OM84-6-P-356: RPT OF WORK PERFORMED IN 1985 ON PROP IN HEARST … · 2017-01-17 · HEARST TWP...
133
MANY METALS DISTANCES FROM D.DH COLLARS TO A CLAIM POST IMITE CLAIMS MAP ,A -J ^* ( - -i 320/4
Transcript of OM84-6-P-356: RPT OF WORK PERFORMED IN 1985 ON PROP IN HEARST … · 2017-01-17 · HEARST TWP...
MANY
MET
ALS
DIS
TA
NC
ES
F
RO
M
D.D
H
CO
LLA
RS
TO
A
C
LAIM
P
OS
T
IMIT
E
CL
AIM
S
MA
P
,A -
J^*
(- -i
320/4
MW
ITT
IE
HE
AR
ST
L496
995
L496
994
1447
515
L452
03 P
)
L400
80(P
LA
RD
ER
LA
KE
L400
8I P
)
L424
35(P
)
L452
04(P
)
L4I6
48(P
)
L4I6
49 P
L4I6
50(P
- -
y;
L505
22(P
)L5
2265
0
L505
23(P
)
L496
442
L496
277
L522
65I
L476
447
L429
935
MANY
M
ETAL
S M
INES
L476
446
L496
276
L477
384
L3I9
453
L495
048
L429
936
L476
659
*es
L477
I87
L522
652
L476
666
L476
665
L495
049
L477
I88
L3I9
452
066&
-I3.
-
" -y
. ^ -
L476
660
L103
640
L478
66I
L477
386
FA
LC
ON
BR
IDG
E
LSM
iTE
D
D N
T A
R !
OD
IST
AN
CE
S
FR
OM
D
.DH
C
OLL
AR
S
TO
A
C
LAIM
P
OS
T
CL
AIM
S
MA
P
GEOP
HYSI
CAL
LEGE
ND
SE
MAGNETIC S
URVE
Y
-2
Mag
netic
con
tour
{g
am/n
asl
• •••
••••
••-.
Mag
netic
axe
NOTE
: Ad
d 58
,000
ga
mm
as
for
tru
e
rea
din
gs
800
-052
CO
RP
OR
AT
ION
FA
LCO
NR
HlO
Ge
CO
Pf-E
fi
-OS
8 JA
ME
S
OP
TIO
N-0
54
LO
WE
O
PT
ION
1
-05
2-0
57
CU
NN
ING
HA
M
OP
TIO
N
-055
CaO
XA
LL
O
PT
ION
LIM
ITE
D
TW
P
PR
OJE
CT
, P
N-6
60
HEAR
ST A
MCE
LROY
TW
PSO
NT
AR
IO T
l
GE
OL
A
LT
EE
Dat
e-'
Sep
t 1
98
5
Inte
rpre
ted
:
Date
:C
. Lavoie
P
h.D
. S
ept.
19855 85
Inst
:S
cin
trex
MP
-3
magnetic
gra
dio
mete
r
N.T
&:
32D
/4P
1 a fi
no
: 85-1
68-0
3
MC
VIT
TIE
HE
AR
ST
LA
RD
ER
LA
KE
TsTn
s 1 1
1 s
'"s
s s
a 5
s s ij i i i i s
i i s
s s
i s
||
s s
s |
K s
s fi^T
s g
g i S
i l'i l~
i llT
ifS
fss l(
|
g AS
s g
s g
g 3
s g
g j
g g
s j! gil i a
g.g
tai s
'g) i s
"s?
iig
iS5S
39S
*153 S
ijaj s
1 1
1,1
a i
sT
-*
"3
i -* \
i
-*
--
^ ^
x
s g
g a
s s
s ss s
g s
8 g
s g
g g
s a
s i is lis
sssiii
s s
s s
**
m l
pi
o
9
ffi
or/
Q
tv
en
ifi
{ym
K 8L
3 g I
g S
's s
i\I
ss
R s
r K
S 2 i
8XK
l* s
s a
s S
r~
r*-r*-?*-K
r^alu
3r".|'-.r~
r~
r~
*^~
r3
GEOPHYSICAL
LE6F
NDs
2 s
S S
S i
* s
S S
S s
S g
S s i
S t
S S
s s
2 s
g i
8
MAG
NETI
C SH
RVEY
tt
o
^.X
9
ID
V2
9
V
B
C-.
3
fip
T*
** h
i m
^Q
s s
s^s
ssIs
SS
sfis s
/s B
SS
NOTE:
AdiTSB.OOO g
ammas
for
true readings
, f
^ J ^—A
r^
njfT
pm
Mr^S
iffl
i S O
2 S
S 3
8 3
? S
s S
5 i S
8 S
5 8
5 g
; 5
5 S
S S
5 S
S i
Ss
s i
a 8
s s
s B s
t E
x i
si a
g e 2
in ^
ir?
s *
s s
s s
s
s s's
sae
s s
i
a a
s s
5 s
8 8's
a/5
s s
s s
s W5
s B
a B
s s
s s
6 B
B s
S S
S B
'l l i l l IX
s 2
rsj
8 S
8 8
8 8
fi^S
5 i
S S
8 i i i B
/i 3
B l g
"S
83
*8
Es
Sw
SaaaOooo&BOo
•^ "
^^5
-052
i ^
^^^
MANY
ME
TALS
BV
! S
B l/B
S S
S s
m 8
iS/
fl S
8 B
S r
g
8E
&B
88
S8
&8
S&
BB
8&
S&
S M
J
\ /t'/ 7
rll
** "
r
i ^
^S
5
cv
S
S t
m
B] ^/n
/r* [
^2
m
v
T
TT
n
m
-**/
kp
* */
-^ l
*r
n
^F
AL
CO
NB
RID
GE
LI
MIT
ED
TW
P
PR
OJE
CT
, P
N-6
60
fiEAR
ST s
, MCE
LROY
TW
PS5j
O
NT
AU
i..*
--
JO
NT
AR
IOIH
EE
T
CO
RP
OR
AT
ION
FA
LCO
NB
RlD
GC
CO
PPER
JA
ME
S
OP
TIO
N
-054
LO
WE
O
PT
ION
(-
052)
-057
CU
NN
ING
HA
M
OP
TIO
N
CR
OX
AU
O
PT
ION
Sc
intr
ex
M
P-3
m
ag
ne
tic
g
rad
iom
ete
r
N.T
S.:
,-
^ ,
. P
lan
nonte
rpre
ted:
Dat
e:
C.L
avo
ie
Ph.D
. S
ept.
1985
32D04SE8172 63.4636 HEARST
23
0
16
. 18
22
17 (
'l*
2
6
ES
TR
AN
GE
ME
NT
3 10
"1
5 \3
d
(74
71
FA
LC
ON
BR
IDG
E
VL
F-N
AA
/N5
S
FRA
SE
R
VA
LUE
S
CO
MB
INA
TIO
N
^^....
CO
NTO
UR
S
K:;.:
.GE
OLA
32D
84S
E8172
63
.46
36
H
EA
RS
T240
GE
DD
ES
/85
01/8
6
Q-S
32
D/4
MW
ITT
IE
LA
RD
ER
//A
/.//
r
' ,
7
6
66
21
13
12
/J
7 O
i
2
57
9573
25
73
1
717
2
2
23
24
17
113
4
32 ^50
55 "50^ 3
1\1
?V
7
O23
2
2
20
24
16
B 6
^2
5
7 3
,x1,2
H
15
^4
10
9
o
-o
o
3 9
10
6 4
7 7
liX
^1
7
S l
03
74
71
10
\ 13
H
\ \
/' '
21
y 35/7
1/1
10'
12
^^(
16
22
2
0
18
15
--1
49
12
11
14
115
4^4
9
47
^4
6^
53
35'
31
39
O5
7 1
3/2
4 r X
34
32
32
41
35
35
2'
4"
t5
12
M9
20 f 28
28
28)
22
18
19
22
22
20
18
22
719
19
l?
71
11
M
14
13
13
'O
6
5
4
-T
O
P-.
-C
"l
in
"I
W
W}
9 '
12
H
6 5
34
48
37
34
32
29
37
37
^-5
8-^
^3
9,^
59
X.4
ft/
58
58
50
53
54
61
63
67
63
71
6H
^i^
*7!
! *?
42
52
51
21
^
28
27
29
28
26
37/2
025
18
33
35
-^1
9-^
7
25
33
31.X
7
10
522
^^1010
10
12
All
7 5
15
30
30
29
36
39
25
O 9
/20
31
/
17
12
12
O
FA
LC
ON
BR
IDG
ELIM
ITE
D
HE
AR
ST
T
WP
P
RO
JEC
T,
PN
-660
ON
TA
RIO
VL
F-N
AA
/NS
S
FRAS
ER
VA
LUE
S
CO
MB
INA
TIO
NC
ON
TO
UR
S
32
D 4
SE
*17
2
63
.46
36
H
EA
RS
T
ES
TR
AN
GE
ME
NT
-C52
C
OR
PO
RA
TIO
N
FA
LC
ON
BR
IDG
E
CO
PP
ER
-05
8
JAM
ES
O
PT
ION
-054
LOW
E
OP
TIO
N
[-0
52
-os?
C
UN
NIN
GH
AM
O
PTI
ON
-055
CR
OX
ALL
O
PT
ION
32D
04S
E0172 6
3.4
63
6
HE
AR
ST
FA
LC
ON
BR
IDG
E
LIM
ITE
D
HE
AR
ST
T
WP
P
RO
JEC
T ,
PN
-660
HEAR
ST s
MCE
LROY
TW
PSO
NT
AR
IOS
^E
ET
31
RO
CK
G
EO
CH
EM
IST
RY
Au(p
pb)
^^^^^ ^^
Sto
le400' O
40
0800
1200
16
00
fi
Su
rve
yed
: p.
NA
DE
AU
Da
re:
12
/85
Inte
rpre
ted:
Da
te;
Dra
wn
.GE
OO
ES
Dale
. 12/8
5
Rev
ise
NT
.S.
32D
/4
MC
VIT
TIE
S4S-
HE
AR
ST
LAR
DE
R
LA
KE
\ \
\ \i \ V45
:6S
DAVE
Y
LAK
E
\8S
\ \ \ t \\\
1
\ \ l
b
\\ \h \i
k
k
-052
365
38
,
.. 40 S
*
\
t
* \b
l
h
l \h
\ #;
\
\
V t \- \
MAN
Y M
ETAL
S
l Y \ \ \S
OS
525
\
\
32D84SEei72 63.4636 HEARST
,, -F
AL
CO
NB
RID
GE
LI
MIT
ED
HE
AR
ST
T
WP
P
RO
JEC
T,
PN
-66
0
HEAR
ST s
, MCE
LROY
TW
PSO
NT
AR
IO
RO
CK
G
EO
CH
EM
IST
RY
Au
(pp
b)
ED
DE
S32D
/4
ES
TRA
NG
EM
EN
T
-052
Est
rangem
on f_
Lake
-052
CO
RP
OR
AT
ION
F
ALC
ON
BR
IDG
E
CO
PP
ER
-058
JAM
ES
O
PT
ION
-054
LOW
E
OP
TIO
N
|-O
S:
-057
CU
NN
ING
HA
M
OP
TIO
N
-055
CR
OX
AL
L
OP
TIO
N
63.4
636
HE
AR
ST
28
0
FA
LCO
NB
RID
GE
LI
MIT
ED
HE
AR
ST
T
WP
P
RO
JEC
T ,
PN
-6
60
HEAR
ST 6
; MCE
LROY
TW
PSO
NT
AR
IO
RO
CK
G
EO
CH
EM
IST
RY
_
__
__
__
__
_ co
2 (Vo
) ____^___
Scale
, l"
^400' O
400
800
12
00
1600
ft.
Su
rve
yed
: P
.NA
DE
AU
Date
-. 1
2/8
5
Inte
rpre
ted-.
Date
:
Dra
wn;
GE
DD
ES
Date
: 12/8
5
Revi
sed
Date
;9i
NIT
.5.
32D
/4
MC
VIT
TIE
HE
AR
ST
LAR
DE
RLA
KE
MANY
ME
TALS
FA
LC
ON
BR
IDG
E
LIM
ITE
D
HE
AR
ST
T
WP
P
RO
JEC
T,
PN
-660
HE
AR
ST
S.
M
cELR
OY
T
WP
S
ON
TA
RIO
RO
CK
G
EO
CH
EM
IST
RY
c 02
V.
NG
EM
EN
T
-052
CO
RP
OR
AT
ION
F
ALC
ON
BR
tDG
E C
OPP
ER-O
58
JA
ME
S
OP
TIO
N
-054
LO
WE
O
PT
ION
[-
052
-057
CU
NN
ING
HA
M
OP
TIO
N
-055
CR
OK
AU
O
PT
ION
HJ
LIM
ITE
D
TW
P
PR
OJE
CT
, P
N-6
60
8IE f
HEAR
ST s
, MCE
LROY
TW
PS"~
^
ON
TA
RIO
Scin
tre
x
MP
-3
magnetic
gra
dio
mete
r
nte
rpre
ted :
Date
.C
. Lavoie
P
h.D
S
ept.
1985
CE
ME
NT
f B
filO
i a i
a li
11 it
M *
M
-s a
i y
i li
HI F
1 T
-052
CO
BP
OR
AT
ION
F
AIC
ON
BR
IDG
E
-058
JAM
ES
O
PT
ION
-054
LO
WE
O
PT
ION
(-
05
2)
-057
CU
NN
ING
HA
M
OP
TIO
N
-055
Cft
OA
AL
L
OP
TIO
N
32
00
45
6*1
72
6
3.4
63
6
HE
AR
ST
310
LIMITE
D
lTW
PHE
ARST
A M
CELR
OY T
WPS
ON
TA
RIO
H
-660
'D&
f #r
Tra
ced:
Dote
;
GE
OL
A
LT
EE
S
ept.
1985
Inte
rpre
ted:
Dare
:C
. Lavoie
Ph
. D
, S
ept.
1985
lust
Scin
trex
MP
-3
magnetic
gra
dio
mete
r
32
D/4
Pla
n
no:
85-1
68-0
2
ES
TkA
NG
EM
EN
T
-052
Estr
angem
ent
Lake
-052
CO
RP
OR
AT
ION
F
ALC
ON
BR
IDG
E C
OP
PE
R-0
56
JAM
ES
O
PT
ION
-054
LOW
E
OP
TIO
N
(-0
52
-057
CU
NN
ING
HA
M
OP
TIO
N
-055
CR
QX
AL
L
OP
TIO
N
50-1
00
)-IO
O
613-
02^
660-
10
LE
GE
ND
MA
G
axis
I P
axis
VL
F
axis
Gra
dio
me
tric
hig
hs
^ 1
00
)
Re
cen
t d
iam
on
d d
rill
hole
s
32D
WS
E0172
63
.46
36
H
EA
RS
T320
FA
LC
ON
BR
IDG
E
LIM
ITE
D
HE
AR
ST
T
WP
P
RO
JEC
T ,
PN
-6
60
HEAR
ST 6
MCE
LROY
TW
PSO
NT
AR
IOS
HE
ET
l
GE
OP
HY
SIC
AL
C
OM
PIL
AT
ION
MA
P
Sca
le
l":
40
0
Surv
eyed:
D a
te -.
Inte
rpre
ted
: M
.B
ER
UB
ED
ate
: 0
1/8
6
Dra
wn .
GE
DD
ES
Da
te:
01/8
6
Revi
sed ;
" NT
. S.
32 D
/4
MC
VIT
TIE
HE
AR
ST
LAR
DE
RL
AK
E
FA
LCO
NB
RID
GE
LI
MIT
ED
HE
AR
ST
T
WP
P
RO
JEC
T,
PN
-660
HEAR
ST s
MCE
LROY
TW
PS
MA
G
ax
isI
P axis
VLF
a
xis
Gra
dio
metr
ic
hig
hs
^ 1
00
Rece
nt
dia
mo
nd
drill
hole
s
GE
OP
HY
SIC
AL
C
OM
PIL
AT
ION
M
AP
052
CO
RP
OR
AT
ION
F
ALC
ON
BR
IDG
E
CO
PPER
058
JAM
ES
O
PT
ION
054
LOW
E
OP
TIO
N
(-052)
057
CU
NN
ING
HA
M
OP
TIO
N
055
CR
OX
ALL
O
PT
ION
3...-
a^^^C
l" r
"" r
"" r
, a
— -S
-—f ..
