p,it 63-545-0 (onn-^-c-03

14
42J*4SEM25 19 PIVABISKA RIVER 010 DIAMOND DRILLING AREA: PIVABISKA RIVER REPORT NO: 19 WORK PERFORMED FOR: Noranda Exploration Co. Ltd. RECORDED HOLDER: Same as Above [xx] : Other [ ] Claim No. P 802232/ 802235 Hole No. FR-88-7 Footage 276.15m Date June 88 Note (D NOTES: (1) W8906-305, date filed June/89 (3) 0^1'^"^ Ma"Ur,a l tcv^ b P,It 63-545-0 (onn-^-C-03 epo4 Or, Dr. /A n^^Sfc y s ^r

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Page 1: P,It 63-545-0 (onn-^-C-03

42J*4SEM25 19 PIVABISKA RIVER 010

DIAMOND DRILLING

AREA: PIVABISKA RIVER REPORT NO: 19

WORK PERFORMED FOR: Noranda Exploration Co. Ltd.

RECORDED HOLDER: Same as Above [xx]: Other [ ]

Claim No.

P 802232/ 802235

Hole No.

FR-88-7

Footage

276.15m

Date

June 88

Note

(D

NOTES: (1) W8906-305, date filed June/89

(3) 0^1'^"^ Ma"Ur,a l tcv^ b

P,It 63-545-0 (onn-^-C-03

epo4 Or, Dr. /A n^^Sfc y s ^r

Page 2: P,It 63-545-0 (onn-^-C-03

LA

TIT

UD

E.

t 2.00 C

DE

PA

RTU

RE

ELE

VA

TION

.

6.0

0

N

NO

RA

ND

A E

XP

LOR

ATIO

N C

OM

PA

NY

LIM

ITE

D

DIA

MO

ND

DR

ILL CO

RE

LOG

Protect N

o. .2

77

Hole N

o..

Su

rfac

e

DIP

AT C

OLLA

R-4

5"

BE

AR

ING

.180"

Ten

Deoin

12.19

Dip

-46"

Mjq

neiic

D

inin

gC

orrected B

ellin

gP

roperlyP

ivab

iska

Riv

er

3-8

4

76.20

TOTAL DEPTH

27

6.1

5CORE SIZE .

BQm

.23-4

2"

228.60 -40"

CORE STOR

AGE.

REMARKS —

Aunor Minesite,

Timmins, Ont.

276.15 -40"

NTS 42

J ^p

Pivabiska

R.. Area.... Mo

^p

B02232

D.,e

i,.r,ed

1

0/0

6/8

8_

__

__

__

__

__

co

mo

,,,.,, 13/0

6/8

8_________

,lrlclo, Norex

Drilling Ltd.__________

S. Parker

Com

Denin A

Lunoiogy

Oesen

otio

n (co

lou

r, grim

sue. te

nu

re, stru

cture, etc.)

Atte

ntio

nM

me

raiita

tion

OW, A-i

. ' AL SURVEY

0-11.58

11.58-58.86

Amphibolitic

Silicified

Mafic Volcani

Overburden (casing)

Dark green

with light

green siliceous

bands, fine

to medium grained,

moderate to

strongly developed

foliation e

40-50 to core

axis-strongly

amphibolitic with intervals

of medium

grained, recrystallized?

subhedral to

euhedral amphibole

crystals within

a cjtz

rich matrix.

Minor dark brown, fin*

grained, micaceous

bands within m.g. amphibolite,

-occasional whit*

concordant gtz/calcit* veins

and discordant, irregular

(deformed) gtz/calcit* veins

and stringers

e.g., 9

21.78m.-trace

(sporadic), medium-grained,

purplish anhedral

garnet crystals

e.g., 23.19m

12.65-12.82m: broken

core 18.17-18.33m:

abundant gtz/calcite

in irregular veins,

minor pyrrhotite disseminated

in mafic component.

(P 21.94m:

lcm gtz

bleb surrounded by

calcite@

28.58m: several

medium grainedgarnets

within calcite vein

-black mineral? in

veins 28.90-29.66m:

interval exhibiting dark

brown micaceous bands within m.g.

amphibole rich

rock.

-amphibolite, chlorite

and minor

micaceous ninerals

(biotite)-local

light green,

silicified zones

g., 26.15-26.21m

-carbonate (calcite)

is found

in association

th many

of the

gtz veins.

l

-trace medium

to fit

grained subhedral

pyrrhotite blebs

within core,

(rock is

weakly magnetic) 0

12.18m: medium

grained, anhedral

pyrrhotite bleb adjacent

to anhedral

pyrite bleb within

cor*.-minor

fine grained

anhedral, disseminated

pyrite.

