42C82NE0054 MUSQUASH 17 MUSQUASH

42C82NE0054 MUSQUASH 17 MUSQUASH

ALGCHA PROJECT

989

Musquash Hest Property, 989-09

AEM Anomaly Location

Scale: l inch to 4 miles

Property Location Sketch Figure 11

Property Location Sketch Figure li

Musquash West Property, 989-09 Q AEH Anomaly LocatJ'n

Scale: l inch to 4 miles

AEM anomalies VLF Lines HEII and Hag Lines Proposed drUl holes Partial Geolooy

Scale: l' - 1320'

(

f

AE M

Map 14 MUSQUASH WEST 9^9-09 AEM ?6

Locdtion Sketch Showing:Sample locations VLF Lines HEM LinesScale: 1cm * 30m

-g-

o

* i&J

MUSQUASH WEST 989-09

AEH 27

Location Sketch Showing:' ' ' VLF Lines:^: HEM 4 MAG Lines

Soil SamplesPartial GeologySca]e: 1cm * 30m____

MINERALS EXPLORATION

DIAMOND DRILL RECORD Holt NoJ?.8.?zO.?JL

,,,,, x... 989-09-1 . Shrcl ....l.......i.,,,,.,.., v Musquash West; 989-09r..ui,-!,,|, Musquash West,,,.)tltll , 1-8 at..6?.5. NE....

I-.V.-I-.! n, ....... ........ ...... ..........••..t. l..* ..-mn

Un B ,h .30^3 -r ——————————IWins ....\. 4 5 E..i,, ......*56 ; ; ...:;;::ioi,.rciivr ......To.. tes,t-an A.E.M,

anomaly *26

c.mm,,,.d Jy.]y25, 1980 .........Completed J u 'y 2 7 i !980Drlllinj Co. ..P.t*Al?y BrOS...............Core Siie -AQ. —— ——————— — — Coilnit Ufl In Hole ".'J.

pip. c-'i-r ,, ,,,-45u , l .,..,. l .

Etch Tell Depth Rdc. True

..-1-.. __ 9.0..5ffl __ .49! __ 4.0L

Xorth

ruim v.

Sctli: IXXXIKXX

•"^"•"•"'Hu6''"*5 DESCRII'TION

0 3.5 : OVERBURDEN - BROKEN ROCK AND CLAY

3.5 4.6 ' PILLOWED ANDESITE

i. 6 5.3 OUARTZ-CARBONATE VEIN TOURMALINE BEARING

S. 3 31.7 j PILLOWED ANDESITE

3!. 7 33.0 : INTERMEDIATE TUFFACEOUS SEDIMENT WITH CHERTY BANDS'

"33.0 35.8 INTERMEDIATE TUFF WITH SILICEOUS HORIZONS : (CONDUCTOR)

1 - up to 30X pyrrhotite- miner pyrite

; - < IS chalcopyrite

"3576 " 43.3 INTERMEDIATE TUFF-

4 3". 3 " 43.6 GRAPHITIC ARG'LLITE : (CONDUCTOR)- sliahtiv conductive * 5X conductivity

"Z3.5 ' D!. 5 ' INTER9EDDEP ARGILLITE AND GrWYWACKE"

5T.5 54,^ 1 GRAPHITIC ARGILLITE (METASE.DIMENTS) : (CONDUCTOR)- moderatelv conductive - up tp 303} conductivity"

5-1.6 60.2 INTERSEDDEO ASGIVJTE. AND GRAYWACKE

Simple No.

y^fl?fiWAOfejUL |C2^JL2,C251T12514IP51532516

From

4,632,913,351,560,26SJL,79,?82,0

To

5i335,843.654.660,563.;79,682.3

nfclWi

.72.9

.3JJl—

TiP.3,4.3

Au ppni

.NilNilNil0,010.01Nil

JiiJL-,

Ag ppm

NilNil

i-NlL-H.0J7_ 0 L05Nil

Nil Nil

f i

Cu ppm

1 5778

1?9JL5J. ^130

125293

Pb ppm

334140

.5.1 ̂ 554647

~Zn

ppm

125 ,118611645 775"

100113

-

———

,

j i

AMAX MINERALS EXPLORATION

DIAMOND DRILL RECORD Holt No-98.9-.Q9iL.Sheet Mo_...-2___

. KuMavr.111 To

.

