DD RPT 50 GUIBORD - Ontario · diamond drill record property dip test angle hole no sheet no j,,3...

$: DD RPT 50 GUIBORD - Ontario · diamond drill record property dip test angle hole no sheet no j,,3 depth(m) etch true hole no m-i* location ^.a total depth l\i" ^ l\^.$
42A08NE0007 50 GUIBORD 010

DIAMOND DRILLING

TOWNSHIP: GUIBORD REPORT NO:50

WORK PERFORMED FOR: St. Joe Canada

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

Claim No.

669748

669749

Hole No.

P86-13

P87-14

Footage

313m

347m

Date

Nov/86

Mar/87

Note

(D

NOTES: (1) #W8808-002, filed in May/88

(2\ comparable -lo arwp submission

DIAMOND DRILL LOGS

COOK - GUIBORD TOWNSHIP

M555

by

STEWART FUMERTON

CHEVRON CANADA RESOURCES LIMITED

Timmins, Ontario

NTS 4 2 A/8 February 1987

LOCATION OF

DIAMOND DR L L

HOLES

LEGEND

Figure 5

DIAMOND DRILL RECORD

PROPERTY

DIP TESTANGLE

HOLE No SHEET No j

,,3

DEPTH(m) ETCH TRUE HOLE No m-i* LOCATION ^.A TOTAL DEPTH l\i"

^ l\^. **\ S ECTION i-a+oc t- D i p , k 5 ^ N LOGGED BY s u. /W/vr*^

'wot. ooV S* BEGUN li n.v tt BEARING W f*"* CLAIM

Uo* Vi*' S* FINISHED COLLAR(elev) CORE SIZE fi Q

0

t*)

*0

1

If

5

7

S

to

LITHO

;-

bu

-

FABRIC

^

ALTERATIONSI carb

M

ser chl H*-

M

"Rf

5yi

L.

M

MAG SUSC

-4.)

7.0

-0-4

Q MINERALIZATIONpy

'i

PO mo 'j mo cpASSAYS

SAMPLE

-

MS" 4lv.

848 U

- 1* 1*-7

-W *'*

-

Au ppb DESCRIPTION

0 -49 m Overburden

49 - 52.5 ra Conglomerate. The rock is m. g. with a few i a en t i f i a b le conglomerate

- pebbles. Generally all textures are obscured by strong epidote and hematite alteration plus sets of parallel calcite

. veins associated with contact metamorphism.

52.5 - 93.3 m Diabase. M. g. dark green massive rock wTtTi sparsely distributed Blagioclase aggregates up to Z c m in size,

pper 3 cm is fine grained and cut by a set of epidote filled fractures.

"59 '- 6 0 m 20 c- of l ost c ore .

SKETCH

'

\


PROPERTY HOLE No m-i* SHEET No *-

4 0

1

2

3

4

5

6

7

8

9

70

1

2

3

4

5

6

7

e9

*0

L1THOPi*-

-

-

.

.

-

-

.

-

-

-

-

-

.

.

.

.-

.

.

FABRIC

*

•*

fc*

*

* *

x///x-

*

ALTERATIONfi corb

VL

M

ser chl ^r

L.

u

L

MAG SUSC

-V)

-1.4

-1.0

- *.z.

-1.3

- J.5

•1,-)

-1.3

-™

-aA

-1.&

-\*

-M

-i.*-

-XI

-i.*

-'•f

-i.*

-^••5

-vS

Q Npy

1V

^'

T"

lT*

poNEf MIZmog mo

iTIONcp

ASSAYSSAMPLE

-

-

-

.

.

-

-

-

-

-

-

-

-

.

-

— *

Auppb DESCRIPTION

DLABASE-

-

-

.

.

-

.

-

-

-

-

.

^

SKETCH


PROPERTY HOLE No ? u- r*, SHEET No

LITHODO-'

-

-

-

-

-

.t OH *

tiv

C* w t

~V fi UC

.tt) M t

~

FABRIC

*x x/

'/X*rx

**

*/'

//xif

,.

',**4

/•S

/o - i .s/*

ALTERATION?l cor^i

nM

}s

se r chl i p

\,

i.

H

H

L.

MAG SUSC

-a.

- J.5

-I.*

-a. t-1.5

- LO

-1.7-T)

-H.O

-0.5

-5.0

-6-3

- 6. r

- a. x

Q Npy

1

5

3

PONSPmag

^LIZATICmo cp

1 ASSAYSSAMPLE

-

-

-

-

-

W* 11- l.?*

' l. lv

I-H-"l^tXi.

I.Xv,

L -

Auppb DESCRIPTION

DIABASE

-

-

86 m 10 cm of lost core.

-

From 90 m the rock becomes fine grained and pyrite appears as discontinuous blebs along fine fractures.

-

93.3 7 94.4m Conglomerate. Highly - strained polymictic conglonTerate with only

?jasper iron formation clasts ( <Z c m) identifiable, rest are highly altered. Some strong narrow shears.

^4.4 -95.8 m J)}abase. Massive, very fine grained black wfUi irregular discontinuous

. calcite aggregates and very finely disseminated pyrite.

95.8 - 97.0 m Conglomerate. Highly

percent of jasper I. F. clasts identifiable. Host clasts CI cm, very strong foliation.

green strongly foliated.

-

SKETCH


PROPERTY HOLE No P s SHEET No i

1* 0

1

Z

3

4

5

6

7

e9

lioi

2

3

4

5

R

7

e

9

10,0

LITHOt* H*

-

~-

FABR1CY'/i '

, VAX.

M̂ tS'/oy.j'/'sf *//'''/'st ' ,'•/-si fi'/•S '-/'s

' * X'/"'"^ s^200

' *'s,, Z; .J*s ^

ALTERATION?1 ??rt

S^-3

5

S

h rt

rtH

H

fi

5

5

-5

}

5

5

5 J

^

se r fhlMAGSUSC

- 4ILT *^*

- t..^

- *.v

-6.7

-O.I

-5.X

- 6. T.

- 0.0

-0.0

-0.0

-0.0

-0.6

. 0.6

-o.o

- o. j

-o-v

-o-x.-o. 1

-li. l-6.)

