1. No category

ARIS
SUMMARY
SHEET
o
District
Geologist
ASSESSMENT
REPORT
ince
P
Pine
LOCATION
LAT
51
UTM
10
NTS
g2N14E
0
CLAIM
OPERATOR
AUTHOR
S
REPORT
YEAR
58
00
LONG
5759398
Weeds 1
l
stowell
S
DIVISION
Confidential
89
06
13
Caribee
Weods
pine
S
MINING
17528
PROPERTY
Off
George
125
12
00
348860
8
o
Serack
M L
1988
34 Pages
COMMODITIES
SEARCHED
FOR
Geld
GEOLOGICAL
SUMMARY
pyrrhetite bearing
aleng
Fifteen centimetre veins of
values of geld cut micredieritic
arsenepyrite
fracture
sub herizental
The
stems
s
veins
are
te dieritic
intrusives
and discentinueus
WORK
DONE
prespecting
PETR
2
PROS
300
Map
0
1
s
092N
s
ha
Scale
14sample
ROCK
FILE
sample
s
s
1
5000
ME
033
n
i
I
I
I
I
LOG NO
RD
Ol
ACTiON
IT
REPO
PROSPECTING
FilE NO
o
WDODS
PINE
NTS
CLAIMS
51 58 N
CARIBOO MINING DIVISION
Pine
1
record
4
Woods 1
8
expiring
on
7832
no
record
no
8573
August
14
1988
7858
7857
8574
7859
7
8576
857
125
92N
12 W
expiring
8577
14E
on
8578
28
July
8579
1989
8580
fILMED
8
J
GEOLOGICAL BRANCH
ASSESSMENT REPORT
OWNERS
and OPERATORS
o
O
Stowell
and
S
l
REPORT PREPARED BY
XARJORIE
P
O
BOX 86913
L
SERACK
GEOLOGIST
HORTH VANCOUVER
Phone
604
986
B C
V7L 4P6
2893
MINISTRY OF ENERGY MINES
AND PETROLEUM RESOURCES
JUNE
10
1988
j
Rec d
J U N 1 3 1986
I
I
n
SUBJECT
FILE
VANCOUVER
B C
INDEX
o
INTRODUCTION
1
LOCATION AND ACCESS
1
CLAIMS
2
HISTORY
2
REGION L GEOLOGY
2
PROPERTY GEOLOGY
2
MINERALIZATION
3
CONCLUSIONS
4
RECOMMENDED PROGRAM
5
STATE
6
NT OF EXPENDITURES
STATEMENT OF
7
QUALIFICATIONS
o
FIGURES
n
1
Location l
2
Claim
3
Prospecting Map
1a
p
2a
Map
in
of the Pine
APPENDIX A
Photographs
APPENDIX B
Petrographic
APPENDIX C
Analytical
Results
Results
Woods
Property
pocket
o
NTS
CLAIMS
WOODS
PINE
5158 N
CARIBOO MINING DIVISION
92N 14E
12 W
125
INTRODUCTION
The
August
on
April
claims
Traverses
information
via
1988
27
were
prospected
and the
1987
12
11 and
Claims
stowell
and O
author
returned
to
helicopter
plotted by
and Woods
the Pine
author
the
to
gather additional
of
means
and
compass
of the main
the vicinity
Detailed measurements in
were
designed
Traverses
made with a survey tape
survey
showings were
earlier
an
regional
indicated by
anomalous areas
survey
pace
to
cross
collected
were
Samples
on
both
trips
Sections
were
with the
aid of
a
microscope
Measurements
of
property
magnification
to the
observed under 40x
cut from these and
grain
sizes
were
An unusual
into the microscope
the scale built
The
sample
in
one of the
samples
observed
where two
silver mineral was
for further study
to Vancouver Petrographics
sent
in
was
included
is
Their report
made of the sample
were
violet
sections
ultra
under
examined
All
samples were
B
utilizing
made
Appendix
o
light
was
also
visited
by
representatives
of
the the
property
who consented to
in November 1987
MineQuest Explorations
of this report
in the submission
of their sample results
use
of the property
view
s
a bird
eye
The helicopter provided
on the property
idea of the structures present
to
give a better
While weather conditions
and to locate other gossanous showings
their
observed
the
sites
of
on
any
did not permit landing
hovering at
and elevations determined by
were recorded
locations
elevation
by
determining the
and
with the showings
of these showings
eye level
Photographs
altimeter
