hole np foo t ago date note · location of collar from f3 post of p-326399 foftm sz2 north . east...

Diamond Drilling42A15SW0036 26 MANN

010

Township of MANN Report NQ: 26

Work performed by: Hollinger Mines Limited

Claim NQ

P 326399

P H19679

-P 413085

UP 419741

Hole NP

MAl-4-75

MA2-3-75

MA2-3A-75

MA5-1-76

MA4-1-76

MA4-2-76

(0

Foo t ago

421'

276'

275'

453'

440'

404'

32 6 "i

Date

Sept/75

Sept/75

Sept/75

Mar/76

Mar/76

Mar/76

Note

(D

(D

(l)

(2)

(2)

(2)

Notes:

(1) #243-75

(2) #50-76

AWL 004(y-6tOri;v.9 72

',002 r,/ 6 G Z J 2 f

y v o •—f* V'

A A^TO

M

7 'i'

LEGEND

r— *- /*-

Black Outline

Yellow Inside

•p.. ,

42570 442ST3 '442362'442564!442561 p- —

24TI-" 4425T2 442563,

1^571849 ^^ . x. .

\f ~ - —---'-p-^i-J

l -" V : ' ^ . -twvi (4)4873 '414892 ' 414888 1414887 l \ 371848 1371849 , v. . ^ ^l*f?"~"T7—p~-^ "~ "p"~jv"""v x-'rvf"

*!*"** i '

•4148*0 J 4148*9 J*'*744 1419^36

414621 l 4I462O 413031 '

358242

Hollinger ClaimsClaims on which drilling is being distributed.

^ ]

V

r f'% c^—— -4--———j Si \A*

i 338(48

9*8241 1358940 e

D i STRICT ; COCHRAM

j PORCUPfNE MINING DIVISION f"

i ID "

AM

ORCUPH

PA(

C^OWN LAM' SALE

LEDGESLOCATES*" LAND

LICENCE G r .ROADSIMPROVEDftAll.WA.YS

tt tt ,.

d t

-, x -'we

7

Z 9

Location of Collar from f3 Post of P-326399FOftM SZ2

NORTH .

EAST ——

E^.EV._

AZIM. —

3+OOSXL 16Egil r--Fa f p

Collar 550 O 300' - 53. 5 O

North 730' East 2 90'

PROPERTY.

DIAMOND DRILL REPORT

MANN #1 GROUP

MA1-4-75

September 23. 1975?7197g

HOLE NO.

COMMENCED . FINISHED ___

PURPOSE OF ————————————————————————————HOLE_____Test F.M anomaly

Claim P-326399 Mann Township Drilled by Bradley Bros,

0

142

168

168.8

1

142

168

168.8

288.8

Casinq

142 - 145 BQ core145 - 421 AQ core.

Green col. Andesite locally cut bysm qtz-cal strs. Minor Po.

168-168.8 - cherty tuff.

Dark green chl. Andesite, fine tocoarse-grained sections; minor fracturingcarrying Po 4- traces of chalcopyrite.

After 200, the andesite is characterizedby fine fractures with carbonate at ashallow angle to the core. Most of thesefractures bear marginal bleaching of theadjacent andesite.

The andesite itself varies from fine tonedium grained - the medium grained portionsusually showing some development of horn-alende. The rock is also very slightlynagnetic.

206.6-208.3 - narrow cherty horizon -

the chert varying from greyish to black with

FROM

168

180

cc

TO

169

185

)RE S AM PL!

RECOV.

,..

SS

WIDTH

5

*

ASSAYDESCRIPTION OF SAMPLE

Bands of Py -f Po

Minor Po + qtz-cal strs.

FORM S2Z

NORTH .

EAST ——

AZIM.

DIP — PROPERTY.


MANN 11 GROUP

HOLE NO.

COMMENCED .

FINISHED ——-

PURPOSE OF-

HOUE ———————

MA1-4-75

Mann Township

1

DESCRIPTION

some graphitic material in the blacksections. The black sections carry a fairamount of pyrrhotite with traces of pyriteand chalcopyrite. The pyrrhotite is rela tively strongly magnetic. Banding isroughly 80-900 to the core.

After the cherty band we return to themedium to dark green andesite. There is arelative increase in the amount of finefractures with calcite here along the hole.Aside from the local coarser grained sec tions with hornblende, there is also somelocal development of blotches, of creamy towhite feldspar.

214.2-215.2; 216.4-216.7 - two narrowsections of more cherty material. Inaddition to these narrow cherty horizons.there are also a few bluish grey to greystringers of quartz along the core withappreciable splashes of pyrrhotite, pyriteand sometimes chalcopyrite. Most of thesequartz stringers are at a very shallowangle to the core axis.

The lower contact with the porphyry is

FROM

207

cc

TO

208.5

JRE SAMPL!

RCCOV.

;s

WIDTH

1.5

ASSAV

1S t l

—— . ———i1

Cherty -w. 71 po, trace py cp.

.

FORM S22

NORTH.

EAST ~-

ELEV. —

AZIM.—

DIP—— PROPERTY.


MANN #1 GROUP

MOLE NO.

COMMENCED — FINISHED M—M PURPOSE OF ™ HOLE: _ — ——

MA1-4-75

Mann Township

FROM

288.8

-

1

TO

421

DESCRIPTION

sharp but broken at 80 .

Contact to a dyke(?) of feldspar por phyry. The upper contact here is notably-onformable at 80O to the core.

The dyke is quite variable in colourfrom buff to light olive and reddish purple.The porphyry is medium to coarse grainedwith numerous whitish phenocrysts of feldsparand erratic bluish grey ovoid to lenticularphenocrysts of quartz. Certain of thefeldspar phenocrysts are stained brightorangy pink (potassic?) , particularly after375.

The dyke is also somewhat mottled inappearance possibly from the weak carboni zation of the rock.

Along the dyke, there are a few in clusions of andesite as: 289.7-290.2 contacnearly normal; 326.1-327.3 contacts @ 75O ;and 400.9-401.8 upper contact with a vuggystringer @ 65O , lower contact normal to thecore. One of these sections (400.9-401.8)is fairly well mineralized with disseminatedpyrite.

CORE SAMPLES

FROM

S

400

i*5^Kfilnut

TO

402

l/?, fi.xC-O" *-

!r— H-E'.iKvikiX u.

IlwMiHS,

RECOV.

'. Cl(ji-^. —— ,

WIDTH

2

jfa^e±d^

; ; ;;s [ihanMTfiD'JIyiilAKiil

ASSAV

(J

DESCRIPTION OF SAMPLE

A2 + For - minor pyrite.

421 END OF HOLE

FORM S22

NORTH.

EAST ——

EI.EV. —

AZIM. —

DIP ——— PROPERTY.


MANN #1 GROUP

HOLE NO.

COMMENCED .

FINISHED ———

PURPOSE OF -

HOLE _______

MA1-4-75

Mann Township

FROM

fi 4- TS

G 4- TS

G 4- TS

G * TS

G + TS

G * TSG 4- TS

G 4- TS

G 4- TS

\

TO

IfiO

195

215

225

250

275

325375

420

GEOCHEMISTRY and THIN SECTION

Buff coloured carbonate zed andesite.Dark green, fine grained andesite, trace pyCherjty section - grey - minor po py cp.Meta-andesite - with hornblende.Andesite with fine calcite stringers.Andesite - trace po py cp w. quartz.Porphyry - mottled.Porphyry - some pinkish stain.Porphyry - mottled.

- - - - -

i

FROM

Ci.

TO

i..- .-JA...i ,-.

3ECOV.

:-'

WIDTH ASSAY

Location of Collar from #2 Post of P-419679FORM S22

NORTH.

EAST —-

EI.EV. —

AZ!M. —

DIP.

XL 28E

North 500'

t^DIAMOKD DRIIL REPORTat- 27-fQQN

____Grid South - 2 O O0 Collar-

Lost hole @ 260' no tests

PROPERTY. MANN #2 GROUP

MA2-3-75

September 3, 1975 September 7. 1975

PURPOSE OF————————————————————————————-————,————— j..Test EM anomaly and ultramafic

HOLE NO.

COMMENCED. FINISHED ———

MOLE

o on t-a r; f-.Claim #P-419679 Mann Township Drilled by Bradley Bros.

0

80

* ———

TO

80

250

Casing.

Blue black, highly magnetic, coarsegrained ultrabasic rock (mottled appearanceto core.

(80-180) fairly uniform appearance,cut by hairlike calcite stringers .andgreen serpentine stringers. Both typescarrying coarse magnetite grains.

Stringers at 45? to 20O to C. A.(180-205) blue black finer grained

serpentinite, grading to a highly alteredsection.

MgCOs rosettes numerous from 205 to220. Banding 85O to C. A.

From 220 to 242, highly shearedsection, occasional fault gouge. At 242,4" fault gouge material.

(242-250) massive fine grained ser pentinite. Non-magnetic, green color tocore with brownish tinge due to micadeveloped.

FROM

CC

TO

171

3RE SAMPt.

RECOV.

iS

WIDTH ASSAY

Grab sample for Cu (.24), Ni (.28)

FORM S22

NORTH . EAST——

EU.EV. — AZIM. ™

DIP____


PROPERTY. MANN f 2 GROUP

MOLE NO.

COMMENCED .

FINISHED ——— PURPOSE OF-

HOLE ———————

MA2-3-75

Mann Township

FROM

250

*

TO

276

276

Dark black green chloritic schist

carrying bands + diss. po and chalco.

(255-247) looks like alt. serpen

tinite: carbonatized tuff?

After 260, the sulphides in theandesite generally occur in irregularstringer- like masses and tiny lenticularblebs. Often, the sulphides are within ormarginal to fine fractures of calcite.Pyrrhotite is the dominant sulphide withquite rare splashes of chalcopyrite. Thepyrrhotite is moderately magnetic.

The andesite at the end of the hole isfairly uniform in appearance, chloritic,with a dark blackish green fresh surface.Aside from the sulphide-bearing stringersthe core is also cut by fine calcite strgrsat 30-500 to the core. Weakly anphibolitized.

END OF HOLE

Hole lost at 276', due to broken rod.A new hole (MA2-3A-75) was collared 25*north with the same declination.

FROM

250

252

254

255

257

260

261

262

265

267

270

273

fa-BUB fl

cc

TO

252

254

255

257

260

261

262

265

267

270

273

276

l,tff

Sen p 5*1 r H — nt~AMil If 1*1 W

IMtMO fl ft&Hfdl U

)RE SAMPLI

RECOV.

fyfjffl.

".Z 1 'WjT!:'j tinlinmm-]

;S

WIDTH

2

2

1

2

3

1

1

3

2

3

3

3

*rf.^S

ASSAY"Co Nxi

% %

045 .07?

044 .06'

111 .215

012 .03]

062 .07:


Oil. schist + Po 4- chalco.It II II

Best min. section Po -f chalco.

Very little min. less chlorite

Dk black sch. incr. in Po -f- chalco.

A2 - 5?i po, splash cp

" 15?; po, trace cp

11 53; po, splash cp

" 10?; po, trace cp

" minor po, splash cp" 3?; po, splash cp

" minor po, neg.cp

All samples assayed for Auran Nil.

