BULK TILL SAMPLING PROGRAM - Geology Ontario

52F84NE965e 63.6161 ADRIAN

MINGOLD RESOURCES INC.

QUETICQ (RECONNAISSANCE) PROJECT

OMIP PROGRAM NO. OM90-094

THUNDER BAY AND KENORA MINING DIVISIONS

ONTARIO

I Bulk Till Sampling Program

May - November, 1990

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If by

G. E. Bidwell

I November 25, 1990

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I I I I I I I I I I I I I I I I I I I

5aFa4NE9658 63.6161 ADRIAN

TABLE OF CONTENTSPage

I Introduction........................................................1

II General Geology and Exploration.....................................!

Ill Quaternary Geology..................................................3

IV Procedures (a) Planning....................................... 4(b) Pieldwork......................................4(c) Analysis of Results............................6

V Shebandowan Area (a) Geology and Mineral Occurrences................7(b) Field Work....................................10(c) Results.......................................10(d) Tinto Block...................................12(e) Greenwater Block..............................14

VI Atikokan Area (a) Geology and Mineral Occurrences...............16(b) Pieldwork..................................... 18(c) Results.......................................19

VII Mine Centre Area (a) Geology and Mineral Occurrences...............22(b) Pieldwork.....................................25(c) Results.......................................25

VIII Emo Area (a) Geology and Mineral Occurrences...............28(b) Pieldwork..................................... 30(c) Results....................................... 30

IX Conclusions........................................................33

X Cert i f icate........................................................ 35

XI References......................................................... 36


FIGURESPage

1. Location Map. ....................................................... .22 . Shebandowan Area Geology. ............................................ 83. Sample Location - NTS 52A/05. .................................... .pocket4. Sample Location - NTS 52A/12. .................................... .pocket5. Sample Location - NTS 52B/08. .................................... .pocket6. Sample Location - NTS 52B/09. .................................... .pocket7 . Sample Location - NTS 52B/10 ..................................... .pocket8. Tinto Claim Map. ................................................... .139. Tinto Geology and Sample Locations. .............................. .pocket

10. Greenwater Claim Map. .............................................. .1511. Greenwater Geology and Sample Locations. ......................... .pocket12. Atikokan Area Geology. ............................................. .1713. Sample Location - NTS 52B/11. .................................... .pocket14. Sample Location - NTS 52B/12. .................................... .pocket15. Sample Location - NTS 52B/13 ..................................... .pocket16 . Sample Location - NTS 52B/14 . ..................................... pocket17. Sample Location - NTS 52B/15. .................................... .pocket18 . Sample Location - NTS 52G/03 . ..................................... pocket19. Mine Centre Area Geology. .......................................... .2320. Sample Location - NTS 52C/09. .................................... .pocket21. Sample Location - NTS 52C/10. .................................... .pocket22. Sample Location - NTS 52C/11. .................................... .pocket23. Sample Location - NTS 52C/14. .................................... .pocket24. Sample Location - NTS 52C/15. .................................... .pocket25. Sample Location - NTS 52C/16. .................................... .pocket26. Sample Location - NTS 52F/02. .................................... .pocket27. Sample Location - NTS 52F/03. .................................... .pocket28 . Emo Area Geology. ................................................... 2929. Sample Location - NTS 52C/12. .................................... .pocket30. Sample Location - NTS 52C/13. .................................... .pocket31. Sample Location - NTS 52F/04 ..................................... .pocket

TABLES

1. Shebandowan Area - sample data and assays. ........................ .pocket2. Shebandowan Anomalies. .............................................. .113. Atikokan Area - sample data and assays. ........................... .pocket4. Atikokan Anomalies. .................................................. 205. Mine Centre Area - sample data and assays. ........................ .pocket6. Mine Centre Anomalies. .............................................. .267 . Emo Area - sample data and assays .................................. pocket8. Emo Anomalies. ....................................................... 31


I INTRODUCTION

In 1990 Mingold Resources Inc. carried out a reconnaissance till sampling program in the Thunder Bay - Rainy River district of northwestern Ontario. The object of the program was to locate bedrock gold occurrences through the study and analysis of the overlying glacial till. Although reconnaissance in nature the efforts were directed within or just down- ice of known gold areas or locations with favourable geological conditions for gold formation.

Large (20-25 kg) samples were collected from shovel dug pits and processed through a series of stages to produce a heavy mineral concentrate. The concentrate was examined for the presence of gold grains and assayed for a 34 element package by neutron activation. Small character samples, unprocessed, were also assayed for a seven element package.

A total of 823 samples were collected from May to September, 1990. Numerous anomalous values in'both gold grain count and gold assays were obtained. Minor follow-up has been undertaken.

II GENERAL GEOLOGY AND EXPLORATION

The project area occurs within the Wabigoon, Quetico and Wawa Subprovinces of the Archean Superior Province (Fig. 1). The Wabigoon and Wawa Subprovinces are granite-greenstone terrains comprised of supracrustal assemblages of predominantly metavolcanic origin and subordinate amounts of sedimentary rocks, intruded by granitoid rocks mainly of batholithic dimensions. The Quetico subprovince consists of an assemblage of predominantly metasedimentary gneissic rocks, their migmatitic derivations and granitoid rocks.

The Wabigoon subprovince is bounded on the south by the Quetico Fault, a major east-west dextral strike slip zone that extends for a distance of 375 km from Dog Lake, north of Thunder Bay to Rainy River on the Minnesota-Ontario border where it passes into the U.S.A. and is masked by recent cover. This major deformation zone has numerous subsidiary faults off the main structure which play or horsetail into the adjacent rocks.

The Quetico project area has a long history of gold exploration dating back to the late 1800's In the western portion of the area both Mine Centre and Atikokan produced gold in the 1893-1902 period. Total production at that time and during subsequent activity totalled 25,000 ounces of gold. Along the eastern section of the Quetico Fault and in the Shebandowan area gold production has totalled about 50,000 ounces from the Ardeen Mine (1932-36) and as a by-product at the North Coldstream mine. In the 1980's the whole belt was extensively explored with major gold programs at Moss Lake and Gold Creek in the Shebandowan Belt, Hammond Reef and Fern Elizabeth near Atikokan and some of the old occurrences in the Mine Centre area.


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III QUATERNARY GEOLOGY

Although four major episodes of glaclatlon have been recognized in the region only the last ice advance, the Wisconsin ice age, considered to be significant in this study. Glacial and interglacial deposits older than the Wisconsinan are not well known. Presumably much of the older material was destroyed and what exists is deeply buried. The Wisconsin ice age began about 100,000 years ago and originated from a source in northern Quebec/Labrador. The orientation of the ice flow features and glacial striae indicates that the continental ice mass spread in a south to southwesterly direction. In the western section of the Quetico Project area recent glacial studies (Mining, 1988, 1989, Cowan, 1987) of the glacial stria have a mean value of 219 (S39W). Approximately 20,000 years ago the ice reached its maximum extent and began to recede. The ice had withdrawn from the Quetico area by 10,000 years ago.

As a glacier advances rock fragments are incorporated into its base and frozen in the ice. The resulting unsorted mixture of fragments, ranging from boulders to sand, silt and clay sized material is called till. When deposited directly beneath the ice by the processes of lodgement and melt out, this debris is called subglacial, lodgement or basal till. When deposited from within, or on the ice as the result of melting it is called supraglacial or ablation till. In mineral exploration an important distinction between the two varieties in that the former tends to reflect the local bedrock and the latter usually contains rock fragments transported within the ice for greater distances.

Waters produced during the deglaciation process may rework and sort the till debris. Glaciofluvial deposits are sand and gravel deposited by streams near the ice margins and form large scale features such as eskers and moraines. The meltwater also transports large volumes of fine sediments into glacial lake basins. These glaciolacustrine deposits form broad flat poorly drained plains.

In mineral exploration, particularly for gold, it is best to sample the unsorted till. It provides primary material (first derivative) directly down-ice of its source. With glaciofluvial and glaciolacustrine second derivation deposits the debris will be moved off line of the ice direction and the gold particles may be concentrated in specific horizons or traps in the glacial drift.

Glacial drift cover in the study area for the most part is quite thin and sporadic except at the extreme west and where a separate ice advance deposited a clay-rich till covering the Rainy River district. Quaternary studies generally conclude the glacial drift is fairly local in origin and has not been transported from great distances.


IV PROCEDURES

(a) PlanningAreas were selected for sampling based on their potential for gold occurrences and also for their accessibility.

Regional-scale shear zones in northwestern Ontario are Important targets for gold mineralization. Most of the major gold deposits, eg. Red Lake, Beardmore-Geraldton, Golden Patricia, Favourable Lake, Musselwhite, are located in the vicinity of large east-west or northwest trending breaks. Recent detailed studies of these structures have shown that most of the occurrences are actually located on subsidiary faults off the major structures. These secondary features generally splay or horsetail into adjacent greenstone belts or along granite-greenstone contacts where a competency contrast exists between the lithological units. The difference in shearing ability along say, an iron formation/volcanic or quartz porphyry/volcanic contact, focuses an initial fault rupture which may later host gold bearing hydrothermal fluids.

With the above thesis in mind it was proposed that a reconnaissance till sampling program be carried out along the Quetico Fault. The location of the Fault just to the north of Highway 11 makes this technique an excellent exploration method. Ice movement was in a southwesterly direction, therefore gold grain counts from occurrences near the structure should be recoverable on or near the highway. As well there are numerous logging roads in the area providing access. With the accelerated gold activity in the Moss Lake area it was decided to extend the program into the Shebandowan greenstone belt as well.

(b) Fleldwork

Sample collection was carried out from May to September, 1990. Ideally samples were taken along NW fences (across the ice direction) with sample sites at 1 km intervals. In areas of known occurrences or very favourable conditions for gold, the sample interval was reduced to K km spacing.

Approximately 60% of the samples were taken along roads by truck. The remaining 40% were collected equally by boat and all terrain vehicles. Most samples weighed in the 20 - 25 kgm. range, hence the need for good access.

