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GEOLOGICAL GEOC CAL
and GEOPHYSICAL REPORT
METS 1 and 2 MINERAL CLAIMS
Lat 57027 North
Long 127022 West
N T S 94 E 6W
LIARD MINING DIVISION
for
GOLDEN RULE RESOURCES LTD
Calgary Alberta
o by
Michael Fox P Geol
TAIGA CONSULTANTS LTD
Calgary Alberta
or
o
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JANUARY 1982 MINERAL Rr J C S C CH
ASSE35 Vl T
3tB
INTRODUCTION
Location and Access
Property and OwnershipPhysiography and Glaciation1981 Exploration
REGIONAL GEOLOGY
PROPERTY GEOLOGYGeneral Statement
c Zone
B Zone
A Zone
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Certificate
SUMMARY
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TABLE OF CONTENTS
1
2
6
7
GEOCHEMISTRY
Sampling and AnalyticalStatistical AnalysisResults
11Procedures
GEOPHYSICS
CONCLUSIONS AND RECOMMENDATIONS
BREAKDOWN OF COSTS
21
22
24
APPENDIX I Analytical TechniquesAPPENDIX II Geochemical Analyses
APPENDIX III Geophysical Report
FIGURES
MAPS 1la
Ib
2
3
4
5
6
7
1
2
3
4
56
3
4
12
1314
15
Regional Location MapClaims Location MapCumulative Probability Graph Au in SoilsCumulative Probability Graph Ag in SoilsCumulative Probability Graph Au in RocksCumulative Probability Graph Ag in Rocks
Property Geology 1 10 000c Zone Geology 1 2 500B Zone Geology 1 2 500
Au and Ag in Silts and Rocks 1 10 000
Au in Soi1s 1 5 000
Ag in Soi1s 1 5 000Au in Rocks 1 5 000
Ag in Rocks 1 5 OOOTotal Field Magnetic Map Plate I Appdix III
o
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CERTIFICATE
I the undersigned of the City of Calgary in the Province of Alberta do
hereby certify that
1 I am a Consulting Geologist with an office at 100 1300 8th St
S W Calgary Alberta
2 I am a graduate of the University of British Columbia with a B Sc
in Geology 1974
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3 I have worked in the field of mineral exploration since 1965
4 I am a member in good standing of the Association of Professional
Engineers Geologists and Geophysicists of Alberta
Res
November 1981
1
1 1 GR BC 7
SUMMARY
o
During August 1981 approximately 27 5 line km of grid lines were
established at the Mets 1 and 2 claims A total of 829 soil samples were
collected at 25m intervals along these lines and semi reconnaissance
geological mapping and sampling were carried out over the property as a
whole utilizing a 1 10 000 scale topographic base A total of 263 rock
samples were systematically collected at grid stations in selected areas
of the grid A total of 98 rock samples were collected during the course
of property mapping Existing silt sample coverage was extended by the
collection of an additional 75 silt samples
g The results of this work have identified two epithermal stockwork
type Ag Au zones referred to in this report as the B and c zones
High Ag in soils values occur over a third area referred to herein as
the A zone Surface exploration of these zones to date is incompletewith all of the zones of interest still open along strike Recommendations
for further work include additional detailed surface mapping and samplingto be followed by trenching
B
II
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BThe above work was preceded in April 1981 by approximately 42 line km
of airborne VLF E M and magnetic surveying Structural interpretationsof geophysical data are included in a separate report appended hereto
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1 2 GR BC 7
1 INTRODUCTION
J Location and Access
oThe Mets 1 and 2 mineral claims form a contiguous block of claims
located in N T S map area 94 E 6W approximately 510 km northwesterlyfrom Prince George British Columbia at the headwaters of Metsantan Creek
Figure 1 The approximate geographic coordinates of the claims are
57027 North latitude and 127022 West longitude Figure 2 The claims
are normally accessible only by helicopterfIJ
aProperty and Ownership
BThe Mets 1 and 2 mineral claims are located in the Liard Mining
Division and are entirely owned by Golden Rule Resources Ltd of CalgaryAlberta The claims are described more specifically as follows
Claim No of Record
Name Units Number Date of Record
Mets 1 20 1253 April 3 1980
Mets 2 20 1254 April 3 1980o
8 Physiography and Glaciation
oThe claims lie within the Cassiar Mountains physiographic subdivision
of the Interior Plateau The region is entirely glaciated and is charac
terized by wide U shaped drift filled major valleys and deeply cut V shaped
upland valleys Mountain peaks in the area average 1980m 6500 ft ASL in
elevation and rise fairly abruptly from the major valleys The topographyof areas underlain by Toodoggone volcanic rocks is usually considerablymore subdued than areas underlain by Takla Group volcanic rocks
Qn
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The southern part of the Mets Group is located over a flat toppedhorseshoe shaped 198Om ridge that slopes steeply down into a deeply cut
south facing basin The northern and eastern facing slopes form steep
cirques and cliffs as a consequence of ice plucking and seasonal alpineglaciation
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127015 127000I
126045I
57015 Cha lIe
Mineral occurrence
Geochemical anomaly Au Ag
III Golden Rule PropertiesD DupontL Lacana
S Serem Agnico EagleSudbury Contact
TG Texas Gulf8
5730 5730
fJIL
8 5715
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MINERAL OCCURRENCE and
LAND MAP
TOODOGGONE Au Ag DISTRICT
7Jwlade
Q0 3 6 9 lJ1ke
57000l lometres
5ToOO
127015 12700 126045
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Figure 2 Location Sketch
of
lETS 1 and 2 Claims
N T S 94 E 6
Scale 1 50 000
I
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PEAK
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UETSANTAN 32961 rSJIIS rlllIll
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2 kilometres
n 5 GR BC 7
l The northern part of the claim group is located over an area of relatively
gently sloping low hills and ridges that are dissected by a number of
tributary streams at the headwaters of the northern fork of Metsantan Creek
Elevations here range from 1400tm to 1700tm ASL In some areas 30m to 60m
deep narrow canyons occur along the streams
Jo
1981 Exploration
Work carried out in 1981 consisted of airborne VLF E M and magnetic
surveying followed by helicopter supported geological mapping and geo
chemical sampling The airborne geophysical surveying was carried out
in April 1981 and the results of the survey are submitted in a separate
report in Appendix III8
nIn August 1981 approximately 27 5 line km of soil sampling were
carried out in two separate grid areas Grid controlled rock geochemicalsampling was also carried out over a 7 1 line km portion of the south
grid area A total of 829 soil samples and 263 rock geochemical sampleswere collected In addition 98 rock samples were routinely collected
from various areas of the claims during the course of geological mappingA total of 75 silt samples were also collected and submitted for analysis
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6 GR BC 7
REGIONAL GEOLOGY
The claims are underlain by intermediate to acidic volcanic rocks of
the Lower Jurassic Toodoggone Formation The Toodoggone volcanics form a
belt 5 20 km wide and 100 km long which is currently the focus of
intense precious metals exploration The belt hosts the Baker deposit
currently being mined by DuPont Canada Ltd and another potentially economic
deposit known as the Amethyst Gold Breccia Zone currently being explored
by Serem Ltd
Four principal subdivisions of the Toodoggone Formation are now recog
nized The following descriptions of these subdivisions are excerpted from