Location of Collar from #2 Post of P-419679FORM 522

NORTH.

EAST ——

27+25N

XL 28Eeusv. ————.AZIM.________r,... Collar @ 55 Q

Snnt-h - 200 Qno further

lost P 275.

North 525' West 2-40'

PROPERTY.


MANN #2 GROUP

MOLE NO.

COMMENCED .

FINISHED ———

MA2-3A-75

September 8, 1975 11. 197S

PURPOSE OF ——————————————————————————————————— .Test sulphides found in MA2-3-75 when hole was lost.

Claim SP-419679 Mann Township BQ Co^e-Drilled by Bradley Bros,

084

1

84266.2

Casing.Ultramafic complex - the suite of rocks

changing from pyroxenite-peridotite typesto more of a carbonate facies further downthe hole.

We collar in a zone of medium to coarsegrained pyroxenite-peridotite that is darkgrey to black in colour. Megascopically,numerous ovoid to subrectangular grains ofpyroxene (?) are seen, plus small lenticularblebs of magnetite and traces of feldspar.Some of the pyroxene grains may in fact beolivine although no crystals were definitelyidentified. There is also a fair amount ofcarbonate in this unit, presumably of themagnesian variety, giving rise to thegreyer coloured portions along the core.This unit is also characterized by numeroussmall fractures and slips at a shallowangle to the core (10-300) , bearing calciteand/or jade coloured serpentine. A steeperseries of fractures and slips (@ 45-700 ) ismore erratically distributed along the .

core.

FROM

CC

TO

JRE SAMPL.

RECOV.

SIS

WIDTH

—————

ASSAY

————————————

——————

FORM 522

NORTH .

EAST ——

DIP PROPERTY.


MANN t2 GROUP

HOLE NO.

COMMENCED . FINISHED ——— PURPOSE OF - HOL.E ———————

MA2-3A-75

Mann Township

t

'T' D ESCRIPTION

At 167 - h " fracture with serpentine-calcite as we enter a finer grained phaseof the pyroxenite-peridotite, and the rockis greyer in colour overall. Certain por tions of this zone are very fine grained,black in colour and notably more serpen-tinized than the adjacent rocks. The rockhere is still strongly magnetic althoughonly locally can tiny blebs of magnetite beseen.

At 226.7 the rocks grade towards thecarbonate phase of the ultramafics. Herethe rocks are dark olive to dark greygreen in colour with a high percentage ofcarbonate plus serpentine and talc. Mostof this section has a rather soapy con sistency. Portions of this carbonate zoneare coarsely speckled with rosettes ofmagnesite (?) to h " in size, set in anolive coloured serpentinized matrix. Theunit is also strongly magnetic althoughno blebs of magnetite were noted mega-scopically. Due to the softer nature ofthe carbonate phase, there are sections of

FROM

CC

TO

}RE SAMPU

RECOV.

ES

WIDTH ASSAY

1l

:

FORM S22

NORTH.

BAST ~—

ELEV. —

AZIM. —

DIP ———— PROPERTY.


MANN f2 GROUP

HOLE NO.

COMMENCED .

FINISHEO ..-,-

PURPOSE OF -

HOLE _______

MA2-3A-75

Mann Township

266.2

i

TO

275

broken core and some fault gouge as :241.4-241.8 broken; @ 243, broken; 244-244.5 blocky; 246.4-246.8 broken; 249-250blocky; 257.8-261.8 blocky with gouge from260. .3 to 261.8; @ 263.7 - 1" gouge.

•Lower contact sharp - slightly chilled,fine grained and black at 55O .

Contact to a volcanic sequence - thecontact being marked by 8" of greyish toblack chert with approximately 15% sul phides - pyrrhotite and traces of chalco pyrite. The pyrrhotite is the non-magneticvariety .

After the chert band, to 269, the rockis andesitic - grey green in colour, weaklyserpentinized, fine grained and rathergranular textured. The core is cut byfine stringers of calcite. This unit isdevoid of sulphides.

At 269, the andesite grades abruptlydarker green, finer grained and moreuniform in appearance. This section isstrongly chloritic and partially amphi-bolitized with shiny needles of amphibole

FROM

266.2

269271.5272.5

cc

TO

266.7

271.5272.5275

3RE SAMPU

RECOV.

iS

WIDTH

0.5

2.51

2.5

ASSAY

———————————

1

1

———————————————————————————————————————————————————

j

Chert - IS5* po, tr.cp

Andesite - very minor po, spl.cpAndesite - 6% po, tr.cpAndesite - minor po, spl.cp

FORM S22

NORTH.

EAST__

Et-CV. —

AZIM. —



MANN f 2 GROUP

HOI.E NO.

COMMENCED . FINISHED ^-—

PURPOSE OF.

HOLE _______

MA2-3A-75

Mann Township

TO

275

DESCRIPTION

noted on some of the fresh surfaces.Irregular stringers and lenses of pyrrhotitmay be found across this zone - locallywith splashes of chalcopyrite. Thepyrrhotite here is moderately magnetic.Scattered fine fractures with calcite at30-400 to the core.

'

END OF HOLE

CyiSP- Y . l Ajfj^(L^\alfjt^KHHp'R ""[.1? j ™!fn

illfilfiillVt UlVl/Aiftiv

FROM

i

cc

TO

5RE SAMPUI

r CCOV.

iS

W. UTM ASSAY

—————


Difficulty in drilling en countered around 275 - after acementing attempt, hole waslost. No Thin Section samplestaken since this hole duplicatrMA2-3-75.

^

l 1 C -fri ) li

Iff

A

A

9 l ' -.1

ge o/l

^MJ- fi/Mfi/

'

m sil Bi

^

o

•'OIHV1HO 'SNIHMi HOT 8KB BB

o*

y

e i?

•v:

y xC?

11li

5f

ft t '/r, /V '/t, tof7, Cone,

it - Mat-

-SO* ,

?

vfl

L- .Y.™

V8

-

March 24, 1976.

Statement Showing Distribution of Assessment Days as at.

Result of 1,297 feet of Diamond Drilling Performed onMann 14 and Mann 15 Groups/ Mann Township, March 4-22, 1976

Claim Number

P-413082413083 .413084413085413086413087413088413089413090413091414619414620414621414622

443379443380443381

443382

44338?

Assessment Days

40404040404040404040 40404040 6363636366

Claim Number

P-414873414874414875414876414877414878414879414880414881414882419736419737419738419739 419740419741419742419743419744 479758

Assessment Days

20202P20202020202020 22222222 22222222

22

.Location otrot***

t. Motrr*EAST-EL.EV. AZIM.

C611ar trom *2 Post ofSil

30+00 NXL 33WsurtaceISO0 az.

Collar 1-500 .300';-490r

P-413085 North West

True (Grid South)100' :-48. '453':-520

5W ; PROPPRTV

100 DIAMOND

MANN

DRILL REPORT

f 5 GROUP

t

COMMENCCOriUKturnPURPOSE OF . ,...

toductor

'JV5-1-76 Kar eh 5,yiarch 3.

test s trona

19761976

H. E. M.near and •parallel

con-to, a jxnr , ultrabasic contact.

FROM

0'8'

11'

40.3'49.5*91*

95.3'149.6'152.9'181'247'

251.3*262'

268. 6 *281.5*293.8'298.5*303*317*

^ 323*336.1*357'

TO

8'1L'

40.3'49.5'91'

95.3'149.6'152.9'181'247'

251.3'262*

268.6'281.5'293.8'298.5'303*317*323*

336.1357*

453*

DESCRIPTION

SUMMARY LOG

CASING - OverburdenBASALTIC ANDESITE to 'ULTRABASIC'ANDESITE AGGLOMERATE (?)

HORNBLENDE GABBROANDESITE TUFF-BRECCIA

BANDED ARGILLACEOUS CHERT1 SPECKLED ' ANDESITEBANDED ARGILLACEOUS, GRAPHITIC and CHERTY Tl'SPECKLED' to FRACTURED ANDESITEBLEACHED ANDESITEBANDED ARGILLACEOUS, GRAPHITIC and CHERTY TlCHERT to PORPHYRITIC RHYODACITEBANDED GRAPHITIC and CHERTY TUFFBANDED and FRACTURED CHERTCHERTY FELDSPAR PORPHYRY to PORPHYRITIC BHXDD2BANDED and FRACTURED CHERTFELDSPAR PORPHYRY'SPECKLED* ANDESITE to ANDESITE CRYSTAL TUIFELDSPAR PORPHYRYALTERED ANDESITEBRONZITE (?) -HORNBLENDE GABBRO

PYROXENITE (?)

CORK SAMPLES

FROM

FF

FF

^TIV

F

TO RECOV. WIDTH ASSAYDESCRIPTION OF SAMPLE

E.O.H. - 453*

from f2 Post of P-413085 3CHOO N

North 355* West

IA.Teuev.

..

XL 33W COMMCNCCO

FINISHED ———

MA5-1-76

March 5. 1976 March 9 . 1976~

18Q0 Jt^..

•inn*.-.400? 453':-520 PROPERTY. MANN #5 HOLE

Claim P-413085 Mann Township BQ CoreFROM

0'

8'

V*

*

11'

TO

8'

11'

40.3*

DESCRIPTION

CASING - Overburden

BASALTIC- ANDES ITE to 'ULTRABASIC 1 - fine-grained;

dark grey to green-black; characterized by tinywhite feldspar laths and microlites (up to 1.5mm long) widely-spaced and randomly orientedthroughout the rock; non-magnetic; non-carbonatized; cut by some hairline irregularwhite carbonate and silica stringers - some ofwhich, along with hairline fractures containsmall blebs of pyrrhotite and traces of chalco pyrite; the unit locally has a tuffaceousappearance - in which case, it could beclassified as basaltic-andesite crystal tuff;the feldspars occur in patches and 'blobs' overlast 0.4 feet; the upper 0.3 feet are quiteblack, very fine-grained, and although non magnetic, apparently ultrabasic in composition.

ANDESITE AGGLOMERATE (?) - fine-grained; grey-green.subrounded to rounded, bleached (?) andesite•fragments' or 'bombs' (up to 70 nan long)closely packed (particularly throughout upper

24 feet of unit) ; the curved surfaces of

CORE SAMPLES

FROM

8'

11'13*

18'

23'

26*

29*

34'

36*

39'

42'

46'

50'

53'

54'

59'

TO

11'

13'

18'

23'

26'

29'

34'

36'

39'

42'

46*

50'

53'

54'

59'

60*

wecov. WIDTH

3'

2'

5'

5'

3'

3'

5'

2'

3'

3'

4'

4'

3'

1'

5'

1'

ASSAV-Oa —— Hippro ppm

73 53

80 56

97 58

82 53

352 75

54 47

86 61

80 60

85 61

84 90

23 119

60 115

101 54

92 74

76 5!

113 215


3%-5% strgrs; 3%-5% po, tr.cp5%_7% M H t, M

S'fc-S'k " 2%-3'fc po,pytt tt ff tt tt

5%-7% " 3%-7% po,cptt tt tt tt tt

5%-10'fc " 2%-3'fc po" " S'k-7% "

3%-5% "

2%-3% " 2%-3% "tt tt tf tt

tt tt tt tt

5%-7% " "

10%-15% " 5%-7% po, tr.cp5%-7% " 3%-5% po

5%-7% "

FORM *3t*

HOItTM.

