i ih rr4 110 b i - british columbia
TRANSCRIPT
I
i S ih rr4 e 110 b
nJ
rl J
on1
D
L
GUICHON EXPLORCO LIMITED
SUMMARY OF PERCUSSION DRILLING
AND
oo
INDUCED POLARIZATION GEOPHYSICAL SURVEYS
ON THE
GN 1 8 CLAIMS
rCLINTON MINING DIVISION
NTS 92 P 14W
nu S10SS N 121023 W
nLC GEOLOGICAL BitASSESSMENT RE
1L
oofi
I
D GAMBLE
SEPTEMBER 1983II
1
1
U
IL
I
IL
rL
TABLE OF CONTENTS
oonCJ
Page
SECTION 1
o
INTRODUCTION
LOCATION AND ACCESS
TOPOGRAPHY AND VEGETATION
CLAIM STATISTICS
PREVIOUS WORK
GEOPHYSICAL SURVEYS
1
2
3
4
5
6
iIL
r
u
nLJ
SECTION 2
A GEOPHYSICAL REPORT BY PETER E WALCOTT
AND ASSOC LIMITED NOVEMBER 1982
InL
o
Do
on
SECTION 3
A GEOPHYSICAL REPORT BY PHOENIX GEOPHYSICS
LIMITED JUNE 1983
SECTION 4
PERCUSSION DRILL PROGRAM
SECTION 5
COST STATEMENT
SECTION 6
CERTIFICATE OF ANALYSES
nI
LJ
SECTION 7
o CERTIFICATE
CERTIFICATE OF AUTHOR
Il iU
r
l
1Ll
LIST OF ILLUSTRATIONS
rI I
nJ
FIG 1 LOCATION MAP OF THE GN CLAIMS
1 100 000
onL
Dnw
CIo
D
FIG 2 LOCATION OF GN 1 8 CLAIMS WITH
DETAILED TOPOGRAPHY
1 50 000
FIG 3 LOCATION OF GN GRID AND
GN SUBGRIDS NOS 1 8
1 50 000
on
on
o
o
1u
nW
D
nnt
fJ
SECTION 1
INTRODUCTION
LOCATION AND ACCESS
nL
TOPOGRAPHY AND VEGETATION
CLAIM STATISTICS
r PREVIOUS WORK
GEOPHYSICAL SURVEYS
qI
IJ
n
fiL
rf11
iI
tr1
II
ri1
n
ntJ 1
lu
rNTRODUCTION
TLi
Two Geophysical Induced POlarization and Resistivity surveys
were conducted over the GN claims by Guichon Explorco Limited
Gin November 1982 and in June 1983 using geophysical contractors
I
During the same periods two percussion drilling programs
totalling twenty 20 percussion drill holes 3355 feet were
r
ocompleted
sII
This report contains the results obtained from these work
programs
rooG
1IJ
nL
f1
U
nu
DrfU
11l i
jL
rI 2
rLOCATION AND ACCESS
j i
UThe GN 1 8 claims are located 12 kms northeast of Lac la
n
n
Hache B C The co ordinates of the centre of the property
are 51055 N 121023 W on N T S map sheet 92 P 14
DAccess to the property is gained via the Timothy Lake Spout
Lake road and then via a series of logging roads that lead
r toward the centre of the property See Fig 1 Location Map
r1
U
Lft
J
Jlnu
ru
rw
rt
II
L
I
r1 i
rY
u
r
f1
iI
Dr
1u
fiC
fo
I
rl
r
ru
1L
L
21W I1 Pout
T
IT I
J
v 7 trl Ie T
111
lJ
I I fl r 7f
ceEv
cJ
II1U r
g JI
I J I
v
121 J5 11 1
lJ I I
J
IIIUf l I
I q IJ
r 0j c j l i
I
I
JItilt
I l CVc
I
J
C GN I i G I e
J bi 1
J 1 L fuOQ 1
L J3 L0I
J
l r r
I 1r
i I it ON 3 jF 1 0
J lJ
r
M ci1 lO l 1 t L
1 j VJJ I h 0
l
rllr ll Ii f
vJ 0 D i
GN rf6i1jt i
If1J J I
J i1
ofu
Q 1 1I k
I
l 1I CO
l f i
Ins
1 lpI G1 7
ll L
JJLJIIcnvj JlfA
0 IJtto
J
II qrAr
I 9o1 r r J t
VL
tr
1 h JJ
ry h I 1
rO rrJ
10 coo foN
I
1 ry 10 Vh
J
lZl f
I r
r J
1
iI I
J dI 000 f
u I 1 fr
IJ
1 rc i
lc s
I YJ 1
JJ7 i r5h
CiI 1
7 Ii iwi
I
wL J
0 l1 yr r
Ii
n
J
I I j
y 0
0 IP
I tt
L C
I b It J 1oJ
i l t If J
I d
1 Ifn S
mJ
if Iil
HI VII Ill ICrxIH9 1111
11 4
Et lInlr if QL k lrl
J I
rJiJIT m
fIJrilf on I
AlJJ 1 uI rv cl
hr
P
IIy 17 J
I
UC iJro
r
rl 111
NJ
r I1 i J V C L Iir i
GJ
i iVJ l i J o s
f
I
Lo w fC k ltoo
I
OJI I Id Ja
j
J l I
Sf J k
Oa 5 FI
1 1rTCf c iJure I
H uui I i1JlOCHlOH
I
JJA 2 H iN CUlrII
I
II
3I
jTOPOGRAPHY AND VEGETATION
IJRelief is rolling throughout the claim group becoming steeper
1
j to the south Timothy Creek valley trends northwest across
nw
the claim group with steeper valley slopes in the south compared
f
to a broad valley in the north part of the claim group
Elevations vary from 3400 feet to 4400 feet asl
r Vegetation consists of fir and pine forests with some logged
J off sections et swampy conditions exist along Timothy
J
tCreek
r11
TiI Ic
I
L
I
w
1fC
r1
GnI
rd
IiJ Iu
u
8 4
CLAIM STATISTICS
o
J
All the claims are in the Clinton Mining Division and are
registered in the name of Guiehon Exploreo Limited of Toronto
L
The names record numbers number of units and recorded date
are as listed
f
iI
riClaim Name Record No units Record Date
GN 1 1125 20 August 28 1981
GN 2 1126 20 August 28 1981
GN 3 1127 18 August 28 1981
GN 4 1128 20 August 28 1981
GN 5 1129 20 August 28 1981
GN 6 1130 20 August 28 1981
GN 7 1131 20 August 28 1981
GN 8 1132 12 August 28 1981
Ii
J
nSee Figure 2 Location of GN 1 8 claims with detailed
topography
til
11I
p
J
nu
niJ
IiU
c
ot
nJ
n
r
R
I
l1nI
Ai
Iiz
r
IiJ
nL
nIIi
nI I
n
r
i
J
IlIJI
7 9
8rriJ
I
t
J
1I
r
tI
I JI
n
oj 1 I
y
bi I
1
1t I
r
iy J
J
J
C
J1
GN Y
7yI
h PJI4I
PGuRE 2
LOCAr ON OF G 1 8CLA S VV 78 DE AIL JEl
70POG RAPY SO 000
9zP 14 VIIII
i fl I I
w
I
K I
iIII
IiI
I
0 J
I
l
nL
5
nPREVIOUS WORK
fluA geochemical reconnaissance soil survey was conducted over
cp
the GN claims by Guichon Explorco Limited in 1981 and followed
up in 1982 by more detailed soil grids filed for assessment
in 1982 The GN grid system and sub grids were utilized in
1iIIL
the current work presented See Fig 3 Location Plan of
GN Grid and Sub grids Nos 1 8
nl
flJr
n
onLC
1
J
n
rlL
nI
G
fn
il 6
nI
GEOPHYSICAL SURVEYS
nc
Geophysical survey lines were selected to cover soil geochemicalIf
LJ
nL
anomalous zones from a previous survey
The selected lines were brushed out to I P survey standard
The grid preparation was accomplished using Amex Exploration
IIL Services Limited and company personnel under field supervision
nl
of G Owsiacki under the direction of D Gamble
fTwo Induced Polarization surveys were carried out over selected
grid lines under the supervision of A Wynne
r1l
The first survey was conducted in November 1982 over 25 1 line
nkilometres by Peter E Walcott and Associates Limited The
c report and results of this survey are enclosed as part of this
work report
r1L
The second Induced Polarization survey was conducted in June 1983
over 6 0 line kilometres by Phoenix Geophysics Ltd The purpose
I of this survey was to further delineate anomalous I P responses
discovered in the November 1982 geophysical survey The report
n and results of the second follow up Induced Polarization survey
iTl
are enclosed and form part of this work report
nThe following two sections contain the contract geophysical
reports and results of the surveys A location map Figure 3
n shows the GN grid system with all the geophysical surveyed lines
indicated on 1 50 000 scale plan
nu
o
c3oN
fNn
nI
Au ANOMALY
r
rL
0
I
j1
t l1
III
I
nu
nL
il
i
h
L
nL
I
II
I
1
IIII
IIII
LI
Ii
n
I0
nI
L
n
LJ
3Q
AuAMMALYSob 7 ION I
SibGrid 6 IAu ANOMAL Y
CN J
DH iGN J Z
OH 6N gN 1 1
ONiIr O
Sub Grid I
0r
11
GN 7
Sub IOH N
OH N Z
GN 8
LOS
L OS
L 20 S
L30S
Y
50Lok
LSOS
DHjN
OH6N S
IIDH N I
11
OH NooJ
Au AMJMALY
LSOS
I
II
G nY Ok
eSELCO
THE G N GRIDTIMOTHY LAKE AREA B C
o PEACUSSION ORILL HOLES
I P CONOUCTORS NOO SZ S ey
r
U
1
U
nU
TimothyLok
EXPLORATIONInc WESTERN CNlDA
I t
IScale I 50 00
0 n OAT N T I
12P t1FIGURE
TIIlAC 0 Y 35 JULY It
Di
L
nr
U
n
1I
I ISECTION 2
o A GEOPHYSICAL REPORT
1IBY PETER E WALCOTT AND
PJ
ASSOCIATES LIMITED
NOVEMBER 1982
J
DntJ
r
I
lL
1L
on
o
o
onu
PETER E WALCOrr It ASSOC LTD
oDo
A GEOPHYSICAL REPORT
ON
oINDUCED POLARIZATION SURVEYS
nTimothy Lake Area Clinton M D B C
510 55 N 1210 23 W
N T S 92 P 14W
ilClaims Surveyed TY 1 2 5 6
GN 1 2 3 5
7
ndSurvey Dates October 27th
November 22nd
1982
1LFOR
Ur
S E Leo INC
Vancouver British ColU@bia
r1BY
o Peter E Walcott P Eng
PETER E WALCOTT ASSOC LIMITEDr
U Vancouver British Columbia
o JANUARY 1983
TlILJ
01n GEOPlIYSICAJ SERVICES
o
nu
PElBR E WAJ CO rr IASSOC LTD
DTABLE OF CONTENTS
DnL
Page
INTRODUCTION 1
1lPROPERTY LOCATION AND ACCESS 2
PURPOSE 3
o PREVIOUS WORK 4
GEOLOGy 5
i
U
o
SURVEY SPECIFICATIONS 6
DISCUSSION OF RESULTS 8
SUMMARY CONCLUSIONS AND RECOMMENDATIONS 11
n
o
on
nLo
APPENDIX
COST OF SURVE i
PERSONNEL EMPLOYED ON SURVEy H
CERTIFICATION Hi
LOCATION MAP TY 1 2 5 Scale 1 50 000 iv
o
oo
n
LOCATION MAP TY 6 GN 1 2 3 5 7
Scale 1 50 000
LOCATION MAP GN 1 2 3 5 7 Scale 1 100 000
PSEUDO SECTIONS OF I P v
oGEOPHYSICAl SERVICES
D PEllm E WAJ COlr ASSOC LTD
nLJ
1
o
o
INTRODUCTION
nL
rjU
n
Between October 27th and November 22nd 1982 Peter E
Walcott Associates Limited carried out limited induced polarizationsurveys for Selco Inc on th ir properties in the Timothy Lake area
of British Columbia
The surveys were carried out over preselected lines 17 in
all of seven reconnaissance compass and chain soil sampling grids
These lines were supposedly cut and rechained and in some
cases established across the geochemical grids to I P specificationsbut in many cases evidence of this was hard to find
1Measurements of apparent chargeability the I P response
parameter and resistivity were made along these lines using the
dipole dipole methof of surveying Readings were made with a 50 metre
dipole and first to fourth separation measurements obtained
nL The data are presented in pseudo section form on individual
line profiles bound in this report
ri
DnJ
n
rI
I IU
nJ
L
1IiJ GEOPHYSICAl SERVICES
r
U
oPElER E WALCOlr ASSOC LlD
2
nLl
Iu
PROPERTY WCATION AND ACCESS
flL
The properties are located for the most some 12 kilometres
east of Lac La Hache in the Clinton Mining Division of British Columbia
r
LJThey consist of the following claims
Claim Name Record No Units Record Date
TY 1 1133 20 August 28th 1981
TY 2 1134 16 August 28th 1981
TY 5 1137 20 August 28th 1981
TY 6 1138 12 August 28th 1981
GN 1 1125 20 August 28th 1981
GN 2 1126 20 August 28th 1981
GN 3 1127 18 August 28th 1981
GN 5 1129 20 August 28th 1981
GN 7 1131 20 August 28th 1981
Access is easily obtainable by 2 wheel drive vehicle from
Hwy 97 at Lac La Hache via the Timothy Lake road and numerous loggingroads that exist in that country
n
oo
o
o
c
D11
Ur
Ll
rL
J
n
oGEOPHYSICAl HEHVICES
D
oo
o
PElER E W ALCO1l ASSOC LlD
3
PURFOSE
nL
The purpose of the survey waa to search for possibleoccurrences of sulphide mineralization within and around the largeairborne magnetic feature on which basis the ground was obtained
on
o
rn
on
o
onLI
U
flJ
oGEOPHYSICAJ SERVICES
II
PE1 Jm E WAI COn ASSOC LrD
rL
4
Don
PREVIOUS WORK
Previous work in the area is believed by the writer to
have consisted of prospecting geochemical and geophysical surveyingand drilling on the Coronex property to the east However the reader
is referred to detailed information held by Selco Inc
IL
n
o
oo
o
G
onII
r
o
D
o
o GEOPHYSICAT SERVICES
ri PETER E WAIcorr ASSOC LTD
o
oorL
5
GEOWGY
The reader is referred to reports and material held bySelco Inc
onL
o
o
o
onu
onI
o
oo
o
o GEOPHYSICAl SlmVICES
r
U PErER E WALcorr lit ASSOC LTD
oo
on
6
SURVEY SPECIFICATIONS
The induced polarization IP survey was carried out
using a pulse type system the principal components of which are
manufactured by Huntec Limited and Phoenix Geophysics Limited ofMetropolitan Toronto Ontario
o
o
o
The system consists basically of three units a receiverHuntec a transmitter and a motor generator Phoenix The trans
mitter which provides a maximum of 2 0 kw d c to the ground obtainsits power from a 2 0 kw 400 c p s three phase alternator driven bya gasoline engine The cycling rate of the transmitter ia 2 secondscurrent on and 2 seconds current off with the pulses reversing
continuously in polarity The data recorded in the field consistsof careful measurements of the current I in amperes flowing throughelectrodes Cl and C2 the primary voltage V appearing between thetwo potential electrodes PI and PZ during the lurrent on part ofthe cycle and the apparent chargeability Ma presented as a directreadout using a 450 millisecond delay and a 650 millisecond samplewindow by the receiver a digital receiver controlled by a micro
processor
nu
o
o
o
The apparent resistivity Pa in ohm metres is proportionalto the ratio of the primary voltage and the measured current the
proportionality factor depending on the geometry of the array usedThe chargeability and resistivity are called apparent as they are
values which that portion of the earth sampled would have if itwere homogeneous As the earth sampled is usually inhomogeneous thecalculated apparent chargeability and resistivity are functions ofthe actual chargeability and resistivity of the rocks
o
oo
o
The survey was carried out using the dipole dipoleelectrode array This electrode configuration and the methods of
presenting the results are illustrated in the appendix Depth penetration with this array is increased or decreased by increasing or
decreasing a and or n
o
In practise the equipment is set up at a particular stationof the line to be surveyed three transmitting dipoles are laid out
to the rear measurements are made for all possible combinations of
transmitting and receiving dipoles the latter consisting of two
porous pota filled with an electrolyte copper sulphate solution a
feet apart up to the fourth separation i e n 4 the equipmentis then moved 3 a feet along the line to the next set up
o
o GIWPIIYSICAl SImVICrS
o PETER E WALCOll l ASSOC LTD
ooo
o
7
SURVEY SPECIFICATIONS cont d
A 50 metre dipole was used on the survey and first tofourth separation measurements were made
In all some 35 9 kilometres were covered using the above
omethod
o
oo
o
o
o
o
oo
o
o
nI
o GEOPHYSICA r SEUVICES
o
co
oo
o
o
onL
o
onLl
o
oIiLJ
l
j
lj
f
1
J
PElER E WALCOTT ASSOC LTD
8
DISCUSSION OF RESULTS
The chargeability results in general showed the areas
surveyed to exhibit a very low chargeability background in theorder of 1 to 3 milliseconds probably occasioned in places by the
fairly thick overburden cover Thus although areas exhibiting chargeabilities of 3 to 4 milliseconds are shown as possible anomalousareas they probably in most cases reflect a change in backgrounddue to a rock type change etc
The widths of the anomalous zones shown here are themaximum possible and in all probability are considerably less thanillustrated
The areas surveyed will now best be discussed on an individual basis
GRID GN 1
Four lines were traversed with the IP method in thisarea As can be seen from the pseudo sections of Lines 56 60 64and 68 S re pectivily the resistivity results reflected the topography and underlying bedrock as can be seen by the higher valuesover the h ll to the east and the lows over the lake swamps etc
Two zones of poor to moderate I P response and limitedstrike extent can be seen striking across the eastern ends of Line60 and 64s respectively
A possible anomalous zone open to the west is observedat the western extremity of Line 68S This zone should be delineatedby additional work
Another possible zone that could extend to the southis observed at depth in the middle of Line 68S
GRID GN 2 3 5
Here five lines were traversed using the I P techniqueLines 24 28 32 36 and 40S respectively and yielded the most
interesting results
Numerous anomaloua and possible anomalous zones are
discernible on the pseudo sections two of which stand out as better