Qu

py

f*

?v

PONEPmag

\LIZ MIC Mmo CD

ASSAYSSAMPLEm^-S

1**

-

^m* iv.

-

888x5 t**.

-

38 6 1.{ 1^

-

M* 1-7 l~l

-

*te^ i-i-

-

MS*1u

'

Auppb DESCRIPTION

^slrpn^fSliatei^A^I.^H-ark'V/eTlj; - colour. Abundant white calcite

aggregates. Possible diffuse hornblende por phyroblastB. Set in this matrix are

- S 1???; (f 1 c m ) clasts whose origins are .difficult to ascertain and have been elongated parallel to foliation,

. with depth the conglomerate does locally nave a green colour.

Locally fine wispy shear zones which are . parallel to foliation and annealed.

115.8 m 10 cm calcite vein probably related to strong alteration.

117 -118 m Low percent of jasper clasts.

- 119.7 m 3 cm calcite vein.

SKETCH

1 .


PROPERTY HOLE No SHEET No 5

\ZO

1

3

4

5

6

7

8

9

1^0

1.

2

3

4

5

6

7

e

9

It 0

LITHO( Nfr

WAtKf-

C. 1.4-

fvxtxC

(|N(-

FABRIC

'',/*

', f f

f/ f̂ ^ s^

s 's^^*

S ^^..^ s-"^

,r™*r **

S Sr ''.s s

"^y^4^S ' *''P-

's f s*c*^

^f^

'/^* ^ ^^^ *-

* sS-*

^

ALTERATIONSI carb

55

5

5

}

5

5 S 5

5

5 Z s ss s

s s5

5

ser chlMAG SUSC

-6. t

- 6,0

-Q.O

- 0.)

-0. J

-O.|

-O.I

-d- 1

-o.x-t-1s

-6-1

-0.3

- t . x-*. J

- oj

- . i.

- O-)

~*-l

-0.)

-0.1

Q Npy

f*

V

00flgf ALIZATIOmog mo cp

i.. . .. ASSAYSSAMPLE

*je-i8 i*-*

-

wvji lv

-

W 4 Wli*

-

WJ*1*

-

*\*1*tI*N

-

m1*?iv

-

u*wN

Au POD DESCRIPTION

CONGLOMERATE

.121 - 122 m Kacke. Green, f. g. and more massive compared lo conglomerate.

122 - 130 m Conglomerate. Same as atsail IB.

130 - 131 m Wacke. Same as 121 m.

:3 99 f m148 ' 5 m Senilemerate. Same as at

" 131 m Low percent of jasper clasts.and by 133 m jasper clasts become f. g. black c lasts.

- 135.6 m Slight bleaching and brecciation adjacent to a pink calcite vein.

~ 139 m 10 cm band of slightly different conglomerate. ? a bedded unit.

SKETCH


PROPERTY HOLE No M SHEET No t

LITHO FABRIC si. corbALTERATION

ser ChlMAG SUSC py PO

NERALIZATIONmo g mo cp

ASSAYSSAMPLE Auppb DESCRIPTION SKETCH

2

3

4

5

6

7

e9

is ot

2

Z

4

5

6

7

e9

140

CtMt

- (p-C

-l,.)- e.e

-O.*

-t.l

-0,4

- o.e

-t-l

-1.0

•6-l

0.0

• *.0

o-*

1.1

9.0

t. *

•M

K

t M f X

1**

C'OXGLOMERATE

148.5 - 150.1 m Wacke- f.g. green matr r"5T

conglomerate. This elliptical ?hornblende

- be porphyroblastic.

Same ae DI.e. to as adjacent

unit also has similar aggregates which may

150.1 - 297.3 99.1 m.

Conglomerate. Same as at

153 m Small shear plane and some shear foliation developed. The shear planes

re filled with sericite and some talc Dcelly. The sericite has a lateritic

stain and is most prominent near a 4 cm calcite vein.

156.5 - 158.2 m Similar shearing to 153 m.


PROPERTY HOLE No P SHEET No 7

U O

1

2

3

4

5

6

7

8

9

1*7 o i

2

3

4

5

6

7

8

9

IS O

LITHO FABRICALTERATION

ser ••fitMAG SUSC Q py PO

K NERALIZATIONmog mo cp


Vu

.0.0

- 4.1

-l,t

- 0.6

- 1.1

- 6.1

- o.u

-c.J

-t. l

-l-1O.I

-D.P-9.0

-o.t

0.0

-p.* p.a

fv

m**

W M(•H

S li 1*7

i*.

484

tttvlv

tttsr

CONGLOMERATE

- 160 - 161 m Similar shearing to 153 m.


PROPERTY HOLE No ri.- SHEET No 9

It 0

1

2

Z

4

5

6

7

e9

l** 0

; i2

Z

4

5

6

7

e

x* 0

LITHOtt M V

FABRIC

s -

S 4/- yj/

y.' S* f

^ f j^ r

f .^

t s^ f

ALTERATIONsi carb

5

l

5

S

5 s

5

S

5

5

M

ser phi

M

H

L

tt-m

M

UT

VI,

VL

V-

MAGSUSC

- e. t

- 0,0

-^ X

-O.I

-1.0

-o.l

-O.I

-0.1

- 6.0

-6. i

-0-1

-O.I

-6.0

-fl./

-6.)

-OX)

- O.I

Q *py

IT

O

O

POfJPf ALIZATIONmag mo cp

ASSAYSSAMPLE**"'

S88S-V

-

**,V 3-

*s,v*?J** 6^ 18U57

1*,84* SI

-

i 4* SI

-

"1"

Auppb DESCRIPTION

CONGLOMERATE

. 180.3 m Multiple and sheared calcite veins.

. 181 m 10 cm calcite vein.

182 - 183 m Chlorite alteration tends to obliterate the hble porphyroblasts.

- 190.5 - 191 m Pebble clasts are distinct and not as severely affected by metamorphism and alteration.

- 193 - 194.2 m The strong hematite alteration results in all phases being different shades of a purple-grey colour. Also extremely finely disseminated Py is associated with this alteration. Clasts are typically darker

. shades than matrix.

198 m Km alteration is apparent in selective, alteration of some clasts and discolouration of hble porphyroblasts.

