GEOL GEOCH CEOPH TNCH & DD€¦ · Golden Maverick Resources Corporation optioned 33 claims in two...
Transcript of GEOL GEOCH CEOPH TNCH & DD€¦ · Golden Maverick Resources Corporation optioned 33 claims in two...
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52N89SWe012 63.4833 BROWNSTONE LAKE 010
1985 GEOLOGY, GEOCHEMISTRY, GEOPHYSICS,TRENCHING AND DIAMOND DRILLING
REPORT OF GOLDEN TERRACE RESOURCES'
- RICHARDSON LAKE PROPERTY -
4DX Ltd. P.O. Box 279 Kleinburg, Ontario LOJ ICO
By: Carry K. Smith
Date: February, 1986
frem 4 DX Limited, RO. Box ? 7 C), K le'inburcj m Ontario IOJ ICO (416) 893-?03S
TABLE OF CONTENTS - PART l
1. SUMMARY l
2. INTRODUCTION 2A. LOCATION - 2B. OWNERSHIP AND STATUS 2
1. Owner 2Z. Interests 23. Property 34. Abandonments 3
C. HISTORY 3 D. PREVIOUS EXPENDITURES 1E. PREVIOUS EXPLORATION 1F. PRODUCTION 6C. OBJECTIVES 7
3. EXPLORATION 8 A. RECONNAISSANCE AND RESEARCH 8B. PROSPECTING 8C. GEOLOGICAL MAPPING 8D. GEOCHEMISTRY 9E. GEOPHYSICS 9F. TRENCHING 9
1. GEOLOGY 11A. REGIONAL GEOLOGY 11B. ROCK TYPES 11C. MINERALIZATION 16
5. GEOPHYSICS 23A. GROUND GEOPHYSICS 23
1. Methods 232. Results 23
B. AIRBORNE GEOPHYSICS 211. Methods 212. Data Presentation 273. Results 29
6. GEOCHEMISTRY 35A. METHODS 35B. DATA PRESENTATION 35C. RESULTS 36
7. DIAMOND DRILLING 37A. CORE HANDLING 37B. ASSAY PROCEDURES 37C. SUMMARY OF RESULTS 37
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Page #
8. FINANCE 12 A. EXPENDITURE SUMMARY 42
9. AGREEMENTS 44
10. STAFF 45
11. CONCLUSIONS 46
12. RECOMMENDATIONS AND 1986 BUDGET 48
13. REFERENCES 49
14. CERTIFICATE OF QUALIFICATION 50
TABLE OF CONTENTS - PART 2
1. LOCATION MAP, PROPERTY MAP (1937, 1985)
2. GEOLOGY MAP (1985)
3. GEOCHEM MAPS - Au, As (1985)
1. GROUND GEOPHYSICS1. NORANOA MAGNETICS MAP (1981)2. NORANDA l.P. MAP (1981)3. DOME ELECTROMAGNETICS
- REPORT AND MAP (1958-59)
5. AIRBORNE GEOPHYSICS1. AERODAT - REPORT AND MAPS (1985)
6. DIAMOND DRILL LOGS1. GOLDEN TERRACE (1985)2. CAMPBELL RED LAKE MINES (1959)3. COCHENOUR WILLANS GOLD MINES (1975)
7. UNDERGROUND SURVEY PLAN1. KOSTYNUK'S SHAFT, 40' LEVEL (1965)
8. ASSAY CERTIFICATES1. ROCK SAMPLES2. CORE SAMPLES3. SOIL SAMPLES
1. SUMMARY
The Richardson Lake Project of Golden Terrace Resources began by
optioning 33 claims from the Kostynuk brothers of Red Lake and
staking additional claims bringing the group total to 142. All
cash, stock and work commitments have been met by the company and a
HI N .S.R. is retained by the vendors.
A detailed airborne geophysical survey was completed over the pro
perty, followed by geological mapping, geochemical surveys and 1,520
feet of diamond drilling proximal to the Kostynuk's old shaft. The
best drill hole to date, K-6, returned values of 0.154 ounces gold
over 9.75 meters (32 feet) Including 0.287 over 3.35 meters (11
feet) within a section of quartz-arsenopyrite-serlcite alteration.
It was apparent from the drill results that a strong structural
focus of N.100W controls mineralization In areas so far Investi
gated and, further, that gold occurs in quartz-sericite-sulphide
alteration zones In brecciated iron formation that form at the
intersection of cross-cutting fracture zones.
Effective exploration tools Include humus geochem for detection of
gold-arsenic mineralization and l.P. for the detection of dissemi
nated sulphide alteration zones.
After a first phase program cost of approximately S215,000, It is
considered that the potential for the existence of an economic gold
deposit is considered high and therefore it is recommended that a
1986 budget of $500,000 be approved.
2. INTRODUCTION
A. LOCATION
The Richardson Lake property consists of 142 mining claims
Including 2 patented mining claims, 11 leased mining claims and
129 unpatented mining claims located in the north-central
portion of the Casummit Lake Area claim map and the south-
central portion of the Brownstone Lake Area claim sheet. The
claims are centered 115 km east-northeast of Red Lake and
immediately north of the past producing Jason Cold Mine. The
property is linked by a 40 km winter road, south to Selco's
South Bay Mine, where power and road access to Ear Falls may be
gained.
Lat.: 51 0 15' Township: Casummit Lake Area C-1751
Long.: 92 0 15' Brownstone Lake Area C-1742
N.T.S.: 52/N/08/W District: Kenora
Province: Ontario Mining Division: Red Lake
Map Reference: ODM Map 46f, Casummit Lake area.
B. OWNERSHIP AND STATUS
1. Owner
Golden Terrace Resources CorporationP.O. Box 1630New Liskeard, OntarioCanada POJ 1PO
2. Interests
The property is owned 1001 by Golden Terrace, subject to a
44 N.S.R., owing to the Kostynuk brothers of Red Lake -
the original vendors of 33 of the mining claims.
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3. Property
142 contiguous mining claims are numbered as follows:
Patented Claims - mining and surface rights
P-KRL 43655 (L.O. 13537)
P-KRL 43663 (L.O. 13319)
Leased Claims
L-K R L 43656 -43662 incl.
L-KRL 43664, L-KRL-375745
L-KRL 375692 and 375693
Unpatented Claims
KRL-697172-697188 incl.
KRL-788599-788601 incl.
KRL-814747-81484S Incl.
KRL-836301-836310 Incl.
4. Abandoments
No claims have been abandoned to date.
C. HISTORY
Golden Maverick Resources Corporation optioned 33 claims in two
groups from the Kostynuk brothers of Red Lake in an agreement
dated January 15, 1985. The company also staked 99 claims in
November 1984 and a further 10 claims in June 1985 as part of
the original agreement.
Golden Maverick amalgamated with Golden Terrace in September
1985 and the surviving company continued under the name of
Golden Terrace Resources Corporation.
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In March, 1986, as an amendment to the agreement, the company
optioned 2 further claims from the Kostynuks' near Mink Lake,
located 5 km west of the main 142 claim group.
D. PREVIOUS EXPENDITURES
Approximately S40,000 was expended by the company completing
preliminary field assessments, claim staking and surveys neces
sary to bring claims to lease. A further $30,000 was expended
on an airborne survey and various compilation reports. An
option payment of $15,000 was also paid on signing the option
agreement.
E. PREVIOUS EXPLORATION
Following the discovery of gold at Red Lake in 1925, prospect
ing activity extended east into the areas around Confederation,
Woman, Shabumeni, and Birch Lakes, where similar rock forma
tions were known to occur. Early In the spring of 1929, A.F.
Hewitt and J.A. Borthwick decided to prospect the Casummit Lake
area and were successful in discovering gold mineralization.
By 1933 a mine site was brought to production on the north
shore of Casummit Lake. Production from the Jason Mine was:
Cold Silver Total Ore Milled Years (oz) (oz) Valued) (tons) Gold Grade
19341936-381949-52
88814,83586,152
871,4338,268
30,673519,378
3,256,842
4,09443,249229,230
0.2170.3430.376
Totals 101,875 9,788 3,806,893 276,573 0.37 ave.
Richardson Lake Property
In or about 1932, Fred "Richle" Richardson discovered gold
mineralization on the north shore of Richardson Lake and
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optioned the property to R.C. Williamson and the Casey Mountain
Operating Syndicate who formed a new company on the property
called the Richardson Lake Syndicate. In 1934 the option was
dropped after a diamond drill program. Sections of core were
reported to assay from 0.04 to 0.628 ounces gold per ton over
widths of 0.9 to 5.3 feet. This showing is located on L8E,
about 30 meters north of the shore of Richardson Lake and is
briefly discussed later in this report.
In 1958 the Kostynuk brothers of Red Lake staked claims KRL
43655 and 43663 on the north shore of Richardson Lake. Later
in the year they discovered an outcrop of heavy arsenopyrite-
pyrite mineralization associated with breccia carrying signi
ficant gold values adjacent to a quartz-vein bearing visible
gold with minor galena and sphalerite.
The property was optioned to Campbell Red Lake Mines Ltd., in
1959 resulting in 9 drill holes totaling 739 m. Apparently the
grade or style of veins was not of corporate interest and the
option was terminated.
In 1962, Cochenour Willans Gold Mines Ltd., under a subsequent
option agreement, drilled 4 holes totalling 639 m on leased
claims KRL 43662 and 43664. Again, these results, although
significant were not of corporate interest and the option was
terminated.
During the period 1963-66, the Kostynuk brothers initiated a
small scale mining operation by sinking a 50 foot shaft on the
showing they discovered in 1958. Approximately 100 feet of
drifting was carried out on claim 43655 resulting in the mining
of 577 tons of rock and the on site milling of the quartz vein
material.
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In 197^ the Kostynuks completed several trenches in areas of
known mineralization including a new showing east of the Jason
Mine on the "south-east claim group".
During 1974-5, Cochenour Willans optioned this "south-east
group" and completed several trenches, magnetic and V.L.F.
surveys and 21 "x-ray" holes totalling 1892 m. Again, although
encouraging, the results were not on a par with the ore grades
being mined in Red Lake and the option was terminated.
Noranda optioned the property in 1981 and completed reconnaiss
ance geological mapping, magnetics and a small l.P. survey in
and about the Kostynuk shaft. Apparently the option was ter
minated when an attempt to renegotiate the terms failed.