B C Ministry of Mines Paper 1981 1 p 125 by T G Schroeter
1 Lower Volcanic Division
This is dominantly a pyroclastic assemblage including purpleagglomerate and grey to purple dacitic tuffs
2 Middle Volcanic Division
This is an acidic assemblage including rhyolites dacites orange
crystal to lithic tuffs and quartz feldspar porphyries It includes
welded tuff The orange color of the tuffs resulted from oxidation
of the fine grained matrix while the rock was still hot A coeval
period of explosive volcanism included the formation of laharic
units and intrusion of syeno monzonite bodies and dykes This event
was accompanied by explosive brecciation along zones of weakness
predominantly large scale faults and attendant splays followed bysilicification and deposition of precious and base metals to varying
degrees in the breccias Rounded fragments of Omineca intrusive
rocks are rare components in Toodoggone tuffs
3 Upper Volcanic Intrusive Division
This division consists of grey to green to maroon crystal tuffs and
quartz eye feldspar porphyries
4 Upper Volcanic Sedimentary Division
This division consists of lacustrine sedimentary rocks sometimes
varVed stream bed deposits and possible local fanglomerate
deposits and interbedded tuff beds
0
7 GR BC 7
J PROPERTY GEOLOGY
General Statement
oGeological mapping of the Mets 1 and 2 claims was carried out utilizing
a 1 10 000 scale topographic base The results of this work are included
in a map in the back pocket Mapping was restricted to major bedrock
exposuresm
uThe southern half of the Mets 2 claim is underlain by green and orange
crystal tuffs corresponding to Division 2 or the Middle Volcanic Division
see preceding section of the Toodoggone Formation In the southeastern
corner of the Mets 2 claim the orange crystal tuffs are transected bya series of northwesterly trending brecciated silicified fracture zones
described in greater detail below In the west central area of the claim
a 25 50 m wide northerly striking quartz porphyry dyke cuts the crystaltuffs A 5 10 m wide zone of massive quartz and quartz breccia can be
traced for a short distance in felsenmeer along its east contact
nu
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oA variety of rock types of rhyolitic composition underlie low lying
areas in the central part of the Mets 1 claim Rock types include heavilypyritized leucocratic feldspar and quartz feldspar porphyries glassytuffs ignimbrites and thinly laminated ash beds the latter two types
being juxtaposed in a chaotic collapse breccia These rocks appear to
belong to Divisions 3 and 4 of the Toodoggone Formation Their presence
here might be explained by graben style downfaulting along northwesterly
trending fault zones
B
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DIIc Zone
oThe souteastern corner of the Mets 2 claim hosts a number of epithermal
stockwork zones of quartz stringers and quartz breccias developed in a fairlyextensive series of zones of pervasive silicification The latter zones
are a characteristic orange color due to oxidation of the crystal tuff host
unit presumably by ascending boiling hydrothermal fluids The alteration
zones are typified by partial to complete replacement by very fine grainedsilica clay minerals epidote carbonate and pyrite Minor amounts of
amethystine quartz were found in felsenmeer and talus in and adjacent to
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1 8 GR BC 7
J the zones Comb structures in cavities are common Feldspar porphyrybreccia fragments are frequently bleached and superficially resemble
rhyolite1
LJThe actual dimensions of the above described zones are somewhat
indeterminate since despite the high elevations bedrock exposures are
scarce Much of the detailed mapping and structural interpretation is
based upon observed distribution of the various rock types and alteration
zones in the blanket of felsenmeer that occurs over much of the highplateau like surface of this part of the property
oThe quartz stringer stockworks occur mainly towards the south end
of the zone in the vicinity of Lines 1 00S 000 1 00N and 2 00N
Exposures and felsenmeer to the north of this area indicate a lesser
intensity of fracturing and brecciation Quartz stringers here occur
most commonly as 1 10 metre wide parallel zones of 2 or 3 narrow stringers
and alteration envelopes rather than the stockworks noted in the southern
part of the zone As far as could be determined from mapping in the
felsenmeer quartz breccias and related quartz stringer stockworks form
pod like or lens like zones ranging from 4 or 5 metres in width to 20 metres
in width and 10 to 50 metres in length These northeasterly to north
northeasterly trending zones are crudely aligned in a northwesterly trendingarray suggestive of an en echelon series of tensional slips and dilations
An alternate interpretation of data acquired to date is that th stringerand breccia zones simply represent a parallel series of ractures and shears
distributed over a broad northeasterly to north northeasterly trending zone
of faulting
B
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o lfuatever the structural controls of the above zones prove to be it
is clear that this tensional regime formed the conduits for a significanthot spring centre Rock geochemical sampling carried out to date indicates
the presence of potentially economic grades of precious metals geneticallyrelated to the breccia and stringer zones The host rocks structural
environment alteration and relationship of mineralization to these zones
are strikingly similar to the Amethyst Gold Breccia Zone being developedby Serem Considerable latitude presently is afforded for tracing extensions
of these zones to the north of the 1981 grid area
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n 9 GR BC 7
J B Zone
8The B Zone is located in the west central portion of the Mets 2
claim area A small detailed grid was positioned here to test geochemicalresponse along the projected strike extension of a spectacular chalcedonic
quartz breccia zone mapped in felsenmeer at L 14N 8 00E The distribution
of cha1cedonic quartz breccia fragments in the felsenmeer suggests the
presence of a 10m 25m wide northerly trending breccia zone This zone
occurs adjacent to the eastern contact of a 50m wide pink northerly
striking quartz feldspar porphyry dyke which cuts Toodoggone dacitic
porphyry flows Division 2 the dyke was probably a major feeder zone
for rhyolitic extrusive rocks higher in the section The breccia zone
can be traced for approximately 50m in the felsenmeer but is quickly lost
to the north under talus covered slopes Very high Au in rock geochemicalanalyses up to 36 600 ppb occur in samples collected systematically at
grid stations along the projected extension of this zone The mineralized
trend eVidently extends off the grid area to the north and may be comprised
of a series of pipes or en echelon zones similar to the C Zone Work to
date is little more than a reconnaissance check of the zone and considerable
follow up work will be required to evaluate the mineralized trend
om
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B Although there is a limited number of data points available for the
B Zone there is a discernible increase in the Au Ag ratio in geochemicalanalyses in comparison to the c Zone The B Zone occurs 100m to 200m
lower in elevation than the c Zone suggesting the possibility pf vertical
zoning in the hydrothermal systems By corollary it would be logical to
expect an increase in the Au Ag ratio at depth in the c Zone
0
o
o A Zone
pU
The A Zone embraces the entire area of the Mets 1 claim that is