SKETCH


PROPERTY HOLE No PU SHEET No s

io o.i

2

3

4

5

6

7

8

9

1

2

3

4

5

6

7

e9

LITHOCOffr

Cs*1 (r

FABRIC

X X'

* ^x

s^ **

s

ALTERATIONS 1 carb

H

M

S

d

M

M

h

n

sM

H

S s

ser

i,

Vi

vi

en 1

fi

\.L.

U

L

u

'H-

H

u

H

u

riM

su

Vu

vU

ur

vu

u

l

L

U

vu

Vv-

t/ L.

MAGSUSC

-0.0

-f -l

-O.I

-O.I

-0-0

-9-1

-0.)

- (.0

- 1.0

-O.J

- o-l

- O.I

- o.o

-OA

-o.)

-o.O

-00

Q Npy

.ci

1f l l

l O

f*

l

0

poNE!mog

ALIZATIONmo CD

ASSAYSSAMPLE

Si i (llv.

&H i ^

41441

M" 1 *

fttUS

-

td U

-

U*W

-

i&iu

Auppb

'

DESCRIPTION

CONGLOMERATE

202.5 - 203.5 m Flasered shear occurs in .which sericite and hematite alteration U stronger along shear planes.

" 206 - 209 m Core is very vuggy due to removal of some mineral.

'208.4 - 209.5 m Flasered shear with only moderate shearing similar to 202.5 m.

209.5 - 211 m Wispy shears occur every 1 - 2 cm in the rock.

- 211 m 20 cm of lost core.

213.8 - 215 m Broader shearing associated with chlorite and some sericite alteration .plus partial obliteration of hble porphyrobfasts but not pebbleClSStfi*

- Below 215 m in addition to the strain induced foliation wispy parallel small shears are common but not necessarily

- pervasive. , *

SKETCH


PROPERTY HOLE No PU SHEET No jo

1X0

1

2

4

5

6

7

B

9

r2

3

4

5

6

7

8

9

VM *

LITHO

-

FABRIC

, Sy 's

j S

;T f

* s* *

f

S j/

t s S f

jf

f S

ALTERATIONSI

s

carb

^

5

5

5

5

5

5

5

S

5

S

ser

r

V Ln

AH

chl HV

t-

VU

vu

H

L

u

k

t,

n

i- ST

VU

h

L.

k

K

v^Vi-,

Vts

V u

MAG SUSC

-t. 1

-t. J

- o.o

•'.l

- (j.fl

- 0.0

-0.0

-o.o

- o.i- 6.0

- D.8

-o.o-0,0

- P.O

-C.)

a. n

Q MINERALIZpy

t^

^

-TV

PO mag moAT IONcp

ASSAYSSAMPLE

WX"

-

( s

-

ii,r'-

lv,

-

118*75

-

8U^tf

-

1*

Auppb DESCRIPTION

CONGLOMERATE

- The possible altered jasper iron formation clastB are no longer present and or identifiable. Rather, any clasts are

- typically nebulous and of undetermined origin.

235 - 236 m Some 1 - 4 cm clasts maybe t r a c h y t i c.

SKETCH


PROPERTY HOLE No PU-'l SHEET No j,

LITHO FABRIC si corb ser chlALTERATION

kinMAG

SUSC py PONERALIZATIONmog mo cp

ASSAYSSAMPLE Au ppb DESCRIPTION SKETCH

2

3

4

5

6

7

8

9

XSO

!

2

3

4

5

6

7

8

9

Y*

^

VK vu

VU

vu

-t.O

-*.)-O.J

-O.I

-J."- 0.'

- O.I

-8-1

-O.J

-o-l

- o.o0.0

-o.)

O.J

-o.)

M

o.o- 0 -1

6.)

-rv

l

1V

M* It

CONGLOMERATE

y p i c a 11 y < 2 cm c l a s t B are the only [entifiable clasta in conglomerate.


PROPERTY HOLE No w SHEET No i

LITHO FABRIC si corbALTERATION

serMAG SUSC Q py PO

NERALIZATIOmag mo cp


C O f l-

2

3

4

5

6

7

e9

0

1

2

3

4

5

6

7

e

9

S

i o

Vu

vua

VL

-t.o

-0.)

-0,1

-ei

- J. i

0-1

M

O.I

O- 1

-0-0

-0-3

VL

-0-1-

O

0

111

Tr

i*

886871*1

80888 lw

86089U

88850

866^1

888UIff

From 260 - 266 m, extension fractures mineralized with a fine grained mafic mineral are ubiquitous and orientated parallel to core. Where this texture i s developed there is a tendency for the host rock to change its appearance. This is apparent by further obliteration of distinction between clasts, porpnyroblasts and matrix.

272.2 - 274.6 m Chlorite alteration overprints Bm alteration and is associated with a slightly stronger shear foliation, plus local development of quartz veins.

275 - 280 m 260m.

Extension fractures as at


PROPERTY HOLE No Ml- SHEET No 13

x?o1

2

3

4

5

6

7

8

9

V) 0

1

Z

3

4

5

6

7

e

9

^* 0

LITHOlovfr

Hkflt. BVHl

FABRIC

*. 'Vr

S S S" ^r

*"

f ,S* S'

^

2/r

•f '*

./r 4*

'/?^

-S.*S^

' * -

f*

S^ *

** S*

Z/"--

' 's

S/r C

'/Sf

ALTERATION51 Wt

5

^

5 S

^^ ss5nM

n ^

nM

^

5

u

L

ser

A

9hl ^*,

k

Ju

vu

L

u

U

t

H

n

M

r

M

MAGsusc

-1.3

-U

-0.T

-O.b

-/,r-0.9• o-e-o.g,

1 1

-3-/

-3-0-1.3

. 0-1

-0.1

-0-1-d. i

-^-;-0./-0.3. -0-1

Q MINEIpy;

1V

I-V

A)

1

*l

l

*J

-rv -f ci

u l i l

i<l

PO

? ? ?

mag^12mo

ttLG'Ncp

ASSAYSSAMPLE

888?31*

see^ u

888^- 1*

88&X, Im

eeesT u

886^6In

ese^9Im

se^ooIm

- '

Auppb

i-

ULOwnlr I ivIN

CONGLOMERATE

Is magnetism due to presence of Po rather than Py?. Most sulphide grains are near

. microscopic in size.