..T
...-
ES
TR
AN
GE
ME
NT
R
S
fi
9
K
MAM
METM
S L
32D04SeB172 63.4636 HEARST
34
0
- GEOPHYSICAL
LEGE
ND
ELECTROMAGNETIC
SURVEY
—— — G
roun
d y.L.F. an
omaJ
y
Y. L. F.
prof
iJe
In-P
hase
D
ot-o
f-Pha
se
In-P
hasB
-/
+ 100
X
-Out
-of-P
nase
-100
X
100X
=
l in
.
—--
^r f
t -052
CO
RP
OR
AT
ION
FA
LCO
NB
H10
GC
CO
PPER
JAM
ES
O
PT
ION
LO
WE
O
PT
ION
1
-05
2)
CU
NN
ING
HA
M
OP
TIO
N
CR
OX
AL
L
OP
TIO
N
Scole
LIM
ITE
D
PR
OJE
CT,
PN
-660
MCEL
ROY
TWPS
ON
TA
RIO
HE
ET
l
(PRO
FILE
S)800
1200
1600
f t-
Troc
ed;
GE
OLA
LT
EED
ote
: S
ept.
1985
nte
rpre
ted
: D
ate
-.C.
Lav
oie
Ph.D
. S
ept.
1985
lns
t .
Frv
q :
S
tal
:
Sci
ntre
x IG
S-2
2
4.0
kH
z.
NA
AfC
utl
erl
32 D
/4P
lan
no
:85
-168
-05
s a
a 2
ssXs
s xsTx
Tv ?
S V t
ES
TR
AN
GE
ME
NT
MANY
MET
MS
l
GEOP
HYSIC
AL
LEGE
ND
ELEC
TROM
AGNE
TIC S
URVE
Y
Fras
er /
netn
oa c
onto
ur
CO
ftPO
ftATi
ON
JA
ME
S
OP
TIO
N
LOW
E
OP
TIO
N
[-052
CU
NN
ING
HA
M
OP
TIO
N
CW
OX
AIL
O
PT
ION
/e
FALC
ON
BR
IDG
E LI
MIT
ED
t^E
^tS
T
TWP
P
RO
JEC
T, P
N-6
60
(FRA
SER
METHOD C
ONTOURS)
Scm
trex
IG
S-2
2
4.0
kH
z.
NA
A
Cu
tler
Inte
rpre
ted
: D
ate
;C
. La
voie
Ph
.D.
Sept
. 19
853S
Da4S
E817
2 63.4636 HE
ARST
ES
TR
AN
GE
ME
NT
GEOP
HYSIC
AL
LEGE
ND
MAGN
ETIC
SUR
VEY
Mag
netic
axi
s
MAG
NETI
C P
RO
FILE
mm
m
m
l i
i T
11!
20
Gra
ttJo
fetr
ic f
frofiJ
e
300
450
350
ISO 50
-15
-25
\-1
0 -
Mtf
fvet
Jc f
frof
JJt
l
GRAD
IOME
TP.I
C PROFILE
NOTE:
Add
58, oO
O gammas fo
r re
al re
adin
gs
32D
**S
e*1
72
63.4
636
HE
AR
ST
36
0
LIM
ITE
D
TWP
P
RO
JEC
T, P
N-6
60^H
EARS
T s
MCEL
ROY
TWPS
ON
TA
RIO T
lFO
LS
cole
: l"
- 4
00
'400
800
1200
leoo
ft.
Troc
edG
EO
LA
L
TE
ED
ote
:S
ept
1985
Inte
rpre
ted :
' D
ate
:C
. L
av
oie
P
h.p
. S
ept.
19
85
Inst
Scin
trex
MP
-3
ma
gn
eti
c
gra
dio
mete
r
N.T
S.
32
0/4
Pla
n n
o s
85-I6
8-04
MCV
ITTI
E
HEA
RST
LA
RD
ER
LA
KE
*!*1
— rtrfi-^
tn
r-
1
~
1
cs
. ™
. -*
m
A
TT
,- f r
i*
T'
.•rJv7?f'7
ritl?
f'fV
'T*"*ri
Sl8
Sg
5S
38
SS
gS
iig
iHS
0S
gB
esS
SB
Rin
sss
i 2 .
3 5
9 5
g^-
7? ?
^?
?3
^?
? ^
y?
^;?
?ys?
S '•
SB
ailB
Bw
BE
ib'1
S|i
SS
BP
E3l5
EB
BS
Ba3asB
|""™
~'~
-*r
*-'-
p"™'-™
Bi'"
F-'^
'-*-'-*
*~
^
X—
™
w,
—
^m
w
— -••"••^
, a.,,,, a
\•f-
*
- T
T
T
*C
-*
\
-.--.-.-,---.
.M,.-...,. ....
w...
w...-.-. .-.-......-..n
-*.^-."-.^----.-
\V. --------a
^-.-.---! \
?v
'T
?5
Tr3
^?
?^
r-"-V
^?
T'T
T:^
VfV
T?
"T
'T^
VV
T'T
Tf?
"T
"T
"f?
?V
T-fvV
™^
vV
fV
T?
^fT
'VT
^^
*rT
T''l''r"f't
j'P
T
OS
•^
tilrT
VyT
t:?
?T
?r''fT
l
*
BB
iBB
BS
BS
BB
BR
filB
Bfi 5
1MftseEaasVissses
sssg^sssjssssssaEg
aRxsaasfasMBS
i;i sg
a easssfiasaaasKRsa
asKsassss'SHass
assBssssaaasiaESsB?
3;9?^?3a9^x33
?333n3
?s sav--73sa3a33?
733
7-t
?9a3-*-. 733999?9399Ba3??3?57^3aa35975979?9?7a39?3a979?9a?999 5-^ 399?99?3339?9999999993?97?9
D, fi
B r' M
a
a s
fi S
B
2
8 S
* B
H 9
S S
fi
B B
B
8 g
Bi
8 K
H s
X fi a
fflE
BlfiH
ES
aH
BE
**5
5e
SB
8*5
58
*S
*B
B*S
SS
SB
BfiR
S83E
B83aS
9S
89(8S
BH
SR
BB
Slf8;
4i4
^^r^l^T
4^^
i?*
7s^2
3Eid
~-S
25
S
saSasBi&SSBaSSBBiE
???T
'5^?T
~V
7'"""5T
?'?
'rT
:'r'?
?i1
7'i''r-7
-1fV
'fi
";T
*
fl g
g s
B s
B s
B s
s B
s a
ft ss B
ni
a g
i B
a B
B a
a a
B i
s a
B i
B B
a s
g fi
s a
B a
s B
8 B
B s
a s
s
.37
33
27
3-.-
!3
73
-3
^-!7
--3
3i3
3i-
!3
53
? S
3 7
9 ?
S
3 3
-.
?
33335?? 5
3
33373-1
335333-.
33
33
33
33
73
3^
33
33
33
33
33
33
3
s a s
s g s
s s 3
s a 1
6 s a
s s n
ss a
K s a
a f s
s a E
B s a
s s s
5 s g
FALC
ONB
RIDG
E LI
MIT
EDTW
P
PRO
JEC
T, P
N-6
60HE
ARST
s M
CELR
OY T
WPS
ON
TAR
IOH
EE
T
-052
C
OR
POR
ATI
ON
FA
ICO
NB
RIO
3C C
OPPE
R-0
58
JAM
ES
O
PTIO
N-0
54
LOW
E
OP
TIO
N
(-052)
-057
C
UN
NIN
GH
AM
O
PTI
ON
-055
C
BOX
At L
O
PT
ION
Sci
ntre
x M
P-3
m
agne
tic
grad
iom
eter
Inte
rpre
ted
:C
. La
voie
P
h.D
32
DM
5E
ei7
2 6
3.4
63
6
HEA
RST
370
MCELROY TWP HEARST fwp"
G) CO G
ES
TR
AN
GE
ME
NT
MANY
MET
ALS
l
GEOP
HYSIC
AL
LEGE
ND
ELEC
TROM
AGNE
TIC S
URVE
Y
——
——
G
roun
d V
.L.F
. an
omaJ
y
L. F
. p
ro f^
JeIn
-Pna
se
Out
-of-P
hase
In-P
hase
-
+ iO
O%
-Out
-of-
Pfia
se
-100
X
100X
s i
in.
CO
RP
OR
ATI
ON
FAL
CO
NBR
tOO
e CO
PPER
JA
MES
O
PTI
ON
LO
WE
O
PT
ION
C
UN
NIN
GH
AM
O
PT
ION
C
HO
XA
U
OP
TIO
N
32D
84S
E81
72
63
.46
36
H
EA
RS
T330
FALC
ONB
RIDG
E LI
MIT
EDTW
P PR
OJE
CT,
PN
-660
HEAR
ST s
, MCE
LROY
TWP
SO
NTA
RIO
SH
EE
T
I V.
L.F
(P
ROFI
LES)
Sca
le:
i :
40
0leo
ott.
Troc
ed:
GE
OL
A
LTEE
Dat
e'
Sep
t. 19
85
Inte
rpre
ted
.
lnst
:
Fre
q :
Scin
trex
tG
S-2
21
.4kH
z5
fat
; N
SS
(Ann
apol
is]
NT
S.'
32
D/4
Pla
n no
: : 85-
168-
07
MC
VITT
IE
HEA
RST
GEOP
HYSIC
AL
LEGE
ND
MAGN
ETIC
SUR
VEY
Mag
netic
axi
s
MAG
NETI
C PR
OFI
LE
LA
RD
ER
LA
KE
GR
ADIO
MET
RIC
PR
OFI
LE
NOTE
: Ad
d 58
,000
ga
mm
as
for
real
re
adin
gs
O A If
E Y
MU
-
MANY
MET
ALS
. FAL
CON
BRID
GE
LIM
ITED
B^R
ST
TWP
PRO
JEC
T, P
N-6
60HE
ARST
s. M
CELR
OY T
WPS
ON
TAR
IOM
EE
TTR
DC
P
IRO
FIL
-052
C
OR
PO
RA
TIO
N F
ALC
ON
BRID
GE
COPP
ER-0
58
JAM
ES
O
PTI
ON
IOW
E
OP
TIO
N
(-052)
-057
C
UN
NIN
GH
AM
O
PT
ION
-055
C
(OS
ALL
O
PT
ION
Sci
ntr
ex
MP
-3
mag
netic
gr
adio
met
er
Lavo
ie
Ph.
D Se
pt.
1985
MC
VITT
IE
HE
AR
ST
SO
N
B
S X
GEOP
HYSIC
AL
LEGE
ND
ELECTROMAGNETIC
SURVEY
Gro
und
y.L.
F.
ano/
najy
Y. L.
f.
pro
fiJe
LA
RD
ER
LA
KE
DAV
E!
LAKE
K fi
,.-
E3 —
. 5 ..
.. 3
—- S
-— S
-052
l ^
HH
I
MANY
MET
ALS
m—
——
m—
——
—d—
——
'5—
——
^
m
S ..
-SS
~—
—S
——
~3
——
--S
-——
-S—
—--
SJ-—
—.3
3
r-
(.
*^-.
T..
—5
——
.1 ,
.—T
— --
, -
—-
, —-
i .
i i
i T
i
T
-i —
—i....
i
— —
—
(V-0
3
^^P
---—
"T-—
T ..
...f
T
S T
9 B
S
S/X
?
1
:^
—V
-*-
--^
fcfn
-*
cy \
PI
i i
' "T
"-~
i
" *
i
FALC
ON
BR
IDG
E
LIM
ITED
TWP
PRO
JEC
T, P
N-6
60s
HEAR
ST s
MCE
LROY
TWP
SO
NTA
RIO
L.F
(P
ROFI
LES)
-052
CO
R f O
RA
TIO
N F
ALCO
NBRI
DGE
COPP
CR-O
58
JAM
ES
O
PTIO
N-0
54
LOW
E O
PTI
ON
[-
05
2J
-057
C
UN
NIN
GH
AM
O
PTI
ON
-055
C
BO
XA
ll O
PT
ION
GE
OLA
LT
EE
Sep
t 19
85S
cint
rex
IGS
-2
24-O
kHz.
N
AA
(Cu
tler)
nte
rpre
ted
. D
ote
:C
.Lav
oie
P
h.D
. Se
pt.
1985
MW
ITTI
E
HE
AR
ST
LA
RD
ER
LA
KE
DAVE
Y
LAKE
GEOP
HYSIC
AL L
EGEN
D
ELEC
TROM
AGNT
IC S
URVE
Y
2 z
s s
rm
V
sffi
2
S 2
S
r-
to
ip
m
r--
r-
o\
i i
V V
T V
-r
tt
CD
at
cu
T*
-vi
i i
i —
cw
tp
"
ip
cu
m
o
f
V
' '
' '
sn R
\\ r
s ffi
s 3
MANY
MET
ALS
\ r-
D
l
r-
cu
/ m
co
\
n
-j l
CM
tr
y
i~
T-
" o
C
* ™
\"
\,
, i
\
CO
RP
OR
ATI
ON
FAL
CO
N B
RID
GE
COPP
ER
JAM
ES
O
PTI
ON
LO
WE
O
PT
ION
(-
052)
CU
NN
ING
HA
M
OP
TIO
NC
BOX
ALL
O
PT
ION
32D
04S
E01
72
63.4
636
HE
AR
ST
MC
VITT
IE
HEA
RST
GEOPHYSICAL
LEGEND
ELEC
TROM
AGNE
TIC S
URVE
Y
Gro
und
f.i.F
. an
omal
y
LA
RD
ER
LA
KE
\™
T --
r ""
? ""
T X
r —
r...
ea
IE
n
in f -0
52l
^H
W
MANY
MET
ALS
i —
.. l ^
'l'
—
M
•*
m
o
f-
lu
SN y
ft —
cJf—
s —
z,
' V
'
'\
'
FALC
ONB
RIDG
E LI
MIT
EDTW
P PR
OJE
CT,
PN
-660
HEAR
ST s
MCE
LROY
TWP
SO
NTA
RIO
L.F
(P
ROFI
LES)
-052
C
OB
POR
ATI
ON
FA
ICO
NB
RID
GE
ODPP
CR-0
58
JAM
ES
O
PTIO
N-0
54
LOW
E O
PTI
ON
[-
052)
-057
C
UN
NIN
GH
AM
O
PT
ION
-055
C
HO
XALL
O
PT
ION
Sci
ntre
x IG
S-2
21
.4kH
z.
NS
SfA
nnap
olis
32D04SEB172 63.4636 HEARST
C.
Lavo
ie
Ph.
D.
Sep
t. 19
85
MW
ITTI
E
HE
AR
ST
LAR
DE
RL
AK
E
:052
MA
NY M
ETAL
S
GM
ttS
tLI
MIT
EDtS
TK
p^tS
T
TWP
PRO
JEC
T, P
N-6
60HE
ARST
s, M
CELR
OY T
WPS
"' '
*t-M
S
ON
TA
RIO
-052
C
OR
POR
ATI
ON
FA
LCO
NSf
ilOG
C C
OPPE
R-0
56
JAM
ES
O
PTI
ON
-054
LO
WE
OP
TIO
N
(-0
52
}-0
57
CU
NN
ING
HA
M
OP
TIO
N
Sci
htr
ex
IGS
-2
mag
netic
' gr
adio
met
er
32D04SE0172 63.4636 HEARST
MCV
ITTI
E
HEA
RST
LA
RD
ER
LA
KE
GEOPHYSICAL
LEGEND
ELEC
TROM
AGNE
TIC S
URVE
YD
AVE
Y
LAK
EF
rase
r m
etho
d co
ntou
r
to
g)
Q
**
r-^*
w
en
PI
rn
i i
i i
S
S Si
S
R
Si
S
V"\*
9
R
m \ e
n (D
o
l/
-w
01\K
i to
CM
// m
**
\ l
l l I
I l
.
t
S
ffi
5)
-052
i ^^^
MANY
MET
ALS
s c
\a V
V"
'"/s
s
vO\
'03
ti
VV
"S
i
•^
I \N
(V
TT
FALC
ONB
RIDG
E LI
MIT
EDTW
P PR
OJE
CT,
PN
-660
^ HE
ARST
s. M
CELR
OY T
WPS
ON
TAR
IO TC
Lt.i:
,;,i'
LViS
I
(FRASER
METHOD C
ONTO
URS)
-052
C
OR
PO
RA
TIO
N F
ALC
ON
BRID
GE
COPP
ER-0
58
JAM
ES
O
PTI
ON
-054
Lowe
OPT
ION
(-052
)-0
57
CU
NN
ING
HA
M
OP
TIO
N-0
55
CR
OX
AU
O
PT
ION
Sci
ntre
x IG
S-2
2
kHz.