R

(J 1389

C E l V E D

Page 3: P,It 63-545-0 (onn-^-C-03

NO

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MP

AN

Y LIM

ITED

DIA

MO

ND

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ILL CO

RE

LOG

Protect N

o.277

Hole N

o

Dem

n 4

Urnoloqy

Descrtoiion (colour, grain site, ten

ure, structure, etc.)

58.86-98.33

SilicifiedMetasedimen(Greywacke?

with Graph!Interbeds

-amphibole crystals

produce crenulation

texture (ie.,

intense micro

folding) '

6 30.58m:

medium grained black mineral?

within gtz/calcite

vein (trace

garnets) 39.68-40.30m:

mg, amphibole

rich vol,

with interstitial

qtz, trace

calcite-2cm

irregular clusters

of large

grainedamphibole

mosaics consisting

of approx.

90* amphibole,

10* gtz.

Fragments of

the a"Bove

m.g. vol.

occurwithin

the f.g.

vol. eg.,

44.10m (flow

texture?)44.67-44.78m:

light grey,

altered cherty

(silicified) zona with minor disseminated

pyrrhotite/pyrite.

-Light grey to

bluish, fin*

to medium

grained, strongly

developed foliated

8 35-45

to core

axis.-contains

black intervals

of graphitic

argillaceous metasediment eg.,

978.95m-locally,

small scale

folding developed

in foliation-minor

bluish gtz

veins and

fragments e.g.,

8 79.80m and

75.85m respectively.

Pfooeriy

Pivabiska

River

3-84

Alteratio

n

49.18-49.25m: light

grey silicified

zone similar

to that

from 44.67-44.78m.

-moderately silicified

and locally

argillaceous-strongly

graphitic in

sections

Mineralization

Hem

ams

9 50.0m,

minor pyrrhotite associated with

gtz/calcite vein 9

51.31m, medium grained

anhedral pyrite/pyrrhotit s

located adjacent to a calcite vein.

t

852.28m:

minor anhedral

pyrrh

otite.(w

eakly

m

agnetic)

-locally

up to 21

combined

fine

to

medium

grain

ed,

anh

edral

pyrrh

otite

/ pyrite

in

clu

sters

and dissem

inated

e.g

., @

61.58m-p

yrrh

otite

is

stron

gly

m

agnetic.

- listinct co

lou

r c lange

from green

grey at co

ntact

sections

of uiit m

ay be s efficien

tlyra

ph

itic to

be

conductive 5 ourcec o

ntrib

utin

g to

th

e

HLEM

z n

om

aly.

Page 4: P,It 63-545-0 (onn-^-C-03

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RE

LOG

Oeoirt ft

Uinoioqy

Descnoiian (colour, grain su

e. texture, structure, etc.)

98.33-102.3

Silicified

Metasedimen

(Greywacke?

58.86-59.13m: light brown

interval, -

transition into metasediment

Q 67.65m:

lent chloritic vein,

containingminor vugs

and It

pyrite77.72-85.04m:

argillaceous graphiticinterval

with up

to 5*

pyrite, no

pyrrhotite.

9 81.36m:

green amphibolitic

fragment ("2cm)

within metasediment.

92.97-93.20m: white

siliceous interval*

93.65-93.75: graphite

(broken core)

9 94.31:

gtz/graphit* (deformed)

94.2-95.43: graphite

(broken core) 0

96.78: white

calcite veining

-Light grey,

medium grained,

massive to weakly

developed foliation

S 30

to core axis

-abundant qtz

lenses define

foliation-locally,

foliation parallel

to core

axis '

99.45-99.50: blue

qtz vein 99.50-100.30:

dark argillaceous

interval within

light greywacke.

Alteratio

n

-high silica

content-abundant

chlorite on

cleavage planes

i No.

Moir N

eFR

-88-7

Pro

otrry

Pjv

ob

icl.?

Min

era

lizatio

n

-locally, 21

pyrite as

anhedral medium

grains, and

fine grained

anhedral pyrite

stringers. 8

63.40m: area

of abundant

pyrrhotite

77.72-85.04: up

to 51

pyrite in

medium sized

aggregates forming

bands parallel to

foliation.-pyrite

nodules at

81.45m.95.91-96.20m:

up to

51 fine

grainedeuhedral

pyrite in

veins (this

intervalis also

gtz-rich)

-minor, fine

grained subhedral

pyrite-minor

disseminated fine grained,

euhedral pyrrhotite

and sheared

pyrrhotite on

cleavage planes

(pyrrhotite is

magnetic)

Rem

arks

po pyrrh

otite

argillaceo

us

inte

rvals.

lyrrh

otite

icreases and

p 'rite

increases

a i you m

ove dow

n t lis

unit.