means of the helicopter
A to this report
in
The
are
Appendix
contained
LOCATION AND ACCESS
Pine
The
B
Lake
C
Woods claims
and 16 km
are
southwesterly
of Williams
B C
on the
Kleene
from Kleena
via
the
accessable
are
located 257
km west
The Claims
1
a
four
by
there
Kleene and from
Kleena
Bella Coola Highway
A spur road leads
claims
road leads to the
forestry access
road
four
access
forest
The
on the property
to the main showings
The property
the Woods claims
southern margin of
runs along the
between the elevations
Klinaklini
River
Figure
to
is
located
of 820 and
coast
1400
m
forest
sandy soiled pine
the
of
located on the margin
The claims are
Nechako
the
contact with
where it comes in
plutonic complex
Plateau
o
in a
I
I
I
I
I
i
i
I
I
i
I
I
I
ir
i
I
I
I
I
tt
I
I
4t
i
I
I
o
I
18
ICOKM
p
1
1270
1210
0
I
CLAIMS
1 4
Pine
o
expiring
7
8579
8578
a
ve
1989
no
8573
8574
8575
expiring
on
August
private
group under
claims h
28
8
been staked
the
agreement
between
the two
post system
on
8577
8576
1988
14
Fadenrecht
stowell and S
O
currently held by
are
They
July
8580
7859
7858
7857
7832
no
record
on
1 8
Woods
as
record
parties
All
2
Figure
HISTORY
property
The
was
found
Woods while
Mr
by
searching
sick
for
from
his
horses
made
had
of substances which
held until their
were
claims
The
privately
water
the
when
drinking
in
1973
and McLeod Copper
to Cadillac Explorations
the
option
in the vicinity of
drill holes were completed
d
iamond
and
a
three
1975
in
Asarco
The ground was mapped by
main shdwing
for
recorded
never
conducted but
was
survey
and
Stowell
Mr
geochemLcal
was staked
by
In 1979 the ground
assessm nt
who conducted a
Inc
to Rhyolite Resources
optioned
and
ntly
subsequ
additional
ground
staked
program
geochemical
regional
The
ground was
program
conducted a follow up geochemical
in
1985
Stowell restaked the main showing
Mr
allowed to lapse
1987
in
Woods Claims
Fadenrecht staked the adjacent
and S
the
source
REGIONA
o
GEOLOGY
in
occur
sediments and volcanics
of
altered
Inclusions
vicinity of the
immediate
terrain in the
granitic to dioritic northeast of the property the dominent
the
To
up
property
Tuff with clasts
to be an andesitic lapilli
been hydrothermally
lithologY appears
tuff
has
In places the
to
15cm in diameter
to
be
in
The tuff
appears
altered to a serecitic assemblage
Creek
Taylor
rocks to the southwest
on
fault oontact with granitic
are
reported to occur
and greywackes
siltstones
shales
Group
Klinaklini River
the banks of the
faults cut
North South striking
and
Northeast Southwest
Tchaikasan
through
the
property
The
Perkins
and
are
fault
Peak
southeast
Mines lies 19 km
faults to the main
splay
Gold
Gold
of Kleena Kleene
Prospect
of the main
showing
PROPERTY GEOLOGY
occur
within
composition
Figure
fine
grained
brown
composition
Outcrops
does
n
roof pendants
volcanic
to
dioritic
granodioritic
of
Hornfels metasedimentary
intrusive
complex
an
results
are
notappear
3
The
volcanic sand
in
alternate
generally
small
commonly grey and
Variability in
siltstones
pendants
or
are
and appear
to be any sulfide
banding
color
2
mm
thick
There
subcrop
hornfels
with the
more
associated
2
as
r
f acl
C
C
ffl r
r lilt
f
0
FIG 2
ClAIM MAP
O
i
I
r
r NZ
0
0
Vf
n
IIlI
IN
j
I
1
i
l
1
0
F
x
S4
OM 3
r
1JSZ
o
l
l
r
It
r
Yi
C