M
SS A
nnap
olis
Sep
t 19
85
C.
Lavo
ie
Ph.D
. Se
pt
1985
ES
TR
AN
GE
ME
NT
-C52
C
OR
PO
RA
TIO
N
fALC
ON
BR
iDG
E C
OPP
CR-0
58
JAM
ES
O
PT
ION
-05d
LO
WE
OP
TIO
N
(-052
-057
CU
NN
ING
HA
M
OP
TIO
N
-055
CR
OX
ALL
O
PT
ION 50
00
L
B2
Div
idin
g lin
e be
twee
n zo
ne
of
Hig
h an
d Lo
w
Res
istiv
ity
Fre
qu
en
cy
Eff
ect
axes
a
nd
id
en
tific
atio
n
letter
[an
d
nu
mb
er
if
segm
ente
d]
32D
WS
E01
7a 63.4
636
HEA
RST
FALC
ON
BR
IDG
E
LIM
ITE
D
HEA
RST
TW
P PR
OJE
CT,
PN
-660
HE
ARST
s. M
CELR
OY T
WPS
*W
.4W
tgS
NETlT0
j o*
**-**
-**t^
9 Ju
l&
i.
1^=3
L
di
INT
ER
PR
ET
AT
ION
I.
PS
cale
1"
- 4
00
' fin
n
19nn
0
40
0
8V
, C
,. r-"'"'/
Surv
eye
d:
R. B
ela
ng
er
Dat
e:
/85
R
^y^^
H
^ , ,
'V''1
.*--*
.'
Inte
rpre
ted:
M. B
erub
e D
ate:
10/8
5
^^/^^*f^^^
16
00
ft.
i
/.'
----
Dat
e.•*
t\
-\ ib
*--9
^
Dra
wn.
Geo
des
Dat
e'
10/8
5
NT
S
32 D
/4
U
^"r.
-,.3
l ':'
.-
MC
VITT
IE
HE
AR
ST
LA
RD
ER
LA
KE
1984
^^^^
^^^^
^^
Pow
er L
ine
1
X.
. .
.^
MAM
META
LS
J H.
R.
FALC
ON
BR
IDG
E
LIM
ITE
Dne
be
twee
n zo
ne
of
Hig
h a
nd
Lo
w
Res
istiv
ity
HE
AR
ST
TWP
P
RO
JEC
T,
PN
-66
0F
req
ue
ncy
E
ffect
ax
es
and
ide
ntif
ica
tion
le
tter
lan
d
nun b
er
IT
Se
gm
en
ted
)HE
ARST
s, M
CELR
OY T
WPS
ON
TA
RIO
- C -F
-IS
t
INT
ER
PR
ET
AT
ION
I.P
ES
TRA
NG
EM
EN
T
LE
GE
ND
RO
CK
TY
PE
V
OLC
AN
IC
RO
CKS
V5 V6 V7
Inte
rmedia
te
or
ma
fic
And
esite
Ba
salte
V1
0J
Agglo
mera
te
V13
l
Ultr
am
afic
flo
ws
SE
DIM
EN
TA
RY
R
OC
KS
Und
eter
min
ed
(D
A
A m D
Qu
art
zite
F4
Iro
n
form
atio
n (c
arb
on
ate
)
INTR
USI
VE
RO
CKS
Sye
nite
Dio
rite
Ma
fic undete
rmin
ed
Gab
bro
3D
l D
iaba
se
3L
l La
mpr
ophy
re
MET
AMO
RPH
IC
RO
CKS
M
l U
ndet
erm
ined
SU
FFIX
ES
t S
hear
ed
Pill
ow
ed
Bre
ccia
ted
insi
tu
Flo
w b
recc
ia
Po
rph
yry
Porp
hyr
itique
Gp
G
raphite
Gn
Gale
na
Sp
Sphale
rite
Pyr
ite
Pyr
rhiti
te
Magnetite
Quart
z
Fuch
site
Sili
cifie
d
Se
rici
tic
Pyr
itize
d
Ca
rbo
na
ted
Ta
lco
se
Epid
ote
Ch
lorite
Chlo
ritized
Py Po
Mt q Pu
SY
MB
OLS
3
Abandonned
shaft
or
pit
D C
laim
post
)——
——
c Tr
ench
o——
——
i D
iam
ond
drill
hole
——
}-
Gla
cial
strie
An
ticlin
e ,
sync
line
Bed
ding
un
dete
rmin
ed, v
ert
ical,
incl
ined
Fol
iatio
n un
dete
rmin
ed,v
ertic
al,in
clin
ed
Ge
olo
gic
al
cont
ours
or
con
tact
s
Hill
ou
tline
Ou
tcro
p,s
ma
ll o
r la
rg
e
Fault
\^
\
V
32D04SE0172 63.4636 HEARST
4S
Q
FALC
ON
BR
IDG
E
LIM
ITE
D
HEA
RST
TW
P P
RO
JEC
T, P
N-6
60A
'^5
T S.
V\:E
-^
J Y
ON
TA
RIO
GE
OL
OG
Y
;, PS
I600
M
'o:e
: D.
Bouch
er
jofe
GE
DD
ES
10
/85
Rev
icd
,Di5
t*
NT
S
32D
/4
MC
VITT
IE
HE
AR
ST
LA
RD
ER
LA
KE
53
,S4
,A,i7
,Py
,Po,
GP
FALC
ON
BR
IDG
E
LIM
ITE
D
HE
AR
ST
TWP
P
RO
JEC
T,
PN
-660
ON
TA
RIO
GE
OL
OG
Y
32D04SE8172
63.4636 HEARST
•490
;r....v
. . -
, ,.,
. v^
5w
A/™
v^
D
Bou
cher
GE
OD
ES
1
0/8
5
-~
-' '*
'
s)
'^i-,
''
V
N '
32
D/4
^J-'e
#^,4
*
t, \.-'
;J~V
.f
REPORT OF WORK PERFORMED IN 1985
BY FALCONBRIDGE LIMITED
on the properties of
CORPORATION FALCONBRIDGE COPPER (PN-66O)
and of
MANY METALS MINES LIMITED (PN-613)
Hearst township, Ontario (NTS 32 D/4)
Dec. 30, 1985 Magloire Berube, P. Eng.
RESUME
During 1985, Falconbridge Limited pursued its exploration program in Hearst township, Ontario.
gol d-ori ented
Falconbridge (FL) owns one group of 132 claims in Hearst andMcElroy townships, Ont., 117 of which having been optioned fromCorporation Falconbridge Copper (CFC) in 1984 and 15 of whichhaving been optioned from Many Metal Mines Limited (MMM) in 1985.
The work done by FL on these 2 properties in 1984-85 comprises:
OptionClaims covered Lines cut (km) Mag survey (km) VLF survey (km) I.P survey (km) Geochemistry ,* Geology *- D. D. Holes Costs li
1984CFC3822.5115.019.356.3--
(3954)6 967*
1985 total 85CFC259.7
62.862.830.062.8(fi^62.8
6(3420)124 281*
MMM CFC9
22.521.021.01O.5
*; 21.0C37/*.;21.0
&C MMM3432.883.883.840.583.8C79/*.;83.8
3(2345) 9(5765)74 213* 198 494*
total 84-85CFC tt MMM
7255.3198.7103. 196.883.883 . 8
16(9719' )385 461*
Most exploration in 1984 was concentrated on the CFC claims requiring assessment work whereas most exploration in 1985 was concentrated on the CFC and MMM claims located in the vicinity of the alteration zone longing the Mitchell-Hearst fault.
A lot of anomalies were obtained from the several surveys performed during 1985.The 9 diamond drill holes bored in 1985 encountered a lot of pyrrhotite, pyrite, graphite or carbonate (Kerr-Addison type) but failed to intersect any significant gold values.
The main data have been interpreted and compiled on maps contained in pockets at the end of the present report. More detailed maps from the same surveys are contained in two separate reports considered as parts of the present one.
Additional work is recommended for 1986: a) on 1985 anomalies left unexplained; b) on claims farther northwest, in McElroy and Hearst townships, where precious and base metals have been reported, and c) on the Hemlar property forming an enclave within the Falconbridge group of properties. The 1986 program has not yet been worked out in detail but should include a complete review of all old data, a systematic gophysical coverage of the Hemlar property and a diamond drill compaign where stripping is not feasible.
The budget 30O OOO *.
for this program is estimated between 200 000 to
32D*4SE9172 63.4636 HEARST
TABLE OF CONTENTS
Title..................................... l
Resume......,......................,...... 2
Table of contents.................... . . . . . 3
Introducti on......................... . . . . . 4
Description of properties................. 4
Regional and local geology................ 4
Previous work............................. 5
Recent work............................... 5
Discussion and interpretation of results.. 7Geophysical surveys.............. 7Geochemical survey............... 9Geological survey................ 10Diamond drill hole campaign...... 11
Cone l us i on. . . . . . . . . . . . . . . .. . . . . . . . . . . . ,. . . . . 13
Recommendations........................... 14
References. . ,, . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 16
Certificate..................... . . . . . . . . . . 17
010C
Appendix A: diamond drill logsBs list of core geochemical samplesC: diamond drill sections
Sets of maps in pockets (in volume 2/2)— claims maps showing location of ddholes— geological map by D. Boucher- VLF compilation maps- General geophysical compilati on map- Geochemical maps for Au•- Geochemical maps for CO2
Annexed volumes:- book of I. P. pseudo-sections (I. P. map i riel.)- Report on mag. and VLF by Geola.....
INTRODUCTION
This report briefly describes the results o-f geophysical, geological and geochemical surveys together with the results of a diamond drill campaign carried out during 1985 in Hearst township, Ontario. This work was performed by Falconbridge Limited (FL) on two adjacent properties optioned from Corporation Falconbridge Copper (CFC) and of Many Metals Mines Limited (MMM).
Many maps are inserted in two complementary geophysical reports, one containing the pseudo-sections provided by Remy Belanger Enrg. who carried out the Induced Polarization survey, and the other one, provided by Geola Ltd who carried out the magnetic and V.L.F. electromagnetic surveys. The maps by Geola also integrate the computerised data obtained in 1984 in other parts of the CFC property. For all types of surveys, the data coming from both the CFC and MMM properties have been plotted together on the same map.
DESCRIPTION OF PROPERTIES
The CFC option comprises 117 claims located in Hearst and McElroy townships whereas the MMM option comprises 15 claims in Hearst township. The claims distribution is illustrated on the claim sketch inserted next page whereas the claims numbers are listed in appendix A. The CFC option itself, for CFC purposes, was sub divided in 12 blocks of claims and/or sub-options.
The center of the properties lies about 2 miles southwest of the mining town of Larder Lake. Most claims are easily accessible: first, highway 66 passes just north of the property; secondly, road 624 relying the towns of Larder Lake and of Englehart straddles the eastern limit of the properties and is opened all year round; thirdly, numerous summer roads and trails open for mining, timbering, hunting or sport purposes lead in or close to most claims.
REGIONAL AND LOCAL GEOLOGY
The geology of the area is well illustrated on map 1947-1 accompanying Volume LV1, part VI 11, 1947, of the fifty-sixth annual report of the Ontario Department of Mines, volume entitled: "Geology of Hearst and McFadden townships".
Geological surveys have been done on both properties by CFC and MMM. The local geology can be summarised by highly folded and faulted, steeply dipping, interlayered sediment^^ry and volcanic formations belonging to the Larder Lake Group. The sediments are mainly represented by greywackes with minor argillites and conglomerates whereas the volcanic rocks, by intermediate to ultramafic flows (classified as tholeiitic and komatiitic by CFC). Several syenitic plugs and dioritic dikes have been mapped or drill intersected.
MCVI
TTIE
TWP.
LAM
DCN
LAK
I
GA
UTH
IER
TWP.
44
H4
7J
, \.^
lf~
^
~~
l
L
ItlT
IO)
I1IT
II
Me
ELRO
Y TW
P.H
EARS
T
9
LE
GE
ND
LEA
SES
PATE
NTE
D
KIN
O'S
HI
GHW
AYS
POW
ER
LIN
ES
CLA
IM B
LOC
KS
CLA
IM
BLO
CK
NU
MB
ERS
BL
OC
K N
AM
ES
AN
D N
UM
BE
RS
Blo
ck
War
n*
C.F
C.
No
FI.
N
o
(M)
CLA
IMS
e.F.
C.
M
031-
TO
M-f
*0
Q
OPT
ION
.MA
NY
MC
ntl
PN
05
4-TO
PH
- M
O
Q
OPT
ION
. CNO
XALL
PN
08
5-70
M
. M
O
(T5)
O
PTIO
N-
HUDS
ON
IAY
PN .
09S
-TO
PN
- M
O
@
OP
TIO
N.C
UN
NIN
IHA
MP
N.O
e7.r
o P
N-M
O
(H)
OPT
ION
. JA
MES
P
N.O
M.r
O
PN
-*W
Q
CLAI
MS
C.F
.C.
PN
-09S
.ro
P
N-M
O
MM
M
MAN
Y M
ETAL
S M
INES
LTD
. P
N-I
IS
FALC
ON
BRID
GE
LIM
ITED
OPT
ION
CO
RP.
FALC
ONB
RIDG
E CO
PPER
O
PTIO
N M
AN
Y M
ETAL
S M
INES
LT
D.
HEA
RST
ctr
McE
LROY
TW
P.
CL
AIM
S M
AP
tOLO
tUTI
OO
l O
tHV
mt
nrf
. (O
I/M
)
r ' m
iMM
RiM
t LT
I.n
rril
tt t
n
(loot
s IM
. (0
1/0*1
- l
44
24
82
l44
24
83
\4
76
66
3
L A K
DE
K
LA
KE
l.
(673146
673143
_
44
14
77
144
1476
*l l
l.
773,9!4
77"6
l Est
ran
gem
ent
2264
01 5
2263
91
l. L
dtf
l.
522660
(52
26
59
* ^-.
-m
'
c.\
5226
621
l.
n
\ L
(322
6635
2266
41
L.
' L
-798831
79
88
33
l 7
98
83
2
1985
HEA
RST
TW
PM
e EL
ROY
break, well known and famous for the prolific in its vicinity, passes just North of Larder separates the Larder Lake Group from the farther North. Two major cross-faults and faults to which gold-bearing deposits are
believed to be genetically or spatially associated, traverse the properties in an almost N-S direction: the Mitchell-Hearst fault and the one crossing the Fitzpatrick Bay in Larder Lake. An almost E-W fault has been assumed to pass underneath Estrangement Lake.
The Larder-Cadillac gold deposits found Lake village and Timiskaming Group, related subsidiary
Wide zones of "dolomitization" with fuchsite have been locally observed along these major faults.
Pyrite, pyrrhotite or graphite zones are frequent. Gold have often been reported associated with syenites, diorites or 'dolomitized' volcanic rocks.
PREVIOUS WORK
Prospecting sporadi cal ly blasting and geochemi cal ,
for gold and base metals has been intensively but pursued on both properties in the past. Stripping,trenching were later followed by modern geological, ground and airborne geophysical surveys carried out
by many companies whose respective works have already been summarized in reports by D. Comba, 1977, F. Balint, 1982 and M. Berube, 1984. Over 100 diamond drill holes totalling in excess of 50 OOO feet have been bored on both properties. Most of this work had been carried out outside the portion of the CFC property intensively worked by FL in 1985.
RECENT WORK
During 1985, Falconbridge Limited (FL) performed the quality and quantity of work on both properties:
foilowi ng
Type of work
Line cutting Magnetometer VLF EM survey I. P. survey Geochemi stry Geology
CFC
9.7 km 62.8 km 62.8 km 30.0 km 62.8 km 62.8 km
MMM
22.5 km 21.0 km 21.0 km 10.5 km 21.O km 21.O km
Total
32.8 km B3.8 km 83.8 km 40.5 km 83.8 km 83.8 km
Diamond drilling 6 holes (3420') 3 holes (2345') 9 holes (5765')
The work done in 1985 covers only the western half of the MMM property and the southern part of the north block on the CFC property. It was concentrated to the vicinity of the Mitchell- Hearst fault structure.
