AN EXPL PROPOSAL FOR THE SHINING TREE AREA PROP
Transcript of AN EXPL PROPOSAL FOR THE SHINING TREE AREA PROP
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41P14SETO56 63.3035 MOND 010
AN EXPLORATION PROPOSAL
FOR THE SHINING TREE AREA PROPERTIES
OFxAMAX POTASH LTD.
TOWNSHIPS OF HALLIDAY, MIDLOTHIAN,
FAWCETT, BURROWS S KNIGHT
LARDER LAKE MINING DIVISION
W. R. Ryall Ph.D. Geologist Timmins, Ontario June 1972
41P14SE8856 63.3035 MOND 010C
TABLE OF CONTENTS
I SUMMARY . . . . . . . . . . . . . . . . . . . . . . . . . . l
II LOCATION . . . . . . . . . . . . . . . . . . . . . . . . . 2
III AMAX PROPERTY POSITION . . . . . . . . . . . . . . . . . . 2
IV PROPERTY DESCRIPTIONS AND EXPLORATION PROGRAMS. . . . . . . 3
Halliday-Midlothian Twps. . . . . . . . . . . . . . . 3
Burrows Twp. ..................... 5
Knight Twp. ..................... 6
Fawcett Twp. . . . . . . . . . . . . . . . . . . . . . 8
V SUMMARY OF PROPOSED EXPLORATION PROGRAM . . . . . . . . . . 10
VI FINANCIAL ESTIMATE . . . . . . . . . . . . . . . . . . . . 11
TABLE OF FIGURES
Fig. l Location Map . . . . . . . . . . . . . . . . . . After Page 2
Fig. 2 Location of claims in Halliday, MidlothianTwp. area . . . . . . . . . . . . . . . . . . . After Page 2
Fig. 3 Location of claims in Burrows Twp. . . . . . . . After Page 2
Fig. 4 Location of claims in Knight Twp. . . . . . . . After Page 2
\ Fig. 5 Location of claims in Fawcett Twp. . . . . . . . After Page 2
i*Fig. 6 Radem VLF Survey, Halliday-Midlothian Twp. . . In Pocket at Back
Fig. 7 Magnetometer Survey, Halliday-Midlothian Twp. In Pocket at Back
Fig. 8 VEM Survey, Burrows Twp. . . . . . . . . . . . In Pocket at Back
Fig. 9 Magnetometer Survey, Burrows Twp. . . . . . . In Pocket at Back
Fig. 10 Radem VLF Survey, Knight Twp. . . . . . . . . In Pocket at Back
Fig. 11 Magnetometer Survey, Knight Twp. . . . . . . . In Pocket at Back
X Fig. 12 Radem VLF Survey, Fawcett Twp. . . . . . . . . In Pocket at Back
Fig. 13 Magnetometer Survey, Fawcett Twp. . . . . . . In Pocket at Back
Page l
I. SUMMARY
Ground geophysical surveys have defined conductive features
in four claim groups in the Shining Tree area, Larder Lake Mining
Division. Electromagnetic anomalies located in Halliday and Fawcett
Townships show coincident magnetic features whilst those situated
in Knight and Burrows Townships have no coincident magnetic features.
As the electromagnetic and magnetic anomalies lie within
greenstone assemblages similar to those hosting economic base metal
mineralization elsewhere in the Precambrian Shield, the anomalies
represent excellent targets for drill testing. To aid in best
siting of drill holes, a program of geological mapping and soil
geochemistry is recommended.
The proposed program is estimated to cost $30,923.00.
Page 2
II. LOCATION
The targets proposed for testing within this program are
located in the vicinity of the village of Shining Tree, which lies
some 70 miles southwest of Kirkland Lake. Specifically, claim groups
are located in Halliday, Midlothian, Burrows, Knight and Fawcett
Townships. (Fig. 1)
III. AMAX PROPERTY POSITION
Amax Potash Ltd. presently holds a total of 29 claims in
the Shining Tree area which are distributed as follows:
Halliday, Midlothian Twps. (17 claims)
L312902-312907 incl., L312910-312911, L312913, L312915,
L312917-312919 incl., L308795-308798 incl. (Fig. 2)
Burrows Twp. (4 claims) L308831, L312947, L312949, L312950 (Fig. 3)
Knight Twp. (4 claims) L316528-316531 incl. (Fig. 4)
Fawcett Twp. (4 claims) L308812, L308813, L308816, L308817 (Fig. 5)
Kirkland Lake Area
\ \ K IRKLAND tLV ' :y c, VX.I "XE^vO^""" Lev,., V\\ l i TtSCiUsJwSSit*".".'' -^y
Cobalt-Gowganda Area
Areas eligible for exploration assistance
Figure 1. Location of claim groups in the Shining Tree Area.
Scale l in = 20 mi.
:N
AMAX POTASH LTD.
Location Map
HALLIDAY, MOND, MIDLOTHIAN, RAYMOND TWPSJ
Scale* l" s 1/2 Mi.
Figure 2
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Mac MURCHY TWP.
FAWCETT TWP.
AMAX POTASH LTD.
Location Map
FAWCETT TWP.
Scale' l" - 1/2Mi.
Figure 5
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IV. PROPERTY DESCRIPTIONS AND EXPLORATION PROGRAMS
(i) Halliday - Midlothian Twps.
Claims; L312902-312907 incl., L312910-312911, L312913,
L312915, L312917-312919 incl., L308795-308798 incl.
Access; Although several old logging roads extend close
to the claim group, bridges are in disrepair and
many swampy patches make float-equipped aircraft
the most feasible method of access for jobs not
requiring heavy equipment. Drill equipment would
best be moved in by crawler tractor from the Hydro
maintenance road which runs NS from the Matachewan
road (W extension of Highway 560).
Previous Work; Radem and VEM surveys have defined a conductive
anomaly some 10,000 feet strike length. In some
places the anomaly is double (Fig. 6). A ground
magnetometer survey has outlined a zone of narrow
magnetic anomalies, in part coincident with the
conductor (Fig. 7).
Geologically the Halliday conductor lies at the
southernmost exposed limit rhyolitic sequences of
the Halliday Dome. In this area the presence of
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graphitic units are known as a result of previous
drilling programs, notably by Cominco in 1965.
Cominco drilled three holes into a ground conductor
that appears to be very similar in character to
that outlined by the present surveys.
Though logs of the Cominco holes are brief, the
conductor is clearly due to graphitic units that are
interbedded with felsic volcanics and argillite.
The graphite characteristically hosts up to ID-12%
pyrite with less pyrrhotite (to 5%) and minor
chalcopyrite and, in one hole, galena. Volcanic
units typically contain minor pyrite and pyrrhotite
(combined to 5*3;) with chalcopyrite variously being
recorded present as "traces" and "blebs". Assay data
is not available to the present writer.
Graphitic-bearing tuffs and argillites at the margins
of felsic volcanic domes are of obvious interest for
the exploration of stratiform base metal deposits.
Proposed Program; A program of geological mapping and soil geochemistry
is proposed to assist in siting drill hole locations.
Initially, two holes are proposed for a total of
800 ft. of drilling.
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(ii) Burrows Twp.
Claims; L308831, L312947, L312949, L312950
Access; Old logging roads traverse this claim group and
make for routine access.
Previous Work; A Radem survey defined a conductor and subsequent
VEM survey, extending outwards from the area of
Radem coverage, indicates that the conductor bends
sharply from an E-W to a NW direction and continues
weakly for 3400 feet, although an alternative
interpretation is that part of the VEM conductor is
reflecting a long fault zone. The magnetometer survey
defined a number of probable diabase dikes although
a weak E-W magnetic feature may flank the conductor.
(Figs. 8 and 9)
Dacitic volcanic units predominate on this group
and are sheared in the vicinity of the conductive
axis. Chloritic alteration is common with sulphides,
generally pyrite with minor disseminated pyrrho
tite being frequently developed to about 5%. Locally,
but rarely, pyrite is developed to 25% though assays
returned from such specimens are typically very low.
(Assay No. 4956 gossanous pyritic volcanic 15% py:
Cu Nil, Zn .013; Ag 0.04 Oz/ton).
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Elsewhere on the group more basic volcanic units
are present and these host small syenitic intrusive
bodies and diabase dykes.
Paymaster Consolidated Mines are known to have
drilled three holes into conductors beneath Little
Marne Lake to the east of Amax holdings, in 1957
but no base metal intersections were made in this
drilling.
Proposed Program: Geological and soil geochemical surveys will be
utilized to site a drill hole designed to test
the conductor.
(iii) Knight Twp.
Claims; L316528 - 316531 incl.
Access; The claims in this township are situated on the
east shore of Pigeon Lake and no summer road is
available onto the group. Access for survey work
is gained by truck road to the west shore of
Pigeon Lake followed by canoe or boat to the claims.
Heavy equipment could be moved in by aircraft
directly to Pigeon Lake or, in winter, pulled
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from Highway 560 via winter road and lake crossing
directly to the set-up.
Previous Work; A Radem survey first detected the conductor on
the ground and, along with the fixed-transmitter
VEM survey, traced the conductor for approximately
4000 feet. The conductor strike swings arcuately
at the south end. The magnetometer survey outlined
a number of narrow magnetic anomalies, some of
which are sympathetic to the trend of the conductor,
while others, probably diabase dikes, trend
obliquely to the conductor. The conductor itself
is without any coincident magnetic anomaly (Figs. 10 St 11)
There is evidence of previous drilling in the
area but no set-ups near the conductors defined by
Amax surveys were noted. Several boxes of core
were found about 700 feet west of the conductor on
line 20 SE. The core is composed of a wide section
of graphite in a dacitic host. The graphite is
associated with pyrite (to 20!fc) and pyrrhotite (to 31).
Assays of graphite return Q.05% Cu, Q.23% Zn, 0.22 oz/ton Ag.
A 25 ft. section of serpentinite from the core yielded
only very weak nickel values (D.03% Ni).
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Proposed Program; Geological and soil geochemical surveys are planned
to aid in choice of a suitable drill site. At this
time one hole of 400 ft. is planned to test the
conductive zone.
(iv) Fawcett Twp.
Claims; L308812, 308813, 308816, 308817
Access; Survey access to the property is gained by following
the old mine road which leaves Highway 560 at a
point 2 miles east of Spruce Shilling camp and
then by canoe about a mile south along the West
Montreal River.
Drill access would best be gained by construction
of a road generally paralleling the river.
Previous Work; A Radem survey outlined a narrow bedrock conductor
with a strike length of 1600 feet. The conductor
is confirmed by the results of a VEM survey. Magne
tic coverage over the conductor outlined a magnetic
feature directly associated with the conductor (Figs. 12 S 13)
Sulphides, predominately pyrrhotite, are consequently
suggested as the cause of the conductor.
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No sign of any previous geophysical work or
drilling was observed, although several old claim
lines were encountered. While the conductor is
overlain by a shallow swamp, outcrop is abundant
elsewhere.
Geological mapping has not been carried out on this
group but a reconnaissance survey has revealed the
presence of a differentiated volcanic suite consisting
of rhyolite and andesite. No sediments were obvious.
The conductive feature is terminated to the E by a
diabase dyke.
The presence of a conductor in this geological
environment with a magnetic association is anomalous
in the Shining Tree area and warrants testing by
diamond drilling.
Proposed Program; The conductor can adequately be tested with a 450 ft.
drill hole, the location of which would be deter
mined with the aid of a soil geochemistry survey and
a related geological survey.
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V. SUMMARY OF PROPOSED EXPLORATION PROGRAM
The program of exploration proposed for claim groups in
the Shining Tree area which contain previously defined ground conductors
can be summarized as follows:
Phase l Geological mapping
Soil geochemistry
Phase 2 Diamond drilling
Estimates of diamond drilling are given below.
High costs, due to remoteness from established
or maintained roads are envisaged in Halliday,
Fawcett and Knight Twps.
Halliday Twp. - 2 holes, 800 ft. @ $12/ft = $9,600
Fawcett Twp. - l hole, 450 ft. @ $ 9/ft ~ $4,050
Knight Twp. - l hole, 400 ft. @ $12/ft = $4,800
Burrows Twp. - l hole, 400 ft. @ $ 8/ft * $3,200
TOTAL $21,650
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VI FINANCIAL ESTIMATE
GEOLOGICAL AND GEOCHEMICAL SURVEY
Geologist 1 month
Geochemist 1 month
Assistant 1 month
Soil Geochemical Analyses
Geochemical consultant, interpretation, material and supplies
Aircraft charter
800
800
500
2500
700
200
DIAMOND DRILLING
5 holes (2050 feet)
Supervision
Geologist l month
Assays
Transportation and camp costs
GENERAL
Drafting, report preparation
Total direct cost
Overhead @ S 5!; of direct cost
TOTAL COST OF PROGRAM
21,650
1000
300
500
500
$29,450
1,473
•HP14SEMS6 63.3035 M OND 020
VOLUME 1
FINAL REPORT OF WORK PERFORMED
IN HALLIDAY-MIDLOTHIAN, BURROWS, FAWCETT
AND KNIGHT TWPS. UNDER ONTARIO
GOVERNMENT MINERAL EXPLORATION
ASSISTANCE PROGRAM.
JULY 1972 - JANUARY 1973
W.R. Ryall Ph.D. Amax Potash Limited Timmins, Ontario
Copy l Ontario Ministry of Natural ResourcesCopy 2 Ontario Ministry of Natural ResourcesCopy 3 Amax Potash Limited, TorontoCopy 4 Amax Potash Limited, New YorkCopy 5 Amax Potash Limited, Timmins
41P14SE0056 63.3035 M OND 020C
TABLE OF
I. SUMMARY. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Page l
II. INTRODUCTION......................................... Page 2
III. EXPLORATION PROGRAM 1972......,........,.,...,,..,... Page 2
(i) HALLIDAY-MIDLOTHIAN TOWNSHIPS
(a) Soil Geochemical Survey.................... Page 2
(b) Geological Survey.......................... Page 5
(c) Diamond Drilling...... .. . .....,. ....... ... . Page 6
(i i) BURROWS TOWNSHIP
(a) Geochemical Survey......................... Page 6
(b) Geological Survey.......................... Page 9
(c) Diamond Drilling........................... Page 10
(111) FAWCETT TOWNSHIP
(a) Soil Geochemical Survey.................... Page 10
(b) Geological Survey.......................... Page 13
(c) Diamond Drilling............................ Page 14
(iv) KNIGHT TOWNSHIP
(a) Geochemical Survey......................... Page 14
(b) Geological Survey.......................... Page'17
(c) Diamond Drilling........................... Page 17
IV. CONCLUSIONS. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Page 18
V. APPENDIX I - SOIL GEOCHEMICAL SURVEYS.............. Page 19
VI. VOLUME 2 - FIGURES A MAPS
TABLE OF FIGURES
Figure l
Figure 2
Figure 3
Figure 4
Figure 5
Figure 6
X Figure 7
Figure 8
Figure 9
Figure 10
Figure 11
X Figure 12
Figure 13
Figure 14
Figure 15
Figure 16
X Figure 17
Figure 18
Figure 19
Figure 20
Figure 21
X, Figure 22
Location Map......................,................. After Page l
Halliday-Midlothian Twp. property map............... After Page 2
Halliday-Midlothian Twp.-Zinc S Copper in Top Soil.. In Volume 2
Halliday-Midlothian Twp.-Zinc X Copper in Sub Soil.. In Volume 2
Halliday-Midlothian Twp.-Lead in Top Soil 8t Sub Soil.. In Volume 2
Halliday-Midlothian Twp.-Geological Map............. In Volume 2
Burrows Twp. property map........................... After Page 6
Burrows Twp. - Zinc X Copper in Top Soil............ In Volume 2
Burrows Twp. - Zinc S Copper in Sub Soil............ In Volume 2
Burrows Twp. - Lead in Top Soil fi Sub Soil.......... In Volume 2
Burrows Twp. - Geological Map....................... In Volume 2
Fawcett Twp. property map........................... After Page 10
Fawcett Twp. - Zinc S Copper in Top Soil............ In Volume 2
Fawcett Twp. - Zinc S Copper in Sub Soil............ In Volume 2
Fawcett Twp. - Lead in Top Soil S Sub Soil.......... In Volume 2
Fawcett Twp. - Geological Map....................... In Volume 2
Knight Twp. property map............................ After Page 14
Knight Twp. - Zinc S Copper in Top Soil............. In Volume 2
Knight Twp. - Zinc A Copper in Sub Soil............. In Volume 2
Knight Twp. - Lead in Top Soil S Sub Soil........... In Volume 2
Knight Twp. - Geological Map........................ In Volume 2
Geochemical Results................................. In Volume 2
Page l
I. SUMMARY
Geophysical surveys conducted in 1971 over four claim groups in the Shining Tree area indicated anomalous electromagnetic conditions that were, in three groups, accompanied by magnetic anomalies. As the geology of the Shining Tree area in general and the claim groups, in particular, was not sufficiently well known it was decided to conduct geological mapping and soil geochemical surveys on each claim group to permit optimum siting of diamond drill holes.
The geological and geochemical surveys indicated targets suitable for drill testing on the Halliday, Burrows and Fawcett claim groups. The geology and geochemical response on the Knight group were considered not to warrant drilling.
Four holes totalling 1525 feet were drilled as follows:
Halliday - 2 holes each 400 ft.
Burrows - l hole 375 ft.
Fawcett - l hole 350 ft.
Although sulphide mineralization was encountered in all four holes, nothing of an economic tenor was intersected.
Page 2
II. INTRODUCTION
Following the definition by ground geophysical surveys of conductive horizons located within four claim groups in the Shining Tree area a request was made to the Ministry of Natural Resources under the Ontario Government's Mineral Exploration Assistance Program to enable geological and geochemical definition of diamond drill targets.
This request was approved and work commenced on the four properties in July 1972. Diamond drilling on three favourable properties began in November 1972 and was completed in January 1973.
The location, access, property descriptions and previous exploration has been summarized in the report "An Exploration Proposal for the Shining Tree Area Properties of Amax Potash Limited Townships of Halliday - Midlothian, Fawcett, Burrows and Knight (Larder Lake Mining Division)" by W.R. Ryall, Amax Potash Ltd., June 1972.
For convenience the area is shown in the location map (Fig 1) overleaf and the property maps are shown with the description of the work performed.
III. EXPLORATION PROGRAM 1972
(i) HALLIDAY - MIDLOTHIAN TOWNSHIPS
The claim group covered by the surveys is shown as Figure 2 and includes unpatented mining claims.
LSI2902-312907 incl., L312910-312911, L312913, L312915, L312917-312919 incl., L308795-308798 incl.
(a) SOIL GEOCHEMICAL SURVEY
Details of collection, preparation, analysis and results which are common to all claim groups sampled are given in Appendix I.
Over the Halliday - Midlothian claim group 420 samples were collected over 800 ft. lines. 800 ft. lines were employed due to the extreme length of the conductor.
Ecology and drainage
The VLF conductor axis follows the crest of a long East-West ridge from one end of the grid to the other. Mature birch and poplar
Kirkland Lake Area
DI..I
fil(.J Vl'M I*'. li* l |HnlHrti*.t l rninn '{'.".H, lflOMHt l______|j . j_______|
t i i ' t " i '
Cobalt-Gowganda Area
Areas eligible for exploration assistance
Figure 1. Location of claim groups in the Shining Tree Area.
Scale l in "a 20 mi.
l)
> l ** s o
—
O
ro
S
o a o Q -o
X l CO o
to
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are thick along the top and sides of this ridge while small patches of cedar and spruce bog lie to the north and south. Spruce and balsam are well mixed with poplar on the lower slopes of the ridge.
The area near the centre of the group is typified as being well drained with no large bogs or marshes. Relief in some sections and more particularly to the east is quite rugged with high birch covered hills and ridges. There are two small lakes located on the grid, one on the south end of L28E and the other larger one at the south ends of L48E and L52E. There are no streams of any size on the grid but there are damp drainage channels between the ridges that are dense with alder growth.
Soils
The tops and sides of the main east-west ridge are covered with well developed podzol s while the lower slopes and flatter sections are overlain with gleysols and humified organic matter.
Podzol s are the predominant soil type encountered on the grid. Some exceptional sections were encountered with leached (AE) horizons developed to 12"-l6".
Geochemistry discussion
Both top and sub soil surveys have been contoured using different threshold levels to outline the areas of interest. The more significant or anomalous values lie within these selected contour levels and are shown on Figures 3, 4 and 5.
Threshold values used to establish the significant and background levels for the two surveys are as follows:
Zn Cu Pb _______ppm______
(A) Top Soil
Background 100 8 50 Significant 200 40 100
(B) Sub Soil
Background 30 20 15 Significant 60 30 30
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Anomalous values occur at the following stations:
Gr i d Location______Soil_______Hot HC104-HN03 extraction
Cu Ni Zn ppm
Pb Ag
T.S. L20W-2S S.S.
T.S. L12W-1N S.S.
T.S. S.S.
T.S. S.S.
T.S. S.S.
T.S. S.S.
L4W-2N
L4E-0
L28E-5N
L36E-0
gleysol
humus
podzol
gleysol
podzol
peat
4020
52
2832
6026
2026
8084
2816
44
2832
4434
2424
4034
410152
13812
430 106
540630
308236
24684
116128
100108
870
5214
3628
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
Both top and sub soil surveys have succeeded in delimiting several similar features.
Top Soils
The most striking feature of the top soil survey is that the 200 ppm zinc contour outlines the conductor axis from one end of the grid to the other. Anomalous copper values tend to be within or flank this and other minor zinc features. Lead presents a more complex picture but shows good coincidence with the major zinc and copper trends.
There are two broad areas or zones outlined in the top soil that exhibit an overall higher concentration of metal values. Their locations are (1) L12E to L4E and (2) between L28E and L36E. In each instance the zones lie along the conductor axis and have highly anomalous metal values over widths of 200 ft. - 400 ft.
