RECORDED HOLDER: SAME As ABOVE : OTHER l l€¦ · 172.10 173.50 174.65 175.70 172.10 173.50 174.65...

;

DIAMOND DRILLING

Fourbay Lake

WORK PERFORMED FOR: Falconbridge

RECORDED HOLDER: SAME As ABOVE : OTHER l l

52je2SWM25 52J02SWM17A1 FOURBAY LAKE

Report No: 36

010

CLAIM No,PA 475234

Tot A L

HOLE No.KB-62 KB-64

FOOTAGE189m 172m

DATE

Nov/85 Nov/85

NOTE

(l) (l)

NOTES; (i) #33-86

LOCATION Q +20E/1+Q5S

R.B. BandLOGGED BY.

FALCONBRIDGE NICXcL MINES L'JyilTZDDIAMOND DRILL RECORD

_____DiRFfrrioN N 02 0 E______ ™o -45'

3.65m.CASING. SHEET No.

fT Mn . KB-62

l

STAPTFH 1 0-11-85 .CORE SIZE. NO .CORRECTED TESTS Multlshot

1?-1

PRnpFRTV K ing Bay Property, PH 520

moM( !T1P

0.00

3.65

13.05

19.00

56.90

50.90

67.80

63.05

73.70

74.35

102.10

103.50

104.80

117.30

119.00

122.50

141.20

143.15

145.50

147.00

155.60

158.60

159.50

TP r0^ )

3.65

13.05

19.00

56.90

60.90

67.80

68.05

73.70

74.35

102.10

103.50

104.80

117.30

119.00

122.50

141.20

143.15

145.50

147.00

155.60

158.60

159.50

160.90

Mag DESCRIPTION

SUMMARY LOG .. .''-iiClA MIN'HIOIV

!^M ' s i B E II tf I [jMASSIVE MAFIC FLOW (la) : L| L' L-. ,, . c ,ODO tt.

PILLOWED MAFIC FLOW (16) ! " " . ,, .. ,, . . ^ .P-''L'.ooMJUl.I^l^B,^

MASSIVE FLOW (la)" "' "- - . 1

MASSIVE FLOW/MAFIC INTRUSION (la)

PILLOWED MAFIC FLOW (Ib)

CHEMICAL SEDIMENT, CHERT, BANDED PYRITE (3a.b)

MAFIC FLOWS AND TUFF; MINOR FAULT at 72.40-72.45 Ma,d)

CHEMICAL SEDIMENT; CHERT, PYRITE, PYRRHOTITE (3a.b.c)

MASSIVE MAFIC FLOWS (la) ; -- . , ..- ' ' ~ "L . -

CALCITE BRECCIA (6) ' V; ... ' ;

DACITE LAPILLI TUFF (2) f r- , .-.

CALCITE BRECCIA (6) 'i ' ' " ! ' ' ~ r^

DACITE; 3X BLACK QUARTZ ANKERITE VE1NS-(2K~ ..-.. '

CALCITE BRECCIA (6)

PILLOWED MAFIC FLOWS (Ib)

CALCITE BRECCIA (6)

DACITE LAPILLI TUFF: St BLACK QUARTZ ANKERITE VEINS ( 2}

CALCITE BRECCIA (6)

MASSIVE MAFIC FLOW (la)

STRONG CALCITE ALTERATION (6a)

DACITE: 202 QUARTZ VEINS: 1-Ticrn (2)

STRONG CALCITE ALTERATION Ua)

rALCONBRIDGE NICXZL MINES LIMITEDDIAMOND DRILL RECORD

LOCATION.

LOGGED BY.

STARTED——.

-DIRECTION.

-CASING——-.

-CORE SIZE.

-DIP- -HOLE No. K8-62

SHEET No..

-CORRECTED TESTS.

FINISHED.

PROPERTY-

""Imatrff)

160.90

172.10

173.50

174.65

175.70

172.10

173.50

174.65

175.70

189.00

189.00

Maq

-

DESCRIPTION

Summary log - cont'd

MASSIVE FLOW (la)


DACITE TUFF, 5X QUARTZ ANKERITE VEINS ('2)

CALCITE ALTERATION (6a)

MASSIVE MAFIC FLOWS (la)

END OF HOLE

Contractor: Midwest Drilling, Winnipeg

Core is being stored on the property.

Hole cut 5 "calcite alteration/dacite"

zones have narrow (generally less than

veins; composite ankerite-quartz veins

, Manitoba

zones. Four of these

2cm) black quartz

are different feature

on this section. These veins carry pyrrhotite plus trace

chalcopyrite. The dacite intersections

from adjoining sections, but intensity

appears to be declining.

Hole cemented, casing left in.

are "on the projections

of quartz veining

FALCONBRIDGE NICXZL MINES LIMITED

LOCATION. 0+20E H05S

DIAMOND DRILL SECORD

N02"E.DIRECTION. .DIP. .HOLE No.. ,KB-62

LOGGED av R.B. Band CASING 3.65m SHEET No..