underlain by rhyolitic flows and tuffs characterized by high backgroundAg in soils geochemistry There are actually two major zones of interest
presently identifiedu
JThe first area is located in the west central area of the Mets 1 claim
in a zone underlain by heavily pyritized porphyritic rhyolite flows
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1 10 GR BC 7
J leucocratic ignimbrites and large blocks of bleached and kaolinized thinlylaminated ash beds and coarse pyroclastic debris chaotically juxtaposed in
a megabreccia or possible collapse breccia Very high Au in silt values
up to 620 ppb were located in this area Reconnaissance mapping and
rock chip sampling in this area have so far identified anomalous concentra
tions of Au and Ag in bleached kaolinized areas of the megabreccia
sample MS 32 300 ppb Au 8600 ppb Ag Highly anomalous Ag in soils
values occur in the same vicinity over an area 400m long by 200m wide
J
o
5 The second area is located in the southeast corner of the Mets 2
claim in a similar zone of widespread high background Ag in soils valu s
This area is underlain mainly by glassy highly fractured rhyolitic tuffs
Reconnaissance mapping and rock chip sampling in the vicinity of one of
the most intense Ag in soils anomalies have identified a brecciated fracture
zone in the tuffs carrying very high Ag in rock geochemical values sampleMS 38 108 ppb Au 10 700 ppb Ag Quartz and alunite occur as open
space fillings and stringers along the fracture system see location of
sample numbers MS 35 36 38
o
B
B
o Further exploration of the A Zone should investigate its potentialas a possible subsidence structure or downfaulted zone in which younger
rhyolitic rocks have been preserved at the stratigraphic level of Division
2 crystal tuffs and feldspar porphyry flows Such structures commonlyexhibit an arcuate or crescent shape as a consequence of radial and con
centric faulting patterns in a classic cauldron subsidence comple
Examples of these are well documented in early Tertiary rhyolitic centres
as at Bennet Lake see GSC Bulletin 227 The controlling structures of
subsidence may also have acted as controls for hydrothermal and fumarolic
activity The relatively flat dips in this area and the apparent relation
ship of soils anomalies to a particular stratigraphic horizon also requirethat the possibility of stratigraphic controls of mineralization be invest
igated
B
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o 11 GR BC 7
J GEOCHEMISTRY
o Sampling and Analytical Procedures
oA total of 829 soil samples were collected from 27 5 line km of grid
lines in two grid areas Line spacings were 100m and 200m Samples were
collected mainly from the B horizon at depths of 0 25m to 0 3Om at 25m
intervals along the lines In a number of areas at higher elevations
sample material consisted of a mixture of organic material talus fines
and poorly developed oxidized soil horizons
oo
Soil samples were collected utilizing mattocks placed in heaCY kraft
paper bellows type soil sample bags and partially dried before shipmentAu and Ag analyses were performed by Acme Analytical Labs Ltd of
Vancouver B C using standard wet atomic absorption procedures
o
o
oIn selected areas of the Mets 2 grid rock chip samples were also
collected at 25m intervals along grid lines The sampling technique used
required the collection of 12 or 15 small chips approximately 1 2cm in
diameter within a 10m radius of each grid station Field assistants were
instructed to collect rock chips that were representative of all the rock
types present at a particular sample point A total of 263 samples were
collected and submitted to TerraMin Research Lab Ltd of Calgary Alberta
for analyses The entire sample volume was pulverized sieved and analyzedfor Au and Ag by combined fire assay and atomic absorption Fwrther details
of analytical techniques are included in Appendix I
o
BD
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oStatistical Analysis
oSeparate cumulative probability graphs have been prepared for Au and
Ag in rocks and soils see Figures 3 4 5 and 6
oNearly 807 of the sample population of Au in soils falls at or below
the detection limit of 5 ppb The accompanying cumulative probability
graph Figure 3 is based on the analytical results of the remaining 169
samples Threshold values occur in the range of 40 ppb to 60 ppb Values
greater than 60 ppb are anomalousJ
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16 GR BC 7
The cumulative probability graph for Ag in soils Figure 4 indicates
a distribution closely approximating a normal distribution Slightinflections in the graph indicate that threshold values fall in the range
of 0 9 ppm to 2 1 ppm and values greater than 2 1 ppm are definitelyanomalous
The cumulative probability graph for Au in rocks Figure 5 indicates
that threshold values above background to probably anomalous occur in
the range of 30 ppb to 50 ppb Values greater than 50 ppb are considered
anomalous Threshold values for Ag in Rocks Figure 6 occur in the range
of 1400 ppb to 1800 ppb values greater than 1800 ppb are anomalous
Results
Ag in Rocks
1 c Zone Area
Rock chip samples collected systematically at grid stations in
the detailed grid area in the southeastern corner of the Mets 2 claim
have outlined two large zones of anomalous Ag values
One zone varies in width from 25m to 200m and extends northwest
wards for approximately 800m along a trend subparallel to Tie Line
13 00E This zone narrows to the north where it is still open alongstrike and extends off the claims to the south A second zone 250m
wide at its widest point trends north northeastwards for approximately300m crossing Lines 2N and 3N 150m to 200m east of Tie Line 13E
Possibly related zones extend the strike length of this zone an
additional 300m to the south The zone is still open to the north
Rock samples collected from zones of mineralization and alteration
within these areas see detailed geology map c Zone have returned
very high Ag and Au geochemical values
2 B Zone Area
Rock chip samples collected systematically at grid stations in
the detailed grid area in the west central part of the Mets 2 claim
have outlined two zones of anomalous Ag values
8 17 GR BC 7
J One of the zones averages 50m in width and extends northwestards
for approximately 300m along a trend subparallel to Tie Line 8 00E
This zone is open along strike to the southeast A second zone
averages 25m in width and extends north northeasterly for approximately40Om The zone is open along strike at both ends and IIlerges with
the first described anomalous zone at its south end Soils geochemistry indicates a probable extension of the northwesterly trending
zone of approximately 600m to the southeast Ag in soils data also
suggest a possible left lateral offset of the north northeasterly
trending zone where it meets the northwesterly trending zone The
soils data indicate a probable 600m long southerly trending extension
of this zone The possible left lateral offset is estimated to be
150m to 200m
o
o
o
3 A Zone Area
No detailed grids were established in the A Zone areas of the
Mets 1 claim Semi reconnaissance mapping and rock sampling have so
far identified two zones of anomalous Au and Ag in rock values
Both zones are associated with Ag in soils anomalies and are described
in greater detail elsewhere in this report see section on Property
Geology
B
o
B
oAu in Rocks
oRock chip samples collected systematically at grid stations in
the B and c detailed grid areas have outlined a number of anomalous
zones that exhibit close spatial relationships to the above described
Ag in rock anomalies