targets for further investigation They are 1 the zone s between
the BL and 6W on Line 40S and 4W and 8W on Line 36S and 2 the zone s
GIWPIIYSICAf SHRVICI S
PElER E WAI COrl lit ASSOC LlD
oo
o
9
DISCUSSION OF RESULTS cont d
nLJ
centred around 12 and 13W on Line 28S and extending from Line 32S
to Line 24S
oThe former is open both to the east and the south and
requires further delineation there whereas the latter is also
open north of Line 24S but appears to be eakening in response
nA case could also be made for extending the latter all
the way through to Line 40S but the writer believes this to be a
separate zone or joined to those on the southernmost extremities
of Line 28 and 32s
Cn
Low resistivity readings are obtained east of TimothyCreek on Line 28S and in the swamp on the eastern end of Line 32S
GRID GN 7
o
o
o
o
o
No resistivity and or IP contrasts are observed on the
two lines traversed here
TY IGRID
A large resistivity low most probably reflecting deepoverburden conditions is observed between 13 and 19 NE on the onlyline traversed here Low chargeability values are coincident with
this feature
Another resistivity break occurs at the 20 meter deepravine circa 5NE as evidenced by the lower resistivity values to
the southwest
o
o
o
Anomalous chargeability conditions appear to exist all
the way across the line but would seem to be caused by changedin background due to the changes in rock type It could well be that
anomalous conditions only exist southwest of the ravine but in
any case additional work is needed to further investigate this
TY 2 GRID
o
o
A moderately strong double peak anomaly suggestive of a
body of limited depth extent is observed striking across the south
western ends of Lines G l and 2 respectively
GEOPlIYSICAI SEUVrCFS
pmEn E WALCOlr ASSOC LTD
oo
o
10
DISCUSSION OF RESULTS cont d
oA zone of higher chargeability open to the north east
can also be observed at the other ends of the lines
o
o
Q
o
o
o
o
Low chargeability readings are obtained over the out
cropping topographic rises clearly discernible on the resistivityresults
TY 5 GRID
Here the resistivity survey suggests four rock type changescirca 4 7 8 5 and 14SW respectively A resistivity low appears to
occur at depth at 13 SW This complex resistivity pattern is attribut
able to patches of outcrop and or boulders encountered in ne emplacement of electrodes from 11 to 13SW It also gives rise to a complexIP pattern Itwould appear that a small zone of anomalous chargeability readings exis s around 11SW and that the reat of the higherreadings on the line are due to a background change caused by changesin bedrock and or oberburden cover Again more work is necessary to
sort out these responses
TY 6 GRID
A strong response caused by a shallow body 0 limited
depth extent is observed centred around 18N on the baseline This
would appear to be associated with a contact indicated by a
resistivity change at 17N
o
o
It would appear that a second possible deeper zone could
be associated with the higher resistivity at 16N
Another resistivity contact could exist at 8 5N
n
o
oo
Three possible anomalous zones are observed on Line lOWwith the southernmost two probably indicative of a background changeas the chargeability values are fairly consistent over some 500 metres
o GIWPHYSICAT SEUVICESI
I
o
oo
PWlEn E WAI corr ASSOC LlD
11
oo
o
o
SUMMARY CONCLUS IONS AND RECOMMENDATIONS
Between October 27th and November 22nd 1982 Peter E
Walcott and Associates Limited carried out reconnaissance I P
profiling over several soil sampling grids for Selco Inc over
their Timothy Lake properties Clinton Mining Division British
Columbia
Several anomalous zones worthy of further investigationof one kind or another are observed over the low chargeabilitybackgrounds
These zones are noted in the previous section
o
o
onJ
Although definition of these zones is sufficient on
GN 2 3 5 for investigation by diamond drilling further I P
work is necessary for better delineation of the rest of the I P
hopefuls
As a result the writer recommends that the results be
studied in conjunction with the limited geology the soil samplingresults and the results of the percussion drilling programme before
committing to further work of any description
o
Respectfully submitted
PETER E WA OTT AS OCIATES LIMITED
dQ J IhPeter E Walcott P Eng
Geophysicist
o
o
oonI
Vancouver
British Columbia
January 1983
n GEOPHYSICAT SI UVICJoS
n PETER E WAI COlT ASSOC LTDU
orl
ooo
oo
oo
o
c
o
oo
o
o
o
0
A P PEN D I X
GIWPlTYSICAI SEUVICES
nu
PElEU E WALcorr lit ASSOC LrD
Qo
oo
o
o
o
o
cr
i
COST OS SURVEY
Peter E Walcott Associates Limited undertook the
survey on a kilometre basis so that the total cost of services
provided was 29 770 10
o
on
o
oo
o
o GIWPHYSICAI SEUVICES
nIlJ
PETEn E WALCOn ASSOC LTD
ooo
o
Name
Peter E Walcott
tlI ILJ G MacMillan
oV A Paslniak
nu
F Von Flotow
o
o
J Walcott
rI
n
o
on
L
onL
n
11
PERSONNEL EMPWYED ON SURVEY
Occupation
Geophysicist
GeophysicalOperator
Typing
Address
Peter E Walcott Assoc605 Rutland Court
Coquitlam B C
V3J 3T8
Dates
Oct 27thNov 22nd 1982Jan 10 12 1983
Oct 27thNov 22nd 1982Nov 25 29th 82
Dec 12 20th 82
Oct 27thNov 22nd 1982
Jan 14th 1983
GEOPIIYSICAI SERVICES
nIIu
PETER E WALCOrr ASSOC LTD
oQ
o
o
Hi
CERTIFICATION
I Peter E Walcott of the Municipality of CoquitlamBritish Columbia hereby certify that
o 1 I am a Graduate of the Univeraity of Toronto in 1962 with
a B A Sc in Engineering Physics Geophysics Option
o2 I have been practising my profession for the last twenty
years
o3 I am a member of the Association of Professional Engineers
of British Columbia and Ontario
4 Ihold no interest direct or indirect in the Timothy Lake
properties nor do I expect to receive any
J oo
onu
o
o
o
o
o VancouverBritish Columbia
oJanuary 1983
n
o
o GEOPIIYSrCAL SERVICES
n f I f lJ lgy
0hLj I Ir 1 1
1 I i il Ir l II j l 1 Ii IO t
HI I 1 1O L 1 l jif IJ v L
i J
n 15 11
riI r rI
jF v jfn r I j i I0 i24 2
1q n L 22
yJ7
r I0 QJr
1 j 1 I rI
hr
L 1 117r t1jy I k I
c i o
rVf 1I r 2i i sO I I
IL J1
I
r IIt 56 I i
II
It rt 7f
J
Jr j r r0I
y c 7J N
rjy vrl 1 1 p c
L J t II
Jr y I
7
I 1 I
FI1Y v I gi b01 i lj 1
1db I I q S I 11 C r1 D I 1
1 I
y 1 J1
1li f7T 1 1 rh k I0 rl
Jcrv II J I
2 J
r q
b1 rnh rt f irf 2Lj r J I
f
I u 4 Ij
L15091
1 JI II I
Jnl 1
r i r 1 c1 Il 71
6 trY j 120
I
U
I l lAl r
1 1 h TI I
TIf r
2 Ll ji LJ rn 1 1 f t rJ I tir Jg i 1
TI
j il jh b r f
2t 1 1o 1q n II q T1
J i I 4I 1 ro X 2 p 1 21 r
r Io g Y it 4 ll 1I f C It
Lt yJo
9J
II1
lJ
it t OOO lI 91 c i
loJ rI
rI J6 l 00
Ii L I i
clrI i H 1
T II
I1 YCh
1011I 101 r
LI tI
I1 61
l rl 1L I uL
1Il
Ii I J
I J rr IL1
I CJj
I1 lI ftt Ll 11 0
IJ 1 li I
J
1
IJ
Ij it I ilr lcrt 6Q 1 rI 1 Lo l
II I
OI I
I
ir
iFI
I I c I i yeAI 1
q 1J I
LI T Y 7 L
1
f I
q 1
f
JI 8
yr R
rl T y1 7 I Jr JjI l I T
7 17o 1h L C P
Rod
y t r A lb 6 1
OL I if L X 1 f u
b ir VC I I i I
VtO ii
2y Y
I
I I S l I t J r1t 0J
O j I i 2 IlI IfA
i
r h
on
ll
4i
tL tI l ol 1 f
I N0 Ji 121 I r c l
I 1 I lA
o 1 J rx t t
1 i 1bfJ i 3o R
0r
I j1M 0 11 v IIl 1
O ILo I 1 C1 J Hl ef
jl n4 1
1 r J0 If 1
l
rT LQlrr
q r SJ r I
1 l 1
AI I 1 1
IIi I
Qo I I 3O 1 1
T
1J S2 J t Z2 1
4 3P r I0 06 OA
0 In 1 df ft If 1tJ A Y 1 N rNn o
J uft TioI O
B 1 C I
LJ fA AJ I D 1 I Pt1
rp Ltl 3 f rp
IJ1
1 Ip 3 I 1 J r iii f
1
i
Oo U 7 Iu 1 I
t7Ii
I I 1 so S I t 4 oc 1
l JI
1
ill i I MII
1kI v
II
jIS
t Li
1y
poUI
J i Jrj
1
cs
j
lcoy
I
00 I
cJ j
J I Ii I
l 1q r1 cr Jc I
j
7 cJi
ycy
11 J
13
r
0J
If
l
7J
l
I
Jl
J1 r r
s V
I
J
VG I I G
Lakef
I 1 lL Q tJ
l 1
L
AJ
Ix
0
Jv
1
C0
c 0w
of R n 11
11
N 3 j1
L
17 KIe
j r 2
Ud LfJmO
I
I
rlJG1i f
yf1
V
U
7
2lJ
J
I
I uII
fI rW
1
Cm
r lJI
I
G 7 f
U
1 nIl l f
I 19
fivl
1
t tojbC t
I
G Jl
1h
0
Vfjid n
h C
q I jd
y 11r1
sIII
y
f 1lI
n
7
fJl
c
I Itr r
JJI
lb
7
m IS I
Jc
II
r c5I15
r J
hI l
III
c
C
j
h
IiVv
i0
cRrJ Hf
A
v err
X r
y U
ifc d
I it
L ytjl
f 1l
1I Iach 9001
0
Ii
V
ih g
Hi II
j
I iJi
7
CpiOI
J YJ
L
iC
1 f5
1 l Sli
l C1
Jo
7
rt fc1ia lr
I
l
t h0c C
IJ 1 4 P 7I
f
1 11
I
i5
FlgU I
I Y 11 C J
UlC 1I0of
GO c 1S
v
0IOOO
T V 111I
j Ij
f
rmiI
I
11
Flhttd
Ifl fol
rL
h
lQttiNli
tj1iJ
r11
lH
tnL1
W1
3
LJ
0n
00
0
0
00
0
0
0
0
0
0
0iJ
I
j
DIPOLE DJPOLE ARRAY
I 0 no 0 J
rQ
IV
2
i
V4
r@
ANOMALOUS ZONE
11 1 POSSIBLE ANOMALOUS ZONE
t t tI
II
I
II
4
r b Ii
jI
I r j LI
1 lO j rc 7 T r1 I I I I
iJI i I J f Jo ljI I 1
n f
I
T y 4A J lL
OJ h I1
j Io CL
PH
1 0 7 rr
C 2g lI r
t I
I J L Tf 1 I p i Co
0 L1
I
t ir fLC e I
DI y I tr L
b
l af f11 fl I I
X II flU i Q
I h 1 I i
rD I 0
I I JIC I I1
1
n1 r t
I I j
1 I I
o JCi I
t
o s ql t I 1j
f 1 r illI
1 Il
Jt f i i
o t J 1 U Pfl bI
o ru l
I
t1 I
Ia
l c i f U III 1
nj o 1 l
F I fL i
L1 v i nI x J
C I w 1 Yl 1 1 c
o I I tJ I4
v
It Ir t I
lllO 0 1V co
1
91 p r10 1
Lf J L j
1
Ii J I Ir1Ti
I T k Epni
P ltl J L fiJ l
t t3 iJ f
UI l TI I I 4r I
i 1 j io
I Al 41 Iue
rV 1
J
oli
lJ
oo
oo
SECTION 3
A GEOPHYSICAL REPORT BY
PHOENIX GEOPHYSICS LIMITED
IILJ
JUNE 1983
n
c
Q
1L
o
o
orI
r
n
nlJ
o
Coo
o
PHOENIX GEOPHYSICS LIMITED
REPORT ON THE
INDUCED POLARIZATION
AND RESISTIVITY SURVEY
ON THE
TIMOTHY LAKE PROJECT
CLINTON MINING DIVISION
BRITISH COLUMBIA
oFOR
o
CDo
o
oo
c
j
SELCO MINING CORPORATION LIMITED
Latitude SlOS2 N Longitude 121018 W
N T S 92 P l4
OPERATOR SELCO MINING CORPORATION LIMITED
BY
Paul A Cartwright B Sc
Geophysicist
Dated
September 16 1983
nL1
o
o
0c
Doo
o
o
o
G
oo
o
PART A
1
2
3
4
5
6
7
8
9
PART B
PART C
o
oC
Q
o
TABLE OF CONTENTS
REPORT 11 pages
Introduction
Presentation of Data
Discussion of Results
Summary and Recommendations
Assessment Details
Statement of Cost
Certificate Paul A Cartwright B Sc
Certificate John Marsh
Certificate Peter Gardner
Notes on Theory and Field Procedure
ILLUSTRATIONS
Plan Map in pocket
1P Data Plots
Location Map
Dwg IP P B 4027
Dwgs IP 5832 1 to 15
Figure 1
PAGE
1
1
2
4
7
8
9
10
11
o
o
1
1 Introduction
on
An Induced Polarization and Resistivity survey has been completedon the Timothy Lake Project Clinton Mining Division British Columbiaon behalf of Selco Mining Corporation Limited
o
o
o
cc
The project area is located immediately northeast of the communityof Lac La Hache B C which is on Highway 97 Access to the
individual grids on the property is via gravel logging roads from
Highway 97
Previous work during 1982 included airborne magnetic surveyingIP and Resistivity surveying was then used to further evaluate anomalous
magnetic responses
Objective of the present IP and Resistivity survey was to providemore complete coverage over some of the anomalous IP zones outlined
during last seasons work
A Phoenix Model IPV 1 IP and Resistivity receiver unit was used in
conjunction with a Phoenix Model IPT l IP and Resistivity transmitter
powered by a 2 Kw motor generator IP effect is recorded directly as
Percent Frequency Effect P F E at operating frequencies of 4 0 Hz and0 25 Hz Apparent resistivity values are normalized in units ofohm meters while Metal Factor values are calculated according to theformula M F P F E x lOOO 7 Apparent Resistivity
D Dipole Dipole array was utilized to make the majority of themeasurements with a basic inter electrode distance of 50 meters
Four dipole separations were recorded in every case Number ofline kilometers surveyed during the present survey was 14 35 linekilometers
n
o
n
Field work was carried out during June 1983 under the supervisionof Mr John Marsh and Mr Peter Gardner geophysical crew leadersTheir Certificates of qualification are included with this report
2 Presentation of Data
G
o
u
The Induced Polarization and Resistivity results are shown on the
following data plots in the manner described in the notes Part B
following this report
Grid Line Electrode Interval
58 008 50 meters
62 008 50 meters
66 008 50 meters
76 008 50 meters
78 008 50 meters
79 00S 50 meters
Dwg No
GN 1 5832 1
5832 2
5832 3
GN 4 5832 4
5832 5
5832 6
o
o
cl
SELCO MINING CORP LTC
LOCATION MAP
TIMOTHY LAKE PROJECT
CLINTON M D B C
N TS 92P 14 SCALE 600 000 FIG
D2
i11
n
Grid Line Electrode Interval Dwg No
TY I I OOW 50 meters 5832 7
2 00W 50 meters 5832 8
TY 2 l OOE 50 meters 5832 91 00W 50 meters 5832 10
TY 5 1 00S 50 meters 5832 11
TY 6 200E 50 meters 5832 12
2 00W 50 meters 5832 134 00W 50 meters 5832 146 00W 50 meters 5832 15
CDnLI
nLAlso enclosed with this report is Dwg IP P B 4027 a plan map of
the Timothy Lake Project area at a scale of 1 20 000 The definite
probable and possible Induced Polarization anomalies are indicated bybars in the manner shown on the legend on this plan map as well as on
the data plots These bars represent the surface projection of theanomalous zones as interpreted from the location of the transmitter and
receiver electrodes when the anomalous values were m a ureaDj
UnJ
Since the Induced Polarization measurement is essentially an
averaging process as are all potential methods it is frequentlydifficult to exactly pinpoint the source of an anomaly Certainly no
anomaly can be located with more accuracy than the electrode interval
length i e when using 50 meter electrode intervals the position of a
narrow sulphide body can only be determined to lie between two stations
50 meters apart In order to definitely locate and fully evaluate a
narrow shallow source it is necessary to use shorter electrode
intervals In order to locate sources at some depth larger electrode
intervals must be used with a corresponding increase in the
uncertainties of location Therefore while the centre of the indicated
anomaly probably corresponds fairly well with source the length of the
indicated anomaly along the line should not be taken to represent theexact edges of the anomalous material
GnL
11
The topographical geologic magnetic and grid information shown on
Dwg I P P B 4027 has been taken from maps made available by the staffof Selco Mining Corporation Limited
G 3 Discussion of Results
o
c
Six separate grids lying within the Timothy Lake Project area have
been investigated by the present Induced Polarization and Resistivitysurvey and are shown on Dwg I P P B 4027
Results from each grid are discussed separately below
oIIU
D
Q
3
Grid GN l
o
Qf1I
Two anomalous IP zones are interpreted in the data acquired on the
three lines surveyed on this grid
D
Both zones are weakly to moderately anomalous with the more
western trend being open towards the west as well as to the north and
south The best defined individual anomaly occurs on the eastern IP
trend in the vicinity of Line 58 00S between station 36 00E and station37 50E Small concentrations of mostly disseminated material are the
probable source of these anomalous IP effects seen on Line 58 00S as
generally high apparent resistivity values are evident coincident with