In most cases the till was sampled in the near vicinity of outcrop since this provided the most likely location for a basal till. It was also considered that the down-ice (SW) side of the outcrop, being on the lee side of the glacial direction, would be the more likely location for till to have been deposited. Almost all the till samples were collected from shovel dug pits averaging K metre in depth. In a few areas of particular interest an auger drill was used which could

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reach a 2 metre depth. At the same time as the main bulk till was collected, which would go through the concentration process, a second "character" sample was taken in a geochem envelope. During collection bedrock lithology was also noted as well as a description of the material sampled.

The 20 - 25 kgm sample was put through the 3 stage concentration process. After weighing the material was fed through a 7.5 inch Knelson concentrator. The Knelson concentrator is essentially a high speed centrifuge rotating at 400 rpm generating 60 g's of force. Before concentrating the feed is first wet screened through a 6mm vibrating screen. The coarse fraction (+6mm) is weighted, examined for its pebble litholigies and is then dumped. The -6mm fraction enters the 7.5 inch diameter centrifuge as a gravel slurry. The centrifuge is a ribbed cone which traps the heavy minerals in the ribs and displaces the lighter material. The replacement of the light minerals by the heavy minerals in the ribs in enhanced by injecting water through a series of perforations in the cone wall thus fluidizing the material. This process results in a concentrate of approximately 2.5 kg.

The 2,5 kg of concentrate is fed through a 2mm screen. The fine fraction then enters a second small Knelson concentrator with a 3 inch diameter bowl. Working on the same principle as the larger concentrator this small unit produces a heavy mineral concentrate of approximately 200 gms. Both the coarse fraction (2-6mm) and the lights from this concentrator are retained for possible examination at a later date.

The 200 gm of heavy minerals then enters the third stage of the concentration process. The material is hand panned down to a maximum of 50 grams. The 50 gm limitation is based on the size of the largest vial that can be used in the neutron activation analysis. In actual fact the sample is panned down to whatever size is necessary to determine if gold grains are present. If gold grains are identified they are counted and examined with a panning scope to determine their size and shape. At the same time estimates of other heavy mineral (pyrite, garnet, magnetite) and their percentages are made.

After the panning is complete the samples are dried and tested with a UV lamp for fluorescent minerals and a gamma ray spectrometer for radiation. The samples were then placed in plastic vials and sent to Activation Laboratories Ltd. for instrumental neutron activation analysis (INAA).

INAA is an analytical technique which is dependent on measuring primarily gamma radiation which is emitted by the radioactive isotopes produced by irradiating samples in a nuclear reactor. Each element which is activated will emit a "fingerprint" of gamma radiation which can be measured and quantified. The samples were analyzed for 34 elements ("Au +33") as listed below.


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detectionelement limit

Au 5 . ppbBa 200. ppmCo 5 . ppmFe 0.02 %Ir 40. ppbNi 200. ppmSc 0.1 ppmTa 1 . ppmW 4 . ppmCe 3 . ppmEu 0.2 ppmLu 0.1 ppm

The "character samples"

detection detectionelement limit element limit

Ag 5 . ppmBr 5. ppmCr 10. ppmHf 1. ppmMo 20. ppmRb 50. ppmSe 20. ppmTh 0.5 ppmZn 200. ppmNd 10. ppmTb 2 . ppm

, collected in a separatedried and sent to Bondar-Clegg for analysis of afollows:

element detectiongold 5 ppbarsenic 1 ppmantimony 0.2 ppmcopper 1 ppmzinc 1 ppmsilver 0.2 ppmlead 2 ppm

limit extractionaqua regia

HC1-HN0 3 {3.1)HC1-HN0 3 {3.1)HC1-HN0 3 (3.1)HC1-HN0 3 (3.1)

As 2 . ppmCa 1. %Cs 2 . ppmHg 5 . ppmNa 500 . ppmSb 0.2 ppmSr 0.2 %U 0.5 ppmLa 1 . ppmSm 0.1 ppmYb 0.2 ppm

soil envelope, were7 element package as

methodFA-AA, 30 gm wgtneutron activationneutron activationatomic absorptionatomic absorptionatomic absorptionatomic absorption

(c) Analysis of Results

All the collecting, processing, laboratory and assay results were compiled on a computer spreadsheet program. The results are shown on Tables 1, 3, 5 and 7.

In order to evaluate the various gold results (grain counts and size, concentrate assay, character sample assay) the data was subjected to various procedures. Initially the gold assay of the heavy mineral concentrate (HMC) in ppb and its mass were used to determine the actual amount of gold in the sample. This is shown in the "concentrate assays" portion of the tables in the "Au mgn" column. These numbers are the actual weight of gold in the sample measured in micrograms. The micrograms of gold and the number of gold grains are then "normalized. Since obviously the weight of the gold and the number of gold grains in a sample will depend on the original sample weight it becomes necessary to "normalize" your grain counts and gold weight to a standard original sample size. The sample size selected was 20 kg of -6mm material. Since the +6mm material was screened off and weighted before concentration this is an easy calculation. The normalized gold grains and micrograms are shown in the two columns to the left of the "concentrate assay" section on the tables.


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A final procedure was required to somehow develop a "gold rating" for each sample which would involve the normalized grain count and microgram data along with the gold assay of the character sample. This "gold rating" column on the right hand side of the tables is an attempt to do this. The gold rating is an abstract number which obtains 60-70% of its value from the concentrate assay, 25-30% from the grain count and 5-10% from the character sample assay.

The gold rating was obtained as follows:

<.05 mm .05 -.1 mm .1 -.2 mm .2 -.3 mm .3 -,4mmgold rating = gold grains + gold grains + gold grains + gold grains t gold grains

3 2 1 0.5 0.25

+.4-.5mm >.5 mm normalized microgms of gold character sample gold grains + gold grains x gold grains + in concentrate + gold assay

0.1 0.05 actual gold 5 35grains

V SHEBANDOWAN AREA

(a) Geology and Mineral Occurrences (Fig.2)

The Shebandowan greenstone belt, stretching 105 km west from Thunder Bay (Figs. 1,2), is located within the Wawa Subprovince of the Superior Province. It is predominantly underlain by metavolcanic rocks, which have been divided into two broadly contrasting age groups: (1) older metavolcanic suites with lesser metasedimentary intercalations, thought to be older than 2.7 billion years; and (2) younger metavolcanic assemblages associated with a large metasedimentary package, both thought to be younger than 2.7 billion years, (Chorlton, 1987). The younger group, which lies unconformably on the old metavolcanic rocks and appears representative of a different depositional environment, is referred to as Timiskaming- type rocks.

The older metavolcanic terrane can be divided into three main associations: (1) massive mafic flows which locally include ultramafic flows and iron formation; (2) mafic to intermediate pillow lavas and pillow breccia with minor iron formation and interlayered metasediments, associated locally with pyroclastics; and (3) felsic volcanic complexes, including abundant pyroclastic rocks and subvolcanic, intrusive to extrusive, rhyolite domes and porphyries.

Several belts of alluvial to fluviatile sedimentary and associated calc-alkaline to alkaline volcanic rocks, Timiskaming-type sequences, unconformably overlie the older succession. The volcanic rocks include nonmarine flow and pyroclastic rocks, consisting largely of hornblende and plagioclase-phypric basalt, andesite and dacite. These rocks are extensively exposed in the eastern half of the Shebandowan greenstone belt where a "Timiskaming-type" volcanic centre has been identified.

Proterozoic lOb diabase 7 sediments

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QUETICO PROJECT

Shebandowan Area


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The earliest intrusive rocks, which include diabase, diorite and ultramafic intrusions, are considered broadly coeval with the older volcanics. Later intrusions include quartz diorite and feldspar or quartz feldspar porphyries. The younger felsic intrusions are more potassic and consist of granite and quartz syenite.

The Shebandowan rocks are deformed along numerous, northeasterly to easterly trending, now carbonatized and sericitized shear zones with an initial sinistral shear sense, and then further deformed by more easterly to southeasterly trending minor fault and shear zones (Chorlton, 1987). The carbonatization may have continued from the earlier shear regime and was followed by the introduction of quartz in multiple veins and stockworks which carry most of the gold values in the area.

Schneiders and Dutka (1988) recognized two distinct environments of gold mineralization in the Shebandowan area:

Type 1) Shebandowan Stock-Contact Zone Type: Gold mineralization occurs in quartz carbonate veins in shear zones, related to the Shebandowan Stock. The gold mineralization appears to be directly related to areas affected by two deformational periods. Examples include the Band-Ore Prospect, Frank West Prospect, Hayne's Shebandowan Occurrence, Lobanor Occurrence, Calvert Occurrence and Ourgold Occurrence.

Type 2) Chert-Stratabound Type: Gold mineralization occurs in a chert-chert breccia unit, with possible syngenetic implications and/or epigenetic concentration during dynamic metamorphism and/or deformation. Examples include the Oawson Road Lots Occurrence, Birch Bay Occurrence, Mattawin Occurrence and Kasper Occurrence.

The area has a long history of mineral exploration. One of the earliest gold mines in NW Ontario, the Ardeen (Huronian, Moss, Kerry) Mine was discovered in the southwestern arm of the belt in 1870 (115 on Fig. 2) and produced 29, 629 ounces of gold in 1932-36. Auriferous quartz veins are sited along northeast trending shear zones. The North Coldstream Mine, on the east side of Burchell Lake (15 on Fig. 2) dates back to 1872 but had the bulk of its production in 1960-67. Disseminated and stringer chalcopyrite hosted by a massive silicious lense produced approximately 2.5 million tons of 2.0% Cu and 0.012 oz Au/ton. The Shebandowan nickel-copper Mine is on the south shore of Shebandowan Lake (SW corner of Hagey Twp.) and was discovered in 1913. It has been in semi-continuous production since 1972 at a rate of 2000 tpd. Nickel-copper sulphides (massive, breccia, stringers) are hosted by an ultramafic unit which may be of intrusive or extrusive origin.