In the c Zone area Au in rock anomalies are somewhat more
restricted in areal extent than the Ag in rock anomalies Anomalous
Au in rock values occur in two prominent trends that closely follow the
anomalous Ag in rock zones The northwesterly trending zone exhibits
continuity and strike length similar to that of the Ag anomaly The
north northeasterly trending zone averages only 25m in width much
narrower than the corresponding Ag anomaly and more clearly defines
the north northeastwards trend of this zone
o
o
o
o
u
u
o
o
o
B
B
o
B
B
D
B
o
DlU
o
o
o 4
J
J
18 GR BC 7
In the B Zone area anomalous Au in rock values show a strong
correspondence to anomalous Ag in rock values in the north northeasterly
trending anomalous zone Continuity of the anomalous Au in rock trend
is not as well defined as the anomalous Ag in rock trend in the
northwesterly striking zone Soils data however suggest an 800m
strike length for the northwesterly trending zone still open to the
north and a left lateral offset of the north northeasterly trendingzone where it crosses the northwest trending zone
No detailed grids were established in the A Zone areas of the
Mets 1 claim Two areas of significant Au in rock values have been
identified by work to date and are described elsewhere in this
report see section on Property Geology
Ag in Soils
1 C Zone Area
Anomalous trends of Ag in soils values exhibit dimensions and
trends similar to those of anomalous Ag in rock trends described above
Ag in soils anomalies tend to be a little larger and more diffuse
as would be expected Continuity of the soils anomaly is not as goodas that of the rock anomaly in the northwesterly trending zone
2 B Zone Area
Anomalous Ag in soils values in this area form two pbpminenttrends closely corresponding to the previously described Ag in rocks
trends
3 A Zone Area
Anomalous Ag in soils trends occur over a 400m by 600m area in
the west central part of the Mets 1 claim and in two sizeable zones
in the southeast part of this claim The most easterly of the latter
two zones is a 25m to 100m wide 600m long northwesterly trendingzone open along strike in both directions A second 25m to 150m wide
400m long northerly to north northeasterly trending zone occurs
approximately 200m to the west
Other Areas
Highly anomalous Ag in soils values also occur at several other
locations in the Mets 1 claim area These zones are smaller than the
o 19 GR BC 7
J three major zones described above but they also warrant detailed
follow up
Two 25m wide 200m long anomalous Ag in soils trends located
in the west central part of the Mets 2 claim also warrant follow up
as does another weakly anomalous zone located near the middle of the
south boundary of the Mets 2 claim
o
o
Au in Soils
Au in soils anomalies correspond closely to the above described
Ag in soils anomalies in the c and B Zones
A moderately to strongly anomalous 800m long north northweaterly
trending zone occurs near the west boundary of the Mets 2 claim This
zones is subparallel to and approximately 200m west of the northwesterly
trending anomaly in the B grid area
In the A Zone area a strong 200m long anomalous trend is
defined by two 300 ppb Au in soil values in the southeast corner of
the Mets 1 claim This zone occurs in the vicinity of glassy fractured
limonite stained rhyolitic tuffs see sample MS 37 and lies approxi
mately midway between the two anomalous Ag in soils trends which also
occur in the southeast corner of the Mets 2 claim
A few other spot highs occur elsewhere on the Mets claims at
L36N 1775E 130 ppb L26N 2775E U20 ppb L6N 0050E 240 ppbL12N 425E 95 ppb and L2N 0900E 155 ppb All of these areas
warrant follow up checks in the field
o
8
o
B
o
oStream Silts
o
Df
Samples JS ST 33 to 35 and JS ST 50 to 54 define two separateanomalous Ag in silt trends at the headwaters of two tributaries of
Metsantan Creek which drain the B Zone area Work done to date on
the B Zone provides a satisfactory check of these anomalies
A single 750 ppb Au in silt value occurs at the sample site for
JS ST 30 in an area underlain by A Zone rhyolites Sampling below
this point failed to confirm the presence of very high Au in silt
values found during an earlier survey see assessment report on the
o
o
J
IJ
nI
20 GR BC 7
J Mets claims by this writer dated March 1981 This area should be
re sampled to confirm the presence of the anomaly at the JS ST 30
sample site and to determine why the earlier anomaly was not detected
o
5
o
B
B
o
B
o
J
o
D
o
oI
o
o
Di 22 GR BC 7
J CONCLUSIONS AND RECOMMENDATIONS
o The Au and Ag rock and soil anomalies in the B and c Zones constitute
attractive epithermal stockwork type precious metals exploration targets
The geologic settings of these zones bear strong similarities to the setting
at the Amethyst Gold Breccia Zone currently being developed by Seremo
rn Further exploration of the c Zone will require additional detailed
rock and soil sampling to trace the extensions of the anomalous trends to
the north Detailed mapping and sampling coverage of anomalous trends in
the B Zone should be similarly extendedB
o Sufficient data have been obtained to date over the c Zone to site
trenches for further evaluation of mineralized trends An estimated 1000m
of bulldozer trenching and detailed trench mapping and sampling Should be
adequate to check the anomalous trend which runs subparallel to Tie Line
13E The severe topography on the northeast facing ridge slopes will
preclude bulldozer trenching in this area However hand trenching and
blasting should be effective enough to clear talus and permit sampling of
the mineralized trends
B
o
o
BThe two anomalous Au and Ag trends in the B Zone will also be amenable
to further evaluation by bulldozer trenching and detailed trench mappingand sampling This work should be preceded by the additional detailed
grid controlled mapping and sampling recommended aboveD
01 IThe widespread Ag in soils anomalies favorable geologic setting and
anomalous Au and Ag values found to date in rocks provide justificationfor further exploration of the A Zone areas This work should consist
of an estimated 20 line km of detailed grid mapping and soil sampling
along lines spaced 100m apart Soil sampling should be augmented bycareful sampling of all rock exposures to try and pin down the somewhat
unpredictable mineralized trends in this area
o
D
o Bulldozer trenching in this remote area will be very expensive
requiring airlifting in of heavy equipment It is therefore recommended
that this program be mobilized on a cooperative basis with other companieswho are also active in the Toodoggone area Work being carried out by
o
o
u
o 21 GR BC 7
8 GEOPHYSICS
o In April 1981 a total of 42 line km of airborne VLF E M and magnetic
surveying were carried out over the Mets claims Instrumentation survey
techniques and the results of this work are described in a separate
report included in Appendix IIIo
B
o
B
o
o
B
o
o
o
0i
01
u
o
u
0
0
0
B
g
D
G
J
0
0
0
0
0
0
J
23 GR BC 7
Lacana Mining Corp Great Western Petroleum Ltd and Texasgulf now Kidd
Creek Mines Ltd has progressed to the point where they may be planningto carry out trenching programs of their own They should be contacted
to see if they are interested in mobilizing and demobilizing heaY equipment on a cost sharing basis
o
1
D
o
u
o
D
o
o
B
o
o
D
o
o
D
D
lJ
CHAPPELLE PROJECT COSTS
Mets Claims
Pro Rata charges see Schedule A
PERSONNEL
M Fox
Aug 7 8 9 23 24 25 30 5 days @ 250 00 1 250 00R Davies
Aug 8 9 24 30 4 days @ 141 88 567 52D Thompson
Aug 7 8 9 10 24 5 days @ 141 88 709 40T Nelson
Aug 7 8 9 24 4 days @ 156 25 625 00D Newman
Aug 7 8 24 3 days @ 120 31 360 93J Selwyn
Aug 7 8 9 15 24 5 days @ 120 31 60155H Larsen