Zone #1 is a 500 ft. wide zinc anomaly with a strong copper and lead core. The more easterly #2 zone is a copper-lead feature with flanking zinc. There is a very strong magnetic anomaly associated with this zone along with a double E.M. conductor.
Page 5
Top Soils
The plotted sub soil values verify the presence of the two zones expressed in the top soil but in a more concise manner.
Zone number one is shown to be two parallel features striking east-west for 1600 ft. The two parts form very strong copper and zinc anomalies with a lead core in the northern segment.
Zone number two is a very broad zinc and copper feature with lead association. The anomaly is 800 ft. long and 500 ft. wide and forms a separate distinct anomalous zone.
In both instances the sub soil survey acted as a screen through which the minor features detected in the more sensitive top soil could be discriminated so that the major and more interesting trends could be defined.
Conclusion
The contoured top and sub soil values present similar pictures but of different intensities. They are both characterized by their coincidence to the VLF Radem conductor axis and the delimiting of two separate zones of anomalous metallic concentrations.
(b) GEOLOGICAL SURVEY
The survey was conducted over a 400 ft. grid system previously established for geophysical surveys. Outcrop is abundant at the centre of the group which is located on a prominent ridge, but to the south and north swampy conditions, with no outcrop, prevail. Near the centre of the property overburden is sandy and generally less than 20 ft. thick.
Bedrock exposed on the property is assumed to be of Precambrian age following the excellent mapping of E.G. Bright, O.D.M. geologist, published as Geological Report 79 "Geology of Halliday and Midlothian Townships" 1970.
The oldest rocks appear to be Archean felsic metavolcanic units consisting of intercalated rhyolite or rhyodacite, rhyolite tuff, and possibly dacite. Intermediate metavolcanic units are apparently interbedded with the more felsic units as are seen on lines 4E and 24E near the base line (Figure 6),
Associated with the rhyolite tuff unit on line 60E are graphite-filled shears containing up to 5/K pyrite and pyrrhotite.
The volcanic formations strike approximately E-W and dip steeply to the South. Outcrop is not sufficient to delimit further
Page 6
structure. Shearing and faulting is recognized only on lin e 20W and 4E.
Intrusive into the felsic units occur several bodies of diorite and gabbro. The former appear to be generally concordant with the country rocks whilst the latter is markedly discordant as seen on line 80E.
Unconformably overlying the Archean formations occur several prominent outcrops of Huronian sandstones, quartzites and conglomerates. These outcrops in the South of the property and form prominent hills and ridges to the East.
(c) DIAMOND DRILLING
Two holes were drilled as follows
Number Location Di p Length
TX-91-72 Line 00, 2+OOS -450 400 ft.
TX-92-72 Line 44E, WON -450 400 ft.
Drill logs are shown overleaf together with assay results of characteristic core sections. Details of the drilling are summarized on the logs.
(ii) BURROWS TOWNSHIP
The claim group covered by the surveys is shown as Figure 7 and includes the following claims
L308831, LSI 2947, LSI 2949-50.
(a) GEOCHEMICAL SURVEY
Ecology and drainage
The area has been recently burned over and is covered with young poplar and jackpine. The bush is open with little underbrush and in some spots very sparse. With the exception of the margins of the two lakes the area of the grid is extremely dry with no creeks or bogs.
Page 7
Soils
The grid covers rolling sand hills and dunes with very little outcrop. Drainage is excellent and as a result podzols are well developed. Most all of the samples collected were sandy podzols save a few gleys near the shores of the lakes.
Geochemical Survey
Discussion
The contoured results of the top and sub soil surveys exhibit a general lack of correlation with each other and to the conductor axis (Figures 8, 9, 10). There are however, two zones that do have some significance in that they both are located in close proximity to the conductive axis and strike in the same direction as the conductor.
Some of the more anomalous values detected in these zones are:
Hot HC104-HN03 extraction
Grid Location
T. S. L4W-4N S.S.
T.S. LO-1S S.S.
T.S. L12NW-4SW S.S.
T.S. L8NW-4SW S.S.
T.S. L4NW-1SW S.S.
T.S. L4NW-3SW S.S.
Background values for both top and sub soil surveys are extremely low and are the lowest encountered on the four grids surveyed. As a result the thresholds for the anomalous or significant values are correspondingly of lesser amplitude than that of the other properties.
Soil
humus
podzol
podzol
podzol
podzol
podzol
Cu
204
2120
248
421
242
406
Ni
1614
2028
3252
3212
208
4012
Zn ppm
20410
20328
24060
87032
818
42048
Pb
724
6812
6016
1528
904
8828
Ag
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
CABOT TWP. C'
AMAX POTASH LTD.
Location Map
BURROWS TWP.
Scalei l" s 1/2 Mi.
Figure 7
Page 8
Zn Cu Pb_____ppm__^_
(A) Top Soil
Background 40 10 25 Significant 200 20 60
(B) Sub Soil
Background 20 4 10 Significant 30 10 15
Top Soil Survey
A strong, well defined, zinc, copper and lead zone parallels the conductor axis south of the baseline from lines 8 NW through to line 0. There is a discontinuous weaker zone that appears on line 4W and extends to line 12NW. The 40 ppm lead contour envelopes this zone which has an interesting Zn "eye" on station IS LO, the eye is coincident to the VEM conductor axis.
Sub Soil Survey
The lack of any great difference between "background" and "significant" values has made selection of contour intervals difficult and interpretation hazardous.
A zinc feature of twice background or better with good copper and some lead association duplicates the parallel zone "B" as shown in the top soil. Zone "A" is very weak in the sub soil and comes through as a two line copper feature on the conductor axis.
A persistent zone of copper, zinc and lead concentration runs along the north ends of all the lines near Little Marne Lake. As the area covered by the grid drains towards the lake this may be a reflection of accumulated metals on the low end of a drainage system.
Likewise a dry marsh covered with gleysols shows up on the north end of line 4NW as a zinc and copper feature within the top soils.
Conclusions
1. Both top and sub soil surveys have outlined two zones ("A" and "B") of anomalous trace metal concentrations that would appear to be associated with the conductor.
Page 9
2. The top soil survey and, more particularly, zinc in the top soil has provided a better guide than lead or copper. Overburden in this area is to be 10-70 ft. and most of this is freely drained sand. (The almost barren sub soils are attributed to be a result of the absence of any organic fraction that would tend to trap any metallic ions).
3. Although the geochemical association with the conductor is weak and erratic in sub soils it is stronger and delimits the conductor better in the top soils.
4. It is assumed that the anomalous zinc and lead in the top soils have a nearby source and that it's most likely location is the conductor previously defined by the VEM survey.
(b) GEOLOGICAL SURVEY
The survey was conducted over 400 ft. lines previously established for geophysical surveys.
Outcrop is sparse on the claim group where thick Pleistocene outwash sands have formed conspicuous dunes.
The oldest formation exposed on the group is probably Archean greenstones of which andesite or dacite is the most prevalent. This formation appears to strike about 3200 and to dip steeply SW (Figure 11).
The andesite is generally a pale green-grey colour in outcrop and is well foliated. It appears massive with no pillows having been observed.
Apparently overlying the andesite-dacite occurs a more felsic group which has tentatively been identified as a rhyolite. This rock is typically of lighter colour than the andesite, commonly shows sericitic alteration and is fragmental in part. It seems likely that this formation is the one identified as a dacite fragmental in drill hole TX-93-72.
Intrusive into the andesite-dacite occur two short bodies of diabase that are observed in outcrop on line 8NW near the base line and near the shore of Little Marne Lake west of the No. 2 post of claim L 312949.
Also showing intrusive contacts to the andesite is the small syenite outcrop occurring at line 8E near the base line.
Page 10
No evidence was found in outcrop of the argillite intersected in drill hole TX-93-72. This unit is graphitic in part and is the cause of the electromagnetic conductor. The argillite formation presumably overlies the andesite-dacite group and is not present in outcrop due to its low resistance to physical forces.
(c) DIAMOND DRILLING (/06S
One hole was drilled as follows:
Number Location
TX-93-72 Line 2E, 1+90S
Dip -450
Length
375 ft.
The drill log is shown overleaf together with assay results of characteristic core sections. Details of the drilling are summarized on the logs.
(iii) FAWCETT TOWNSHIP
The group surveyed is shown in Figure 12. Claim numbers are as follows:
L 308816-17, L 308812-13.
(a) SOIL GEOCHEMICAL SURVEY
Drainage and ecology
The area covered by the grid varies in relief with many low rocky ridges and many small bogs and depressions scattered throughout. The major drainage pattern is to the north and east towards a large swamp and small lake.
The bush is well mixed over the grid with no large stands of any particular species. It is a mature mixture of birch, poplar, black spruce and alder.
Soils
Podzol s are well developed in the rougher, better drained ground while much gleysols and deep humic material are found between the ridges and in the bogs. The majority of samples analyzed were podzols. Overburden is estimated to be in the order of 10'-20' over most of the conductor, which outcrops on lines 4E and O on the base line.
MocMURCHY TWP.
JL4M
FAWCETT TWP.
AMAX POTASH LTD.
Location Map
FAWCETT TWP.
Scale' l" si/2 Mi.
Figure 12
Page 11
Geochemical Survey
Discussion
The plotted zinc, copper and lead values show a strongly anomalous pattern coincident to the conductor axis in both the top and sub soil (Figures 13, 14, and 15).
Background and the more significant values detected in the survey have been determined as follows.
(A)
(B)
Lack of any great variation between background and significant levels in the subsoil makes selection of "anomalous" zoned sifficult but can be done with some confidence when a series of even slightly enriched samples form a pattern similar to that in the top soil. There are a few sample points with highly anomalous values in all three elements that have been duplicated in both the top and sub soil. The more interesting of these are tabulated below.
Hot HC104-HN03 extraction
Top Soil
Background Significant
Sub Soil
Background Significant
In
80 200
30 40
Cu ppm
25 40
12 20
Pb
65 100
12 20
T. S.S.S.
T. S.S.S.
T. S.S.S.
T. S.S.S.
T. S.S.S.
T. S.S.S.
Grid Location
L12E-3N
L4E-3N
LO-1S
LO-2S
L4W-1N
L8W-2N
Soil
Podzol
Gleysol
Gley sol
Podzol
Gleysol
Podzol
Cu
406
4640
800328
23248
76228
404
Ni
4016
3628
4644
6820
2444
4420
Znppm
21226
200188
3232
59032
328540
30426
Pb
12012
44148
1616
10812
168
12412
Ag
.5
.5
.5
.5
1.5.5
.5
.5
.5
.5
.5
.5
Page 12
The surveys have detected what would first appear to be one continuous zone of enrichment following the conductor axis with a wider concentration on line O and 4W.
However, closer examination of the geochemical results with the aid of the magnetic survey separates the one zone into two components.
The main zone outlines the conductor to the north of the base line from L12E through to 8W. This zone is a prominent copper, zinc and lead feature strongest around line 0.
A much smaller though very strong anomaly exists south of the base line and runs from L4W to LO at 2+OOS. This is a very interesting feature in that it is coincident to an identically short strong magnetic expression.
Top Soil Survey
The 200 ppm zinc contour and 40 ppm copper contour outline the conductor axis. A strong lead feature forms a "core" to this main zone. There is metal enrichment north on line 8E, but this is attributed to concentration due to local drainage. A small though strong copper and zinc anomaly exists south on LO, the 100 ppm lead contour defines this feature as a separate entity from the main zone.
Sub Soil Survey
The geochemical expression in the "B" horizon is more subtle but recognizable and as in the top soil delimits the conductor axis.
The smaller southerly zone appears as a broad copper anomaly with a strongly anomalous nucleus on line O - IS. Zinc serves to define the main zone while copper and lead have an intermittent weaker expression within the zinc contour.
Conclusions
The geochemical sampling has delimited the conductor axis and pointed to two areas of relatively higher enrichment. The main zone has its highest values located on L4W-1N while the smaller feature is confined to LO and L4W at 2S with the heart on LO-2S. Both of the zones detected have accompanying geophysical expression.
Page 13
(b) GEOLOGICAL SURVEY
Outcrop in this group is virtually restricted to claims L 308812 and L 308817, elsewhere light, bouldery overburden prevails with numerous small swampy patches occupying depressed areas {Figure 16).
The geology underlying this claim group is complex with the metavolcanic suite having suffered metamorphism to the albite-epidote- amphibolite facies and is strongly sheared and intruded by at least two pulses of basic rocks.
The stratigraphy of the units has not been able to be determined and to do this would require survey of a much larger outcrop area.
Metavolcanic units present in outcrop include rhyolite, rhyolite breccia and andesite. The rhyolitic units are generally grey coloured in outcrop and range from massive to finely foliated in tuffaceous sections. Strong shearing, in places obliterating the foliation, is very common and is associated with development of heavy sericitization and lighter chloritization.
Sericite schists mapped in the south quarter of claim L 308812 may represent more intensely sheared felsic volcanic units.
Andesitic volcanics occur north of the felsic units and may underlie them. The andesites are massive, dark green-black in colour and show abundant development of chlorite. Shearing is not as well developed in the andesitic units as in the felsic units, located further south. Chlorite schists mapped near the south boundary of the property may represent, in part, sheared equivalents of the andesitic suite.
A generally East-West trending gabbroic intrusive occurs at the contact of the felsic formation and the schists. This intrusive appears to be about 200-300 ft. in outcrop width and bifurcates near the east of claim L 308812 enclosing rhyolitic and schistose country rocks. The gabbro appears closely similar to that intersected in drill hole TX-94-72.
There is no evidence in outcrop of the argillite units encountered in the drilling. These units are graphitic in part and apparently are the cause of the conductivity indicated by the electromagnetic survey.
Page 14
(c) DIAMOND DRILLING Uo&S
One hole was drilled:
Number Location
TX-94-72 Line 00, 0+20S
The drill log is shown overleaf.
Dip -450
Length
350 ft,
(lv) KNIGHT TOWNSHIP
Claims covered by the geological and geochemical survey are numbered L 316528-31 incl. and are shown on Figure 17,
(a) GEOCHEMICAL SURVEY
A total of 356 soil samples were collected from 100 ft. stations on a 400 ft. grid that covers the VEM conductive axis defined by previous survey.
Ecology and drainage
The property is extremely rugged with high rock cliffs and ledges that form local land marks. A steep scarp forms the shoreline of Pigeon Lake and continues to rise until approximately 1500 ft. laterally from the lake shore when it slopes less steeply to the east. This ridge divides the property into two main drainage systems, one into Pigeon Lake and the other into a series of bogs and creeks to the northeast. There are many minor hills and ridges that locally disrupt the major drainage pattern.
Thick stands of birch and poplar cover the flatter hill tops but are well mixed with spruce and balsam in the lower areas, Spruce becomes more common to the northeast and forms a large spruce and labrador tea bog in the northeast quarter of the grid. Large white pines cover the dryer tops of the exposed rock hills.
Soils
Freely drained areas on the sides of the many hills have formed deep podzol s while the dips and ravines are filled with gleysols. The large spruce bog in the northeast has a depth of peat development that prevented penetration with the auger available.
f
\
N
Q.
h-
QL
N
KNIGHT TWP.
TYRRELL TWP.J
AMAX POTASH LTD.
Locotion Mop
KNIGHT TWP.
Scole- l" - 1/2 Mi.
Figure 17
Page 15
Geochemical Survey
Discussion
The results of the top and sub soil surveys present a complex picture with no easily definable trends (Figures 18, 19 and 20). There is a loose east-trending-zinc feature in the sub soil while the 80 ppm lead contour in the top soil roughly approximates the location of the conductor axis. Significant and background values for the two surveys have been determined as follows.
Zn Cu Pb______ppm
(A) Top Soil
Background 100 25 45 Significant 200 40 100
(B) Sub Soil
Background 22 20 10 Significant 40 40 20
As the conductor lies on, or close to, the crest of a ridge, the complex drainage patterns coupled with the large hills have tended to disrupt any clear picutre of metal enrichment in the vicinity of the conductor. There are many isolated highly anomalous sample points the majority of which are concentrated on lines 2N and 6N near the base line.
These anomalous locations are situated on the down-hill slopes of a ridge underlain by the conductor, these high values therefore are attributed to metal!ics originating from the conductor with their location displaced by drainage.
The more anomalous values were recorded at the following stations.
Hot HC104-HN03 extraction
Grid Location Soil Cu Ni Ag Zn Pb________ppm^_______
T.S. L2S-2E podzol 32 32 .5 400 112 S.S. 6 20 .5 24 12
T.S. L2N-3E podzol 40 44 .5 820 96S.S. 4 16 .5 40 10
T. S. L2N-2W podzol 36 36 .5 352 104S.S. 4 20 .5 28 8
Page 16
Hot HC104-HN03 extraction
Grid Location Soil Cu Ni Ag Zn Pb________ppm______
T. S. L6N-2W humus 52 40 .5 384 132 S.S. M.S. - outcrop
T.S. LION-IE podzol 36 40 .5 224 176 S.S. 6 20 .5 20 12
Top Soil Survey
The only obvious feature outlined in this survey is the concentration of anomalous zinc and lead values on lines 2N and 6N on either side of the base line with the more intense being the one to the west. A series of sporadic high zinc values enclosed by an 80 ppm lead contour extends from the southeast towards the intense area on L2N. There is good correlation between the conductor axis and lead values from lines 2N to 6N.
Sub Soil Survey
Once again the lack of any appreciable spread between the assumed significant and background levels of enrichment plus the drainage problem has made interpretation tenuous. There is however, an identifiable zinc feature running at right angles to the lines that starts at L14S and terminates on line 6N. Along with this zone occur higher values along line 2N such as that seen in the top soil.
A weak copper feature runs from L6S at 13E to LION at 6E, it is located at the bottom of a steep hill and bog throughout its entirety and is attributed to down hill drainage and enrichment of the organics at their confluence.
Conclusions
It would be tenuous to attribute the source of the geochemical features present on the property to the outlined conductor with their scattered and non-definitive nature due to complex drainage patterns.
The direct correlation of some of the anomalous geochemical zones with the well defined magnetic features which are non-related to the conductor, places some of the magnetics in a position where they could be considered a possible source of the geochemical expressions. An example of this would be the coincidence of a lead feature to the magnetics on lines ION and 2S.
Page 17
(b) GEOLOGICAL SURVEY
The geological survey was conducted over 400 ft. lines on a grid used for previous geophysical surveys.
A complex of Archean metavolcanic units ranging in composition from basalt to dacite have been intruded by gabbroic and peridotitic masses (Figure 21). Unconformably overlying these units is a sequence of Huronian sediments that form the westerly boundary of the extensive tract of Huronian sediments that outcrop from Gowganda, in the south, through to Montrose Township, in the north.
The metavolcanic units extend in N-S bands on the W of the property particularly in claim L 316528. Outcrop is not sufficient to determine structure with confidence but it appears the basalt-andesite suite may be the oldest rocks exposed.
The oldest intrusive rocks present in the area appears to be the peridotite which occupies all of claim L 316530 and most of claims L 316529 and L 316531. This intrusive is differentiated in part, at least, with a hornblende-rich phase being observed near the East boundary of claim L 316530.
A N-S trending elliptical-shaped body of gabbro outcrops in the centre of the claim group and appears to be intrusive into other Archean units. The gabbro is dark grey in colour, massive, poorly jointed and is composed of interlocking pyroxene crystals showing only minor interstitial feldspar. The rock is moderately altered with ragged amphibole and chlorite surrounding pyrozene crystals. The rock is moderately magnetic.
Overlying the Archean formations is a thick sequence of Huronian sediments consisting of quartzites, arkose, and conglomerate. These rocks have been described in much detail in many ODM Reports and are generally held to have no base metal potential. Only a cursory examination of these rocks was made in the field.
(c) DIAMOND DRILLING
The electromagnetic conductor was seen from the geological survey to transect several rock types ranging from peridotite to gabbro to felsic metavolcanic. This coupled with a weak, poorly defined soil geochemical signature indicated the conductor to have a low priority for drill evaluation. Consequently, no drilling was attempted on this property under the present Exploration Assistance Agreement.
Page 18
IV. CONCLUSIONS
In the Halliday-Midlothian, Burrows and Fawcett Township claim groups geological and soil geochemical surveys enhanced the likelihood of conductive horizons, outlined by prior geophysical surveys, having economic tenor. Targets were tested by diamond drilling and, although the conductors were found to be due to graphitic argillite units, sulphides were encountered in each hole. Unfortunately, assaying these sections proved them to be of no economic significance.
The claims in Knight Township were covered by geological and geochemical surveys but the results did not lend encouragement to drill testing the conductor outlined by previous surveys.
Limited Timmins^Ontario
Page 19
V. APPENDIX I SOIL GEOCHEMICAL SURVEYS
(i) Sampling
Soil samples were collected at 100 ft. stations on 400 ft. lines over the Burrows, Fawcett and Knight Township properties. 800 ft. lines were employed for sampling the Halliday-Midlothian Township property due to the extreme length of the conductor. On this property closer spaces sampling was planned if results of preliminary diamond drilling warranted.
Field collection and sample preparation was supervised by Randy Roussain, Amax Potash Limited, Timmins.
Two samples were collected at each station -No. l in the sub soil represented the B horizon and No. 2 in the top soil represented the A horizon. In low lying, swampy areas considerable accummulations of humified organic matter were encountered and in such areas two samples were collected: No. l from immediately below the forest litter and No. 2 from a depth of 12-18 inches. In very wet areas where the soil was not sufficiently cohesive, only one sample was obtained.
A total of 1122 samples were collected as follows:
Halliday-Midlothian Twp. : 434Burrows Twp. : 172Fawcett Twp. : 160Knight Twp. : 356
(11)Samples were placed in wet-strength Kraft envelopes, shipped
to the Timmins office and dried. Further preparation and analysis was performed at the Amax Laboratory, 2225 Springer Avenue, Burnaby, British Columbia.