u
I
I
o
2000
1000
METRES
PS
0
Q
3
z
20
3000
The
o
altered
present
variable
may
5
upto
also
phases minor
percentage of quartz
Quartz eyes approximately 5
be
of
outcrops
sandy soil
a
which
some
are
ridges
amounts
showing trace
and sphalerite
dioritic
It
well
weathers
more
silicified
in the
present
vicinity
chalcopyrite
to
portions
dominent
the
is
diameter
forms
western
is
disseminated
of
in
especially
are
also
matrix
when
matrix
of
the
in
main
arsenopyrite
visible
are
the
main
phases
occur
At
which
pyrite
In
showing
away from the main
areas
em
appears to be
Trace
from the air
observed
the
intrusive
in the
a
intrusion
grey to white
is
partially
in
sparsely vegetated
places although
in most
and forms resistant
The
samples
Woods claims the intrusive
the
of
biotite is
some
The
in
seen
rounded
form
In
matrix
is
property
phases
phase appears to be a
places the hornblende
In
chlorite
to
in the
the
on
Several
dominent
The
diorite
hornblende
present
intrusive
granodiorite
present
are
lithology
predominent
dioritic to
showing
Massive
it
appears
if
as
arsenopyrite
three different
occurs
near
or
at
a
to andesitic dyke which has been
microdioritic
grey black
mafics
as
hornfels
d
some
Microscopic
geologists
interpret
by
See Appendix B
examination however indicates a
origin
dark
primary
XI NERAL I Z
AT ION
silver mineralization occurs with arsenopyrite
and
The five
zonal fissure viens cutting the microdiorite
Gold
in subhor
most
along
o
viens each average 15 em thick but
locally
may
The veins are undulating and appear to occur
significant
swell
40
upto
em
structural breaks
There are
reports
in the
of
similar
Faulting is evident
arsenopyrite
assemblage of galena sphalerite
and
pyrrhotite is present
argentite
pyrite
the hornfels
is
a
The
of
pyrrhotite
differentiate
bronze
tinge
through
its
in the
fracture
dominent sufide appears to be
arsenopyrite which
in
also
color
There
appears to be a large
grey
silver
percentag
in
chalcopyrite
An
fillings
viening
of mineralization
area
from
to
it
magentic
in the
matrix
is
it
although
hard
to
as
it has only a slight
arsenopy rite
detected
The presence of pyrrhotite is best
trace
amounts
of
chalcopyrite
affinity Only
the
be present in the mineralization at the main showing
to
appear
mass
These app ar as small isolated blebs within the the sulfide
or
on
the margins of fracture viens
Chalcopyrite does however
with
minerals
associated
the
trace
high
appear to be one of
arsenic
gold
values
Resources survey
Another
from
the
significant
work done
trace
in the
mineral
previous Rhyolite
indicated
by
the
petrographic
Rhyolite survey is
in Appendix B
identifies
It
study on sample 87M2L is included
tellurides
as
being present
possible bismuth
conducted
Vancouver
The
by
petrographic
study
the
of
fine
also
presence
grains of free
Petrographics
reported
within
the
gold
arsenopyrite
value
19
showed
an
elevated
MS 02 88
ppm in
Sample
elevated values of bismuth
Scandium
o
which is anomalous
Scandium
3
has
A
recently
been
the
focus
It
Europe
in
exploration
of
used in the electronics
is
industry
The
o
10
matrix
finely
contacts
fissure veins themselves
the wall rock
contamination
of
the
are
upto
pyrite
The
show
and
sharp
The
by
sign of
in length
contains
white
and
arsenopyrite
dissem nated
viens
