010 DIAMOND DRILLING AREA: KEEZHIK LAKE REPORT NO:l A …

sap lessees M KEEZHIK LAKE 010

DIAMOND DRILLING

AREA: KEEZHIK LAKE REPORT NO:l A

WORK PERFORMED FOR: Pure Gold Resources I ne./Severide Res

RECORDED HOLDER: Same as above [xx]: Other [ j

Claim No.

TB 656475

TB 919497

TB 656486

TB 656475

TB 656478

Hole No.

KL-87-12

KL-87-13

KL-87-14

KL-87-15

KL-87-16 KL-87-21

Footage

206.3m

210.9m

203.3m

203.3m

279.5m 285.6m

Date

July/87

July/87

July/87

July/87

July/87 July/87

Note

(D

(D

(D

(D

(D (D

NOTES: (1) #423-87 , filed Feb/88.

DIAMOND DRILL PROGRAMME LOGS AND SECTIONS

l l l l l l

HINZER OPTION/KEEZHIK LAKE PROPERTY

l SEVERIDE RESOURCES LTD./ PURE GOLD RESOURCES LTD,

l

l

l

l

l

l

l

l

l

l

l

l

F R O t'l. H O R Ci M C O EX PI C K L

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

10

100

140

180

1BO

. 200

, 120

. 240

it m *r*oKL-87-12

~-!lo~

- EMO OF HOLES 206.3 MUrt,

/'t

QVBWttN

18ABI aUAOTZ FELOSPW

NORAMCO EXPLORATION

Keezhik Lake (1441) Diamond Drill Section

Atlwtht

Or*im COREL06 100

-brt*i

08-24-1987: :09J6

LES EXPLORATIONS NORANCO IftC.

mm mn m

KL-87-12

t

t

c

(

'c

(

_ .^.. .

Property: fcdiik !ake(U'l]

Partner: btlen Like sotras

Aziuith; 13: degrees

Logged By: I c ,-hrl Cooper

tete Started: j.'l}14 1)87

Core Size: t

Drill Company: In^ear

H. K'Si

JllSr b?f

Oaii *J IBKM'5

Dip: -50 ffi;rees

Casin9: wt

fate Conoletd: July 16 198?

Core Location: teezhkLake

Overburden: 1,2 ieers

(ci^Dt^lBts

30 deg. t 1.

.. ... ..^.... ,. ..., ...... ..- ...... ........ ... --...-...- ' C1m

^ 0

Coordiicts: 153*2511 , 12*485 p

Length: 206.3 leters

Elevatioi; Surface ^

Dat? Land: July 19 1967

Samples Hipped:

c

(20^.3 a 4lkg.

b:est the b*nd^ extatsior. of 90!c scheeir.e irrg war? viin occwrin? in trenches.

Doric! us i oris

fecouendatiois

'i l bif id ne frw H7.7 to 148.3 (0.6 i vttlh) ;a1fta hitjassociat?ff visible gold,

kriter d'illbj is -ec

r

f

fLES EXPLORATIONS NORAHCO INC.

NMOND OR1LL LOG -- SUttWV

KL-87-12

Page ?

Frot(i) !o(i) ——-—-———--Description——————~——————————HineraSizationis)-—-—-————Alteratiomsj———-

0.0 1.2 OVEISIRCEN

1.2 206.3 [Bte] OOWTZ FaPSPW HRPHWPyrite (4*) Carbonate (1-21) Tourwline WJ) Yelloc-Green Sericite Ml**-Green Sericite ( trace) Gale/a (trace) '/isible fold ( trace)

c

i

206.3 END OF HOLE.

3

ZO

3r O

O

m x

LES EXPLORATIONS

08-24-19??: :09:36 DIAMOND DR1I

f ro- jc .... ——————— . — oKcr jp^on— ....... — - ——— ...t.) W

0.3 1.2 OVERBURDEN

1.2 286.3 [8W] QUARTZ FdPSPAR PORPHRV

Nettled light to GreenQuartz : 402K-feldspar: 302-: 301AphaniticHassiveIfeakly Fractured (5 Fractures/Neter)'-li Ouartz-Carbonate Veining at 80 Deg. tax. - Avg. Kidth

1 c*Pyrite! WToursaline: ^*: traceCatena: traceVisible Gold: traceCarbonate Alteration: 3 -Z*Yellow-Green Sericite Alteration: 5JNon HajnetkVM Conductive

Overall tte core is a pale green colour nith about 30}qtz (l-2w) anhedral subrounded to subangular pheno crysts. There are at least ?-3l larjer (2ni-hii) an hedral to siihedral feldspar phenocryst*. They art typ ically ronecf; beige to slightly flesh coloured withsquare to rhoifck plawr X-sections and ra-?rpseudohexagonal X-sections. The outer grain boundariesof these feldspar phenocrysts are ail di y corroded.In places the occurances of the 'eidspar phew:rystsincreases to 5-lOi but does not exhibit any flow typetriefi'dtian. ^iere is w obvious foliation at sil, Th?

NORA!

A LOG

SaipleNo.

126511265212653126541265512656126571265812659126601266112662126631266412665126661266732663126691267012671326721267312674126751267612677126781267912690

*CO 1

Froid)

21.7023.3023,9025.5027.2027.8D27.9029.1030.2031.3032.1033.1033.9034,7035,7036.2037.2038.4038.7910.0041.3042.7044.0045.0045,7047.5049.2950.8052.5053. W

[NC.

To(•)

23.3023.9025.5027.2027.8027.9029.1030.2031.3332.1033.1033.9334.2035.7036.2037.2038.4036.7040.0041.3042.7044.0045.0045.7047.5049.20SO, 80S2.SO53.90K.?0

KL -87-12

Midth Au M Cu In Pb Sb As Ho(i) (pw) (ppi) (PPI) (ppi) (PPI) (ppi) fa*) (ppi)

1.603.601.601.70D.600.101.201.101.100.801.000.300.30l.M0.501.001.200.301.301.301.401.301.000.701.801,701.601.701.401.30

(^ *-*

r *

f: : T?r:T7~~~r':rvr'

OB-24-1987: :W.-36

LES EXPLORATIONS HORAHCO INC.

NAMOV Mill toe

KL -87-12

Froi To ——— - — ------ —— Description —— -— — ~--~- --(t) d)

overall pale green colour is due to the soft seric-itized licrofelsic groundless. A white ctoulky(illite?) nature of the groundmass is also present.1-21 carbonate is pervasive throughout. Long linotenicrofractures as a coating possibly indicatingprevious ftuid ^ration and subse^ent alteration oftbe 9rouno*3ss, Accessory trace hbl. and 4S py dis-sesinated throughout ^<-lB[). barrow qtz-carb veinletsoften toiirwline coated.

SaipleNo.

126811268732683125841258512686126871268812689

froid)

55.2056.0057.4058.8060.2-361.8063.2064.9066.50

To(i)

56.6057.4058,8060.2061. ft)63.206*. 9066.5068.11

Width(i)0.801.401.401.40L601.401.731.601.60

Au Ag Cu ?n Pb 51) As Mo(ppi) (ppi) (ppi) (Dpi) (ppi) (ppi) (ppi) (ppi)

73 O

Z O 73 D 3 O O

m xTJ

O

POTASSIC ALlfRATION AREAS

Pyrite: 4?Potassic Alteration: *eak (IGtj Potassic Alteration: loderate (301) Potassic Alteration: strorvo (50*)

W-*eafc potiask alteration -> (ie faint i patchy)N-aoderate -"- (if consistent purplish colours)S-strona - B - (purplish red colour)Genera?l y toy contact areas. Also contains feldsparphenocrysts but they are slightly pinker.H5,9-*.8;21.1-?Uj29.1-30.2;3?.l-33.1;35.?-36.25?.5-53.9;79.5-79.8;130.5-13J,9;l??.H9UH-3.0-5,9:12.6-i4.0;H.5-16.0{33.9-34.2:45.H7.5;134.4-143.0;203,6-?04.1S-?9.8-80,6;139,5-190.5;194.7-19?,1:397,7-201.5;204.1-205,4

SILICIFICATION AREAS

12690126911269?12692126941269512696126971269812699527001270112702127031270412705

68.1069.6070.2071.6072.9074.6075.2076. SO78.1079.5079.8080.8083.2082.1082,6083.90

69.6570.2071.6072.9074.6075.2076.5078.1079.5079.8080.8081.2082.1062.6063.9084.90

1.500.691.401.38J. 700.601.301.6C1.400.301.000.400.900.501,301.00

(

(

(

12706 84.90 86.50 1,60

C

f

LES EXPLORATIONS NOR AM C G INC.

08-24-1987: :09: 36 DIUDND WILL LOG

Froi lo —— — - -— — — -Description------ ---- — — — - Saiple(i) (i) No.

19.8-i9.9;23.3-?3.9;37.2-3M;38.M4.0;63.2-7(U;72.9- 1270?75.2j31.2-82.1;32.HH.9;167.9-16B.2 12708Froi 52.7-150.0 the core exhibits s iDderats degree of 12709silicification as 3 whole. Tiere is a slight increase 12710in disseminated pyrite (^1). Trace fo occurs at 95.1and face 93) end occurs at 115.1 i. Fro* 147.7 to 118.3 12711the silicification is a aors prominent grey colour 12712ihich totally issks the rock fabric (visible gold; 12713galena). Froi 176.1 to 205.3 th;re is a loderate degree 12714of silicification. 12715

32716327171271}1271?127201272112722127231272412725127261272712728127291273032731127321273312734127351273612737

Fm 1(d) (4

8t50 81.088.00 81.06^0 9.. D9110 9.'.3

92.20 91.394?0 9S.O9S50 9\D97.10 9IJ9&70 t(M,l)

loaio 10:. 310L?0 1K.3303.?0 10'. 8104.JD l(h.4106U 10:.8107 W 10? J109 K IK.TiIIO'O 111.3312 M ll-.e113 SO 13!. "h115! (0 llf.7)116 '0 IK. D118.0 11*.8119*0 121.0121 W 123.8122 tO 12 -,7i123 D 12^.211?5!0 12(.5126SO IZi.gi12710 125.21129:0 13C.7I130 '0 13/.0!

