SUMMARY REPORT
on the
GOLD KING PROPERTY
(NI 43-101 Compliant)
Pemberton - Tenquille Lake – Birkenhead River Area of
British Columbia, Canada
N.T.S. 92J/7W, 92J/10W & 92J/11E
Latitude 50º31’02”N/Longitude 122º53’14”W
for
Wolverine Minerals Corp.
1205 – 789 W. Pender St.
Vancouver, B.C.
V6C 1H2
Phone: 604-685-9181
Fax: 604-685-9182
Prepared by:
Sean Butler, B.Sc., P.Geo.
3252 Ganymede Dr.
Burnaby, B.C.
V3J 1A4
Phone / Fax: 604-421-5959
E-mail: [email protected]
December 21, 2006
Revised January 11, 2008
Table of Contents
SUMMARY -------------------------------------------------------------------------------------------1
INTRODUCTION------------------------------------------------------------------------------------1
RELIANCE ON OTHER EXPERTS -----------------------------------------------------------2
PROPERTY DESCRIPTION AND LOCATION---------------------------------------------2
ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND
PHYSIOGRAPHY ----------------------------------------------------------------------------------6
HISTORY ---------------------------------------------------------------------------------------------8
GEOLOGICAL SETTING ---------------------------------------------------------------------- 12
DEPOSIT TYPES--------------------------------------------------------------------------------- 14
MINERALIZATION ------------------------------------------------------------------------------- 15
EXPLORATION ----------------------------------------------------------------------------------- 15
DRILLING ------------------------------------------------------------------------------------------ 19
SAMPLING METHOD AND APPROACH ------------------------------------------------- 19
SAMPLE PREPARATION, ANALYSES AND SECURITY----------------------------20
DATA VERIFICATION -------------------------------------------------------------------------- 20
ADJACENT PROPERTIES--------------------------------------------------------------------21
MINERAL PROCESSING AND METALLURGICAL TESTING---------------------- 21
MINERAL RESOURCE AND MINERAL RESERVE ESTIMATES ----------------- 21
OTHER RELEVANT DATA AND INFORMATION -------------------------------------- 22
INTERPRETATION AND CONCLUSIONS------------------------------------------------ 22
RECOMMENDATIONS AND BUDGET ---------------------------------------------------- 23
REFERENCES ------------------------------------------------------------------------------------ 24
DATE AND SIGNATURE ---------------------------------------------------------------------- 27
CERTIFICATE OF AUTHOR ------------------------------------------------------------------ 28
Table 1
Table 2
Table 3
Table 4
Tables
Holdings of Wolverine Minerals Corp., on Nov 10, 2007.---------------3
Holdings of Wolverine Minerals Corp, on Nov 10, 2007.----------------3
Exploration Costs by Wolverine Minerals. -------------------------------- 19
Geochemical Analysis of samples collected by author--------------- 19
Figures
Figure 1 - Claim Locations ---------------------------------------------------------------------4
Figure 2 – Generalized Location in British Columbia, Canada--------------------7
Figure 3 - Regional Geology and Historical Showing Locations --------------- 11
AT THE END OF THE REPORT
SJ GEOPHYSICS INDUCED POLARIZATION CHARGEABILITY AND
RESISTIVITY PLANS
FIG 6-STEPENSON’S SAMPLES
FIG 7-GENERAL LOCATION OF ROCK SAMPLES MAP
FIG-7b DETAIL OF AREA II LOCATION OF KRAUSE’S ROCK SAMPLES
FIG-7c DETAIL OF AREA I LOCATION OF KRAUSE’S ROCK SAMPLES
GEOCHEMICAL ANALYSES FROM 2005 PROJECT
SUMMARY
The Gold King Property is large and centered about 20 km northwest of the town of Pemberton or
145 km north of Vancouver, in British Columbia, Canada. There is an active recorded history of
mineral exploration, for base and precious metals on these claims dating back almost a century.
The author, Sean Butler, B.Sc., P.Geo. was retained to advise Wolverine Minerals Corp. (formerly
named Goldking Mining Ltd.) on the merits of the property and make recommendations for an
appropriate exploration program to be conducted on the Gold King property.
J. T. Shearer, M.Sc., P.Geo. acquired by staking in 2003 the Gold King mineral claims totalling 149
units. He entered into a Mineral Claim Purchase Agreement with Goldking Mining Ltd. (the issuer) on
July 6, 2004. In July of 2004 Goldking Mining Ltd. added the Dale 1 to 19, Ogre 1 to 9 and Owl 1 to 4
by staking. In March 2005, the RR 1, RR2 and RR 4 to RR 12 were added. The mineral titles law
changed in British Columbia in January 2005 and all the claim holdings have been converted to the
new mineral title format, Cell Claims, during 2005. Some additional area was included with the cell
claims.
Despite a long history of mineral exploration on this property there is a reasonable opportunity to find
an economic deposit. The surface showings have been found. A review of the exploration history
does not include an abundance of deep exploration. The recommended exploration program is
developed to determine the vertical extension of the previously discovered surface zones or nearby
buried zones.
This property has a wide variety of mineralization styles and metals to explore for. The largest variety
of mineralization is associated with sulphide minerals. This should allow Induced Polarization (IP)
geophysics to charge up these zones.
The target areas should be focused on the Gold King, with the Li-Li-Kel, Number 4 Zone and Crown
areas being possible follow up zones. These areas have been heavily explored on surface and near
surface. These zones have little or no deep exploration that is documented beyond the probable drill
holes on Gold King and limited underground development on the Li-Li-Kel.
The recommended program includes diamond drill program targeting the IP geophysics targets on
the Gold King zone. Contingent on positive results further diamond drilling of the Gold King zone is
recommended in Stage II.
INTRODUCTION
Wolverine Minerals Corp. (then named Goldking Mining Ltd.) retained the author, Sean Butler, B.Sc.,
P.Geo., to review the project, draw conclusions, make recommendations and propose an appropriate
exploration program to evaluate the property. The company commissioned this summary report to
file with the TSX Venture Exchange to document the merit of the property upon vend in of the claims
to the company.
The author was advised by company officers that this report is intended to establish the property as
one of merit for submission to the TSX Venture Exchange of Toronto and Vancouver. This report
complies with the 43-101 format and may be used for disclosure in fundraising over $250,000.
The major source of information has been the numerous historical Assessment Reports on the area
within the B.C. Government Ministry of Mines MINFILE database. These reports are readily
available on microfiche and online dating back to 1961 on work conducted for Phelps-Dodge Ltd.
and then various companies up to 1992. Prior information is contained in the Annual Reports of the
BC Minister of Mines 1913-1937 and 1961. Several geological maps from the Geological Survey of
Canada and the BC Ministry of Mines were also reviewed in the preparation of this report.
Summary Report
on the Gold King Property
Revised on January 11, 2008
1
The author visited the property on July 9, 2004 after Goldking Mining Ltd. agreed to acquire the
claims. The author was also on the property for an extended period during fieldwork and supervision
of a work program on this property in 1987 for Ajax Resources. Another visit was made on
December 1, 2007.
Some aspects of the report are based on prior description or historical reports by other professionals.
Some of the sampling was completed personally by the author as noted and more sampling was
done by the author and also under his supervision in 1987.
RELIANCE ON OTHER EXPERTS
The author has not relied on other professionals.
PROPERTY DESCRIPTION AND LOCATION
Claim Status
During the time of the preparation of this report the mineral claim title process changed in British
Columbia from a ground based location system to an online map based geographic location process.
The legislation changed in December, 2004 and became active on January 12, 2005. Tenure of a
Legacy Claim, the term for the location based claims located before December 2, 2004, could then
be transferred to the map based tenure location, related to the Mineral Title Online Grid Regulation,
known as Cell Claims. A land survey is not required for secure tenure location. This new Act uses
map coordinates as the basis for the location of the mineral title. The converted cells could have the
same expiry date as the previous overlying legacy claims or changed to coordinate with other claims
in a group.
The land area covered by the “legacy” mineral titles under agreement to Goldking Mining Ltd. (later
renamed Wolverine Minerals Corp.) were converted to the new online map based system. This
conversion was done for several reasons, including most importantly improving the mineral title
certainty. The author understands that the converted claims are included under the original terms of
agreement between Goldking Mining Ltd. and the vendor, Mr. Shearer for the previous overlying
legacy claims. Due to differences in the size, location and shape of claims between the two systems,
exact legacy claim locations could not be exactly duplicated. It is the author’s opinion that the best fit
available was accomplished.
The Gold King I to IX claims were located in March 2004 and are centered about 20 km northeast of
Pemberton in map sheet 92J/10W and were owned by J. T. Shearer, M.Sc., P.Geo. having been
located by R. D. Machray. The claims covering this land area are all within the Lillooet Mining
Division and were subsequently transferred by Mr. Shearer to Wolverine Minerals Corp. pursuant to
the terms of the mineral claim purchase agreement dated July 6, 2004.
The land holdings covering the area described above are presently registered to Wolverine Minerals
Corp. as the following claims after conversion to cell claims of Gold King I to IV and Gold King VI to
IX as well as the Owl Creek 1 to 4. The converted cell claims often do not have a claim name in the
provincial database only a record number. The Gold King I to IX had a nominal area of 3,725
hectares. Following conversion the Gold King One to Nine covered 3,964 hectares.
Summary Report
on the Gold King Property
Revised on January 11, 2008
2
Table 1
Holdings of Wolverine Minerals Corp, owner number 211090, when checked on January 10, 2008.
Tenure
Claim Name
Owner
Good To Date
Status
Area (Ha)
Number
509086
Gold King One
211090 (100%)
2008/OCT/15
GOOD
493.040
509087
Gold King Two
211090 (100%)
2008/OCT/15
GOOD
493.039
509088
Gold King Three
211090 (100%)
2008/OCT/15
GOOD
513.348
509089
Gold King Four
211090 (100%)
2008/OCT/15
GOOD
513.379
509090
Gold King Five
211090 (100%)
2008/OCT/15
GOOD
513.738
509091
Gold King Six
211090 (100%)
2008/FEB/15
GOOD
513.286
509092
Gold King Seven 211090 (100%)
2008/FEB/15
GOOD
41.056
509093
Gold King Eight
211090 (100%)
2008/FEB/15
GOOD
513.533
509271
Gold King Nine
211090 (100%)
2008/FEB/15
GOOD
369.837
Total Area
3964.256
In July of 2004 Goldking Mining Ltd. added some previously located claims and contracted to have
more located between the Gold King group and the RR claims. They included the Dale 1 to 19 and
the Ogre 1 to 9. These claim groups ultimately extended into 92J/7 and 92J/11. The above claims
were a mix of two and four post legacy claims and following their conversion to cell claims have a
total surface area of 9,840.044 hectares as listed below.
Table 2
Holdings of Wolverine Minerals Corp. owner number 211090, when checked on January 10, 2008.
Tenure
Claim Name
Owner
Good To Date
Status
Area (Ha)
Number
514206
211090 (100%)
2008/FEB/15
GOOD
1667.383
514209
211090 (100%)
2008/FEB/15
GOOD
1768.678
514211
211090 (100%)
2008/FEB/15
GOOD
1479.977
514219
211090 (100%)
2008/FEB/15
GOOD
984.398
514221
211090 (100%)
2008/FEB/15
GOOD
1209.368
514412
211090 (100%)
2008/FEB/15
GOOD
432.410
517468
GK NORTH 1
211090 (100%)
2008/FEB/15
GOOD
513.105
517471
GK NORTH 2
211090 (100%)
2008/FEB/15
GOOD
513.061
517476
GK NORTH 3
211090 (100%)
2008/FEB/15
GOOD
512.914
517504
GK NORTH 4
211090 (100%)
2008/FEB/15
GOOD
512.731
517512
GK NORTH 5
211090 (100%)
2008/FEB/15
GOOD
246.019
Total Area
9840.044
The area of the combined converted cell claims is 13,804.3 hectares.
Summary Report
on the Gold King Property
Revised on January 11, 2008
3
Figure 1 - Claim Locations
Summary Report
on the Gold King Property
Revised on January 11, 2008
4
To remain in good standing all cell claims require $4.00 per hectare of registered assessment work
applied in each of the first three years and $8.00 per hectare per year thereafter. The assessment
cost remains comparable to the previous claim tenure system for the “legacy” claims or converted
cell claims. Claim assessments are recorded as being valid according to the dates shown in the
tables.
The Gold King claims are centered on NTS map 92J/10W with some outlying claims listed above on
maps 92J/07W, 92J/07E and 92J/11E. The center of the claims is near Latitude 50º31’02”N /
Longitude 122º53’14”W. The general trend is roughly northwest /southeast and extends for over 25
kilometres.
The legacy claims had not been legally surveyed for location, but the converted cell claims have
location boundary certainty since the boundaries are defined in the provincial location database. The
Mineral Titles Online http://www.mtonline.gov.bc.ca/ is the location for registering claims in BC.
Tenure
The Gold King claims, comprising nine claims, Gold King I-IX, were originally recorded in the name
of Robert Douglas Machray, and the claims were transferred to J. T. Shearer, M.Sc., P.Geo. by Bill
of Sale and subsequently transferred these claims to Wolverine Minerals Corp. pursuant to a mineral
claim purchase agreement dated July 6, 2004 which provided for the following terms:
Execution Date
$15,000 cash & 50,000 common shares
Six Month Anniversary
$15,000 cash
Twelve Month Anniversary
50,000 common shares
Eighteen Months
$10,000 cash
Twenty-four Months
$10,000 cash & 50,000 common shares
Thirty Months
$10,000 cash
Thirty-six Months
$10,000 cash & 50,000 common shares
2.5% NSR & 10km perimeter clause on claims staked to the south
The claims located by Wolverine Minerals Corp. in July 2004 were located by contract stakers under
the supervision of, Robert Krause, an officer of Wolverine Minerals Corp. and Mr. David Deering.
Surface rights in the immediate area of the Gold King property are owned by the Province of BC.
Surface access for exploration and development is available under the mining law of BC with
permits.
The author is not aware of any back in rights, payments or other agreement except the perimeter
clause with J. T. Shearer and encumbrance to which the property is subject and the 2.5% net
smelter royalty up to $1,000,000 to George Nicholson on the area underlying the former RR claims.
The area covered by the converted "cell claims" 514219 and 514221 totalling 2,193.766 hectares
(see Table 2 under the heading “Claim Status” above) covers most if not all of the area of the former
RR claims.