the fissure
surrounding
fissures
are
no
short
At the mainshowing
and appear to be discontinuous
vertical foot exposure
lenses were detected within the 15
22
I
Significant
Year
1973
Values
i
are
Au
No
Sample
108
oz
Ag
t
oz
As
t
96
3
inches
4
ft
1973
109
38
tr
1973
110
20
1 50
1973
111
22
tr
4
01
I
4 ft
I
I
5 ft
1973
Campbell
1
76
44
29
51
Grab
1973
Campbell
2
1 52
74
33 83
Grab
I
22
4
94 5 95 5ft
I
0233
108
01
I
0234
532
09
I
0235
905
90
0236
011
01
0237
242
50
1983
rx6
439
55
1987
M1L
87
228
07
87M2L
878
06
I
220
2
ddh
1981
0
ZR
170
ZR
175
AMS161
ZR
174
B16
BB
MS04
FMSOl
BB
MS03
BB
I
I
20
865ppm
220ppm
50ppm
88
MS02
99
9820ppm
38500ppm
1675ppm
7150ppm
345ppm
AMS 160
1988
REFERENCES
Assessment
GSC
GSC
Reports
File
Open
Map 2103
4572
11114
11994
1163
1925
CONCLUSIONS
the main showing are
at
sulfide
and
abundance
their
themselves
discontinuous and small within
The deposit
a
bulk
target
lead to
tonnage
good gold values may
a
in
and
oriented
controlled
to be
structurally
appears
the
data
gathered
direction
north south
Interpretation of
areas
with
the
gossanous
previously by Rhyolite Resources along this
the
indicate
survey
detected
on
during the course of
main
the
to
for other
mineralized zones parrellel
While
the
lenses
of
potential
o
I
Width
24
4
Zon
showing
of
in locatiqn
o
shown
have
other
A
strong
in
the
id
nt
signifiG
showings
from
evident
structural fabric is
the
air
as
terrain appears to
Appendix
photographs
in at least two dominent directions which makes
A
in
The
ifaulted
been
correlation of the
existing showings
detailed
work
surface
This
did
survey
located
on
of
outcrop
of the
that
determine
further
source
the
merits
property
limited scope no new showings
is
detailed
much
more
survey
Within its
exploration
continued
some
without
difficult
structures may be the
These
silicific tion observed in
were
may be
intrusive
tion within the
A
the surface
required
RECOMMEND D PROGRAM
of
staking
2
Grid to be constructed
at
lines
3
M
I
c
4
6
out
ological
over
the
Cd
with
Mapping
the
intrusive
C6nstruction
of
an
y
be
the
advisable
Bi
anomalous
alteration of
protection ground
with
property
entire
m
intervals
to
flown
to
structure
base base
if this
this
have
to
be
base metals
Ag
targets
geophysical
orthophoto
area
surveys
As
regard
is
done
map
to
and
This may
it
necessary
with a combined
rbourne
geophysical survey
Blanket sampling of the Main
a
0
for Au
sampling
require having
7
36 units as
Resistivity
gnetometer and VLF
mpleted over the grid
Seil
G
of
over
intervals and stations at 20
100m
be carried
5
a
less
or
o
minimum
1
areas
Showing
detected in this survey
5
and
the
gossanous
o
STATEMENT OF EXPENDITURES
WOODS MINERAL CLAIMS
PINE
LABOUR
M L
SERACK
10
Aug
13
1987
7
O
Stowell
Aug
10
days
1987
4
x
27
200
days
29
1988
00 per
125
x
3
VEHICLE
4
SUPPLIES
days
x
2
ETC
VANCOUVER PETROGRAPHICS
two
sections
submitted
by
St
1400 00
day
x
SECTIONS
incl
00 per
35 00 per day
men x
00
50
days
per day
Fuel Vancouver Kliniklini return
CAMP COST
FIELD
13
April
day
500
00
210
00
200
00
123 00
69
00
120
00
158
25
11 O
00
Joe Canada
ASSAYS
M L Serack Chemex Labs
MineQuest Explorations
8
samples
at
13 75
each
2890 25
SUB TOTAL
325 00
REPORT
3 215 25
TOTAL
j
6
o
STATEMENT
I
OF
MARJORIE
Vancouver
1
I
QUALIFICATIONS
L
SERACK