KL-87-12

Page 5

Width Au Ag Cu Zn Pb Sb ^s (to(i) (ppi) (ppi) (ppi) (ppi) (ppi) (ppi) (ppi) (Ppi)

1.501.60l.W1.60

2.001.401.501.601.401.601.501.601.601.40l.M1.401,501.401.601.501.401.501.401.601.101.501.301.401.3d",.50:.3D

T) O

ri3 O O

m x

o7;

t

c

LES EXPLORATIONS NORAMCO INC.

OB-24-1987: :09:36 DIAHONO DRILL LOG

Froa lo -~.~— — - —— - — -Ascription ——— - ————— — - Sanple(t) (i) Ho.

1273B12739127401274112742127*312?4412745127461274?127461274912750133011330?133031330413330i133BS1330?13303133091331013311133121331313314133151331613317135181331913320

Froi To(B) d)

132.00 133.40133.40 134,90134.90 136.30136.30 137.70137.70 139.20139.20 140.60140.60 142.10142,10 143.60143.60 144.90144,90 146.30146.30 147.70147.70 14O148.30 150.00150.09 151.50151.59 15?.*)152.99 154.50154.53 155.9015S.90 157.50157.50 158.90158.90 160.40160.40 161.90161.90 163.50163.50 165.00165.00 166.60166.60 167.90167.90 168.20168.20 169.80169.60 171.40171. W 173.00173.00 174.50174.50 176.10176.10 177.70177.70 179.30

KL-87-12

Page 6

tfidth Au Ag Cu Zn fb Sb As tod) (ppi) (ppi) (ppi) /ppn) (ppi) (ppi) (ppi) (ppi)1.401.501.401.401,501,401.501.501.301.401.400.601.70i.SO1.401.601.401.601.40I.SO1.501.601.501.681.300.301.601.601.601.501.601.60l.bfl

zo7) l!•3.

Oomx•D

O

TP

-J

2 ;;

8

S

m w m

s t

fO

*-

-O

^O

-

CD

O

C

5O

O

OU

O

&

C*

W^

-^

^^^ ^

O"t

C

D

*JTI

C

O

s w o jo s o o

i f f* i!

f

f #

r 09 l N)

l l l l l l l l l l l l l l l l l l

8 "d

1X

3 l d

X

3 O

OU

tiaO

N

UO

JId

FRO

M

NO

R&

MC

O

EX

P I C K L

P.

9

*TJ 4-*

CO

LT

*

Sl

00

s

(VI —

lC

^

li

m

"Smi

sfO

m

FROM, HORfiMCO EX fICKL P. 4

AZIMUTH; too Tib-

100

140

1(0

20)

220

-~t*

izi HWIC VOLCANIC,

MAFIC VOLCANICS

i MAFIC W

BRAKITIZED VOLCANIC TUFF,

I6AS) QUARTZ FELDflP^

CHO CF HOLE! MO.

KL-87-13

rNORAMCO EXPLORATION


sL 4t i,t" ii" ~

8-22-1987;:10:31

LES EXPLORATIONS NORAMCO INC

DIAMOND DRILL LOG

KL-87-13

Property: Keezhik Lake (1441) NTS: 52 P Township:

Partner: Severide Resources Claim K: 919497 Coordinates: L 46 H , 21 * 50 S

Aziiuth: 180 degrees Dip: -50 degrees Length: 210.9 meters

Logged By: ^, r Mark Cooper Casing: Out Elevation: Surface

Date Started: July 18/87 Date Completed: July 21/87 Date Logged: July 25/87

Core Size: 8Q Core Location: Keezhik Lake Samples Shipped: July 31/87

Drill Company: Longyear Overburden: 7.3 meters

Acid Dip Tests

l 1. 108.8 s 49 deg. t 2. 210.9 m 45 deg.

PurposeTo test IP anomaly near photo-linear (335 deg.)

ConclusionsThe IP anomaly can be explained by the overall occurence of "11 pyrite ; and the slight enrichment (up to 21 pyrite) in bleached silicified areas.

RecommendationsRecoamendations pending assay results on the mineralized (pyrite) silicified zones.

LES EXPLORATIONS NORAMCO INC, KL-87-13

8-22-198?::10:31 DIAMOND OR 111 LOG -- SUMMARY

Description-Froifi(in) lo(ffi) ------------------

0.0 7.3 OVERBURDEN

7.3 210.9 [8AB] QUARTZ FELDSPAR PORPHYRY

-Mineralization(-i,)---------------- ------Aherat ictus)---- ---------------

18.2 19.7 [2] HAFIC VOLCANIC

57.5 59.5 GRANITIZEO HAFIC VOLCANICS

108.8 112.1 GRANITIZEO MAFIC VOLCANICS

112.1 118.7 GRANITIZEO VOLCANIC TUFF

Pyrite W)TouriDdl ine ^1)Yellow-Green Sericite ( trace)

Pyrite (<l)

Magnetite (5)

Magnetite (5)

Magnetite (5) Pyrite { </•- 1)

Carbonate (1-2) Yellow-Green Sericite

Cniorite (50) Biotite (10)

Potassic (5) Carbonate (2)

Silica (5) Biotite (5)

210.9 END OF HOLE.

LES EXPLORATIONS NORAMCO INC. KL-87-13

08-22-1987::10:31 DlArtOND DRILL LOG POQ? 3

From To .........—....~....^^ r ^\m....................... Sample From lo Width Au Ag Cu 'In Pb Sb As no(ffi) (ffi) No. (m) (m) (li) (ppm) (ppni) (ppm) (ppni) (ppm) (ppni) (ppiti.i u-?;i0.0 7.3 OVERBURDEN

7.3 210.9 [SAB] QUARTZ FELDSPAR PORPHYRY

Mottled Light to Green 13343 16.20 16.40 0,20 Quartz: 40 13344 16.40 17.90 1.50 K-Feldspar: 25 13345 17.90 19.70 1.80-: 35AphaniticMassiveWeakly Fractured (6 Fractures/Meter)*:1 Quartz Veining at 60 Deg. Cax. Avg, Width lcmPyrite: ^Tourmaline: ^: traceCarbonate Alteration: 1-2Yellow-Green Sericite Alteration: 5Non MagneticNon Conductive

This hole is very similiar to KL-87-12. It is overall apale green color with Hrnrn quartz phenocrysts (301). Thelarger 2iiim-km feldspar phenocrysts however are not quiteso abundant as hole KL-87-12 ("21).

They are also zoru/d and corroded. There are also patches of5-102 of these larger feldspar phenocrysts as in holeKL-87-12. Ihe groundmass is again a softer serializedmicrofelsitic material with a clay (illite?) content.

The sphalerite mineralization (eg, at 38,7m) may or may notactually be sphalerite, The rock is massive with noapparent foliation, Approximately 1-21 carbonate occursalong microfractures and as a coating on the largefeldspar phenccrysts,

2-11 hornblende and "42 pyrite occur throughout with the

8-22-1987;:10;31

LES EXPLORATIONS NORAMCO INC,

DIAMOND DRILL LOG

KL-87-13

From (i)

To (l)

-Description-

pyrue increasing close to 21 in seme /nore fractured andsilicified areas.

Some silicified areas contain only patchy greyish quartzinfiltrations while other areas entirely lack the originalrock fabric and consist almost entirely of quartz and "l*pyrite. Some whiter colored bleached silicified areas haveup to 2! pyrite

(eg. 184.9m ^ 186.0m) . From 17.8m to 75.7m moderatesilicification overall with sections strongly silicified.The following sections contain moderate silicification :132.1 o 133,5m ; 138.0 ^ 142.4u ; 158,1 -^ 164,8m ;173,4 ^ 174.4m ;

l??.2 o 177,8m ; 184.9 o 186.-y 201,4m ; 208.8m -) 210.3m.

Sections of stronger silicification include; 90,8 o 92.Oro ; 124.1 o 126.1m155.6 ^ 156,5m ; 167.8 -) 169.0m

The weakly potassic alteration areas are only faint andpatchy with generally hazy contact areas, Larger feldsparphenocrysts are present and are slightly pinker, eg; 44.7-) 46,k ; 53.4 -) 60,6m ; 62.6 o 64.2m ; 69.5 ^ 7?.3ni ; 154.2 -:- 154,5m

; 165.5 ^ 166.6in. Some weakly potassically altered arras contain "12 magnetite, eg: 75.7 ^ 81.4m ; 120.0 ^ 123.2m,

Sample From To Width Au Ag Cu Zn Po Sb As ftc No. (m) (m) (m) (ppra) (ppm) (ppm) ippm) (ppm) (ppfi,1 (ppm) ;;?.T.

193,1 -) 194.5r,i ; 195.2

149,584.4 -) 85.(

) 152.8m ; ^ 181.hi

-Sub Units-

18.2 19.7 [2] HAF1C VOLCANIC

Dark Black to Green Hafic Hinerals: 70 -: 30Fine Grained Schistosity "70

13346133471334813319133bO

19.7021.3022.8024.3025.50

21.3022.8024.3025.5027.10

1.601.501.501.201.60

LES EXPLORATIONS

08-22-1987: :10:31 DIAMOND DRILL

From lo ~---.~. . .-......()escr ip^ orr .--...---,... ... ..W d)

Highly Fractured (20 Fractures/Meter)Pyrite; ^Chlorite Alteration: 50Biotite Alteration: 10Non MagneticNon Conductive

This small unit begins and ends with a sharp contact withpatchy quartz pods and stringers concentrated near thecontacts.

Small narrow quartz-carbonate stringers ( </- limn) strungout along schistosity ; resulting in a dark-light coloredfine banding, The higher degree of fracturing is relatedto the schistose nature.

Ihis unit likely represents a mainly chlohtically alteredmafic volcanic roof pendant. An identical occurencc isfrom 16.2 -y 16.4m,

57.5 59.5 GRAN1TIZED HAF1C VOLCANICS

Dark Purple to BrownQuartz: 40Mafic Minerals; 15-: 45Fine to Medium GrainedFoliation at 40 Deg. Cax.Weakly Fractured (9 Fractures/Meter)Magnetite; 5

NORAMCO INC.

LOG

SampleNo.