Environmental Liabilities
A preliminary site assessment by Teck Corp in the early 1990’s and localized to a very small area,
found elevated levels of iron and aluminium and acidic pH in the area of ferricrete zones in the
Tenquille Valley. However, these appear entirely natural in the absence of detailed sampling and
analysis. These elevated metal levels and low pH are already found naturally occurring in nearby
creeks. The aqueous sulphate concentrations being less than 20 mg/L indicate there is no
widespread Acid Rock Drainage (ARD). The acidic conditions are probably enhanced by additional
processes like organic acid. These are considered to be controllable. A lined pond or other
applications of limestone could be one method of control.
Summary Report
on the Gold King Property
Revised on January 11, 2008
5
There are numerous old workings recorded in the historical record that have not been examined by
the author. These are not anticipated to be a problem due to their small scale. There has been forest
logging activity in the area in the past with the associated land disturbance and road building, along
the Birkenhead River and Tenquille Creek valleys. This forest disturbance is the responsibility of
others and should not be a liability to the mineral tenure holders.
Permits
The company and property will be subject to the mine permit regulations of British Columbia. A
permit will be required for any bulk sampling and proposed drilling. Some permit applications have
been prepared for the proposed exploration.
ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND
PHYSIOGRAPHY
Location
The Gold King claim group is between 1,370 and 2,400 metres elevation, centered a distance of,
approximately 20km north-northwest of the town of Pemberton, B.C. The length of the combined
claims is over 25 kilometres and is about ten kilometres north of town at its southern boundary.
Access
Access to the claims is by helicopter from Pemberton or from logging roads up the Birkenhead River
and Tenquille Creek valleys, which end within the east claim boundary. This is below the Number
Four zone and Li-Li-Kel areas. There are old overgrown cat trails and foot trails leading from the road
into the upper valley.
Several foot trails from the west are available to the area of Tenquille Lake from the Lillooet valley
and the Hurley River Road, north of Pemberton. The Hurley River Road is within the northwest
boundary of the property. As well, a network of foot trails and ATV trails in the alpine cross the
property allowing movement from one mineralized zone to another.
Summary Report
on the Gold King Property
Revised on January 11, 2008
6
Figure 2 – Generalized Location in British Columbia, Canada
Physiography and Climate
The area of the Tenquille Claims has been heavily affected by the Pleistocene Glaciation with arêtes,
cirques, tarns and hanging valleys common in the area. Steep slopes are common and often
covered by talus.
The lower levels of the property are heavily forested but above about 1600 metres elevation this is
replaced by scrubby alpine trees and grass where soil exists. There is adequate water from several
creek drainages for mineral exploration on this property.
The elevations in the property vary from about 1,370 meters above sea level above the Owl Lake
Valley to about 2,400 meters above sea level at Tenquille Peak to the northwest of Tenquille Lake.
The snow often stays on the ground in the higher areas into June and July in many years. Field work
can continue most years into October and occasionally November at the higher levels. Activities
such as diamond drilling may continue longer in some areas. The lower parts of the property are
subject to the climate typical of the Interior of BC.
Summary Report
on the Gold King Property
Revised on January 11, 2008
7
Infrastructure and Local Resources
There are logging roads leading up Tenquille Creek valley that provide access to the east side of the
property. It is likely feasible for future limited access within the property by extending this road if
required, although the author has not surveyed a route. The topography at the end of these routes
up to most of the showings is quite steep. The nearest electrical power is presently in the Lillooet
River valley, below to the west and in the Birkenhead River valley to the east. There are also roads
in the Lillooet River valley and the Hurley Forest Road to the northwest of Tenquille Lake that could
possibly be used for starting points of access roads.
There is a well developed system of recreational backpacking and trail biking trails leading through
the property having been developed since the author’s work in 1987. This could provide convenient
access between zones for the exploration of the various properties in the early stages of exploration.
The Town of Pemberton, within commuting distance, is located on a major highway and railroad. The
town has the commercial services to support exploration and development work.
HISTORY
Preamble
The area has a long history of mineral exploration being a relatively short distance southwest of the
prolific Bridge River Camp, which includes the Bralorne-Pioneer Gold Mine, the largest producer of
lode gold in British Columbia. The proximity to the PGE Railway (now CN Rail) also allowed easy
access and stimulated exploration in the area in the early years. The abundance of mineralization
and several mineral deposit types has continued to maintain interest in this area and contributed to
the frequent efforts to move this property forward.
Prior Exploration
1913 – 1960’s
The first recorded work in the region is near the mouth of Owl Creek in 1913, but from the description
was apparently started before this. The information on the work recorded in this report during this
early period is sourced in the various BC Minister of Mines Annual Reports. The mineral
occurrences located in the Tenquille Lake area were found around 1916 during the construction of
the Pacific Great Eastern Railway, now the Canadian National Railroad through Pemberton. Reports
of work in 1918 indicate starting a trail from the railroad up Birkenhead Creek and Tenquille Creek
that was completed in 1919. Access before 1919 was by a trail up the steep side of the Lillooet River
valley which was very trying. A bond was taken on the Crown property with a group out of Seattle, on
the summit between the Lillooet and Tenquille valleys, and work reports high grade gold on
magnetite fissures, without any values reported. The camp was shut down over the winter. In 1923
the Crown property had works including a 40 foot deep shaft and short crosscut from the bottom
reported. Silver values of about 60 oz/ton are reported, with poor continuity. The intensive
investigation of the Tenquille Lake Area was completed during the period 1923 to 1932 when several
different groups including two major corporations, Federal Mining and Smelting and Britannia Mining
and Smelting, developed several camps and completed their investigations. Federal completed the
two drifts on the Li-Li-Kel Property and Britannia Mining and Smelting completed trenching and
underground programs on the Crown and Gold King claims. In 1923 a 4 or 5 foot wide sample on
the Li-Li-Kel showing ran Gold 0.60 oz. and silver 1.5 oz/ton. In 1926 Federal ran an approximate
250 foot long tunnel on Li-Li-Kel. A further 400 feet was added and about 300 feet in another tunnel
below this was done in 1927. A sample on the Gold King in 1927 where an additional 5 or 6 feet of
development were added was 0.2 oz/ton Gold, 55.5 oz/ton silver, 1 % copper, 8% lead and 1 % zinc.
In 1930 a short shaft was developed and a sample at about 26 feet assayed 0.56 oz/ton gold, 9
oz/ton silver, 0.8 % lead and 6.8 % zinc. A limited amount of diamond drilling was done on the Gold
Summary Report
on the Gold King Property
Revised on January 11, 2008
8
King in 1932 when the Kamorley Oil Company of Kamloops and Calgary optioned the property with
poor results.
Work is first reported on the Eva (aka Moffat and later Avalanche) showings on the north side of
Tenquille Creek. This is reportedly on a six foot wide siliceous, sericitic schist, with surface assays
up to 8% copper. There was extensive underground development in 1923 to 1925 by several
syndicates. A 200 foot tunnel and 30 foot crosscut were developed in 1923. Work reportedly
continued in 1924 but no details are available. By 1925 over 500 feet of tunnelling was complete.
Work in 1926 reports striking a lens of ore in continuations of the underground workings. This lens
assayed Gold 0.01 oz., Silver 0.9 oz/ton, Copper 3.8 % and zinc 0.1 %. There was an ongoing
summer program on this property until about 1930.
The showings in the Tenquille Lake area were acquired by one owner in 1937 and held under the
name of the “Gridiron” Property. There was little work reportedly completed in the Tenquille Lake
area until 1961 when Phelps Dodge carried out an exploration program on the copper-iron showings
located on the western side of Tenquille Lake. This work is detailed in the report by D.C. Malcolm
(1961). It outlines the mapping of the major lithologies in the area and nature of the mineralization.
The Copper Queen (in lower Owl Creek Area south of the claims) showings were first reported
in1913, but were likely worked prior to this. By 1916 a trail and a 70 meter adit had been completed
across the shear zone. A small plant was built in 1917, but no further detail is available. In 1928
Britannia Mining and Smelting optioned the property and completed three diamond drill holes with up
to 300 feet of low grade copper found in several zones of probable porphyry type deposits including
what sounds like fault zone concentration zones. Owl Creek Mines completed a program in 1960
(Fawley, 1960). The work included sampling and geological mapping that indicated low gold values
in the sulphides and zones of abundant magnetite. Further work was reported in 1964 by the Mining
Corporation of Canada, involving a stream sediment geochemical survey and magnetic study. The
access road to near the south end of the claims of the present report and a 280 meter drill program
was completed in 1968, by Pine Lake Mining.
1970’s
There is an assessment report from 1972 (Weymark) that indicates airborne geophysics were
completed over the center of the present Gold King claims surrounding Tenquille Lake. There is little
detail presented in this report and interpretation is difficult to determine.
In 1973 the Owl Creek area claims were optioned by Utah Mines from Pine Creek Mines. Further
geochemistry, geology and geochemistry was completed. In 1974, IP, ground magnetic and soil
geochemistry surveys were completed (Gatchalian and Witherly, 1974). Further work including four
diamond drill holes of 550 meters were completed later (Rayner and Witherly, 1974). There is a
report of a diamond drill intersection of 91.4m averaging 0.4% copper and 0.029% Mo mentioned in
BC Assessment Report 15597, D. G. Allen, 1986, attributed to a report by W.R. Bacon from 1972 for
Pine Point Mines. The report on the drilling is not available to the author of this report.
1980’s
In the early 1980’s Tenquille Resources (various reports by Deleen and Curtis) did exploration
mapping and sampling in the Li-Li-Kel and Number 4 areas. The work included mapping, sampling
VLF-EM geophysics in 1982. One sample collected by P.G. Curtis returned 1.280 oz/ton gold and
14.3 oz/ton silver over 0.5 feet on the No. 3 zone. In 1983 further geophysical geological mapping
and, geochemical sampling was completed. In 1983 Amazon Petroleum drilled 17 NQ diamond drill
holes totalling 1,605 meters on several different showings.
Caliente Resources worked on the Avalanche claims, to the north of Tenquille Creek, starting in
1984 (reports by Cavey, et. al.). The work included soil and rock samples as well as magnetic and
VLF Electromagnetic surveys.
Summary Report
on the Gold King Property
Revised on January 11, 2008
9
In 1987 the property on the south side of Tenquille Creek was explored by Ajax Resources including
geological mapping, soil and rock geochemistry, VLF-EM and ground magnetic geophysics focusing
on the Gold King, Number 4, Seneca and Crown zones among others. The author of this current
report, Sean Butler, supervised this program.
There was also work done focusing near the Seneca showing by New Camp Resources in 1989.
This consisted of soil and silt geochemistry, geology, ground magnetics and VLF-EM geophysics
(Christopher, 1989). This report states work was done in 1988 by Cyberquest Exploration Services.
This was confirmed by the author in personal communication with the field personnel. The report or
details on what was done were not available to the author on this work.
There was more work in the Owl Creek area including a program of geological mapping,
geochemical sampling and magnetic and VLF-electromagnetic geophysics reported in BC
Assessment Report 15597, D. G. Allen, 1986. This work is near the south end of the Gold King claim
group.
1990’s
Teck Corp. undertook extensive exploration of the Avalanche (the former Moffat and Eva) on the
north side of Tenquille Creek. Field work in 1990 consisted of airborne VLF, geological mapping and
geochemistry. This was followed by geochemistry, ground HLEM geophysics and ten diamond drill
holes over 1,914 meters in 1991. Further ground geophysics and mapping were completed in 1991.
A further eight BQ diamond drill holes totalling 1,419 meters, were completed in 1992.
Teck also explored the Sungod property, a lensy massive pyrrhotite skarn near Cerulean Lake in
1990 (Paulter, 1991A). This work included an airborne geophysical survey, preliminary 1:10,000
scale mapping with concurrent geochemical sampling, and local soil and ground magnetic surveys to
follow up the geophysical anomalies.
Cominco explored in the Owl Lake area including soil and silt geochemistry in 1992 and magnetic
geophysics. In 1993 induced polarization and resistivity over 13.4 kilometres were completed. The
work on these claims was targeted at copper and molybdenum porphyry style mineralization.
2000’s
The author is not aware of any further exploration work on this property until 2004. Wolverine
Minerals Corp. funded a work program in 2004 undertaken and supervised by Johan T. Shearer,
P.Geo. This program included mapping, geochemical sampling including soil profiles and rock
petrology of six samples centered on the Gold King and No. 4 zones.
In September 2005 Goldking Mining Ltd. completed approximately $20,000 of field work that
includes geochemical sampling. This fieldwork was subcontracted by Goldking Mining. A report on
this work was prepared and filed for assessment by J. T. Shearer.
In April of 2006, SJV Consultants (Pezzot, 2006) was retained by Goldking Mining to undertake a
compilation of the existing data. In the memo from SJV they have acquired BC government TRIM
maps of elevation and regional geology in electronic formats. These have been transformed into GIS
formats. As well electronic copies of the federal government airborne geophysical data was acquired,
including geomagnetic data.
The federal government geomagnetic data was transformed using the UBC 3D Inversion algorithm.
This was then printed as a colour contour plan. The feature that is most prominent is a magnetic high
interpreted as a near vertical pipe like body on the north end underlain by Miocene volcanic rocks on
the geology map. This data shows the northwesterly trends of the major rocks units, but also hints at
Summary Report
on the Gold King Property
Revised on January 11, 2008
10
northeasterly faults. There are several other zones with magnetic increases. These correlate to some
known deposit zones, but other are large and may correlate to lithological units.
Further data compilation is recommended in the memo. There are also field study recommendations,
including ground geomagnetics and 3D Induced Polarization studies.
Figure 3 - Regional Geology and Historical Showing Locations
Summary Report
on the Gold King Property
Revised on January 11, 2008
11
GEOLOGICAL SETTING
Introduction
The property is largely in a northwest trending volcano-sedimentary belt known as the Cadwallader
Group. This is an island arc group of Triassic age rocks. The Cretaceous Fire Lake Group occurs on
the southwest side of the northwest trending Owl Creek Fault. This contact runs along the southwestern boundary of the claim block.
The history of exploration is long and detailed in this area. The target mineralization over the years
has included gold, silver, copper, molybdenum, lead and zinc. The major mineralization occurs in
veins, skarns and shears. The early exploration targeted the garnet-magnetite-epidote skarns
developed in limestone beds and pods. These often developed along the edge of porphyritic dykes
that intruded the limestone beds and related shears.