'{(DA 60,'.5 _î' :

} ' J

.i, | 67.1

!i'

-H- T -69.8

!

i

ll^ 90.5

90.5

ii

( i

j

DESCRIPTION

GRAPHITIC ARGILLITE : (UONUUCIUK) "'1 - < 201 conductivity

INTERMEDIATE TUFFWACKE- oreastppal gravwacke/argllHte Interbedded * lithic_ fragments

- pvrrhntite^section at 62.8 - 63.1 - highly ccndu-tlve,ub to 100* conductivity

INTERMEDIATE FLOW (DACITE)- some cherty layers

. . ... . . - very s.lliceous .- gradual gradation Into..andes1te

PILLOWED ANDESITE- disseminated pyrrhotite with minor chalcopyrite between

79.2 - 79-6 and 82.0 - 82.3 metres. These sections arehighly magnetic and CONDUCTIVE

END OF HOLE

l

No.

,

From To Lennth

,

————

-

" —————————

1

i

————

. ...... ——

————

'

.

-"'

'-.1

-

-'

r*

"..

~

"

*

\'


DIAMOND DRILL RECORD Hole.Vo,9J?iQ9-!........^No.__3___,., _ .,.

KO..UL-O metres- —— — --—— ——— DESCnil'TION!-|-MI)l ' To

0 .3.5 OVERBURDEN - BROKEN ROCK AND CLAY

3.5 ' 4.'6 ,'yillOWED AN'DESntT' '' ' ' ' " ' " 1 " ' " - '' The andesite 1s an overall lignt green colour, it is Tiomo-

, .... gnneous in composition and there is a strong foliation deve-, loped. Beddinq is present but 1t is not very oronpunced.

The rock is massive lookina and fraoments are absent. Cal-; cite strit.fjers are found jn, opposing directions apd are inte, J . oreted to be remnant pillow salvages. The calcite stringersi j iveraoe 3mm in width. The section is non-conductive.A"^-,-^

mineralisation is absent.

--- ; - Fo1iat;iorLto (.ore axis: at 4.0m - 42^! Beddina to cor? axis: at 4.0 - 6 C

l

i, 6 ' 5.3 j QUARTZ-CARBONATE VEINThe quartz-carbonate vein measures .7m ^n width. There

j *ppm t.o hp comp Jmpuritles but fio.s.uijjM'te mfptrajlzatloni^ prpipnt, ThK tpct.ion was split for assay purposes,TnsirtTwHnp Is prptipnf t.hrouqhniJt.

-S.J-, ,- 31,7 .-i.-PJi^WFO.-ANOFÎTF... , 'This unit is very similar to that described for 3.5 - 4.6m.

; ' In some olaces (i.e.. at 21m) there is a lot of carbonatematerial present, This is interpreted as being a possible

; . Junction ooint where 2 or more pillows met. As ie/pre,, thebeddina Is poor but the foliation is strongly developed.

- Foliation to core axis: at 24m - 36"Beddinn to core anis : at 21m - 4**

•^*^1 33.0 INTERMEDIATE TUFFACEOUS SEDIMENT WITH CHERTY BANDS'

This unit is an overall dark grey-qreen colour. The frag ments within this horizon average around Irm in diameter.Carbonate stringers are seen throughout and the ma.iority

: appear brecciated. Cherty bands average 3mm In width andare a cream colour. Mineralization consists of stringer

S n m pi* Xo,

".

:2509

Prom

-

4.6

T*

5.3

Ws

.7

'Au ' .ppi".

Nil

AgPPm

CuD^m

-

fbppm

-

^n ,ppm . i.. . .

ii

.1

1

*i

-''

i f'

j .i

--

i

.

AMAX M INERALS EXPLORATION

DIAMOND DRILL RECORD Hoi, No,98?-0?-L- Sheet No__.A.____

~M~ '"'.'"'''""rii —— DESCRIPTION

1.7 .:.-J3.0 _ (.iCQ.ntinu.edj ___ pyrite and pyrrhotite. At 31,7m the mineralization is mostj concentrated, averaging approximately 10X, Overall, the

section is non-conductive and has a very siliceous appear ance.

, - Foliation to core axis; at 32m . 420Peking to core axis : at 32m - 6U

4^'-V .3.5,8. INTERMMATE TUFF .WITH SILICEOUS HORIZONS : (CONDUCTOR)- up to 30X pyrrhotite- minor pyrite- d* ch.a,l.coDvr1te

t! The intermediate tu/f Is 8 light cream colour. This section

is very jijiêous and the majority of the mineralization 1s; restricted to the more siliceous portions. Host of the

mineralization is pyrrhotite and within the pyrrhotite theconductivity averages 60ST. At 34,1m. a smaTl concentrationof Dvrite with < \% c halcopyrite may be seen.