285 m 4 cm of shear zone mineralized with Mm and sericite.

"297.3 - 300.1 m Mafic dyke. Discordant contact to foliation ~o7 "Von g lorne r a te.

. 10 cm contact metamorphic zone in which Hm alteration destroyed. Mafic rock is m. g. - f.g. dark green and massive.

SKETCH


PROPERTY HOLE No m- o SHEET No ,u

3^0i2

3

4

5

6

7

B

9

LITHO FABRICALTERATION

S2d2MAGsusc Q py 00

NERALIZAT1C 5mag mo cp SAMPLE Auppb DESCRIPTION SKETCH

if

S

l u

L i

uVu

Vi-

V-

L

n

1.3 t.3

2.3.

O.i

oiO.I

O.I

D.I0.3

o-i0-3

6. S

(•b

A* 1.3o.i /.s

*.\-2. k

fy

1o

1

o

Im

ee'jozU

889^3

8890*

U,

88908

80^10 Im

00.1 - 320 m Conglomerate same problematic conglomerate conifstinff of small claets which are locally obliterated by the alteration.300 - 305 m possibly some wacke horizons

for the rock tends to be massive with *no clasts, no porphyroblae ts and chlorite alteration is selective.

313 m A total absence of possible clasts, but lots of porphyroblasts identical to those in the conglomerate still occur. Rock is dark brown spotted with calcite rich matrix.

320 E. 0. H. .


PROPERTY

DIP TESTANGLE

DEPTH (m) ETCH TRUEO 3(,o 4 5

HOLE No SHEET No J

HOLE No P*T- IH LOCATION *-rw SECTION 1.^*00 s DIP -**' BEGUN a f*u. ,7 BEARING W

-FINISHED 7 H**- 1-7 COLLAR (elev)

TOTAL DEPTH ^7 LOGGED BY *- l -'*"*v*

* Lo*'*

CLAIM CORE SIZE

LITHO FABRIC si corbALTERATION

chl H*,MAG SUSC py po-M

NERADZATIOmag mo cp


o i - 0.)

(O

1

X

3

7601

''/

c. " c

•70

i*/*

K

•O-'i.

o.x

o. \

o.o

c.*

"•t 1 \

l*.

0 - 58 m Overburden

68 - 279.4 m Debris Flow this unit consists of a variable X intermediate to mafic volcanic clasts. These range in size between 2 ran to 40 mn but typically less than 20 mm. locally the clasts are rounded but usually are angular with some restricted occurrences of shear elongation. In places the clasts are zoned by either primary or secondary alteration. H. B. this is a less altered equivalent to the nebulous conglomerate in hole P86 - 13 small quartz / calcite veins common in core down to 164 m.

65 m Some hematite alteration of fragments

68 m Small calcite vein fills fracture

69.4 to 70.4 m The percentage clasts and their size drops dramatically.

lv,


PROPERTY HOLE No ?*7 . | tr SHEET No -

7 O

1

2

3

4

5

6

7

8

9

S O

1

2

3

4

5

6

7

B

9

L1THO FABRIC si corbALTERATION

se r chlMAG

SUSC py PO.M NgRALlZATION

mpg mo cpASSAYS

SAMPLE Au ppb DESCRIPTION SKETCH

7k '* S* lC t

eali

' f*

H

M

•Tr

H

-1 .o• 0.0

•6.1

6-1

•O.f

• 9 -1

•0.)

0-1

O-/

0-(

0.0

0.6

2151/2-5 5l ft AC

Nik

•Hi/lv,

DEBRIS FUCK

75 l 77 m some zoned hematite altered clasts

79 - 79.4 m Some py l cp aggregates occur in the hematite altered zone

86 - 88 m Some hematite altered clasts

88 - 89 m M inute sulphide crystals are sparsely disseminated


PROPERTY P, k HOLE No f SHEET No 5

LITHO FABRIC si carb se r chl n^ALTERATION MAG

SUSC py DONERAL1ZAT10Nmag mo CD

ASSAYSSAMPLE Au ppb DESCRIPTION SKETCH

- X

6 ift *

o i

\ * ^tl it -VA

too

" - e i i '

' (t

'. *\0

-O./

. c. i

(••.l

•c. i

•o, t

.0.1

•C i

•O.I

00

•o.o

C. D

f., P

0-1

^

l DEBRIS FLOW

94 m Some hematite altered clasts

NIU

Kit.

fl.!fi,o.HI*.

HIW

107 - 109 m Ncmatization of clasts. More strongly foliated at 45 - SO* to C.A.


PROPERTY ?,i^ 3. v HOLE No r r;. SHEET No ;/

//o 12

Z

A

5

6

7

8

9

/*0

!

2

3

4

5

6

7

8

9

LIT HO

- 3

Jtt 5(Q- X

FABRICH- ' * ' -* t

•H * *-" . *". S *.,*J* too

f e '*-"J,- t J *

* 0 *j,*

15 ik * *

* t i^ i^K J' tr * J J ":-:{;** *4

•* *. 40*- *

0 - o •L S.*,C " c

jj y ,. 4

t. 0 y

0 * "*O V V

A .1 O o 0

*J "* SjH "f* " (

^?"o'-•^;

ow J."C/

ALTERATIONSI carb

M

M

^ S M M

S

*\

M

SAA

S^sM

S

5

S

M fA

se r cbl ^

L

W

AA

S

S

L

L

L j

/tr

r-

L.

M

U

M

U

m

S

M

V-

u*v\

U

v^

U

t-i.L

MAG SUSC

-0-0

-CO

-el

-o.i

-f. D

-O.I

- p.t -e.i-o.f-0.0

-f. f

-O.I,

•^ r

-P.I -P.I -r c

- (M

-0.0

-f."l" . f

Q Npy

Tr

~\r•\,

T,"ir

t'

PO

*

N.ERALIZATIONmag mo cp

t* T,

Tr

ASSAYSSAMPLE

-

HI*"

0*

-

luit. l.***

-

OUT|.t*

•Wl*

i.O"

-

•KM

. (.tt..Ik*

. l.llfIbll v.n.,*k\ii**Sil* W11*1ifrif

^.Oi*^. lciw1-Ll.g11. 1 1

Auppb

m*-

Nl"'

NIU

NtU

IIHI L

NIL

Nik

Nik

KIU

—lL-. " W'k-

—

DESCRIPTION j SKETCH

-

-

-

-

DEBRIS FIjQW

117.0 - 118.0 n Occasional dusty to granular py dissemi nations.