the higher than background Per Cent Frequency Effect P F E values
While a narrow zone of lower resistivity material is evident near the
western margin of the zone it is not clear if more conductive
mineralization is present or if an ionic conductor such as a fault is
the causeCrL
Depth to the source of the IP response is indicated to be less than
50 meters in the case of the northern end of the east zone with the
zone apparently plunging towards the south Additional surveying would
be required to fully define the western margin of the second IP zone
G
G
en
Grid GN 4
The IP and Resistivity results recorded on the three lines from
Grid GN 4 are interpreted to show three separate weakly anomalous
trends all striking north south There is some uncertainty in this
evaluation due to the fact that the most westerly zone is undefined
along its western mar in
The highest magnitude IP response is noted on Line 76 00S
interval between station 5 50W and station 5 00W where a local
high exists set within a background of less anomalous values
the source in this case is less than 50 meters subsurface
in the
P F E
Depth to
rLGrid TY 1
nJTwo lines were surveyed on this grid area during the 1983 IP
program Strongly anomalous responses are evident in the data from both
lines In each case there appears to be a central zone of concentrated
mineralization surrounded by considerable widths of less sulphide rich
rock
r
U
oThe highest magnitude response is detected on Line 1 00W centered
on station 2 00N where depth to the target is less than 50 meters
subsurface
nL
Although the lines are orientated north east the core of the IP
zone may strike in a more northerly direction and appears to be more
deeply buried towards the south
IL1
D
DC
I
4
Grid TY 2
The most encouraging results Been in the IP data collected on this
grid are noted on Line 1 00E between station 1 00N and station 2 00Nwhere a moderately anomalous response is interpreted A flat lyingshallow conductive zone appears to cover the area between station 0 50Nand station 2 50N and may be caused by a superficial deposit such as
thick swamp However depth to the top of the polarizable material is
less than 50 meters
nu
rJ
On the second line Line 1 00W the IP response is much lessanomalous while displaying a more complicated signature Two separatenear surface sources are interpreted in the data
Grid TY 5
rI Line l OOS was the only line surveyed on Grid TY 5 during the
present IP program Two weakly anomalous responses are outlined by the
data The western anomaly consists of somewhat anomalous IP effects
accompanied by moderate magnitude apparent resistivity values situatedon the eastern flank of a very resistive rock unit which seems to be
hosting small amounts of disseminated sulphide judging by the
relatively high magnitude of the P F E values recorded within the highresistivity rock unit
on
e
On the eastern end of the line small concentrations of polarizablematerial are the probable source of the IP anomaly
Grid TY 6
r
l
One very anomalous IP zone is evident striking roughly in a
northwesterly direction It is seen in the data on all four lines
surveyed with the highest magnitudes being indicated on Line 2 00W
between station 0 50N and station 1 50N The source of the trend lies
within 50 meters of the surface on the three most northerly lines but
appears to be slightly deeper in the case of Line 2 00E as well as
being wider
o Although apparent resistivity values in the general area of the
anomalous IP effects seem to be quite low in absolute terms there does
not appear to be any clear correlation between the P F E patterns and
the resistivity patterns This suggests that the sulphide rich zone is
hosted by loosely consolidated or weathered rockserL 4 Summary and Recommendations
CThe Induced Polarization and Resistivity survey of six separate
grid areas within the Timothy Lake Project area has recorded anomalous
values in every area
nr
U
D
E
5
Grid GN I
i
UTwo anomalous IP zones are evident A drill hole located so as to
pass through a point 75 meters tinder Line 58 005 station 36 50E wouldtest the source of the eastern zone
DIU
Additional IP coverage is required to fully outline the westernmargin of the other zone before drill testing is considered
Grid GN 4
oAlthough three separate weakly anomalous zones are interpreted in
the IP data from Grid GN 4 only the center zone which is slightly more
anomalous than the others should initially be considered for drilltesting unless other information is available to recommend them Adrill hole spotted so as to intersect a point approximately 50 metersbelow Line 76 00S station 5 25W is suggestedr
nlJ
Additional IP and Resistivity surveying is needed to close off thewestern side of the most westerly zone
r
l
Grid TY I
uOne highly anomalous IP zone is detected on this grid
hole situated so as to pass approximately 75 meters beneathstation 2 00N is recommended to test the source of the most
response
A drill
Line I OOWanomalous
n
n1
Grid TY 2
L
One anomalous IP zone is detected on Grid TY 2 A drill holelocated to intersect a point approximately 50 meters under Line I OOEstation 1 75N would test the most anomalous response
Grid TY 5
n A single line was surveyed on this grid and two weak IP anomaliesare noted in the data The western response could be drill evaluated on
a low priority basis by a drill hole spotted to pass approximately 50meters beneath station 10 85W on Line I OOSc
Additional IP and Resistivity surveying using shorter electrodeintervals is recommended to better define the source of the eastern
anomaly before drilling is considered
nJ I
fl
c
n6
riL Grid TY 6
u
n
A very anomalous IP zone is outlined by the data from this grid A
drill hole located so as to intersect a point approximately 50 meters
below Line 2 0 station 1 00N is recommended
c
on
nL
PHOENIX GEOPHYSICS LIMITED
UJJ LIAPaul A Cartwright B Sc
Geophysicist
Dated September l6 1983
c
nn
CLI
orr
U
r
o
Dn
I
j
c7
nU ASSESSMENT DETAILS
U
rL
l
PROPERTY Timothy Lake Project MINING DIVISION Clinton
SPONSOR Selco Mining Corp Ltd PROVINCE British Columbia
LOCATION Lac La Hache B C
nu
TYPE OF SURVEY Induced Polarization
and Resistivity
liJ i
OPERATING MAN DAYS 27 DATE STARTED June 8 1983
EQUIVALENT 8 HR MAN DAYS 40 5 DATE FINISHED June 19 1983
CONSULTING MAN DAYS 4 NUMBER OF STATIONS 302
DRAFTING MAN DAYS 6 NUMBER OF READINGS l716
TOTAL MAN DAYS 50 5 KILOMETERS OF LINE 14 35
SURVEYED
r1ILl
rU
cCONSULTANTS
Paul A Cartwright 4238 W 11th Avenue Vancouver B C
n
LrlIL1
FIELD TECHNICIANS
J Marsh 200 Yorkland Blvd Willowdale Ontario
P Gardner 393 Connaught Avenue Willowdale Ontario
G Richardson 4161 C own Crescent Vancouver B C
DRAUGHTSMEN
R C Norris 2499 Linwood Street Pickering Ontario
o
cPfZG1f J iPaul A Cartwright B Sc
Geophysicist
fDated September 16 1983
crLr
n1
rl8
iiI
Li
USTATEMENT OF COST
Selco Mining Corporation Limited
onu
Induced Polarization and Resistivity Survey
Timothy Lake Project Clinton M D Lac La Hache B C
Crew J Marsh P Gardner G Richardson
Period June 8 1983 to June 19 1983
n14 35 lkm @ 780 00 lkm 11 193 00
IjL
Cf
Drv
PfiE1S2fLEPaul A Cartwright B Sc
Geophysicist
G
Dated September 16 1983
oru
1i
cG I
II
I
iI
I
II
Qfl
1u
n
o
oD1
u
u
p
1
9
CERTIFICATE
I Paul A Cartwright of the City of Vancouver Province ofBritish Columbia do hereby certify that
1 I am a geophysicist residing at 4238 W 11th Avenue
Vancouver B C
2 I am a graduate of the University of British Columbia B C
with a B Sc Degree
3 I am a member of the Society of Exploration Geophysicists and
the European Association of Exploration Geophysicists
4
5
I have been practicing my profession for 13 years
I have no direct interest directly or indirectly in the
properties or securities of Selco Mining CorporationLimited or any affiliate
6 The statements made in this report are based on a study of
published geological literature and unpublished privatereports
7 Permission is granted to use in whole or in part for
assessment and qualification requirements but not for
advertising purposes
DDated at Vancouver B C
This 16th day of September 1983 fJJ 4 aL 0Paul A Cartwright B Sc
nJ
G
c
U
c
nDrhi
II
10
rJI
ro
iCERTIFICATE
nLJ
nu
I JOHN MARSH of the Municipality of North York OntarioNorth York Ontario DO HEREBY CERTIFY THAT
l I am a geophysical crew leader residing at
200 Yorkland Blvd Willowdale Ontario
r
Lli
L
2 I am a graduate of the City of Norwich Technical CollegeU K ordinary National Certificate Electrical Engineering
rLJ
3 I worked with McPhar Geophysics Company from 1968 to
1975 as a geophysical crew leader
r4 I am presently employed as a geophysical crew leader by
Phoenix Geophysics Limited of 214 744 West Hastings Street
Vancouver B C
Dn
J
Dated at Vancouver B C
This 16th day of September 1983 L ft1afJohn Marsh Ir
n
onJ
G
Qo
nrd
11if i
o
oCERTIFICATE
nL
I Peter Gardner of the City of Toronto Province ofOntario DO HEREBY CERTIFY THAT
o1 I am a geophysical crew leader residing at
393 Connaught Avenue Willowdale Ontario
U 2 I am a graduate of Radio College of Canada inElectronics Technology
r11 3 I have been practicing my vocation about six
years
ru
r
D
4 I am presently employed as a geophysical crew
leader by Phoenix Geophysics Limited of 214 744 West HastingsStreet Vancouver B C
Dated at Vancouver B C
nThis 16th day of September 1983 PJ
Peter Gardner
1LJ
Cn
n
rt
L
j
onu
DnL
PART B
o PHOENIX GEOPHYSICS LIMITED
rjL
nI I
NOTES ON THE THEORY METHOD OF FIELD OPERATION
AND PRESENTATION OF DATA
I
FOR THE INDUCED POLARIZATION METHOD
c Induced Polarization as a geophysical measurement
nLJ
refers to the blocking action or polarization of metallic or
electronic conductors in a medium of ionic solution
Go
Dn
conduction
This electro chemical phenomenon occurs wherever
electrical current is passed through an area which contains
metallic minerals such as base metal sulphides Normally when
current is passed through the ground as in resistivity measure
ments all of the conduction takes place through ions present
nL
in the water content of the rock or soil i e by ionic
conduction This is because almost all minerals have a much
Qr
higher specific resistivity than ground water The group of
minerals commonly described as metallic however have
specific resistivities much lower than ground waters The
Ginduced polarization effect takes place at those interfaces
where the mode of conduction changes from ionic in the solutions
riU
filling the interstices of the rock to electronic in the
metallic minerals present in the rock
rJL2
The blocking action or induced polarization mentioned
oabove which depends upon the chemical energies necessary to
allow the ions to give up or receive electrons from the metallic
1L
u
nu 2
o
oo
surface increases with the time that a d c current is allowed
to flow through the rock i e as ions pile up against the
metallic interface the resistance to current flow increases
Eventually there is enough polarization in the f rm of
excess ions at the interfaces to appreciably reduce the amount
Jof current flow through the metallic particle This
polarization takes place at each of the infinite number of
o
oQ
D
solution metal interfaces in a mineralized rock
When the d c voltage used to create this d c
current flow is cut off the Coulomb forces between the charged
ions forming the polarization cause them to return to their normal
position This movement of charge creates a small current flow
which can be measured on the surface of the ground as a decaying
potential difference
nJ
nLJ
From an alte nate viewpoint it can be seen that if the
direction of the current through the system is reversed
repeatedly before the polarization occurs the effective
Cnu
resistivity of the system as a whole will change as the frequency
of the switching is changed This is a consequence of the fact
that the amount of current flowing through each metallic inter
J
or
face depends upon the length of time that current has been
passing through it in one direction
The values of the per cent frequency effect or F E are
a measurement of the polarization in the rock mass However
since the measurement of the degree of polarization is related
to the apparent resistivity of the rock mass it is found that the
o metal factor values or M F can be useful values
nw
D
oo
3
determining the amount o polarization present in the rock
mass The MF values are obtained by normalizing the F E
ovalues for varying resistivities
The Inducep Polarization measurement is perhaps the
n most powerful geophysical method for the direct detection of
o
oI
n
metallic sulphide mineralization even when this mineralization
is of very low concentration The lower limit of volume per
cent sulphide necessary to produce a recognizable IP anomaly
will vary with the geometry and geologic environment of the
source and the method of executing the survey However sulphide
mineralization of less than one per cent by volume has been
detected by the IP method under proper geological conditions
UThe greatest application of the IP method has been
in the search for disseminated metallic sulphides of less than
n120 by volume However it has also been used successfully in
the search for massive sulphides in situations where due to
r source geometry depth of source or low resistivity of surface
layer the EM method cannot be successfully applied The ability
on
to differentiate ionic conductors such as water filled shear
zones makes the IP method a useful tool in checking EM anomalies
which are suspected of being due to these causes
In normal field applications the IP method does not
differentiate between the economically important metallic minerals
nL such as chalcopyrite chalcocite molybdenite galena etc
j and the other metallic minerals such as pyrite The Induced
Polarization effect is due to the total of all electronic
rU conducting minerals in the rock mass Other electronic conducting
c
n
nI
4
materials which can produce an IP response are magnetite
o pyrolusite graphite and some forms of hematite
ILIn the field procedure measurements on the surface
oo
c
are made in a way that allows the effects of lateral changes
in the properties of the ground to be separated from the
effects of vertical changes in the properties Current is
applied to the ground at two points in distance X apart
The potentials are measured at two points X feet apart in
Gline with the current electrodes is an integer number n times
the basic distance X
The measurements are made along a surveyed line with
nu a constant distance nX between the nearest current and potential
uelectrodes In most surveys several traverses are made with
