1989 till sampling using a wink sonic vibra core drill€¦ · geology * previous work: see page 1...
TRANSCRIPT
42Ae8SE8876 3.13201 BENOIT 010
1989 TILL SAMPLING
USING A WINK SONIC VI BRA CORE DRILL
ON
JOHN JASPERSON'S GOLD PROSPECT
BENOIT TOWNSHIP, ONTARIO
JANUARY 23, 1990 JO WARD
ABSTRACT
From Oct.30 to Nov.4th, 1989 inclusive a program of overburden
drilling was carried out on John Jasperson's Benoit Township
property using a Wink Sonic Vibra Corer. Unexpected difficulty
in penetrating till prevented target depths from being reached.
Since additional information gathered does not detract from the
original objectives, continuance of the overburden sampling is
recommended using a reverse circulation drill at an estimated
cost of less than $20,000..
Respectfully submitted,
page i.
O10C
ABSTRACT
INDEX
page i
page 11
PROPERTY LOCATION AND ACCESS: See page 1 of Ward's May 30 1989report, in appendix
GEOLOGY * PREVIOUS WORK: See page 1 to 8 of Ward's May 301989 report, In appendix " '- ~
,:?r.-.-; - ^ : , -^ - -:;.-.-.. t
1989 TILL SAMPLING USING WINK VIBRA CORE DRILL
REASONS FOR CHOICE OF WINK VIBRA CORE DRILL
THE PROGRAM (OCT. 30 TO NOV.4TH INCLUSIVE)
page 1
page 1
page 2
DRILL PERFORMANCE: See Jasperson's OPAP report of 90/1/24, appendix "L", page 1.
RE INTERPRETATION OF RESISTIVITY SURVEY
BINOCULAR MICROSCOPE INSPECTION OF TILL
GENERAL COMMENTS
HUMUS SAMPLING
CONCLUSIONS AND RECOMMENDATIONS
page i i .
OA/T, .w
page 3.
page 3.
page 4.
page 5.
page 6.
OF W iA/K Vt O A. A C 0^6 T*LU
ACTIVITY UOG- OCt, Jo- ^O^oA //989
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page 1.
1989 TILL SAMPLING USING WINK SONIC VI BRA CORE DRILL
REASONS FOR CHOICE OF WINK SONIC VI BRA CORE DRILL.
The backhoe used in the 1987-88 till sampling program had a
maximum depth reach of 6 meters. Heavy scavenging of gold,
pyrite, and other mobile minerals was noted throughout the 6
meter depth of sampling. ... (Inspection of gold grains by
SEM in 1988 showed removal of the outer 2 microns of gold by
scavenging thereby exposing contained minerals as projections
from the gold grain surfaces. Pyrite left only cubic formed
depressions in the gold grain surface.) ... The implication of
these observations was that all pyrite and all original gold
grains in the till smaller than 4 microns thickness had been
totaly removed by scavenging. It was therefore mandatory to
sample till deeper than 6 meters in order to determine the
original gold and pyrite content of the till.
The Wink Vibra Corer (see OGS Open File Report # 5481) was
chosen for the 1989 sampling program because of following
considerations:
1. Reasonableness of cost ( approx $1,0.00/dy as against |4,OOOXdy for Reverse Circulation drilling).
2. Larger sample than the Wacker drill or Cobra drill (MOOO grams compared to ^00 grams).
3. Claims of contractor of depth penetration that was > double Wacker or Cobra. ... (depth ,of drilling was important to reach bedrock basal till).
4. Reverse Circulation drill overburden sampling loses half
page 2,
of the 10 micron - 100 micron gold content in till and nearly all of the < 4 micron gold. This defeats the possibility of determining the fine gold content of the till.
5. Mobilization and demobilization was quick, flexible, and inexpensive.
6. Portability permitted traversing and sampling in swampy terrain before freezeup. Also, necessity of meeting permit requirements for Reverse Circulation Drill trails avoided.
7. Flexibility in obtaining variable depth sampling usefull in determining probable up-ice distance to anomalous bedrock mineralization sources.
PROGRAM (OCT. 30 - NOV. 4, 1989, INCLUSIVE)
The program was laid out on the expectation of achieving the
contractors suggested performance of 300 feet per day
production. Traverse VT was the most convenient place to
start, to expedite mobilization. One of the difficulties not
anticipated of using the contractor's ATV was the necessity of
cutting a 6 foot wide trail to accomodate equipment carried.
Since the entire southwest flank of the anomaly was heavily
forested and we had not acquired the appropriate cutting
permit, we avoided the forested areas of the sampling program,
leaving only traverse V1 and V2 to be sampled.
For log of daily performance, sample location and depths and
other pertinent activity refer to appendix "M" in Jasperson's
1989 OPAP report dated Jan. 24, 1990.
For drilling equipment description and performance refer to
page 3.
appendix "L" in Jasperson's 1989 OPAP report dated Jan. 24,
1990. Also see OQS Open File Report # 5481.
RE INTERPRETATION OF RESISTIVITY SURVEY.
The EM16R restistivity survey of 1987 was interpreted as a 2
layer system. The Wink Vibra Corer results indicate that
al though the thickness of the first layer was accurate, the
second layer at the main resistivity low was glaciofluvial
till, not bedrock. Since the glaciofluvial till has a
resistance of approximately 80 ohm-meters to 200 ohm-meters and
the apparent resistivity computed low is 50 ohnrrmeters,
therefore the third layer at the main resitivity low must be
less resistive than 50 ohm-meters.
Through geometrical consideration it is estimated by the writer
that the bedrock third layer resistivity is approximately 40
meters wide with a resistivity of approximately 30 ohm-meters.
This is compatible with the presence of a quartz carbonate zone
with approximately 10& disseminated pyrite, or alternatively a
heavily chloritized schist. No evidence has been observed to
date of chloritic schisting in the tills to the south of the
main resistivity low, however chlorite is a very soft mineral
and will not travel far in till.
BINOCULAR MICROSCOPE INSPECTION OF TILL.
The writer inspected the samples with binocular microscope to
page 4.
identify the nature of each till sample. Classification
recorded in the SAMPLE LIST, appendix "E", in Jasperson's 1989
OPAP report dated Jan. 24, 1990.
GENERAL COMMENTS. First, the wet gumbo clay that stuck to the
drill rods in traverse V1 consisted of 95* ,5 micron to 3
micron quartz fragments flocculated in a gel by Van der Waal
forces. The very few clasts greater than 20 microns observed
were predominately sharp edged and therefore of local origin.
(See ODM report, appendix "H" for table concentrate ratios to
sample weight as indicative of the ratio -20 micron fraction to
+ 20 micron fraction. Mixing of portions of lower till into
upper till may have occurred during the Cochrane Advance (9000
BP).
Secondly, the writer estimates that 70fc of the pyrite fragments
in the combined sample V2-000 t V2-060 north were of local
origin and predominately displayed twinning which is
characteristic of marcasite, a hydrothermal form of pyrite.
A Ithough ODM indicates the pyrite count of HMC for this^-S
combined sample to be 200 using 4 power magnification, the
writer counted virtually 2000 fragments of sulphides with the
60 power binocular microscope.
Thirdly, V2-120 north is at the south end of a glacial outwash
area. Microscope inspection by the writer verified that 80fc of
page 5.
the clasts were very badly worn by glacial fluvial transport.
The writer therefore suggests that no local area mineralization
indicators are determinable with V2-120 north samples.
HUMUS SAMPLING.
On Nov.5th the writer inspected the site of Noranda's drill
hole 67-1b and located a half meter diameter black muck hole in
the moss which he sampled for humus. Then following what
appeared to be the original drill road 100 feet grid north
west, the,writer located a similar black muck'hole in the moss
centered in a clearing oriented grid northeast southwest, 10
meters wide and 20 meters long. One humus sample was taken
from the site and 4 others at locations 5 meters grid southwest
to 10 meters grid northeast.
\
Noranda's original 1967 cut survey lines at the site were
relocated (line 8 west on Noranda's northeast southwest grid
and line 16 west on Noranda's northsouth grid). Noranda's
original picket 13+00 south line 16 west was also located
permitting assumed drill hole, labelled #2, location to be
accurately identified at 16+15 west (ft) 13+15 south (ft) on
Noranda's northsouth grid .
The original hope of the writer was to assay the humus samples
for entrapped minerals from drill hole water runoff. The assay
results were unexpectedly much lower than background humus
page 6.
Samples for the property assayed in 1987. The writer then
inspected the humus sample pulps by binocular microscope and
noted that most of the organics had been washed out of the
humus and that the vegetation that remained was in various
states of silicification. At least 10* of the material was
100* replaced by silica in the form of petrified wood. The
similar condition of the humus material at both the known and
suspected drill site suggests both were drill hole sites. It
is suggested by the writer that future sampling for drill hole
water minerals entrapped by humus be attempted larger distances
down drainage.
CONCLUSION AND RECOMMENDATIONS.
The features of no water, mobility and size of sample are the
positive factors of the Wink Vibra Corer drill. The overburden
drill results demonstrated that the EM16R resistivity survey
interpretation was accurate in determining the thickness of the
clay till layer. The paucity of the gold grains encountered in
the Wink Vibra Corer upper till samples, in contrast to the
anomalous gold grain counts of the '87 - '88 basal till
sampling, reinforces the conclusion that the hydrothermal gold
grains of the basal till on John Jasperson's property are of
local origin.
page 7.
It is recommended that the original objectives of the Wink
Vibra Core sampling program be completed by reverse circulation
overburden drilling at an estimated cost of less than $20,000.
Respectfully submitted,
January 23, 1990
Page 8
CERTIFICATION
l hereby certify that all the work covered by this report was
carried out by myself and under my direct supervision and that
the financial interest l hold in the property described is 3/4
of ^ % n et smelter return. l further certify that l have been
engaged in geophysical mineral exploration in Canada for most
of the last 35 years as a geophysicist, contractor, and
consulting engineer.
Former employment includes the positions of Senior Geophysicist
- Barringer Research, Rexdale; Geophysicist - Derry, Michener b
Booth, Consulting Geologists; Geophysicist - Patino Mining
Ltd.; and Staff Geophysicist - UrangeselIschaft Canada Ltd.,
and that of Self-Employed Consulting Engineer in the periods
1970 to 1972, 1974 to 1982 and February 1984 to present.
T. Ward
January 23, 1990
BENOIT
1988
OMEP ASSISTED EXPLORATION
OF
JOHN JASPERSON'S GOLD PROSPECT
BENOIT TWP ONT.
O20
MAY 30, 1989JOHN T. WARD
ABSTRACT
till was sampled at 21 new sites on the stoss side of outcrops
400 meters to 600 meters down-ice from the main resistivity low
anomaly on John Jasperson's Benoit Twp gold prospect. Of 18 basal
till samples processed, 15 exceeded the 90 percentile range
determined for BRIM backhoe lodgement till samples covering 37
townships 1984 to 1988.
Twenty gold grains recovered from John Jasperson's sampling sites
88-01 to 88-10 were photographed and x-ray analyzed by Scanning
Electron Microscope. 90* of the grains were interpreted as having
moved less than 500 meters from their bedrock source. Intergrowth
minerals protruding from the gold grains were noted to be typical of
gangue minerals associated with hydrothermal gold deposits.
Seven large clasts ranging in size from 10cm to 20cm were selected
from the basal till on the basis of their high degree of angularity.
Upon diamond saw cutting and thin section interpretation, all but
one exhibited either 20* to 40* carbonatization or high strain, and
multiple fracturing associated with a prolonged active faulting
environment.
It is concluded that the above gold grain, and large angular clast
studies are overwhelming evidence, that John Jasperson has a viable
hydrothermal gold prospect closely associated witjju-ti^e main
resistivity low anomaly of his Benoit Twp. Group.
THIS PROJECT WAS PARTIALY FUNDED BY OMEP.
Respectfully submitted,
42A88SEWI76 2.13201 BEND l T
TABLE O F. CO._____
- ABSTRACT
- FIG. 1 KEY MAPFIG. 2 JASPERSON CLAIMS: LOCATION OF SIGNIFICANT DETAILS
- PROPERTY LOCATION AND ACCESS
- GEOLOGY AND PREVIOUS WORK
- BASAL TILL SAMPLING AND ASSAYING
- SEM STUDIES OF GOLD GRAINS AND MINERAL GRAINS
- LARGE CLAST STUDIES
- CONCLUSIONS AND RECOMMENDATIONS
- CERTIFICATION
- APPENDIX:FIG. 3 BASAL TILL TRENCHES FIG. 4 GOLD GRAIN COUNT FIG. 5 NORMALIZED GOLD GRAIN COUNTFIG. 6 STRUCTURE INTERPRETATION TIMMINS LARDER LAKE
by C.J.HODGSON
REPORT OVERBURDEN DRILLING MANAGEMENT 10/25/88 BASAL TILL SAMPLES: 88 A 3 TO 88 A 10
REPORT OVERBURDEN DRILLING MANAGEMENT 12/13/88 BASAL TILL SAMPLES: 88-05 AND 88-12 TO 88-21
REPORT BARBARA MURK PETROGRAPHIC DESCRIPTION 5/10/88 HEAVY MINERAL FRACTION 87-1 AND 87-2
REPORT BRUCE JAGO, SEM STUDIES GOLD GRAINS 2/14/89
REPORT BRUCE JAGO, THIN SECTION AND ROCK SAMPLE 5/12/89ANALYSIS PLUS SEM MINERAL GRAIN ANALYSIS
NORANDA EXPLORATION LTD.-1967 DIAMOND DRILL LOGS AND GRID LOCATIONINTERPRETATION WITH RESPECT TO RESISTIVITY SURVEY
REPORTS X-RAY LABS - #6160, #6972, #7326, #7412, #8131, #8281,#8299, #8334
FILE BKLGWGT5 - J.JASPERSON DEC/88: DATA AND ANALYSIS COMPARINGBRIM BACKHOE LODGEMENT TILL HMF GOLD GRAIN COUNT TO JOHN JASPERSON'S BENOIT TWP. GROUP RESULTS.
Page l
BASAL TILL SAMPLING OP JOHN JASPERSON'S GOLD PROSPECT
BENOIT TWP., ONTARIO
PROPERTY LOCATION AND ACCESS
The property lies central to the east half of Benoit Twp., Larder
Lake Mining Division, Ontario, being halfway between the communities
of Kirkland Lake and Matheson, Ontario.
The property can be approached by automobile within one half mile on
three sides, east, south and west. The only access without
tresspassing is from the east. This access is gained by driving 2
miles east and l 1/2 miles north by gravel road from Bourke's
Corners on Highway # 11.
The property consists of 12 unpatented mining claims, L884080 to
L884083 inclusive, L992204-5, L992254-5, L1059464, and L1041489-91
inclusive held by John K. Jasperson of Stouffville, Ontario. The
writer and partners retain a 1.5Z net smelter return interest in the
group.
GEOLOGY AND PREVIOUS WORK
The property is transected east-west by the axis of the Benoit
Syncline which is a possible axis of mid-continent subduction. The
property is underlain by layered dacitic flows predominantly
outcropping and interflow sediments predominantly eroded and covered
by overburden. Flow tops dip 70 to 80 degrees southward north of the
Benoit Syncline axis and 70 to 80 degrees northward south of the
Benoit Syncline axis. These steeply opposed dips are present even
within several meters of the axis, thereby indicating that a fault-
Page 2
kfcke discontinuity must exist along the fold plane. Algoman age
diorite intrusive plugs bound the property on the south and
northwest. These diorite plugs account for local distortions in the
strike and dip of the flows due to their stability during post
Algoman strain of the Benoit Syncline structure. The Black River
fault strikes NW-SE centrally through the property and is eroded
deeply, coinciding with the main axis of the Noranda Exploration
Ltd. 1966 Vertical Coil E.M. conductor. The flows and interflow
sediments strike approximately N 70 degrees W. At Kirkland Lake in
August, 1987, the writer was advised by G. Gabrowski , Acting
Resident Geologist, and H. Lovell, Research Resident Geologist that
heavy fracturing or brecciation should be expected in the interflow
sediments due to late straining of the Benoit Syncline volcanics,
especialy close to cross-faults like the Black Creek Fault. They
further advised that such fracturing would have been continually
regenerated and would have been open to mineralized fluids at all
epochs.
The Thompson-Mcleod (circa 1921) adit and incline shaft on an
auriferous quartz vein lies within the northeast corner of the most
south-east claim of the John Jasperson Group. The quartz vein in
the adit strikes N 30 degrees W, lying alongside a N-S fault
traversing Maisonville, Benoit and Cook Twps., exemplified by and 80
foot high vertical cliff running from 50 meters north of the shaft
to 200 meters nortlyof the shaft along the east boundry of the next
claim north of the shaft.
Three drill holes averaging approximately 170 meters each were
drilled within a 6 claim group centered about the THompson-Mcleod
Page 3
and shaft. These holes were collared in l to 2 meters of
overburden and tested andesitic flows for quartz veins containing
gold. The core was logged and sampled by J.H. McBean in 1945 but no
record was kept of the assays or location of the drill holes. No
intersections of interflow sediments were logged, however 10 meters
of brecciated volcanics were logged in hole 0 3 and it was annoted
by J.W. McBean that much of the core may have been lost. A
comprehensive geological survey and report of past history of the
property and environs was prepared by J. Gauthier, P. Eng., Nov.,S&& A**A(*nfe*r
1983 for Minefinders Corporation Ltd., (file* 26218).
John Jasperson's 12 claim gold prospect essentialy covers a half-
mile strike length, weak conductivity conductor discovered by a 1966
Noranda Explorations Ltd. Vertical Coil E.M. survey. This conductor
is the only conductor in the area and lies l mile up-ice from the
Ontario Geological Survey's KLIP Overburden Drill Hole 80-09 in
which the shaker table concentrate, heavy medium fraction of a 5
foot section of till assayed 140,000 parts per billion Au. The KLIP
data indicated that the anomalous till was derived from a heavily
carbonatized zone associated with minor graphite.
In August 1987 the writer completed a Geonics EM16R VLF Apparent
Resistivity survey of the property. A print of interpreted second
layer resistivity and of interpreted overburden thickness is
included in the appendix of this report.
On June 20th and 21st, 1988 airborne VLF and Magnetometer surveys
were flown by Terraquest Ltd. for Nordex Explosives Ltd., which by
agreement between Nordex and J. Jasperson covered the majority of
Page 4
}n Jasperson's group. The results of these surveys are available
through inspection of the ODM Assessment Filetf W8808:399.
