1989 TILL SAMPLING USING A WINK SONIC VIBRA CORE DRILL€¦ · GEOLOGY * PREVIOUS WORK: See page 1...

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 .

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page 3.

page 3.

page 4.

page 5.

page 6.

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ACTIVITY UOG- OCt, Jo- ^O^oA //989

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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

,

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

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

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

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

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.

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.


January 23, 1990

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.


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-

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

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

}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)

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

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

^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.

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).

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.

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

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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- 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


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


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


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


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 sausseritized 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.


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.


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


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.


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.


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


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.


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.


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


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.


No thin section provided for description.


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.




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.




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.



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.


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.


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

xxxx

xxxx

XXXX XXX

XXXX XX

xxxx x

xxxx

XXXX XX

XXXX XX

xxxx

xxxx x

XXXX XX

XXXX XX

xxxx

XXXX XX

xxxx

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)


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)


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)


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)


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)


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)


1885 LESLIE STREET ' DON MILLS, ONTARIO M3B 3J4 * CANADATEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152


REPORT 8 2 8 X


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.


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)



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)


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


CUSTOMER No.

DATE SUBMITTED 9-May-89

40


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


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)



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 -*

1989 TILL SAMPLING USING A WINK SONIC VIBRA CORE DRILL€¦ · GEOLOGY * PREVIOUS WORK: See page 1...

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Transcript of 1989 TILL SAMPLING USING A WINK SONIC VIBRA CORE DRILL€¦ · GEOLOGY * PREVIOUS WORK: See page 1...