various values of n i e n 1 2 3 4 etc he kind
n of survey required detailed or reconnaissance decides the number
o
o
o
of values of n used
In plotting the results the values of apparent
resistivity apparent per cent frequency effect and the apparent
metal factor measured for each set of electrode positions are
plotted at the intersection of grid lines one from the center
nL
point of the current electrodes and the other from the center
point of the potential electrodes See Figure A The
oresistivity values are plotted at the top of the data profile
above the metal factor values On a third line below the
M
U metal factor values are plotted the values of the percent
frequency effect The lateral displacement of a given value is
o determined by the location along the survey line of the center
nw
rL
oo
oo
oC
D
o
5
D
point between the current and potential electrodes The
distance of the value from the line is determined by the
distance nX between the current and potential electrodes
when the measurement was made
The separation between sender and receiver electrodes
is only one factor which determines the depth to which the ground
is being sampled in any particular measurement The plots then
when contoured are not section maps of the electrical properties
of the ground under the survey line The interpretation of the
results from any given survey must be carried out using the
combined experience gained from field results model study
results and the theoretical investigations The position of
the electrodes when anomalous values are measured is important
in the interpretation
In the field procedure the interval over which the
potential differences are measured is the same as the interval
over which the electrodes are moved after a series of potential
readings has been made One of the advantages of the Induced
Polarization method is that the same equipment can be used for
both detailed and reconnaissance surveys merely by changing the
distance X over which the electrodes are moved each time In
the past intervals have been used ranging from 25 feet to 2000
feet for X In each case the decision as to the distance X
and the values of n to be used is largely determined by the
expected size of the mineral deposit being sought the size of
the expected anomaly and the speed with which it is desired to
progress
on
o
oCnL
o
o
o
r
L
Q 6
riI ILJ
The diagram in Figure A demonstrates the method used
in plotting the results Each vaiue of the apparent resistivity
oo
oc
oo
apparent metal factor and apparent per cent frequency effect
is plotted and identified by the position of the four electrodes
when the measurement was made It can be seen that the values
measured for the larger values of n are plotted farther
from the line indicating that the thickness of the layer of
the earth that is being tested is greater than for the smaller
valUeS of n i e the depth of the measurement is increased
The IP measurement is basically obtained by measuring
the difference in potential or voltage b V obtained at two
operating frequencies The VOltage is the product of the current
U
o
o
through the ground and the apparent resistivity of the ground
Therefore in field situations where the current is very low
due to poor electrode contact or the apparent resistivity is
very low or a combination of the two effects the value of
AV the change is potential will be too small to be
numeasurable The symbol TL on the data plots indicates this
situation
o In some situations spurious noise either man made
or natural will render it impossible to obtain a readingrI i The symbol N on the data plots indicates a station at which
it is too noisy to record a reading If a reading can be obtained
oo
but for reasons of noise there is some doubt as to its accuracy
the reading is bracketed in the data plot
In certain situations negative values of Apparent
o Frequency Effect are recorded This may be due to the geologic
nL
Q
n
oo
7
environment or spurious electrical effects The actual negative
frequency effect value recorded is indicated on the data plotj
however the symbol NEG is indicated for the corresponding
value of Apparent Metal Factor In contouring negative values
nL
the contour lines are indicated to the nearest positive value
oin the immediate vicinity of the negative value
The symbol NR indicates that for some reason the
QnJn
operator did not attempt to record a reading although normal
survey procedures would suggest that one was required This
may be due to inaccessible topography or other similar
reasons Any symbol other than those discussed above is unique
to a particular situation and is described within the body
oof the report
nU
PHOENIX GEOPHYSICS LIMITED
o
o
U
o
onu
o
rl
0rjlJ
o
o
onL
o
c
n 4
n 3
n 2
n I
c
c
o
oo
METHOD USED IN PLOTTING DIPOLE DIPOLE
INDUCED POLARI2ATION AND RESISTIVITY RESUL TS
x 7 nx re x
r0l 1
2 3 4 5 6 7 8 9
Stations on lins x Electrods sprsad lenothn Electrode ssporation
p p P1 2 6 7 2 3 7 8 3 et9
p p p P1 2 5 6 2 3 6 7 3 4 7 8 4 5 8 9 Apparsnt Rssistjvity
p P P P P1 2 45 2 3 5 6 3 4 6 7 4 5 7 8 56 8 9
P P P P P1 2 34 2 3 4 5 3 4 56 4 5 6 7 5 6 7 8
9
n I M F M F M F M F M F M F1 2 3 4 2 3 4 5 3 4 5 6 4 5 67 5 6 78 67 6 9
n 2 M F M F M F M F M F1 2 4 5 23 5 6 3 4 6 7 4 5 7 8 5 6 S 9
n 3 M F M F M F M F1 2 6 2 3 6 7 3 4 7 8 4 5 8 9 Apparent Mstal Factor
n 4 M F M F M F1 2 6 7 2 3 7 8 3 4 8 9
o n
on 2
n 3
n 4
nJ
o
o
y yyF E F E F E F E F E F E
1 2 3 4 2 3 4 5 3 4 5 6 4 5 6 7 5 6 7 8 6 7 8 9
F E F E F E F E F E1 2 4 5 2 3 5 6 3 4 6 7 4 5 7 8 5 6 8 9
FE FE E El 2 5 6 2 3 6 7 3 4 7 8 45 8 9
F E F E F E1 2 6 7 2 3 7 8 3 4 8 9
9
Apparent Pereent
FrsQuency Effsct
Fig A
1
cJr1
J
J
J
CJ
r1
Cl
cJ
CJ
SELCO
TItlOTHLAKEGll
1
59HHlS
x
5tH
RHO
OHMH
35HIE
370eE
3geaE
380lJE
3660E
Ilea
1449
2
IIII
IIS
N
o
r
J
Cl
LJf1
t
N
2
N
3
t1
04
H
oL
jjijtuH
R
OORQltlATE3400E
I
JJJ
EEPED
lcQ
1
1
1
2
V
2
7
3
I
1
6
1
4
11
2
1
2
4
26
1
3
2
3
1
2
26
2
5
26
21
2
1
IA
M
U
U
M
IS
3900E
SELCOTIMOTHYLAkEGH
I
58
009
X
SOH
FE
3S00E
3700E
380tlE
ODeE
4HIOE
112
11
3
1
1
7
Il
5
2
1
1
12
3
1
I
1
1
H
2
1
3
2
1
I
1
1
3
16
1
2
1
6
1
1
Jl
ot
11
5
H
11
6
11413
H1130e
100E
6
3600E
HlOE
ii
ii
39130
SELCO
TIMOTHLAKEG
I
58
13139
nYbLllEl
I
L
9QU1
Qt
LOE
3
M
L
2
I
2
9
2
2
1
I
11
2
3
1
9
1
6
1
5
1
1
r34
3
23
1
6
1
1
1
1
2
2
I
@d
I
2
CJI
12
14
19
2
9
1
1
23
2
2
2
6
2
3
22
14
13
1
2
X
SOH
METALFACTOR
3800E
115
II
L
000E
IQ
E
QJ
9
9
1
2
1
1
i6
9
It
I
11
2
H
J
II 11
6
Cl
Cl
1
J
rJ
CJ
cJ
olle
NO
1
P
59121
SELCOlItHHGCORP
TIMOTHYLK
PROJIGIIl
GPI0
C
LIIlTOtlH
0
IB
C
LitlENO
S9lillJS
X
lfX
PLOTT1
HG
POINT
l
1
SURFACEPPOJECTIOIIOF
AIIOHALOUZlIlE
OEFIIlITE PROBABLEUIIIIII
POSSIBLE
FREQUEHCYHERTZ
ed
25
DATESUIlVeVEo
JUIl
193
3
APPPQVEO
HOTE
COHToURS
AT
lOCflRITHI1IC
ItlTERIJALSt
I
Z
3
7
5
18
T1 S61T
681
DATE
PHOEHIXjEOPHYSICS
LTO
INDUCEDPOLAPIZRTIOtl
PlHoPEStSTIVTTVSU
VE
l
J
L
1
1
I
J
CJ
CJ
cJ
o
CJ
C
J
Cl
CJ
CJ
CJ
cJ
J
1
r
1
U
c1
SELCOTIHOTHLRKE011
1
LEi2ololtl
X
SON
RHO
OHI
M
HIG
110
I
59322
CjijROIHATE
34llJE
35lOE
360UE
3700E
3800E
3
OeE
IHTEPFRETATI
011
1
r
1
1
11
1
S8
3
61
H
2
96Yll06
535
II
3
eee
IJe5
1053
1202
e
1
11
1131
12e
897
850
oeOE
10tE
JIS
tl
6
3sa
0
II
I
313
201
287
H
21
SELCOt1I1INGCORP
97
291
258
27
tl
3
TIMOTHYLie
PPOJCII
l
iPtO
oIeG
3
1
277
H
CLIIITOtlH
o
Ie
c
11
5
H
6
LINE110
62
US
SELCOTIHOTHYLRkEGH
l
L62ees
3QM
peE
X
H
X
O
J
X
0M
oHOLEilUM
I
2
I
3
OOROIHATE3400E
35eOE
J600E
J
ITERPRETATI
ot 5
I
a
I
11
2
2
1
1
7
6
1
1
8
3
2a
a
3
1
3
S
11
617
1f1
fOOOI
T00E
3ieOE
38JOE
J9lJlE
x
a
t1
1
3p
7
a
H
2
11
3
21
2
1
t
e
8
1
1
a
tl
04
H
PLOTTIHC POUlT SURFACEPROJECTIOHOF
AIIOHALOIJSZOIlE
DEFIllITE PROBPlBLE
11111
POSSIBLE
11
1
1
I
fSr2
2
2
2
7
III
G
6
6
2
6
1
1
1
1
16
804
39
Lf2
2
2
2
22
W
1
5
2
a
I
2
5
It
5
14
2
1
1
2
5
2
1
35
s
2
7
3
2
9
tl
I
U
2
FPEQUEHCYHERTZ
DATESUkUEYEOJlJtl
1961
04
e
0
25
RPPPOUEO
tlOTE
COtlTOURS
t1Jc
AT
LOGARITtlHIC IHTEPALS
1
1
56fT
6
0
2
3
5
75
11J
lATE
9ELCOTIMOTI
LAkECll
l
LG20es
tIUMBIfi
12
I
COORDINATE3400E
3S00E
7
X
OM
METALFACTOR
3600E
3700E
3eOOE
3900E
040tOE
E
112
l
3
H
PHOENIXGEOPHYSICSLTD
114
11
04
Ih5
H
I
UOUCEO0
LRRI
ZAT1011
HD
REsrSTIIlYSUIlUEV
H
H
Cl
cJo
cJ
CJ
CJ
CJ
CJ
CJ
SELCOTIMOTHYLAkEGH
l
L660es
X
SON
RHO
OHMH
OLe
NUtIBlnCOORDINATE
3400E
I
lTERPPETATIOH
tI
l
513
11
2
7eeE
3aeeE
3sa0E
360eE
3900E
tl
3
367
o
CJ ooeE
4
Jao
3
e
as
588
0413
04013
J89
519
oC7l
9
421
532
523
oJJ
317
6
394
za6
2
0
20472
1
225
s
5B7
5
11
6
204
L
I
CJBE
H
I
H
2
H
3
H If H
uaOE
HI0E
5ELCOIINOTHY
LAKECH
I
L66
0S
X
SUM
PFE
lPOLEHUMB
COORDINATE304llE
3S00E
IITERPPETATIOU 111
t
E1
1
7
1
9
I
2
3J
1
2
8
u
a
2
6
2
2
1
a
II
2
2
2
6
2
1
11
5
11
6
8013
360l3e1
6
I
5
I
a
1
7
I
1
1
2
U
1
1
e
1
6
1
611
18Y
2
22
2
6
22
2
fIJ2i15
15
aeBE
1
1
y
7
1
1
1
1
1
e
11
1
1
1
3
H H
2
H
3
fl 11
5
H
1
2
SElCOTIMOTIY
LAkEGN
L66OOS
X
SOM
tlETRLFACTOR
lE
iIUHB
CO
ROIHA1Et
I
II
I
3400E
J500E
3600E
3700E
H
2
3
7
S
V
3
04
7
2
22
2
3
1
04
8
A
i
5
3
2
3B
5
7
14
3
6
9
2
1
4
9
3
33
04
2
6
39
32
3
B
7
3
3
3
tl
3114
1
5
tl
15
22
35
04
04
8
7
04
3
4
9
7
2
H
l
H
2 3
H u H
L
J
1
CJ
rloc
JO
G
NO
I
e323
SELCOlINH1GCORP
TIMOTHYLtc
PftOJGN
GRIQ
CLINTOIIM
0
J
B
C
l
II
r 0
PLOTTING POINT
L1I1EHO
66
es X
50tt
SURFACEPROJECTIOIIOF
ANOMRLOUSZONE
DEFUIITE
PROBABLE POSSI
BLE
F
EPUEHCVHERTZ
04
0J
2
HOTE
CONTOURSAT
LDCfIIRITHMIC INTERVflLS1
1
5
2
3
5
7
11
DATESU
VEVEDJUN
191B
APPPOVED DATE
J3Js SePT
o7
3ee0E
3900E
04000E
04
PHOENIXGEOPHYSICSLTD
INDUCEDPOLARIZATION
AHDRESISTIVITVSURVEY
l
J
I J
J
CJ
LJ
rl
SELCOTIMOTHY
LAkECH
4
L
6
ges
so
octlTiJH
COOROIIArE
eo
w
r
IIT
EPfEUBL1lllL
t1I
5
4
615
354
S63
697
213
433
587
5
3014
191
621I7
0011
600i
534
56
lIc
3
97
t13
792
7
76
7iS
1l
4
Il
5
t1
S
CJ
CJ
C1
o
CJ
CJ I15
1
eOI
252
11
2
tl
3
H
4
U
S
SELCOTIMOTHYLA
E
CII
4
L7600S
COOROlliATEeOOI
fIjijTf
6001
JllLEPPP
ETATJONI
I
29
25
2
2
a
2
6
N
2
2
z
a
27
ZZ
1
5
33
H
3
1
5
27
2
3
2
1
2
7
3
4
2
11
4
1
13
1
7
1
02
5
27
3
13
3
5
1
5
t1
6
RHO
OHI1M
4sew
30W
O
10
In
stl6
385
306
xse1
E
SELCOTIMOTHYLAKECH
4
L7600S
Y
S011
5JH1W
41jll1
30lW
e0lJ
3
3
2
5
4
1
3
3
2
3
28
8
2
6
3
2
1
2
5
2
9
3
I
3
I
l023
25
27
1
2
6
rj
METALFACTOR
POLE
NUrHjER
t
2
I
1
I
4
lOOR
T
1UIII
Il
203W
II
I
52
5
4
39
3
3
6
3
2
3
4
4
2
3
H
2
3
4
3
3
3
3
Z
Z
3
29
47
V32
Ho
S
2
62
3
9
32
3
4
32
4
3
2
3
3
2
4
26
3
2
33
U4
4
3
3
3
39
36
2
4
33
3
1
46
2
5
jj
IlIIL
LJ 10eW1
1
U
Z
H
3
t
4
Il116
cJt
1
H H
l 2
H
3
H
4
t
J
1
J
CJ
C1
D
IG
110
r
I
58324
SELCOt1HlItlGCORP
TIHOTHYLIC
PROJ1N
f
GRIt
CLIHTOHtI
0
I
El
t
LitlE110
6
0135
X
H
H
X
PLOTTING OUIT
X
lIH
SURFACEPROJECTlOHOF
AUQMALQUSZQUE
DEFIIUTE PROBABLElu
lIlrUI
POSSIBLE
FREQUENCYHE
TZ
4
0Je
25
DATE
SURE
ED
JIJll
iSI3
RPPROVED
ttOT
CQIHOUIIS
FIT
l
aGft
flTIlHIC
IHTEPUftLS
1
l
2
3
5
7
5
10
m 56fTt83
DATE
PHOENIXGEOPHYSICSLTD
IIIDUCEOPDLftFIZATIQIl
RUORESISTIVITVSUIllEY
CJ
ClOCl
lJ
11JC
cJ
cJ
1
J
C
CJ
CJ
60011
00
SELCOTIMOTHYLRkECII
L7aOOS
X
HIM
RHO
OHNM
oCOOiffiTjATE
8001
EBEUATIOH11
1
40571
tot
11
2
325
11
sse
11
3
301
I
746
H
3Sl0
441
61S
70Ellol
50ew
40014
oou
0
7
173
1O
3
94
459
409
513
741
600
1256
1250
9133
99S
Gae
304
650
525
474
632
HI80
1
53
8Y9t91
30
697
619
IDS
818
Jlil45
895
72e
SJ
35S
93
115
H
6
1
1
11
2
I
J
11
4
H H
SELCOTIMOTHYLAkECII
4
L7S00S
PFE
X
SOM
COORDlHATE
BllOW
70ell
600101
50011
480101
3DtW
290
IIHEPPPETATIOII
T
T
T
t
1
7
2
3v2
6
1
9
11
2
1
8
22
2
5
31
3
3
26
1
1
13
2
3
1
e
tI
3
2
1
2
26
26
2
26
3
28
22
81
3
3
3
23
4
1
9
2
7
131
3
3
2
B
iS26
27
25
1
8
11
1
6
33
115
II
H 11
2
H H H H
ifiii1B
COOROItIATE80014
700
7
2001
SELCOTINQTHYLA
E
CH
4
L7se0S
50N
METALFACTOR
4lHlW
a00lol
6lt1
500101
1111
2
H
3
I
115
H
6
2
2
25
2
vJ
7
W
4
3
4
U
U
6
1
U
Y
4
U
24
2Ky
9
5
6
1
J
U
U
u
7
H
l
H
2
u
a
11 f1 H
cJ
CI
cJ
cJ
CleFCJ
OWC
NO
I
P
58J25
SELCOt1INItG
CORP
TIMOTHYLK
PROJJCH4
CP10
l
NX
X 0x
nOTTINC POIHTCLINTON11
D
IB
C
LItlEHO
79
0tlS X
StH
SURFACEPROJECTIOHOF
AHOHfIllOUZOHE
DEFIHITE PROBABLEIIIIIUO
UU
paSSElLE
FPEQUEHCYHERTZ
0JfI2
UOTE
CONTOURSAT
lOCIRITHI1IC IHTERVIlS
I
IS
2
J
S
7
S
Ie
DIII1ESURJEYEDJII
tot
1
3
RPPPOUED
DRTE56PT
tIS
PHOENIXGEOPHYSICSLTD
INDUCEDPOLRRIZRTION
RNDREStS1I
VITVSURVEY
CJ
l
JOJ
o
l
J
cJ
L
J
CJ
J
CJ
CJ
cJ
SELCOTIMOTHYLAKEGH
L790eS
RHOCOHNH
l
el
X
SOI1
OIPOlEHUtlBER
12
I
3
I
I
5
I
I
I
13
I
9
I
I
t
I
COORDINATEacow
700101
60014
50011
HHIW
300
20
INTEFPRETATIOI
1
T
1
I
3013
g19
0404
ce2
905
528
Gl
1
376
312
325
112
41
Gi5594
563
553
739
eV664573
673
39
25g
H
3
373
3S
337
7138iS
6ca
7G
661
tj
352
11
4
33
47j
04
5
915
132
4
5Ei3
feelIiMi
970fiiS
5S5
719
501
U5
11
6 SELCOTIMOTHVLAKECH
4
L7900S
X
SOM
PF
i
leOH
QhDN COORDINATE PPPETRTH
e
400U
200ll
toow
60
101
500101
11
2
80014 H
I
1
2
1
7
1
2
1
1
1
9
1
13
2l5
2
1
1
6
VI
1
7
2
3
2
6
24
1
1
1
U
M
M
IA
1
I
IS
1
B
1
M
lS
2
1
27
2
1
2
3
19
I
a
21
2
1
9
12
2
2
I
a
7
IOJ
3
11
4
I
5H6 SELtO
TI
OTHYLAKECII
L7l
OOS
METALFACTOR
10014
X
5111
LE
t1UlBEP
COORDIIIRTE
snlW
700W
5
6
I
I
I
9
I
I
1
fOCW
SOOW
40lB
30tlll
2001
11
1
11
2
4
7
J
S
2
7
25
2
1
6
1
5
3
3
y
3
3
5
S
55
4
23
25
28
2
5
26
r6
1
4
4
6
04
7
04
62
22
2
2
J
32
3
1
2
1
5
7
5
9
2
5
26
29
3
1
26
1
9
22
4
3
J6
1
6
Il H H H
l
I
H
l
11
2
11
3
11 11
5
11 II
I
11
2
H
3
I1l leiS n
I
H
2
11
3
11
4
N H
iS
LJ
CJ
ClCrcJ
CJ
owe
tlO
J
P
51326
SELCO1IHIHG
CORP
TIMOTHVLK
PROJell
e
lo
CLINTONH
D
JB
C
LIIIENO
7
HS
X
HX
X
PLOTTr
HG
POIIIT
5
H
SU
FACEPROJECTJOHOF
AHortALOUSZONE
OEFIHITE PP08ASLEII
UIIIUIII
POSSIBLE
FREQUENCYHERTZ
4
0J0
25
DPlTESURVEVEIHI
19133
F1
PPOVED
HOTE
CONTOUS
AT
LOGARITHMIC INTERVALS1
1
5
2
3
5
7
5
10
56Pr
83
DATE
PHOENIXGEOPHYSICSLTO
INDUCEDPOLAPIZATIOII
AHD
ESITIVtTYSU
UEV
I
@ECTI0N 1
PERCUSSION DRILL PROGRAM
i
J
i
U
D
I
0C
D
Q
0nu
Q
0n
0OJ Q LOS
fN 0L OS
rJ
o
o
o
o
IAu ANOMALY
SlbGdd 3
0
0 1
nJII
1IIII
III
II
o
o
o
o
oI
III
IIII
I
IIItIII
1I
II
II1
o
o
o
Q
o
GN 4N 1
CN 1
IONqqN r
OHtNN J
ION UNIO
Sub Grid I
I
GN 5
GN 7
GN 8
L 20 S
L30S
QY Lok
5
L50S
ONGN
OH6N S
OH6N I4
tN S
DH N S
Au AMJMALY
Leos
C
I
II
G ny Ok
EXPLORATIONSELCO InC WESTERNCANAllA
o PERCUSSION DRILL HOLES
I p CONDUCTORS NOVSZ SoMEY
oo
o
o
rimothy
Lak
THE G N GRIDTIMOTHY LAKE AREA B C
9
Scale I 50 00OIl H IV OAT H T S
1P 1FIGURE
fIIlAC 0 Y 3J S JULY I n
I
IJ
II
i
PERCUSSION DRILLING
o
o
o
o
o
o
During the period November 19 1982 through to December 17
1982 sixteen 16 percussion drill holes totalling 2555 feet
779 m were completed to test soil geochemical anomalies that
had been previously outlined in earlier surveys
In addition during the period May 26 1983 through to May 30
1983 four 4 percussion drill holes totalling 800 feet
244 m were completed to test Induced Polarization anomalies
outlined in the November 1982 I P survey Drill hole locations
are tabulated in a summary table and drill hole collar locations
are shown on the accompanying GN Grid plan Fig 3
IU
o
o
o
on
Summary Table