In an agreement dated January 1985 and subject to a work com
mitment. Golden Maverick Resources acquired a 10(^ interest in
the property, which by way of amalgamation is now lOOt. owned by
Golden Terrace Resources (GTR).
F. PRODUCTION
The Kostynuks1 produced the following:
Gold Silver Ore Milled Gold Grad Years (oz) (oz) (tons) (oz/ton)
1963-66 1,126 102 577 1.95
(It should be noted that the ore was "hand cobbed" and, as
such, only the vein material was milled making the true grade
more likely to be on the order of 4.0 ounces to the ton.)
After milling, a gold button was made and shipped to Englehart,
Ontario, for collection by the Bank of Nova Scotia.
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C. OBJECTIVES
The objectives of the 1985 exploration program were to con
centrate initial efforts in the area of past work on this large
property and to begin upgrading the data base of the surround
ing areas. To this end a detailed airborne survey of the
entire property was completed. Most of the ground work was
concentrated in the vicinity of the Kostynuk shaft where de
tailed mapping, humus geochemistry and diamond drilling was
thought necessary to begin to develop an exploration model for
gold mineralization on a property-wide scale.
Previous exploration on the property had only dealt with the
classic high-grade quartz-vein hosted gold mineralization.
This 1985 program was designed to test the hypothesis that the
known gold mineralization occurred within stratigraphic shear
zones developed within sedimentary units dominated by slate,
greywacke, chert and jasperoid-magnetite-chert iron formation
within a greenstone sequence.
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3. EXPLORATION
A. RECONNAISSANCE AND RESEARCH
A property examination was carried out in the Fall of 1984 by
visiting the main showings at the shaft and on the "south-east"
group.
Samples of waste material taken from the rock dump at the shaft
revealed that the arsenopyrite-pyrite rich host rocks to the
quartz veins were running ore grade. No evidence could be
found that would suggest that this gold potential had been
tested In any direct way.
A sample from an arsenopyrite rich showing on the south-east
group ran 0.6 ounces gold over a narrow width.
B. PROSPECTING
In the Fall of 1985, Alex and Mike Kostynuk led a two day tour
of the old workings where they had prospected during the
1960's. They pointed out numerous localities where they had
panned gold or had gold "kicks". It became apparent that a
significant number of gold showings were located along a sinu
ous, yet property wide, iron formation.
C. GEOLOGICAL MAPPING
Mapping was confined to Noranda's previously cut grid and
served to check previous work and offer a more detailed geo
logical interpretation.
Selected outcroppings of sulphide mineralization within the
brecciated iron formation as well as previously known showings
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were assayed for gold. Grid geology is presented on Map RL85CI
at a scale of 1:2,500.
D. GEOCHEMISTRY
Geochemical sampling of the property was restricted to "A"
horizon humus sampling along existing grid lines. 485 samples
were taken at 25 metre intervals and assayed for gold and
arsenic. During a property examination, Goldfields Canada
sampled humus at 12.5 metre intervals and assayed for gold.
The combined data is presented on maps RL85GCI-Au and As in the
appendix.
E. GEOPHYSICS
A reconnaissance V.L.F. and magnetometer survey was carried out
over areas of known mineralization with negative results. The
only method to return valuable data so far is the 1981 Noranda
l.P. survey.
During 1981-1982, Noranda completed a magnetometer survey of
the cut grid area and a small I.R. survey of the grid south of
the base line. These results are presented in the appendix.
An airborne geophysical survey was carried out in 1985 by Aero-
dat Ltd. A total of 400 line kilometers of data were collected
at a nominal spacing of 100 meters. Equipment operated includ
ed helicopter borne 3-frequency electromagnetics, magnetometer,
VLF-EM and a radar positioning system. Data and equipment are
discussed in the geophysical section of this report.
F. TRENCHING
Limited trenching and stripping was carried out by the company
In the Fall of 1985. During a second or third visit by
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Coldflelds, Wajax water pumps were used to clean out existing
trenches along the lakeshore west of the shaft.
4DX Ltd. carried out l meter channel sampling of the cleaned
out trenches and assayed for gold. These results are discussed
in detail in the Mineralization section.
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H. GEOLOGY
A. REGIONAL GEOLOGY
All bedrock in the area Is Archean in age and is part of the
Birch-Uch! Lakes metavolcanic-metasedimentary belt within the
Uchi Subprovince. Rock types of a volcanic origin are pre
dominantly mafic In composition and have been correlated to
Thurston's Cycle II (Thurston, 1976) in the Birch-Uch! Lakes
area.
The overall metamorphic facies found in the rocks mapped to
date Is lower greenchlst with epidote and chlorite the most
common metamorphic minerals. Cordierite has been noted in some
of the mafic rocks logged in holes RL 3, 4 and 5, suggesting a
local hornblende-hornfels contact aureole.
The following is taken from Norwood's (1937) description of the
structure of the area:
"The structure in the basin of Casummit Lake is a syncline with its plunge to the west and south. Its irregular shape, and the variation in the strike of the axial plane, suggests that, rather than being a syncline formed by simple folding, it is a regional drag-fold syncline produced by forces acting as a couple, one from the west, the other from the east.
The various beds all have steep dips, usually about 80 degrees, although 70 degree angles were found near the centre of the syncline. In the vicinity of the Argosy (Jason) mine, there is some overturning along the north limb of the syncline. In places, beds of iron formation, greywacke and slate have been turned through 100 0 degrees so they dip 80 0 degrees north.
After the synclinal structure was developed and after the grandiorite and quartz diorite masses had been intruded, the rocks were sheared by the original east-west couple or by a similarly acting set of forces. The direction of the shearing, N75 0 E was controlled to a considerable degree by the general strike of the syncline and of the bedding along the limbs. As localized shear zones are rare and as no apparent faulting accompanied the deformation, it is probable that the amount of
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movement along any one plane was small and that the stresses were distributed more or less evenly throughout ali the rock formations. The force couple probably produced very minor strains in a N100W direction but as this direction was at high angles to both folded structures and bedding, any breaks that did occur were very minor. Later forces produced well-defined fractures along this direction and were responsible for the openings that contain the most Important veins so far discovered."
Horwood (1937) further describes the gold mineralization in the
Casummit Lake area and the Jason (Argosy) mine as follows:
"All the gold deposits of the area are similar to each other when considered from the standpoint of mineralogy. The same suite of minerals is present in all the deposits examined, although the relative amounts vary considerably, and in places different members of the suite are absent. On a structural basis the deposits may be divided Into two classes: (1) those that follow the early direction of shearing and displacement, and strike approximately N75 0 E (Richardson Lake North Pro perty), and (2) those that follow the later fractures and strike approximately N100 W (Richardson Lake East Property, Jason (Argosy) Mine."
Deposits of the first class occur in greenstones, sediments and
quartz diorite intrusive rocks..
"The deposits are mineralized fracture or shear zones, which contain one or more quartz veins of white to grey quartz. The veins and the included fragments of wall rock are minera lized with arsenopyrite, pyrite, sphalerite, galena, and vari able amounts of native gold. Veins that have been fractured and veined by a later generation of quartz contain larger amounts of gold than does the massive unfractured type. The limited amount of data available to date suggests that gold is present In appreciable amounts when arsenopyrite, sphalerite, and galena are the principal sulphides. Where pyrite alone is present values have been found to be low."
"Deposits of the second class have so far proved to be of more importance than the first type. The deposits are veins that find their best development in fractures along which there has been little actual displacement. In one or two places the rock In and along fractures has suffered some shearing. In almost every case the veins have been fractured and veined by a
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later generation of quartz. With the later quartz variable amounts of arsenopyrite, pyrrhotite, pyrite, chalcopyrite, sphalerite, galena and native gold were deposited. Carbonate, most of which is the iron variety, siderite, was brought in with both generations of quartz but before the introduction of the sulphide minerals. Inclusions of wall rock and the wall rocks themselves are altered and mineralized with arsenopyrite or pyrrhotite, and contain small amounts of gol-d. Pyrite, sphalerite, and galena are not as plentiful as the arsenopyrite and pyrrhotite; chalcopyrite is very rare. Cold seems to be present in greater amounts where there Is a concentration of arsenopyrite. This condition is best developed in the slates or in interbedded slates and greywackes."
"The wall rocks of both types of deposits have suffered some alteration. In the greenstones, siderite Is the principal mineral developed. The plagioclase has been altered and the hornblende so bleached that the resulting rock is much lighter in colour. Only very small amounts of chlorite or sericite have been formed. Variable amounts of arsenopyrite and pyrr hotite, and In some cases pyrite, have been developed in the altered rocks. In the sediments there has been some carboniti- zatlon and also some later sericitization. Both carbonitiza- tion and sericitization were more active processes in the slates than in the more massive greywackes. In general, the alteration is confined to a narrow zone, seldom over one foot along the wall of the veins."
"The deposits that trend N75 0E will probably have better continuity along the strike than those striking N100W. The former occur in zones that follow the regional direction of shear, whereas the latter are in fractures that cut at high angles across this older direction. The N100 W veins will tend to be lenticular and to pinch out, and they occur en echelon along the strike. Both types of deposits will probably persist to considerable depths. The most important vein at the Argosy (Jason) Mine has been developed to a vertical extent of 500 feet and does not appear to have varied. As the rock forma tions dip at very steep angles there should be little change from a structural stand point."
Production from the Jason (Argosy) Mine during the time periods
1935-1940 and 1946-1952 totalled 113,827 oz gold and 9,788 oz
Ag from 311,801 tons of ore grading 0.365 oz/T gold.
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B. ROCK TYPES
Mafic to Intermediate Volcanics
The most common mafic rock on the claim group is andesitic in
composition. The rock varies from massive to tuffaceous to
highly sheared schist. Massive varieties often have a weather
ed surface showing "chicken track" textures. Rare pillowed
structures indicate tops to the north. Typical, unaltered
andesite is massive, fine-grained, olive green to dark green
and is made up of 40 to 50*2, andesine, 50 to 601 hornblende and
minor amounts of epidote and magnetite. Owing to regional
shearing and metamorphism, the andesine and hornblende are
generally, more or less, altered to epidote, sericite, car
bonate and chlorite. Distinguishing an altered, silicified
andesite from a dacite Is often very difficult in the field,
resulting in the two units being mapped together for "first
pass" simplicity.
