Departure: 60.00E Reading : N670W Corrected 88*€¦ · · 2017-01-1741N02NE0054 KINCAID24...
72
41N02NE0054 KINCAID24 KINCAID 010 DIAMOND DRILL LOG PROPERTY : Tribag Mining Co. Limited Location : Batchwana Bay, Ontario Latitude : 12.00 S Departure: 60.00E Elevation: Azimuth Hole No. E.B.2 Dip tests Dip 90 0 Depth : 687 Footage : 677 Commenced : September 26, 1963 Finished : Sept. 30, 1963 Reading : N67 0 W Corrected 88* 0.0 Casing 10.0 10.0 Altered tuffaceous volcanics, with admixed argillaceous siltstone material and interlensed argillaceous ailtatone, part of which contains some fragments and fines of volcanics 3/32 inch and smaller in particle size. Well mineralized with pyrite, trace amountso f chalcopyrite and sphalerite. Zone also contains considerable amounts of several sulphides, possibly pyrrhoite and/or pentalandite and lesser amounts of a sulphide resembling violarite. Through sampling awaits arrival of check assays. Minerzliation is of both the disenuninated and spotty types with spots of massive sulphides upto lJ inches in size. Some joining S p lanes are chloritized and/or steatized and a few are molybdenite plated. 247.5 247.5 Diabase gabbro?, dark grey green, fine grained, massive, with light tomedium chalcopyrite, minerzliation as disseminated fine 1/32-1/10 inch spots and some thin 1/32-1/10 inch veinlets,traces of molybdenite, plating on aa some joinint S planes. The interval from 285-335 is estimated to run .75-1.3% Cu. 309.0 309.0 Altered tuffaceous volcanics with admixed argillaceous siltstone, slightly calcareous throughout. Lightly mineralized, chalcopyrite, traces of sphalerite and molybdenite and minor amounts or possible nickel sulphides and/or araenides. 340.0 - Green steatized claystone and some altered volcanics 342.5 - Altered tuff and admixed argillaceous siltstone as at 309. 350.0 - Siltstones argillaceous and with minor amounts of admixed volcanics and trace amounts of sulphides. 391.5 391.5 Fairly pure siltstone. 397.0 - Altered tuffaceous volcanics, with minor admixed argillaceous siltstone, light chalcopyrite minerzliation and in places fairly strong sulphide development possibly N. sulphides. 441.0 441.0 Agglomertic, slightly calcareous, volcanics fragments 1/32-3 inches in size, 1/32-3 inches in size. Patches of epidotization 1/4-1} inches in size. 495.0 495.0 Altered volcanics, mixed tuffaceous and agglomeratic with trace of minor amounts of chalcopyrite, nickel sulphides and/or areenides.
Transcript of Departure: 60.00E Reading : N670W Corrected 88*€¦ · · 2017-01-1741N02NE0054 KINCAID24...
41N02NE0054 KINCAID24 KINCAID010
DIAMOND DRILL LOG
PROPERTY : Tribag Mining Co. Limited
Location : Batchwana Bay, Ontario
Latitude : 12.00 S
Departure: 60.00E
Elevation:
Azimuth
Hole No. E.B.2
Dip tests
Dip 90 0
Depth : 687 Footage : 677
Commenced : September 26, 1963
Finished : Sept. 30, 1963Reading : N67 0W Corrected 88*
0.0 Casing10.0
10.0 Altered tuffaceous volcanics, with admixed argillaceoussiltstone material and interlensed argillaceous ailtatone, part of which contains some fragments and fines of volcanics 3/32 inch and smaller in particle size. Well mineralized with pyrite, trace amountso f chalcopyrite and sphalerite. Zone also contains considerable amounts of several sulphides, possibly pyrrhoite and/or pentalandite and lesser amounts of a sulphide resembling violarite. Through sampling awaits arrival of check assays. Minerzliation is of both the disenuninated and spotty types with spots of massive sulphides upto lJ inches in size. Some joining S planes are chloritized and/or steatized and a few are molybdenite plated. 247.5
247.5 Diabase gabbro?, dark grey green, fine grained, massive, with light tomedium chalcopyrite, minerzliation as disseminated fine 1/32-1/10 inch spots and some thin 1/32-1/10 inch veinlets,traces of molybdenite, plating on aa some joinint S planes. The interval from 285-335 is estimated to run .75-1.3% Cu. 309.0
309.0 Altered tuffaceous volcanics with admixed argillaceous siltstone, slightly calcareous throughout. Lightly mineralized, chalcopyrite, traces of sphalerite and molybdenite and minor amounts or possible nickel sulphides and/or araenides.340.0 - Green steatized claystone and some altered volcanics 342.5 - Altered tuff and admixed argillaceous siltstone as at 309.350.0 - Siltstones argillaceous and with minor amounts of admixed volcanics and trace amounts of sulphides. 391.5
391.5 Fairly pure siltstone.397.0 - Altered tuffaceous volcanics, with minor admixed argillaceous siltstone, light chalcopyrite minerzliation and in places fairly strong sulphide development possibly N. sulphides. 441.0
441.0 Agglomertic, slightly calcareous, volcanics fragments1/32-3 inches in size, 1/32-3 inches in size. Patches ofepidotization 1/4-1} inches in size.495.0
495.0 Altered volcanics, mixed tuffaceous and agglomeratic with trace of minor amounts of chalcopyrite, nickel sulphides and/or areenides.
PROPERTY:
DIAMOND DRILL LO*Tribag fining Co. Li*ll*d
Batchawaa* bay, Ontario
HOLE NUMBER:
DIP TESTS
Departure:
Elevation:
Azimuth:
rz-oos.
O O Depth
Commenced: Sap?*. 26,
Finished:
Footoge
tnnReading Corrected
ASSESSMENT WORK
NOT TO
0.0
IfcOenCO
o -r
UlUJo:
247.3
309.0
391.3
Ul.O
DESC8.PTION THE OFFICE OF THE RESIDENT
GEOLOGIST, ONT. DEPT.
10.0 Ut*r*d
SAULT STE. MARIE
OF MINES
ONT.
ttt/fneoou* T*loanloa. with
eoataliui *c** frsc**nt* nad fin** of volcanic* 5/32la pajrtielo ait*, -all alaoraliaod withof eh*l*9pyrit* aad
aid*raalo aaMKiat* of aevaml solphldoa, pooolbly and/or pvnmlandit* aad l*a**r naouata of a violarit*. Twrough aaapllag aw*it* *rriv*l of eh** Mia*r*li*ation l* of both ta* di***ftin*t*6 aa* a pot apo*a of o*aair* Mlphido up to 1) inch*a la alto. jointing S plan*a ar* ehloritiaod aad/or 9t*atie*4 olybdonit* platod. 247.3
dark gray fir**a t Tin* grain*d t 9*9
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light to aadiua chaloopyrit*. inaraliaatioa aa dia*w*u**wv fla* 1/32-1/10 inch apota tind aon* thin 1/32-1/10 li eh v*lnl traeaa of nolybdanito plating on ao*)* jointing 5 pi Th* interval fron 9^3*333 la aatlwat*d to run .73*1 309.0Alt*r*d ttiffaeaoaa voloaaioa with Mlaixod alightly talesrooua throughout.Lightly min*r*lia.*d, ehaloopyrit*, tr***a of aphaloilto aad aolybdanita aad Minor ABottnto of poaaibl* niekol an! .phid** aad/or araanldaa.3^0.0 - O r* an ataatiaod elayatono *nd *o*j* altarad I'oleaaii 342.3 - Altorad toff aad adnlxod argillaooowi ailtat.oao a* a k 309* 330.0 - ii Ut a t oo* a argillaeooaia aad with oinor aoottiita of admlxa)d Yolovaloa aad t r* o* aoottnt* of avlphid**:, 391.1Kairly pur* tiltatoao.397*0 - *ltar*d taffaeaova V9lo*iaiea v with alaor adiiixod arglllaeooa* alltatoao, light obalcopyrito alaoralli atioa la pl*caa fairly ttrong aulphldo d*volopa)*at poa*lb: y X. aul^Hidas Ul.OXggloaoratlo. allghtly oaloar*oa*t TOla*nla fragaonta 1/32*3 la ait* f 1/32-) inekoa la ala*. Ntohaa of opidotls atloa 1/4*1i imchea la also. 493*0A It ara" voloaaloa. eiaod tuTfaeaoua aad agj;loa*ratli wlta
to minor aaouata of *haloopyrlt* v alekol **lphid*a aid/or
aa!
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No. Hole No.S.B.2
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DESCRIPTION
perhaps are slightly more abundant, also there are traces of molybdenite and sphalerite. 51JJ.O - Shear sone, schistose volcanics, chloritised and with some quarts carbonate. 526.0 - Some tuff bands have e near massive appearance within their boundaries and night be interpreted as diabase gabbro by some. 600.0 - Shear aone, schistosity parallel to the core contain ing chloritlsed volcanics and quartz carbonate. 6H*.0 - Altered volcanics slightly calcareous, aainly tuffaceous as at ^95.0 with minor in situ, shattering and fine veinlet inter fragment quarts carbonate material. 687.0 - End of Hole.
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DIAMOND DRILL LOfPROPERTY:
LOCATION:
Latitude: 14 003
Departure: 62 JO i
Elevation:
Azimuth: 3/A
fining Go* t iaittd
Dip: 90O C^r* 5 |H*
Depth: 116.5
Commenced:
Finiihed:
HOLE NUMBER: Z.3.5
DIP TESTS
Footage Reading Corrected
k, \ 96} -loaded by: 3-3 ^
SAMPU NUMBER
DESCRIPTION
0.0
u.o~ 1-2*. I-spur* Tolea&ic ant w ri
grsnitt U 93-94 i
ow to
Tight sfcntt*r*d? volcanic*, 3 and ?lnk granitic f*l*it* 3-5
14*9 tO ** p*ra*ibillty (dilataaey?) w** too
any ixoxint of ^u*rt* carbonate AT M or is it a coarse clastic unit with a f*w finvr jrainsd I*AIK* 6 lac h* a te l or 2 f**t t)iick r* iadivtingttishnbl* f r s* larger fr3^*nto in Xpidotixation le pronounced in i.--* Toloanic f Ir to constituting th* coa*irtiaj! matrix o* tfc* fr*sa*ntal or
pyroelnstie. Low jgrad* eh*lo3^1*11* andi* ^roiint as x1li*vttin4Ve4 fin* a?* t s nai
winlwta.
^ ,^
^ovNOV 7 196.)
ASSESSWEN
r' O i" RESIDENT' . -^ S
STE. MARIE
wMck oora.
DIAMOND DRILL LOG
PROPERTY :
Location :
Latitude :
Departure:
Elevation:
Azimuth :
Tribag Mining Co. Limited
Batchawana Bay, Ontario
14 DOS
62 OOE
N/A
Hole No. E B 3
Dip : 90 0Core size li"Depth : 116.5Commenced : October 2, 1963Finished : October 4, 1963Logged by : Ross Shields.
0.0 Casing14
14.0 Tight shattered ? volcanics, quartz l-2%. Impure granite, and pink granitic felsite S-5%; volcanic material 93-96%; cementing material seems to be volcanic fines, suggeting porosity permeability (dilatancy) was too low to admit any amount of quartz carbonate if it was available or is it a coarse clastic unit with a few continuous finer grained leases 6 inches to l or 2 feet thick which are indistingushiablefrom larger fragments in core. Epidetization is pronounced in the volcanic fines constituting the cementing matrix of the fragmental or coarse pyroclastic. Low grade chalcopyrite and pyrite mineralization is present as disseminated fine spots and short discontinous veinlets. 116.5 - End of Hole.
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irj.cre r" End Kail. The roc^ nas t highly breccistra a r*:; e -rt r.r- ar.- ccr.?ist.e of 1C** surreuncei a.nc fcr.fTultr fine ."raines, ir r, rrecr. fragments {
c: di c r-:.frr.*r,t; ir. ir cr*nt.e.:: eticotir-^c a'aa f irreruiar inclusion*, cf
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^ *, ** ^ *N ^ * *i ^i,- , r , py 2-3,*, po 1-2,*.21... 5 Siliceous TO.TB, 4.0-50.vnitt ir.trocussc quarts, vi t.- i.0* red acidic inclusions and 5/i chltritltet pstcr.es. Trac^ cpy, l-?* p*,py. Trace M*S? .
Volcfer.ici, dirk ?reer. fine grained t? aphanitic, rfl- a'iveiv frear. ano cassire, 5-7^* epidste -st-rir^ers ajsc r at c r.-s. lea? i-har. l^i quart?, strir.gers. li pT* 222.; Kinerf.li7eo sor.e, 5-6i* py, 5* po, ir. a fin* rrtiriftc rtle cresn, medium c&rbo.iati ree tr.d chltriti* r-c recK. Note ^phaltrit* ir. E 5r.e fracture at 22^.6.
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ry^•. .v*ri.^ i zee "CM, 2-3* po . 1-:-.2.:.; i:: t .T.*--:U~. fr5.rnr.er^ea pae r^^*1 - roct st'e^li".?. ?-ftc frr.d *r?v-. acidic frariserst; le?r i -.K r. Ifi,l"-'-.i3c ir. ^0 springer* , rstc^es anc ir.rlusiorr ( 5-.-..7J-) -a 5-V. -'.•ciujt n^t:— rrJLor? MrEtior. of r*dcis:f--- rrtin-d (a^liteTj rac^.0 -, ,*?5." .. , Gattr*ir r on* frorr 2}^*7 ^o 2): .5..2..'!'." i.rlit*T fir.f rrain*:., pele preer.i sr. ,cro*fr. . Su-rtr^ texture, r*sit^ively naaclve..ii.1.' .''.ir.ersliT f z t ane, as E' 225.0,i-iT.'7 Siliceous ^one: dan rreer., ap^ia^.i^ic, ver}-r.f.-i roci ; 2•-3> v.-.iie quar*-t strinrtrr ZLT.C pf.tcr.ee;I -.r*- ci sse^infcwft': py , DBcostinf ptle preen, dut t*etr: citii&'.ler, fror 2^i,.0 -jr..
l e yells*d.?r; f;r*er.. f: ne trainr 1 faintly f*liat*ic at 5f 0 c. r*.
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Mineral irac ror.i, 2-3^ py ; 1-2^ p*, trace cpy with rcinor l*cal cence/vtratiens . Ttie rocx. is grayish gr**ix elterec ano f rttrrser.ted. hi^r. rt'.cny :nvad*!l by 5-"1 * wr.\tt O'jarti stringers a.nc scr.e xitr. e'nlecce- frfacr.*.-.ia 1 5-2C t k sic rock.