- at 35m foliation 42V

35,8 43.3 l I NTERMEDIATE TUFFThe intermediate tuff Is an overall Ught-grey colour. The

: fragments average 1mm irL diameter and are both mafic and: siliceous in cpfnpositlon (the maiorHv being sillcpom),

The intermediate tuff. 1s, massive looking but, 1s both foliateand bpddpd The bpdding consists of both cAert bed^ )\nri /il*tuffaceous horizons. Overall the section 1s non-cond.uqt1ve

: however, there is some mineralization consisting of ^Sstrinoer ovrrhotite. . .... .i

i - at 40m foliation 46"i bedding 60i

•^3.3^ 43.6 GRAPHITIC ARGILLITE : {CQNWCTQRj- Slightly conductive * 5X conduptivltv

i

Sump)* No.

C2J5ia

-

CP511

i

From

33,0

43.3

To

35,8

43,6

ifcrTft

2.8

-JM

Au.ppm

N11

N11

Agp w

Nil

Nil

Cu-RDTl—

57

7fi

Pb -W1U—

-33^

41

Zn ;ppm .... j

l

i

|

125

i,

j

;

1

ii

t1

118 .

1


DIAMOND DRILL RECORD Hoi, Sheet No..

~~ ~"''":-'—— —— DESCRIPTION

..31.7 ,: 33.0 _ t (continued) pyrite and pyrrhotite. At 31.7m the mineralization is mostcongentnted^ averaging approximately 10X. Overall, thesection is non-conductive and has a very siliceous ajjpear-?nce.

! - Foliation tc^core ax.1s: at 32m - 42"Bedding to core axis : at 32m - 6U

33.0 , 35.8 INTERMEDIATE TUFF WITH SILICEOUS HORIZONS L (CONDUCTOR)- up to 3056 pyrrhotite- minor pyrite

. - <U chalcopyrite

The intermediate tuff isâ Hqht cream colour. This st.:t1onis verv siliceous and the majority of the mineralization 1srestricted to the more siliceous portions. Host of themineralization is pyrrhotite and within the pyrrhotite the

j conductivity averages 60X. At 34.1m, a small concentrationi of pyrite with < \% chalcopyrite may be seen.|! - at 35m foliation 42"

35.8 43.3 : INTERMEDIATE TUFF; Th? intermediate tuff is an overall Hoht-arev colour. The

fragments average 1mm ir, diameter and are both mafic and; .... siliceous in composition (the majority being siliceous).....j The intermediate tuff j s passive looking b"^ is both foliate

and bedded. The bedding consists of both^ chert beds and als; tuffaceous horizons. Overall the section is .non-conducliv^.; however, there is some mineralization consisting of î

stringer pyrrhotite.

; - at 40m foliation 461-! bedding 60l

f3T3~, 43.6 ' GRAPHITIC ARGILLITE : (COKDUCTOJl) —.- Slightly conductive s 5X conductivity

. — ...™. ———— . ——————— — ——————— ————— — ..— —————————————————————————

Snmplt No.

.CE510

CP511

From

33.0

,43lJ

To

35.8

.13.fi

iffffr

2.6

.3

Au,PPm...

Nil

Nil

Ag nun

Nil

-iUJL

Cu

57

78

PbDDTl

i^33

1J

Znonni

i

125

i

j

i

i

!

118


DIAMOND DRILL RECORD Hoi. No r .Shott No.__..5

"i.,,,,, " ' Tu i D K S C R 1 i 1 T l 0 N

/.3.3 .. .43.6 —— (ccntinupd) , .. .. ,. ..-Jhe.graphitic argillite 1s a dark gr^y t,p hlflclLCQJOur ,-—. ....- .... .. ———— . ... Bedding is fairly prominent; consisting of bands of dark ,..,,,

: - araiJL'.te^ This section was split; as a, test for eonduetl-.. .......... . ........ . . vitv. The arqilliê 15 pnlj/ sJisLyj/ CWKtucllve - ';p to SX,

- ... . : . ,,,,.. ....... . Calcite..strill9etâj:eîejL-tlu:QiiabiLL(jus.uaJLb' cojicoxdaot —. .. . with beddinc) and average 2mm in width, Snrnp" 1,'tMr fr*g.