(i i i) Analytical Procedure
-80# fractions were analyzed for Cu, Ni, Pb, Ag, and Zn by Atomic Absorption techniques following digestion in hot HC104-HN03. Sample numbers, field coordinates and analytical results are included in Volume 2 as Figure 22.
GEOCHEM SAMPLE INDEX
Township
Halliday
-
Grid
Grid #1
*
.
i
n
i
ji
l
l
i
t
t
l
Co-ordinate
L20W 8+OOS
7+OOS
6+OOS
i
1 5+OOS
4+OOS
3+OOS
2+OOS
1+OOS
0+00
1+OON
2+OON
3+OON
4+OON
5+OON
6+OON
Sample Type
Soil
1
-.
*
!
1
'
' 7+OON
! :
!?
8+OON
L12W 8+OONi
Horizon
S.S. 40"
T. S. 4"
S.S. TfVS.o/c
T. S. 6"
S.S. 14"
T. S. 2"
S.S. 8"
T. S. 2"
S.S. 12"
T.S. 4"
S.S. 10"
T.S. 2"
S.S. 10"
T.S. 2"
S.S. 8"
T.S. y, ' 2"
S.S.' 10"
T.S. 6"
S.S. 30"
T.S. 6"
S.S. 14"
T.S. 3"
S.S. ft.S. o/c
T.S. 2"
S.S. 16"
T.S. 3"
S.S. 8"
T.S. 3"
S.S. 12"
T.S. 2"
S.S. 8"
T.S. 1"
S.S. 14"
Sample No.
805
806
807
808
809
810
811
812
813
814
815
816
817
.. 818
819
820
821
822
823
1 824
825
826
827
828
829
830
831
832
833
834
835
836
a:7
T.S. 2" j 838i
S.S. 14" j - 839
T.S. 2" 840
1 r
GEOCHEM SAMPLE INDEX
Township
Halliday
,
|
Grid
Grid #1
'
1sr
i
Co-ordinate
L12W 7+OON
6+OON
5+OON
4+OON
3+OON
2+OON
, 1+OON
0+00
1+OOS'
2+OOS
3+OOS
; 4+OOS
; 5+OOS
.
6+OOS
7+OOS
8+OOS
L4W 8+OOS
Sample Type
Soil
u-
i
7+OOSi
\
Horizon
S.S. 18"
T.S. 2"
S.S. 10"
T.S. 1"
S.S. 14"
T.S. 2"
S.S. 10"
T.S. . 5"
S.S. 8"
T.S. 3"
S.S. lf|.S o/c
T.S. 2"
s.s. r\.s. o/0T.S. 3"
S.S. 16"
T.S. 2"
S.S. 12"
T.S. 3"
S.S. 12"
T.S. 2"
S.S. 14"
T.S. 3"
S.S. 18"
T.S. 2"
S.S. 10"
T.S. 3"
S.S. 18"
T.S. 6"
S.S. 4"
T.S. 2"
S.S. 10"
T.S. 4"
S.S. 15"
T.S. 3"
S.S. 12"
T.S. 2"
' Sample No.
841
842
843
844
845
846
847
848
849
850
851
852
853
854
855
856
857
858
859
860'
861
862
863
S69 ?*V
865
866
867
868
869
870
871
872
873
874
875
876
GEOCHEM SAMPLE INDEX
Township
Halliday
'
-
i
Grid
Grid #1
Anomaly #1
.
Co-ordinate
L4W 6+OOS
5+OOS
4+OOS
3+OOS
2+OOS
1+OOS
0+00
1+OON
2+OON
3+OON
, 4+OONi . i
5+OON
i
6+OON
7+OON
i 8+OON
L4E 8+OON
: 7+OON
6+OON
Sample Type
Soil
.i
Horizon
S.S. 12"
T.S. 4"
S.S. 2"
T.S. 1"
s.s. y). s o/cT.S. 2"
S.S. 8"
T.S. 3"
S.S. 22"
T.S. 6"
S.S. 10"
T.S. 2"
S.S. 8"
T.S. 1"
S.S. 14"
T.S. 2"
S.S. 13"
T.S. 2"
S.S. 16"
T.S. 3"
S.S.' 16"
T.S. 2"
S.S. 8"
T.S. 2"
S.S. 14"
T.S. 3"
S.S. 12"
T.S. 1"
S.S. 10"
T.S. 4"
S.S. 12"
T.S. 4"
S.S. 10"
T.S. 4"
S.S. 24"
T.S. 2"
Sample No.
877
878
879
880
881
882
883
884
885
886
887
888
889
890
891
892
893
894
895
896
897
898
1 899
900
901
902
903
904
905
906
907
908
909
910
911
912
GEOCHEM SAMPLE INDEX
Township
Halliday
.
Grid
Anomaly #1
'
Co-ordinate
L4E . 5+OON
4+OON
3+OON .
2+OON
1+OON
0+00
1+005
2+OOS
3+0031
4+OOS
5+OOS
6+OOS
7+OOS
8+OOS
L12E 8+OOS
7+OOS
6+OOS
i
5+OOS
i
Sample Type
Soil
i
!
Horizon
S.S. 14"
T. S. 3"
S.S. 20"
T. S. 3"
S.S. 14"
T.S. 2"
S.S. 12"
T.S. 2"
S.S. 14"
T.S. 1"
S.S. 22"
T.S. 14"
S.S. 8"
T.S. 1"
S.S. 10"
T.S. 3"
S.S. 8"
T.S. 3"
S.S. 20"
T.S. 3"
S.S. 14"
T.S.' 1"
S.S. 16"
T.S. 1"
.S.S. 14"
T.S. 1"
S.S. 14"
T.S. 1"
S.S. 6"
T.S. 1"
S.S. 24"
T.S. 15"
S.S. . 36"
T.S. 20"
.S.S. 48"
T.S. 6"
Sample No.
913
914
915
916
917
91-8
919
920
921
922
923
924
925
926
927
928
929
930
, 931
932
933
934
935
936
937
938
939
. 940
941
942
943
944
945
946
947
948 .
GEOCHEM SAMPLE INDEX
Township
Halliday
.
-
i
Grid
Anomaly #1
i
i
i
i
.
i
i
Co-ordinate
LI 2E 4+OOS
3+OOS
2+OOS
1+OOS
0+00
1+OOS
2+OON
3+OON
4+OON
5+OON
.
6+OON
7+OON
8+OON
L20E 8+OON
7+OON
6+OON
5+OON
4+OON
Sample Type
Soil
i
Horizon
S.S. 38"
T.S. 6"
S.S. 36"
T.S. 6"
S.S. 42"
T.S. 6"
S.S. 30"
T.S. 6"
S.S. 12"
T.S. 2"
S.S. 8"
T.S. 4"
S.S. 40" jT.S. 8"
S.S. 42"
T.S. . 12'
S.S. 36'
T.S. 8'
S.S. 40'
T.S? 12'
S.S. 46'
T.S. 16'
S.S. 36'
. T.S. 8'
S.S. 40'
T.S. 12'
S.S. 36'
T.S. 12'
S.S. 16'
T.S. 10'
S.S. 28'
T.S. 8'
S.S. 12'
T.S. 3'
S.S. 8'
T.S. T
Sample No.
949
950
951
952
953
954
955
956
957
958
959
960
961
962
963
964
965
966
967
968
969
970
971
972
973
974
975
976
977
978
979
980
981
982
983
984
GEOCHEM SAMPLE INDEX
Township
Halliday
Grid
Anomaly #1
*
Co-ordinate
L20E 3+OON
2+OON
. 1+OON
0+00
: i+oos
2+OOS
i
| 3+OOS
: 4+OOS
5+OOS
6+OOS
i
7+OOS
8+OOS
Sample Type
Soil j
-
-
Horizon
S.S. 8"
T. S. 2"
S.S. 10"
T. S. 2"
S.S. 6"
T.S. 2"
S.S. 12"
T.S. , 1"
s.s. lo"T.S. 2"
S.S. 12"
T.S. 2"
S.S. 10"
T.'S. ^-5"
S.S. 6"
T.S. 1"
S.S. 8"
T.S. 3"
S.S. 4"
T.S. 1"
S.S. 12"
T.S. 3"
S.S. 28"
T.S. 8"
Sample No.'985
986
987
988
989
990
991
992
993994'
995
996
997
998
999
1000
1001
1002
1003
1004
1005
1006
1007
1008
/;
GEOCHBM SAMPLE INDEX
Township j Grid
Halliday. .
1 ,
_
'
1
AN: #1
1
1
j
|It
f! \ ' i
:
Co-ordinate
L28E 2+OOS
1+OOS
0+00
1+OON
2+OON
3+OON
i
4+OON
5+OON
6+OON
7+OON
. i 8+OON
L36E 8+OON
7+OON
6+OON
5+OON
4+OON
3+OON
Sample Type
Soil
i
'
;
:
: ' *
V i
! : ! : ' '
i . ' .ali
2+OON \•ii
' ' ' l
Horizon
S.S. 32"
T.S. - 12"
S.S. 30"
T.S. 10"
S.S. 42"
T.S. 12"
S.S. 10"
T.S; 2"S.S. 8"
T.S. 2"
S.S. 14"
T.S. 3"
S.S. 10"
T.S. 4"
S.S. 12"
T.S. 4"
S.S. 4"
T.S. 10"
S.S. 14"
T.S. 8"
S.S. 8"
T.S. 3"
S.S. 8"
T.S.' 2"
S.S. fl.S o/c
T.S.' 8"
S.S. 12"
T.S. 3"
S.S. 12" .
T.S. 2"
S.S. 5"
T.sL 2"
S.S. 8"
Sample No.
1009
1010
ion1012
1013
1014
1015
1016
1017
1018
1019
1020 -
1021
1 022
1023
1024
1025
1026
1027
1 028
' .1029
1030
1031
1032
1033
1034
1035
1036
.1037
1038
1039
1040
1041
T.S. ] 2 " j 1042
S.S. ; 16" 1043
T.S. .3" l 1044
GEOCHEM SAMPLE INDEX
Township
Halliday
.
Grid
AN: #1
l ; . Co-ordinate \ Sample Type
L36E 1+OON
Q+00
1+OOS
2+OOS
3+OOS
4+OOS
L44E 6+OOS
5+OOS
4+OOS
1
3+OOS
2+OOS
1+OOS
0+00
1+OON
'* 'i 1
. 2+OON
3+OON'
if\
j' i
l
4+OON
Soil
:
' i -
1 ' i
V
^
i
5+OON |
4
Horizon
S.S. 10"
T.S. 2"
S.S. 14"
T.S. 6"
S.S. 16"
T.S. 2"
S.S. 14"
T.S. 1"
S.S.- 10"
T.S. 2"
S.S. ' 10"
T.S. 2"
S.S. 12"
T.S. 2"
S.S. 12"
T.S. 2"
S.S. 12"
T.S. 2"
S.S. 12"
T.S.. 2"
S.S. 32"
T.S. 12"
S.S. 14"
T.S. 4"
S.S. 10"
T.S. 2"
S.S. 10"
T.S. 1"
S.S. 12"
T.S. 2"
S.S. 10"
Sample No.
1045
1046
1 047
1048
1049
1050
1051
1052
1053
1054
1055
1056
1057
1058
1059
1060
' 1061
1062
1063
1064
1065
1066
1067
1068
1069
1070
1071
1072
1073
1074
1075\
T.S. 4"
S.S. 8"
T.S. rS.S. 10"
T.S. 3"
1076
1077
1078
; 1079
1080
.
GBOCHEM SAMPLE INDEX
t
Township j Grid
Halliday
'. '
-
.
AN: #1
'
-
'
.il
i
- 'i
-
.1
Co-ordinnte f Sample Type
L44E 6+OON
7+OON
8+OON
9+OON
L52E 8+OON
7+OON
6+OON
5+OON
4+OON' \
3+OON
2+OON
. 1+OON
0+00
1+OOS
i
1 2+OOS
Soil }
.
i
V
: ' *
i " - ' 1 '. ,'. :: 3+OOS' ,
4+OOS
5+OOS
1
i :i
l '
Horizon
s.s. Yl-S.o/cT.S. 3"
S.S. 8"
T.S. 2"
S.S. 14"
T.S. 1"
S.S. 16"
T.S. 4"
S.S. 12"
T.S. 2"'
S.S. 14"
T.S. 2"
S.S. 10"
T.S, 2"
S.S. 10"
T.S. 1"
S.S. 12"
T.S. 2"
S.S. 16"
T.S. 3"
S.S. 10"
T.S. 1"
S.S. 14"
T.S. 6"
S.S. 8"
T.S. 2"
S.S. ' 10"
T.S. 4"
S.S. 5"
T.S. 2"
Sample No.
1081
1082
, 1083
1084
1085
1086
1087
1088
1089
1090
1091
1092
- 1093
1094
1095
1096
1097
1098
1099
1100
1101
1102
1103
1104
.1 1 05
1106
1107
1108
, 1109
1110.S.S. 12" j 1111
T.S. 1" j 1112
S.S. 12"
T.S. . r1
S.S. 12"
1113
1114.1115
T.S. 4" j 1116
GEOCHEM SAMPLE INDEX
Township | Grid
Halliday
.
.
i
AN: #1 ;
- ' l
j
j
( '1
1AP•j1
f
l
lll
'
1
Co-ordinate
L60E 5+OOS
Sample Type
Soil
4+OOS
3+OOS
2+OOS
1+OOS
0+00
1+OON
2+OON
3+OON
4+OON
5+OON
6+OON i
7+OON
8+OON
,.
.
i
V
9+OON * -*
:" ! :1 'L68E 10+OOtj
19+OON
1
8+OON
!
|
1
Horizon
s.s. \vs.o7cT.S. 4"
S.S. 6"
T.S. 1 2"
S.S. .8"
T.S. 2"
S.S. 15"
T.S. -1"
S.S. 14"
T.S. 2"
S.S. 10"
T. S.. 1"
S.S. 16"
T.S. 2"
S.S. .22"
T.S. 4"
S.S. 14"
T.S. 2"
S.S. 12"
T.S. 2"
s.s. Y\-S. 0/ 0T.S. 8"
S.S. 10"
T.S. 2"
S.S. 4"
T.S. 2"
S.S. 14"
T.S. 2"
S.S. y^5 o/c
T.S. 2"
S.S. 10"
T.S. 2"
S.S. 10" j
T.S. 2"
S.S. VV5.0/C
T.S. 2"
•Sample No.w
1117
1118
1119
1120
1121
1122
1123
1124
1125
1126
1 1 27
1128
1129
1130
1131
1132
1133
1134
1135
1136
1137
1138
1139
1140
1141
1142
1143
1144
1145
1146
1147
- 1148
1149
1150
1151
1152'
GEOCHEM SAMPLE INDEX
Township
Halliday*
•'
i,
l.
.'
Grid
AN: #1
•j
i
ij.
j
'
^
'
'
i
M
Co-ordinate
L68E 7+OON
6+OON
5+OON
4+OON
3+OON
2+OON
. .1+OON
-
0+00
1+OOS
2+OOS
3+OOS
4+OOS
5+OOS
6+OOS
L76E 4+OOS
3+OOS
2+OOS
1+OOS
Sample Type
Soil
.
:
i
| . . "" '.
A
l ;
;
Horizon
S.S., 12"
T.S. 2"
S.S. 10"
T.S. 2"
S.S. 10"
T.S. 2"
S.S, 6"
T.S. 3"
S.S. 12"
T.S. i 3"
S.S. 16"
T.S. 4"
S.S. 14"
T.S. 3"
S.S. 6"
T.S V . 1" "
S.S. 12"
T.S. 3"
S.S. 8"
T. S; 2"
S.S. 20"
T.S. 3"
S.S. 12"
T.S. 2"
S.S. 24"
T.S. 3"
S.S. 10"
T.S. 4"
S ^ Vi cr n/r * ' Fi * j '
T.S. 2"- '
S.S. 24"
T.S. 2"
S.S. 26"
T.S. 1"
S.S. 12"'
T.S. 3"
Sample No.
. 1153
1154
1155
1156
11 57
1158
1159
11 60
1161
1162
1163
1164
1165
1 1 66
1167
1 1 68
.1169
1170
1171
1172
1173
1174
1175
1176
1177
1178
1179
1180
1181
1182
1183
1184
1185
1186
1187
1188
GBOCHEM SAMPLE INDEX
Township f Grid | Co-ordinate | Sample Type
Halliday AN: #1•-
'
-
a
'
'.
.
L76E 0+00
1+OON
2+OON
i
3+OON
i
4+OON
5+OON
6+OON
7+OON
8+OON
9+OON
10+OON
11+OON
1 2+OON
1 3+OON
a
\ ' '
| '
j
i !i
i i
L84E 1 6+OON
1 5+OON
1 4+OON
1 3+OON
Soil
i
i
,.
i -
•-
V
i ..
i
5
j ; ' .-
•; ' j ' ' : ' - -
Horizon
S C \A f* A /O
* ^ * |\ O* ® ' ^
•T.S. . 1"
S.S. 8"
T.S. 2"
S.S. 3"
T.S, 2"
S.S. 11"
T.S. 2"
S.S. 14"
T.S. 3"
S.S. 8"
T.S. 4"
S.S. 12"
T.S. 1"
S.S. 12"
T.S. 2"
S.S. 9"
T.S. 2"
S.S. 24"
T.S. 3"
S.S. 11"
T.S. 3"
S.S., 14"
T.S. 1"
S.S. 8"
T.S.' 2"
S.S. 8"
T.S. 3"
S.S.' 13"
T.S. 4"
S.S. 11"
T. Si 2"• iS.S. 22"
T.S. 3"
.
Sample No.
1189
1190
1191
( ' 1192
1193
1194
1195
1196
1197
1198
1199
1200
1201
1202
1203
1204
1205
1206
1207
1208
1209
1210
1211
1212
1213
1214
1215
1216
.1217
1218
1219
i 1220
1221
! 1222
S.S. : 12" j 1223
T.S. 3" 1224
i
GEOCHEM SAMPLE INDEX
Township
Halliday
fi -Grid
AN: #1
Co-ordinate
L84E 12+OON
11+OON
10+OON
9+OON
8+OON
. 7+OON
6+OON
Samplei Type
Soil
1
:
Horizon
S.S. 8"
T.S. . 2"
s.s. YVS. 0/0T.S. 8"
S.S. 8"
T.S. 3"
s.s. y\.5.o7cT.S. 6"
S.S. 8"
T.S. 3"
S.S. 5"
T.S. ^ 1"
S.S. 10"
T.S. 5"
Sample No.
1225
1226
1227
1228
1229
1 230
1231
1232
1233
1234
1235
1236
1237
1238
GEOCHEiM SAMPLE INDEX
jTowiisln j)
Knight
.
Gv:i.J
AN: i!8
.
'
tV
i
i
i
Co-ordi.nal,o
L22S 15+OOE
14+OOE
13+OOE
L18S 7+OOE
8+OOE
9+OOE
10+OOE
11+OOE
12+OOE
13+OOE
14+OOE
1 5+OOE
16+OOE
L14S 16+OOE
-' 15+OOE
14+OOE
13+OOE
Mnmplo -Typo
Soil
i
' !
i
: r
i
i ,
V
flf
-
v. :
1 2+OOE i
l' :
Horixon
S.S. 14"
T.S. 4"
S.S. ' 3"
T.S. 1"
S.S. 4"
T.S. 1"
S.S. y\.s.o7cT, S. 2"
S.S. y^ ^ 0/C
T.S,,^ - 1"'
S.S. 7"
T.S. 4"
S.S. 10"
T.S. 2"
S.S. 8"
T.S. 3"
S.S. 14"
T.S. 3"
S.S. 7"
T.S. 4"
S.S. 12"
T.S. 2"
S.S. 11"
T.S. l"
S.S. 12"
T.S. 1"
S.S. ' 11"
T.S. .2"
. S.S. 10"
T.S. 3"i
SciifijiJo Mo.
1287
1288
, 1289
1290
1291
1292
1293
1294
1295
1296
1297
1298
1299V
1300
1301
1302
1303
1304
1305
1306
1307
1308
1309
1310
1311
1312
1313
1314
, 1315
1316
S.S. , 9" j 1317
T.S. 2"
S.S. 10"
T.S. . 1"
1318
j' 1319
. 1320
S.S. . 9" | 1321
T.S. 3" j 1322
. i '
GEOCHEM SAMPLE INDEX
Township | Grid | Co-ordinate
Knight
,
.
'
i
AN: 18 :
t
i
.
L14S 1 1+OOE
10+OOE
9+OOE
8+OOE
7+OOE
6+OOE
5+OOE
4+OOE
LI OS 1+OOW
0+00
1+OOE
2+OOE
3+OOE
4+OOE
5+OOE
6+OOE
7+OOE
8+OOE
i
1
Sample -Type
Soil i
. i
-
-.: '
;' ' j, 1
v :
*
(
j' . : -
Horizon
S.S. 12"
T.S. 3"
S.S. 13"
T.S.' 2"
S.S. 12"
T.S. 3"
S.S. 6"
T.S, '1"
S;S. 10"
T.S. 2"
S.S. 9"
T.S. 2"
S.S. 10"
T.S. 3"
S.S. YVS/o/c
T.S. 1"
s.s. y\.s o/cT.S. 1"
S.S. 10"
T.S. 3"
S.S. 6"
T.S. 3"
S.S. 10"
T.S. 3"
S.S. 6"
T.S. 3"
S.S. 12"
T.S. 3"
S.S. 18"
T.S. 6"
S.S. 14"
T.S. 2"
S.S. 10"
T.S. 2"
S.S. 10"
Sample No.
1323
1324
1325
1326
1327
1328
1329
1330
1331
1332
1333
1334
1335
1336
1337
' 1338
1339
1340
1341
1342
1343
1344
1345
1346
1347
1 348
1349
1350 ..