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DIAMOND DRILL LOf"I
PROPERTY: T rib us ttiniag So.LOCATION: ftttehavftitt Bay* 3nt*rio
v. ,.lotitude: JjJ 003 ^*P: 90
Departure: 61 OOF. Depth: ggO,
Elevation t
Azimuth: Finished:
HOLE NUMBER: I.B.4
DIP TESTS
Footage Reading Corrected
Cor* st.* U" ASSESSMENT WORKCommenced: QctOb*r J f 1963
vMPU JMBER DESCRIPTION THE OFFICE OF THE RESIDENT
0.0 Gating
11.0
124.0
t/3
lif i -i•n "
o—enUJo:
H5.4
GEOLOGIST. ONT. DEPT. OF MINES
SAULT STE. MARIE. ONT.
whit* settling, airur*Us*d,in platina, si if h t ly
Volcanics, 2T*y gr**n andfin* grsin*a, frA&tont*! ^•lt*r*d.fairly abundant prrit*, lov to s*dloB er*4o Cu. aspo*5ibly 9o*j* ohsloocit*, stronger ain*rallsatian eecur* b*i w**
chile os13 *nd 93. Jointing Sfairly
Trno* amount a of aolybdonix* plating oxpliB** tract at*ouir.s of *phal*rit*.
pyrrhotit*, povsibly on* or aurora l
79and arn*nid***
asphibolit* in tuff96 -
favoorable oonpoftikion approxioAtin^ that ofalt*r*4
pyrit* 1U.O A l to rod
r*cry *tiito** f^int tuf.f^ecott* bnodini; trac** of
toffao*ou* b*dding *nd
di****ln*
lnt*noix( K) fraceMmtalin4id 4
pyrrhctit* wit!
withailtston* son* a* l*n**s and
die**9innt*d *pot pyrit* throughout •in or tfhJtleoprrit* spivAl*rit* end wolyb^snit*. Fron 153 to 239.) aHo** low to * 7t chalcopyrite air er* li t at with traces of n ph ala ri t** \*AAt 191. A not* b is alt fr*,*?vxit 9 ^phJinitic with oooehoidal frttetur*.Variation in carbonnt* content o*rr** to otttlin* tuff bandi ai indicated by diff*r*nt d*^r*** of *ff*nr**c*MO tador o*
oaldan au*
and
At 217.3 not* scriclt* d*v*lo^d on jointing S 230 - light gr**nish y*llo** ^rfillneoou* with *OM **rioitio ftnd *t*4titt*d S pla 232 - Alt*r*4 Tol9ftnio9 ** at 124t with aoa* pyrit* notite nin*r*liftAtioB aad troc*o of chaloopyrit*. occur a* tpota and it fow nhort diaoontinoota* 315. ij lightly *mlllac*oua Btllt&toa* and aow* pvro tilt a too*, o
f is* cr&iRvd oRtad*tco* with Minor toffac**m* •at*ri!ilv*ryla p*rt, boff oolourod, fino
niok*l
aahibo
oa
sl r Sheet.No. 2. Hole No. B.B.4DESCRIPTION
328.0
372.3
401.0
407.0
tti 5"
UO
™- oS"> Ulo x S v~Ul lven ou ui o uo tH O
H Ul O IZ
415,4
440.0 ^ xo S
- *
J 3
n ui B-o SoH V-Ww J L..jO 3 COOJOw o
328.0Altered volcanics in part tuffaceous with tuff banding and acme intermixed ailtatone and argillaceous siltstone as at 124; son* disseminated 1/4-1/2 inch spot pyrite and pyrrhotite mineralization.331.2 - Stressed and fractured arkosic material t some quarts pseudo phenocrysts, and sub-rounded to sub-angular 1/16-1/8 inch in sis*.Pseudo felsitic, but some of the feldspar matrix is bleached or altered a light cream colour giving a two tone Dink and cream banded groundmass.333 - Altered volcanics, in part tuffaceous and with intermixed siltstone a.nd argillaceous siltstone as at 124. 372.BSpotted siltstone, argillaceous, light groenioh tan, upper contact with interlensed tuffs and siltstones is irregular, rock is calcareous with several bedding bands. Spots are of the same rock type, but darker in colour and seem to be fragments of another siltstone, also calcareous. Spots range in siae from 1/32 to 1/4 inch, with a few silt- atones fragments up to 1/2 inch in major dimension. 401.0Fragmentalised and recemented fatrly pure siltstone, hard tough, very fine grained greyish blue, purer siltstone, parts are only slightly calcareous and only along Jointing S planes. 407.0Spotted siltstone as *t 372.8, but nljo containing larger fragrnents 1/2-3 or 4 inches in diameter *nd very similar in composition to the lost siltstone.Traces of pyrite, chalcopyrite, pyrrhotite and possibly one or two other sulphides. 415.4Siltstone in part argillaceous and interlansed volcanics and with fragments of each occurring in the other. Mineralized with low to medium chalcopyrite, pyrite. pyrrhotite and traces of chalcocite,galena and sphalerite. 440.0Tuffaceous volcanics with ninor siltstone and argillaceous siltstone fragments, lightly mineralised, calcareous in part, minor epidotization, note a few granitic pink felsite fragments.465 - Schistose, tuffaceous volcanics with siltstone and granitic pink felsite fragments, slips well chloritised and also show some nuddy stentiaation. 477 - Tuffaceous volcanics as at 440.0. 488 - Schistose tuffaceous,volcanics with siltstone and granitic pink felsite fragments as at 465.0. 493.8 - Tuffaceous volcanics aa at 440.0 501.0 - Schistose tuffaceous volcanics aa at 465, 542.0 - Note fine granitic fragments or arkosic material in tuffs.543.0 - Tuffaceous volcanics as at 440.0. At 576.6 - Note molybdenite veinlet in granitic pink felsite fragment.^ r .,.
i * "' -' ' * *"" - - . .
DESCRIPTION
601.3 601.3 Arkosic lense or fragment, quarts grains 3/32 inches in
sixe in a pink pseudo aphanitic groundmass feldspathic,upper contact gradational into tuff, lower contactirregular *nd fairly sharp, unminer-*limed.602
602 Tuffaceous volcanics with siltstone and granitic pinkfelsite as at 440, lightly mineralised.613.4
613.4 Spotted siltstone as at 372.3 with irregular arkosic,upper contact, arkosic zone is one to three inches thickgrading into spotted siltstone. Lower contact is likewisefairly sharp, irregular and strongly arkosic over a 1/2inch thickness, also slightly arkosic over a thickness of4 to 5 inches adjacent to the contact.633.0
633.0 Volcanics, tuffaceous calcareous with intermixed lensesand fragments of siltstone and argillaceous siltstoneand fragments of pink granitic felnophure.641.0
641.0 Volcanics, dark to medium bluish grey green, calcareouswith some tuffaceous banding generally fine grained withsome of the bands showing coarser dork rock fragments.Only trace amounts of fine pyrite noted. Minor epidotizationand possibly some amphibole recrystallization.6*9 - End of Hole.
ASSESSMENT WORK
O T
? .tt -". t-
o x , o-- oor o
DIAMOIPROPERTY. Tribag ni&Lng C*. Limited NOV 2 0 1 95LOCATION: !*atCR*waai) Bay, Ontario
Latitude: 11
Departure: 39 00&
Elevation:
Azimuth: S/A
Dip: 90*RESIDENT GSLiLOGISThj
SAULT iiTE. MASiF J
HOLE NUMBER:
DIP TESTS•ri ut 500
tt'
Footage Corrected
Depth: 510Cor* aisoa l a*Commenced: OctOO+r l*, 1963
Finiihed: OctObor 14, 19&3 Logged Sy, &O8* Shield*
SAMPU DUMBER
s z0 u2 9Q w3 s^ U0 I2 Hs sw wa 0g It*~ oH 1U0 xZ H
i
DESCRIPTION
0.0
14.0
39.0
2*4.0lizi ^~
5J6.5D. iJl K
3 S'
D en "
n j3 DJ inu 119.7D
122.0
175.0
il RECEIVED
Caaing14.0Argillao*oua ailtotco*, bright y*llowieh sreoniah t r^uarta oarbonato wita low grado ehaleopyrito 1/10-1•potn and pyrit* and trao** of *phal*rit*, whit* apirounded SOBM Tttwrta, p*rhapa t*hit* f*ld*par, ailtate*loar*oua in part, 'iwarta oarbooat* and ninor vinooeow in a.'*ooiatlon with ninor breaoiation, and itslointinn i- d^anos.39.0Shatter eon*, quart! carbon* t* f:O#.Sow* flhaloopyrit* 1/16-1/4 inch tipota, trac** of apand atolybdanit*.44.0Arglll o*-His siltaton* aa at 14.0.56 - ^tt^rtB enrbonat* velnlet truce o only, of oh a loand pyrit*.56.5Qr**ni*h toff to t sup* fin* banded siltstone. Minorion of of siltfttono with mm* quart! oarbonat* lensi* para 11*1 to oor* in ra** plao*a and tt a alightangl* in others.69^siltatoo* t whUtoa* p*rall*l feaddinjj at ao* t
^*9.4Craaaty pink f*l*optiyro (atreaaed .trkosie granit*?)brecciated with a\a**rou* jointing S plan**. Quartsor pa*odo phenocryst* 1/16-1/6 Inch in *i*o, slight few qoartfl vein let a lA^-1/4 Inch thick aloog aoawS plant*, 000* oontainieg traea* of *olyb4*oit* aa119.7Omrk grey cherty f el ait*, alightly oaloarorjua.122.0Pink anJ gre^n eowpoaito rock t y p*, a toff,porhapointeraUad pink feldspar, although rook ttxturo i* to diaba&lo, notabl* •pidotiaaclon throughout, grai 1/32-3/32, alightly ealoar*nua throughout.175.0Dark bluieh grey groen ch*rty f*lait* t with aoa* pi(or possibly feldspathic apote) alightly oalotreoua light ohaloopyrite ainoraliaatioa and aoaM arao&opy
n, aoett '4 inchta s**i-
m* la•allxAtiaabundant
*
alar i t*
>pyrit*
bracci ata, baadi* 25
t oor*
ilightlyjh*noorypLy o*l oarolntlngtt 91. d.
fith *r*rlUilar
ik chart
n ^CC OS:^uS'nU
• colife•^^
to•OU*K
ly
in parti •it*t fro*
NOV 1 2 1963
2.DESCRIPTION
Hole No.K.B.5
210.5
265.3
341.0
195-205, 205-203 is estimated at l to 1.5* Cu; 208-210.5estimated at .2 to ,4# Cu.210.5Mixed pink granitic felsite and greyish blAck chertyvolcanics, volcanics schistose and chloritiaed in part,zone is epidotiaed throughout, with sone faint bandingparallel or up to 15O to core axis.210.5 - 235 la estimated at .3 to .4# Cu.235 - ?55 la estimated at .7 to .9^ Cu.255 - :65.3 is estimated at .5 - . 8fr Cu.Zone is mineralized with disseminated chalcopyrite, *oaapyrite, perhaps some arsenopyrite and traces of molybdenitegalena and sphalerite.265.3Volcanics very slightly to slightly calcareous throughout,altered, abundant amphibole recrystallization and soaeoepidotization, some faint banding parallel or up to 15to core axis.265.3 - 294 is estimated at .15 - ,25# Cu.294 - 302.5 is estimated at l - 1.4# Cu.302.5 - 320 is estimated at .15 - .25# Cu.320 o 331 is estimated at .9 - 1.3* Cu.331. - 341 is estimated at .15 - .3* Cu.Zone is mineralized with disseminated and short discontinuourveinlet chalcopyrite, some pyrite, perhaps some arsenopyriteand traces of molybdenite galena and sphalerite.j-iore strongly mineralized zones from 294 to 302.5 and 320to 331 have considerable quartz carbonate content.341.0Volcanics, very slightly to slightly calcareous throughout,grey bluish green, mostly fine grained, but sone coarsergrained zones (amphibole recrystallization) giving Q texturesimilar to diab^r/ic, containing some faint tuffaceous orpseudo-tuff nceous banding, ninor scattered zones ofepidotization and scattered zones of trace to minor amountsof disseminated pyrrhotite for a few inches, some with trace;of disseminated chalcopyrite; fairly aoundnnt Jointing Splanes with fine quarts and some quartz carbonate filamentstringers, also a few thicker quartz veinlots 1/4 - 2 or 3inches thick.An nt437, quartz material 6 inches thick with abundantepidote and chlorite and volcanic fragments.455.5 - -iuarta veinlet 1/2 inch wide and 3 foot longparallel to the core.From 432 - y54, note curved Joint with 1/16 inch of quartzcarbonnte parallel to the core.At 492, quartz vein 3 inches thick, with a few volcanicfragments nnd abundant epidote, containing raassivo pyrite.510 - End of Hole. A
NO"1" TO
RECE VED NOV i 2 1963 GEOLOGIST.
DIAMOND DRILL LOG
PROPERTY
LOCATION
LATITUDE
DEPARTURE
ELEVATION
AZIMUTH
Tribag Mining Co. Ltd. HOLE NUMBER: EB-6
Batcbawana Bay, ONT DIP TESTS: Pajari
11-00 S Dip: 90 0 Footage Reading Corrected
60-00 E Depth: 485.0' 485.0 1 N39 0 W -88 0
95.6' above El Commenced: Oct.18, 1963
Finished : Oct.20, 196gOgg^d by : Matthew Blecha
0.0
10.0
63.8
77.6
100.0
118.6
129.0
298.0
Casing10.0Gabbro, dark grey, ed, grained, massive.13.0 silicified, with 20% irregular quartz'str.
slightly brecciated. 15.0 as at 10.056.8 Med. chlor'd, fractured at 80-90 0 to em. 58.0 F. gr'd, si. epidotized, tr. epy. 62.0 Shear zone, H. Chlorite, H. Shear at 55-60 0 to
em, med. carb'd,Felsite, pale pink, very hard, siliceous, aphanitic, el. fractured, with 101 irregular, inclusions of fel'd(45 0 to en) el. chlor'd vole. rock. Upper contact sheared, lower contact gradational, Tr. epy, py and Ma8 2 (?) Gabbro(?), altered, ir.ed. epidote, v.g.dis'd py, very hard, silicified, less than 5!*; carb, stringers. 86.2 Greenish, si. foliated at 50" to cn.N siliceous, with brown feldspathic (?) alteration and few irregular faint inclusions of feldspathic mateiral.94.7 Grey, f. gr'd, massive less than 11 epidote stringers, hard.Fault zone, med. to high chlorite, 151 carbonate, fractured and sheared at 80-90 0 to en. Core is 101 broken up. Rest is gabbro.116.8 Brecciated, h. all sil., .ned. carb'd, Q.5% epy, Q.5% py, tr. Mo 2Min'd zone, 101 f.diss'd py, traces Ma8 2 in a pale grey, massive, fine gr'd rock, med, carb'd (probably altered gabbro).Gabbro, dark grey, f. med. gr'd, massive, minor local epidotization and carbonatization, Pink qutz-carb. stringers 21.187.0 Altered gabbro, med. epidote, low earth, med. sil anddar} brown soft alterations. Irregularly foliated at 60-70 0 to en.188.9 Gabbro is at 77.6. Epidote 51, qtz. str. 2-31, locally silicified and faintly foliated at 70 0 to en. 15-201 of very fine gr'd phases, Note }" qtz. str. with Mo8 a at 251.0291.0 High epidotization and brownish, feldspathis ( ?) alteration, faintly and irregularly foliated, slightly brecciated.Felsite, Pale reddish-brown, al. fractured, aphanitic, h. silicified. 2-31 epidote, stringers, few miner. q 1 s s tringers, two shot 0.8 and 1.0' inclusions of foliated silecious dark grey, ( ?????????????????????) material at 311.0 and 312.4 Becomes med. fract'd from 322.0 on.
OIAMOND DRILL LOGj93*1*1 CO. ITP.
E*TCfU*4tA 1AY, WT* fit:
11*60 a o*40-OO t D.pth:
95*4* *OOTO 10*1 Comm.rx.d- Got* l*f
Foatog*
HOLE NUMKfl:
CHf TESTS
7* la Vi
by i
at 00^0* W *u i tr. trr. '
•Hlorit*, E. tb0*r at 55-40* to aa* . oerb'o.
0.010.0
10.0 Oobbro. dark froyt **4* t*** t Moaiva*13*0 ftilloiria*. viDi to* lr*of. *to tt r,IJ.O Aa 4t 10.0', 54.ft n*d. ohlorM
S .O 7. tf'4, tl. .0 Sbotr Ko*4 t
63.4 f3,4 /*ltitO| aala piak, vary
TO lo* rook. Dp^rr oof**ot ^hoaro4 y lo*/*/ oont&at 77.4 t . -
77.4 0*btnro (T), alters, ued. •rlaot*i v*{* ^ift'O ry^ Tory hard t flodf loo* tikan 9^ carfe, ttrintorf* ;
.7 Or*jr* f. cr*(J t c*** lv*, l*** 100JO
100.O faalt ifWfJI^* i* feUA c^iorii** MT+* tt SO**T^ te 9f(. Oftr* t t lo* vi^* 116. ft 6r*iKi^r4 f li. •il. ( M4
li
w. ft*** tt e
•triiii4rv 9 h* ffi; an*
IP.lift.4 Mln'a lotto, lOi f. 4itt*d r y. traooo NoS* la B fclo'UNy*
flAO f?*4 rook 9 oorf. oaroU (fvooably altaroas foobt*}.