123.0 - 127,0 n Dusty to granular disseminations of py X cp in hematized zones and in hematized clasts; occasional granular aggregates.

126.0 m Large angular clasts (1 cm - 3 cm); hematized; samples taken based on intensity of alteration

1


12

S

4

5

6

7

8

9

•/o1

2

3

4

5

6

7

B

9^ i

PROPERTY r?A, i^,,. HOLE No ^ sv,, SHEET No s

LIT HO

7u.

. COiS

i

FABRIC

r\v^

'* *' * T

f Dv/*8 d -*

* CJ l1 t J J

J o * "^ *-* t *

o 1 J

o

t 1

l) 'Ik f f

ALTERATIONSI wb

M

S

S

S

AA

L

M

M

i-

M

i.

M

5

se r phi H~L

U

R-fi,

L

L

fcA.

U

L

L

L

M

u

t,t,

i*l

•A

MAG SUSC

-O.i

-n c-Di

- C .I

- o i -c-;-0-0

-C.I

-e./

- (5. P

-P. 6

-C, i

-0.0

Q Mpy

T/

r- ..t T, Tr

PO^PFALIZmog mo ^IIVcp

V

TV

vj ASSAYSSAMPLE

oxi. -/"iV^

7* M

-fe*.

Ik li

'i.li,e.ii1I.M

- 0.41

-^

D.l.•Ml

-

in*i.J*

-

*.(H

-

t'. 1C

- Hkl

cfi-'Zff

lul

AuppbHIUNil-

xs/,,

Nik

Nil-

Hit

NIU

is/ii

5ut /no

nil.

HIU

Nit-

HIUNIL

H' kNik

DESCRIPTION SKETCH

-

-

~

DEBRIS FIX)K 130.0 - 133.0 m Hematized section; granular aggregates

and disseminations of py; occasional cp

133.0 - 137.0 m Py and trace cp in hematized clasts as granular disseminations finely disseminated through matrix

Samples taken based on intensity of alteration.

1


PROPERTY A k* HOLE No p SHEET No ,:

r; o1

2

3

4

5

6

7

B

9

1

2

3

4

5

6

7

8

9

LIT HO

u.

- tfe

: ,

FABRIC

{ ^vC

J **

tf **

V "

0

7

t

V td

f * * *

f *

* t *

y * '

* -* * ^ #* ^ f

ALTERATIONSI corb

M

/A

U

i,

i.

U

L

se r chl u~Vt.

tfL

VU

fv-f

5t-

J,

w

U

L

U

VU

sS

MAGSUSC

- 0.(5

-o.o

-o.c

-0 ' •c.i

-o.l

-PC

-f i -0-0

-Of'

- p . p- D 1

C.,

- P- C

Q py PONFRALIZATIONmog mo cp

ASSAYSSAMPLE-SP- —

11.31

-

It w

-

HI!

- in*

-

1.51

*^

lv:7til

!V*

::i

AuppbNIUNit-

Hlkk

HI

M/11

**

Mlk

K.k

H.k

OIL

HIL

Nik

DESCRIPTION

~

-

—

-

DEBRIS F^)W

SKETCH

151 m Subangular to rounded pale green clasts (1 cm - 3 cm) in dark green matrix; matrix supported.

158.0 - 159.65 m Slightly brecciated due to intrusion of bull quartz vein; pinkish tinge to quartz where it contains calcite.

162.0 m trace amounts of specularite 1 hematite within quartz / hematite 1 carbonate vein 3 cm wide.

164.0 - 167.0 m Subrounded to rounded clasts which are slightly hematized; some sericitization of clasts (0.5 - 1 cm).

1


PROPERTY p k, KL. i--*HOLE No i-s'i- SHEET No ^7

LITHO

V}

eu

FABRIC

: *; *,V:"*4 -* *•t f-

* b

t ^ k

* V

* t

V

v .

H ^

* * o\ y

0 J , i

D

1 *O

l, ,

O *4 b

*-

ALTERATION?" fOft?

S

5

nM

L

i

U

M

M

L

t,

s

ser phi

VI-

Hm

v/t

Vt

v/L

U

L

U

MLM

Ar,rt

L

L.

L

L

MAG SUSC

-C.I

-01

- " -i

- i -i-

"" l V.

- .'-l

~ ,' ^

"~ ' 1

1

Q wpy po

NERALIZATIONmog mo cp

ASSAYSSAMPLE

-

7"!-

7"~-'"I

!." 87***

709^.v^.7*"

-

?47i

-

Auppb

Mil*

Hit

• 1-

NU-

WU.

Mtl.

Nil.

Hit-

DESCRIPTION SKETCH

DEBRIS F1CW-

175.0 - 176.0 m Minor hematization of clasts

-

180.0 - 183.0 m Hematization / Bericitization of clasts(1 cm in size)

1

-

-

r/ o i2

3

4

5

6

7

8

9

iro1

2

3

5

6

7

8


PROPERTY F! k, , HOLE No PO ,, SHEET No 6

12

3

4

5

6

7

8

9

:*t.- o i

2

3

5

6

7

e9

LITHO

-

- 23

V-i 1

FABRIC

4 ^

O *

"* 4

b

. y

C 4i

* t

* V

'X rH

* j

O *V

i u

fL

* 4

* ^ - U

ALTERATIONSI carb

U

S

i.

Al

S sM

S

AlM

MfV^

s

se r phi tv

L

L

tt-

i.

i.

L

l

1V/)M

L

U

L

L

A)

M L

L

L

M

L

L

t-

VL

l/L

MAGsusc

-c./

- o- 1 - t "1 - i

-r. j

- 1.-, y

- P.I-r./

- f i

- M

Q wpy

Tr

Tr

T,

DONSfmog

ALI2ATIOmo Cp

TK

Ir

T/

*J ASSAYSSAMPLE

M.