.CORE SIZE.NQ

.CORRECTED TESTS..mu11 i s ho t

FINISHED.12-11-85

K'ino Say Property, PN 520

ITtOM (

0.00

3.65

13.05

net?? s)

3.65

13.05

17.95

Mag DESCRIPTION

CASING

MASSIVE MAFIC FLOW (i*)

Dark green, very fine to fine grained (max. 1mm) equigranular,

coarser sections 152 white feldspar. .Individual flows marked

by 30cm amygdaloidal margins; flows 3-4m thick. Marginal

phases have 12 po as 2 -3mm blebs.

8.10-10.40 1 to 3cm epidote-quartz-calcite, 0.52 po, 0.52

py, sub-parallel to core axis.

PILLOWED MAFIC FLOW Mb)

Dark green, fine grained. Pillow rims are epidote-calcite,

-2cms. Pillow margins are calcite-amygdaloidal , but no po.

22 irregular 1mm calcite veinlets. Upper contact (13.00-13.70)

's brecciated with calcite - probably flow breccia sealed with

calcite - fragments to 5 x 2cms, angular.

16.65-16.75 3cm (true width) 400 core ang-l,e, possible

fault zone, pale green epidote/calcite with flattened chloritic

mafic fragments 1 to 2cm x 1 to 2mm (502) plus 32 po, 12 py.

again parallel to flattening.

This could also be interpillow material, but sulphides are

not normal in interpillows.

18.10-18.34 Calcite vein; margins are angular and "stoped"

by vein; 52 2 x rvnm wall rock fragments, 22 po. Looks like

a dilation vein, no movement. 20" core angle.

17.80-17.95 Light-green calcite t 302 angular chloritic

FALCONBRIDGE N iCXZL M ii^cS LiMITSDDIAMOND DRILL RECORD

KR - n LOCATION niwrrrioN nip wot F wn

LOGGED2

BY CASING ejWF Nn

rnpp *5i-7P rnoQtrrTFn TF^TC;

FINISHED

PROPERTY

FROM,- Lmp

17.95

56.90

TOtr0(0

56.90

60.90

Mag DESCRIPTION

mafic fragments 1mm to 2 x 5cm - margins of zone at 40 CA,

looks like a flow contact.

MASSIVE FLOW (la)

Dark green, grain size ranging from fine to fine-med. (1mm)

3-52 calcite veining.

26.20-26.80 Flow contact: 4 ZxScm fine hyaloclastite zones

separated by amygdaloidal rounded "pillow-buds". Flows above

and below this unit are amygdaloidal for 10 cms. There is

also a 2cm calcite vein with 12 po. Flow contact at 55".

26.80-56.90 Massive flow, very minor (12) calcite velnlets.

0.52 sulphide blebs scattered through as 13mm rounded blebs

mainly po, minor py.

37.60-37.70 5cm calcite vein, 600 CA

38.00-38.80 Srscciating 2-10cm calcite vein, 12 py, sub-

parallel to core axis.

39.10-39.40 2 x 3cm calcite veins brecciating, 300 CA.

MEDIUM-COARSE GRAINED MAFIC FLOW/INTRUSION (la)

Massive, dark green; 702 dark green amphibole as equant 2 x 3mm

grains; 202 white feldspar, as 1mm grains, interstitial to

amphibole grains; feldspar grains pick out a weak folitation

banding at 40* CA, 102 dark green-black pyroxene; 12 diss. po.

Upper contact is gradational against overlying massive flow.

Lower contact shows gradual grain size reduction over 30cm.

This is probably a coarse grained basal phase of the massive

DIAMOND DRILL RECORD

1 OCAT10N

LOGGED HY

STARTITO

FiNisweo

DiRFrrriON OIP KCLC wn. ND-O^

fASINrt 5JWFC-T Mn 3

mnt? Git* criBRecTFn res-r*;

PROPERTY-

ntoi*t metre?) Mao

60.90

67.80

68.05

71.60

72.40

72.45

67.80

68.05

71.50

72.40

72.45

73.70

flow, rather than an intrusion.

PILLOWED MAFIC FLOW (15)

Dark green, fine-grained. Pillow rims l-2cm epidote plus

calcite plus l* po. Pillow marginal phases have calcite

amygdules plus IX po, as 2-3mm rounded blebs. Pillows are

approximately 1m., minor calcite veining.

CHEMICAL SEDIMENT UNIT: CHERT, PYRITE (3a,b)

67.80-67.95 Chert, finely banded, 15X py, picking out

chert banding at 40" CA. (10cm true width)

67.95-68.05 (4cm true width) 40X pyrite, 255 cpy, li Zns.

Flow above this unit has X diss. po for 20cm above contact.

MAFIC FLOW (la)

Dark green, massive fine-grained, 0.5X diss. po, concentrated

near sulphide horizon.