Sub GeochemicallyP D H grid Coordinates Dip T D Elevated Values
GN 82 1 2 L36 00mSj 6 00mW 900 1201 AsGN 82 2 2 L32 00mSj 8 00mW 90 100GN 82 3 2 L28 00mSj 8 00mW 90 1651 AuGN 82 4 5 L28 00mSjlO 50mE 90 200GN 82 5 6 L12 00mSj10 00mE 90 200 CuGN 82 6 7 L2 00mS j 9 00mE 90 200 CuGN 82 7 7 L4 00mS 12 00mE 90 200 CuGN 82 8 2 L32 00mSj 3 00mW 90 1801 AsGN 82 9 2 L40 00mS 2 00mW 90 180GN 82 10 2 L42 00mS 3 00mW 90 180GN 82 11 4 L76 50mSj 4 50mW 90 190 I Ag AuGN 82 12 4 L77 50mS 4 50mW 90 110 Ag AuGN 82 13 1 L63 00mSj31 00mE 90 150 AgGN 82 14 1 L64 00mS 33 00mE 90 200 Cu Ag As Au Pb ZnGN 82 15 1 L62 00mSj33 00mE 90 80 AgGN 82 16 1 L59 00mS 33 00mE 90 100 AgGN 83 1 2 L40 00mSj 1 00mW 90 200 AgGN 83 2 2 L36 00mSj 4 50mW 90 200 Ag AsGN 83 3 3 L32 00mS 12 50mW 90 200 AgGN 83 5 1 L64 00mSj 3 50mE 900 200 Cu Ag
lJ
I
l
J
f
no
oo
o
o
o
o
o
o
o
o
o
D
A record of each hole was constructed on a wooden slat by
washing and sieving a portion of each drill chip interval The
cleaned and dried recovered coarse fraction was then glued to
the appropriate scaled off intervals on the grooved slat The
log chip boards for each hole were then examined under a bino
cular microscope and logged Accompanying this report are drill
logs for each percussion hole
DRILL RESULTS
The drill holes returned low uneconomic values for copper
silver arsenic gold lead and zinc There are however
elevated geochemical responses that offer some encouragement
The maximum concentrations from all holes are 276 ppm copper
25 0 ppm silver 67 ppm arsenic 120 ppb gold 750 ppm lead
and 382 ppm zinc The elements that are geochemically elevated
in each hole are tabulated in the summary table
The following holes offer the best results
Q
o
o
P D H
GN 82 6 140 ppm Cu over ISO 50 200
GN 82 7 135 ppm Cu over 40 150 190 I
GN 82 11 3 15 ppm Ag over 60 10 70
GN 82 11 82 5 ppb Au over 20 130 150
GN 82 12 3 83 ppm Ag over 65 15 80 I
GN 82 14 193 5 ppm Cu over 20 30 50
GN 82 14 1 05 ppm Ag over 201 30 50
GN 82 14 660 ppm Pb over 20 30 50
GN 82 14 280 ppm Zn over 20 30 50
rJLJ
nlJ
oo
ooo
o
ooo
o
o
o
oo
oJ
P D H
GN 82 14
GN 82 14
GN 83 5
GN 83 5
25 0 ppm Ag over 10
115 0 pp Au over 10
229 0 ppm Cu over 10
4 2 ppm Ag over 10
180 190
180 190
130 160
130 160
CONCLUSIONS
Encouraging geochemically elevated values only were obtained
in a number of the percussion drill holes Percussion drill
hole GN 82 14 was the most encouraging and further examination
in this area seems warranted
nLJ
o
o
L
I
cl
r
oLJ
1
LJ
HOLENO
GN82
1
SHEETNO
1
LOCATIONL3600mS6
00mW
PIlOPEIlTYl
J
J
L
I
CJ
cJ
cJ STARTED
rJ
I
J
SElCOMININGCORPORATIONLIMITED
PERCUSSIONDRILLRECORD
mLlROJECT
SUBGRID
t2
BEARING DIPCOLLAR
900
CJ
CJ
L
I
01ELEVATION TOTAL
DEPTH120FEET
3
2
CORESIZE2
INCHWET
NOV19
82
COMPLETEDNOV
20
82
SAIIE
COftE
COlliE
ASSAYS
FiliON
TO
DESCRIPTION
FIIO
TO
IID
REMARKS
NO
LENGTHPO
n
Aq
As
Au
n
n
O
R
o
20
CasinqBrokerodat90
I
0
120
SILTSTONEANDESITETUFF1
206130
40
10
59
2
48
5
EOB
naleareen
areenishwhitefineqrained
206240
50
10
76
1
35
5
aranularsucrose
chipsofsiliceous
206350
60
10
52
1
43
5
siltstonewith
occasionalarev
chins
n
n
7n
n
hiotite
insorneofthelTTeV
2206570
80
10
52
1
43
5
chiTls
206680
90
10
55
1
38
5
disseminatedDvritein
tracearnoun
ts
206790
100
10
45
1
46
5
scatteredthrouahoutinterval
2206100
110
10
38
3
39
5
moderatetostrana
CO2as
carbonatechins
2069110
120
10
60
1
63
15
andas
interstilialcarbonate
occasionalfeldsparfraqrnents
are
sausseritized
chlorite
wiseandknotsthe
mafic
mineralsarevaquein
crystalcharacter
n
0
C
O
5
maaneticsusceotibilitvl
Merritt
Funk
0
2J
19
cJ
cJ
cl
C
J
1
1
C
c1
Cl
I
I
I
SElCOMININGCORPORATIONLIMITED
HOLENo
GN82
2
SHEETNo
1
LOCATIONL3200rnS8
00rnW
PERCUSSIONDRILLRECORD
PROPERTY
PRO
lEeSUBGRIDt2
BEARING DIPCOLLAR
900
l
J STARTEDJ
cJ
I
cJ
J
cJ
CJ
01ELEVATION TOTAL
DEPTH
3
2
CORE
SIZE2
COMPLETEI
r 100FEET
INCHWET
rtvv
LJJ
0
JIUV
SAPLE
eOIlE
eOllE
ASSAYS
FROM
TO
DESCRIPTION
FIIOM
TO
IlIte
REMARKS
NO
LENGTH
0
en
As
An
0
20
OIB
I
n20
Icring
20
200
S
ca1cmeousl
070
20
10
57
n
I
k
cf
riMin
ElJH
ca1eareento
cpeento
ishwhitedri
DS
22071
30
40
10
64
1
14
ven11v
f
tm
thathavea
fine
ulartexture
particlesizeuP
2207240
50
10
52
1
16
5
to
0
5
Innbut
vervfilE
arained
07
SO
60
10
48
whiteffirlnnatedrics
0
0
70
10
46
1
norate
tostrona
interstitialcarlxmateinthe
22075
70
80
10
43
6
siltstoIEchiDS
22076
80
90
10
53
1
16
U
disseminatedpyritetIuouohoutsection
2207790
100
10
46
tracedisseminatedbiotiteflakesthJouahout
section
1
2
c
a
s
nacmeticsusceptibilitv
tIuouohout
interval
p
C
LA
JoarittFunk
0
cC10
ClCJ
Clcc
c
I
SEARING
3L
OIPCOIvR
900
STIoRTEOW
2282
co
5
15
flEtoa
ftK
SIJlol
1
cQllE
cQftE
FflO
0
tE
ttQlt
V
OZSGRP1
ON
NO
ps
AA
FIIO
CU
en
tn
e
0
6
S
7
6
enaIlQ
n
flcbi
of2019
60
O
1J1l
e
n
O
n
n
su
li@
arat1
10s
on
n
c
nO
edsiJS
arjc1e
si
100
5
wt
n
M
n
0
e
1
0
0
s
inteQtitialJth
lr
ut
n
nn
0
in
n
nO
1
on
0
ssiO
dli
unsS
t@
fl
0
0
C
MC
40to
65
as
ve
buttlla
nPtio@le
n
1
n
n
ofmjte
and
in1o
V1
d
sUt
i
0
1
0
c
s
bid
illonl
t@
0
I
n
0
0
S
0
S
tiiJj
7A
7
SlGIlal7f
S
LCOMIIlIIlG
coaoa
TIOIlL1MITO
PERCUSSIONOR
RfCOROn
11
3
EI
EVloT10l
l
TOT1
OEpTl65
rest
Z
coRESIE
2
INcaWEl
l
COIllPIElEOW
2482
IlO
11l1l
SEARING
o
OIPCOIvR
90
tIOI
E
NO
GN823
SIEEl
NO
O
8OQnl
Q
LEO
81
tt
r
0
ClCI
COCl
CIcl
CC
CIcl
L
5
82
cot
SJl
tE
eo
eORE
SSAYS
F
OJol
to
oE
SCRlwTtON
0
0
11
R
M
RKS
NO
LEHG1H
10
cu
15
1U
n
nn
o
o
casinq
EOR
0
50
o
samn1erecovered
n
Ian
nl
n
5n
200
sandnrains
multi
comoositiona
n
nn
n
0
c
roundarainS
ofbasaltfe
OSoar
nn
on
nO
n
rob
uartZand
siltsize
nn
nO
0
n
0
4
roatet
ia1
on
nn
nO
o
V
7ff
nO
Iy
ittFunk
SlGNEO
c7
OPlIlTt
SECOM
tUNGCOR
PORAtONl
MlTEO
p
CIlSSIONDRRECORD
GN
nT
GRJlBEARING DIP
COR
900
3
E
EVT10N TOTpspH
200
YEBX
CO
SIZE2
INCll
WBX
COMPETSO
NOV
27
82
HOENO
SHECINO
LOCTIOtlGN
82
4
L2800u60
50mE
STARTSO
NOV
25
82
0
r100
0cJ
r3C
rJ
C
t
OE
NOSlIEET
NOOCl
loN
GNB25
1 1l2
OlIS
IOollllttl
saCO
MIlING
COllpOllT
ONUMITEO
loNOR
RfCORO
OPlltlO
1
Su@JD
t
6 aEAlING
o
PIP
COl
90
3
ELEVION
1
0
1
PEPTti200
mer
2
COlE
SIZE2
JtPl
IEr
COp
EfEOWv
J
82
Srll
rEPWIT
J
82
OlllUED
a
1UtlI
1
rIO
110
SltEE1NO
LOcrTIONo
CJO
GN82
6
1 12
00III
S
9
00
oC1
Gr
C1
CJ
1
SEICO
MINING
CORIOR
1l0NUMlTEO
l
BRCGSStON
DRll
RfCORD
PIlOPEIl1t
UNl
ROJBCT
S1JBURtP
2
SElR1NG
DIP
couAR
3
900
STARTEDpec1
82
IlIB
ELEVATION TOTAlDEPTlt
200
FB8T
2
CORSIZE2
tNCIItWST
COMPLETEDPEC
l
82
C
CJ
Q
11
rl
cl
1
c1C
CI
C1
l
J
cl
L
L
I
L
1
CJC1CJ
SElCOMININGCORPORATIONLIMITED
BEARING DIPCOLLAR
900
013
2
ELEVTIONTOTALDEPTH200FEET
CORESIZE2
INCHWET
COMPLETEDDec
2
82
HOLENo
GN82
7
SHEETNo
1
LOCATIONL400mS1200mE
PROPERTY
PERCUSSIONDRILLRECORD
GNPROJECT
SlJBGRTn
7
SAMPLE
COptE
CO
E
ASSYS
OM
TO
DESCRIPTION
FIIlO
TO
REMARKS
NO
LENGTHInCOV n
0
n
n
n
n
on
01B
In
10
Rnl1
20
200
SYENITE
tel
1
2
2n
n
I
n
Q
I
n
rranoonto
Iredium
brownchios
mifonn
I
n
n
1
0
I
n
in
sitionald1aracter
tlrrouohoutinterval
I
1
n
on
I
no
00
0
0
n
re
I
1
on
on
I
n
I
0
n
1
0
on
n
Ion
0
1
n
0
on
on
hn
O
I
n
tao
interstialcarlxmate
0
27
80
90
10
35
1
9
0
1rnn
on
2212
90
100
10
6
0
0
22129100
liD
10
46
1
10
I
n
M
tic
Susceili
22130liO
120
10
A
n
1
c
a
S
2030
22131120
110
no
0
I
n
0
n
s
0000
22
2
0
40
0
0
0
I
1
to
1
c
S
60200
22133140
150
10
49
n
22
34150
160
no
I
l
I1n
22
5
160
1n
0
I
n
n
22136170
180
10
I
0
22137180
190
10
2
n
22138190
200
hn
0
1
I
I
n
MerrittFInk
S
GNED
j
DRILLEDI5Y
STARTEDDec
2
82
CJ
r
I
Cl
r1
cJ
f
I
l
t1r1
C1
J
SElceMINING
CORPORATIONLIMITED
Cl
PERCUSSIONDRILLRECORD
OPERTYrN
PRO
TF
T
SURRIn
HOLENo
GN82
8
SHEETNo
1
LOCATIONL321tS
3
00mQ
1
1
t
C1LJc
STARTEDDee
r1
L
I
01ELEVATION TOTAL
DEPTH180FEET
3
2
CORESIZE2
INCHDRY
3
82
COMPLETEDDec
3
82
BEARING DIPCOLLAR900
00
TO
DESCRIPTION
SAMLE
COilE
CORE
ASSAYS
00
F
OM
TO
LENOTHIIIC
O
REMARKS
1
1I11lI
rn
n
n
n
n
n
O
B
n
lnl1
1
180r
Hitfaultlost
air
retrn
stoppedhole
10
180
SILTSTONEas
GN1
2
3
213910
20
10
45
1
67
10
EOH
Daleareentoareenishwhite
calcareous214020
30
10
55
1
61
10
witharev
siliceousnon
calcareouschios
214130
40
10
74
1
27
5
arannlarsucrose
texture
2
42
40
50
10
79
1
32
5
1
21disseminatedDvritethrouahoutentire214350
60
10
79
1
32
10
interval
214460
70
n
83
1
55
5
traceenidoteinDaleareenishwhitechin
214570
80
n
An
partsofthesectioncouldrenresenta
An
On
10
75
1
29
10
finearaineddioritel
b
d
gn
00
n
A
10
5
disseminatedmaanetitefrom80
180
intervaI
nn
11n
n
7
maaneticsusceotibilitv
b
1
0
O
72
1
25
5
2
c
s
10
80
b
17n
nn
n
7n
10
4
5
c
q
s
80
180
loOT
TOnI
TAn
n
I
140
150
10
45
1
39
5
2215150
160
10
70
1
30
5
2215160
170
10
80
1
45
5
2215170
180
10
84
1
45
5
MerrittFunk
YtZAr
cl1
r1
clc
ol
J
0 o
OE
1010
S
EET1010
OCTOIol
00
TO
o
O
O
50
4
s
coMINING
COROR
ON
U1EO
1EJlCJSS
1ottOR
RfCORO
3
aEtlIolG
900
DIP
COtl
STJltTEP
lec1
82ssYS
eoe
TO
COftf
flJC
111
S
tlE
ItO
I
EHG1tl
OlIO
Cl1
Q
2n
nO
p
bzlc56110
pttopuff
GN829
1 t40
00o
2
0QmW
OfSCft1Pf
Otl
ors
l
5
20
bl15S
0
2
59
40
SltlfIOllE
nicJ
odiOJite e
f
e
ain
a
tet
d
si
tonefine
ainedbiotl
P
cte
a
s1lS
is
0
2
to0
4
c
c
S
oJeJ
inte
l
0
1
o 40
O
50
10
l
41
fjETf
OIol
1oTId
DEPT
80
FET
CottESizE2
INCIlOlt
Co
pETEOlee
1 e
RlC5
otO
casJnrt
Tzt
SIGNEO
CJ
J
1
r
I
1
J
CJ
Ll
HOLENO
GN82
9
SHEETNo
2
LOCATIONL4000mS2
00mW
0E
LEVATION
TOTALDEPTH180FEET
3
2
CORESIZE2INCHDIlY
COMPLETEDDec
7
82
LJ
rJ
C1
n
c
CJ
J
SEtCOMININGCORPORATIONLIMITED
PROPERTYGNPROJECTSUBGRID2
PERCUSSIONDRILLRECORD
BEARING DIPCOLLAR
900
rlC1
I
J
rJ
CJ
STARTEDDec
7
82
SAMPlE
COilE
COilE
ASSAYS
FIlOIo
DESCRIPTION
FROM
TO
1IItc
REMARKS
NO
IENGTH
1111I11
Cu
Au
As
Au
0
160
MONZONITE
216050
60
10
45
1
11
15
arevwhite
topaleDinkincolour
216
60
70
10
43
1
9
5
feldsnarsconsistofpalepinkwhite
n
on
n
1
In
andarev
white
colouredcrvstals
o
on
on
n
7
4
indescriDtqreen
mafiaschloriteas
minor2164
90
100
10
17
1
11
5
constituent
nn
11n
n
2
1
I
5
n
1
llnl17n
n
4
Ueoidote
121
2n
1
n
In
2
iT
hrnwnhinHe
flakes
n
l14n
n
26
11
5
wiThh1oritechipsand
4n
gn
nl
ocwhitcalcitechios
gn
1
n
In
2
1
14
5
itsl1sceotibilitvis
n
7n
n
1
11
5
in
ns
overinterval
121
n
I
on
n
77
n
n
1n
n
SILTSTONEmicrodioritel
asorevious
170
180
MONZONITEEOH
asorevious
n
C1
13
1
CJ
C1
HOLENo
GN82
10
1l0PEIlTY
SHEETNo
1
LOCATIONL4200n63
00mW
CJ
rl
C
CJ
L
J
CJ
rII
J
rJ
r
CJ
SElCOMININGCORPORATION
LIMITED
PERCUSSIONDRILLRECORD
M
PROmCT
St
RTnI
BEARING DIPCOLLAR
900
0ELEVATION TOTAL
DEPTH180FEET
3
2
CORESIZE2
INCHDRY
STARTEDDec
8
82
COMPLETEDDec
8
82
FIIlOM
AMPLE
COlliE
CORE
ASSAYS
TO
DESCRIPTION
FIlOM
TO
EC
V
REMARKS
NO
LENGTHItlll
Cu
Aa
As
Au
0
20
O
B
n
nl
lOa
g
20
180
DIORITESILTSTONE
I
siliceous
2173
20
30
10
29
1
43
10
EllI
nediurnlioht
amvfine
chins
2174
30
40
10
28
1
27
10
UIllErmicro
finemanular
texturedandilooks
2175
40
50
10
28
1
50
10
0
a
siliceoussedinentH1atis
lioht
to
12176
50
60
10
33
1
22
10
rrrIlnsh
teinrolour
1
n
n
n
5
wellde
biotite
talsu
to
5
mnin
7n
An
1n
1
size
An
n
In
1
tlace
ovrite
2180
90
100
10
29
1
11
10
carIonate
12ll180
asinterstitial
2181
100
liO
10
31
1
10
10
IlBoneticsusceotibilitv
2182
liO
120
10
32
1
li
10
1
c
a
s
2ll90
2183
120
130
10
29
1
11
4
C
rT
S
9ll180
2184
130
140
10
30
1
12
5
2185
140
150
10
29
1
15
5
b2186150
160
10
32
1
17
1n
122187160
170
10
29
1
14
15
2188
170
180
10
27
1
16
15
MERRITTFUNK
n
J
LJl
l
l
I
rlor
CJ
L
J
CJ
l
L1
o
C
C1
C
lJ
cl
L
lJ
C1
SELeoMININGCORIORATIONLIMITED
SAMLE
COlliE
COilE
ASSAYS
FIIlOM
TO
DESCRIPTION
FftOM
TO
REMARKS
NO
LENGTHG EllIE
Cu
Acr
1
Au
Zn
0
10
om
o
10I
Cisina
10
70
SnllSIDNE
2189
10
20
10
51
2
6
17
10
lichtcnev
todatkcnev
withSOlle
bladfi
i22l90
20
30
10
28
2
0
50
10
arainedsiltstonechips
bOlo
30
40
10
32
A
20
10
5
disselllimted
PVritethmuchoutentilesection
b102
40
50
10
30
4
1
14
5
nechimcne
rrassiveovritewhile
othezsshow
g
so
60
10
33
19
12
5
te
strinF
b294
60
70
10
52
3
0
12
5
stJOnqintezstitia1
camonate
6070
lichtcnev
siltstonebedf
l
70
100
lINIE3ITEIDFFSEllIMENT
b
g
70
80
10
61
0
2
oalecneentorediun
cneentocnev
tuffsedinentb
g
RO
gO
10
59
n4
fi
araid
b
o
gO
nn
10
59
0
1
7
5
noaerateto
stronq
intertitialcarlonate
100
160
SnllSIDNEHANllESlTETUFF
Imoo1
00
lln
n
I
n
0
0
oalecneen
calaueotBfinecnainedsiltstone
b100
1110
l
n
10
11R
I
R
nocerateto
stronqcazIa1ateintezstitial
000
TOn
TOn
n
7
n
0
0
n
whitefeldsparcrvstalnieCESin
chi
on
TOn
An
n
OT
n
0
n
oon
no
lAn
Tn
In
19
n
0
22203150
160
10
42
0
8
3
5
Mmitt
FUTk
L
STARTEDtee
9
820IOLEVATION TOTAL
DEPTH190FEEr
3
2
CORESIZE2
INCHDRY
COMPLETEDIec
9
82
PERCUSSIONDRILLRECORD
HOLENo
GN82
ll
SHEETNo
1
LOCATIONL765CnS4
50nW
PROPERTYGNPROJECTSUBGRIDJt4
BEARING DIPCOLLAR900
0
c
G0
oel3
cJ
0
J
L
q
SEJRING
3L
OU
COM
900
STRTEP
Dee9
82
COI
ASSAYS
flEMRS
co
coJlf
ot5CR1P1ION
SAtE
0
0
tUTtt
o
n
frlOtoll
0
NO
cu
l
0
n
01
0
o
0
0
on
0
n
no
Innno
on
no
n
n
are
finerainedse
i
1011
on
nn
n
n
n
0
0
n
disseminatedtl
rouahoutall
10
70
interl
Je
troni
ersi
i
0c
S
7
7a
SIGNED
SEtCOt
ItlltlGCORpOR
OtltIM
lED
PERCUSSIONDR
RECORD4
3
EEY
TIOll
TOT
DEpTH1
90
FEE
2
CORESI7
E2Il
CIl
Ollll
COplefEO
pec
9
82
tlO
itlfl
SEJRING
OU
CovR
900
82
jo
OtENO
GN82n
SHEEfNO
2
oCTION1
76
S0mS4
SOnW
a
uEOt
11
CJ
L
I
rJ
0
J
Cl
tICc1JLt
ct
CJ
CJ
lt
LJ
rJ
CJ
SELCOMINING
CORPORATIONLIMITED
FIlOM
TO
OESCRIPTION
SAMLE
COllE
COilE
ASSAYS
NO
FIlOM
TO
lENGTH
tco
REMARKS
P
CU
Ag
As
Au
n
T
D
0
10I
casina
15
no
SlLlS1DNE
ANIESITE
lUFF
n7
15
20
5
25
5
0
10
55
EDFl
1530
e
fine
d
stroninterstitial2220820
30
10
26
2
5
9
10
cmlonate
22209
30
40
10
38
1
9
11
25
tJaoatoU
disseminatEdovrite
2221040
50
10
44
6
0
12
15
fn
T
m
ensedinents
2221150
60
10
57
2
5
10
55
50
30
1e
creamwhiteto
le
fine
2221260
70
10
17
7
5
15
stronercarlx1ate
2221370
80
10
27
2
0
14
15
80110
Me
n
tobuffa
lowed
fire
hd
22214
80
90
10
54
10
10
10
2221590
100
10
50
0
1
15
10
Mi
eticSUSCEotibilitv
22216100
110
10
54
0
5
12
5
0
1
c
er
s
thronolYut
section
I
Lovof
L
DRILLEDBY
ttFulk
SlGNED
J
STARTEDDec
9
820ELEVATION TOTAL
DEPTH110FEET
3
2
CORESIZE2INCHDRY
COMPLETEDDec
9
82
PERCUSSIONDRILL
RECORD
HOLENoGN82
12
PIlOPERTY
GN
PROJFCT
SUBGRIDlJ4
SHEETNo
LOCATION1 L77
50mS4
50mW
BEARING DIPCOLLAR
90c
CJ
1
1
l
J
CJL
I
I
1
HOLENO
GN8213
SHEETNo1
LOCATIONL63HJQnS
3HOOrrE
PROPERTY
1
I
l
I
rJ
l
l
CJ
SElCOMININGCORPORATION
LIMITED
PERCUSSIONDRILLRECORD
GNProJECT
SlEGRIDU
BEARING DIPCOLLAR
900
STARTEDLee1782
1
cJ
rJ
CJ
CJ
rJ
01ELEVATION TOTAL
DEPTH150FEEr
3
2
CORESIZE2
DRY
COMPLETEDIec
1782
FIIOM
TO
DESCRIPTION
SAMPLE
COlliE
COIlE
ASSAYS
NO
FIIOM
TO
LENGTHIlIECV
REMARKS
11111
CU
In
As
Au
n
n
nlR
010
Cisinq
n
n
It
2217
10
20
10
31
2
5
5
mH
2
5
nmm
l
2218
20
30
10
27
1
3
5
a
microsCOD
2219
30
40
10
25
1
3
5
l
tn
an
withwhitefe1dsoar
2220
40
50
10
29
2
3
5
i
1
0
n
1
50
60
10
42
3
3
5
1enh
0722260
70
10
51
1
4
5
n1
2223
70
80
10
20
1
4
5
ntyITSllQIlQlJ
n
n
ar01
22224
80
90
10
38
5
5
5
hnl
2222590
100
10
26
1
3
5
i
i
is
0
0
a
S
nur
enMre
100
I
n
10
62
6
3
5
1
7
11n
I
2n
0
43
2
3
5
InnR170
1
0
10
47
4
2
10
2222Q120
140
10
44
2
2
5
b
On
TAn
n
0
50
3
4
5