The line cutting has been contracted by Exploration Colinex Inc. of Rouyn, Que. Most lines have been cut in an E-W direction, with pickets at lOO-foot intervals along lines 2OO feet apart. Much time has been spent in the field looking for old base lines, old
pickets and claim posts in order to be able to overlay any plan •from previous works (once reduced at the scale of new plans,!" ^ 4OO') and in order to tie the sets of claim posts recently localized, with the new grid of lines. The new claim map integrates all new lines, all old base lines and most claim posts.
The geophysical surveys carried out by Geola Ltee of Val d'Or, Que. include measurements of both the total field and the vertical gradient of the earth magnetic field, at intervals of 50 feet and also the readings of a VLF electromagnetic survey measured on 2 frequencies, at intervals of 1OO feet. The computerized results have been presented as profiles and/or contours on maps accompanying the report by Geola. The author re—interpreted all VLF results on a new VLF compilation map to be found in pocket at the end of the present report.
The Induced Polarization (I.P.) survey had been carried out by Remy Belanger Enrg of Evain, Que., with Phoenix 1PV—l and 1PT—l instruments working in the frequency domain. Both the Frequency Effect (F.E.) and the Resistivity (Res.) were measured at spacings of 20O feet and for depths of N ^ l to 5. Remy Belanger provided a set of pseudo-sections showing all readings of Res. and F.E. altogether with the calculated metal factor. The author interpreted the data contained in the pseudo-sections by reporting anomalies as bars on his own plan, bars later joined by axes from line to line.
The geochemical survey was conducted by a crew of 2 technicians (Si Iles Carrier and Paul Nadeau) who walked along all the lines for mapping and sampling all outcrops of bedrock. Each sample was theorically composed of several pieces of rock aggregating about 5 pounds and broken within lOO-foot radius from the reported location on the geochemical map. The 332 geochemical samples collected that way were sent to Chimitec Ltee of Sainte-Foy, Que. , who prepared them by fire assay before sending them at Bequerel Laboratories of Mississauga to be assayed for gold in ppb by neutronic activation; Chimitec Ltee also had then assayed for C02 by a gravimetric method.
The geological survey has been executed by Donald Boucher of Kirkland Lake, Ont., who visit, mapped and sampled the outcrops previously outlined by the crew of technicians doing the geochemistry. In addition, the author also presents in pocket a geological map compiling data from recent and previous geological mapping, from diamond drill results, from a few visits on the property and from geophysical interpretation.
The diamond drilling campaign has been contracted by Domini k Drilling (1981) Ltd of Porcupine, Ont. All the core have been logged and geochemically sampled at Kirkland Lake before being transported to the Timmins core shack for storing. The logging has been done by M.Berube, Donald Boucher or J. Andre Carrier. Splitted core samples have been sent to Swastika Laboratories Limited and geochemical samples of core have been sent to
Ch i mi tec Ltee of Sainte— Foy for assaying. Each geochemical sample was composed of pieces of core l" to 2" long taken at intervals of 1.8 feet along a same geological unit (more samples were taken in units exceeding 100 feet). The diamond drill logs are inserted herewith as appendix A, the diamond drill geochemical results, as appendix B and the diamond drill sections for each hole , as apendix C.
DISCUSSION AND INTERPRETATION OF RESULTS
Geophysical surveys
Let's first describe the results for each type of geophysical surveys before comparing them with each other.
s*nd g.radigmetri.c results
Geola Ltee plotted the magnetic and the gradiometric results on 4 sets of maps (each set comprising 2 base maps provided by FL, one covering the northern part, the other, the southern part of the properties). Results of all other surveys carried out by FL are all shown on the same set of base maps.
The broadest magnetic features contoured on the magnetic map have a northwest-southeast direction and are refered below from the southwest to the northeast:
- a high mag O 1OOO g), caused by ultramafic rocks (see geology)- a low mag K 2OO g), 500-1OOO' wide, underlain by volcanic and
sedimentary rocks (could be the low side of polarised high mag)- a medium low mag (2OO-50O g), 15OO-2OOO' wide, underlain by
sediments- a medium high mag (600-1000 g), probably underlain by
intermediate volcanic rocks
These broader magnetic features are locally cross-cut by smaller linear anomalies marked Mag-1 to 12 on the general geophysical compilation map, and briefly described below:
Mag-1: bi-polarized mag., oriented N 2O E, sub-parallel to line 84 E in its north part: massive py, po, graphite at places.
Mag-2: low mag., oriented N 35 E, sub-parallel to the southern extension of the alteration zone (see geological map)
Mag-3: high mag. problably caused by ultramafic flows or syenite
Mag-4: high mag., E-W, possibly a gabbroic dyke stopping against the fault passing by theal teration zone (Mi tchel l -Hearst fault)
Mag-5: high mag. probably caused by a gabbroic intrusion because such an outcrop has been observed in its centre
Mag-6: high mag., concordant linear structure, unxplained
Mag-7: low mag., unexplained
Mag-8: high mag., explained by heavy pyrrhotite in hole 66O— 08
Mag-9: high mag., explained by pyrrhotite in hole 660-O9
Mag-10: high mag. , explained by pyrrhotite in hole 660- i Q
Mag-11: high mag., one outcrop of iron formation reported nearby
Mag-12: high mag., over a pit containing a 6-3O" wide copper- bearing quartz vein
There are other still smaller magnetic anomalies that might indicate mineralization, specially if confirmed by other surveys. Offsets along bigger anomalies may also be structurally important because possibly caused by cross-faults.
A gradiometric map on which the highest absolute readings have been contoured succeeded to pin— point most of the anomalies described above. This gradiometric map had not been included herewith but the more significant anomalies appear on the general geophysical compilation map in packet.
VLF electromagnetic results
Geola reported the VLF results on 4 other sets of maps. The more significative sets are the ones showing the In Phase components from the NSS station as profiles and contours. The set showing the In Phase components from the NAA station is not valid because the profiles have been drafted along E-W lines instead of theorical N-S lines on the profile presentation and because the filtering has also been done along E-W lines instead of theorical N-S lines on the contour presentation. For this reason, the author re-calculated all In Phase readings from NAA along theorical N-S lines, using the Fraser method.
Then the author integrated all In Phase data on a new set of map proceeding that way: first, only the positive values contained on on both NSS and NAA maps have been transfered on a new map; secondly, all values have been countoured by Geodes (with author's own method); finally, the contoured amplitudes have been interpreted as explained below.
The strongest anomalies have been labelled from VLF-1 to 1O on the VLF compilation map accompanying the present report, as a matter of reference only, before being classified as real or false anomalies.
Poarization Hi.Pj.1
On the pseudo-sections, the higher Frequency Effect (F. E.) are generally associated with the higher Resistivity (Res.) readings and they also largely coincide with area of outcrops, suggesting
8
that most anomalies are sub-surface or false anomalies. The F. E. peaks or axes are almost always closely associated with high Res., apparently marking the crests of hills.
Once transfered on an I.P. compilation map, most F. E. axes are effectively located over the area of outcrops. The have been labelled from A to F, these letters being followed by numbers when axes are segmented.
One rare I.P. anomaly whose F. E. is associated with a low Res. and do not seems to correspond to an outcroping area is anomaly F which has been explained by diamond drill hole 660-08. This hole cut a lot of sulphides with minor graphite.
Correlation between Mag.^ VLF and IJ..P... C.esul,ts
A general geophysical compilation map has been specially built to superpose the main VLF, I.P., Mag. and gradiometric axes, for comparaison and interpretation.
The new VLF compilation map outlines both sub-surface (false) and bedrock (real) conductors. The first rule of thumb used to differentiate between both types of anomalies consists to superpose the VLF compilation map over a well documented geological map (one outlying rocky hills and swamps or conductive overburden, for example). In the absence of real conductors (in bedrock), the highest amplitudes will coincide with vallies filled with conductive overburden whereas areas of rocky hills stay blanks. Then, a VLF anomaly located over a hilly area have a better chance to be a real one. The second rule of thumb to discreminate between false and real conductors inside as well as outside hilly areas consists to superpose the VLF compilation map over the I.P. compilation map. While most false VLF anomalies are located outside areas of outcrops, most false I.P. anomalies, on the contrary, are located inside areas of outcrops, then not coincident. When a VLF and an I.P. conductor coincide, then the conductor have a better chance to be caused by a real or bedrock conductor, by sulphides or graphite. See anomaly VLF-5 for i nstance.
When a VLF anomaly and/or an I.R. anomaly coincide with amagnetic anomaly, the reliability for a real conductor is stillbetter, as i t happens over anomalies VLF-5 and VLF-8
Unfortunately, on the claims surveyed during 1985, coincident anomalies are very few and, which is still worse, axes of different surveys are cross-cutting instead of being parallel to each other.
Geochemical survey
Two complementary geochemical surveys (with local overlapping) have been conducted over the property, the one previously conducted by CFC and the recent one, by FL. Samples were assayed
for precious, base metals and for oxides by CFC and samples -from surface and from diamond drill holes have been assayed for gold and C02 by FL.
The geochemical map in pocket shows the geochemical results obtained by FL in 1985 but also shows a few gold assay results obtained from a reconnaissance geochemical survey done by FL in 1984, when localised in 1985 by observation of flaggins left in 1984.
To make it short, very few assay results for gold are anomalous and most highly anomalous assay results for CQ2 have been obtained over the main alteration zone. The previous surveys by CFC yielded much more anonalous gold assays (the area covered was not necessarily the same as the one covered by FL) .
Geological survey
Let's sub-divide the geology into lithology, structure, alteration and mineralisation. The legend for the symbols used on the geological compilation map in pocket is inserted as appendix D.
pocket other three flows There
and all
The lithology appearing on the geological compilation in is not much different from the ones previously filed by companies like CFC, MMh, etc. It is mainly composed of units: sediments (mainly greywackes) , ultramafic (komatiites) and intermediate volcanic (tholeiites) rocks. is a big difference, though, between the governmental mapcompanies' maps: the rocks forming the hill over the Mitchell- Hearst fault, identified as syenite on the government's map are identified as altered volcanic and sedimentary rocks on companies' maps.
Structure
The main structures are locally identified by geological observation and magnetism: the NW-SE trending contact betwenn ultramafic and intermediate flows is well defined by the magnetism except to the SE, on the southern extension of the main alteration zone where the ultramafic flows become 'demagnetized' by alteration. Elsewhere, on the property, the magnetism, the I.R. and the VLF do not seem very effective tools to define the structures, maybe because of local intense alteration and complex folding and faulting.
Several faults however have been tentatively drawn on the geological compilation map.
The bedding and even top determinations have often been observed at many places over the sediments and the volcanic rocks.
Both sedimentary and volcanic rocks have been frequently
10
breccicated in situ and their hairline fractures have been filled by some black graphite, as observed on surface and in many drill holes, but these breccias are not always easily followed by geology or geophysic.
The more important type of alteration is the "dolomitization" of volcanic and sedimentary rocks, along the Mi tchel 1-Hearst fault. This alteration has hardened the rocks to the point of forming a hill, because more resistant to erosion. This hill is by far the strongest topographic feature on both properties.
Pyrite and pyrrhotite has been found at many places, often associated with graphite. For instance, heavy nodular pyrite has been encountered in the wide pit at coordinates 26 S-83 E and in hole 66O— 08 , hole which also contains some heavy pyrrhotite. All sulphide mineralizations have been assayed for gold and, except for weak values intersected in hole 66O-13, no significant amount of gold or base metals have been obtained from geochemistry, geology and diamond drilling in 1985.
Diamond Drill hole campaign
On CFC
The first five diamond drill holes on this option were drilled under I. P. anomalies located outside outcrop areas and the sixth one was drilled across the northern extension of the alteration zone exposed on the MMM option, farther south.
I. P. anomalies in the first 4 holes are well explained by a variable amount of graphite, pyrite and/or pyrrhotite, and do not carry any significant gold values. From the log, there is no good explanation for the I. P. anomaly in the fifth hole that the author has not seen yet. The sixth or last hole did cut the alteration zone but the alteration is reported weaker than in the third hole drilled on the MMM option to the south. This hole cut an anomalous gold zone averaging 190 ppb Au over 22 feet from 284.5 to 306.5 feet. A more detailed summary of the geology of each diamond drill hole follows:
The numbers of holes begin with 660-08 in 1985 because holes 660- 01 to 07 have been drilled in 1984.
Hole 660-08
016-542: interlayered argillites, greywackes and conglomerates (or breccia?)
This hole cut several sections containing light to heavy sulphides, nodular pyrite and/or disseminated pyrrothite and some slightly graphitic sections. Fuchsite was
11
observed from 166 to 186 feet in an alteration zone.
Hole 660-09
042-297: interbedded argillites and greywacke*, often brecciated in situ, the hairline fractures filled by graphite. Frequent py. and po.
297-606: intermediate volcanic rocks, partly brecciated, graphitic but barren of sulphides.
Hole 660-10
O20-506: mainly mafic volcanic flows, local tuffs and a dyke of gabbro. These rocks are brecciated in situ from 157 to 251 and from 339 to 463. The hairline fractures in the breccia are black, being filled by graphite. The first breccia contains traces to 17. pyrrhotite and pyrite and the second one, up to 57. py-po.
Hole 660-11
074-526: mostly intermediate volcanic rocks, locally described as dacite, andesite, basalt and tuffs. a 15' dyke of syenite is noted at 461'. Graphite has been identified at 92', 121', ISO- 132 ' and at 262'. Frequent traces of pyrite.
Hole 660-12
080-282: intermediate to mafic volcanics, chloritized;282-341: mafic valcanics, "341-511: intermediate to mafic volcanics, "511-516: gabbro—amphibolite
From the anomaly.
log, there is no explanation for the I.P.
Hole 660-13
061-225: mafic and ultramafic volcanics;225-379: altered J.dgl.gmiti.zedji. mafic volcanics?,
local fuchsite, traces of pyrite; 379-708: weakly altered ldgl.gmiti.zedl metasediments,
local graphite; 708-716: basic dyke.
65 core samples have been splitted in this last hole, the most anomalous ones being 5 consecutive samples splitted from 284.5 to 3O6.5: they averaged 190 ppb Au over 22.0 feet. The other best values are scattered and are 140, 100, 40, 30 and less.
12
On MMM
The 3 diamond drill holes 613-O1 to O3 have been drilled before having received the results of the geochemical survey. The first two holes were drilled across the southern extension of the Mitchell-Hearst fault and across the western extension of the Estrangement Lake fault, in an area covered by overburden where ultramafic rocks were not expected because of much lower magnetism. These "Z diamond drill holes encountered mainly talcose and "de-magnetized" ultramafic volcanics without any sign of the expected syenitic intrusions, 'dolomitized' alteration zone or gold-bearing quartz veins. The third hole has then been collared farther north so as to sample the carbonate zone, mid-way between the first two holes and a previous set of holes under the showing area. Here is a more detailed summary of the geology encountered:
Hole 613-O1
072-629: highly talcose ultramafic flows; 629-794: slightly carbonated intermediate flows.
Both intermediate and ultramafic flows are cut by \2.7. of diorite dykes (6 of them). The shearing from 575 to 752 might have been developed by the Mitchell-Hearst fault.
No significant gold assay results were obtained.
Hole 613-02
023-726: talcose ultramafic flows all along.
No significant gold assay results were obtained.
Hole 613-03
006-368: intermediate to mafic volcanic rocks;368-382: amphibolite or mafic tuffs;382-576: ^iteration zone, bleached sediments, some
fuchsite;576-637: arkosic arenites637-747: alteration zone, similar to above;747-825: mafic to ultramafic volcanic rocks.
The highest assay results from 114 core samples were: 6OO 110, 90 and 70 ppb Au.
CONCLUSION
The magnetic map helps to better define larger geological structures (contacts, faults) and to pin-point concentrations of magnetic mineralization. Anomalies labelled Mag-1 to 12 on the general geophysical compilation map are described in the present report. The gradiometric anomalies have also been countoured on the same general map.
13
The VLF compilation map (the one combining both the NAA and MSS results, with the author's method) clearly differentiates areas of positive In Phase amplitudes (generally underlain by conductive overburden) from the one of negative In Phase amplitude (generally underlain by rocky hills). The 1O sharpest anomalies are labelled VLF-1 to 1O on the map. Very few of them are real bedrock conductors.
The I.R. compilation map contains numerous F.E. axes labelled A to H (each followed by nmbers when segmented), most of them taught to be caused by sub-surface effects, some by graphite or sulphides.
A general geophysical compilation map have been drawn to better show the associations between magnetic, gradiometric,, VLF and I.R. anomalies.