1335113352133531335413355133561335?1335813359133601336113j62133631336413365133661336?13368133691337013371

133?213373133741337513'j761337/133/813379

From(m)

27.1028.5030.0031.6033.0034.4035.9037.4039.0040.5042.0043,4044,9046.4047.9049.3050.8052.5054.0055.3056.90

57.5058.5059.5061,0062.6064.2065.706/.20

lo(B)

28.5030.0031.6033.0034,4035.9037.4039.0040,5042,0043,4044.9046.4017.9049,3050.8052.5054.0055.3056.9057.50

58.5059.5061.0062,6064.2065.7067.2068.60

KL-87-13

Page 5

Width Au Ag Cu Zn Pb Sb As K(m) (ppm) (ppm) (ppm) (ppm) (ppm/ (ppm) (ppiM ipp?.;1.401.501.601.401.401,501.501,601,501,501,401.501.501.501.401.501.701.501,301.600.60

1.001,001.501.601.601.501,501.40


08-22-1987: :10:31 DIAMOND DRILL LOG

From lo - - -- ---Description--------------------( ) W

Potassic Alteration: 5Carbonate Alteration: 2Moderately MagneticWeakly Conductive

The upper 10cm of the unit begins at a sharp contact andcontains a strong hematitic alteration. This portion israther rubbly.

The strong hematitic alteration ends rather abruptly andthe rest of this unit contains only moderate hematiticalteration. Ihere is one km by 2cm K-feldspar crystalpresent in the center of the unit,

The lower contact is sharp (g 30 deg.) and is proceeded byapproximately 10cm of foliated ( */- finely brecciated )material, This foliation is not obvious anywhere else inthe unit,

The Magnetite is very finely disseminated. Ihis unit couldbe a granitized mafic volcanic roof pendant.

108.8 112.1 GRANITIZED MAFIC VOLCANICS

Same as 57.5 ^ 59.5mMagnetite: 5

Sample FromNo. (in)

1338013 M1338213383133841338513386133871338813389133901339113392133931339413395

1339613397133981339913400131011340213403;3404

134051340613407

68/O7072747577788081828485878990

969799

10010110210410510?

108110112

.60

.10

.80

.30

.00

.70

.20

.70

.20

.40

.90

.40

.90

.40

.00

.50

.00

.40

.00

.40

.00

.70

.30

.80

.40

.80

.40

.10

7070727475777880818?848587899097

9/99100101102104105107108

110112113

lo(m).10.80.30.00.70.20.70.20.40.90.40.90.40.00.50.00

.40

.00

.40

.00

.70

.30

.80

.40

.80

.40

.10

.80

KL-87-13

Page o

Width Au Ag Cu In Pb Sb hi K(m) (ppm) (ppm) (ppm) ippsi) (ppm) (ppm) Ipp-V) '.ppm)1.500,701.501.701.701.501.501.501.201.501.501,501,501.601.501.50

1.401.601,400.601.701.601,501.601.40

1.601.70J. 70

08-22-1987: :10:31

from To -------(B) (ffi)

StrongSem

142.4

MottledQuartz:

LES EXPLORATIONS

DIAMOND OR RI

----------------Description------------ --------"

sharp contacts at 70 deg. Moderate foliation withinof either contact g 70 deg.

148.7 GRANITIZEO VOLCANIC TUFF

Purple to Brown40

Hafic Hinerals: 15-: 45fine to Medium Grainedfoliation at 55 Deg, Cax.Weakly(li Qua

1.5cm

fractured (6 Fractures/Heter)rtz-Carbonate Vening at 40 Deg. tax. -- Avg. Width

NORAMCO INC.

LOG

SampleNo.

134081340913410134111341213413134141341513416

1341?

13418134191342013421

13422134231342413425134261342?13428

13429

from(m)

113115116118120121123124125

132

138138140141

14214414514?148149151

155

.80

.40

.90

.40

.00

.60

.20

.10JO

.10

.CO

.90

.10

.40

.40

.00

.50

.10

.70

.50

.20

.60

115116118120121123124125126

133

138140141142

144145147148149151152

156

lo(m)

.40

.90

.40

.00

.60

.20

.10

.30

.10

.50

.90

.40

.40

.40

.00

.50

.10

.70

.50

.20

.80

.50

KL-87-13

/ige 1

Width Au Ag Cu in Pb Sb As M(m) (ppm) (ppm) (ppni) (ppm) (ppm) (ppm) (ppni) l^u;

111111010

1

0111

1111011

0

.60

.50

.50

.60

.60

.60

.90

.20

.80

.40

.90

.50

.00

.00

.60

.50

.60

.60

.80

.70

.60

.90Hagnetite: 5Pyrite: </'- l 13430 158 .10 159 .80 1 ./O

8-22-1987::10:31


DIAMOND DRILL LOG

From lo .--..----..-----...[)escr |ptj on-.--.--..--.--.-------( ) (B)

Silica Alteration: 5Biotite Alteration: 5Weakly Magnetic -mNon Conductive -w

Quartzofeldspathk subrounded to stretched lapillifragments 2-5wi. Weak foliation exists in central portion("55 to C. A,) and stronger foliation exists within 20cm ofupper and lower contacts.

Overall appearance of groundmass Material is the same as5?. 5 -^ 59.5m ( compositionally S coloration ). Foliationis marked primarily by planar fabric of aligned biotitegrains.

There is one quartz-carbonate veinlei with some pinkfeldspar internally and chlorite on the contacts, Minorpatchy silicification exists in the central area of thesubmit. The upper contact is at ~60 deg. and the lower at"70 deg.

SampleNo.

13431334321313313434

13435

13436

1343?13433

13439

13440

1344113442

13443134441344513446

P r(

159161162164

165

16?

1721/3

17?

180

184193

195196198199

omffi).80.30,90.20

.50

.80

.20

.40

.20

.00

.90

.10

.20

.80

.30

.80

161162164164

166

169

173174

l/?

181

18b194

196198199201

lo(m).30.90.20.80

.60

.00

.40

.40

.80

.10

.00

.50

.80

.30

.80

.40

Width(ffi) (1.501.601,300.60

1.10

1.20

1,201.00

0,60

1.10

1,101.40

1,601.501.501,60

Au Ag

KL-87-13

Page 8

M In Pb Sb(ppm) (ppm) (ppm) (ppni) (ppii) (ppi*) ippau ippm)

1344? 208,80 210.30 1,50

210.9 END OF HOLE.

3-22-198?:;10:31


DRILL LOG - GtOCHEH SAHPLES

KL-87-13

Sample From lo Width Au Sb As Ba Cd Cs Cr Co Cu Eu Hi Ir re La Ho Ni Rb S: Se Ag 1;; ; le InNo. (m) (m) (m)

14116 8.10 15.20 7.10

14117 93.50 95.00 1.50

14118 127.10 131.40 4.30

14119 134.20 137.20 3.00

14120 153.00 154.50 1.50

14121 169.20 170.70 1.50

14122 175.00 176.50 1.50

14123 178.00 179.40 1.40

14124 181.70 184.60 2.90

14125 186.30 192.30 6.00

14126 202.40 208.50 6.10

ppb ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppb pet ppm ppm ppm ppm ppm ppn. ppm ppn. ppm ppm ppro ppr ; ppn,

Sample Scan: k!13

Fire Assay 13343 to 1344?

Geocheu 14116 to 14126

ERROR REPORT

: Sample Data File Missing!

1 FROM. NORfiMCO EX PICKL P . 5

AZIMUTH; 110.4.^.., — —i-* — ..T- -J-- -- — —1-^*- rto Tio

10

100

120

140

110

110

DC or HOU;

KL-87-14

GUARTt FELDSPAR PCWWRY

NORAMCO EXPLORATION

too Keetelk Ukc 1441 Diamond Drill Section

TR:'B4400N

110[Dipt M ifagrt DiU On^nt

Tciiit! tl IBMOt 1000

3-22-1987::10:31

Property: Keehzik Lake 1441

Partner: Severide Resources

Azinuth: 180 degrees'TvvC.^.V.cc,,,-.

Logged By: C^K. Zazulak

Date Started: July 21 1987

Core Size: BQ

Drill Cospany: Longyear


DIAMOND DRILL LOG

KL-87-14

NTS:

Liau, f:

Dip:

52P

TB 656483

-50 degrees

Casing: out

Date Completed: July 23 1987

Core Location: Keehzik Lake

Overburden: 3.14 Beters

Acid Dip Jests

l l, 102.7 K 48.5 deg.

Purpose

Conclusions

to test IP anonaly

pending assay results

fonnship:

Coordinates: 54+OOW , 23+50S

Length: 203.3 neters

Elevation: Surface

Date Logged: August 2 1987

Samples Shipped: August 7 1987

l 2, 203.3 B 47.5 deg.

— — - —— - ——-" — — — — — — — — — -- — — —- — - — -- — - —— — - — -- — — — —-~—-—— — -- — ---- — —- — - — - — --- — ----——-----~--~---- — -- — -- — -- — -~—- 1---'--*--" — — -- — -- — -- — — --------.•- — ------ — -~---------------------- "J^™^ - - -


08-22-1987: :10:31 DIAMOND DRILL LOG -- SUHhARY Pa',? 2

Fron(ji) lo(ro) -----------------------[jescription---------"------------------------'--------------^^

0.0 3.1 OVERBURDEN

3.1 203.3 SAB QUARTZ FELDSPAR PORPHYRYPyrite ( trace-2!) Carbonate i l-li] Tourmaline ( Trace) Vellow-Green Sericite i 2-':';) Chalcopyrite ( trace) Potassic ( up to 501)

203.3 END OF HOLE.


8-22-198?; :iO:32 DIAMOND WILL LOG Facie J

Fromd)0,0

To -(m)0.0 OVERBURDEN

-------Description-------------- -- ---- Sample

No.From

(ffi)lo(B)

Width(ci)

nU

(pptii)Ag tu

(pptii) (pf.m)i \ \ i \J J f

Ippni) (ppid) (ppuii (ppuifi.'

!,3pH'.'