MLttFIlnk
7
CJ
Cl
I
I
cJ
L
J
CJ
1
CJ
cJ
l
1
r
1
CJ
C
I
J
I
cJ
CJ
C
I
CJ
1
SEtCOMININGCORPORATIONLIMITED
PERCUSSIONDRILLRECORD
OM
SAMrE
COIlE
COllE
ASSAYS
TO
DESCRIPTION
FROM
TO
REMARKS
NO
LENGTH1110
0
11I
Cu
Aa
As
Au
Ph
Zn
0
10
ANIE
TUFF
n
Tn
Tno
Tn
Tn
57
213
I1Ediun
fire
inedwithmitefelA
r
withmitefaldsoarlmncrvstal
Piecessorre
rusty
tTlssanolS
Dits
weakcazbanate
10
80
ANIESITEBllSALTFIlM
I
10
20
10
29
0
1
6
5
8
li3
finerined
daDqzey
basaltfl
witl1occasional2223320
30
10
33
0
1
6
5
10
81
olivire
tals
SOIlemite
faldsoarlaths
12234
30
40
10
250
1
2
10
5
750
382
weaktoncderate
interstitialcarlxmate
2235
40
50
10
137
0
9
10
5
570
178
12223650
60
10
51
0
1
9
5
70
79
80
90
ANDESITETUFF
I
n
n
n
n
85
173
mleareen
anCEsitetuffmiJed
withnTPV
basalt
20
0
00
10
I
o
22
liO
d
fDnnabve
22
1
0
90
10
13
0
2
7
5
II
107
mle
n
finearainedwitl1mitefeldsoarchips
tzacecvriteandchalOOPYrite
o
analrusty
8OOnschio
weakcaJxmate
interstitial
90
100
ANDESITEBASALTFLOW
on
nn
ln
n
l
17
98
ren
ahaniticflowas
nrevious
traceweakcarbonate
V
f
dZ
DRIUEDBY
MiitbFmk
SIGNED
STARTED
01ELEVATION TOTAL
DEPTH200FEET
3
2
CORESIZE2
INCHDRY
Dec
14
82
COMPLETEDDec16
82
HOLENo
SHEETNo
LOCATIONGN82
14
PIlOPEIlTY
1 L6400mS33
00mE
N
PlIDJFrfI
lmRTn11
BEARING DIPCOLLAR
900
CJ
C
c
rt
CJ
CJ
HOLENo
GN82
14
PROPERTY
SHEETNO
2
LOCATIONL6400ms33
00lllE
CJ
cJ
Cl
Cl
I
J
CJ
CI
CJ
SELCOMININGCORPORATIONLIMITED
PEReUSSIONDRILLRECORD
GNPROJECT
SUBGRIDU
cJ
L
J
CJ
J
CJ
01ELEVATION TOTAL
DEPTH200FEET
3
2
CORESIZE2
INCHDRY
STARTEDDec
14
82
COMPLETEDDec
16
82
BEARING DIPCOLLAR
900
0101
TO
SAMLE
CORE
CORE
ASSAYS
DESCRIPTION
FROM
TO
REMARKS
NO
LENGTHce
v
111111
Acr
AS
An
Pb
Zn
nn
2n
MIXEDBASALTFLOW
ANDESITETUFFFRAGS
22241100
liO
10
29
0
5
6
46
170
darkorev
basaltasor
gnL
unitmixed
0
11n
n
n
00
n
41
164
withpaleto
mediumqreen
andesitetuff
fracnnentsasinfOllowingunit
weaktomoderateinterstitial
carbonate
n
TAn
TUFF
on
TOn
10
T
n
n
23
138
Dalecreen
finegrained
10n
4n
n
0
on
175
199
stronqcarbonateinterstitial
occasionalfeldspar
crystalsinchios
tracepvrite
130140rusty
aossanouschios
151
40
170
ANDESITEBASALTFLOW
22245140
150
10
42
0
6
16
10
50
144
lasprevious10
80
22246150
160
10
4l
0
1
9
5
17
103
arevfine
arainedflow
22247160
170
10
67
18
35
10
147
173
occasionalbleachedandesitefraamPntsfrom
160170orobab1vreoresentinothebeoinnino
ofthe
underlyingunit
weakto
moderatecarbonatecontentthat
with
andesitefraaments
Dresent
traceto
euhedralpyritecrystals
7L
hA
MerrittFunk
0
ooooCJ
o00
L
J
l
LJ
evtullG
5
33
oomJ
PIPCOIvR
900
COpIETEO
Dec
6
82
STRTEP
Dec
4
82
SSIYS
flEtA
RKS
co
colE
SA
E
F
O
0
LE
HJf14
1lJC
ll
lb
In
oESCftlPtlON
0
0101
0
235
202
n
n
1
n
0
0
no
ll
UESrc
tJI1F
l
I
1JO
210
110
02249SO
90
10
250
20
stron
carbonate
intersti
tia
n
4
0
2
0
111
ale
reenfine
rainedcalcareous
tuff
2250
00
I
on
t
ssib
a
sedl
tllentasiltst
Onel
trace
euheoral
Iyrite
crystals
nn
n
gQs
n
n
n
n
n
n
l
n
O
n
02
0n
nO
1J
f
1
sG
ED
5
SEICO1I
GCORPOR
O
11I
EO
lJ
RcllSsrONORll
RECOROGR1D
3
EiEVI
TlOll
OT
pEpTZOO
FEJT
l
CORESIZE2
rNClltDRl
ao
1Y
evRIllG
PIPCOIvR
900
OlE
110
GNS2
14
stEET110
3
n
Rf
JO00
00000r
CJ
A
eoRING
3
0
PIP
COvR
90
OEC
3
82
CO
0
STARTEDIo5S
5
P
E
R
co
t
GOfte
l
PlO
TO
tENO
r
AU
O
RlyT1Oto
NO
C1
AS
O
TO
n
0
n
n
n
tt
L
on
n
n
0
bean
to
U
0
nn
n
0
n
n
0
n
Q
n
reducedto
2
andost
air
1
ieeS
a
L
forcedto
abandOn
n
n
L
n
T
retUrn
on
0
0
T
n
n
n
hOeat
80
n
n
on
8
0
4
225660
10
0
10
80
0
55
0
5
30
2251
n
S
O
n
0
oft
0
bl
71lj
SIGNED
o
SECOMlt
INGCORPORA
Ot
I1EO
PERCIlSSI0N
DR
RECORD
3
EII
TION
I
01I
pEPTt80
FEET
2
CORESItE
3
INCllOl1Y
cOtAPffED
pe
3
82
0
11
eoRING
o
PIP
CovR
90
HOENO
GN82
l5
StEET
NO1
I
ollIEaf
NerJitt
FuTk
CJ
cI HOLENO
SHEETNO
LOCATIONCJ
CJ
CJ
C
CJ
CJ
CJ
Cl
Cl
CJ
C
SELCOMININGCORPORATlONLIMITED
BEARING DIPCOLLAR
CJ
CJ
J
CJ
cJ
r
J
0ELEVATION TOTAL
DEPTH100FEET
3
2
CORESIZE3
INCHDRY
COMPLETEDDEC12
83
GNPROJECTSUBGRIDl
PERCUSSIONDRILLRECORD
LE
COPlE
COlliE
ASSAYS
FIIIOM
TO
DESCRIPTION
FIIOM
0
Rev
REMARKS
NO
LENGTHmm
Aa
As
Au
0
20
ANDESITETUFF
n
In
In
4
17
0
10
CaRing
paleareen
andwhitechioswith101rusty
In
n
1
n
0
1
chins fineqrained
stronacarbonateinterstitial
n
n
ANDESITEBASALTFLOW
n
n
In
1
7
mediumarevto
darkgrey
fineqrained
2226
0
4n
n
1
7
porphvritic
qreenmafics
6
4n
n
n
4R
1
6
moderateinterstitial
carbonate
50
100
ANDESITETUFFas
previous
6
n
n
n
EOB
n
7n
1
n
In
1
4
Maanetic
susceotibility
7n
on
n
11
0
20
0
0
c
q
s
on
00
1
n
7
7
20
50
0
3
c
a
s
226
on
nn
n
0
11
50
1000
0
c
q
s
j
j
Mo
1
1
GN8216
1 L5900mS33
00mE
PIlOPEIlTY
900
STARTEDDEC12
82
CJ
cJ
CJ
IJ
L
J
C
J
Ll
CJ
CJ
CJ
l
I
CJ
cJ
CJ
CJ
CJ
Ll
clCJ
SELCOMININGCORPORATIONLIMITED
403
2
PERCUSSIONDRILLRECORD
GNPROJECT
SUBGRIDt2
HOLENo
PROPERTY
GN
83
2
1 L3600mS4
50mW
ELEVATION TOTALDEPTH
SHEETNO
LOCATION
200Feet
BEARING DIPCOLLAR
CORESJZE
2
InchWet
STARTEDMay27
1983COMPLETEDMay27
1983
900
SAIolLE
CO
COIllE
ASSAYS
ftOM
TO
DESCRIPTION
I
OM
TO
REMARKS
NO
LENGTHIICC Cill
O
Cu
Ag
As
Au
0
20
O
B
20
100
DIORITEMONZONITE
2255820
30
10
39
0
3
63
15
Disseminatedpyritees
tirnated
mediumgrey
finegrainedoverall
59
30
40
10
47
0
4
53
5
2
overinterval20100feet
subhedralwhitefeldsparlathsina
medium60
40
50
10
40
0
3
61
5
greysiliceouslookinglookingfine
61
50
60
10
44
0
3
81
5
grinedgroundmass
Finecrystalline
62
60
70
10
4l
0
4
99
5
biotite
impartsa
brownishtingeunder
63
70
80
10
38
0
1
101
5
themicroscope
64
80
90
10
36
0
3
92
5
disseminatedpyrite
magnetitethroughout2256590
100
10
34
0
2
75
5
traceepidote
weakmoderate
interstitialcarbonateplus
occasionalcarbonatechip
Thisrockunit
possiby
magneticsusceptibilityismoderate0
4
representsa
contactor
border
to
0
5
as
explainedbythe
presenceof
phaseto
theunderlyingclean
1
disseminatedmagnetite
Monzonite
1
MerrittFunk
n
lAL
CJ
CJHOLENO
SHEETNo
LOCATIONCJ
rJ
cJ
J
L
J
CJ
CJ
CJ
l
I
CJ
C
CJ 03
2
GN83
2
cont
2 L3600rnS4
50mWPROPERTY
CJ
C1clrJ
SELCOMININGCORPORATION
LIMITED
PERCUSSIONDRILLRECORD
GNPROJECT
SUBGRlD12
BEARING DIPCOLLAR900
STARTEDMay27
1983COMPLETEDMay27
1983
CJ ELEVATION TOTALDEPTH
CORESIZE
200Feet
2
InchWet
TO
5
1E
COlliE
CORE
ASSAYS
1110101
DESCRIPTION
FiliON
TO
REMARKS
NO
LENGTH11
0
l
Er
CU
Ag
As
Au
100
200
MONZONITE
22566100
liO
10
32
0
1
77
5
Disserninatedpyrite
estimated
EOH
whiteto
lightgrey
feldsparrichchips
67
liO
120
10
31
0
1
53
5
2
overinterval100200
feet
Occasionaleuhedralwhitefeldspar
crystals68
120
130
10
27
0
4
30
5
inwhitetogrey
whitefeldspathicground
69
130
140
10
21
0
3
24
15
mass
22570140
150
10
26
0
3
30
5
1
mmbiotiteeuhedralto
subhedralcrystals71
150
160
10
24
0
1
32
5
Patchygreen
alterationassociatedwith
72
160
170
10
26
0
1
35
5
thebiotitecrystals
73
170
180
10
28
0
2
36
5
traceepidote
74
18Q
190
10
26
0
1
36
5
approxirnated15
ofchips
aresimilarto
22575190
200
10
29
0
1
50
5
ChipsfrompreviousDioriteinterval
Contactappears
gradationalbetween100
to
120 Magneticsusceptibility
100120feet
0
4
c
g
s
120200feet
0
1
c
g
s
weaktomoderatecarbonateinterstitial
andminor
carbonatechips
I
1
MerrittFunk
j
1
Cl
cJ HOLENO
SHEETNO
LOCATIONcJ
CJ
L
J
rl
CJ
l
J
CJ
cJCJ
cJ
CJ
CJ 03
2cJ
cJ
J
cJ
l
J
ELEVATION TOTALDEPTH200Feet
QiI83
3
1
L32HlOrrS
1251lnW
PIlOPEIlTY
SEleaMINING
CORPORATIONLIMITED
PERCUSSIONDRILLRECORD
GNPROJECT
SUaGRID13
BEARING DIPCOLLAR900
STARTEDMay28
CORESIZE
2
InchWet
1983COMPLETEDMay28
1983
FJIlOIoil
TO
DESCRIPTION
SAMPLE
COlliECOJllE
ASSAYS
OM
TO
REMARKS
NO
LEIIIClTH
OYCIIC
CU
Ag
As
Au
0
60
o
a
60
200
DIORITE lightgreyto
mediumgrey
colouredchips
22567
60
70
10
38
0
2
6
5
Finegrainedchipsize
generallyfinegrained
77
70
80
10
42
0
2
6
5
60to
120feete
occasionalcream
whiteeuhedralfeldspar78
80
90
10
49
0
4
7
10
crystalsin
greysiliceouslooking
79
90
100
10
39
0
1
7
5
Traceto
1
pyrite1oca11Ya
aphaniticgroundmass
80
100
liO
10
53
0
4
10
5
disseminatedmagnetite11
81
liO
120
10
55
0
3
li
5
magneticsusceptibility0
2
to
0
3
o
g
s
82
120
130
10
45
0
3
10
5
moderateinterstitial
carbonate
83
130
140
10
47
0
2
7
5
84
140
150
10
40
0
4
6
10
85
150
160
lOr
46
0
4
7
15
86
160
170
10
42
0
3
7
5
87
170
180
10
38
0
3
7
15
88
180
190
10
36
0
3
7
10
22589
190
200
10
36
0
2
9
5
1
A
AL
MerrittFunk
cJ
JHOLENo
SHEETNo
LOCATIONC
cJ
cJ
J
cJ
cl
cJ
cJ
CJ
CJ
cJ
SElCOMININGCORPORATION
LIMITED
PERCUSSIONDRILLRECORD
GNPROJECT
SUBGRID2
BEARING DIPCOLLAR900
STARTEDMay26
1983COMPLETEDMay27
1983
CJ
CJ
cJCJ
GN83
1
PIlOPEIlTY
1 L4000
1
00mW
CJ
CJ
AD3
2
ELEVATION TOTALDEPTH
CORESIZE
200Feet
2
InchWet
IlO
TO
DESCRIPTION
5AMLE
COIlE
COIlE
ASSAYS
IIOhl
TO
REMARKS
NO
LENGTHtcov lI
t
Cu
Ag
As
Au
0
10
O
B
22539
10
20
10
31
0
5
39
15
GOodchip
recovery
40
20
30
10
35
0
4
14
15
15
200
MONZONITE
41
30
40
10
31
0
4
12
15
Disseminatedpyriteis
found
EOH
chipsarelight
greyto
greygreenin
42
40
50
10
29
0
3
24
10
throughoutthe
following
colour
uniformthroughout
43
50
60
10
28
0
2
9
10
intervals
chipscnosistofeuhedralto
subhedral
44
60
70
10
30
0
4
11
5
10
30
1
romfeldsparcrystalsthat
varyfrom
45
70
80
10
26
0
4
10
5
60
170
creamwhite
bufftan
palegreygreen
46
80
90
10
I
32
0
5
14
10
lyingina
finegrained
greygreen
ground
47
90
100
10
30
0
5
15
10
mass
48
100
110
10
28
0
4
7
15
nondescriptgreenandblackcoloured
49
110
120
10
26
0
3
7
10
mafiasthatareveryfinegrained
50
120
130
10
44
0
4
12
5
pyritedisseminatedlocallythroughout
51
130
140
10
30
07
10
10
fromtracetoupto51
oversome10
foot
52
140
150
10
29
0
8
10
5
intervals
53
150
160
10
30
0
5
9
10
moderatecarbonatealterationthroughout54
160
170
10
31
0
5
20
5
entirehole
55
170
180
10
33
0
5
11
10
magneticsusceptibilityis
lowthroughout56
180
190
10
32
0
2
19
5
hole0
0
to
0
2
c
g
s
22557190
200
10
31
0
1
10
10
1
Merritt
Funk
1
I
faeU
oj
L
J
HOLE
No
SHEETNo
LOCATIONcJ
cl
CJ
CJ
CJ
cI
cJCJ
CJ
J
IJ
CJ
GN83
5
PROPERTY
1 L6400mS
31
50mE
SELCOMININGCORPORATIONLIMITED
PERCUSSIONDRILLRECORD
GNPROJECT
SUBGRIDU
BEARING DIPCOLLAR900
J
CJ
CJCJ
cJ
03
2
ELEVATION TOTALDEPTH
CORESIZE
STARTEDMay29
1983COMPLETEDMay3D
200Feet
2
InchWet
1983
OPo
0
DESCRIPTION
SMPlE
CO
E
COlliE
ASSAYS
NO
FIIOM
0
LENGTHIlKv
REMARKS
elle
Cu
Ag
As
Au
0
10
OIB
10
200
ANDESITETUFF
22501
10
20
10
46
0
6
3
15
EOH
mediumgreenandpalegreenish
grey
2
20
30
10
40
0
5
3
5
colouredchips
3
30
40
10
22
0
3
4
10
finegrainedgranulartextureexhibited
4
40
50
10
l2
0
3
3
15
bygreen
maficandwhitefeldspathic
5
50
60
10
l2
0
3
4
10
fragmentsandroundedsiliceousgrainsin
6
60
70
10
13
0
4
4
10
eachchip
7
70
80
10
14
0
3
4
10
someclayalteredfeldspar
8
80
90
10
20
0
8
5
5
stronginterstitialcarbonatethroughout
9
90
100
10
8
0
5
3
5
entirehole
22510100
liO
10
6
0
5
4
10
magneticsusceptibilityis
0
0
to
0
2
0
9
5
li
liO
l20
101
5
0
2
4
5
novisiblesulphides
l2
l20
130
10
71
1
8
4
10
13
130
140
10
260
5
1
5
5
14
140
150
10
276
5
1
4
5
15
150
160
10
150
2
5
5
5
16
160
170
10
101
1
8
5
5
17
170
180
10
46
0
9
4
5
18
180
190
10
34
0
4
5
1
10
22519190
200
10
39
0
4
5
5
Merritt
Funk
r
u
1
I
1i
I
J
o
o
ne
SECTION 5
COST STATEMENT
o
o
o
o
o
o
o
o
II
II
I
nI
U
o
c
u
oo
o
ontJ
1
o
o
o
o
o
o
o
o
o
o
c
o
o
COST STATEMENT
GN 1 8 RECORD 11125 1132 INCL 150 units
Road and Drill Site Preparationa November 1982
D8H Tractor bulldozer work
as per Invoice November 10 1982
Katchmar Construction Ltd
27 5 hrs @ lOO OOjhr 2 750 00
b May 1983
Moving charges for D6 Tractor
bulldozer as per Invoice
May 26 1983
R McMillin 167 75
c D6 Tractor bulldozer work
as per Invoice May 31 1983
McNeill Sons Logging Ltd
applying 80 of 1210 00 968 00
2 Percussion Drilling
a November December 1982
16 Percussion drill holes
totalling 2555 feet
GN 82 1 to GN 82 16
as per Merritt Funk Brothers
Drilling Co Ltd Invoices
dated
i December 2 1982
6153 75 2540 00
ii December 23 1982
13 197 00 315 00 12 882 00
3 613 75
I
L
oo
o
o
o
nrlJ
o
o
o
o
D
o
o
o
o
o
o
2
2 Percussion Drilling Con t
b May 1983
4 Percussion drill holes
totalling 800 feet
GN 83 1 to 3 and 5
as per Merritt Funk Brothers
Drilling Co Ltd Invoice
dated May 31 1983
10 109 88 1522 00
c Low bed service to move
drill between holes
as per R McMillin Invoice
May 29 1983
3 Field Supervisioni flagging in drill roads to drill sites
6 man days @ 138 75 day4 man days @ 204 00 day
ii supervision of drill road construction
and site preparation6 man days @ 138 75 day
iii drill supervision November 20 1982
December 17 1982 May 25 1983 May 30
34 man days @ 138 75
iv drying and splitting of percussion
chips packaging8 man days @ 138 75
2 man days @ 204 00
v preparing drill chip logboards logging drill holes
5 man days @ 138 75
2 man days @ 204 00
1983
8 587 88
77 25
832 50
816 00
832 50
4 717 50
832 50
408 00
555 00
408 00
IILJ
oo
o
o
o
o
o
o
o
o
o
oo
o
o
o
o
3
4 Accommodation
Cabin rental @ 485 00 month
1lmonths
5 Food
67 man days @ 22 50 day
6 TransportationVehicle operation41 days @ 25 00 dayLease charges @ 375 00 month
6 weeks @ 93 75 week
7 Field Supplies
Sample bags flagging tin
foil drying pans wooden
drill chip log boards
shipping charges
8 Geochemical AnalysisChemex Labs Ltd as per
Invoice 18214717
December 15 1982
60 samples @ 12 96 each
777 50
1 574 50
1 025 00
562 50
350 00
II
IIIII
777 60
r
I
n 4
n 8 Geochemical Analysis Con It
0Chemex Labs Ltd as per
Invoice 18214950
January 10 1983
n 96 samples @ 12 974 each 1 245 51
0 Chemex Labs Ltdil as per
Invoice Rl8310121
G January 31 1983
51 samples @ 12 96 each 660 96
c Chemex Labs Ltd as per
Invoice 18311616
l June 10 1983J19 samples @ 13 32 each 253 08
0Chemex Labs Ltd as per
r Invoice HI8311644IL June 10 1983
n 51 samples @ 13 32 each 679 32
IJ
I
Chemex Labs Ltd I
Qas per
IInvoice HI8312356
IJuly 13 1983 I0 20 samples @ 2 52 each 50 40 i
I
0 iIi
n 9 Report Compilation Reproduction Typing JIo J 3 man days @ 204 00 612 00
0 Reproduction costs typing of report 300 00
0
0
rLJ
00
10
L
011
L
CCD
G
0
0n
0
0nu
0
00
5
Reclamation Costs
Slash cleanup along drill site access
roads and at drill sites as per
Amex Exploration Services Ltd Invoice
July 30 1983
Cost per drill hole 7 000 00 30 holes
20 holes @ 233 33 per site 4 666 60
51 983 60
o
o
onLi 1
onL
CGC
DrJ
n2
o
o
j
oFlLJ 3
n
o
COST STATEMENT
GN 1 8 RECORD H1125 1132 150 units
Grid Preparation to I P Standards
a November 1982
19 8 kms @ 137 34 km
as per Invoice November 15 1982
Amex Exploration Services Ltd 2 719 33
5 3 kms by Company personnel5 man days @ 204 00 day 1 020 20
b May 1983
6 0 kms @ 188 60
as per Invoice June 3 1983
Amex Exploration Services Ltd 1 131 60
Induced Polarization Surveysa November 1982
25 1 kms @ 829 25
as per Invoice January 1983
Peter E Walcott Associates Ltd 20 814 18
b June 1983
6 D kms @ 780 00 km
as per Invoice H3677
June 30 1983 Phoenix Geophysics Ltd 4 680 00I
II
IIII
iI
IIII
II
i
Field Supervision for Linccutting I P Surveys12 man days @ 204 00 day 2 448 00
o
rilJ
4
n
rLJ
5
rl
D 6
Cr
nnI 1
7
I
l
nlJ
D
o
c
cij
2
Accommodation
Cabin rental @ 485 00 month
2 weeks @ 485 00 2 242 50
Food
17 man days @ 22 50 day 382 50