1351
1352
1353
1354
1355
13561
1357
T.S. 2" j. 1358
J ;- .' ' -
o GEOCHEM SAMPLE INDEX
f Township | Grid
Knight j AN: #18; -. - ' - - |
1
1
1'
' . j
iik t i
j
Co-ordinate
LI OS 9+OOE
10+OOE
11+OOE
12+OOE
13+OOE
14+OOE
15+OOE-
L6S 4+OOW
3+OOW
2+OOW
1+OOW
0+00
1+OOE
2+OOE
3+OOE
4+OOE
Sample Type
SOU l
.i i
;
:
-
-' '
!
V
l'' ' '
5+OOEJ :
6+OOE
1 : ; ; .
Horizon
S.S.' 9"
T.S. 3"
S.S. 10"
T.S. 2"
S.S. 16"
T.S. 3"
S.*, 12"
T.S. 4"
S.S. 10"
T.S. ; 3"
S.S. 10"
T.S. 2"
S.S. 10"
T.S. 2"
S.S. fts.o/c
T.S. 5"
S.S. 14"
T.S. 4" .
S.S. 6"
T.S. 3"
S.S. 4"
T.S. 3"
S.S. IT"
T.S. 3"
S.S. 10"
T.S. 2"
S.S. 10"
T.S. ' .4"
S.S. 9".
T.S. 4"
S.S. 4"
T.S. 4"
S.S. 13"
T.S. 3"
S.S. 10"
T.S. 3"
Sample No.
1359
1360
1361
1362
1363
1364
1365
1366
1367
1368
1369
1370
1371
1372
1373
1374
1375
1376
1377
1378
1379
1380
1381
1382
1383
1384
1385
1386
1387
1388
1389
1390
1391
1392
1393
1394
o GEOCHEM SAMPLE INDEX
Township j
Knight'
,
'ii
,
1
Grid
AN: #18
t
' ;
i1
11 - 1
j
1
.' 'ii
l
11
.;
i
Co-ordinatej
L6S 7+OOE
8+OOE
i 9+OOE
1 0+OOE
n+ooE
12+OOE
j13+OOE
14+OOE
15+OOE
L14N 1 0+OOE
9+OOE
8+OOE
7+OOE
6+OOE
5+OOE
4+OOE
3+OOE
2+OOE
I
Sample Type
Soil
i .
t '' -
: "
\ '
\
j
V
i :'
j :
1 ' :
Horizon
S.S. 26"
T.S. 12"
S.S. 10"
T.S. 2"
S.S. 7"
T.S. 4"
S.S. 12"
T.S. 3"
S.S. 12"
T.S. 1"
S.S.' 10"
T.S. 2"
SSS. V 15"
T.S. 2"
S.S.' 9"
T.S. 3"
S.S. 10"
T.S. 1"
S.S. 13"
T.S. 3".
S.S. 30"
T.S. \ 1 0"
S.S. 36"
T.S. 10"
S.S. 36"
T.S. 10"
S ^ \\ C n/r * o * r i *^ '
T.S. 3"
S.S. 7"
T.S. 6"
S.S. 8"
T.S. 2"
S.S. 5"
T.S. 1"
S.S. 3"
T.S. 1"
Sample No.
1395
1396
1397 .
1398
1399
1400
1401
1402
1403
1404
1405
1406
' 1407
' 1408
1409
1410
'1411
1412
1413
1414
1415
1416
1417
1418
. 1419
1420
1421
1422
1423
1424
14251
1426
1427, ,
1428
1429
1430
GEOCHEM SAMPLE INDEX
Township j
Knight
- -;*
.
.
Grid
AN: #18
*
j
'
i
Co-ordinate j
L14N 0+00
l
: 1+OOWi
: 2+OOW
3+OOW
: 4+OOW
5+OOW
6+OOW
: 7+OOW
i j
8+OOW
L2S 15+OOE
14+OOE
13+OOE
12+OOE
11+OOE
lOitOOE
9+OOE
8+OOE
j7+OOE
\ '
m
Sample Type
Soil ;'
: '
:
' :
j .' v
*
:
.
V ' - '
'i ' ;*
1
l
Horizon
S.S. 14"
T.S. 2"
S.S. 10"
T.S. 3"
S. S . 1 8"
T.S. 6"
S.S. 18"
T.S. 6"
S.S. 9"
T.S. 2"
S.S. 8"
T.S. 2"
S.S. 8"
T.S. 1"
S.S. 10"
T.S. 1"
S.S. 10"
T.S. 2"
S.S. 18"
T.S. - 2"
S.S. 8"
T.S. 1"
S.S.' 8".
T.S. 1"
S.S. y\ c 0/C
T.S. 1"
S.S. 32"
T.S. 10"
S. S J 8"
T.S. 2"
S.S. 11"
T.S. -l"
S.S. ; 10"
T.S. 1"
S.S. 22"1 .
T.S. T
Sample No.
.1433
1434
1435
1436
1437
1438
1439
1440
1441
1442
1443 ;
1444
1445
1446
1447
1448
1449
' 1450
1451
1452
1453
1454
, 1455
1456
1457
1458
1459
1460
1461
1462
T463
1464.
1465
1466
1467
! 1468
o GEOCHEM SAMPLE INDEX
Township
Knight
- -
.
1
- ( \
..
r
i
i .
Knight i
1
Grid
AN: #18
, •,
\
:
9
'
AN: #18 -
I
i
Co-ordinate
L2S 6+OOE
|
5+OOE
4+OOE
3+OOE
2+OOE
1+OOE
0+00
1 1+OOW
'
2+OOW
] 3+OOW
L2S 4+OOW
5+OOW
6+OOW
7+OOW
•t*
LION 10+OOE
;
9+OOE1
8+OOE
j 7+OOE'i
l
Sample Type
Soil ;-
_
-
;
Soil
V-
' ' -' ,-
Soil
.
3
Horizon
S.S. 10"
T.S. 2"
S.S. 11"
T.S. 2"
S.S. 10"
T.S. 8"
S.S. 12"
T.S. 2"
S.S. 12"
T.S. 1"
S.S. 10"
T.S. 1-1/2'
S.S. 10"
T.S. 3"
S.S. 9"
T.S. 2"
S.S. 19"
T.S. 1"
S.S. 10"
T.S. 2"
S.S. 12"
T.S. 1"
S.S. 10"
T.S. 3"
S.S. 14"
T.S. 4"
S.S. 8"
T.S. 2"
S.S. 36"
T.S. 10"
T.S. 10"
S.S. 26"
T.S. 10"
S.S. 40"H
T.S. 10"
Sample No.
1469
1470
1471
1472
1473
1474
1475
1476
1477
1478
1479
1480
1481 : ' 1482
1483
1484
1485
1486
1487
1488
1489
1490
1491
1492
1493
1494
1495
1496
1497
. . ,. 1498 ,
1499
1500
. 1501
1502
l 1503
1504
GEOCHEM SAMPLE INDEX
Township j Grid jj Co-ordinate j Sample Type
Knight
.
'
AN: #18
' -
'
! .
*t
.
'
-
'
i
i
LI ON 6+OOE
5+OOE
4+OOE
3+OOE
2+OOE
1+OOE
0+OOE
1+OOW
2+OOW
3+OOW
4+OOW
5+OOW
,
6+OOW
i 7+OOW
: 8+oow
9+OOW
L2N ! 11+OOW
soil i
, .
.
[ . ' ,.
'
' ' \ -
: ' *- .-
\
10+OOW j
i
i !
Horizon
S.S. 40"
T.S. 6"
S.S. 12"
T.S. 2"
S.S. 15"
T.S. 1"
S.S. 9"'
T.S. 2"
S.S. 26"
T.S. 1"
S.S. 8"
T.S. 1"
S.S. 13"
T.S. 1"
S.S. 9"
T.S. 1"
S.S. 10"
T.S. 2"
S.S. 36"
T.S. 10"
S.S. 34"
T.S. 10"
S.S. 10"
T.S. ' 2"
S.S. 11"
T.S. 1"
S.S. 7"
T.S. 1"
S.S. 9"
T.S. . 1"
S.S. , 4"
T.S. 2"
S.S. 15"
T.S. . 1"
S.S. 7"
T.S. 1"
Sample No.
1505
. 1506
1507
1 508
1 509
1510
1511
1 51 2
1513
. 1514 '
1515
1516
1517 '
1518
1519
1520
1521
1522
.1523
1524.
: 1525
1526
1527
1 528
1529
, 1530
1531
. 1532
1533
1534
1535
1536
1537
1538
1539
I54d
o GEOCHEM SAMPLE INDEX
Township
Knight
1
Grid
AN: #18
ktii
i
i Co-ordinate
L2N 9+OOW
8+OOW
7+OOW
6+OOW
5+OOW
4+OOW
3+OOW
2+OOW
1+OOW
0+00
1+OOE
2+OOE
3+OOE
4+OOE
5+OOE
6+OOE
7+OOE
1
8+OOE
1
Sample Type
Soil i
i
i '
1
i
-
i -
i . : t "
1 ' i
i
j
i. - - .
\
l ' '':-
: - . '
Horizon
S.S.' 14"
T.S. 2"
S.S. 10"
T.S. 1"
S.S. 9"
T.S. 3"
S.S. 8"
T.S. 1"
S.S. 13"
T.S. 1"
S.S. 12"
T.S,, , , 1"
S.S. 6"
T.S. 1"
S.S. 8"
T.S. 2"
S. S f 7 "
T.S. 1"
S.S. 10"
T.S. , 1"
S.S. 8"
T.S. T
S.S. 11"
T.S. 2"
S.S. 7"
T.S. 2"
S.S. 16"
T.S. , ' 1"
S.S. 10"
f- q "P"1 t O * c.
S.S. 13"
T.S. 2"
S.S. 40"
T.S, 8"
S.S. 48"
T.S. 10"
Sample No.
1541
1542
1543
1544
1545
1546
1547
1548
1549
1550
.1551
1552
1553
1554
1555
1556
1557
1558
1559
1560
1561
1562
1563
1564
1565
1 566
1567
1568
1569
1570
1571
1572
1573
1574
1575
1576
i "'," . .
o GEOCHEM SAMPLE INDEX
' 1 Township f Grid j Co-ordinate
Knight
.
,
i i
-
AN: #18
i
,.
.- - ;
'
i
L2N 9+OOE
10+OOE
11+OOE
12+OOE
13+OOE
14+OOE
15+OOE
L6N 15+OOE
14+OOE
13+OOE
12+OOE
11+OOE
10+OOE
9+OOE
8+OOE
7+OOE
6+OOE
Sample Type
Soil
! -;:' :
f.
\ ' "
j ' . ' .
!
i
1
.
V .
:
1 ' 'a 5+OOE j
1 ; '' . .-J . l ;
Horizon
S.S. 48"
T.S. 10"
S.S. 28"
T.S.) 10"
S.S. 48"
T.S. TO"
S.S. 136"
T.S. 10"
S.S. 33"
T.S. 10"
S.S. 40"
T.S. 10"
S.S. 36"
T.S. 6"
S.S. 48"
T.S, 10"
S.S. 40"
T.S. 8"
S.S. 36"
T.S. 10"
S.S. 28"
T.S. 10"
S.S. 10"
T.S. 6"
S.S. 36"
T.S. 8"
S.S. 34"
T.S. 10"
S.S. 40"
T.S. 8"
S.S. 36"
T.S. 10"
S.S. 26"
T.S; 10"S.S. 18"
Sample No.
1,577
1 578
1579
1580
1581
1582
1583
1584
1585
1586
1587
1588
1589
1590
1591
1592
1593
1594
1595
1596
1597
1598
1599
1600
1601
1602
1 603
1604
1605.
1606
1607
1608
1609
1610
1611. -
T.S. .3" j 1612
''- . i : : ij -' . a ,
GEOCHEM SAMPLE INDEX
Township
Knight
'
C
-.'
- -
p
-
j
Grid
AN: #18
,
i
1
- -
f
'
-
Co-ordinate i
L6N 4+OOE
3+OOE
2+OOE'
1+OOE
0+00
1+OOW
2+OOW
3+OOW
4+OOW
5+OOW
6+OOW
7+OOW'
8+OOW
9+OOW
^ . 10+OOk
f
1
.
Sample :Type1
Soil
1 ' l
1
' ' . ;
t
. '
l . .;-'.'
i ; .
i
. . | . .
!
If" ,
:i
| . . . '
.
Horizon
S.S. 16"
T.S. ' 1"
S.S. 10"
T.S. 3"
S.S. 15"
T.S. 2"
S.S. 8"
T.S. 1"
S.S. 9"
T.S. 1"
S.S. 11"
T.S. 1"
S.S. yrc o/c
T.S. 1"
S.S. 8"
T.S. 2"
S.sl 9"
T.S. 3"
S.S. ; 18"
T.S. 2"
S.S. 8"
T.S. 2"
S.S. 22"
T.S. 10"
S.S. Y\^ 0/0
T.S.' 8".
S.S. 9"
T.S. 3"
S.S. 12"
T.S. '3"
Sample No.
1613
1614
1615
1616
. 1617
1618
1619
1620
1621
1622
' 1623
1624
1625
1626
1627
1628
1629
1630
1631
1632
1633
' 1634
1635
1636
1637
1638
1639
1640
1641
1642
1
'
.
GEOCHEM SAMPLE INDEX
i Township
Burrows '
t
-
.
Grid
Bu #2 Gp. 1
t
\
' l\\
'
:
i. ,
Co-ordinate . j
L4E 6+OON
i
5+OON
: 4+OON
3+OON
2+OON
i 1+OON
l 0+00. t
1+OOS
;
: 2+OOS
: 3+OOS
4+OOS
5+OOS
6+OOS
L4W 6+OOS
5+OOS
4+OOS
3+OOS
2+OOS
i
Sample : Type
Soil
l
i ' '
' ,. -.
: '
i *
i i , ' i.* i
i . i*
1
1 . ;
Horizon
S.S. 14"
T. S. 1"
S.S. . 8"
T.S. 2"
S.S. 5"
T.S. T1
S.S. 9"
T.S.' 2"
S.S. 6"
T.S. rS.S. 7"
T.S. 1"
S.S. 8"
T.S. 1"
S.S. 3"
T.S. 1/2"
S.S. 4"
T.S. 2"
S.S. 9"
T.S. ' 1"
S.S. 8"
T.S. 1"
S.S.' 19"
T.S. 4"
S.S. 9"
T.S. 3"
S.S. 15"
T.S. 1/2"
S.SJ 10"
T.S. 2"
S.S. :19"
T.S. 1"
S.S. 3"
T.S. 1"
S.S. 16"
T.S. 1/2"
Sanple No.
.1651
1652
1653
1654
1655
1656
1657
1 658
1659
1660
1661
1662
1663
1 664
1665
1666
1667
1668
1669
1670
1671
1672
.1673
1674
1675
1676
1677
1678
1679
1680
1681
1682
1683
1684
1685
1686
GEOCHEM SAMPLE INDEX
Township
Burrows
,
1
Grid
Bu #2 Gr. 1'
'
lf
,
i
'
,
i Co-ordinate
L4W 1+OOS
0+00
1+OON
2+OON j
Sample Type "
Soil i
'
1'
; i3+OON
4+OON
5+OON
i- 6+OON
LO 3+OONE
2+OONE
1+OONE
0+00
1+OOSk
2+OOSk
3+OOSk
4+OOSk
5+OOSh
6+OOS1*
1 i "
i .
, i. ' :. -
l
- ;
.
V
.i
.
,
i :
i3 n
1 .1
Horizon
S.S. 10"
T.S. 3"
S.S. . . 13"
T.S. .1"
S.S. 8"
T.S. 1"
S.S. 11"
T.S; l"
S.S. 9"
T.S. 1"
S.S. 36"
T.S. 10"
S.S. 3"
T.S. 1"
S.S. 17"
T.S, 1"
S.S. 16"
T.S. 5"
S.S.. 12"
T.S. 1"
S.S. 14"
T.S. 1"
S.S. 13"
T.S. rS.S. 12"
T, S. . 1"
S.S. 4"
T.S. 1/2"
S.S. 10"
T.S, 1/2"
S.S. 3"
T.S. 1/2"
S.S. 8"
T.S. 1"
S.S., 6"
T.S. 1/2"
Sample No.
1687
1688
1689 '
1690
1691
1692
1693
1694
1695
1696
1697
1698
1699
1700
1701
1702
1703
1704
1705
1706
1707
1708
1709
1710
1711
1712
1713
1714
1715,
1716
1717
1718
1719
1720
1721
1722
GEOCHEM SAMPLE INDEX
Township \ Grid ' Co-ordinate ; Sample Type |
Burrows \ Bu #2 Gp. 1 LO 6+OOS j Soil:1 - ! ' i :
! ; ' . -; i 5+oosi ' :
i 1 4+oos 1 i . '
i 1' ' .' 1 -\ 3+OOS j
; : i i . \ v i--i j ' 2+OOS P 1 ; 1 -
l . - ' 1 ' ' : ^ !- - :1 1 i+oos l \l ' ' l . ' - . ;^ 0+00* , H
- 1 " i ' . .:3 ' ' - '? ' i '. fJ
'S 1+OON 1
S ' ' . . 1 " ' ! 'f ' . 1 '
, i 2+OON j i
i '- ' i r' . 3+OON ] i
j ' ;
l . - 4+OON I
i ; j ' | ;1 1 5+OON j 1
J ' l 1 '\ \ 6+OON j ".j\ \ ' i :
; 1 ! j . . . .
) Bu #2 Gp. 2 )L12NW 6+OOSWJ\ l* l '
: l - 5+ooswf
l l :fl 4+OOSWJ
i | l j ;3+OOSVl'
. ' ' . ' "l ' \ l
\ 2+OOSW;( '-. ' ' : •} . i
. ^ ' i :
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
S.S
T.S
Horizon
7"
1"
12"
1"
5"
1"
11"
1"
5"
1"
8"
2"
8"
r9"
1/2"
6"
1/2'i4"
1/2"
14"
1"
9"
4"
9"
2"
12"
1"
9"
1"
9"
Sample No.
1723
1724
1725
1726
1727
1728
1729
1730
1731
1732
1733
1734
1735
1736
1737
1738,1739
1740
1741
1742
1743
1744
1745
1746
. 1747
1748
1749
1750
1751 '
1752
1753
1" | 1754i
3" f , 1755
. , 1/2"10"
1756-1757
' i1" | 1758
GEOCHEM SAMPLE INDEX
Township
Burrows
Grid
Bu #2 Gr. 2
Co-ordirmto
L12NW 1+OOSW
0+00
1+OONE
2+OONE
3+OONE
- 4+OONE
5+OONE
6+OONE
L4NW 6+OOSW
5+OOSW
4+OOSW
,. . .... . ... ...
Sample Typo
Soil i
i . '
- '
i! '
j
Horizon
S.S. 13"
T.S. 2"
S.S. TO"
T.S. 1/2"
S.S. 6"
T.S. 1/2"
S.S. 4"
T.S. 1/2"
S.S. 15"
T.S. 1/2"
S.S. 9"
T.S. 1"
S.S. 12"
T.S. 1"
S.S. 9"
T.S. 1"
S.S. 10"
T.S. 1"
S.S. 9"
T.S. T"
S.S. 13"
,. .'.'.,. ... '-. ' . ;
Sample No.
1759
1760
1761
1762
1763
1764
1765
1766
1767
1768
1769
1770
1771
1772
1773
1774
1775
1776
1777
1778
1779
f-
V
GEOCHEM SAMPLE INDEX
Township
Burrows
.
Grid
Bu #2 Gr. 2
j
.... -
Co-ordinate
L4NW 4+OOSW
3+OOSW
2+OOSW
/f 00 W
0+00
1+OONE
2+OONE
3+OONE
Sample Type
Soil
i'
i
' ; . *'
-
. Horizon
T.S. 1"
S.S. 7"
T.S. 1-1/2"
S.S. 15"
T.S. rS.S. 12"
T.S. 2"
. S.'S. 40"
T.S. . 30"
S.S. 40"
T.S. 8"
S.S. 11"
T.S. 2"
S.S. 9"
T.S. 2"
Sample No.
180.0
1801
1802
1803
1804
1805
1806
1807 :
1808 ,
1809
1810
1811
1812
1813
1814
*
GEOCHEM SAMPLE INDEXf
m iTownship |
Burrows
'
.
Fawcett
fGrid l Co-ordinate- 1
Bu #2 Gp. 2 L4NW 4+OONE j
L8NW 6+OONE. '
5+OONE j
4+OONE j, j
3+OONE i
"i i| 2+OONE j
; J 1+OONE
. 1 ' \
l O+OONE
il+OOSWi
1 1 2+OOSW"
. 3+OOSW
. ,
| 4+OOSW.
i | 5+OOSW
i ' '
l 6+OOSW
Gp. 1 |L8W 6+OOSi!
! 5+OOS
jtt
^ \ 4+OOS
j
3+OOSr \
lii
'
Sample 1 Type j
Soil
j
. '
i
.
r
i ii . ;1 '- .
jf . :1 ;
i| '" :
! ' i ' ,l s' - ' ' - : . i
. l - -' . " '
i
1 ; j -
,Horizon
S.S. 1
T.S.
S.S.
T.S.
S.S..
T.S.
S.S.
T.S.
S.S.
T.S.
S.S.
T.S,
S.S.
T.S.
S.S.
T.S.,.
S.S.
T, S.
S.S.
T.S.
S.S.
T.S.
's.s.5IT.S/i S.S.iIT.S.:S.S.iT.S.
Is.s.. T.S.
! S.S.! T.S.
S.S.
T.S.
S.S.
T.S.
13"
1"
9"
1"
11"
1"
10"
2"
10"
1"
10"
1"
22"
1"
4"
1"
17"
2"
14"
•3"
32"
6"
4"
2"
10"
1/2"
8".
1"
10" .8"
17"
4"
40"
2"
8"
1"
Sanole No.
, 1815
1816
1817
1818
1819
1820
1821
1822
1823
1824
1825
1826
1827
1828
1829
1830
1831
1832
1833
1834.