—————— i —— ——— raeatS-ir.e.pCfiSCnt f^QSt^probahly graywaekp In cnmpnîfinnand reach up to Snmi in ":ijjp

i

-at 45m bedding 6 U

•'•3,6 51,5 INTERBEDDED ARGILLITE AND GRAYWACKE

,.. ..-.. ,,:,. ..... , ...,. , ,l ... - — . ..— ..-, .- Jê.,sectlon.has.4fuov.ecallâxJogce^ôlQur-ccmi±5.tJjig.Ql—.j !?'ack argillite a.nJi_9rey_gravwacke, The section^ is both

____ L- bedde.d and foJiHe,d^Jhelt^din4j.s^JiSuaJlv fine, ciiyipg an-. ...- . . . - . ; - ...- oyera.]l.ma.s.5.i.V5. Inipressjon, Jiincrallzj.UQ/L-CO/lSlsl^pJ^VP^

to 2 1 slrmqer Pyrite, Strincer pyrite 1s well represQrtfedat 16,5m. Carbonate content is fairly hiqh Tthere are cfew carbonate stringers) and consequently, the rocl^ is notvery siliceous. Overall, the section is non-conductive.

' - at 47m foliation 36U; beddino 6U

Jl.5 54.5 GRAPHITIC ARGILLITE (METASEDIMENTS) : (CONDUCTORJ! -. Moderately conductive - up to 30IS conductivity1

The section is an overall dark grey colour. A foliationis weakly developed but therp Is a pronounced beddinq. Theconductivity is largely due to the graphitic horizon, howevethere is some minor (up to 3XJ sulphide mineral lytion pres ent. Pyrite and pyrrhotite are both present. The pyriteoccurs in nodular form and reaches a maximum concentrationof 5i. Pyrite nodules may be observed at 51,8m. The pyrr hotite present is present in stringer form (up to W ,There is more carbonate material than there is silica pre sent throughout the section, ihe section has an averageconductivity of about 1SS.

Surnplt No.

C?*}?-

From

51, i

To

54.6-

i

' ' -at 53m foliation 36011 ' ' hodflinn la" !

itK.th Au A9 C u ' P b Z n metres ppm ppm 'pom ppî pom

,3.JL..

. j i

i

j

—t|j

-,. ,,-.. - ...—

i

Pi.Pl,

———

Nil 139

i ! 1

40

. . .,. ..., - ,..

1

1

j

i

1

611 .

j

ij

l

i


DIAMOND DRILL RECORD Hole NtJsS^y- Sheet No....,..6.

-l

* f-iVoMCf

V.,,.,i To

.5-1.6 ..;.6C^~

~

~

-

-

( . i i

-

~

-

7

- 50.2 60.5 _ ,--"•~•~--

i- 50.5 67,1

i

-i

-;

t---

| DKSCRIPTION

ÎNTERBEDDED ARGILLITE AND.. GRAYWACKE

Th.i*i section is an overall BTCy colour It appofl*1 ; fsj — ....... - though ,thR niajor^ty of the rocXj? grsywiCke "Hh Illnor., bed?..., .. ...... . nf argillite Average, bedding, thiqkne^ .of We, argi 1 Hte is

ahnuf r.mm, The iprtinrv i* ve ry^flne.^9 Mined, Saving * mas.1 sive annpaMnrp f.arhnnatp <tr^nop^4 arp nrp^pnt/avpraolno

3nint in width) Sr,d arp di5CftnW""d?nt to hprfding Hinpralira,tipn CQnjistijtf 12 strinqer pyrrhotite, Generally speakingthere ii both a foliation and a bedding developed and thesection is non-conductive.

-at 60m foliation 38"bedding 60

GRAPHITIC ARGILLITE - (CONDUCTOR)- < 2 W c onductivity

This is just another small section of graphitic argillitewhich was split to check conductivity, The average conduc tivity is about 15X, however in some sections the conducti vity reaches a maxlniym of 302". Withfn this section there issome sulphide mineralization present consisting of approxi mately IX pyrrhotite and < l% chalcopyrite.