CAST —,

euev. —AZIM. —


PROPERTY. MANN f5

MOCE NO.

COMMENCED. FINISHED —— PURPOSE OF. HOI.E————

KA5-1-76

FROM

M

40.3'

TO

49.5*

DESCRIPTION

adjacent 'fragments' create angular

interstices which are filled by dark green, fine grained to very fine-grained andesitic material;at first glance, this unit has the appearance ofan andesite breccia in which the dark greenangular interstices are fragments - the 'bomb'interpretation, however, seems more correct;tiny blebs of pink-bronze pyrrhotite, commonlywith chalcopyrite are found throughout - usuallywithin the dark green interstitial material

and/or with blobs of grey chert (esp. @ 25.7'and 26.8'); several straight seams of grey-whitesilica with marginal bleaching cut the core @

150 to 200 to C. A. (and contain traces ofpyrrhotite); the fine thread-like stringers

present at the top of the hole are persistentthrough this unit as well; the dark-greenandesitic material present in interstices atthe top of the unit, predominates at the base.

HORNBI.ENDE GABBRO - fine- to medium-grained; mottled

grey-green and creamy-grey with a few verywidely-spaced large black subhedral hornblende (?

phenocrysts (up to 4 mm lona) ; locally very

cone SAMPLES

FROM

1

TO

-

necov. WIDTH ASSAVDESCRIPTION Of SAMPUE

1

FORM *2X

NOWTM. CAST——eucv. —AZIM. —

DIP ———


PROPERTY. MANN #5

MOLE NO.

COMMENCED .

riNISHED .-—— PURPOSE OF -

HOLE——-———

MA5-1-76 3.

FROM

49.5'

w

TO

91'

DESCRIPTION

weakly carbonatized; non-magnetic except for

tiny blebs and specks of pyrrhotite disseminated

throughout; lower contact sharp and distinct @

65O to C. A. ; upper contact indistinct and

broken.

ANDESITE TUFF- BRECCIA - fine-grained; generally

dark green with tiny disseminated white feldspar

microlites (as @ top of hole) although much

more tuffaceous in appearance - and

interspersed with numerous sections of

breccia ( central subrounded green to green-

grey 'fragments' up to 50 mm diameter, are

surrounded by envelopes of bleached fine breccic

up to 20 mm wide, and the angular interstices

are filled by dark green to green andesite) ;

the breccia 'envelopes' are composed of

numerous tightly-packed, angular to subangular.

medium green, fractured, andesite fragments

(up to 1.5 mm) with white rims in a green to

creamy-grey cement — individual fragments are

similar to types found in delicate aquagene

tuffs; blebs of pyrrhotite, commonly with

chalcopyrite, are present throughout -

CORE SAMPU.es

FROM TO RECOV. WIDTH ASSAYDESCRIPTION Of SAMPLE

*xx

NORTH.

CAST——

euev. —AZIM. —

01 f ————


PROPERTY. MANN #5

MOLE MO.

COMMENCED .

FINISHED___

PURPOSE or.HOLE ———————

MA5-1-76

FROM

t

91 '

-

TO

95.3'

DESCRIPTION

particularly along narrow white-grey carbonate-silica stringers; numerous narrow-cream to grey-white carbonate-silica stringers - many @ 10Oto 20O to C. A.; large fragments in lower partof unit are dark green andesite with numerouswhite feldspar microlites; @ 59.3* po is ingrey carb, strgr with felted amphib. laths

- 53' to 53.9' - strong breccia with greycherty cement and stringer zone @ 70O toC. A.; fine pyrrhotite and chalcopyritealong foliations; dark green andesite (?)fragment ghosts (up to 25 mm) left increamy-green altered cement.

BANDED ARGILLACEOUS CHERT - fine-grained to veryfine-grained; black argillaceous bands

(some' weakly crenulated) @ 65O to C. A. pre dominate in centre of unit, and alternate withgrey-white chert; tan-grey chert predominatesat top of unit, and fractured green-white chert-silica is predominant from 92.8* to base; theupper contact is sharp and distinct @ 10O toC. A., and the basal contact is sharp and

distinct ? 45O-50O to C. A.; pink-bronze

CORE SAMPLES

FROM

90'

92'

94'

TO

92'

94'

96'

RECOV. WIDTH

2'

2'

2'

ASSAVDESCRIPTION OF SAMPUC

5%-7% strorsj lL0%-12% po^cpfi M If ft H

" " S'fc-lO'i po

-

-

NORTH.CAST ——

EI.EV. —AZIM. —

DIP____

-DIAMOND DRILL REPORT

PROPERTY. MANN #5

MOLE MO,

COMMENCED.

FINISHED ———

PURPOSE OF .

HOLE ———————

XA5-1-76 5.

•i "V TO

i

j

i

95. 3'

l".V,6*

-—

--™

149.6'

152.9'

——————

i

DESCRIPTION

pyrrhotite, chalcopyrite, and some pyrite arecommon throughout - usually parallel to foliatic- @ 93' and 94.5' are straight pyrrhotite seamsup to 3 mm wide parallel to the foliation (andstrongly conductive) .

'SPECKLED' ANDESITE - fine-grained; medium to dark

green with scattered darker green 'patches' andgrains as well as pervasive white-grey materialin matrix; very weakly magnetic; non-carbonatiztseveral narrow grey-white silica- carbonatestringers cut the core - usually @ 20O to. C. A.;considerable very fine-grained pyrrhotitedisseminated throughout and/or along stringers.

BANDED ARGILLACEOUS, GRAPHITIC and CHERTY TUFF -

fine-grained to very fine-grained; foliation @650 to 700 to C. A.; strongly magnetic; cut bynarrow white carbonate seams @ 20O to C. A.;upper contact sharp and distinct @ 80 to C. A. ;lower contact sharp and distinct @ 45O to C. A./straight pyrrhotite seams up to 3.0 mm wide

i are @ 150' and 150.5', are parallel to foliatio.j —————— i ———————————————————————————————————————— ' ' ancL.are stronqly conductive.

iCORE SAMPUES

FROM

i;

115'

118'

a

150'

151'

i.

TO

118'

120'

151'

153'

RECOV. WIDTH

3'

2'

'______

1'

2'

ASSAYDESCRIPTION OP SAMPLE

'

,

3%-7'k strgrs; 3%-7% po" 3%-5% "

ij1———— l, ———————————————————

-'

3%-7% strgrs; 5%-10% po,tr.cp,pyft H W tt tt W

I———— 1 ———————————————————

1

FORM Si*

NORTH.

EAST—— ELEV, —, AZIM. —. Oil*____


PROPERTY. MANN #5

HOLE NO.

COMMENCED . FINISHED ___ PURPOSE OF.

HOLE ———————

MA5-1-76

FROM

152.9'

181'

x.

TO

181*

247'

-

DESCRIPTION

'SPECKLED' to FRACTURED ANDESITE - fine-grained;medium to dark green; numerous dark green grainsor 'patches' especially from 158' to 168'; non magnetic to very weakly magnetic; non-carbonatized except for narrow creamy-whiteseams and stringers @ 45O to 70O to C. A. thatare quite common toward base; pyrrhotite ispresent as blebs along fractures and stringers,especially over upper seven feet; broken corefrom 161 . 6 * to 168 ' ; upper contact is somewhatbleached for 0.1 feet; @ 177.5' 2" seam offriable brecciated (?) vuggy carbonate and greenchert @ 250 to C. A.

BLEACHED ANDESITE - fine-grained; mottled lighttan-grey and dark grey-green depending onextent of alteration; non-magnetic except forblebs of pyrrhotite along stringers, fracturesand within the rock; non-carbonatized exceptfor narrow grey-white silica and/or carbonateseams that cut the core @ angles of 10O to 45Oto C. A. (particularly from 218' to 238'; @238.3' is a 1.5" seam of green chert-silica

and carbonate @ 15O to C. A. ; short sections of

iCORE SAMPLES

FROM

179'

182'

TO

182'

185'

RECOV. WIDTH

3'

3'

ASSAVDESCRIPTION OP SAMPLE

1

5%-10% strgrs; 3%-5% pol(tt-^ "

,

.,

FORK* S22

NORTH.

EAST —— ELEV. —

AZtM. —

01f ————


PROPERTY. MANN #5

NO.

COMMENCED . FINISHED —— PURPOSE OP-MOLE ———————

MA5-1-76

FROM

247'

251.3'v

262'

TO

251.3'

262'

268.6'

DESCRIPTION

cream-tan coarse- to medium-grainedgranophyre @ 182. 5 ', and 184' to 185.2'; thereare numerous white to cream tiny feldsparspecks below 237'.

BANDED ARGILLACEOUS, GRAPHITIC and CHERTY TUFF -fine-grained to very fine-grained; foliation @800 to C. A.; upper contact sharp and distinct@ 650 to C. A.; lower contact sharp and distinct@ 650-700 to C. A.; pyrrhotite seams from 1 to 3mm wide, either parallel to foliation or sub-parallel to C. A. are @ 249.5' and 251' (mixedwith graphite and are strongly conductive) .

CHERT to PORPHYRITIC RHYODACITE - very fine-grainedlight to medium grey with numerous widely-to medium-scattered white feldspar phenocrysts(up to 3 mm); non-carbonatized ; considerablefine-grained pyrrhotite disseminated throughout

BANDED GRAPHITIC and CHERTY TUFF - fine-grained tovery-fine-grained; foliations @ 60O to C. A.;upper and lower contacts @ 75O to 80O to C. A.

CORE SAMPLESFROM

225'

227'

230'

235'

237'

240'

242'

245'

247'

249'

250'

252'

255'

257'

260'

262'

265'

TO

227'

230'

235'

237'

240'

242'

245'

247'

249'

250'

252'

255'

257'

260'

262'

265*

268'

RECOV. WIDTH

2'

3'

5'

2'

3'

2'

3'

2'

2'

1'

2'

3'

2'

3'

2'

3'

3'


8*^1^ strgrs; 3%-7% po,cpS'k-lO'fc " 3%-5'fc po

" " 2%-3'fc "" " 5%-10% po, tr.cp

2*1-311 poM ft MM

5*^-7** " 5%-7% po,cp" 5%-10'fc po,cp

" " 7%-10% po,py,tr.cp3*k-51 " 7%-10% po, tr.cp

" 5%-10% portr.cp5%-7% po, tr.py

24,3t B MM-

M tt M M M

2%-3'fc " 2%-3% poS'fc-S'fc " 5%-7% po, tr.cp

" 3%-7% po, tr.cp

NORTH .

EAST ——

DIAKOKD DRILL REPORTwo. -'AS—l—76 8.

AZIM.

DIP PROPERTY. MANN #5

COMMENCED .

FINISHED ——

PURPOSE or.HOI.E ———————

268.6'

281.5'

.

293.8'

TO

281.5'

293.8'

298.5'

DESCRIPTION

BANDED and FRACTURED CHERT - fine-grained to very

fine-grained; pale grey to greenish-yellow'bands' alternating with pinkish-grey to dark

grey 'bands'; 'foliation' @ 80O to C. A.;

pyrrhotite blebs are scattered throughout -

especially along fractures (some of which are

open) ; speckled with large dark green grains

from 275' to 276'; lower contact sharp and

distinct @ 80O to C. A.