Aug 7 8 9 3 days @ 9156 274 68M Plumbtree
Aug 8 9 24 30 4 days @ 9156 366 24B Moffatt
Aug 7 8 9 24 30 4 days @ 120 31 54140R Netolitzky
Aug 23 24 1 days @ 300 00 450 00 5 746 72
39 man daysPro Rata labour charges 39 man days @ 29 53 1 151 67
HELICOPTER
Aug 7 4 2 hours
Aug 8 5 1
Aug 9 5 0
Aug 10 0 5
Aug 15 0 5
Aug 23 15
Aug 24 3 0
Aug 25 10
Aug 30 12
22 0 hours
22 0 hours
22 0 hours
@ 375 hour
x 100L @ 1 25L@ 195
8 250 00
2 750 00
42 90
Fuel
Oil 11 042 90
CAMP ACCOMMODATION
Taiga crew 39 man days heli crew 10 man daysFood 49 man days @ 18
Camp Equipment 49 man days @ 12Pro rata camp and accommodation charges
49 man days @ 6 06
882 00
588 00
296 94 1 766 94
2
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IB
Chappelle Project CostsMets Claims Page 2
TRANSPORTATION
3 4 ton 4x4 pro rata 49 man days @ 4 88 239 12
EQUIPMENT RENTALS
two SBX ll transceiver radios
pro rata 49 man days @ 2 02 98 98
FUEL pro rata 49 man days @ 1 27 62 23
EXPEDITING SERVICES
pro rata 49 man days @ 4 88 239 12
FIXED lUNG SUPPORT
pro rata 49 man days @ 22 77 1 115 73
DISPOSABLE SUPPLIES
Sample bags flagging notebooks etc
Pro rata 49 man days @ 2 36
38155
115 64 497 19
FREIGHT COURIER
pro rata 49 man days @ 6 17 302 33
MISCELLANEOUS EXPENSES
oTelephone photocopying maps etc
pro rata 49 man days @ 2 48 1n 52
DTRAVEL EXPENSES
pro rata 49 man days @ 14 06 688 94
DHANDLINC CHARGES
127 of third party expensespro rata 49 man days @ 3 53 172 97
DGEOCHEMICAL ANALYSES
906 Au and Ag analyses of soil and silt samples @ 5 40 4 892 40332 Au and Ag analyses of rock samples @ 9 00 2 988 00 7 880 40
11U AIRBORNE GEOPHYSICAL SURVEY
VLF EM and magnetic surveys 41 95 line km @ S84 56 3 547 29
o POST FIELD EXPENSES
o
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Report preparation data plotting etc
DraftingSecretarial
Photocopying reproductions
2 500 00
500 00
150 00
300 00 3 450 00
GRAND TOTAL 38 124 05
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CHAPPELLE PROJECT EXPENSES SCHEDULE A
Schedule of Expenditures General Labor Costs Travel Expenses Crew MobilizationCosts General Project Expenses to be applied on a pro rate basis to variousclaim blocks as per man day formula total of 297 man days on the project
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Schedule A Page 2
FIXED WING SUPPORT Service
Aug 2 Caribou5 n
2 039 007 n
11 Cessna 185 449 0019 n
497 0020
n
491 0022 n
4910025 n
491 0027 DC 331 n
2 306 00
6 764 00
Service flights apply to various claim
groups on a pro rata per man day basis
Fuel Mob flights apply to various claim
groups according to heIi hours and
average cost per litre for transport
Fuel Mob
2 267 00
2 067 00
2 235 00
6 569 00 13 333 00
6 764 00297 n 77 man day
Aug 2 2267 18 x 205L drums 3690L 6144 6101
1 2245 L x 3690 4 518 40
Aug 7 2067 18 x 205L drums 3690L 5602 6101
117 L x 3690 4 317 30
Aug 27 2235 14 x 205L drums 2870L 7788 60961 3884 L x 2870 3 984 71
10250L 12 820 41
1 251 L average cost
125 10 fuel cost per heli hour
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APPENDIX I
Analytical Techniques
OMACME ANALYTICAL LABORATORIES LTD
Assaying Trace Analysi852 E Hutings St Vancouwr r B C V6A 1 R6
Talaphon 253 3158
GEOCHEMICAL LABORATORY METHODOLOGY 1981
SAMPLE PREPARATION
1 Soil samples are dried at 600C and sieved to 80 mesh
2 Rock samples are pulverized to 100 mesh
Geochemical Analysis for Ag Bi Cd Co Cu Fe Mn Mo Ni Pb Sb V Zn
0 5 gram samples are digested hot dilute aqua regia in a boiling water bath and
diluted to 10 ml with dimineralized water
All the above elements are determined in the acid solution by Atomic Absorptiondemotes background correction
Geochemical Analysis for Au
10 0 gram samples that have been ignited overnite at fiOOoC are digested with
hot dilute aqua regia and the clear solution obtained is extracted with
Methyl ISObutyl Ketone
Au is determined in the MIBK extract by Atomic Absorption using backgroundcorrection Detection Limit 5 ppb direct AA and 1 ppb graphite AA
Geochemical Analysis for Au Pd Pt Rh
10 0 30 0 gram samples are subjected to
techniques to prOduce silver beads
The silver beads are dissolved and Au Pd Pt and Rh are determined in the
solution by Atomic Absorption
Fire assay preconcentration
Geochemical Analysis for As
0 5 gram samples are digested with hot dilute aqua regia and diluted to 10 ml
o As is determined in the solution by Graphite Furnace Atomic Absorption
o
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MIN RESEARCH lABS LTD14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668
GOLDEN RULE RESOURCES
SAMPLE PREPARATION
Soil and sediment samples are dried and sieved to 80 mesh approx
200 mi on
Rock Samples
The entire sample is crushed to approx 1 8 maxinum and splitdivided to obtain a representative protion which is pulverized to
200 mesh approx 90 micron
rR
MIN RESEARCH LABS LTO14 2235 30th Avenue NE Calgary Alberta T2E 7C7
o
oGOLDEN RULE RESOURCES
0
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ANALYTICAL METHOD FOR GOLD AND SILVER
Approximately 1 assay ton of prepared sample is fused with a litharge
flux charge to obtain a lead button The lead button is cupelled to
obtain a prill The prill is dissolved in nitrichydrochloric acids
aqua regia and the resulting solution is analysed by atomic absorp
tion spectroscopy
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APPENDIX II
Geochemical Analyses
bFo
TERRAMIN RESEARCH LABS LTD
ANALYTICAL REPORT
o Job 81 286 Date January 25 1982
oClient Project
B
o
B
GR BC 7 Page 1 21
El
Sample No Au Ag
ppb ppb
MS L 000 11 00 E 6 300
11 25 6 660
11 50 142 26000
11 7S 2 280
12 00 2 140
12 25 164 13600
12 50 56 16200
12 75 126 42000
13 00 2 360
13 25 2 140
13 50 4 160
13 75 12 710
14 00 6 260
14 25 4 180
14 50 4 80
14 75 10 330
15 00 336 3000
15 25 6 530
15 50 10 540
15 75 6 90
16 00 6 920
16 25 4 530
16 50 14 1050
16 75 20 500
17 00 16 820
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14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
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B
o
B
o
B
A RESEARCH LABS LTD
ANALYTICAL REPORT
Job II 81 286 Date January 25 1982
Client Project GR BC 7 Page 1 2
01 I
Sample No Au Ag
ppb ppb
MS L 000 11 00 E 6 300
11 25 6 660
1150 142 26000
1175 2 280
12 00 2 140
12 25 164 13600
12 50 56 16200
12 75 126 42000
13 00 2 360
13 25 2 140
13 50 4 160
13 75 12 710
14 00 6 260
14 25 4 180
14 50 4 80
14 75 10 330
15 00 336 3000
15 25 6 530
15 50 10 540
15 75 6 90
16 00 6 920
16 25 4 530
16 50 14 1050
16 75 20 500
17 00 16 820
J
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D
01I
U
u14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
o tJgJtAMIN RESEARCH LABS LTD
oANALYTICAL REPORT
o Job 81 286 Date January 25 1982
o
o
B
g
D
8
o
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D
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Client Project GR BC 7Page 2 21
Sample NoAu Ag
ppb ppb
MS L 000 17 25 E O 1210
17 50 12 640
17 75 2 290
18 00 2 840
M5 L IN 11 00 E 4 460
11 25 2 800
11 50 2 3300
11 75 2 160
12 00 14 220
12 25 8 1360
12 50 74 230
12 75 32 400
13 00 6 180
13 25 8 150
13 75 2 20
14 00 4 400
14 25 2 60
14 50 2 270
15 00 4 90
15 25 4 280
15 50 2 170
1575 6 130
16 00 8 120
16 25 28 2400
14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
oA IN RESEARCH LABS LTO
ANALYTICAL REPORT
Q Job 1 81 286 Date January 25 1982
0Client Project GR BC 7 Page 3 21
D
Sample No Au Ag
ppb ppb
MS LlN 16 50 E 12 250
16 75 12 560
17 25 8 240
MS US 11 00 6 110
11 25 16 400
11 50 20 110
11 75 4 320
12 00 2 200
12 50 24 4400
12 75 16 1160
MSR L2N 13 00 18 3500
TL L2N 13 00 306 2300
MSR L2N 13 25 20 6000
13 50 10 750
13 75 6 500
14 00 14 1320
14 25 2 370
14 50 4 170
14 75 10 4500