On April 7, 1989, Noranda Exploration Co. Ltd. advised John
Jasperson that they had tested John Jasperson's Group by a 400 foot
drill hole in 1967. A copy of the drill logs supplied by Noranda
Exploration Co. Ltd. is included in the appendix of this report
along with a 1986 grid location interpretation by J. Hard and J.
Jasperson.
BASAL TILL SAMPLING AND ASSAYING
The basal till sampling program using a backhoe started in 1987, was
continued in 1988 with 21 new sampling sites. Sampling was carried
out where possible on the stoss side of the nearest outcrops down-
ice from the main resistivity low anomaly. Basal till was sampled
within 30 cm of bedrock where possible. However, bedrock was far
below the 6 meter reach of the backhoe in the deep overburden areas
of 88-#7, #8, #9, #13. Sample #13 was a quartz sand till. Samples
88-#10 and 88-#ll had no basal till since heavy clay rested directly
on bedrock. Sample 88-#16 and 88-#18 were coarse boulder rubble
with the majority of the till matrix washed away with surface water
runoff.
The clay content of the till samples was reflected by the ratio of
HMF to the till sample weight. Therefore gold grain counts were
normalized to grains per 10 grams of HMF following the methodology
of John Steeles, BRIM Geochemist for the O.G.S.. Overburden
Drilling Management tables listing gold grain size and degree of
delicacy can be found in reports 10/5/88 and 12/13/88. (SEE
APPENDIX)
Page 5
Ctold grains were removed from HMF samples for SEM studies prior to
submission to X-RAY Labs for assay analysis. Therefore the computed
contributions of the gold grains listed by Overburden Drilling
Management should be added to the ppb assay by X-RAY Labs to obtain
assay values comparable to O.G.S. methodology of reporting HMF gold
values.
The writer using O.G.S. reports and maps identified 74 lodgement
till samples encountered in over 250 backhoe samples by BRIM 1984 -
1988. BRIM only panned the HMF when 2 or more grains were noted on
the shaker table, therefore by adding l grain to all BRIM's
lodgement till samples of O or l grain, the writer arrived at a
statistic indicating a backhoe lodgement till background of .43
grains per 10 grams of HMF. The 90 percentile range for BRIM
backhoe lodgement till was determined by the writer to be 1.1 grains
per 10 grams HMF which is exceeded by 90Z of the lodgement tills
sampled on John Jasperson's 1988 sampling program.
It is noted that several of the very high BRIM gold grain counts
were encountered in outwash tills closely flanking the edges of
large eskers.
90JC of the BRIM 90 percentile, normalised, backhoe lodgement till
\ samples were noted by the writer to be lying closely down-ice from
former producers or advanced gold prospects.
X-RAY Lab report #6160 is for -10 mesh fraction of basal till. The
till is scavenged of fine gold by downward perculating surficial
waters. The assays greater than 0.5 ppb indicate the presence of
Page 6
ild grains large enough to survive scavenging.
Report # 6972 exhibits monotonic values except that a correlation is
evident between higher Au and higher Ga.
Report # 7326 are assays of an 8cm wide quartz main vein striking
N 35 degrees H from the THompson-McLeod shaft and sampled 20 meters
N 35 degrees W of the north end of the Thompson-McLeod adit. The
vein carries 31 pyrite and very minor arsenopyrite (see JAGO
Petrographic sample John Jasperson #3 in the appendix of this
report.) Other assays for the sample are report #8131 for nickel
and silver and whole rock analysis, and #8281 for sulphur and
arsenic to quantitize the presence of pyrite and arsenopyrite. The
low CaO assay of 0.26Z is not consistent with JAGO's petrographic
observations of carbonatization of the same sample.
Report #7412 shows a remarkable increase in the resampled 88-05 gold
assay. 13 grains of gold have been removed from this sample after
panning, therefore a nugget effect is not a suitable explanation of
the high assay of 4200 ppb for the HMF. No other element appears to
relate to the higher gold value. Later assays in report #8299 and
#8404 negate high nickel assays of the order of 10 times background
for HMF samples as indicated in report #7412. Sample #88-14
returned consistently high rare earth assays in report #7412
SEM STUDIES OP GOLD GRAINS AND MINERAL GRAINS
Twenty gold grains from HMF pannings of samples 88-02, 03, 04, 05,
06, 08/09 and SHAFT AREA by Overburden Drilling Management were SEM
analysed by Bruce Jago Petrographic Services. (Some grains were
Page 7
^advertently lost in handling.) All but 2 of the 20 gold grains
were interpreted by Bruce Jago as having bedrock sources less than
500 meters up-ice. SEM photos and x-ray analysis indicate that
minerals included in, and protruding from, the gold grains are
representative of gangue minerals of hydrothermal gold deposits t
Bruce Jago's report is in the appendix of this report.
Heavy mineral grain fraction from backhoe basal till sample sites
87-1 and 87-2 were mounted in thin section by Geoplastek and
analysed by Barbara Murk. The garnet count was 20Z lower than the
average Matheson-Kirkland Lake basal till and the epidote almost
halfthe average. However 2Z to 3Z sphene was double the average.
John Ward examined sample 88-13 looking for the 1000 marcasite
grains reported by Overburden Drilling Management. The writer
observed closer to 5000 in number, being perfectly round spherules
ranging in size from 20 microns to 70 microns in diameter. It is
expected by the writer that these marcasite spherules were ofq. i
supergene origin and formed post Pleistocene.
Bruce Jago inspected HM course fraction grains from K.L.I.P.
overburden drill hole 80-9 by binocular microscope and SEM x-ray
analysis. Sample A was from 80-9 sample 2.and sample B was from
80-9 sample 5. Note that sample 5 assayed 140,000 ppb Au.
Surprisingly no gold was identified optically or by SEM x-ray
analysis. However Bruce Jago noted that the source of the grains
was probably a gabbro. This is consistent with the existence of a
mapped gabbro lying along the south boundry of John Jasperson s
Group.
Page 8
LARGE CLAST STUDIES
Seven large clasts ranging in size from 10cm to 20cm were selected
from basal till on the basis of their high degree of angularity.
Description and thin section analysis of these angular clasts are
contained in the May 12, 1989 report by Bruce Jago Petrographic
Services. All but the first of the seven samples selected from
backhoe basal till exhibited either 20X to 40X carbonit ization
mineralization or high strain and multiple fracturing associated
with a prolonged active faulting environment. JJ1 is an outcrop
sample from a fresh, 100 acre extensive, feldspar-phyric andesite
intrusive, l kilometer to the east of John Jasperson's Group. The
observation that this 'fresh' feldspar-phyric andesite contains 10
to 12 percent carbonate is indicative that the 20X to 40X
carbonitization noted in the clasts from the till central to John
Jasperson's Group may well be related to an extensive system of late
Archean carbonatization.
C.J. Hodgson of Queens University has held that much of the gold in
the Timmins, Kirkland Lake and Larder Lake Camps may have been
preceded by a central extensive source of carbonitization possibly
associated with Alkali Intrusives of the 'Matheson Kirkland Intrusive
Belt*. In Hodgson's model, brittle fracturing of the carbonates
then provided channelways and host for hydrothermal gold bearing
solutions and gold deposition. See figure # 6 in the appendix of
this report reproduced from 'Structure and Geological Development of
the Porcupine Camp - A Re-Evaluation 1 C.J. Hodgson. (OGS MP 110,
1983).
Page 9
CONCLUSIONS AND RECOMMENDATIONS
It is concluded that the backhoe sampled, basal till heavy medium
fraction, normalized, gold grain count is anomolously equal to BRIM
sampling results short distances down-ice from former gold
producers.
It is further concluded that the studies by Bruce Jago indicating
that 5 out of 6 large angular clasts from the basal till 500 meters
down-ice from the main resistivity low anomaly indicates the
presence of an extensive system of carbonatization and repeated
brittle fracturing- (Both of these conditions are necessary for the
formation of hydrothermal gold deposits.)
It is further concluded that the gold grain studies by Bruce Jago
using SEM and x-ray analysis, clearly indicate that the anomolous
gold grains in the basal till came from a hydrothermal gold source
less than 500 meters up-ice from the backhoe sampling sites.
It is further concluded that the diabase sample in Bruce Jago ' s
large clast study, not being carbon i t i zed, indicates that the
extensive carbonitization is pre-Keweenawan. It is still further
concluded that the brittle fracturing due to the Black River Fault
setting is necessarily Late Archean, i.e. postdating the formation
of the Benoit (Blake River) Synclinorium. These conclusions lejsd to
a temporal restraint concomitant with C.J. Hodgson's concept of a
single major central source of carbonatization for Timmins, Larder
Lake and Kirkland Lake immediately prior to emplacement of
hydrothermal gold.
Page 10
Igether, all of the above form overwhelming evidence that John
Jasperson has a viable gold prospect closely associated with the
main resistivity low anomaly on his Benoit Twp. Group.
A preliminary diamond drilling program of 600 meters is recommended
at an estimated total cost, including core logging and assaying, of
per meter.
Respectfully Submitted,
May 30, 1989
Page 11
CERTIFICATION
I hereby certify that all the work covered by this report was
carried out by myself and under roy direct supervision and that the
financial interest I hold in the property described is 3/4 of l* net
smelter return. I further certify that I have been engaged in
geophysical mineral exploration in Canada for most of the last 35
years as a geophysicist, contractor, and consulting engineer.
Former employment includes the positions of Senior Geophysicist -
Barringer Research, RexdaleJ Geophysicist - Derry, Michener 6 Booth,
Consulting Geologists; Geophysicist - Patino Mining Ltd.; and Staff
Geophysicist - Urangeselischaft Canada Ltd., and that of Self-
Employed Consulting Engineer in the periods 1970 to 1972, 1974 to
1982 and February 1984 to present.
May 30, 1989
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Black Tp
\L
Detail refers to the Ont Geological Survey study ofbackhoe samples of basal till for the Black-River Matheson (BRIM) area of Onl, norm of the Ja:pe[iDJLd aims
N -McCool Tp -
130
032^, *7TTX-
*1S2
- McCool Tp -
s-- Michaud T|
Michaud Porcupine Prspct'
1065
Guibord
- Cook Tp
Cook Tp'i ' i
-r-
Davidor | Mine ^ j-
BOURKES i
4 H-VI
4Asp.ersoh Claims
-Kimberlite fryke
Michaud Tp
. Barnet Tp . -i i li
OGS Backhoe Till Samples Black River - Matheson Project for the year* of 1984 and 1985 shovimg - - gold grain count.
?elb* - Melba Tp
Benoit Tp, 31
Maisonville.
Barnet Tp.- -
- MelbS
Bernhardt
Toburn Mine Sylvanite Mine *
FI6.
LocationJasperson Claims
Benoit Twp. ONTARIOapprox. 400 milesnorth of Torontoand half way between gold mines near the Porcupine Destor Fault, 12 miles north-west and the gold minesnear Kirkland lake, 12 miles south - east
Bisley
Kimberlite
.i:4 "M
Lebel Tpirris Kirkland Mine Kimberlit^yke
v v
VrigM Hargreaves Mine . l- Lakpshore Munc
Tech Hughes Mine Kirkland Lake Mine * *
Macassa M' rSvastika,l l t
'Kirkland Lake
Upper CaflWa" Mini
Data^aiven is the site " and the of grains, if any, no grains - no "
tx Cost (k Present Mines * Significant Prospects
Backhoe Till Sampling for Goldo 1984 Gold Grain Count
' * 1985 Gold Grain Count
TH - j. T1 l -Denoit lownship Larder Lake Mining Division
1989/01/23
'
Hwui••™ T*
| |" '
r Nos.
LI 041489 LI 059464 L1041490 L1041491 L884083 L884082 L992254 L992204 L884081 L992255 L992205 L884080
|
VI
V
H-
BOURKESm
Me J b a -Mine
f Jasperson
Claims I "
IIIl
IIBSIH
liBenoit Tp j l |6 .5 l 4.5 l
Miles
Kilometers
o 1.6 3.2 4.8 6.4
Jasperson Claims located 2 miles east of Highway l l half way between Kirkland Lake and Matheson in the Province of Ontario, 400 miles north of Toronto.
f l,
i-
Jasperson Claims: location of significant details.
Location of GEOHICS EM 16R resistivity anomaly interpreted as containing a possible sulphide (pyrite) or carbonatised zone under 20 meters of Abitibi clay.
Over all length is about 1000 meters having a vidth of 100 meters.
1 Mile
Easy access for men and machinery via a gently sloping trail on firm ground from the road to the trenches.
Location of trenches arid pits from BACKHOE LODGEMENT TILL sampling of (he UP-ICE side of outcrops seeking the GOLD GRAIN values south of the GEONICS ANOMALY.
Anomalous gold values are present. 12 of 18 of the of the samples exceed 9558 of the gold grain counts from 74 comparable lodgement (ill samples from the OGS BRIM project 1984- 1987.
Location of Ontario Geological Survey (OGS) Kirkland Lake Incentive Plan (KLIP) overburden drill hole 80-09: reverse circulation till sampling, 1980
4 —— l
Claim Numbers
[| Hole 80-09 produced unusualy high gold values over 11 feet with very
H little evidence of sorting suggesting a possible up ice source of under 2 miles.
LI 041489L1041490L884085L992204L992205
LI 059464 L1041491 L884082 L992254 L884Q81 L992255 L884080
TIU- F/G
Geophysics and Geology on Jasperson's Benoit Tp Claims, Nov. 1966 With Basal Till Trendies / ASTRO
NORMAL QUADRATURE
9:00 N
Gtonics Resistivity Anomelu
mctrrs•••••o too
E. F0 R ASS/^ys A^^ S6-M
GOLD GRfvttt COUNTGeophysics and Geology on Jasperson's Benoit Tp Claims, Nov. 1988
With B*isaJ Till Trenches
f Ut**.
1 ASTRO NORTH
Diabase dyk 992254
8:00 WAERIAL VLF
NORMAL QUADRATURE
9:00 NSt clay
100 ohm neters
Geonics EM 16R Resistivity Anomaly
fL 992255l
L 992204] l v -4-10 L-AERIAL VLF
REVERSE QUADRATURE
clay
4:00 N88-M~^ ^12 Chamber
#-^ ^shaft * adit It decline iCold Gram
L 9922051
""J^"**^** * v x
Nli :00 n
9.-OOK
Cetnlei EH 16K (tcflsUvllg Anemily;
TABLE CONCUtCIK-Afl OF RC OD DU 00-0'J
Non Mognctic Hcnvij PrncUon of Onsnl iiii
HO,000 ff)i told
I7,ooo tn
47'-SO' (11.5- IV.S rnj ij tpprexlmttclij tlic imounl a t t iny covering the Geonio IM l fi v. inomolg
Trout 27- l,. IK. I I. cenlfnuouxltj .tnitHi.il
1 IS': keltom c f h ot.- l..i
NORMALISED for (lie LODGEMENT (Dnttl) TILL limpid meinj the count in fold flrttnj per 10 grim) ef the IICAYY FRACTION ef CONCENTRATE.
Ellmlnitei the dUlorllAf effect *f virrylng imountt ef cUJ), In the iimplei, md maid them eempirible.
BACKGROUND fer BRIM vn .43 f r lin* if gold per timple (tiurce: JT Wird.
O!;.0
Hntnr in (icohtgicM Vittrvet) Keverye Circulation Ovcrlinrdcn Drill Hole " nn-09. Kirklintf Like Incentive
LEGEND. Note: Input Anomaly rating is rHnterpreUtion brJ.T. Ward using threshold o( 0.? division instead of 1.1 divisions.ftat is ustialr implored in base metal exploration, IS rears of experience has verified that 4 out l of the O J division threshold Input Anomalies are bedrock structure and alteration related.
li f. Wire the 0.2 dw threshold channel numbs increasingln strength from ] to 31-
o O Basal til backhoe ** trenches.
fsTI Normalised gold (rain count.
•^r
Ontario Miscellaneous Paper 110 Geological Survey, pgs 211 to 225
The Structure and Geological Development of the Porcupine Camp — A Re-Evaluation
C. l HODGSON
CJ. Hodgson Department of Geological Sciences, Queen's University, Kingston
Middle PrecombrlonOf ftok*
Rivtr Croup Ftbic Volconic Unit
Sidiminiory and Iniruiivi Rocki
Early PrecambrianMajor Granitoid Boditt
Major Eotl-Wttt Fault iOominonlly Ouortj-Frti
Ftltic Slockt
Yaungir Sttfimtntory end Volcanic Rockt
Kirkland Fouii tidiminti)
Old if Stdiminiary
X^V
r J Mining Camp
.. -. Show Oorni
Michaudl \nuuswe
John Jasperson's Benoit Twp. Group
Synclinorium
vvvvvvvvvvvvvvvvvv vvvvvvvvvvvvvvvvvvV
vvvvvvvvvvvvv yvvvvvvvvvv vvvvvvvvvvv
V V W V V Vvvv*
i*. Porcueint Desior Fouil
Kirklond Loke Comp
Figure 2. Geology of the Timmins-Kirkland Lake area (Irom Hodgson 1982 alter Pyke e( al. 1 973).
OVERBURDEN DRILLING MANAGEMENT LIMITED 107-15 CAPEL.L.A COURT, NEPEAN, ONTARIO, K2E 7X1
T e L-EF-W O M El < A l 3! ) SS3!*.— J TV l X t TT A
FAX MO l
D A i A T R A N S M I T T A L REPORT
DATEs
CLIENT:
ATTENTION:
2S~Oct-88
John Ward 9 Willamere Drive Scarborough, Ontario M1M 1W5
PROJECT!
FILE NO:
WARD
WARD10CT.WRI
A3 to A10
NO. OF SAMPLES:
NO. OF PANNIN6S:
HEAVY MINERAL CONCENTRATES:
sent to Analytical Lab
are included in this shipment
REMARKS:
/ion -mag.
Duane Parnham Laboratory Nanaqer
SAMPLE FRACTION DESCRIPTIONS
1. Overburden Geochem - Standard soil envelope. Representative .whole sample split of original overburden sample received by our laboratory. We recommend you store the geochems indefinitely.
2. Overburden +10 - 10" x 14" plastic bag containing all + 10 mesh pebbles and cuttings; suitable for binocular pebble counts. The overburden +10 is retained by some clients and discarded by others.