Basalt appears In lesser amounts along the north-west shore of
Richardson Lake and In some drill cores. The rock has the
appearance of a typical basalt and is dark green, massive,
weakly foliated with 40 to 50"i andesine, 50 to 601 hornblende
with minor epidote and magnetite. Alteration is in the form of
epidote, sericite, carbonate and chlorite. A coarsening adjac
ent to diorite sills make field recognition difficult.
Intermediate to Felsic Volcanics
The west and central portion of the property Is dominated by a
thick wedge of pillowed and massive dacitic volcanics. The
rocks are light to medium green, siliceous and often pillowed
with magnetic rims. The units are typically rhythmically
layered pillowed and non-pillowed making it very difficult to
distinguish from silicified andesites.
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Narrow bands of sericite schist, often sulphide rich, have been
noted in both areas of significant gold mineralization so far
detailed. The rocks may be altered dacites, but for the most
part, may be referred to as quartz-sericite-sulphide felsic
tuffs and are generally auriferous.
Sediments
A band of greywacke, slate and conglomerate, which so far
appears to be Intercalated with volcanic flows, outcrops along
the north-west shore of Casummit Lake and along the west and
north-west shore of Richardson Lake. The slates, argillites
and wackes are dull grey to black, often graphitic, weakly
magnetic and display a high degree of soft sediment deforma
tion. The conglomerates are often sheared to the point of
having the quartz and chert pebbles alter to quartz sericite
schist.
Iron Formation
Bands of iron formation vary greatly in composition, facies and
mineralization. Bands may be a meter thick or 20 to 30 meters
thick. Varieties of chert and magnetite. Jasperoid, silicate
and arsenopyrite rich facies have been noted on a property wide
scale. It Is believed that thinly bedded chert-sulphide iron
formation gave rise to the considerable thickness of breccia in
and about the "shaft zone". Assays of over 1 ounce gold per
ton have been returned from this material (without quartz-vein
enrichment) therefore making it a high priority exploration
target.
Intrusive Rocks
A diorite sill complex forms an eastward thinning wedge that
conformably intrudes the contact between volcanics and grano-
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diorite. The rock has the appearance of a typical diorite and
is massive, may be weakly foliated, often weakly magnetic, and
has a dark green to medium grey "salt and pepper" texture. The
rock is 6(H andesine, 404 hornblende and displays epidote-
chlorite alteration. The sill is often gradational to both the
mafic volcanics and the later granodiorite.
A mass of granodiorite intrudes the volcanic sequence north
east of Richardson Lake and spans most of the northern portion
of the property. This grey rock is coarse grained and consists
of andesine, orthoclase, quartz and biotite. Some phases are
very low in potash feldspar and may be better classified as
quartz diorites. The rocks are generally gneissic, display all
the late phase structural jointing, fracturing and faulting
seen in the volcanics and are weakly mineralized by chalco
pyrite, arsenopyrite, pyrite and gold. In general, the mass
dips southerly at 60 to 75 0 .
C. MINERALIZATION
The 1985 program looked principally at two zones of gold
sulphide mineralization:
The "Shaft Zone" is located at the base line between L13E and
L14E. Cold occurs within both quartz veins developed in highly
fractured, brecciated, altered cherty metasedimentary rocks
ranging from slaty material to jasperoid iron formation and
within a quartz-sulphlde-sericite alteration zone developed
within the breccia. The zone, which is an excellent l.P.
anomaly, strikes west-southwesterly across the property for 800
meters. The correlation with gold mineralization and associ
ated arsenopyrite, pyrite and l.P. strongly suggests lateral
continuity for potentially economic strike lengths. Limited
drilling of this zone has revealed a significant amount of
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structural complexity and the probability of epigenetic con
trols on ore focus.
A level plan was made available for the underground workings
carried out by the Kostynuks1 during the time period 1963-1966.
The plan (see appendix) reveals a rotation of the ore In a
manner consistent with dextral shearing. It was postulated
during the field mapping that a low angle deformation zone of
mylonite displaying ductile-dextral sense shearing spans the
property, intersecting the shaft zone and giving rise to the
breccia units. Samples of the non-vein material "waste rock"
from the Kostynuks1 workings found on the shaft dump returned
the following assays from sulphide banded breccia:
Ounces Cold/Ton
0.153
0.817
1.270 (All samples are checked, see
0.087 certificate 24850 in appendix)
1.700
0.450
The "Arseno-Zone" is a north tending trench located just west
of L10E that exposes about 11 meters of heavy arsenopyrite and
pyrite mineralization in silicified dacites and quartz-sericite
schist. It is suspected that this zone is in fact a N10 0W
structure cross-cutting favourable geology and not a strati
graphic target, unless rotation of 90 0 has occurred. Three
drill holes designed to sample the zone failed to encounter any
mineralization of significance. Initial trench sampling re
sults are shown on sketch "Trench 9+80E".
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NTRENCH 9+80E
Channel Sampling ' '
i ^i \.022 ~~~'~\~~7r
1.008 \ **
\.030 \ is
.002 ^6
Felsic Tuffs . 066 \very siliceous, \5-30* pyrite andnr d arsenopyrite, .uotstringer and disseminated
.048
.020 — "Qtz-Sericite-Py- Aspy-Scnist15-20* pyrite. -092 and arsenopyrite (aspy neediest
.016
.094
^average grade - .056 / 7 metres
\ Diorite, massive** minor sulphides
\
\ l5\ Dacite, foliated,\ J-70% pyrite, /% arsenopyrite
^ minor intermixed Felsic Tuffsx^ Type Sample "A", -.002
"~ "" T* "" "^) 2 li/ y -022
J7\"~"^O3 ]T x .010/ j.- — ———
^M 3t H ! . 026^4- it ' Type Sample "B",
\M\ W/ .004 -' 05-^ — — TTT 1" '
\w \ u/ ; .044v \ -*-^^ r ^M l 5 ^(7 7 7 .052 Type Sample "C", \\ 3t j- f - .070M W/ -304
V\ M// -046
- Sericite Schisttrench hurried
*average grade - .079 / 6 metresincluding - .MB / 2 metres
4
all samples taken by continuous . -channel - chip and assayedgold by fire-assay method.
for '" metr.30123
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Three other zones were sampled or geochemical!/ tested, but
were not part of the drill program.
A trench at L8E, about 2+20S, is in fact the original Richard
son Lake discovery zone. The zone was explored in 1931 by
Casey Summit Cold Mines for 30 feet in surface workings and
for 210 feet in six short drill holes. According to Horwood
(1937) the results are as follows:
"The fracture zone strikes S80 0E, dips 60 0S, and contains veins up to 30 inches In width. According to Furse, one pit has two quartz veins, each of which averages about 1 foot in width. They are about 5 feet apart. Pyrite, sphalerite, and some galena are associated with wall-rock Inclusions In the vein, and specimens with native gold have been reported. Sec tions of core assayed form 0.04 to 0.628 ounces of gold per ton over widths of 0.9 to 5.3 feet. At the time of the writer's examination, in July 1936, the trenches had caved in. Since that date, diamond drilling has Indicated a continuation of the vein structures."
Two samples taken by the company returned trace and 0.180 oz.
gold.
In 1932 Furse reported that he visited another trench located
approximately 300 m east north-east of this zone (10+75E,
1+50S) along the same stratigraphic horizon.
"He reported four irregular quartz stringers ranging in width from 3 inches to 1 foot in a band about 5 feet wide. The strike is east and west, and the dip about 60S. Thin streaks of altered wall rock in the veins are well mineralized with pyrite, sphalxerite, galena, and a little arsenopyrite and native gold. Bands of wall rock between veins are carbonated and pyritized. The quartz of the veins has been fractured and cemented by very fine quartz, which carries arsenopyrite, gold, tourmaline, chlorite, and carbonate. No assay results are available."
In 1962, Cochenour Willans Mines Ltd., under an option agree
ment with the Kostynuk brothers, drilled 4 diamond drill holes
- 19 -
totalling 639 m in this zone. The results of this work is
unknown.
Work by the company using Wajax pumps and considerable "muck
ing" revealed that the 4 Irregular quartz stringers in trench
10+75E were in fact l quartz vein displaying intense deforma
tion including "S" and "Z" folding and dips ranging from flat
to vertical. Further, the unit hosting the veins is believed
to display dextral-ductile shearing suggesting the presence of
a mylonite deformation zone (see trench sketch 10+75E).
The third zone of anomalous gold is, in fact, a soil geochem
anomaly (L16E,S of BL.) greater in magnitude than results
gathered in and about the high grade surface dump at the shaft.
One small outcrop on strike with the anomaly suggests a north-
south strike to the possible bedrock source. Although I.R. was
carried out over the anomaly, the survey line ran over and
parallel to the gold values thereby making subsurface data
unreliable. It was decided not to drill this target until
better geophysical data could be gathered. It should be noted
that this gold target is the highest geochem anomaly on the
property. Is a completely new discovery and has a strike length
of 150 meters open to the south where it passes Into Richardson
Lake (see geochem map for Au).
Areas of interest, but receiving little or no work, are briefly
described as follows.
Some northerly striking black "chatter" quartz veins were
located approximately 100 meters west of the extreme south-west
corner of Richardson Lake. Horwood reports in 1936:
"...a quartz vein in a poorly developed fracture in greenstone has been exposed at intervals by trenching for about 195 feet. It is very irregular and changes in strike from N.35 0 W at the south end to north-south at the north end. It dips about 45 0 W
- 20 -
TRENCH 10+75E Channel Sampling
N
Results - Au161718192021222324
.164
.026
.010
.002
.006
.016
.010
.008 trace
25 - .03626 - .00827 - .00628 - .00229 - trace30 - .00231 - trace32 - trace
___o i a 3
-21-
and has a maximum width of 26 inches. Except for one high
assay, the results from eight samples averaged 0.216 ounces of
gold per ton. Visible gold has been reported from surface
workings."
The company sampled one of the trenches that was not too over
grown and returned 0.068 oz/ton and several trace gold assays.
Old trenching located Immediately east of the north arm of
Casummit Lake has not yet been Investigated. Horwood reports:
"A considerable amount of trenching was done in 1932 and again In 1936 in an attempt to locate the possible northward extens ion of the veins that are being worked on the Argosy property. This work, which was supplemented by a diamond drilling pro gramme after the writer's examination, proved to be unsuccess ful.