15 00 10 9600
15 25 8 13000
15 50 32 2400
15 75 14 3600
16 00 6 1950
o
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o
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DII
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14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
D8o
Job I
o
o
B
B
D
8
lill TERRAMIN RESEARCH LABS LTD
ANALYTICAL REPORT
81 286 Date January 25 1982
Client Project GR BC 7Page 4 21
o
Sample NoAu Agppb ppb
MSR L2N 16 25 E 8 3600
16 50 16 1900
1675 4 4000
17 00 8 1470
17 25 a 10 8100
17 25 b 8 3000
17 50 4 460
18 00 70 220
MS L3N 11 00 E 4 740
11 25 2 430
11 50 2 530
11 75 24 2100
12 00 6 910
12 25 2320 11200
12 50 6 430
12 75 4 140
13 00 6 60
MSR L3N 13 25 E 6 100
13 50 4 110
13 75 4 200
14 00 12 900
14 25 6 610
14 50 16 1360
14 75 10 820
Uii1
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D
U
D
u14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
DJ
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o
B
o
8
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D
Oi
D
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A N RESEARCH LABS LTD
ANALYTICAL REPORT
Job II81 286
Date January 25 1982
Client Project GR BC 7 Page 5 21
Sample NoAu Ag
ppb ppb
MSR L3N 15 00 E 16 1350
15 25 6 230
15 50 6 450
15 75 10 720
16 00 38 5800
16 25 26 2800
16 50 30 4100
16 75 8 1060
17 00 8 780
17 25 6 400
17 50 8 3700
17 75 6 500
L4N 1100 EMS 20 700
11 50 18 680
11 75 264 1320
12 00 266 12800
12 25 6 630
12 50 6 140
12 75 2 600
13 00 4 550
13 25 6 20
13 60 2 190
13 75 6 50
MS L5N 11 00 E 6 330
14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
J l MIN RESEARCH LABS LTD
ANALYTICAL REPORT
Job IU 286 Date January 25 1982
o
B
o
B
o
B
J
J
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D
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Client Project GR BC 7 Page 6 2 1
Sample NoAu Agppb ppb
MS L5N 11 25 E 4 460
11 50 6 4000
11 75 8 1130
12 00 6 320
12 25 4 1350
12 50 4 410
12 75 8 1840
13 00 2 90
13 25 2 90
13 50 2 10
MS L6N 11 00 E 2 610
11 25 4 300
11 50 2 70
11 75 8 620
12 00 6 1020
12 25 4 810
12 50 2 1140
12 75 2 420
13 00 2 3300
13 25 18 360
13 50 2 180
M LIS 11 00 E 2 1020
11 25 8 3200
11 50 386 46000
14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
b 3r IN RESEARCH LABS LTD
J
0L Job
ANALYTICAL REPORT
8 286 Date January 25 982
o Client Project GR BC 7 Page 7 2
o
B
o
D
B
o
o
o
o
0
J
J
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Sample NoAu Agppb ppb
M LlS 75 E 20 2900
2 00 24 5600
2 25 O 3100
2 50 42 50
2 75 O 2020
13 00 2 680
4 25 130 720
4 50 84 3800
4 75 6 250
5 00 8 330
5 25 2 520
5 50 2 710
5 75 2 090
600 8 3500
6 25 2 390
6 50 2 780
6 75 6 760
17 00 6 320
7 25 4 690
17 50 4 200
7 75 38 030
8 00 24 OOO
MS L2S OO E 56 2000
25 4 940
14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
0l
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oJob I
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B
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B
D
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I RESEARCH LABS LTD
ANALYTICAL REPORT
81 286 Date January 25 1982
Client Project BC7 I M Page 8 2
o
Sample NoAu Ag
ppb ppb
MS L2S U 50 E O 1300
U 75 4 880
12 00 28 10200
12 25 4840 3900
12 50 10 2300
12 75 240 18700
14 50 2 100
14 75 2 160
15 25 2 130
15 50 2 40
15 75 64 680
1600 4 980
1625 4 640
216 50 250
16 75 110 620
17 00 2 300
17 25 2 170
18 00 2 1040
MS U5N 5 00 E 2 10
5 50 2 650
5 75 2 340
6lQO 2 40
25 2 20
6150 2 50
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J14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
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B
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D
o
o
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lIJf9 TERRAMIN RESEARCH LABS LTD
ANALYTICAL REPORT
Job I 81 286 Date January 25 1982
Client Project GR BC 7Page 9 ll
Sample NoAu Agppb ppb
MS L15N 675 E 2 330
7 00 2 120
7 25 4 2900
7 50 2 2400
7 75 6 1060
8 00 E 1010 2150
8 25 14 240
8 75 2 350
900 2 250
925 24 130
950 2 240
975 10 180
1000 4 690
MS L16N 5 00 E 42 770
525 2 60
5 50 2 50
6 50 2 400
675 2 40
7 00 2 140
7 25 10 3200
7 50 6 11100
7 75 2 750
8 00 4 940
8 25 2 90
14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
0
o
o Job
o
B
o
B
A1IJi9 TERRAMIN RESEARCH LABS LTD
ANALYTICAL REPORT
81 286 Date January 25 1982
Client Project GR BC 71 age
10 Zi
o
B
o
o
o
o
D
D
Sample NoAu Agppb ppb
MS L16N 8 50 E 2 100
8 75 6 940
900 26 2500
925 14 1300
950 5120 1350
975 544 1300
1000 36600 1640
MS Ll7N 5 50 E 2 180
5 75 2 230
600 104 180
625 24 190
6 50 14 520
675 2 350
7 00 2 1630
7 25 1294 900
7 50 6 1330
7 75 4 120
8 00 2 90
8 25 2 50
8 50 4 30
8 75 8 60
900 4 900
9 25 2 380
950 2 360
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14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
o
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yTERRAMIN RESEARCH LABS LTD
ANALYTICAL REPORT
o Job 81 286 Date January 25 9B2
J
o
B
o
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Client Project GR BC 7 Page 11121
Sample NoAu Agppb ppb
MS L17N 975 E 2 170
OOO 322 900
MS L1BN 500 E 2 170
5 25 2 100
5 50 2 30
5 75 2 30
6 25 2 20
6 50 2 40
675 2 270
7 00 2 290
7 25 2 490
7 50 224 620
7 75 2 200
8 00 60 760
8 25 1 2 770
8 50 2 50
8 75 2 330
900 2 70
925 2 120
950 2 160
975 2 410
1000 8 110
MS 8 10 2200
9 14 1730
14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
DJ
10
o
B
RA RESEARCH LABS LTD
ANALYTICAL REPORT
Job II 81 286 Date January 25 1982
Client Project GR BC 7 Page 12 J
o
BQ
o
B
o
o
o
u
o
Sample NoAu Agppb
ppb
MS 9 14 1730
10 180 5200
11 32 4000
12 2 1420
13 10 1350
14 30 3300
15 2 80
16 4 1040
17 2 140
18 2 290
20 2 110
21 616 6100
22 7p 2200
23 4560 1880
26 40 80
27 2320 1400
28 8 200
29 2 130
29 a 2 210
30 2 310
31 92 860
32 300 8600
33 2 290
35 2 600J
J
U14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
ANALYTICAL REPORT
o Job 81 286 Dale January 25 1982
o Cfienl Project
o
8
o
B
o
o
o
D
o
oII
GR BC 7Page 13 21
Sample NoAu Agppb ppb
MS 36 20 2300
37 2 1290
38 108 10700
39 2 100
41 8 1240
42 2 80
43 2 350
48 2 120
49 26 820
u14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
o
o
B
o
8
o
B
o
o
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U
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ANALYTICAL REPORT
Job 81 286 Dale January 25 1982
CDenl Project GR BC 7 Page 16 21
Sample NoAu Agppb ppb
MSl7r 1 2 50
11 2 60
12 2 40
18 2 300
20 2 590
14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
o
o
B
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B
o
B
D
J
D
o
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ANALYTICAL REPORT
Job 81 286 DateJanuary 25 1982
Client Project GR BC 7 Page17 21
Sample NoAu Ag
ppbppb
M5DT 21 182 101000
22 18 1600
23 6 3500
25 2 2000
26 2 320
28 12 3600
29 10 880
30 172 5600
31 36 520
32 848 8800
33 12 540
34 6000 41000
35 788 13800
36 18 3600
37 36 I 60PO
38 2 430
39 8 2400
40 24 380
42 6 1650
43 856 2500
44 42 6300
46 68 540
14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
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B
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RAMIN RESEARCH LABS LTD c gc 7
ANALYTICAL REPORTGOLDEN RULE RESOURCES LTD
Job 81 289 Date September 25 1981
Client Project Gl f Page 1 1 D o II
Sample No Au Ag
ppb ppb
4157 8 780 7 enJ tat4
4158 1464 148000eAll rpH pfp A9trr
tIV 3S r
4160 4240 31000 v ji fft fp7 PJ Me11
4161 2 130 dL1J Ij d S 17 t
rz vJj wrJry ze
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14 2235 30th Avenue N E Calgary Alberta T2E 7C7
403 276 8668 Telex 03 821172 CGY
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on
36 75 2 005 i 4Zfilo