9 4af* groy* f* oortottBtltatiom. O 41torod tateo^t vo4. ooloota*
144,9 teooro tt at TT.4* x^oto p. ^n atr •ifloJ *oyi faiiitl) folia tod tt ?0^ to om, 15
l* .*. Itr. vitta HoGf at 251*0.
vU*. 2-
ii '
looal ifi4o4ic*iin;-
ir'*
faintly 6** irrost^larly foll~t*d, i t+4.faltltay Pala roMl*o-orovnt tl. fraotvro^^8?.
jaj.9
h*
at J1UO . frmot'U.
SSIlif^^
S.P..V -;. 323.9
327.9
- 2 -
485.0
Min'd zone, 1.5l fine, dias'd cpy in an irregularfoliated (80-90 0 ??????) contact zone between felsiteand the lower volcanics. The zone contains manyirregular angular fragments of felsite and volcanics,is med. silicified, low ephifi'd.(Gabbro) Volcanics ?? Very fine gr'd, dark greenishgrey, cut by 5% very fine epidote stringers, tracecpy in first 5 fejt.375.0 Epidote stringers and patches increases toID-15%. Rock is very fine gr'd to aphanitic, veryhard, generally massive, with minor local slightlyfoliated sections, etc.475.0 Minor cpy. tr. po in ah. epidotized phase ofthe volcanics.479.7 as at 375.0End of Hole
•^^F'?"^T;; -.T" '^g^^^;-:'r-
9&35-1','*-'. . ' ."-j-,,'t- - ~. ; - -J1S; J -v,,..,'- ^.^r,-, — -, e? . .———- ,—
DE ; ION
. i:: 1 ;. ::.-.^*JV i,;;* ilr.:- -.irs'd ir-;- ir, t r. -I'-c^a -'s^-v-" ^sr.cr.c^ ;-.r-:.^'. ::ro i":', :acv. f-il- it.?
or felr.lt,e and vyicanic* f is fcwl. silicified,* ' "^ " '
v ^: f;- \t-j r ir r rrJY -,x?-c-r:.c r-, t 5.0 ri-*vi-;c- ?t.-Ir. r-: ir vj/;; ;iv.r ^ t.-Lvv, vith idr^?r
: ir^.-ila^ *
, xr* o
.prrxr-i*i.c v v
•y lo ri r rt " fcp^
t? 10-15^. ^, c rctrsiiy ?e2tisn3j etc*
Of t-44
r^ijoO -.^ * ITOLT
ftSCEIVEOKOV 12 1353
JK;i -, .J'-V: mi-- DIAMOND DRILL LOO
m:- i*-*.
; C oapnny 6 Liraited
Batchavana Day, Ontario
13 00-j D|P' 900
6000K
HOIE NUMBER, BB-7
DIP TESTS
Rtadlng Corr*d*d
623.4
1963
Fini\h*d: logged by:
O.C'
7,0'
oj,r
r i
O
IT
7.0*JU.iorallzeJ Zone. Chalcopyrite 1.^, pyrrhotitepyrite tr,' ^0*2* qta-carb, 5,*e Me-iiua carbonatization,lov-uo'Uun chloritization; low-radium fragmentation ofa ;;:ibbroic ( fi hoot. Kinu grained cvci-iic frntjnonts5/S (t-i" avft" aieeK ^Irut fuv ffot ero ru.ity and
29*0 Gobbro, m*'J. ^Miinc^i, nsis^ivr, Trash, tracoa ofchalcopyrite an-i pyrrhotite^
34.0 Minoraliae-i aone; Caalcopyrita Ijt, pyrite 13 pyrrhotite, U&, J^o3 2 truce, italic cwi bonatization, m* i chloritization. Iqw-med. fra^.'.eatatlon of a gabbro ic host. WtB-carb 3-7^ 064nO Aa abovo, but chalcopyrite iricre&iea to 3-ii fll.5 fabbro, med, ^raiued p relntivoly 'laeairo, aaphi bolo rich (66)). minar opotty Lrown, soft alteration,
(micaceous?), low epidotization,85.0 Gabbro (?). very fina i^rcine/i, Jiaaaiv*, relatlraly freah. Minor epidote ^trinjara, (l)*) . 9XD.6 Hineralisaj aoae. Chalcopyrite 1^, pyrrhotite 2-351*, pyrite, 1^. HoS^ trace. Medium carbouatiBatiob iuuJiun tjijotty chlorittxation, qta-cttrb 5)^. I*ow frag- xontution of giibbroic host, 100.0 i f above, but at^rqnxef fragmentation, aoidia,
o
rt ;,iianj ,,104.0 Mineralized rone, ChA^copyritu 3)*, aosoc'dwith qti-carbonate strikers and patches, ( lojlj.Acidic frosu^nts apr e nuaeroua, (20jt), aeiiiua frafi-mentatlon*116.2 Ga bro, fine-neUiuu grained, relatively auaa.lifresh, pyrite truce,117.4 Mineral i aed aone. Chalcopyrite 6ji, pyrrhotite43*, low carbon&tiaation, r.ediun silicification, aediu ifr gmentation.120.0 Hineralixed aone. Chalcopyrite 1.5!it pyrrhotitJ-4J&J mediujn chloriti/atioft, low-nediun carbonatiaati m,me'liua frngnentation of a gtibbroiov?J hoat^124.J Mineralised mono. Chalcopyrite 1.55*, pyrrhoti1-2 ^j alteration as abovo but increase in acidicment* to 50 ?k. The fragments ari pale brownish fciw, v —some porphyritic,(qta phenocryjts). range in sice frx* ij^ - 2".
DC O 3:H 2bJSU)a) LJ
ED " 0V 12 1983
sss^fi"*- ! ' ' "SS'feV:'.-:.^.-
DESCRIPTION
LI S. 5 Kinaralire:; ions, Alteration as abov*'| py: ^ --it 2-3*, tract- chn1cr?T*-f. Kr'V-.:- :"r-;.:-:-.r.-,i^n 'r.ul
* *
r,:.i:n*.r
16.3 Cicbbrc, fine r;r^i^*-* csssivs. cinor brownish n:ict.ct-rur alteration, (itz-ca-fc: 1-2;*, Irsce pyrite elong *-r-ni-'- Lov;er contact foliated at 3CO c.n.
3.C Felsophyra. Fa l* brovr.isn prey, hichl"- silic-ous, slir^r.tlj- fr^cturei, 10? qta pseudophenocryst? netr end. Kele-iveiy shirrp upper ccntact ut tCw' c.c.
f,.3 Minertlitpd tone-, ro: 3-5^, pyi 1-2.1:, tre.:e chalcopyrite, .with local concentrations. M*di.u- pitchv chloritization. lex carbonatization, asdius sericitization. Co.ttcir.s l Co* highly Bericitizacd, pale brown, anr,uia: fins -.reined frs?- renta in e Tiae ^.r^inad, chloritic tianrix*
;^ fe 0 !c: . i-i !.w a lV- D S
,i;o ^. U C o j
i; I t jl- w
i J Z li:.*-
*w
i
15^.^ AS ftcva t but increaas of cnalcoovri'tc to , f,*156.7 As at U5.316^.5 Highly altered zone; .hi{*h sericite, 5cft, talcyellowish fr?y rod:, becoming h^rc--' (eiiicocus)'froz 16^.: -r..\?robftbly an altered acidic rock).H-c.r Kir.-rs!ii*d sone as at 1/o/J; rel. lov tit era tier.,
r-r-rpV.Titic, ccd. carbor.ttinerl dyk-lt*v , S.^sro* 1^-er or.-Itcz f.t Cf 0 c.n.1{?,D uabirc., f ine coined, fresh, Tasnire. becor.inr rri v^feltF.r*d with t rift brc i?*h -.5 r- r"c--.:r C5 ' ;-.i :r .1 ". l:.-. ",
;-.hi,r .ti:,l"!.:, r^ifite, pale bro'k'nich?.-.rrp lower contact at 1C0 c.r.'.'l":.? ?',inertii2ed rona. highly sltere:i, re^ju::. f rc,-.r..ur.t od-, '.7,ediuc Cbrbonatired, ratdiuc chloritett-d. Tr, cr.i.lco^;.-ri\.e,
177.5 Highly altered tone; high sericite, core partly di- sinta^ret-d. Fragmentetion partly obscured tv aiterati-jr.. 1^1.2 Hinsraliied r.cr.e, ae at 1^5.3. Po:3-5Ji, py: 3-5 , traces of chalcopyrite and aolyLdenite.. hirrh patcny ch.c- rltiration, nediut: carbonatitation, hig:h frapsier.tction. 7.':t ?7r.e contains 5-75* ri.iu cr^insc f lericiticed, and sili-.,cificd acidic frtrssnts U-3*). Cu*w by t 0.5* groen cykel^t'^ s at 166. 2\ t a t 207.3. .219. ' ' t A cidic frfcEtt-ntr increase to ?r^,({-3 ir ); fine grainec chloritic natrir, Trace sulphides. Keoiu^ fragii-ntation,low clierKtior, spotty epiactiration.
22':.;. j.-eonish porphyritic dyke, as at 2C7.3, contacts cbscura. 227.5 Hinoraiirad rone, fo.py 1-2^, trace chalcopyrite; osd-..:r.frc^raftntation, c-diur aericitisation and carbonjtisfcticn. .l i.l c c^^ca, sericitized fragments (t-l")-5Si* Fine prair.ei, chloritic natric FOK snort (.',-5"j foliated, fine gr*:aed dark siliceous phases. Two 1-2" ctr strikers. Short (lass. then one fott) grtaa porphyritic drkeleta tt 2i,3', 25-^', 262 f , ar.-J 261**. Qtr-carboru? fc *t 2-^...:- n4.^ :.:.wiferj-.*-bi -or.e, ss aoort.-;l*. Aitcraticn as above, vitj-car^: 5'-.299.C Mineralized aonc, chalcopyrit* 3?*, qtt-ctrb: 2:Di.Acidic frigsants l2C^) in a finr irrtlneJ rrreen. chloritic
tc
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No. Hoi* No. -
DESCRIPTION
481.2.-^_.-. Cpy incraas^o to 3)t t P7 3#. taoco sphalerite. Rock ia Icds siliceous, cedlua chloritixed, tcodiun oericitize-i, carbooatited, end aediuua 'fri-gaentod. Pele aericitised silicified frngaents ( iioe then i") lc-153*. /*^^*3 As above, but, only trace cpy, po and py l- 500.0
500,0 Zono of Fragmentation and Alt^rntion. Greyish graej? siliceou;^^.L, M nrs^4.^4 n ,. ^** i-..ie'i ^-.*j*- --i - —.-- -j-i- --j ————
life,* 1
rock conoiating of lo-15^ acidic, palo greoa, pink, and grey, ahanitic fraftnants (i"-5 rt ) in a fino p.rainod nrMftn. ailiccou.-apanc raftnans - n a no p.raino nrMftn. aiccslightly Bdrloitized, -aatrlx. Kofiiuw patchy chloritization,low-aod. epidotization. Qtxi 2-3/*. no carbonate. Tree opyrite find chalcopyrito, an aolybacajta.548. 5 P*lnit9 (?J pele pinkish gray, highly siliceous,aphanitic r ;ck. Sharp contacts at O c. a. Medium fractured,with chlorite along fracture plnnao.552.5 Aa at 5oo*9, with few slightly c&rbonatistd ioao*.Note: thin sane (from 500* on) in part rosetablts therhyolitio agglomarfttt described at J76.5, but differs fronit by scalier quantity of quart*, ami by ito aotr a* w*llbrecciated appearance. - s-' 'invv^d.U
Volcanics (?) Very fine trained, dark greon, highly aili- co )us rock; low chlorite, minor goft brown! oh olcacoooa .alteratioh. Faintly f iliatad at 60O c.n. ,623.fl r - -
623.3 Sad of hole.
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.-. ( --*tj.rf.ir, (7) V.'hitish ^rej* e aphanitic, r.ediurD f"actured, v.'. 1::: IC'.w irregular inclusions of pele Rrex'ich creen cr^crlt-ic a&teri&i. D istftsiinjated pvrite iji.'T."f, -— s J m s
WRuCi Kf /i^r-- " - --—— .V- ,.,r,; ~ 3ag S,' E . lcj-0 ?y ;Sj c ?y tr^^
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and fr^^entcd. ?y ,*-5^ r ~ "r^^entcd. ?y ,*-5^ r.-^re, vit-i Ij'.-^l epncentrat ic^~frc.t 195.""- l??. 9. r- r.lc. ; - cr.loritiaa-
.-, rrc^usrir f dieted, j^rt, dcrk:l-.-.'i^--re:- rcci:, trnc* pyrite; lcw~r contcct sutrp r i i.0 v :C". .o Kir.earfcliren' tone s? a r I SS.3. ?y '5-7 J*, po I-2x, •^r?.cf cpy, i*'t,*-crrb. 5-5x. r 15. ? .V-in-raliswd Lon*. Cr-v 3^ pj- l-2?t, in a rsediua:"r^.T.-.-r.t.-c, c,o-f, crfcri^onatised, cnicritised end aeri-ritl*-, .1 — . ^f- ^ . ...'- *'•'
. --.-r.: ^r ?ili cifi cation find f prrentctisr.. f^.lf jrr^er^ :.tr .:, r li^r.: lv Tr prrentei roci:7 beconiar d.irk sre^fh i-c*"- -t 220', a r t t 109.5'. -6y, cpy ^, qt*-r*rb* 0*5^-
V-: 'J-ei. rv 3.""i cIV*-; "J" ! r03 * nd -^Ja^ted.^ricit^atianraAd P^U"ftfCtChy ?^tisa^^* ^----, paia-wAi-liar. cr^"?"-^"^ 10^?^ indiB^t,^c1?^: s::s;^;;'2:^f^.0ter-tu colcnir or ^r;/"^^"^ SUS^KJJ Ss^SSS-it JSoic" s ^r Kin-r M 7 ^ r^-, ,. ,. .. r , ^ '... - 1 :vi'--r" c 6--ve, rut decr*ae.."oi I
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DIAMOND DRILL LOGTribe g Mining Co. Ltd.,
Batchavdia 8*y, Ontario
33.? O 3
5900 S -
Dip, 90C
.p 708.0* D**pqalj\g from 500*7*
Commenced. Jlonr. 22, 19
Flnkhed. lor. 24, 1963
Footoge
500.0 3 160 H
by, Bitch*',VMHI DI* C 1 1 f T ION
.
Hot*i Oa re-measuring of the depth of XS- D.D.H. SB-3 vat found to b* at 507.
at 500.7 V *" bad b**a reported ic log. Ho oor* val lost*
8 th* botto* of C', rather than the first part of th*
- -
537,0 Highly s*rioiUt*i Zou*. Soft, y*Uoviah ^re*a, highlv altered rock, cut by 10JI qts ttriiigerB. Flas grained ""Aadj" textur*.
pyrita. Qta Btrin/jeru abutly ori*at*d at tha rock a locally bande-i appdaracc*.
ct-j highly chlorititod, slightly br*coiat*J zoc.es vith 255tqta, ^i j -5* py froa 616.0-517.0, sad A^o 513.8 - 519 J.
••C^^'l Highly siTicitii*i Zont), a s abcTa, tat roclc becosss d-i ^a U M^h chloritii&tion. Qli 1C*-1!^, py i.'-; Z.