There are also several shear zone related mineralization zones, such as the Grizzly Shear targeted
by Teck Corp. on the north side of Tenquille Creek in the early 1990s. These often include quartz
gangue, breccia and silica. There were also suggestions of possible volcanogenic massive sulphide
deposits, including one by Peter Christopher, P.Eng., (1988) in his report, as well as other reports on
adjoining properties to the east.
Regional Geology
The Tenquille Lake area is located just east of the margin of the Coast Intrusive Complex, a major
northwest trending tectonic belt in the Canadian Cordillera. The area underlying the property appears
to be a roof pendant of the Coast Intrusive Complex of largely Cadwallader Group rocks.
The rocks of the Tenquille Lake area consist of a series of andesite flows, tuffs and breccias and
some minor flows of rhyolite breccia. Also thin beds of slate, argillite, limestone and conglomerate
outcrop within the sequence. This unit is mapped as part of the Cadwallader Group of Upper
Triassic Age (Woodsworth, 1977) and appears to be the Pioneer and Hurley Formations of this
group (Riddell 1990).
Intruding these units from the southeast is the Cretaceous Spetch Creek Pluton of granodiorite,
probably related to the Coast Intrusive Complex. Related to this intrusion are a series of dykes and
sills throughout the volcanic sedimentary package. The dykes are likely coeval with the volcanic
flows (Riddell, 1990) in the central Gold King claims. Several small intrusive plugs occur around and
just to the north of Tenquille Lake.
There are a number of northwest trending shears and folds. The Owl Creek Fault is a major regional
northwest trending fault (Riddell’ 1990) that separates major rock units. This fault zone is traced over
a 100 kilometres and is an extension of the regionally significant Harrison Lake Fault Zone .The
rocks to the southwest of the fault are the Cretaceous Fire Lake Group, largely tuffs and sandstone.
The rocks to the northwest are a Triassic and post Triassic group of often undifferentiated
volcaniclastic, tuffaceous and sedimentary sequence of the Cadwallader Group and Cretaceous
diorite intrusives. The Grizzly Shear is a major northwest trending mineralized shear through the
former Avalanche property and is either an extension or a splay of this regional shear. The northwest
trending folding in the area south of Tenquille Lake, as located by several authors was apparent in
the visit to the Gold King showings in 2004.
Local Geology
Geological mapping was completed in the area by Deleen & Curtis, 1982, covering the Li-Li-Kel and
the No. 3 zones. The rocks in this area are well exposed, and an outcrop map was not completed.
These veins are located at an elevation of approximately 3,000 metres. The area is above the
treeline and it was possible to trace the zones until they were covered by talus. Diamond drilling was
Summary Report
on the Gold King Property
Revised on January 11, 2008
12
reported by Curtis in 1983 for Amazon Petroleum. The results include 0.30 meters of 25.82 oz/ton
silver and 0.24 oz/ton of gold.
The rocks in the area are a series of andesitic flows and breccias. The Li-Li-Kel zone was mapped
for a distance of approximately 400 metres and the No. 3 zone for a distance of approximately 175
metres. Both the Li-Li-Kel and the No. 3 zones appear to be mineralized shear zones which contain
irregular lenses of quartz and sulphides. The minerals noted in hand specimens were galena,
sphalerite, pyrite and possibly argentite. The mineralized zones vary in width from a few centimetres
to approximately 2.0 metres; the silver values vary from 0.01 to 192.0 ounces per ton and the gold
from 0.001 to 0.73 ounces per ton. The Li-Li-Kel zone has a northeasterly strike and dips to the east
and angles from 75º to 85º. The Li-Li-Kel drift appears to be driven on a weakly mineralized zone
which is parallel to the main zone. The samples from the lower drift contained only low values of
precious metals.
The Number 4 zone is located upslope and southwest of the No. 3 and Li-Li-Kel zones. A survey grid
was established over this zone to gain ground control by Blank & Butler, (1988), for geology,
geochemistry and geophysics. Five rock units were recognized and mapped by Blank & Butler,
(1988), as follows:
Unit 1:
A highly fractured volcanic sequence consisting of andesite/dacite flows and pyroclastics,
which are cut by numerous fine to medium grained dykes, (Unit 2).
Unit 2:
Fine to medium grained dykes.
Unit 3:
Less fractured volcanic sequence consisting of andesite/dacite flows.
Unit 4:
A sedimentary package which includes sandstones, siltstones, conglomerate and thin
beds of limestones.
Unit 5:
Intrusive rock unit defined as diorite. Medium grain, intermediate rock.
For the most part, the rock units dip to the northeast. A major fault trends north-northeasterly
producing major shearing in this direction and other cross cutting fractures with no preferred
direction.
The northerly section of grid was located over the transition of Zone 3 to Zone 4 and is
predominantly green andesite flows. Some mineralization was found in irregular lenses along shears
related to the Zone 3 workings. Rock samples collected here returned significant values in gold,
silver and copper including SB-005, collected by the author of this report in 1987, with 71,800 ppb
gold. To the south is a large gossanous section about 500 by 1,000 meters in size over the Main
Number 4 Zone. The mineralization in this area occurs along narrow northerly trending shears.
Anomalous values of copper, lead, zinc, silver and gold were noted. Next is a section of sediments,
with minor volcanics and intrusives in the extreme south end of the grid.
The Gold King showings outcrop in a valley floor and along the base of the valley wall. This showing
is located some 700m west of Zone 4. These showings were visited by the author and Jo Shearer,
P.Geo., on July 9, 2004. Two rock samples were collected from this zone during this visit and
analyzed for 34 elements and fire assay gold and silver geochemistry. There is extensive trenching
and some collapsed shafts in evidence. Also seen were drill hole collars, anchors and some drill
rods for possibly a Winkie Drill. No drill core was found. This may be from the 1932 drilling, but
appeared to possibly be more recent. No record of later drilling was noted for the Gold King.
In 1925 an open cut was taken to 10 feet and sampled on the Gold King. The sample ran 1.30 oz/ton
gold, 0.70 oz/ton silver, trace of lead and 14 percent zinc (BCMMAR 1925).
Three Rock units were described as follows in Butler and Blank (1987):
Unit 1:
A volcanic sequence consisting of andesite/dacite flows, pyrotclastic (tuffs and
agglomerates).
Unit 2:
Iron skarn development in apparent limestone pods.
Unit 3:
Basic dykes which cut both the volcanics and Iron skarns.
Summary Report
on the Gold King Property
Revised on January 11, 2008
13
For the most part the rock units appear to dip in an easterly direction. Fracturing in all directions
precludes determination of any dominant structural pattern.
Three zones of mineralization were identified at the Gold King showings in 1987:
The first zone is an iron skarn developed on the contact with an andesite/dacite. Old workings are
located on this contact zone. Rock chip samples collected within this zone include two significant
samples R1215 (1436 ppm Cu, 5.8 ppm Ag, 126 ppb Au) and R1218 (1933 ppm Pb, 452 ppm Zn,
150.6 ppm Ag and 2480 ppb Au). Outcrops and old workings located approximately 40m to the south
have minor skarn development. The skarn is generally developed along the beds of limestone that
occur as interbeds in the tuffs and siltstones. This area shows a soil sample anomaly in gold, silver,
lead, zinc and copper.
There are several other targets identified nearby defined by coincident anomalous magnetic and soil
geochemistry. Surface weathering is deep, often with little or no sulphide minerals seen on surface in
many parts of this zone. There were abundant pitted rocks after disseminated pyrite and possibly
pyrrhotite though. Deep sampling here would be beneficial.
The Avalanche showings occurring on the north side of Tenquille Creek were originally named the
Moffat and Eva properties. A major northwest trending fault, the Grizzly shear zone, bisecting the
Moffat prospect is sub parallel to the Owl Creek Fault. The fault is composed of a complex set of
anastomosing northwest shears. The Grizzly shear zone contains more zinc-rich mineralization
associated with quartz sericite schists. Mineralization has been discovered at three main showings
on the Moffat prospect: the Eva, Grizzly shear and along shale contacts. (BCMM MINFILE
092JSE047).
The Eva showing is the original discovery in the Moffat claims. Mineralization consists of chalcopyrite
and minor pyrite, sphalerite and bornite with quartz blebs and chlorite. The mineralization occurs in a
3-metre wide silicified pyritic zone hosted in a larger sericite altered zone in a thin quartz feldspar
porphyry flow or sill. In the shaft, irregular pyrite and chalcopyrite veinlets cut a rusty chloritic rock
with quartz blebs. (BCMM MINFILE 092JSE047). A grab sample from an old shaft, collected and
reported by Teck Corp has 33% zinc, 6% copper, and 25 g/t silver. The diamond drilling on the
Avalanche property returned results that include DDH 91-5 with 0.75% Zn over 17 meters.
The Engineer showing is over several gossanous zones explored for epithermal copper in a volcanic
rock roof pendant. Exploration by Canadian Nickel and Noranda was done in 1983 on two properties
in this area. Work was done in 1989 also.
DEPOSIT TYPES
The BC MEMPR Paper 1989-3 Precious Metal Enriched Skarns in British Columbia (Ettlinger and
Ray, 1986) outline a number of characteristics of skarns containing gold and silver. This includes
enhanced values in bismuth and/or tellurium. The showings in this area, Seneca, Crown, Gold King
are mentioned as Location 34 in this publication. A skarn is a mineral deposit type that is formed by
the interaction of hot mineral bearing fluids and carbonate mineral rich rocks. In this area the skarns
are formed along the beds of limestone that occur as interbeds among the other sediments. The
skarns form either on the edge of porphyritic intrusives or fractures leading from intrusives.
The paper on Gold Skarns by Mienert, (1996) reinforces the paper by Ettlinger and Ray with “The
highest grade (5-15 g/t Au) gold skarn deposits are relatively reduced, are mined solely for their gold
content, lack economic concentrations of other metals, and have a distinctive Au-Bi-Te-As
geochemical association. Most high-grade gold skarns are associated with reduced (ilmenitebearing, Fe2O3/ (Fe2O3+FeO) << 0.75) diorite-granodiorite plutons and dike/sill complexes. They
typically occur in clastic-rich protoliths rather than pure limestone and skarn alteration of dikes, sills,
and volcaniclastic units is common.” These characteristics are present in this property. The skarns
on the Gold King property are worth continued study for buried deeper targets.
Summary Report
on the Gold King Property
Revised on January 11, 2008
14
The south end of the property near Owl Lake and Little Owl Lake has had exploration for porphyry
copper type targets including diamond drilling programs as described in the history section. There is
also shear and vein deposits described in the Avalanche
MINERALIZATION
This is a large property with many mineralized zones and showings. There is as well several styles of
mineralization from the disseminated copper porphyry style targets in the Owl Lake area of large fine
and medium grained pyrite and chalcopyrite in intrusive bodies to the silicified shear hosted zones in
the Eva and Avalanche with associated sulphide mineralization and associated precious metals and
the gold bearing magnetic skarns seen at the Gold King, Seneca East and Crown which contain
magnetite and pyrrhotite and the Wonder which is a non-magnetic occurrence.
The mineralization near the Owl Lake that has been explored for is copper porphyry style
disseminated chalcopyrite and pyrite zones. There is an indication in some reports they may in part
be shear zone related. They occur within zones of silicification and veinletting that have associated
disseminated sulphide minerals.
The Avalanche showings occurring on the north side of Tenquille Creek were originally named the
Moffat and Eva properties. A major northwest trending fault, the Grizzly shear zone, bisecting the
Moffat prospect is sub parallel to the Owl Creek Fault. The fault is composed of a complex set of
anastomosing northwest shears. The Grizzly shear zone contains more zinc-rich mineralization
associated with quartz sericite schists. The Eva showing consists of chalcopyrite and minor pyrite,
sphalerite and bornite with quartz blebs and chlorite. The mineralization occurs in a 3-metre wide
silicified pyritic zone hosted in a larger sericite altered zone in a thin quartz feldspar. The Silver Bell
and Li Li Kel are also vein related zones.
In the Gold King zone the major mineralization is skarn and quartz veins. The skarn is generally
developed along the beds of limestone that occur as interbeds in the tuffs and siltstones. These
calcite (or ankerite) skarns contain chlorite, epidote and quartz as outlined in thin sections observed
by J.T. Shearer (2005A). The sulphide minerals include sphalerite, pyrite, pyrrhotite, chalcopyrite and
galena. There is also hematite noted in the sulphide mineralized samples. The sulphide minerals
vary from near massive pyrrhotite with hematite forming veinlets to clumps of chalcopyrite with
disseminated pyrrhotite and galena on the edges of the chalcopyrite grains. The primary controls are
the limestone beds, now heavily folded and somewhat faulted within the volcanic and sedimentary
layers. The mineralization is in close spatial relation to dykes and sills of intrusives and vein
containing shears. The visible gold mineralization has not been seen in the petrographic work done
to date, but the base metal sulphide minerals especially pyrrhotite and sphalerite and gold have a
good correlation in assays. There are number of old workings, trenches and shafts within the zone
exposing sulphide rich mineralized zones. These workings extend over a length of several hundred
meters. The soil geochemistry of 1987 indicates about 350 meters of soil anomalous values and it is
open in several directions. There is extensive cover of soil and till in the mineralized area so
continuity over this distance is undefined at this point due to lack of outcrop. Massive sulphide zones
with some magnetite occur in several parts of the Gold King zone.
EXPLORATION
Wolverine Minerals Corp. has undertaken several campaigns of exploration. The company undertook
the first two projects of this work to meet the assessment work limits to maintain title and advance
the geologic understanding of this property. The geophysics was undertaken by Wolverine Minerals
Corp. as recommended by the author in an earlier report version as well to meet assessment
requirements.
The first project was the geological mapping and geochemistry under the field supervision of J.T.
Shearer (2005A). This field work done in September of 2004 and focused largely on the Gold King
Summary Report
on the Gold King Property
Revised on January 11, 2008
15
zone consisted of four soil profiles, six petrology samples and eleven rock samples for geochemical
analysis. The petrology included four samples of mineralized skarn, a massive pyrrhotite sample as
well as a tuff. The rocks were analyzed for 34 element ICP geochemical analysis plus gold and ore
grade zinc at ALS Chemex of North Vancouver, BC. The results show elevated values in several
metals in the rocks and soil profiles. The most significant rock sample was “Creek Zone” which
returned 132 ppm silver, 12.05 % zinc and 1.54 ppm gold.