69.00-69.10 5cra true width calcite, quartz,vein,

brecciating, 35 0 CA

MAFIC TUFF, CARBONATISED (Id)

Med. grey, strong calcite alteration. Fine colour banding

on 1mm scale, occasional flat 1mm x 5mm dark green-black

fragments. Banding at 40* CA.

CHLORITIC. MINOR FAULT ZONE

MAFIC FLOW (la)

Fine grained, dark green, massive, hard

s HiCXcL. Mi.NcS LiiviiTID

LOCATION.

LOGGED BY.

STARTED——

DIAMOND DaiU. SECORD

.DIRECTION————————^

.CASING—-———-^—^———

-DtP. .HCL5 Mn KS-62

SHEET No..

.CORE SIZE. .CORRECTED TESTS.

FINISHED.

PROPERTY.

me TOres i Mag TON

73.70 74.35

74.35 89.20-

89.20 92.40

CHEMICAL SEDIMENT (CHERT. PYRITE. PYRRHOTITE) Qa.b.c)

73.70-74.20 Banded chert, 400 CA

74.20-74.35 Banded sulphide, 101 po, 10* py, balance

chert plus chloritic sediment


74.35-75.00 Light grey-green, moderately hard, 10* 2-5mm

calcite veins - flow top?

75.00 Dark green, fine-med. grained equigranular; 5-10X

white feldspar, generally 1mm grainsize; fairly hard. Minor

(21} wide-spaced l-2mm calcite vein.

85.00-88.80 Medium grained flow, or intrusion? equigranular,

2-3mm, medium green, 25X feldspar, 75X amphibole. Contacts

are gradational to fine grained, lmm.

MAFIC TO INTERMEDIATE TUFF, CARBONATISED?

Med. grey, moderate to strong matrix calcite^ No foliation

or banding - could be carbonatised - upper section of flow.

51 calcite veining as planar, 2-5mm veins.

89.70-89.75 Calcite-quartz (10*) vein; abundant 2mm

chloritized wall rock fragments, l* black prismatic tourmaline

to l x 2mm 15 po. Tourmaline and po extend 5cm into wall

rock. Fine colour banding adjacent to vein could be

wall rock alteration or primary tuff bedding. Vein at 600

CA.

90.80-90.85 2 x lcm cherty grey quartz vein, with calcite

NICX2LDIAMOND DMU. KECCRD

LOCATION.

av

.DIRECTION.

CASING

.DIP. S No.K8-62

ST No..

S7ARTED.

FINISHED.

PROPERTY.

"•"flnelrel? Mag

92.40

102.10

103.50

104.80

117.3U

102.10

103.50

104.80

117.30

119.00

•t- li po, l J tourmaline, 50* CA. Both tourmaline and po

extend 10cm into wall rock.


Medium-dark green, fine-medium grained, 151 white feldspar to

l-2mm, equigranular hard. Very occasional (less than IX)

1mm calcite line joints.

Upper contact shows finer-grained margin gradational into

overlying unit. Lower contact shows gradation in grain-

size and colour to lower unit. Lower contact based on

calcite alteration of matrix and start of 2-5mm brecciuting

calcite veins.

CALCITE BRECCIA (6)

Light-medium grey, 1W brecciating calcite veins; breccia

fragments, 5 x 5cms rood.-strong matrix calcite.

DACITE LAPILLI TUFF (2)———————^—————————————— -V,

Large fragments greater than 10cm, pale grey, hard dacite

separated by finer with stretched fragments of more chloritic

material IxSmm, finely banded at 35" CA. Finer material is

chloritic. Non-magnetic.

CALCITE BRECCIA (6)

Med. grey, mod. calcite alteration, fairly soft, brecciated

by 0.5 to 2 cm calcite veins.

DACITE ( 2)

Med. grey, strongly magnetic due to diss. po. No foliation or

LOCATION.

DIAMOND DRILL RECORDKB-62

-DIP- .HCLE No..

BY. SHEST No..

FINISHED.

PROPERTY-

"""frnei

119.0

122.50

141.20

res?

122.50

141.20

143.15

^ag

*.

ocscnirnoN

fragments.

Minor veining as follows:

117.60 5cm calcite - follows grey qtz vein, 600 CA

117.70-118.0 5X brecciating BBQ-ankerite vein with 2* po.

118.30 lcm calcite/qtz, 60* CA

118.85 0.5cm BBQ, 800 CA

119.15 le BBQ, 70e CA

119.85 O.Scm/S.Scm calcite, 600 CA

NB - Calcite veins follow pre-existing BBQ veins.

CALCITE BRECCIA ( fi )

As above: gradational lower contact, colour change pale grey

green, strong matrix calcite alteration. Relic pillow rim

visible at 122.50 shows that the calcite breccia is at least

in part replacement of pillow flows.

PILLOWED MAFIC FLOWS M h )^•*

Dark green, fine grained, 5X white feldspar. Pillow rims 1 to

2cm epidote-rich; minor amygdaloidal phases. Locally 1*

diss. po at pillow margins.