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Like most gold areas the Shebandowan greenstone belt was extensively explored in the 1980's. Two gold occurrences continue to be of particular interest as they both have a large tonnage low grade gold potential. The Stewart property in the north central portion of Conmee Twp., and the Snodgrass prospect in the western part of the belt (4 km east of Ardeen Mine) continue to attract special attention. At the Stewart property gold and minor copper values are associated with breccia on a contact aureole of an alkalic stock. At the Snodgrass prospect gold mineralization is in albitized shear zones and fractures in an altered diorite stock.

For a complete listing of mineral occurrences in the area see the 50,000 scale data maps.

(b) Fieldwork (Fig. 3 to 11)

Till sampling in the Shebandowan greenstone belt was mainly carried out on the south (down-ice) side. A total of 199 samples were collected with a large majority being taken along logging or other access roads in the area. Sample spacing was normally 1 km but preference was given to areas with intermittent outcrops where drift cover was thin. The bulk of the samples were collected by truck with a minor proportion by ATV.

(c) Results (Table 1)

A total of 199 bulk till samples were collected in the Shebandowan area with an average weight of 25.7 kgm. The majority of the tills were taken on the south (down-ice) side of the central part of the greenstone belt from Kaministikwa to Greenwater Lake (Fig. 2). Overall pebble counts of the coarse +6mm fractions of the tills indicate the source lithologies of the drift is 50% felsic intrusives, 40% metavolcanic and 10% of metasedimentary origin.

Gold counts in the 199 samples totalled 500 grains for an average of 2.5 grains per sample. Approximately 90% of these grains were less than 0.2 mm in diameter. Five grains were panned in the 0.4 - 0.5 mm range, the largest particles seen in the area. The highest count in a sample was 13 colours in GL 43 from the Greenwater area.

The percentage of magnetite, pyrite and garnet in the concentrates varied considerably with maximums of 95, 30 and 20% respectively. As all the samples were taken from shovel dug pits, within 1 metre of surface, most of the sulphide minerals have been oxidized. The presence of copper (chalcopyrite or native copper) was noted in 2 concentrates. Lamping with a UV light indicated minor scheelite and zircon. Spectrometer readings gave only background radiation levels.

TABLE 2 SHEBANDOVAN ANOMALIES

Normalized ValuesSampleNo.

MG 53MG 55MG 56MG 58GB 45GB 46GB 48GL 9

NTSLocation

52B/0952B/0952B/0952B/0952B/0952B/0952B/0952B/09

no. of samplesminimummaximum

meanstandard dev.

anomalous threshold(mean + 2 std.dev.)

GoldGrains

221155

16114

16

1990

22339

GoldMicrograms

84.164.0

216.938.961.530.618.534.0

1990.0

216.99.8

19.047.8

CharacterSampleAu ppb

747

5936---3

1843

886

1027

GoldRating

2417662221181717

1990

6646

16

Notes

all samples located in Greenwater claim block (Pig. 11)


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Gold assays In the concentrates reached a maximum of 5,250 ppb Au. The mean value was 288 ppb Au. Converting the assays to the weight of gold (mlcrograms) In the sample and normalizing the value to a standard sample weight results in an average of 9.8 microgms of gold per sample with the maximum value of 216.9 micrograms.

Several elements in the 34 element assay package for the concentrates were below detection levels. In particular all the silver, bromine, mercury, iridium, molybdenum and strontium values were below the detection limits. No in depth analysis or correlation of the concentrate assay results was carried out, however the number of samples, minimum values, maximum values, mean, standard deviation, variance and an anomalous threshold (mean + 2 standard deviations) for each element is given at the bottom of Table 1. Nor correlation of high gold values with other elements is obvious.

Most of the sample sites had character samples taken as well as the bulk tills. In all 184 character samples were collected. Four samples had gold values greater than 50 ppb. A minor correlation of these gold values with zinc is noted. No other elemental associations with the better gold values was detected.

Gold ratings, as outlined in Section II, have been determined for each sample. The mean rating for the Shebandowan area is 4 and the anomalous threshold is set at 16. Eight samples exceed the threshold, with a maximum gold rating of 66. The samples are listed in Table 2. All eight tills are located in Begin Twp. southeast of Greenwater Lake. A block of 40 claims was staked to cover the probable source area for these anomalous tills. This activity is discussed separately in a following section (Greenwater Block). It is interesting to note that GL43 with the highest gold grain counts of the Shebandowan area does not have an anomalous assay value. One must conclude that in this till not all the particles counted were actually gold. However a more general comparison of the gold grain counts and the gold assay values indicates a reasonable similarity in determining anomalies.

(d) Tinto Block (Figs. 8, 9)

During the course of the 1990 reconnaissance program in the Shebandowan belt two claim groups were staked because of anomalous gold assay results and favourable geology. In the Tinto Lake area of Lamport Twp. 6 km south of Inco's Shebandowan Mine 32 claims were staked (Fig. 8). The Tinto block was acquired because of a favourable mafic metavolcanic sequence with intercalated iron formation and mafic intrusives at the west end of the Mattawin Iron Range. Northeast directed faults have provided a plumbing system for possible injection of gold.


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Figure 8

MINGOLD RESOURCES INC.EASTERN DISTRICT THUNDER 8AY OFFICE

SCALE'

0

TINTO LAKE CLAIMS

(claim map G-668)

i________ miles

MTC'

DRAWN

Nov./90


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The property consists of 32 claims staked in July of 1990 within the central portion of Lamport Twp. and are located on claim map G-668, of the Thunder Bay Mining Division. The claims are numbered: 1164351 to 1164382 inclusive (Fig. 8). The claims are currently held in the name of Mingold Resources Inc. (license No. T-4617) located at P.O. Box 28, Toronto Dominion Centre, Toronto, Ontario M5K 1B8.

A one week geological mapping and basal till sampling program was completed over the claim block. Mapping and sampling was mainly confined to the shorelines of Dakota and Tinto Lakes. The rocks consists of felsic to mafic volcanics along with clastic sediments and magnetite iron formation in the northerly part of the claims. In the southern portion of the claim block local small granite plugs and gabbroic intrusives lie, within the volcanics. No significant alteration or mineralization was observed during the mapping program. A total of 29 bulk till samples were collected on the claim block with some additional sampling outside the claims (Pig. 9).

During the mapping program no significant mineralization or alteration was observed and there was a total absence of sulphidation of the magnetite iron formation. None of the follow-up till sampling produced anomalous results. Since both the gold grain particle counts and gold assays obtained from the till samples collected on the Tinto Lake block were negative the claims should be allowed to lapse.

(e) Greenwater Block (Figs. 10, 11)

The Greenwater Lake claim group was staked in response to anomalous gold values in reconnaissance bulk till samples along forestry roads. Samples MG53 to 58 gave anomalous grain counts and gold assays in the regional survey. To confirm the original results GB 38 to 52 were collected as an initial follow-up. The anomalies were substantiated and the claim group was acquired.

The claim block in the south central part of Begin Twp. touching the southeast arm of Greenwater Lake. Access to the area is by Canadian Pacific Forest Products logging roads (Hough Lake and Otto Lake Roads). Good access to most parts of the claims within the block is provided by a network of trails and skiddo roads.

The property consists of 40 claims staked in the summer of 1990 within the south centre portion of Begin Twp. and are located on claim map G- 643, Thunder Bay Mining Division. The claims are numbered: 1164301 to 1164340 inclusive (Fig. 10). The claims are currently held in the name of Mingold Resources Inc. (license No. T-4617) located at P.O. Box 28, Toronto Dominion Centre, Toronto, Ontario M5K 1B8.

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1164302

"64314

, ,1164307

! ~ !v{ 1164312 { 1(64311 (1164310 I 1164309 j 11643—h--f——f--f---H ! "I ' i !

164315 '|I643I6 JH643I7 11164318 | 0643!9 i »6432C

i ' ' *î i1164328 "'64327 I D64326 i *4325 \ «6432'i H6432' B64322 | »64323

1164329 064330 1164331

/

Figure 10

MINGOLD RESOURCES INC.EASTERN DISTRICT THUNDER BAY OFFICE

GREENWATER LAKE CLAIMS

(claim map G-643)

. OATC<Nov./90

milesOMAWN BY'

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A one week program of geological mapping and basal till sampling was completed on this 40 claim block. The mapping and sampling was concentrated along logging and skidder roads. The bedrock geology is dominated by mafic volcanic rocks along with minor felsic tuffaceous rocks to the south. The volcanics are intruded by lenticular gabbroic sills. The northeast trending volcanic-gabbro contacts are marked by sheared choritic contact zones. Granitic intrusives occupy the extreme southeast corner of the claim block. A total of 76 bulk till samples were collected up-ice and in the claim area with 37 of these within the claims. A few of the samples produced anomalous results bur neither an up-ice cut-off nor a well defined dispersion train was outlined with the limited work. For processing data, gold grain counts and assay results see Table 1. The more westerly tills came from sandy-gravelly material which does not appear to be a good basal till. Grain size analysis of this material is required.

It is recommended that (1) detailed till sampling be carried in close proximity to the anomalous tills and (2) a brief study be undertaken of the glacial drift in the general area to determine its relationship to the anomalous values.

VI ATIKOKAN AREA

(a) Geology and Mineral Occurrences (Fig. 12)

Atikokan is located approximately 200 km west of Thunder Bay. The area is underlain by Archean rocks of the Superior Province, including parts of the Wabigoon and Quetico subprovinces. The east trending Quetico Fault marks the boundary between the subprovinces.

The Wabigoon Subprovince, north of the fault, is composed of narrow metavolcanic belts and granitic batholiths. The metavolcanics are mainly metamorphosed varieties of mafic to intermediate flows interdigitated with felsic volcanic rocks and minor sedimentary units. The Marmion Lake Batholith in the east-central part of the study area is a complex of gneissic trondhjemites and monzonites. The Dashwa Lake Batholith in the western half of the area is composed of mainly biotite and hornblende granite, quartz monzonite, quartz diorite and granite gneiss. Minor granodiorite and trondhjemite occur in the contact zone between the metavolcanic belts and batholiths.

South of the Quetico Fault, the dominant metasediments form a belt which is contiguous across the southern part of the study area. The rocks consist of metamorphosed wackes, argillites and carbonaceous sediments. Small ultramafic sills and granitic stocks occur throughout the metasedimentary belt.