INTERMEDIATE TUFFWACKE- occasional graywagke/argillite Interbedding * lithic

fraoments- pyrrhotite sections at 62.8 - 63jl - highly conductive -

UP to 100X conductivity

This section is almost identical to the one described for35.8 - 43.3m. The section is an overall light grey colour,bedding and foliation are both present. Fragments averagearound 2mn and the grain size is very fine. In some placesthe calcite almost appears brecciated but it is interpretedto be a soft-sediment deformation structure. Generallyspeaking, the section is non-conductive, however, there isa .3m section consisting of approximately 30Z pyrrhotitewhich is 1001 conductive.

No.

C2513

C2514

From

60.2

v2,8

To

60.5

to.l

W4

.3

.,,3,

mi —..PP"!...

0.01

Nil..,,

AgCOT,

0.7 1

0,95,

Cu-PPH _

153

.139.,,

Pbt-PPflL ,

51"

55

2n '-con ——

'

545

ii

l

275

——————

|

,——— i ——


DIAMOND DRILL RECORD Holt NShttl No___7

,, — .^-"^ —— DESCRIPTIONf r. .. M ' To

00.5 67.1 j (continued) - at 65m foliation 42"beddina 4"

67.! 69.8 j INTERMEDIATE FLOW (DACITE)1 - some cherty layers

- very siliceous- oradual gradation into andesite

i This section is a light grey colour. It has a massive ap-i pearance and is very siliceous. Brecciation may be seeni throughout the entire section, Carbonate veins are possiblyi pillow salvages. The section U non-conductive and mineral-| ization is absent.j

- at 68m foliation 32Ubedding 60

69.8 9C.5 PILLOWED ANDESITE' - disseminated pyrrhotite with minor chalcopyrite between

79.2 - 79-6 and 82.0 - 82.3 metres. These secHvins arehiqhly maqnetic and conductive

The pillowed andesite is very similar to the andesite foundat the beginning of the hole. It ir lioht green, brecciat ed and homogeneous in composition. The small sections(aoproximatelv 1/3 of a^metre each in lenstLh).cmtain-iJ[Ut{L

j 2 W pyrrhotite. The pyrrhotite has UD tp tOO?f conduqtivjty^: Towards the end of the hole, the rock starts to become

fracjment-rich. Most of the fragments are mafic in composi tion and average 3nm in size.

- at 90m foliation 46"bedding 4

3C.5 END OF HOLE

Srmplt No.

C2515C2516

'

From

79.?82.0

To

79.68^3,]

Unrthmetres

-4.3

Auopm

AgDWl

CuDcm

Nil Nil 125Nil Nil ; 293

i

Pb ™Dpmr

1647

j

! i1 ! 1

i i'

ii

-

Zn .Dr"i '

(

i

,

ii1i!!

loo :113 i

i|

i1i


DIAMOND DRILL RECORD Holt

tut, N.. ..989-09..2, ShMl .2.

Toln^ln "Musquash~West"l ' ".. "~•oc.t.on West o.f Magpie River

^CC^BV G. Yule/ J. Affleck'•we LocMtonTlfnmlnS

Ltnjtth JPS^Sm^ ^^ ___ Commenced Jl.UJJf ?.7j. 1.580 rj| p .llCArini; .2.2.5-.. _ ......^. ^..^ ..-- __ Completed ,. J.Y.l.y. .2.9.J.....1.9, ftQ.Dip -45 DriiiinR Co Bradley B. re. 5, __ ., Ettxoi-jcciivf .To. itest.,Anpmajy. i *27.iii.i.. , core siie -AQ....... . , , , , M ,, ,, ,,., ,, ....., , . L

Collir -

Teit

.450

Depth Rdir. True108.8 440 380

1 -

KO..I.C* metresKi.-ni 1 Tu i

D E S C It 1 l' T 1 0 N

0 ( 1.8 j OVERBURDEN - BROKEN ROCK . .. .

1.8 ; 8.2. I.MAFJLC. VOLCANICS

B.? ' 10.7 SllKEOUSJCrASfniMFNTS WITH TNTFRRFDDFn PYRRHOTITE f CONDUCTOR}- strinqers of *:10X of core; seams UD to 1.5cm

10.7 11.9 ' MAFIC VOLCANICS' '

"1119 ' 54.4": COARSE GRAINED MAFIC FLOWS - AMPHIBOLITIZEO WITH THIN INTERFLOW SEO MINTS. FLOWS! ARE FINE fO COARSE GRAINED TO GABBROIC TEXTURE - SOME FLOW BRECCIA 1 ]