The following is an excerpt from the Shearer (2005A) report:
“A suite of 6 specimens were collected for petrographic analysis. …….
This suite of 6 specimens consists of mineralized skarn (4 samples) and highly altered
(chloritized) relict porphyritic tuff and Epidote-chlorite skarn.
The principal carbonate in all skarn specimens appears to be ankerite, mafics and
possibly garnet have been replaced by chlorite.
Sulfides consist mainly of pyrrhotite and pyrite with lesser sphalerite, chalcopyrite and
galena.
The altered, highly chloritized relict porphyritic tuff has distinct ghosts of completely
replaced feldspar phenocrysts. The specimen of Epidote-chlorite skarn is composed
mainly of sub-euhedral epidote.
The Creek Zone sample assayed 132 ppm Ag, 4 770 ppm Pb, 12.05% Zn and 1.54 ppm
Au.
A total of 4 soil profiles were dug in the Gold King Area in an effort to characterize the
nature of soil development in region. Results are contained in Appendix II and locations
illustrated on Figure 8.
Profile A has a slight increase in silver, cesium, cobalt, copper, lead and arsenic,
suggesting that the profile has a more residual character. Profile B is uniformly low
throughout the depth, which possibly reflects the poor soil development in the profile
area. Profile C, located farther south up the valley shows a marked decrease in metal
content with depth indicating the transported nature of the near surface anomalous
results in copper, lead, silver with the exception of Zinc which is a well known mobile
metal.
Profile D was dug in the 4 zone area and also shows a decrease in metal content with
depth suggestive of transported soils.
The same general pattern is exhibited for both the hot and cold extraction methods.”
The second work program undertaken by Wolverine Minerals consisted of the collection and analysis
of rock samples completed under the supervision of Robert Krause in September 2005 and reported
by Jo Shearer (Shearer, 2005B). This program consisted of 148 rock samples sent for analysis in the
Gold King zone and several other nearby areas. Analysis was for 30 elements by aqua regia
digestion and ICP analysis plus fire assay preparation and ICP analysis for gold at Acme Analytical
Labs of Vancouver, BC. Several samples contain elevated and anomalous values in copper, zinc
and gold. Copies of the assay values as reported by Acme Analytical Labs of Vancouver, BC are
attached at the end of this report.
The report outlines several traverses in which many of the rock samples were collected and a
description of some of the samples.
Summary Report
on the Gold King Property
Revised on January 11, 2008
16
Several significant samples are highlighted next. Sample GKLS 1 collected from a mineralized zone
near the helicopter pad returned 867 ppm Cu, 2242 ppm Pb, >10,000 ppm Zn35.1 ppm Ag and 1185
ppb Au. Sample 291068 is a felsic tuff with up to 30% magnetite and analyzed at 1805 ppm Cu,
6378 ppm, >10000 ppm Zn, 56.8 ppm Ag8895 ppb Au. It was likely collected in the lower part of the
valley. Sample 291081 returned values of 965 ppm Cu, >10000 ppm Zn, 0.7 ppm Ag 2176 ppb Au.
The locations of some samples collected in this project are shown on Figures 6, 7, 7b and 7c at the
end of this report.
SJV Geophysics was contracted for a geophysical review of information in the public domain
(Pezzot, 2006) and later a field IP Geophysical Survey (Rastad, 2006). The review of public domain
information was government airborne magnetic data that was processed using a recently developed
inversion formula and then draped over the surface and geology. The results reflect the underlying
geology well. A pipe like buried body was defined in this study. Since pyrrhotite and other magnetic
minerals are known to be related to the sulphide zones on Gold King this data process may be
valuable for better defining target areas on the property.
The surface IP geophysical program was done in August 2006 by SJ Geophysics (Rastad, 2006).
The study was done on seven lines with a 50 meter spacing between lines and 25 or 50 meter
spacing along the lines. The lines are oriented north-north-west to south-south-east. A modified poledipole configuration with a 3.6Kw transmitter was used in a 2 second on / 2 second off cycle in the
three dimensional IP array (3DIP). The data analysis was by three dimensional inversion techniques
developed to improve the interpretation of data. This allows the overlay of the 3DIP data on the
terrain which due to its steep nature improves the definition of its buried location.
Quoting the Rastad (2006) report:
“The inverted 3DIP data set revealed a distinctive east-west tending resistive break, suggesting a
possible lithological change. This separates the grid region into two zones, with the lower
resistivity zone being to the north. The inversion revealed two distinct chargeable bodies. Both
chargeability features are located on the western portion of the grid. Both are associated with the
a low resistivity zone.”
Plan maps were prepared after the inversion and are included at the end of this report.
The following is quoted from the Rastad (2006) report:
“DISCUSSION OF RESULTS
The following discussion of the geophysical data will provide a brief interpretation of each
individual geophysical parameter (resistivity and chargeability), and then look at the associations
between these parameters for a complete compilation. All locational references will be based on
the local coordinate system for this grid. Please refer to Figure 2 for orientation of the grid. Figure
3 below shows a plan view of the inverted resistivity model for a depth of 100m below the surface.
Examination of the model clearly illustrates the existence of two zones: a southwestnortheast
trending zone of lower resistivity values in the north and a higher resistive zone to the south. The
linear break between the two zones may suggest a geological contact or a possible fault.
The inverted chargeability models reveals two small pods of anomalously high chargeability
material located near surface at approximately 200S on lines 6E and 7E. These are highlighted
on Figure 4 by the annotated black dashed circle. In addition to these two smalls pods, two larger
chargeability features exist at depth (Figure 5). They appear to start approximately at 50m and
extend past 150m. The depth extent of these features can not be determined as it may be below
the depth of investigation for the survey.
The northern chargeability feature is situated between 200S and 400S. The higher chargeability
values (> 32ms) extends from line 6E all the way to the east. A zone of moderate chargeabililty
extends out to the west and slightly north. As for the southern chargeability feature, it is situated
between 600S and 800S and extends from 5E all the way to the east. Similar to the the northern
Summary Report
on the Gold King Property
Revised on January 11, 2008
17
feature, a zone of moderate chargeability extends to the west. Both these features are open to
the east and to the west and require additional follow up to fully delineate the chargeability
features.
The steep topography of this project adds a level of complexity to the interpretation, especially
viewing the inverted results with 2D plan maps. The use of a visualization package allows greater
sense of location in relation to the topography especially with a DEM surface overlaying the
model. Figure 6, shows the chargeability and the relationship in depth between the small pods
and the two features at depth.
Another strong feature with visualization program is the ability to view multiple parameters
simultaneously. This enhances the interpretation process by illustrating the direct associations
between the different parameters. Figure 7, shows a compilation of the two geophysical
parameters resistivity and chargeability.
From the compilation it is clear that there are some significant associations between the two
geophysical parameters. The most noticeable association is the direct correlation between the
two chargeability features at depth with both the low and high resistivity zones. The northern
chargeability feature appears to be flanking the southern edge of the low resistive zone.
Whereas, the southern chargeability feature is flanking the southern edge of the high resistive
zone. Both chargeability features appear to situated slightly below both the resistivity features.
CONCLUSIONS
SJ Geophysics Ltd. acquired 3D Induced Polarization data over Goldking Mining Ltd.'s Gold King
property concentrating on the Tenquille Lake region. From the inverted resistivity and
chargeability models two anomalous chargeability features have been noted as well as two
smaller pods of high chargeability at the surface.
Under ideal conditions, the Tenquille Lake grid should be extended to the east to determine the
full extent of the two chargeability features. It may also be wise to extend an extra two lines to the
west to determine the trend of the moderate chargeable material extending from the two features.
Extension of the grid would require some thought to ensure it is logistically feasible on the steep
topography. Some ground work should be conducted to determine if any outcropping is
associated with the smaller pods at surface to determine if any mineralization is present.
A more exhaustive investigation of the geophysical data with the geological data may unearth
more subtle features that may provide further insight to direct future drilling targets. These
geophysical results have detected two interesting anomalous features that should be examined
along with previous exploration data (geochemistry and other geophysical surveys etc.). When
some drill data is available for this property, the geophysical data should definitely be revisited
and a detailed review of the inversion models should be conducted. Examination of the
geophysical data with drill data can act as a control and greatly enhance the interpretation of the
geophysics by relating the cores with resistivity values and then tracking the associated trends.”
The cost of the exploration as reported to the Province of British Columbia for assessment work
values and reported as such in the reports filed to document the work completed since the property
was acquired by Wolverine Minerals are reported below.
Summary Report
on the Gold King Property
Revised on January 11, 2008
18
Table 3
Exploration Costs by Wolverine Minerals:
Report Number and Basic Description of Activity
27806 Geology, Geochemistry and Petrology
28234 Geology and Geochemistry
28607 IP Geophysics
Total
Costs Reported
$16,061.12
$19,678.08
$78,856.61
$114,595.81
DRILLING
Wolverine Minerals Corp. has not yet done any drilling.
There is a history of drilling by previous operators on the property as outlined in the History section of
this report.
SAMPLING METHOD AND APPROACH
Three rock samples were collected by the author on July 9, 2004. The GK 1 and GK 2 were collected
as grab chips of the mineralized Gold King skarn zones. The Camp Adit dump was a grab sample
from the dump in front of a short adit located at the former camp of Ajax Resources established by
the author in 1987. This is located between the Gold King and Number 4 Zones. A copy of the assay
values, as reported by ALS Chemex Laboratories of North Vancouver, BC, is inserted here for
reference.
Table 4
Geochemical Analysis of samples collected by author
VA04044463 - Finalized
CLIENT : "BUTSEA Butler
Sea
n"
# of SAMPLES : 3
DATE RECEIVED : 2004-07-13
PROJECT : "GK"
CERTIFICATE COMMENTS : ""
PO NUMBER : " "
MEGR
A21
MEGR
A21
MEICP
41
MEICP
41
MEICP4
1
MEICP
41
MEICP
41
MEICP
41
SAMPLE
Au
Ag
Ag
Al
As
B
Ba
Be
DESCRIPTION
ppm
ppm
ppm
%
ppm
ppm
ppm
ppm
GK-1
GK-2
0.1
0.42
<5
24
0.9
37.2
0.58
2.16
5
168
<10
<10
40
10
<0.5
<0.5
CAMP ADUT DUMP
12.1
39
56.8
0.98
8430
<10
<10
<0.5
MEICP
41
MEICP
41
MEICP
41
MEICP
41
MEICP
41
MEICP
41
MEICP4
1
MEICP
41
MEICP
41
MEICP
41
Bi
ppm
Ca
%
Cd
ppm
Co
ppm
Cr
ppm
Cu
ppm
Fe
%
Ga
ppm
Hg
ppm
K
%
<2
15.5
<0.5
12
63
112
13.35
<10
1
0.09
63
1.02
10.7
11
92
485
28.8
10
2
0.03
24
0.08
12.7
10
149
656
8.91
<10
2
0.01
Summary Report
on the Gold King Property
Revised on January 11, 2008
19
MEICP
41
La
MEICP
41
Mg
MEICP4
1
Mn
MEICP
41
Mo
MEICP4
1
Na
MEICP
41
Ni
MEICP
41
P
MEICP4
1
Pb
MEICP4
1
S
ppm
%
ppm
ppm
%
ppm
ppm
ppm
%
<10
0.21
7360
3
0.03
8
450
4
1.27
<10
<10
0.5
0.24
3580
979
46
8
0.01
<0.01
6
7
730
170
1300
5550
1.52
2.3
MEICP
41
MEICP
41
MEICP
41
MEICP4
1
MEICP
41
MEICP
41
MEICP
41
MEICP4
1
MEICP4
1
Sb
Sc
Sr
Ti
Tl
U
V
W
Zn
ppm
ppm
ppm
%
ppm
ppm
ppm
ppm
ppm
<2
5
2
13
36
2
0.01
0.03
<10
<10
<10
<10
23
154
10
<10
31
4710
18
5
2
<0.01
<10
<10
28
<10
3930
These analyses were from surface rock samples and they were fairly heavily weathered. The
samples were collected by the author and remained in his possession and control until personally
delivering them for analysis at ALS Chemex in North Vancouver, BC. No check or blank samples
were inserted by the author.
No samples were collected during the December 1, 2007 visit due to a snow covering of about one
meter depth limiting the ability to correlate relationships.
SAMPLE PREPARATION, ANALYSES AND SECURITY
Analysis was done by ALS Chemex Laboratories of North Vancouver, BC.
The following is a description of sample preparation and analysis.
Sample preparation:
CRU-31
Fine crushing the sample to 70% less than 2mm.
PUL-31
Pulverizing a split of up to 250 grams to 85% less than 75 um in a ring pulverizer
Sample Analysis (units are indicated on the Analysis Certificate)
ME-GRA-21
Au Ag 30g FA GRAV Finish Gold and silver analysis by fire assay and
gravimetric finish. 30 g nominal sample weight.
ME-ICP41 34 elements analyzed by aqua-regia acid digestion and ICP-AES analysis. The following
elements will be incompletely digested in most sample matrices; Al, B, Ba, Be, Ca, Cr, Ga, K , La,
Mg, Na, Sc, Sr, Ti, Tl, W.
The samples were collected in the field and labelled by Sean P. Butler, P.Geo., the author of this
report. The samples remained in his possession and control until delivery by the author to ALS
Chemex Laboratory, in North Vancouver, BC on July 13, 2004.
ALS Chemex Laboratories is located at 212 Brooksbank Avenue, North Vancouver, BC, Canada,
V7J 2C1
DATA VERIFICATION
No verification of the historic analytical work or drill core descriptions was directly possible for the
historic work since the samples and core has long ago been disposed. The samples collected by the
author and under his supervision in 1987 confirm the nature and potential high grade of the
Summary Report
on the Gold King Property
Revised on January 11, 2008
20
mineralization on this property. No blanks or known control samples were inserted by the author
during the 2004 property examination or the project done under his supervision in 1987.
The author is not aware of any control or blank samples inserted into the sample stream by the
geologists in the work programs done by Wolverine Minerals in 2005 and 2006. All samples were
delivered under the supervision of the project leaders, Shearer and Krause, to the laboratory.
The author recommends that a data verification program including insertion of blank and reference
samples be done in all future programs.