The geochemical maps failed to show any geochemically anomalous gold zones but clearly picked up the main carbonated alteration zone. Moreover, these maps were sometimes useful l for VLF interpretation when outlining areas of rocky hills from those of conductive overburden.
The geological compilation map differs from the government map 1947-1 which shows a wide 'syenitic' dyke instead of carbonated volcanic and sedimentary rocks along the Mitchell-Hearst fault. It does not differ much from the different companies'maps but permits to compile all old geological data and to compare then with the recent mapping.
None of the 9 recent diamond drill holes intersected significant gold intersections although they succeeded to explaine the geophysical anomalies or to cross-cut the structures looked for.
RECOMMENDATIONS
Only 72 of the 132 claims have been explored during 1984 and 1985. Some of these, the remmant of claims plus some adjacent properties deserve an aggressive exploration program for 1986.
Many geophysical anomalies are left unexplained in the area explored during 1985, particularly in the northwestern portion where some mineralization is present in a few pits and where the geology is structurally disturbed. Some VLF anomalies for instance should be detailed by I.P.along short N-S or E-W lines. Then, a few of them could be explained by stripping or by diamond drilling, depending on overburden conditions.
The northwestmost portion of the CFC option has not been explored yet by FL. Interesting mineralization and alteration has been reported from there, namely the base metal showing on claim MR 25 and many carbonate zones elsewhere. Geochemical anomalies of gold and CO2 deserve a second look with I.R. before stripping or dri 11 i ng.
14
The Hemlar property located southwest o-f the MMM option and the portion o-f Larder Lake covering the Mi tchel l-Hearst -fault extension, as -for north as the Raven River and Laguerre gold deposits also constitute good prospecting ground.
f YLJL-...l Maz\o\!s BtiUbe l
December 30, 1985 Magloire Berube, P. Eng.
REFERENCES
Balint, Frank: 1980 Drill Program, Larder Lake Project Areas, PN 630 to 637 inclusive, McElroy-Hearst townships, Ontario, NTS 32-D-4, Corporation Falconbridge Copper, December 10, 1980
Balint, Frank: Larder Lake project 1981 Summary Report, PN 030, 032, 033, 034, 035, 036, McElroy and Hearst Townships, for Corporation Falconbridge Copper, April 1982.
Berube, Magloire: Report on a Diamond Drill Campaign by Falconbridge Limited on Project PN-66O or Property o-f Corporation Falconbridge Copper in Hearst township, Ontario. December IB, 1984.
Comba, Dave: Davey Lowe's Gold Claims Property Examination, memorandum to Dave Watkins, Corporation Falconbridge Copper (appendix Xlll in Balint's report), September 28, 1977.
Seguin, M. K. and Berube, fi.: Geophysical Report on IP, MAG and VLF surveys on 3 blocks of claims of Corporation Falconbridge Copper, Hearst Township, Ontario. December 18, 1984.
16
CERTIFICATE
I, the undersigned, Magloire Berube, residing at 1077 avenue Louis Jobin, Sainte-Foy, Province of Quebec, certify as follow:
1- I received a B. Se. A. degree in Geology from Laval University in 1958 and I practice the profession of Geological Engineer since then;
2- I am a member of the Corporation des Ingenieurs du Quebec, of the Canadian Institute of Mining and Metallurgy, of the Prospectors and Developers Association and of the Quebec Prospectors Association;
3- I do not hold, nor I expect to receive an interest of any kind in the claims held by Falconbridge Limited, in Hearst and McElroy townships, Ontario, nor in any other properties of Falconbridge Limited;
4- The present REPORT OF WORK PERFORMED IN 1985 by FALCONBRIDGE LIMITED on the properties of CORPORATION FALCONBRIDGE COPPER and of MANY METALS MINES LIMITED, Hearst township, Ontario, dated December 1985, is based on 27 years of experience in exploration, development and mining in Northwestern Quebec and Northeastern Ontario, and on a good knowledge of all previous and recent work done on the properties of Falconbridge Limited in Hearst and McElroy towmships, Ont.
Sainte-Foy, December 30, 1985 Magloire Berube, P. Eng.
17
~o -6 o
H y
Dril
led
by:
D O
Sta
rted.
Z
Ende
d. 1
Z/ IO
/8S
f /C
"
Falc
onbr
idge
Ltd
.H
OLE
NO
:P
AG
E:
Pro
perty
:
Tow
nshi
p:
Logg
ed b
y:
O.
So
ucH
SR
FX)(
.eof
*B*'D
fifLa
titud
e:
Azi
mut
h:
Ele
vatio
n:
'/l/Lo
ngitu
de:
Dip
: -S
O'
Leng
th: 5
'^2
fe
et
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
FRO
MTO
LEN
GT
H
K,
1C,
72
-
li.
foiO
.6
C- H
EK
T
r? *-~d
~ od
- 18
2.O
.C f
o!7
.i ^
QjM
r*^-
i\
2. 7
. i f
0 i 8
- 8
C
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
: O
PAG
E:
Dril
led
by:
Star
ted:
Ende
d:
Pro
perty
:
Tow
nshi
p:
Logg
ed b
y:
Latit
ude:
Azi
mut
h:
Ele
vatio
n:
Long
itude
:
Dip
:
Leng
th:
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
FRO
MTO
72-
zoo
Hi.-
z.i-t
7i.
f S
/^rs
re/O
c~J
CO
AJ6
JLcJ
flg
A.'*
TeS
j A
AE
W (
TCS
77^
ie,
87.7
A
RB
to\T
t m
&J
r. j.
Man
ne u
tt
l )
l l
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
: O
B
PAG
E:
FRO
MTO
DE
SC
RIP
TIO
NA
u
Q*o
*f*}
~
CD
SA
MP
LE N
O
FRO
M
TO
LE
NG
TH
.
, K
er""-
l H
pp
b
______
V*
Coo
l 6,
601
/CH
I
r
3tf
4-0
3*7
30
0.0
49
O.S
4-0
O.4
0O
0.7
60
T.J
. U
DO
Kf
IT i
C
o2
00Ooz utd
oz
oDC
O
0) O)
.0
o ^o(O
l
Falc
onbr
idge
Ltd
.H
OLE
NO
: O
SPA
GE:
l l
l l
l l
1111
Falc
onbr
idge
Ltd
.H
OLE
NO
: Q
8
PAG
E:v//
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
FRO
MLE
NG
THA
u
6 37?
37?^
o ^#
2. I
M TE
A ae
oo e
o
3 f
8•S
--730
o.ve
l l
l l
) l
Falc
onbr
idge
Ltd
.H
OLE
NO
:PA
GE:
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
TH
3*77
l l
Falc
onbr
idge
Ltd
.HO
LE N
O:
O Q
PA
GE:
//X
//
FRO
M
TOD
ES
CR
IPTI
ON
SA
MP
LE N
O
FRO
M
TO
LEN
GTH
NO
TE:
Z,
/?c;
o D
/P
TEST
S
^-•
^ c
rvT
-^ar
iX
J
T.
J.
M0
04
C t
Dril
led
by:
PO
I*I
l *l
K
Sta
rted:
Z
.1//
0/
8 S
"
Ende
d:
Z*//O
/65
Falc
onbr
idge
Ltd
.H
OLE
NO
:P
AG
E-l/t
Pro
perty
: (g
^O
)c.o
(?P
o*i*
T7o
w
Tow
nshi
p: H
EA
RS
T
Logg
ed b
y:
O.
Sou
cwe/
^
Latit
ude:
Azi
mut
h:
Ele
vatio
n:
POST
40
+00
ELo
ngitu
de:
Dip
: - tS
0
Leng
th:
C O
G f
eet
l l
l l
l l
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
: O
*J
PA
GE
.
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.TO
LEN
GTH
K a.
peat
CO
*
22. S
7
187+
0 2.O
O.C
AR
GIL
UT
E
tv*-
C^ ^f^
^M
^jl ^
j-n/n
CM
^ L
eJjL
j,
2.J7
. 7P
.
2.37
.7 /-
o 2
Vo
9"
602.
2-
602.
J
zzft
*
6oi
- 7
1.3
^•7
-
•y
z.7
70
ML
70
A^S
-
A//
0.J
O0
0.79
6
J,61
l l
Falc
onbr
idge
Ltd
.H
OLE
NO:
O
?
PAG
E:
FRO
MD
ES
CR
IPTI
ON
SA
MP
LE N
O.
FRO
MTO
LEN
GT
HA
uji
/y*.
/A)
S/T
U
Z*?
/
2?7.
3X
AJ
S/T
O
BR
EC
CIA
f V/
JL^O
.
4^-
*-Z
i
*U-c
rvoL
5"
b2.^
.5-
2.9
3,
2.9
7-7
Z.
1.2.
2.3
7
l l
) l
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
: O
7
PAG
E:
FRO
M
TOD
ES
CR
IPTI
ON
SA
MP
LE N
O.
FRO
M
TO
LEN
GTH
/AJS
/TU
B
ftE
CC
lA
Oti
-3
7.'
Falc
onbr
idge
Ltd
.L
10-3
4 VO
i L
HO
LE N
O:
PAGE
:
TlM
C
50+
00*
po
i 1
H If i u
t
Dril
led
by:
DO
/"1'*
"*
Pro
perty
: (g
gC
ycoR
Pofif
ino/v
F /*
tt0/
* 3*
15*5
6 eo
pPft/
e La
titud
e:
Long
itude
:
Sta
rted:
'Z
-5//
O/8
5
Tow
nshi
p:
W f /4
AS
T
Azi
mut
h: /S
/^S
0^
Dip
: -^5
^
Ende
d:
Z&
/ /0
/ 8
5
Logg
ed b
y:
O.
Bo
ucn
en
. E
leva
tion:
Le
ngth
: i"
O6
fee
t
FRO
M
0
2.0
VS
.i
TO
20'
**3
5-,
DE
SC
RIP
TIO
N
O^e
rtB
Ort
DfM
*:rt
gr\
O tc
H :
C/Q
/
f^fiF
tC-
V/O
^C
/^A
J'C
, O
/^JL
V
o^-A
A^r
. ^t-
-rxfi.
^x-#
-*^*
'-*t
fc/
a-r
w^
/^X
Y
f jL
#*A
) Q
jV-4
-^-^
LX
^ ~
fa~
4T
*1*
-3-
J-
-TO
3
D
Q~
~^J
^a
f*
JtS
-4-f
-*-i\f
ir
njL
A-J
Lv*^
^ V
^+
o H
i.l
l^A
F/C
T
(J
P P
ciS
^Ji.
at^
ji^i
rrvd ps^-^
^-J
jtAjL
^n
lut^
/LJ-
^J
*7~
2- G
SA
MP
LE N
OFR
OM
TOLE
NG
TH
l )
Falc
onbr
idge
Ltd
.H
OLE
NO
: f
PA
GE
:
FRO
MD
ES
CR
IPTI
ON
SA
MP
LE N
O.
l FR
OM
|
TO
| LE
NG
TH
86. S
"
i^s-y
^u^
-cfcX
80
A-f/f
fT
-
60
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
: /
O
PAG
E:
FRO
MT
OD
ES
CR
IPT
ION
SA
MP
LE N
O.
FRO
M
TO
LEN
GT
H
III
157
/AJ
S/r
u
At
ivo
' - (f
"
it
At
HI'
r. J
. M
00H
C L
l l
]]])
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
: l
O
PAG
E: t
^/C
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
. FR
OM
TO
LE
NG
TH
2,/
Z
'Ll'i
.s
;TU
i p?
h m
.2.
AJ 'l l'f- t'\
1-ld+
o 2
Z 9
. 5"
l l
l l
Falc
onbr
idge
Ltd
.HO
LE N
O:
l Q
PA
GE:
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
. FR
OM
TOLE
NG
THIf
S3,*
?V
OLC
AN
IC-
A;
S/T
U
^U
o-4.
2.*?
2.!T
to 2
-
-^
-^-*
——
y99.
T
3.7C
VN
IL
l l
l l
Falc
onbr
idge
Ltd
.HO
LE N
O:
[ O
PA
GE:
G/C
FRO
MD
ES
CR
IPTI
ON
SA
MP
LE N
O.
FRO
M
TO
LEN
GTH
Au
, r
VO
^C4A
y,c
/W 4
^,,
/i —
i
OF
NO
TE:
SIL
/loo
zoo'
w
oo'
reo
l l
Falc
onbr
idge
Ltd
.L
yqiz
-76.
J.t
-'O
HO
LEN
O:
&&
O-II
P
AG
E'A
Dril
led
by:
Q O
M//O
l /
C
Sta
rted:
Z
.0/ JO
/05
Ende
d:
2 9
/ Jo
/ 6
5
Tow
nshi
p: H
EA
RS
T
Logg
ed b
y:
p.
Qo
UC
Heff
.
Latit
ude:
Azi
mut
h:
fJ
Elev
atio
n:
PO
ST
6
V*o
oE
Lo
ngitu
de:
Dip
: -V
5"
0
Leng
th:
5"2
-6
-fe-
efr
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
TH
O 7 H
7V
O V
S f
i &
U r
t P
C
z., r f o
y '^
"
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
: 11
PA
GE:
2. f
C,
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
. FR
OM
T
O
LEN
GT
H
.C
OZ
y,
2-57
I2.1
.L f
0 I3Z
t6 f
+0 t
&L
/A
J s
/ru
(3
rt te
c 1
/4
A**
A.
-2.^8
MIL
HIL
S. 6
6
0.66
l l
l l
l )
ll
l)
l
Falc
onbr
idge
Ltd
.H
OLE
NO
: O
8
PAG
E:
11
)1
)
Falc
onbr
idge
Ltd
.H
OLE
NO
: 0
8
PAG
E:
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
TH
2/6
fa
2.3
^ C
O
2 "ST
/JO
i/avy
JU
^-t.
4-
Aft.
ciij.
ire
JU
f jL
fl
7 "
f P
6
Py
V
JIA
M
P'fy
i-
2.6
3.6
26
6 /
o 2
ff 3
2 7?
,
253
to 0J"
7. f
o-nc
j^t,
f j —
— ,
2^8.
1.2.
50.7
2- "
MIL
NIL
25 'C,
Ztl
-rA
/IL
0.4
T?
3.2
1
r. j.
Moo
^r t
rie
l l
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
: O
S
PA
GE
: gt/
f)
FRO
MD
ES
CR
IPTI
ON
SA
MP
LE N
O.
FRO
MTO
LEN
GTH
Au
T. t
. M
OO
ftl
IF* l
2*^*
02.7
3 A
RZI
LLIT
E
fuU
***4
,
•^
C
^u
LiiL
^,
30
8 f
a
'o j P
y
J
2 -
MIL
60
7Jo
g. Z
3 //.r
MIL
(,6'
7
Got
8
Afl
L
A/It-
3V/.
i 3 V
(f. ^
z. r z. o
O.&
00
0.5
77
0.55
6
111)1)1
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
: t f
PA
GE
:
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
. FR
OM
TO
LE
NG
TH
s TV
PF
J~ H
O
T.J
. M
OO
'C i
rrff
l l
l l
l
Falc
onbr
idge
Ltd
.H
OLE
NO
: J
/ PA
GE:
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
THA
-
2."?
?3
10
3/0
i O
"
y .
.^-^
tyxC
T-
OJU
L&
, "
f t
J. ——
Aff
Ll.z
o
) l
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
: li
PAG
E:
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
. l
FRO
M
| TO
l
LEN
GTH
5~o*
/
57?
5-2-
4
TU
PP
/rut
j
luJL
&J
H O
"t a
f
/jc/o
' -3
7*
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
:i/
PA
GE:
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
TH
^L4
JA*
J-i^
k**
^b,
V
Falc
onbr
idge
Ltd
.H
OLE
NO
:PA
GE:
/ o
f J
Drill
ed b
y: D
OM
IMiK
W
ILU
/ve
. (/
90l)
'"
C.
Prop
erty
: H
fAti
ST
Star
ted:
8
S /f
04-
Tow
nshi
p: o
f
Ende
d:
BS
ft
0
5
Logg
ed b
y:
J
(P#
-66
0)
Ca
rrie
r
Latit
ude:
2
7+
O0
S
Azim
uth:
/3
5"*
Elev
atio
n:
——
——
Long
itude
: 6
0+
00
f
Dip:
- 4
S'(
co
llaA
,
Leng
th:
5V 6
-fe
et
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
TH
Au
R&
feat
O O
Bo
~3 eo
eo
eo 5V6
00
2^2,5
-
-c**
.~*.