3. Overburden -10 - 10" x 14" plastic reject. Normally discarded.
*- Overburden Li g h. t. s - Kraft paper bag. 3.3) float reject or shaking table mid-density minerals that may be diamonds, industrial minerals, etc. the Lights indefinitely.
bag of shaking table
Methylene iodide (S. G. preconcentrate J contains useful indicators for We recommend you store
5. Overburden Mag - Plastic vial in compartment in cardboard vial box, adjacent to corresponding 1/4 H split. Heavy magnetic split (magnetite and drill steel of methylene iodide sink concentrates.) We recommend you store the mag indefinitely. 3' Over burden 1/4 H - Plastic
vial box . methylene ana lysis retained
vial in compartment in cardboard 1/4 split or heavy non-magnetic poration or iodide sink concentrate. - (Note: Where check or part of the 1/4 split has been required. the split is marked 1/8 or 1/16 H.) We recommend youstore the 1/4 split indefinitely.
7. Overburden 3/4 H - plastic vial with 3/4 split of non-magnetic portion of heavy mineral concentrate. Submitted to independent analytical laboratory. pulped and analysed. Surplus pulp, if any, is stored by analytical laboratory.8. Bedrock +10 - Kraft paper bag. Plus 10-mesh (Tyler) chip . sample split of 'bedrock sample, for binocular examination. We -recommend H.he Bedrock +10 be stored indefinitely.9. Bedrock Oversize - 10" x 14" plastic bag of surplus bedrock whole sample remaining after separation of Bedrock Geochem and Bedrock +10 splits, normally discarded.
DVEREURDEN DRILLING MANAGEMENT LIM.TED
COURT, N EPEAN. C NTAR|a K 2107-,.
SAMPLE PROCESSING FLOW SHEET
± 250g STORE
STORE
Lisrht Fraction STORE
. C.- W W
Bulk . Samnl e
8 - 10 kg
Shaking Table Gold Grain Count
PanningGold Grain Count
(selected samples)
Heavy Liquid Separation (Methylene Iodide SG 3.'
Marnetic Fractioni
Magnetic Separation
lA STORE Split
l3A Ship to
Ar.aly~ical Laboratory
'i^ra 4 - sampla Proceasir* Flow Shaat
IsNU
MBE
R A
SSIG
NED
TO
SAM
PLE
IN T
HE F
IELD
| if
Wei
g'ht
' of'
f he
wfib
lV*
sam
ple"
as "
rece
ived
" fr
om"
the
"fie
ld",
' "le
ss "
a "25
0" g
ram
" "
" "l
" "
'J, ^
" "
" f*
repre
senta
tive
spli
t,
(geo
chem
) |
~i P
Qm
""^
Weight of sample greater
than 10 mesh
,. J
i i
I Tt J*
S R
Dry
weight of h
eavy m
ineral cone,
recovered
from shaking
table
l g;*
l 21 CO
" K
Weight of light fraction (less
than 3.32 specific gravity) from H
eavy
r" ~
S
Liquid Separation of table concentrate
*-
**
"^
"
VB B W
**
*K
WB
H
V*
A*,
H.K
Ma.
V*.
O.V
M*
Vfl.
W
H
H
MK
**
AW
~" '
Wei
ght
of h
eavy
min
eral
fra
ctio
n (
gre
ater
tha
n 3.
32 s
pec
ific
gra
vity
) l
s i
! f
from
Hea
vy .L
iqui
d^Se
p.ar
atip
n. 9
X.ta
bXe
.con
cent
rate
.. .... ..,.,. ..............
,... .
.L...
^ "
**
"W
eigh
t of
Non
-Mag
netic
fra
ctio
n o
f H
eavy
Min
eral
Con
cent
rate
l
Pi
o i
Wei
ght
of M
agne
tic
frac
tion o
f H
eavy
Min
eral
C
once
ntra
te
T 5
- "
E l
J O
^
3C
Num
ber
of V
isib
le G
old
Gra
ins
from
the
sha
king
tab
le a
nd p
anni
ng
IS
--
sp
Cal
cula
ted
PPB
valu
e ba
sed
on t
he V
isib
le G
old
^ K
5 "*
Cla
s"si
Trc
afi6
n"o"
f "tK
e"-f
l6"
clas
t"s'
izeV
Cob
bles
,Peb
bles
", o
'r'G
rant
lieV
"
" "
"" "f
" ""
-_
^^
^ ^^
-
, _
--
^.^
^-
—-i
- ^^
_
^^
__
^^
^-
^.^
. -
—-.
- ^.
^ -
_
- _
--
—-
_ ^
-.-
. —
-. —
^ ^
^^
_
-^
^^
.^
^—
^^
^^
^^ 1
^^
—^
fcj
Cla
st p
erce
ntag
es o
f V
olca
nic/
sedi
men
tary
, G
ranit
ic a
nd L
imes
tone
^ **
**
S5
w*
xy
l Presence of other material, refer
to footnotes
l Sorted or U
nsorted
dejBcription of Matrix
^| ^
"
~ Presence of s
and
in T
ill, or size of s
and grains in G
ravel
or. Sand
|
j|f" "Presence" of" silt" ~ " "
" "" "
" ~~ ^ ~ ,
[ " 7 "
" "
" "" 7
~~
I "J.
" " "
"" "
I"
" " Il~ Z 3
l" ""Presence* of^clay" ~ ~ ~ ~ "
* ~
~ " ~ ~ " ~ " ~
~ " - " ~ ~ ~ " ~ "
" ~ ~ " ~
**j~ ~ g
l Colour of
sand m
atrix.
^ ^
^
^\ ? S
5
L. .
.c.?l o
u.r. ?.:f
..c.layMi
natrix^
.
. ^
^
^^
- -^ ^ -
- ^
-,. ^
.. ^
.... ^ ,
. ,.,. .
.I.. ? l T
CLASSIFICATION OF S
AMPLE, ie.
Till,
Sand,
Gravel
' K
OVERBURDEN DRILLING MANAGEMENT LIMITED - LABORATORY SAMPLE LOG
ABBREVIATIONS
DATA LOG
Clast:
Size of Clast: G: Granules P: Pebbles C: Cobbles BL: Boulder Chips BK: Bedrock Chips
t Clast CoiDosition: V/S: Volcanics and Sedinents GR: Granitics LS: tilestone OT: Other Lithologies
(Refer to Footnotes Below l TR: Only Trace Present NA NOT APPLICABLE
HatriiiS/U: Sorted or UnsortedSD: SandST: SiltCY: Clay
Y: N:
Yes Fraction Present Fraction Not Present
F: FineM: He d i ut:C: Coarse
Colour;B: Beige6Y: GreyGB: Grey BeigeGN: Green66: Grey GreenBN: BrownBK: BlackOC: OchrePK: PinkOE: Orange
Class
BID: BDK;
Boulder Chios Bedrock Chios
GOLD LOG
Nuiber of Grains;
Thickness:
T: Nuiber Found on Shaking Table P: Number Found After Panning
C: Calculated Thickness of Grain M: Actual Measured Thickness of Grain
Footnotes:
A: Gritty Clay Lumps Present
B: Siooth Clay LUIPS Present
C: Organics Present
D: Oxidized
PAGE l J. WARD 10/25/88
Nardf|p*rl OVERBURDEN DRILLING MANAGEMENT LIHITED TOTAL l OF SAMPLES IN THIS REPORT s 7
LABORATORY SAMPLE LOGi
SAMPLE WEIGHT (KG.WET) WEIGHT (6RAMS DRY) AU DESCRIPTION CLASSNO, B8SSX3XS3SSSSSSSSZ SSSSCSSSXSSSXSSSSSSSSSSSSZSSSZZ S3XSESSSSES BSSSXESBXBXEEX888XBXBEXB8BX88X83XXX38S8E8 BXXX888888
M. I. CONC CLAST MATRIXXSSSSE5ES8ESXB8X BBB8XSBBBBBXBBBB8BB 8X888*8*88888888*88*8
TABLE +10 TABLE TABLE H.I. CONC. NON NO. CALC SIZE l S/U SD ST CY COLORSPLIT CHIPS FEED CONC. LIGHTS TOTAL HAG MAG V.6, PPB xsssBrBssxBSBSB ******
V/S6R LS OT SD CY
HARDA3A4ASA6A7
A8-9AiO
9.98.3B, 89,49.28.46.8
3.01.10.71.50.80.71.0
6.97.28.17.96.47.77.8
103.0140.9115.096.1138.9102.4115.0
81.8118.791.771.0106.773.594.8
21.222.223.327.132.228.920.2
14.816.017.621.023.821.215.2
6.46.25.76.18.47.75.0
813
114846
3966235
17914533035
CPPpFPp
95305090908070
5705010102030
NAmNANANANANA
CCCCccc
uuuuuuu
YYYYYYY
YYYYYYY
YYYYYYY
8BBBBBB
BBBBBBB
TILLTILLTILLTILLTILLTILLTILL
PAGE l J. WARD 10/25/88
GOLD
VISIBLE GOLD FROM SHAKING TABLE AND PANNIN6
NUMBER OF GRAINSNirdloct.NrlT01AL l OF PANNINGS 7 —.—.......——————..——....
ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.SAMPLE l PANNED ~ssss*s r*SS8BSSS *:*.*s.e c**.. HAG ASSAY
Y/N DIAMETER THICKNESS T f T P T F' 6MS PPB REMARKS
HARD A3
A4 Y
A5 Y
A6 Y
A7 Y
A8-9 Y
A10 Y
25 X25X50 X100 X125 X
25
50100150
25 X 50
25 X25 X50 X50 X50X75 X
25 X25 X50 X75 X75 X
50 X50 X
. 75 X125 X
25505075
10075
2550
100100125
5075
11*5
175
25 X 25
5 C8 C10 C20 C27 C
e c
5 C 8C 10 C 13 C 15 C 15 C
5C8C15 C18 C20 C
10 C 13 C 20 C 29 C
s c i
25 X25 X25 X50 X50 X75 X150 X
255075507575200
5 C 1e c i i10 L 110 C 1 113 C i15 C 134 C 1
31211
8 14.8
4"fi.
12211
13 16.0
1
1 17.6
224411
14 21.0
23111
8 23.6
11l1
396
623
5
179
145
NO SULPHIDES
4 21.2
3
NO SULPHIDES
NO SULPHIDES
NO SULPHIDES
NO SULPHIDES
NO SULPHIDES
330
NO SULPHIDES
PAGE? J. WARD 10/25/88
fioJRtSSIFICATIONKCBSCBXCBBUSCSrZXE
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
NUMBER OF GRAINSMArdloct.MriTOTAL t OF PANNIN6S 7 ~~—...~——........————-.
ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.SAMPLE l PANNED rsssrsrs ssassessr sssssxcs rccrs HAG ASSAY
Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS
HARD25 X 50 50 X 50
8C IOC
6 15.2 35
OVERBURDEN DRILLING MANAGEMENT LIMITED 107-15 CAPELLA COURT, NEPEAN, ONTARIO, K2E 7X1
TELEPHONE: (613) 226-1771/1774 PAX NO: (611) 226-S7S3
DATA TRANSMITTAL R E P .0 R T
DATE:
CLIENT:
ATTENTION:
13-Dec-88
Mr. J. Ward
9 Willamere Dr. Scarborough, Ontario HIM 1W5
PROJECT:
FILE NO:
WARD
UIARD1DEC.WRI
88-05 to 88-21
NO. OF SAMPLES:
NO. OF PANNINGS:
9
9
HEAVY MINERAL CONCENTRATES:
_______ sent to Analytical Lab
REMARKS:
are included in this shipment mag .non-mag.
Duane Parnham Laboratory Manager
JOHN UARD 12/13/88
COLD CLASSIFICATIONIisizzzzzzzz::zz::z
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
NUMBER OF GRAINSUARD1DEC.UR1TOTAL l OF PANNINGS 9
ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.SAHPLE l PANNED rzrzsin zzzzzzzzz zzzzzzzz zzzzz MAG ASSAY
V/N DIAMETER THICKNESS T P T P T P GfIS PPB REMARKS
UARD 88-05
88-12 V
8-13
88-14 Y
88-15 Y
88-17
88-18,19
25 X25 X50 X50 X75 X
100 X
25 X25 X75 X75 X
100 X200 X
25 X25 X50 X50 X50 X75 X75 X
25 X25 X
150 X
50 X50 X75 X75 X
255050100100125
255075
100125275
25505075
10075
100
2550
200
507575
125
5 C8 C10 C15 C18 C22 C
5 C8 C
15 C18 C22 C44 C
5 C8 C
10 C13 C15 C15 C18 C
5 C8 C
100 C
10 C13 C15 C20 C
1
1
1
21
NO VISIBLE GOLD
25 X25 X
2550
5 C8 C
NO SULPHIDESGOLD SEPARATED INTO 3 VIALS ONE GRAIN CHROME DIOPSIDE
(500 MICRONS)
13 17.0
12 l l l l
286
NO SULPHIDESGOLD SEPARATED INTO VIALS
7 18.7
l1212 l l
1213
EST. 1000 HARCASITE PELLETS GOLD SEPARATED INTO VIALS
9 31.4
2 5 l
121
NO SULPHIDESGOLD SEPARATED INTO VIAL
8 24.6
33ll
952
NO SULPHIDESGOLD SEPARATED INTO VIAL
8 34.6 111
NO SULPHIDES
NO SULPHIDESGOLD SEPARATED INTO VIALS
2 18.9
TA6E i JOHN UARD 12/13/88
OVERBURDEN DRILLING MANAGEMENT LIKITEDTOTAL l Or SAMPLES IN THIS REPORT z 9
LABORATORY SAMPLE LOGf
SAMPLE HEIGHT (KG.UET) WEIGHT [GRAMS DRY) AU DESCRIPTION CLASSNO. xzzzz::zzzzzzzz:zz zzzzzz:zzzzzzzzzzzzzzzz:zzzzzzz :::zzzzzzz: zzzzzzzzzzzzzzzzzzzzzzzzszxzzzzzzxxxzxxzx c::z:z::i:
fi. I. CONC CLAST MATRIXzzzzzz::zz:zzzzz zzzztzzzzzzzzzzxzxz zzzzxzzzzzzzzzxzzzzzz
TABLE *10 TABLE TABLE B. I. CONC. NON NO. CALC SIZE * S/U SD ST CY COLORSPLIT CHIPS FEED CONC LIGHTS TOTAL HAG HAG V.G. PP6 zzzzzizzzxxzizz xzzzzz
V/S GR LS OT SD CY
UARD88-0588-1288-1388-1488-1568-17
88-18,1988-2088-21
8.76.09.78.98.57.410.05.77.2
0.50.50.01.20.50.60.70.40.5
8.25.59.77.78.06.89.35.36.7
218.1143.9189.2194.3217.9322.2327.6167.5172.4
192.9119.2157.3162.2172.1293.7303.0144,0165.1
25.224.731.932.145.828.524.623.57.3
17.018.731.424.634.620.618.919.56.6
8.26.00.57.511.27.95.74.00.7
1379880252
2861213121952111NA6
7060
PPTRPPPPPP
6060NA706060706050
40iONA3040to304050
NANANANANANANANANA
NACNACCNANANANA
UUSUUUUUU
YYnYYYYYY
YYYYYYYYY
Y.YYYYYYYY
6Y686YBB8BB6
6YBB6YBB8BBB
TILLTILLSANDTILLTILLTILLTILLTILLTILL
PACE 2 JOHN WARD 12/13/8
CLASSIFICATION
VISIBLE GOLD FROM SHAKING TABLE AND PANNING
NUMBER OF GRAINSUARD1DEC.UR1TOTAL l OF PANNINGS 9 —-——--——~————...
ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.SAflPLE t PANNED sinszrs i:n:rit: tzz::::: rnz: HAG ASSAY
Y/N DIAMETER THICKNESS T P T P I P 6MS PPB REMARKS
HARD
B-20 Y 25 X 5050 X 5050 X 7550 X 100
8 C10 C13 C15 C
1111
88-21 25 X50 X
2575
5 C 13 C
5 19.5
NO SULPHIDESGOLD SEPARATED INTO VIALS
70
NO SULPHIDESCOLD SEPARATED INTO VIALS
2 6.6 60
PETROGRAPHIC DESCRIPTIONS
Submitted by: Geopiastech, Inc, Petrography by: Barbara Murck
Client: John Ward
Locality- Project:
Date Completed: Oct. 5, 1988
436-278-9696 416-828-5416
BARBARA W MURCK PhB Geologist
37 MiaslssaugardS. MisaOnt. L5H-2H3 Canada
J
PETROGRAPHIC DESCRIPTION
SAMPLE No. WB-87-01-1/4 (heavy mineral separate (3.0 split) ft grain mount thin section)
COMMENTS
The following list comprises the minerals that I was able to identify in this grain mount by optical techniques alone. The percentages are very approximate; it is difficult to make a visual estimate of modal percentages when a certain amount of matrix (i.e. epoxy) is present, and a point-count would be preferred. It would also be helpful to have polished thin sections, for two reasons: (1) optical identification of opaque phases; and (2) access to microprobe or S.E.M. analyses if optical identification is uncertain. Finally, it would be helpful to have an idea of the nature of the source rock for this material.
Some notes on the mineralogy: There is a mineral with moderate pleochroism from pinkish-orange to green, which I have included with the orthopyroxenes (see below), but I am not sure if all of this material is the same mineral (the pleochroism in some grains is probably too strong for an orthopyroxene). Two minerals which I did not find (surprisingly?) were tourmaline and apatite, in spite of looking specifically for them.
MINERALOGY
Garnet: clear, very pale pink, occasionally with minor very fine inclusions of quartz.
Opaques: some grains have rims of leucoxene and/or very fine chloritic material; opaque grains also occasionally occur as very fine inclusions in amphibole grains; minor hematite (translucent red).
Amphiboles: there appear to be at least three amphiboles present: (1) a moderately pleochroic, "forest" green variety, probably hornblende; (2) a strongly coloured, blue-green amphibole, probably an alkalic variety; and (3) a green fibrous variety, most common in lithic fragments and 'altering pyroxene grains, probably actinolite.
•"1056 Pyroxenes: orthopyroxene (hypersthene-enstatite) with pale pinkish pleochroism and parallel extinction in prismatic sections; pale green clinopyroxene, often altered to fibrous amphibole.
Epidote: typical, almost "neon" yellowish-green
pleochroism and high, patchy to slightly anomalous interference colours.
•*b\ Ldthic k Polycrystalline Fragments: none of thefragments is large enough to get a textural description or rock type; varieties include quartz * garnet ± opaque; fibrous amphibole ± pyroxene; epidote Polycrystalline clasts.
"*2-3?6 Sphene: rhomb-shaped grains with very high birefringence.
