DD RPT 50 GUIBORD - Ontario · diamond drill record property dip test angle hole no sheet no j,,3...
Transcript of DD RPT 50 GUIBORD - Ontario · diamond drill record property dip test angle hole no sheet no j,,3...
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
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
'
\
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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 .
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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.
DIAMOND DRILL RECORD
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
ASSAYSSAMPLE Auppb DESCRIPTION SKETCH
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.
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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.
DIAMOND DRILL RECORD
PROPERTY HOLE No w SHEET No i
LITHO FABRIC si corbALTERATION
serMAG SUSC Q py PO
NERALIZATIOmag mo cp
ASSAYSSAMPLE Auppb DESCRIPTION SKETCH
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
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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. .
DIAMOND DRILL RECORD
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
ASSAYSSAMPLE Auppb DESCRIPTION SKETCH
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,
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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.
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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.
DIAMOND DRILL RECORD
•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
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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 ;
-
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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
DIAMOND DRILL RECORD
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 '
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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.
.
- //' ffl J^P J* \
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