0VF
R B
il R
OE
*
/Kl
61 6
7
61 6
6
/•H 6
1 70
rt
61
71
S* 6
1 7i
73
157.
0
I7Z
.5
ZIZ.
O
Z6Z
.O
Z(,
7.O
139.0
I76
..0
Zld
.O
274-
(?
279.
^7
Z69-0
Z7+
.0
Z73.0
Z62.S
z.o
3. S
S. O
2.0
5.0
5.0
3.5
V/i
.
VIL
JVIL
fi
/IL
M
IL
AflL
.A
flL
Falc
onbr
idge
Ltd
.H
OLE
NO
: G
6o
-/Z
PA
GE:
2 - f 3
SA
MP
LE N
O.
FRO
M
TO
LEN
GTH
.-t*
.*./
**
PORP
HYRI
TIC
VOLC
ANIC
Ke
ck
——U
t-M
t^X
i
To
-"
tAF
lC
VO
LC
A#IC
.
*t**J^~
J. /rf.
T.
J.
MB
BA
f L
T/
l )
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
:PA
GE:
3* f 3
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
THA
u
*-yT**
l (343),
5V/
b^
JL
r*r*
-~7
*~l..**l f
*"P
* t*
vtltjr
-A.
/j *
r~
*
-^^ ,
..^^
...f
/^ .
/--i-.
-•—u,
~ft
*e*
. T
-jt+
J:
5I&
E/V
&
OF
H
-OL
f.
y .x/
2 y
l l
Dril
led
by:
Star
ted:
8
5
II
O7
Ende
d:
BS
/t
O
?
Falc
onbr
idge
Ltd
.H
OLE
NO
: k6O
~l3
P
AG
E l
of
5
z iP
rope
rty:
Tow
nshi
p: *f
Logg
ed b
y:
J.A
nJre
C
arr
ier
,
-c-
To"
TLa
titud
e:
S Z
+O
O S
Azi
mut
h:
2.7
0'
Ele
vatio
n:
——
Long
itude
:
Dip
: -4
S*'
(.c
of/
ar)
,
Leng
th:
7/6
O 0 61 61 IZ2
TO
62 716
61 JZZ
A 4
DE
SC
RIP
TIO
N
2.8
O V
&A
Au
# D
f A
/
^p
L*t
..i"
/- -
7*-
*^f
jt*h32*~
*A
u^** x
9
^4*c*~
-, M
'J^J.^i'
•~*
**
.-'*
"~
9'
.'i
f '-
t-
^Z
i..
To
U
irR
A&
AF
ICA
oC
KS
MijA
tJL
l-^
'/f
-j~
-*3}
-'*~
tf3M
, ^
ti4^
^
SA
MP
LE N
O.
/M 6
164
6/6
1
FRO
M
I4-S
.0
/4-e
.O
TO
H/-
0
/+8
.0
LEN
GT
H
5.0 3.0
Au
0/L #IL *tL
2.
0
Rep
eat
ML
Falc
onbr
idge
Ltd
.H
OLE
NO
: &
6O
- X 3
PA
GE:
2 o
f 5
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
THA
ut*
-22
5
y /4
Z-M
5.
vote
**//c
AO
CKS
379
4~^M
——
^U
^tt
. 3
Z-
(sm
u*L
Aj~
^im
iJ~
Jtt
-*
* *-
-a-
-**
^3
t-J,
-^LU
.
61 61
S6/.
0
ZO
Z.O
s: o
5.0
3.0
S. O
ZZ
O.O
ZZS.
O
ZZ
5.0
2
50.0
Z30.0
Z S
9. S
Z
6+
-5
17
+.0
Z64-
.S
Z 6 9
. aZ
7+
4
Z7
9.S
4--5
A
S"
5-.^
4-
. S
S. O f. 5
ML
ML
M
L
ML
Mi.
ML
M
L M
L 3
0
Falc
onbr
idge
Ltd
.H
OLE
NO
: 66(?
-X3
PAG
E. 3 o
f 5
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
THA
um
Rep
eat
/*\
.5
260.5
Z
93.5
Z
96.O
201.
0 Z
63.0
Z6
4-5
zee.5
Z 93
. S
Z98
.0
30
/.0
306.5
3 a
3,^
2/2
" v
r .
'
3/6-
0 32
/.0
3Z6.
5 33
0.0
334-
0 33
9.0
3/6.
0 3Z
/.0
3Z6.
5
334-
0 33
9.0
3424
/* 6
Zn
/H s* 6
ZZ
{
349.
0 35
0.5
3 53
.S
350-
5 35
-3.5
WF
AK
L y
Ztx
vf
^ —
—t^l±~
^(
——
—^.
46^U
e**-
^o-
^-~
.—^
*jjt
Z^
d**^
c^-~
2*,
-**.
e.^
-fc
f'
i .
. .
— l
i j
Jt s
42
2-5
-
/H
373.0
379.
0
3 91-
5
4Z/.0
453.
04
57
.5
363.
0
379-
0
3B4-
0
394-
0
426.
o
457.
5 46
1-0
Z.0
/•
S4-
05-
0 4.
S 3.
0 5.
5 4-
5 5.
0 5.
0 5.5
3.
5 4^
5-0
3x7
4-o
/-5
3.0
4-S
5-0
6.0
5-0
2.5
5.0
4.5
3.5
/0
ZO
ZO
-ze
o z/
o
Z0
/0 S0
S4-0
Z0
ML
ML
ML
30
/0 ML
ML
4*
/0
ML
ML
/O
410
110
fit
30
Falc
onbr
idge
Ltd
.H
OLE
NO
: &
60
-J3
PA
GE
: 4
'f
T.
J.
UO
OJ
ir
) l
l )
Falc
onbr
idge
Ltd
.H
OLE
NO
: G
60
-/3
PA
GE:
S *f 5
FRO
MT
OD
ES
CR
IPTI
ON
SA
MP
LE N
OFR
OM
TOLE
NG
TH
Au
7/6
T, t.
M
00
4C
LI/C
OF
-4-3
' f+
00),
-3
6'
(600).
/X
l l
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
:P
AG
E:
; O
f 1
Dril
led
by:
DO
AII
i K
Sta
rted:
O
C.T
. "i
^ ,
l^ 9
^
Ende
d:
OC
.T.
t. f
c,
t "i
3-5
Pro
perty
: w
W /"
^u
S
M.A
.S
Tow
nshi
p: rtf "S
T,
OW
T.
Logg
ed b
y: l
" fi
6L 01
w*
B6R
.ee.
Latit
ude:
Z.
-
Azi
mut
h:
Ele
vatio
n:
Long
itude
: D
tp:-
f S"
Leng
th:
FRO
MT
OD
ES
CR
IPT
ION
UO
P.E
S
IZL6
SA
MP
LE N
O.
FRO
MTO
LEN
GT
H
77
.
TL
.O-
rr-C
s^l
^ *
!L4
i. /J
-
T.J
.MO
O.I
L'l
l
Ill)
l l
l )
l l
Falc
onbr
idge
Lt
d.TR
OU
NO.:
^3
-01
PA
GE:
2
J)-
V
DE
SC
RIP
TIO
NE
chan
tillo
n N
oD
ELo
ngue
urJfe
.
&Z9
.0
; (7
fa,
Z
.^1^
, 'lil
-
'J'-~r*
*rr
A ft-
l-^vi*
J
OP
**/*
f w
S
/
9 1
-D,0
(, (T
n
: D
/ oft,
'/L 9
*
tow
•i. s'
NIL.
2.16
) l
) l
ll
ll
l
Falc
onbr
idge
Lt
d.TR
OU
NO
-:
(i/3
-O/
PAG
E: 3
4
. Y
DED
ES
CR
IPTI
ON
Echa
ntill
on N
o |
DE
| A
|
Long
ueur
f, (,
o.o
LT
t-o
11 Z
.o
r.j.
i-n
a.r
nil
592,
^-4-
22, S
:Vt
f 7. f
-
r; M
01* lo"
Falc
onbr
idge
Ltd
.HO
LE N
O:
^ /
'J -
O
t PA
GE:
V
JV H
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
TH
75
2.0
Ft-
t*rt
J
750-
014
03.
i/* T
*
//s',
op-
D, p
resr
i ;
2.0-0
' i
4-2"
650'
- 36
-5"
Dril
led
by:
DO
^ l
H '
Star
ted:
Ende
d:
Falc
onbr
idge
Ltd
.tu
ft!*
L
.-H-?
k6fe
zH
OLE
NO
: G
/3-0
2.
PAG
E: //S
"
Prop
erty
: (t
l
Tow
nshi
p:
Logg
ed b
y: D
. B
OU
CH
ER
Latit
ude:
Az
imut
h:
Elev
atio
n:
Long
itude
:
Dip
i-H
-ff"
Leng
th:
726
FRO
M
27-5
-
Z3
DE
SC
RIP
TIO
N
kJLo
-eA
.
SA
MP
LE N
O.
l FR
OM
TO
l LE
NG
TH
Falc
onbr
idge
Ltd
.H
OLE
NO
: O
2-
PA
GE
:
Dril
led
by:
Sta
rted:
End
ed:
Pro
perty
:
Tow
nshi
p:
Logg
ed b
y:
Latit
ude:
Azi
mut
h:
Ele
vatio
n:
Long
itude
:
Dip
:
Leng
th:
FHO
MT
OD
ES
CR
IPT
ION
SA
MP
LE N
O.
FRO
M
TOLE
NG
TH
3V7
Z&
ULT
RA
r\A
?\C
- \J
O)-
.CA
fJ\C
-
l l
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
:PA
GE:
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
. FR
OM
TO
LE
NG
THR
epeat
fy-t
nm "
2-7
T /
o
2.9
2.
A- j-
i i/
f o
333
QJ^
JJ*,
AT
3-7
0 l"
'-'O
f f
*-*-
It
JLi
tt
5 •
•rN
ILi.e
e
33
3VI
L.
TZ
fOIS
O
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
:. 0
2-
PAG
E:
FRO
M
l TO
DE
SC
RIP
TIO
NS
AM
PLE
NO
. l
FRO
M
| TO
|
LEN
GTH
-rf^-
c-a.
-W-*-
A-*-j
f ^V
'V
'O '
*/*/
6
T. j. u
oai
c LT
/C
) l
l l
l l
Falc
onbr
idge
Ltd
.HO
LE N
O:
O 2
. PA
GE:
TOD
ES
CR
IPTI
ON
SA
MP
LE N
O.
FRO
MTO
LEN
GTH
X?/
S""
t***tt
EAJD
J
jLif
N OT
E :
of
-2.0
0 -H
O*
1400
-H
I0
7oo
-t
e'
CO
RR
EC
TS
O
fJo
F-U
Ltht
*XL
o*.
95
/O
Z9
End
ed:
85
S/
OS
Falc
onbr
idge
Ltd
.H
OLE
NO
:- #
3
PA
GE
:
L-H
Z'H
SO
Property "
™sr ™
"*A^
~frAi
Tow
nshj
p. ^
^
(P*-6t*)
Logg
ed b
y: j: 4
W re
Carrie
r, **
3.
. 7O
+PO
S
Ele
vatio
n:
Long
itude
:
Dip
: -4
-5--
(c
Leng
th:
02
5"
FRO
M
O o 12.
-3
TO
/2 12#2
5"^
4
DE
SC
RIP
TIO
N
TO
/*A
Fic
KOCK
S
SA
MP
LE N
O.
-At
6060
&O
&2.
56.0
6
/.O
63.0
64
.5
6S.S
17.0
83.0
TO
56.0
61.0
64
.5
6S-.S
67
.0
69.5
73
.5
177.
0 S 6
1.O
/ee.o
LEN
GT
H
f.5
5
.0
Z.O
I.
S
2.5
4.
0
6.0
i* p
pi
ML
/O
JO
2.0
VIL
ML
ftefe
a
V/L
l l
Falc
onbr
idge
Ltd
.H
OLE
NO
:
-/Z
fc^
-f J
S- 7
3. f.
**J
~
Falc
onbr
idge
Ltd
.H
OLE
NO
: 6
/3-^
3
PA
GE
: 3 o
f
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
TOLE
NG
THRe
peat
30
2S
76.5
JL
J3
f"^
f- 3
80
.
362.
0(P
t*J.
. if
^C
^^4^
...*'^
*C -*
fc*.
./Ajjy
-x36
7.0
392.
0 39
+.0
39
6.0
7-f
75"
76
6*77
7
390.
0
, 4
/6.S
- 4/
7.5"
,
, 5V
/- 5
V^
, 5
79
-^2
2.5
, 5-
5-0.
S,)
/H /*1 6
^? 7
9
/M 1
0#0
At
60 Q
l
+09.S
. a
45-
M 60
03XM
6-5
04
SI 6
0 05
M 6
0 86
4/9
.5
42A
5 42
4.x;
42
9.x,
434^
43
?. o
44
4-?
4
47
. -P
409.
541
3 J)
4/6
.54/9
.54Z
/.5
4Z+.
042
.9.0
433.
043
4-0
439.
044
4.5
447.
045
2.0
f.o
e. o
z,o
4-0
3.0
4-5
3.5-
2.5
5.5"
2.?
413.
046
3.0
466.
0
10
ID
/V/Z
.to
S
o
S 00
Z0
ZO
#U
Zo
ML
45
0
j 0
0
Falc
onbr
idge
Ltd
.H
OLE
NO
: 6
/3-^
3PA
GE:
4 O
f
FRO
MTO
DE
SC
RIP
TIO
NS
AM
PLE
NO
.FR
OM
LEN
GTH
~ f
f C
/A fa
—
576.
563
7
/H /H
. S
47
2.5
94-
4-72
.5
4-17
.54S
/.0
40
4. f
40
0.0
49
2.0
61
01
So
4.0
5-0
4.0
5V/.
^I5
V315
-^ /e
. s
5V/.
5
/3.5
S/ 8
.5
SZ
Z.S
52
.7.0
61tt
.7.0
S4/
.0/X
ffa
.oS
Z6.
0 S
t/.O
3.5
-
61\S~
66.o
56e.
oS7
Z.S
5-72
.5
f 76
. S
3.5
3,5
3.0
3.5
2.
S
5.0
5.0 z.a
4S
4.0
MIL
ML
/ViL
NIL
NIL
Afl
L
ML
V
IL
ML
ML
ML
ZO ML
M
L
/O
ZO
ML
T. J
. M
00
*( L
T/C
Falc
onbr
idge
Ltd
.H
OLE
NO
:-^
3
PAG
E: S
of
6
FRO
MT
OD
ES
CR
IPT
ION
SA
MP
LE N
O.
FRO
MTO
LEN
GT
Hin
ffb
Rep
evt
747.
5A t
. rf*
A ri
e*
x o* f /-
2?S
667-
67S
* 743-7
45).
xH At
6(2.
1
x*1
^/2
Z
xM
^/2
3
XM
^/2
*-
^ 6
1 Z
S
- 74
-6.
7o6-7
o?,
7/9
-726
f 7Z
7.5-
72.9
,
fi~
e. —
-j^*
~
747.
5
/*f
6/3
3
61 3
5
61 ^
6
6/
37
42
x**
6f
+G,
61 4
-7
5-7
6.5
r?*,
s
6/3.
06/
8.0
623.
0
632.
0 63
7.0
642.
0 64
7.0
6*2.
4
657.
066
2.0
667.
0
673.
? 67
8.0
683.
0 68
8.0
656.
S
700.
0 7o
?.0
7/o.
e
7/8.
5 72
.2.0
7Z
6.0
6/0.
0 62
3.0
(.2-6
.0
632.
0 63
7,0
642.
0 64
-7.0
657.
06,
62.0
667.
0
673.
5 67
80
603.
0 68
6.0
6*3.
0 69
6.5
700-
0
7/0.
0 7/
3.5
7/0.
5 72
2.0
726.
0 7 '2
9. 5
r.o
5.0
5.0
+U
T
5.0
5.0
5.0
5.0
5,0
5.0
4-.0
Z.5
4-.5
5.0
5.0
5.0
3.5
3.?
5.0
5.o
3.5
5.0
3.5
4.0
3.5
ML
30 50
3o 30
30
30 ^0
30 lo 30
30
30
30
30
30
V
lt.
A'/
L
Mt.