•s'2-3% Zircon: uniaxial positive; some euhedral, prismatic grains, strongly zoned.
0*2-3/6 Quartz: most commonly attached to other grains or as inclusions, but occasional free grains of quartz are also present.
Ace. Feldspar: plagioclase, with lamellar twinning; no alkali feldspar was identified.
Tr. Rutile.
PETROGRAPHIC DESCRIPTIONSAMPLE No. WB-87-02-1/4 (heavy mineral separate (3.0 split)
k grain mount thin section)
COMMENTS
Same as above. Mineral proportions are slightly different in this sample.
MINERALOGY
Garnet: as above.
Pyroxenes: clinopyroxene (probably augite) is dominant; colourless or very pale green, with exsolution blebs and lamellae; orthopyroxene as above.
Opaques: as above.
Epidote: as above; polycrystalline fragments dominated by very fine-grained epidote are also common.
Amphiboles: as above.
*5S6 Lithic Si Polycrystalline Fragments: mainly epidote- dominated, with and without amphibole; at least one very fine-grained quartzofeldspathic fragment, and one amphibole * chlorite fragment.
'*2-3% Zircon.
•*2-3?6 Sphene.
Ace. Quartz.
Ace. Feldspar.
Tr. Rutile.
Bruce Jago Petrographic Services 1517 -35 Charles Street, West, Toronto, Ontario, M4Y 1R6
May 12, 1989
John Jasperson 18 Byron Street, Stouffville, Ontario, L4A 7X3
Dear John,
Please find attached the report you and John Ward commissioned on rock samples and heavy mineral concentrates from your Kirkland Lake area overburden sampling program.Thin section and rock sample analysis of rock debris from one of your overburden pits revealed a mixture of metasedimentary and metavolcanic lithologies, all of greater than Proterozoic age and of greenschist facies metamorphic grade. All of the samples examined with the exception of JJ - l, a feldspar - phyric andesite and JJ - 2, a fine grained diabase are substantially carbonatized, sericitized and/or epidotized and exhibit structures characteristic of both brittle and ductile deformation. Unfortunately, there is no sulphide or precious metal mineralization in these samples with the exception of minor pyrite. The single polished thin section is from a narrow quartz vein. The mineralogy is dominated by highly strained quartz with minor sericite, chlorite and carbonate and lesser pyrite with trace amounts of sphalerite and chalcopyrite, both as inclusions in pyrite. Microfractures and microbreccias are oriented parallel to the vein contact and are sericite -H/- carbonate rich.A total of 188 mineral grains from the two heavy mineral samples were examined with the binocular and Scanning Electron Microscope. The results of the analysis are given in Table 1. The heavy mineral concentrates from both Samples 'A' and 'B 1 are similar mineralogical although in detail there are substantial differences. These are noted in the body of the report. In general, the mineralogy is characteristic of samples derived from Archean metamorphic and metavolcanic terrains and dominated by clino - and orthopyroxene, amphibole, epidote, garnet (almandine - spessartine - andradite), ilmenite (both magnetic and non magnetic) and pyrite, either as single grains or more commonly intergrown with quartz, plagioclase and amphibole and possibly sericitic (K - rich) or phengitic (Na - rich) micas. None of the pyrite is auriferous or argentiferous within the detection limits of the SEM nor does it contain any inclusion of native gold. Two grain aggregates containing Cu, Zn and Fe - bearing sulphides were found. The presence of clino - and orthopyroxene suggests that a mafic igneous body such as a gabbro or alkalic complex may be a major regional lithology. Although not apparent from
Table l, epidote also is very abundant in both samples. This mineral is characteristic of the transition from greenschist facies to lower amphibolite facies metamorphism and also of some types of hydrothermal alteration. Epidote alteration is strongly developed in several of the highly altered rock samples that were examined and it is possible that strongly epidotized lithologies may be present locally.
I hope that this report meets with your satisfaction and that you will not hesistate to discuss any aspect of it with me at our mutual convenience.
Bruce Jago, H.B.Se.,M.Se. Consulting Petrologist
If
Sample Number:John Jasperson l
Rock Name:Intensely K - metasomatized granodiorite to granite
Rock Description:
The rock is sub - angular to subrounded, pinkish weathering in colour and massive to weakly foliated. Surface pits are roughly cube shaped and probably reflect the weathering from the sample of pyrite (l ife) which is present locally as cubes up to 1.5 mm on fresh broken surfaces and in narrow fractures. The mineralogy of the sample is dominated by strongly fractured to fresh, reddish alkali - feldspar as large zoned porphyroblasts and as a finer grained matrix component and irregular patches of smokey - grey coloured quartz. The sample is traversed by relatively rare, narrow ( < 2 - 3mm wide) quartz +/- pyrite and quartz - carbonate +/- pyrite veins.
Thin Section Description:
In thin section, the sample is dominated by highly included and strongly exsolved orthoclase porphyroblasts and a matrix dominated by sodic plagioclase, orthoclase and quartz with accessory microcline, zircon, apatite and biotite and secondary chlorite, sericite, pyrite, goethite and trace carbonate. The orthoclase porpyroblasts are compositionally zoned to more potassic margins, strongly exsolved with intense perthite develop - ment and contain large, matrix sized inclusion of plagioclase and quartz. The primary minerals in the matrix are dominated by relatively coarse grained, highly strained and weakly sausseri- tized anhedral plagioclase, relatively fresh and coarse grained anhedral microcline, fine grained strongly inequigranular, anhedral, highly strained quartz, coarse grained, irregular pat ches of quartz grains and trace amounts of interstitial sub- prismatic apatite and anhedral zircon and biotite. The secondary minerals include very coarse grained orthoclase porphyroblasts, partial microcline pseudomorph^ after plagiocalse, anhedral to euhedral pyrite, fine grained, interstitial porphyroblastic chlorite and weakly developed sausserite (sericite, epidote, carbonate) and chlorite alteration after plagioclase and to a lesser extent orthoclase. Goethite is developed along mortar- textured grain boundaries.
Minerals Present Percent Abundance Status
Orthoclase 30-35 Primary/SecondaryPlagioclase 30 - 35 PrimaryMicrocline 3 - 5 (?) Primary/SecondaryQuartz 25 - 30 PrimaryApatite Trace PrimaryZircon Trace PrimaryBiotite Trace PrimaryGoethite < l SecondaryCalcite Trace Secondary
Sample Number:John Jasperson 2
Rock Name:Quartz - feldspar Porphyry
Rock Description:
This sample is a strongly carbonatized and sausseritized quartz - feldspar porphyry of probable sub - felsic to felsic, sub - volcanic to volcanic origin. The rock is massive, light brown weathering and sub - round ellipsoidal in shape. There is no pyrite visible and the brown weathering nature may be ascribed to the oxidation of matrix magnetite or very fine grained pyrite. The rock reacts weakly with 5 % hydrochloric acid.
Thin Section Description:
In thin section, the sample is a strongly carbonatized, moderately sericitized and sausseritized and weakly chloritized, quartz - feldspar, glomeroporphyritc sub - felsic porphyry. The primary phenocryst mineralogy is dominated by strongly carbonatized and sausseritized glomeroporphyritic aggregates of orthoclase and plagioclase, lesser strongly resorbed, weakly strained and fractured quartz, prismatic microphenocrysts of apatite and wholly chloritized and oxidized, round to oval phenocrysts of unknown, but probable mafic silicate origin. The matrix is dominated by medium grained, strongly poikiloblastic carbonate intergrown with very fine grained, anhedral sericite, chlorite and possible epidote and anhedral, strongly interlocking quartz and possibly wholly pseudomorphed feldspar. Sericite is strongly developed in fine grained fractures associated with a spaced, weakly to moderately developed foliation. The opaque mineralogy comprises fine to very fine grained anhedral magnetite (?) and relatively coarser grained anhedral to euhedral pyrite.
Minerals Present Percent Abundance Status
Phenocrysts 35-40
Orthoclase/Plagioclase 35 - 37 Primary Quartz 2-3 Primary
Matrix 60-65
Quartz 15-20 PrimaryApatite Trace PrimaryCarbonate 15 - 20 SecondarySericite 10 - 15 SecondarySausserite 10 - 15 (?) SecondaryChlorite 3-5 SecondaryMagnetite 1-2 Secondary (?)Pyrite < l Secondary
Sample Number:John Jasperson 3
Rock Name:Weakly foliated, pyrite - bearing quartz vein
Rock Description:
This rock is a weakly to moderately foliated, pyrite- bearing quartz - vein. Quartz is the dominant primary mineral with trace to accessory pyrite as subhedral cubes to 3 mm. The secondary minerals have been introduced along fractures which are strongly developed parallel to the vein contacts. Fracture mineralogy is dominated by sericite with lesser chlorite, apatite, pyrite, magnetite (?) and trace carbonate. The sample reacts only weakly with 5 % hydrochloric acid.
Thin Section Description:
In thin section, the sample is dominated by highly strained, very coarse grained quartz and lesser secondary, fractured related sericite, chlorite, apatite, pyrite and trace carbonate. Quartz has developed very strong deformation banding both sub- parallel to and at a high angle to the vein contacts. Very fine grained opaque minerals are arranged in a linear fashion at 90 degrees or at a high angle to the orientation of the deformation banding. Where deformation bands have developed into fractures they invariably parallel vein contacts and may form irregular lensoid zones of quartz - sericite - rich microbreccia.
The opaque mineralogy is dominated by pyrite with accessory magnetite (?), goethite/limonite and trace amounts of sphalerite and chalcopyrite. Pyrite occurs as anhedral to subhedral, strongly fractured and deformed grains up to 4 mm across and may contain tiny inclusions of quartz, very tiny inclusions of euhedral sphalerite and very tiny, fracture related chalcopyrite. Some of the pyrite which is not obviously associated with sericitic fractures may be primary. There is no native gold in this sample.
Minerals Present Percent Abundance Status
Quartz 87 - 90 PrimarySericite 5-8 SecondaryChlorite Trace - l SecondaryCarbonate Trace SecondaryPyrite 3-5 Secondary (?)Chalcopyrite Trace SecondarySphalerite Trace SecondaryMagnetite/Goethite/Limonite 2-3 Secondary
Sample Number:John Jasperson 4
Rock Name:Intensely altered glomeroporphyritic intermediate metavolcanic
Rock Description:
This angular rock sample is a brown weathering, weakly to moderately foliated, very strongly oxidized and weathered, pyritiferous, intermediate (?) metavolcanic of extrusive origin. The sample is traversed by several narrow ( < 3 mm wide) quartz- carbonate - pyrite veins and reacts weakly to moderately with five percent hydrochloric acid. The brown weathering rind on the sample'is 2 - 3 cm thick.
Thin Section Description:
In thin section, the sample is an intensely carbonatized, weakly sericitized, glomeroporphyritic metavolcanic rock of probable intermediate, sub - volcanic to extrusive origin. Relict plagioclase (?) phenocrysts are very abundant but wholly pseudomorphed by sericite - carbonate and carbonate - epidote (?) assemblages. Probable relic mafic phenocrysts have been wholly pseudomorphed by opaque - carbonate - ??? assemblages. The primary mineralogy of the matrix is indeterminable due to the extreme nature of the carbonate metasomatism. Sericite is locally, but rarely developed as anhedral, fine grained porphyroblasts. The remainder of the matrix is composed of anhedral quartz strongly intergrown with poikiloblastic carbonate. The thin section is traversed by two narrow, barren, quartz - carbonate veins. One vein is dominated by very coarse grained carbonate and the other by quartz. Limonite/goethite is developed as a weathering product along carbonate grain boundaries.
The carbonate mineralogy probably is dominated by ferro- carbonate.
Minerals Present Percent Abundance Status
Phenocrysts 20 - 25
Feldspar 13 - 15 Primary Mafic silicate (?) 10-12 Primary
Matrix 75 - 80
Carbonate 40-45 SecondaryQuartz 8 - 10 (?) Primary/SecondarySericite 15 - 20 SecondaryLimonite/Goethite 5-10 Secondary
Sample Number:John Jasperson 5
Rock Name:Fractured and hydrothermally altered chert
Rock Description:
This angular to weakly sub - angular rock sample is a strongly fractured and weakly foliated white weathering chert. Fractures up to 3 mm across are developed in an orthogonal pattern. The intersection of the larger fractures results in the formation of locallized breccia zones. The fractures are barren of visible sulphide mineralization but do contain calcite and probably some sericite. Localized hydrothermal activity is suggested by the calcite - sericite assemblage.
Thin Section Description:
No thin section provided for description.
Sample Number:John Jasperson 6
Rock Name:Intensely fractured and silicified/carbonatized hydrothermal breccia
Rock Description:
This very angular and slightly rusty weathering rock sample is an intensely fractured and altered hydrothermal breccia. Due to the intensity of alteration it is not possible to accurately determine the protolith, however, it may have been an intermediate to felsic metavolcanic or a ferroan chert. There are at least two and possibly three hydrothermal events that have affected this sample. The development of a reddish coloured quartz vein marks the first stage hydrothermal activity. This is transected by a very complex web of quartz and quartz - carbonate veins which impart a intensely brecciated appearance to the rock. Many of these fractures are sigmoidal suggesting an origin by shear. This type of deformation is apparent in most of the quartz stockworks in the Kirkland Lake gold camp. The last stage hydrothermal activity deposited minor pyrite mineralization in very narrow ( < 1mm wide) chlorite - sericite - pyrite veinletes which transects the sigmoidal veins at a high angle.
Thin Section Description:
No thin section provided for description.
Sample Number:John Jasperson 7
Rock Name:Calcite - epidote metatactite (?) (metaskarn)
Rock Description
This angular, light green - white weathering rock sample most probably is a calcite - epidote metatactite (metaskarn). The sample is strongly deformed with a locally developed intensely folded internal rock fabric and a well developed spaced rock cleavage. Due to the intensity of deformation, the protolith can not be determined with any degree of confidence.
Thin Section Description:
No thin section provided for description.
Sample Number:John Jasperson 8
Rock Name:Strongly deformed and intensely carbonatized and epidotized intermediate metavolcanic
Rock Description:
This angular and light green weathering rock sample is a strongly deformed, pervasively carbonatized and locally carbonatized and epidotized, intermediate metavolcanic. The sample has suffered intense ductile deformation resulting in the formation of a 6 - 7 cm wide zone of strongly folded and brecciated calcite and calcite - epidote injection veins. Despite the intensely altered nature of the sample, it is barren of any sulphide mineralization.
Thin Section Description:
No thin section provided for description.
Sample Number:JJ - l
Rock Name:Feldspar - phyric andesite
Rock Description:
This sample is a plagioclase glomeroporphyric andesite. The handspecimen is angular, weakly foliated and quite fresh with the exception of a narrow ( < 3 mm thick), slightly bleached weathering rind. The sample is white weathering, traversed by very narrow ( < l mm wide) calcitic fractures and does not appear to contain any sulphide mineralization.
Thin Section Description:
In thin section, the sample is dominated by glomero porphyritic aggregates of intensely sausseritized, weakly resorbed feldspar and recrystallized quartz and a very fine grained, structurally isotropic matrix composed of quenched textured, partially sausseritized and carbonatized plagioclase and/or pyroxene and stubby to sub - prismatic weakly sausserit ized and carbonatized plagioclase and apatite. The portions of the matrix interstitial to the stubby and quench textured silicate minerals may be devitrified and wholly sausseritized and carboantized volcanic glass and comprise epidote, sericite, carbonate and quartz. Irregular to sub - round quartz - chlorite assemblages are irregularly distributed throughout the sample and may be relict amygdules. Several narrow ( < l - 2 mm wide) sericite, sericite - quartz and quartz - carbonate veinletes traverse the sample. These are barren of any sulphide mineralization and appear to be associated with the silicification of several feldspar phenocrysts.
Minerals Present Percent Abundance Status
Phenocrysts 12 - 15
Quartz/Feldspar 12 - 15 Primary
Matrix 85 - 88
Quartz 20 - 25 Primary/SecondaryPlagioclase 20 - 25 PrimaryApatite Trace - l PrimaryCarbonate 10 - 12 SecondarySericite 15 - 20 (?) SecondaryEpidote 15 - 20 (?) Secondary
Sample Number:JJ - 2
Rock Name:Rusty weathering, very fine grained diabaseRock Description:
This rock is a rusty weathering/ very fine grained/ weakly foliated to massive/ equigranular diabase. The sample contains a trace of pyrite and does not react with 5 % hydrochloric acid.Thin Section Description:
In thin sectin the rock is a sub - ophitic textured, amphibolitized quartz diabase. The mineralogy is dominated by stubby prismatic to prismatic/ weakly to moderately sausseritized plagioclase, wholly amphibolitized augite/ anhedral/ interstitial quartz and single and multi - grain aggregates of opaque. The latter is dominated by fresh subhedral to euhedral magnetite with lesser anhedral pyrite. Pyrite is associated with rare, narrow ( < 1mm wide), quartz - bearing fractures.
Minerals Present Percent Abundance StatusPlagioclase 40-45 SecondaryAmphibole (Augite) 35-40 SecondaryQuartz 3-5 Primary/SecondaryMagnetite 3-5 PrimaryPyrite Trace - l SecondarySausserite 5-8 Secondary
Analysis of Heavy Mineral ConcentratesTwo samples of heavy mineral separates were examined as part
of this study. All of the mineral grains were examined under 40 x magnification with a binocular microscope and selected grains were examined with an oil immersion mount ( n - 1.570 ). A brief description of each sample is given below and is followed by photographs of selected grains. -
A - The silicate mineral assemblage in this sample is dominated by light to dark green/ angular to sub - rounded/ equant to sub- prismatic and prismatic clino - and orthopyroxene/ amphibole and epidote and angular to highly rounded/ medium brown to light pink garnet with subordinate dark brown sphene and clear glassy to white quartz. The sulphide assemblage includes only pyrite which occurs as single broken grains/ as subhedral to euhedral cubes and anhedral grains intergrown with chlorite and amphibole in rock fragments. The oxide assemblage is dominated by low Mg ilmenite with lesser rutile.
B - The mineralogy and texture of this sample is very similar to that of A. It differs in containing a smaller proportion of rock fragments, a greater proportion of larger mineral and rock fragments and a greater proportion of sub - rounded to rounded rock and mineral fragments. In addition/ it contains a single/ sub - rounded REE - apatite, several phlogopite - bearing rock fragments and two Cu - Zn - Fe - bearing sulphide grain aggregates.