CHERTY FELDSPAR PORPHYRY to PORPHYRITIC RHYODACITE -

medium-grained; numerous cream and white

feldspar phenocrysts (up to S mm) as well as

angular dark green 'fragments' (up to 6 mm

long) that are surrounded by yellow-greenalteration rims up to 3 mm wide; broken core

from 583' to 285'; trace of disseminated

pyrrhotite specks and a few blebs of pyrite;

non-carbonatized; lower contact streaked,

sharp, and distinct @ 85O to C. A.

BANDED and FRACTURED CHERT - generally similar to

section from 268.5' to 281.5V; short sections

of green speckled andesite from top to 295* and

FROM

268'

270'

273'

275'

278'

280'

282'

cc

TO

270'

273'

275'

278'

280'

282'

285'

——————

)RE SAMPLI

RECOV.

———————————

— : —— — -

ES

WIDTH

2'

3'

2*

3'

2'

2'

3'

ASSAV

3%-5% strgrs; S'fc-7% po, tr.cp

" 3%-7% po,tr.cp,pyfi *l It t* tf tt

5%-7% " " " " "

3%-5'fc " 3%-5% po, tr.pyH ii H ii M

2%~3% po, py

ii

FORM S2Z

NORTH .

CAST ——

DIAMOND DRILL REPORTAZIM.

DI f —— PROPERTY. MANN #5

HOLE NO.

COMMENCED . FINISHED ——— PURPOSE OF -

HOUE ———————

MA5-1-76

r ROM

298.5'

303'

9

303'

317*

DESCRIPTION

296.8' to 297.3' -

FELDSPAR PORPHYRY - medium- to coarse-grained;

grey-green mottled with scattered white feldsparphenocrysts (up to 2.5 mm) and numerous darkgreen grains (altered amphibole?) speckledthroughout; cut by white and pink silica-carbonate seams @ 5O to 10O to C. A. withscattered small blebs of pyrrhotite and smearsof pyrite; lower contact sharp and distinct @650 to C. A.

'SPECKLED' ANDESITE to ANDESITE CRYSTAL TUFF -

fine-grained; medium grey @ top with scattereddark grey-green grains ........to dark grey-green @ base with numerous scattered whitefeldspar(?) laths and dark green fragments; cutby narrow white carbonate stringers parallel tothe C. A. and @ 30O to 40O to C. A. ; non-magnetic;

non-carbonatized; a few smears of pyrite andpyrrhotite

- 303.4' to 304' - banded, very fine-grained.cream and medium grey chert; upper andlower contacts sharp and distinct @ 55O

PROM

cc

TO

)RE SAMPUf

RECOV.

:s

WIDTH ASSAV

——————————— |

,

| ———————————————————————————————————————————————————'

-C* X- * t\ m

J

FORM SZZ

NORTH .

CAST ——


AZIM.

DIP PROPERTY. MANN f5

HOLE NO.

COMMENCED .

FINISHED———

PURPOSE Of -HOLE———————

MA5-1-76 10.

FROM

317'

323'

336.1'

TO

323'

336.1'

357'

DESCRIPTION

- 307.5' to 309.7' - as from 303.4' to 304' -

only contacts @ 85O to C. A., and some

green chert.

FELDSPAR PORPHYRY - similar to unit from 298.5' to

303 ' ; contacts very sharp and distinct @ 82O to

C. A. ; non-magnetic; non-carbonatized.

ALTERED ANDESITE - fine-grained; generally grey-

green with pervasive mottled pink - yellow-greei

tinge; upper 3.6' are similar to crystal tuff

section above 317' - and there is a sharp

contact @ 700 to C. A. @ 326.6'; parts of the

unit below 326.6' have a siliceous appearance -

possibly due to two fine-grained yellow-green

'feldspar porphyry' sections from 333.2' to

333.4' and 335.8' to 336' (@ 50O to C.A.);

non-magnetic; non-carbonatized; scattered blebs

of pyrrhotite and chalcopyrite over upper 2

feet.

BRONZITE (?) -HORNBLENDE GABBRO - medium-grained;

randomly-oriented grey-white feldspar laths

set in grey-green matrix along with numerous

CORE SAMPLES

FROM TO RECOV. WIDTH ASSAVDESCRIPTION OF SAMPLE

————— | ————————————————————————

1

———— { —————————————— : ——————II

'

ftORTM ,

CAST —


PROPERTY. MANN #5

MOLE MO.

COMMENCED .

FINISHED ———

POWPOSE OP .

H O Ut ———————

.XA5-1-76 11.

PROM

,

357'

TO

453'

DESCRIPTION

dark grey grains (hornblende? or black

pyroxene?) and bronze grains (bronzite?) ; non-

carbonatized; very weakly magnetic; cut by

narrow pink-cream and green-white carbonate-

silica seams @ 15O-25O to C. A.; upper contact

sharp and distinct @ 15O to C. A.; lower contact

broken; few traces of sulphides

- 350.2' to 350.8', 351' to'351.4', 353.4' to

353. 5' , and 353.7' to base - very fine

grained grey chert sections @ 45O , 55O ,

700 , and 45O to C. A. respectively; all

feature numerous scattered euhedral black

to bronzy amphibole (?) crystals (up to

6 mm long)

PYROXENITE (?) - fine- to medium-grained; dark grey

to black, and speckled throughout with numerous

scattered black to 'bronzy' grains (up to 3 mm

diameter) ; cut by several narrow seams of pale

green serpentine (?) material - @ 45O to 60O to

C. A. - and subparallel to C. A. (these appear to

be open fractures near top of unit) ; the whole

unit (except for up to 5 feet @ top) is strongl;

CONE SAMPLES

FROM

413'

TO

-

414'

RECOV. WIDTH

1'


2%-3% strgrs; 3%-5'fc po, cp

MORTM.

CAST ——

AZIM.

DIP

DIAMOND DRILL REPORT MOL.C WO.KA5-1-76 12.

PROPERTY. MANN #5

FINISHED PURPOSE orHOL.E

.

TO DESCRIPTION

to very strongly magnetic; non-carbonatized; thecore is locally soft, but only over short lengthmuch of the unit appears finely brecciated withsubrounded to subangular fragments (up to 20 mm)distinguished by paler . grey to whitish alteratiothe last 20 to 25 feet also contain a fewscattered tiny reddish-brown grains that appearto be garnet; slips and fractures throughoutare chloritic; sulphides are generally rare andare seen only on a few stringers (as @ 413.3').

E. O. H. - 453'

~*

/^S^\fef vi\IS P. J. BATEMAN j* \ j————————————————————————— L* ——————— /O - * l, 1V ̂ \ flLj^ h\^,c ts^-^jf

^^*~"^

PROM

'f

i;

1

|

J-I**C

/^Y&Yhg— ——jo PAUL;bfi^u

X* f r-j ^fc^ 4*

ccTO

•^r/T^^v2S^s^<

BATEMAN

^^ y^—— ̂ ^ vv-1 "V.LWJ'^^'

)RE S AM PUt

RECOV.

LBAo J t. f± fy

:sWIDTH ASSAV

——

DESCRIPTION Of SAMPLE

i

PROPERTY

feL i \Ll W i'vi

MANN *5

HOLE "O.

COWMCMCEO.FINISHED —— PURPOSE OF . MOLE ———————

KAv-l-76

CORE SAMPLESDESCRIPTION " ———————— FROM

1

AU and GEOCHEM i

l

1

!;

i;

j;

j!

li

i;

jj

M

i

i;

-,... . ——— j- —— ——— ,..—— ,. —— .,, DeSCRIfTION OF SAMPLE TO RECOV. WIDTH ASSAY j

j!

i ! l i

i i ;;

i i :;

i li i ji

i t'| l ',

i

i i '

l j '.

: li ii| ;;1 ji

i ! i-1 i:r

! 1 f. h

| i;

l i ''

l i p -! !'

1 i i '

j i'

Location ot Collar from *2 Post of P-419741 i^ortr. ^2'FORM S2Z V)*c*- s; T noL.ft,o VZ.4-1 — 7*35+00 N DIAMOND DRILL REPORT ' " v^ch , 2 , 97,tLEW. __ .,,...

A TIM. ..,,,11, -

mi* C*^

Surface18 00 ,

TlflrT-qO'30D ' s-4

az. True (Grid South) .. ..^0? 100':-480:60t 440' :-

PROPERTY ™™N

viuK^.r. v^rfh 15 1^76

*4 GroUP •""' to test H- E - M - conductor

Mann Township BQ Core Drilled by: Bradley Bros.

FROM

0'

32'

91'

107.6'111'

186.5'191.3'207'

209.6'

215.7'

267.1'271'

283.6'294' *

304.6'

332. i 1339.7'

358.5'

TO

32'

91'

107.6'111'

186.5'191.3'207'

209.6'

215.7'

267.1'271 r

283.6'294'

304.6'

337.1'

339.7'

358.5'440'

DESCRIPTION

SUMMARY LOG

CASING - OverburdenBASALTIC ANDESITE to ANDESITE

BLEACHED ANDESITE with CHERT

ANDESITE BRECCIA

COARSE 'B' FLOW to 'SPECKLED 1 ANDESITE

'SPECKLED' ANDESITE BRECCIA

BANDED GRAPHITIC and CHERTY TUFFANDESITE PORPHYRYANDESITE to 'SPECKLED' ANDESITE

COARSE 'B' FLOW to 'SPECKLED' ANDESITEFELDSPAR PORPHYRY to ANDESITE PORPHYRY

COARSE 'B' FLOW'SPECKLED' ANDESITE

COARSE 'B' FLOW

ANDESITEANDESITE PORPHYRYANDESITE to 'SPECKLED' ANDESITE

ANDES ITE(?)

E. O. H. - 440'

CORE SAMPLES

FROM TO RECOV. WIDTH ASSAYDESCRIPTION Of S AM PL. C

i

i!li

li

1

! ; ....................t————————————

1

Ji

j

i

1 ;

Location,, o^f Collar from *2 Post of P-419741

35+00 N

North 850* West 50',

CAST XL 6 Wflfv Sur±aceAZIM.01P

180" az..Collar:-50w ; :

300' :-460:True (G

LUO' :-4y440' :-

rid South)D ; iPROPERTY.

DIAMOKD DRILL REPORT

MANN f4 GROUP

MOCC~O. VA4-1-76

FINISHED

PURPOSE or HOUE

March 12, 1976March 15. 1976

Claim P-419741 Mann Township BQ Core

0'

32'

t

32'

91'

DESCRIPTION

CASING - Overburden

BASALTIC ANDESITE to ANDESITE - very similar to

unit @ top of MA5-1-76 - especially insofar as

numerous tiny white feldspar 'microlites 1 are

randomly scattered through a fine-grained, dark

green matrix; however, the overall unit is

more siliceous than in MA5-1-76 (i.e. closer

to andesite) ; several localized zones (e.g.34.5' to 35.3', 41.6' to 48.2', 51' to 51.9',

58.2' to 60.5', 73.6' to 77.2', and 87' to 89')

exhibit weak ' agglomerate ' -type texture and

brecciation similar to the andesite agglom erate in MA5-1-76; there is a narrow zone of

brecciated white feldspathic material from

50.6' to 51' @ 600 to C. A. with blebs of

pyrrhotite and some chalcopyrite along lower

contact; there are several bleached, finelybrecciated zones with quartz stringers andpronounced foliation @ 50O to 40O to C. A.

from 40' to 40.8' (broken and vuggy) and53.5' to 53.8' respectively; also there are

numerous narrow stringers, some bleaching, and

some grey-blue quartz stringer material from

FROM

——————————

51'

52'

53'

55'

j

cc

TO

52'

53'

55'

57'

)RE S AM PH

RECOV.