Page 5: P,It 63-545-0 (onn-^-C-03

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D

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ND

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ILL CO

RE

LOG

Sn

*ti Ha

-OF

.

De

em

A

Uin

oio

gy

ffoieci H

a.

Pio

oerty

277M

oir No

FR-8B

-7

Pivabiska River

3-84

OescriD

iion (colo

ur, g

rain s

ite, textu

re, structu

re, etc.)

102.39-108. Silicified

Micaceous

Hetasedimen

108.80-196. Anphiboliti

Mafic Volca

.1

Dark grey,

fine to

medium grained, massive

to weakly developed

foliation 3

35-40 to

core axis,

-minor qtz

veins parallel

to foliation,

-minor calcite

associated qtz

veins.-locally,

minor medium-grained

anhedral garnet

crystals eg.,

102.22m-minor

amphibolitic intervals

eg., 106.50m

105.48-106.05:} 106.60-107.16:)

Broken core

107.73-107,83:}

Dark green,

with brown

micaceous bands,

fine to

medium grained,

massive to

weakly ic

developed fabric

0 35-45

to cor*

axis.-fabric

is defined..by brown micaceous bands,

gtz/calcit* veins, and allignnent

of amphibole crystals

-first 4.5m of unit

contains abundant qtz (minor

calcite) stringers and

irregular veins.

Quartzy veining is present,

although less

abundant past this interval.

113.45-113.55m: qtz/calcite vein

114.11-118.83m: example

of massive, homogeneous,

amphibolitic vol with

little gtz

veining.-texture

similar to

that from

11.58-58.86-euhedral

amphibole crystals

are common

in m.g. sections.

highly amphibolitic

minor micaceous

minerals-trace

calcite-minor silicification

-minor (locally

l*) anhedral

disseminated-pyrite

and sheared

pyrite on

cleavage plane:

-minor, medium

grainedanhedral

pyrrhotite and

pyrite blebs.

.

-similar to

that from

11.58-58.86

Page 6: P,It 63-545-0 (onn-^-C-03

Deo

tn 4

U

ino

ioq

y

NO

RA

ND

A E

XP

LOR

AT

ION

CO

MP

AN

Y U

MITE

D

DIA

MO

ND

DR

ILL CO

RE

LOG

Descrip

tion

(colo

ur, g

rain size, textu

re, structu

re, etc.)

-abundant (*5*)

irregular, wispy

qtz/ Fe-carbonate/calcite veins,

blebs and

stringers eg.,

6 131.28

-abundant medium grained

(recrystallized?) amphibole

bands created by a mosaic

of euhedral

amphibole crystals

eg., 9

145.85 f

170.14: i/2cm wide wavy

qtz/carbonate vein.173.52-176.59;

green, medium grained,

massive, recrystallized

amphibole, mica

qtz-rich volcanic. Becomes

finer grained

towards lower contact.

Very distinct differences

over the

finer grained,

foliated, amphibole-rich volcanic.

0 178.34:

4cm irregular gtz/Fe-carb bleb

9 179.90:

pinching and swelling m.g.

amphibole band*

189.58-189.67:

192.42-192.49:

qtz/calcit* veingrey

qtz vein 193.10-193.43:

strongly foliated

interval i

40 to

core axis

(sheared pyrrhotite on

cleavage planes)

193.94-195.16m: foliated,

amygdaloidal, siliceous,

amphibolitic vol. -medium grained

(qtz?) amygdaloids

195.16-196.63: silicified,

altered zone

with minor py/magnetite 9

195.56m and an

increase in pyrrhotite/pyrite down section

Alteratio

n

-highly silicified.

• OF ,

,277H

oi* N

oFR

-8B-7

Pivabiska River

3*84

Min

era

lizatio

n

132.14-132.64:

up to

30* massive pyrrhotite,

3* medium sized anhedra

pyrite blebs

-zone is

highly magnetii due

to pyrrhotite

-abundant calcite

162.46-162.82: minor

fine grained

euhedral to

subhedral white

sulphide mineral

(arsenopyrite?)

-trace chalcopyrite

blebs at

179.78

Remarks

-up to

3* pyrrhotite

in veins and

disseminati throughout.-medium

sized anhedral

magnetite crystals with

associated pyrite.