SEM - probe Analysis of Sulphide and Selected Silicate and Oxide Grains.
A combined total of 188 grains were examined under the electron beam with the Scanning Electron Microscope. This total comprises 72 mineral and rock fragments from Sample A and 116 from Sample B. The results of this analysis are given in Table 1.
Table l
Results of SEM - probe of Mineral Grains *
Sample A - 72 grains Sample B - 116
Number of Grains Number of Grains
PyroxeneAmphiboleGarnetEpidotePlagioclase
6 3
14 3 l
Quartz/Silicate intergrowth OSphene 2Pyrite OPyrite/Quartz 11Pyrite */- Plag/Amph 11 **Pyrrhotite OCu - Zn - Fe sulphide OZircon V Plag/Spinel 2Ilmenite 15Ilmenite/Plagioclase 2Magnetite lCr - spinel OREE - apatite OMixed rock fragments l
19 9 5
10 l l 3
21 17 1012 O
10 O 5 l l O
**
* It is very difficult using the SEM to distinguish between some garnet and amphibole minerals due to the similarity in their analytical spectrum. For this reason, the total number of grains for each may be incorrect. Mineral intergrowths also are very common and denoted by +X- or simply /.
** This assemblage may include trace to minor chlorite, sericite and phengite.
Bruce Jago Petrographic Services ~i!7 - 35 Charles Street, West, ronto, Ontario,
M4Y 1R6V
February 14, 1989
John Jasperson, 18 Byron Street, Stouffville, Ontario, L4A 7X3
Dear John ,
Please find attached the report you commissioned on gold grains recovered from basal till samples from Benoit Township, North Eastern Ontario. The report is divided into three sections. Section one includes gold grain descriptions and accompanying photographs, Section two is a table of semi - qualitative grain compositions and Section three is a simplified description of glacial till including a description of gold grains recovered from different glacial and fluvial depositional environments.
In general, all of the gold grains exhibit physical characteristics which can be attributed to physical processes operating in strictly glacial environments with only minor evidence of glacio - fluvial processes. The majority of grains are weakly rounded - to strongly ovoid - tabular although there are several striking examples of sub - equant to equant and partially faceted grains. Most grain surfaces are flaky to weakly laminated, porous to strongly porous and commonly pitted. Bent grain edges are rare. Surface pits are round to cube - shaped suggesting the former presence of pyrite or quartz. Several grains are strongly intergrown with silicate minerals which occassionally protrude from the grain surface. Striated surfaces are very common and two striation directions are typical. All of these physical attributes are typical of gold transported in basal till and suggest that the gold grains have not been transported a great distance, perhaps less than 500 meters from the source rock.
Compositionally , most gold grains contain minor to trace amounts of Ag and sometimes significant amounts of Si with or without minor Na, K, Al and trace amounts of Ga, Fe , Mg and S. This suggests that the gold sometimes is intergrown with quartz, paragonitic (Na - rich) to sericitic (K - rich) mica and trace amounts of pyrite. These are typical guange minerals associated with hydrothermal gold deposits, the Kirkland Lake camp being an excellent example. The presence of paragonitic to sericitic mica is particularly significant in light bf the petrogenetically important relationship between gold mineralization and alkaline intrusive activity in the vicinity of Larder Lake Break and to the close proximity of the samples to economically important, fault related gold mineralization found less than two kilometers away.
Table l, epidote also is very abundant in both samples. This mineral is characteristic of the transition from greenschist facies to lower amphibolite facies metamorphism and also of some types of hydrothermal alteration. Epidote alteration is strongly developed in several of the highly altered rock samples that were examined and it is possible that strongly epidotized lithologies may be present locally.
I hope that this report meets with your satisfaction and that you will not hesistate to discuss any aspect of it with me at our mutual convenience.
Bruce Jago, H.B.Se.,M.Se, Consulting Petrologist
TraSample Descriptions
Tire notation Para - Ser. denotes paragonitic (Na - rich) and sericitic (K- rich) mica.
Sample A3
Photo #
Shape
Surface
Size (microns)
Intergrowth^
Grain lA3 - l
ovoid tabular, irregular
spongy, pitted, striated
164 x 107
Tr. qtz. Para - Ser.
Grain 2A3 - 2
round to ovoid sub - tabular to equant
spongy, flaky, pitted
73 x 55
none
Grain 3 A3 - 3
sub - equant irregular
spongy, flaky
31 x 21 x 14
abundant Para - Ser.
Sample AA
Photo #
Shape
Surface
Size (microns)
Intergrowth^
Grain l A4 - 4/5
Equant, faceted
Flaky, striated Weakly porous
75 x 70 x ??
Tr. Para - Ser.
Grain 2A4 - 6
Flat, angular (See note below)
Striated, angular
66 x 41
Tr. qtz
Grain 3 A4 - 7
Equant, faceted
Flaky, striated Porous
33 x 33 x ??
Qtz.
Note:Photo 5 is a close - up of the top right portion of photo 4.Grain 2 probably was broken by shearing during sample processing.
Sample AS
*Photo l
Shape
Surface
Size (microns)
Grain lA5 - l
Ovoid tabular, irregular
Flaky, weakly porous
200 x 160 x ??
Intergrowths Abundant Para - Ser. Tr. qtz (?)
Note:This is the largest grain of gold encountered in this study,
Sample A6
Photo #
Shape
Surface
Size (microns)
Intergrowths
Grain l A6 - l
Equant to sub - tabular
Porous , flaky Weakly striated Bent edges
50 x 50 x ??
Para - Ser.Fe - Mg silicate
Grain 2 A6 - 2/10
Irregular, Sub - tabular Laminated (?)
Strongly striated Flaky, porous
90 x 60 x ??
Minor qtz
Grain 3A6 - 8/9
Irregular, Ovoid tabular
Flaky, porous Pitted
69 x 47 x ??
Qtz.,Para - Ser.
Note:Grain two is striated in two directions. May be a composite of two grains or a single strongly foliated or smeared grain. Photo A6 -9 is a close - up of photo A6 - 8 and shows circular and roughly cubic surface pits.
ample A6
Photo #
Shape
Surface
Size (microns)Intergrowths
Grain 4A6 - 4/5
Irregular, ovoid tabular
Strongly striated Porous , pitted
89 x 54 x ??
Minor qtz.
Grain 5 A6 - 6
Ovoid tabular
Strongly striated Very porous, pitted
43 x 22 x ??
Tr. qtz Prag - Ser.
Note:Photo A6 -5 is a close - up of A6 - 4 and shows pitted and striated nature of the grain surface, two striae directions. Note the curved striae in photo A6 - 6 of Grain 5.
Grain 6 A6 - 7
Thick, ovoid tabular
Strongly striatedPorous , flaky
Hammered surface
61 x 42 x ??
Tr. qtz., Para - Ser.
the strongly porous, Note that there are
Sample A7
Photo 9
Shape
Surface
Size (microns)
Grain lA7 - 12
Ovoid tabular
Grain 2 A7 - 2
Irregular, thick ovoid tabular
Porous, pitted, flaky Flaky, pitted Weakly striated Porous
117 x 50 x ??
Intergrowths Tr. to minor qtz.
48 x 36 x ??
Tr. qtz
Grain 3A7 - 10
Irregular, thick ovoid tabular
Very flaky, Porous, weakly striated
122 x 67 x ??
Qtz. Para - Ser.
NoterGrain 2 contains several quartz inclusions visible in the top middle of the photo.The surface of grain 3 is highly irregular and is suggestive of a collapsed shell. It appears that the original gold grain was highly intergrown with silicate minerals or pyrite and that these have been strongly leached, perhaps during weathering of the till or during sample processing. The gold shell then appears to have collapsed around the central void. The euhedral grains on one corner of the grain probably are quartz.
Sample A8/9
Photo 0
Shape
Surface
Size (microns)Intergrowths
Grain l A8/9 - 6
Irregular, round to ovoidPorous, pitted, flaky Slightly bent edges63 x 49 x ??
Minor qtz., Py, Tr. prag - ser.
Grain 2 A8/9 - 7/8
Irregular, sub - equant, laminated (?)
Flaky, pitted Porous, striated
70 x 53 x ??
Minor prag - ser Tr. qtz. (?), py
Note:A subhedral quartz grain is attached to grain 1. This is visible on the left side of photo A8/9 - 1.Photo A8/9 -8 is a close - up of the highly striated grain surface shown on photo A8/9 - 7
Sample A10
Photo i
Shape
Surface
Size (microns)
Grain l A10 - 9/10
Thick, round to ovoid tabular
Pitted, porous, weakly striated Bent edge
71 x 57 x ??
Intergrowths Minor qtz, Tr. para - ser,
Note:Several prominent pits dominate the surface of this grain. The sub- equant shape of these suggests that the gold was intergrown with either quartz, alkali - feldspar or pyrite or a combination of these. Photo A10 - 10 is a close - up of the extreme top - right corner of Photo A10 - 9
Semi - Qualitative Composition of Gold Grains and Silicate IntergrowthsAmple Au Ag Si Al Na K No. Ca Mg Fe
A3 -
A3 -..n;.
A3 -
: AA -AA -
"
I AA -
i A 5 -
A6 -
A6 -l '
A6 -
: A6 -; A6 -
A6 -'
S A7 -
- A7 -
i A7 -
A8/9
A8/9
A8/9
l' A10t:-I:
xxxx1 XXX? XX
f: . x1
IT,.r-
12
3
1
2
3
1
1
2
3
A
5
6
1
2
3-
-
-
- 1
mm
-
xxxx
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xxxx
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1 XXXX XX
2 xxxx
3 xxxx
XXXX XX
Major Peak Moderate PeakMinor PeakTrace
XX X X
XX X X
XX X X X X
XX XX XX X XX
x x
XX
XXX XX XX XX XX
XX XX XX XX XX XX
XX XX
XX XX XX
XX
x x
x x
XX X
XX
XX XX XX XX XX
XX XX XX X X
XX XX XX XX XX
XX XX XX XX XX
XXX XX X
8
A Simplified Description of Glacial Till
Glacial till can be classified into unstratified and stratified drift. Unstratified drift is considered to be material deposited directly from a glacier while stratified drift (glacio - fluvial sediment) is material deposited from glacial streams and lakes during from glacial meltdown. Unstratified drift is further sub - divided in ablation till, material which is transported in the middle or top of the glacier and which later is deposited by the downmelting of the ice sheet, and basal till, material that is produced, transported and deposited at and by the base of the ice sheet.
Basal till is composed of rock debris derived from the underlying bedrock and is transported only a short distance prior to deposition. Three types of basal till are recognized. Lodgement till is glacial debris deposited by the process of lodgement. This process occurs during rapid ice movement at low temperatures and results in a smearing of the debris onto the underlying rock surface. It is highly compact as fine rock flour, formed by the comunition of rock fragments, is forcibly pressed into voids between large particles. The local lithology dominates because the rock debris is not transported a great distance from the source. The debris in lodgement till is angular and shows no size sorting although rock fragments typically are alligned parallel to the direction of local ice movement. Basal melt - out till is compacted less than lodgement till because the material is deposited by melting, stationary ice. It contains debris whose lithologic composition may vary from a local to a distal source with distal material often dominating. Clasts are aligned sub - parallel to the direction of ice flow and the sediments are better sorted and may demonstrate a weak stratification compared to those in lodgement till. Deformation till consists of partially digested local material. Glaciodynamic structures such as folds, shear planes, bedding overthrusts, injection breccia and mylonite are characteristic of such deposits. The material is formed by differential movement or high compressive stress during the lodgement process.
Stratified or glacio - fluvial sediments occur as long, narrow ridges called eskers or in complex glacio - lacustrine deposits formed at the leading edge of a melting ice sheet. Eskers range up to 50 meters in height, 50 to 7000 meters in width and 100's to 80000 meters in length ( including gaps in otherwise continuous deposits). The sides of the deposits are steep and the crests are smooth or broadly hummocky. They typically occur in areas of low relief and are elongate parallel to the direction of ice movement. The sediments are reworked till consisting of sand, pebble and cobble sized material with very little fine grained rock flour. The sediments are deposited by streams flowing on the top (superglacial), in the middle (englacial) or under/at the base of the ice sheet (subglacial). The centre of such deposits are well stratified while layering on the sides is parallel to the side slope. The environment of deposition is similar to that of a short - lived, sediment laden stream. Sediments generally travel less than five kilometers from their original rest position.
In all glacial sampling surveys, basal till is the most sought after material as it has travelled the shortest distance from the source.
Physical Characteristics of Gold Particles Recovered from Different Source Materials
Gold is extremely malleable and therefore its shape can change easily during transportation depending on the environment in which it is transported. Several workers who investigated the genesis of the Witwatersrand paleoplacer deposits discovered that gold particles which had been transported for a short distance in rivers (5 to 30 km) had bent and hammered edges while some of the original crystalline texture was still preserved. With an increase in transportation distance (80 to 100 km), the original crystalline texture was lost and the particles became "nugget- shaped" with a dough - like micro - texture and numerous, small, randomly orientated scratches. Gold particles which had travelled a great distance (150 km), were flaky with no trace of the original crystalline morphology. In addition, the particles were flattened and bent several times to form a characteristic sandwich structure. Round, crater - like indentations also are developed.
An laboratory study of gold particle abrasion demonstrated that cobbles are responsible for most of the abrasion and physical changes that occur to gold particles. The study also found that the presence of sand greatly reduced the abrasive effects of pebbles and cobbles, sand submerged in water abraids gold more effectively than dry sand and the velocity of water, not the distance travelled in water controls the extent of abrasion.
A study of the particle size distribution of gold in till was carried out by the Geological Survey of Canada to determine an optimum representative grain size range in weathered and unweathered tills as an aid in gold exploration. The study demonstrated that the grain size distribution of gold in unweathered tills reflected the original size distribution of native gold in the source rocks. Gold in weathered tills occurred predominantly in the fine fraction. It size distribution reflected a combination of the original grain size of native gold in the source rock and the fine grain size of gold released from weathering auriferous sulphides.
A morphological study of sixty gold particles separated from glacio fluvial sediments and basal till was conducted at University of Toronto by Judy Wong for Hudson Bay Mining and Smelting Company in 1985. This study found that gold is more angular and some of its original crystalline structure and protrusions are preserved in basal till compared to gold from glacio - fluvial environments such as eskers. Deep, large, abrasive marks typically are developed on gold grains from till while only small randomly orientated scratches are seen on gold from eskers. Gold particles from eskers are flat and flaky with bent edges and scaly textures suggestive of extensive hammering of the grain surface by sand and pebbles during sub aqueous transport. Such features generally are absent in gold particles from basal till unless melt - down tills have been sampled rather than lodgement or deformation tills. Gold particles from rivers exhibit similar textural features to those encountered in glacio - fluvial environments, however, as the river transport distance increases, gold particles become more flattened and may be bent several times.
r;*'*T^*- *^W
?V;u,
norandaNoranda Exploration Company, Limited(no personal liability)60 Shirley St. South, P.O. Box 1205 Telephone: (705) 264-2368Timmins, Ontario (70S) 267-1194P4N 7J5 Fax: (705) 264-8132
April 7, 1989
Mr. John K. Jasperson RR #2Stoutfville, Ontario L4A 7X3
Dear Mr. Jasperson,
RE; Benoit Township
Enclosed is the log of the hole drilled by Noranda in 1967 that you requested. I have also enclosed a copy of the EM survey showing the location of the EM conductor that was drilled.
I am not able to comment on the gold grain analysis of your property as I am not that familiar with the subject. We thank you, however, for providing this information to us.
Yours truly,NORANDA EXPLORATION COMPANY, LIMITED(no personal liability)
G.J. Koleszar Geological Technician
/aaf
'" POOTAOI "
FHOM
0
TO
160
.. ,. .'-' -.1-. •••r--; -vr^,-'-:-. - v. . 'A^Wi&jf-f*-:^--.-." . - ,-' .-'- ••••- i
DMCNirnON
Caain* (0-6}' - Cla/, 85' - UO' - Sand aad boulder* ,HO 1 x 160' x Coaraa boulder* and *and.)
Hole loat at 160' without r*aohlnf bedrock.
SAMPLENo.
v V ;:::
. " ASSAYS V-" . . 7- '
AU OZ
'
AG OZ *cu * ZN
. "V
K m*'r--i ••. r~:--
'•-•'
'
,,,,
-.•.-.;--
CORE LENGTH
FROM TO
Y 1
ACCWIDTH
.- ;' ; V'
*lll)
CONTRACTOR
rOOTAOK
TODESCRIPTION SAMPLE
No.
ASSAYS
AUOZ AGOZ •K, ZN * m• CORE LENGTH -.l
FROM TO ' ACC WIDTH
0.0 116.0 Casing (0-70' - Clayj 70' - U6' Sand and grtyel)116.0 121.5 Dacite; massive.Light grey coloured. Medium - coarse
grained. Occasional quart* phenocryst and
occasional spot of pyrite.121.5 176.4 Dacite; pillowed. Fine grained. Numerous irregular
carbonate threads and stringers. Occasional
quart* phenocryst, Very occasional pyrite apot. Occasional chlorite spot.
H3.3'- 145.8 1 - Sheared tone. Cor* broken.
9 U3.6' - Chloritic, graphitic banding
at 600 to core. Appears to be too narrow to be tht causative conductor.
176.4 180.6 Welded Tuff} with some D*oitic breccia fragments
to 8", cemented by numerous 1/8" - shards.
CONTRACTOR.Boyles Bros,
LOGGED BY.E. i. Gallo
SURFACE
N. 330 E.
CollarEM X-OVER
V-
Colina,
Chloritic , Grookitlc
Bonding
CI.,
Sond ond Grottl
—- — \, MauTvfDocTtt
Plllovid Docllt
Wlldcd Tuff
oso
Pillow! d Docllt
1053NORANDA EXPLORATION CO. LTD
NORANOA, P. Q.
SECTION !, o/l HOLE 67-lBENOIT 1-66
BENOIT TWP, ONT.
seoie : i"* too' Don: DEC. ze, raeDrown By i E.A,G. /li.TS. '. 4 2-A-8 }
XRAL
CERTIFICATE OF ANALYSIS
REPORT el6O
TO: JASPERSON HOLDINGS LTD ATTN: JOHN K. JASPERSON R.R.#2, 18 BYRON STREET STOUFFVILLE, ONTARIO L4A 7X3
CUSTOMER NO.
DATE SUBMITTED 2-Sep-88
774
REF. FILE 2620-03 Total Pages l
8 SOILS
AU PPBMETHOD DETECTION LIMIT FADCP l.