Proterozolc I Ob diabase 7 sediments

/ ffi ( 3^7 . l:

~' r j : '

3 metasediments2 acid volcanics1 basic volcanics

MINGOLD RESOURCES INC.EASTERN DISTRICT THUNDER BAY OfTfCE/

QUETICO PROJECT

Atikokan Area


- 18 -

The Quetlco Fault is the dominant regional structure, it extends easterly across the area, marked by prominent lineaments and bounded by zones of schistose to mylonitic rocks. Movement along the fault was primarily right-lateral horizontal displacement. East of Perch Lake, several lineaments trend toward the northeast from the Quetico Fault. Some of these lineaments can be traced up to a distances of 80 km.

Gold occurrences are common throughout the area and these general types of mineralization have been recognized (Wilkinson, 1982):

i) Marmion Lake Batholith Type - quartz veins within shear zonesassociated with northeast - trending lineaments in the batholith;

ii) Contact Zone Type - quartz-carbonate veins within narrow shearzones located at or near the contacts of batholiths andmetavolcanic belts; and

iii) Metavolcanic-Hosted, ' Stratabound Type - concordant lenses of chert or carbonate with associated quartz-carbonate veins, hosted by metavolcanics.

Gold, in all three styles of mineralization, is concentrated in quartz and quartz-carbonate veins with subsidiary silver, copper, lead and zinc. The process of gold enrichment into the veins is multi-stage and is a combination of some or all of the following:

. deposition or emplacement of the host granitic rock into thecountry rock;

. alteration of the host granitic rock by hydrothermal solutionsand formation of the veins; and

. hydrothermal mobilization of gold and its ultimate deposition inthe veins.

The first gold discoveries in the Atikokan area were in the 1890's but very little production has actually taken place. The Sapawa Mine, 17 km east of Atikokan (#6 on Fig.12) produced 4,500 oz of gold in 1964- 66. Gold values are in quartz veins hosted by felsic intrusions of the Marmion Lake Batholith and minor mafic volcanic units. Minor production has also come from the Sawbill, Harold Lake, Hammond Reef, Elizabeth and Sunbeam properties.

For a complete listing of mineral occurrences in the area see the pertinent 50,000 scale data maps.

(b) Fieldwork (Figs. 13 to 18)

Sample collection in the Atikokan area was accomplished by both road and lake access. A 50 km stretch of Highway 11 from Eva Lake west to Banning was sampled at 1 km intervals. This gave good coverage 2-8 km down-ice of the Quetico Fault. Sampling by boat was carried out on Marmion, Crooked Pine, Crayfish and Baril Lakes. The western part of the Upsala greenstone belt was also sampled as part of this area. Access is by Highway 623 which leaves Highway 11 at the Sapawe corner.


- 19 -


A total of 246 bulk till samples were collected In the Atikokan area with an average weight of 24.4 kgm. The coarse (+6mm) fraction averaged 6.0 kgm. A general outline of the area sampled is shown on Figure 12. Pebble counts of the coarse fraction indicate the drift lithologies are approximately 40% felsic intrusives, 35% metasedimentary and 25% metavolcanics.

Gold counts in the 246 samples totalled 156 grains for an average of 0.6 grains per sample. This is a considerable reduction in gold particles as compared to the Shebandowan area. The majority of the Atikokan grains were in the 0.05 - 0.3 mm range. Two samples from the Upsala greenstone belt has large gold grains in the 0.5 mm range. The sample with the most gold .grains was A87 with 13 counts.

The percentage of magnetite, pyrite and garnet in the concentrates varied considerably with maximums of 80, 20 and 45% respectively. Minor sphalerite was noted in two of the concentrates from the Upsala greenstone belt but, as elsewhere, samples were taken from oxidized drift and few sulphide grains could be expected. UV lamping and spectrometer readings indicated nominal or background levels.

Gold assays in the concentrates reached a maximum of 3250 ppb Au. The mean gold value was 242 ppb, only slightly below the Shebandowan mean value. The normalized gold values for a 20 kgm standard sample size averaged 9.7 micrograms of gold. The maximum was 148.1 micrograms.

As in Shebandowan there is no obvious correlation of the better gold values with any other element in the 34 element package. In fact for half the elements the majority of the individual values are below the INAA detection limits making that portion of the data meaningless. A statistical summary for each element is shown at the bottom of Table 3.

Character samples were collected along with the bulk material to be concentrated. Only two of the character samples has gold values greater than 50 ppb Au and neither of these had corresponding elevated gold in the heavy mineral concentrate.

Gold ratings in the Atikokan area have a mean value of 3 and an anomalous threshold of 13. The maximum rating was 41. Twelve samples are considered anomalous.

In NTS area 52B/11 (Fig. 13) sample A 58 has a rating of 16 based largely on its concentrate assay. Its grain count, normalized at 2, is low but the particles are moderately large. There is no correlation with other elements except for slightly elevated copper in the character sample. This sample was taken on Highway 11 approximately 5.5 km down-ice of gold showings on the north shore of Sapawe Lake. No follow-up was undertaken.

TABLE 4 ATIKQKAH ANOMALIES


A 58ARE 7A 81A 113A 101A 103A 104A 144A 147A 199A 245A 259

no.

NTSLocation

52B/1152B/1252B/1352B/1352B/1452B/1452B/1452B/1452B/1452B/1452G/0352G/03

of samplesminimummaximum

meanstandard dev.

anomalous(mean + 2

thresholdstd.dev. )

GoldGrains

314325000

1022

2460

13114

GoldMicrograms

62.2106.376.162.0

148.179.863.3125.765.721.444.036.9

2460.0

148.19.718.446.6


383

226735

19333

2460

8458

20

GoldRating

162128254122132514132925

2460

4135

13

Notes

on til (Arami L.) down-ice of Sapawe L.on Oil west of AtikokanFinlayson L. (Fin-Lan Copper)west shore Marmion L. (80 degree)Lower Seine Bay on Marmion L.Lower Seine Bay on Marmion L.Lower Seine Bay on Marmion L.Reserve Island areaReserve Island areaMagnetic L. areaeast Red Paint L. areaeast Red Paint L. area N3

O


- 21 -

Sample ARE 7 was also collected on Highway 11 eight km west of the Atikokan turn-off (Fig. 14). No known gold occurrences are in the area but the Quetico Fault is 4 km up-ice. Only one gold grain was observed but it is in the 0.4 - 0.5 mm range. The HMC assayed 3100 ppb Au.

Samples A 81 and A 113 were taken north of Atikokan on ME trending splays or breaks on Finlayson and Marmion Lakes respectively (Fig. 15). Both locations are in the vicinity of or directly down-ice of known gold showings. Sample A 81 has a rating of 28 with 3 moderately large gold grains and an anomalous gold assay in the concentrate. It is located in the area of the Fin-lan copper showing and 3 km down- ice of the Golden Twin gold prospect. Sample A 113 is a short distance to the southeast on the west shore of Marmion Lake. Its rating of 25 is due to a high gold value in the HHC and 2 large angular gold grains. The character sample is slightly anomalous in gold as well. The sample site is 1 km down-ice of the "80 degree" occurrence. As with the remainder of the Atikokan anomalies no follow-up has been undertaken.

Samples A 101, A 103 and A 104 were taken by boat in the eastern portion of Marmion Lake in the NV corner of McCaul Twp. All three samples have anomalous gold in their HMC, especially A 101 with 148.1 micrograms, the highest value of the Atikokan area. The gold counts tend to be low but somewhat coarse. Sample A 104 had no observed gold. The only known gold occurrence which could provide a source for these tills are 10 kms up-ice (Fig. 16), however a major splay off the Quetico structure passes through the area providing a focus for further exploration.

Samples A 144 and A 147 were collected in the Reserve Island area of the Seine River in the SW corner of Ramsay Wright Twp. (Fig. 16). Neither sample had observed grain counts but they have good to excellent gold values in the HMC. Sample A 147 also has elevated gold in its character sample. Samples A144 is 5 km down-ice of the Pittigrew occurrence. A 147 is down-ice of the Sunbeam and A1308 showings. The Reserve Island gold showing is also in the near vicinity.

Sample A 199 was collected on the north shore of Magnetic Lake in the west central area of Trottier Twp. (Fig. 16). The main Quetico Fault passes through the lake. The White Lily gold showing is 1.5 km north of the sample site. Seven gold grains were seen in the 0.1 to 0.3 mm range, four of which were delicate to angular in shape indicating a near source. The coarse fraction was 30% quartz vein material. The HMC assay was elevated but it is not considered an anomalous value. It's high rating is predominantly due to its grain counts and their size.

- 22 -

Samples A245 and 259 were collected on roads in the Upsala greenstone belt In NTS area 520/03 (Figures 12 and 18). A 245 Is located west of Richardson Lake along the E-w trending granite/greenstone contact.

Sample A259 is situated between Gargoyle and Hematite Lakes. The location of mineral occurrences in the area has not been researched. Both samples have only 2 grain counts but in each case one grain is very large. Sample A245 has a 0.6 x 0.3 mm gold grain with an anomalous assay of 1370 ppb gold. A 259 has a 0.5 x 0.3 mm grain and 1000 ppb Au in its HMC. There are no anomalous values in other elements.

No follow-up of the Atikokan anomalies has been undertaken.

VII MINE CENTRE

(a) Geology and Mineral Occurrences (Fig.19)

The rocks of the Mine Centre - Fort Frances area occur within the Archean Superior Province in a fault-bounded wedge between two subprovinces, the Vabigoon granite-greenstone terrain to the north and the Quetico metasedimentary terrain to the south (Poulsen, 1984). The Quetico and Seine River - Rainy Lake Faults define this dextral wrench zone which displays distinctive stratigraphic, structural and metamorphic relationships.

The structure of the Wabigoon granite-greenstone terrain is dominated by domal features of variable size. The largest of these, such as the Rainy Lake Complex and Irene-Eltrut Lakes Complex, are greater than 50 km in diameter and are composed of smaller gneissic domes, central batholiths and marginal crescentic granitoid intrusions. Supracrustal metavolcanic and metasedimentary rocks now occupy the margins of the gneissic domes. Metavolcanic lithologies dominate and comprise metabasalt flows with local accumulations of flows, and pyroclastic and epiclastic rocks of intermediate to felsic composition. Metasedimentary rocks such as conglomerate, wacke, mudstone and iron formations form units within the volcanic sequences.