129.30-130.00 12cm calcite vein, 5Z white qtz, 400 CA

129.80-129.86 Calcite vein, 45' CA, 5* qtz.

CALCITE BRECCIA (^

Upper contact shows gradational alteration or colour change

from green to medium grey accompanying increasing matrix

calcite alteration, with pillow rims being most resistant.

9 LCCATIOr

LOGGED

STARTED

FINISHED

PROPERT

" "tine

143.15

145.50

147.0

J

QY

Y

re??

145.50

147.00

155.60

Mag

r.ALw^isic.tiCGc iNSv.Xc- //tt r i cd !-:*vtiT-^


KB 62niRFCTION Q1P HCL* Mn

CASING SWirtrr Mn, 7

fntte S I7IT rnRRPCTPn TFJ5TS

oescatrnoN

142.0-143.15 302 calcite supporting elongate angular

grey clasts. Fragment elongation at 45 0 CA. Fragments look

as though they could be fitted back together - so no

movement.

DACITE LAPILLI TUFF (2)

Fragments vary from light grey to creamy grey to light tan.

Fragments strongly magnetic due to diss. po; very fine grained

and hard and siliceous. Matrix is strongly calcite-bearing.

Fragments unsorted, 10cm to 1cm x 2mm. Smaller fragments

are flattened at 5:1 to 10:1 and include white, fine grained

very siliceous fragments, sometimes with sharp re-entrant

angles. Finer sections show crude banding/elongation of

fragments at 45 0 CA.

Quartz veins at:

143.23-143.32 Black QV 2cm * ankerite; 22 po, 30" CA

143.42-143.46 2cm BBQ * ankerite, 50" CA

143.75-143.95 Brecciated by ankerite and 0.5cm BBQV.

144.70-144.80 3 x lcm ankerite-qtz veins * 32 po, 55" CA

145.15-145.20 1cm BBQ/ankerite; 22 po, 45 0 CA

CALCITE-8RECCIA (6)

Med.-grey, 5-102 calcite stockwork veins, medium to strong

matrix calcite. Gradational lower contact.


Dark green, fine-grained, 5-102 feldspar, sometimes clotted

r,-\LCCH5rtiDGc iSiCXjEL JviiruES UJvuTZDDIAMOND DRIU. RECORD

LOCATION.

LOGGED BY.

STARTED——

-DIRECTION.

-CASING—--

.DIP. .HOLE No.K3-62

SHEET No.


FINISHED.

PROPERTY-

PTtOMf mn

155.60

158.60

159.50

160.90

TOtr?s )

158.60

159.50

160.90

172.10

Mag ocscHirnoN

together to form 5mm feldspar spots. Very minor ( 2-31) l -2mm

calcite- lined joints.

STRONG CARBONATE ALTERATION (6a)*

Medium grey, strong matrix calcite alteration. Upper contact

is gradational, with grey-caldte replacement of volcanics

along cracks. 5-10X 3mm calcite veins at 55" CA, parallel

to weak foliation. Grain size varies from 1mm to fine-grained.

3ACITE (2)

Light-grey fine-grained, strongly magnetic due to diss. po;

strong calcite in matrix. No fragment or foliation.

Quartz veins as follows:

153.60-159.05 Sit brecciation by Q.S-l.Ocm black quartz *

ankerite veins, with 2-31 po. , tr cpy.

159.07-159.10 2cm black quartz, ankerite, 2X po; tr cpy

45 0 CA*

159.27-159.44 llcm zoned black qtz., grey quartz vein,

600 CA, 2* po splashes, tr cpy.


As above.

MASSIVE FLOW/MAFIC INTRUSION (la)

Med.-dark green, 2535 white feldspar, 65S green amphibole,

101 dark green black pyroxene. Med. grained, equigranular

l-2mm. This is similar to "intrusion" in KB-61, but it could

be a massive flow. At the lower contact there is a fairly

LOCATION.

LOGGED BY.

STARTED__

r/NLCONbkJLXjc, N lCKcL MINESDIAMOND DRILL RECORD

-DIRECTION.

CASING

-DIP- .HOLE No. KB-62

SHEET No..

.CORE SIZE. .CORRECTED TESTS-

FINISHED.

PROPERTY-

FROM—— C**

172.10

173.50

174.65

175.70

TOy*fn" j

173.50

174.65

175.70

180.00

Mag DBscmpnoN

sharp colour contact, but there are relics of the med. grained

"intrusion" bounded by alteration out from 500 fractures.


Light-med. grey, strong calcite alteration. Mod. -strong

foliation at 60e , followed by Irani calcite veinlets; fine

grained.

DACITE TUFF (2)

Light grey, strongly magnetic, strong calcite. Finely

granular (1mm) mod. colour-banding at 45 0 CA.

173.67-173.85 Grey quartz-ankerite vein, 1* po, 0.5* py,

400 CA

174.30-174.66 2 x lcm qtz-ankerite veins.


Med. grey strong calcite alteration. Calcite replacement

gradational into mafic flow.