DATE 13-SEP-88
X-RAY ASSAY LABO!
CERTIFIED BY
X-RAY ASSAY LABORATORIES LIMITED 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947 Member of the SGS Group (Societ6 Generale de Surveillance)
KRAL 15-SEP-88 REPORT 6160 REF.FILE 2620-03 PAGE 1 OF 1
SAMPLE AU PPB
i ' 88-2S 88-3
; 88-5- 88-6f. 88-7
•O3
<1•d<1
s 88-8+9, SHAFT1• :' SHAFT2
X-RAY ASSAY LABORATORIES LIMITED 1885 Leslie Street Don Mis Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947 Member of the S GS Group (Soci^t^ G^n^rale de Surveillance)
C ERTI FI C AT E
REPORT
OF ANALYSIS
69 V 2
TO: JOHN T. WARD9 WILLAMERE DRIVE SCARBOROUGH, ONTARIO M1M 1W5
CUSTOMER No.
DATE SUBMITTED 27-Oct-88
40
REF. FILE 3234-X5 Total Pages 3
7 HEAVY MINERAL CONC.
AU PPB NA PPM CA 3,
SC PPM CR PPM FE X CO PPM NI PPM ZN PPM AS PPM SE PPM RB PPM MO PPM AG PPM SB PPM
METHOD NA NA NA NA NA NA NA NA NA NA NA NA NA NA NA
DETECTION LIMIT5.
500.1.0.1
10.0.025.
200. 50.2.5.
30.5.5.0.2
METHOD DETECTION LIMITBA PPMLA PPMCE PPMSM PPMEU PPMYB PPMLU PPMH F PPMTA PPMW PPMIR PPBT H PPMU PPMWEIGHT GM
NANANANANANANANANANANANANA
100.1.3.0.10.20.20.051.1.4.
20.0.50.50.01
DATE 22-NOV-88
X-RAY ASSAY LAB'
CERTIFIED BY
X-RAY ASSAY LABORATORIES LIMITED 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5765 Fax (416)445-4152 Tlx 06-986947 Member of the SGS Group (Socie'td Ge'ne'rale de Surveillance)
22-NOV-88 REPORT 6972 REF.FILE 3234-X5 PAGE 1 OF 3
SAMPLE AU PPB NA PPM CA SC PPM CR PPM FE X CO PPM HI PPM ZN PPM AS PPM
A3A4 ,A5 '
A6A7
A8-9' A10
78903952
190
7075
22002200200018001700
19002000
68
11612
76
102.98.4103.94.897.2
95.395.4
1000910930990950
8601100
19.218.119.017.020.2
17.718.3
3330302631
2632
^00^00*200^00^00
^00^00
100.140 '90130220
130.140
O4^ .45<3
^<^
X-RAY ASSAY LABORATORIES LIMITED 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5765 Fax {416)445-4152 Tlx 06-986947 Member of the SGS Group (Societe Generale de Surveillance)
22-NOV-88 REPORT 6972 REF.FILE 3234-X5 PAGE 2 OF 3
SAMPLE SE PPM RB PPM MO PPM AG PPM SB PPM BA PPM LA PPM CE PPM SM PPM EU PPM
A3 ^A4 , *1A5 ^A6 <1A7 *:1
A8-9 <1A10 <1
0 ^00 <300 ^00 <300 <30
0 ^00 <30
<6^<5<56
<5^
<5<5<5^^
^<5
*0.2 500^.2 400^.2 400^.2 400^.3 600
<0.2 <400•^.2 <400
409379440433380
436452
625592632654650
621643
35.535.734.934.145.8
33.536.1
7.88.67.48.38.1
7.47.1
X-RAY ASSAY LABORATORIES LIMITED 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5765 Fax (416)445-4152 Tlx 06-986947 Member of the SGS Group (Soci^te Generale de Surveillance)
22-NOV-88 REPORT 6972 REF.FILE 3234-X5 PAGE 3 OF 3
SAMPLE
A3A4 .A5A6A7
A8-9A10
YB PPM
26.726.626.424.228.2
24.824.7
LU PPM
4.014.114.253.934.51
3.904.07'
H F PPM
190190210220180
210200
TA PPM
1616101012
1110
W PPM
15^7
109
810
IR PPB TH PPM
^0 140.^0 130.^0 150.^0 140.^0 180.
^0 140.^0 160.
U PPM
18.613.116.614.117.0
14.715.7
WEIGHT GM
11,4 ,12.213.516.018.2
16.311.5
X-RAY ASSAY LABORATORIES LIMITED 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5765 Fax (416)445-4152 Tlx 06-986947 Member of the SGS Group (Soci6t4 G6n6rale de Surveillance)
CERTIFICATE OF ANALYSIS
REPORT V 3 2 6
TO: JOHN T. WARD9 WILLAMERE DRIVE SCARBOROUGH, ONTARIO HIM 1W5
CUSTOMER No.
DATE SUBMITTED 19-D6C-88
40
REF. FILE 3789-A5 Total Pages l
2 ROCKS
AU PPBMETHOD DETECTION LIMIT FADCP l.
*** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS 180 DAYS *** AND REJECTS 30 DAYS FROM DATE OF THIS REPORT
DATE 23-DEC-88
X-RAY ASSAY LABORATORIES LIMITED
CERTIFIED BY .
X-RAY ASSAY LABORATORIES LIMITED 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-086947 Member of the SGS Group (Socie'te' Ge'ne'rale de Surveillance)
23-DEC-88
SAMPLE AU PPB
REPORT 7326 REF.FILE 3789-A5 PAGE 1 OF 1
Q.VEIN-83-100 Q.VEIN-88-101
23002200
X-RAY ASSAY LABORATORIES LIMITED 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947 Member of the SGS Group (Soci6t6 Ge"n6rale de surveillance)
XR'AL 23 -DEC-88 REPORT 7326 REF.FILE 3789-A5 PAGE 1 OF 1
SAMPLE AU PPB
Q.VEIN-63-100 2300 Q.VEIN-88-101 2200
X-RAY ASSAY LABORATORIES LIMITED 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-6765 Fax (416)445-4152 Tlx 06-986947 Member of the SGS Group (Societe Generale de Surveillance)
X-RAY ASSAY LABORATORIESA DIVISION OF SQS SUPERVISION SERVICES INC.
1885 LESLIE STREET - DON MILLS, ONTARIO MSB 3J4 - CANADA TEL: (416)445-6755 TELEX: 06-986947 FAX: (416)446-4162
CERTIFICATE OF ANA.H. Y SI S
REPORT "7412
TO: JOHN T. WARD9 WILLAMERE DRIVE SCARBOROUGH, ONTARIO HIM 1W5
CUSTOMER No.
DATE SUBMITTED 15-D6C-88
40
REF. FILE 3771-X5 Total Pages 3
9 HEAVY MINERAL CONCENTRATES
AU PPB NA '/, CA K SC PPM CR PPM FE K CO PPM NI PPM ZN PPM AS PPM SE PPM MO PPM AG PPM SB PPM
METHOD NA NA NA NA NA NA NA NA NA NA NA NA NA NA
DETECTION LIMIT 30.0.051.0.1
10.0.025.
200. 200.
2. 20. 20.5.0.2
BA PPMLA PPMCE PPMSM PPMEU PPMYB PPMLU PPMH F PPMTA PPMW PPMIR PPBT H PPMU PPMWEIGHT GM
METHODNANANANANANANANANANANANANA
DETECTION LIMIT200.
1.3.0.10.20.20.051.1.
10.50.0.50.50.01
DATE 09-JAN-89 CERTIFIED BY Jean H.L. Dpi
Member of the SGS Group (Societe Generate de Surveillance)
09-JAN-89 REPORT 7412 REF.FILE 3771-X5 PAGE 1 OF 3
SAMPLE
88-0588-1288-1388-1488-15
88-1788-18,1988-2088-21
AU PPB
4200^0^0^040
^0^0<3070
NA 7.
0.150.14^.05^.05^.05
0.120.130.130.13
CA K
868
147
7^57
SC PPM
81.086.288.6179.88.1
79.385.286.498.5
CR PPM
660770
11001400750
61010009601200
FE K
15.915.714.632.416.4
14.117.116.217.7
CO PPM
2220224724
22202224
NI PPM
^00*500^00^00^00
200^00^00^00
ZN PPM
200200300400200
^00^00300200
AS PPM
,c5^^^*5
^<5<5<5
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5765 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Societe Generate de Surveillance)
09-JAN-89 REPORT 7412 REF.FILE 3771-X5 PAGE 2 OF 3
SAMPLE SE PPM
88-05 ^088-12 ^088-13 ^088-14 ^088-15 <20
88-17 3088-18,19 6088-20 ^088-21 ^0
MO PPM AG PPM
^0 <5<20 <5<20 ^<20 <5<20 <5
^0 ^<20 <5<20 ^<20 <5
SB PPM
0.6^.31.02.81.0
0.5^.50.70. 4
BA PPM
200500^00600600
300700
*3001100
LA PPM
426389454685385
293450355387
CE PPM
6676487751220611
499745574714
SM PPM
58.856.066.4
112.54.2
49.258.250.360.7
EU PPM
5.56.09.314.07.1
7.55.36.48.1
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario MSB 3J4 (416)445-5765 Fax {416)445-4152 Tlx 06-986947Member of the SGS Group (SociStS G6n6rale de Surveillance)
09-JAN-89 REPORT 7412 REF.FILE 3771-X5 PAGE 3 OF 3
SAMPLE
88-0588-1288-1388-1488-15
88-1788-18,1988-2088-21
YB PPM
25.826.131.655.227.0
23.429.326.930.6
LU PPM
4.454.254.668.554.21
3.674.974.205.10
H F PPM
200180260290200
130200150180
TA PPM
89
122410
1314119
W PPM IR PPB TH PPM
10 ^0 170.^0 ^0 150.^0 ^0 170.^0 ^0 280.^0 ^0 150.
^0 ^0 100.^0 -SO 190.•OD ^0 140.<10 <50 170.
U PPM
23.620.136.948.119.5
16.819.416.620.6
WEIGHT GM
12.012.822.818.025.2
15.013.814.44.85
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario MSB 3J4 (416)445-5765 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Societe Generate de Surveillance)
XRAL X-RAY ASSAY LABORATORIESA DIVISION OF SGS SUPERVISION SERVICES INC.
1885 LESLIE STREET ' DON MILLS, ONTARIO M3B 3J4 * CANADA TEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF
REPORT 8X31
ISf xzmTO: JOHN T. WARD
9 WILLAMERE DRIVE SCARBOROUGH, ONTARIO HIM 1W5
CUSTOMER NO.
DATE SUBMITTED 13-Mar-89
40
REF. FILE 4267-PH Total Pages 3
l PULP
WRMAJ % NI PPM WRMIN PPM AG PPM
METHOD DETECTION LIMITWR 0.01DCP 1.WR 10.GFAA 0.02
DATE 12-APR-89 CERTIFIED BYJean H.L. Opde
Member of the SGS Group (Societe centrale de Surveillance)
12-APR-89 REPORT 8131 REF.FILE 4267-PH PAGE 1 OF 3
SAMPLE NI PPM AG PPM
Q-VEIN-83-100 25 1.15
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5765 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group ( Soci6t6 Ge'ne'rale de Surveillance)
XRF - WHOLE ROCK ANALYSIS 12-APR-89 REPORT 8131 REFERENCE FILE 4267 PAGE 2 of 3
SAMPLE \ K S I02 AL203 CAO MGO NA20 K20 FE203 MNO TI02 P205 CR203 LOI SUM
Q-VEIN-83-100 90.9 2.57 0.26 0.46 O.01 0.69 2.84 0.02 0.20 0.07 0.04 1.70 99.8
XRF W.R.A. SUMS INCLUDE ALL ELEMENTS DETERMINED. FOR SUMMATION, ELEMENTS ARE CALCULATED AS OXIDES
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755 Fax (416)446-4152 Tlx 06-986947Member of the SGS Group (Soc16t6 centrale de Surveillance)
XRF - WHOLE ROCK ANALYSIS 12-APR-89 REPORT 8131 REFERENCE FILE 4267
SAMPLE \ PPM RB SR Y ZR NB BA
Q-VEIN-83-100 44 <10 ^0 19 ^0 168
PAGE 3 of 3
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group ( Soclete Generale de Surveillance)
XRAL X-RAY ASSAY LABORATORIESA DIVISION OF SGS SUPERVISION SERVICES INC.
1885 LESLIE STREET ' DON MILLS, ONTARIO M3B 3J4 * CANADATEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF ANALYSIS
REPORT 8 2 8 X
TO: JOHN T. WARD9 WILLAMERE DRIVE SCARBOROUGH, ONTARIO M1M 1W5
CUSTOMER No.
DATE SUBMITTED 18-Apr-89
40
REF. FILE 4 478-PH Total Pages l
l PULP RE: W0# 4267
S % AS PPM
METHOD DETECTION LIMITXRF 0.01FAA 0.1
DATE Ol-MAY-89 CERTIFIED BYJean H.L. Opdeb^sck, Vlc^Presldent Operation^
Member of the SGS G roup (Soci^t^ G6n6rale de Surveillance)
01-MAY-89 REPORT 8281 REF.FILE 4478-PH PAGE 1 OF 1
SAMPLE S X AS PPM
Q-VEIN-83-100 1.23 160.
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5765 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Socie'te1 CeVieYale de Surveillance)
XRALfi*X-RAY ASSAY LABORATORIES
A DIVISION OF SGS SUPERVISION SERVICES INC.1885 LESLIE STREET * DON MILLS, ONTARIO M3B 3J4 - CANADATEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF
REPORT 8
S
ST.
TO: JOHN T. WARD9 WILLAMERE DRIVE SCARBOROUGH, ONTARIO M1M 1W5
CUSTOMER No.
DATE SUBMITTED 2l-Apr-89
40
REF. FILE 4501-PH Total Pages l
9 HEAVY MINERALS(FROM W.O.3771)
NI PPM AG PPM
METHOD DCP GFAA
DETECTION LIMIT 1. 0.02
DATE 02-MAY-89 CERTIFIED BYJean H.L. Opdebee^, Vice P/esldent Operations
Member of the SGS G roup C Soci^t^ G&ie'rete de Surveillance)
02-MAY-89 REPORT 8299 REF.FILE 4501-PH PAGE 1 OF 1
SAMPLE NI PPM AG PPM
88-0588-1288-1388-1488-15
88-1788-18,1988-2088-21
1615121513
18161520
0.06^.020.030.05^.02
^.020. 02O.020.02
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario MSB 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member o f the SGS G roup (Soci6t6 GeVieYale de Surveillance)
XRAL X-RAY ASSAY LABORATORIESA DIVISION OF SGS SUPERVISION SERVICES INC.
1885 LESLIE STREET ' DON MILLS, ONTARIO M3B 3J4 * CANADA TEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF ANAHL. Y S
REPORT 8 4 O 4 . 5
TO: JOHN T. WARD9 WILLAMERE DRIVE SCARBOROUGH, ONTARIO M1M 1W5
CUSTOMER No.
DATE SUBMITTED 9-May-89
40
REF. FILE 4622-PH Total Pages l
9 PULPS RE: W0# 3771
NI PPMMETHOD DCP
DETECTION LIMIT 1.
DATE 16-MAY-89 CERTIFIED BY .Jean H.L. Opdebe
Member of the SGS Group (Sociltl Generate de Surveillance)
16-MAY-89
SAMPLE NI PPM
88-17 88-18,19 88-20 88-21
REPORT 8404 REF.FILE 4622-PH PAGE 1 OF 1
88-0588-1288-1388-1488-15
4946474646
52414452
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-6765 Fax (416)445-4162 Tlx 06-986947Member of the SGS Group ^ocie'te' Ge'ne'rale de Surveillance)
XRAL X-RAY ASSAY LABORATORIESA DIVISION OF 8GS SUPERVISION SERVICES INC.
1885 LESLIE STREET ' DON MILLS, ONTARIO M3B 3J4 * CANADATEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF AJSTA1L, Y SI S
REPORT 8334
TO: JOHN T. WARD9 WILLAMERE DRIVE
i SCARBOROUGH, ONTARIO M1M 1W5
CUSTOMER No.
DATE SUBMITTED 8-Mar-89
40
REF. FILE 4254-PH Total Pages l
9 HEAVY MINERALS
NI PPM AG PPM
RE: W0# 31012,3234
METHOD DETECTION LIMITDCP 1.GFAA O.02
DATE 09-MAY-89 CERTIFIED BY .Jean H.L. Opdebeec^, Vice Pijesldent Operations^
Member of the SGS Group (Socie'te' GgneYale de Surveillance)
09-MAY-89 REPORT 8334 REF.FILE 4254-PH PAGE 1 OF 1
SAMPLE NI PPM AG PPM
WB87-01UB87-02A3A4AS
1415232320
0.020.020.040.060.04
A6 A7 A8-9 A10
19201821
0.040.020.020.05
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5765 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Soci^te" Generate de Surveillance)
File BV16V1G15: BRlft Backhoe LOtGEKEUT Ull Sup l HEAVY MINERAL MGT DATA (Normalised) t BENOIT TP DATA.
The following comparison is made between a selection from the 06S BRIM BACKHOE sauples of LODGEhENT TILL SAMPLES and the results of Backhoe Lodqrcent Till sampling on the Jasperson clains, BENOIT Township under the direction of John T. Ward P.Eng.. A goal is to seasure backgoiind and establish Khal is anomalous. The'entire BRIM project results covering the Black River Matheson area were sade available on diskette late October 1988, froa the 06S.
NORf&alised Visible Gold count (NQRJ/G) is the actual gold count divided by the sun of the non magnetic reaainder and the sagnetic resainder (NONMAGJ3H t HAGJMi multiplied by a factor of ten so the gold count is cosparable to a ten gran unit of heavy ainerals. Of the entire BRIH backhoe project (84-87), 2B2 saeples, or.ly 111 had visible gold grains, and the average of the SUB of the norualised count, 223,49/282 : 0.793/sspi.
Background for the 282 saisples can be calculated by cutting back the top 18X of values to an aisount not exceeding the lowest fisuber. Also the sane for the lowest 16/1 being increased to a value not below the highest aesiber of the group. (28*0+28*2.24+82.2)7282=8+62.72t82.2M44.V282^512;sspl.
LODGEMENT TILL SfiHPLES SELECTED FROH BRIM BACKHOE SAMPLES: Of 282 backhoe saiples only 74 can be classed as Lodgeaent Till both by checking the recorded field designation and evaluating the notes describing the iiaterial as collected and processed by OSS.