'J.-^,. : ?ajlt High chlori tiiation, acd s*r: cit ;4o.*.-ica. .sh*trorl at
, and rock la lass itsoft, ard partly diTiatttgi . w, s^dr.5J.'.C i s s lave, but ohloritiiati :r, due:9! ;c'irad, c/ut still highly sarici Lijed, a^.3 T.. rvfjt.5 Highly suricitited, parti;/ disitte ,;r-'.t*d rock. 3trongshu'-.rin^ ut
W '
D Feiiit^-rihycHte? Ghloritizitiva acd laricitiiation gradually decreases, and the rock becones highly liLicecus, greeaiah y*Hc**, with pale reddish phase*, iphanitic, and m^ilua fractured. Kinor short eectioas of Baricite alteration, (as at 507.0), vith associated traces of pyrit*. Kioor local baodirxg at 50^0,a.- Ifote highly lericitisaed fracture at 80oo.a. at 566.5-567.0'. Bole fine grained, grey dykelet, parallel tp cor* from 569.8 to 571.0', with p&rtly broken up coro. Sot* i* opy •tr.(500o.B.) at 571.0 Falsite-Rhyolit*? W*ll btsdad at ^O03.c. Th* baads are 1-10 M thick, fairly regular, aad rajt-j in colour from pal* gr**tt to yello-rf and pink. The rock l* siliceous, hard, with minor, eofi sericitised phase*. Minor fraotaring. la flake* the rock appear brecciated! with angular fragments of of r*latlr*ly fresh and stricitiza*l rock (t*-l') 3*pir;t*.i by hair-thin qta *tring*r*. TcUl qtii 2-jJ.
Felsite-Rhyollte, as aboT*, but Still landed, but includes 609.0
o pinkish colour oaasiT* sections*
*ryk
oisgly
5U.6
O
'it*''
^m^'f;NO; : 'i
DES^SH'TIONHol.No.li4
''"V-fcK-",.-l V.-isV ' '
U.D.,9
627.2
j J. j
677.9
7CO.O
702,0'
609..0 Br*2ciat*d Z ne- 501 yelloqi^h aad piaklsh angular subrvjaded fragaents (l-f*0 as) est^iifri in a qti aatrlx. Uppercontact sharp aad Irregular, lc-wer contact "sharp at 55oo.a.610.9
Felsite^Rhyolite. Val* r-i"W*h fcrcvr. , aphanitic, highly siliceous,massive, with aicor well fcarJvd •ectlon (70uc.a.) Minorfracturing, ainor short laricitiiej zone. Hlnor qta *tricg*raparallal to tanding,627,2Altered Zee*, ttnt 10" highly brecciated with 5C^ pink *ub-rouaied, aoLdic, fr^sh fragnerits (ij -i*) in a grey, siliceousmatrix. Froe 623,0 on the rock bccoaAi highly fiericitixed,and chloritiaed, very soft, and partly di*iotagruted. Shearing;at 60-900c',iu partly obicu;*i by altcretion. (faultt) TSxe *oae.includts ^ealtively aataiTe, p ink, fresh section of felelte-rhyolite froa 628.2-^28o6 aad froa 6J0.5-601.7
Pelsit*-Rhyolite. Ai at 6lo,9. FVor. 6^2.4 the oor* ia badly broken up.
Lost core.Fei ntite -Rhyolite. RelatiTely fra -h, tut highly fractured,
with high *ericiti:atior. of f.-acvure ;.lane4. 1J py, Qta 5*. 664.J
Volcaiiics (7). Dark grey, fine grainal relatiToly fresh, tod DU i si* e. Locally asjjhibolitizc-i.. Minor -epldtftl silica, 1-2J py. 677 0 9RhycliU (?) Dark re-i-iJ h gre*n r hl-hly siliceous, cherty rock, comistic^ of indistinct dark r'.vidin:. fra^co&ta a.vl fatche^ Lti- a dark green siliceous raatriXo Locally well barded tt 70^80oo.n. Dark reddish green jt.asoi dilerttrvatit^ with fcrcea lection. - Qta2-33i* 700.0Siliceous zone, iiark green, i*ry hard, fins grained rock, aedia* fragTwnted, nediua patchy epi Jotitation. Qta 1CJ. py, 2-JJl. 708^0
of Hoi*. . .
'^) ,
K0:
DIAMOND DRILL LOG
- ' : sy, Or.t riv-~\ "*, ~
Dipi -' *"
HCX.E NUMBBb
D* TKTS
Footag*
FinUh.di *v. f, l C, T, j K. Placha
DISC ION
C ne i-.r19.0CVi'bro. •Fiuc-r.-ciiura r;rain2d, cvor. t xt-ure, Irsrk greenh^rd, r.ncclv*. ?0-3C"- felspar, in p-.rt ?tiin-ci--rad.P? c!; is cot by l!* hair-thin ^-:a~t^ strir^-.-rs at randonA.i^lea. I-'.inor 3tr*?c.ks of ej.-'H^t?. Th(? -one -v.ntalr.3foy r.nnor (3-^") ror.es of r::-?dir, - "i Melf ic?t ion, epi-
r-.*:ion, with nssociatcd tr^c^s r;f -:v-ite.ft ^ * i ra* ..- ^ - ,. ^ . j . ^. .i j^.. T****
vithln*~ * - o ' ,*i -*^ i '" *", ^ " T* f^ U "^ ^ ^ P* *^*i'f'-^'^ i^* r *^ \ *"o *^5or -- v J 1 i,.-'- -. i -- * -^^ J j i ^ ....i. i p j r a ..e ^ /*, rt !,.7 C^U-ro, 3; at.19.0', -F.ssiv. ?cn,io e-p i'-i o*. 1,781 i on and silicification hccve more (?C-'4 CSj, ar.-j the rod: 1- cut by 3 fov; (
silicified
of nodtuir
c;rbop.?t*? r t r.l rrt **(^L ^(*T-4 ™ ^ •l *- '
^C.C 'o'i-.:T -r.l^rltize !
91.0'dabir-ro, aa at 19.c', 1^3-^ '"-abbr^, ?.n ab f ve,
l* j w hi t o
'.'r: cture.1,
.ne of'fcldgpaj
: ter -,- d -'i-:- -pl-' J-ei, s-ili-lfiod, y cred
'v * i * " " /*~ i; .'i:. :"* ^ '/ec. ' . * : r^ 0;n^nt-it-: jr., tr-:.L'i py.
r.-r f.pi:'iti:'.*d civl -jiUcifiod phases. Minor re E t v. l r. i 03 cf feldspar. Qt^-carb lcac'than 1^.-'159.3 Altered jnbbro. an at 140.o Truce ^ itl vu. 152.C Cfnbbro, aa at 19.0; red follrpAr increases to 2 Ittt.Z G sbbrora as abovo, bjt cpre partly broken up. Carbonate filled fracture parallel t^ cors. 1S5.C Gabbro-, aa abovo; a i nor short 20.103 of low *pi- 'Jctirction, and rad felJnpur ctnin^.r.j. v?itii trccsa of i pyrl*s. Cp o partly broken up fr^s led'-100*.^•\^^*B l^i. l * * ••.-' -- ' "-' '-Alt fire J
2s3.C C^bbro aa above, but lew epidotization, 405* ^ red felspar. c:rn.-r silicific;-ticr:x Trace py. Cort'c^^- trokr-. up frc/r 257.0-;::?.',, :,ni fror 25^.5-*59.3 V/sS •?d ' . .- ; '.-- r"S'
very
69'
**^ r""*CvJ!
^5p|K
fet^f
No. ro-9|
DESCRIPTION
I *S'
? : 'w-^- *T'-~ ' -
-?/''-'*: : :
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5. -ntche
fractnre lant*-. "r 1frort
L '
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r frsctrrl'!-. 2-3# py along ti?~. vore belly broken
r n r-51 v e,p-.' .^ -, -; '-; r--.
:.v S r-r*r•ill ",rra 4 than. and minorthin li* w run j
stringers. Occiui^nAl r:r. jr f-*;r.t bandinr nt" 700 c.n.Troc3 pyrite aloru; fractures. ~290.G to** cor*294.0 Felstle-rhyolin* (?) as P", 27o.,4 Core badly brok-*n--up froa 298.1 - 299.0,315.0 Felsite-rhyolite (?), an ?,bove. but highly fractured.Fracturns filled wit!: CO-ITS--/ r.-rvstalline quartzcarbon?, t". (15/0 f316,0 FelMto- rhv.)i:t*J-tirrKi-ru Q t z l-;..*-.321.2 i'-i.-.hly frr;:":r-3 ;...- *--ji J.;t Lzvd fei-- ite-rhyolite.322.; rel3Jt2-rh;-o:it.-' ( li t f r^sh, but '-.till slightlyfractury-i. Mi r/or r:-*r' citl 7 jti i.- nlon^ frc-turen with tracesof pyrite.325J* Qtz vein, v:hit*, n.a^ilve, r.nrr*n quartz, sharp/ " "'
•:ive, as before, low api-
?26,C 'r eioiti -rr.yol It-s, a? before. r.3Esivi*, fresh, ixcept. for nlr.or rr.-sdi'im-h? r^hly o^rici-i r*a pntch-;c, Feint banding
n.) Icc2lly jvl'Jcnt , sit?. 3tr!n^^r3 !-C#, no carbonate, iirs^'ninatoii jpyrl*^ ~ ;.-:o." i - t v:rl with c; er'd patches.
3i*4.5 Qu:irt7 Veir.. whit?, ^-.-sive riur.rt^, Contains a 2" red f**ldp3athic irclusi^n i.". centre. Trace pyrite aldng fracture^. Upjrr contact loot, lower contact irregular, frr.ctur*d, with 7.ir.-..- f*ldcj,atfiie inclusions. 3/^7.4 Felcitc-rhyolite (?), * - before, qtz str.ingers 5^* traca pyrite alor.,; fractures.352.0 Wuartr, vein. ^,s3ivc, white, barren quartz. Sharp- ircegulcr contacts.354.0 Felsite-rhyclite (?), as before, nodiua fractured, patchy sericitization .2-3.** Qta stringers and veinlete \- 51** Trace disseminated pyrite associated with serlci-
• } *O t-lzod patches. Trace dork Krey metallic nincral along fractures (molybdenite?). Noto'trace sphalerite along
- fractures at-377*5 .- 377.C Felsite-rhyolite (?) as above. Fracturing increase.' -
. to highj core badly broKen up from 372-373*, and from 3?3-3o6 . Mediua sericitization oAdng fractures. Jisaoninated pyrite 15i. .38^.5 Felsite-rhyolite i?), slightly .fractured,. 1-2* qtz stringers, 'minor sericitization, along alip plants, : 4 trace pyrite, Faint banding at flOd c.n.. r-^L^A^l::
416.0 Altered zone, pale yellowish gree*n, tifed, minor quartz strin.-.orfl, high f*; 418.0 Feloite-rhyolite C?) as before, ninor sericltited patches.
l-*•t
420.4 Quarts vain, white Rasclve, barren 421.1 Felslte-rh-'olite '"* " J-- " . 426.0
^i;-,:" "".- '" w;.^;;."*"*
No.' - :; ' " •••- HcJ. No.-KB-9DESCRIPTION
. c FelDitc-rhyolite
m35^
452.0
Core baldly broken u: b vfore, but highly fractured. frr-f*-rent3 of highly chloritlzed
dark ^rev rock f^ur.d anon~ t i;- broken felsitic core. .. , 431.3 Felsit*-r:-.y--lire, slightly fractured, 3-5* qta stri ngers. Note chloritic*! b-lip planr at 70 c.n.t at 437.5 443.0 Sheared nr.-l altered zone. Irregular high shearing ftt .45-700c.n., high chloriti?ation, silicification of a greenish black rock./,45-0 Feloito-rhyolite (?) as before, ulijjhtly fractured. Qtz-cerb stringer . Iec3 than 1^,Note: Tho sericitize.t phases of the above felsitic rack resemble tha hrLjhiv dericitir-.ed rock encountered at the bottom of D.D.K. i3~8. 452.0 . 'Gabbro - volctnico l?J dark green, fine grained, hard. slightly brecciated reck with 5-lW indistinct felaltic. inclusions lavg* ;5ir.e ln j," ^e-iium silicified^"'sTlgh'tly' chlcritised. Trace cpy. . 455.0 K'r.ezalized ;one 2-3^ very finely diaoeainated cpy in a fine grained volcanic (?) rock as described at 452.0*. 457.0 Gabbro* Abrupt increase in grain size to fine-xediua. Low fracturing, r!jnor petchy epidotization, i" calcite stringer at lower contact.
Volcanics (?) vc-ry fi:; f* grained, dark green rock,- ;r brown micaceous alteration,r-., ( flow structure?)ir fliinro, trace, cpy,. leas.. . .
hard; nir.or ^pidotirr.tion,...
Trace rjolybdenito rilcr.;: fr.v, v'.ban V1* c arbonate,C f-.l± . O G abbro ( ? l f i i : :: - :r.c i : . '.;ncpidotiraticn. r.r.tr kc3 4 ; --r.:parallel to coro f/^.r ^''--j.^ .'466,0 Volcanics, fine .;r.-.ir.*^..minor brocciation in fl'-^t I?pale sr*y foldep.'tide f^:-^.--T.ts (5-20fracture with t~;-ce cpy at t?;,O Notefrcc r.uros with tr-.co rr.olyc i^./ito bnf^^3*5 ^reccictfjH :'". rl alccrvd CTHO.
minor ong a fracture
as at 459.2contains 5*
Carbonate-filledor hair-thin ^77-^79*,
30^ indistinct acidic
t. i r. e d"races
iarkinches
, rr.;-, i s i v e 'of cpy a
.^reea, as Rock c
fra-:t".'-'?-J fragT.-r.ta in R fine -rained, ailiceouo Short, dirtir.ctly foliated zonrs fros 4*5.5-? 4S6.0.
finely di 33*^1 nr. ted Mineralized ^-)ne.
Traco cpy.pyrite in a l" qta stringer at
ir, a' ',*3.5; 1-v* p , Core partlyJ, 9. 4 Brecciated.Vrokon up from 493'495', 1-ers then lx o/.t-carb.495.0 Gabbro, f l r.* -rt j i un '-gained, fresh, aacclye. Minor*^'id^te, traie pyrit*.49^.0 * - . -Kr.d of hole. . ' '! "
Z*: *- . * -,.. .-. *^-; l u *, ' //l T'V'v-r.V- !-*^v, *- *rli*~''"*^'**"- - -
.f *x v i -'' l. ?-v
' *- -l f -' r' " .T;,.- -WiA.V?-.:-r-v..."-'.- s .-^
DIAMOND DRILL LOG
PROPERTY
LOCATION
LATITUDE
DEPARTURE
ELEVATION
AZIMUTH
Tribag Mining Co. Ltd
Batchawana Bay, Ontario
Dip: 90 Footage
800E Depth: 502.5 500.0 S74 0W
Commenced: Nov.7/1963
Finished : Nov. 9A963Logged by
HOLE NUMBER: EB-10
DIP TESTS:
Reading Corrected-89'
M. Blecha
0.0 Casing16.0 Zone of alteration. Dark Green, fine grained rock,
highly chloritized and sericitized, medium fractured. Trace pyrite, Core badly broken up.
17.4 Mineralized zone, Py S-7% cpy less than I I, sphalerite, l-2%, in a highly altered fragmented zone. High seriicitization and chloritization, med. carbonization. QC 50*4, zone is locally strongly brecciated, with l" to l" angular fragments of QC and of altered basic material.20.0 ?? ??? sphalerite tr. in a dark green, med. chloritized, sericitized and medium fractured rock. 21.7 Py 7-10*fc sphalerite S-4%, traces of a dark grey, soft, metallic mineral (chalcocite ?) along fractures. Trace cpy. A highly altered, fractured zone, medium chlorite and sericite. QC 15-20*4 in a fracture parallel to core.23.5 Py 3-5% tr. cpy, in a highly altered, fractured rock. Medium chloritization and sericitization, medium epidotization. Rock is soft, dark, greenish, grey, QC 2-3*6
28.5 Zone of alteration. Greyish-green, fine-mediumgrained, S-7% epidote stringers and patches, medium patchy carbonization, low-med. sericitization. QC stringers 1-21, py. l-2%, trace sphal.