The structure of the Quetico Subprovlnce contrasts with the of the Wabigoon (Poulsen, 1984). It is characterized by a consistent sequence of metasedimentary units sub-parallel with the Seine River- Rainy Lake Fault. Near the northern boundary, low grade metasedimentary rocks of the Quetico subprovince dip steeply. Southward, the metasedimentary rocks become migmatitic and primary structures and cleavage are obscured. Major antiforms are commonly cored by massive granitoid bodies of irregular shapes. The metasedimentary biotite schists are metamorphosed to assemblages indicative of a southward increase in metamorphic grade.

Proterozoic 1C diabase

4 :laHt;c sedin-ent;' ciastic3 alkalir nafir vole2 felsic volcanics1 mafic volcanics

MINGOLD RESOURCES INC.EASTERN 0/STR/CT THUNCCR BAY OFFICE

QUETICO PROJECT

Mine Centre AreaiJ&j*""^^^^ ——irn> * ii _-——T——-—&~~ -~—-~r—"_V__.-Sx'-"" '"

- 24 -

The Mine Centre district was the site of Intensive prospecting for gold in the 1890's and again in the 1940's. Total production from the area is at 21,000 ounces of gold with the bulk from the Golden Star, Poley, Olive and Cone Mines. The deposits are concentrated along the subprovince boundaries and are related spatially to the major faults and their splays.

Quartz vein mineralization is of two types. Molybdenite, with pyrite and local chalcopyrite, occurs in quartz stockworks and extensional veins within granodioritic intrusions near contacts with metasedimentary country rocks. In contrast gold, along with carbonates and base metal sulphides, occurs in lenticular quartz veins associated with shear zones and regional cleavage. Gold-bearing veins occur in a variety of rock types and are restricted to zones of greenschist facies metamorphism, (Poulsen, 1984).

Low grade iron-formations are also common in the region and tend to be concentrated near the subprovince boundaries. Several significant prospects containing base metals also have been discovered. Two broad types are present: zinc-copper mineralization occurs at specific horizons within metavolcanic successions and copper-nickel mineralization is associated with mafic and ultramafic rocks, particularly intrusions. Although some of these prospects have been extensively developed, very limited base metal production has been reported from this region.

Clearly there is a strong spatial correlation between known mineralization and the subprovince boundary (Poulsen, 1984). Laminated gold-bearing quartz veins occur in ductile shear zones and as dilation of the regionally developed cleavage. These structures are related kinematically to large transcurrent faults in the region. Poulsen (1983) considered the gold mineralization to be entirely epigenetic and related to seismic pumping of fluids during faulting. A similar spatial relationship between gold and large fault zones exists throughout the study area and is the basis of the reconnaissance program.

The Mine Centre sampling also included tills from the Manitou Stretch 40 km north of the Quetico Fault. Like the Quetico structure the Manitou Stretch is an east trending deformation zone in the Vabigoon subprovince. It lies within the Manitou Lakes greenstone belt near its the junction with the Pipestone-Cameron Lake greenstone belt.

All bedrock in the area is Archean consisting primarily of steeply dipping folded strata of low-grade metamorphosed and deformed mafic volcanic rocks and lesser intermediate and felsic volcanic rocks and associated intrusives subvolcanic stocks sheets, and dikes. The metavolcanics are intruded by and bounded by large granitic masses of intermediate to felsic composition, and by minor late lamprophyre and gabbro dikes.

- 25 -

The area is approximately bisected by an east-trending zone of cataclastic deformation, the Manitou Stretch-Pipestone Lake Fault, which is of regional dimensions and has been traced from Lake of the Woods in the west to Upper Manitou Lake in the east.

Gold was mined at the old Straw Lake Beach mine in the late 1930's (33,7000 ounces) and several gold occurrences are located along the main deformation zone.

(b) FieIdwork (Figs. 20 to 27)

Till sampling in the Mine Centre - Manitou Stretch was carried out by road and lake access. Approximately 60% of the tills were taken along Highway 11 as well as recreational access and forestry roads. Boat work was done on Rainy Lake,and the Manitou Stretch.


A total of 214 reconnaissance bulk tills were collected in the Mine Centre area with an average weight of 233 kilograms. The coarse fraction averaged 6.9 kgms. A general outline of the area is shown on Figure 19. Pebble counts of the coarse fractions indicate the overall drift lithologies are approximately equal proportions of felsic intrusives, metavolcanics and metasediments.

Gold counts in the 214 samples total 582 grains for an average of 2.7 grains per sample. This is comparable to the Shebandowan area average grain count (2.5) and four times the Atikokan average (0.6). Almost 98% of the grains were 0.03 mm or less. Three samples had single grains larger than .5 mm in diameter. Two samples, both from the same site on Esox Lake, had the area high grain counts of 42 and 43 gold particles.

The percentage of magnetite, pyrite and garnet in the HMC varied considerably with maximum of 70, 25 and 90% respectively. Seven samples noted chalcopyrite grains. UV lamping and spectrometer readings were at background levels with minor scheelite and zircon observed.

Gold assays in the concentrates reached a maximum of 18,200 ppb Au. The mean gold value was 730 ppb gold which is almost three times the means for the Shebandowan and Atikokan areas. The grain count differences for Mine Centre and Atikokan would suggest that the assay differences is natural for the two areas. The big discrepancy between Mine Centre and Shebandowan is not expected and most likely reflects modification in the method of producing the HMC in the two areas. Normalized gold values for a 2JLkgm standard sample size averaged 28.3 micrograms of gold, again a significant increase over the Shebandowan and Atikokan areas.

TABLE 6 MINE CENTRE ANOMALIES


M 79MRE26MRL23M 74M 102MCN22MCN63GB124MCN52

no.

NTSLocation

52C/1052C/1052C/1452C/1652F/0252F/0352F/0352F/0352F/03

of samplesminimummaximum

meanstandard dev.

anomalous(mean + 2

thresholdstd.dev. )

GoldGrains

37303

539

527

2140

5336

15

GoldMicrograms

128.3219.5165.7292.3339.1585.4239.4539.1354.8

2140.0

585.428.371.5

171.4


363-

1250--3

2020

4326

3067

GoldRating

5280495869

13651

124116

2140

1369

1844

Notes

west end of Grassy L. west end of Grassy L. Northeast Bay area, Rainy Lake Bennett - MacPherson L. area on Highway 502, Korpi L. area Cedar Narrows, Esox L. area Cedar Narrows, Esox L. area Cedar Narrows, Esox L area Manitou Stretch

Ito


- 27 -

As in the two prior areas there is no correlation of the better gold values in either the HMC or in the character sample with the other assayed elements.

In the character sample data set only two samples had gold assays above 20 ppb. Gold ratings in the Mine Centre area have a mean value of 9 and an anomalous threshold of 44. Nine samples exceeded the threshold and are considered anomalous.

In NTS area 52C/10 (Fig. 21) two samples collected by boat in the Grassy Lake area are quite significant in gold values. Sample H79 on the south shore of the lake had only three gold grains but one was >0.5mm in diameter. The HMC assay 2610 ppb Au and its normalized contained gold was 128.3 microgzams. To the west only 0.5 km sample MRE 26 had 4 grains (normalized to 7) including a 0.6 mm x 0.4mm particle, the largest obtained in the Mine Centre area. The smaller grains were generally angular. The HMC assayed 3600 ppb Au and normalizes to 219.5 micrograms of gold. There are no known gold occurrences in the vicinity or close up-ice although the main Shoal Lake showings (eg. Cone, Foley, Mackenzie Gray) are 10 km to the BNE. The Seine River Indian Reserve 23B lies on the north shore of Grassy Lake directly up-ice. The Seine River Fault passes through Grassy Lake.

Sample MRL 23 was taken on Baseline Bay in the southeast corner of NTS area 52C/14. The sample was collected by boat but the location is only 1 km east of Highway 502. Three large gold grains, in the 0.2 - 0.5 mm range, are accompanied by anomalous gold in the HMC assay.

The HMC contains 165.7 micrograms of gold. There are no known gold occurrences in the area but the main Quetico Fault passes through Crowrock Inlet 2 km to the north.

In NTS 52C/16 (Fig. 25) sample M74 is located north of the Bennett Lake - McPherson Lake area. There are numerous gold occurrences (eg. Independence, Cedar Lake) reported down-ice of the location but no showings to the northeast. No gold grains were observed in the panning although chalcopyrite was seen. The nearby showings have copper and gold values. The sample assayed 12,500 ppb gold for a normalized value of 292.3 micrograms of gold. The HMC also had elevated tungsten at 150 ppm V.

Along Highway 502 in NTS area 52F/2 (Fig. 26) sample M 102 was collected east of Arms Lake. Only one gold grain was panned (normalized to 3) but the concentrate assay normalized to 339 micrograms giving the sample a rating of 69. Follow-up sampling was carried out including a duplicate from the same pit. This sample, GB 131, had a rating of 27 which is below the anomaly threshold but its HMC had 3,090 ppb gold. Sample GB 132 only 0.5 km to the north had a rating of 37 and 5,200 ppb in its concentrate. Regional mapping indicates that a northwest trending granite/greenstone contact passes between the highway and Arms Lake.


- 28 -

In the Manltou Stretch area (NTS 52F/03, Fig. 27) two locations exceed the anomalous threshold. At Cedar Narrows on the south shore of Esox Lake sample MCN 22 was taken along a logging road. A total of 43 gold grains (37 8 <0.05 mm) were observed with the few coarse particles being quite angular. This indicates a nearby source. The concentrate assayed 12,500 ppb Au and the character sample ran 50 ppb Au. Two follow-up samples were taken from the same shovel pit and nine other tills were taken within 1 km up-ice. The locations are all shown on Fig. 27, either on the main map or the enlarged portion. Samples GB 124 and MCN 63 from the same pit are also anomalous confirming the original result but the area detail is negative. This would suggest a very local bedrock source or else a gold concentration in the drift due to glacial processes.