TransportationVehicle Operation14 days @ 25 00 dayLease charges @ 375 00 month
2 weeks @ 375 00 2
350 00
187 50
Report Compilation Reproduction Typing
3 man days @ 204 00 day 612 00
400 00Reproduction costs typing of report
34 987 81
r
i IJ
lC
Cn
rLJ
cc
on
Qnnu
V IL
n
o
o
cn
AMEX EXPLORATION SERVICES LTDA A AB ABLETT
rrConfidential Work
BUS 376 0433
RES 376 7490
BOX 286
KAMLOOPS B C1714 CLIFFORD AVE
V2B 4C6
November 15 1982
Dr Hugh SquairGuichon Explorco Limited402 535 Thurlow Street
Vancouver B C
STATEMENT OF ACCOUNT
Re Field projects lac La Hache B C as listed below
CORE 1 3 4 mineral claims Grid layout and Soil Collections
44 8 km grid layout @ 144 50 km44 8 km soil collections @ 19 50 km
6473 60
873 60
7347 20 7347 20
CORE 5 CORE 6 and CORE 7 Fr Staking
Staking 41 units @ 45 86 unit 1880 26 1880 26
GN 4 7 Grid cleanout to IP standard
19 8 km grid cleanout @ 137 34 km 2719 33 2719 33
TY 9 Staking
Staking 6 units @ 89 17 unit 535 02 535 02
TY 1 Grid Layout cleanout to IP standardLINE IG
2 2 km grid IP standard @ 281 km 618 20 618 20
TY 2 Grid Layout c1eanout to IP standard
LINES G1 andIG2
2 6 km grid IP standard @ 281 km 730 60 730 60
Total requested 13830 61
Respectfully submitted
tt pre
9 E ior t ion Services Ltd
OVER 125 000 MINERAL CLAIMS AND UNITS STAKED FOR THE MINING INDUSTRYu n In r f l ICUr eIlDlE Ve I U CT VIP I I U IC IITTIIlr C IIRlI V t lf eTr
AMEX EXPLORATION SERVICES LTDA A AB ABLETT
BUS 376 0433RES 376 7490
Confidential Work
L
Cnu
1714 CLIFFORD AVE
V2B4Gf
BOX 286KAMLOOPS B C
June 3rd 1983
rLJ
Selco Inc
402 535 Thurlow Street
Vancouver B C
CrU
Attention Mr Dave Gamble
STATEMENT OF ACCOUNT
or
G
Re Grid Preparation on GN TY
Mineral Claims Lac La Hache
Clinton MininK Division
area
jl
GRID BREAKDOWN
TY 1 2 2 km @ 188 60 km
TV 5 1 0 km @ 188 60 km
TY n 9 4 8 km @ 188 60 km
TV 2 2 2 km @ 188 60 km
GN 1 3 0 km @ 188 60 km
GN 4 3 0 km @ 188 60 km
414 92
188 60
905 28
414 92
565 80
565 80
J ikl
TOTAL REQUESTED
on Respectfullv submitted
fl A A Ablett President
Amex Exoloration Services Ltd
nAmex Job Number 83 80
onL
AAA da
o
oOVER 125 000 MINERAL CLAIMS AND UNITS STAKED FOR THE MINING INDUSTRY
MANnnMnFR ANn rmfHEMICAL SURVEYS CLAIM STAKING LINE CUTTING SURVEYING ETC
J
I1
LJ
nd
nU
r l
i iI
iilJ I
l1
r jU
n
u
L
U
0n
n
QI rl H tuo llco1lCU
ffL
fW
o
10
I i L f
I
p 11
J I ILMLN I
I
Iodlf lf l
1 L 1 i
I I V
II Idf j 11
il J 11lI IJoJlo
II
11PI 2rt L i
iIr
i
0 1 1 Bl rl
J4 IJ 4
kSrY J
frI J I
III I
I
if II
iIfI
1 I
II
I
I
i
I rJL 4 J
r LV
i 1
J f i
1
rJ 4
11 II It I VI1 J t ot1
J r I Ij
1
I
1
1IV
to C1jy5 11
if
1
1S u C AJL lit SD It J oJ ll L
i 2 1 ltu II It 1 Il l
fJ 1 l II I
lOWBED IlI BOY SERVICE
h j Jl
INSURED
r
n
Ii
pot
J
08954
z4 rSACESMAN
TERMS NET 15 DAYS INTEREST AT
2X Ell MONTH ON OVE OUE ACCOUNTS124r ANNUM
F O II
f5s7 f
I
I
I
I
II
III
II
ii
II
I
II
I
o
iIIII
iI
II
Ii
tl fr7J I
I uI
J
J
J
ItJ
n
Q
toOSOLDTO
SHIPl W TO
lI
I ADDAESS
U
Z
I
1
CARlBOO LATH CO LTD TRUCKINGBOX 647 100 MILE HOUSE B C VOK 2EO
RADIO PHONEPHONE JS 7LOl
3952872 CHANNEl7L083BL94
0 AA cL A
VIA
3
0LOWIJED I HI BOY SERVICE
nLi
CnLJ
w
INSURED
I
III
I
08954
III
I
ITERMS NET 15 DAYS INTENEST AT
nI PEft MONTH ON OVERDUE ACCOUNTS
114 PER ANNUMl
F O ll
I
I
iI
i
I
II
I
o
I
r
ioru
nLJ
J
GOLD TO
C HIPPED TO
ADDRESS
o
nw
o
o
1 I IIf 1 i
fl tL j
I If i
II
II
l
CARIBOO LATH CO LTD TRUCKINGBOX 647 100 MI LE HOUSE B C VOK 2EO
RADIO PHONEIS 7LOI
CHANNEL3
1Af
PHONE3952872
1
VI
3
n HP4lD ItOUq IUIUCAtlClM
r
II
1
IJ
LOWBED HI BOY SERVICE INSURED
08962
TERMS NET 15 DAYS INJunT AT
Z Eft MONTH ON OVERDUE ACCOUNTS
12 Eft ANNUM
F Oi
iI
iI
II
I
Ii
iIIjiIiI
iI
I
IIII
II
iiIJ
iLJ
o
oo
McNeil Sons Logging Ltd
P O BOX 70 100 MILE HOUSE B C
phone 604 395 4604
iay 1 198
nL J
3elco Incorporated7182 Blackwell Rd
i R 2
Kamloops B Cn2J
oco
To D 6 cat rental May 26 27
191 2 Hrs 60 00 1170 00
1 day P U Rental 40 00
12l0 00
rU
1
j 0
fLf l Jt lI
I r
1J i1
I
f7 v1l Jc
Ii JI L
II t
y
7L
Ii
J
i
iJ
J
1I
W
n
onu
1 1 I I IDJI
en IJ
L1
I
i 1 r
IS w
1I
0c
lkSrI
N0
Qj
I
en gI 10 rM
D ojen
JJ4
J
t
G 5 lil
J
J
r0
f1
1C
f
J
en 0r
I
10N MD
oon
o
o111
L
on
ri
o
j IfLi
I
I I J I
B
e
I
IiI
IIII
I
III
I
II
1IJ
1
I
n
o
o
on
c
o
o1t
c
o
o
o
10
YUKON N W T BRITISH COLUMBIA AIUfmA USA
I
IeMEtatt Junk BlOt uu fbtdti129 COlnpan1ilnlted
Explol tlon Ind Dev lopm1nt
G fllll nl fllnll
c rl Funk
1 0 J H l1O Of H6I1333
Abordoon Ro d Lo NIcOl B CP O BOt 2077M IIt 8C VOK 280
DEe 6 982
Dccb8r 2 1 2
SILCO INCSuite I 4025 5 Thurlo Street
Vancouver I B C
V6E JL2
t i l 1n5HiCEIVHJ
F5 OKn
DEXTf NSIlN CHFCf LJ
OK F P PA clZ
JllJ CODENIJMa R
l 29C1O D O t 2
J J 40 O 4S 3
Attentions Dr H Squair
Dear Sire I4O DO v
Cg l5Re I ACCOUIlTS PAYABLE
The follo ing is our inY01c for Percussion Drilling on yourTi othy Lake Property during t pr1od of Nov 16 to Nov 27 1962
Hole NoTY6 82 5TY6 82 6eN 82 1eN 82 2eN 82ell 824
Dellth of OYertNrden Dellth of Hole Sbe of Hole later Su1l1lly
80 feet 200 t et 2 1nch truck
55 teet 200 teet 2 inch 400 w l
0 teet 120 feet 2 inch 100 1f120 feet 100 t et 2 inch 100 w
feet 165 teet 2 inch 00w
150 feet 200 teet 2 inch 00 1
Drilling ChArgea 2 965 feet 5 75 per foot 5663 75Water Supply Charsea water Une 1200 teet 10 00 per 100 120 00
water truck 1 hole 200 00 per 200 00
Moving Charges frail TY6 62 6 to eN 62 1 k4 hrs toW 2 hra 8S 00 per hour 170 00 V
Total Charges 6153 75AdYanees
TOIAL AIfUNlroB 6153 75
Thank youYours truly
rCary E Funk
Merritt Funk Brothers
Drilling CompanyLilli tad
hrfiJ
on
II
po
Ii ILJ
D
o
pIII II
LJ
nu
YUKON N W r 1J11111S11 COLUMIJIA ALlJ 1l1 US
cMElutt Junk 23toth a tiLing Company LimitEdExploration and Development
C fuunlllFunk
Cilly E FunJo
T lnllllon Jill 41J2 0 J7112J J
AbtJfd en Road LOWQf Nicola B C
P O Box 2077M rrlll B C VOK 2BOjfN 3 983
December 2 11932
C1 1 1
Ri r Ult
DrJcr 0
G rN310 1or rORr y ril
1
Attention Dr H Squair k r OOf
Dear Sirs 0 l We
Re ACCOUNTS PAYABLE
The foUowinlis 0 iorferculrnt1l1f Di ng on yourTimothy Lake Property during the period of lov 30 to Dac l 19821HOLE No Depth of O B Depth of Hol S1ze of lole dater SU1 lY OtherGN 92 5 90 feet 200 feet 2 I 00 I
II 1 2t hr move
GN 82 1 50 feet 200 feet 2 200 II I
N 82 7 20 feet 200 feet 2 100 w lGN 82 8 10 feet 180 feet 2 airCN 32 9 10 fest 180 feet 2 airGN 32 10 20 feet 190 feet 2 airGN 92 11 10 feet 190 feet 2 airGN 32 12 15 feet 110 feet 2 airGN 82 i6 0 feet 100 feet 3 air
GN 32 15 0 feet 120 feet s O 0 2 airGN 82 14 10 fset 200 feet 2 airGN 82 1 10 feet 150 feet 2 air
SliLCO INC
Suite 402
535 Thurlow Strset
Vancouver D C
V6E L2
1t hr move
hr move
1St hr move
6 hr move
Drilling Charges 2 1830 feet5 75 por foot 10522 50190 feet7 40 per foot 1 2 00
Water Supply Charges 2800 ft waterl10A @ HO OO 100 210 00Co
I
Moving Charges I 21 hrs total 11 hrs @ l5 00 por hr il062 O 1 J 5Total Charges h31 rOO I J
II IIAdvances
TOTAL AMOUNT DUE 17t9oOOI
C ITHANK YOU AND WISHING YOU AND YOURS
THE MERRIEST OF CHRISTMASES AND THE Yours truly
BEST OF THE NEW YEAR
eJ fl ICary E Funk
Merritt Funk Brothers
Drilling CompanyLimited
lJ
YUKON NWr BRITISH COLUMBIA ALBERTA U S A
i eMEnLtt Junk BtOthE t1 rptL rng Company mLtEdExplorltlon nd Oevelopmonl
u
oonw
a Eug n Funk
C lyE Fun
TlJhtphon 118 41 2 01 3112333
Aberdeen Road Lower NlcolB B CP O Bo 2077Merritt B C VOK 2BO
l y 31 t911i T r
lH 502 l35 i udow 3trPOt
l Q lVfn 1j G
o
I g271 llacklell o l
l ll 03 u l
I n
ttentton i U mble
o r tr
n
JUn 1 J r1 Y
f ll Jn t tlr lnvoic flr lNllll tO l lUJ nr on YOil
l y La t r J I t ay 5 to y 11 1 Y11
o
o
o
o
o
C
1 r
1 feat1t f1et
0 feJt
10 faot
11 et
l of I I j
l 200 footot
O feot
2 0 feet
JO fM
otol FootBl o 100 fa
lay 25 mobil1 e1 to Lac Lo iac 5 hra ay 2 moved to 1 5st up
and Iul lf1 ay 27 111110i t moved to C r lr111od t 2
11lY 21 moved to C 1 2 hra drilled G J So from previoW iisitas
all ztole 1 a lionoj dua to lack vf dcce 31 ay29 waite1 for
lowbad and moved to 1 5 1 hl6 total I fvJY JO lrilled CIl I l Ve l to
irll13d moved from lalt sl o r I 1y 3t 1oM nl oi f
I i t h 3or O
r
nG
nu
DRTI LING G IARCS 1000 f e I 7 fl psr foot ll O
M03ILPATION Q uaG J tepat to first site 2 25DiMOSILI ATIO 1 CilAHGtI 3 last 81 to to depot
f
r 5I W G iA G 2 to 2 blurs 2 2 asp97 75 l n
GN l to GN 5 3 hours 3 2 f 97 75 50Toto1 Chac es Hl1 9 n
J lvance5 ttTOTAA OJJiT DlJ 10109 33
o
o
o
1tn y IYours truly
J
dXy0
lllnk
iordtt Funk l3rotlErl
Dr1l1ing 00 Ltd
AMEX EXPLORATION SERVICES LTDA It AI AILETT Conridcnllal Wort
i
BUS 3760433
RES 376 7490 1714 CLIFFORD AVE
V2B4G6
BOX 286
KAMLOOPS l C
oo
o
o
July 30 1983
Selco Inc
402 535 Thurlow Street
Vancouver B C
Attention Mr Dave Gamble
STATEMENT OF ACCOUNT
oRe Slash clean up along drill site access roads
Lac La Hache Area Clint ion Minin Division
o Amex Feel
IiI
10 kilometers @ 700 00 per kilometer 7000 00
total requested 7000 00
Respectfully lubmitted
Ameresident
oration Services Ltd i
1
I
I
1
Amex Job No 83 81
OVER 125 000 MINERAL CLAIMS AND UNITS STAKED FOR THE MINING INDUSTRYnnUITI R AMn m nrIlFMIr AI IJRVrY 1 AIM RTAKINr UNF CUTTING SlJRVEYING ETCfJ
o
oo
o
o
o
o
o
o
o
c
o
c
oo
o
o
o
c
21tf
PHOENIX Geophysics Limited
200 YORKlANO alVO WIl I OWllAl I ONT ARID rANAOA M Jill lflEPHONE 4161 4916350r I 06 986856
Cab PHEXCO TORONTO
INVOICE
INVOICE No 3677DATE June 3D 1983
Selco Mining Corp Ltd55 University AvenueSui te 1700Toronto OntarioM5J 2f7
OUL J 198
REFERENCE Geophysical Survey Contract PV 1405IP and Resistivity Survey Lac La Hache B C
J Marsh P Gardner G Richardson
June B 1983 to June 19 1983
CREW
PERIOD
14 35 l klll 780 0011 km
One Operating Day SSO OO day
o YO
C ll 193 0fz Mr
II
12 043 00 V
OAlr GOons flUl1 ce r1 oJ L 1 3 198IE S K
xTENS DIY CHE KEOo f FA YMINT
JOBNUIh3ER
l
J2
J24110
J If 0
1 IO
O II
t
liP II
S S b 0SS 7C So
So Cle
Vancouver Office 214 744 West Hastings Street British Columbia V6C IA6Telephone 604 669 1070Denver Olllce 4891 Independence SI SUite 270 Wheal Ridge Colorado 80033 U S A Telephone 303 425 9353
I
U
Qo
0o
CHEMEX L BS LTD I 11111 J JK UANk AVf
NQAl Ii VANCOUVE R B C
CANADA VI 1 2Cl
ANALYTICAL CHEMISTS GEOCHEMISTS
rI
I VJI CE
SELCG MINING CORPORATION LTD
REGISTERED ASSAYERS
IUfPIIUNI IOU4 9U4 0221
1 EL X 043 2597
IInvoice N 18214717
o DEe 1 982 DateP O
Project
liJ OEC JNONE
10145
STE 402 535 ThURLCW STR ETVANCOUVER B C
V6E 3L2
O n o fnr onalytl ol nLk reportea on
Analystld for
011ant ity cIHla de sc ript lOA120 002 Cu pnm
006 Ag pprn
013 AS ppm
100 Au FA AA OPD
cer U f I c tls LJR 1471 7 nnl t L1llLl
un i t
IJr J C8 amount
o II 90 1428 00
o Sawple preparation and othtlr ch rJe
120 205 Rock geochem RING 2 50 300 00
oo
TOTAL
01 scount 10 l
S 1128 00S 172 80
Please pay this amount S 1555 20
ORMS NET 30 DAYS5 per month 118 per annum charged on overdue dccounts
o
n
0
o
o
o
0
t t GOOrJECEIVED
PI IC S O K
Xl cNsa CHECI rn
OK FOil P Y I N
v
JOB CODE
NUMBER
l
ill J C S
2 7 0 5
10 00
t53S lO
STA
o
oO
nvoice for analytical work
0Ana lysed for
uant i ty cOCle Clescr i pt ion
94 002 Cu pprn006 Ag ppm
013 AS pprn100 Au FA AA ppb
o000
o
on
o
o
o
O RMS
5 t
0
oInLJ
nJ
0
ANALYTICAL CHEMISTS GEOCHEMISTS
1 1 N O I t E
SELCO MINING CORPORATIDN LTO
II UII liK U NK AVlNOnTli VANCOUVER Be
CANADA V7J 2Cl
LLtPHONF 1604 984 0221
REGISTERED ASSAYERS I Ll x 043 52 91I
II
CHEMEX LABS LTO
Invoice N 18214950
STE 402 535 THURLOW STREET
VANCOUVER B CV 6 E 3 L 2 1fN
985
Da teP D NProject
10 JAN 83
NONE
L N
repo teCl on s t ifJe3 A8214950 001
un it
fl c amoun t
to 003
11 90 111B 60
2 002 Cu
005 Zn
006 Ag013 AS
100 Au 12 65 25 30
ppm
pprn
pprn
pprnppbFA AA
Sawple preparation and other charges
96 205 Rock geochern RING 2 50 24C 00V
TOTAL S 1383 90D scolJnt 10 t S 138 39
Please pay this a ount S 1245 51
NET 30 DAYS
per month 18 t per annum charged on overdue ccounts
00TE GCI lSnECE1i
jtl 1 f i us 3r lIGr o
Ly r NIONCH
OK FORr 11T c C
JOO CvDI
NUMBERc
uD
g 1 D IC 11
1lUVI Ii
jl0
0
IC ell
Ii
U
oo
0o
CHEMEX LABS LTD 1 HIli II J nMJ VI
NOH III VAN lJlJVlli U CCAN DA V71 CI
L1I II IoU4 UU411
ANALYTICAL CHEMISTS GEOCHEMISTS REGISTEREO ASSAYERS HIIX 0401 97
u n U i O I E JJSELCO MINING CORPORATION LTD Invoice 18310121
STE 402 535 THURLOW STREETVANCOUVER B CVbE 3L2
CJlVOi e for analvtlcal wOrJL UlllQLt ed on
Analysed for
code dAscr iJl1LQD002 Cu ppmOOb Ag ppm013 AS ppm
100 Au FA AA ppb
o
nuant v
o
o
DateP O 1
Project
3l JAN 83
NONE10145
cer tif i cateLsl A83 10lllllOl ill lO2
un i t
II r I CJL amaunL
11 90 bOb 90
Sample preparation and other charges
51 205 Rock geochem RING
00
O RMS NET 30
5 t per month
0
00
l0
0
0n
CTJ MEMnEA
2 50 127 50
TDTAL S 734 40DI scount 10 t 73 44
Please pay this amount bbO 9b
DAYS
1Bt per annum charged on overdue accounts
DATE GOODS CEB9
lECEiVi1t I TJJ1
p ICES o K
N C ECKED 0
rOR rA MNT0 1
CODEtOll 11 lc
HU 6tn
C c cW
1lIe lj j
t 1 11 c J
2
oCHEMEX LABS LTD
111 1 III B 1 11
cIHll1 vt NI fllVI H 1
IUd V
1111 IJlttlNI Ibll1 1Il1
nI
ANALYTICAL CHEMISTS GEOCHEMISTS HEGISTEAEO ASSAYEAS II II Y 1 1 I 1 1
DT L C II I C
I
iI
t III J t
f Iy
I
I
I1 C I n v J i c 1 Ii I 11 1 4
S T t 4J 2 5 T Ii i l T C T J 1 J l
oV C lJV
V6 Ll
rof
PrcJ t
r
Ie
l iYul frjr 1r IY ll 1 h fr r CCflCIj
O tr I pC fer
IG q t I tt C C J S C r I j I Q r
70 Jet u Crt
L Lit I i I t L c 3 1 ll 1 L J
I t
rl iiCt n
n C1
lCC u FL b
pr
n
IJ 1 I l J 1 C
D S c rrJ IE J r j d r t I n J fC 0the r t r r 1
o 7C 205 CCk ge c I C r 17 CC
o
o
TCTAlr I C Lnl t r
L 1 3 r j
t 1 C t
l I J J t r I I C v t r 2 4rJ
CRWS iT JC n Yi
D ner month 4 per rruHl ChofC on IVf r lJ Jcrcntfi
o
o8w cin
JU N 1 3 19 83CEI 1S O
h
i IXl WSION
1CI K fOR PA IMFII J1
riii r7 j lll Ii II l
l I I lll C
o
I
I Il
rjII
n
M MIII h
l ANAUIAN rU IINti0l 1 TIt
L
r
III
LIo
CHEMEX LABS LTD II H 1J1 Hld ll
Illll 1I Nfl 1 11
11
NALVTlCAL CHEMISTS nlOCHlMI jl 1J11 1 IlHl1l A AHRSIi II I ll Ill
III
1 11 ll
1
I
o L C vlt J r C T f l7 1 1 4 I I J 1
T j T l L l T
or I
l1
1
1 1 sl r J
1 v I I LlJ r
O Nl1 ty
r J I y I J I a r I r r
f J I y t j Jr
c rt J hJ i 1 llJnS 2 oJ 1 T
J It
II
I I t
1 I
1 11 y 1
r I l 11 1t
QA OToVv
I lS Jor
1 A J A I A Jj 7Vv
o I C L 1 t
T T L S
1 S
dl
J 12 r
III
II
oJ f I I t lr1t lcn 1l otlr r c r
o L lJ och q ocr l C 71
f
orI oJ I UI III ir t Z 1
JJ
0I
e yr n l t 1 i per 1 rJT 1 rlldr r l en V r J r r vrl
o
o
J FG SJ UN l O 1 9 83I
lt tl
i f 0 K
I iljr CI 7lKK fOR PI I IENltf 1
JI f lT
j
l17 1 I
u
o
1 If
I
I
IIiIIIIi
o
n I
o
OJ MI Mhlll
t lllt t I IlfI
1 1 111
ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS
I Blinn Iil
NOHl H VANCOUCANADA V J
TELL PHONE 16C 904 0
TELEX 043 525 1
tI
J CHEMEX LABS LTD
o
o
JUL 1 4 1983
I V lr
SELCQ KI INC COPPC ATION LTC
II
ro InV0ic rB31n o
nLJ STc 402 535 TH RLCh ST ET
VANCGUVER e c
Vet 3L2
o nv 0 ICE for na I y tic a I o r eEo r led D n
Ana Iysoc for
cede description004 Po ppm
OC5 In pprr
la teP