3.1 203.3 SAB QUARTZ FELDSPAR PORPHYRY

Mottled Light to Green 16001 3.11 3,96 0.8? Quartz: 40 16002 3.96 4,56 0.60 K-Feldspar: 30 16003 4,56 5,24 0.68 -: 30 16004 5,24 5.96 0.72 Fine to Medium Grained 16005 5.96 6.66 0.70 MassiveWeakly Fractured (5 Fractures/Meter) 16006 29.5? 30.41 0.84 less than l * Quartz-Carbonate Veining at Random Angles -- 16007 30.41 31.11 Q. /O

AYQ. Width 0,5cmPyrite: trace-2l 16008 41.4? 42.06 0.59 Tourmaline: Trace 16009 42.06 42.90 0.84 Chalcopyrite: trace 16010 42.90 43.53 0.63 Carbonate Alteration: 1-21Yellow-Green Sericite Alteration: 2-51 16011 59.75 60,53 0.78 Potassic Alteration: up to 50! 16012 60,53 61.50 0,97 Non Magnetic 16013 61,50 62,94 1.44 Non Conductive

16014 74.09 75.12 1.03 The unit is flesh (tan) to pale green in colour; fine tomedium grained; massive; 16015 89.35 90.2? 0.92

contains up to 20? quartz as l-2mm subrounded phenocryst^; Ibul6 90.27 91.51 1,24also contains 2min-lcii (ave 5-7mm) subhedral to subrounded

flesh coloured feldspar phenocrysts 2-3* (up to 52 in loDl/ 106,90 107.57 0.6? heavily feldspar altered sections) which locally may be 16018 107.5? 108.22 O.b'j zoned ;

overall the unit is weak to moderately carbonate altered 16019 115.48 116.14 0.66(locally strongly pervasive sections) and contains 16020 lib. 14 116,71 0.5?

It less than HIM wide quartz-carbonate fracture fillings 16021 116.71 117,40 0.69and veinlets at random core angles (locally vuggy and\or J60?? 117.40 118,00 0,60

tourmaline lined); the unit is also weakly to moderately

8-22-1987: :10:32

LES EXPLORATIONS NORAHCO INC,

DIAMOND ORiLi LOG

KL-87-14

Froni(ffi)

lo(m)

Description

sericitized which locally imparts a yellowish green tingeand increases proportionally with the degree of

SampleNo.

1602316024

From(m)

132,95134,1?

lo(m)

134.17135,32

Width(ra)1,221.15

nU ny

(ppin) (ppm)Cu

(ppffl)in

i ppm)Pb So(ppm) {ppm)

As pic(pprc; i ppi;

silicification and carbonate alteration; the entire hole is feldspar altered imparting a mottled

appearance (weak in silicified sericiti/ed zones) up tointense

zones (usually 1-2 feet wide) locally; the unit alsocontains lrace-3! clay minerals (kaolinite) within thegroundmass

and infill oxidized leached fractures and ve in lets;mineralization consists of trace to l\ pyrite (0.5-U ave)

which occur as euhedral disseminations less than 1mmthroughout and trace chalcopyrite as minute disseminations

(mineralization increases in silicified\sericitized zones) Silicified zones (m): 29.57-31.11; 42.06-42.90 59.75-61,50; 74.09-75.12; 89.35-91.51; 106.90-108.22;

115.48-118.00; 132.95-135.32; 195.10-196.30

16025 188,49 189.5? 1.03

160261602?16028160291603016031

194.195.196.197.198.198.

3?1030210472

195.196.19?.198.198.199.

10302104y 260

0./3J. 200.910.830.6?!O.iiS

203.3 END OF HOLE.

8-22-1987:;10:32


DIAMOND DRILL LOG -- GtOCHf'H SAMPLES

KL-87-14

Page 5

Sample FromNo. (m)

14351 6.66

14352 12.3?

14353 19.74

14354 32.79

14355 38.34

14356 43.96

1435? 49.75

14358 55.45

14359 64.32

14360 70.11

14361 76,02

14362 83.03

14363 91.77

14364 97.63

14365 103.3?

14366 109,90

1436? 119.34

lo (s)

11.97

18.28

26.95

37.02

41.21

48.30

54.00

58.30

68.52

73.13

81,50

88.80

96,15

101.92

106,32

115.00

123.70

Width Au (m) ppb

5.31

5,91

7.21

4.23

2.8?

4.34

4.25

2.85

4.20

3.02

5.48

5.7?

4.38

4.29

2.95

5,10

4.36

Sb As Ba Cd Cs Cr Co Cu [u Hf Ir f e La Ho rti Rb Se Se Ag L ;., le l ppn] ppm ppm ppm ppm ppm ppn ppm ppm ppm ppb pet ppn ppm ppm ppM ppm pprn ppm ppm pp,n ppci o pp:/ ppni ppfi. pi-

LES EXPLORATIONS NORAMCO INC KL-87-14

8-22-1987::iO:32 DRILL LOG -- fetOCHtH SAHPLL'S

Sample No.

14368

11369

14370

11371

14372

11373

14374

14375

14376

14377

F n(i

125

136

143

149

155

163

171

179

190

199

Dill

1)

.00

.50

.81

.63

.35

.14

.0?

.76

.96

.98

lo (

132.

142.

148.

153.

161.

169.

178.

185.

194.

202.

)

22

30

15

85

22

60

27

48

20

7?

Mi (

7

5

4

4

5

6

7

5

3

2

dth Au Sb As 8a Cd k Cr Co Cu tu Hf Ir fe La Mo Ni Ro Se Se ACJ \-, ;s le :,l rt b r: r, ni) ppb ppm ppm ppm ppn; ppm ppm ppji ppir, ppm ppm ppb pet ppm ppm ppm ppiri ppni ppm ppra ppm ppai ppm ppa pppi ppni ppm p^c,

.22

.80

.34

.22

.87

.46

.20

.72

.24

.79

Sample Scan: kill

Fire Assay 16001 to 16031

Geochea 1-1351 to 14377

ERROR REPORT

WARNING: Sample Data File Hissing!

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

FROM, NORflMCO EX F'lCKL P. J

AZIMUTH! 1BO digKL-B7-15

10

40

100

140

2CO

220

. 240

-jL.. . ....^j . . , ^.j... .. ..—u....^....—j—. ..——.4—-—- . 4 ..1* Ik ifc lo ib ^o JT

DO OP HOU: 209.8

OVERDUnOCM

(M8) OWm- FEUWPWl PCflWKY

rNORAMCO EXPLORATION

Keezhik Lake Diamond Drill Section

"LMMttoni U^OOT ( 1 (

"bljit-fo.^! 203,1

TBB5M7B i j t 1000

08-22-1987::10;32


DIAMOND DRILL LOG

KL-87-15

Property: Keezhik Lake (1441)


Azimuth: 180 degrees

Logged By: {*r G J Forbes

Date Started: July 16 1987

Core Size: BQ

Drill Company: Longyear

1 1. ' 102. 7 a

NTS:

Claim H:

Dip:

Casing:

Date Completed:

Core Location:

Overburden:

An

52 deg.

52P

IB 656475

-50 degrees

Out

July 18 198?

Keezhik Lake

4 meters

d Dip Tests

Township:

Coordinates:

Length:

Elevation:

Date Logged:

Samples Shipped:

1 2. 203.3 i 44 deg.

L54*00y , 11+OOS

203.3 meters

Surface

July 24 1987

July 27 1987

Purposelo test IP anomaly

ConclusionsIP anomaly possibly caused by weak pyrtie (11) mineralization.

RecommendationsAbundant sericite and potassic alteration was observed with only a minor amount of silicification. Further drilling

recommended pending assay results.

8-22-1987::10:32


RIM LOG - SUMMARY

KL-87-15

Page 2

Description-Froiii(ic) IO(IB)

0.0 4.0

4.0 203.3 [SAB] QUARTZ- FELDSPAR PORPHYRY

-Mineral kfition(s)"-------—-•----••----Aheration(sj----- ---------

Pyrite { 1) lourmaline ('-1)

Yel low-Green Sericite ( id) Potassic ( 3) Carbonate ( 2) Silica ( <l)

203.3 END OF HOLE.


3-22-1987;:10:32 DJArtOND DRILL LOG Page 3

From W 0.0

Tn —--. — . ...,....10

(i)

4.0 OVERBURDEN

—---Description- ——--—— --------- Sample No.

From (tt)

To (m)

Width (m)

Au Ag (ppni) (ppm)

Cu 2n (ppti) (ppni)

Pb Se As f ppni) { ppm)

fi: (Ppn.)

(.0 203.3 [SAB] QUARTZ- FELDSPAR PORPHYRY

Light Grey-White 16001 3.14 3.96 0.82Quartz: 50K-Feldspar: 30-; ther 20AphaniticHassiveWeakly Fractured (5 Fractures/Meter)^ Quartz-Carbonate Veining at 45 Oeg. Cax, -- Avg. Width

leaPyrite: l Tourmaline: 4Yellow-Green Sericite Alteration: 10 Potassic Alteration: 3 Carbonate Alteration: 2 Silica Alteration: ^ Non Magnetic Non Conductive

The groundemass is asphanitic and the phenocrysts are medium grained. The unit contians feldspar phenocrysts Mem) and quartz phenocrysts Wim). Pyrite occurs as disseminations ; anhedral masses and euhedral crystals

The entire unit has seritic alteration with small sections of potassic (purplish red) alteration. Both of these alterations have been locally overprinted by silicification.

The sercitic alteration is a light green white colour and is chalky in nature. The carbonate alteration is found along microfractures throughout the unit.

8-22-198?;:10;3?


DlArtONO DRILL LOG

KL-87-15

From To (a)

-Dtscription-

Ihe tourmaline crystals are found along fracture planes and in small veins Wnim). Feldspar phenocrysts in the sericitic alteration areas are pale white to beige , feldspar phenocrysts in the potassic alteration areas are ligth pink.