54.4 ' g?,? ' CHERTY/SILICEOUS ' METASEDIMENTS

51.?-! 71,4 [ G RAPHITIC ARGILLITE TO SILICEOUS JCHERH M.ETASEDIMENTS

r.nnrfiirt.nrs 0

: W . fiO . GRAPHITE t INCREASE PYRRHOTITE TOWARD BASEfi? "i r f,t G RAPHITE . . ..fi^? . fiî. ft GRAPHITE70 0 , 71.3 PYRRHOTITE PIUS fiRAPHITE BEDS

Jl f, Ipfl R MAFIC METAVOI CANICS . PIMOUFfl ANO MA'sSIUF TO FO! IATFO. FFI OSPAR X OIIART7 EYF, B TAR IN'1, 70NF?;i

IDA. 8 END OF HOLE

it* m pie No.

C2517C2518C2520C?521

From

5,58,6

62.570.7

l

To

5.69,1

60,06170,9

Uneihnetres

. i

.332r 5r;?

Location Sketch No

CUli

Set!

Au

0.04NilNilNilNil

Ag

NilN110,3MlNil

i

l

m

-..27218812368

rt1

n

i:

Pb

...3034

-5537

K

irxJOGCXKX

ZnDOT ;

1...344 L310

J50 j72 i

i

i

i

il

t


DIAMOND DRILL RECORDHob N.J89r09-

2

-,jf~*XS ——— D B S C R t 1- T 1 0 N(•roro To

0 1.8 OVERBURDEN - BROKEN ROCK1

"::T"""" 8.2 j MA'FTrVOL'CAWlCr- 'PILLOW" ANtJESfTC "j

The section of the core is an overall mecMum-qreen colour.1 The rock is brecciated throughout. The carbonate conant 1s

hicih averaqing ID-15%. Opposite verainq calcite veins arei | interpreted to be remnant pillow salvages. Mineralization

consists ut' uj) to 5* disseminated pyrrhotite. The pyrrho tite appears to be concentrated in places where the rock isbrecciated. The rock is fine qrained and has a massive ap pearance^ Beddinq is absent but the rock is moderately

; foliated. Overall, the section is non-conductive.

; (To core axis) - at 7m foliation 400

5.2 1 0.7 .SILICEOUS MEIAS.EDI.MENTS WIIHJNTERBEDDED PYRRHOTITE r CONDUCTOR)

The rock appears similar in texture and colour tn thp prp.i vious section, however, there i? a wpak dpvplonmpnt nf hpri^\ Disipminated pyrrhotite is ipen throughout flnd flyfagpt! around ?K. Calrito dtringpr-; arp "ttlll ahiinriant., thus i r\i\.

irating ^ high rarhnnatp rnntpnt Hnwpuor^ thp rnrk *pppartmnrip^fltply îli'Mfipd A ^mall pnrtinn was ?plif /it A Tmto pxaminp the pyrrhnt.ifp rnntpnt ^nri tn tp^t rnndnrHvlty

, : W ithin thp pyrrhr.Htp U/tPlri, thp rnndiirt.iv^ty rP^rho? 100Shut thrnu^hnut thp êrtion the "ock is only sliohtly con-riuf.tivp.

- at 10m foliation 44"i hPriding ?a

0.7 11.9 VAFIC VOLCANIC TO ULTRAMAFIC

This section is very similar in comoosition to that foundat the beginning of t!, hole, It is massive IpoMnfl *pdbrecciated throughout. The rock is broken MP and mottled.,,.,,through weathering. Mineralization consists of IX strinqerpyrrhoti te,

. M llrr, fnlistinn ^PO

Sum picNo,

C25J7

CPS18

i

^L3

8^6

To

5.6.

9.1

me-t^'s

. ..1

.3

1

Auown

JLSi.

Nil

AqDpm

-N-ILJ

Nil

CuDDm

mm m

WL^

PbD Dm

B ~*

—3CL-

ZnDCXTI '

• n .

,

j

i

.

,

1

1

j

3441l

1'i1

,

\

i

AMAX M INERALS EXPLORATION

DIAMOND DRILL RECORD Hoi. No .l. Shttl N'n___3

J"(*rt'^l"f

•l-ni To !