Two veins In the southern part of claim 9,852 have been explor ed in trenches and pits. The one to the east, termed No. 6 by the Argosy company. Is a network of small quartz veins, one of which has a maximum width of H inches, in a 3-foot zone in greenstone. The fracture, which is poorly developed and con tains quartz veins for a length of about 30 feet, pinches out to the north and south. The vein to the west, termed No. 7, has been exposed in trenches and one pit for approximately 200 feet. It is in two separate sections, a south lens and a north lens. The south lens is 80 feet long on the Ellen property (CTR) and has a maximum width of 22 inches; it contains a s mall amount of arsenopyrite and. In a few places, small specs of native gold. In the pit It dips 60 0W. The north lens is 100 feet long with a maximum width of 2 feet. It pinches and strikes off to the southeast at the south end and disappears under overburden at the north end. Work was discontinued In the autumn of 1936 and no assays are available."
- 22 -
5. GEOPHYSICS
A. GROUND GEOPHYSICS
No ground geophysics were carried out by the company during
1985. However, work by Noranda in 1981 carried out on the
current cut grid included a magnetometer and limited l.P.
survey. The data was replotted and tied Into our new coordin
ate system (see appendix).
1. Methods
A dipole-dipole l.P. survey was carried out at 12.5 or 25
meter spreads reading nzl-4 in the 4 and 25 Hz range. A
total field magnetic survey was carried out using a GP70
instrument over most of the grid.
2. Results
As can be seen by the l.P. Survey Plan of Percent Frequen
cy Effect at 1 =2, the mineralization in and about the
shaft zone is very responsive to the l.P. "effect". It is
recommended that a 50 m line spacing at 25 meter spreads
be carried out along with some east-west lines over the
arseno-trench and the L16E geochem anomaly.
The magnetics show a conspicuous linear following the
north-west lake shore and converging upon the shaft zone
where It fades out. This may suggest the trace of a
magnetic iron formation that has a easterly facies change
from oxide to sulphide or is structurally broken up by
Intersection with a mylonite zone.
The granodiorite volcanic contacts are also conspicuous
across the map.
- 23 -
B. AIRBORNE GEOPHYSICS
The following Is taken largely from Aerodat's "Report on Com
bined Helicopter-Borne Magnetic and Electromagnetic Survey,
Richardson Lake Project, Ontario" and dated September, 1985.
1. Methods
From June 30 to July H , 1 985, a total of 400 line kilo
meters of data were collected at a nominal spacing of
100 meters. Equipment operated included a 3-frequency
electromagnetic system, a magnetometer, a VLF-EM system
and a radar positioning system (described later in this
section).
The index map below outlines the survey area. In order to
optimize response, flight line direction was varied accor
ding to client's instructions - in the following manner:
a) Block A - east-west; b) Block B - north-south; c) Block
C - approximately N 40 degrees west.
- 24 -
The helicopter used for the survey as an Aerospatiale
A-Star 350D owned and operated by Maple Leaf Helicopters
Limited. Installation of the geophysical and ancillary
equipment was carried out by Aerodat. The survey aircraft
was flow at a mean terrain clearance of 60 meters.
Electromagnetic System
The electromagnetic system was an Aerodat 3-frequency
system. Two vertical coaxial coll pairs were operated at
932 and 4527 Hz and a horizontal coplanar coil pair at
4147 Hz. The transmitter-receiver separation was 7
meters. Inphase and quadrature signals were measured
simultaneously for the 3 frequencies with a time constant
of 0.1 seconds. The electromagnetic bird was towed 30
meters below the helicopter.
VLF-EM System
The VLF-EM system was a Herz Totem 1A. This instrument
measures the total field and quadrature component of the
selected frequency. The sensor was towed in a bird 12
meters below the helicopter. The transmitting station
used was NAA (Cutler Maine, 24.0 kHz) for all lines.
Magnetometer
The magnetometer was a Geometrics C 803 proton precession
type. The sensitivity of the instrument was 1 gamma at a
0.5 second sampling rate. The sensor was towed in a bird
12 meters below the helicopter.
Magnetic Base Station
An IFC proton precession magnetometer was operated at the
base of operations to record diurnal variations of the
earth's magnetic field.
- 25 -
The clock of the base station was synchronized with that
of the airborne system to facilitate later correlation.
Radar Altimeter
A Hoffman HRA-100 radar altimeter was used to record
terrain clearance. The output from the instrument is a
linear function of altitude for maximum accuracy.
Tracking Camera
A Ceocam tracking camera was used to record flight path on
35 mm film. The camera was operated in strip mode and the
fiducial numbers for cross-reference to the analog and
digital data were Imprinted on the margin of the film.
Analog Recorder
An RMS dot-matrix recorder was used to display the data
during the survey. In addition to manual and time
fiducials, the following data was recorded:
Channel Input Scale
O Low frequency inphase 2 ppm/mm
1 Low frequency quadrature 2 ppm/mm
3 High frequency inphase 2 ppm/mm
3 High frequency quadrature 2 ppm/mm
4 Mid frequency inphase 4 ppm/mm
5 Mid frequency quadrature 4 ppm/mm
6 VLF-EM total field 2.5%/mm
7 VLF-EM quadrature 2.5%/mm
13 Altimeter (500 ft. at 10 ft./mm
top of chart).
14 Magnetometer 5 gamma/mm
15 Magnetometer 50 gamma/mm
Digital Recorder
A perle DAC/NAV data system recorded the survey on
- 26 -
magnetic tape. Information recorded was as follows:
Equipment Interval
EM 0.1 seconds
VLF-EM 0.5 seconds
Magnetometer" 0.5 seconds
Altimeter 0.5 seconds
MRS III 0.5 seconds
Radar Positioning System
A Motorola Mini-Ranger (MRS III) radar navigation system
was utilized for both navigation and track recovery.
Transponders located at fixed locations were interrogated
several times per second and the ranges from these points
to the helicopter measured to a high degree of accuracy.
A navigational computer triangulates the position of the
helicopter and provides the pilot with navigation Informa
tion. The range/range data was recorded on magnetic tape
for subsequent flight path determination.
2. Data Presentation
See appendix for the maps indicated in the following
sections.
Base Map and Flight Path
A photomosaic base at a scale of 1:10,000 was prepared by
enlargement of aerial photographs of the survey area.
The flight path was derived from the Mini-Ranger radar
positioning system. The distance from the helicopter to
two established reference locations was measured several
times per second, and the position of the helicopter
calculated by triangulation. It is estimated that the
flight path is generally accurate to about 10 meters with
- 27 -
respect to the topographic detail of the base map. The
flight path is presented with fiducials for cross-refer
ence to both the analog and digital data.
Electromagnetic Profile Maps
The electromagnetic data was recorded digitally at a
sample rate of 10/second with a time constant of 0.1
second. A two stage digital filtering process was carried
out to reject major sferic events, and to reduce system
noise.
Local sferic activity can produce sharp, large amplitude
events that cannot be removed by conventional filtering
procedures. Smoothing or stacking will reduce their
amplitude but leave a broader residual response that can
be confused with a geological phenomenon. To avoid this
possibility, a computer algorithm searches out and rejects
the major sferic events.
The signal to noise ratio was further enhanced by the
application of a low pass digital filter. It has zero
phase shift which prevents any lag or peak displacement
from occurring, and it suppresses only variations with a
wave-length less than about 0.25 seconds. This low
effective time constant permits maximum profile shape
resolution.
Following the filtering processes, a base level correction
was made. The correction applied is a linear function of
time that ensures that the corrected amplitude of the
various inphase and quadrature components is zero when no
conductive or permeable source is present. The filtered
and levelled data were then presented in profile map
form.
- 28 -
The inphase and quadrature responses of the coaxial 4527
Hz, and coplanar 4147 Hz configurations were plotted as a
two colour overlay on a mylar base.
Total Field Magnetic Contours
The aeromagnetic data was corrected for diurnal variations
by subtraction of the digitally recorded base station
magnetic profile. No correction for regional variation
was applied.
The corrected profile data were Interpolated onto a regu
lar grid at a 25 m true scale Interval using a cubic
spline technique. The grid provided the basis for thread
ing the presented contours at a 10 gamma Interval.
The aeromagnetic data hs been presented with flight path
and electromagnetic anomaly information on the base map.
VLF-EM Total Field Contours
The VLF-EM signal from NAA (Cutler, Maine) was compiled in
map form.
The mean response level of the total field signal was
removed and the data was gridded and contoured at an
interval of 2%.
The VLF-EM total field data has been presented with flight
path and electromagnetic anomaly information on the base
map.
3. Results
Magnetics: The principal magnetic anomalies appear to be
associated with the metasediment* within the volcanic
series and are most likely due to iron formation.
- 29 -
A strong, northeasterly magnetic trend, In the southeast
corner of the survey, appears to be at odds with the
geology. However, iron formation was mapped near the
north end of this trend. Northwesterly magnetic trends,
in the northeast corner of the area, correspond to meta
sediments along the granite/volcanic contact. Iron
formation was mapped along this sedimentary zone to the
southeast of the survey.
Similarly, the magnetic highs northwest of Casummit and
Richardson Lakes appear to relate to metasediments and
therefore are likely from iron formation. Ultramafics are
not Indicated on either of the geologic maps.
A northwesterly magnetic trend, also apparent from the
negative inphase response, passes through the area of the
McMarmac Mine property.
The magnetic trends suggest a lithologic control with some
possible structural displacements along the northeasterly
lineament. Most likely, these are vertical displacements.
Granitic Intruslves have complemented faulting to give a
segmented appearance to the magnetic trends.
VLF - Total Field: Moderate to high lake bottom conduc
tivities appear to be the major influence on the total
field response. A few exceptions exist - the extreme
northeast corner of the survey and the east-central edge,
the latter falling along a coincident magnetic/electro
magnetic trend - but there is little or no evidence that
structure plays an important role in controlling the VLF
response.