The potassic alteration is divided into three parts. Weak potassic alteration (faint purplish colour and patchy){ 12V.l-133.ls 135.4-139.3; 140.9-141.5; 143.6-144,5; 159.3-162.9; 165.7-171.i; 179,9-183,0; 19?.2-200.? }

Moderate potassic alteration (light purplish colour) {15.2-15.9; 17.2-18,8; 30.5-34.8; 41.4-44.8; 65,9-76.0; 87.6-92,8; 99.7-102.4; 106.1-108.3; 110.1-119.0; 144.5-148.1; 183,0-190.9}

Strong potassic alteration (deep purplish red colour) {83,9-85. h 120.2-124.4; 192.0-195.7}

Silicified area 12.4-13.1. Fault gouge (52.6). Shear zone around fault gouge (50.8-53.7) with quartz fracture- fillings. Quartz vein (52.3-52.4) Intense shearing around fault gouge (52.4-52,7), Potassis alteration with overprinting of silicification (158.2

Sample From lo Width Au Ag Cu Zn Pb Sb As i* No. (PI) (m) (m) (ppm) (ppm) (ppm) (ppn;) (ppm) (ppm) (ppe) (

203.3 END OF HOLE.

l l l l l l l l l

FROM HORftMCO EX PICKL P. 6

i. 4)

. 80

loo w

KL-87-16

"ilb" "T& ~1o "~ to

1*1 PtLSIC TUTF

(4CJ

(4ft FO8IC LW1U.I TUFF,

//

11111

1111111

J. /h100 //y s y

/^jf/

I ^//' ^\*\ tune upjLLi turf

/x~ ^

OD OF HOLE; tn.B wUrt,, tao

240

(K) IKTOWeOIATt IAP1U1

ici reusjc lAPiai nrr!C) FBJ1C LAPILLI

to ra.6ic LAPILLI nrr

•tlMI ttMKTZ RXOSPAR

r ...... .... . ...

! NORAMCO EXPLORATION

il


't***. kUt July J^/T

178.6 "1144801 , "

Ife-wj!1

* 1 lJU",-.*-.-*-

08-22-1987;:10:56

Property: Keezhik Lake (1441)


Azinuth: 135 degrees^VvV^K-laUx.-.-

Logged By: ^ Hark Cooper

Date Started: July 23/8?

Core Size: 8Q

Drill Conpany: Longyear


DIAMOND DRILL LOG

KL-87-16

NTS: 52P

Claii t: 919497

Dip: -50 degrees

Casing: In

Date Cospleted: July 27/87

Core Location: Keezhik Lake

Overburden: 8.8 meters

Acidjiip Tests

S l, 96.6 i 46 deg. f 3. 279.5 M 44 deg.

Township:

Coordinates: L54+50W , 15+45S

Length: 279.5 neters

Elevation: Surface

Date Logged; July 31/87

Samples Shipped: Aug. 8/87

f 2. 188.1 w 45 deg.

To test IP anomaly near NE trending photo-linear.

Conclusions

Recomaendations

The weak chargeability of the IP anomaly is due to a slight increase in the pyrite content 2-3! within the silicifiedfelsic tuff sections.

The weak lagnetic anonaly is due to the sagnetite content within the felsic tuff. A silicified section (79.l-79.7in ; .82.8-85.2n) appears very siiniliar to the auriferous zone intersected in KL-87-12.

Further drilling pending assay results.

8-22-1987::10:56


DIArtONO DRILL LOG -- SUHHARY

KL-87-16

Page 2

Froffl(it) To(ifl) —————————Description-

0.0 8.8 OVERBURDEN

8.8 44.5 [4E] FELSIC TUFF

••-Mineralization(s)-"""---------" —---Aiteration(s) —----------—'

44.5 158.0 [SAB] QUARTZ FELDSPAR PORPHYRY

79.7 82.8 [3E] INTERHEDIATE LAPILLI IUFF

121.4 127.S [IE] FELSIC LAPILLI TUFF

131,3 133.7 [4E] FELSIC LAPILLI TUFF

158.0 279.5 [4E] FELSIC LAPILLI TUFF

Pyrite W!) Magnetite (61)

Pyrite

Tourmaline

Pyrite Wt) Magnetite (21)

Pyrite Magnetite (51)

Pyrite W Magnetite

Pyrite (l!) Magnetite (14) Tourmaline

Fellow-Green Sericn? (20i Potassic (2-i) Carbonate (21)

Yellow-Green Sericite (5*j Carbonate (11)

Chlorite ((strong 501)) Carbonate (101)

Yellow-Green Sericite (IV. Chlorite (31) Carbonate (11)

Yellow-Green Sericite iiOI) Chlorite (3 ;i) Carbonate (11)

Silica (51) Biotite (21) Chlorite (14 Carbonate

6-22-198/1:10:56


DIAHIM) DRILL LOG -- SUHHARV

KL-87-16

From (B) To(ti) -----------------------[) e scnption-------

158.0 158,3 [4E] FELSIC LAPILLI TUFF

160,5 1/0.8 ME] FELSIC LAPILLI TUFF

-Mineral i;:ation(s)

Pyrite (3s.)

Magnetite (71) Pyrite WD

1/0.8 195,8 [4E] FELSIC LAPILLI TUFFPyrite ('11) Magnetite (i?

-ftherationu)-

Silica (20',)

Silica (51) Chlorite (11) Biotite (21)

biotite (iO'c Chlorite Sericite (li Green Mica Silica (21 Garnet M

279.5 END OF HOLE.

08-22-1987: :10:

From lo(ffi) (i)

0.0 8.8

8.8 44.5


56 DIAMOND DRHL LOG

—— -,. — -. ———— pescr jp^ on............ — . ———

OVERBURDEN

[4E] FELSIC TUFF

Banded Light-Tan to Green-GreyQuartz: 40!-: 60!fine to Medium GrainedSanding at 45 Deg. Cax.Weakly fractured (8 Fractures/Meter)41 Quartz-Carbonate Veining at 50 Deg. Cax. -- Avg. Width

5mmPyrite: ^lMagnetite: 6!Yellow-Green Sericite Alteration: 20!Potassic Alteration: 2!Carbonate Alteration: 2!Moderately MagneticNon Conductive

SampleNo.

134481344913450

13451134521345313454

13455

13456

13457

from(m)

12.9014.3015.60

22.7024.3025.8027.30

33.50

37.80

43.20

loW

14.3015.6017.10

24.3025.8027.3027,90

34.90

38.80

44.50

KL-87-16

Page 4

Width Au Ag Cu ?n Pb So As do(m) (ppm) (ppm) (ppm) (ppm) (ppm) (ppin) (ppsi) (ppir.;

1.401.301.50

1.601.501.500.60

1.40

1.00

1.30

Other 60! includes 201 feldspar due to incompatible programcode. It is a buff light green-grey color with very slightsalmon (k-alteration) patches.

The grain size is a homogenous O.Snn! to v.f.g. In twoplaces over a few centimeters there are coarser fragments(2-4mni) of feldspar subangular to subrounded lapilli(20.9m l 37.5m).

The f.g. magnetite grains are disseminated with a fairlyuniform distribution, The bedding angle varies from 15-55deg. and is only distinguishable in 20! of the unit due toa strong wavy sericite pseudobanding.

In a few places the pyrite content increases to 2-3! alongpitted carbonate stringers ; and surrounding these is amore pervasive sericite halo (37,6-38.8m).


08-22-1987: :10:56 DIAMOND DRILL lOt Page 5

From lo -————.---—.--[)escr ipti on--—..-..-.---—... Sample From lo Width Au Ag Cu 2n Pb Sb As(m) (K) No. (m) (in) (in) (ppm) (ppm) (ppm i (ppm) (ppm) (ppsO (ppnj

The lower contact of this unit with the QFP (11,5m) is of awavy sutured nature at 30 deg. to the C.A. Ihe wavysericite alteration is quite strong within 10cm of thislower contact,

At 40 deg. to C.A, (90 deg. to bedding and wavy sericite)are tiny fractures offsetting the bedding and wavysericite material (leu displacement).

The core exhibits a chalky surface when touched indicatinga possible clay (illite?) component to the sericitizedgroundmass,

44.5 158,0 [SAB] QUARTZ FELDSPAR PORPHYRY

Mottled Light-GreenQuartz: 401K-Feldspan 25*-: 351AphaniticMassiveWeakly Fractured (6 Fractures/Heter)(\\ Quartz-Carbonate Veining at 60 Deg. Cax, -- Avg. Widthkm

Pyrite: M Magnetite: TRACE Tourmaline: 41Yellow-Green Sericite Alteration: 51 Carbonate Alteration: U Non Magnetic Non Conductive

This unit again is a QFP similiar to KL-87-12 and Kl-87-13. The core is a pale green color with 301 quartz (Hmia) anhedral subrounded to subangular phenocrysts.

08-22-1987::1Q:56


DRILL LOG

KL-87-16

frois (si)

ToW

-Description- Sample No.

from lo du)

tt of the unit contains larger zoned feldspar phenocrysts.In places they increase in abundance to 5-81. Accessoryhornblende (up to 51) sometimes appears aligned in a weakfoliation in some of the silicified areas (60 deg. toC.A.).

The groundmass is a white chalky (illiite?) and pale greencolored sericitized microfelsitic material,

Hinor carbonate is pervasive throughout alongmicrofractures and as a coating on the feldsparphenocrysts.

A minor shear at 58.8m is 25cm wide and contains 2-31pyrite in a strongly foliated (45 deg. to C.A.) mainlysericitic material,

Small 2mm quartz-carbonate stringers are parallel to thisfoliation in the sheared area. The upper 5m of this unithas a weak magnetic response.

Tourmaline coated fractures are common, from 143.5-158.0the porphyry appears slightly greener and at 146.5m thereis a small km by 2cm splotch of green mica.

At 149.6m is a patch over 5cm of bright orange carbonate.

44.5 158.0

The potassic alteration areas containing O! pyrite are as follows; W - Weak potassic alteration (ie, only faint and 13460 patchy) ; n - hoderate potassic alteration (ie. consistent pink purplish color) ; S - Strong

potassic alteration (ie. purplish red color), The contact areas are generally ha?y and the larger feldspar phenocrysts are slightly pinkr,

: 44.5-45,Oni 105.8-116.6m

49,5-51.4m ; 52.O-53.li ; 89.7-92.Om

Width (m)

Au Ag Cu 2n Pb Sb As .lo (ppai) (ppm) (ppii) (ppni) (ppc;) (ppm) (ppsi) ippiii)

39.3-143.bm fi: 45./-49.5m

134581345913460134611346?134631346413465131661346?