39.4 Altered Gabbro. Fine-medium grained, low chlorite, medium epidotization, low patchy carbonization, medium red hematite (?) staining of feldspar constitutents, and minor local patches of reddish feldspatchic alteration. QC stringers l-2%. py l-2%.
60.5 Zone of alteration. High white patch carbonization medium patchy red feldspathic alteration, med. epidotization, and silificiation, patchy medium chloritization. QC stringers 2-3*4 (some with tr. sphal) Tr. Cpy, py 1-2*1. Locally gabbroic texture evident.
agii.Ait : .^f-^ 'tsv-'v1 ""::^ ".T -- -'-'--mg-
ftfK-te-:^' '
e*-4 ; -- - ""''':^f:--, v'-vj*•j*^:. -H:--^••^S'-'.y, ' - 1
^rf- ;X ;-,Ol-.'--'- ,.-C
i - -. '
u-p
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ed /vo t****
NUMBER
DtP USTS
Footoye Rvoding
o5^.c ^9. S 74^
logged by M. Blechatt'.
.jr.* cf - li -?r .-.*. .on ,. - -.1.-.-. ,.--f:-i fi:m rr^inpa rock, '.J .-e:-: c :' , .-3 ^*Ji\^n t ri,
ir-r, andzone,
carb*- y Jtron,rly br*c~
~^','i, : .*.:iU'-. -: iii or 11 .'* i..J *-
' - ~ ^!' ' " ,'•" r a k . i-.*,-.1^15 t n 'Jr 11 *.:u i
- * . .- . . . - - --Lt ; -, - i. , - .-
: :"r., -c:;r-'j rock*- -. :* : c. .i, a-irk-. i*.e? ) fllor,^ ', c r -id . f;- -j : t UT 9-d
*C 1; -I'.'A.- in
altered, f rae cur sericitization dark j. /Trsis
• one o: a.. ' "-dt ion, -T-V.:-. *J, 5-7* *piio'*T s^ru-,
f jr.atiiat i o:: , lo^;-ru patches, medium
-TJ.. Kir.e - -," Ji .n ^ralnsd, low chlorite, o:i7dti3r low pat.-.;./ carbonatization, a^iirttite (? ; stair.:.-.,: of feldspar con-eldspa
of reddish f , py
i?h v/iiit* pitchypatchy :-iv: fV. -. ,-;-...i- alteration, , and oi-1 ",f: x.: .-j- h patchy m*5di-.ira
• u , x-^ .'-' --:,;-r* . - . -i. ? :i.;'-.4 with tr.-2^X'. i-3-u.l-' ,..v,ro^. texture tvicUnt'.
R; f.; r^- l 5 UKsp) ad)
NO. 'EB-nlDESCRl 3TJON
74,2
69*0 Altered Gabfcre. D*rk srr^n. nediur--fine grained, '; medium-high chloritization; speckled with 53* leucoxene (1-2 cos}. Minor epidotization, and minor red feldspathic alteration, wC 3trir..-;*r3 I0*fc
74,2Zone of Alteration- 3'ale green, high patchy white carbo natization, medium epidotization, silicification, and minor pitchy red feldspathic alteration, Locall/gabbroic texture is evident. - 85.3 Mineralized ^on*. 4 ^ ^ p ilerite, associated wit h an irregular QG string;- parallel to core, in a highly apidotizned, siliceous, and carbonatized rock, Tr. py, 'cpy. 88,0 Altered Zone, aa at 74.2. Py 1-254. 96.5
96.5 Mineralized Zone. finely disseminated pyrite, in ahighly altered, pale green rock. High silicification, ced. carbonatization, high patchy chloritization* Minor iniis- tonct patches, of red feldspathic alteration. 102.0 Mineralized Zone, as above* Finely crystalline pyrite increases to 15^. Intensity .of chloritization seems proportional to acount of pyrite,, 103*0 Pyrite increases to 30^. irac* cpy. 0.2* lost core at 107o9108.1 Min'd Zone, as above, pyrite 5-7#. Froa 109.4 to 109-6* 60# red feldspathic alteration with 10* highly - chloritized rounded (10 ma) pat"-.:e3, Median patchy carbo natization; QC 5-7.**112.3 Min'd Zone, as'at 96.5, .with a l" white barren qtz veinlet at 86 c.n.113.4 Hin'c Zone, as at 96 0 5, with 2-3;i finely disseai*- nated pyrite, trace sphalerite along fractures. High* patchy chloritization!114.7
114.7 Altered'Zone, Pala grey, fairly soft, raadiua aoriciti'sod,chloritized fine grained to aphanitic acidic rock*
Medium fracturing, with chlorite along fracture olattoa. Cut by 2-3^ qtz stringers; tr, cpy, leas than 1# py, 116.6 As above, bat colour changes, to pale greyish grooa, due to increase in chloritization and sericitization. Sharp lower contact at 55 c.n.118.6 . ' ,.:::*,'*'' V . ..- t . *;;:,
118 fc O Volcanics. Dark ,green, fine-ffledium grained, 'rolativoly :^.tfresh, cut by 10^ epidote and carbonato strin^or*,1 ,.*v
. -., fand 2-3/C Qts stringers. -Note lOjt pale green, rol.vhar^A : streaks of alteration, associated with opidoto stringer**.'
irregular patches and streaks of roddish * -^- -*-fractured feldspathic ( 1) material.129.4 Mineralized Zono, 50?b finely, crytftallino,30^ fine pyrite in a distinctly bandedepldotizaed and silicified rock.130.0 Fine grained, dark green, mediuasericitized rock, cut by 5'A qtz stringers.fragmented, 3-4# py aleng faactures.132.0 Volcanics, fine grained to aphanitic, darkhard, massive, cut by 2-3?* qtz-carb stringers? containsI-2^ pale brownish subrounded .and angular inclusion*.* '^:II-20 ea), l?* pyrite along fractures, - ; - ?; "' 136.5 Altered Zone. Pale greenish-grey, highlV earbO- natized; 5-7^ opidoto natches.and stringers. 100& pmtehtL- of Uark brown, soft, oicacooua material. QC strln^or* 1*2
Sheet No. 3 EB - 10
???????? mainly concentrated in first 6'. ???????? volcanics as tt t 132 0 . Epidote stringers 5%, QC stringers, l-2% Minor patchy cabonization. 152.9 As above, but epidote stringers and patches increase to 10 k. Pale green, relatively hard alteration material (as described at 118') gives rock a streaky appearence. The zone contains few minor brecciated phases in which fine grained, dark green, volcanic fragments (5-20 mt) are embedded in a silicified and epidotized matrix. Minor ?????? feldspathic alteration patches between 169.5 - 171.0 2-3% py concentrated in the more epidotized and silicified zones, and along fractures. Note : J" to l" quartz stringer parallel zones, and along core to 247.5 to 248.5249.0 Volcanics, massive and fractured, Minor epidote minor pyrite at 253.0 QC stringers less than l * epidote l *. Note a few magnetite stringers at 271.0 283.0 Volcanics, high patchy white carbonization, medium epidotization, l-2% py associated with epidote stri r ers.295.c ilcanics as at 249.0
302.0 Altered and Fractured Volcanics. Med-high chloritization the zone contains two highly sheared zones at 303.1-303.3 (?????????) and at 308.0-308.8 (75-801 ctn) These shear zones contain 501 white carbonate; at 311.1- 312.0 a fracture zone with 501; carbonate. Total1-2% pyrite.
305.0 Volcanics as at 249.0 Relatively massive and fresh.2-3% epidote stringers, l-2% pyrite along fracture
330.0 Mineralized zone, py S-7% less than 11 cpy alongfractures. Fractures mostly oriented at 70-90 0 c.n. The mineralization occurs on medium fractured volcanics as at 302.0. Epidote S-7% carbonate stringers l-2%.
333.5 Volcanics relatively fresh and massive 53; epidotetr. py.
335.5 Zone of Brecciation and Amphibolitization. Dark green, hard volcanics(?) with 50-601 medium to coarse grained dark green amphibole needles, oriented at random. 337.5 Rock is still amphibolitized, but contains 40% fractured, angular and sorrounded pine red acidic fragments. (l-20mm), in a dark green fine grained matrix. Less than l i cpy. 1-2*1 py. Acidic fragments gradually disappear at 340.0
342.5 Volcanics relatively fresh and massive, l-2% QC bcrin^er^ 346.0 Mineralized zone. 2% cpy, l-2% py. associated with qt^-
epidote stringers (151). Minor patches white carboniatization.
351.9 Volcanics, as before, relatively massive and fresh. Qtz- epidote stringers S-8%, 11 py along fractures. 361.7 Fractured and weakly mineralized zone. 1-21 py. 10% qtz. stringers, mostly at 70 0 . Minor carbonatization and red feldspathic alteration. 364.0 Volcanics, as before. The rock is very fine grained. Almost aphanitic; epidote stringers and patches S-7%. Minor patchy carbonatization, minor red feldspathic ??????????? 11 py along fractures.???????? Volcanics, Epidote and carbonate alteration ??????????????????V???? to short zones. ?????py and
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"NO. V Hole No.DESCRIPTION
422.5
narrow cpy-filled fracture. -H?.-epidote stringers 1-2;C,Kote tr. Ho3 2 alon^; fracture -*t 418."!* Minor reddishfeldspathic patches or inclusions (?) near snd.422.5Zone of Amphibolitization and Foliation. Mediua'grained,distinctly foaiate-i rock, OO-400c.nJ. Foliation due t*p&rallel orientation f t a mphibole, needles. First two feetmineralized w th 5* py aic.v. fractures.431.5Gabbro. Upper contact v~rv- ^national, Reck la fine toraediu^ grained, sar.aive, dar ; reddish green, due to redstaining of feldspar constituents,434.0 As above, bur. rock ia blenched to a pale reddish-grean colour. Minor patchy tepidot ration, qtz stringers 1-2?:,447.7 Miiiralized Zone. 3# cpy concentrated in two patchesassociated with white siliceous stringers at 65*C.n.The zone is reddish-jirey due to high red staining of feldspar,449.7 Gabbro-, as at 434.6. No t, e a n i rregular l" qtz patchaU51 ol,451.5 fabbro, aa abov-. -J or e rartly broken up-along aherr.&tlle-c.-.rbcnate-fiMrj; : ,,,:'u:-e p^.v.llel to core.455.0 fabbro, as at ^/l.c, '-c"..o :..uior offsetting ei epidotestringers around i.5 l'J.O ,tu l - ;X epidote 2-3/'. Finelyjr. .".*) . , . -- *' t ^ 4
before, t f c o:: i r* -' r; l i.. * '' ' r'.- T -?. r r tv '
h-grey, har4, apnanitic
i'tly fractured, and carbonatized frem
i- : sd feldspathic alten
i e? s t h.s r. l'*. ?- 466.0 ilo.'i*: of streaky , r-j:itly i.o6,9 fabbro, (t: i ri*: a 11 zed (I**
46^.5' on,468.5 Gabbro, nei;un e]o-u -'- ; :,- -., ns tion, tr^py,474.5 Altered Zone Dark ^;eer., .-aediuts rainor patches of brown ncft r.icaceous alteration. Rock con tains minor dark .^rerr-., very f.ir.e s'ained-aphanitic siliceous patches and ninor :-?S felssotUc patches. Qtz stringers IS. 460,C ' "6 *rFelaoph/re - Rhyolite (?) Dark r-ddiah jrey, siliceous-rock, distinctly banded at 45-850 c.n. Consists of 30-40J& indistinct reddish, hard pseudoporphyroblasts, elongated parallel ta the banding (1-5 ^, in a dark reddish-grey, siliceous, and locally chloritize-i matrix. Upper contact sharp and fractured at 80*c.n.4^3.5 Aa above, but rock is stringers l-2f
fragmented. Carbtnate
485.0 As at 460.0, but fracturing of medium intensity. QCstringers 1-2;*. trace disseminated py.4##.3 As at 4flOoO, b :t not fractured^ Distlnpt.lv hnn^A*! *As atfiO-900 c.n.
:t not fractured. Distinctly banded tt
50C.1
502.5
499.0 Hhyoiite. Brick-red, finely fractured; pseudoporphyr*- blasts absent. Th? rock is highly siliceous, aphanitic, and; contains 10-15# d urV. grey, siliceous and epidatised patches an stringers (1-20-jtm). 0.5^ carbonate stringers. i500.1 ...,-v. :--. hi^;i?iVolcanics, dark gre*n, very fine grained, faintly fa] 35 c.n. Few minor chlcritized fractures. Net*'a* J reddish qta patch (tx3") with rr.cpy at 5! End of Hele li
DIAMOND DRILL LOPROPERTY: Tribag Mining Co. LimitedLOCATION: Batoaawaaa Bay, OntarioLatitude: 13003 Dip: -6}*
Departure: 6000B Depth: 4^7*
Elwvation: Commenced: April 3, 196X
Azimuth: 3 30* F inished: April 6, 1964 Logged by: MatthOW
HOLE NUMBER: 28-14
DIP TESTSPejari at 440* * 64* I29*tf(Maga)
Footoge Reading Corrected
SAMPLE MUAUER
*
0.0 Ci1J14.0 KJ
Wh! •1VIhi•t iiK1,CL
126.0 l (r Pl.
137.0 HPC'si
201.5
217.0
DESCRIPTION
to, 2-frag] tented,
i wrioiti-jaad
10-15* 2-3* qua
Tkis xrts j ne
5-17*ale greenish
Casing
Mineralised Zone. 1-2* chalcopyrite, 2-3* pyrrhot: pyrite, with local concentration, in e highly fra. highly altered tone. High patohy chloritization, sat i on and carbonatization. First 10 feet oxidise* vuggy. Predominantly basic (gabbroic?) fragmental highly aeriaitised, indistinct felsitic fragnentci stringers end patches. Trace HoS2 along fraetu?es is identical to that encountered in top of EB-2. 104.0 - As above, but mineralisation increases to pyrrhotite, 3-4* chalcopyrite. 107.7 - Oraea felsophyre, high sericitised,, eoft,e How) I* pyrrhotite, pyrite, trace sphalerite..09.5 - Mineralised fragmented zone as before.