Electromagnetics: The electromagnetic data shows two
bedrock conductive zones of moderate conductivity In the
- 30 -
eastern part of the survey. Both are associated with
magnetic trends. There fs, in addition, a weak, possible
bedrock conductor associated with a minor, secondary
magnetic high. The central part contains an east-west
trending zone of low apparent conductivity lying beneath
Richardson Lake near its south-eastern shoreline. A
second possible conductor, just east of Casummit Lake,
coincides with a power line - portrayed on the topographic
maps - Into the Jason Mine property. Although this is
probably inactive, the wires are quite good conductors if
they are still on the poles. This should be checked on
site.
Throughout the surveyed area, the magnetics have caused
strong, negative inphase responses. Where conductivity is
evident - from the quadrature response - it is very weak,
based on the ratios of high to low frequency response.
There is little or no possibility that bedrock conductors
have been missed due to Inphase suppression.
Lake bottoms and some swamp covered areas show weak con
ductors, generally not strong enough to mask the inphase
negative peaks. Although considerable sferic activity was
recorded during the survey, the average amplitude was
quite low so that the sferic filtered data is clean.
Anomaly l - (Lines 1250 to 1360): This anomaly is a
multi-banded conductive zone that lies along a strong
northwestern magnetic trend. Apparent conductivity is
classed as moderate but has probably been affected by
inphase suppression (see for example, the response on line
1250). The probable extension of this conductive zone to
line 1400 (and beyond) Is masked by the effect of strong
magnetic peaks with resultant inphase negatives. Although
this extension may be interpreted as a bedrock conductor,
- 31 -
apparent conductivities would have to be lower than those
along the zone to the south.
The strongest response was recorded on Line 1280 where at
least three separate bands were registered. This con
ductive zone Is most likely an iron formation along the
western contact of a wider, northeasterly trending meta
sediment.
Anomaly II - (Lines 1590 to 1600); This anomaly resembles
Anomaly l in most of its characteristics except that the
coincident magnetic trend is not as strong. Highest
amplitudes and apparent conductivities were recorded on
Line 1600 so one can assume that the zone continues to the
north-west, beneath Brownstone Lake. Like Anomaly l,
Anomaly II appears to lie along the western contact of a
northwest trending metasediment.
Anomaly HI - (Lines 2020 to 2080): This appears to be a
single, east-west trending conductive band. It lies along
the northerly contact of a group of magnetic highs near
the southeastern shore of Richardson Lake and extends
beneath the lake. The western end of this conductor
terminates against the northeasterly trending structural
lineament (mapped as a shear by Furse). Both geologic
maps suggest that the anomaly is underlain by basic vol
canics but sediments have been mapped in the vicinity.
Anomaly IV - (Lines 2010 - 2020): This is classed as a
possible conductor that has been affected, at least on
Line 2010, by strong magnetic highs. It may be a southern
complement to Anomaly 111. The east-west lines flown over
the area showed a weak conductive response over a small
lake with the attributes of a conductive lake bottom
sediment. Again, as with Anomaly III, the area Is under-
- 32 -
lain by basic volcanics, but Iron formation has been
mapped in the immediate vicinity.
Anomaly V - (Lines 1190 6 1200): This anomaly consists of
two very weak responses that are coincident with a short,
northerly trending, secondary magnetic peak. Magnetic
data suggests a minor, northesterly trending structural
break to the north, whereas the geologic maps indicate
that this Iles close to Iron formation. There is no
obvious tie-in between this possible bedrock conductor and
the strong, northeasterly trending magnetic zone to the
east.
Anomaly VI - (Lines 2070 to 2100): This conductor follows
along cut lines leading to the former Jason Mine property.
Department of Natural Resources topographic maps show a
power line, probably abandoned, along this route. Al
though 60 cycle noise was not noted on the analog records,
the line need not be live for the existing wires to act as
conductors. A ground check should be made in view of the
proximity of this apparent conductor to this property.
Comments:
Although the area of the Jason Mine did not produce an
apparent bedrock conductor, bedrock response was regis
tered on the electromagnetics in the form of a negative
inphase trend. Lacking any specific anomaly, it is sug
gested that the Iron formation around Casummit Lake be
carefully examined, particularly In the vicinity of the
postulated northeast structure. It would not, however, be
possible to make a recommendation on this without know
ledge of the form of mineralization present at the Jason
property.
- 33 -
Recommendations:
Anomalies l, II, and III are recommended for ground
follow-up. Standard reconnaissance ground electromagnetic
and magnetic methods would be adequate. Induced polariza
tion might be considered for Anomaly III and possibly IV,
if III proved encouraging. Anomaly V, classes as a poss
ible bedrock conductor, would also be an I.R. target.
Anomaly VI should be checked for the presence of abandoned
power lines.
6. GEOCHEMISTRY
A. METHODS
In the Fall of 1985, 485 humic samples were collected from the
existing grid, at 25 meter Intervals and submitted for Instru
mental Neutron Activation Analysis. The following description
of the INAA technique is quoted from "Biological Prospecting
for Cold with Reference to Some Canadian Cold Deposits", by
E.L. Hoffman and E.J. Brooker, 1983:
"Samples of approximately 20 - 50 grams of material are col lected, screened (-30 mesh), dried and macerated. Eight grams of this material are brlquetted In a press at 30,000 P.S.I., to form a 40 mm briquette about 6 mm thick. Briquettes are then batch irradiated and thermal or epithermal neutron fluxes, depending on the elements besides gold that are to be deter mined. The irradiated samples are allowed to decay, from four days to one week, after which they are counted singly, using a hyper-pure germanium detector linked to a multichannel analyzer - computer system. Detection limits may vary with the type of material being analyzed, but will usually be in the 0.1 to 1 ng/g range."
Samples were dried in the field and shipped to Nuclear Activa
tion Services Limited in Hamilton, Ontario, and analyzed for
gold and arsenic.
B. DATA PRESENTATION
The data is presented on Maps RL85GC1-AU and As. Contour
intervals were randomly picked to emphasize stratigraphic
correlation. Surveys carried out by Coldflelds during a pro
perty examination were requested by the company so that their
results could be compared and incorporated with our own.
- 35 -
C. RESULTS
A geological bias was incorporated during the Interpretation of
results. General trends of gold mineralization is directly
correctable to areas of known sulphide showings. Arsenic
shows property wide trends and correlates to the presumed
strike direction of the rock units. High gold values were
associated with the arseno-zone, shaft zone and L16E east
zone.
Generally, the use of the exploration techniques confirmed the
presence of all known gold showings and zones and should there
fore be considered on a property-wide scale.
- 36 -
7. DIAMOND DRILLING
A drilling program to test two areas of known mineralization was
completed in January 1986. A total of 463.4 meters (1,520 ft.) in
10 holes were contracted to N. Morissette Diamond Drilling of
Halleybury, Ontario. Total costs of $94,133 or $203 per meter
C$62 per foot) were Incurred (Including sampling and geological
support).
A. CORE HANDLING AND SAMPLING PROCEDURES
All holes were logged at the drill camp-site. The core has
subsequently been removed from the camp site and is presently
stored on the property at 16+50E, 1+65S (on the lakeshore).
All material of Interest was split and assayed for gold by the
fire assay method.
B. ASSAY PROCEDURES
Assay splits and rock samples were shipped to Custom Fire
Assaying Ltd., in Cochenour (Red Lake), Ontario, and assayed
for gold in ounces per ton. Consistently excellent "turn
around times" were achieved. A check of assay results was
carried out by Bell-White Analytical Laboratories Ltd., In
Hafleybury, Ontario. A heavy mineral separates "pulp and
metallic" test did not Indicate any problems from the free gold
"nugget effect" associated with some high grade deposits.
C. SUMMARY OF RESULTS
Drill sections, plans and logs are located in the appendix
attached.
- 37 -
RL-1
Commenced and completed: December 13, 1985ObjectiveCollarAzimuthDipLengthGeology
Assay Results (Au)
to test shaft zone 13+10E, 0+60S O0 (north) -45 0 47.96 m 0.00 - 8.84 8-84 - 21.18 21.18 - 33.00 33.00 - 37.00 37.00 - EOH
33-0 - 34.0 34.0 - 35.0 35.0 - 36.0
OverburdenSlate-Argillite-WackeBrecciaAlteration zoneBreccia
Custom Fire Assays, Au (oz/ton)
Ol0.080.14
BellWhite(oz/ton)
670930.0780.146
RL-2
Commenced andObjectiveCollarAzimuthDipLengthGeology
completed: December 15, 1985 to test shaft zone 13+85E, 0+40S O0 (north) -45 0 54.57 m 0.00 - 4.00 4.00 - 11.63 11.63 - 15.15 15.15 - 40.00 40.00 - 40.50 40.50 - 53.23 53.23 - EOH
Assay Results
RL-3
OverburdenBrecciaSlate-Argillite-WackeBrecciaAlteration zoneBrecciaDiorite
no assays of Interest.
Commenced and completed: December 17, 1985ObjectiveCollarAzimuthDipLengthGeology
Assay Results
to test 10E arseno-trench zone9+72E, 1+35.5SO0 (north)-45 060.05 m0.00 - 6.52 Overburden6.52 - EOH Intermediate Volcanicsno mineralization encountered.
- 38 -
RL-4
Commenced andObjectiveCollarAzimuthDipLengthGeology
Assay Results
RL-5
completed: January 11, 1986to test 10E arseno-trench zone9+76.5E, 0+86SISO 0 (south)-45 045.72 m0.00 - 1.831.83 - 13.0713.07 - 13.50
13.50 - 34.83 34.83 - EON
Overburden Mafic Volcanics Quartz vein (py, gal, cpy, po)Intermediate Volcanics Mafic Volcanics
no assays of interest.
Commenced and completed: January 11, 1986ObjectiveCollarAzimuthDipLengthGeology
Assay Results
RL-6
to test 10E arseno-trench zone 9+51.SE, 0+86S 25m due W of RL-4 180 0 (south) -45 0 45.72 m0.00 - 1.83 Overburden 1.83 - 4.94 Broken Ground
(overburden?)4.94 - EOH Mafic Volcanics minor mineralization, no assays of interest.
Commenced January 14, 1986, completed January 15, 1986Objective
CollarAzimuthDipLengthGeology
Assay Results
to test shaft zone for north dippingstructures13+69E, 0+07.5N180" (south)-45 045.72 m
OverburdenGranodioriteMafic VolcanicsBrecciaSiliceous Rock, alteredQuartz-vein,arsenopyrite, v.g.Breccia0.20, 0.24, 0.32 oz/ton
0.00 - 3.66 3.66 - 10.44 10.44 - 23.58 23.58 28.40
28.4030.27
30.27 - 30.57
30.5730.27
EOH 30.57
no mineralization or assays of interest.