Page 7: P,It 63-545-0 (onn-^-C-03

NO

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ILL CO

RE

LOG

Dra

in ft

Uin

oio

qy

196.63-211.

Sulphide Ircn

Formation

(MassivePyrrhotitePyrite,SilicifiedZones

and Qtz)

Descrip

tion

(colo

ur, g

rain size, textu

re, structu

re, etc.)

-brown pyrrhotite,

bronze pyrite,

white to

milky quartz,

green silicified

zones and

mafic components,

fine to

large grained

sulphides, predominantly massive

with local

zones of

weakly developed

fabric f

50 to

core axis,

(a very

homogeneous interval)

202.44-204.93: highly

altered, brown

to green,

fine grained

silicified volcanics,

moderately developed foliation

9 50

to core

axis. Total

of 81

combined sulphides

(pyrrhotite >

pyrite) within

gtz rich

mafic volcanics.203.86-204.38:

silicified, mafic vol

with a

fine network

of gtz/carb veining producing

a brecciated texture.

No sulphides.

9 209.96:

lea Fe-carbonate fragment

within massive

pyrrhotite interval.

9 211.48:

folding of gtz/mafic bands near massive

sulphide/mafic volcanic contact.

-the mafic

intervals are

highly silicied

196.63-202.44: 80*

massive pyrrhotite,

12* medium to

large grained

anhedral pyrite

blebs and

nodules, St

medium to l

arge sized

gtz eyes,

trace mafic

components. Pyrite

and gtz

gives rock

a spotty

texture. 199.31-199.69: siliceous

interval with

only 30t

pyrrhotite, S*

pyrite. The

remainder i*

silicified mafic

vol.

204.93-209.03: silicified volcanic wit) sulphide

content increasing

drastically towards

bottom of

secti Abundant

gtz veins

and blotches.-5*

sulphides grading

into massive sulphides

(pyrrhotite/pyrite) similar to that

from 196.63-202.44. 209.03-211.70m: massive

sulphide interv

similar to that

from 196.63-202.44. Pyrite

modules occur

locally and

are not

evenly distributed

throughout the

massive

This unit

represents the

Drincipal cause

af the

near :oincident

HLEM and

magnetic anomalies.

n.yrrhotite

Page 8: P,It 63-545-0 (onn-^-C-03

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LOG

Sn

vri No

Protect No

27

7M

oir N

oFR

-88-7

-OF

.

Pro

piriy

Pivabiska River

3-84

Oeotn ei

Litnoiogy

Descrtonon (colour, g

rain su

e. texture, stru

cture, etc.)

Alteratio

nM

ine

raliia

tion

Rem

ans

21

1.7

0-2

76

.15

Silicified

AmphiboliticMafic

Volcanic

Light green,

fine to

medium grained, weak

Q to

moderately developed

foliation e

30-45 to

core axis.

-abundant qtz,

qtz/calcite veins and

stringers, generally

paralleling foliation

-locally, small

intervals (10-20cm)

contain massive

sulphides (po)

similar to previous

unit, eg.,

215.77-215.96 and

irregular po/py bands

interbanded with the

volcanics eg.,

213.36-213.47 218.82-218.88:

milky qtz

vein-minor

vugs in

pyrite vein*

eg., 9 212.35

229.52-232.95: medium

grained, strongly

foliated (recrystallized?)

amphibole rich,

with minor micaceous

minerals. Similar to

medium grained texture

noted in

first unit.

Silicified, minor

qtz/calcite stringer

stockwork, and

trace fine

grained po/py blebs.

229.96-230.02: heavily

silicified interval.

232.95-234.51: dark

grey, fine

grained, foliated,

silicified, highly

altered interval

with abundant

qtz/calcite veins.

Tight folding

of qtz

veins S

233.55m. Light

green, carbonated

(calcite-rich) breccia

texture from

233.77-233.85. g

252.47: medium

grained black mineral,

weakly magnetic

(magnetite?) 254.06-254.24:

altered qtz/carbonate

veining260.28-260.44:

80* milky

qtz, minor

calcite, minor pyrrhotite

veining. 262.43-262.46:

milky discontinuous

qtz vein

moderately silicified

strongly amphibolitic

calcite is

associated ith

the majority

of f

qtz veins.