1835
.1836
1837
1838
1839
1840-
1841
1842
1843
' 1844
1845
1846
1847
1848
1849
j 1850
1 ' '
GEOCHEM SAMPLE INDEX
- 9Township
Fawcett
.
1
Grid
Gp. 1
i
i
l i:i
i
li
i !
\
i
'
.p
\Co-ordinate j
L8W 2+OOS
i
1+OOS•1
]
0+00
1+OON;i
2+OON
i
j
3+OONi|
4+OON"1
5+OON
6+OON
L4W 6+OON
5+OON
! 4+OON'
1'
3+OONi
1 2+OON'
1+OONit
0+00
\1+OOS
s|i 2+OOS
|\
Sample Type l
Soil'
1
.
, • '
-
1
.
j
*
l
i*ijj
1:'
(
fl
i ,*
j' -
Horizon
S.S.
ir. s.s.s.T.S.
S.S.
T.S.
S.S.
T.S.
S.S.
T.S.
S.S.
T.S.
S.S.
T.S.
S.S.
T.S.
S.S.
T.S.
S.S.
T.S.
S.S.
T.S.
S.S.
T.S.
S.S.,
T.S.
c c o . o .
T.S.
S.S.
T.S.
S.S.
T.S.
O .b .
T.S.
S.S.
T.S.
6"
2"
14"
•2"
10"
1"
13"
4"
7"
1"
18"
2"
10"
2"
12"
1"
17"
4"
10"
1"
9"
1"
10"
1"
10"
1"
13"
1"'36"
12"
36"*
14"
12"
3"
8"
1"
'
Sample No.
1851
1852
1853
1854
1855
1856
1857
1858
1859
1860
1861
1862
1863
1864
1865
1866
1867
1868
•' 1869
1870
1871
1872
1873
1874
1875
1876
1877.
1878
1879
- 1880
1881
1882
1883
1884
1885
1886
; ,
GEOCHEM SAMPLE INDEX
r 1 1 Township f Grid jj Co-ordinate j
Fawcett j Gp. 1 j L4W 3+OOS |
-
'
is S
4+OOS 1i
i ' 15+OOS
:j
6+OOS j
|LO 6+OOS ]
1
j 5+OOS |
\ 'l 4+OOS .1
| 3+OOS
1| 2+OOS
jj 1+OOSl
. ii 31 o+ool
j i
\ 1 +OONt i1 i1 . js I]: 3 2+OON 1 1r !: 3+OONf 1? f
' 1 i' j -- 4+OON\ \
\
[ l 5+OON
i 1' 5 r
j . 6+OON
•' t, 1 ? L4E 8+OONi i
Sample Type | Horizon
Soil
'
t
1
ii| .
|
j
" '
:
i ' ji5t. \i
H
,
j
i
i
ii
1
l
l I '
j
f
S.S. 6"
T.S. 1"
S.S. 16"
T.S. 1"
S.S. 11"
T.S. 1"
S.S. 7"
T.S. 1"
S.S. 7"
T.S. 2"
S.S. 10"
T.S. 1"
S.S. 12"
T.S. 1"
S.S. 11"
T.S, 2"
S.S. 9"
T.S. 2"
S.S. - 28"
T.S/ 16"
S.S. 36"
T.S. 2"
S.S. 12"
T.S. .1"
S.S. 5"
T.S. 1"
S.S. 8"
Sample No.
1887
1888
1889
1890
1891
1892
1893
1894
1895
1896
1897
1898
1899
1900
1 901
1902
1903
1904
1905
1 1906
1907
1 908
1909
19101
1911
1912
1913
T.S. 1" j 1914
S.S. 32" 1915
T.S. 4" i 1916! \i ^
S.S. 9" j . 1917
T.S. 2" 1918j
S.S. 8" j 1919
T.S. 1" ! 1920
S.S.' 12" 1921ii
T.S. 1" I 1922\
* s
GEOCKEM SAMPLE INDEX
Township J Grid | Co-ordinate j Sample Type
Fawcett Gp. 1
-
j' j
1
i
*
j
|
fj ; -.i
' r i
i
L4E 7+OON
6+OON
Soil
5+OON i1 ; - -4+OON 1
3+OON
2+OON
i -
'
1+OON j
i0+00 f
J)11
,
1+OOS i
l 2+OOS
3+OOSl
4+OOS j
j :5+OOS j
!L8E 6+OOS
5 " . .5+OOS
4+OOS
i
iv
3+OOS j
l2+OOS J
j
- j .
1 . 1
Horizon
S.S. 9"
T.S. 2"
S.S. 27"
T.S. 2"
S.S. 9"
T.S. 1"
S.S. 14"
T.S. 2"
S.S. 9"
T.S. 2"
S.S. 22"
T.S. 2"
S.S. 8"
T.S. 2"
S.S. 9"
T.S. 1"
S.S. 12"
T.S. 3"
S.S. 10"
T.S. 2"
S.S. 12"
T.S. 1"
S.S. 10"
T.S. 1"
S.S. 8"
T.S. 1"
S.S. 11"
Sample No.
1 923
1924
1925
1926
1927 '
1928
1929
1 930
1931
1932
1933
1934
1935
1936
1937
1938
' 1939
1940
1941
1942
1943
1944
1945
1946
1947
1948
1949
T.S. 2" i 1950i
S.S. 18" l 1 951.!
T.S. 2" 1952
S.S. 11" 1953
T.S. 1" j 1954
S.S. 9" j . 1955
T.S. 1" | 1956
S.S. 8" 1957
T.S. 1" j 1958
t'
GEOCHEM SAMPLE INDEX
t!
Township
Fawcett
'
-
i
Grid
Gp. 1
''
'
Co-ordinate jj
L8E 1+OOS j
0+00
. j
l+OON
2+OON
3+OON
4+OON
5+OON
6+OON
7+OON
L12E 7+OON
6+OON
5+OON
4+OON
3+OON'-
2+OON1
l+OON
0+00
j 1+OOS!H
!1
\ Sample Type
Soil
.
-
' -
i
! .
:
1 v
l ' i*
l
jli ,i 5i : -
Horizon
S.S. 13"
T.S. 1"
S.S. 3"
T.S. 1"
S.S. 8"
T.S. 1"
S.S. 10"
T.S. 2"
S.S. 8"
T.S. 2"
S.S. 6"
T.S. 1"
S.S. 4"
T.S. 1"
S.S. 18"
T.S. .1"
S.S. 7"
T.S. 1"
S.S. 11"
T.S. 2"
S.S. 9"
T.S. 2"
S.S. 15"
T.S. ' 1"
S.S. - 14"
T.S. 1"
S.S. 12"
T.S. 1"
S.S. 8"
T.S. 1"
S.S. 8"
T.S. 1"
S.S. 10"
T.S. 1"
S.S. 8",
T.S. 1"
Sample No.
1959
1960
1961
1962
1963
1964
1965
1 966
1967
. 1 968
1969
1970
1971 '
1972
1973 '.
1974
1975
1976
1977
1978
1,979
1980
1981
1982
1983
' . 1 984
1985
1986
1987
1988
1989
1990
1991
1992
1993
1994 '
'
GEOCHEM SAMPLE INDEX
Township
Fawcett
1 I Grid | Co-ordinate \ Sample Type
Gp, 1
' -l ' - '
j
L12E 2+OOS
3+OOS
Soil
-
4+OOS 1!
5+OOS
Horizon
S.S. 7"
T.S. 1"
S.S. 17"
T.S. 2"
S.S. 16"
T.S. 1"
S.S. 8"
T.S. 1"
Sample No.
1 995
1996
1997
1998
1999
2000
2001 '
2002
FIGURE 2 2. ANALYTICAL RESULTS . SHINING TREE AREA.
Halliday | 805
(Grid fi) K 806
1 8071? 808l!l 809i 1 810
s! 811rb
: | 812: l
f 81 3! 1•i 8 14
s i 1 ' 815i ' *
j 1 816' ' vi r 8i7 -
[ 818fi
li 819^
l f
16
12
NO
16
8
16
8
16
12
12
.12
24
j 20
i 40i
i 8j
16
14
AMPLE
16
18
12
. 18
. 16
20
8
24
12
16
28
16
.5
.5
.5
.5
.5
.5
.5
,5
.5
.5
.5
.5
.5
.5
100
104
58
42
152
28
136
48
132
28
152
152
410
1- wbo
1
8
20
28
12
68
8
60
20
30
8
82
12
i . 138^
lJ 16i
i "
- 1 1
,
ki'iCifi - .j/'
Siu
w
TOWNSHIP
1
i
, SAMPLE NO. |t;
Halliday
(Grid #1)
: 820
821- L' -
.822
. j. 823. - . 'i'j ' 824 -
825.
J ' 826- ' P. . i . 827
| 828
829 '
830
831
832
833
834
1 835, . - - i* . -
836P ' '
: .- j ' ' 837 " :-
,. '
'
i
ANALYTICAL RESULTS IN P. P. M.
(Hot
Cu
28
4
12
120'44
12
20
NO S
204 -
28
4 .
28
8
12
8
24.
8
j 838 . 24i -' ' - ' \ 839;
- - 840 --v. M
{ 841i* * '
' | 842
[j 843 'l
: ' 1 844
- ' | -845..
| 846
f 847 '. \
1 848 -j .
849' Pf 850
1 851f '1 852
ij 853i
| ' 854
; 855l
1 856
i 4
34
6
16
4
16
4
28
4
4
6"24
-N0i -
36
NO
52' 8
,
8' " ' 1t i
;,) H C'
Ni
. 24
4
8
24
14
12
20
AMPLE
20
16
28
16
20
20
8
12
20
14
24
8
24
20
12
16
16
16
28
12
8
. 20
20
5 AMP LE
24
5 AMP LE
.44
16
12
0^-i!\C
Ag
.5
.5
- .5
,5
-' .5
.5
.5
.5
.5
,5
.5
.5
,5
5
.5
.5
.5
,5
,5
,5
, .5
5
.5
. -5
.5
.5
,5
.5
.5
..5
3
Zn
384
20
. 116
76
64
40
140
88
24
62
24
72
32
60
32
.144
36
140
16
134
24
84
24
120
26
178
28
44
36
176
.5 118
.5
.5
430
60
ij
Pb |̂120f
Cu
' '8|
44
': 1 2;. - f
22
12
56
72
. 8
60
10
62
-'.12-
38
8
80
10
80
':
. '
j ' ; - . j ' .' ' '
'i12 l .84
12
48
10 !:
60 j
. 10
76
10
. -
. 24
12i ' !
52 \ - .
' 64 j - ,-
106
12 :j'
,5 52 1 20 1
i i l
Ni
'Mti . .......
Ag
'. -
Zn ..
Pb
!
\.
.
^
'l
i
.4
TOWNSHIP W
Halliday
(Grid 11)
.
1
SAMPLE NO.
857
858
859
860
860B
861
862
863
864
865
866
867
868 .
869
870
.871
872
873
874
875
876
877
878
879
880 881 882
883
884
885
886
887
888
889
890
891
892
893
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03 f ( Edta)
Cu
4
24
6
12
18
6
16
4
16
8
8
..54
6
. 12
8
24
4
52
4
8
.20
6
44
40
8
28
28
60
8
4
24
4
8
32
N1
20
20
20
12
20
16
16
16
16
28
12
46
14
16
20
.20
24
56
24
24
20
16
52
44
20
32
16
30
8
20
24
16
22
32
Ag.5
.5
.5
.5
.5
.5
.5
.5
..5
.5
.5
.5.
.5
.5
.5
.5
. .5
• 5
.5
.5
.5
• 5
•5
.5
• 5
,5
.5
• 5
.5
•5
.5
.5
.5
.5
Zn
36
192
56
36
188
28
104
20
68
24
20
58
24
68
28
104
36
180
32
60
96
28
430
224
44
284
100
32
52
48
304
46
44
630
Pb
8
60
16
36
50
10
56
10
50
8
12
16
14
38
12
.56
,12
96
12
12
508 '
82
116
16
74
28 .
16
16
10
80
14
12
108
Cu
. .. .. .....^..-..-.
. ... . . ..
i
-
Ni
t
-
Ag
t.
Zn .
,
Pb
p- J
TOWNSHIP W j SAMPLE NO.
.......^ t 894fi
(Grid #1) 895
j 896i
. . | 897f l 898 .i
i 8991 -
1 . 900i
. 901
' | 902
903
.i 904
ANALYTICAL RESULTS IN P.P. M. .
(Hot) HC104 -HN03 i ' ( Edta )
Cu28
Ni Aq Zni?
Pb \ C u .k \ "i28
6; 20
8
6
8
4
4
4
32
8
20
j 905 8' 'i; 906 20i
907 8
908 6
909.
910i!
•j 911
i 912i 9 13t'.
\ 9 14ij
1 9 16|1 917f
918Vf 1
I 9195'
[ 920•'1 9 21
S .922;
j 923
l 924. Jir 1
l 925ai 926
j 927
i; 928
' 929!
l 930f
. g
24
4
12
8
8
8
16
34
4
,n 20|
1 . 4l
30i
4
20
26
60
i 4
32
4
20ii 24| 28
i
12
20
20
12
6
18
28
20
24
20
16
24
8
20
8
16
20
24
12
30
42
8
16
16
20
12
. 16
. 34
44
16
30
12
24
34
24
.5: 540 |- 100 jj .
.5
.5
.5
.5
.5
.5
.5
• 5
.5
.5
. .5
• 5
.5
.5
• 5
.5
.5
•5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
;5
.5
.5
.5
. .5
.5
26
108
26
72
20
54
24
180
30
148
22
88
18
16
40
16
50
22
28
24
30
148
20
140
28
380
46
302
236
308
30
440
34
242i
12 j. ; .
- ' 28 jK
12 ,
40 l8
.10'
24
12
116
16
62
10
60
14
12
36
- 6:
30
6
4' :'
16
16
10
72
. .
:
-
.
;
;j
8
48 j ''
8 1
68 j
12
70
8
12 ;t
82
10
44 ' \ \ ;
\ ''i
.5 112 \ 1 6 i:i -e - ;
.5 - 148 j 60 :;
} .
Ni"
Ag l Zn .t
' ' r1|
i1
. ls
;
Pb
t
ii
l . .
5
|
4
1* 'i
l l '
ANALYTICAL RESULTS IN P.P.M.•:
• iTOWNSHIP i SAMPLE NO.
(Hot) HC104-HN03 . | . . ( Edta)
CuF . . j
Halliday | 931
(Anomaly #1)1 932 .
' ' i 933 -: .. . ] ' ' 934 . .^,
p
. - j 935' ' l
936' F
| 937 "
i '938• i
939i
1 940
. .. .....-.-•... .--'i 941 "-
942
j 943
944
945
i 946
J 947i
fi " - '
' i 948jj . 949 .iii 950
j. 951 'K
l 952R
P '953
j! 954V-'i 9 55;
956i 957
1 958^1 959
| 960; j
| 961lly'
l 9 62
.j 963i -l 964
l 9 65f: 966
j 967j 1.ti 968i
l -
4
20
4,
. 24
4
40
4
12
8
28
4.'44
8
12
16
16
14
16
20
14
18
16
16
12
6024
4
32
8
i 16
40
24
32
16
10
12
: 2 4i
1 8
.
•Ni
8
16.
20
20
24
40 .
24
12
28
28
20
40
24
12
8
16
8
12
4
4
8
8
8
4
80.2012
28
12
.12
.32
16
12
- 12
8
12
12
12
Ag.5
.5.
. ..5
.5
.5
.5
,5
.5
.5
.5
.5
.5
•5
.5
.5
.5
'--..5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
•5
.5
.5
.5
Zn22
146
32
208
34
86
26
38
20
70
28
138
20
46
50
48
44
100
26
28
28
36
40
52
749038
212
22
66
56
44
60
40
, .5
.5
.5
.5
30
34
42
40
1 Pb 1. Cu
lil
•14 1
.48. l . .
16 '
48 ji
•'12 | -
82
12
36
12
72
14
90
10
38
10
; 1210
50
6
10
12
14
6
12
124610
72
. -
•i
!'i
8
32
12
168'- \
. ;! '6 ij
814'
. 8
20 6i
Ni1
Ag 1 Zn .?
|
'^i
•'
Pb
-
.
it i l
j
. jt 1
i
ANALYTICAL RESULTS IN P.P.M.
(Hot) HC104-HN03 (Edta)m
TOWNSHIP^ 1 SAMPLE NO.
Halliday 9691 1
(Anomaly #1} j 970
l 971
1 972r! 973i
974 .il 975
j 976
i 977S1 9 78
i 979n
980
981
982
983
984
985
j 986
l 987P '1 988Rj 989l'i 990
i 991' .
i 992i\ 993i'I 994t.l 9 95jji 996il 997j]f 998
l 999t't1000
f!'] 1 001
f\ 1 002
l 1 003i :r 1004
11
Cu1 Q
1 O
12
8
8
20
16
12
12
10
22
14
16
4
16
4
20
4
24
4
2411 4
j 22
! 8
18j1 *ii 1 4i 41j 36
1 4
36
4i
24ij 4
12
4
i 1 6j
t
Ni12
12
6
8
12
12
20
16
24
20
28
24
24
16
16
24
20
28
24
24
16
24
24
16
16
16
20
36
12
28
14
28
16
8
18
20
Aq :
' 5 i
.5
.5
. .5
.5
.5
.5
.5
.5
,5
.5
.5
.5
. .5
.5
.5
.5
...5J
.5
.5
.5
•5
•5
.5
.5.
•5
.5
.5
.5
.5
.5
.5
..5
.5
.5
s
jZn
40
54
40
44
24
26
34
36
32
64
30
30.
24
72
22
64
26
136
46
182
36
216
60
134
40
140
48
160
36
180
28
122.
32
52
42
86
pb S8 j
30 i
•' 12 j
24 i
8^- 8!
' .10'- 8!
12
10
46
O
8
6
46
14
64
• : 10
80
10.72
8
64
6
68
12
44
12
82
8
70
12
76
14
24
32
l 5 61
j
Cu .
.
:'
'
'
1ji
i
|
i.
i'if ' -
[tj;'j 1,
Jji-
1
lii•i i)
;jj!
j'iiii.;ri'
: .
rlP 'fiY.
' t
ij;f:
'l
1f
(j in
\\i;
i . .
E - '
Ni Ag \-
\
.
\
Zn .
l!
Pb
t
\*i
i\\ii
1i\itt
.'
TOWNSHIP
Halliday
(Anomaly #1)
-
'
! SAMPLE NO.
! 1005
1006
! .10071
1008
| 1009
1010
ion1012
1013
1014
1015
1016
- 1017
1018 ;
. 1019
1020:
.1 1021J ! .
. ' l ' 1022 '
f 1023*I , 1024.
| 1025
| 1 026
- , . l - . 1027 "
1 1028
1029- i -
1, 1 030
j 1031
"- - . ; | 1032
. 1 1 033
1 1034 (
J 1035 i ! 1036
1037 .
1038
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03
Cu
4
8
4
4
6
12
14
12
24
32
4
.12
4
24
60
160
26
20
34
32
36
32
12
12
12
16
NO
18
4
14
i 1 4
12l1 1 039 32f f 1040 26f ' Fi'!
!i '.;;
Ni12
8
6
4
6
10
12.
8
20
24
12
10
20
28
28
28
24
24
20
32
32
24
32
10
20
16
SAMPLE
8
10
16
24
20
36
24
A9.5
,5
.5' .5
'••5,
.5
,5
. .5
.5
' -5
: .-5
.5
.5
.5
•....5
.5
.5'
.5
.5
.5
.5
.5
.5
,5
.5
,5
.5
.5
.5
.5
.5
1.0
.5
Zn26
40
12
20
28
48
20
24
80
108
28
64
34
268
60
104
84
246
48
, 44
128
88
44
76
24
40
96
20
72
40
96
110
92
Pb \
(Edta)
Cu l Ni' ' - I2 i" -18J
::
.8 !1-2
•12
20
8
16
52
80
10
48
12
80-14
.52
14
52
40
; 24; 14
18
20
48
i . ' - f . .i
5 - .
ii; .
j ••••-i!,'. . .|-.". . "
'.
14
32
, 40
12
52
16,
; 4428
52
•' . i'
Aq
'
i
Zn . Pb
-
-
ti '
-
\ 'it Q
i
ANALYTICAL RESULTS IN P.P.M.
. ' i• i S SAMPLE NO.
. - 5Halliday
(Anomaly #1)
i 1041
1042
| 1043 .
f 1044
'
t"
-
.
'
1 045
1046
1047:1 1 048
1049.
! 10501 1051 .
1052
1053
1054
1055
1 056
f
'
1057
1 1058It\ 1 059l!
1 1060
i]p
. i. 106211
, ,. | 1063' . . i
^ -s1 1064
1 1065' . ^
' | . ' * 1066F
. 'j 1067B '.J!
1 1068| 'j . 1069
j 1 070
1 1071
! 1072i| '
1073BS 1074|3 1075Sf 1076
i 1 077ijt 1078- s1'
(Hot) HC104-HN03 j ( Edta)
Cu
10
12
4
36
10
10
84
80
4
206
24
4
10
4
18
4
14
4
. 4
12
28
6
36
76
24
16
28
4
20
4
24
4
.24
8
38! ' ' 4
40
Ni
20
12
24
28
. 12
16
34
40
18
142420
24
8
14
16
12
12
20
16
8
28
12
28
24
16
12
28.
20
20
20
28
22
28
28
36
22
34
Ag
.5
.5
.5
.5
;5.5
,5
.5
..5
.5' .5
.5
.5
.5
.5
,5
•5
.5
.-••5
•5.