- 39 -
RL-7
Commenced January 15ObjectiveCollarAzimuthDipLengthGeology
Assay Results
RL-8
Commenced January 16ObjectiveCollarAzimuthDipLengthGeology
Assay Results
RL-9
1986, completed January 16,to test shaft zone12+99E, 0+64S336"-45 045.72 m0.00 - 8.538.53 - 18.0318.0321.7122.65
1986
26.27 -
26.58 - 33.11
21.7122.6526.2726.5833.11 EOH
OverburdenArgillite-WackeIntermediate Lapilli TuffSulphide Sericite TuffBrecciaSulphide Siliceous Rock(altered)BrecciaDiorite
no assays of interest.
1986, completed January 17, 1985to test westward extension of shaft zone13+OOE, 0+69S319 0-45 045.72 m0.00 - 10.97 Overburden10.97 - 22.44 Argiliite-Wacke
Quartz Lapilli TuffMafic TuffQuartz Lapilli TuffBrecciaSiliceous PorphyryDiorite.06 oz. Au/T
22.4425.3026.0027.1840.8043.1233.18 -
25.3026.0027.1840.8043.12EOH34.18
ObjectiveCollarAzimuthDipLengthGeology
Commenced and completed January 17, 1986to re-test original K-6 zone13+OOE, 0+61SO 0 (north)-45 045.72 m0.00 - 10.3610.36 - 17.9017.90 - 19.3019.30 - 21.4421.44 - 22.3022.30 - 34.4834.48 - 41.0041.00 - 45.72
Assay Results 32.30 - 33.3035.48 - 36.4844.00 - 45.00
OverburdenArgillite-WackeSufphide Sericite TuffMafic TuffQuartz BrecciaBrecciaSulphide Sericite TuffBreccia0.10 oz. Au/T0.08 oz. Au/T0.06 oz. Au/T
- 40 -
RL-10
Commenced and completed January 18, 1986ObjectiveCollarAzimuthDipLengthGeology
Assay Results
to test dip of shaft zone stratigraphy 13+OOE, 0+45SO0 (north) .45026.52 m 0.00 - 4.27I.27 - 11.50II.50 - 19.84 19.84 - EOHno assays of interest.
Overburden Quartz Breccia Breccia Siliceous Porphyry
Check Assay Results; previous drilling
K-2
Collar
Results
13+32.SE, 0+38.55S
Interval (m)9. 14 - 10.39 10.39 - 14.33 14.33 - 14.63 14.63 - 14.93 20.12 - 20.73 20.73 - 21.55 28.04 - 28.35
Au (oz/ton)0.30 tr 0.28 0.10 0.64 0.14 0.22
Width (m)1.25 3.94 0.30 0.30 0.61 0.82 0.31
K-6
Collar
Results
Grade
13+02E, 0+59S
Interval28.35 - 29.57 - 30.48 - 32.00 - 33.53 - 35.05 - 36.88 -
(m) Au (oz/ton) Width (m)29.57 30.48 32.00 33.53 35.05 36.88 38.10
0.24 0.14 1 0.06 tr 0.32 0.26 tr
.22 ).91 .52 .53 .52 .83 .22
0.154/9.75 m (32 feet) including 0.287/3.35m (11 feet)
41 -
8. FINANCE
A. EXPENDITURE SUMMARY
Previous
Preliminary property examinations-helicopter 6,988.90-wages 4,375.00-accommodation 213.00-assays 77.00-report compilation 1,108.14-miscellaneous 1,428.64 Option payment-on signing 15,000.00 Claim staking-99 -f 1 0 claims 14, 162.90 Airborne survey-Aerodat 28,560.00 Survey-bring 3 claims to lease 9,453.15
total 81,366.73
1985 Program
Geological and geochemical surveys-wages 23,550.00-fixed wing 2,545.51-mobe-demobe 1,704.07-camp costs 1,226.75-geochem assays 3,977.00-rock assays 1,668.64-accommodation 1,322.51-food 1,158.55-boats, motors 600.00-miscellaneous 927.97 Diamond Drilling- contract-mobe-demobe 15,000.00 . .
, .,,. ,, ~ 0 , t n f 4 9,223.10)-drilling 34,223.18-fixed wing 13,357.92
- 42 -
Diamond Drilling- geological-mobe-demobe 3,203,33-wages 21,450.00-assays 2,455.20-accommodation,meals 2,509.94-camp costs 597.98-snowmobile 559.44-miscellaneous 151.05
Report Compilation-wages 3,300.00-typing,drafting 713.20
total 136,202.24 ( CEE
Previous total 81,366.73
1985 CEE total 136,202.24217,568.97 Phase 1 completion
note- CEE refers to the Canadian Exploration Expenditure expenses that qualify for flow-thru tax credits.
- 43 -
9. AGREEMENTS
A summary of the Option Agreement between Golden Terrace and the
Kostynuk brothers is as follows:
In an agreement dated January 15, 198S, the company obtained 33
mining claims from the Kostynuk brothers for $15,000 cash, a 4% Net
Smelter Royalty, and 250,000 free trading common shares. In addi
tion to these optioned claims, the company staked 109 claims in the
same area. The company further committed to expend $200,000 on the
combined 142 claim group by February 8, 1987. (AH commitments have
been met by the company as of February 8, 1986.)
- 44 -
10. STAFF
The following were present during part or all of the initial field
exploration and drill program:
Project Supervisor: Carry K. Smith
11 Valley view Court
Klelnburg, Ontario
LOJ 1CO
Geologist: Richard B. Scratch, Ph.D
6239 Edenwood Drive
Mlssissauga, Ontario
L5N 3B5
Technician: Alasdair J. Mowat
712 Latchford Street
Haileybury, Ontario
POJ 1AO
- 15 -
11. CONCLUSIONS
1. Cold occurs in quartz veins associated with arsenopyrite,
pyrite, sphalerite, galena and sericite.
2. Cold occurs In quartz-sericite-sulphide alteration zones in
brecciated Iron formation that form at the Intersection of
cross-cutting fracture zones. The two dominant cross-cutting
structural trends are N75 0E and N100W.
3. Stratlgraphlcally controlled shears occur principally within
sedimentary units dominated by slate, greywacke, jasperoid.
Iron formation and chert developed within an Intermediate
volcanic sequence.
4. Widths and grades of drill intersected gold mineralization are
consistent with the possible existence of an economic gold
deposit.
5. l.P. correlates well with areas of known sulphide-gold mineral
ization and presumably will be an effective geophysical tool on
the rest of the property.
6. Humus soli geochem for gold and arsenic is an effective tool
for regional surveying.
7. The potential for the existence of an economic gold deposit is
considered high.
- 46 -
1 —————— PROJECT ESTIMATE
^ f^bjECT DESCRIPTION
[WM E : R ICHARDSON LAKE- GTR
TYPE: cold expl. P ROV. OntarioPROJECT No. RL.86 N .T.S. 5 2 N g
No. Of CLAIMS AND/OR LOCATION
142 claims- Richardson Lake
Casummit Lake G- 1751 and G- 1742DUE DATE OF CLAIMS
SUMMARY OF WORK PROGRAMME
1985 follow-up, detail qrid
geology, geochem, trench samplin
and prospecting.
diamond drilling
PROJECT SUPERVISOR; G . K. Smith
No. OF EMPLOYEES
l^EG 3 TEMP. 2
I^REEMENT DATED:l
PARTIES
WORK COMMITMENT
JOINT VENTURER
PROJECTED START UP Man 27 7 86
COMPLETION DATE : Fefo.28 X 87
l PREPARED: G./C. smith1 DATE April 1 5 / 86l APPROVE D :
^fc^^
AUTHORIZ E D:
ESTIMATED COST ACCOUNT DAYS at 9
Ol
02
03
04
15
16
17
18
19
20
21
ftO
31
32
33
34
35
36
37
38
39
40
41
42
43
44
46
49
50
51
52
55
57
59
62
riLLD DAY- ncc G EOL - 2 40 3 00GEOPH. 1 50 200
GEOL. 80 1 00HLLU UA.S ,bMK 6 EOpH
OFFICE DAYS REG. G EOU 1 0 * 00
GEOPH.
GEOL.OFFICE DAYS TEMP. — —— — —— —— —— —— — —— — —— GEOPH.
EMPLOYEE BENEFITS
OFFICE SUPV. 8 TRAVEL
DRAFTING SERVICES
FOOD ft ACCOMMODATION
Motels 20 o t S200Camp food 25wks a t S300
SUPPLI ESTRAVE L
COMPANY EQUIPMENT R 8 M
COMPANY EQUIPMENT RENTALS
Camps- 7 months @ 1,000
Boats/motors- 7 months @ 1,000CONTRACT EQUIPMENT RENTALS 8 R 8 M
Truck- 7 months @ 1,000
FUELFIXED WING AIRCRAFT
HELICOPTER
GROUND SURVEY -GEOPHYSICS
AIRBORNE SURVEY- GEOPHYSICS
LINE CUTTING 1 85kmCL, 1 SkmBL o f 5200,250STAKING at SBULLDOZING at S
DIAMOND DRILLING 6,000 ft at S 4 0
PROBING at S
CONTRACT GEOCHEM o' *
CONSULTANTS FEES
ASSAYING 3oo rock- Au @ 10
FEES, LICENCE S
DATA PROCESSING includedOPTION PAYMENT
GEOCHEM ANALYSIS
/OO /cms x 40 Au, As, @ 10
LEGAL FEES
TOTAL EXPE NSE
RECHARGES O .M.E.P.
NET EXPENSE
AMOUNT S
72,000
30,0008,000
4,000
10, 000
1 ,000
4,000
7,5002,500
7,000
7,000
7,000
500
15,000
50,000
271,500
3,000
40,000
500,000
-125,000
375, 000-47-
12. RECOMMENDATIONS
1. Detailed l.P. should be carried out in areas of anomalous gold
geochem.
2. The entire property should be line cut and geologically mapped In detail with selected follow up humus geochem were indicated.