rcJect
13 JLLNSr
lC14
Quanti t
39
ertJf c to s AB312356 JOl
un j
EL h allclnt
2 a c 109 20
0
o
100
Saffple pre araticn and other c ar Je
39 214 3ay pulp o c co
TClALOi scclnt 10 S
109 20
lC 92
Please p3y t 15 till Ount Ie 2e
noJ J 77 J
1
i
IIII
I
I
iI
III
I
I
l S ET 30 CAYS
OJ Z uer month 13 per anr ml charged OP overdue dcccunts
o
o
o
OATE GOCOSRECEIVD JUl 1 4 1983
PRICES OK
F XTEII ION CHECKED
JONUMuER
O K fO PAYMENT
cc S
n
o
0
rUOOER
CANADIAN TESTING
ASSOCIATION
CERT F ChTE5 OF hN 5 5
ii
GG
1
QDU
nu
u
TELEPHONE 604 984 0221ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS TELEX 043 52597
r lm D A LYSIS IfS LCO lIfl IiG CIJll POll A r0 TTb CERT N AB214717 002
INVOICE N 18214717DATE 15 DEC 82P O H NONE10145
c
oo
C
C
C
o
C
o
oo
G
Te
CHEMEX LABS LTO
STS 402 535 THURLO STREETVf NUlUVtR 5 CV E 3L 2
ATT GEO JWSIACKI
saTIp Te Prep
J8scription codenntz 04 1 za5
22042 205
22043 20522044 20522045 20522046 205
22047 20522043 2 5
22049 20522050 20522051 20522052 20522053 20522C54 2022055 20522056 205
22057 20522058 20522059 20522060 20522061 20522062 20522063 205
22004 20522065 20522006 20522067 20522068 205
22069 205
22070 203
22071 205
22072 20
22073 205
2 074 20522075 20
22076 20522077 20522078 2052 079 0522000 205
D
o
co
o
o
DME MBEIl
CANAUlAN TESllNAssociATION
IEC 91
CC SELCO KAMLOOPScu A A S
ppm ppm ppm29 l 5
6 0 2 4
5 0 1 4
5 0 1 35 0 1 3
36 0 1 3
40 0 1 345 0 1 3
48 0 1 4
45 0 1 6
35 0 2 6
35 0 1 933 0 1 6
37 0 1 9
35 0 2 9
51 O I 1254 0 3 7
60 0 1 671 0 1 6
53 0 1 6
59 0 2 4q76 0 1 3552 01 4
51 O I 43
32 JI 43
55 0 1 3845 001 46
38 0 3 3960 0 1 63
57 0 1 10
64 0 1 1452 0 1 16
4d 0 1 16
46 0 1 1643 0 1 16
53 0 1 16
46 0 1 16
63 0 1 1461 0 1 16
55 0 1 25
212 BROOKSBANK AVE
NORTH VANCOUVER B C
CANADA V7 J 2C1
Au FA AA
ppb5
5
5
555
5
5
55
5
53
5
55
5
5
5
5
5
5
55
55
5
5
15
5
55
5
5
5
5
5
5
5
25
Certified hy
o
DTD
I
rL
nv
11L
fj
I
cG
D
o
o
o
o
0
CHEMEX LABS LTD
STc 402 535 THURLOVAlCO JV R 3 C
VoE 3L2
ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS
r J J A T A LY 1SELCO lNING CCRPO AT N LTJ
Ol SIACKI
Prepcode
205205
205
205205
205
205205
205
205205
205
205205
205205205
205205
205
205
205
205
205
205205
205
205205
205
l05205
205
205205
205205205205
205
STKEt T
ec 3ELClCu
ppm
6943
48
5365
64
8057
61
27
31
27
2729
71160
80
53
7053
7643
50
49
180104
125
114121
123
109102
135270
141
139liB220157130
12 BROOKSBANK AVE
NORTH VANCOUVER B CCANADA V7J 201
TELEPHONE 604 96 0221
TELEX 043 52597
CERT
INVOICEDATEP o
10145
A8214717 0031821471715 C C 82
lOJElEe 1 9S
KA Lacps
49ppmo I0 1
0 1
0 1
0 1
01
O L0 1
0 1
O I0 2
0 1
0 10 1
0 1
0 10 1
010 1OJ
0 1
0 1
0 1
0 1
0 20 1
O I
0 1Od
0 1
0 1
O L
0 1
0 10 1
01
O 1
0 2
O 1
001
ATTN GEORGE
fi samTe
descr iption2206122082
22083
2208
22085
22036
2208722088
22069
2209022091
22092
2209322094
220952209622097
2 09822099
22 100
2210122102
22103
221042210522 I06
22107
2210822109
221102211122112
22113
2211422115
22116221172211822119
22120
o MEMBERCANADIAN TESTING
ASSOC1ATION
AS Au FA AA
PpfTl ppb22 516 5
12 20
L 4 5
II 5
19 5
23 5L 2 5
L I 5
6 5
5 5
4 5
4 55 5
6 5
10 10II 5
L L 5
12 1014 5
12 10II 5
II 5
12 10
L 4 56 5
6 5
6 55 5
5 5
4 55 5
6 5
6 56 56 10
5 5
5 5
5 5
5 5
lC rtifiod by
ILJ CHEMEX LABS LTD 212 BROOKSBANK AVE
NORH VANCOUVER B CCANADA V7 J 2C 1
U 1 ELIoPHONE 604 984 0221
ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS TELEX 043 S2597
0 1 Eii i FIe A T EU O F A LY S IS
TO SHCO lINING CCRPORATION LTD CERT H A8214950 QOl
IC INVOICE II 18214950STE 402 535 THURLOW STREET OAH 10 JAN B3 IVANCOUVER B C P O I NONEV6E 3L2 p H0I
o GAM8LE lCAMLOOPS 1
IjSal1 p Ie Prep Cu Zn Ag AS Au FA AA
L description code ppm pprn pprn pprn ppb22121 205 115 0 1 9 1022122 205 49 0 3 7 10
II 22123 205 55 0 1 9 5J 22124 205 12 0 1 11 5
22125 205 61 0 1 10 5
0 22126 205 57 0 1 11 1022121 205 35 0 1 9 1522128 205 61 0 1 9 5
022129 205 46 0 1 10 10
22130 205 18 0 1 10 1522131 205 83 0 1 5 1022132 205 54 0 1 5 15
n 22133 205 49 0 1 10 5L 22134 205 112 0 1 11 10
22135 205 125 0 1 20 10
n 22136 205 192 0 1 15 5
J 22131 205 112 0 1 19 10
22138 205 51 0 1 11 10
G22139 205 45 0 1 61 1022140 205 55 0 1 61 10
J 22141 205 14 0 1 27 522142 205 19 0 1 32 5
n 22143 205 19 0 1 32 10I 22144 205 83 0 1 55 5
22145 205 80 0 1 33 5
n 22146 205 15 0 1 29 10
L1 22141 205 82 o 1 19 522148 205 15 0 1 17 10
n22149 205 12 0 1 25 522150 205 10 0 1 27 10
d 22151 205 55 o 1 32 522152 205 45 0 1 39 5
0 22153 205 10 0 1 30 522154 205 80 0 1 45 5
22155 205 84 0 1 45 5
022156 205 42 o 1 25 522151 205 31 0 1 24 5
22158 205 39 0 1 12 10
022159 205 41 o 1 16 5221 60 205 45 0 1 11 15
0 MEMBER Certified byCA NADIAN TESTING
ASSOCIATION
CHEMEX LABS LTD 212 BROOKSBANK AVE
NORTH VANCOUVER B C
0CANADA V7J 2Cl
TELEPHONE 6Q4 98 0221ANALmCAL CHEMISTS GEOCHEMISTS REGISTERED ASSAVERS TELEX 0 3 52597
0 rH n
uQ1 IFICA E F NALYSISJ hTO S EL CO I INING CORPORATION LTD CERT N AB214950 002
n INVOICE N 18214950
LJ STE 402 535 THURLOW STREET DATE 10 JAN 83VANCOUVfR B C P O N NONE
V6E 312JJ
0 j 1CC D GAMBLE KAMLCOPS
Sample Prep Cu In Ag AS Au FA AA
I descr I pt ion code ppm oom ol2Jr pom opbC 22161 205 43 0 1 9 5
22162 205 17 0 1 7 10
0 22163 205 57 0 1 14 522164 205 17 0 1 11 522165 205 24 0 1 14 5
022166 205 25 0 1 14 522167 205 26 0 1 12 5
2216B 205 26 o 1 11 5
22169 205 26 0 1 15 5
0 22170 205 24 0 1 14 522171 205 56 0 1 11 522172 205 27 01 10 10
022173 205 29 0 1 43 1022174 205 2B 0 1 27 1022175 205 2B 0 1 50 10
n22176 205 33 0 1 22 1022177 205 55 0 1 43 5
Li 2217B 205 51 0 1 39 522179 205 30 O 1 30 5
r 22 180 205 29 0 1 11 1022181 205 31 0 1 10 10
221B2 205 32 01 11 10
n22183 205 29 0 1 11 5
J 22184 205 30 0 1 12 5
22185 205 29 0 1 15 5
Q22186 205 32 O 1 12 10
22187 205 29 0 1 14 1522188 205 27 0 1 16 1522189 205 51 2 6 17 10
0 22190 205 28 2 0 50 1022191 205 32 5 3 20 1022192 205 30 4 1 14 5
022193 205 33 1 9 12 522194 205 52 3 0 12 5
2 2 1 5 205 61 0 2 7 5
22196 205 59 0 4 6 15
L 22197 205 59 01 7 522118 205 53 0 2 9 5
iO22199 205 18 1 8 6 5
22200 205 27 0 2 9 10
C fJCertified byMEMIER
CANADIAN TESTINGASSOCIATION
ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS
IL R T F C E NA LY S S I fTO SELCO NING CORPORATION LTD
c
oo
Qo
CHEMEX LABS LTO212 BROOKSBANK I
NORTH VANCOUVER
CANADA V7 J
TELEPHONE 604 984
TELEX 043 5
STREET
A8214950
1821495010 JAN 83
NONESTE 402 535 THURLCW
VANCOUVER B CV 6 E 3L 2
1
1
CERT H
INVOICE II
OATEP O tI
nCC D GA 8LE
Sampledescription
22201
22202222032220422205
2220622201
2220822209
2221022211
2221222213
2221422215
22216
I
01o
o
o
o
onLJ
oo
o
o
o
o
KAMLOOPS
Prep Cu
code ppm
205 21
205 19
205 42
205 62
205 44
205 40
205 25
205 26205 38
205 44
205 57
205 17205 27
205 54
205 50
205 54
Ag AS Au FA AA
pprr DPm ppb0 1 9 120
0 2 3 45
0 8 3 5
0 1 6 10
0 1 14 10
0 2 25 5
5 0 10 55
2 5 9 10
1 9 11 25
6 0 12 152 5 10 55 I7 5 6 15 I
2 C 14 15 I
1 0 10 10
0 1 15 10
0 5 12 5
In
ppm
90
84
MEMBER
CANADIAN TESTINGASSOOATION
Certified by
i CHEMEX LABS LTD 212 BROOKSBANK AVENORl H VANCOUVER 8 CCANAOA V7 J 2CI
r lLU HCJNL 604 984 0221ANALYTleAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS TELEX 043 52597
0 c ERT FI A O L s i ii
TO SElCO IINING COR PORA T 1 ON lTD CERT N A8310121 001 10 INVCICE 1 18310121OATESTE 402 535 THURLOW STREET 31 JAN B3 I
VANCOUVER B C P O N NONE
0V6E 312 10145
Ceoa FOItG nllttCKI J AlllnOl S
0Samp I e Prep Cu Ag AS Au FA AA
sescrifltioA code pflm ppm PPRl ppb22217 205 31 0 2 5 0 5
22218 205 27 0 1 3 0 5
0 22219 205 25 0 1 3 0 5
22220 205 29 0 2 3 0 5
22221 205 42 0 3 3 0 5
022222 205 51 0 1 4 0 5
22223 205 20 0 1 4 0 5
22224 205 38 0 5 5 0 5
22225 205 26 0 1 3 0 5
0 22226 205 62 0 6 3 0 5
22227 205 3 0 2 3 0 5
22228 205 47 0 4 2 0 10
022229 205 4 0 2 2 0 5
22230 205 50 0 3 4 0 522231 205 44 2 2 10 0 10
022232 205 29 0 1 6 0 5
22233 205 33 0 1 6 0 5
22234 205 250 1 2 10 0 522235 205 137 0 9 10 0 5
22236 205 51 0 1 9 0 5
22237 205 61 0 5 7 0 5
22238 205 31 0 1 7 0 522239 205 33 0 2 7 0 5
U 22240 205 35 0 1 7 0 5
22241 205 29 0 5 6 0 5
022242 205 38 0 7 7 0 522243 205 12 0 3 10 0 522244 205 76 2 6 32 0 2022245 205 42 0 6 16 0 10
22246 205 41 0 1 9 0 5
22247 205 67 1 8 35 0 10
22248 205 42 1 0 57 0 20
22249 205 73 25 0 20 0 115
lJ 22250 205 57 4 2 17 0 5
022251 205 B9 0 4 7 0 5
22252 205 29 01 3 0 522253 205 19 0 1 5 0 5
22254 205 35 0 1 10 0 5
22255 205 35 0 3 27 0 522256 o Al n 41 0
MEMBER Certified byCANADIAN TESTING
ASSOCIATION
CHEMEX LABS LTO
1 1 rPHONr
ANALYTICALCHEMISTS GEOCHEMISTS REGISTERED ASSAYERS TELEX
F N YS i l1TO SELCO INING CORPORATION LTD CERT H
INVOICE NDATEP o It
10145
o
o STE 402 535 THURLOw
VANCOUVER B CV6E 3L2
STREET
oCC GEOR IDLSJ1 lJ LKAMLOOP S
Samp I e Prep Cur1 r l p t i nIL CD d1L PPD
22257 205 5522258 205 53
22259 205 39
22260 205 35
22261 205 31
22262 205 48
22263 205 5522264 205 10322265 205 37
22266 205 7222267 205 38
o
o
IDi
O
o
Q
o
o
Ie
o
oo
o
0M MBER
CANADIAN TESTING
ASSOCI TlON
AgPPID
0 5
0 4
0 20 1
0 1
0 1
0 5
1 2
0 20 7
0 2
212 BROOKSBANK AVE
NCJII H VANCOUVER 8 C
CANADA V7 J 2C 1
604 904 0221
043 52597
A8310121 00lIB31012131 JAN 83NONE
AS Au FA AA
pnm p rh30 0 5
17 0 5
16 0 5
7 0 57 0 5
6 0 5
25 0 5
24 0 511 0 515 0 5
11 0 5
Certified by
c
ANALYTICAL CHEMISTS
CHEMEX LABS LTD
o
o IIGEOCHEMISTS REGISTERED ASSAYERS
llr lC l liL C 1 t i C C r 11 T I
I l 1
o J L Lc TT GEGRGE CWSIACKl
jr I rr CL
E fi t Cc u1L JL J JJJ Jlllf2ZliCl 2 4
2 C5 4CC ZC3 27
2 7 t i lj 1
Z C5 CJ 12
225 2S5 1322 7 2C3 Ii22r 2G 2C225CQ 2 S2 2 1 0 C 6
2211 2CS22i12 2C52213 2C
o T 4C2 533 T rLGhV r VCp C
v 3L
or1L
o
o
o 22514
Z 1 5
c 162517
t
c
i 1
o 2 G I
ci tj11
22 S 1 L
onI
IIU
o
o
o
o
jUi
MEMBERCANA DlAN TESTING
ASSOCIATION
ST rT
717 C
276
15C
10146
343
1l
r V r C f
T
l I c
12 IJi JUf SBANK AVEIfJIIIII li IJUVI It 13 L
CANMJi V7J 2Cl
LLl tHUNL bU4 984 0221
TELfX 043 52597
1 1 rl
l31hl
J L 1r
J u r 1 AI
n r I JJl mJ
I0
1 0H
0
4 I0 J 1Jo 4 1
t 4 l0
3 4 cV
1 5Jo
G 5 4 1
0 2 4 5
3 4 II 5
1 4 J
0 C
1 J
S IeJ ot
l 4
r I I 1
C
Q0
0
0
0
0
0
0
0
0
0
0
00
0
0
o
erg
CHEMEX LABS LTO I 1111111 IK I ANK AVl
NUllllI VANCOUV n c
CANADA V7J 2C1
ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS1 I
rv 1I E T J riel If J I
1 I
ILLH HUNl 604 9 4 0221
TlLf X 043 52597
LC I lf S C TI2 LTC
T I
ll v IS r I
311b44 CGIr 111 4 4
l JLT
2 3i TrC LCh ST1 r T T
Pvtc v r
L 1 1
ce GECP G CWSIACKI
J J 1 i I l r 1
J2i cr 1 J L n uf LC2 C
Sur
fL t
L iL Ll
I J
2
l
i 5 it
22 3t
2 lY 2C2 t c
L1
C1
2532
2L 33
J
2
zc
22 4
l21I
7
2 51
JJ
2
20
2
ZC
2 5
3 Ir
d
35 J l
3 I 17 J
2 Ie 11
3D 1 I
2 i 1 r
32 i 5 ill ll
os 7 Iv
26 7
4 l7
3 j 7 1S Jr 1
3 I r
I IJ
32 C 1
1 I I J
3r 3 I1 1 2
3
Z537
2 C
i 1
Zr
Ir
iC
I
2 I lI 7
rL
1
t I
J
r f
r l
i
12 la
I
t
I
J
01
r r
1
z 1J
MEMBER
ANAtltAN I IING
ASSOCIATION
iLl r I t J
CHEMEX LABS LTO212 BROOKSBANK AVE
tll 111111 VAIlfl lVllI IJ
CANADA V7J 2Cl
oo n
D
ANALYTICAL CHEMISTS GEOCHEMISTS
CE I lCl
SELCJ I I G CCRrCRATI LTD
REGISTERED ASSAYERS
ILlll lluNL LOt1 JU4 Ui 1
TELEX 043 52597
L Y j
o
o
o
o
o
o
o
o
o
TE 402 535 ThU LC
V C LVP 3 C
V L 3L 2
5TRr T T
3116 4 002
c311644
10 Jtt 1
c h T
VS Ie
H
1 Io
JUI
o
o
cc GECKGE J S 1l C rI
S ler J Ie Ore c 1J l I
l cr i lltlcr CJL1L QUir a lHi JI
22 o1J 2C3 4 1
Z2Sel 4 I 1
z 41
2 5 1 3 2 3
2Li64 205 36 0
22 i J 5 2 34 r
22 6 32 r 1 71 JJ
22i 7 2 C 5 31
S 3 205 27 t
2 Z t 205 Z 1 10
U570 a 20 1
2ZS 71 2Clj 24 1 c oj
22572 2CS 26 0 1 S i
2257 2nc ze v 6 5J
2 H 2 26 6v
2 75 2 5 29 0 1 S
22576 2C5 3E 0 2 IJ
22577 2 42 8 2 Iv J
Z2 7 no 41 t 7 10J
27579 20 39 1 7 cJ
25JO 205 53 1 4 10 5
o l 205 55 G 3 11 5
72 H J n 45 3I 5cv v
Z 3 3 2C 47 C O 7 5
2 5 4 C 4G fJ t I 10
2J 46 4 7 15c J
2 5 L 2CS 42 C 3 7 5
23 28i0 0 3 7 15J
I 2 3 0 1 7 101
j l 36 C 1 5J J
oo
o
o firMEMBER
CANADIAN TESTING
ASSOCI liON
C rtifie r J
Ci CHEMEX LABS LTDJUL 1 4 1983o
ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS
0 no U TE AUL YS I S JjTG SClCG I I G CCRPCRATIC LTC
o
Co
STE 402 5 5 TbURlCh STREETVANCCUYE 3 CYeE L2
0
o
CC GECRGE
SalTIe
aescriticn222312223222233
22234
2223522236
222312223B
22239
2224C2224122242
222 3
22244
2224522246
22241
22248
222492225C22520
225212252222523
22524
22525
2252622521
22528
2252922530
22531
22532
2253322534
22535
22536
2253722538
CWSIACKIPr e
CCGe
214
214
214214
214214
214214
214214
214
214
214
214
214214
214214
214
214
214
214
214
214
214
214
214
214
214
214214
214
214
214
214
214214
214
214
o
noo
o
o
n
o
n
o
c W MEMBER
CANAOlAN TESTING
ASSOCtATION
K AJ L OC P S
PI
PPIT
51
e
1C
75057C
1085
22
1117
46
41
23
1755011
141
235
IIC21e
Jill 1 4 1983
eeRT It
rr v IeE
CATCP c tl
le14
In
porr
213113
81
392
17819
113110
1079d
110
164
138199
144103
113202
21C
171
i212 BROOKSBANK AVENORTH VANCOUVER B C
CANADA V7J 2C1
TELEPHONE 604 964 0221TELEX O 3 52597
A8212356 001q 18312356
13 JUL 83I O E
II
1
II1I
I
IIII
Certifiec cyl
ii
i
I
CERTIFICAJ
CERTIFICATEOF AUTHOR
i
i
Ii
I
SECTION 7
i
n
DQQ
D
QnQ
Q
Dl
r
o
oo
o
o
o
o
o
o
o
o
o
o
o
o
o
o
CERTIFICATE OF AUTHOR
I George Owsiacki of 631 Lyne Road Kamloops British Columbia
hereby certify that
1 I am a geologist residing at the above address
2 I am a graduate of Queen s University Kingston Ontario
with an Honours B Sc degree in Geology 1981
3 I have practised my profession for more than 1 year full
time and for 4 summer field seasons
4 I co supervised the field activities described herein
5 I hold no interest direct or indirect in the GN 1 8
Claim Group which is the subject of this report
Respectfully submitted
G Owsiacki
Field Geologist
Kamloops B C
J
c
n
Qoo
CERTIFICATE OF AUTHOR
I Alan Wynne of 8573 Eboy Terrace Sidney British Columbia
hereby certify that
1 I am a geophysicist residing at the above address
nu 2 I am a graduate of the University of British Columbia
with a B Sc in Geology Geophysics 1976
o
o
oo
o
o
o
3 I have practised my profession for more than seven years
4 I supervised and interpreted the geophysical work described
herein
5 I hold no interest direct or indirect in the claims
which are the subject of this report
Respectfully submitted
IlJ
A Wynne
Geophysicist
o
oo
o
Vancouver B C
c
oo
oo
oo
o
o
o
oo
o
o
o
o
o
D
D
CERTIFICATE OF AUTHOR
I Dave Gamble of 7182 Blackwell Road Kamloops British Columbia
hereby certify that
1 I am a geologist residing at the above address
2 I am a graduate of the University of Ottawa with an
Honours B Sc degree in Geology 1973 and have completed
two years graduate studies leading to a M Sc at
Laurentian University
3 I have practised my profession for more than 7 years
4 I supervised the survey work on the GN 1 8 Claims and
interpreted the results of the survey described herein
5 I hold no interest direct or indirect in the GN 1 8
Claim Group which is the subject of this report
Respectfully submitted
A P D Gamble
Project Geologist
September 1983
Kamloops B C