-

JC.7V

X.7S-

-

?*7t

**"

J4.7V

l.ttn

7fiJ*!T74*1./.'/f.

-

tw

-

±9^

AuppbKiu

Mil-

mu

(•ii-

Kl'-

XI k

HIU

HIK

NIU

mi.

hiu

Mlk

DESCRIPTION SKETCH

-

-

-

-

-

PEBRIS FLOW

193.0 - 204.0 D General minor heraatization of clasts; i 1 cm in size, occasional 2 cm clast.

193.0 m Flaser type foliation anastomosing around clasts f porphyroblasts along chloritic planes.

204.0 m Trace py X cp as granular disseminations along side of l or within calcite veins.

206.0 m Sericitized 1 hematized clasts.

207.0 m occasional py 1 cp granular dissemination.

210.0 m very weak hematization of clasts.


•j.\ o 1 z3

4

5

6

7

B

9

,?i 0

1

2

3

4

5

6

7

e9

PROPERTY P/,, R,, HOLE No P.-O . ;V SHEET No ',

LITHO

3

u.

w (2

FABRIC- * *

j *^* * i

0 B 0O

4 U

ti

V f *

y

* *; *!D*,\

^~ * *

* * *

fc * -*-

*

* V

* n ^

^

ALTERATIONSI corb

5

5

M L

W

S S

S

5

S

S

5

S

S

5

se r Cfll Km

VL

L

U

/^

L

i.

rt M

H fi. A

S

l

l

VL

Vi.

Vi

S

5

Al

M

S

S

s5

M

5S

MAG SUSC

-t1 .*'

-6.2.

- t- C

"f- t

- r."'.'

- ''.t/

- t' .1

~ i 1 , t

Q

Dr

K'py

Tr

poNERALI2ATIONmog mo cp

ASSAYSSAMPLE

/.o

-

/.*w

-

/•Dm

/.fm

-

7t"w-/.**1

i. fm

f.) t "

- ^4fy

- ;***',*J -71

~

AupDb

N* u

NIC

Hli-

HIU

Nik

HlU

UlU

H 1*-

Nli.

Nil.

HIK

DESCRIPTION

| DEBRIS FLOW

~-

216.0 - 218.0 D Greywacke? unit; relatively

most fragments ^.5 co.

alteration, low to moderate hematization zone

cm in size.

i

-

SKETCH

massive n green;

orbonate ; clasts 5 on - 1


PROPERTY HOLE No P* 7- SHEET No | 0

; ?,0

12

3

4

5

6

7

8

9

i-, 0

1

2

3

4

5

6

7

e9

LITHO

"?u.n

. tt O. *

FABRICo-1" *'* - 4 '•* -t- t- * "

* *. 1 ** o "' ' **

Ll V (j

* Jtli 1)

•3 J ' '

* •* ^ "~-~*^ ^ *- *-

* *""T T-\'

J i•V-'-' . l

v o

f 'J

J 1 , J

i A k e

* *V '

J ' ti i tc.,.

t 0.••"J

ALTERATIONSI carb

Ss s rt5/vi

M

S(A

S

l"\

W

fA

M

S M fA S1^ rt

se r phi Hnvu vuVL

l i-

i.

vtVL

VL

VI

v/U

n

L

PmiflM

5Nl

L

L

U

M

S

U

M

U

t-

^L

VL

L

Mi.

VL

L l. L

MAG SUSC

" I/.U

- ,r./

* r. i- c .i- C. f

-t.\ - ( f- L'.C

- ''.f

- C' 1

- ; 1

- d .c

- f i

- '-i

i '"

~ .' i

i

Q wpy

TV

PONfRALIZATIONmag mo cp

ASSAYSSAMPLE

•7***

/.//-i

-

•)t11 l.tm

-

'Wf

t,ti~

Ml - t St*

-

77*ei Oi*

1)01 I.OM

-

77*t 1-

-

Auppb

Niu

Niu

Nil-

Hll-

^

5

5

--

-

-

-

-

DESCRIPTION SKETCH

DEBRIS FLOW

233.0 - 236.0 m Low to moderate carbonate alteration zone with hematized clasts (0.5 - 1 cm); 65X clasts not hematized, but dark green within a pale green somewhat eericitized matrix.

236.0 - 241.0 o Moderate to highly carbonatized zone with selective hematization of 20X of the clasts.

244.0 - 245.0 m Moderately to highly carbonatized 45 - 50X of clasts are hematized.

247.2 - 247.4 m Grit unit?; clast supported gritty appearing section; moderately sericitized hematite / specularite between clasts.

1


PROPERTY HOLE No t' SHEET No H

LITHO

- oj li.

(A ri

~ COwa

- .

FABRIC

* 0j

9^ '^^

* **'

f i , * t

* 00. i

t4^

c 00 s,J * V

4 t*

C fc -)'/*

* -,* 0* * * *

* t *' *x^X"

'V

u 'i

*"**

C , 0b

t, J 1. o ' ji * *

•r ' * , j * 't - '1

*.' ** * .

r C -* -1

' *

ALTERATIONSI carb

M

L

L

^

l

ff\

t\

H

rf

/"l

M

M

S /M

H

M

L

M 5 ^

se r chl V\rV/l-

vi

L-

L L t-

L

L L-

\,

L

l-vu

VL

VL

V L

t

L

t /^

4rrCM

L

'1

W

t

L

L

rtL /"l

5

Mi-

l

ML

tf

M

4 W

MAG SUSC

-/-.l

-f.l

- A i

- i".'

•M

-:.'

- f.'- C .I

~ f .i- '..t. ,'.'.(}

-c'. I

- 0'

-f 1

-' 1

. ; i

Q r*py 1 po

TV

T,

TV

"\f

TV

^

NgRALIZATIONmog mo cp

ASSAYSSAMPLE•w*

lo

-

lit-/ I.Om

-

??C6|.Cm

-

??*k |.8m

-

It tt\t~

-

J?**' 1C*

Dell'~llit

1 *m

Ijll 1 **\

Auppb

NIL

MIL.

NIL

HIU

S /HIU

Mtl.