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1 25 2 Oos 67 50 I 005 I 177 7 L 005 I Its
I I 1 lURHlO OO iI
8 4 000 I 108150 005 I t I 11llL7 i nne i i I I I 12ou nn I I I i i 13
1 9 25 3 005 1 I i 149f5n I nn
I I 152 15 51 DD5 i I
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16lCl1illl LJoos I 17
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1Lj i I I13 25 N S
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301 WQ 3 7
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To Golden Rule Resources
150 1300 8th S W
Calgary Alberta
T2R 1P2
Assaying Trl Analysis852 E Hastings St Vancouver B C V6A 1R6
phone 253 3158
Ltd
File No 81 1333
cc Taiga Consultants Ltd SoilslYpe or Samples
GEOCHEMICAL ASSAY CERTIFICATEDlSpOSltion
S AMPLE No
Mo M
T Au I I I I I I I IAg
All reports are the confidencial property of clientsAll results are in PPM
DIGESTION
DETERMINATIONn
DAlE SAMPLES RECEIVED lPJ fi 1981DAlE REPORTS MAluD iU1 Z J2 L
ASSAYER
DEAN TOYE B Sc
CHIEI CHEMISTCERTlnED C A AYER
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Golden Rule Resources LtdA1S ying Trace An lysis
852 E Hastings St Vancouver B C V6A 1R6
phone 253 3158
File No 81 1333
SoilsIYpe of Samples
GEOCHEMICAL ASSAY CERTIFICATEDisposition
TTAglAUI T T T I I I I I
DAll reports are the confidencial property of clients
All results are in PPM
DIGESTION
DAlE SAMPLES RECEIVED Sept 6 1981
DAlE REPORTS MAILED Sept 17 1981
LJDETERMINATION
U
ASSA YERr
DEAN TOVE B Se
CHIEI CHEMIST
CERT I1ED ac A5SAVEIt
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OS AMPLE No
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To Golden Rule Resources Ltd
M l IVIIM I JLTIILAL LAtjUtiA IUtiII LIU
Assaying T Analysis852 E Hastings St Vancouver B C V6A 1 R6
phone 253 3158
81 1333Fae No
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Dispolition
1234
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All reports are the confidencial property of clients
All results are in PPM
DIGESTIDN
DAlE SAMPIES RECEIVED Sept 6 1llL
DAlE REPORTS MAILEDSept 17 1911
DETERMINATIDNASSAYER
UiDEAN TOYE B Sc
CHIEF CHEMIST
aRTIPJ1D C IiAYEfI
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OSAMPLE No
IL3N
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To Golden Rule Resources Ltd Assaying Trace Analysis852 E H8Stings St Vancouver B C V6A 1R6
phone 253 3158
File No l1 3Soils
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Dilpoation
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A P PEN D IX III
Geophysical Report
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REPORT ON A
HELICOPTER VLF E M AND MAGNETOMETER SURVEY
ON TEN PROJECTS IN THE
TOODOGGONE RIVER AREA
OMINECA MINING DIVISION
BRITISH COLUMBIA
FOR
GOLDEN RULE RESOURCES LTDSuite 115 1300 8th Street S W
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SURVEY DATES April I to May I 1981
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July 3 1981Vancouver B C
Apex Airborne Surveys LtdRonald F Sheldrake B Sc
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TABLE OF CONTENTS
1 SUMMARY
2 INTRODUCTION
3
4
5
GEOLOGYCLAIMS
LOCATION AND ACCESS
DATA PRESENTATION
DISCUSSION OF RESULTS
CONCLUSIONS AND RECOMMENDATIONS
BIBLIOGRAPHY
Page No
1 1
2 1
2 42 52 6
3 1
4 1
5 1
FIGURE 1 SURVEY AND CLAIM LOCATION MAP
FIGURE 2 DETAIL ANOMALY LN 5 SAUNDERS PROJECT
PLATE 1 MAGNETIC CONTOUR MAP METS GROUP
PLATE 2 MAGNETIC CONTOUR MAP BELLE GROUP
PLATE 3 MAGNETIC CONTOUR MAP SAUNDERS GROUP
PLATE 4 MAGNETIC CONTOUR MAP JOCK GROUP
PLATE 5 MAGNETIC CONTOUR MAP RICH GROUP
PLATE 6 MAGNETIC CONTOUR MAP MC GROUP
PLATE 7 MAGNETIC CONTOUR MAP JC GROUP
PLATE 8 MAGNETIC CONTOUR MAP NIKA GROUP
PLATE 9 MAGNETIC CONTOUR MAP INGE GROUP
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PLATE 10 MAGNETIC CONTOUR MAP SUS GROUP
APPENDIX I INSTRUMENTATION
APPENDIX II IN FLIGHT RECORD AND FLIGHT PATH RECOVERY
CERTIFICATION
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I SUMMARY
The geophysical data have provided a useful overview of magnetic character of
the rocks underlying the claim groups An electromagnetic target has been identified
in the Saunders Claim Group that warrants investigation
Recommendations for follow up have been made
o 2 I
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2 INTRODUCTION
This report describes the results of 420 linear kilometres of combined VLF and
Magnetic Helicopter Survey undertaken over II claim blocks in the TOODOGGONE
D
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RNER AREA B C
The claim blocks are located near or along regional strike to the Chappelle and
Sawyer gold deposits within the Intermontane Belt A description of the Chappelle
deposit and environs is available in apublication by Mr D A Barr of Dupont ofCanada
Exploration Ltd
The purpose of the helicopter magnetic and electromagnetic surveys was to
provide targets for ground exploration and to assess in a general sense if similar
environments as those present at the Chappelle and Sawyer properties could be
recognized
The survey was flown using an Aerospatiale Gazelle Helicopter as a platform for
the geophysical system
DD A Barr Chappelle Gold Silver Deposit British Columbia
Geology and Exploration pp 66 79
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The survey conditions were difficult for the most part because of inclement
weather conditions and steep terrain
The electromagnetometer used on this survey was a Herz TOTEM I A VLF
device It utilizes the primary fields emitted by the military communication
transmitters The E M fields from the stations Cutler Maine and Jim Creek
Washington are essentially perpendicular to the direction to the station and
horizontal
The EM sensor is suspended five metres below the helicopter to minimize
helicopter interference and comprises of three coils whose axis are orthogonal The
electromagnetometer senses the change intotal field and quadrature values These
are the two measurements recorded on the analogue chart and magnetic tape
The VLF electromagnetometer although described as avery low frequency radio
signal 15 25 khrz is rather a high frequency signal for geophysical purposes This
means that the system senses rather large low conductance targets that are within a
few tens of metres from the surface
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The magnetometer used on this survey was a Geometries G803 total field
instrument which measures the field strength with a sensitivity of one gamma The
sensor is suspended below the electromagnetometer 15 metres
Appendix 1 gives the details of the geophysical equipment used for this survey
Appendix IT describes the in flight record and flight path recovery process
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GEOLOGY
The geology of the Chappelle Deposit and environs is described by Mr D A Barr
of Dupont of Canada Exploration Limited
He reports that The Chappelle property lies near the eastern margin of the
Intermontane Belt The quartz vein systems which contain the gold silver
mineralization occur within a smaIl window of Takla Group volcanic rocks of UpperTriassic age which are intruded by granitic stocks of the Omineca IntrusIons and
overlain unconformably by Jurassic and younger volcanic and sedimentary rocks
Rocks in the property area have been subject to extensive normal block faultingfrom Jurassic to Tertiary time and by thrusting of the Asitka Group rots over the
Takla Group rocks during Middle Jurassic time
No detailed geology of the ten survey blocks described in this report is available
to the writer at this time
Ibid
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LOCATION AND ACCESS
The claim blocks are all located in the Omineca Mountain Range The easiest