MASSIVE MAFIC FLOWS (la)

175.70-178.70 Dark green, fine-med. grained, 1.5-2mm

equigranular, 20* fspr.

179.80-180.40 Flow top breccia: angular fragments to

greater than 10cm, all med. -green, mafic volcanics.

Matrix is finely granular, soft, white and green fragments

calcite-free; 2% po. At upper contact matrix is banded, ^

parallel to 'overlying' flow contact at 45 0 CA.

180.40 onwards: Dark green, fine-grained, 10* feldspar,

.becoming coarser with depth.

FALCONBRIDGE N ICKEL MINES Li,Vtl7cDDIAMOND DRILL RECORD

LOCATION. -DIRECTION. -DIP.. .HOLE NO-LOGGED BY.STARTED——.

..CASING. SHEET No..

KB-52

10


FINISHED.

PROPERTY-

i mf tref?;

189.0

Mag ocscntrnoN

182.80-183.50 Weak calcite alteration, 15Z, 0.5cm

white calcite-quartz veins, 25 po; subparallel at 40-600 CA.

END OF HOLE

Contractor: Midwest Drilling, Winnipeg, Manitoba


Hole cut 5 "calcite alteration/dacite" zones. Four of these

zones have narrow (generally less than 2cm) black quartz

veins; composite ankerite-quartz veins are different feature

on this section. These veins carry pyrrhotite plus trace

chalcopyrite. The dacite intersections are on the projections

from adjoining sections, but intensity of quartz veining

appears to be declining.

Hole cemented, casing left in.

*v, ~

FALCONBRIDGE NICKEL MINES LIMITED ^

0.97S

DIAMOND OKU.!. RECORD

N02 0E-DIRECTION. J3IP.

BY. - Band .CASING. 4.40m

November 14. 1985 mav S ITF N O

November 16, 1985

.CORRECTED Trgrs Multishot

King Bay Property (PN 520)

FHOM

0.0

4.40

16.50

18.00

45.25

49.20

49.40

55.30

56.45

60.10

77.20

80.50

86.25

90.20

94.20

101.40

104.75

109.10

115.60

118.80

124.70

129.00

131.00

135.10

Q TO

ptrp? l

4.40

16.50

18.00

45.25

49.20

49.40

55.30

56.45

60.10

77.20

80.50

86.25

90.20

94.20

101.40

104.75

109.10

115.60

118.80

124.70

129.00

131.00

135.10

137.60

SUMMARY LOG oacximoH

CASING


P1LLOWLD MAFIC FLOW (Ib) ' PA1WiftiA inK-vnniu. '"

MASSIVE MAFIC FLOW (la) U) E 8 IE t\^ E ffi]uU \sJ

PILLOWED MAFIC FLOW (Ib) FE3 " 6 19861 - - - ' A.M. P.M.

CHEMICAL SEDIMENT (3a. b) /|0|?ilpiljil*!l?iifl4lfo?

MAFIC TUFF (Id) *

MAFIC FLOW

CHEMICAL SEDIMENT (3a, b, c)

PASSIVE MAFIC FLOW (la)

WFIC CRYSTAL TUFF, CARBONATISED (Id, CA)

^IICRODIORITE (4)

HYALOCLASTITE (le)



PASSIVE MAFIC FLO* (la)



CALCITE BRECCIA (6)



iYALOCLASTITE (Tc)

1ASSIVE MAFIC FLOW (la)


FALCONBRIDGE NICKEL MINES LIMITED

LOCATION.

LOGGED BY.

STARTED—-

FINISHED.

PROPERTY-


.DIRECTION-

.CASING———

.DIP- .HOLE No.KB-64

SHEET No..

.CORE SIZE- .CORRECTED TESTS.

PNOM

137.60

163.20

165.70

167.90

TO

163.20

165.70

167.90

172.0

Summary log - cont'd DOCRIPTTOH


CARBONATE ALTERATION (6b)

ALTERED DACITE (2d)


Contractor: Midwest Drilling, Winnipeg, Manitoba.


No significant quartz veining intersected. The zones of

strong calcite alteration could be the up-dip equivalents of

the "calcite-alteration-dacite-quartz vein" zones intersected

in drill holes to the east. This suggests these zones may

plunge below the intersection level in DDH KB-64.

"i significant assays.

"••^

FALCONBRiDGE NICKEL MINES LIMITEDDIAMOND DRILL RECORD

0+OOE 0+97S N02 0 E .DIP- KB-64

BY.R. B. Band 4.40m

November 14, 1985

November 16, 1985

.CORE NQ .COntMTCD Mult i shot

(PN 520)

Trfctr

0.00

4.40

16.50

18.00

e s f0

4.40

16.50

18.00

45.25

coo****

CASING

MASSIVE FLOW, MAFIC (la)

Dark green, fine grained, (0.5mm) equigranular, lOX-20%

feldspar.

4.40-9.30 0.5X widely scattered white felsic grains or

blebs, irregular shape to 3x5mm.