.5
.5
.5
.5
.5
:' .51 -'
•: .5
•5
•5
,5
.5
.5
.5
.5
.5
.5
.5
•.5
Zn l Pb' l Cui50
40
40
150
76
40
128
116
24
15832
294
- 32
60
28
124
30
66
40
40
78
152*
20:70
84
34
56
68
28
68
32
96
36
98
54
128
44
266
1 '16
20 j
i2j140 jj . ,
40
10
28
36
10
801480
10
64
: 1472
12
40
14
12
40
. 88
16
60
34
16
20
! 42'12
52
16
70
12
56
14
.
; ' ' '
i ' ' ' ' - '
i ' 'i -j;
-
i ' ' : .s
1
ii ' '
r :-
i. '- -. ;: 68 r '
12 j
84lI i
Ni Ag i Zn .\l
. l'
-
\
Pb
ii
!j
" - | ' ,i
j
- iTOWNSHIP f" SAMPLE NO.
Halliday j 1079
(Anomaly #l)f 1080
-
1081
1082
1083
1084
1085
1086
1087
1088
1089
1090
1091
1092
1093
1094
1095
| 1096
| 1097
J 1098 .
1 1099;
.
i 1100
j 1101
11021. I 1103
' l 1104'
j 1105
1106
f 1107B
1108
1109 .
momi1112
1113
1 1114l
. l 1 115.
i '
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03 j ( Edta)
Cu
4
16
NO :16
, 4
16
6
22
6
12
4
8
4
24
4
14
12
Ni
6
12
AMPLE
12
8
12.
14
20
20
12
24
12
20
20
20
16724
323 26
.4
24
8
24
4
32
4
10
14
88
44
6
40
8
36
6.
40
4
16
20
16
16
16
28
20
8
28
4
16
32
20
40
24
40
20
44
. 16
Aq
,5
.5
.5
.5-
.5
,5
.5
,5
.5
.5
.5
.5
.5
. .5
.5
,5
.5
-5
.5
.5
.5
.5
.5
. .5
.5
.5
.-5
.5
t u
ct *J
.5
.5
.5
.5
. -5
Zn26
120
66
20
84
20
52
26
44
32
88
' 56
510
48
160
32
188
22
120
38
120
36
220
24
24
30
30
32
164
40
224
32
, 264
24
130
20
Pb I Cu '
8
40
42'lo
52
10
70
12
34
10
38
14
92
16
42
18
92
12
88
14
44
16
112
12
20
1
1
j ;
.
j
1 -
f
l
j. yp
i!
'
.
i '
12
24
10 l
76
12
106
14
.100
16
96
j 1.2
j
; .
|r \ .
1- '.'-'
l
Ni Ag f Zn .
! .t
H
i
r
Pb
i
!ti -
TOWNSHIP 1 SAMPLE NO.
Halliday j 1116lil
(Anomaly #l)j 1117
i me .j . 1119
1120
1121-
i 1122i
1123
1 1 124jif 1125
1126
1127
1128j1
1129
i 1130- ii ii3i' i!| H 32
f 113311 1134
| 1135R
j] 1 136
! 1137
j 1138
1139r!
| 1140
i 1 141" ! l 142
11143
r
| 1144
ANALYTICAL RESULTS IN P. P. M:
(Hot) HC104-HN03 f ( Edta)
Cu
24
NO
24
8
32
8
36
4
24
12
32
20
24
8
28
4
20
4
40
36
24
.NO
16
8
12
1 41j 20jJ. 8!
l 1 01 p| 1145S! 1146P,j ' 1147fl
| 1148 '
f 1149
! 1150
Ni
24
SAMPLE
28
20
32
24
44
14
24
20
36
32
20
16
16
4
16
20
36
40
20
SAMPLE
20
32
14
12
20
28
16
Ag 1 'Zn
.5
.5
.5
.5
.5
.5
.5'•5
.5
.5
.5
.5
. .5
.5
.5
.5
.5
.5
.5
.5
. .5
.5
.5
.5
.5
.5
,5
64
160
40
88
36
252
24
72
34
272
32
92
20
236
16
76
24
244
144
100
72
24'64
20
180
iPb I Cu
: 52 |'
; l; n \ ..14 1
108 1
,14|V
86
14
44
12
100
14
84
6
68
10
80
12
.
''
, . " '.
h132 1-
22
36
28
1 '"
l - .y
ll
: 10 |fi
.36
10
54
28
56i
12
i
i.1 - '6
; 28 jb
i NO SAMPLE .:: . . , ;" [;.i
72
4
20
6
38: 1 ' ,
\ 1 151 NOr H
' ii
4 ' tt
.
38
24
•5
.5ti24]' ,5
20
36
SAMPLE
.5
.5t .
276
24
96
; 40,
188
|i 94 [ .
141 60
12
.76
1 r.!
l ' ''
j.
: ' - ' -\ s* .
; !
j ' ,;
j
Ni Ag 1 Zn .
' j
. 1t
'
Pb
'
ji
l - -
i
' . 1
,'
.TOWNSHIP
- Halliday
(Anomaly #1
j
i
SAMPLE NO.
| 1-152
) 1153
1154
1155 -
1156
1157
1158
1159
1160
1161
1162
1163 .
1164
1165
1166
1167.
1168
1169
1170
' 1171
1172 '
1173
1174
.1175
1176
1177
11781
1179t*1180
-
~
-
j 1181,ij 1182:
J 1183 i1 1 184 -
1185i
| 1186rj
l 1 187
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104 -HN03 j ( Edta)
Cu
38
4
38
6
30
4-36
8
20
6
28
10
12
4
32
4
32
4
28
6
32
16
32
36
34
12
40
44
44
NO
32
4
12
8
22
10
Ni
32
24
36
16
32
16
34
16
20
12
32
24
16
16
36
16
28
12
32
12
36
44
28
32
36
32
36
32
. 24
SAMPLI
24
24
. 20
20
28
18
A9.5
.5
.5' ,5
•5
.5
.5'-.'.5
.5
.5
.5
.5
.5
.5
.5
, -5
.5
.5
.5
.5
.5
• 5
,5
.5
.5
.5
.5
.5
.5
t
.5
.5
.5
.5
.5
• 5
Zn176
64
220
36
260
40
244
52
126
52
200
48
88
40
164
30
336
24
56
20
100
48
244
92
98
62
72
72
08
116
24
92
36
184
52
Pb78
14
114
12
; 98
10
1 00
12
. 44
14
78
12
34'.10
70
10
94
8
] 68
10
68
12
. 96
20
42
12
60'58
56
80
Cu
i
is tijj
i
t '
i
j
l
\1
\f!
i!
1
12 l -' .48 |
i12
90
. 16
.j
i
\ T ;
i- l
Ni Aq Zn . Pb
i
t
j
j
TOWNSHIP
\
SAMPLE NO.
Halliday j 1188i
, -(Anomaly Jl )g ., 1189
^ ~ - - l '1190 .
- | 1191- .
'
.
1192
1193
1-194,
1195
1196
.1197 .
1198
1199
1200
1201
1202
1203
1204
1205
1206
| 1207
| 1 208liB 1209jf 1210P li)| 1211li
1212
| 1213i!i
i 1 2141I 1215'
12168 .
ANALYTICAL 'RESULTS IN P. P. M.
(Hot) HC104-HN0 3 | ( Edta)
Cu
20
NO
34
10
28
4
28
8.
40
4
20
4
40
4
18
8
18
: 430
816
i4
32
8i
40
8jt
44
10
j 24
. | 1217 I 8
1 1 218tj 121931 1220f| 1221
t
16
i 1 0
j 24
162 ' l l 1 222 | 121 1 1 223 12
i l
Ni
28
SAMPL
32
22
30
10
26
18
34
16
26
12
32
12
20
24
18
16
26
18
16
14
32
26
36
13
32
20
28
19
16
28
26
28
16
27
Ag
.5
. t '
.5
.5
.5
.5
,5
.5
.5
,5
.5
.5
1.5
'-r.. 5
.5
•5
.5
.5
. .5
.5
•5
.5
.5
.5
.5
.5
' .5
.5
.5
.5
.5
.5
.5
,5
.5
.5ij
Zn
410
450
54
100
30
254
44
272
36
7436'
168
. 52
84
68
204
78
212
50
92
52
180
64
700
72
220
56
348
24
56
24
112
20
Pb fi Cu1
72
148
18
'
j . -: ;,68 j
12
84
14
108
12
60
10
72
12
48- ' '
14
50
j. ;. ' -' -it . . -
i'
10 i78
12
j-;- :,
42 ;i
12
84
16
86
. 14
88
12
80
12' t'44 | .
•i12 !i!
H80
14
52 36| :
20 ; 14
ij . .
,
l
tt
i
u
Ni Aq l Z n .
r '
;
'
Pb
i
1
li'
. fi
ji\'f
il -1
' ' . ji
i
f
j
r '
TOWNSHIP
Halliday
(Anomaly #1
.
SAMPLE NO.
1224
1225
1226
1227
1228
1229
1230
1231
1232
1233
1234
1235
1236
1237
1238
ANALYTICAL RESULTS IN P.P. M:
(Hot) HC104-HN03 l
Cu
16
8
12
NO S
26
10
22
NO S
50
12
40
16
36
12
20. ;
Ni
16
14
12
AMPLE
20
15
16
AMPLE
20
9
36
20
28
18
12
Ag
.5
.5
.5
.5
.5
.5
. .5
.5
.5
.5
.5
.5
.5
'Zn
38
16
. 52
36
20
44
40
28
84
. 24' 76
26
52
(Edta)
Pb 1 Cu1
36
10
24'
44
10
44
76
20
112
14
80
12
22
i
i i' . J,.
Ni Ag Zn . Pb
'
*
V
^
tTOWNSHIP
Knight
: SAMPLE NO.
1289i1 i
(Anomaly #li ) 1290
1291
| 1292
1293
1294
1295
1296
1297
1298i, 1299
1300H
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03 j ( Edta)
Cu
8
16
4
44
NO
46
NO
60
8
16
6
16
1 301 4
1302
1303
1304
18
6
12
f 1305 6a
l 1 306
'.
.
l 1307
18
6.b '
1 308
i 1309i! 1310
.1311i•' | 1 312
: 1 -' 1313.' "-.' l ' '
| 1314
- 1315t
1316
1 1317
1. . 1318
: f 1319
| 1320*i i 1321B
1322
- j :1323
J. | 1324
:' . -- r '
30
4
16
6
32
4
20
j 1 2,
36
6
20
6
36
6
24
8
j 24
-- - J' ' ' ; J. -
Ni
80
56
48
172
SAMPLE
58
SAMPLE
44
68
44
42
36
16
28
24
12
24
18
20
32
16
20
00
36•20
20
24
40
16
20
2 4
40
20
20
12
28
Ag
.5
•5
.5
•5
.5
.5
.5
.5
.5
.5
.5
.5
.5
,5
.5
. .5
.5
.5
.5
.5
.5
.5
, .5
, .5
•5
•' .5
,5
.5
.5
.5
.5
. .5
.5
.5
Zn
64
80
36
132
224
148
28
40
22
-100
20
60
20
52
28
112
26
124
32
: 80'
26
400
48
212
42
340
24
68
24
172
40
120
36
94
'.Pb 1 Cui
16
36
8
92
136
68
8
14
8
48
8
52
;12
28 ;12
44
12
76 .
10
40
12
80
8
48
16
82
10.
40
12
100
12
72
'-. 8
60
.
i
; i .
i
i
tjif.
\1
.
V - - -
(l
S,
- . , .
.'
:
y ' - - '
i ' ' '
i ' ''
; ' '. " .
j
•j.'
'! : 'i i
NiI
Ag \ Zn ,
ii
. | ' '
•' j
*
Pb
l
k
TOWNSHIP SAMPLE NO.S
ANALYTICAL RESULTS IN P
(Hot) HC1Q4-HN03 f
Cu Ni Ag Zni
i
Pb i Cui ' a -. .
.P.M.
(Edta)
Ni Ag l Zn .,' Pb
Knight ji;
(Anomaly #J8)
f1287 . 4"
1288 | 12; ii
j
24
20
.5
.5
24
80'
t- ' '8 1; [i
32i , - -
1!•'i ?
i - i
- ;
i
r:
i,
TOWNSHIP
Knight
(Anomaly #18
.
SAMPLE NO.
1325
l) 1326
1327 '
1328
1329
1 330
1 331
1332
1333
1334
1335
1336
1337
1338
1339
1340
1341
1 342
1343
1344
1345-
1346
1347
i 1348i - !1349
1350
1351
1352
f 1353
l 1 3541 f 1355
1 1356i
1357
1358*
j 1359t| 1360•'i
i
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03 j
Cu
6
36
10
24
8
40
16
36
4
40
12
42
NO S
18
NO S
32
14
20
6
24
4
26
8
34
8
20
70
130
8
26
12
28
8
20
78
| 80
Ni16
44
28
32
20
48
28
36
20
40
36
36
AMPLE
16
AMPLE
60
124
64
36
70
50
48
22
44
20
16
. 104
148
. 30
28
24
26
20
16
72
114
Afl.5
.5
,5
.5
.5
.5
.5
. .5
.5
.5
.5
.5
* *.J
.5
.5
.5
.5
.5
.5
.5
•5
.5
.5
.5
• 5
\5
.5
.5
.5
,5
• 5
.5
.5
,5
,5
Zn28
240
24
196
40
430
24
84
24
160
24
64
32
60
32
78
28
132
24
. 76
22
72
12
26
20
24
20.
192
20
192
20
; 56
112
272.
(Edta)
Pb i Cui
12
112
12
76
14
156
12
116
16
128
20
96
•28
58.
14
40
8
58
12
76
12
78
12
44
16
28
12 .
88
16
92
12
,44
. 16
28
'
,
. .
1 '
i ii i
j ' :1
it
j•1
i i ,
iirj
Ni ' Aq 1 Zn i
'
Pb
t,
4
TOWNSHIP
Knight
(Anomaly #18)-
.
'
i
' SAMPLE NO,
j 1361
i 1362
! 1363
1364i
1365
1 366
1367
1368
1369
1370
1371
1372
1373
1374
1375
1376
1377
1378i 1
| 1379'
' ANALYTICAL RESULTS IN P. P. M.
. (Hot) HC104-HN03 f ( Edta)
Cu
8
24
8
20
16
38
10
28
4
36
4
30
NO S
40
36
26
4
34
8
. 1380 .141
! 1381 4l -.., l" .j- . - 1382
: 1 1 1383
. ' 1384
' : J "1385. . '. '
J 1386V -li
1387
. ; . 1 1388
l 1389
'.' ' . . 1390
1391
1392
1393 ;-1394 .
| 1395
\ 1 396
l 1 397 ;
. 1' ;
20
4
32
4
24
6
16
6
32
12
6
8
20 .
: 12
12
6
Ni
24
. 24
20
20
32
32
18
24
20
52
20
24
AMPLE
104
440
120
80
268
72
32
28
24
36
38.
24
28
22
. 16 .
16
20
26
8
22
.16
14
12
24
Ag
.5
.'5
.5- . 5
.5
-.5
.5
,5
.5
.5
.5
,5
.5
.5
.5
.5
.5
.5
. .5
•5
v' .5
•. .5
.5
' -5
.. .5
.5
; .5
.5
•5
.5
.5
.5
.5
.5
.5
.5
Zn
36
144
20
72
24
192
38
112
- 44
960
76
470
144
38
40
28
12832'
52
20
100
32
144
28
68
32
132
40
376
. 24
24
20
92
60
52
2.0.
Pb 1 Cu
16i
80
10
72
10
100
20
68
12
184
12
92
104
22.
62
12
92
14
52
10
80
16
108
16
84
16
56
14
. 48 .
12
20
8
52
24
36
12
l - j -
!ri. ,'-
i
i
j ' -.'-,
j- :' . ;i 'i .I.- . '- . \\ ' ' 'i'i, : .i-i L '
1 ' '
Ni Ag Zn .
i
Pb
'
i
'l.
TOWNSHIP
.
-
SAMPLE NO.
Knight j 1398
(Anomaly. #18;
:'
'
1399
1400
1401
. . 1402
1403
1404
1405
i 1406
i 1407i -
1408
1409
1410
1411
1412
1413
1414
1415i
14161 E 1417 .B
' 1 1418
1 1419' ' '1
| 1420
i| 1421i '
1422
1423
1424
1 1425
1426
1427M
j . 1428
' f. ' 1429- ' : fj | ' '
1 1430. '
: ;! 1 431
. . f 1432
. ' j'" 1433 ; .(\ ' .
lf
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03
Cu
8
22
20
12
26
8
38
12
36
46
38
12
40
8
30
8
.8
24
20
12
12 .
12
12
NO !
40
4
4
6
16
16
20
28
16
8
30
6
. ,
Ni
12
22
24.
20
24
20
36
24
36
104
44
24
40
22
28
10
6'6
8'4
10
8
8
AMPLE
28
12
8
.16
.14
12
12
20
12
.22
32
16
Ag
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
1.0
..5
.5
.5
.5
.5
.5
.5
.' .5
.5
.5
.5
..5
,5
,5
.5
' ,5
.5
.5
.5
,5
• 5"'-.5
.5
Zn32
24
56
24
60
40
440
28
188' 28
48,
24
156
20
220
12
22
22
20
16
30
20
28
88
16
20
16
44
38.
, 46
92
96
16
80
16
Pb
16
12
74
•; 12
52
16
132
16
108
16
36
12
60
12
92
121 14
8
12
8
20
4
8
68
8
8'4
40
8
24
16t
40.
: 8
64
4
(Edta)
Cu
ii j iii - .t
i if
i!
r . -l
i
iiji'" - :j V . . V|. ;is ';
'
1 . -'
- f•;. t
NiI -
Aq f Zn .-
Pb .
v
k
TOWNSHIP
Knight
(Anomaly #18
.
"-
SAMPLE NO.
1434.
! 1435 -
1436 .
1437
1438
1439
1440
1441
1442
1443i-1444
1445
1446
1447
1448
1449
1450
l 1451
i 1 452i
1453
j 1454
j 1455
j 1456
| 1457
1 1458i
' , J 1459
1460
1461
1462
1463
i 1464
\ 1 465
1 1466
| 1467
' f, 1468
i K69B
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03. ; j ( Edta)
Cu
16
4
16
4
12
4
10
6
12
6
8
4.
12
4
124'
12
8
10
12
' 18
8
20
NO
18
44
32
10
44
4
28
6
30.4 '
10
4
*
Ni
12
10
12
8
8
8
4
12
16
1,6
. 12
12
16
16
18
28
16
24
14
24
24
20
24
SAMPLE
18
26
26
32
62
20
36
28
36
16
16
18
Ag
.5
.5
- ..5
' .5
.5
,5
.5
. .5
.5
.5
.5
.5
• 5
•5
.5
.5
.5
.5
•5
.5
.5
.5
.5
k "
,5
.5
;s.5
•5
.5
.5
.5
.5
.5
.5
.5
Zn60
. 12
60
12
44
12
32
. 14
. 76
20
38
12
120
20
108
20
136
30
66
24
96
. 60
160
100
28
52
28
120
24
184
32
208
20
80
20
i ' Pb
44
12.
. 52
4
30
6
; lo: 4
44
4
16
4
34.
". 8
32
10
40
! 1 2
j 36
8
: 44
12
72
60
16
3.2
10
126
12
112
14
112
8
24
10
Cu
-
i .
; ,' '
j '
l.; f '
Ni Ag i Zn . Pb
l
li ^TOWNSHIP™
r1 SAMPLE NO.
e . . " Knight \ 1 470
(Anomaly #18J) 1471'. - . - -
:-, l . : '
'
1 472
1473..
1474
1475
1476 .
1477
! 1478
1479
1480
1481
1482
1483
1484
1485
l I486-ii
'
| 1487ii-. 1488.i
1489
i 1490it
1491
1492
1 1493
1494
J 1495
. 1496
Knight J 1497
(Anomaly #18) 1498
1499
1 500!
1501
1502ij 1503. f| 1504 ,r
|, 1505it ii
f
J
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03 f ' ( Edta)
Cu -
24
4
20
6
22.
4
36
6
32
-4
20
6
24
6
28
4
12
10
36
SAMP
16
12
NO S
8
6
32
8
8
34
N1 .
32
16
20
22
40
18
28
20
32
28
16
20
32
20
32
20
16
22
32
LE MIS
6
4
UMPLE
4
2
4
4
2
8
'Aq
.5
,5
.5
.5
.5
.5
.5
.5
.5
.5
'rr,5
.5
,5
.5
.5
.5
.5
.5
.5
;ING.
.5
,5
.5
.5
.5
.5
.5
.5
Zn136
28
138
32
128
24
132
24
400
•24
96
16
204
28
204
20
132
46
264
36
14
21
10
36
20
17
24
Pb ;96
Cu "
4s
48
4
40
16
88
12
112
12
i 48
8
80
12
92
' :. '8
52
14
152
, '
'
20
8
20
8
20
16
16
16
-
.i '
. ,
i
; ' :i ii; ''ii l
1
i
1
Ni A9 Zn .
*
Pb
'
.
t
TOWNSHIP SAMPLE NO.S
Knight J 1506•f .(Anomaly #18) 1507 '
1
' . .
.•- .
1508
1509
1510
1511
. 1512
1513 ..
1514
1515
1516
. 1517
1518 '
'1519;1520
1521
............'.—r-- j 1522•3 . .' .
i .1523
i 1524
1525
j 1526
1 1527 .•.
.
.
j 1528t
i 1529
j .1530
j 1531
1532
f 1533
| 1534
~
; 1535i | 1536
j- 1537
\ 1 538 .
' 1539
f 1540i - i 541' "i
ANALYTICAL RESULTS IN P, P. M.
(Hot) HC104-HN03 f. ' ( Edta) .
Cu
32
8'
16
6
•12.
6
34
4
16
. 6
36
6
12
4
28
6
24
168
128
24 .
16
4
28
4
30
4
16
4
14
8
16
4
20
16
28
8
Ni
12
12
. 14 .