Mlu

HIU

NIL

DESCRIPTION SKETCH

i PPBRIS FUOW

251.0 - 272.0 m Generally a median to dark green with minor sericitization and hematization of clasts and / or matrix; little variation throughout section except for carbonate content; occasionally trace py seen asgranular disseminations and subangular to rounded.

-i1

1

-i

-

265.0 - 267.0 m Section with pale green to buff clasts (sericitized?), 1 - 2 cm in size.

1

•rf O

1

2

3

4

5

6

7

B

9


PROPERTY HOLE No SHEET No

.r, o i2

Z

4

5

6

7

B

9

5. (TO

1

2

3

4

5

6

7

8

9

LITHO

\ lV*

- S Z

3* MI 3Sf9ti|a

1 1

'HI-Ir-Js

ou. fiSU 1r-J

FABRIC

t O

'J- ' l v4 -* ^

i -t'J 0

t ^k

^ V

(JC i

" , Vt "

'j^

/* *J

*

" . "

9 i

:Vl

ALTERATION?' Qorb

s1*S* ML

L

h AVL

N/L

VU

S

HH

M M Hnrt

se r phi H"t L.

n rt

L

rA vLVL

VL vL t-vL

L-

Awj"L

LnLL

L.

L.

L i-

L

L

t

L.

L.

C

i~

L

L L.

l

MAGSUSC

- C l

- i.l

- ,'.(

- C I

-l i

. fi i

- c.';.

- ~,(-

. j .'

- ss- ' .'t

-C.I

- c.c*

- 1. 1

Q Vpy

TV

TV

I' -p.

Tr

Tr

DO

'l.

UFFALIZATK Mmog mo cp

ASSAYSSAMPLE

•77(1/.**

n/j i.tm•nw t.t*.

-

-n,f u~•mi \.o*-lin i*iiieCM l

Tin- Hi -'

1IWl.tl11V M*•mii.**•1711

1.**•mn

i.**

-

i; IT l.'1 -*

AuppbKiv.

MIUV^

fJIU

5

55

S

10

MIL

5

5

lo

MIL

DESCRIPTION J SKETCH

DEBRIS FpOW

272.0 - 279.4 m Median green, massive section withsericitized and/or hematized clasts, generally less than 1 cm in size, subangular to rounded; occasional

-

277.3 - 277.9 n Diabase Dyke (as described below) 277.91 - 279.4 m Debris Flow (as above)

279.4 - 282.0 n Diabase Dyke dark grey, massive, weakly

(hairline to Iran); sharp upper contact 80* to C. A.; gradational lower contact fine grained ^0.5 mo).

282.0 - 284.0 m Debris Flow moderately carbonatized deformed zone; pale to medium green; fine grained ( ^.5 ran) with occasional 1 - 2 mn clasts in extremely deformed zone; quartz / epidote veins ( 1 mm) ; epidote also occurs within and adjacent to occasional large clasts; low to moderate hematizationin section ( reddish cast to rock); minor sericitization; has a somewhat "wispy" appearance 0.5X py occurs as cubic to granular disseminations; occasional granular aggregate.

284.0 - 285.0 m Deformation still in matrix although most i clasts (0.5 - l cm, occasional 3 cm) appear

unaffected ;

-


i-i-'O

12

3

4

5

6

7

8

9

;, 0

1

2

3

4

5

6

7

:l

PROPERTY P, k . K.- HOLE No H*V H SHEET No r*

LITHO

3- 3u.Mri

- COtilA

^ ,

FABRIC

n

cO .. ' '

0 J

Vf

4 o O

v o

-VX̂ wt

O

•^ ^

ALTERATION5'

i

corbfi

n rt n

s 59

fV\

fV\

F Ss

s

se r chl H"VL

VL

VL

i

L

lL

f^fiL

L

L

L

L

L.

L-

L

vi

v/U

MAGSUSC

- c .c-

- t . i

1 . f

- C.I

- .''.i

Q K'py

T,

Tr

TV

Tr

POtj*l ALIZATIONmag mo cp

ASSAYSSAMPLE

-

i.**

-

MI.

" */*-

a*•m*

•Wl

-

M*

-

- 7JM

Auppb

5

5

5

5

S5/7&

.0

5

10

DESCRIPTION SKETCH

-

-

~

hematization concentrated in clasts but also appears pervasive throughout section in low amounts.

285.0 - 294.0 m Medium green, relatively massive section; clasts (O cm) are subangular to rounded and appear sericitized; only minor hematization in clasts or matrix; trace py as cubic or granular disseminations.

294.0 - 296.0 m Appears clast supported with clasts of 1 - 3 cm (typically 1 cm) dark greeni little or no sericitization 1 hematization of clasts or section.

296.0 - 302.0 m Average clast size of 0.5 cm occasional 1 - 2 cm clast which are sericitized or slightly hematized; pink calcite interstitial with clasts (due to hematite content?)

300.5 m Sericite zone; slip planes -70 -80'toC.A.; waxy yellow colour; clasts also sericitized.

304.75 - 305.65 m Bull quartz X tourmaline vein; massive; minor sericite; minor carbonate.

306.0 - 319.0 m Moderately to strongly carbonated sections; slight hematization of clasts and matrix; interstitial calcite normally has pinkish tinge; trace py as granular disseminations and occasional aggregates.

1


PROPERTY ?,b HOLE No ?^ SHEET No H

oi 0

1

2

3

4

5

6

7

8

9

s^ o1

2

3

4

5

6

7

I"

LITHO

(j,i*l

FABRIC

k.

t

J

* ^

V

i

O

0

0

It o

0 u

o

o

D y 0

V ^

ALTERATIONSi carb

M

M

rt

M S

S

S

S S

m

M M M

5

ser chl HmVi.

U

VL

L t-

l tU M

U LL

L

L.

L

LL

IW

i/U

VI

M L

Vt-

MAG SUSC

-C.i

- C.i

- r i

•C.i

- c i

- C l

- f. t -1:1

~ l', C

-i' -i

Q wpy

T.

TV

Tr

T,

Tr

poNERALIZATIONmog mo cp

ASSAYSSAMPLE

•mv

)i*rI.IK,

-

^^*—

nn

lin

lin

-

tl-lt le*

it™

:

Auppb

5

IP

10j.