9.30-10.00 fine-grained 101 sub-parallel calcite veins,

possible flow-top

10.00-16.50 as above, but minus felsic blebs

Badly broken core sections at 10.35-10.50; 11.75-11.90; and

12.95-13.00.


Dark green, fine grained, pillows tightly packed, no inter-

pillow epidote material. Pillow margins are amygdaloidal

with a dark green-black chloritic rim.

17.50=18.00 Interflow breccia/tuff: angular mafic clasts

from Ix2mm to Ix2cm, in a strongly foliated chloritic tuff/

sediment. 3? po as flattened lenses (1mm x 10mm) in

foliation at 55" CA.

MASSIVE, MAFIC FLOW (la)

Dark green, generally fine grained (less than 0.5mm), 15-20S

white feldspar. 3mm roui.ded blebs, tr cpy.

24.70-26.70 irregular 2-3mm clear quartz/calcite vein, sub

parallel to core axis. 356 po concentrated along vein margins.r***- - :

F ALCONBRiDGE NICKEL MINES LIMITEDDIAMOND QUILL SECORD

LOCATION.

LOGGED BY.

STARTED——

-DIRECTICi*.

-CASING——

.CORE SIZE.

-DIP- HOLE No.

2

KB-64

SHEET No.

.CORRECTED TESTS-

FINISHED.

PROPERTY. King Bay Property (PN 520)

n*OM .(r

45.25

49.20

49.40

etres)

49.20

49.40

55.30

DKSOtIP 1 IUN

28.65-28.80 Broken core, chloritic, fault zone

33.40-44.50 Medium grained, dark green, 20* feldspar, 80t

dark green amphibole; feldspars O.Simt are interstitial to

2- 3mm amphi boles. This gives a weak mineral alignment, picked

out by feldspar, at 55* CA. IS diss. po blebs.

Upper contact at 60*. Lower contact is gradational through

to fine-grained flow.

At 41.50-42.70 very fine grained feeder dyke,, sharp contacts

at 60".


Green-black, very fine to aphanitic pillow margins are

amygadaloidal. Pillow rims l-2cm, epidote. Minor (1-2X)

irregular calcite veinlets. Lower 10cm (49.10-49.20) has 5X

1mm po blebs.

CHEMICAL SEDIMENT (3a, b*

Banded chert and pyrite (30t); banding at 62 0 CA.

MAFIC TUFF (Id)

Dark to med. green, generally fine grained, with 30cm section

of coarser material, 30X white feldspar fragments to 2mm and

mafic fragments.

53.50-55.30 med. green, well foliated, with 40* 2x4mm

mafic fragments, strong calcite alteration.

.

FALCONBRIDGE NICKEL MINES LIMITEDDIAMOND DMH. RECORD

LOCATION.

LOGGED BY.

STARTED——.

.DIRECTION.

.CASING-—.

.CORE SIZE.

.DIP. HOLE No,

3

K8-64

SHEET No.

.CORRECTED TESTS.

PROPERTY.King Bay Property (PN 520)

FHO^(mf

55.30

56.45

60.10

77.20

80.50

tre?L.

56.45

60.10

77.20

80.50

86.25

DCSCmPTKMI

MAFIC FLOW

Upper contact at 50". Dark green, fine grained

CHEMICAL SEDIMENT (3a,b)

56.45-57.50 Finely colour banded chert, banding 500 to CA.

57.50-58.80 Dark green, fine grained mafic flow

58.80-59.20 Chert

59.20-59.55 Interbedded pyite, pyrrhotite, soft-pale green

"lay-rich sediment and chert. lOl py, 10* po

59.55-60.10 Light green, fine grained, moderately hard

sediment/tuff.


Medium grey green, fine-med. grained, 10-1556 feldspar laths

to 0.3x2mm, sometimes in clumps. Colour of this unit is

lighter than flows in other drill holes. No matrix calcite.

Occasional widely spaced calcite-lined joints-only.

From 70.0 on, feldspar increases to 20* with rare feldspar

phenocrysts to Ixlcn.

CRYSTAL TUFF, MAFIC, CARBONATISED (Id, CA)

Medium grey green, 20* white feldspar fragments, to 2mm, dark

fragments l-2mm. 15* calcite veining 2mm veins, spaced

regularly lcm apart, all parallel at 55 e CA.

MICRODIORITE (4)

Med. grey, 30-40* feldspar, 10* pyroxene, 50-60* amphibole,

equigranular 1mm. Much higher feldspar content than mafic

FALCONBRIDGE NICKEL MINES LIMITEDDIAMOND DRILL RECORD

LOG AT: ON.

LOGGED BY.

STARTED——

.DIRECTION.

CASING

.CORE SIZE.

-DIP. HOLE No..

4

KB-64

SHEET No.

.CORRECTED TESTS.

FINISHED.