:.9 54.1 1 COARSE GRAINED MAFICE TO ULTRAMAFIC FLOWS-- -- ! - AMPHIBQLIZEO WITH THIfUNIfmOOMMENTS

i . FLOWS APF piNF TO roARSF GRA'NFP TO r.ARRnnir TF.WIKF. snuF FI nw npFrriA

Generally speaking, this rock has an intrusive lookinq tex-t.urp. Throughout this section, the grain si?e is continual-

i ly changing It apppars a*; th. n l |0 h thp fpls'c minprals havpbeen reolaced bv darker ferromagnesium during alteration.This increase in the dapker minerals (e?pecia.lly Notite)

i gives the i"OCk a very dark orev coloi""- In the coarser, portion 1;, the phenocryst5 rparh vtp to ?mm in diamptpr.

Thrnughnut thp rock there are such structures as brecciai and remnant pUlow sc'va^ges- which clearly define this unH

as a flow. Good^ examples of flow breqcia are seen at 41.8m' (138'). In some sections (i.e.. 26.8m) the rock appears

layered or banded. It is possible that these are either. interflow sediments or segments of laroe fragments. Overall; the section is non-conductive, sulohide mineralization isi absent, bedding is absent and there is a strong foliation' (for the mostjartjrovided J)v the biotite minerals).

- at 15m foliation 42"25m foliation 50U35m foliation 46g45m foliation 50U55m foliation 52O

'..'. 57,2 - CHERTY/SIUCEOUS METASEOIKENTS

Th\s section has an overall light gr"y rnlniir. It is hothfoliated and bedded^ H APPârs as though thp rncl^ it aninterbedded araywacke/aroi 1 lite which has been moderately

; silicified. The more siliceous segments contain smallfraciments, aoproximatelv 3mm in diameter. Mineralizationconsists of H pyrrhotite in stringers averaging 2mm in

....,.,..., . , width. These st r i"9ers...appe.ar tonc.ord.a.n.t..,to.,,bed()ing,a.nd...,disconcordant to the foliation. Small offsets (faults) arecommon with this unit.

- at 57m foliation 500

No.

, t

To nitre'sAuppm

Agppm

Cujpm

Pbppm

Znppm .

i,l|

1 ^ , --l

J

lt

1

1

1

|1j

|!,i

1

.


DIAMOND DRILL RECORD HoitNo-S89*09-2-..

Font n e* nrcrnirTintjr rom ! To

57.? * 71.1 GRAPHITIC ARGILLITE TO SILICEOUS CHERTY METASEOIMENTS,

This unit is an overall light qrev colour. It 1s moderatelyi silicified, fraoment rich, and mineraliyLtloji con^ 5 ** o f

[jvrrhotite/minor pyrite and < \% ch^copyrj^te. . Graphite isalso oresent and is responsible for tne'maiority of thpconductivity.

Conductors P

57.0 - 6QjO Graphite and increase of dis^pminatpdpyrrhotite toward the b^ê

62.5 - 64.0 graphite, stringer pyrrhotite, OXi chalcoDvrlte

j i 65.2 - 65.8 qraohlte, ^W strlnqcr ovrrhotUe

70,0 - 71.3 strinqer pyrrhotite plus some graphi tic beds

at 60m foliation 45" bedding 40. 65m foliation 48U bedding 6U

70m foliation 50" bedding 60

'I.'. 100.8 i MAFIC MEtAVOLCANICS. . ...: ..- : - PILLOWED AND MASSIVE TO FOLIATED

- FELDSPAR AND QUART7 EYES RFARINR 7DHFS

; This section is an overall light grepn rnlrsnr ft U v?vy. . ,. ,. .... ,... homoQeneotis in-Compo,sj.t.i.o.n.,an.d..h,a.La.,nia..s.s.ly.e.ftpp.aa.rancc,. I

^ : The carbonate content is moderately high. The carbonateoccurs as pillow salvaqes. small veins and small fraoments.The fragments aupear to have originated from the small veins

i ( s 2mm in width). Bedding is absent but there appears to bedifferential layerinq due t.o differences in grain size.Where the carbonate content; Is high ^ 405!) epidote is pre sent. In some places tht core appears to be enriched In

Sample No,

.C2.512.

Ji2520

C2521

From

57.0

JU

-TJOJL

To

,6.QJL

64

70 9

nVWfc3

2.5

9

AucomNil

Nil

mi

——

Ag om0.3

Nil

N11

i

i

CuDOT

.188—,

JL23^

,68,,.

.i

Pbj)pm-34—

LAO

-JJ—J

Zn ;pom i

-310.....iiii

;

*

.850. i. .

|

.72i

i

j

t

-

j


DIAMOND DRILL RECORD Hoi. No—989-09-2—..Shott Mo.___....5—. ....