hold
a
B Sc
University
2
of
25
British Columbia
I have
of
Honours
4
Whitely
do
Degree
Saskatchewan
Court
hereby
in
been
I
am
I
retain
no
self
employed
interest in
claims
n
Geologist
10
1988
7
North
state
Geology
from
the
1979
years
presently
geolgist
5
o
4P6
practicing my profession for
being employed by such firms
Saskatchewan Mining Development
Cominco
Lornex Mining Corporation
nine
June
2556
lL
V
as
the Pine
a
the
past
as
Limited
and
consulting
or
the Woods
mining
n
APPENDIX
A
PHOTOGRAPHS
o
or
8
co
0
co
I
o
l
f
co
co
1
2
o
I
l
0
co
t
o
I
I
c
CD
CD
n
c
orl
f
CD
c
1l
r
n
c
1l
c
c
orl
rl
i
orl
CD
CD
il
J
or
c
z
i
0
or
oj
l
S
o
c
CD
CD
91
o
1l
bI
Z
C
Q
0
0
c
I
l
c
1l
o
rr
II
re
aM
j
A
l
Sa
Dle
site
87M1L
showin
diorite to
Pine bods
texture
seen
Arsenopyrite
rusty color
in fractured
icrodiorite
structural
Bast shows the dominent
Property looking North
corner
hand
lo
r left
of the
on
uch
property
A 2
CREEK
SHOWING
gossan
was
taken
margin
NORTH SHOWING
as
facing
of the
gossanous
was
observed frolllthe air
taken
A
north
The
photograph
The creek is
at the lower
pidure
areas
as
seen
from
a
distance
The
photo
facing North
IV1c
F
er
to the gossanous
Photographs taken clos
NORTH SHQ ITNG
anomalies shown on the previouS page
ve etation
A 4
o
APPENDIX
PETROGRAPHIC
o
I
B
RESULTS
3 1
Atroraji
f
II
I
l
if
d
o
JAMES VINNELL
JOHN G PAYNE
Repo
n
I h
FORT LANGLEY
VOX lJO
or
Ucol011ist
Kennedy
Dave
st
419
B
sub massive
gold
mine
8Jl80
ite
containing Gold
L
p
F6
ock is a st
chlo
with much less
icite
coa se
to
of fine
patches
abundant
one side
ecciated along
st
ongly
and a few
in
als may
in Assay
lA
ct
p1
by
assemblage dominated
ongly altered ite and minor Ti oxide
The host
se
tz and
b
unknown
part
13Z3
v6C lX6
C
Arsenopy
y
contains
which is
B C
pHONE 604 734
InvOlce
May 1988
Inc
Joe canada
street
553 Granville
VANCOUVER
qua
BOX 39
SH STREET
BBB7 N
t for
summa
2tct
tCd
P o
II
sample
lfel
JlCO
mine
contain
als
Bi
with
occu
and
of
a
arsenopy
ained
g
Native
sample
the
senopy
ite
It
ite
the
unknoWn
Te
fr
lfGt
PAI1ATIO
FOR
MICROS
PETROGRAPHICREPORTS
SPECI
STUDI
LGEOLOGY FIELD
B 2
sample
M
o
Altered
Rock
patches
of
phases
possibly
Arsenopyrite
contains
The rock
of
altered assemblage
Native gold
Ti oxide
of ni
and
Te
Ag
patches of arsenopyrite enclosed in a strongly
with much less chlorite and
quartz sericite
and
few
a
and
Chalcopyrite
arsenopyrite
sericite
Chloritel with Abundant
with Native Gold and unknown
Quartz
unknown
pyrite
phases
are
occur
in
fractures
arsenopyrite
in brecciated
quartz
20
25
Mineral
sericite
12
15
chalcopyrite
3
4
pyrite
5
native
Bi Te
chlorite
Ti oxide
0
55
arsenopyrite
rock
The host
of
with
with
concentrated
is
trace
trace
gold
Ag
minerals
trace
by very fine grained quartz intergrown
fine to locally very fine grained sericite
dominated
extremely
patches
quartz
Locally
60
0 1
minor
X
medium
mainly adjacent
grained patches
These arsenopyrite grains commonly have euhedral
arsenopyrite
Chlorite forms ragged flakes and patches
terminations against quartz
It is light greyish green in color
averaging 0 2 0 5 mm in size
are
patches of extremely fine
Associated with many chlorite patches
grained Ti oxide
It is
Arsenopyrite forms very fine to medium grained aggregates
of
the
side
locally
sample