ADJACENT PROPERTIES
There are several adjacent properties described in the BC Ministry of Energy, Mines and Petroleum
Resources MINFILE located within fifteen kilometres of the Gold King including:
Bank – (MINFILE Number: 092JSE031) a shear or vein zone of silver, lead and zinc with some gold.
Located one kilometre southwest of the confluence of Tenas Creek with Birkenhead River to the east
of the Gold King property.
Sylvan - (MINFILE Number: 092JSE020) a massive pyrite and pyrrhotite skarn on the western
slopes of Birkenhead Peak to the east of the Gold King property.
Aurum – (MINFILE Number: 092JNE147) is a gold vein property on the Birkenhead River and the
slope of the mountain to the north of Tenquille Creek. It includes a grab rock sample of 15.2 g/t gold
in a trench. There is reportedly gold, copper, lead, zinc and molybdenum. This is located to the east
of the Gold King property.
Copper Queen - (MINFILE Number: 092JSE004) is a copper porphyry or shear zone explored by an
underground adit developed in the early 1900’s for copper. It is located just south-east of the Gold
King property in the lower reaches of Owl Creek. There were several programs of exploration for
Copper Porphyry targets inside and on the southern boundary of the Gold King property and
extending down Owl Creek to the Copper Queen. This was included in the History section due to the
overlap of these programs with the Gold King property.
Lizard – (MINFILE Number: 092JSE029) a tungsten-molybdenum skarn located on Birkenhead
Creek to the east of the Gold King property.
Owl Mountain – (MINFILE Number: 092JSE014) a massive magnetite, pyrite and arsenopyrite with
gold related to arsenopyrite. This is located near the microwave tower on Owl Mountain to the southeast of the Gold King property.
The Gold King property is located about 35 kilometres south-south-west of the Bridge River mining
camp that includes the Bralorne and Pioneer gold mines, the largest producer of lode gold in British
Columbia.
MINERAL PROCESSING AND METALLURGICAL TESTING
The author is not aware of any mineral process and metallurgical work.
MINERAL RESOURCE AND MINERAL RESERVE ESTIMATES
The author is not aware of any Mineral Resource or Reserves estimates having been done on this
project.
Summary Report
on the Gold King Property
Revised on January 11, 2008
21
OTHER RELEVANT DATA AND INFORMATION
The author is not aware of any other relevant data not addressed in this report.
INTERPRETATION AND CONCLUSIONS
Based on the evidence in many reports reviewed, my field and supervised work in 1987 and property
visits in 2004 and 2007 to the claims, secondary data sources, experience and professional
geological and marketing judgement, it is my opinion that the Gold King Project constitutes a
property of merit and justifies further work to explore for commercial gold opportunities.
The geological environment can be defined as a complex intrusive-skarn zone developed along the
contact of the Spetch Creek Pluton and Triassic Cadwallader Group volcanic and sedimentary rocks.
The primary skarn is compositionally zoned from zoisite-diopside-quartz skarn, through quartz-minor
epidote skarn, siliceous quartz skarn and dark green chlorite-pyrite-pyrrhotite skarn. Brown garnet
occurs irregularly in the zoisite and epidote zones. Significant amounts of disseminated pyrite and
pyrrhotite are relatively constant throughout the area tested and can form semi massive to massive
sections associated with the chlorite skarn and epidote skarn. There is a long history of finding zones
in drifts and drill intercepts of significant grades of gold, silver, copper, zinc and lead.
The Gold King property is located over the Owl Creek fault. This is a northern continuation of the
regionally important Harrison Lake Fault Zone that can be traced over 100 kilometres. Several
splays, including the Grizzly Shear, also cross the property. This shear includes several Triassic
aged intrusives within or near it. Metal mineralization is common along and near this shear from the
Copper Queen in lower Owl Creek in the south to the Grizzly Shear, explored by Teck in the north.
The proposed work program has been broken into several phases that are contingent on positive
results in the previous stage. This is a large property with a number of mineralized targets and
representing several ore deposit types including veins, skarns and porphyry copper. The initial focus
of work is recommended in and around the Gold King zone.
Summary Report
on the Gold King Property
Revised on January 11, 2008
22
RECOMMENDATIONS AND BUDGET
In Stage I Diamond drilling of targets identified in the IP Geophysics as completed by SJ
Geophysics on the Gold King zone. These targets are identified and copied from a memo from SJ
Geophysics signed by Shawn Rastad (2007). Total depth identified here is 1,300 (4264 feet) to
1,750 (5,740 feet) meters of diamond drilling. Several of these holes may be longer or shorter
than identified and 4,500 feet of drilling should confirm these targets.
Summary of Drill Targets – Intersection Coordinate at specified depth.
E
N
Inters.
ID
LABEL (Nad83z10) (Nad83z10) Azimuth
Depth
1
GK-01
507296
5596378
vertical
25m
2
GK-02
507328
5596400
vertical
25m
3
GK-03
507359
5596341
vertical
25m
4
GK-04
507472
5596340
345
100m
5
GK-05
507484
5596304
345
100m
6
GK-06
507495
5596264
345
100m
7
GK-07
507609
5595933
165
100m
8
GK-08
507624
5595890
165
100m
9
GK-09
507643
5595842
165
100m
10
GK-10
507528
5595903
vertical
100m
Drill Depth
75-100m
75-100m
100-150m
150-200m
150-200m
150-200m
150-200m
150-200m
150-200m
150-200m
Due to the undulating and locally steep surface topography the final collar locations and drill hole
orientations may need to be evaluated on site prior to starting drilling to intersect the targets.
In Stage II continued diamond drilling of the targets as found in Stage I and later possibly some
work in the Number 4 zone for the contact zone precious and base metal targets
Later, but unbudgeted in this report, work could include airborne geophysics on this large
property and IP follow up including the extension of the IP grid on Gold King. The Gold King grid
extension may be difficult due to steep local topography. The Owl Creek area has the potential for
porphyry copper targets to be developed as well as several other potential contact zone targets
as potentially indicated by the previous work in this area. The extension of the Gold King IP grid,
as recommended by SJ Geophysics, could be considered if positive results were seen in the
Stage I drilling.
Stage I
Diamond Drilling on Gold King
Planning, final selection and site confirmation
Diamond Drilling of targets on the Gold King zone
4,500 feet at $70/foot all in cost including helicopter
access, camp development and operation and drilling
Sampling, analysis and characterizing studies
Supervision and core logging, permit application,
report preparation
$10,000.00
$315,000.00
$20,000.00
$40,000.00
$385,000.00
Stage II
Total
$385,000.00
Continued Diamond Drilling on Gold King and possibly Number 4 Zones
Follow up Diamond drilling of targets on Gold King
$175,000.00
and possibly other zones 2,500 feet at $70 /foot
Analysis and sampling
$20,000.00
Geological study, reports and project management
$30,000.00
$225,000.00
$225,000.00
$610,000.00
Summary Report
on the Gold King Property
Revised on January 11, 2008
23
REFERENCES
Anderson, R.B., and Witherly, K., 1973:
Geological, Geochemical, and Geophysical Report on the Owl Claim Group, Owl Creek,
Pemberton, BC, Assessment Report 4958.
Blank, M. E. and Butler, S. P., 1988:
Report on the Tenquille Claim Group, Lillooet Mining Division, British Columbia. Assessment
Report #17261 for Ajax Resources Ltd. dated Feb. 27, 1988.
Cairnes, C. E., 1925:
Pemberton Area, Lillooet District, British Columbia. Geological Survey of Canada Summary
Report 1924, Part A, pp 76-99.
Cavey, George and Helgason, Robert, 1984:
Report on the Avalanche Claims for Caliente Resources, Assessment Report 14,244, December
12, 1984
Cavey, George, Lebel, Larry and Helgason, Robert, 1985:
Phase II Report on the Avalanche Claims, Caliente Resources, Assessment Report 14,208,
October 3, 1985
Christopher, P. A., 1989:
Geological, Geochemical & Geophysical Report on the Zul Property, for New Camp Resources,
BC Assessment Report 19,169, October 1989
1990:
Geological, Geochemical and Geophysical Report on the Zul Property for New Camp Resources,
BC Assessment Report 20642, December 1990
Condon, F., and Scott, J.S., 1964:
Geological and Geochemical Report, Owl Creek Area, BC, BC Assessment Report 599, October
1964.
Curtis, P. G., 1982:
Geophysical and Geological Report on the P.T. Rex and Hiag 81 Claims for Tenquille Resources
Ltd. Assessment Report #10299.
1983:
Diamond Drilling Program on the Hiag Group owned by Tenquille Resources Ltd., Lillooet Mining
Division for Amazon Petroleum Corporation, Assessment Report #11418 dated October 25, 1983.
Debicki, E.J., 1983:
Geological Geochemical and Geophysical Report on the HAG 1 to 3 Claims for Canadian Nickel
Company Ltd., Assessment Report 11496, dated October 1983.
Deleen, John, 1982:
Report on the Tenquille Lake Claims of Tenquille Resources Ltd. dated September 17, 1982.
1983:
Report on the Work Completed on the Tenquille Lake Claims for Amazon Petroleum Corp and
Tenquille Resources Ltd. dated October 31, 1983.
1986:
Report on the Tenquille Lake Claims for Tenquille Resources Ltd., August 15, 1986.
Summary Report
on the Gold King Property
Revised on January 11, 2008
24
Deleen, John and Curtis, P. G., 1982:
Geophysical, Geological, Trenching, Sampling and Prospecting Report on the Hiag 2, Hiag 3,
Hiag 81, Early 1, Early 7, Rex 81, Saint Paul, Crown Fraction, Santa Barbara and Pt. Rex 81.
Assessment Report 11,011 for Amazon Petroleum Corporation dated September 17, 1982.
Ettlinger, A. D. and Ray, G. E., 1983:
Precious Metal Enriched Skarns in British Columbia. An Overview and Geological Study, B.C.
Ministry of Energy, Mines and Petroleum Resources, GSB, Paper 1989-3, 120pp.
Fawley, Allan P., 1960:
Geological Report on Claims Numbers 393622 – 393635, of Owl Creek Gold Mines Limited
N.P.L., Pemberton Area, British Columbia, BC Assessment Report 361.
Gatchalian, F.; Witherly, K, 1974:
Geological, Geophysical, Geochemical Report on the Owl Creek Claim Group, Owl Creek,
Pemberton area, BC, BC Assessment Report 5292
Hall, D. 1993
IP / Resistivity Survey on the Pemberton Property for Cominco, Assessment Report 23,145,
October 1993
Jackisch, I., 1993:
Assessment Report IP /Resistivity Survey on the Owl Property for Cominco. BC Assessment
Report No 22991
Malcolm, D. C., 1961:
Tenquille Project No. 34, Geological Report for Phelps Dodge Corp of Canada, B.C. Assessment
Report No 365.
McLaren, G. and Rouse, J., 1989:
Geology and Geochemistry of the Tenquille Creek to Owl Mountain Area, BCEMPR, Open File
1989-26
Mienert, L., 1996:
Web site http://www.wsu.edu:8080/~meinert/aboutskarn.html#Gold%20Skarns
Noakes, S., 1992
Geochemical Report on the Owl Claims, for Cominco, BC Assessment Report No , 22889,
November 1992
Page, P. E., 1967:
Geological Report and Mineral Examination, 20 miles north-east of Pemberton, B.C. (Tenquille
Lake Area).
Pautler Jean, 1990:
1990 In House Report Geological, Geochemical, Geophysical Report on the AVALANCE
Property, Teck Corp., BC Assessment Report 21,272, December 1990
1991A:
Geological, Geochemical and Geophysical Assessment Report on the SUNGOD Property for
Teck Corporation, BC Assessment Report 21,274, April 1991
1991B:
1991 Assessment Report on the AVALANCHE Property, Teck Corp., BC Assessment Report
22,247, December 1991
Summary Report
on the Gold King Property
Revised on January 11, 2008
25
1992A:
1991 In House Geological, Geochemical and Diamond Drilling Report on the AVALANCHE
Property, Teck Corp., March 1992
1992B:
1992 In House Diamond Drill Report on the AVALANCHE Property, Teck Corp, December 1992
Pezzot, E. T., 2006:
Memorandum to Bob Krause on the Goldking Property, April 26, 2006
Rastad, S., 2006:
Geophysical Report on the Gold King Property for Gold King Mining September 2006
2007:
Memorandum: RE: 2006 3DIP Geophysical Survey on the Gold King Property, February 28, 2007
to Bob Krause
Rayner, G. H,, and Witherly, K., 1974:
Geological, Geochemical, Geophysical and Diamond Drilling Report on the Owl Creek Group,
Pemberton, BC, BC Assessment Report 5455.
Riddell, J. M. 1990:
Stratigraphy of Mesozoic Rocks East of Pemberton, British Columbia, and the Setting of Mineral
Showings (92J/2, 7, 10), Geological Fieldwork 1990, EMPR, Geological Survey of BC
Riddell, J.M. Helm, S.M. and Pautler, J.M., 1991:
Geology of the Tenquille Lake, Owl Creek and Lillooet Lake Area, OF 1991-12 (92J/1, 2, 7, 10
(compilation map at 1:100 000), EMPR, Geological Survey of BC
Roddick, J. A. and Hutchison, W. W., 1973:
Pemberton (east half) Map Area, British Columbia, Geological Survey of Canada, Paper 73-17.
Shearer, J. T., 2005A:
Geological and Geochemical Report on the Gold King Property for Gold King Mining, June 30,
2005, BC Assessment Report No. 27,806
2005B:
Geological Report on the Gold King Property for Gold King MIning, October 30, 2005, BC
Assessment Report No. 28,234
Weymark, W. J., 1972:
Assessment Geophysical Report on the Ivan 1-16 Mineral Claims, B.C. Assessment Report No.
4154.
Woodsworth, G. J., 1977:
Geological Map, Pemberton map Sheet (92J) Geological Survey of Canada Open File 482.
British Columbia Minister of Mines:
Annual Reports 1918, 1919, 1920, 1922, 1923, 1924, 1925, 1926, 1927, 1928, 1929, 1930, 1931,
1932, 1937, 1960.
BC Ministry of Energy and Mines, MINFILE - properties in the Tenquille Lake and Owl Lake area
and surrounding region.