M
L
Falc
onbr
idge
Ltd
.H
OLE
NO
:P
AG
E: 6
of
Q
FRO
MT
O
ezs
DESC
RIPT
ION
f"*
O
F
#O
Lf
.
yf*
*'
-C,f
c*l'.M
, s&
fT *
i~,
2*4,^
+1*.
.
j l
*/
SC
* ~
,,.~
.4
.. //4/ -
J^W
- .
AW. *
*^t**
L, -~~
w*~-
y***
/', y^
w~
-~ -A
.-,-
Mi.
c.it
'i'"-
- -~
t*l.
tn2
t/!
a* f
ir'^
sZi*
, }
*L*J
~ rZ
fc'
Le.
-JL
*h.
^xrl
U*, (W
-C
^u^-
y,)
.ff
*.^ci*
jmj*.
^^
-*L3z*
~^~3ii*
~^...
- 44
'(Zeo
), -
38'(
40*
), -
34' (
600)
f -3
i-[8
oo}.
J
^vA
fr
(Cr-
t*-*
* , iC
y,,
#5- /
X 2
/
SAM
PLE
NO
.
A1 6
146
At ^
/49
A1
^/5V
3s*
61
SI
/M ^
/5"2
XH ^
/5"3
xvi
^/5"^
XH 6
1 55
x*l
^X 5
-6xn
^X
5-7
xn
^/
5"^
/*t^
/ 5-
^X
Mlf
/ ^^
xtf
^X
^/
xH 6
162.
S46I
63.
/H 6
1 64
A\6
I65
FRO
M
729,
573
4.?
738.
074
0.O
74
3.5
7*64
747.
575
Z.5
757.
S76
Z.3
765.
5 77
0.5
774.
077
6-5
7B/.5
766.
57 -s
y. 5B J
/.a
TO
734.
573
6.0
74-0
.O74
3.5
746.
074
7.5
752.
575
7.5
76Z.
O76
5. 5
770.
5 77
4.0
776.
518
/.576
6.5
-79/
.*)
797.
0
616.
0
LEN
GTH
Z.o
3.5
Z.O
3.5
2.5
/.S
S-.o
5.0
4.5 3.5
S.O 3.5
2.5
5.0
5.0
5.0
S. 5
5:0
Au
JH p
pb
Af/
L
60 AflL
Ar/
L
ML
WL.
AS/L
V/L
#11
/0
2.0
70
#IL
ML
ML
tf/L
0
/L MJL
fafe
it
eo 30
1.1
. U
OO
.ttT
fl
-o o M X
AU GBOCHQCSTW ('
Diamond Drill Hole not H~CCO-O8 Township t f4 E A R S T
Log Sunnary | Geochflmiatry Sample
Location (m)From To
/^ Z0.6-LO. 6 2.7-3Z7.3 . 38'.*/
"38.V If/'J-O : i9/^6 J/3X.0
~ /32.. 1 X 86. 2^y #6^2.35:41
-Z35".6J2.^./Z6^. J U0Z.0
^301,0 !3^/-^3*y7.r| 377.0*57/ !3*?7V?7 i ^/Z6^2.6 i ^/^s~
-^yc/5- j /-/7 /^7/ j H8&
- HBB j 6~fit5~b(* j 6"^/^
~ —— i ———i— i —- — i ——i— i ——ii
—i~— r*-i— i ——
—— i ————- — -i ———
Rock type
-- '"^~ •"••"••--.fj
- — -^
^;:. : .-.: : ' S
3
f " "" -""' -
tv :;;,' ' " " " '
- r
*
Sanole no.
o\02.o^ -\o-t los-o 6, ioT080?; ot 1\i~12/Y/5-
; 6/7/a
.~
Location (m)Rcon ; l*?:
.-' . -
, r'fi: ';- "--^ :-:i
i^~ - ^- '-' - VT- ^— . ^
; '-^ ~-'T
! 1;v^-:.f*;:tg^^ipv-'i
: 1 - i
-r : 1 j^r:--- i" - - !| \:U': ;j , ,^- J
-1: -!' J
1 1
11 11
111
—————
— ——— — r
.
: :. :^:.
1—— j —— —— i ———— i ———— i ———
Au (ppb);- ., r.L.: H-;
•: -.•/• ; ^ii:^::-c/:'^/.^•-^^!*-[ l^-^/^r i^ -/-H ;
- ; : -r : 5I. :
^h-^'Wf:! f'-- i: X : " ; V: .- 'v: /K, .'-. : T : T: ^7-n '
2. ^ :^ :f; i
z ^'\^1f
*l1 .12.2
j ; , . ;
j ,--
Reroarks
;i, - •-•- : -- ";i:
-M . - : .h; ^:: 5
;
•;
- -
AU GBOCHEKTgTRY
Dianood Drill Hole not \]~C(eO ~ O 7 Rwnshipt H E A A S T
Log Suonary
Location (m)From To*V2-
too)5~0
~ 2.00
too) 5-02.00ZZ8.7
i
~ ZV3 Z*?/Z 9 f Z f 7. 3
- Z*?7.3 S : rD fZ6~O Ho 0^00 HS~C)t*i 5~(D 5~# O :*5~PO ^ 5~O
~ 5~5~D 6 06
—
— ii
—— H —— : —ii- — i —-—\i
—ij'i : 'ii —— i ———— L
Rock typea
: . |
it
"1
l
'h ; - .:.:, : '-.•-•^•^ ; -;
i..... ..-- --
: ; - —
*
GeochemiBtxy Sanple
jpfpnDXQ no.
^0 (oZ03OHoZ~oCo~^08071 o1 11 2.13
. -:-V'
^. ..-., -:--,^.,
-^'
-j
:; v. : .--^- ;-. .^
*f" -- :^v:F" i ""
'
Location (m) iFrom To
: ; ;^'~- ; t
i.fe 1
! : "i ^"'""T"" i
v :: . " :^ :i:i
-. - - - --
; "i J
-.i ' - i^
•j--- : ja^fesi- - - -' ^ --T ' ?--:"^^ ; -
"- - : -: -~. ~ : - - ^^^ :
' , r :*S: :-
: :^
"- . : ;-^:vH y : v-#-;-St?a;
-: - -^-*-J ":-. : :4'-:^--
Au (ppb)
^r-y-^--
"—:2.--- -
t
21-c/ I-t"/'
-^y i^x
1ff
.
- --; ~" : : T .T ^.
:^— -^-Fv^ i:4:: :-- -. T-: . - -~ ~~-: 7- ".L-..-. j;,-i--.: -' - .-^- -~ -
~ - . - . ; - -. - :. -.; -' ;--'~-.: ---: : -.- -
,: friW^;-^ :- :i ;
-^ ' ;i: "" ; ' : ;
--4|ejiJ:;.;-l; ^L M^r
: .--±-
Remarks
-i-;i^ s :; 4 ;* ;"^ : : ' -
T-:—— : : .-?':^-
: - ^'
5^.^ l ^T^^tl:
-
AU CT30CHEMISTRY
Diaicod Qrill Hole not M - C CO ~ lO Tbunshipt HEARST\
Log Sumary
Location (m)From To
Z 0 GOC O 100f 00 \ IS7
"/6~7 \J9t-2-X 9 7-2- Z5~/
-2. 57 500T,OO 33*?
^33*? Vost^OO tjfc 3^63 *5~6 t.
r——
—
—
^^
' —
1
-~ -1
^~
^
.
Rock type
*
Samol^ no.
O/0 Z,0 3o Ho ro^07o bol1 o
-
Gflocheroi0trY SanclA•* "^
Location (m)From To
!i
iii
———————— .
i
--i i',:.
Au (ppb)
</
11
^11
^1<|
22l
.
,
Remarks
-
J-)ianond Drill Hole n
AU GEOCHEMISTRY
oi /y-^0-// Township: H Eft A S T
Log Suonary
L Location (m)From To
-7V 7 2.9z /ro
/5~O Z00^&o 2-V5~2.V5- 2. ^V
"2. 5~*-/ 3 0 0100 S 6^0
-^^0 H 0 O-too H (f f-^(,l ^76f 7 C, 5-77sn s~2-/
—
—
, —
- —
—
^ ii
.
Rock type
J NT. \J OL C-,x ^/^x/
TAACHyTE ?J NT. \JCLC.
niin
DIO HireItiT. VOJLO.
nAfic VOJLC.
Geochemistry Sanple
Sample no.
0 102.0 30 V0 5T0 60 7OS0?y oJ 1] 2.
Location (m)From To
\t
Au (ppb)
12
^7-:/
16115*
^ 1^1•*l
a
Remarks
-
1diamond Drill Hole n
fa GEOCHEMISTRY
DI &&O-I2. Townships of HfARST
Log Suimary
J- Location (ft,)From Tot — i ——
i
-~
—
^™"
—
—
^~~
~-
^ \-
\
Rock type Sample no.
660-IZ-ol-*z-03-04
-05-0(,-07-oe-0V
LL0-/Z-/0
fjf^jfihftpi itt-n
Location (ft)Eton To
8 o. a {/r0.0/?0.a \ 2*0.02.ZA0 \Z62.f(2.60.0 294*0)1*00.0 33te)262..S 34/.0Z4/.0 4/4.024/- 0 4/4-0414.0 SJ/,04-14.0 S"//-*^Me? 5/6.0
—— \ ——\\t
i
iii
f Sample
Au (ppb)
x f1
4 ;
1
,C ;
4 lt;
5z
4j
Remarks
t;**-*i*i**lm
h * 5 *l.o*l
^CFftt Cl^* Of9r y
lea d^*M* 1ftrtHqcrs only
/ess *Ao*e 1
-
AU QBOCHQD5TRY
Jianond Drill Hole not &G0-I3 Townships t* f H&Afisr
Log Suimary
- Location (ft,)From To
^
~
—
—
*"
—
-~
^
~~
—i
^- ii————— i ———————
Rock type
Geochemistxy Sannple
Sarrole no.
Z60-/3-0/-01
-03-04--05-06-07-OB-0?
6SO-/3 -10
-/f-/2-/3-/4-IS-/t-n-/e-i?
460 ~/ 3 -20-Zl
Location (flfrjFrom To
6/.* J S 22.0IZ-2.0 JZ/.0j 2.2.0 \Jff.0
IS/.0 \Z00.02.6O.O j Z25V4*
2 2 r.*? Izt+.O2.64.0 352.0
2.64.0 \ 352J2.1+.0 \BSZ.03S2..0 \379.a
Z9/.S j 3^ 3.^Z7V.O \4I7.04 f 7.0 \4-tt.046t.0 ^4-79,0479,0 \ SZ.5.0&2.S.O j 560. 05 'Qo.0 \6oe.0S'Bo.o \6ae.O600.0 \6S0*06Z0.0 J ?06. 5"&S0.0 \ 70 6. 5708.5 7I&.0
\\\
Au (ppb)
< \" \< 1
13
to
15
31Z
Z.
50
1; -i
</fc,i
f. j
Remarks
c*/*/**-*flS4t-TZ. **Sy
/tss above 1
^Mtrtz o*Xx
•fZtZtfte- K'aX
/tfSS 2 4kov*
qua ft t. f*i*l a*5*ye4
/ess d&otf* i
fttar-tz-cApbo- ttatf att/y
Je. f S abeve "i
q iS4 Hht —C-ai^bo- Hdte *xXy
/ffS-5 rf Aeffi ^
-
1Diamond Drill Hole n
AU GBOCHQCSTRY
ot 6/3 -O/ Townshipi - H&flRST f o NT
Log Sumary
J- Location (m)From To
1- 77 t8H
1
^"*
vev i SBOl5"OO JTSS
sss S7S^ J
6 6 o j 6 7 V^- 67V 7/fc
lit. -7ST
151
*~"
—
—
l
1
1
l
•7*JV
yVoTC t
1
1
1—
— 1'
^
Rock type
Ot-TH/t/H/l P/C t-AVffi
•f *
N ^
o */
•i "
•t w
P/0/^iT-E j/xif*) Pv
ULTRA/HA flf. L/itr/tS
"DlOAlTC i Vji/j Py*
/^ TP/tJi . p/. O IV S
D/^irt py*ftfT&Kfll- Ft-0*fi
SJItMEvt s/LjeiF. turf /Ut. f.
nrren.*. f L. •^•ontttT^,
i ArTGjt/rt , Pt,o ***j
j^anolB npr
6/3-0/- o/ot030*)
05
Ob
OT
ofi09
; on12;3/Y
S**,* /77^*f
Geochemistry SwipleJ V
Location (m)From To
-72.
/39
/39
Z.OC,
i^J ^ 1 75
*7S 35^
3SB V3t
*#3t v ayV*Y soo
5-00 5SS
SSS 57S
629 6feo
^^ 0 (f7tf
b7t 7/r
•7/2. -75*-
7St 77^
(5W.& - 3C^.y*/^*
l
1
——————
i
——————
——————
l
1
l
Au (ppb)
< \Z
< 13
< t
< l
3
* ll
< J
1
frleiW
..
r*** vi--r*t
Remarks
^/*AXC. yr^.^
-
1almond Drill Hole n
AU GEOCHEMISTRYi^ M^l^H^Mi^BMi^^HMH^M^^^^i^MM
ot W -6/3- O Z. Township* H 54 rtSr
Log Sunmary
L Location (m)From To
1 2-S-2*7,5"
3V100
2*?.r^^.o(00
i 5-0/5-0 ! 2(50
"~ 2-OO 1-7-5-
Z75- |7-?Z
^2L?2L ! 3 5-0
55-0 j ,y0/-Hot *-So7. 5"
V07.^ V^O^^^O \ T od
^oo 5-5-4t?56 600600(.S '0*—
(o ^072-6
— \- ———— j —————
^ i
i—— 1 ——ii
^
~-
~-—————— r
Rock type
U1TA/4 /^AF/^.GA&&ROUAT/^/4 A^AP/^
/x
f f
't
k'OrtfT/r
OATA/J/'l/f^jo' x'
b/o flareULT/IXJAIAF/C
/^/xx//xX/
Geochemistry Sanple
Sarole no.
O/02,fl 30 V0 ^0 Co ~ro BQ 7f 0H17-\ZiH1 5~
1 L
Location (m)From To
ii
Au (ppb)
</1
/5l
<l</
/
B
Remarks
-
Diamond Drill Hole IK
Log Sx
Location (ft.)From To
—
—
r—^
- —
—
. —
^~
—
—
—
K
5: 6/3 -03
jnnmary
Rock type
J GEOCHEMISTR
Sample no.
613-03-01-VL
-03-64
-05
-06
-07-oe-09
1 13- 03, -lo-n-11-J3-14-S5-'t-n-/6-J?
6/3-03-20-21-22
If
Township: of
Geochemistry
Location (f t JFrom To
12.0 5*0.550.5 6*5
62..S LS.069.5 130.0
J30.0 1/&02/64 2.&I.0241. 0 16+.0264^0 3/C.O3/0.0 366,0360.0 36Z.O36^.0 469.S38Z.O 469.936Z.4 46?,S~469.5 499.0495-0 576. 549?.o f?6. S499,0 S76.SS76.5 637.0&X7.0 706.0637.0 706.0706.0 747.5706.0 747. 5706.0 747.5747.5 82.5
\\
\\\
j
HfAA*r
f Sample
Au (ppb)
35"
1Z
<^
\z3
Z
1
4*. 1
* 1
' \
^HZ.
3*l
•t
i•L
Remarks
lett ^ 4cxz~ o*e*tt*i*tm vmftt
btfdyAj)
fjur-tz. vein (assayed)
qtfdftz. att/y
fveAt&e-rtcJi
Jets 2 Above.
qoar-t* o tt /y
fl*4s;*e-ricA
/e** ZdWe
9M0^Z only
/ess *J*t,c. l
QV&t^&i G*t 'Y
S*e2fsVtte-Av'c4
/ess, 2 a^fc
DDH 660-00+Q+OOS
1M-17 BRUNING A-105 MIX. 1-71
VV5 in-situ 4 ^ G p
FALCONBRIDGELTD.
OD//44+00 S
SCALE f ; j 2OO
DATE eSj/27TRACED r X. Carr/e*-IM-I7 aWJNING 40-105 MIX. 8-71
DO H &GO-IO
vnto S 4-Q+OOS
IM-17 BIWNINC 40-105 MIX. 8.71
iercing
x
//
X
x^
"V
FALCONBRIDGELTD.
DO G GO -II p,V
S&CTJ0A/ Z + +OOS
SCALE y r Xg s /X 29
D. BoucherTRACED
MM-17 MtUNItire 40-105 MIX.