44.5046.1047.8049.4051.0052.5054.0055.5057.0058.50

46.1047,8049,4051.0052.5054.0055,5057.0058.5060.10

1.601.703.601.601.501,501,501.501.501.60


08-22-198?: ;10:56 DIAMOND DRILL LOG

Prom To -- — ---------------tJescription-----------------------M d)

51. 4-52. On ; 53. 1-53. 6m S: 120. 1-121. 4mIhe silicified areas containing 1-21 pyrite are as follows:

A moderate degree of silicification exists at 15. 0-66, lin; 111. 6-11?. 1m ; 116. 6-121. 4m ; 129. 1-131. 3m ;133.7-156.7i,

A stronger degree of silicification with loss of theoriginal fabric exists at 66, 1-85. 2m ; 127. 5-129. lin ;156. 7-160, 5m,

Very similiar to the auriferous zone in KL-87-1? is thesection froir, (79. 1-79. 7m ; 82.8-85.2ni) which contains thesame dark grey-blue quartz and sericite stringers.

Ihe upper contact is gradational while the lower contact(85.2m) is sharp at 47 deg. to the C. A. Some more bleached

SampleNo,

13468134691347013471134721347313474134751347613477134781347913480

From(B)

60.1061.6063.2064,9066,4068,0069,5071.1072.5074.1075.8077.5079.10

loW

61.6063.2064.9066.4068,0069,5071.1072.5074.1075.8077.5079,1079.70

KL-87-16

J'ACjf ?

Width Au Ag Cu Zn Pb Sb As f,o(m) (ppm) (ppm) (ppm! (ppwj ippir,} (ppai) (ppm) (ppo^1.501.601,701,501.601.501.601.401.601.701,701,600,60

silicified sections with minor surface pitting contain up to 2-o pyrite.

———————Sub Units———————

79.7 82.8 [3E] INTERMEDIATE LAPILLI TUFF

Nottled Black to Green 13481 79.70 81.20 1.50 Mafic Minerals: 601 13482 81.20 82.80 1.60 Carbonate: 104 13483 82.80 84.10 1.30-: 30". 13484 84.10 85,20 1,10 Fine Grained 13485 85.20 86,70 1.50 Foliation at 75 Deg. Cax.Moderately Fractured (10 Fractures/Meter) 13486 91.00 92.40 1.40 ^1 Quartz-Carbonate Veining at 60 Oeg. Cax. - Avg. Width

2cai 1348? 101,30 102.70 1.40 Pyrite: (liMagnetite: 21 13488 111.60 112.10 0.50 Chlorite Alteration: (strong 502)Carbonate Alteration: 101 13489 113.60 115,10 1,50 Weakly Magnetic 13490 115.10 116.60 1.50


08-22-1987;:10:56 DIAMOND DRILL LOG Page 8

From To ...—-—-—.—-—[)escr ipti on ------------...--------- Sample From lo Width Au Ag Cu Zn Pb Sb As no(a) (w) No, (m) (m) (m) (pptii) (ppni) (ppui) (ppm) (ppm) (ppm) (ppai) (ppai)

Non Conductive 13491 116.60 118.00 1.4013492 118.00 119.40 1.40

This unit is a strongly altered intermediate volcanic. 13493 119.40 120.10 0,70 The 2-4mm lapilli (IDS) Maintain their slightly stretched 13494 120.10 121.40 1,30

form parallel to the foliation but have been replaced bycarbonate.

The one veinlet mentioned above has no associatedmineralization. Approximately 12 of the unit consists ofthin 2imi!-5mm wavy carbonate stringers subparallel to thefoliation.

Contained within this unit is a section of the QFP from81.7-82.In that exhibits a weak bleached silicification,

On both sides of this unit is the strongly silicifieddarker grey-blue material similiar to the auriferoussection in KL-87-12. The upper and lower contacts are verysharp at 70 deg. to the C.A.


Mottled Grey to Green . 13495 121.40 122.80 1.40 Quartz: 50? 13496 122.80 124.30 1.50 Lapilli: 301 13497 124.30 125.30 1.00 -: 201 13498 125.30 126.80 1.50 fine to Medium Grained 13499 126.80 127.50 0.70 Foliation at 55 Deg. Cax. 13500 127.50 129.10 1.60 Weakly Fractured (6 Fractures/Meter) 16032 129.10 130.60 1.50 Pyrite: m 16033 130.60 131.30 0.70 Magnetite; 51Yellow-Green Sericite Alteration: 1\ Chlorite Alteration: 3* Carbonate Alteration: 11 Weakly Magnetic Non Conductive


08-22-1987::10:56 DIAMOND DRILL LOG P d ge 9

From lo ————————------Description—-----—----------- Sample From To Width Au Ag Cu In Pb Sb As do(li) (m) No. (m) (m) (m) (ppm) (ppm) (pp/n) (ppw) (ppm) (ppin) (ppm)

The lapilli range in size from 2na to 3cm, Host aresubangular to subrounded fragments stretched within thefoliation plane with a flattening ratio of 3:1.

Most of the fragments are quartzo-feldspathic incomposition ; and many of the feldspar rich fragments havebeen altered strongly to sericite.

Finely disseminated magnetite occurs throughout the matrixand rarer larger magnetite fragments (up to 2cm) with tinypyrite cubes in the center are present.

The pyrite occurs mainly as tiny (1mm) cubes within thesericite-chloritized matrix material. Narrow l-2nincarbonate stringers are generally parallel to thefoliation.

A narrow band of intense shearing (leu wide) at 121.6mcontains only finely ground up rock,

The upper and lower contacts are sharp at 55 deg. to theC.A. with the QFP. A slight increase in pyrite to lioccurs within 20cm of the lower contact,

131.3 133.7 [4E] FELSIC LAPILLI JUFF

Same as 121.1-127.5 16031 131.30132.80 1.50Foliation at 55 Deg. Cax. 16035 132.80 133.70 0.90Pyrite: 4* 16036 133.70 135.10 1.70Magnetite: 5! 16037 135.10 137,00 1,60Yellow-Green Sericite Alteration: 101 16038 137.00 138.60 1.60Chlorite Alteration: 31 16039 138.60 139.30 0.70Carbonate Alteration: li 16010 139.30 110.70 1.10

16041 110.70 112.20 1,50This unit is the same as that of 121.1-127.5m basically. ib042 112.20 113.60 1.10

The upper contact is diffuse and sericitization is very 16013 113.60 145.00 1,10

08-22-198?: :10:56

From loW W

strong

LES

--———--Description

over the upper 20cn.

EXPLORATIONS NORAMCO INC.

Overall there is more sericite thanfoliation is also not quite as

The lowerto 3mm)50 deg.

Below 133(hi).

D1AHOND DRILL

from 121.M27.5i. Ihewell developed.

50cm has more pyrite (H). Ihe lower contact atto the C. A,,7m the QfP exists with

133as euhedral cubes (up,7m is fairly sharp at

a narrow chill margin

LOG

SampleNo.

160111601516016160171601816049160501605116052

From(m)

115.00116.50118.10119.60151.20152.70151.20155.70156.70

11611811915115?151155156158

lo(m).50.10.60.20.70.20.70.70.00

Width(B)1.501.601.501.60i. 501.501.501.001.30

KL-87-16

Page 10

Au Ag Cu Zn Pb Sb As no(ppm) (ppm) (ppm) (ppiii) (ppm) (ppm) (ppm) (ppia)

158.0 279.5 [4E] FELSIC LAPILLI IUFF

Mottled Dark to GreyQuartz; 601Lapilli: 251-: 151Foliation at 60 Deg. Cax.Weakly Fractured (6 Fractures/Meter)4! Quartz-Carbonate Veining at 50 Deg. Cax. -- Avg. Widthkm

Pyrite; 11 Magnetite: 11 Tounnaline; 4! Silica Alteration: 51 Biotite Alteration: 21 Chlorite Alteration: l! Carbonate Alteration: 41 Weakly Magnetic Non Conductive

Lapilli fragments (mainly felsic) vary from 2m to slightly greater than 6cm (ie. bombs). The average lapilli size is

3-22-198?::10:56


D1AHOND DRILL LOG

KL-87-16

Page 11

From (M)

To (K)

-Description-

lcm,In general the fragments have a fairly high sphericity and

range from angular to subrounded, Tiny ^mn fractures sometimes displace broken fragment halves a few millimeters.

The matrix material is almost universally altered to varying degrees with biotite and quartz. liny microfractures up to veinlet size fillings of carbonate (*/- vuggy) are present intersecting at random angles to the C.A.

Hore strongly silicified areas other than those mentioned as subunits to follow are located at ; 203.4-204.6m ; 208.1-208.?m ; 213.1-216.1m ; 221.5-222.1m i 224.3-226.9m ; 233.1-238.?m ; 243.6-247.Om 5 254.0-255.6m.

Magnetite occurs throughout in the matrix and as fragments sometimes. The unit is basically a felsic lapilli tuff withan agglomeritic (*/- breccia) character in places,

Some felsic fragments have sharp angular quart? phenocryst? (rhyolite?). A 20cm portion of the core at 273.4m has a low angle (5 deg. to C.A.) intersecting carbonate .vein.

-Sub Units-


Mottled Grey to JanQuart?: 601Lapilli: 'hi-: 151Foliation at 50 Deg. Cax.Weakly Fractured (5 Fractures/Meter)Pyrite: 3!Silica Alteration: 201

Sample No.

f rom lo (n)

Width Au Ag Cu 2n Pb Sb fts (m) (ppm) (ppmj (ppm) (ppai) (ppiri) (ppu; (ppsi;

r, o

16053160541605516056 160b?

158.00 158.30158.30 158.80158.80 159.00159.00 159.20159.20 160.50

0.300.500.200.201,30

8-22-198?::10:56


DIMM) DRILL LOG

KL-87-16

Page 12

From To (m)

-Description- Sample From No. (m)

lo Width Au Ag Cu Zn Pb Sb As Ho (ppiii) (ppm) (ppm) (ppm) (ppm) (ppm) (ppaO (ppsu

Non Hagnetic Non Conductive

This silicified section as well as 158.0-159.Om and 159.2-160.5m represents the contact area between the main QFP and a large section of 4e.

It lacks any magnetite in the matrix or fragments. Some of the larger fragments contain 2m silicified rims and some are broken with networks of quartz filling the fractures.

In general all the fragments are quite angular. Silicified portions of the QFP lie within the sections of this unit noted above, Minor Ml) carbonate is present as narrow 1mm fracture fillings.

The section from 159.2-160.5m gradually grades into the next altered portion to be discussed later, In general the fragments are mainly a light buff beige to salmon color and are very obvious against the darker matrix.

Ihe contacts between these sections of this unit and the intervening QFP vary from 30-55 deg.