126.0Zone of eerloitisation and fragmentation. High sellaite, pile yellowish crumbly rock as at 107.7. The tone aontrins s predominantly basic fragmented tone from 120.0-130
sulphides. 137.0Mineralised Zone, ae at 14.0. l* chalcopyrite, pyrite. High, patchy ohloritiaatioa, •arleitisatinn carbonatization. Intludee a relatively mase!ve ga aeetloa frcei 140.0-143.0. 2-3* quart! carb&aate. 390.0 - Mineralised Zone - 3-5* pyrite, l* ehaleo highly fragmented soae. The host ie a cherty we i-regularly beaded (tuffaceous?) roek. Medlum-hlg] ly CKjLoritised and eericitised.197.5 - Fragmented Felaite, pale yellowish grey, erelatively fresh, minor eericitisatioa.201.5Zone of Fragmentation - rredominaatly pale green,felsitie(T) fragmentsi 1-2* aulphidea. Kediom20* ohloritised basic fragments.217.0Xlneraliped Zone, l* ehalcepyrlta, 5* pyrite, pyrrhotite,a highly fragmented, predominantly basic sone. HIahlorltlsalion, aerioitimetioa and earbonati*utlonquarts esrbcaate* LocaUy evident gabbroic textur
O.
pyrrhoti ;aad
b rolerep! riill, b
to ia ibut
lieeoue,
erleltis^dcart onatised
Nigh patchySS
2, Hole No. EB-UDESCRIPTION
245.0 - Gabbro - relatively massive and fresh, medium grained, amygdule-rich.247.0
247*0 Fragmented Gabbro - medium patchy epidotixation; 3-49*disseminated pyrite; low fragmentation.259*0 - Fragmented Gabbrot?) as above, mineralizationincreases t o 5# pyrite, 1-2* chalcopyrite with localconcentration.282.0
282.0 Fault Zone(?) Core broken up. nedium-highly chloritized.Partly disintegrated around 234.0. Qua*-ts carbonaterich aone from 286.0-287.0.287.0
287.0 Mineralised Zone. 5# pyrite, trace chalcopyrite, ina nedium fragmented, patchy medium chloritixed andepidotixed rock.300.0
300.0 Gabbro - still slightly fragmented, almost massive,dark grey, medium grained, amphibole-rich. Low chlorite,medium carbonatization, minor brown micaceous alteration.311.0
311.0 Mineralized Zone. 10# chalcopyrite, 5# pyrrhotite,pyrite, in a fragmented, fine grained basic zones.Faint, irregular foliation, low chlorite. Mediumepidotization and carbonatization.316.0
316.0 Volcanic? Gabbro, fine grained, dark grey, relativelymassive rock. Medium chloritixed, becoming relativelyfreoh at 319.0. l-2# pyrite, trace chalcopyrite.Gradually becoming coarser grained, distinctly gabbroic.Minor local fragmentation.337 * 0 ^ ~, 337*0 Mineralized Zone. 15-173* chalcopyrite, 10# pyrite andpyrrhotite in a dark grey, medium chloritized, silicifiedand carbonatized rock (gabbroic?)/342.0 - Gabbro - dark grey, medium grained, "spottv"texture, due to darker colour of amphibole xals.Massive, fresh, with few short chloritixed phases.1-2JC unevenly disseminated chalcopyrite, l-2# pyrite.359.7
359.7 Fault Zone. Highly chloritized, core badly broken up,gabbroic host.360.0
3oO.O Gabbro, as at 342.0.365.0 - Quartz carbonate vein.366.0
366.0 Zone of Shattering. Highly chloritised, low-mediumshattered basic rock. 5* quartz carbonate.368.0 - Becoming relatively massive, but still highlychloritixed. Probably part of a composite fault toneextending from 359.2-378.0.
3. Hole No.DESCRIPTION
370,0
373 1 5
37S. O
370.0Volcanic*, fine grained, relatively fresh, massive.373.5Fault Zone. Highly chloritiaed, shattered basic rock,core broken up. 2-3J& quarts carbonate,373.0Volcanics. Pine grained, mottled and streaky appearancedue to epidotization. Saae as in botton part of EB-6.First 10 feet aineraliced with it chalcopyrite, 1-2*pyrite and slightly fractured, 2-3S& narrow quart*carbonate stringers. Minor sulphides throughout.467.0End of Hole.
DIAMOND DRILL LOPROPERTY: Tribag Kiaing Co. Limited
LOCATION-. Batchawana Bay, Ontario
Latitude: 13003 Dip: -60*
Departure: 600QB Depth: ^r" l l ' **
Elevation: Commenced: April 7)
Azimuth:-(Qrid) d*e West F inished: April 10, 1964 Logged by: Matthew
FootageFajari at 450'
HOLE NUMBER:
DIP TESTS
Reading
IB-15
Corrected
IMRER
9
9
DESCRIPTION
0.0 Casing0.0
0.0 Mineralised Zone. l-2jt chalcopyrite, 1-2J& pyrite. '. in a highly fragmented cone, predominantly gabbroiegreyiah feisitie fragments. Medium chloritization isation and epidotisation. First 12* oxidised and Tepidotization throughout.76.0 -0.5* of 7-0JI ehaloopyrite.76.5 - Chloritisation, serlcitisation and carbon* t idecreases to low, rock gradually becomes nore epidodistinctly gabbroic, with 5-7* red felsitic fregmem1-2^ pyrrhotite and pyrite.110.0 - Mineralised Zone, as at 0.0. Less than 1* i5? pyrrhotite and pyrite j gradual increase in chlorsericite] decrease in epidote) 10-15* grey feisitieDistinctly predominantly gabbroie.125.2
125.2 Kinaralised Zone. 1-231 chalcopyrite, 5# pyrrhotitein a highly fragmented Bone. High patchy chloriticserioitisation and medium oarbonatisation. 10# gre;fragment s { 2-3J* quarts carbonate.100.3
100.3 Felsite - pale greenish brown, well banded at 00-90'Highly serioitiied. Loo Ally, tuffaceous appearancerook encountered in EB-19 at 76.0.107.7
107*7 Zone of fragmentation, low fragmentation, low alt engrained, dark grey vole (t) host. 2-3!* pyrite, 556 e190.5 - Highly fragmented, ehloritived and serleiti1-23* chalcopyrite, 2-3# pyrite and pyrrhotite. ?aVUnrecognisable host.195.0
195*0 Felsite, greyish brown, medium serioitised and fregv196.0
196.0 Volcanics? Massive, fine grained, relatively freah197.5
197.5 Mineralised Zone. 2-3* chalcopyrite, 3-t* pyrite 1fragmented tone. High patchy Chloritisation, eerieand carbonatization) locally evident gabbroie textta
C c"-' - - -- -
with 10nd eerieig*y. Mi
ationised.B. {i C
haleopyrte andfragment
and pjrrit ion,
r felsiti
c.n.similar
t ion, fidrtote.ied.thy appea
tented.dark iff
t a high!tisation•e.
otiteti-ler
y- 1t*,*
•t
lsto
se
ranee*
•y*r
..- . J
SKeet No. 2. Hole No. *B-
DESCRIPTION
211.0211.0 Shatter Zone{?) High "wet" type chloritization; core
badly broken up; numerous striated slip planes; partly disintegrated rock. Probably a fault cone. l-2# chalcopyrite, l-2# pyrite. 219.0
219.0 Mineralised Zone. High chloritiaation. 1-23& chalco pyrite, 1-25& pyrite. Kediun patchy carbonatization. Medium fragmentation. Chalcopyrite concentrations around 235.0-236.0 ( 7-1&). Local "wet" type chloritiz ation and occasional striated slip planes. Probably a continuation of the above fault zone. 249.0 - k-5t sphalerite, in a highly sericitized fragmented, partly disintegrated, pale greenish grey rock. 251.0 - 15& chalcopyrite, l* sphalerite, in a slightly fragmented, medium chloritized, predominantly fine grained, basic rock. 253.6
253.8 Felsite - Pale, brownish green, highly sericitized, soft, mineralized with U-5# sphalerite. 3-A# pyrite. (15* pyrite at 257.0-258.5).271.2 - Sphalerite mineralization increases to 6-7#. 273.5 - High shatter and sericitization. 5^ sphalerite.275 * 5
275.5 Mineralized Zone. l-2# chalcopyrite, 2-3?* pyrite in aslightly fragmented, relatively slightly chloritized gabbroic rock.281.5 - Becoming highly fragmented and chloritized. 1# chalcopyrite.283.3
283.3 Green Felsite - medium grained, pale yellowish green,porphyritic with 5-10# indistinct quartz phenocrysts.Same as in EB-20 nt 35.0.286.0
286.0 Zone of weak fragmontati on. pasic fine grained host.Medium chloritization; 2-3/fc fine quartz carbonateB ringers. Highly brecciated near end.290.5
290.5 Felsite - Pale grey, fractured, but not fragmented.292.5
292.5 Gabbro, diorite - relatively fresh and massive.Good dioritic texture. Less than 1J& chalcopyrite alongfractures.320.0 - Gabbro(?) Becoming fine grained, indistincttexture, relatively fresh and massive. Less than 1#chalcopyrite, 1# pyrite. Possibly volcanics?Minor epidotization and amphibolitization.332.5
332.5 Volcanics - (Andesite?) Fine grained, dark green, low chloritization, minor local fragmentation, medium epidotization. Trace chalcopyrite. Development of chlorite along occasionally striated slip planes, 5^ fine quartz carbonate stringers. Same as in bottom part of KB-6.
Hole No. KB-l 5DESCRIPTION
350.5 350.5 Qabbro(?) Dark greenish grey, medium-fine grained
"spotted1* texture; massive, low chloritiaation.361.7
361.7 Shear Zone. Highly chloritized, sheared 45* c.n.,locally highly brecciated; contains a carbonate-riehzone from 362.5-363.0. Gabbroic host.364.5
364.5 Gabbro, dioritic, medium grained, dioritic texture,massive, fresh, pinkish staining of feldspar constituents.399.5
399.5 Volcanics, Andesite - Sharp upper contact at 90* c.n.Fine grained, dark greenish grey, locally weakly foliatedat 600 c.n. Minor epidotization and local fragmentation.1-25& quartz carbonate stringers.435.5
435.5 Gabbro - Medium grained, dioritic texture, distinctlyfoliated at 45* c.n. Relatively fresh. 15* pyritealong fractures.479.0
479.0 End of Hole.
'lAMOND DRILL LOPROPERTY: Tribag Mining Co. Limited LOCATION: Batehawana Bay, Ontariolotitude: 13003 Dip: -65*
Departure: 5900B Depth: 397-5
Elevation: Commenced: April 12, 1964
Azimuth: 3 30* F inished: April 16, 1964 Logged by. Matthew
Footage ReadingPajari at 390' -65*
HOLE NUMBER: XB*l6
DIP TESTS
Corrected
SAMPLE NUMBER DESCRIPTION
0.0
7.0
29.0
77.0
39.0
110.0
112.0
115.0
it.,s-
ted.
and
Casing7.0Zone of Fragmentation. Predominantly gabbroic material, wit*204 pink felaitie fragments. Medium ehloritisati on- epidotlmat ion and carbonxtisation. 1-2JI pyrite, l* aa than 0.5Jt tpy.18.5 - Fragmentation daeraaaea to low, felsitic fragmentedecrease to l-23t. l22.0 - Dloritio Gabbro - medium apidotiiation. 2-3^ diaaaaiin^tedpyrita. J27.0 - ione *f Fragmentation, aa bafora, 5> pink falaitiofragnanta.29.0Kinaraliaad Kona. 2-35* ohaleopyrito, 2-3^ pyrrhotlta and pyTtraoa Mo52, in a fr&gnentad aona, aa before. Kadiui ehloritlation, oarbonatiaation. and epidotiaation. Prodeoii antIrgabbroic, with 5J* felaitio frAgnenta, locally highl) aerieit52.5 - Oabbro - awdiuai grained, relatively fraab aw aaaaiva"spotty" texture due to darker colour of anphibola jala.Trace KoS 2 along fracture planea.5X.5 - Mineralised tone. 1-2^ ohaloopyrite. 2-3^ pyrrhotitepyrita in a highly fragmented a one. 5* aaidia fragment a.Hedim ehloritiaation and oarbonatiaation, low-aediift epidot60.0 - Mineralised 1C one, aa above, but chalcopyrite daaraaaato trace.77.0Voloaaloa, Andesite - greylah green* fine frnined, locally wfllfoliated at 55-60* c.n. Low chlorite, 2-3* epidote patcheaand atraakji, 1-2* pyrite, increasing to 3-4jt fro* d! .0 on.The lone contains a highly fragmented section frtm 77*0-78.289.0Mineralised Zone. 5-65 pyrrhotite and pyrita in a lighlyfragaanted aona. Patchy high chlorltisation, aerialtiaatioaand earbonatiaation. Unrecognisable host.110.0Felsit*-Rhyollta(?) Pala greenish brown, pseudoporphyriticwaU banded at 60-90* a.n. Medium aericitiaation.112.0Zona of Low fragmentation - Almost maasiva. relatively freshl tolow chloritised, fine grained, grey (role?J host. ]p pyrita115.0Mineralised Zone. 3-i* pyrite, trace chalcopyrite j a a highly
Sheet No. 2. Hole No. SB-16DESCRIPTION
fragmented sone. High patchy chloritization, sericitii- ation and carbonatization. Core partly broken up between 121.0-123.0. 135.0 -
135.0 Fault 'Zone. Highly chloritized, almost black rock, fragmented. Core badly broken up from 136.0-137.0. 137.0 - Lost core.13#.5 - Highly fragmented zone - high chlorite, aericite. Angular chloritic fragments (30&) in a pale groyiah green, fragmented matrix.144.5 - 2one of extreme pale groen clayey alteration. Includes a 0.7' green relatively hard felsitic sectionn at 11*5.0. Highly fractured. Core partly broken up.U6.5
11*6.5 Zone of Fragmentation. Highly fragmented, chloritizedand sericitiaed. Predominantly felsitic host.Mineralized with 5.2 pyrite, trace sphalerite.157.5 - As above, but alteration Increases to very intense.Ohlorite, sericite and groenish-brown clayey alteration.Pooflibly still a part of the above fault zone. Highlyshattered core,partly disintegrated from 162.5-163.0^5-7# between 157.5-160.4.165.0 - Fragmented Felsite - alteration (sericite)decreases to medium-high; trace pyrite.166.7 - Fragmentation decreases to low, but alterationstill high. Chlorite and sericite; l-2# pyrite.170.0
170.0 Zone of Shearing and Fragmentation. Distinctly foliatedat 45-55* c.n. Highly chloritiaed and soricitized rock.Host unrecognisable, but probably predominantly felsitic.2-3^ pyrite, trace sphilerite.173.0 - Chloritization decreases, rock becomes palegreenish c',ray, still highly foliated and sericitized,predominantly felsitic. Minor local fragmentation.190.0
190.0 Zone of Fragmentation. High fragmentation, high serici tization, nediura carbonatization. Predominantly felsitichost, mineralized with 3-4# pyrite.193.0 - As above, but high chloritization. Core partlybroken up, around 194.5. l-2# pyrite, less than 0.5jtchalcopyrite.206.0 - Fragmentation decreases to low. Host distinctlygabbroic. Low-medium chloritization and epidotization.l-2# pyrite.209.0
209.0 Gabbro - Dark greenish grey, medium grained, massive,amphibole-rich. Low chlorite and epidote. l-2# pyritemostly along fracture planes. 1# chalcopyrite withminor local concentrations. Prominent red staining offeldspar constituents. 1-2^ quartz carbonate stringers.Mineralization mostly associated with epidotization.Note sphalerite at 246.0.
l
l Sheet No. 3. Hole No. SB-16DESCRIPTION
273.0273.0 Zone of Fragmentation - mineralized with 2-jC chalcopyrite,
1-256 pyrite. Predominantly felsitic material, medium carbonatization. 274.0 [
274.0 Zone of Foliation and Amphibolitization. High, but \ irregular foliation due to parallel orientation of l amphibole needles, mostly at 70"-90* c.n. Minor epidot ization and brown micaceous alteration. Similar to zone encountered in EB-5 at 265.0. Less than 1# cpy. l-2# quartz carbonate.307.5 - Quartz vein, pale grey fractured quartz, barren. 308.5
308.5 Gabbro - First one foot silicified and epidotiaed,becoming medium grained, fresh and massive. Locally dioritic, with minor red staining of feldspar constituents 315.5 .
315.5 Mineralized Zone, 4-5* chalcopyrite, pyriteassociated with high epidotization in a massive gabbro,as above.316.1
316.1 Gabbro, as at 303.5.331.0 - Gabbro - medium chlorite! zed and shattered, with5/9 red carbonate.332.5 - Gabbro, as at 308.0. .olatively fresh andmassive. 15* pyrite, Ijt pink carbonate along fractureplanes. Becoming chloritic near end, and slightlyfragmented.352.5 - Gabbro - Dark grey, medium grained, massive andfresh, but different from the above gabbro. Characterizedby "spotted" texture due to darker colour of amphibolexals. Cut by 2-3# fine quarts stringnre. No mineraliza tion. Upper contact fairly abrupt, lower contactepidotized.377.3
377.3 Volcanics - dark green, fine grained, locally distinctly foliated at 500 c.n. 5-7# epidote stringers, and 2-3# reddish feldspathic patches and streaks. 1-236 quartz carbonate stringers, 1# pyrite, trace Mc^. Note 0.7 f fractured quartz vein at 393.0.397.5
397.5 End of Hole.
DIAMOND DRILL LOmf
PROPERTY, Tribag Kiaiag C*. Uaittd LOCATION: BatuhtMtJUi Bay, OntarioLatitude: 13008 Dip: -65*
Departure) 6lOOS Depth:
Elevation!