Also on Fig. 27 sample MCN 52 had a gold rating of 116. This sample was taken by boat along the Manitou Stretch. It had 7 gold grains including one at 0.6 mm x 0.3 mm. The HMC assayed 11/500 ppbû. Numerous gold showings have been discovered along this deformation zone. The old Straw Lake mine is 11 km to the west along the same structure. There are no known showings that can be directly related to MCN 52 although an antimony occurrence is nearby and the Gates Lake gold prospects are 4 km to the northeast.

VIII EMO

(a) Geology and Mineral Occurrences (Fig. 28)

The Emo sampling area extends from Rainy Lake west to Emo and north to include the Burditt - Pipestone Lake system.

The southern portion of the district is the westward extension of the Quetico Fault system described for the Mine Centre area. The Quetico structure crosses Rainy Lake passing just south of Northwest Bay and continues into the Rainy River farming district. Due to extensive glacial cover the fault is masked on surface but geophysical evidence indicates the system continues SSW passing into Minnesota near the town of Rainy River. Major subsidiary faults splay along northwest Bay and to south near Stratton.

This area is underlain by Archean supracrustal, ultramafic, intrusive and granitoid rocks (Johns, 1987). The supracrustal rocks can be divided into two stratigraphic units, a lower mafic unit consisting of massive and pillowed flows overlain by an upper diverse unit comprised of interbedded mafic and intermediate debris flows and pyroclastics. The intermediate to felsic granitoid intrusive rocks can be divided into pre-to syntectonic stocks and batholiths and postectonic stocks.

PrDterozoic 10 diabase

5 chemical sediê^ts clastic sedinients

4 clsstic ssdi'snts

2 felsic volcanics

MINGOLDEASTERN DISTRICT

RESOURCESTHUNDER BAY OFFICE

Ql'ETICO PROJECT

Emo Area


- 30 -

Further north in the Burditt - Pipestone area a major NE trending deformation zone coincides with the chain of lakes. The zone is composed of an Archean metavolcanic assemblage with mixed sequences of massive, porphyritic and pyroclastic mafic volcanics. Felsic to intermediate plutonic rocks intrude the supracrustal units (Blackburn, 1976). Three small felsic stocks within the belt are considered synchronous with the deformation.

At the north end of the till sampling area, south of Kagagi Lake, mafic to intermediate metavolcanics with synchronous ultramafic units form the southern portion of a major northwest trending deformation zone. This structure is called the Pipestone - Cameron Fault and extends from the Manitou Stretch in the east to Lake of the Woods to the west.

Mineral exploration in the'northern portion dates back to the early part of the century. Numerous gold showings are related to the Pipestone-Cameron fault, of which the most well known is the Cameron Lake deposit. These occurrences occur in zones of shearing and carbonate alteration with a close spatial relationship to the deformation. In the Burditt Lake area mineralization found to date consists of chalcopyrite and sphalerite within the mixed felsic to mafic metavolcanics. Further south, in the Emo-Barwick area, copper - nickel sulphides are associated with border phases of an ultramafic intrusion. In the farming district to the west exploration is hindered by the extensive glacial cover but recent till work by the OGS (Bajc, 1988) has indicated areas with significant number of gold grains related to a southwest - directed till package.

(b) Fieldwork Figs. 29 to 31)

Almost all of the till sampling in the Emo area was carried out by truck access. Minor sampling was done by boat (on Burditt Lake) and by all terrain vehicle along power lines and on older roads.

In the north and east areas of the sampling the drift cover is thin and typical of the Superior Province. However to the south and west the drift thickens considerably and the lower southwest directed till is overlain by a clay-rich till with a source to the west. This upper till basically prohibited sampling west of Tait Township.


A total of 164 reconnaissance bulk tills were collected in the Emo area with an average weight of 26.8 kilograms. The coarse fraction averaged 8.5 kgms. A general outline of the sampled area is shown on Figure 28. Pebble counts of the coarse fraction indicate the drift lithologies are approximately 50% metavolcanic, 45% felsic intrusives and 5% metasediments.

TABLE 6 BMP ANOMALIES


P 94FRE 8FDER 9FTRY 8FTRY10FPIP28FPIP40

NTSLocation

52C/1352C/1352F/0452F/0452F/0452F/0452F/04

no. of samplesminimummaximum

meanstandard dev.

anomalous threshold(mean t 2 std.dev.)

GoldGrains

518572

10

1640

3344

12

GoldMicrograms

67.9187.684.6159.883.5

188.3187.6

1640.0

188.322.631.866.2


33

713

1133

1580

2197

2047

GoldRating

28393157346553

1640

659

1028

Notes

Panorama L. area .Panorama L. areaPipestone Rd. area-down-ice of Cameton L. Pipestone Rd. area-down-ice of Gameron L. Pipestone Rd. area-down-ice of Cameron L. Pipestone Rd. area-down-ice of Cameron L. Pipestone-Slender Lakes area

fault fault fault fault

jCO


- 32 -

Gold counts In the 164 samples total 524 grains for an average of 3.2 grains per sample, the highest of the four districts. Only 7% of the grains are greater than 0.3 mm In diameter. Two samples have single gold grains larger than 0.5 nuns. The highest gold grain count in the Emo area was 14 grains from F107 taken at Yoker Lake in the southwest corner of Menary Twp. However this sample had only background gold levels in the HMC and it is assumed that particles were mid-identified as gold. Two follow-up samples in the same vicinity had background levels.

The percentage of magnetite, pyrite and garnet in the HMC varies with maximums of 85, 20 and 60% respectively. Copper, mainly chalcopyrite but perhaps some native copper was seen in 8 samples but there is no relationship with gold assays or grain counts. UV lamping and spectrometer readings were at background levels.

Gold assays in the HMC reached a maximum of 8,680 ppb Au, The mean gold values was 757 ppb gold which is very similar to Mine Centre values and significantly higher than Atikokan and Shebandowan. Normalized gold/values for a 20 kgm standard sample size averages 226 mgms of gold.

There is no correlation between HMC gold assays and assays of other elements in the concentrate. Within the character samples only one of six anomalous gold is also a HMC anomaly. The gold ratings in the Emo area have a mean value of 9 and an anomalous threshold of 28. Seven samples exceeded the threshold and are considered anomalous.

Two of the anomalies are located near Panorama Lake in NTS area 52C/13 (Fig. 30). Sample F94 had 4 grains (normalized to 5) of which 3 are in the 0.3 - 0.4 mm range and are quite angular. Its HMC gold assay although certainly elevated was not considered anomalous. Sample FRE 8 is 3 km to the south of F94. It had only one gold grain but its concentrate assay was .8^68.0 ppb Au, the best of the Emo area. Both of these samples was situated on the west flank of the NE trending greenstone package that parallels the Burditt - Pipestone chain of lakes. Two showings, one gold and one zinc are known in the area but neither could be the source of these anomalous samples. Some follow- up had been undertaken but additional sampling is required.

Four gold anomalies are situated on logging access roads in the Katimlgamak Lake area of NTS 52F/04 (Fig. 31). Sample FDER 9, located north of Derby Lake, had 9 grain counts (normalized to 8). Its HMC assay normalizes to 84.6 micrograms of gold. The character sample is also anomalous in gold with 71 ppb Au. To the north and west samples FTRY 8, 10 and FPIP 40 are located on a NE trending road paralleling the ice direction. Grain counts vary from 2 to 8 colours and include the two large grains mentioned earlier. Sample FTRY 8 had one gold particle 0.8 x 0.3 mm. Its contained gold normalizes to 159.8 micrograms. Sample FPIP 28 had a 0.7 x 0.3 mm grain and 188.8 micrograms of gold. The Katimogamak area is dominated by a sequence of east trending mafic metavolcanic units intercalated with mafic


- 33 -

Intrusives. A number o£ northeast breaks crosscut the volcanlcs. The locations of the mineral occurrences in the vicinity has not been researched but Kakagi Lake to the north has a number of gold prospects related to the NE trending Cameron Lake Deformation Zone (Fig. 28).

In the Manomin River area between Pipestone Lake and Burditt Lake sample FPIP 40 was collected. Six gold grains (normalized to 10) and 187.6 micrograms of gold give the sample a rating of 53. No gold showings are known in the general area but a volcanic/felsic intrusive contact is nearby. Further sampling is required.

IX CONCLUSIONS

The purpose of the bulk till sampling along the Quetlco Fault structure was to help locate and define bedrock gold occurrences in the area. Although in no cases have anomalous grains counts and/or assay values in till been traced back to a definite bedrock source U_...firs.t order anomalies and many more lesser anomalies have been outlined. Some of the anomalous samples have mineral occurrences in the vicinity which may very well be the source of the gold values in the till but this has not been confirmed. Nevertheless from the results to date it can be concluded that this method of using heavy mineral concentrates to search for gold is a viable exploration technique. Obviously follow-up is required on most of the anomalies discussed in this report.

Although time has not permitted an in-depth analysis of the results some conclusions can be drawn from the concentrating and assay data.

(1) There is a general correlation of anomalous gold grain counts and anomalous gold with HMC but it is also obvious that there are instances of missed gold grains and grains mis-identified as gold. For instance, in three of the four areas the samples with the highest grain counts did not assay as gold anomalies. In the future more care should be taken to train and maintain a higher level of competency in the panning.

(2) As an alternative to (1) if it is found that the panning data is too inconsistent and/or time consuming to undertake correctly then the grain counting should not be carried out, at least on the reconnaissance scale, and anomalies would be determined solely by the HMC assays.

(3) There is no apparent correlation between anomalous gold values in the HMC and any of the other elements assayed for in the 34 element INAA package. One reason for this is that a bedrock gold source may have base metal sulphides associated with it but our samples are from shovel dug near-surface pits where most if not all the sulphides would be oxidized and therefore not found in the HMC. If follow-up work were carried out with RC or sonic drilling, even deep backhoe trenching, one may very well find associated or indicator sulphides with anomalous gold.