Nuab BITE T SPLIT KG PTEN KG T FEED KG T CON 6H H LIGHT GM NONHA6 6M HA6 6M MO V6 NOR V6 m i )95X 5 79 84289 7,6 B.3 7.3 148.6 119 25.B 3.8 8
12 84012 7.3 0.8 6.5 138.4 111 22.2 5.2 2 0.73013 8401317 8481718 8481819 8481921 8482123 8482324 B482427 B4B2729 8482935 8493538 84638 8.5 8.6 7.9 119.9 97.6 18 4.3 l 8.44842 8484243 8484344 84844 6.4 8.8 5.6 127.2 111.9- 14.4 8.9 2 1.307 1.3145 8484546 8484649 8484952 8485253 8485354 84854 6.2 1.9 6.3 110.6 75,2 27.5 7.9 655 84855 6.5 8.9 5.6 147 188.8 38 8.2 2 8.52456 8495657 84857 7.4 g.6 6.8 123.6 81.8 33.5 8.3 E58 8435868 8406861 B436162 84862 7.1 2.1 i- 1 45.6 118 32.2 3.4 2 8.56264 84E6468 84B68 7,8 l 6.8 199.1 143.3 42.7 13.1 l 8.17969 84369
Pace l of 5
76.37.67.38.88.58.16.76.67.66.67.66.47.98.57.3
86.49.97.67.17.37.5e. 26.56.17.47.66.96.61 1 1 * 1
6.97,86,3
8.4e. 78.3B.S8.91.12.58.48.66,78.68.70.80.58.61.2
18.82.71.31.82.3
11.98.98.8g. 6E. SE. 83.72.1
f
ii
0.7
6.65.67.36.57.97.45.66.3
66.9
66.95.67.47.96.1
75.67.26.35.3
56.56.35.65,36.86.B6.1r- Q*.'. 7
6
4.96.8
- 5.6
113.4129.6148.6138.4141.7114.1121.776.5
115.994.679.3B7.6B1.6
133.1119.9162.1151.8127.2167.5159.4147.4123.1116.2110.6
147145.3123.6138.6168.7
147145.6198.8199.1
154
98.6184.7
119111
115.579.877.750.492.364.558.857.251.899.897.6
125.9114.1111.9-127.1128.6119.688.885.775,2
188.8115.181.8
166141.8115.3
118154.9143.3123.9
18.522.725. B22.226.127.733.821.120.724.323.524.324.524.4
1827.9
3014.429.824.528.727.4
2427.5
3824.533.526.421.424.732.232.242.726,3
4.32.23.85.28.16.6
18.25
2.95.8
56.15.35.94.38.37.78.9
18.66.37.16.96.57.98.25.7B.34.25.5
73.4
11.713.15.2
File MGNGT5: ERIN Backhec LODSEIO1 TILL Espi HEfiVV MMML WGT DATA (Normalised) t BENOIT TP DATft.
Nuiib 71 72737476776587888995
105109117122129133138139142148149154174168181186187188189190193206211217223243248252253
SITE TJ B4071 84872840738407464076648778486584887648668488965882B5812658166582485829850368584(38584585846850498505585856850618588185102851038510885189851108511185112851158512885133851398514586802868878601186012
iPUTJCB PI 6.4 7.6
e6.75.56.86.55.86.9
78.59.99.99.4
18.19
18.89.1
1910.811.69.9
P18.99.4
10.98.99.39.2
11.19.5
98.1B. fi8.76.2
11.518.512.210.4
fENJ;S T, 1.2e. 81.60.88.51.10.66.6e, 5e. 60,6
11
2.10i.
0.81.51.13.68.81.62,61.6B. 91.7
11.4
11.41.91.31.61.53.11.31.31.48.41.81.2
FEEEJJG T 5.2 6.66.45.9
C
5,75.95.26.46. s7.78.98,97.36.16.29.3
e8.4
1810
7,37.4
187.79.97.58.37.69.26.27.46.65.77.46.9
18.110.118.4
0 1i , i.
,CONJK H, 129.6 191.528B.4217.877.1
215.1213.4223.8
283190
137.1274.9
139274.1256.4180.1277.9338.6301.2341.2115.269.6
149.2284.3134.8154.9228.2238.7228.4292.924B.9248.8
171168.2170.4172.2145.5150.9241.6172.9
IIGHTJM NO 94.2
181.6241,4206.4
4B.4284.5
167180.6169.5159.196.5
248.5131.1248.2225.784.3
239.9294.8268.9
29975.8
61117.2
268116,9116.220E.3283.9199.9264.9
217225.5142.7
118138.6146.6103.5110.4-189.7144.3
NHftBJH H 28.8 7.5
33.68.6
23.48
21.133.227.525.631.517.712.418,522.4
1126
34.623.831.827.819.524.517.9
1429.119.923.321.622.323.316.218.221.5
1721
31.93248
21.7
IAGJ5M N 6.6 2.4
13.42.85.32.64.6
106
5.39.18.75.57.48.34.8
129.28.5
10.411.69.17.56.43.99.6
83.56.95.78.67.1
10.136.722.84.6
10.18.5
13.16.9
O.VG " 0
01e4818000
2884880045380280
1524
92883288e3e
NOR.VB
8.213
1.394
0.389
0.758
1.383
8.9481.2691.049
1.117
5.5978.4213.2140.627
e. 5158.503
0.565
)90X )95X
1.39 1.39
1.38
1.27
1.12
5.68 5.598.42 8.423.21 3.21
Total 74 less the top 8 and bolton 8 131.63-123.6+Blh B.81 gold grains. 31.631 23.6 Sitple Ave.s 31.6/74 * 8.4274
Of the 74 Lodgeeent Till samples only 22 have visble grains and tha average is 31, 631/74=8. 427/sepl. fts above, correcting for extrese values we have 18*0+8*1. 12+8.
Of the 74 lodgenent till samples seven are identifiable down ice trains fros knoKn occurrences. Six sites are down ice fros the small but incredibly rich forcer producer, the Croesus Hine (that faulted off after producing 15888 oz gold frcic 5EB3 tons) and the values are probably enhanced by crossing the White Guyatt Prospect and the Gold Pyraaid Prospect en route.
f'eae 2 of 5
File BkL6W6T5: BRIM Backhoe LODGEMENT TILL Empl HEAVY MINERAL NET DATA (Nomalised) t BENOIT TP DATA.
GOLD TRAINS
Numb SITE T SPLIT KG PTEN KG T FEED KG T CON-BM H LI6HT BM NQNHA6 6H MAS BM NO V6 NOR V6 "160186187188189190
8513285108851B9851108511185132
9.4B.99.39.211.19.5
1.71.4
11.41.91.3
7.77.5e. 37.89.28.2
134.8228.2238. 7228.4292.9248.9
116.9288.3283.9199.9264.9
217
1419.923.321.622.323.3
3.98
3.56.95.78.6
20152492
1.117
5.597B. 42!3,2140.627
5.698.423.21
The one remaining is down ice fros a Harker Tp. Prospect, 122 85829 10.1 2 8.1 256.4 225.7 22.4 8.3 4 1.383 1.30
6.89.49.28.48.6
0.71.50.88.7
1
8.7.8.7.7.
19478
11598.1138.9102.4
115
91.771
106.773.594.8
17.621
23.821.215.2
5.76.18.47.7
5
1148.46
0.4295.1662.4841.3842.970
5.172.4B1.382.97
5.162.48
2.97
20.280
BENOIT TOWNSHIP LODGEMENT (Basal) TILL SAMPLING (Jasperson Clains). Till type: Matheson Till at 170 deg.. Saeples of varrying weight greater than 20 Ibs were taken fro* 18 saiaple sites over a period froi Noveiber 1987 to November 1988. The estimated depth of the till varried from 6 to 8 feet when taken near to outcrops but was always within 3 feet of the bed rock. Where the samples were sone distance fro* an outcrop and the bed rock not evident, the depth Has increased to 15 to 18 feet.
)BRIM)BR1HSMPL.f SITE T .SPLIT KG F'TENJG T FEED KG T CON BM M LIGHT GK NONHAGJM MAG BM NO.VS NOR.V6 98X 95* 87-81 67-81 8.5 0,8 7,7 " 311.3 " 280.3 24.5 6.5 " l 0.32387-02 87-82 IE.6 l 9.6 226,9 188.T 29.2 9.6 4 1.031
A3 88-03 9.9 3 6.9 103 81.8 14.8 6.4 B 3.774 3.77 3.77A4 88-02 8.3 1.1 7.2 148.9 118.7 16 6.2 13 5.B56 5.86 5.B5A5 88-05A6 88-86A7 88-07
A8&9 BB-8WA10 Shft
88-05 88-85 8.7 0.5 8.2 218.1 192.9 17 8.2 13 5.1595.165.1588-12 88-1288-13 88-1388-14 88-1488-15 88-15B8-17 68-17-IBU9 -18419B8-2D 88-2088-21 88-21 7,2 2.5 6.7 172.4 165.1 6.6 8.7 2 2.7402,742.73
When the BENOIT results ire cospared to BRIM, we find that Benoit has 12 values or 66X of all its values greater than 95 li of ali the BRIM values. The Benoit saeples are cocparable to BRIH as they were processed by Overburden Drilling Management, the saise method and people nho processed the BRIM project. Also, the visible grains have been "normalised" (NOR.VGI by referring the® to the sane ten gram weight of HEAVY MINERALS lNONHA6.6RHtMflG.6RH).
A SMALL DIFFERENCE: One difference between processing methods did ocurr. Sold grains were isolated both by the shaker table and by panning. IR the Benoit case every sanple was panned including those that were zero for grains froa the shaker table. BRIM did it differently and only panned when 2 grains of gold were first spotted on the shaker table. This opens the possibility that very snail grains in the 25X25 aicron class were iftissed in the nil shaker table samples. To correct fer this the BRIM values have been adjusted so that there are no nil saaples. Every nil grain saisple has been arbitrarily assigned 2 grains. The new values follow:
fage J of 5
69.76.98.57.413
5.7
0.50
1.20.50.68.70.4
5.59.77.7
86.89.3K 7J t i.'
143.189.194.217.322.327.167.
9239•jx
65
119.2157.3162.2172,1293.7-
303144
18.731.424.634.620.618.919.5
60.57.511.27.95.7
4
7988025
2.8342.8212.4921.7470.0000.8132.128
2.832.822,491.75
2.13
2.832.822,491.74
2.12
File BHGWGT5: BRIM Backhoe LODGEMENT TILL Snpl HEAVY MINERAL WGT DATA (Nomalised) * 6EN017 TP DATA.
limb5Tl
9121317181921232427293538424344454649525354555657586861626468697172737476778587883995
105189117122!29133138139142
SITEB4E0584007B400984012848138401784018B4019840218402384024840278402984035840388404284043840448484584046840498405284053840548485584056840578405884B6E84061840628406484068840698487184872840736487484B7684077840858408784088B40898580285012850168582485029850368584085S456504685049
T.SPLITJCG7
6.37.67.38.88.58.16.76.67.66.67.66.47.9B.57.3
e6.49.97.67.17.37.58.26.56.17.47.66.96.67.16.97.86.36.47.6
86.75.56.86.55.86.9
7e. 59,99.99.4
16.19
10.89.1
1018.8
PTENJ60.40.70.30.86.91.12.58.40.60.70.60.70.88.50.61.2
10.82.71.31.82.3
11,90.95.88.60.68.88.71.1
i
S8.71.20.61.60.80.51.1B.68.60.50.60.8
11
2.12
8,81.51.11.60.8
TJEED KG6.65.67.36.57.97.45.66.3
66.9
66.95.67,47.96.1
75.67.26.35.3
56.56.35.65.36.86.66.15.9
64.96.85.65.26.B6.45.9
55.75.95.26.46.47.73.98.97.38.16.29.3
88.4
10
TJIONJjH" 113.4
129.6148.6138.4141.7114.1121.776.5
115.994.679.387.681.6
138.1119.9162.1151.8127.2167.5159.4147.4123.1116.2110.6
147145.3123.6138.6168.7
147145.6198.8199.1
154129.6191.5288.4217.877.1
215.1213.4223.8
203190
137.1274.9
139274.1256.4100. 1277.9338.6301.2341.2
(U1GHTJ3M NOW96.6
104.7119111
115.579.877.758,492.364.5 '58.657.251.899.897,6
125.9114.1111.9127.1128.6119.688.865. 775.2
106.6115.181.8
106141.8115.3
118154.9143.3123.994.2
181.6241.4286.4-48.4
284.5187
168.6169.5159.196.5
248.5131.1248.2225.7
84.3239.9294.8268.9
299
lAG.GM18.522.725.822.226.127.733.821.128.724.323.524.324.524.4
1827.9
3014.429. B24.528.727.4
2427.5
3824.533.520.421.424.732.232.242.726.326.6
7.533.66.6
23.48
21.133.227.525.631.517.712.418.522.4
1126
34.623.831. B
HAGJiH f4.32.23.85.28.16.6
18.25
2.95.8
56.15.35.94.38.37.78.9
10.66.37.16.96.57.98.25.78.34.25.5
13.4
H. 713.15.26.62.4
13.42.85.32.64.6
186
5.39.18.75.57.48,34.8
129.28.5
18.4
IO.VG222222222222221222222222222222221222124212222222422224
NOR VG )98X0.8770.8838.6768.7380.7638.5838.4558.7668.8478.6646.7828.6588.6716.660 .8.4488.5528.5311.307 1.318.4958.6498.7190.5838.6568.5658.5248.6628.4780.8138.743P. 63!0.5628.4568.1798.6358.5652.8288.2131.7541.394 1.391.887B.3B98.4638.5978.6478.4938.7581.1178.7721.383 1.381.2668.5268.4578.6198.948
W5X O8Z
8.45
8.44
0.458.17
8.21
1.39
8.388.46
8.45
4 o f 5
File BkLBMGTS: BR1H Backhoe LODGEMENT TILL Sap! HEAVY MINERAL WET DA!A (Nomalised) * BENOIT TP DATA.
flush148
.149154174188181186187188189198193286211217223243248252253
SITE TJPLITJCG FTENJCG TJEED.KG T850558585685861850818510285183851888518985110851118511285115B512B85133851398514586882868878601186812
11.69.9
918.99.4
18.98.99.39.2
11.19.5
98.18.88.78.2
11.518.532.218.4
5.62.63.68.91.7
11.4
11.41.91.31.61.53.33.31.31.48.4l.B1.2
1C7.37.4
107.79.97.58.37.89.28.27.46.65.77.46.9
18.1ie,i10.49.2
.CON.Gh1 KJ.IGHTJ5M NONMAGJH HAGJH NOJ/G NORJ/B )98X )95X OBX" 115.2
89.6149.2284.3134.8154.9228.2238.7228.4292.9248.9248.8
171168.2378.4172.2145.5158.9241.6172.9
75.861
117.2268
116.9116.2288.3283.9199.9264.9
217225.5142.7
ne130.6146.6183.5118.4389.7144.3
27.819.524.517.9
1429.119.923.321.622.323.316.2IB. 221.5
1721
31.93248
21.7
11.69.17.56.43.99.6
83.56.95.78.67.1
18.136.722.8
4.618.18.5
13.16.9
5322222
1524
92223222232
1.269 1.271.8498.625B. 8231.117 1.128.5178.7175.597 5.688.421 8.423.214 3.218.6278. 8588.7878.5158.5838.7810.4768.4948.5658.699
5.598.423.21
Total 74 less the top 6 and bolton 8 [69.8-l23.6i3.85> 43.13 gold grains. 69.88823.6 3.85Siiple Ave.* 69.8/74 - 8 .9433
Background for the 74 Lodgeaent Till saaples can be calculated by cutting back the top 301 of values to an aaount not exceeding the lowest neaber. Also the sate for the lonest 10X being increased to a value not below the highest nenber of the group.(8M4+8U. 12+43.13)/2B2:3.68*8.96*43.13=55.77^ 8.754 /siipl. This corrected value seeas a bit high for background as it is above the background of .512 for the larger picture of 282 sasples. The true Normalised Background is probaly closer to .512/sapl.
Consent: All that has changed is background and not by luch. Nothing else has changed. The Benoit saiples are still significantly anomalous when cospared to the BRIM results and coapare favourably to the doKn ice train fros the Croesus Mine.
Paae 5 o? 5
N
Jospersoo Hydrothermal B old Prospect, Benoit Twp, Larder Lake M ining Division, Kirkland Lake, Ontario
Overburden Drill Sampling Oct. 30 to Nov. 4, 1989 using the Wink Sonic Yibracore Drill
AMD
9 :OOHCLAlH LSMOB3
/OS"/Z
*. — ® -8 :00ft
A,
7:
6 :OOH
5 :OOH
4 :OOH
Traverse Vector
CLAIM L884082nnuiriiiruiuuiuniiiiMiKiiHrinmBminHmiirMiffiiiiniHiniimniiil]
**2 42/l"r 120
f* d*Pth- 2 ft of muskeg,6 ft varved clay f 1 3 ft wet clay , 2 ft sand -fr fine gravel. 1 ft smpl clay amd 1ft smpl sandy outwash till.
Y2J060: 50 ft depth : 3 ft muskeg 1 0 ft vlrvedf clay, 32 ft soft clay, 5 ft till. 2 try s: 1st pulled for larger injector core, 2nd stuck in till. 4 smpls: 2 clay fc 2 till.
1 2 :OOV 8:25N .4. V2 000: 48.S feet total depth: 3 ft muskeg,
5 ft varved clay, 38 ft soft c lay, 2.5 ft of till. •r 2. try s: 1 st stopped by Sem rock in injector core,""""""" 2nd by dry till. 4 smpls: 2 clay and 2 till, f*
i iVI 000: 2 611 stopped by boulder. 1 f oot clay sample.VI 005: 36 ft stopped by boulder. 2 5-foot clay samples. VI 015: 40ft clay*- b oulder top.VI 060: 86ft total depth; stopped in fine beach
sand? 1-foot samples at 64-65'ft and 4-at 85-86ft. C lay ends at 55ft.
VI 100: 65 feet total depth. Clay est. 50ft 1-ft sample at 14-15ft (clay) andI-ft sample at 64-63ft (till).
VI 140: 48 feet total depth. Clay est. 40ft. 5-ft sample 35-40ft (clay). 4-ft sample 42-46ft (till) and 1 -ftsample 47-48ft (till). S tuck in till.