Pnnpgnrv K ing Bay Prnpprty (PN 520)

"""V

36.25

90.20

94.20

tres)

90.20

94.20

101.40

DaCftirnOM

flows, grain size more consistent. Chilled lower and upper

contacts. Lower contact at 55".

HYALOCLASTITE (le)

Large rounded fragments are medium green, very hard, and

porphyritic with 2X white feldspar laths 2mm x 1mm and also

glassy needle-like crystals to 2mm x O.lmm, similar to those

in "dacite". These are hard and were called quartz in dacite.

These clasts are up to 20cm. They also have soft, black spots,

generally rounded, possibly amygdules.

Matrix is made up of sharply angular pale green "honeycomb

textured" glass fragments.

Texturally this is like the typical mafic hyaloclastite.

Compos i tionally the large clasts may be "dacite" rather than

mafic.

86.25-86.35 10* pyrrhotite in 3 void filling (?) splashes

5cm x ?cm.

Lower contact at 65 0 .

MASSIVE MAFIC FtOW (la)

Dark fine-grained, 5-10X 1mm white feldspars, hard, 35J 1mm

irregular calcite lined fractures.


Med. dark grey, strong matrix calcite. Soft. Varies from

fine to medium grained - coarser material has 40* white spots

2 x 4mm which are most probably calcite, but could be tuff

FALCONBRIDGE NICXEL MINES LIMITEDDIAMOND CTUU. RECORD

KB-64LOCATION.

LOGGED BY.

STARTED__

.DIRECTION.

.CASING-—.

.DIP. .HOLE NO.-5 .

SHEET No..

.CORE SIZE- .CORRECTED TESTS-

FINISHED,

King Bay Property (PN 520)

rao*"tin* tre?) OKSCHIPDON

101.40 104.75

104.75 109.10

109.10 115.60

115.60 118.80

fragments. Coarser phases have weak foliation, at low core

angle.

Alteration intensity increases gradually at margins of this

unit.

From 94.20-98.90 there is 5Z sub-parallel calcite veinlets.

98.10-98.35 2 lcm black quartz-ankerite veins, 2S po, tr

cpy; 25 0 CA


Dark green, fine-grained, low calcite. Is this an unaltered

relic?

STRONG CALCITE ALTERATION (6a )

Light to m"d. grey, strong to rood, calcite alteration, but

strong alteration is patchy. Moderately soft. Generally

fine-grained.

105.65-105.80 Brecciating lcm grey qtz vein, 31 po, tr

cpy.

PILLOWED MAFIC FLOW (lb)

Medium green; fine-grained, epidote-rich pillow rims 2-3cms.

Gradational alteration, initially from grey-green moderately

altered mafic, with relic pillow rims.

CALCITE BRECCIA fc)

Light-med. grey, fine-grained, 10-15* stockwork of calcite

veins. Matrix has moderate calcite.

FALCONBRIDGE NICKEL MINES LIMITEDDIAMOND DRIU RECOftD

KB-64LOCATION-

BY.

-DIRECTION.

CASING

.DIP. .HOLE NO..

6SHEET No..

STARTED .CORE SIZE. .CORRECTED TESTS.

FINISHED-


FMOMf me

118.80

124.70

129.0

131.00

135.10

tre^

124.70

129.00

131.00

135.10

137.60

ocscmrnoN

115.90-116.20 Light-grey, fine-grained, diss. po (Q.5%)

magnetic dacite?


Dark green, fine-grained, 101 feldspar

CALCITE ALTERATION (6a )

Med. grey, strong matrix calcite alteration. Only

calcite veining.

Gradational contacts.

125.25-125.35 8cm composite black quartz, calci

quartz vein. 65 0 CA.

HYALOCLASTITE (le)

75* light green hyaloclastite/calcite matrix with

from 1mm to 5cm. Fizzes strongly. Hyaloclastite

are pale green, honeycomb texured, with chert infi

Very minor (less than IX ) po.

25X med. green mafic clasts, either rounded, to

angular to 10cm.

minor (31)

te white

fragments

fragments

lling.

20cm or

Matrix shows an alignment and flattening of fragments at

35 0 CA.


Dark green, fine grained (1mm), 10* white feldspar.

CALCITE ALTERATION fca )

Med. grey, soft, strong matrix calcite.

FALCONBRIDGE NICKEL MINES LIMITEDDIAMOND DRILL RECORD

LOCATION.

LOGGED BY.

.DIRECTION.

CASING

.DIP, HOLE No.

7

KB-64

SHEET No.


FINISHED.

PROPERTY.King Bay Property (PN 520)

FROM{me137.60

163.20

165.70

167.90

tre^163.20

165.70

167.90

172.0

172.0

DESCRIPTION

MAFIC MASSIVE FLOW (la)

Dark green, fine to medium grained, generally TO-15% feldspar.

Less than U calcite on joint places.

145,0-153.50 becomes gradually coarser grained to 2mm,

uppar and lower gradational contact? are over 3.0m and 1.5m

respectively.

153.50-163.20 Fine-grained massive flow, very hard and

"rings". From 158.0 5X feldspar.