20
12
16
32
14
16
20
40
18
16
s 16
32
24
20
10
12
6
•4
14
20
16
28
24
20
22
16
40
28
16
22
92
60
14
Ag
,5
' .5
,5
,5
•5
.5
.5
- . . 5 .
•.'..5-
.5
.5
•5
' ,5
.5
' .5.
.5
.5
.5
.5
.5
.5
. -5
. . 5
.5
- .5
,5
.5
.5
. .5
.5
.5
.5
' .5
.5
- .5
.5
2n
40
16
44
16
64
16
172
12
66
20
224
26
86
14
104
18
156
64
86
30.
48
16
230
22
228
24
92
20
104
84
100
12
52
- 80
180
52
Pb
20
36
12
32
12
128
10
60
12
176
- 16
52
12
80
10
80
16
12
18
32
12
92
8
' 105
, 1 2
72'16
56
10
44
6
96
- 16
1 52
.12
Cu
,* '
'
\ ' ' '
r '.j ' ;j
Ni Ag ( ' 2n .
'. .
-.
S
' P b
'!
*
*
*TOWNSHIP
Knight ;
(Anomaly #18}
'- . ' i '
SAMPLE NO.
1542
1543,. '1544
1545
1546
1547
1548!
1549
1550i . . - i
. 1551
1552
15531 ' " -
1554
1555 ;
1556
1557
1558 -
1559
1560
\ ; 1561 .
l 1562i -
i 1563
' . j' 1564.
... : ' - .
\ J 565 ' :
j 1566 .
i 1567; !
^'- l 1 568. .f! - '
^ ' 1- 1569
' \ 1 570'•^- i; , _ . ...----.
1 1 571
j 1 572
i! 15731 ^ .:. \ "1574
|
\ 1 575\ ' 1576 -'
l 1 577P
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03 | ( Edta)
Cu
28
8
26
8
40
4
20
4
36
4,
48
8
12
4 .
32.4-;20
8.
28
440'
4
32
4.
40
4
52
4
36
8
16
42
28
36
28
20
ii S "-'
Ni
36
30
36
28
36
22
20
22
36
4
40
22
24
20
36
12
. 20
20
32
20
44
20
32
16
44
12
68
1&:32
20
.14
28
32
32
36
12
i A9
.5
.5
,.5
•5
.5',5
.5
.5
.5
.5
•' .5
•5
' -5
.5
.5
.5.'
' ; .5
.5
.5
,5
.5: ',5
,- .5
-5'.5
.51 .5
:,:.J5
,5
.5
. -.5
.5
.5
.5
.5
.5
Zn
380
40
300
32
290
28
230
22
248
16
520
38
180
28
352
28
120
. 40
290
44
420
50
510
40
820
18
580
270
24
50
44
46
36
34
26
32
Pb
88
10
j 92
i 8
132
; 10
"60
1096
4
1 164.
10
44
8
. 104
6
48
20
92
8
116
; 14
116
10
96
8
156
: 8
104
: 10
52
: 16
20
16
24
24
Cu
•;; ; '';,'.
ii . ii ' .> 'i . ' ^l j ,-is . -
Ni Ag
,
-.
Zn . Pb
.
t
TOWNSHIP
Knight
(Anomaly #18
i SAMPLE NO.
1578
) 1579
1580
1581
1582
1583
j 1584
1585
1586
1587t
1588
1589[j
.1590'
.
.
'
1 591
1592
1593
1594
1595
j 1596
j 1597
j 1598 .
\ 1 599j
1600 .
1601
1602*
1603
1604
1605
1606
1607
| . 1608
1609
1 1610
1611
f . 1612f k
. 1613.
V | 1614
ANALYTICAL RESULTS IN P. P, M.
(Hot) HClp4-HN03 ; | - . ( Edta )
Cu
14
12
8
8
8
8
8
8
12
8
4
10.
12
8
6
6
8
12
6
12
14
6
12
4
12
4
4
6
8
16
20
20
16
36
.16
4
24
Ni .
8
8
10
6
4
6
4
. 4
10
2
4
6
8
4
4
4
8
6
4
6
12
20
' 12
4
10
4
6
6
, 8
8
8
16
38
24
16
16
24.
Ag
. .5
,5
.5'i 5
,5
.5.'.5
.5
-5
.5
.5
.5
.5
.5
.5
,5
.5
.5
.5
.5
-5
•5
.5
,5
•' .5
- .5
.5
.5
,5
.5
.5
.5
.5
' ,5
.5
.5
.5
Zn30
32
• 40
20
24
28
24
40
44
16
20
32
40
16
16
: 14
44
10
8
22
60
24
.36
12
40
18
28
16
28
32
22
20
200
28
126
18
194
: Pb
12
40
32
16
..'16
20
20
' 20
•34
8
.16
28
40
12
8
12
36
8
10
12
52
20
16
: 840
8
14
- 1 2
20
! 16
20
;.io24
• 6
r 3212'
Cu -
! ; .- so f. . ;
Ni '
.
Ag l Zn .
j
-
-
Pb
-
y '
TOWNSHIP
Knight
{Anomaly #18
-. ^
' .
~~ ,
~ . . ...-.-....'.-— ~-
SAMPLE NO.
1615
1616 '
1617
1618
1619
1 620
1621
"1622 .
1623
1624
1625
1 626
1627
1628
1629
1 1630
J 1631•i
.
-
-
1632
! .1633
1634
1635\
1636i i1 1637\
' .
;
i 1638
1639 i
1640
1641
. - -.1642.1. .
' ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03 : | . (Edta)
Cu
2
16
3
' 16
4
24
4
24
8
14
NO S
52
3
12. 4-
^24
8
26
6
30
24
44
NO i
20
6
18
4
.24
N1
16
16
20
20
20
28~ 20
. 32
24
24
AMPLE
40
20
28
24
24
20
36
24
36
20
20
AMPLE
' 44
: 40
32
24
32
Af
.5
T-;-
. 5
' .5
c
Zn
. 18
284
18
86
38
. 364
34
380
20
96
384
16
100
18
340
18
104
20
248
.' 30
50
450
36
204
20
: 206.
Pb I Cu; 8
36
8
36
8
48
12
60
8
36
132
8
52
10
68
12
44
92
12
i 24
; ,- -.
28
10
40
1 4 ;88
'
"' : ' ;".'; :
' i
. . . ii ' -r.- -i
- .- ' ••' i
iis. -. -. , ..
Ni Ag
'
•'•Zn..
'
. '
-
Pb '
t
. V
TOWNSHIP
'
; SAMPLE NO.1,
Burrows ji 1 651
{Bu #2, Gp l) 1652. . . ' t .
.
'
i 1653
1654.
1655
1656
1657
1658
1659
1660
1661
1662
1663
1664
1665
j 1666
1 1667•l" | 1668^ ~~ - - ' \ ' ~'
.^'
5 1669 -j
J 670i\ 1 671ti 1 672ii
,,:,J 1673
- | 1674
'f 1675 :
j 1676
•1677
l 1 678[l1 1 679
l 1 680c
1681l -
16828| 1683.|
- 1684 '•^1685
f 1686
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03
Cu
6
14
4
18
10
20
B.'ip.
6
9,':'4- :
4
3
12
5
1
2
1
2
4
4
4
12
. 8
8
16
2
6- ^
2
8
2
4
4
4
2
4
I"
Ni
28
32
•20
16
40
22
36
12
16
16
20
8
16
10
16
8
20
8
-22
10
12
6
28
24
16
12
12
8
- 20
12
8
6
24
10
20
8
Ag.5
• 5
. .5
• 5
.5
,5
.5
.5
. -5
-5
.5
,5
.5
.5
.5
•5
.5
,5
- ;.5
.5
.5
- ' .5
•5
.5
.5
.5
.5
. .5
.57 -5
.5
.5
,5
.5
.5
.5
.•.
;. Z n .
36
232
32
132
40
216
26
60
36
124
24
36
24
. 36
20
6
28
TO
20
20
16
15
18
18
14
84
10
24
14
36
15
20
20
18
16
18
Pb12
96
14
46
12
48
8
.16
6
40
8
12
8
16
4
4
4
4
6
16
8
16
10
.8
4
36
4
16
4
20
6
.8
. 4
8
4
12
(Edta) '
' Cu
. .' ;
.;: ;-v
,,"'
. '
i p -
p i
1 . :. . ''r :i :l ,\ ;
r ' 'iii,1iil -1tf i
Ni
^
Afl'
j .
Zn .
•'. ; -
,
Pb
'.
•' ' :
f
ii'i
- ' '1
'i
'•' ; J
f
l
1
l
i
f
TOWNSHIP^
Burrows
SAMPLE NO.
1 687
(Bu #2, Gp l| 1688
j 1689
1 690
1691
-
1692
1693
1694-J 1695
j
1696
1697
1698
1699
1700
1701
1702
1703
l 1704P\ 1 705
I 1 706
j. 1707
! 1708
j .1709
f l 7 ! 0
f . v'1711-
| 1712
1 l 713
| 1714
f 1715
| . 1716
1717
| 1718
1719
1720
1721
j 1722\ ' ' l 1 723
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03- j ( Edta )
Cu
1
1
2
12
16
16
4
28
2
20
4
16
8
4
2
8
2
2
4
28
3
23
. : l'
25
4.
35
4
5
2
2
11
80
3
12
4
8
6.
Ni
12
6
20
14
22
16
18
24
12
16
14
12
20
12
14
4
12
8
16
20
16
. 20
8
24'28
16
20
4
-20
8
.18
10
20
12,
16.
52
Af)
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5
.5'.5
.5
. .5
.5
.5
.5
.5
. .5
.5
.5
.5
.5
.5
.5
•5
.5
.5
.5
,5
.5
-5
Zn
10
4
16
44
19
112
14.
186
10
204
10
- 84
20
20
12
18
12
12
10
148
16
126
10
124
. 16
32
16
24
16
12
20
24
14
. 44
32
26
58
Pb
4
4
6
38
8
60
8
92
4
72
4
40
8
12
8
12
4
8
. 4
92 .
12
80
10
64
TO
40
8
.16
.4
8
12
20
6
36
8
16
20
Cu
i ' . ' . . ~j - ' . : '
l'
i . ' ' .
i '-. ;i .
i - t1 , : '
Ni Ag Zn , Pb
.
1
l
TOWNSHIP^
Burrows
(Bu #2, Gp '
-
, :.
: ' . .
;-- .^
- .
.
1
•'".
-
'
-. j' ' i
.
; .
-
Burrows
SAMPLE NO.
1724
1725
1726
1727
1728 .
1729
1730
1731
1732
1733 *
'1734
1735
17361737V '
.1738
1739
1740
1741
1742
i 1743
j 1744
.1745
1746"
1747
1748
1749
(Bu #2 Gp 2| 1750.
1751
1752
f 1753i1754
1755
1756
1757
1758
1759
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03
Cu
10
10
8
7
4
4.
. 4
8
12
4
21
.10
6
2]
6
1
11
. 4
V 4
4
16
.10
14
1
24
3
4
8
24
32
8
n10
3
10
4
.Ni
24
32
12
12.
12,
30
. 12
28
40.
24
20
28
12
20
8
8
12
20
12
28
16
36
20
16
24
16
12
52
; 3252
20
40
22
20
14
. 16
Ag
•5
.5
•5
-5
.5
: - 5.5
.5
.5
.5
.5
.5
•5
.5
.5
.5
.5
.5
.5
--•5
.5
.5
.5
.5
.5
. .5
.5
.5
.5
.5
.5
,5
• 5
. .5
.5
.5
Zn
88
32••'..44
16
40
16
23
30
60
' 20
203
28
40
16
44.'•19
83
12.
18
18
88
18
45
' 12
76
33
47
60
240
60
68
36
76
15
68
16
Pb
36
8
40
16
12
8
16
14
32
6
68
12
20
6
28
8
36
4
12 -
10
32
12
24
10
64
4'16
16
60
20
36
12
24
8
32
10
\
(Edta)
Cu
' - ;.
•••' , . ;
1
i
Ni
*
,-
- -
AS
, " ' '
Zn .
•C . -
'••••' , '
' '
'Pb
--
.' : " '
- . -
'
.
i
TOWNSHIP ™ 1 SAMPLE NO.
Burrows 1 1760 '
(Bu #2 Gp 2)* 1761
-. .
'
.
j 1762
.1763
. 1764
1765
\ ;1766
l 1 767
1768
- ' '
'
J
.
1769
/'l 770 '
1771
1772
1773
1774
1775 ,
1776
1777 "- .1778
i 1 779Foleyet, j 1780 .
ANALYTICAL RESULTS IN P. P. M.
(Hot) HClp4-HN03 - | . , ( Edta)
Cu24
3
1
2
1- 4
2
. 2
5
4
n3
4
2
24
2
6 : '.3'
4
4
16
Ni20
20
;10
20
8
24
10
20
8
24
•' 16
20-. ' 4 :
16
24
.20
8
16
: 628
.10
•Afl
,5
.5
.5
\ . 5
..5
.5'.5
. -5
..5
. .5
: .5.5
.5
•5
.5'.5
.5
.-5
•5
.5
i Z n64
16
12
20
8'16
10.
24
28
20
72
; 18
26
16
19216'
22
25
2518'.
24:
Pb B Cu68
4
8
8-•'' 4
•4
:. 6
8
J 16
8
40
8
, 16
.l 10 '
88
'J 10
.30
8
V16••;. 8
, 6
j;",; .
,
.' -, v
r ... .... -'.i ' " 'i ' ' ' ' " * "! ' ' ".'. '
i
i ' ; .' i .''•".. ; :-:,i ' ' ' ' , : '. '
i - '- ;' -|j--'; : :;;;
Ni
1
Ag 1 Zn .
. ..
"
,-
. Pb '
•, :
, *
•. . ' ;
i
'.w,,,,-,,., SAMPLE NO,
ANALYTICAL RESULTS IN P.(Hot) HC104-HN03
Cu Ni Ag'Zn
Hg1
Pb II Cu
P.M.
(Edta)Ni' Aq i '2In' Pb
Burrows
(Bu n Gp 2)^
i 1800 ,f1 1 801 ;li
| . 1802
| 1803
•1804.i!t) '
1 805
1806
1807
1808
1809
1810 :
1811
1 1 812
1 1813f1 1 814 -S1 1815
'j 1816
jj 1817
j 18181
1819
j 1820 '
1 1821i 'j 1822
i 1823
j 1824\l 1 825
i 1826
| 1827 :
S 1828t| . - 1829
f 1830. '\ ' m]f-'' " --J
6
6
40
6
7
24
2
4'4
4
12
3
24
4
10
14
32' 4
6'
40
28
8
25
2
8
4
: 5
2
6
1-..
i ' K1 -
h-*.:
1 .
8 .
32
40
12
•44
20
8
16
8
14
14
12
20
24
12,
52
28
1 12
16
80
44
28
32
14
8
20
. .8
16
8
16•"14.
.36
' .5
.5
.5
.5
•5
.5
.5
.5
.5
.5
1.0
1.0
•1.0
". -5
.5
.5
,5
.' .5
.5
.5
.5
.5
-•5
,5
.5'.5
.5
• 5
.' .5
.5
.5
•;. .5'
35
40
420
48
28
;81
8; 14
12
18
60
8
88
1460 '
22
78
12
56*
32
300
24
260
12
30
12
16.
12.
. 32
16
60
16 .
20
12.'
88
28
12
90
j 4
\ 4
4
: 420
8
68
-12"44.
16
68
8
20
12
84
8-
48.
8
l 6
8
12
8
. 20
10
40 .
B!
1
..•-... ,' .
1 'V:.'-'J5 ' . . '1 '"' ; -" :-i!i
ii j -
i ' 'ii - -'
.'
- .-
.i -lii .
1 ' ' ;i -' ' ''l - ' ,''t , - , *
"i -'l ' '
l'' - -'.
L --
i
- ' : (
j
'•' '' -
i - . , -.~
' - '
1
j
' !
i •; ' i" i
i
i 1
i'- -
t
i
TOWNSHIP
Burrows
(Bu #2 Gp 2)
Fawcett
(Gp. 1)
SAMPLE NO.
1832
j 1833
1834
1835
1836
1837
1838
1839
1840
1841
1842
1843
1844
1845
1846
1847
1848
1849
1850
1851
j 1852i
1853
1854
1855
1856
1857
1858
\ 1 859i'
i
-
1860
1861
1862
1863
1864
1865
| 1866
i 1867'
l
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03 f ( Edta)
Cu
16
1
1
4
12
1
42
2
1
1
1
20
32
10
22
8
12
8
14
8
30
16
26
8
12
6
12
4
40
6
8
8
30
12
28
16
Ni
18
14
8
16
. 16
12
32
12
6
20
12
28
28'•'16
20
10
12
28
12
20
28
24
24
16
12
24
12
20
. 44
16
8
24
32
28
32
26
Ag
.5
.5
.5
.5
.5
.5
;l.o.5
.5
.5
.5
.5
. -5
:- .5
.5
.5
.5
. ,5
.5
.5
,5
.5
.5
•5
•- .5
.5
.5
.5
.5
.5
. .5
.5
.5
.5
. 5
ci ^
Zn52
12
8
12
20
32
870
24
.12.
20
16
32
48
24
62
16
48
24
en28
68
28
76
20
48
20
" 40
26
304
24
34
22
102
- 2 2
52
32
' Pb
76
TOi-12
4
24
8
152
8
8
8
8
S
16•10
26
1 8' 36
6
i 32
6
56
6
64
4
16
12
r 2812
124
12
24
8
70
8
. 48
12
. Cu
i v-j :. .
i \ j .i1 ' .
i
i 1
1 .
!
i . - . '
|. .-...'•,-i. ; . ;i " " . * '
; ' . : . :
t 1 ' .'i ' : - i ' ' -
i
i ' . ,; ,'. ii '
j ; ;
Ni Aq 1 Zn
iPb
.
*
* f
TOWNSHIP
Fawcett
(Gp. 1)
•; . .
-
^ -
- i••^
'
h
.
SAMPLE NO,
1868
1869 -.
j 1870
1871
1872
1873' - '1874
1875 .
1876.
1877
18781
1879
1880
1881 y.1882
1883
1884
1885
1886 * .
1,887 -.
1888
' 1889
1890-
1891
1892
1893 '
1894
1895[i .| 1896|
1897l)\ 1 898
\ 1 8998r
j 1900 .i
1 1
1 9011
1.902
1903
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03. : f , ( Edta)
Cu
20
28
36
12' 2.4 -
16
ie:8
24
6
22
228
76
42
44
6
24
12
32
12
12
4
16
6
14
4
36
4
20
4
24
8
8
4
32
48
Ni
24
24
32
36
28
36
20
16
28
24
24
44
. 24
. 20
20
24
24
24
36-
28
20
24
20
16
24
16
38
24
.28
20
32
24
8
16
34
20
AB• 5
•5
.5
.'5
.5
.5
.5
.5
.5
.5
•5
.5
.5
.5•:'.- 5 '
.5
.5
.5•-.-B-
.5
.5
. .5
.5
.5
.5
.5
.5
,5
,5'Is
.5
.5
.5
,5
.5
,5
: zn.eh42
120
44
118' 84
76
16
140
28
86
540
328"'..36;
64
16
84
28
168
36
80
16
40
24
76
22
72
20
112
36
208
18
. 26
20
388
32
: Pb16
20
88
10
64
28
44,
8
84
12
52;.'.: :'- : 8-
;1612
20
8
72
10
124
10
36; 12
44
12
48
14
72
, 8
.60"12
72
8
.16
8
84
! 12
' Cu
; . . - ; ; : '
t
' -
' .
iii ' . . . 1
'
N1
- ''
. ,
. ' '
Afl
j .
.
Zn .
. -—
.
Pb
.--
. ';
"' ". '
x f
TOWNSHIP
Fawcett
SAMPLE NO.
1904
(Gp, 1) 1905
1906
.
.
'
1 '
1
1907
1908
1 1909
1910
1 1911 1
1912i
1913
1914
i 1915
1916
1917
1918
1919
1920 ,i - .
1 921
- 1922
1923
1924
1925
1926
1927
1928
1 929
1930
1931
1932'
: l 1933 ' :
' 1 1 934
\ 1 935-
.
•- , .
.*-
, . \
1936
1937
1938*
"1939i | 1940!
i
' ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03 f ' . ( Edta)
Cu
232
328
800
16
42
10
34
12
48
12
26
16
20
20
24
16
. 32
4
20
8
32
16
40
4
10
8
18
40
46
6
20
12
24
6
38
22
34
Ni
68
44
.46
24
12
30
44
16
60
32
32
24
16
40
20
24
36
24
30
28
36
24
24
12
.16
28
30
28
36
24
20
32
20
12
36
. 20
20
Ag
.5
.5
1.5
. .5
.5
.5
. .5
.5
.5
.5
.5
• 5'..5
.5
.5
• 5
. .5
.5
.5
' .5
.5
.5
. .5
.5
••5
.5
.5
• 5
.5
: . -5.'•'-.5
.5
. .5
. .5
.5
•5
, .5
Zn
590.
32
32
24
40
' 28
144
20
152
48
88
44
88
24
68
' 2 rr
92
20
68
28
124
32
128
16
32
96
124
188
200
52
88
24
84
14
104
20
60
Pb
108
16
:16
8
14
12
88
16
112
12
52
1.2'•44
8
72
12
84
1 12
i 68
12
80
•14
36
8
40
12
34
44
14?
.12.
48
: 12
48
8
132
8
i 32
Cu
' ,.
;. -'. -
- '. ' ' ' '
1 '
i '
li i i
t
ij]is . -.
Ni
' .
^• : '
Ag f Zn .
,
-
Pb
-
-
.
-
yrTOWNSHIP SAMPLE NO.
Fawcett t 1941li{Gp. 1) 1942
19431j 1944:
- -
' i
ff il \
1 945
1946
1947
1948
1949
1950
. 1 951
1952
1953
1954 '
1955
1956
1957
1958
1959
1960
1961
1962
1963
1.964
P 1965 '
.