Same as 158.0-279.5 16058 Mottled Light-trey 16059 Quartz: 60* 16060 Lapilli: 251 16061 -: i SI 16062 Foliation at 60 Deg. Cax. 16063 Weakly Fractured (4 Fractures/deter) 16061 12 Quartz-Carbonate Veining at 70 Deg. Cax. — Avg, Widthkm

Magnetite: 21 Pyrite: ^

160.50 162.00162.00 163,60163,60 165.20165,20 166,70166.70 168.20168.20 169,70169.70 170.80

1.50 1,60 1,60 1.50 1,50 1.50 i.10

8-22-1987::10:56


DIAMOND DRILL LOG

KL-87-16

Paqe 13

Fron (ffi)

| 0 --.- — .-..-,--.-.----..-f)escr ip(i on..-...-.-.-..--.---..-

Silica Alteration: 5! Chlorite Alteration: l! Biotite Alteration: 2! Weakly Magnetic Non Conductive

This upper section is moderately silicified. A zone of weakpotassic alteration stretches f roil 167.0-170.8m. Thepink-brown coloration of the alteration is strewn out invague patches within the matrix.

There is about l! quartz-carbonate veining with the largerveins (l-3cm) having interiors of quartz with carbonateeating in from the contacts.

Other Hum veinlets are more common. Rare felsic fragmentswith fine scale parallel (km) banding of light pink-beige(felsic) material,

170.8 195.8 [IE] FELSIC LAPILLI TUFF

Same as 158.0-279.5mMottled Dark-Grey to GreenQuartz: 55!Mafic Minerals: 20!Lapilli: 25!Foliation at 60 Deg. Cax.Weakly Fractured (4 Fractures/Meter)^! Quartz Veining at 80 Deg. Cax. -- Avg. Width 4cmPyrite: *llMagnetite: l!Biotite Alteration: 10!Chlorite Alteration: WSericite Alteration: l!Green Mica Alteration: ^!

No.From To Width Au Ag C'u 2n Pb SD As rio (ci) (m) (DI) (ppm) (ppm) (ppm) (ppm) (ppm) (ppu) (ppr,i) (ppit)

3-22-198?: ;10; cj6


DRILL LOG

KL-87-16

Paqe H

From (M)

lo -Description- Sample No,

from lo Width Au Ag Cu In Pb Sb A:. (m) (in) (m) (ppm) (ppm) (ppm) Ippm) (ppm) (ppit)

Silica Alteration: 11 Garnet Alteration: *:lt Weakly Magnetic Non Conductive

Ihe darker color of this subunit is due to the chlorite andbiotite alteration which has also affected many of thefragments making them less discernible.

Ihe weak foliation is mainly expressed by the subparallelalignment of the chlorite and biotite. Ihe fragments aremainly felsic (2mtHcm) and are a medium grey color.

One quartz vein occurs at 185.0m with trace pyrite,Magnetite is disseminated throughout the matrix and occursin small patches (previous fragments?).

The pyrite occurs as small 1mm cubes within the alteredmatrix.

279.5 END OF HOLE,

08-22-198?: ;10:56


DRILL LOG -- GEOCHEH SAMPLtS

KL-87-16

PdQf 15

Sample From lo Width Au Sb As 6a Cd C's Gr Co Cu tu Hf Ir Fe La Mo Ni Kb Se Se Ag la Ib Te Ih * U Yb Ir-No. (B) (m) (m) ppb ppji ppm ppni ppni ppu ppm ppu ppm ppn ppm ppb pet pp.ii ppm ppin ppni ppm ppni ppm ppm ppai ppn; ppm ppm pps p?n; P?

1412? 9.70 12,50 2.80

14128 17.20 21.40 4.20

14129 28.40 32.70 4.30

14130 35.60 36.90 1.30

14131 39.50 42.20 2.70

14132 87.40 90.20 2.80

14133 93.20 100,60 7.40

14134 103.80 111.20 7.40

Sample Scan: k!16

Fire Assay 13448 to 13500 16032 to 16142

Geochera 14127 to 14134

ERROR REPORT

WARNING: Saoiple Data File Missing!

Sub-Unit ERROR: (44,5-158.0) and (79.7-82.8)

f R O H N O R ft M C O EX F' l C K L P. 7

i,'

AZIMUTH: iae—~-.4,.---.^ . ....J-..- -.——4...

200 1*0 ife

KL-87-21

100

. 120

i 140

zoo

120

.. 140

WfHW

NORAMCO DCPLORATION

DO OF MOLE: as.

Keezhik Lake Diamond Or Ml Section

LW40C* , OtUi Jlty

1000

08-22-1987::10:34

Property: Keezhik Lake 1411


Aziiuth: 135 degrees' l IvfevA-Wo........

Logged By: (^ Jim Davis

Date Started: July 27/8?

Core Size: BQ

Drill Coipany: Longyear


DIAHOND DRILL LOG

KL-87-21

NTS:

Claii f:

Dip:

52P

18 656478

-50 degrees

Casing: In

Date Completed: July 30/87

Core Location: Keezhik Lake

Overburden: 6.4 deters

township;

Coordinates: L54+OOW , 14*555

Length: 285.6 meters

Elevation: Surface

Date Logged: August 4/87

Samples Shipped:

Acid Dip Jests

l l, 108.8 ft 47 deg. l 3. 285.6 ft 46 deg.

1(2. U i 47 deg.

Conclusions

Recoil itendations

lo test I.R. anomaly and the strike extent of silicified zones intersected in DDH's KL-87-12 and KL-87-16.

Silicified zones intersected.21 pyrite mineralization accounts for I.R. anomaly.

Await assay results.

3-22-1987::10:34


DRILL LOG - SUrtHARY

Frotn(ffi) To(m) -——-——-----—-

0.0 6.4 OVERBURDEN

6.1 285.6 [86] FELDSPAR PORPHYRY

•Description- -Mineraii?ation(s)

Pyrite (21) Tourmaline

KL-87-21

-AHeration(s)-

Yellow-breen Sericite (5?) Potassic (31) Carbonate (21)

285.6 END OF HOLE.


08-2?-198?;:10;34 DIAMOND DRILL LOG

From lo ————— - ———— Description--- — --..----.------.-(ffi) (i)0.0 6.4 OVERBURDEN

6.4 285.6 [86] FELDSPAR PORPHYRY

Mottled White to Light-GreenK-Feldspar: 50!Quartz: 20!-: 301Very Coarse GrainedMassiveWeakly Fractured (2 Fractures/Meter)11 Carbonate Veining at Random Angles -- Avg. Width BitmPyrite: 11Tourmaline: (\\Yellow-Green Sericite Alteration: 51Potassic Alteration: lilCarbonate Alteration: 21Non MagneticNon Conductive

Geology: photo-linear trend 048. Geochemistry: nil.Geophysics: weak chargeability flanking resistivity high;weak magnetic anomaly.

Composition "other" includes; plagioclase sericitecarbonates and opaques, Feldspar phenocrysts are zoned andrange in si?e from 2- limn.

K alteration zones: 12.3/23.2 68,2/71,0 165.3/167.0190,8/193.5 202.7/215.8 236.2/253.6 282.5/285,6(11.

Silicification zones: light mottled grey/highlysilicified/ronimon random fracture infilling includingtourmaline carbonate/increased mineralization/in partcompletely alters original fabric.

Silicification; 30.5/36.7 51.5/54,5 66.7/68.2 72.8/78,389,0/91.? 100.1/144.9 182.3/190,8 194,2/202,7 215,8/278.5

SampleNo.

13901

13902

13903

13904

13905

13906

1390?

13908

13909

13910

13911

139121S913139141391513916

1391713918

from(m)

6.50

8,10

9.40

11.00

12,30

14.60

17.50

19.30

21.70

26,20

29,90

31.5033,0034,5036.0036.50

38.3039.80

lo(m)

7.00

9.10

10.40

11.60

13.30

15.10

18.50

20.30

23.20

27.20

30.90

33.0034.5036.0036.5037.60

39.8041,30

KL-87-21

Paqe 3

Width Au Ag Cu Zn ;;'S Sb As no(m) (ppm) (ppm) (ppm) (ppm) (ppi) (ppin) (ppiu ippmj

0.50

1.00

1.00

0.60

1.00

0.50

1.00

1,00

1.50

1.00

1,00

1.501,501,500.501.10

1,501.50

08-22-1987::10:35


DIAMOND DRILL LOG

KL-87-21

Pale 4

From lo ~.— — ~~ -.~- — — Qescr ipti on-.-— ......— ........ Sample(m) (m) No.

262.2/267.7 .ftafic xenolith 148.9/153,0; dark grey mottled lapilli tuff 13919

with replacement of lapilli by cal cite/extreme biotitealteration/some pyrite mineralization. Intrusive is little 13920altered near xenolith and phenocrysts are coarser thoughprobably by coincidence. 13921

In outcrop intrusive weathers pink.Sample series; 13901/14000 16251/16258. Geoctiem samples; 13922

14501/14515. 1392313924139251392613927

1392813929139301393113932

13933139341393513936mi13938

13939

Frofi:(B)

44.20

46.30

4?. 80

49.2050.9052.3053.0054.5056.00

66.7067.7069.2070.7071.30

?2.8073.7075,2076.707/.30

80.40

85.80

lo(M)

44.70

47.10

48.70

50.2052.3053.0054.5056.0057.50

67.7069.2070.7071.3071.80

73,7075.2076.7077.3078.80

82.20

87,50

Width Au Ag Cu 2n Pb Sb As Mo(m) (ppm) (ppm) ippni) (ppm) (ppm) (ppm) (ppm) (ppm,'

0.50

0.80

0.90

1.001.400.701.501.501.50

1.001.501.500.600.50

0.901.501.500.601,50

1.80

1.70


08-22-198?: :10:35 DIAHOND DRILL LOG

From lo — — .--— — — -----Description — ---------..---------- Sample(m) (in) No.

13940139111394213943

13914

13945

139461394?13948

1J949139!)0! 39511395/139531395413955139561395?