5S

WIDTH

1'

1'

2'

2'

ASSAY

——————————————————————

i1

i

iii

ii 5%-7% strqrst 3%-5% pojco

2%-3% " l%-2% PO

3%-5% " 3%-5% po,tr.cp

51-7*?; " 2%-3% po

j

i

S22

MOWTM ,

EAST__

EUEV. —

AZIM. —

DIP ___

DIAMOND DRILL REPORTFINISHED

or

PROPERTY. MANN #4 MOCE

91'

i

107.6'

55.8' to 57.2' (foliation @ 60O to C.A.) - all

of these bleached sections (from 40' to 57.2')

have very fine-grained pyrrhotite and traces

of chalcopyrite disseminated throughout the

lower part of each zone; from 36' to 38' and

78" to 85' there is considerable broken core——————————————————————————————————————————— 1

due to closely-spaced fractures @ 15O to C.A.

(some are open and/or vuggy, and coated with

chlorite, carbonate, or epidote) ; bleached

from 71.5* to 72'; non-carbonatized; non

magnetic .

-

BLEACHED ANDESITE with CHERT - fine-grained to

veryfine-grained; andesitic sections are

grey-green to dark green with numerous

scattered white feldspar microlites and local

brecciation-agglomeration (whitish 'ghost*

subrounded fragments with angular green

andesite interstices) ; there are tan to

greyish-brown fractured chert sections from

93.5' to 96.8' and 99.1' to 101.5' - contacts

are sharp and distinct @ 15O to 20O to C. A.;

the upper contact of the unit is sharp and

distinct @ 20O to C.A. ; non-carbonatized; non-

FROM

CC

TO

)RE SAMPUI

RECOV.

ES

WIDTH

j

I

1

ASSAYDESCRIPTION OF SAMPUC

i

————————————————————————————————————————————————————

1

1

'

i

1

i

magnetic.

WORTH . DIAMOND DRILL REPORT : MO.

COMMENCED

XA4-1-76

EUCV.AZIM.

DIP

or

PROPERTY. MANN #4

107.6'

ill 1

111'

186.5'

——————

ANDESITE BRECCIA - fine-grained; green to grey-greer1 fragments ' in green to dark green ' cement ' ;cut by several vuggy, open fracture systems @850 (older) and 20O (younger) to C. A.; uppercontact is sharp and distinct @ 35O to C. A. -and is paralleled by pyrrhotite seam andsome chalcopyrite @ 107.7'; lower contact ismarked by bleached zone from 110.9' to 111' -the upper contact of which is @ 55O to C. A..... lower contact being @ 45O to C. A.; theoverall zone contains up to 15% pyrrhotite andlocal tiny blebs of chalcopyrite - large blebsof pyrite, bordered by semi-open 'cracks' or'vugs', occur within the pyrrhotite.

COARSE 'B' FLOW to 'SPECKLED' ANDESITE - fine- to

medium-grained; generally mottled green andgrey-green due to fine gabbro-like texture;

this unit is comprised of coarse 'B '-type flowand finer, green 'speckled' andesite with agradational contact between the two @ 150.1';there is also a gradational contact @ 184.6'

——————————————————————————————————————— . ———to bleached light-grey-green andesite; unxt

is cut by several narrow white-cream carbonate

rnoM

107'

109'

.

——————

111'

121'

i\ 1l ——— ,,,,.,i

cc

TO

109' .111'

114'

123'

3RE SAMPL!

RECOV.

IS

WIDTH

2'

2'

.

3'

2-

ASSAY

t

S'fc-S'fc strgrs; 2%-3% po,tr.cp2%-3'i " 5%-15% po,py,cp

l!ii1! .ii!ii!i!i

ii

P l!

jj

|i

———————— j; —————————————————————————————————————j:lij!

~——j———————————————1J!

!| 2%-3% strgrs; 2%-3% poii i

i!

i! 10%-12% strgrs; 2*^-3^^ po

lii'

ti—————— . ——————————————————————————————'!i:;;i;

MOKTM. EAST ——

DIAKOHD DRILL REPORTAZIM. Oil* PROPERTY. MANN #4

COMMCNCCO .FINISHED —— PURPOSE or.MOLE _______

186.5'

4

191.3*

TO

191.3'

207'

*

DESCRIPTION

silica seams @ 35O to C, A. - commonly withtiny blebs of pyrite or pyrrhotite; very weakljmagnetic to non-magnetic; non-carbonatized ;

numerous narrow stringers @ 35O to C. A. from120.5' to 122.5'; a prominent quartz fracture

@ 155.8* appears responsible for a narrow

bleached zone from 155.2' to 156.8'.

'SPECKLED' ANDESITE BRECCIA - fine-grained; grey-green; strong breccia zone with pyrrhotite-

rich fragments (up to 12 mm) and narrow white

carbonate-silica stringers top to 187.1' @450 to C. A.; whitish-grey vaguely-outlined

small 'fragments' are speckled through rest ofunit; very weakly magnetic; non-carbonatized.

BANDED GRAPHITIC and CHERTY TUFF - fine-grained to

very-fine-grained; alternating bands of black

graphite and grey-white chert impart afoliation of 650 to 75O to C. A. (some crenu-

lations) ; there is considerable pyrrhotitethroughout - either parallel to foliation or

web- like around large rounded graphite

' fragments ' ; chalcopyrite is found in blebs -

FROM

186 1

191'

193'

195'

197'

200*

202'

205'

cc

TO

187'

193 1195'

197'

200'

202'

205'

207'

)RE SAMff.1

RECOV.

:s

WIDTH

1'

2'

2'

2'

3'

2'

3'

2'

ASSAV

——————————

j

1

-

7%-10% strgs; 5%-7% po,tr.cp

3%-5% strgrsf 5%-7% po,py,cp

2%-3% " 10%-12% po,py,cp

S***-?** " 5%-10% po,py,cp3^5,). ,, ft tt t. t.

2%-3'fc " 5%-7% po,pytt n tt 11 M

3%-5% " 5%-10% po,py,cp

DIAMOKD DRILL REPORTor

PROPERTY. MANN #4 HOI-E

especially along chert contacts; upper contact

is sharp and distinct @ 65O to C. A.; the lower

contact is very sharp and distinct @ 82O to

C. A.; chert predominant from 199' to 205.3'.

ANDESITE PORPHYRY - fine-grained; dark grey-green

with numerous scattered white subhedral to

euhedral feldspar microlites , laths , and

crystals up to 1.5 mm; similar to unit at top

of hole except feldspar crystals are more

distinct, and matrix is much darker grey;

lower contact is very sharp and distinct @

700 to C. A. (such sharp contacts suggest

intrusion but no noticeable decrease in grain

size or marginal bleaching near contacts) ;

locally, has a cherty 'look'.

.

ANDESITE to 'SPECKLED' ANDESITE - fine-grained;

green to dark green; massive with a few

-mattered dark green to black fragments (?) or

-rains; cut by narrow white carbonate-silica

.,eams subparallel to C. A.; non-carbonatized ;

non-magnetic .

FROM

t

1

cc

TO

———————————

}RE S AM PU

RECOV.

| ————————— !

ES

WIDTH ASSAY

—————

t

1

1 ————————————————————————— 1

i i

ii

i

j

ijli

ii!!

i

MOITTM.

CAST ——

e LEV. _AZIM. —

DIP____


PROPERTY.MANN #4

FINISHED PURPOSE OF HOLE

FROM

215.7'

4

267.1*

TO

267. l 1

271*

DESCRIPTION

COARSE 'B' FLOW to "SPECKLED 1 ANDESITE -

essentially 'B 1 flow as found below 111' - and

even coarser-grained; relatively massive; non-

carbonatized ; very weakly magnetic; cut by

narrow carbonate-silica seams @ 25O to C. A.

and a few @ 55O to C. A. (with blebs and smears

of pyrite and/or pyrrhotite); from 253.3* to

257.3' is a 12 to 20 mm wide seam of white

quartz and marginal pyrite (as small cubes)

subparallel to C. A.; from 261' to 265.3' are

numerous narrow white quartz seams, both sub

parallel to C. A. and @ 60O to C. A., with

considerable cubic pyrite along margins -

resulting in a section impregnated with small

pyrite cubes; trace of mud gouge (?) @ 261' .

FELDSPAR PORPHYRY to ANDESITE PORPHYRY - medium- to

coarse-grained; numerous scattered white

feldspar phenocrysts (up to 2.5 mm) and some

scattered dark green 'patches'; matrix

generally grey green to dark green; upper and

lower contacts sharp and distinct @ 70O to

C. A.; from 267.5' to 268', the feldspar

phenocrysts are much scarcer, whereas there

CORE SAMPLES

FROM

253V

255'

261'

263'

TO

255 1257'

263'

266'

'

RECOV. WIDTH

2 1-

2'

2 1

3'

1


S^k-lC^ strgrs; IC^-^*; py

S'fc-ltn py

5**-^ strgrs; 5%-10% pyIf fi It li

i

it

NOftTM .

EAST ——

DIAMOND DRILL REPORTCOMMENCED .

AZIM.

DIP PROPERTY. MANN #4PURPOSE OF

HOLE

PROM

271'

283.6'

4

294'

304.6'

TO

283.6'

294'

304.6'

337.1'

DESCRIPTION

are scattered dark green to black euhedral

crystals, and blebs of pyrite - this zone seems

transitional as contacts are sharp but not

distinct; non-carbonatized ; non-magnetic.

COARSE 'B' FLOW - as from 215.7' to 267.1';

non-carbonatized; non-magnetic.

'SPECKLED' ANDESITE - fine- to medium-grained;

numerous dark green to black grains or

'fragments' speckled throughout grey-green

matrix; considerable cubic pyrite disseminated

along margins of quart z- carbonate stringers

from 285' to 287' and 290.8* to 291.6'; non-

carbonatized except for narrow seams; non

magnetic.

.COARSE 'B* FLOW - as from 215.7' to 267.1'; non-

carbonatized; non-magnetic; disseminated

pyrite along narrow quartz-carbonate seams.

ANDESITE - fine-grained; dark green; fractured

throughout - the fractures being filled by

narrow seams of quartz- carbonate; relatively

CORE SAMPLES

FROM TO RECOV.

t

WIDTH

•j-

ASSAVDESCRIPTION OF SAMPLE

rani* szi

MOfTTM ___ DIAMOND DRILL REPORTEUEV. .

AZIM. .