MUM NO 40-105 MIX. 8-71
V7-V/3 o
SECTiw
BKUNING XO-lOi MIX. 8-71
l J*. IT MUNINO 4^1KS MIX, 8-71
D O H 6/3-^3 UM t o S^Tc ?-/^^ 72
IMW17 BRWNING 40OOS MIX. 8-71
GEO LA LTtEPHYSIQUE L O G l Q U E
EXPLORATION - SERVICES
GEOPHYSICAL SURVEYS
PROPERTY OWNED BY FALCONBRIDGE LIMITED
LARDER PROJECT HEARST TOWNSHIP
PROVINCE OF ONTARIO
OCTOBER 1985 CLERMONT LAVOIE, Ph.D.
1020, 3e AVENUE EST (ROUTE 117 SUD), C.P. 418, VAL D'OR (QUEBEC) J9P 4P4 T6I.: (819) 825-8212
- 2 -
GEOPHYSICAL WORK
During the period of August l to August 30, 1985, a V.L.F. electromagnetic survey ( station NAA and MSS) and a magnetic survey were done on the property.
A total of 49.9 miles of lines was sur veyed with the V.L.F. electromagnetic method using stations NAA and NSS. The readings were taken at 100 foot intervals. The instrument used was an IGS-2 from Scintrex.
A total field and vertical gradient magne tic survey ( 51.4 miles ) was also done at 50 foot intervals. This survey was done using a proton magne- meter IGS-2 from Scintrex having a sensitivity of 0.1 gamma. The usual diurnal ar.o datum corrections were made using an automatic base station recorder (MP-3) from Scintrex.
DISCUSSION ON THE METHODS
The V.L.F. electromagnetic method is normally used in non-conductive overburden areas to obtain information on the geological structure, reflec ted by conductive zones such as faults, shear zones and naturally, massive sulphides.
GEO LA LTEEPHYSIQUE L O G l Q U F
INTRODUCTION
A V.L.F. electromagnetic survey (stations NAA and NSS) along with a magnetic survey were carried out over a property owned by Falcon bridge Limited in Hearst township, province of Ontario. These surveys were an extension of the previous surveys done in November 1984. We are referring you to our report of November 1984.
The V.L.F. electromagnetic survey was done to locate conductive zones which may contain economic mineralization. The magnetic survey was done to help the interpretation of the V.L.F. ano malies and to define the general structure.
PROPERTY, LOCATION AND ACCESS
The property is located approximately 10 km South of Larder Lake, in Hearst township, province of Ontario and includes two groups of option's claims. A list of these groups of claims are given at the end of this report.
Access to the property is easy from Larder Lake by using highway # 624 which crosses the northern part of the property. Also some bush roads surround the property.
GEO LA LTEEPHYSIQUE L O G l Q U E
- 3 -
The conductive zones are picked up with varying amplitude readings depending on the following parameters: overburden conductivity, conductivity of the zone, depth, angle with the transmitter station and the geometry of the conductive zone.
Normally, a V.L.F. anomaly is not a diamond drill target on its own. It has to be tested with other geophysical methods, especially in an conductive overburden area.
During a survey, it is a good policy to use two (2). different stations perpendicular, to one another. This can allow the detection of more conduc tors. However, due to the electromagnetic fields line distorsion present at the edge of a conductor, a false short conductor may be obtained with another perpendi cular transmitter station.
Concentrations of minerals having magnetic susceptibility will give rise to variations in the earth's magnetic fields. Systematic observation of the earth's total magnetic field has allowed us to contour the data outlining magnetic patterns or anoma lies.
Minerals haying strong magnetic susceptibility are magnetite and pyrrhotite and are usually, but not necessarily, associated as primary or accessory minerals in massive sulphide deposits; thus, coincident magnetic and electromagnetic anomalies could be important, but are not necessarily required.
GEO LA LTEEPHYSIQUE L O G l Q U E
- 4 -
DESCRIPTION AND INTERPRETATION
The V.L.F. electromagnetic survey done on this property has allowed us to detect 58 new anomalies with the NSS station and 3 new anomalies with the NAA station with respect to our previous survey done in November 1984. We are referring you to our report of November 1984.
Each new anomaly is described in tabular form and is provided with the following parameters:
- location of the anomaly: line, station;
- intensity of the peak to peak, which reflects the validity of the anomaly or its signals with respect to the noise ratio since the noise is approximatelyl to 2ft;
- length of the anomaly;
- magnetic association.
(refer to tabular forms at the end of this report).
Among the 58 V.L.F. anomalies found with the NSS station, 23 of these were classified in second priority. Many of these anomalies were also detect with the NAA station, but were not renamed. With the NAA station, 3 anomalies were detected only with this station and they were classified in second priority.
GEO LA LTEEPHYSIQUE L O G l Q U E
- 5 -
Magnetic survey
The total field magnetic data was contoured at 0,200,500,750,1000,1500,2000 and 3000 gammas. The total field and vertical gradient magnetic data were also profiled.
Taking into account the small scale of the map and the small interval between the lines, we have used the exponential profile method in order to see the small anomalies. The strong anomalies were attenuated.
The magnetic contours reveal some North-Wes t and North-South magnetic trends. With the help of the geological information, these magnetic data should be interpreted to define the geological formations and the structure.
CONCLUSION AND RECOMMENDATIONS
The V.L.F. electromagnetic survey has allowed us to detect 58 new-anomalies. The second priority ano malies should be tested with an I.P. survey before recom mending to drill them. With the help of the geological information, the magnetic survey should be interpreted. Using all this information, Tt should then be easier to prepare a diamond drilling program.
GEO LA LTEEPHYSIQUE L O G l Q U E
Ano maly no.
S-ll
S-12
S- 13
S- 14
S-15
S- 16
S-17
S-18
S-19
S- 20
S-21
S-22
S-23
S-24
S-25
Line
44 S
54 S
48 S
52 S
48 S
48 S
52 S
32 S
30 S
24 S
42 S
54 S
54 S
24 S
30 S
DESCRIPTION OF V.L.F. ANOMALIES
STATION (S) : N S S
Station inter section
80+75 E
78+50 E
76+75 E
73+15 E
69+05 E
65+75 E
6 3+75 E
72+45 E
66+35 E
64+75 E
54+25 E
54+45 E
52+75 E
51+15 E
45+60 E
Ampli tude
23
18
22
8
54
27
11
12
13
21
14
^0
^6
MO
47
Length
( )
300
300
300
300
1400
1000
700
1000
400
1000
1300
600
400
1000
400
Magnetic association
-
-
Possible contact.
-
-
-
'
Possible contact.
-
-
-
200 *on L.48S
-
Possible contact.
Possible contact.
PROJECT: PN-660
TOWNSHIP: Hearst
Notes
Possible overburden. Better define on L. 44 S
Poor cross-over
Reversed ano. with NAA. Poor cross-over.
Poor cross-over
Well define. Also detects with IIAA.
Well define on L. 48 S. Also detects with NAA.
Poor cross-over. Also detects with NAA.
Weak. Possible Extension of Ano. No. 15
Vfeak
Weak. Possible Iforth-West fracture.
Poor cross-over
Wide cross-over. Possible overburden
Also detects with Naa. Poor cross-over.
Also detects with Naa. Well define.
Well define
Priority
3
4
3
4
2
2
4
3
4
3
4
2
4
2
2
Ano maly no.
S-26
S-27
S-28
S-29
S- 30
S-31
S-32
S-33
S- 34
S-35
S-36
S-37
S-38
S-39
S-40
Line
34 S
48 S
44 S
26 S
36 S
42 S
48 S
24 S
32 S
42 S
42 S
26 S
20 S
28 S
54 S
DESCRIPTION OF V.L.F. ANOMALIES
STATION (S) : N S S
Station inter section
41+10 E
42+30 E
29+80 E
34+60 E
25+30 E
23+80 E
19+65 E
20+80 E
17+20 E
13+70 E
10+50 E
15+00 E
16+00 E
10+80 E
1+05 E
Ampli tude
44
15
^0
69
56
^67
34
12
20
29
62
22
26
86
29
Length
( )
800
-
1400
800
3500
900
900
600
500
700
2400
400
400
2600
400
Magnetic association
-
300 * possible
-
Possible contact.
-
200 * possible on L. 38 S.
-
-
200 *" possible on L. 34 S
-
-
-
-
-
Possible contact.
PROJECT: PlJ-660
TOWNSHIP: n^^
Notes
Wide cross-over. Also detect with NAA. Possible overburden
Poor cross-over. Also detects with NAA. May be real.
Poor cross-over. Also detects sith NAA. Possible overburden
Better define on L. 26 S. Alsi detects in part with NAA.
Wide cross-over. Also detects in part with NAA. Possible ovprhurripn-Also detects with NAA. Poor cross-over
Also detects with NAA. Better define on L. 48 S.
Poor cross-over
Poor cross-over
Poor cross-over. Possible extension of Ano. 34. Possible overburden efff*-rh-Also detects in part with NAA. Possible overburden effect.
Weak. Possible extension of ano. 36.
Poor cross-over.
Poor cross-over. Follow a creek. Possible overburden effect.
Poor cross-over.
Priority
5 3
2
3
) 2
2
3
2
4
4
3
3
2
4
3
4
Ano maly no.
S- 41
S-42
S-43
S-44
S-45
S-46
S-47
S-48
S-49
S-50
S-51
S-52
S-53
S-54
S-55
Line
52 S
42 S
22 S
28 S
26 S
68 S
60 S
64 S
64 S
58 S
56 S
64 S
60 S
88 S
74 S
DESCRIPTION OF V.L.F. ANOMALIES
STATION (S) : jj s s
Station inter section
2+80 W
1+00 W
6+70 E
2+80 E
1+60 E
77+50 E
75+50 E
72+70 E
67+00 E
64+50 E
55+00 E
56+20 E
52+30 E
49+50 S
46+60 E
Ampli tude
P 40
^40
72
26
61
64
17
60
21
^0
101
24
>IQO
43
16
Length
( )
400
400
600
800
-
1900
1000
400
3800
700
1000
800
400
1000
-
Magnetic association
-
Possible contact.
-
-
50 i" possible,
-
-
lOO^possible on L. 64 S
Possible contact
-
-
Possible contact
-
-
-
PROJECT: PN-660
TOWNSHIP: Hearst
Notes
Poor cross-over. Limit of survey.
Poor cross-over. Limit of survey.Also detects in part with NAA. Better define on L. 20 and...22-5.,-..Poor cross-over. Also detects with NAA.
Well define. One line only.
Well define. Also detects with NAA.
Wide. May be overburden.
Poor cross-over. Also detect; with NAA.
Poor cross-over. May be overburden effect.
Poor cross-over. Also detects with NAA.
Better define on L. 56 S. Also detects with NAA.
Poor cross-over. Also detects with NAA.
Poor cross-over
Poor cross-over
Poor cross-over. Also detects with NAA.
Priority
4
4
2
3
2
2
3
}
3
3
3
3
3
3
3
3
Ano maly no.
S-56
S-57
S- 58
S- 59
S-60
S-61
S-62
S-63
S-64
S-65
S-66
S-67
S-68
S-69
Line
64 S
60 S
64 S
72 S
64 S
62 S
92 S
92 S
92 S
90 S
88. S
64 S
62 S
68 S
DESCRIPTION OF V.L.F. ANOMALIES
STATION (S) : N S S
Station inter section
43+80 E
39+70 E
36+20 E
41+90 E
30+40 E
25+30 E
39+40 E
37+80 E
34+50 E
26+50 E
23+70 E
23+40 E
17+50 E
16+70 E
Ampli tude
32
14
13
66
17
83
M5
40
35
11
36
21
26
62
Length
( )
500
700
300
2400
800
3000
700
400
600
500
800
400
800
1400
Magnetic association
-
-
-
-
3000 gammas on L. 62 S
Variable
-
> 500 V
Possible contact.
-
-
100 V possibl
-
-
PROJECT: PH- 660
TOWNSHIP: Hearst
Notes
Better define on L. 64 S.
Poor cross-over. Also detects with NAA.
Poor cross-over
Well define. Also detects with NAA.
Poor cross-over. Also detects with NAA.
Well define. Also detects with NAA.
Better define on L. 94 S.
Poor cross-over. Also detf with NAA.
Poor cross-over. Also dete with 1IAA. May be disturbs•}~iy f\jY~i 6 3
Poor cross-over. Creek
Poor cross -over. Also dete with 1IAA. Limit of survey
3 Poor cross-over.
Poor cross-over. Also dete with UAA.
Better define on L. 68 S. Also detects with WAA.
Ano maly no.
V-03
V-04
V-05
Line
46 S
26 S
88 S
DESCRIPTION OF V.L.F. ANOMALIES
STATION (S) : N A A
Station inter section
41+10 E
7+50 E
48+00 E
Ampli tude
^30
> 40
^5
Length
( )
7000
4200
1100
Magnetic association
-
-
-
PROJECT: PN- 660
TOWNSHIP: Hearst
Notes
Possible East-West fracture.
Possible East-West fracture.
Extension of Ano. S-61
Priority
2
2
2
———
LIST OF CLAIMS
C.F.C. OPTION PN-660
103640319452319453420721429935429936447513477514476446476447476601476664476665476666477384 to 477389.495049496276
MANY METAL OPTION PN-613
411210429150429934476661476662495017495018496570511621
The V.L.F. and the magnetic survey have covered in part each of these groups of options's claims.
GEO LA LTEEPHYSIQUE L O G l Q U E
GEO LA LT&EPHYSIQUE L O G l Q U E
EXPLORATION - SERVICES
STATEMENT FOR ASSESSMENT WORK
I, the undersigned, Clermont Lavoie, for Geola Limity, certify to the following.
During the period of August l to August 30, 1985, a V.L.F. electromagnetic survey ( 49.9 miles ) using the NAA and NSS stations was carried out over a property owned by Falconbridge Ltd. A magnetic survey ( 51.4 miles ) was also done on the property.
This property is located approximately 10 km South of Larder Lake, in Hearst township, pro vince of Onrario and includes two groups of option's claims, which claims are given at the end of this report.
V.L.F. Instrument:
Mag. Instrument:
Operator: (. 27 days)
IGS-2 from Scintrex Precision: 0.1 gamma.
IGS-2 from Scintrex Precision: 0.1 gamma. MP-3 ( base station) from Scintrex.
M. Jean Paul Cloutier R.R. # lD'Alembert P. Q. J9X 5A3
Respectueusement soumis,
ont Lavoie, Eft-.D.
1020, 3e AVENUE EST (ROUTE 117 SUD), C.P. 418, VAL D'OR (QUEBEC) J9P 4P4 T6I.: (819) 825-8212
GEO LA LTtEPHYSIQUE L O G l Q U E
EXPLORATION - SERVICES
CERTIFICATE
7. I, the undesigned, CdeAmont Lavoie, Aeiiding at 114B B&ioAd Avenue, Vat d'0/i, Quebec, g/iaduated wi-th a 8.Se.A. degiee -en Geology tf/iom Eco-t"e Po-e"y- technique -en J965. I have ob-tained a M.Se.A degree-en Geophyiici ^om Eco.de Potytichn^qae. -en 1965, and-teee-tved a Ph.P. -en Geopnt/A-ee* tfiom McG-oc^
.n 7972.
2. I am a member o^ -the OndeA o^ Engj.ne.zu o 6 Quebec, -the Canadian Ini-tcta^e o^ Mining and We^acXaAgt/,
Quebec Pio-ipecto-t-6 Ai^ociateon and -the Socxett/
3. I do no-t kotd, noA do I expect -to receive, an in-teAe4-t oft any kind in -theae ct^aim6 h&td by FALC0WBRIPGE LIMITED noA in any o-theA mining c/aimi t/iey may have.
4. The in-teApie-ta-tion and /lecommendationi deicAibed in thi-6 /tepo-^t oAe baied paA-tdy on a peA^onad and technical expedience in -thii diA-tvtx.ct o
Signed in (fat d'0A, -thii eight; [Sth] day ofa the month o fa Oc-tobeA, one thousand ni.ne /lundAed and eighty-^ive f 79*5 ).
esunont Lavoie, Ph.v.
1020, 3e AVENUE EST (ROUTE 117 SUD), C.P. 418, VAL D'OR (QUEBEC) 'J9P 4P4 T6I.: (819) 825-8212
![Patricia Hearst [Book]](https://static.fdocuments.us/doc/165x107/568bd85c1a28ab2034a31296/patricia-hearst-book.jpg)