3. All existing trenches should be located, mapped and sampled.
4. A substantial program of diamond drilling should be carried out on existing targets along with new ones as they arise from the 1986 field exploration. Priority areas are as follows:
1. The shaft zone in the vicinity of holes RL-1, RL-9, RL-8,
K2 and K6.
2. The southeast claim group.
3. The southwest trench areas.
- 48 -
13. R EFERENCES
Andrews, A.J., and Hugon, H.1985: Alteration, Metamorphism, and Structure associated with
Archean Volcanic-Hosted Cold Deposits, Red Lake District;Studies in the Campbell and A.W. White Mines In Summary ofField Work, O.D.M., 1985, p. 193-200.
Furse, Geo. D.1933: Geology of the Shabumenl-Blrch Lakes Area In O.D.M. Vol
XL11, Part VI, p.21-51.
Harding, W.D.1936: Geology of the Birch-Springpole Lakes Area. O.D.M. Vol
XLV, Part IV.
Hoffman, E.L., and Brooker, E.J.1983: Biogeochemical Prospecting for Cold with Reference to Some
Canadian Cold Deposits.
Horwood, H.C.1937: Geology of the Casummit Lake Area and the Argosy Mine,
O.D.M. Vol XLVI, Part VII.
Hugon, H., and Schwerdtner, W.M.1985: Grant 149 - Structural Signature and Tectonic History of
Deformed Gold-bearing Rocks In Northwestern Ontario in O.D.M. Summary of Research 1984-1985, p.62-72.
Podolsky, G.1985: Report on Combined Helicopter-Borne Magnetic and Electro
magnetic Survey, Richardson Lake Project, Ontario, for Golden Terrace Resources Corporation, by Aerodat Ltd.
Williamson, J.D.1984: Twice Around the Pan. Williamson Publications, Toronto,
Ontario.
49
CERTIFICATE Of QUALIFICATION
I, GARRY KEITH SMITH, of the Town of Vaughan, Municipality of York, Community of Kleinburg, Province of Ontario, do hereby certify,
That I am a geologist and reside at 11 Valleyview Court, Kleinburg, Ontario.
That I graduated from the University of Waterloo at Waterloo, Ontario in 1977 with an honours Bachelor of Science degree in the Earth Sciences.
That I am an associated member of the Geological Association of Canada.
That I am an affiliate member of the Association of Exploration Geochemists.
That I am an associated member of the Canadian Institute of Mining and Metallurgy.
That I have been practising my profession in the field of mineral exploration since graduation.
That I was intimately associated with the generation of all technical data pertaining to this report.
Dated:
Garry K/ Smith Exploration Consultant
- 50 -
td o o RL-6
O
o o-t-
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O K-2
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5 OS
O RL-1GOLDEN TERRACE RESOURCES "RICHARDSON LAKE PROJECT"
SHAFT ZONE PLAN
RL-6 Oi 10 t
20
/ : 500 meters
75S
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"RICHARDSON LAKE PROJECT"Dec. 1985 - Jan. 1986
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DRILL HOLE GEOLOGIC LOG HOLE MUMBf B Rt..-/
PAGE No.
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LOGGED BY Gi - K - C
P.D.H D DATE TEC- I V
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Dec. 1985 - Jan. 1986O 10 go
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DRILL HOLE GEOLOGIC LOG HOLE NUMBER. PAGE No. ——
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DRILL HOLE GEOLOGIC LOG HOLE NUMBER. PAGE No. .
PROJECT - KOLZfAJ ..TYPE OF HOLE D.O.H D R.D.H. DLOGGED BY.
P.O.H D DATE ————
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RL-913+OOE, 0+61Snorth azim.RL-1013+OOE, 0+45S north azim.
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY. ONTARIO TEL: 672-3107
QJrrttftrai?NO. B 1445-84"C"
SAMPLE(S) OF: R ock (7)
SAMPLE (S) FROM:
DATE: December 11, 1984
RECEIVED: D ec " 4' ' 9 84
Mr . A. Mowa t 4DX L imi t ed
rv M o K.
Shaft waste
Granodiorite
S a mp l o N o .
4516
451 7
" 4518
" 4519
Sheared mv+slate 4 520
4521
4522
Go l a ppb
1 52
75
1 1
1 6
3
0.089** chert sulphide brx
14+60E 1+25N aspy alteration
ir
unaltered
aspy-f carbonate
0.6 7 9** 3 0 ife aspy
::::;: Checked
IN ACCORDANCE WITH LONG-T^TAC
OTHC RWISE GOLD AND SILVER VAL Ut HUSF bUCtTS MAvr NOT Bt t N AI1JU-.SATE r OR LOSSES AND GAIN? IN ne ML
LIGHtD NORTH
nrromcD ON111 TO COMf'l N-
1 IN 1 ME l I RCASSAY P ROCLSS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
Pr;n.
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187. HAILEYBURY, ONTARIO TEL: 672-3107
NO. 22287 . DATE: October 10, 1985
SAMPLE (S) OF: Rock(3) RECEIVED: October, 1985
SAMPLE(S) FROM: Mr. A. Mowat, Golden Terrace Resources Corp.
Sample No.
A
B
C
Oz. Gold
0.002*
0.105**
0.070
* Estimated. ** Checked.
type samples from 9+80E Trench
IH A CCORDANCE WITH LONC-ESTABLISHED NORTH AMF.niCAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHTRWISE GOLD AND SILVER VALUES REPORTED ON TiirsE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN-•.*T: foR LOioci A ND GAINS INHERENT I N THE F IRI
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187,
NO. 22825
SAMPLE (S) OF:
SAMPLE (S) FROM:
HAILEYBURY, ONTARIO
of AnalgaisTEL: 672-31O7
DATE: October 16, 1985
Rock(56) RECEIVED: October, 1985
Mr. Richard B. Scratch, 4DX Limited, Kleinburg, Ont.
PROJECT: Richardson Lake
Sample No.
RL #123456789
RL#10123456789
RL#2012345678
Oz. Gold Sample No, Oz. Gold
Trace 1 6E,2N? floatTrace IF pits sofSE RLTrace "Trace "Trace Black chatter veinTrace " country rock W sideTrace " " E side0.068 Black chatter veinTrace 4 E,U50sTrace 4 E,o+50sTrace 4E,2+25N0.010 4 E, chert, b rx float— at lakeshore Trace "Trace 8E, 2+1 OS Trench0.480** "0.164**0.0260.0100.002*0.0060.0160.010 1 0+75E0.008 TrenchTrace0.0360.0080.0060.002*
RL #29RL #30
123456789
RL #40123456789
RL #5012345
RL #60
Trace , n 7 (.0.002* l™5*Trace TrenchTrace0.0220.0080.0300.002*0.0660.0540.0480.020 9+aofi0.092 Trench0.0220.0100.0260.0040.0440.0520.304**0.0460.0940.014 2E,5+50N0.018 2 E,6+OONTrace 1 E, 3+OONTrace 1 E,1*OONTrace 2E, 3+OON0.016 9 +80E
* Estimated. ** Checked.
IN ACCORDANCE WITH LONG.ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON IXLOr. SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN. LA-IE FOR LOSSES AND CAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
Pin
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY. ONTARIO TEL: 672-31O7
Gkrttfirat? of AnalgateNO. 24850
SAMPLE (S) OF: Rock(l 7)
DATE: October 24, 1985
RECEIVED: October, 1985
SAMPLE (S) FROM: Mr. Richard Scratch, 4DX Limited.
PROJECT: Richardson Lake
Sample No,
RL 57 RL 58 RL 59 RL 61 RL 62 RL 63 RL 64 RL 65 RL 66 RL 67 RL 68 RL 69 RL 70 RL 71 RL 72 RL 73 RL 74
Gold ppb
19
Oz. Gold
169206
585147
10212224852
13E,0+25S0.153* 0.817* 1.270* •0.087* 1.700* 0.450*
samples of gulohide chert breccia rromShaft waste dump
16E,0*15S Trench
14+70E,1+20N15E, 0+05N float H
IF pits NE RL H
* Checked.
IN ACCORDANCE WITH LONG.ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY, ONTARIO
af AnalgataTEL: 672-31O7
NO. 26228
SAMPLE(S) OF: Metallic Rock(6)
SAMPLE(S) FROM: ^DX Limited, (Mr. R. Scratch)
DATE: October 28, 1985
RECEIVED: October, 1985
Proj: Richardson Lake
Sample No.
RL-41
RL-47
RL-48
RL-49
RL-50
RL-60
Oz. Gold
0.098
0.058
0.311
0.038
0.093
0.014
pulp and metallic check of 9+80E trench samples
IN ACCORDANCE WITH LONG.f STABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUTA REPORTED ON THESE SllttTS HAVE NOT PUN AflJIIf.TIP TO COMPCN. SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
PER,
Core Samples
PAUL'S CUSTOM FIRE ASSAYING LTD. Phone: Bus. (807) 662-8 Res. (807) 662-3
4-DX-Exploration Ltd.
PAULOKANSKI.Assayer Box 253, Cochenour, Ontario POV l LO
ASSAY CERTIFICATE Date:. Dec. 20-85
l2
34
5
67
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
2425
Sample No.
501
02
03
04
05
06
07
08
09
10
11
12
13
14
1516
17
18
19
20
21
22
Description
RL-85-1
oz/ton Au
Trace
•i
ii
.01
TraceH
M
.01
.08
.08
.14
.01
Trace
M
H
.01
Trace•i
H
.01
Tracett
oz/ton Ag
Assayer:
PAUL'S CUSTOM FIRE ASSAYING LTD. Phone: ^l. (W7) eeta
4-DX-Exploration
PAULOKANSKI.Assayer Box 253, Cochenour, Ontario POV l LO
ASSAY CERTIFICATE Date:. Jan. 20-86
12
34
5
67
8
9
1011
12
13
14
1516
17
18
19
20
21
22
23
2425
Sample No.
523
24
25
26
27
28
29
30
31
32
33
34
3536 '
37
38
3940
" 41
42
43
44
45
46
47
Description oz/ton Au
Trace
M
M
II
M
II
.02
.02
Trace
.01
TraceM
tl
M
It
II
II
II
II
II
II
II
M
II
II
oz/ton Ag
Assayer:
A PAUL'S CUSTOM FIRE ASSAYING LTD.~Phone: Bus. (807) 662-8
Res. (807) 662-3
4-DX-Exploration
PAULOKANSKI.Assayer Box 253, Cochenour, Ontario POV l LO
ASSAY CERTIFICATE Date: Jan. 20-86
12
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
Sample No.