brecciated very strongly along one
fractures up to 0 01 mm wide in these
occur in
and
pyrite
chalcopyrite
forms
fine
to
to
brecciated
zones
to
o
0
06
Chalcopyrite also forms a very few lensy inclusions up
long in arsenopyrite
Mineral X forms an anhedral grain 0 8 rom across
In sample lA
It is moderately soft
light grey with
associated with arsenopyrite
blue
distinctive
a
with
and moderate anisotropism
a
low reflectivity
this
altered
and is
slightly along
color
It has one good cleavage
high relief minerals
and moderately along grain borders to secondary
sulfo salt of bismuth or
It may be stibnite or a more complicated
rom
lead
native gold occurs in a few patches enclosed in
Sample lB
interstitial to very fine
one grain 0 05 mm long occurs
arsenopyrite
a cluster of
few
occur in
A
submosaic arsenopyrite
grained
in a medium
enclosed
mm
in
size
irregular grains averaging 0 005 0 0 2
cluster
in
this
with
native
gold
Associated
grain of arsenopyrite
one
of
two
in
size
005
mm
phases
few grains averaging 0
are
a very
In
tellurides
these may be Bi
grey colored
in a coarse
of
inclusions
mm
to
0
15
cluster up
long
including two
consists of three or four phases
and
colored
cream
Another
arsenopyrite
one
grain
minerals which may be
Grain size averages 0
0
01
poor
0
02
mm
in
polish
size
and
and
Bi
005
it
creamy
0
or
02
has
grey
a
Ag
mm
tellurides
One
moderate
color
phase
and minor
forms a few
reflectivity
Another
forms
native gold
grains
masked
one
grain
by
0
from
very
01 rom
and a greyish white
high reflectivity
it has a good polish
be
sphalerite with
color
Another grain 0 02 mm across appears to
Native gold forms one
abundant exsolution inclusions of chalcopyrite
across
elongate
o
grairi
0
015
mm
in
length
Ol
MS
SAMPLE
n
B 3
B
Appendix
MainshDwing
LOCATION
HANDSAMPLE
DESCRIPTION
Fine
the
with
rom
and
matrix
Light grey
sulfide
appear to be arsenopyrite
Fractures are
feldspars
sulfides
quartz
DiDrite
weathers
CDntains up tD 2
very fine
averages 1 rom
SDme
disseminated
DUt
matrix
grains
thrDugh
Grain size
1
grained
hDrnblende
grained
buff brDwn
of
88
Fine
fractures
1
thick
rom
healed
are
CUT SECTION
2
disseminated honey tD brown resinDus sphalerite
up tD
The matrix
as
iSDlated
occuring
grains up tD 2rom in diameter
fine crystaline translucent clear to cream colored
cDntains up to 25
Trace translucent blue mineral possibly apatite occurs in the
quartz
ground
mass
The
the
mafic
predominent
Minor
matrix
contains trace
brown
biotite is also
patches
with the
textures
mDre
up to 2
pyrrhotite
cDnsisting
evident
which
occurs
present
The
magnetite
The dominent sulfide
forms
is hornblende
in
the
of
appears tD be
the matrix
Grains Df
of
pyrrhotite
pits
and
Arsenopyrite
arsenopyrite display
elongate
dominated
quartz
blemishes
areas
up to 5
sample
which
is also
of
also
locally
present
exolution
Arsenopyrite
along poorly
is
defined
lineations
One
sample
o
grain
of what appears to be
sphene
was
present
in the
examined
AlsD observed
silvery
was
1
grain
metallic mineral with
a
of
a
rippled
highly
reflectant
bright
surface
ULTRAVIOLET LIGHT
The
minerals
o
sample
were
was
detected
examined under ultraviolet
light
No reactive
B
Appendix
SAMPLE
o
B 4
ME
LOCATION
02
At
88
creek
level 7
HANDSAMPLE DESCRIPTION
and
arsenopyrite
have
ground
occur
in