CARBONATE ALTERATION/CARBONATISED fea )

Med. grained with white-grey grains 4 x 1mm in med. grey

weakly foliated matrix. These could be calcite grains, or

felsic fragments, as unit is strongly calcite (fizzy). Weak

foliation at 55 0 .

ALTERED DACITE (2d)

Soft, light-med. grey, fine grained, non-magnetic, but has

acircular glassy crystallites, as in dacite. Soft, but only

weakly calcitic. In part it is a coarse fragmental. Lower

section is "calcite breccia". Has soapy feel suggesting high

sericite.


Fine grained, dark green, hard. Minor (IX) calcite lined

fractures.

END OF HOLE

Contractor: Midwest Drilling, Winnipeg, Manitoba.

FALCONBRIDGE N ICKEL MINES LIMITEDDIAMOND DRILL RECORD

LOCATION-

LOGGED BY.

STARTED——

-DIRECTION.

CASING

-DIP. HOLE No..

8

KB-64

SHEET No.

.CORE SIZE- .CORRECTED TESTS.

FINISHED-


FROMi met

T0res )

DESCRIPTION


No significant quartz veining intersected. The zones of

strong calcite alteration could be the up-dip equivalents of

the "calcite-alteratlon-dacite-quartz "vein" zones intersected

in drill holes to the east. This suggests these zones may

plunge below the intersection level in DOH KB-64.

No significant assays.,X7 .rf ff Xy-Mtf-*^

" y '2 ft

i r r ^ 2f i! , r: c r , , , , n ;

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52J88SW**2S 52JeeSW**3t7At FOURBAY LAKE 300

Ministry ol"NaturalResources

Report of Work

Ontarioit- The Mining Act

IrtMructioo* - Si*plv? rtqttir*d d*ti on a separate form lot eachtype w work to be recorded lw* table below).

- For Gep-uehnical work use form no. 1362 "Rtportol Work (Geologic*!, Geophysical. GeochemicaJ andExpenditure*)".

'ottal Add r MI of Recorded H older

Falconbridge Limited (51*) Steep Rock Resources Inc. (49X)Prospector's Licence No.

A21647, A1851440th Floor, Commerce Court West Toronto, Ontario MSL 1B4——-—-

302-45 Sheppard Avenue, East ^ c*f North York. Ontario M2N 5W9 5(?u*W lAtft" C'-3i40

Summary o* Work Performance and Distribution of CreditsTotal Work Days Cr. claimed

for Performance of th* following work. (Check on* only)

Shaft Sinking Drifting or other Lateral Work.Compressed Air, oth*r Power driven or mechanical equip.

Power Stripping

Diamond or other Cor* drilling

All the work was performed on Mining Claim(s); Pa437022 (705 days) Pa 475234 (479 days).Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)

Midwest Drilling 180 Cree Crescent Winnipeg, Manitoba R3J 3W1

Drilling carried out 10-11-85 to 16-11-85,

KB-62 KB-64

189 metres 172 metres

PATRICIA MITNGDIV.E B E 1 V E

Dan Of Report

Februar 4/86Certification Verifying Report of Work

l hereby certify thet l have a personal and intimate knowledge of the facts set forth In th* Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion end the ennened report is true.

Neme end Postal Address of Person Certifying

R.B. Band, 100-3074 Portaqe Avenue, Winnipeg, Manitoba R3K OY2Date Certified

February^ 4/86Table of Information/Attachments Required by the Mining Recorder

•;*fi

"

c ?

E

Type of Work

Manual Work

Shaft Sinking. Drifting or other Lateral Work

Compressed air, other power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

Land Survey

768 181/3)

Specific Information per type

Nil

Type of equipment

Type of equipment and amount expended. Note: Proof of ectual cost must be submitted within 30 days of recording.

Signed core log showing; footage, dlemeter of core, number and anglas of holes.

Name and address of Ontario land surveyer.

Other Information (Common to 2 or more types)

Name* end addresses of men who performed manual work /operated equipment, together with detes and hour* of employment.

Neme* and addressee of owner or operator together with date* when drilling/stripping done.

Nil

Attachments

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

Work Sketch la* above) in duplicate

Nil

FALCONBRIDGE LIMITED

Suite 100 - 3074 Portage Ave.Winnipeg, Manitoba. R.IK OY2Telex 07-57251 Telephone 204/888-9860

Summary of work performance and distribution of credits - cont'd

Pa824?35824736824737824738821739824740824741824742

20 days 20 days 20 days 20 days 20 days 20 days 20 days 20 days

fei

FE3 -6,966A.M.7|8|9tlOillii2i l|2|3

RECORDED HOLDER: SAME As ABOVE : OTHER l l€¦ · 172.10 173.50 174.65 175.70 172.10 173.50 174.65...

Documents

Transcript of RECORDED HOLDER: SAME As ABOVE : OTHER l l€¦ · 172.10 173.50 174.65 175.70 172.10 173.50 174.65...