VI 180:15 feet total depth 4 times - stopped b y b o y l d e r s. 1 - ft s a rn pie (till).
A1 000: 21ft total. 5 smpls f o. A i 000 | all till. 7-T! ft, -LII-12ft, 1 6~20ft, 20-21twice. B oulder top.
A2 000:26ft total depth. 3 smpls all t ill: 14-15ft.20-25 fc 25-26. Boulder top twice. * T-
BiiiMiiiiimiiiimamniiimi
8:50V 6:20N
Traverse **1 Vector **1
1 00 metersmJimmnimMBitiiiiHBi
si
/p,
ACTIVITY L06 JASPERSON BENOIT TUP PROJECT OCT. 30 - NOV.4, 1989
File|:\Expl\BEN\BNLG89NV.wrl
Oct. 30, 1989:Monday: loving on site; setting up; drilled, logged and bagged saiples froi:
VI 015 and VI 005
The convention adopted for identifying the location of the overburden drill holes is t base point plus direction of traverse vector and distance along vector.
Traverse l, Vector l, starts at coordinates 6:22 N, 8:50 U and has en aziiuth of 222 deg.Traverse 2, Vector 2, starts at coordinates 8:25 N, 12:00 U and has an aziiuth of 42 deg.Point Al 000 is located 10 leters north of foner trench 88-09 and point A2 000 lies closeby to Al 000 but on a line between Al 000 and VI 180.
Traverse l has drill holes at: 000, 005 (5 leters along vector), 015, 060, 100, 140 and 180 (180 leters along vector) with a heading of 222 deg..
Traverse 2 has overburden drill holes at: 000, 060 (60 leters along vector) and 120 with a heading of 42 deg.
Vi 015: over all depth 40 ft; stopped by a boulder top. Approx 3 to 4 ft of sand followed by 36 ft of clay. Hole stopped in clay with only a stall saiple taken fron the bit at the end.
VI 005: location changed to 10 leters north east. 2 holes put down to 36 ft. Top 3 to 4 feet of sand followed by 32 to 33 feet of clay. Both holes stopped by a boulder. Two saaples of 5 ft of core froi 31 to 36 ft.
Oct. 31, 1989:Tuesday: drilled, logged and bagged saiples froi VI 000 and VI 060 and lost half a day tothe mechanical failure of the hydraulic lifter to extract the drill pipe froi VI 060.
VI 000: Overall depth 26 feet, stopped by a boulder: 3 to 4 feet of sand followed by 22 to 23 feet of clay. Only one saiple, 12 inches of core, taken froi 25 to 26 ft.. Since the siallest core barrel - 12 inches - has the greatest chance of penetrating to depth, it was often being used at the tiie a decision was lade to abandon a hole due to an iipenetrable obstruction. When we penetrated to till the decision was lade to change to a 5 foot core barrel to obtain as such saiple as possible, froi the greatest depth attainable.
VI 060: overall depth 86 feet but it took three atteipts before being stopped in till: sand for 3 to 4 feet followed by clay to 55 feet with till estiiated to 86 ft. 2 atteipts got to 66 ft. and a third with the stall core barrel got to 86 ft. 4 saipels were taken: l 9in saiple froi 64 to 64.75 ft and another 3 inch saiple froi 64.75 to 65 ft. Again, the 12in core barrel stuck in sandy till at 86 ft. After great difficulty the drill was withdrawn and a l ft. saiple of two parts was taken: l saiple of 9in froi 85 ft. to 65.75 ft. and
page
ACTIVITY LOG JASPERSON BENOIT TUP PROJECT OCT. 30 - NOV.4, 1989
another Sin saiple froi 8S.75 to 86 ft.
Brush cutting was required to provide a trail for the ATV. The ATV Mas too siall to push over anything but the siallest spruce and alders and since the equipient box could only be carried long-way at rightangles to the trail the path had to be doubly wide. Also, in order to save the soft tires the saplings had to be cut flush rather than with a point, a proceedure that is lore laborious and tile consuiing.
Nov. l, 1989:Wednesday'location toved to the site of the foner trench f 88-09 where the depth of this trench was known to be over 18 ft. The drill reached 10 ft. 4 tiies, stopped by boulders in till but no samples were taken. Two holes in till were supled at Al 000 and A2 000, both located near trench 88-09. Site Al 000 is located 10 teters north of trench 88-09 and should have been lapped a bit further northwest than it was. Site A2 000 lies on a line near Al 000 betweei Al 000 and VI 180.
Al 000: overall depth 21 ft., 2 attests stopped by boulders: 5 saiples taken: 4 ft of till froi 7-11 ft. and l foot froi 11-12 ft. Also, 4 ft. froi 16-20 feet and l ft twice froi 20-21 feet. All of it till and all stopped by boulders.
A2 000: overall depth 26 ft. with 3 saiples froi 2 atteipts all in till and stopped by boulder tops, l saiple of l ft. froi 14-15 ft. and l saiple of S ft. fro* 20 -25 ft. and a third saiple of l ft. froe 25-26 ft..
Brushing out trails continued.
Nov.2, 1989: Thursday: repair parts picked up and installed to facilitate dealing with sticky clay and iiproving the hydraulic pipe-lifter. Moved location and coipleted Vector! 1; drilled, logged and bagged saiples at sites 180, 100 and 140 leters along vector.
VI 180: 4 atteipts to probe deeper than 15 ft. blocked by boulder tops. The last atteipt produced a l ft. saiple of till froi 14-15 ft..
VI 100: overall depth 65 ft.: consisting of 3-4 ft. of sand followed by clay to the 50 ft. depth and till thereafter to 65 ft. where the drill stuck in till. 2 1-ft. saiples were taken, the first froi 14-15 ft. (clay) and then froi 64-65 ft. (till).
VI 140: overall depth 48 ft. clay estiiated to 40 ft and the hole stopped in till at 48 ft. 3 saiples were taken: l fron 35-41 ft for 6 feet of clay and l froi 42-46 feet for 4 feet of till and a third froi 47-48 ft for l foot of till.
Brushing out trails continued.
Nov. 3, 1989:Friday: coipleted trail clearing and loved to Vector! 2. Also, drilled, logged and bagged
page 2.
ACTIVITY LOG JASPERSON BENOIT TUP PROJECT OCT. 30 - NOV.4, 1989
saiple V2 120 and part of V2 060.
V2 120: overall depth 23 ft. consisting of: 2 ft. of mskeg, 6 ft. of varved clay, 13 ft. of wet clay and 2 ft. of sand plus fine gravel. 2 trys: the first stopped tt 21 ft. and the 2nd at 23 ft. 2 1-ft. saiples were collected as 4 saiples: 2 clay saiples froi 20-20.83 ft. and 20.83 to 21 ft.; 2 sandy outwash till saiples froi 22-22.67 ft. and 22.67-23 ft.
V2 060: overall depth 50 ft. consisting of: 3 ft. miskeg, 10 ft. varved clay, 32 ft. of soft wet clay and 5 ft. of till. 4 saiples were taken: a 1-ft. clay saiple at 24-25H,, a 1-ft. clay saiple at 44-45ft., 3.5 ft. of till froi 45ft. to 48.5ft. and 1.5ft. of till froi 48.5ft. to 50ft. Soie of this work was coipleted on Satarday.
A trip had to be lade for extra gas.
Nov. 4, 1989:Satarday: coipleted hole V2 060 and V2 000; drilled, logged and bagged saiples atboth sites. Coipleted project: packed up and loved out.
V2 060: coipleted this hole and collected saiples.
V2 000: overall depth 48.5 ft. consisting of: 3 ft. of tuskeg, 5 ft. of varved clay, 38 ft. of soft clay and 2.5 ft. of till. 4 saiples were taken: a 5-ft. wet clay saiple at 41-46ft., (first try), a l ft. till saiple 46-47 ft. (first try), a 5 ft. net clay saiple at 42-47 ft. (second try), a 1.5 ft. till saiple froi 47-48.5 ft. (second try).
page 3.
F' 6* 3
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'JAN 10 '90.. 15:12 X "RAY ASSAY LAB LABORATORffiSA DIVISION OF SGS SUPERVISION SERVICES INC.
1885 LESLIE STREET ' DON M1US, ONTARIO M36 3J4 ' CANADA TEL: (416)445-5755 TELEX: 06-986947 FAXi {416)445-4152
O:Ff o
TO: JOHN K. JASPERSON182 THREE VALLEYS DRIVE DON MILLS, ONTARIO M3B 3L8
CUSTOMER No*
DATE SUBMITTED 21-NOV-89
40
REF. FILE 6350- Total pages l
7 HUMUS
AU PPBCU PPMZN PPM
METHODNADCPNA
DETECTION LIMIT 1. 0.5
20.
*** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS 90 DAYS *** AND REJECTS 30 DAYS FROM DATE OF THIS REPORT
DATE 19-DEC-89 CERTIFIED BYJean H,L. Opdetf/ack, Vi President Operations)
of the SGS Group (Societe Generate de Survai Hence)
•JfiN 10 '90 15=12 X-RftY fiSSAY LflB 416 445 4152
19-DEC-89 REPORT 10512 REF.MIE 6350-
P.2
PACE 1 OF 1
SAMPLE AU PPB CU PPM ZN PPM
DDK-A DDH-8 OOH-C DbH-D ODH-e
DDH-F ODH-G
15.016.022.014.021.0
19.022.0
40303030
SO 30
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (418)445-5755 Fax (416)445-4152 Tlx 06-986947of the SGS Group (Soci^t* Generate de Surveillance)
. Ministry of ' Northern
andxMffyes
Mining ActReport of Work{Expenditures,
Type of Work Performed
Instruction*
- Refer to Subsection 7709). the Minlno Act for assftssmftnt
Recorded Holder 900
Address /g- Telephone No.-ST-.
Work Performed By
geo M/C.Name and Address d Author (of Submission) Oat* When Work wis Performed From: .To:
All the work was performed on Mining Claim(s): Indicate no. of days performed on each claim. 'See Note No. 1 on reverse side
Mining Claim No. of Days Mining Claim No. of Days Mining Claim , No. o) Days
toMining Cwm No. o( Days
Mining Claim No. of Days
2-Mining Claim No. o) Days Mining Claim No. of Day* Mining Claim No. of Days Mining Claim No. of Days Mining Claim No. of Days
Mining Claim No. of Days Mining Claim No. of Days Mining Claim No. of Days Mining Claim No. of Days Mining Claim No. of Days Mining Claim No. of Days
Instructions Total days credits may be distributed at claim holder's choice. Enter number of days credits per claim in the expenditure days credit column (betow).____^__^______^__^_
Calculation of Expenditure Days Credits Total Expenditures_____
S 77*
Total Days Credits
Total Number of Mining Claims Covered by this Report of Work
15Mining Claims (List in numerical sequence). If space Is insufficient, attach schedules with required InformationMining Claim
Prefix
I^Tt—
L
^^
Numberlg j\,^ , 1
S'o' ^ tJ F ~L-
793-1&
9*9 tt rf
Expend. Days Cr.—3-^
12-
2-0
7,0
Mining ClaimPrefix
k/
Total Number of Days Performed
NumberExpend.Days Cr.
Total Number of Days Claimed
Certification of Beneficial Interest "See Note No. 2 on reverse side1 hereby certify that, at the time the work was performed, the claims covered of work were recorded in the current recorded holder's name or held under a ben by the current recorded holder.
in this rep eflcial inter!
Mining Claim | Expend.Prefix
ONtAHA:,
Number Days Cr.
—— R-f-eewoo n————— ArK U
MIMIMQ^LAM0 OSOLOGICAL SURVEY* fiS^nr;P n i W
rt st
Total Number ofMAY 16 1990
Dapj1p^ C E- 1 V E C**t* fT/ 9 ci
)Recon
Mining ClaimPrefix
mNumber
^
i mnj T
S SECTION
Expend. Days Cr.
ays to be Claimed at a Future Date
sd Holder or Agent (Signature)^ivT^, f" n/o-v-^rCertification Verifying Report of Work
l hereby certify thai l have a personal and intimate knowledge of the facts set forth in (he Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.Name and Address ol Person Certifying
-
For Office Use Only
678 (89/06)
Northern Development and Mines
Report of Work Mining Act (Expenditures, Subsection 77(19)},
2 O lIntti- Please type or print.- Refer to Subsection 77(19), the Mining Act for assessment work
requirements and maximum credits allowed under this Subsection.- Technical Reports, maps and proof of expenditures In duplicate
should be submitted lo Mining Lands Section, Mineral Development and Lands Branch.
Type of Work Performed Mining Division Township or Area
Recorded Holder
KProspector's Licence No.
Address. L 4-A
Telephone No.
Work Performed By
____p ^ * ** r y_ r+^r 1 1-^ v" ^ i ^ * -J l
Name and Ajroress of Author (of Submission;lA 6 O -
SC/VZ.& c/gjS-tUi K QA^T'—-
Date When Work was Performed From: , To:
l Mo. l Yr.9Myy |
6? /.
All the work was performed on Mining Claim(s): Indicate no. of days performed on each claim. 'See Note No. 1 on reverse side
Mining Claim No. of Days Mining Claim mg Claim No. of Days Mining Claim No. ol Days
Mining Claim No. of Days Mining Claim No. of Days Mining Claim No. of Days Mining Claim No. of Days Mining Claim No. of Days Mining Claim No. of Days
Mining Claim No. of Days Mining Claim No. ol Days Mining Claim No. of Days Mining Claim No. of Days Mining Claim No. of Days Mining Claim
i2FNo. of Days
Instructions Total days credits may be distributed at claim holder's choice. Enter number of days credits per claim in the expenditure days credit column (below).___ _______________
Calculation of Expenditure Days Total Expenditures
Total Days
Total Number of Mining Claims Covered by this Report of Work
-t^"2fl^
Mining Claims (List in numerical sequence). If space is insufficient, attach schedules with required informationMining Claim
Prefix
LL
UL
Number
?-?ito4-
f 92.2.0.T
9??-i-f#
99 v r^~
Expend. Days Cr.
&0
(pO
3t^o
Mining ClaimPrefix
Total Number of Days Performed /X\A/-tee?- 204 P-'
NumberExpend. Days Cr.
Mining ClaimPrefix Number
Total Number of Days Claimed
) 7 1*
Expend. Days Cr.
— R
MINI
M ning ClaimPrefix
ECl* V*
APR :
Number
EIVEDIB 1 V k l^
1 1990
^G LANDS SECTIO|
Expend. Days Cr.
N
Total Number of Days to be Clainwd at a Future Date
3^ 7^ JT^JCertification of Beneficial Interest 'See Note No. 2 on reverse side
1 hereby certify that, at the time the work was performed, the claims covered in this report of work were recorded in the current recorded holder's name or held under a beneficial interest by the current recorded holder.
Date
/^d/rAoRecordedJtaU*r or Agent (Signature)
&L)' \A*JfCertification Verifying Report o( Work
l hereby certify that l have a personal and Intimate knowledge ol the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.Name and Address of Person Certifying
Ofi/ -nvt ' 4/6.Telephone No.
- Z &f-IA 77Date CertHUdBy/Signature)J&L7- '"Received Starfip
For Office Use Only
Date App/oved as Recorded l Proftndial ManagerTltfitin&tftxK
878 (89/061
Cook Twp.s.R
LT0454CM!3 S Hi 5 8 iL 1045403
~ L"
L 9*0633 L 9960V ~- -i - " ~
LBB8428M. 89842
Ml W23 1 (111422 .l ^, L W4B4l5ji, I04S4I2
L 1025681 L.IO2S679
li ^3!f i
L 1026106 "1-1088107l, i rf J 3 t "*f l J !l*W l "
Maisonville" Twp.42A*6SE0a76 2.13201 BENOIT
i Ml* i C.LS Mi: r.v
THE. TOWNSHIP' OF
B E NO'1DISTRICT OF
'' COfHRANE
f LARDE.R LAKE/ ' MINING DIVISION -'' ' n-
SCALE'1-INCH: 40 CHAINS
LEGENDPATENTED LAND CROWN LAND SALE LEASESLOCAT&D LAND LICENSE OF OCCUPATION MINING RIGHTS ONLY SURFACE RIGHTS, ONLY' ROADS -
IMPROVED ROADS KIND'S HIGHWAYS RAILWAYS ' ' V - POWER . LINES y . MARSH OR MUSKE& MINESPATENTED S,R;O, ' CANCELLED
or
or c.s.
' Loc. L.O.
M.R.O. S.R O,
f.fr
NOTES
400' Surface rights reservation around all take* S.
rivers.
Gravel Reserve .Shown Thus;
400 1ron)age on BuMci Lake withdrawn from disposition for pfoposed summer resort development, "* File 164586
withdrawn from staking under Suction )f the Miging Act f ? -- ,) ;"'ot
^ 1 ( ' j' 1 ? ——
DATE OF ISSUE
FEBV
PLAN N0.-M.326";o-
MINISrr^Y Gf N ATURAL RESOURCES. ' ^ v t
5 AND MASHING BRANCH
tt/s-A
k)C/I CD
H
HO
CD
CD M Ol
Cook Twp.
12
LOCATIONMaisonville Twp.
oCD
42A08SEM76 2. I32C1 BENOIT El0 t Z C LAIMB.D.
p'
THE TOWNSHIP' OF
BENOIT'
DISTRICT OF fCOCHRANELARDER LAKE. MINING DIVISION'
1 T
SCALES i-iNCH" 40 CHAINSLEGEND
PATENTED LAND CROWN LAND SALELEASESLOCATED LAND 1 -LICENSE OF OCCUPATIONMINING RIGHTS ONI^Y - ; "SURFACE RIGHTS. ONLY'ROADS.'IMPROVED ROADS 'KIN^ HIGHWAYS ^RAILWAYS '^ ' ' .^ .POWER .LINES XMARSH OR MUSKEfeMINES ; ' ' PATENTE^) ! CANCELtfO
NOTES
400' Surface rights re*ervation around all lake* ^rivers. - ' v "'' - \ '
Grave;, Reserve Shown Thus;- ^^ —X * "
400' frontage on Build Lake, 'withdrawn V from disposition- for proposed sgmmer ^ resort development. ' * , File 164586 ' -,
withdrawn f rpm staking under Section , T )f the Miging Act t ? *^ o *"0j
File Date
.m
PLAN NO.- M .326^/0ONTARIO
MINISlKY GF NATuPAL RESOURCES. 3 ''', ' -' V
o AND MAPPING BRANCH
\ODm
'Hr
\
•s*'
. t.'. r^jj -*