548
S&49
50
51
52
53
54
55
56
57
58
59
60
61
62
63
64
65
66
67
68
69
70
71
72
Description oz/ton Au
Trace
M
II
II
II
.01
Trace
ti
M
II
II
tt
M
II
II
.01
TraneM
n
H
M
II
II
II
II
oz/ton Ag
4-DX- Exploration
PAUL'S CUSTOM FIRE ASSAYING LTD.
PAULOKANSKI.Assayer Box 253, Cochenour, Ontario POV l LO
ASSAY CERTIFICATE
Phone: Bus. (807) 662-8 Res. (807) 662-3
Date: Jan. 20-86
12
34
5
67
8
9
10
11
12
1314
1516
17
18
19
20
2122
23
2425
Sample No.
573
74
75
76
77
78
79
80
81
82
83
84
85
86
87
88
89
90
91
92
93
94
95
96
97
Description oz/ton Au
TraceII
II
.20
.24
.32
TraceH
.01
Trace•i
.02
TraceH
M
M
M
II
II
II
II
II
II
M
II
oz/ton Ag
PAUL'S CUSTOM FIRE ASSAYING LTD. Phone: St
Au A*
4-DX-Exploration
PAULOKANSKI.Assayer Box 253, Cochenour, Ontario POV l LO
ASSAY CERTIFICATE Date: Jan. 20-86
12
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
2425
Sample No.
598
99
600
01
02
03
04
05
06
07
08
09
10
11
12
13
14
l^
16
17
18
19
20
21
22
Description oz/ton Au
Traceii
M
II
II
X .02
.02
.0?
Trace
K
M
.02
.01
Trace
M
n
.02
Trace
•i
ii
•i
M
II
II
II
oz/ton Ag
?t^**4.S/ij/ZS^?*". c-
Au A*
4-DX-Exploratcbon
PAUL'S CUSTOM FIRE ASSAYING LTD.
PAULOKANSKI.Assayer Box 253, Cochenour, Ontario POV l LO
ASSAY CERTIFICATE
Phone: Bus. (807) 662-8 Res. (807) 662-3
Date: Jan. 20-86
12
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
2425
Sample No.
623
24
25
26
27
28
29
30
31
32
33
34
35
36
37
38
39
40
41
42
43K44
45
46
47
Description oz/ton Au
.01
Trace
•i
M
II
tl
.02
Trace•i
it
H
ti
it
H
•i
ti
n
.01
Trace
it
H
H
ti
•i
.06
oz/ton Ag
4-DX-Exploration
PAUL'S CUSTOM FIRE ASSAYING LTD.
PAULOKANSKI.Assayer Box 253, Cochenour, Ontario POV l LO
ASSAY CERTIFICATE
Phone: Bus. (807) 662-i Res. (807) 662-:
Date: Jan. 20-86
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
Sample No.
648
49
50
51
52
53
54
55
56
57
58
59
60
61
62
63
64
65
66
67
68
69
70
71
72
Description oz/ton Au
Trace
.01
Trace
M
M
.02
Trace
it
•i
H
•i
o
it
•i
M
II
It
II
II
II
II
II
II
II
II
oz/ton Ag
Assayer.
PAUL'S CUSTOM FIRE ASSAYING LTD. Phone: ^ g^ w-l
4-DX-Exploration
PAULOKANSKI.Assayer Box 253, Cochenour, Ontario POV l LO
ASSAY CERTIFICATE Date:. Jan. 20-86
12
34
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
2425
Sample No.
673
74
75
76
77
78
79
80
81
82
83
84
85
86
87
88
89
90
91
92
93
94
95
96
Q7
i Description oz/ton Au
Trace
II
.10
TraceH
.08
T^aceii
•i
•i
M
II
II
.06
Trace
.06
Trace
.32
.26
Trace
.24
.14
.30
Trace
.28
oz/ton Ag
Asuyer:
4-DX-Explorat{bon
PAUL'S CUSTOM FIRE ASSAYING LTD.
PAUL OKANSKI, Assayer Box 253, Cochenour, Ontario POV 1LO
ASSAY CERTIFICATE
Phone: Bus. (807) 662-E Res. (807) 662-5
Date: Jan. 20-866
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
Sample No.
698
99
700
01
02
Description oz/ton Au
.10
.64
.14
.22
Trace
'"I
oz/ton Ag
NO. 0215
BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-3IO7
Gfcrttfirat? nf Analysis
SAMPLE (S) OF:
SAMPLE (S) FROM:
Rejects(56)
Mr. A. Mowat, 4DX Limited.
DATE: February 7, 1986
RECEIVED: February, 1986
Sample No.
5089
51012
5989
600630
123456789
66456789
. 670123
* Estimated.
** Checked.
Oz. Gold
0.002*0.0940.0780.146**0.002*0.012TraceTraceTraceTrace0.010TraceTraceTraceTraceTrace0.0180.002*TraceTraceTraceTraceTraceTraceTraceTraceTraceTrace
Paul'sCustomFire AssayingOz . Col d
.0?
.08
.08
. 1 4
.02TRTrTrTrTrTrTrTrTrTrTrTr-:-TrTRTrTrTrTrTrTrTrTrTr
Sample No,
67456789
680123456789
690123456789
700 l
Oz. Gold
Trace0.0700.0120.002*0.0960.0080.002*0.0140.002*0.0040.0080.0180.0160.0080.0260.0040.288**0.146**0.0140.185**0.0840.211**0.0200.250**0.0260.483**0.058
Tr. 10TrTr
.08TrTrTrTrTrTrTr
.06Tr
,06Tr
.32
.26Tr
.24
.14
.30Tr
.28
. 10
.64
. 140.165** . 22
Bell-White check a ssays of Paul's Custom Fire Assaying
IN ACCORDANCE WITH LONG-FSTABLIEHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN. SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
Pen.
Soil Samples
—f
C
c; r
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c; c c
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"
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X O i c- o x-
11
DAJ'E: 29-GCT-35
^^ SAMPLE if/------.-.-.-.-.-....
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K-043K-O'+'i-K-04f'
NUCLEAR
REPORT:
A3 PPM
1 110
. 5.39.29.17.37.20.1
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ACTIVATION SERVICES LIMITED
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RF. PORT i 4994 FI Le NUMBER: 6613
S A P L L AS PPM
PAGE:
AU PPB
K - 0 4 6k-047K -04 SK-OV9K-050K-Oi*lK-C52K - 0 5 3K-054K-035K -056K-057K -05 3K-OS9K - 0 6 0K-061K-Oo2K.-063K-064K-065K-Oo6K-C67K-06flK-069K-070K-071K-072K-073K-07^K -07 5K-076K-077K-073K-C79K- 030K-081K-082K-OG3K-CiAK - 0 c) 5K-OS&K-087K-038K-089K- 090
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NUCLEAR ACTIVATION SERVICES LIMITED
DAT t: 29-OCT-3ii REPORT: 4994 FILE NUMBER: 6613 PAGE:
S A M ? L E A3 PPM AU PP3
K- 001K- 09 2!K-093K -09 AK-095K-096K-097K -09 SK-099K- 100K-101K-l 02K-103K- 10 4K-105K- 106K-107K-103K - 1 0 9K-110K-lllK-l 12K - 1 1 3K-l 14K - 1 1 5K-l 16K - 1 1 7K - 1 1 8K-l 19K-120K-121K-122K-123K-l 2 'tK - 1 2 5K- 126K - 1 2 7K-l 28K-l 2 9K-130K-l JlK - 1 3 2K-l 33K- 134K-135
5 . 37.24. 25.29.817
7.73.612
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NUCLEAR ACTIVATION S ERVICES LIMITED
JATL-: 29-OCT-63 Rt PORT: 4994 F.tLE NUMBER: 6613 PAGE:
S A M P L C AS PPM AU PP3
K - 1 3 6K- 137K-133K-139K- 140K-141K - 1 4 2K - U 3K-144K-145K-346K- 147K- 14 8K-149Y. - 1 5 0K- 151K-152K-153K - 1 5 4K- is 5K-l 56K-137K-153K-159K-160K- 161K- 16 2K-163K-lo/tK-165K-166K - lo 7K - 1 6 PK - 1 6 9K- 170K-171K-172K-173K- 174K-175K-1T:6
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S A Ki P L f;
NUCLEAR ACTIVATION SERVICES LIMITED
REPORT: 4994 FILE NUMBER: 5 613
AS PPM
PAGE
AU PPB
K-1G1K-132'K-133K-lo4K-ld5K-136K - 1 8 7K-183K-159K-190K - 1 9 1K- i ? 2K-193K- 19 4K- 195K- 196K-197K-198K -199K-200K-201K-202K-203K-P04K -2 05K-200K-207K - 2 0 8K -2 09K-?10K- 211K-212K-213K-214K-215K-216K-217K-218K-219K - ?. 2 GK -2 2 1K-222K - ? 2 3K-P24K -2 2 f*
6.213
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SAMPLE
NUCLEAR ACTIVATION SERVICES LIMITED
RUPQRT: 4994 FILE NUMliEk: 6613
AS PPM
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AU PPB
K-226K-227K - 2 2 3K-329K-230K-231K- 23?K-233K-234K - ?. 3 5K-236K- 2 3 7K-233K - ? 3 9K-240K-2'tlK-242K-2.43K -244K-245K-246K-247K-243K-249K-250K- 251K-252K-253K- 2. S 4K-255K-236K-257K-?5?K- 2 3 9K- 260K- 261K-262K-263K - 2 6 4K-265K-?66K-267K~ 2 6 3K-269K-270
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DATE: 29-OCT-85
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REPORT: 4 994 FILE NUMBER: 6 613
AS PPM
PAGE:
AU P P3
K-271K-272K-273K. - 2 7 4K-273K-276K-277K-273K-279K- 2 COf-?31K - ? H 2K - 2 3 3K - 2 3 4K-235K-2o6K-2S7K-26 RK- 28 9K-290K-291K-292K-293K- 2 9 4K-295K-296K-297K -2 9 8K- 2 99K-30QK-301K- 30 2K-303K-304K -3 05K-306K-307K-308K-309X-310K-31 1K-312K-31 3K-?, 14K-315
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