Summary Report
on the Gold King Property
Revised on January 11, 2008
26
SJ Geophysics Induced Polarization Chargeability and Resistivity Plans
FIG 6-STEPENSON’S SAMPLES
FIG 7-GENERAL LOCATION OF ROCK SAMPLES MAP
FIG-7b DETAIL OF AREA II LOCATION OF KRAUSE’S ROCK SAMPLES
FIG-7c DETAIL OF AREA I LOCATION OF KRAUSE’S ROCK SAMPLES
GEOCHEMICAL ANALYSES FROM 2005 PROJECT
On the pages following:
Summary Report
on the Gold King Property
Revised on January 11, 2008
29
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>40
36−40
32−36
28−32
24−28
20−24
16−20
12−16
8−12
4−8
<4
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Chargeability (ms)
False Color Contour Map
Depth 25m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate C−1
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>40
36−40
32−36
28−32
24−28
20−24
16−20
12−16
8−12
4−8
<4
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Chargeability (ms)
False Color Contour Map
Depth 50m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate C−2
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>40
36−40
32−36
28−32
24−28
20−24
16−20
12−16
8−12
4−8
<4
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Chargeability (ms)
False Color Contour Map
Depth 75m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate C−3
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>40
36−40
32−36
28−32
24−28
20−24
16−20
12−16
8−12
4−8
<4
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Chargeability (ms)
False Color Contour Map
Depth 100m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate C−4
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>40
36−40
32−36
28−32
24−28
20−24
16−20
12−16
8−12
4−8
<4
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Chargeability (ms)
False Color Contour Map
Depth 150m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate C−5
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>40
36−40
32−36
28−32
24−28
20−24
16−20
12−16
8−12
4−8
<4
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Chargeability (ms)
False Color Contour Map
Depth 200m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate C−6
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>40
36−40
32−36
28−32
24−28
20−24
16−20
12−16
8−12
4−8
<4
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Chargeability (ms)
False Color Contour Map
Depth 250m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate C−7
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>7200
5160−7200
3700−5160
2650−3700
1900−2650
1360−1900
970−1360
690−970
490−690
350−490
250−350
<250
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Resistivity (Ohm−m)
False Color Contour Map
Depth 25m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate R−1
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>7200
5160−7200
3700−5160
2650−3700
1900−2650
1360−1900
970−1360
690−970
490−690
350−490
250−350
<250
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Resistivity (Ohm−m)
False Color Contour Map
Depth 50m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate R−2
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>7200
5160−7200
3700−5160
2650−3700
1900−2650
1360−1900
970−1360
690−970
490−690
350−490
250−350
<250
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Resistivity (Ohm−m)
False Color Contour Map
Depth 75m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate R−3
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>7200
5160−7200
3700−5160
2650−3700
1900−2650
1360−1900
970−1360
690−970
490−690
350−490
250−350
<250
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Resistivity (Ohm−m)
False Color Contour Map
Depth 100m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate R−4
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>7200
5160−7200
3700−5160
2650−3700
1900−2650
1360−1900
970−1360
690−970
490−690
350−490
250−350
<250
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Resistivity (Ohm−m)
False Color Contour Map
Depth 150m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate R−5
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>7200
5160−7200
3700−5160
2650−3700
1900−2650
1360−1900
970−1360
690−970
490−690
350−490
250−350
<250
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Resistivity (Ohm−m)
False Color Contour Map
Depth 200m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate R−6
507750
507500
507250
1E
2E
3E
4E
5E
6E
7E
5596500
>7200
5160−7200
3700−5160
2650−3700
1900−2650
1360−1900
970−1360
690−970
490−690
350−490
250−350
<250
0S
0S
S
200
Legend
Survey Stations
Contour Lines
Rivers
Lakes
S
200
Survey Information
5596250
4
00
19
Instrumentation:
RECEIVER: SJ−24 Full−Waveform Digital IP Receiver
TRANSMITTER: GDD Tx II 3.6 KW
00S
3D IP array:
N = 12a = 50 to 100m
400
Survey by: SJ Geophysics Ltd.
3D Inversion by: S.J.V. Consultants Ltd.
Processing Date: Sep., 2006
S
600
Projection: UTM meters, NAD 83 Zone 10
NTS Sheet: 092J10
Base Map: TRIM−BC Data Source − scale 1:20000
Mapsheet 92J056
Lillooet Mining Division
Mapping Date: Sep., 2006
S
5596000
00
20
600
GOLDKING MINING LTD.
S
Gold King Property
Tenquille Lake Grid
Pemberton, BC − Canada
00S
8
2100
1E
2E
3E
4E
SJ Geophysics Ltd.
00S
7E
SJ
8
5E
6E
5595750
3D Inversion Model
Interpreted Resistivity (Ohm−m)
False Color Contour Map
Depth 250m Below Topography
0
50
100
150
200
250
GRASS 6.3
Plate R−7
T
2158
M
507500 mE
2056
507000 mE
506500 mE
506000 mE
505500 mE
M
2000
c
L
E
O
509086
D
2057
5596500 mN
5596500 mN
GKLS 3 to 9
GKLS 22 to 25
2127
2100
GKLS 14
GKLS 21
GKLS 10
GKLS 11
GKLS 12
GKLS 13
5596000 mN
Creek Showing
GKLS 28
GKLS Float
GKLS 20
X
GKLS 19
k
GKLS 2
GKLS 1
GKLS 16
e
GKLS 15
GKLS 17
H
Helipad
5596000 mN
GKLS 18
e
2178
509271
514211
r
GOLD KING MINING INC.
5595500 mN
5595500 mN
C
Date:19/11/2007
LOCATION OF
ROCK SAMPLES
Author:
y
Office:
2100
2000
d
FIGURE: 6
Scale: 1:10000
n
0
1900
As provided by L. Stephenson
GOLD KING PROPERTY
LILLOOET M.D.
by L. Stephenson
Projection: UTM Zone 10 (NAD 83)
METRES
500
515000E
510000E
505000E
500000E
495000E
GROUTY
PEAK
5610000N
514221
517512
514219
FACE
MTN.
517504
5605000N
517476
B
517471 517468
509092
5600000N
509091
N
H
E
A
D
AREA I
Krause’s Samples
509088 509089
509086
509093
509087
E
R
LL
E
IV
LI
K
R
Area of
Stephenson’s
Samples
IR
O
5595000N
O
ET
509271
AREA II
Krause’s Samples
509090
514211
THE
CAMELS BACK
5590000N
R
Y
A
N
RI
514209
VE
MT.
RONAYNE
R
514206
R
IV
E
514412
R
5585000N
GOLD KING MINING INC.
GOLD KING PROPERTY
MINERAL TENURE MAPS 092J/045,046,047,
092J/055,056 and 092J/065,066
NAD '83 ZONE 10
GENERAL LOCATION OF
L. STEPHENSON AND R. KRAUSE SAMPLES
5580000N
DATE:
SCALE:
Nov., 2007
As shown
FIGURE:
7
0
As provided by L. Stephenson
Kilometres
5
511000 mE
510000 mE
509093
1400
5598000 mN
291051-291054
1300
291055291058
509093
1400
1 50
1600
0
291059-291061
AREA II
5597000 mN
LEGEND
186
Traverse
1700
GOLD KING MINING INC.
509087
Date:19/11/2007
Author:
Office:
1800
FIGURE: 7b
Scale: 1:10000
GOLD KING PROPERTY
LILLOOET M.D.
LOCATION OF
ROCK SAMPLES
Taken by R.G. Krause
Projection: UTM Zone 10 (NAD 83)
METRES
As provided by L. Stephenson
0
500
509000 mE
508000 mE
AREA I
291101-291105
509086
509087
291116-291121
291111-291115
5597000 mN
291106-291110
291122-291126
291145-291150
18
19
00
00
20
00
291139-291144
291127-291132
2093
LEGEND
Traverse
291133-291138
5596000 mN
514211
GOLD KING MINING INC.
509090
Date:19/11/2007
GOLD KING PROPERTY
LILLOOET M.D.
Office:
LOCATION OF
ROCK SAMPLES
FIGURE: 7c
Taken by R.G. Krause
Author:
Scale: 1:10000
Projection: UTM Zone 10 (NAD 83)
As provided by L. Stephenson
0
METRES
500
From ACME ANALYTICAL LABORATORIES LTD. 852 E. HASTINGS ST. VANCOUVER BC V6A 1R6 PHONE(604)253-3158 FAX(604)253-1716 @ CSV TEXT FOR
To 695809 B.C. Ltd. PROJECT Gold King
Acme file # A505102 Page 1 Received: AUG 30 2005 * 85 samples in this disk file.
Analysis: GROUP 1D - 0.50 GM SAMPLE LEACHED WITH 3 ML 2-2-2 HCL-HNO3-H2O AT 95 DEG. C FOR ONE HOUR, DILUTED TO 10 ML, ANALYSED BY ICP-E
ELEMENT
Mo
Cu
Pb
Zn
Ag
Ni
Co
Mn
Fe
As
U
Au
Th
Sr
Cd
Sb
SAMPLES
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
%
ppm
ppm
ppm
ppm
ppm
ppm
ppm
291051
32
407
10
555
2.3
2
5
988
3.38
18
<8
<2
<2
1
1.5
<3
291052
17
438
143
1658
9.7
6
11
3591 11.17
271
<8
<2
2
1
9.1
<3
291053
2
21
4
114
0.5
4
16
1048
4.78
8
<8
<2
<2
25
<.5
<3
291054
<1
3
<3
63
0.3
10
16
1238
5.65
<2
<8
<2
<2
27
<.5
<3
291055
4
111
<3
150
0.6
5
17
1190
6.39
25
<8
<2
<2
31
0.6
<3
291056
5
88
<3
457
1.2
9
31
1491
7.32
12
<8
<2
<2
11
2.2
<3
291057
4
155
4
75
1.3
4
24
1018
8.08
23
<8
<2
<2
18
<.5
<3
291058
<1
44
7
144
0.7
5
18
2000
4.91
10
<8
<2
<2
22
0.5
<3
291059
4
134
4
207
1.7
9
37
1664
7.37
12
<8
<2
<2
15
0.9
3
291060
3
99
<3
226
1
14
24
1123
5.3
9
<8
<2
<2
20
0.7
<3
291061
4
70
4
49
1.2
5
34
2693
6.12
45
<8
<2
<2
33
<.5
3
291062
1
248
7
180
1.6
8
91
1391
11
24
<8
<2
<2
13
0.6
5
RE 291062
4
240
5
179
1.6
7
90
1372 10.83
24
<8
<2
<2
13
0.7
7
291063
8
276
12
271
1.6
5
35
797
10
10
<8
<2
<2
9
1.4
8
291064
4
239
4
346
1.5
10
42
2736
9.33
13
<8
<2
3
11
1.2
5
291065
5
115
6
142
0.9
2
18
374
5.14
10
<8
<2
<2
12
<.5
4
291066
1
235
9
150
1.9
8
30
2103
6.77
6
<8
<2
2
24
0.5
<3
291067
3
249
52
1195
2.5
3
26
530
6.76
977
<8
<2
<2
16
6.8
9
291068
94
1805
6378 >10000
56.8
4
79
720 15.62
525
<8
9
<2
2 400.1
13
291069
11
152
21
237
2.2
5
24
2246
9.03
34
<8
<2
2
20
0.8
8
291070
14
274
53
1708
2.9
2
5
2324
8.47
16
<8
<2
<2
6
9
8
291101
22
290
<3
219
2.5
13
10 22543
12.3
142
<8
<2
<2
25
1.3
19
291102
23
97
12
136
2.3
9
7 10730
8.25
368
<8
<2
<2
31
<.5
13
291103
13
56
<3
114
2.5
7
7
8041
8.67
1122
<8
<2
2
31
<.5
19
291104
9
210
<3
224
1.9
3
4
7279 16.05
39
<8
<2
3
20
1.7
13
291105
6
228
<3
69
1.2
2
4
7332 15.83
30
<8
<2
<2
21
1
13
291106
15
108
<3
35
1.3
2
4
3853
14.2
24
<8
<2
3
1
0.9
13
291107
10
96
<3
33
1.4
6
5
3715 15.33
21
<8
<2
<2
1
0.6
17
291108
7
214
<3
24
1.2
10
21
2981 18.77
<2
<8
<2
3
1
0.8
12
291109
16
182
<3
15
0.3
2
5
2339 22.48
2
<8
<2
<2
1
<.5
13
291110
6
288
9
109
2.7
5
23
5631 14.16
16
<8
<2
3
6
0.5
8
291111
4
332
9
96
2.6
5
49
5677 10.48
6
<8
<2
2
16
0.7
13
291112
7
383
5
38
3
2
9
1429 19.27
189
<8
<2
2
3
<.5
<3
291113
8
280
15
64
5.6
1
7
3467 17.43
455
<8
2
5
2
<.5
8
STANDARD DS6/OxF41
12
124
30
144
0.5
25
11
714
2.89
22
<8
<2
4
40
6.1
4
291114
<1
2359
<3
140
<.3
11
356
923 32.32
<2
<8
<2
<2
2
<.5
<3
291115
236
382
5
3717
0.5
10
18
5633 16.76
9
<8
<2
2
4
18.1
9
RE 291115
232
369
291116
1390
176
291117
205
46
291118
1428
149
291119
37
1167
291120
57
1455
291121
8
1195
291122
24
1040
291123
<1
49
291124
1
43
291125
<1
12
291126
<1
27
291127
<1
288
291128
1
8
291129
1
32
291130
2
21
291131
<1
102
291132
<1
3221
291133
<1
343
291134
1
84
291135
1
65
291136
1
21
291137
<1
25
291138
1
198
291139
<1
181
291140
<1
66
291141
<1
90
291142
<1 >10000
291143
1
130
291144
<1
151
291145
3
37
291146
1
949
STANDARD DS6/OxF41
11
123
291147
3
1117
291148
4
96
291149
3
54
RE 291149
3
55
291150
4
427
291151
4
2409
291152
3
154
291153
5
71
291154
3
122
291155
5
104
<3
3687
9
2435
3
958
7
287
12 >10000
9
7872
16
2453
15
7569
<3
191
4
135
<3
182
3
147
4
62
<3
70
4
58
10
245
7
120
5
153
10
64
9
100
7
81
11
89
<3
118
6
39
7
128
4
174
11
175
29
147
3
49
4
187
7
71
7
63
28
142
15
83
6
183
11
50
7
51
7
41
3
246
8
133
7
156
7
76
5
25
<.3
0.6
<.3
<.3
1.3
1.7
2.7
1.4
0.5
3.1
1.1
0.6
6.1
0.5
1
0.7
1.4
>100
6.1
4
1.3
0.7
0.5
4.5
2
1.6
1.1
>100
6.5
15.5
1.6
>100
<.3
>100
1.6
1.5
1.5
6
13.6
1.1
0.7
2.8
2.6
9
5
6
2
18
15
24
18
1
2
6
4
1
2
1
2
2
1
<1
7
3
3
2
1
2
15
18
1
1
8
1
1
25
2
19
1
2
<1
7
2
5
4
3
17
15
14
10
167
161
207
188
14
5
20
15
4
4
8
10
14
5
6
15
7
9
14
4
12
24
24
7
3
27
7
3
11
3
23
4
4
3
26
11
18
8
3
5638
6647
5869
5078
3229
2282
3997
4487
3223
928
4016
3050
1646
3336
1741
6499
5379
37037
3321
2233
3329
1792
2256
3737
2402
2811
3234
795
664
3742
1023
1726
698
847
3675
1203
1177
885
5167
2110
2945
1774
1049
16.64
9.88
6.79
11.65
20.23
19.21
24.1
20.03
4.03
1.03
5.64
4.58
1.36
1.54
2.09
2.57
5.15
5.48
2.98
2.82
2.14
3.23
4.46
1.49
3.42
6.46
6.51
2.65
1.68
6.88
2.63
1.19
2.84
1.28
6.43
2.08
2.03
1.15
6.14
4.68
5.69
2.64
0.92
3
2
9
3
6
11
5
11
6
7
7
4
19
19
7
28
26
369
12
41
27
41
<2
40
18
41
76
1175
19
17
12
169
22
110
84
4
3
30
485
18
7
9
8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
13
<8
<8
<8
<8
<8
<8
<8
<8
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
3
<2
<2
<2
<2
<2
<2
<2
<2
4
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
2
<2
2
2
3
<2
3
2
2
<2
2
4
2
2
2
4
12
15
2
5
5
11
15
48
3
39
39
11
8
17
9
18
15
83
7
8
17
29
5
23
10
26
4
14
13
13
11
40
14
37
22
22
6
28
27
14
12
10
17.8
13.1
3.8
2
70.2
35.7
11.6
34.9
1
<.5
0.7
0.6
<.5
<.5
<.5
1.6
0.5
2.4
0.9
0.6
<.5
<.5
<.5
<.5
<.5
<.5
0.5
7.4
<.5
<.5
<.5
0.6
6.1
4.4
0.6
0.7
0.7
1.4
1.6
0.7
0.9
0.8
1.3
7
9
<3
3
<3
<3
10
8
<3
<3
6
<3
4
<3
6
3
<3
26
<3
21
17
4
<3
38
35
7
<3
488
21
23
5
155
4
67
6
<3
4
25
305
8
13
11
12
291155B
4
267
291156
2
221
291157
3
2089
291158
4
268
291159
2
1724
291160
9
279
291161
2
326
STANDARD DS6/OxF41
12
121
12
8
972
14
16
10
4
29
123
166
73
156
77
90
117
141
19.1
3.6
>100
2.7
24.1
3.3
3
<.3
4
2
2
1
3
2
2
23
12
4
3
7
6
5
13
10
2925
6297
1387
16435
4107
16407
1992
684
3.92
1.87
1.38
4.29
2.32
3.22
4.58
2.84
13
14
242
82
42
72
42
22
<8
10
<8
<8
18
<8
<8
<8
<2
<2
<2
<2
<2
<2
<2
<2
3
3
<2
2
3
2
3
3
18
7
12
61
5
19
14
41
1.3
1.7
7.1
1.3
1.3
1.3
1
5.5
7
4
54
34
6
24
<3
3
(604)253-1716 @ CSV TEXT FORMAT
TO 10 ML, ANALYSED BY ICP-ES.