' - ' i
1966
1967
1968,
1969,
! 1970
1971
1972- :
^1973
.1974
1975
1976
1977'
ANALYTICAL RESULTS IN P. P. M.(Hot) HC104-HN03
Cu
8
28
8
16
3
8
6
20
4
24
10
18
12
28
24
20
8
16
12
18
26
28
22
16
4
14
8
.16
6
32
8
54
8
42
16
40.
,8
Ni
22
24
26
22
16
12
20
28
20
26
12
16
28
30
28
32
16
18
24
16
28
24
18
20
20
20
26 .
16
-.20.'36.'-
20
56
20
46
16
36
20
A9
.5
.5
.5
.5
.5
•5
.5
.5
.5
. .5
•5
.5
.5
.5
.5
, -5
.5
.5
.5
.5
,5
.5
.5
.5
..5
•5
'j . 5
•5.
,5
.5
,'- 5.'5
.5
.5
.5
•5
.5
Zn
16
108
30
64
32
68
24
144
36
172
16
60
28
232
28
88
20
28
28
48
48
144
34
58
30
84
40 :
: 92,48
188
46
156
24
144
42
120
30
Pb |10
76
6
44
6
28
12
80
10
60
, 8
44
8
88
12
.144
8
28
8
34
18
60
12
46
12
40
12
66
16
70
12
84
8
116
14
92
12
(Edta)
Cu
. ' -
,-'-v.',
'. /. '•
- ' . ' -''
i ' i ' -i i ' , -;i '. i i '
j :
Ni.
. --
(
^ '
Afl
.
Zn .
f
Pb
'
• '
T
-
l
v
\
^^
V ' '\\
TOWNSHIP l SAMPLE NO. '.
Fawcett J 1978li
(Gp. 1) \ 1 979f\ 1 980i-
1981
1982
1983
1984
1985
1986l
1987
'-
1988
1989
1990
1991
1992
1993
1994
l 1 995
f 1996
\ 1 997j \ 1 998
j 1999
l 2000"ifi 2001
: 1 Z002L. ™.. - .. . fi
— i-wjj^.^ ,, .
ANALYTICAL RESULTS IN P. P. M.
(Hot) HC104-HN03 f (Edta)
Cu
16
16
36
60
32
18
16
6
40
4.
24
4
124
10
30
10
30
4
44
8
28
12
16
16
18
Ni
20
16
34
32
22
24
24
16
40
20
.26
8
28
24
32
16
16
16
38
20
32
32
20
24
28
Ag
.5
,5
.5
,5
•.5
•5
.5
•5
•5
.5
.5
.5
.5
.5
,5
.5
.5
.5
.5
.5
.5
.5
.5
,5
. .5
Zn
56
40
180
84
168
•44
140
26
212
32
144
28
64
32
116
34
156
36
296
30
180
34
68
28
40
Pb l Cu
30
20
70
14
56
16
28
12
120
.14 -
60
1284 '
. 16
68
12
56
14
108
12
96
8
24
12
26
;
1 ' . i ,
i
1 '
i
i
1
i
J '"' -
i
Ni A9 Zn . .Pb
.*
'
i j
i'-
i1
i
Raymond Twp.-M.244
44404 l 399B7 t 3 9596 ( 4 *424 l Q
Tyrrell Twp.- M.253
C\ls
l CL
oCO
c: o
THE TOWNSHIP OF
KNIGHTDISTRICT OF TIMISKAMING
LARDLR LAKE MINING D IVISION
SCALE: 1-INCH-4O CHAINS
LEGEND
PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLED
*C.
NOTES
400* Surface Rights Reservation around all lakes and rivers.
DATE OF ISSUE
r* 2 81972
ONT. DEPT. Of MINES AND NORTHERN AFFAIRS,
PLAN NO- M.228
ONTARIODEPARTMENT OF MINES
AND NORTHERN AFFAIRS
41PI4SEWI56 63.3935 MONO 200
65
as
20W I6W I2W 8W 4W O 4E 8E I2E I6E 20E Z4E 28E 32E 36E 40E 44E 48E 52E 56E 60E 64E 68E 72E 76E 80E 84E
I6N
TRANSMlTTER STAT l ON
CUTLER MAINE: L32E - 52E INCL.
SEATTLE WASHINGTON^ L 20W - 28E INCL.
L56E - 84E I NCL.
DIP ANGLE' l" : 40 0
CONDUCTOR A XIS'
OPERATOR C BRITT
2N
O
AMAX POTASH LTD.
VLF RADEM DIP ANGLE SURVEY
HALLIDAY TWP. - ANOMALY NO. lTIMMINS
SCALE' l" ^ 400'
NTS NO 41 P/14
TO ACCOMPANY REPORT BY W R RYALL TIMMINS
ONTARIO
PROJECT NO 302 ST
DATE AUGUST 16,197.
41PI4SE8656 63.3935 MOND 210 , . 0*3)
Figure 6
LAKE
8S
20W I6W I2W 8W 4W O 4E SE I2E I6E 20E 24E 28E 32E 36E 40E 44E 48E 52E 56E 60E 64E 68E 72E 76E eoE 84E
2N
O
INSTRUMENT MCPHAR MF-|
SERIAL NO .- 6485
OPERATOR' L. KYDD
BASE STATIONS' t
BASE STATION VALUE' 500 GAMMAS
CONTOUR INTERVAL^ 1000 GAMMAS
100 GAMMAS
4IPI4SE0056 63.3*35 MOND 220
AMAX POTASH LTD.
MAGNETOMETER SURVEY
HALLIDAY TWP. -ANOMALY NO. lTIMMINS
SCALE' l" ^ 400'
NTS. N O 41 P/14
TO ACCOMPANY REPORT BY W.R.RYAL TlWlNS
ONTARIO
PROJECT NO' 302 S T
Figure 7
LiTfLE MARNE LAKE
INSTRUMENT CRONE LARGE LOOP TRANS,
FREQUENCIES^ HIGH 1800 CPS.
LOW 480 CPS.
TRANSMITTER SET UP ' \
CONDUCTOR AXIS' Q
DIP ANGLE SCALE l" * 40"
OPERATORS' M LAITINEN, L. KYDD
4IPMSEa*S6 63.3835 MOND 330
AMAX POTASH LTD.
CRONE VERTICAL LOOP SURVEY
BURROWS TWP. - GROUP NO 2ANOMALIES 485
TIMMINS ONTARIO
SCALE: -400N.TS NO 41 P/14
TO ACCOMPANY REPORT BY W. R RYALL TIMMINS
PROJECT NO 302 ST
Figure 8
LAKE
NSTRUMENT Me PHAR FLUXGATE MF-
SERIAL NO 6485
MAG. BASE STATION
CONTOUR INTERVAL - 1 00 GAMMAS
OPERATORS M.LAITINEN, L KYOD
41P14SE0e56 63.3035 MOND 2-40
A MAX POTASH LTD
MAGNETOMETER SURVEY
BURROWS TWP. - GROUP NO. 2ANOMALIES 485
TIMMINS ONTARIO
SCALE l"-400'NTS NO 41 P/14
TO ACCOMPANY REPORT B Y W R RYALL T IMMINS
PROJECT NO 302 ST
Figure 9
o
PIGEON L AKE
TRUE CONDUCTOR
TRANSMITTER STATION- BALBOA PANAMA
DIP ANGLE SCALE -- \" ^ 4 00
CONDUCTOR
OPERATOR M. LAITINEN
A MA X POTASH LTD.
VLF RADEM DIP ANGLE SURVEY
KNIGHT TWP. - ANOMALY NO.I8
TIMMINS ONTARIO
SCALE' 1-400NIT- NO 41 P/10,11
^ Z- ^jrtfTO ACCOMPANY REPORT BY W R.RYALL TIMMINS
PROJECT NO. 302ST
DATE: JULY 10-12/71
41P14SE8BS6 63.3035 MOND 250 Figure 10
PIGEON LAKE
INSTRUMENT McPHAR FLUXGATE
MAG. BASE STATION
BASE STATION VALUE. 500 GAMMAS
CONTOUR INTERVAL 1000 GAMMAS
200 GAMMAS
OPERATORS' L.KYDD, C. BRITT
AMAX POTASH LTD.
MAGNETOMETER SURVEY
KNIGHT TWP. - ANOMALY NO. 18TIMMINS ONTARIO
SCALE -400NTS. NO 41 P/10,1
6?-TO ACCOMPANY R EPORT BY WR.RYAl.i TIMMINS
4IPHSE8656 63.3035 MOND 260
PROJECT NO. 302 ST
DATE' JULY 12-15,1971
Figure 11
INSTRUMENT: McPHAR FLUXGATE MF-
SERIAL NO.' 6485
MAG. BASE STATION
CONTOUR INTERVAL' 100 GAMMAS
OPERATORS' M. LAITINEN, L.KYDD
41P14SE0056 63.3835 MOND
AMAX POTASH LTD.
MAGNETOMETER SURVEY
FAWCETT TWP. - GROUP NO. lANOMALY NO. 31
TIMMINS ONTARIO
SCALE -400NTS. NO- 41 P/ll
TO ACCOMPANY REPORT BV W R RYALL T IMMINS
PROJECT NO: 302 ST
Figure 13
TRANSMITTER STATION- CUTLER MAINE
DIP ANGLE SCALE l * 400
CONDUCTOR AXIS'
OPERATOR' L. KYDD
TRAVERSES' M. LAITINEN
AMAX POTASH LTD.
VLF RADEM DIP ANGLE SURVEY
FAWCETT TWP. - GROUP NO. lANOMALY NO. 31
TIMMINS ONTARIO
NTS. NO^
SCALE: 1^ = 400'
63-PROJECT NO- 302 ST
TO ACCOMPANY REPORT BY' W.R.RYALL TIMMINS DATE - O CT. 1-3, 1971
41P14SE0856 63.3035 MOND aso Figure 12
20W 12W 28E 36E 44E 52E 60E 68E
LEGEND:
Hot Extraction- HCI04 HN0 3
Soi! Samplers* R.Roussoin, C. Britt, M. Pickens
Date: ju|y 26, 1972
Base L ine
76E
ZINC IN TOPSOIL
HALLIDAY TWP. - ANOMALY No.
OVERLAY No. lScate* l" s 400'
NTS,. No 41 P/14
TO ACCOMPANY REPORT BY i
PROJECT 302 ST
AM AX Ltd., Titmiins, Ontario
41P14SE0056 63.3935 MOND 290 Figure 3 a
20W 12W 28 E 36E 44E 52 E 60E 68E
LEGEND'
Hot Extraction - HC104 HN03
Soil Samplers 1 R. Roussain, C. Britt, M.Pickens
Date; July 26, 1972
M Base Line
76E
COPPER IN TOPSOILHALUDAY TWP. - ANOMALY No.
OVERLAY No. 3Scale: l" s 400'
NTS. No. 41 p/14
TO ACCOMPANY REPORT BY'
PROJECT 302 ST
AMAX " Timmins
41PMSEW56 63.3035 MOND 300 Figure 3b
20W 12W 28 E 36E 44E 52E 60E 68E 76E
LEGEND'
Hot Extraction - HCI04 HN03
Soi l Samplers * R Roussain, C. Britt, M. Pickens
Date* July 26, 1972
Base Line
ZINC IN SUBSOILHALLIDAY TWP. - ANOMALY No.
OVERLAY No. 2Scale' l "s 400'
NTS. No. 4IP/14
TO ACCOMPANY REPORT BY;
PROJECT 302 ST
AMAX Potash ^d, Timrn.ns , Ontario ,
41P14SE0956 63.3035 MOND 310 Figure 4a
20W
L312905
L312906
5i
L312907
L312910
12W 28 E 36 E 44E 52 E 60E 68E
L308798
-n
LEGENDi
Hot Extraction- HCI04 HN03
Soil Samplers* R. Roussain, C. Britt, M. Pickens
Dote* July 26, 1972
Base Line
It "f
76E
COPPER IN SUBSOILHALLIDAY TWP. - ANOMALY No.
OVERLAY No. 4Scale' l" = 400'
NTS. No. 4l P/14
TO aCCOMPANY REPORT BY:
PROJECT 302 ST
AMAX Potash Ltd., Timmins, Ontario
4IP14SEe056 63.3035 MOND 320 Figure 4b
20W 12W O
L312904
L312911
4E 12E 20E 28E 36E 44E 52 E 60E 68E
L306798
Legend:HOT EXTRACTION- H CIO4 HNO 3
Soil Samplers : R Roussain C B'I". M P c
Date : July 26, 1972
Base Line
76E
LEAD IN TOPSOIL/SUBSOILHALLIDAY TOWNSHIP, ONTARIO - ANOMALY No. 1
Overlay No. 5Scale :r*400'
NTS. NO. 4IP/14
TO ACCOMPANY REPORT
NO- 302 ST
AMAX Potaih Ltd., Timmins, Ontario ~" ( ~/
41P14SESH&SS 63.3035 M OND 330 Figure 5
as
20W 16 W f?W 6W 4 W 4E 8 E l? f" I6t 20E ?4E 36E 40E 44E 48 E. 56E GOE 64 F. 6SE 76E so? 84E
l \
U 2D Diorite
Q 3 G Gabbro
chl Chloritic
graph Graphitic
^jf HI Conglomerate
fH H4 Quartzite and s andstonek Sericitic
(T~) V!D DaciteQ VIR Rhyolite
0 V2A Andesite
H V4 Rhyolite tuff
y Porphyritic
Area of outcrop
Contact assumed
Stream and direction of flow
FO U 1 1
Swamp
Rood
Sample no. and location
DDH
IS
AMAX POTASH LTD.
GEOLOGICAL SURVEY
HALLIDAY TWP.'ANOMALY NO.TIMMiNS
SCALE
TO ACCOMPANY REPORT BY DATE'
4IP14SE8856 63.3035 MOND 340Figure 6
Little l/Aarne Lake
L312950
LEGEND'
Hot Extraction - HCIfy HN03
Zn ppm Ooo ^
Soil Samplers* R. Roussoin, C Britt, D. Hawk e
Date' August 4, 1972
ZMC-COPPER IN TOPSOIL
BURROWS TWR,ONTARIO - GROUP No.2
OVERLAY No.2Sco*t'ltt-4OO'
NTS. NO. 4IP/I4
TO ACCOMPANY REPORT BYi
AMAX PottNh Ltd., Tim mini, Ont
PROJECT NO. 302 ST
DATE'
41P14SE8856 63.3035 MONO 350 Figure 8
D
Marne Lake
LEGEND'
Hot Extraction - HCI04 HN03
ppmppm
Soil Samplers' R. Roussain, C. Britt, D. Hawke
Date: August 4, 1972
ZINC-COPPER IN SUBSOIL
BURROWS TWR,ONTARIO - GROUP No.2
OVERLAY ISIo.1l" * 400'
NTS NO. 41 P/14
TO ACCOMRfcNY REPORT BYi—
AMAX Potash Ltd., Tinvnins, Ont
41PMSE0056 63.3035 MONO 360 S? "XS? 3
PROJECT NO. 302 ST
DATE:
Figure 9
Base Line
L312949
Little 'Marne Lake
Legend:HOT EXTRACTION - HCIO4
Soil Samples: R.Roi.sioin . t. fir it t D.Howke
Datet Auqus* 4
LEAD IN TOPSOIL/SUBSOILBURROWS TOWNSHIP, ONTARIO - GROUP No. 2
Overlay No.3Scale :l":400'
NTS.NO. 4IP/U
1O ACCOMPANY REPORT
AMAX Pntoil. l k)., Timi,
PROJECT NO- 302 ST
DATf-
41P14SE0056 63.3035 MOND 370 Figure 10
Little Marne L ake
Q l H Syenite
Q 28 Diabase
Q VIR Rhyofite
[Tj V 2A Andesite
Area of o utcrop
—' — Contact assumed
——— Contact observed
^—*--r Schistosity or f oliation
x6 Sample no. and l ocation
ODH
AMAX POTASH LTD.
GEOLOGICAL SURVEY
BURROWS TWP. - GROUP NQ 2ANOMALIES 485
TIMMINS ONTARIO
SCALE^ l"-400NTS. NO. 41 F/14
TO ACCOMPANY Rt PORT
4IPMSE0*56 63.3035 MOND 380 Figure 11
CNUJ(N
\
\\
L308816Base L me
\
\
\
LEGEND^
Hot Extinction - HCI04 HN0 3
Soil Samplers' R. Roussoin, C. Britt, D. Hawke
Dote' August 5, 1972
ZINC-COPPER IN TOPSOILFAWCETT TWR, ONTARIO -
OVERLAP No. 2
GROUP No.
NTS. NO. 4IP/II
TO ACCOMPANY REPORT BY'*—***^
AMAX Potash Ud., Timmins, Ontario
PROJECT NO. 302 ST
DATE ;
41P14SE*e56 63.3935 MOND 390 Figure 13
\\\
LEGEND'
Hot Extraction - HCI04 HN03
Soil Samplers* R. Roussain, C. Britt, D. Hawke
Date* August 5, 1972
41PMSE6856 63.3035 MOND -400
ZINC-COPPER M SUBSOILFAWCETT TWR, ONTARIO - GROUP No.
OVERLAY No. lScate l"*400'
NTS. NO. 4IP/II
TO ACCOMRWY REPORT BY:•^*
AMAX Potash Ltd., Hmmin*, Ontario
PROJECT NO. 302 ST
DATE
Figure 14
\
CN
\
Legend:HOT EXTRACTION - HCIOd HNO 3
Soil Samplers 1 R.Rousicim. C Bri*t D Hawk e
Date. Angus! 5 . 1972
LEAD IN TOPSOIL/SUBSOILFAWCETT TOWNSHIP, ONTARIO
Overlay No.3Scale -.l":400'
GROUP No. l
NTS NO. 41P/II
TO ACCOMPANY REPORT BYi*
AMAX Polosh Ud . Tirnmins , Ontario
PROJECT NO- 302 ST
DATE
41P14S60056 63.3935 MOND 410 Figure 15
00 O
L308817
Jfcr
\
Jt
^ff13 ' -K..X*
v^fi
L308816
Jt
\^nnr 1" lv-,"
It:
Jfe
X.
TOST
306812
•^f
, *^ ' v| .A*.' ; -. ^A
Z6 CniErfl)
-*t
1'^
thl.
//,
'Sf/s eM.k.^m /-
yy/!
rW.-^^"
/s* LI NE
/
L308812
41PMSEW56 63.3935 M OND -4S0
a 2B(3 3G
c
cbl
h
k
D MQ Ml
qv
D V IR V2A
D
x 18
O "O bO 66
Gabbro
Quartz
Chlorite
Horneblertde
Sericitized
Schist
HornfeU
Quartz vein
Rhyolite
Andesite
Rhyolite b reccia
Area of o utcrop
Contact a ssumed
Schist osi ty or foliation
Sample no. and l ocation
DDH
\ f/ * XTi i ^i si
L308813 ^ .S l
v ^ ^r
AMAX POTASH LTD.
GEOLOGICAL SURVEY
FAWCETT TWP.ANOMALY
1 IMMiNS
SCALE:r::-,, "j c. i! F-/-:
TO ACCJMF-ANY KtPOfc"! Hi" sb-A-^L.
- GROUP NO. INO. 31
ONTARIO"-4UU1
1 h: i| Li NO- .V'', ! '
J0 * ****flL*\^^ Ot-xC^-^ OA I^t"
7 Figure 16
PIGEON L AKE
LEGEND*
Hot Extraction* HCI04 HN03
Soil Samplers^ R . Roussam, C. Britt, D. Hawke
Date* August 2, 1972
ZINC "COPPER IN TOPSOIL
KNIGHT TWR, ONTARIO - ANOMALY No. 18
OVERLAY No. 2Scot* I N-400'
NTS. NO. 4 1 P/10, II
TO ACCOMPANY REPORT ^—^
AM A X Pot o* h Ltd., Timmins,
PROJECT Na 302 ST
DATE:
41PI4SE0056 63.3035 MONO 430 Figure 18
"fe\
PIGEON LAKE
41PUSE8856 63.3035 MOND 4-40
LEGEND:
Hot Exlroctiont HCI04 HN03
laCu ppm
Soil Samplers' R. Roussain, C. Britt, D. Howke
Date- August 2, 1972
ZINC -COPPER IN SUBSOIL
KNIGHT TWR, ONTARIO - ANOMALY No. 18
OVERLAY No. l
Sea* l"* 400*
NTS. NO. 4IP/IO.II
TO ACCOMPANY REPORT BY'v.
AMAX Potash Ltd^ T immins, Ont
PROJECT NO. 302 ST
DATE:
Figure 19
PIGEON LAKE
Legend:HOT EXTRACTION-MOO,, HNO 3
Soil Samplers R.Rousiain, C Britt. D.Hav/ke
Date August 2 1972
LEAD IN TOPSOIL/SUBSOILKNIGHT TOWNSHIP, ONTARIO - ANOMALY No.18
Overlay No.3Scale :l"--400'
NTS NO 41P/1Q. 11
TO ACCOMPANY REPORT
PROJECT NO 302 ST
AMAX Potash Lid . Timmins DATE
41P145ETO56 63.3835 M OND 450 j 7*'J1 2 3 Figure 20
Pigeon Lake
3H hornblendite
3E Peridotite
3G Gabbro
H l Conglomerate
H2 Arkose
H4 Quartzita
VID Dacite
VIR Rhyolite
V2A Andesite
V2B Basalt
Area of outcrop
-— — Contact assumed
-. .— Contact observed
x 1 8 Sample no. and location
POTASH LTD.
GEOLOGICAL SURVEY
KNIGHT TWP. - ANOMALY NO. 18
TIMMINS ONTARIO
SCALE: 1=400NTS. W. 4! P/10,
70 A'iCOMPAMY
PROJECT NO. 302 ST
4IPMSEB356 63.3835 MOND 460(S 6'
Figure 21