DIP___ PROPERTY.MANN #4

FINISHED ——

PORPOSC or MOLE

FROM

337.1*

339.7*

V

TO

339.7*

358.5*

massive; non- carbonat i zed; non-magnetic.

ANDESITE PORPHYRY - more similar to unit from 207'

to 209.6' than unit from 267.1' to 271'; very

sharp and distinct contacts @ 720 (upper) and

77O (lower) to C. A.; non-carbonatized; non

magnetic ; has .cherty look in places .

ANDESITE to ' SPECKLED ' ANDESITE - fine-grained;

grey-green to dark green with sections

characterized by numerous small grey-white

'specks' or clusters of 'specks' (348.5' to

349', 350.1' to 351', 351.3' to 352', 354.4'

to 355', 356.2' to 356.4', and 358.3* to base)

- the attitude of these 'speckled* zones

isn't always clear, but a few seem to be @

400 to 450 to C. A.; from top to 343.2' is a

zone of breccia with numerous narrow white-grej

quartz-carbonate stringers; the narrow quartz-

carbonate stringers are also plentiful below

the breccia zone to 348'; there is considerabl*

disseminated pyrite and some pyrrhotite in

the breccia and stringer-rich zones.

CORE SAMPLES

FROM TO RECOV.

1

WIDTH ASSAV

——————————— t


11 - '~

i

1!li ... ...... ............ ....... ^.... ..... ———————————————————————

...---1

. ... . 1 ————————————————————————————————————————————— . ——..-.... ——— .. ——————— ...—— ..... .................. ... . . .

t|

NORTH.

CAST——

EI.EV. —AZIM. —

DIP____


PROPERTY.MANN #4

MOLE HO.

COMMENCED .

FINISHED --—

PURPOSE OF .

MOLE ———————

XA4-1-76

PROM

358.5'

-

440'

DESCRIPTION

ANDESITE (?) - fine-grained to very fine-grained;

from top to 383 ' , the unit is so fine-grained

and dark grey that it resembles a raeta-

siltstone to meta-argillite; the entire unit

is cut by numerous narrow green-white carbonate

seams @ 15O to 40O to C.A. ; from 383' to 392'

and 402* to 403', the core is ligher-grey,

more bleached, and more siliceous- looking;

from 360.6' to 367.7' are widely-scattered

large blebs (up to 5.0 mm) of pyrrhotite;

considerable pyrite is found along seams as

smears and blebs - especially below 389 ' ; non-

carbonatized; non-magnetic; narrow zone of

fine breccia @ 65O to C.A. @ 361.8'; narrow

breccia zones with considerable pyrrhotite in

cement @ 396. 2O (70O to C.A.) and 415.6' (60O

to C-.A.); large green andesite (?) and white-

grey quartz blebs or fragments (?) (up to 6 mm)

throughout and usually feature cores of

pyrrhotite; narrow straight seam of pyrrhotite

@ 750 to C.A. @ 411.8'.

E. O. H. - 440*

PROM

389'

l

cc

TO

392'

)RE SAMPLI

RECOV.

—————— f

f ~-

i a.

\

is

WIDTH

3'

^^^/^

-V. J. C 't

f

X^Cco,**B M l* t

ASSAY

^N"x^^Xmmf ^** \7- '

"S" ' f "

*sff).v*?^/''^f^~

——— 1t1


5%-7% strcrrsj 3%-5% po.py

X^^VT^Vjr ^3^-— -~Cl y^?0\

/.O C \^G\

UiJAUL J. BATEMAN Ql

\ .O x. S C*-s t

V^Tn^'^^ — -^"

NORTH DIAMOND DRILL REPORTEL.EV. .

AZIM. .

DIP___ PROPERTY. MANN f 4

HOLE MO.

COMMENCED . FINISHED ———

PURPOSE OF .

HOLE ——————

FROM

@

ieee9999999999.@9@

TO

33'67'

88'

100'

132'

151. 5'174'216'

233'

269'

288'

312'

347'

368'

389'401*

417'

439'

DESCRIPTION

Au and Geochem

-

CORE SAMPLES

FROM

!

TO

.

RECOV.

i

WIDTH ASSAYDESCRIPTION OF SAMPLE

li

li ___________________________________________________

I,.,... .,.,.,,,,

1——————————— li —————————————— ... ——————————— ....... ———————————————— .

li

J

.Location of Collar from 22 Post of P-419741North 360'S22

NORTH.

EAST__

30+00 NXI.-Surface

AZIM.. Grid South -18QQ-500; P 1QQ' -

O 300' -51.50

West

PROPERTY.

L'fxtt.k

MOLE NO.

COMMENCEDFINISHED ^^ PURPOSE OP

MA4-2-76

March 16, 1976Varch 20,J

MANN *4 GROUP Te s t EX—s

Claim P-419741 BQ

PROM

0

21

117.9

4

175

206.4

TO

21

117.9

175

206.4

257.1

DESCRIPTION

Core Mann Twwn&hxp Drilled by: Bradley Bros.CORE SAMPLES j

j FROM

lSUMMARY LOG

Casing.Andesite:

TO

i j

l

21-44.7 - dk gr., e.g., sim. to 'B' type;44.7-47.8 - porphyritic andesite.47.8-60.4 - dk gr., f. g. 'andesite.60.4-99.3 - variably bleached andesite.99.3-117.9 - dk gr., f. g. andesite.

Chert, Cherty tuff and Carbonaceous tuffsequence.

Chert xns: 117.9-118.9; 118.9-122.4;123.6-135.9; 139-146.4.

—————

RECOV. WIDTH

t

1 'i ;

i

i

i

Carbonaceous xns: 122.4-123.6; 135.9-139; jj147.3-155.9; 160-165.4; 170-175.

Cherty tuff: 155.9-160; 165.4-169.1;169.1-170.

\

146.4-147.3 - porphyritic horizon.Feldspar porphyry - with inclusions ofmeta-andesite @ 181.5-185.3 and187.4-189.4.

191.4-193.5 - Band of carbonaceous tuff.

Chert, Cherty tuff and Carbonaceous tuffsequence :

ASSAY !i——————————— P —————————————————————————————————————————————————— -

t

t

——————————— j, ———————————

|

ri:

j;

li

i

it ri i

j j

! '

1 t : ]

: ;s

i

l l

lli

i

i

i

i :

i i; i

j1

i

FORM sil

NOWTM.

CAST -—

ELCV. —

AZIM. —

DIP____

DIAMOND DRILL REPORTMOLE NO.

COMMENCED .

VA4-2-76

or

PROPERTY, MANN GKOTTPHOtE

Mann Township

206.4

257.1

276.8

4

257.1

276,8

404

404

SUMMARY LOG (cont'd)

Chert: 206.4-208.3; 236.6-257.1 (mixed).Carbonaceous tuff: 210.2-236.6.Cherty tuff: 208.3-210.2239-249 - highly fractured.

Meta-andesite .273.6-275.9 - porphyritic andesite.271.7-273 - Anorthosite dyke.

Mafic to Ultramafic Intrusive276.8-298 - gabbroic, nonmagnetic.298-315 - transitional, magnetic.315-400 - pyroxenite.400-404 - serpentinit e.

-

END OF HOLE

FROM

C*

TO

^RE SAMPU1

RECOV.

:s

WIDTH ASSAY

1

jj

ij

1

i

11 a

,

1

"

i

Location of Collar from #2 Post of P-419741FORM S21

30+00 NNORTH ,..,.,,.,,,. ,,

e**T XL 6WfL-Kv- Surface**,M Grid South - 180"

Collar @ -500 ; @ 100' -51W

North 360* West 50'

PROPERTY


MANN f 4 GROUP

MOI-CNO. MA4-2-76 ,-,v~~r ..,- rt, March 16. 1976nu.curn MA Tf h 22 197fi

Hntr Test EM and Mag.

1

S 300' -51. 50BQ Core Mann Township Drilled bv: Bradley Bros.

0

21

4

21

117.9

Casing.

Andesite - which may be subdivided

into a few individual units across this

distance.Up to 44.7, the andesite is dark green

medium to coarse grained and relatively

uniform in appearance. In places, this

section is at least marginal to the 'B'type, coarse flow units in the area.

Although the rock is fairly coarsegrained, the only minerals recognized mega-

scopically are feldspar, chlorite and

hornblende .All along this unit, there are

scattered fine, to hairline fractures of

quartz-carbonate, most of which show a

slight amount of bleaching adjacent to

stringer margins. One wider stringer, at

43.9, carries some coarsely disseminated

pyrite, and has a wider zone (l n ) of

bleaching, adjacent to the stringer margins.

These fine quartz -carbonate stringers are

at variable angles to the core, but most

are fairly shallow (from 30O to 40O ) .

FROM

:

: i 1

ci

TO

5RE SAMPUI

RECOV.

ES

WIDTH ASSAV

———————————

———————————


t1i

i

i

i

i

iif

FORM 322

NORTH.

EAST__

CUEV. —

AZIM. —

DIP™- PROPERTY.


MANN *4 GROUP

note MO.

COMMENCED .

FINISHED ———

PURPOSE Of -

MOLE ———————

MA4-2-76

Mann Township

*

TO DESCRIPTION

44.7-47.8, contact to a narrow unit ofporphyritic andesite. Both contacts ofthis unit are a little irregular, and some what diffuse suggesting that this horizonis probably part of the flow sequence,rather than a dyke. The upper contact isroughly at 35O to the core, lower at 45O .

The porphyritic andesite is grey greenin colour with scattered phenocrysts offeldspar and chlorite to 1/16". Phenocryst.vary from subrectangular to elliptical inshape. As before, there are a few hairlinefractures with quartz-carbonate in thisunit at a shallow angle to the core.

After the porphyritic unit, the andesitebecomes considerably finer grained and darkblackish green in colour. This unit issimilarly cut up by scattered fine fractureof quartz-carbonate, plus occasional widerstringers to h " bearing disseminated pyrite.

At 51.1 - rusty, broken carbonate

stringer.Around 60.4 the andesite becomes much

more variable in nature and there is an

FROM

j -" '

————————————

i

11

!

j

i

i

f

!1

1

3

l

j

cc

TO

5RE SAMPL1

RECOV.

1 ———— '

, ————————————

!S

WIDTH

|

ASSAV j;li

i

IIlt

i

1;

1

l

1

lj!

:\ 1!

———————— j —————————————————————————————————————

l———————— K ————————————————————————————————————

1lil:

j

|i

t

row"* s

NORTH.

CAST...

EUEV. —

AZIM. —

DIP ____

D1AMOHD M il R EPOHT XA4-2-7C

PROPERTY, MANN *4 GROUP

FINISHED

PUWPOSC

HOLE

Mann Township

4

TO

overall increase in the number of stringerspresent. This zone (from 60.4 to 99.3), ischaracterized by lighter green patches ofbleached andesite separated by the darkblackish green andesite as seen in the justprevious unit.

Although there is a marked increase instringer content here, the erratic zones ofbleaching do not appear to be related to anexcess of stringers. It is noteworthy,however, that the marginal bleaching aroundthe carbonate stringers in the blackishgreen andesite is identical in colour tothe wider bleached patches in this zone.The bleached patches, on the other hand,are noncarbonatized - with exception toareas immediately adjacent to the finecarbonate-stringers.