-local intervals

of massive

pyrrhotite, 51

pyrite, and

minor amphibole

blebs eg.,

215.77-215.96-locally

2* fine

grained pyrrhotite

in veins parallel

ing foliation

eg., 8

212.76-locally,

l-4cm sized

irregular pyrrhotite/ pyrit* clusters

eg., 219.48215.52-215.60: massive

pyrrhotite similar

to that

from 215.77-215.96 220.12-220.16: massive

pyrrhotite

minor irregular

pyrrhotite/pyritediscontinuous

veinsand

stringers.227.85-227.88:

pyrrhot teminor pyrite blotch238.29-238.33:

irregular pyrrhotiteblotch.239.14-239.16:

pyrrhot .teminor pyrite v

ein

242.03-242.06: pyrrhot .te

minor pyrite vein.

256.53-257.15:

up to 3

-similar to that

rom 11.58-58.86

Ithough contains

iore sulphide

nineralization-calcite moreabundant than?e-carbonate

Page 9: P,It 63-545-0 (onn-^-C-03

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LOG

i NO277

Sri**i NO. "

OF

FR-88-7M

oir No

Pivabiska R

iver 3-86

Deoin 8.

Liinoiogy

276.1

5

Deserioiion (co

lou

r, grain

sue. textu

re, structu

re, etc.)

270.16-270.37: qtz/calcite vein with

minor mafic minerals, pyrrhotite

and pyrite.

272.79-273.10: pinching and swelling,

'lea wide calcite vein trending approx.

parallel to core axis.

End of Hole.

Alteratio

nM

ineralizatio

nR

eman

s

This texture

is exhibite l

locally in

other section

268.24-268.30: 70*

pyrrhotite, 30*

minor calcite/qtz,

mafic component.

Page 10: P,It 63-545-0 (onn-^-C-03

•r*

eon

UJo oc\i

l l

P8O2232

Q90*

FR-BB-7

P 802235

P 80223

P 802234

-BLO

Pivabiska River 3-84 (Grid "G")

Collar Location: 50m North and 2OOm East of *3 Post P8O2232 Grid Co-ordinates: L2.OOE/6.OON Azl8O0 af-45*

at visio

POOJ M? 277MT.S.o*G. H;

LOCATION PLAN D.D.H. FR-88- 7

PROJECT: EOX RIVERsutvtrioiri.OAAWM Ifi——

OATnAUO/88- . son. riO.QOO

NORANDA EXPLORATION CO.LTDomen.

Page 11: P,It 63-545-0 (onn-^-C-03

inistry of Northern Affairs and Mines

Report of Work

JUMENT6906*

OntarioMining A 42J84SE8825 19 PIVABISKA RIVER 90©

Name at- ,tal Address of Recorded Holder

Noranda Exploration Company, Limited (no personal liability)

Suite

Prospector's Licence No.

A-34387

1300-4 King St. West, Toronto, Ontario M5H 1B6Summary of Work Performance and Distribution of CreditsTotal Work Days Cr. claimed

for Performance of the following work. (Check one only)

[~~| Manual Work

J Shaft Sinking Drifting or other Lateral Work.

J Compressed Air, other Power driven or mechanical equip.

j Power Stripping

Diamond or other Core drillingLand Survey

All the work was performed on Mining Claim(s): P-802232 A 802235

Required Information eg: type of equipment. Names, Addresses, etc. (See Table Below)

Contractor: Norex Drilling Ltd., P.O. .Box 88, Porcupine, Ontario

Date Drilled: June 10 to June 13, J988_____.

DDH f FR-88-7

Bearing: Az 180 0Dip: -45 0Size of Core: BQLength: 276.15m (906.0 ft)On Claim No.: P-802232*235 feet k

ONTARIO GEOLOGICAL SURVEY"ASSESSMENT FILES

OFFICE

JUN O

RECEIVED

RECORDED

OCT 13

P-802235-*671 feet.t

Credits to be filed late*-: 906-340 = SS6- days i

Core stored at 60 Shirley St. So, Timmins, OntDate of Report

. Oct. 11/88Recorded Holder or Agent (Signature)

Certification Verifying Report of Workl hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person CertifyingR.C. Denommee, P.O. Box 1205

Timmins, OntarioDate CertifiedOct. 11/88

Certified by (Signature)

Table of Information l Attachments Required by the Mining Recorder

Type of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed air, other power driven or mechanical equip.

Powtr Stripping

Specific information per type

Nil

Type of equipment

Type of equipment and amount expended. Note: Proof of actual coit mutt b* submitted within 30 days of recording.

Other information (Common to 2 or more types)

Names and addresses of men who performed manual work/operated equipment, together with dates and hours of employment.

Name* and addresses of owner or operator together with dates when drilling/stripping

Attachments

Work Sketch: these are required to show the location and extent of work in relation to the nearest claim post.

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