along
SECTION
but
occassional
places
sample
The
mafic
flakes
the hornblende
been healed
The
with
a
oontaining gnash vienlets of
arsenopyrite
Sample appears to
Microdiorite
places
is
of
It appears as a mottled
rusty orange
7
mafics in an equigranular
magnetic
cutting
hairline fractures
CUT
from DDH 3
It contains
outcrop
The
mass
downstream
disseminations
been silicified in
grey color
m
2
very fine
the
grained
sulfides
sample
mineral appears to be dominently hornblende
of red brown biotite are also present
In
crystals are fractured
assemblage
and the fractures have
sulfide
sulfides consist of subround
to
irregular
isolated blebs
of
Trace white cubic pyrite bearing a
arsenopyrite and pyrrhotite
faint yellowish tinge is also present
Occasional grains of
chalcopyrite are also apparent as are occasional grains of red brown
resinous sphalerite
A bright silvery mineral was also observed but
unidentified
grained metallic steel blue sulfide which formed rods
radiating texture were also observed associated with mafic
In some places these give the sample a feather like texture
they were associated with quartz
A single trace grain of apatite was observed
A fine
in a semi
clots
where
o
ULTRAVIOLET LIGHT
There
sample
o
when
were
exposed
no
to
ultraviolet reactive minerals
ultraviolet radiation
present
in this
o
B 5
B
Appendix
03 88
MS
SAMPLE
30
LOCATION
fault
Out
zone
gouge
level
creek weathers to
crop in
near
bright
a
vertical
orange and
gossanous colour
brown
diorite
with
upto
The
clDts
sulfides
equigranular
sulfides disseminated
CDntains up tD 3
has been stained Drange by the DxidatiDn Df
hairline fractures which have been
it is cut
2
mafics
matrix
In
and grey black
Mottled white
DESCRIPTION
HANDSAMPLE
as
down stream from 87M1L at creek
ro
by
places
The
CUT SECTION
cDntains very fine grained sulfides of which
is cDmposed of light
and the remaining 2
This
sample
is
strDngly magnetic
annealed with sulfides
sample
makes up 1
to grey bronze cD1Dred pyrrhDtite fDrmed in irregular masses
Associated with it is a fine
and clots
The pyrrhotite is magnetic
sulfide
mineral
which
cubic black
may be tetrahedrite Dr
arsenopyrite
bronze
grained
The sulfides tend tD
tennantite
the
areas of
sample
Fractures
quartz
a
and
of
o
fine
with
1
generally
wide and have been
giving
in
the fracture
the fractures
generally
a
mDre
rom
mafic rich
in diameter
generally
fi ed with
vuggy appearance
5
pyrite Dccures
associated with fractures
grained hDney
as
does
tD
occur
tD
brown
resinous
sphalerite
Dccurs
in fractures
silver metalic mineral as sketched
in this sample and may be a silver mineral
A dendritic
seen
rom
Dccur es
sulfide
disseminations and
was
2
is
galena
Trace
as
stibnite
bright yellDw
traces
1
sulfide minerals
Trace
as
Crystal
are
be associated
size
bright
below
sulfides appear tD follow lineatiDns and are assDciated
The sample appears tD have been
with more mafic bands in the matrix
The mDst prDminent
at
least
two
directiDns
fractured and annealed in
to
each
Dther
at
20
fractures intersect
degrees
The
ULTRAVIOLET LIGHT
No UltraviDlet
was
reactive
submitted tD ultraviDlet
minerals
light
o
M
were
nDted when this
sample
B 6
B
Appendix
SAMPLE
o
112L
87
LOCATION
above DDH 3
on a
narrow
HANDSAMPLE DESCRIPTION
as
occuring
fracture