5

NIL

5

Mil.

Nil

7 f vi r

-

-

-

DESCRIPTION SKETCH

DEBRIS FLOW

320.0 - 323.0 m Slight to moderate hematization of clasts and matrix; strongly carbonatized; occasional carbonate 1 sericite f hematite slip plane -80" to C.A.itrace amounts py as granular disseminations and aggregates.

329.8 - 330 85 m Shear zone? bull quartz / tourmaline vein, brecciated appearing and deformed; adjacent host rock foliated at 40 - 45* to C. A. along hairline to 1 urn sericitic slip planes, clasts (0.5 cm and less) have been stretched into the plane of foliation.

t


PROPERTY U, R..., HOLE No rv; ,M SHEET No i*

0

12

3

4

5

6

7

e9

0

i2

3

4

5

6

7

e9

LITHO

~

-

-

^

^

' JVI5.to

-

^

.

-

FABRIC

e '

^*** '

. . - *

" *

"

. -, ' . '

K'

*

, '" '

- - f .

"" ' "

•" '

' ' *

* j?

1)

' O )

' '

l

ALTERATIONS [ corb

5

HM

aft*ssss5

MSsss5

se r chl

L™

iMMHLLf^\

N\

L

L

Vi.

i-

UMMH

/M

MAG SUSC

- o . c" * ' J

t '. t'

- ; ,

(

i . 1

f ,

— f ',,.

i

- C.C

-O.i

-C.I

-1:1

-c. t

—

-

Q wpy

TVT,T/

T,

T,Tr

1V

TV

poNEP XLIZ VTIC Mmag mo cp

ASSAYSSAMPLE

^ell- ?m

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DESCRIPTION J SKETCH

DEBRIS FLOW

" ; 330. 85 - 333.0 m Foliation still present at 60* to C.A. as sericitic l chloritic slip planes; clasts (up to 1 cmhave been sericitized, slightly heroatized andstretched along foliation; trace amounts py asgranular disseminations.

-

337.0 - 347.0 m Weakly to moderately foliated at40 - 45* to C.A. with chloritic zones; clastsappear to be weakly contained within the foliation;weakly to moderately hematized; selectivehematization of clasts with minor hematite in matrix; trace amounts of py as granular aggregates anddisseminations.

347 E.O.H.

.

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Ministry of Northern Devel and /dines

Mario

Wrrteiind P(gBk^ddreis of Recorded Holder'" ' j? "' -ISAUBNbUBG/ b(9 GUIBORD

St. Joe^inada Inc. ' , . ,,^^

f 1116 - 111 Richmond Street West, Toronto, Ontario

900————— 1

Summary of Work Performance and Distribution of CreditsTotal Work Da y t Cr. claimed

4097.77for Performance of the following work. (Check one only)

Manual Work

PrefixMining Claim

Number

t Sinking Drifting or other Lateral Work.Compressed Air, other Power driven or mechanical equip.

Power Stripping

Diamond or other Core drillingLand Survey

667887

667888

667889

667890

667891

667892

667893

667894

Work Days Cr.

Mining ClaimNumber

667895

667896

667897

667898

667899

667900

667904

667905

Work Day* Cr.

Mining ClaimPrefix Number

667906667907667908667909667910

20 66791120 66791220 667913

Work Dayi Cr.

60 l 60

J&O.60

J&Q-6060

All the work was performed on Mining ClalmU): L667947j L669748) L669749

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

DRILLING PERFORMED BY BRADLEY BROS., TIMMINS, ONTARIO

EQUIPMENT USED: BRADLEY BROS MOBILE DRILL - BQ CORE

DRILLING PERFORMED BETWEEN NOVEMBER 16, 1986 and MARCH 13, 1987

ASSESSMENT r; i i.,-J Rt:St:;AMCH C ri" l w-:

)Qf}

MININO DIV.

®iJ AN O 41988

RECEIVED

Certification Verifying Report of Workl hereby certify that l have a personal and intimate knowledge of the facts tet forth In the Report of Work annexed hereto, hayjjig performed the work or witnessed same during and/or after Its completion and the annexed report Is true.

o, having

s]Name and Postal Address of Person Certifying

W.E. Glenn , Staff Geologist #1714 - 390 Bay Street, Toronto, OnCertifi

Table of Information/Attachments Required by the Mining Recorder

Type of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed elr, other power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

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 Ontario land surveyer.

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 post.

Work Sketch (es above) In duplicate

Nil

768 (85/12)

NUMBER DAYS NUMBER DAYS

L66-;L66791L667916L667920L667921L667922L667923L667924L667925L667926L667927L667928L667929L667930L667931L667932L667933L667934L667947L667948L667949L667950L667951L667952L667953L667954L667955L667956L667957L667958L667959L667960L667961L667962L667963L667964L667965L667966L667967L667968L667969L667970L667971L667972L667973

602020202020606060606060606060606020202020202020202020202020202020202020202020202020202020

L667974 L667975 L667976 L667977 L667978 L667979 L667980 L667981 L6679.82 L668007 L668008 L668009 L668013 L668014 L668015 L668016 L668019 L668020 L668021 L668022 L668023 L668024 L668025 L668026 L668027 L668028 L668029 L668030 L668031 L668032 L668033 L668034 L668035 L668036 L668037 L668038 L668039 L668040 L668042 L668043 L668044 L668045 L668046 L668059 L668060

206060606060606060606060606060606060606060606060202020202020202020202020202020202020206037.77

k•X j .

667911 j 667926

6(791} j 6C7024 7KIOI l 714102 l

7UIOO |7l4u99

9*f*4**4**444S?'t* f 4 lzi|*ft.

- -667901 . 667904

667602 i 6 67903

669764 j 669766669762 i 669765

669769 J6ES766 669767 j 669766i" "~"i r i

66977? 1(6977C]9Jl 1 6679546C8082 668007r.66T65Z C679J3 6 63776766'* 7 74

66977* .6697;*

669781 ( 669780 L"~~ fi" ' ~

l

t102699* t 1020640

-t* J t#* 11 fi? (.6 J

tOMMB ' I02**4I

DD RPT 50 GUIBORD - Ontario · diamond drill record property dip test angle hole no sheet no j,,3...

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