- 34 -

I

I

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I

I

I

I

I

I

I

I

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I

I

I

(4) The "character sample" data set provides very little useful Information on a reconnaissance scale. Although some elevated gold values are obtained,the results are sporadic and are of marginal use in determining follow-up work. The character samples may contribute when one has a nearby source, in the same way as regular soil or humus geochemistry will define targets, but on a reconnaissance scale it is of little value.

- 35 -

I

I

I

I

I

I

I

I

I

I

I

I

X CERTIFICATE

I" I, Gerald E. Bidwell of the City of Thunder Bay in the Province of Ontario

hereby certify:

1. That I am a geologist employed by Mingold Resources Inc.

1 2. That I am a graduate of the University of Saskatchewan with a Bachelor of Arts and Science (Geology) degree granted in 1967. I have been practising my profession for twenty-two years.

3. I am a fellow of the Geological Association of Canada.

Dated at Thunder Bay, Ontario the 25th day of November 1990.

GeVald E. Bidwell

1111111111111111111

XI REFERENCES

Bajc, A. F.1988:

Berger, B. 1988:

Blackburn, C. 1976:

Chorlton, L.1987:

Cowan, W. R.: 1987:

Edwards, G.R.1983:

Johns, G. W. 1988:

Minning, G. 1988:

1989:

Poulsen, K.H. 1984:

1983:

- 36 -

Gold Grains in Rotosonic Drill Core and Surface Samples (1987 - 1988); Ontario Geological Survey Prel. Map P.3140.

Geology of the Manitou Stretch Area, District of Kenora; in Ontario Geological Survey Miscellaneous Paper 141.

E.Geology of the Off Lake-Burditt Lake Area; Ontario Divisionof Mines, Geoscience Report 140.

Geological Setting of Gold Mineralization in the Western Part of the Shebandowan Greenstone Belt, Dist. of Thunder Bay, Northwestern Ontario; Ontario Geological Survey Open File Report 5636.

Quaternary Geology Lake of the Woods Region, Northwestern Ontario, Year 1; Geological Survey of Canada Open File Report 1697.

Geology of the Straw Lake Area; Ontario Geological Survey, Geological Report 222.

Precambrian Geology of the Rainy River Area; Ontario Geological Survey, Map P.3110.

Quaternary Geology, Lake of the Woods Region, Northwestern Ontario; Geological Survey of Canada Open File 1968.

Quaternary Geology, Lake of the Woods Region, Northwestern Ontario; Geological Survey of Canada Open File 2080.

The Geological Setting of Mineralization in the Mine Centre - Fort Frances Area; Ontario Geological Survey Open File Report 5512.

Structural Setting of Vein - Type Gold Mineralization in the Mine Centre - Fort Frances Area: Implications for the Wabigoon Subprovince, in the Ontario Geological Survey Miscellaneous Paper 110.

- 37 -

I sado, E.v. and carswell, B.F. 1987: Surficial Geology of Northern Ontario; Ontario Geological

Survey, Map 2518.

J Schneiders, B.R. and Dutka, R.J.1985: Property Visits and Reports of the Atikokan Economic

Geologist, 1979 - 1983; Ontario Geological Survey Open File Report 5539.

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977.

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(b)

frag

men

tal

Ult

ram

afic

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etav

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nics

Cla

stic

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etas

edim

ents

(ear

ly p

latfo

rm s

eque

nce*

}

GE

OP

HY

SIC

S

Mag

netic

A

nom

aly

o—

ai

rbor

ne

oo—

gr

ound

«,-r

m

agne

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ow

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ctro

mag

netic

^\

air

bo

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( tin

gle

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nd

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nom

aly

airb

orne

grou

nd

MIN

ER

AL

OC

CU

RR

EN

CE

^

(1)

Gol

den

Star

(2)

Paci

tto(3

) Is

abel

la(4

) Fe

rgus

on(5

) G

olde

n C

resc

ent

(6)

R.C.

Co

ne M

ine(7

) Co

ne P

rosp

ect

(8}

Stag

ge(9

) Fo

ley

(10)

Bea

r Pa

ssag

e(1

1) O

ttert

ail

Lake

(12)

You

ng-C

orrig

an(1

3)

Gagn

e La

ke(1

4) t

find

Bay

(15)

Loc

kart

Lake

(16)

Far

ringt

on B

ound

ary(1

7) S

eine

Bay

Fe

(18)

Stan

g(1

9) S

tell

ar(2

0) M

acke

nzie

-Gra

y(2

1) D

inos

aur

(22)

Luc

ky C

oon

(23)

Ma

nhat

tan-

Dec

ca(2

4) P

idge

on(25) Sh

oal

Lake Iron

SOURCES OF DATA

(1)

OGS

HOEG

TS 54

(2)

OGS

Map

P.20

64 (data)

(3)

OGS

Hap

P.2202 (geol.)

(4)

OGS

Map

P.2201 Eg

eol.)

(5)

OGS

OFR

5512

(6)

OGS

OFR

5539 (pro

perty descriptions)

(7)

OGS

OFR

5334

(p

rope

rty

descri

ptio

ns)

(8)

OGS

MDC

16 (p

rope

rty descriptions)

MA

GN

ETI

C

DE

CLI

NA

TIO

N :

DA

TE

RE

VIS

ED

-

TABL

EAU

D'AS

SEM

SLAG

E DU

SYS

TEM

E NA

TION

ALDE

mER

ENC

E CW

IOG

R*PH

IQU€

93

30

92'0

0 4900

52C

,M

52 C

'6

48'1

51.

. 93

30

5267

52C/

16

S2C

/9

52 C

.'S

48 1

5'9Z

OQIN

BEX

TO A

DJOI

NING

MAP

S OF

TH

E M

ATIO

NAL

TOPO

GRAP

HIC

SYST

EM

SY

MB

OLS

""*

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crop

(t

ub

- ou

tcro

p)

• co

nta

ct

(ass

umed

)

- fa

ult

lm*a

men

t

bedd

ing,

(d

ip)

pillo

w

( to

p fa

cing

)

folia

tio

n

•hea

ring

Imeo

tion

sync

line

antic

line

glac

ial

»frt

ae

min

eral

occ

urre

nce

pit

, tre

nch

shaf

t

clai

m p

ost

GE

OC

HE

MIS

TRY

O

t.ti0

soil

E3

rock

(26)

Em

pero

r(2

7) G

ibso

n(2

8) S

rayl

ie(2

9)

Isla

nd B

ay C

oppe

r(3

0)

Thom

pson

(31)

Ano

maly

4U

(32)

Bar

ber

Lake

Bas

e M

etal

(33)

Bar

ber

Lake

Au

(34)

Sco

tt Is

land

(35)

Sw

ell

Bay

(36)

Tun

nel

Bay

(37}

Moo

se P

oint

(38)

Unn

amed

(fro

m O

GS P

.293

){3

01 B

ad V

erm

illio

n La

ke(4

0) B

ad V

erm

ilion

Lak

e 2

(41)

Unn

amed

(fro

m O

GS P

.293

)(4

2) B

ear

Pass

(43)

Bea

r Pa

ss 2

(44)

Gag

ne L

ake

2(4

5) R

yan

(46)

Sei

ne B

ay F

e 2

(47)

Blis

s La

ke

(9)

OGS

GR 1

15

(Sei

ne B

ay,

Map

2279

)(1

0) O

GS H

ap P

.204

8 (d

ata)

(11)

OGS

Map

P.29

3 (g

eol.)

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21

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13HR

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F

31

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to 2

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lN

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192

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ansv

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catn

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EOAJ

IDIS

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E DC

S CO

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S M

PiE

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1927

vc

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ES

ET

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pM

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197

6 V

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catio

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n 19

77.

Publ

iee

en

1979

P

art

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aine

rfp

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ite «

n pa

rtie

d JO

'ts d

es c

arte

s (I

»9)

fouf

mes

par

le

GEOL

OGIC

AL S

URVE

Y K

S

ETAT

SUNt

S

Cet

car

les

son!

en

rent

e au

Bur

eau

des

Carte

s du

C»n

«da.

m

mrs

tere

de

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tgie

. des

Min

es e

l des

fl«5

ourc

ei. O

ttaw

a.

ou c

êi l

e ve

ndeu

t Ic

plus

arts

.

C 1

979

Sa M

aint

e La

Rei

ne d

u C

hel d

« C

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a H

imst

tre

o> it

nerg

ie.

des

Mine

i tl d

ci R

es so

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PRO

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Late

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(a)

torly

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(OF

F)

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ock*

Cla

stic

S

idim

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p« )

in

clud

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lkol

ic ~

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calk

ahc

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(a)

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(b)

frag

men

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Met

avol

coni

c*

.

Cto

stic

M

etas

edim

ents

(eor

iy p

tatf

orm

seq

uenc

es)

GEO

PHYS

ICS

Mag

netic

A

nom

aly

~°—

——

o —

• ai

rbor

nt

-co-

— o

o—

grou

nd—

o-n

-o-r

w

ognt

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trot

nagn

vtic

A

nom

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grou

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VL

F-

EM

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mal

y

oirb

orn*

grou

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MIN

ERAL

O

CC

UR

REN

CES

(1)

North

rock

(2)

Trav

erse

Inl

et(3

) H.

H

upch

uck

(4)

Miro

nsky

(5)

Redg

ut B

ay(6

) Be

lacoin

a(7

) Po

cket

Pond

(8)

Horan

da P

ocke

t(9

) Hc

Tavi

sh(1

0) P

aram

aque

(11)

Dal

ey-G

albr

aith

(12)

Nick

el La

ke(1

3) W

allac

e(1

4) S

iias

Stat

ion

(15)

Bru

nette

(16) We

lss

Copp

er(17)

Stan

ol P

rospec

t(18) R

ocky I

slet B

ay(19)

Bear

Pass

Iron

(20) Dr

awbr

idge

(21) Highway

11 Mo

(22) Rice B

ay(23) M

oose

horn

(24)

Kotnick

(25)

Reef P

oint

SOURCES OF DATA

(1)

OGS

NOEG

TS 53

(2)

OGS

OFR

5512

(3)

OGS

OFR

5539

(4)

OGS

GR 11

5 (Rice

Bay

Map

2278)

(5)

OGS

GR 1

07 (F

ort

Frances, Ma

p 2263

)(6

) OGS

Map

P.2032 (data)

(7)

OGS

Map

P.31

37 (

Qua

tern

ary

geol

.)