Bi
V
ppm
ppm
3
39
12
107
<3
33
<3
83
<3
72
<3
91
<3
43
<3
65
<3
106
7
35
<3
39
<3
80
<3
78
<3
38
5
71
<3
54
<3
83
<3
35
97
15
<3
107
<3
38
<3
58
4
117
3
119
6
26
<3
28
<3
10
<3
8
6
6
16
11
5
53
<3
41
<3
45
7
43
4
57
<3
6
<3
18
Ca
%
0.01
0.02
2.72
5.46
2.23
2.17
1.21
3.38
3.24
2.18
10.11
2.35
2.3
2.13
1.69
0.73
3.46
1
0.06
1.87
0.18
14.08
12.46
11.72
12.46
13.65
8.63
8.89
9.44
7.32
1.51
5.09
0.18
0.26
0.89
0.41
10.5
P
%
0.007
0.027
0.073
0.064
0.09
0.068
0.084
0.071
0.036
0.047
0.042
0.047
0.047
0.055
0.067
0.056
0.06
0.064
0.006
0.048
0.034
0.115
0.061
0.052
0.065
0.077
0.021
0.014
0.014
0.046
0.058
0.051
0.054
0.061
0.079
0.011
0.028
La
ppm
1
1
9
6
2
2
<1
2
1
3
2
2
3
1
2
1
1
1
2
3
2
1
3
4
3
2
1
2
2
2
2
2
2
4
14
<1
<1
Cr
ppm
4
6
<1
<1
3
5
<1
5
23
17
4
<1
<1
1
15
7
10
<1
1
9
4
53
13
15
22
23
7
3
7
10
18
8
9
14
189
<1
9
Mg
%
0.21
1.14
0.83
0.68
1.39
1.18
0.86
1.14
1.11
1.14
0.83
1.31
1.3
0.54
1.39
0.28
0.53
0.45
0.07
0.99
0.74
0.25
0.72
0.9
0.1
0.11
0.01
<.01
<.01
0.01
0.82
0.72
0.25
0.4
0.59
0.04
0.01
Ba
ppm
12
8
76
18
16
9
23
17
13
20
5
16
16
18
13
28
17
15
5
16
11
4
10
9
65
59
15
19
8
17
10
7
10
13
167
12
13
Ti
%
<.01
0.01
0.01
0.02
0.1
0.11
0.1
0.08
0.09
0.06
0.05
0.07
0.07
0.07
0.09
0.09
0.05
0.06
0.01
0.08
0.06
0.01
0.05
0.02
0.02
0.03
0.01
0.01
0.01
0.02
0.08
0.05
0.09
0.07
0.08
0.01
0.02
B
ppm
5
18
<3
<3
5
4
<3
3
6
6
4
12
17
11
17
6
14
3
15
19
15
15
22
39
22
11
17
16
8
<3
27
23
15
24
16
<3
<3
Al
%
0.95
3.19
1.43
1.61
3.99
2.46
2.61
2.79
2.51
2.53
1.4
2.61
2.59
1.39
2.52
1.2
2.02
1.63
0.29
2.25
2.19
1.22
1.81
1.97
0.82
0.91
0.45
0.37
0.22
0.34
2.33
1.97
1.15
1.51
1.94
0.14
0.41
Na
%
<.01
<.01
0.03
0.03
0.22
0.03
0.13
0.1
0.07
0.1
0.01
0.05
0.05
0.02
0.02
0.07
0.09
0.13
0.01
0.03
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
0.01
<.01
<.01
0.08
<.01
0.02
K
%
0.07
0.04
0.09
0.08
0.08
0.05
0.1
0.09
0.1
0.09
0.04
0.14
0.14
0.15
0.14
0.18
0.2
0.11
0.05
0.11
0.07
0.01
0.06
0.03
0.07
0.05
0.01
0.01
0.02
0.01
0.08
0.09
0.08
0.09
0.15
0.01
0.05
W
ppm
<2
<2
<2
2
3
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
>100
<2
<2
<2
2
<2
3
<2
8
14
26
17
<2
<2
<2
<2
3
<2
16
Au**
ppb
13
36
2
<2
16
39
16
10
5
3
18
2
3
5
5
2
15
170
8895
20
44
143
16
9
51
35
10
10
381
35
16
3
81
406
813
69
359
<3
7
<3
<3
10
6
30
11
<3
<3
<3
<3
3
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
4
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
17
16
65
24
13
9
8
13
14
5
36
25
10
18
7
5
42
30
15
25
13
24
19
7
19
64
70
11
8
56
11
8
56
9
70
8
9
11
46
14
39
17
10
10.47
10.8
3.43
5.21
1.01
1.33
4.1
5.8
5.75
0.29
3.75
3.5
0.92
0.48
1.44
0.07
0.63
0.72
5.35
0.26
0.08
1.23
2.68
0.11
2.58
0.65
1.74
0.17
0.87
0.88
0.82
1.45
0.86
0.8
1.87
1.41
1.4
0.47
2.72
1.82
0.91
0.87
0.55
0.028
0.021
0.07
0.04
0.017
0.02
0.012
0.015
0.05
0.017
0.046
0.046
0.023
0.024
0.032
0.032
0.073
0.028
0.013
0.072
0.034
0.042
0.062
0.018
0.045
0.075
0.07
0.017
0.021
0.056
0.028
0.025
0.078
0.015
0.067
0.025
0.024
0.024
0.053
0.059
0.046
0.03
0.018
<1
<1
1
<1
1
1
<1
<1
10
<1
9
8
1
2
6
9
7
9
5
2
3
5
9
6
6
4
3
9
5
3
6
3
14
2
3
6
6
1
3
9
8
3
2
7
13
5
5
5
<1
2
<1
4
7
13
5
15
14
2
5
3
12
6
7
6
5
<1
6
7
6
4
6
6
16
8
10
184
13
10
4
8
7
8
4
7
9
11
0.01
0.01
0.28
0.05
0.21
0.18
0.12
0.2
0.7
0.08
1.05
0.87
0.12
0.11
0.16
0.01
0.48
0.25
0.42
0.08
0.02
0.29
0.82
0.02
0.48
0.66
0.78
0.07
0.21
0.43
0.29
0.44
0.58
0.11
1
0.27
0.27
0.06
0.86
0.91
0.39
0.22
0.12
13
7
25
16
20
12
21
15
21
11
16
17
12
30
52
59
35
10
21
15
35
32
24
17
21
57
34
19
23
27
33
14
164
17
18
19
18
11
20
18
17
14
12
0.02
0.01
0.13
0.04
0.03
0.03
0.01
0.02
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
0.08
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
<.01
0.01
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
15
<3
<3
<3
<3
<3
4
<3
<3
<3
9
6
<3
<3
3
7
<3
<3
4
8
9
6
16
12
14
15
17
6
13
14
16
16
14
0.4
0.25
1.76
0.72
0.5
0.44
0.24
0.34
1.33
0.19
1.95
1.5
0.27
0.43
0.67
0.26
1.3
0.33
0.69
0.31
0.29
0.47
1.85
0.2
1.2
1.65
1.21
0.26
0.66
0.55
0.96
0.18
1.92
0.35
0.9
0.65
0.62
0.24
0.49
1.99
0.51
0.29
0.27
0.02
0.01
0.07
0.05
0.01
0.01
0.01
0.01
0.01
<.01
0.01
0.01
<.01
<.01
0.01
0.01
0.02
<.01
0.01
0.01
0.01
<.01
0.01
<.01
0.02
<.01
0.01
<.01
0.01
0.01
0.01
<.01
0.08
0.01
0.01
0.01
0.01
0.01
0.01
0.01
0.01
0.01
0.01
0.06
0.04
0.14
0.1
0.04
0.04
0.05
0.04
0.13
0.1
0.12
0.12
0.09
0.08
0.17
0.14
0.13
0.06
0.07
0.13
0.12
0.14
0.15
0.13
0.15
0.16
0.18
0.09
0.15
0.14
0.18
0.09
0.15
0.09
0.14
0.13
0.13
0.09
0.15
0.13
0.13
0.11
0.08
19
7
<2
10
6
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
3
2
<2
<2
<2
<2
<2
<2
<2
<2
<2
362
591
9
277
1077
817
3367
1165
62
5
3
3
2
3
3
2
2
160
2
2
7
6
4
8
<2
3
3
243
4
6
5
34
799
31
6
<2
2
4
2
3
<2
<2
3
<3
<3
<3
<3
3
<3
<3
5
32
13
11
19
9
22
35
57
1.17
0.41
0.73
0.1
0.09
0.42
0.82
0.76
0.048
0.028
0.019
0.04
0.018
0.031
0.069
0.07
3
3
5
6
6
2
3
12
10
6
6
5
7
6
6
147
0.23
0.13
0.1
0.03
0.03
0.12
0.58
0.54
24
14
10
35
31
15
17
142
<.01
<.01
<.01
<.01
<.01
<.01
<.01
0.08
19
14
<3
16
16
17
13
17
0.62
0.32
0.23
0.37
0.28
0.42
1.28
1.98
0.01
0.01
<.01
<.01
<.01
0.01
0.01
0.08
0.11
0.11
0.08
0.15
0.12
0.12
0.09
0.14
<2
<2
<2
<2
<2
<2
<2
3
9
9
77
10
55
5
4
806
From ACME ANALYTICAL LABORATORIES LTD. 852 E. HASTINGS ST. VANCOUVER BC V6A 1R6 PHONE(604)253-3158 FAX(604)253-1716 @ CSV TEXT FOR
To 695809 B.C. Ltd. PROJECT Gold King
Acme file # A505342 Page 1 Received: SEP 9 2005 * 63 samples in this disk file.