access to the properties is by helicopter from either McKenzie or Smithers B e
The location to the centre of each claim group is as follows
CLAIM GROUP LATITUDE LONGITUDE
METS 590 24 N 1270 17 W
BELLE 570 24 N 1270 10 W
SAUNDERS 570 18 N 1270 02 W
JOCK 570 15 N 1260 52 W
RICH 570 15N 1260 40 W
MC 560 52 N 1260 30 W
JC 560 50 N 1260 28 W
NIKA 560 49 N 1260 22W
INGE 560 37 N 1260 B W
SUS 560 30 N 1260 46W
N T S
94 S W
94 S W
94 S W
94 S W
94 S W
94 S W
94 S W
94S W
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3 DATA PRESENTAnON
The data have been presented as plan maps of aeromagnetic contours at a scale
of 110 000 The location of VLF E M anomalies interpreted lineaments and photo
lineaments have been plotted on these plan maps The maps display sufficient
drainage to key them to the photo mosaics that were supplied to fly the survey
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4 DISCUSSION OF RESULTS
Twelve test lines of survey were flown over the Chappelle and Sawyer Gold
properties in order to identify any characteristic geophysical responses that could be
recognizable on any of the ten present survey areas
For the most part no specific feature is correlatable with surety however it is
apparent from the records that the magnetic environment of the ten present survey
areas are similar to that of the Chappelle and Sawyer areas
No VLF E M responses were recorded on the Chappelle and Sawyer test lines
The Golden Rule survey blocks are small in areal extentforan airborne
reconnaissance survey and therefore limit the effectiveness of their in Jpretation
however in general many of the specific features reported by Mr Barr may be
interpreted from the data namely fracture zones contact areas and possibly block
faulting
Ibid
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Any attempt to identify qu tz veins from the aeromagnetics however is
probably not justifiable for the following reasons
1 Ground magnetic surveys over the Chappelle have not been reliable in
extending quartz veins
2 The magnetic character of the survey areas is very complex
3 The quartz veins are probably too small to be identified from an airborne
survey
A brief interpretation has been made of the magnetic contour map for each
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claim block The geophysical lineaments that were interpreted may be either contact
or fault lineaments Predominant photo lineaments have also been plotted here they0
D1are informative very often because of their contradition to the geophysical map
rather than their coincidence
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It should be noted that the contouring process tends to filter the data and that
the in flight recording indicates greater detail than the contour maps As groundevaluation proceeds detailed study of the smaller and numerous responses on the
recording may be useful
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UIbid Page 77 Geophysical Investigations
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The VLF EM technique over some of the survey areas and the test lines has
not been successful as a survey tool A combination of steep terrain and inclement
weather conditions made it difficult to maintain a constant sensor orientation in the
fixed VLF E M transmitted field However useable VLF E M recordings were
collected over the Belle Mets and Saunders Projects and one VLF anomaly on LN5 on
the Saunders project warrants immediate ground investigation See Figure 2 for a
detail of that record A schematic diagram has been provided that is meant to
indicate the relative location and attitudes of the targets and will not reflect the true
complexity of the geological situation
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400HEL COPTER TERRAINE
CLEARANCE200
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VLF QUADRATUREfi
I CONTACT OR
VFAULT ZONE
GROUNDX X X X SURFACExxxx
XXXzcI XX MAGNETIC
1 ZONE
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FIGURE 2
NOTES
Coincident With InferredMagnetic Contact
2 Possibly Extends to LN 6and LN 7
DETAIL ANOMALY SAUNDERS CLAIMSLINE 5 NORTH
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CONCLUSIONS AND RECOMMENDATIONS
The geophysical survey has provided useful information that will serve to guide
the upcoming exploration program
Further one VLF E M target appears quite substantial and warrants
investigation
It is recommended that each of the areas be mapped geologically and stream
samples taken wherever possible
For the anomalous response on LN5 in the Saunders Area several traverses of
ground VLF EM ought to be undertaken to assess its validity an dUctiVe
response
Respectfully Submitted
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BIBLIOGRAPHY
D A Barr Chappelle Gold Silver Deposit
British Columbia
GEOLOGY AND EXPLORAnON
CIM Bulletin February 1978
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APPENDIX I
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APPENDIX I
INSTRUMENTAnON
VLF Electromanetic Instrument
Type
Frequencies
Manetometer
Type
Cycling Time
Sending Head
Design
Ancillary Equipment
Helicopter mounted total field quadrature instrument manufactured by Herz Industries Ltd Toronto Ontario
Cutler Maine 17 8 kHz NAA
Jim Creek Washington 18 6 kHz NLK
Proton precession model G803 manufactured by Geometries
Corporation Toronto
1 0 second
5 inch diameter Toroid
UDAS Digital Acquisition System with recorder
Geocam 35 mm Flight Path Camera
Bonzer RadioAltimeter
Geometries G806 Magnetic Base Station and recorder
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APPENDIX IT
THE ANALOGUE CHART AND FLIGHT PATH RECOVERY
The flight tape is a roll of chart paper which moves through the digital printer at a
speed of 5 48 cm per minute
The digital printer chart facilitates the use of a full alpha numeric system Allheader sensitivity and fiducial information is printed automatically
The chart is 520 dots wide as follows
DOTS
o 100 magnetometer coarse 2000 gammas full scale
100 320 magnetometer fine 440 gammas full scale
320 400 total field 25 full scale
400 480 quadrature 25 full scale
48lF52D altimeter OltlO N
The helicopter flight path is recovered from 35 mm film which is osed at 2 0second intervals during the flight traverses After processing and anotating r gnizablefiducialsare pin pointed on the photomosaic map
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CERTIFICAnON
I RONaLD F SHELDRAKE of the City of Vancouver Province lOIiBritish Columbiahereby cert y as follows
1 I am President ofApex Airborne Surveys Ltd a company incorpmated under the lawsof the Province of British Columbia
2 The Yanc ouver Office of Apex Airborne Surveys Ltd is located at fuilite 512 625 HoweStreet Vancouver British Columbia
3 I lec ejYed my B Sc in Geophysies from the University of British Columbia in May1974
4 I haMejPJilctised my profession since that date
5 I did ililotexamine the claims area but I am not aware of any claim conflictand bclievethat 1he data presented herein is reliable
6 I halle no interet direct or indirect in GOLDEN RULE RESOOR JLTD or itsa1es nor do I expect to receiveany
7 Lwnsent to the usescoft this report in Dr in C9nnection Witb a 1lroectJJS or iriaJitateJDent of MaterlaltFactsi 1llt tt v
Ronald iF SbeldIalre
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STATEMENPOF COSTS
Type ofSUilYeyDate s ofFieJdwork
SurveYt KUOmetres
COst pen
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July 3 19 c
April 1 to May J lJ9 l
Combined VL a cMagnetic Helicop u y1
420 kilometres
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