13958

13959

From{m)

88.1089.0089.6091.10

92.80

93.80

99.0099. /O101.20

104.10105.6010?. 10108.60110,10111.20112.90114.40116.10

119.00

120.60

loW

89.0089.6091.1091.90

93.60

94.60

99. 70101.20102.50

105.6010?. 10108.60110.10ill. 20112.90114,40116.1011?. 00

120,00

121.40

KL-87-21

P;i9*' 5

Width Au Ag Cu Zn Po Sb As Ho(m) (ppm) (ppm) (ppm) (ppm) (ppm) (ppir,) (ppm) (ppu)

0,900.601.500.80

0.80

0.80

0.701,501.30

1,501.501.503,501.101.701,501.700.90

1.00

0.80


08-22-1987: ;10;36 DIAMOND DRILL LOG

From lo ——— - ———— -----Description----------- — -----.-- Sample (m) (ffi) No.

13960

13961 13962 13963

13964

13965

13966 1396?

13968

13969

13970

M

13972

from (n)

122

124 125 12?

129

132

134 135

13?

139

140

143

14?

.80

.40

.70

.10

.40

.70

.40

.70

.50

.20

.80

.80

.50

124

125 127 128

131

133

135 13?

139

140

142

144

148

lo (ffi)

.00

.70

.10

.00

.00

.80

.70

.20

.00

.10

.30

.90

.90

KL-87-21

Page 6

Width Au Ag Cu ?n Pb Sa k v (iti) (ppm) (ppm) (ppm) (ppm: (ppm) (ppm) (pprc) ippir)

1.

1.1. 0.

1.

1.

1.1.

1.

0.

1.

1.1.

20

30 40 90

60

10

30 50

50

90

50

10

40


08-22-1987: :10:36 DIAMOND DRILL LOb

From lo --- — ------— - —— ..oescr jp^ on -.....-. — ......--...-. Sample(ffi) W Ho,

139/3

13974

139751397613977

13978

139/913980

1398113982

13983

1398413985139861398?

from(m)

157.30

158.30

160.10161.60163,10

180.00

182.30183.80

186. CO187.50

194.20

195.50196.80198.30199.50

loW

158.00

159.40

161.60163.10163.70

181.30

183,60185.40

187.50189.00

195.30

196.80198,30199,50200,80

KL-87-21

Width Au Ag Cu 2r. PC So As le(m) (ppm) (ppm) (ppm) (ppm) (ppin) (ppm) (ppm) ippni

0.70

1,10

1.501,500.60

1.30

1,501,60

1,501.50

1.10

1.301.501.201.30

13988 204.20 205.60 1.40


08-22-198?: :10;36 DIAMOND DRILL LOG

From To — --.--— — -— ..-— oescr jption --------------------- Sample(i) (m) No.

1398913990139911399213993139941399513996

1399?

13998

13999

1400016251

16252

16253

1625116255

fromdi)

215,217.218.220.221,223,225.226.

233.

238.

245.

247.248,

251.

258.

261.263,

5000500080001070

00

20

50

0050

10

30

9070

21?218220221223225226228

233

239

246

248250

252

259

263265

loM

.00

.50

.00

.80

.00

.10

.70

.50

.80

.70

.70

.50

.00

.20

.90

.70

.20

KL-87-21

Pef)s 8

Width Au Ag Cu In Pb So As rt o(m) (ppji) (ppm) (ppm) (ppm) (ppm) (ppm) (ppm j (ppm)

11111211

0

1

1

11

1

1

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.50

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.80

.20

.10

.60

.80

.80

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.20

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LES EXPLORATIONS NORAMCO ]

08-22-i987;:10;3? DIAMOND DRILL LOG

From lo —— - —————— — Description--- ——— ------. —— -- Sample froni (ffi) (i) No, W

16256 265.20 1625? 266.70

[NC. KL-87-21

Page 9

lo Width Au Ag Cu 2n Pb Sb As 10 (li) (m) (ppm) (ppm) (ppm) (ppm) (ppn:) (ppip) (pp,:) (ppm)

266.70 1.50 26?. 70 1.00

16258 278,00 279.50 1.50

285.6 END OF HOLE.

8-22-1987::10:3?


DIAMOND DRILL LOG - GEOCHLM SAMPLES

KL-87-21

Page 10

Sb As Ba Cd Cs C r Co Cu Eu Hf Ir Fe La Mo Ni kb Se Se A9 \a fb le In k u ft. ppm ppin ppm ppin ppai ppm ppm ppm ppm pptii ppb pel ppm ppm ppiii ppm ppiii ppm ppm ppm ppm ppm ppai ppu ppm ppm

Sample FromNo. (m)

14501 25.00

14502 25.60

14503 58.80

14504 149.90

14505 165.30

14506 171,30

1450? 17?.00

14508 190.80

14509 210.10

14510 229.80

14511 234.90

14512 240.50

14513 253.60

14514 269.00

14515 284.00

lo d)

25.10

25.70

63.30

153.00

166.80

174.20

178.60

193.50

215.40

232.90

237.90

244.50

258.00

277.50

285,60

Width Au (m) ppb

0.10

0.10

4.50

3.10

1.50

2.90

1.60

2.70

5.30

3.10

3.00

4.00

4.40

8.50

1.60

Saraple Scan; k!21

Fire Assay 13901 to 14000 16251 to 16258

Geochew 14501 to 14515

ERROR REPORI

WARNING: Sample Data File Missing!

Ministry ofNorthern Developmentand Mines of Work

///W*

emeîîYostal Address of Recorded Holder

L 'L l Ll l!.. l U LL UAl L v~

Mjr 5ZP,6SWee06 M KEEZHIK LAKE 900 ?

J ProspefctV's Licence NO.

-.-;.X"-^gL—

Summary of Work Performance and Distribution of CreditsTotal Work Da ;r. claimed

LVJT \.Work

Days Cr.

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

D Manual Work

J {

t Sinking Drifting or other Lateral Work.

Compressed Air, other Power driven or mechanical equip.

Power Stripping

or other Coredrilling

] Land Survey

All the work was performed on Mining Claim(s): t M li", (e 6fc*i"Trj ,l*5kH8(p ,

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

61 - 8-T - IS en - /t61 - Z\

t ex m c r* ci

. ./HI. v

Xv

ONTAAIO CECIOBIC^ SJIASoL-!.:^.-it-N i MLl:o•:. i -i'ju

SEP 3^87

; E i v E D

THUNDER BAYMINIM LllV!::iCN

AM PM

Date of Report Receded Holder or Agent (Signature) ^

Certification Verifying Report of Work1 hereby certify that 1 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 end/or after its completion and the annexed report Is true.

Name and Postal Address of Person Certifying .

A/o^î-tyô ci *îpr^vft(Vl5 Jo)IL) /IdLLHs /JA, (4, "i A/oK^'h Ofl~M , \jy^V, r ID o)(jOfc' f f j Date Certified Certified by (Signature)

l^hulAât JS- 1X7 '^fcLe/ff^-uf^fi^Table of Information 1 Attachments Required by the Mining Recorder {J

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 coredrilling

Land Survey

Specific Information per type

Nil

Type of equipment

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

Signed core log showing; footage, diameter of core, number and angles of holes.

Name and address of Onterio land surveyor.

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.

Names and addresses of owner or operator together with dates when drilling/strippingdone.

Nil

Attachments

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

Work Sketch (as above) in duplicate

Nil

768 (85/12)

NOTICE TO CLMMBOLDBR

Ret Grouping of Work Credits on Mining Claims *4g Claims

** K*JL*L \ *LjL j

(Description) ../yMAtA' PA

Pursuant to subsection 76(6) of the Mining Act, R.S.O., 1980, c. 268 work credits as submitted in the Work Report dated tf^ftiAt J# ,9f7_____ (as attached) were grouped and credited in the manner requested. As you held no recorded interest in the claims in question at the time the work was performed, we have accepted the application to record such work on the assumption that you held a beneficial interest in the said claims at the time the work was performed. Please be advised that if this assumption is not correct, there is a possibility of a challenge by a third party to the validity of the work credited.

DateMining Recorder

KEEZHIK LAKE -f HINZER OPTION CLAIMS CONI'D

CLAIM tt tt DAYS CLAIM tt tt DAYS CLAIM tt tt DAYS CLAIM tt tt DAYS

120.0012.4512.451 2 . 4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.5112.4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.45

TBTBTBTBTBTBTBTBTBTBTBTBTBTBTBTBTBTBT BTBTBTBTBTBTBTBTBTBTBTBTBTBTB

920 1 989201999349019349029349039349049349059349069349079349089349099349109349119349 1 293491393491493491593491693491793491893491993492096823896823996824096824 1968242968243968244968245968246968247968303

12.4512.4512.451 2 . 4512.4512.4512.4512.4512.4512.4512.4512.4512.451 2 . 4512.451 2 . 4512.4512.4512.4512.4512.4512.451 2 . 4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.45

TBTBTBTBTBTBTBTBTBTBTBTBTBTBTBTBTBTBTBTBTBTBT BTBTBTBTBTBTBTBTBTBT B

968304968305968306968307968308968309968310968311968312968313968314968315968316968317968318968319968320968321968322968323968324968325968326968327968328968329968330968331968332968333968334968335968336

12.4512.4512.4512.4512.4512.4512.4512.4512.4512.4512.451 2 . 4512.4512.4512.4512.4512.451 2 . 451 2 . 4512.4512.4512.4512.4512.4512.4512.4512.451 2 . 4512.4512.4512.4512.4512.45

TB 968337TB 968338TB 968339TB 968340TB 968341TB 968342TB 968343TB 968344TB 968345TB 968346TB 968347TB 968348TB 968349TB 968350TB 968351TB 968352TB 968353TB 968354TB 968355TB 968356TB 968357TB 968358TB 968359TB 968360 TB . 968361TB 968362

12.4512.4512.4512.4512.4512. 4512.4512.4512.4512. 4512.4512.4512.4512.4512.4512.4512.4512. 4512.4512.4512.4512.4512.4512.4512.4512.45

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LE&END

:^H /' ViVT BRESNAHAN L

COMPLETED DIAMOND DR-ILL HOLENORAMCO EXPLORATIONS INC

^KEEMK:IAKE'PROJEC""DIAMOMD DRIL;

5LOCK D

t O 000 i , ^"ULY j 87—-~ -- -- -- -f -

SQQOO52P16SWWae M KEEZHIK LAKE 200

010 DIAMOND DRILLING AREA: KEEZHIK LAKE REPORT NO:l A …

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