As before, there are a few wider,greyish quartz-carbonate stringers here wit]some coarsely disseminated pyrite - raresplash of pyrrhotite. This zone of coreis also quite blocky in nature.

The lower contact of this variably

i

FROM

1

i

|j ————————————————————————————-;

; 1jf1

l

CC

TO

)RE SAMFUI

RECOV.

:s

WIDTH

———————————

i'

ASSAY !

i

j;

!.

i

!

j -. .IIij

|i

!i

1

j;

;'

'i

li

•jtti

ij!!t

!.

M SZZ

NOHTM.

EAST ——

EI.EV. -.

AZIM. —

DIP———— PROPERTY.


MANN #4 GROUP

COMMENCED -

FINISHED ———

PURPOSE OF.

MOLE ———————

Mann Township

4

TO

bleached zone of andesite is cut by numerouswider stringers of quartz-carbonate withcoarsely disseminated pyrite (over 6") .Associated with this accessory stringercontent and sulphides is some stronger sili cification and buff coloured alteration ofthe rock. Lower contact broken.

At 99.3, return to the dark blackishgreen, fine grained, fairly uniform andesite,as the unit 47.8-60.4. There is a markeddrop in stringer content in this unitalthough a few fine fractures with carbonateand marginal bleaching persist. Several ofthese fine fractures run right along thecore axis producing contorted and ovoidpatterns .

Within this unit, there are a fewblebs of sulphides - much coarser,, and moreconcentrated towards the base. The base ofthis unit, from 114 to 117.9, containserratic silicified patches, black togreyish buff in colour, plus a few blebsand stringers of pyrrhotite-chalcopyrite.

Chalcopyrite is the minor constituent.

FROM

j

B

1

i

cc

TO

)RE SAMPUI

RECOV.

:s

WIDTH

———————————

ASSAV

———————————


|-

|j

l

j

1 .. . .,,,—.,,,,,,,-,,.,.,..,,.,,,.,,.,,, —————————|l . .,, ,,,,,, ,,., ,,,,, ,, .., ———————————————— - ——— —

tj

\

i

i

i

i

HORTM .

EAST ——

et.ev. —AZIM. M

OIC——— PROPERTY.

DIAMOHD DRILL REPORT

MANN f 4 GROUP

FINISHED

Mann Township

117.9

t

TO

175

Lower contact of the andesitic volcanicsis along a pyrrhotite stringer - irregular,but averaging 55O .

Contact to a whole sequence of chertto cherty tuffs, rhyolite tuffs and darkcarbonaceous tuffs. Individual units aregenerally very narrow and usually magneticfrom the presence of pyrrhotite - eitherfinely disseminated or in coarse blebs andstringers. Units include:

117.9-118.9 - Grey to brownish greychert - sugary textured with some finelydisseminated pyrrhotite plus a few coarserblebs and narrow stringers of pyrrhotite-pyrite.

118.9-122.4 - Greyish, to brownishgrey and locally bleached to yellowishcream chert. The chert is sugary .texturedwith coarse stringers and blebs of pyrrhotite± pyrite. Upper contact gradational,lower sharp, slightly banded at 57O .At 122. 1 - few blebs of sphalerite, tracechalcopyrite .

122.4-123.6 - Black, carbonaceous tuff

rROM

., .,,,, ,,

1

;

i

t t

!

i

i

i

i

————1i

|

i

cc

TO

3RE SAMPLI

RECOV.

ES

WIDTH ASSAYDESCRIPTION OF SAMPLE

i

i

l

i

|l

l

j

|

i

i |

'

i

FORM SZ2

NORTH.

EAST ——.

E LEV. —

AZIM. —

DIP ____ PROPERTY.

DIAMOh'D DRILL REPORT

MANN f 4 GROUP

HOLE MO.

COMMENCED .

FINISHED -

KA4-2-76

PURPOSE Of .

MOLE ——————

Mann Township

^

DESCRIPTION

with coarse, irregular blebs and stringersof pyrrhotite - splash of chalcopyrite .Lower contact fairly sharp at 81O .

123.6-135.9 - Dark greyish to greyishbrown and slightly greenish chert. Thechert is locally bleached to yellowish greyin colour, plus there is a faint banding at70O to the core. Most of the sulphides inthis unit are very finely disseminatedpyrrhotite - rare larger blebs or narrowstringers with pyrite. There are also a fevnarrow carbonate stringers and fractures inthis unit.

135.9-139 - Dark grey to black carbon-.aceous tuff with erratic cherty patches.Pyrrhotite in this section is in coarseblebs and irregular stringers with/withoutpyrite. Some broken core here from 138 to138.7 possibly due to the presence of ir regular chloritic fractures. Upper contactbroken, lower sharp, nearly normal to thecore.

139-146.4 - Dark greyish sugary tex-tured chert with an occasional patch of

FROM

120.2

122.5

139.7

i

C(

TO

120.4

122.7

140.0

3RE S AM PU!

RECOV.

ES

WIDTH

r .2

.2

.3


Grab Samples GEM

FORM SZ2

WORTH.

HAST ——

ei.ev. —AZIM. —

Otf ————

D1AMOHD mil R EPORT

PROPERTY. MANN #4 GROUP

•-Oi-t "O.

COMMENCED .

FINISHED ——-

PURPOSE OF .

MOLE ———————

.".A4-2-76

Mann Township

TO

black, carbonaceous material. A couple ofcherty fragments to V size were noted nearsome of the carbonaceous patches. Somenarrow carbonate stringers at 10O . Pyrrhotiteis the only sulphide noted, and is veryfinely disseminated.

146.4-147.3 - Broken contacts to agreenish porphyritic horizon. This sectionis weakly chloritic and fairly well sili cified. The core here is speckled withvery fine (to 1 mm) subrectangular pheno-crysts of feldspar plus a few fine blebsof chlorite.

147.3-155.9 - Black carbonaceous tuffgrading to black carbonaceous rhyolitictuff around 150, where scattered quartzphenocrysts are first noted. Up to 150only a few fragments are noted. .After 150,however, numerous ghost fragments to 1/16"size are noted, producing a general lineationat 610 to the core. This unit is moderatelmagnetic from numerous tiny blebs and finedisseminations of pyrrhotite. There areoccasional fine stringers of pyrrhotite as

1 iFROM

-

1 115118

1 120123125130

1 135j 140i 145

! 150155

i 160165

i 166170172

IT 175

; i

cc

TO

118120123125130135140145150

155160165166170172175180

JRE SAMPL.I

RECOV.

ES

WIDTH

323255555

55514235

ASSAY

|

Andesite - ID'S po tr.cpChert - 7% po pyChert et al - 171 po py tr.ZnS cpChert et al - 7% poChert - 51 po pyChert - S1* po pyChert et al - 121 po py tr.cpChert - 7-101 fine po

l Chert et al - 7-101 po py spl.cp! D^t - 12-151 po py spl.cpi Dit -f cherty T. - 51 po pyi Carbonaceous - 101 po py

" 251 " "Cherty tuff - minor po pyCarbonaceous - 151 po py

i " 71 po py1 Porphyry - very minor po py

;

i

szz

notrrn .CAST ——

ELEV. —AZIM. —


DIAMOKD DRILL REPORT

MANN # 4 GROUP

VA4-2-76

PURPOSE Of

MOLE

Mann Township

FROM TO DESCRIPTION

well, plus a few slips with pyrite.155.9-160 - gradational contact to a

zone of dirty chert, or cherty tuff. Thisunit appears to coalesce with the preceding

CORE SAMPLES j

FROM

l

carbonaceous horizon. The cherty tuff isgreenish to brownish with a few, veryscattered fine blebs (fragments?) of ichlorite to 1/16". Lower contact broken -

i appears normal to the core. jj

160-165.4 - Black, carbonaceous tuff -jsimilar to the previous rhyolitic tuff with;ghost fragments, but this zone is withoutquartz phenocrysts. There is a similarweak lineation at 6 O0 to the core. Fineblebs and very finely disseminated pyrrhotite± pyrite may be found throughout this unit- the basal portion, however, being charac terized by subparallel stringers . of pyrrhotitwith splashes of chalcopyrite, at 80O-90Oto the core. Lower contact at 90O .

165.4-169.1 - Greyish green, dirtycherty tuff (?) with light, cherty and dark,chloritic ghost fragments to 1/8" in size.

;

. ————— . . . ..

Fragments are crudely spherical in shape, :

TO Recov.

1i

WIDTHh utsi-Kir i ion t>^ SAMPLE

ASSAV j'i

i————————— | ————————————————————————————————————————————

i

l!

j'

]

i;

ij

j

{i

J:

i:

jil

1!

i!'iii ij1! i1'

row** szz

NORTH

EAST ——

CLCV. —

AZIM. —

DIP ____ PROPERTY.


MANN 14 GROUP

HOLE wo.

COMMENCED .

FINISHED . .. -

PURPOSE or -HOLE _______

XA4-2-76

Mann Township

4

\ —————

TO

often with diffuse margins. The matrix isjjreyish green to brownish, sugary texturedand cherty with traces of chlorite, feldspa:and tremolite (?) . Lower contact sharpalong a hairline carbonate stringer at 73O .Effectively negligible sulphides in thisunit.

169.1-170 - Much darker grey, dirty,cherty tuff with well developed, crudelyspherical blackish green fragments to 1/8"in size. The matrix here is a bit morecherty than the just previous unit andthere is also a moderate amount of finelydisseminated pyrrhotite.

170-175 - Dark grey to black carbon aceous tuff with one section from 172.3 to173.4 bearing numerous ghost fragments toh" in size. Ghost fragments are seenelsewhere in this zone, but are not asnumerous nor as well developed as thesection 172.3 to 173.4. Pyrrhotite isfinely disseminated, locally in coarserblebs and narrow stringers.

FROM

r

li ————

GC

TO

3RE SAMPl.

RECOV.

ES

WIDTH

II

ASSAY i

1

li

i!iil!l!

li

1

1

t

|l

,1

|

|!

j!i

i

iiii

'i

row** szz

NOHTM.

EAST __

ELEV. —

AZIM. —

DIP ____ PROPERTY.


MANN # 4 GROUP

FINISHED -—

PURPOSE Or

HOLE

Mann Township

175

.

TO

206.4 Broken contact (over 6 ") , to feldsparporphyry. The porphyry is brownish grey toqreyish green in colour with coarse whitephenocrysts of feldspar up to 1/16" in size.The matrix of the porphyry is very chertyand fine grained to nearly amorphous.

Within this whole zone, there are 3apparently conformable units of volcanics.The porphyry, however, is not chilled orfiner grained around two of these zones(181.5-185.3, and 187.4-189.4) suggestingthat these volcanics may be includedmaterial.

These first two zones are medium tocoarse grained me ta- andesite. In bothcases, the andesite is much finer grained,baked and cherty within 6" of the porphyrycontact. The porphyry in turn shows novariation in grain size approaching theseunits, in fact the coarsest part of thewhole zone of porphyry is noted at thecontact of the first unit - at 181.5.

The andesite is medium to dark greenin colour with several metacrysts (?) of

FROM

"

1

CC

TO

3RE S AM PU!

RECOV.