fractured
in color
in
2
prior
to
mm
Sulfides weather to
mush
diorite
grained
weakly magnetic
with
to be
Pits
up to
are
2
Grab
pyrrhotite
brown
cream
brown
is
barely distinquishable
coloration to it
There
in the
arsenopyrite
arsenopyrite grains and may
fine grain of gold observable
very
trace grey black metallic cubic to
lmm diameter
sulfide is very fine grained
The
a
cutting the arsenopyrite
randomly dispersed or occuring
ures
stibnite
in small
aggregates
Trace
Quartz
lmm diameter
chalcopyrite
forms
3
of the
fractures and results in
euhedral
buff
contained within the
Possible
in hairline frac
Trace to 1
or
light
spots
faint bronze
a
observable
inclusions
occurs
in
a
which weathers to
Arsenopyrite
quartz
which has
Sample
rectangular crystals
o
vertically
thick
arsenopyrite with up to 2 quartz
Sample has the appearance of crushed
also contains
along
em
Predominently arsenopyrite composed of ragged crystals
Crystals show signs of having been fractured
healing
indicate
clots
up to 10
in diameter
pyrrhotite
appears
matrix
and
and 5 ft
Massive
fine
is
Sample
SECTION
up to
from
arsenopyrite showing
filings
crystal
color band with
CUT
level
from subhorizontal upper vein
sample
and
creek
10 ft above
showing
Main
crystals
are
up to
l
matrix
as
discrete grains
It also
vuggy texture
3mm in length and
a
occurs
The
1
mm
as
crystals
translucent
in dia
eter
ULTRAVIOLET LIGHT
No ultraviolet reactive
was
o
submitted to ultraviolet
minerals
light
were
noted when this
sample
SAMPLE
o
B 7
B
Appendix
MS 04 88
LOCATION
Arsenopyrite containing
HANDSAMPLE DESCRIPTION
mineral associated with
appears to have formed
of
to
quartz
up
subeuhedral
are
also appear
1
cm
and
in
and
length
in diameter
are
The
to the
elongated subparrallel
crystals
4cm
in color
white
long
silvery
Sample
crystals
pistachio
as a frothy crystal
milky
sulfide
framboidal
a
green alteration mineral
Contains
mush
quartz
The
showing
float from creek at main
Arsenopyrite
The
crystals
arsenopyrite crystals
dimension of the
fractured and have been annealed with
quartz
SAMPLE
FMS 01 88
from creek at main
LOCATION
HANDSAMPLE
showing
Dark grey to
DESCRIPTION
in contact
black microdiorite
blebs of
pyrrhotite upto 1 cm
quartz viening contain ng irregular
from
the blebs of
is
in diameter
The pyrrhotite
distinquishable
in
the
its
strong magnetism faint
sample by
arsenopyrite also present
with
bronze
color and
The
o
CUT SECTION
Fine
approximately
blue grey
slightly larger
itself
microdiorite
3
1mm
grained
quartz 5
to grey
Sulfides
are
vugs or fractures and
blue grey sulfide was
of the extremely fine
The
sphalerite
contact
o
at this
sample
equigranular groundmass composed
up to
hornblende
15
70
of
dark
feldspars
distributed within the
variably
approximately 5 of
pyrrhotite and minor pyrite
identify
moderately magnetic
serecite
make up
to
masses
is
are
it
The
Sulfides
to
occur
grained nature
magnification
also contins
concentrated
are
associated with
seen
a
prevalent
more
quartz
with bronze
as
the
quartz
near
and
it is
of brown
open
A steel
fillings
pyrrhotite
of the sulfide
trace amount
mainly along
groundmass
dominent sulfides appear to be
Because
impossible
resinous
microdiorite
o
APPENDIX
ANALYTICAL
o
o
C
RESULTS
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