Azimuth: 330*
HOLE NUMBER: SB-l?
DIP TESTS
Footage Reading Corrected
Commenced: April 17,
Finished: April 20, 196fc Logged by: JdtthtV Blttttt
AMM.E 'UMBER DESCRIPTION
0.0
12.0
224.0
2)0.0
Gating12*0Kintralittd Zoao. 3-4* pyrrhotitt, 3-4* pyritt, 3ttt than0.5* thaltopyritt, trato MoSa in a highly alttrcd,fragttatad ttat, at la KB-2. Patthy, pala gray,ttrieitittd, oarbtaatittd and thloritittd rttk.hoot, probably gabbroit. Flrtt 5 f tat oxidlaod10* pink Aoidit frag* artt ia firn, 10 foot. Lotagabbroit ttscturt.1X3.5 ~ Dyktt Darkggr*y. alaott black, vary fiathard, thtrty. Tratt pyritt, thaltopyrita, aaativf151.0 - Xlatralisod Zoao, at at 12.6. 5-7* pyritepyrrhotita, tract taaltopyritt and HoS2t probably jabbrolt165.5 - Qrtta Dykt, fiat graiaod, tvgar'y ttxtart, highly ttrititivtd, rtlativtly Mattiva. Tratt pyritt. Iod 40 - Miatralittd Koat, at btfort. l-2jt thalooyyritt
toattatr* kioat
t arttogai! abla vaggy.
y tYidwitgraintd.
pyrrhttitt. 1-2^ pyrit** witb lotal toftttatrat atioB rtamin* higa, at at 12,0. Ottationtl it
•lip plaatt. Mott pala ytlloviia-grtta highly phaatt at Ii5.3-18o.9 *ad 164.7-1&9.9. Frta) 175.: thaltopyritt gradoally dttrt*ttt to l*. Oabbroitloeally tTidtat.215.0 - At aboTo, bat rook naialy highly thlorititthloritixatioa)216.5 - Fragwinttd Zona. Alttr*tit* rtaaiat high.prrrhotitt, tract thaltopyritt. Qradual dttrtattof fragMtntation.224.0Gabbro - Dark grty, alnoot black, •tdloM graiatd.•ataivt, txttpt for firtt ftv f tat, whlta art ttil fragatatad. Low chloritt, looally "apottad* ttxt darktr aaphibolt xali. 3-4^ apidott, tratt " H pyritt. Frtgatat enaajct of grain tito fro* 251.0 ^ Miatralivtd Zoat. 1-9 thaltopyritt, 2-3* pyrraot pyritt, tratt MoS2 ia a patthy, ntdlve thlorititad and oarboaatittd rook.
O
triattd tit oa
ttrititiatd
2-331 pjritt, La d*grt4
rtlttiYtly alight3 y
d*o t4thaleo yyritt,
' , Vi tO ft
Ltt, 3-4* ttriti! ittd
Sheet No. 2. Hole NoZB-17DESCRIPTION
283.5
295.0
307.0
330.5
3U).0
360.0
365.0
367.5
372.0
381.0
39*. O
275.0 - As above, but pyrite increases to 10J&-15S&.280.0 - Mine rallied Zona, pyrite 1#, pyrrhotite 1-2JC,mediua epidotization.233.5Dyke - dark grey to black, fine grained, cherty, massive.3-Wfc epidote, trace pyrite.295.0Mineralized Zone. 5-7jC pyrite, in a medium-highlychloritised and carbonatized, patchy, fragmented rock.298.0 - Pyrite decreases to 2-3#.307.0Zone of Weak Fragmentation. Dark grey, f ine-mediumgrained host (gabbro-volc?) , high epidotization (10-1556),medium chloritization; l-?** nyrite with local concentra tions. Epidote gives rock a "patchy* appearance.Probably gabbro.330.5Mineralized Zone, k-5% chalcopyrite, 20J& epidote,low-nediua chloritization of a dark grey - black(gabbroic?) host, as above.
Mineralized Zone. Less than 0.5# chalcopyrite, 1-2?Cpyrite, in a fragmented patchy rock. Mediua chloriti-sation and brown micaceous alteration. Trace MoS2.360.0Zone of Weak Fragmentation. Fine grained, dark grey toblach host (gabbroic?), highly chloritiaed, locallyepidotized.365.0Fault? High "wet" -type chloritization, high, irregularshenring. Core broken up. No mineralization.Numerous striated slip planes.367.5Gabbro - Medium grained, relatively massive, medium-highchloritlzed, mineralized with 2-3# finely disseminatedpyrite. Minor epidote. 2-3# quart* carbonate, traceMoS2.372.0Mineralized Zone. 7-8# pyrite, less than it chalcopyritein a medium fragmented, gabbroic zone. Medium-highchloritization. 5-7^ greenish brown sericitized felsiticfrajnnents.381.0Zone of Fragmentation. Predominantly yellowish-green,medium-highly sericitised felsitic material. Less thanIjt pyrrhotite and pyrite.386.0 - Gradually becoming predominantly gabbroic.Medium chloritization and brown micaceous alteration.3-4* pyrite.391.0Gabbro - Relatively massive, spotty texture, due to darkstubby amphibole crystals. 3 -A3* epidote, medium chlor itization, 1# sulphides. Minor local fragmentation.
Sheet No. Hole No.BB-17DESCRIPTION
39^.0
406.0
418.2
419.0
427.0
505.5
5X8.3
546.5
398.0Volcanics, Andesite(?) Dark green, fine grained,relatively massive, low chloritization, cut by 2-,,apidote, 2-3^ quarts carbonate stringers, and mineralisedwith 2-3^ pyrite along fractures.406.0Shatter Zone. Low shatter first, increasing to highat 408.5. High chloritization, and sericitization!?).152& quartz carbonate. Unrecognisable fine grainedbasic host. Gore partly broken up, from 412.5-413.51with numerous striated slip planes. Most probably afault zone. Prom 412.5 colour of rock changes tobrown, possibly due to change of host rock to felsite.418.2Gabbro - Pine-mediun grained, highly chloritized,relatively massive.419.0Mineralized Zone. 7-8^ chalcopyrite, 5# pyritedisseminated in irregular streaks at 70-80* c k n.Medium chloritization and carbonatization in a fragmented,predominantly basic (gabbroic?) zone. Note 25# reddishquartaite-like angular fragments (poesibly deformedgarrets?- See specimen 423.5?)422.5 - Mineralisation decreases to 1# pyrite, tracechalcopyrite.427.0Volcanics (Andesite) Greyish green, fine grained;10# epidote and pale gree . alteration, giving it astrenky nnd mottled appearance. Identical rock to thatencountered in the lower part of EB-6. Locally foliatedat 35-40* c.n. Note 2-3/6 scattered epidote paeudo-anyedules (1/2-1 in.). l-2# quartz carbonate stringers,trace pyrite and chalcopyrite.505.5 "Gabbro - Medium grained, nassive, relatively fresh,dark Rreen, "spotted" texture. 1-23* quartz streaks,2-3# epidote. Upper contact indistinct. Lower sharpnt 30* c.n.518.3Volcanics, ac before. Note fine-medium grained gabbroicdyke or sill from 519.8-521.8.
End of Hole.
DIAMOND DRILL LOPROPERTY Tribeg Mining Co. Limited
LOCATION: Batehawsna Bay, Ontario
latitude: 13003 Dip: -65*
Departure: 62008 tepth: 570.3
Elevation: Commenced: April 21 1964
Azimuth: 330* Finished: April 24, 1964 Logged by:
HOLE NUMBER: IB -
DIP TESTS
Footage Reading CorrectedFajari at 500.0* - 33**. -63*
SAMPLE DUMBER
0.0
6.0
i ea. 5
221.5
239.5
DESCRIPTION
Casing6.0Highly fragmented mineralised sono. Pale greyish•patchy* rockl medium serloitised. ohloritimed andunrecognisable basic host, with li reddish acidicMineralised with 2-3* pyrite, 1-2* pyrrhotie, losschalcopyrite, tr^oe *oGj, 5-7* apidote. First 5 "and vuggy, duo to surface leaching. Zone is in,-. .or cut by 5* dark grey, fresh, massive, fins grainedaphanitic dykelets (or volcanic material) from 31.47.9-55.0.,- 76.5-47.3. These dykelets are vonkly mwith 1-2* pyrite, and are oat by 2-3* epidote stripatches. Total quartt lets than 5*.?7.3 - Fragmented, mineralised sono, as above, but. - ana. anaraao son*, aa aove, la ol*ar!r 5*^roio, locally dioritie. Tho sono
relatively fresh gabbroic aoctiona froai 9 119.3-124.0. Mineralisation grtdnally inersasoa t pyrrhotite. 2-3f pyrite, leas than l* ehaloopyrite quart* 3-4*.
ireen,sarbonat ragments, than l*
rusty•y
to J-32.0
footinterrupted
l.sedi
a sars
lha hosttaina
.0-102.5,3-4*traoo
la is
Gabbro - Dark groen, a*diuai grained, relatively fro ih•a BS i ve) 5-6^ epidote stringers nnd patches j ainera2-3* finely disseminated pyrite, lose than 0.5* ohaMinor local fragmentation. Koto 2* felsitic inolos203.5, and a highly epidotisotf tone at 216.0-219.0.221.5Zone of fragmentation. Qabbroio host, low chloritecarbonAtisation and epidotization. 3-4* pyrite, lal* ohaloop yrite. The sons contains a few. short,gabbroic aostiona. Note fractured, pale pink felsiinclusion at 237.0-23(1.0.239.5Zone of Foliation. Distinctly foliated (55* c.n.)rich gabbroic rock, locally slightly fragmented.is duo to parallel orientation of amphibole crystal ilocally high brown micaceous alteration. Similar 1amphlbolitised sono encountered in D. D. H. KB-5. l*Dip of foliation gradually changes to 70-60* c.n.
cha .copyriti L on at
medium than
laasive. ic
H* 82 ^
and ised with
. amphiboSs- F )liation
the sulphides,
Sheet No. 2. Hole No.EB-ldDESCRIPTION
253.0253.0 Voleanics(?)-Gabbro(?) Fine grained to aphanitic,
dark grey-black, relatively massive, hard rock, locally fragmented, similar to "dykes" described at 6.0*. Local indistinct foliation (50-70* c.n.) and amphibolitization. 1-2*" finely disseminated pyrite., trace chalcopyrite, trace MoS2 along fracture planes. Low-medium brown micaceous alteration. 265.0
265.0 Zone of Fragmentation and Minemlization. Patchy,medium chloritiaed, sericitized, low carbonatization. Mineralized with U-5% pyrite, lass than 0.5& chalcopyrite, 5-7* epidote, 3-1** quartz. Gabbroic host. 271.0
271.0 Gabbro. Reddish green, due to red staining of feldspar constituents, raediuta epidotized, consisting of 50^ feldspar, 50* mafics. Massive, low chlorite. l-?# pyrite, trace chalcopyrite, less than l* pyrrhotite. [ 300.0 - Epidotization and mineralization gradually j increases to 3-l*# pyrite, 2-3** pyrrhotite, less than l*1 chalcopyrite, trace MoS2. Medium carbonatization, \ minor local fragmentation. In places, high epidotization i obscures gabbroic texture. Gradually becoming finer grained.31*3.0 - Gabbro - An abrupt increase in grain size to medium-coarse. Massive, low chlorite, low-medium epidotization. l-2# pyrite, trace chalcopyrite. 356.0 - Gabbro(?) Abruptly becoming fine grained.
362.0 Zone of Low Fragmentation. Dark grey, fine grained basic host, hard,relatively fresh. Contains 5-7** reddish grey, cherty acidic fragments. Less than 2# epidote, 1# pyrite, trace chalcopyrite and MoS?. 370.0
370.0 Gabbro-V0 lc{?) Dark grey, almost black, fine grained, similar to "dykes" described at 6.0'. Slightly fractured, and mineralized with i-2% pyrite along fracture pianos. Gradually becoming slightly coarser, gabbroic. 335.1*
365.1* Quartz-Carbonate Vein. Fractured, with 15-20** basicinclusions and fragments. Mineralized with chalcopyrite,pyrite near lower contact.367.5
367.5 Volcnnice-Ar^esita(?) Fine grained, green, locallyslightly fragmented; distinct tuffaceous(?) banding at 30-1*0* c.n., accentuated by brown micaceous alteration. Cut by a fine network of epidote stringers, and associated pale green alteration. 1# pink, felsitic material (fragments?) aligned parallel to banding. Ij4 pyrite. 1*09.8
1*09.6 Felsophyre Dyke (Hhyolite-Porphyry?). Pinkish brown rock, consisting of 10-15* white rounded quartz phenocryst* (1-3 ma) in an aphanitic matrix. Sharp upper contact at 15* c.n., lower at 20" c.n. Trace pyrite.
Hole No. EB-18
DESCRIPTION
Ml*. 4
1*25.6
470.5
482.5
435.0
500.0
543.3
570.3
Volcanics, as at 337.5. Minor fragmentation at116.5. Becoming slightly coarser, and aaphibolitisednear lower contact.1*25.6Gabbro - Dark greyish green, medium-coarse grained,relatively massive and fresh. The rock is characterizedby "spotted" appearance, due to 25-30?t prismaticamphibole crystals (3-4 mm.) which are slightly darkerthan the natrix. 1-2J& fir* quartz stringers, tracepyrite, minor epidote. Gradually becoming f ink-mediumgrained near lower contact.l* 70. 5Volcanics, ^ndesite(?), as before. Indistinct uppercontnct, weakly mineralized with pyrite. Mottled withpale green alteration. Indistinctly foliated in places.3-4# epidote.432.5Zone of Amphibolitization and Fo?1ation. Medium-coarsegrained rock, consisting of 50# amphibole needles(l x 5-7 mp-.J showing sub-parallel orientation at 50" c.n,435.0Fault Zone. Highly chloritized, sheared (60 0 c.n.) andshatterfd badic rock, cut by 5-7J* reddish carbonatestringers.436.5 - Becoming relatively fresh and massive, weaklyaziphibolitized and foliated at 600 c.n. Distinctlygabbfoic.495.0 - High ahearing at 60 0 c.n., high chloritizationand local shattering, high carbonatization. 155tirregular white carbonite stringers. l-2# pyrite,500.0Volcanics, Andesite{7), a s at 470.5. First three feetmineralised with 2-3# pyrrhotite and pyrite. Cut by10-15/6 epidote stringers and pat:hes which give therock a aottled appearance. Nota minor irregular flowstructures. Trace HoSj along fractures.540.0 - Becoming slightly coarser grained, and weaklyamphibolitized. Decrease in epidote to 2-3#.547.7 - Quartz vein, pale grey, fractured, trace cpy.543.3Volcanics, Andesity(?), as at 500.0.Note; these volcanics are identical to those encounteredin the lower part of D/D.H. EB-6.570.3Knd of h .le.