:s

WIDTH

t

——————————— 1 DESCRIPTION OF SAMPLE ASSAY i

li

j——————————— ( ———————————————————————————————————————————————————

i1

)

i

i

i

1

1

i

1

i

i

FORM S22

NORTH.

EAST ——

EUEV. —

AZ1M. —

DIP ____ PROPERTY.


MANN *4 GROUP

VA4-2-76 11.COMMENCED .

riNlSMEO -PURPOSE of -MOLE ———————

Mann Township

--J^ROM

"— - '

A 206.4

TO

257.1

DESCRIPTION

of feldspar, hornblende and chlorite seenin the central parts of these units. Theinclusions are effectively unmineralized.

A third zone from 191.4 to 193.5 con

HCORE SAMPLES |

FROM

190sists of black carbonaceous tuff with minor|| 191.5cherty material. The contacts with theporphyry are nearly normal to the core and Jithere is a slight decrease in grain sizeof the porphyry approaching this unit. Thedark carbonaceous unit carries coarse blebs———————————————————————————————————— i, —————and stringers of pyrrhotite-pyrite and is jcrudely lineated at 80O to the core. i———————————————————————————————————————————————— (! ——————

The porphyry is locally cut up by finej!carbonate fractures along the core whichshow some marginal bleaching. Sulphides(mainly pyrrhotite) , are also scattered invery minor amounts throughout the porphyry.

Lower contact of the dyke very slightlfiner grained over 6" - contact @ 56O .

Return to the sequence of cherty andcarbonaceous tuffs seen just previous tothe feldspar porphyry intrusion.

f

207. 8

TO

191,5193.5

RECOV. WIDTH

1.52

Util-KIMI ION (J* S*AMPI.t ASSAY

|i

i

; ; Porphyry - trace po pyf Carbonaceous - 8% po pyi

jit

iti] 1 1 i

i

208.1 .3

t-

lii

i'.i

l!1

H i

; Grab Samples CDM

lii)

209.7 210.0 .3 i!206.4-208.3 - Grey cherty unit with i 211.0 211.3 .3 i

FOWM sil

NORTH.

EAST —.

E1.EV. —

AZIM. _

DIP ____ PROPERTY.

DIAKOHD DRILL REPORT

MANN #4 GROUP

HOLE NO.

COMMENCED .

FINISHED ———

PURPOSE OF-

HOLE ———————

MA4-2-76 12.

Mann Township

TO

1

coarse blebs and irregular stringers ofpyrrhotite.

208.3-210.2 - Broken contact @ 68O todark grey green cherty tuff with lighterghost fragments to 1/8" size. Only minimalpyrrhotite seen in coarse blebs. Lowercontact very irregular.

210.2-236.6 - Whole zone of dark greyto black carbonaceous (some graphite?) tuffwith only minor cherty material near thebase. The tuff is well mineralized withcoarse blebs and irregular stringers ofpyrrhotite ± pyrite. Traces of chalcopyritewere noted in a few stringers, and occasion ally along slip faces. The core is moderateto strongly magnetic.

229-235 - Blocky.236.6-257.1 - Sharp contact at 80O to

a whole zone of chert to cherty tuff, whichin places is thoroughly fractured andbroken. This zone varies in colour frompale greenish to cream coloured, grey andbrownish grey. Fine pyrrhotite, with onlyisolated coarser blebs or stringers is

FROM

206.5

210

215

220

225

230

235

240

245

i 250

255

1

cc

TO

210

215

220

225

230

235

240

245

250

255

260

)RE S AM PL!

RECOV.

ES

WIDTH

3.5

5

5

5

5

5

5

5

5

5

5

ASSAY

——————————— 1

i

! Carbonaceous - S-7% po! " 12 s?; po py tr.cp

" 8% po py tr.cp" 12* po py

1 " l(ft po py" 10% po py

l Carb * Chert - minor po1 Chert - minor po py! Chert - 5% po pyChert - S-5% po py

j Chert et al - minor po py

i

i

i

i

|i

NORTH.

EAST ——

ELEV. .

AZIM..

DIP__ PROPERTY.


MANN #4 GROUP

KA4-2-76 13.COMMENCED .

FINISHED ———

PURPOSE or .

MOLE ———————

Mann Township

FROM

257.1

*

TO

276.8

DESCRIPTION

characteristic of this unit.Most of this zone, but particularly

CORE SAMPLES

FROM

from 239 to 249, is fractured with open jjfractures bearing dark blackish greenchlorite and minor serpentine (?) . Alteredvuggy carbonate stringers also contributeto the amount of broken core here.

Broken contact to meta-andesite.The andesite here is medium to dark

green and grey green in colour and fairlywell silicified. No individual bands ofchert are noted within this unit, butcertain sections of andesite, particularly

__________

near the upper contact, are very hard and jcherty in nature.

The andesite is medium to coarsegrained and rather granular to sugarytextured. After 260, metacrysts of feldspa:hornblende and chlorite (after hornblende?)are noted along some fresh surfaces. Themosaic pattern of many surfaces (quartz andfeldspar?) plus the presence of a felted

'r

j

TO RECOV. WIDTH

j

i l . . . .

j

mineral (tremolite?) , make many mineral I i

ASSAV

1; DESCRIPTION OF SAMPLE,

:

i

j

————— i —————————————————————————

iiii .... ,.,....., - .1

——— , —————————————————— P!i

l

'

i

li

row** szz

NORTH.

EAST —.

Et-EV. —

AZIM. —

Off ———— PROPERTY.

DIAKOHD DRILL REPORT

MANN #4 GROUP

MOLE NO.

COMMENCED . FINISHED —^

PURPOSE or ,HOL.E _______

MA4-2-76 14.

Mann Township

276.8 ,

TO

404 '

determinations difficult, however. Onlyvery minor fine pyrrhotite was noted.

273.6-275.9 - narrow unit of porphyritandesite. This section is characterized bynumerous tiny (to 1 mm) laths of feldsparplus a few blebs of hornblende and chloriteContacts are broken.

271.7-273 - Broken contacts to a narro'unit of milky white feldspar with medium todark green chlorite - anorthosite. The coreis quite badly broken here with fine, openchlorite-serpentine slips.

The lower contact of this whole unitof andesite is broken.

Mafic to ultramafic intrusion, thecontact. with the overlying andesite beingbroken, and not exactly pinpointed.

Up to 281.7, the rock is medium tofine grained and dark brownish to blackishgreen in colour. This section is com pletely nonmagnetic, and from succeedingmembers, a gabbroic composition is suggested.

Following the contact zone, the rock

FROM

.C

j

*

C(

TO

)RE SAMPL.C

RCCOV.

:

:s

WIDTH ASSAY

i

——

,

i*l

row** s**

NORTH.

CAST ——

EI.CV. —

AZIM. —

DIP——-. PROPERTY.


MANN #4 GROUP

MOLE NO.

COMMENCED .FINISHED __ PURPOSE OF .MOUC ———————

MA4-2-76 15.

Mann Township

-

becomes rapidly coarser grained and lighterin colour to grey green and brownish greygreen. This zone, from 281.7 to 298, isgabbroic in composition with pyroxene,tremolite-actinolite and traces of horn blende megascopically visible. Rare tracesof an olive coloured mineral - (olivine) ,are also noted within this zone.

The first part of this coarser grainedgabbro, to 285, is quite brownish in colourfrom the presence of a bronzy brown mineral- bronzite (?). Some scattered white flecksof feldspar are also noted here. After285, however, the gabbro grades grey greenin colour and feldspar is not distinguishedmegascopically, nor is the bronzy mineralas dominant.

At 298.5, a magnetic contact isindicated - the rocks after this pointbecoming progressively more magnetictowards a contact with pyroxenite at 315.Further, the rocks after 298 grade pro gressively darker in colour - transitionalfrom gabbro to pyroxenite. Pyroxene is the

FROM

CC

TO

JRE SAMPLI

RECOV.

:s

WIDTH ASSAYDESCRIPTION or SAMPLE

!

1

|

i

i

i

i

1

'

FORM S2I

NORTH,

EAST ——

euev. —AZIM. —

DIP____ PROPERTY.


MANN #4 GROUP

MOLE M O.

COMMENCED . FINISHED —— PURPOSE OF -

MOLE ———————

XA4-2-76 16.

Mann Township

4

TO

only mineral meqascopically distinguishablehere. The rock is dark green to blackishin colour.

From 315 to 400, the rock is pyroxeniti- black in colour and very strongly magneti*Pyroxene is the only mineral visible otherthan occasional grains of magnetite.

Around 400, the pyroxenite grades a bi'finer grained and blue black in colour.This section appears to be closer to ser pentinite or serpentinized peridotite incomposition. These ultramafics are slightrless magnetic than the adjacent pyroxenite.There are also a couple of slips here withgraphite (?) .

This whole intrusive sequence is cutby scattered open fractures and slipscoated with jade to deep turquoise, and azureblue serpentine. Calcite is usually associated with most of these fractures - eitheras thin coatings or narrow stringers to \ "surrounded by serpentine.

Sulpnides in tne intrusion are relative!: rare with only a few blebs of pyrrhotite --pyrite noted in the section 308.8-313.9.

FROM

s

t.f *

*"

j " ' " '

i

ri

310

j —————

cc

TO

ns

)RE SAMPUS

RCCOV.

i

:s

WIDTH

S

ASSAY

———————————

-

i

i

i

j

Transit-ion M^-TC-i - vr*ry L minor pQ-py

l

———————————————— X? /i —— ,. j. ***y ——— .j (JJJWV^D^ l -- -

j......... ...... .... —— ..... .... ...... . ———— - — .... ———————— . ......

404 END OF HOLE

FORM szi

NORTH. EAST ——

ECEV. —

AZIM. —

OIP ———


PROPERTY. MANN GROUP

MOLE H O.

COMMENCED .

FINISHED __-

PURPOSE o r .MOCE ———————

MA4-2-75 17.

Mann Township

FROM

,

TO

22.5

48

67.5

87

102

132

280

305

340

379

403

DESCRIPTION

Au -f Geochem Samples

CORE SAMPLES j

FROM

Fairly coarse grained andesite - close to j'B 1 type - dark green.

Grey green feldspar porphyry - porphyriticandesite with white euhedral feldspar phefio-crysts and black fragments and/or phenocrysts.

Bleached, greyish fine grained andesite to. — n ——— dacite with a seam of py. jj

i Dark green, fine grained andesite - ghosts jof fragments, with fine fractures and \minimal bleaching. i

Dark green, fine grained andesite - some ivery fine bleaching, chloritic slips - jsimilar to sample @ 87'.

Medium to dark grey cherty horizon (tuff?)some faint banding at 45O-50O .

Medium grained gabbro - dark brown greenin colour.

-

Transitional zone - coarse grained gabbro (?j)11to pyroxenite, magnetic. i

Black pyroxenite.

TO RECOV. WIDTH

1

j

i t

| 1

1

ASSAYi.

i

ii

liii

i—— , ————————————— iji

i. i i'

1 i

i l i

r!

i.

j.

|

i; i

j( -

Black, magnetic pyroxenite. ! ; ' j 1Serpentinite, fine arained, blue black, ; ; 1 '

f

magnetic.

hole np foo t ago date note · location of collar from f3 post of p-326399 foftm sz2 north . east...

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