— r~*y;f —— j D K s c n i r T i o NVrnm ; To j

71.4- ' --IQB.ft ^continued)

i feldspar and quartz eyes. Such zoryx r*n h" nhsprvpd Aroundi 5fl mptres- Sulphide m1npraH7AMnn U ahtpnt.*nrf i.hft..*i*rJi.lni | ... i* nnn.r.nnriiir.Mvp, . ..

ji *t 80m foliation 420 beddlno 4"

90m foliation 44U bpddi^g flul 100m foliation 44 0 bedding 60j

108.8 ! END OF HOLE1 -,- -. -- - ,- . --

i

[; NOTE: BETWEEN 66' AND 76' (JO. 1m - 23.2m) THERE IS ONLY 2' (.6m) OF CORE

1 REPRESENTING 10' (3.1m) OF CORE ACTUALLY ORIt,LEO. THIS IS INTERPRETED; , , . TO BE A FAUL.T ZONE WITHIN THELAMPHIBOj.IJiEO M/VFIC VOLCANICS, t.A FAULT

WAS MAPPED LN J.HE.. FIELD. OCCL'RING WITHIN SIMILAR ROCKS. THIS PRQPOSFDi FAULT IS A PLAUSIBLE EXPLANATION Fi) R THE ALTERED/METAMORPHOSED ROCK

i 1 FOUND IN THIS SECTION OF THE HOL?.l

, ,i

l

|

Rumple No.

•\

l

From To Ltnulti

1

—

'

;:

i

1

!

-.,. 1

1

li

1

!

1

,

ji —— .

5.3 31.733. n35.843.343.651.0

60. c.' JiJ.5e;.i69.S 90.5

31.7 33.0 35.8 J3.313.5 il.S 34.6 60.2 CO.5. 67.1 69. S 50.5

OVER'BURDEN PILLOWED ANDESITF

-QUARTZ'VE IKPILLOWED ANDESITE - :- '- ••• ..INTERMEDIATE. TUFF. .. . .... ... ..: ... ... .. :.:.;.... . ..INTERMEDIATE TUFF WITH SILICIOIIS HORIZONS (CONDUCTOR) Py * INTERMEDIATE TUFF ........ ...~..

' GRAPHITIC •ARGILLITE'(COflt'UCTpR)ARGILLITE AND GREYWACKE"GRAPHITIC AR6ILLITE {COHCUCTOR} - -ARGILLITE AMD GREYUAUt'

.GRAPHITIC ARGILLITE (CONDUCTOR)IHTERMEOIATE TUFFHACKc""""""""

liHERMEOIATE FLOW (OftCITE)PILLOWED ANDESITE (79.2-71.6 * 52.0-32.3 - conductive)END OF HOLE

W "'

r77 "'

nno^pm^xgiiiB. iiMW' *"**' i JJT tmri-|nfr^|y---i'-—-- — "~^r -— ̂ —~..~-, -

-'

.CONDUCTORS:. . .,. . .. ..A/27-0 - 60.O qraphito/pyrrnoiite5/62.5 - ob.o yrapMteC/70.0 -71.3 graph!te/pyrrhotite

O -I.3 -8.3 -

10.7 -II.9 - 54.4 - 57.2 -'

71.4 - IDS. O

OVERBURDENMAFIC VOLCANICS"-"" -•-- ' ' " ' 'SILICEOUS HETASEOIHENTSi^WFIC -VOLCANICS-- —-.-- ---. . .........-COARSF. GRAINED I1AFIC TO ULTRAMAFIC FLOWS CHERTY/SILICEOUS HETASEOIMENTS ARGILLACEOUS AN6 GRAPHITIC ARGILLITE

57.0 - 60.0 GRAPIIITt/PHYYHOTITE62;5 - 64.'O GRAPIIITf " "-:"65.5 - 65.3 GRAPHITE70.0 - 71.J ..PYRRHJTSTE/GRAFHITE CpHOUCJOR103.3 MAFIC METAVOLCANICS--

Elil) Or HOLE - - - - - - -•-- —

I.3 S. 2 10.7II.9 54.4 57.2 7i.4

CONDUCJOK CONDUCTOR'

....AMAX :.

NAMCS sr.A : -.Ha,.; ///L.

•'.NO-1 f f .

'w*. :.-H.TJ..H*

SCAU 1 cm , : 25 m .

LINE No. 3

mm.

Documents

42C82NE0054 MUSQUASH 17 MUSQUASH