••fDIAMOND DRILL LO
PROPERTY: Trlbag Mining Co. Linite*
'LOCATION: B atchawiaa Ray, Ontario
latitude: 1139.755 D'P: -90*
Departure: 6104.598 Dspth: 55^.3
Elevation: Commenced: April 271
Azimuth: —— Finished: May 2, 1964
fHOLE NUMBER: SB-19
DIP TESTS
Reading Correctedrootage Reading Correct*500' i -*7' t *3Wt ?*Jart)
Logged by: H. B leCha
SAMPIE NUMBER
0
0
DESCRIPTION
0.0 Casing20.0
20.0 -on a of Fragmentation and Mineralisation. Patchysoft rock, wortluR-htghly ehloritised , Mrlcitiswicarbonatli+d. Mineralised with 5-7* pyrite, trmpyrit*. Fir*t f IT* font vuggy, and oxidised.32.5 - Fragmentation, Hlnerallsatlm and Altcrst!to low. rock beconwfl Apidotlsvd {5-7?i) t locally d gnbbroio, d Ark jprvy, flne-omJlua grained j 1-2^ pyimottled )tppear*aoe ( doe to •pidotlmatlon.50.0 - Alt. or H t Ion lner*Hnea to iMrdlun, vainly bron3-4# Viiry finely dleeonlnJitfKi pyrrhotite.53.3
52.3 ?*one of :;erleltlsAtlon. Tale, yellowlah gr^nn. Yorunbly rock, highly eerieitls*d. 1-25* diaewnina'lent than 1# blobs of sphalerliie. Irientieal to tt*ired In HB-8 at 500.0, and KH-4 *t 230.0. Probw1highly altered acidic dylrs? Containa a 0.7* sect:fractured rock At 53.1*.69.0
69.0 /.one of Pracaentntlan. Tale groy, patchy, highlyserl6it\rr4 and oarbonatised rock. Kineralived wpyrit*, pyrrhotite, trace chalcopyrite. Locally74.4 - Carbonate Vein, parallel to core.75.0 - Ae at 69.0, but locally cherty appearance.76.0
76.0 Tuff? -ell b*n4ed (45-60* c.n.) k grey, cherty nwpinkish grey and grey bands, 1-5 BM., fractured aiised with l -ZL pyrite, tr^oe chalcopyrite and HoSsiallar to rook encountered in SB-5 At 51. d, batnot as wo 11 defined.94.7
94.7 felsite, pale pinkish brown, fr*oture4 and looallwith 10^ dark gr* y Inclusions.100.0 - Becoming grey, chftrty with nlnor pinkishfractured, locally rmxnanted. W pyrite. Irregi silicified lower contnot. Sheared at 6C* o.n. st
P*l* KTande cKa4.cc
n decre*stinctl" ite}
ra, *icac
ry noft,ed pyrittt encatily Bon of gr
chloriti.th 1-25&pidotise
ik| irregid silnera;. Verylandlnc
' f rftjpeen•hases.Liar,106.5-10
i
'Tt9b
SOS
•00*.
*lS-
•y
••J,i.
AlarL-
:ed,
7.3.
2. HoleDESCRIPTION
116.0lid.O Gabbro. Medixno grained, massive, reddish green, due to
red staining of feldspar constituents and aediua epidotization. 50# feldspar. Minor local fragmentation. Trace pyrite. 146.5
146,5 Zone of Foliation. Siliceous, well banded {45-60* c.n.) rock, probable a contact zone. Medium brown micaceous alteration. .'rnce sulphides. 151.0
151.0 Gabbro - Different fron that described at 116.0. Dark nrey, fine-nediura grained, amphibole-rieh. "Spotted" texture due to slightly darker colour of amphibole constituents. Massive, except for few minor foliated aones. Cut by l-2# pinkish carbonate stringers. Note aediinn chloritlzed, hematite-stained, foliated (65 0 c.n.) zone fron 154.7-156.5, with minor secondary quartz carbonate. Note 1.0* fragmented, epidotized zone at 200.2-201.2. 224.0
224.0 Zone of foliation and ^.mphbilitization. Distinct foliation due to parallel orientation of amphibole needles, nnin}.y at 60-70* c.n. Gradual change in texture to medium-coarse grained. Gabbroic in composi tion, but locally almost an amphibolite. Minor hematite staining. 2-3"^ quartz ~irbonate stringers.241.5
2U1,5 Gabbro. An abrupt ending of foliation. Dark grey,medium grnir.e\ well devolopod, "spotted" texture, (same as in EB-18 at U25.6)^ massive, except for f*.,* minor folintod zones, 2-3* epidote stringeru, 1;* carbonate. 283.3 - Mineralized Zona. 5/* pyrite, trace chalcopyrite, in a silicified, apidonizod , irregularly foliated, aaiphibole-rich gabbro.285.5 - As at ^1.5. Increase in epidote stringers and patches to 3-4^. The epidotizod sones are commonly weakly raineralizod with pyrite, trace chalcopyrite. Note highly epidotized zones at 312.5-315.0 and 316.7 to 317.7. Wetee-hfci!kiy-epfc*'efriBo**-*ei*e Minor fragmentation with red felsitic fragments at 321,5. 323.5 - Gabbro, as at 241.5. Massive, epidote 5*. 336.0
336.0 Zone of Foliation and Amphibolitization. V.'ell developed foliation at 70" c.n., gradually charging to 90 0 c.n. Minor epidote,341.5 ,
341.5 Gabbro, as before, medium grained, massive. 3-55* epidote. 348.5 - Zone of alteration. High chloritization and carbonatiaation. Mineralized with 3-4# pyrite, 1# cpy. 358.0 - Gabbro, as at 341.5.362.5
362.5 Shear Zone. Highly sheared (80-90* c.n.), highly chlor- itiaed, amphibole-rich zone, locally shattered, and invaded by 10?5 white carbonate. Numerous striated slip planes with minor development of serpentine. Probably a major fault.
/Sheet No. Hole No.EB-19
f. DESCRIPTION
372.C372.0 Gabbro - as ct 341.5. Dark greenish grey, medium
chloritlzed. 5J* epidote, 2-3# carbonate stringers. 384.0
384.0 Shatter Zone - Modium-high chloritization. 5-7* white carbonate. Gabbroic host. Probably still a part of the above fault, cone. 387.0
387.0 Mineralized Zone. 4-5^ pyrite, less than 0.5* chalco pyrite, trace KoS2 *n a medium chloritized, slightly fragmentod^rock. Probably gabbroic host. 405.0 - l* chalcopyrite, l-2jt pyrite, associated with quartz carbonate (15#) in a highly sericitized, pale greyish green unrecognisable rock.406.0
406.0 Zone of Fragmentation. Patchy, highly sericitiied andchloritised rock, unrecognizable basic host. 2-3^pyrite, less than 0.5^ chalcopyrite, trace pyrrhotite,quartz carbonite 2-3^. Note quartz carbonate richsone at 410.5-411.3. 2-3** pink felsitic fragments.423.0 - Mlnernlined Zone. 4-5?* chalcopyrite, in a. nediura chloritized frs^montcc1 rock,425.0 t
425.0 Mineralization decreases to 1-2* chalcopyrite, 1-2^pyrite. The host is low-medium chloritiaed. Relativelymassive volc(?) rock. Trace Mol*2*434.0
434.0 Volcanics. Dark grey, fine grained, relatively massive,except for minor fragmented zone; 5-6^ epidote;contains several short highly epidotized phases.2 3?* corbonnto stringers, 1-2^ pyrite, trace chalcopyritemostly aaaociated with epidotiaation.491.5
491.5 Volcanics, as nbove; mineralizfltion decreaofcs to trace.5*^ epidote. Game ns in bottom ptrt of KD-6.519.0
519.0 Shatter Zone (Fault) High chloritization. 5-7)* epidote,High shutter and local irregular shearing. 3-4i*carbonate.525.0 - Shatter Zone - high shatter, hj 'h chlorite.15-20?* white carbonate.537.0
537.0 Volcanics - Abrupt ending of shatter xone. Fine grained,uniform, relatively massive and fresh. 2-3# carbonateand epidote stiingern. Trace pyrite.558.3 - End of Hole.
/.'/7'ha
DIAMOND DRILL LO(PROPERTY: Tribag Mining Co. Ltd. HOLE NUMBER: rB-25
: Batchawana t3*y, Ontario DIP TESTSLatitude: I6,d20fi D 'P: -90* Footage Reading Corrected
Dep-irture: g^tlON DePth' 50^.0*
Elevation: Commenced: June 3 1 1965
Azimuth: Finished: Ju,,. 7^ ^965 Logged by:
SAMPU NUMBER
0.0
177.0
231.5
DESCRIPTION
0.0 Casing.a. oZone of High Fragvontation. Pale, greyish-green rock, aediunchloritised and carbonatized, consisting of 15J& pali felsitic and felsophyric fragments, 5# banded acidicin a matrix of fin* grained, green (basic vole?) Material.
pyrite, trace chalcopyrit
pink fragments,
e thrcugit-Weakly mineralised without. Quarts carbonate 2-72.0 - As above, but acidic fragments increase to62.0 - Baaic volcanics? dark green, fine grained, fairlyMasuive and fresh rock.85.4 ~ Aa at 3.0. Mineralisation gradually increaseU to2-3# pyrite, less than IjC pyrrhotite, leas than 2jt dhalcopyrJIncrease in epldotisation. Rote 2" carbonate veinlefc at 137177.0Quarts Porphyry. Pink, aphanitic, acidic rook j 10# quartsphenoerynts (anhedral) fairly fresh, but st.rongly fractured,with few fractured, coated with MoSj. 3-i,^ quarts carbonatestringers.199.0 - b coming highly sericltised, and locally banied(sheared, alsiost parallel to core axis).Note extreme earthy alteration at 223.0-225.0.225.0 - Quarts Porphyry - as before, fairly fresh.231.5Zone of High Silicification. 60/C fine quarts, fomiag a"stockKorke" of intersecting stringers. Quarts porp Mote traces of MoS2 coating occasional fracture. 253*0
252.0 Felsite - aphanitic, pinkish green, duo to high serl Weakly aineralised with traces chalcopyrite, and NoS fractures. Fairly strongly fractured and out by 2-3' stringers.263.0 - Felsite, at above, but becoming fairly fresh but still fractured. Trace MoSj. Quarts carbonate 329.0 - Increase in quart* stringers to 10-15^. 335.0
335.0 Fragment a basic roloanice, low fragmentation, sjedlum 2-3Jk pyrite, trace chalcopyrite. Minor epidote and alteration.
yry hos
itisaticn. along quarts
Dink,
chlorite Te Id spath i a
te, 5.
No: 2.DESCRIPTIO
Hole No. KB-25
371.0 371.0 Mineralized Zone. 7-*# pyrite, trace pyrrhotite,
less than 0.55& chalcopyrite in a fragmented, highlyaltered, patchy zone.Local strong pyritization (up to 30-40*^ pyrite).Note fractured carbonate vein at 37&.0-3&1.0.451.0
451.0 Zone of High Fragmentation. 15-209t acidic fragments,in a predominantly fine grained basic volcanicmatrix; 2-3?t quarts carbonate; 1-2^ pyrite, tracechalcopyrite, trace MoS2; medium chlorite and epidote,500.0 - Felsitic fragments absent.503.0
50tf.O End of Hole.
G GGMPAN* Lli-lITLD
i.T WORK, STRIPPING AttD TRENCHING
AREA
Stripping and Trenching done by John Halonen,Mill'iken, Ontario.
Work carried out between July 1st and August 31stin the total of 20 - 12 hour days — 240 hours
Assessment credit thereof equals 240 or 40 nan-days.6
All stripping and trenching was performed on Claim 62209
Trench completed was approximately 100 feet in length, and -iverared 3-4 feet in depth, and 3-4 feet in width.
TO BE R TMOVED F.^OM
THE orr. \ v t.!~ r;H-iCENT
QECLGG; , , . -. o, -. c;-' WINES
SAUL , -,. L :. . .; A..:Z, ONT.
\ u vnSo
l l
DIAMOND DRILL LOGPROPERTY: Tribag Mining Co. Ltd.
'LOCATION: Batchawana Bay, Ont.
Dip: -45* Footagelatitude:
Departure:
Elevation:
Azimuth:
HOLE NUMBER: X-24
DIP TESTS
Reading Corrected
Qrid North
Depth: 101.3'
Commenced: July 1965
Finished: July 1965 Logged by: L. Koskitalo
SAMPLE NUMBER DESCRIPTION
0.0
35.3
37.l
sa.5
91.1
99.4
0.0Volcanics - Greenish black, hard, non magnetic, fin* grained,fairly massive, cut by 1/10?* quart* and trace carbonate in1/2 - l mm. stringers at all angles to c.n. with averagepreference of 20-35/t c.n.(?) - rock is an andesite? butslightly, if at all, altered.35.3Rhyolite - Pale pink, acne buff, fine grained to massive, hard, cut by hairline stringers quartz,
aphanitic minor
carbonate.a?.iVolcanic,, aa above, but sheared - shearing wavy but it ant contacts with adjacent rhyolite average 20*-25* c Alteration medium-low? - sericite and minor epidotizationaa. 5Rhyolite - grey and black streaked by hairline partingsat average 30* c.n.91.1Rhyolitic Rock - grey in colour as streaked by 25mafic bands at average 35* c.n, banding averagesis somewhat indistinct.99.4Rhyolite.101.3 - End of Hole.
12-33-55* greenstone - 2* band.
.
NOV 23 1955
RES1DCNT GEOLOGISTSAULT STE. MARIE
SSM
x-24-
SSM. GII34-
DIAMONDS k: ET C M SMOWIMQ
C**!TLI.O.r4. O FT
^^ v ' f ' ! - r* a o o 1r '
DIAMOND DRILL LO9PROPERTY: Tribag Hlnln* Co. Ltd.
y,GUI* SSK 6219V
LOCATION: Bateh&wana Bay. Ont.Latitude:
HOLE NUMBER: X-2J
DIP TESTS
Departure: 12503
Elevation:
Azimuth: — **
Dip: .90*
Depth: 103.3'
Commenced:
Finished: S
Reading Corrected
J, 196J
.Pte*b.r 7, 1965 bysSAMPU NUMBER
t)
t
DESCRIPTION
0.0 0.0 Baalc Volcanic* (Andeelte?) - Dark croanlsh grey,
grained to aphanitic, fairly fra ah and nattitivr; cu 2-3;* epidote otrlnftert. Trace pyrite. 20.0 - Fairly abrupt Incranne In epi*1ot* atrln^*rt pa t eh* B to 10-15.^ at random an^es and alight Incr In chloritiaatlon. Not* 1" carbonatfl-hen^tlte *tr at 60* o.n. at 74.0*. Lost core at 96.0-97 0 103.5
103.5 End of Hole.
r' c ( lQ s^i-1 "' c"^
; 7//, ' *t ttaj (n id(4
Mnt*7
*n4 ateftfcor
.r. 3-",:*V :"K'*:" ' -i'u 1,1DIAMOND DRILL LO
Yribag Mining Co. Ltd.
f[LOCATION: Batftbavana Bay. On t.
Claim SSN 62194latitude L7tB
Departure: 12JOS
Elevation:
Azimuth: SOUth
Dip: -70*
Depth, S 104.0
Commenced: StptfN&ftr d,
S*pt*ab*r 13, 19651*99*1 fay H.
HOLE NUMBER: 1-26
DIP TESTS
Footoge Reoding Corrected
SAMTIC NUMBEI DCSCIIPTION
0.0
104.0
0.0Baaie Volcanic* (Andesite?) - Dark graaniah gray, fin*grained, fairly aaaaiva and froah. Cut by 2-35* epldotaand carbonate atringara, locally fractured.22.0 - Basic Vqloanlce - dccraaaa in apidote wtrinj*rato leaa than 1^.51.0 - Bnoio Volcanic*, aa at 0.0*.104.0Xnfl of Hoi*.
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Note:
Diamond Drill Hole N-15, 502', collared in Claim SSM 61139, was projected approximately 276 feet into Claim SSM 35127, part of a separate group of contiguous claims.
Hole N-16, 459', collared in Claim SSM 61139, was projected approximately 321 feet into Claim SSM 35127.
Hole N-17, 4#6', collared in Claim SSM 35127, was projected approximately 340 feet into Claim SSM 61139.
Hole N-19, 805'. collared in Claim SSM 62207, was projected approximately 7o5 feet into Claim SSM 62209, part of a separate group of contiguous claims.
Hole N-20, 726', collared in Claim SSM 62207, approximately 690 feet into Claim SSM 62209.
projected
Hole N-22, 566', Eollared in Claim SSM 62209, was projected approximately 226 feet into Claim SSM 62208, part of a separate group of contiguous claims.
Hole N-26, 509', collared in Claim SSM 61131, was projected approximately 204 feet into Claim SSM 62206, part of a separate group of contiguous claims.
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