, as follows: G 3264', radioactivity is2 x background}
3297.5 radioactivity is 4-5 x background;fron 3308-3312 radioactivity is 1.2-3 x backgroundifrom 3360-3363 scattered 1-2 inch zones with up to 2 x back ground, No abnormal radioactivity at basal contact.
Ai'cheiiJi Basement
Ke '.-.'.volcanics, prob.-ibly basic tuff, very dark green to black}hardness of argillite, uneven schistocity but planes of abundantpyrite probably in planes of bedding lie at JO to axis of core.Sulphides, 2/' mostly pyrite.
T-1 - 3509'
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BOIS 143-2 - ELLIOT LAKE PROJECT
~33^yf tt.- ? * - ..
Poota^e
0'3065150250350430555650850
11501350145016501750185019502050215022502500265028502950305031503200
Acid Test Dip
#89*
9089
-87
8280&83828280&78787877?8,77s783-75z77t
Tropaxi Dip
89090
8987
8683
e
80
77
•'
77
Test Azimath
.1190251
181197
202202
212
230
224
231
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iJoriaontal plot of tho course of 3MILL HOiaTovnship 143, Ontario
N
60 I-Declination
P.D.H. 145-2 intersects the Horizontal Projection of the "S-W" Claim Line O a dr-11 hole depth of 27J1' at a point 206 feet vssi, and 300 feei sou^h of zhe collar
3uriV.ce data fron Coapass and Pace Surve^ Drill Hole -ata froa Acid i Tropari C?ests
f
Notet all clain ' lines approximated j
lJftoa el&ia cap
13730? 137306
Scale in feet
Plotted ay
ICO 200 5CO
David P. 2eii Geologist
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Sin.
DHILL PItOCRSSS LOG BRILL EOL2 ME-3ER 14J-2 Data
KERR-HcCHB XRPOfiATIONELLIOT LAKE PROJECTScale .0 klOO feet
. —--. . ; -itai.-.^t.^ry-
m*.K*#-c---.- -teA- -. : . ~
7JH1LL HD12 LOCATION
TOUBSHIP 143
KERR-MCGEE CORPORATIONSCALE* i 1*- i
r .J O -. Grovel -.5
LEGEND
L oh t Swompy tod*
Rlvtr, Slrtom
Swamp
Dom - Bcovtr, ttc
Rapid*
Reed, Track , Troil
Ovicrep
Pit
Cmbenhntnl
TO w rt jh l p Boundary, Milt pott
Perk Boundary
C vi Line
Hydro Lin r
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work Site, tlc
1 ^ o
V *~- Twp 145
l Calaite whore —-—l "3? coro is stored 11*5.7 ?^ i y* ^ . ^L l *0
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May Lake^
Iilll4
\ '.331 IS
32677!j
133122 1V2675 ! i3tS6*
1326*6 .32*
152663 S-M
*i* !S; K*' i^ l;* '^'U..* Ii33li6 '133121 1^32674 1324p
j 143-1
:3;6?i . i26?0 'i32663 ''326:
I3Z6!
KERFS-MCSEE CORPORATION
ELLIOT LAKE PROJECT Location Map Drill Hole 143-2 Township 143 Ontario, Canada
300 i'e e t north ar.d 20 west of the No. 2 i*ocw OA Claim No. S-143217Scale: 2 inches ^ l mile O 5280'
r- r1 ^ l 1 O O tS b L* - A A ^ w -
41J97NEet69 M16A1 JOUBIN 900
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CORE S P B C I M E H S
Core specimens from this hole are available for examination at the resident geologist's office, Ontario Department of Mines and Northern Affairs, Sault Ste. Marie.
Company
Hole no. .
Footage sampled t
Xf: M. f
Rack no. .
File no. . ffAM/.fJL
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DISTRICT OF ALGOMA
SUDBURY MINING DIVISION
i?SCALE:l-lNCH^O'^CHAIN^
PLAN NO M "l 21 5
DEPARTMENT OF MINES
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Proctor Twp.