Analysis: GROUP 1D - 0.50 GM SAMPLE LEACHED WITH 3 ML 2-2-2 HCL-HNO3-H2O AT 95 DEG. C FOR ONE HOUR, DILUTED TO 10 ML, ANALYSED BY ICP-E
ELEMENT
Mo
Cu
Pb
Zn
Ag
Ni
Co
Mn
Fe
As
U
Au
Th
Sr
Cd
Sb
SAMPLES
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
%
ppm
ppm
ppm
ppm
ppm
ppm
ppm
291071
3
88
9
71
<.3
3
6
251
2.47
3
<8
<2
<2
32
<.5
<3
291072
2
1483
32
906
<.3
8
<1
597
>40
<2
<8
<2
<2
1
<.5
<3
291073
<1
79
<3
1890
<.3
3
4 13168
11
11
<8
<2
<2
13
7.4
3
291074
4
110
<3
324
<.3
3
<1 17760 28.98
160
<8
<2
2
9
<.5
<3
291076
2
5189
23
8407
5.5
5
17
7879
21.5
93
<8
<2
2
1
39.3
3
291077
2
37
<3
485
<.3
4
<1
5654 10.03
37
<8
<2
<2
21
1.4
3
291078
8
4764
31
247
2.1
9
19
970
>40
<2
<8
<2
3
1
<.5
<3
291079
5
2593
40
524
0.4
7
3
1088
>40
<2
<8
<2
2
2
<.5
<3
291080
1
86
4
38
<.3
7
9
273
3.3
<2
<8
<2
<2
15
<.5
<3
291081
<1
965
23 >10000
0.7
1
26 12682
9.24
12
<8
<2
<2
8 200.6
<3
291082
1
83
4
529
<.3
2
<1 23958
30
240
<8
<2
2
2
1.9
8
291083
16
2240
43
265
0.7
5
<1
2516
>40
<2
<8
<2
<2
3
<.5
<3
291084
6
3131
13
772
0.7
17
13
8599
23.3
10
<8
<2
3
11
2.2
3
291085
12
3935
34
325
2.1
7
<1
1241
>40
<2
<8
<2
2
2
<.5
<3
291086
1
34
<3
293
<.3
35
21
3538
3.74
5
<8
<2
2
45
<.5
<3
291087
<1
49
3
1764
<.3
1
<1 23503 28.86
48
<8
<2
<2
6
9.6
<3
291088
<1
4178
29 >10000
<.3
5
15
4095 36.15
7
<8
<2
3
1 119.5
<3
291089
12
365
9
408
0.4
7
5
3069
7.95
117
<8
<2
2
21
2.6
<3
291090
4
408
32
2153
<.3
15
45
4728 30.55
28
<8
<2
<2
2
11.6
<3
291091
<1
1519
41 >10000
<.3
4
<1
4458
>40
4
<8
<2
4
2 170.2
<3
291092
4
5670
37
287
2.2
7
6
550
>40
<2
12
<2
<2
1
<.5
<3
291093
37
493
129
413
2.5
6
33 14701
>40
3659
<8
<2
4
7
<.5
<3
291094
1
72
<3
123
0.4
3
<1
1878
34.6
16
<8
<2
3
1
<.5
9
RE 291094
1
71
9
121
<.3
4
<1
1882 34.79
11
<8
<2
<2
1
<.5
5
291095
3
63
<3
65
<.3
2
2
2597 13.13
7
<8
<2
<2
2
<.5
3
291096
6
637
<3
821
0.5
2
24 11466 10.73
11
<8
<2
3
21
3.3
5
291097
35
471
1905
6965
7.6
5
26 32434
>40
56
<8
<2
4
24
22.4
7
291098
2
450
10
68
2.7
11
172
1616 27.24
42
<8
<2
<2
1
<.5
4
291099
1
672
14
70
3.2
11
155
1381 36.15
36
<8
<2
2
1
<.5
<3
291100
22
411
820
1664
6.6
5
43 12757 37.61
386
<8
<2
4
3
4.5
<3
GKLS 1
59
867
2242 >10000
35.1
13
109
1980 21.73
160
<8
<2
2
1
51.6
<3
GKLS 2
4
<1
11
63
<.3
7
13
2011 35.34
14
<8
<2
<2
4
<.5
<3
GKLS 3
1
<1
8
67
<.3
9
14
2140 37.66
21
<8
<2
<2
4
<.5
5
GKLS 4
2
<1
6
39
<.3
13
12
2096 34.88
7
9
<2
2
2
<.5
<3
STANDARD DS6/OxF41
12
120
29
141
<.3
24
10
691
2.79
21
<8
<2
3
40
5.7
4
GKLS 5
<1
30
171
2047
95.5
8
19
3205 37.13
15
<8
<2
4
27
18.7
13
GKLS 6
<1
483
5027
9035
>100
8
20
4673 33.14
47
<8
<2
<2
99
71.8
29
GKLS 7
<1
550
GKLS 8
<1
<1
GKLS 9
<1
9
GKLS 10
2
75
GKLS 11
1
9
RE GKLS 11
<1
8
GKLS 12
2
14
GKLS 13
3
636
GKLS 14
5
7
GKLS 15
1
31
GKLS 16
<1
3
GKLS 17
4
38
GKLS 18
1
6
GKLS 19
2
24
GKLS 20
4
4
GKLS 21
3
158
GKLS 22
<1
226
GKLS 23
18
548
GKLS 23A
3
287
GKLS 24
<1
453
GKLS 25
<1
289
GKLS 28
2
474
GKLS 61
7
1152
GKLS 62
7
28
GKLS 63
4
1057
GKLS FLOAT 23-24-25
<1
1563
cop. Lsex
6
1101
STANDARD DS6/OxF41
11
122
1872 >10000
13
144
<3
75
3
61
4
143
10
142
<3
45
8
1732
<3
1614
3
50
5
53
8
95
3
48
<3
84
20
776
18
288
33
2916
151
3703
33
2175
84
5122
65
2419
<3
23
5
113
3
34
17
584
4819 >10000
51
190
29
143
>100
1.7
0.6
<.3
<.3
<.3
<.3
0.9
<.3
<.3
0.4
0.3
<.3
0.7
2.2
4.3
1.5
1.8
1.7
3.9
2.1
<.3
<.3
<.3
1.3
48.1
1.1
<.3
10
10
9
17
7
7
4
5
6
4
1
7
4
5
7
14
9
53
13
33
1
16
<1
5
9
20
3
25
21
12
19
15
14
14
6
49
49
6
6
17
5
17
7
33
17
54
28
30
23
69
<1
14
18
165
<1
11
4854
2363
1345
518
1235
1224
390
12151
17973
540
1453
1433
807
1572
28749
8867
3884
7310
7339
2500
2279
8968
235
435
1445
2441
2208
710
27.77
21.88
35.52
5.09
12.6
12.7
2.58
6.33
8.36
2.81
2.63
5.15
5.28
5.68
6.7
6.93
12.2
15.78
17.64
13.22
6.27
18.59
>40
6.38
17.24
33.48
>40
2.82
37
<2
4
<2
<2
<2
<2
56
30
28
6
14
11
16
5
1695
11
17
9
6
36
<2
186
<2
119
37
3
22
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<8
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
4
<2
<2
<2
3
<2
<2
<2
<2
<2
2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
<2
2
<2
<2
<2
<2
2
2
3
35
6
2
38
32
32
26
34
52
16
34
30
9
80
155
128
10
15
8
15
3
13
1
5
10
1
3
40
125.9
2.1
1.5
<.5
1.7
1.8
<.5
8.5
9.5
<.5
<.5
0.5
<.5
<.5
5.2
2
18.6
21.5
13.7
27
19.7
1.8
1.1
0.9
3.8
276.6
2.4
5.9
6
<3
3
<3
<3
<3
<3
<3
<3
<3
<3
3
<3
5
7
15
6
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
4
(604)253-1716 @ CSV TEXT FORMAT
TO 10 ML, ANALYSED BY ICP-ES.
Bi
V
ppm
ppm
<3
138
71
7
<3
18
<3
14
12
26
<3
37
51
6
64
11
<3
68
7
9
<3
10
68
35
31
32
56
17
<3
63
<3
8
115
11
18
28
106
15
98
19
71
10
47
46
<3
20
<3
18
10
11
<3
48
40
56
12
10
10
12
34
98
64
36
3
17
<3
18
<3
14
5
55
<3
10
4
16
Ca
%
1.15
0.01
11.77
6.76
6.82
13.44
0.09
0.06
0.71
6.99
3.36
0.13
3.61
0.08
3.15
5.75
0.19
3.89
3.48
0.13
0.05
0.29
6.06
6.09
9.16
3.83
1.03
4.66
2.68
0.18
0.09
7.15
8.04
8.86
0.85
6.05
7.29
P
%
0.057
0.009
0.021
0.017
0.018
0.069
0.008
0.023
0.053
0.014
0.012
0.051
0.031
0.028
0.05
0.009
0.023
0.029
0.033
0.037
0.01
0.045
0.02
0.019
0.005
0.051
0.012
0.011
0.017
0.024
0.037
0.044
0.043
0.022
0.078
0.021
0.045
La
ppm
2
1
2
2
3
4
<1
1
1
1
3
2
3
1
3
1
1
3
1
1
<1
4
2
1
2
2
7
7
4
4
1
2
2
2
14
1
1
Cr
ppm
19
2
4
7
4
25
4
10
13
3
6
34
30
19
65
1
2
12
14
20
11
8
17
8
6
4
4
6
9
25
8
14
11
10
167
5
13
Mg
%
0.5
0.03
0.06
0.2
0.02
0.27
0.03
0.09
0.51
0.04
0.17
0.19
0.55
0.09
2.01
0.09
0.15
0.47
0.22
0.24
0.03
0.3
0.02
0.02
0.04
1.33
0.13
0.04
0.05
0.66
0.24
0.02
0.02
<.01
0.57
0.11
0.43
Ba
ppm
23
5
10
27
9
5
7
12
23
6
18
19
16
9
15
21
5
10
14
16
6
28
5
5
2
5
11
21
22
7
5
9
9
17
163
10
12
Ti
%
0.37
<.01
0.04
0.02
0.01
0.06
<.01
<.01
0.16
0.01
0.01
0.01
0.03
<.01
0.12
0.01
0.01
0.11
0.01
0.01
<.01
0.01
0.02
0.02
0.02
0.14
0.01
0.01
0.01
0.01
0.01
0.02
0.02
0.02
0.08
0.01
0.01
B
ppm
<3
<3
4
<3
<3
<3
<3
<3
<3
<3
<3
<3
<3
13
4
<3
<3
11
<3
4
<3
<3
<3
<3
<3
17
<3
<3
<3
<3
<3
<3
<3
<3
16
11
6
Al
%
1.02
0.11
0.89
0.66
0.26
1.73
0.16
0.32
1.03
0.17
0.49
0.7
1.3
0.36
2.46
0.33
0.19
1.77
0.99
0.47
0.12
1.14
0.39
0.38
1.28
2.23
0.82
0.31
0.3
4.19
0.75
0.48
0.55
0.6
1.89
0.36
0.66
Na
%
0.07
<.01
<.01
<.01
<.01
<.01
0.01
<.01
0.1
<.01
<.01
0.01
0.01
<.01
<.01
<.01
<.01
0.01
<.01
<.01
<.01
0.01
<.01
0.01
0.01
0.03
0.03
0.01
0.01
<.01
<.01
0.01
0.01
<.01
0.08
0.01
0.01
K
%
0.08
0.01
0.02
0.05
0.01
0.01
0.01
0.02
0.12
0.01
0.03
0.04
0.09
0.02
0.15
0.06
0.01
0.02
0.04
0.03
0.01
0.03
0.01
0.01
0.01
0.02
0.03
0.01
0.01
0.01
0.04
0.01
0.01
0.02
0.15
0.04
0.04
W
ppm
<2
58
<2
<2
5
<2
22
55
<2
2
<2
51
20
25
<2
<2
29
<2
>100
<2
62
3
<2
2
<2
<2
12
8
5
<2
<2
5
5
2
2
3
<2
Au**
ppb
20
9
8
2
21
19
20
11
3
2176
12
10
6
39
39
6
34
10
10
64
12
305
6
10
11
3
32
8
6
427
1185
7
14
4
830
<2
15
<3
<3
<3
8
4
3
<3
8
<3
<3
<3
<3
<3
<3
<3
<3
<3
4
<3
9
<3
6
8
<3
15
83
69
6
17
55
32
132
119
117
29
11
23
59
19
56
64
84
30
45
124
80
92
14
24
8
10
187
119
14
36
56
9.32
8.19
5.64
0.97
1.88
1.86
0.5
4.65
12.12
0.76
4.47
5.59
0.47
6.11
18.09
14.39
1.46
4.51
1.55
2.59
0.33
6.95
0.03
0.42
1.02
0.06
0.11
0.87
0.019
0.081
0.035
0.059
0.073
0.072
0.028
0.035
0.021
0.033
0.036
0.05
0.057
0.058
0.015
0.035
0.096
0.188
0.121
0.122
0.034
0.032
0.032
0.054
0.07
0.013
0.047
0.078
3
4
2
1
2
2
3
2
1
3
2
7
4
6
3
3
2
3
3
6
3
2
<1
2
2
<1
2
14
6
17
7
57
9
5
10
9
9
10
9
11
9
15
10
17
34
56
39
6
2
7
3
13
21
<1
42
182
0.28
0.16
0.02
1.48
0.09
0.09
0.65
0.19
0.27
0.08
0.19
0.93
1.65
1.95
2.72
1.02
1.34
0.92
1.19
0.36
0.54
0.16
<.01
1.14
1.11
0.17
0.17
0.57
10
9
9
33
5
5
6
25
22
12
16
15
11
5
7
9
9
13
27
28
31
38
4
45
23
4
17
165
0.01
0.11
0.06
0.26
0.18
0.18
0.12
0.04
0.05
0.05
0.09
0.01
0.08
<.01
<.01
<.01
0.15
0.06
0.09
0.03
0.03
0.02
0.01
0.25
0.14
<.01
0.01
0.08
3
9
9
3
7
7
<3
22
16
7
26
3
3
13
9
20
11
5
6
4
9
<3
<3
5
15
16
10
16
0.47
1.28
0.66
2.26
0.61
0.61
1.17
0.38
0.56
0.68
1.05
1.85
1.99
1.07
0.34
0.35
2.72
2.12
2.61
1.24
1.32
0.65
0.15
1.21
2.21
0.45
0.67
1.9
<.01
<.01
<.01
0.18
0.06
0.05
0.1
0.01
0.01
0.05
<.01
0.03
0.05
0.03
<.01
<.01
0.01
<.01
0.01
0.01
<.01
<.01
<.01
0.06
0.02
<.01
<.01
0.08
0.02
0.01
0.01
0.53
0.02
0.02
0.03
0.05
0.02
0.04
0.03
0.13
0.08
0.02
<.01
<.01
0.09
0.1
0.1
0.21
0.17
0.1
<.01
0.49
0.06
0.01
0.03
0.15
5
<2
10
2
3
<2
2
8
2
<2
2
<2
<2
2
<2
<2
<2
<2
<2
<2
<2
4
2
<2
4
>100
60
3
10
<2
<2
2
8
2
<2
12
<2
6
2
<2
19
5
3
76
18
31
27
38
23
583
61
8
32
13518
21
815