MA

GN

ETI

C

DE

CLI

NA

TIO

N :

DA

TE

R

EV

ISE

D

-

4900

TABI

EAU

D'AS

SEM

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E DU

5YS

TEM

E NA

TION

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REF

EREN

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CRAP

MlQ

UE

WM

W

30 49-0

0'

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94 0

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92 3

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NING

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THt

IMTH

WA

l lO

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SY

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OLS

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g

t d

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thoo

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Croo

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iller

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y(2

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opki

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ay(2

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from

OGS

P.2

93)

(30)

Unn

amed

(fro

m O

GS P

.293

)(3

1) F

rog

Cree

k(3

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ocky

Isl

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ay

GEO

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CLA

IM

MA

P

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EX

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CONCENTRATE ASSAYS

SAMPLE LOCATION BEDROCK Nc. .V.T.r.

3 45 67 8 9

1013 14 15 16 17

MG 29 HG 30 MG 31 HG 32 MG 33 KG 34 MG 35 MG 36 HG 37 HG 38 MG 39 MG 40 MG 41 MG 42 MG 43 MG 44 MG 45 MG 46 MG 47 MG 48 HG 49 KG 50 MG 51 HG 52 HG 53 HG 54 MG 55 MG 56 MG 57 HG 58 MG 59 HG 60 MG 61 HG 62 HG 63 HG 64 MG 65 MG 66 HG 67 HG 68 HG 69 HG 70 MG 74 NG 75 MG 76 MG 77

SB 6 SB 7 SB 13 S.B 14 sfe 15

SQ 1 SQ 2 SQ 3 SQ 4 SQ 5 SQ 6 SQ 7 SQ 8 SQ 9 SQ 10 SQ 11 SQ 12

GS 1 GS 2 GS 3 GS 4 GS 5

P 1 P 2

B 2 B 3 B'7

B 8 B 9 B 10 H 11 B 12 B 13 B 14 B 15 B 16 B 17

GB 38 GB 39 CB 40 GB 41 CB 42 GB 43 GB 44 GB 45 GB 4G G5 47 GB 48 GB 49 GB 50 GB 51 GB 52

GL 1GL 2 GL 3 GL 4 GL 5 GL 6 GL 7 GL 8GL 9GL 10GL 11GL 12GL 13-_• • iGL 15GL 16GL 17GL 18GL 19CL 20GL 21GL 22GL 23GL 24GL 25:L :<GL 27GL 28GL 29GL 30GL 31GL 32GL 33GL 34GL 35GL 36GL 37GL 38GL 39GL 40GL 41GL 42GL 43GL 44GL 45

BN 7

TL 1TL 2TL 3TL 4TL 5TL 6TL 1TL 8TjL 9t 10TL 11TL 14dTL 14bTL 16TL 17TL 18TL 19TL 20TL 21TL 22TL 23TL 24TL 25TL 26TL 27TL 28TL 29TL 30TL 33TL ?4TL 35TL 36TL 38TL 39TL 40TL 4171 4:TL 43TL 44TL 45

Sfl 34SH 35

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52B/08 52B/08 52B/09 granite 52B/0952B/09 52A/05 52A/05 52B/08 granite 52A/05 52A/05 52A/05 52A/Q5 volcanic 52A/05 52A/05 52A/12 52A/12 52V12 52B/08 52B/08 52B/08 granite 52B/08 granite 52B/03 52B/Q8 52B/08 52B/09 volcanic 52B/09 volcanic 52B/09 52B/09 52B/09 52B/09 52B/09 52B/09 52B/Q9 52B/09 528/09 52B/09 52B/09 volcanic 52B/09 volcanic 52B/09 52B/09 52B/09 mafic vole 52B/09 mafic vole 52B/09 52B/09 mafic vole 52A/12 52A/12

52B/09 mafic vole 52B/09 52B/0952B/09 528/09

52B/10 gneiss/mig 528/10 migmatite 52B/10 52B/10 52B/10 52B/10 52B/10 granite 52B/09 52B/10 52B/10 mafic schist 52B/10 iron fm 528/10

52B/08 52B/08 52B/08 52B/0952B/09

52B/09 52B/09

528/10 intrusive52B/10 basalt 52B/09 52B/09 mafic vole 52B/09 volcanic 52B/09 volcanic 52B/09 volcanic 52B/09 volcanic 52B/09 volcanic 52B/09 iron fm 52B/09 volcanic 52A/12 52A/12

52B/09 mafic vole 52B/09 52B/09 52B/09 volc/intrus 52B/09 felsic intru 52B/09 mafic vole 52B/09 mafic vole 52B/09 iwfic vole 52B/09 52B/09 mafic vole 52B/09 52B/09 52B/09 mafic vole 52B/09 52B/09

528/0952B/09 52B/09 52B/09 52B/09 52B/09 52B/09 52B/0952B/0952B/09 volcanic52B/09 volcanic52B/09 mafic vole52B/09 felsic vole528/09528/09 gabbro52B/09 mafic vole528/09 gabbro52B/09 mafic vole528/09 gabbro52B/0952B/09 mafic vole52B/09 mafic vole52B/09 mafic vole52B/09 gabbro52B/09 ;ufic vole:."5/09 mafic vole528/09 mafic vole52B/09 mafic vole52B/09 mafic vole52B/0952B/0952B/09 gabbro52B/09 gabbro52B/0952B/09 volc/gabbro52B/09 volc/gabbro528/09 mafic vole52B/09 mafic vole528/09 gabbro52B/09 tuff52B/09 gabbro52B/0952B/0952B/0952B/09

52B/09 volcanic

52B/09 volcanic52B/09 volcanic52B/09 intrusive52B/09 sheared vole528/09 volcanic52B/09 felsic tuff52B/OS gabbro52B/0952B/09 volcanic52B/09 volcanic52B/09 volcanic52B/0952B/0952B/0952B/09 granite52B/0952B/09 volcanic52B/09 volcanic52B/Q9 volcanic52B/09 mafic vole52B/G9 felsic vole52B/09 felsic seds52B/09 metaseds52B/09 metaseds52B/09 metaseds52B/09 seds t IF52B/09 seds + IF52B/0952B/09 granite/volet *7 •":

52B/09 volcanic52B/09 volcanic

. 52B/09528/09 volcanic52B/09 volcanic52B/09 volcanic^B'O 11 volcanic52B/09 volcanic52B/0952B/09

52A/1252A/12

no. of samplesminimum valuemaximum valuemean valuestandard deviationvarianceanomalous threshold

WEIGHT |kg) +6mm

Total Frac.

22.5 29.0 21.1 25.4 17.8 20.7 24.5 29.0 26.0 23.3 25.9 25.1 25.0

25.4 26.3 26.8 25.1 23.5 24.3 21.8 27.2 26.7 27.5 26.7 19.0 23.5 23.5 24.8 27.0 28.0 26.6 25.4 29.0 24.7 25.0 23.5 23.0 26.8 26.6 26.7 25.9 22.7 26.7 26.7 25.2 24.8 28.0 24.5 29.0 30.0 30.0 34.0 28.4 28.5 30.0 27.5 30.0 29.0 28.5

27.0 20.6 30.0 20.1 21.7

20.0 24.8 27.0 26.3 23.1 22.0 23.1 27.4 28.5 20.4 21.2 24.9

29.0 27.5 26.9 28.5 23.8

25.8 26.7

28.0 27.0 25.8 13.6 23.0 22.3 25.7 21.5 27.5 26.5 20.1 19.3 20.7

43.6 34.930.5 33.4 32,438.1 33.227.0 37.0 35.5 33.1 34.2 26.0 39.0 43.7

37.7 35.5 36.9 34.3 27.7 42.7 32.6 39.828.027.42S.426.629.025.521.224.521.725.122.923.222.030.022.825.031.225.930.23D.O32.133.030.026.832.026.532.030.025.031.030.033.125.032.033.430.030.0

28.5

28.021.325.726.025.722.7:4.:26.218.915.613.121.521.720.319.422.316.914.315.015.817.822.217.116.017.013.515.319.019.620.418.014.617.119.413.427.019.014.418.224.5

24.120.9

19913.143.725.7

5.732.837.2

10.1 10.3

5.98.6 2.8 5.1 6.5 7.7 4.7 6.6

11.4 5.8 7.0

6.4 7.5

11.8 2.8 9.7 8.4 5.7

10.0 4.5 8.2 3.4 7.4 7.0 5.5 7.9

15.7 5.0 8.2 8.4 6.5 4.9 5.9 6.7

15.9 13.7 15.7 13.5

3.7 5.4 9.6 5.4 5.5 5.4 4.7 6.3 5.7

10.4 8.7 6.7

10.9 7.1

14.4 9.7

22.4 6.4

12.51.7 5.4 3.3'

4.8

2.5 1.9 4.6 0.1 0.2 5.8 6.0 6.9 1.8 1.5 2.9 3.8

6.8 3.2

11.2 9.6 8.6

8.1 8.8

10.4 6.42.1 2.7 3.0

11.1 3.0 6.3 1.2 8.2 1.8 1.8 3.2

11.8 12.7 7.8

11.0 7.0 8.3

11.8 13.0 18.8 8.0

14.9 13.1

6.1 7.1

14.9

14.68.0

12.1 8.6 6.7 6.0

14.1 18.314.2

9.98.03.47.01.44.24.64.87.96.0

10.61.75.41.06.53.56.75.29.67.57.25.74.52.58.49.55.84.54.88.65.36.3

15.64.86.02.5

6.5

6.39.32.77.13.88.2?.54.73.9 •4.72.72.12.43.74.54.00.55.58.1

10.44.03.93.24.61.3

7.32.17.45.?3.01.63.93.62.52.41.94.01.54.3

0.49.3

1980.0

22.46.73.9

15.614.6

TILL DESCRIPTION PEBBLE

C 0 S CS CA Vole Int

1 1 3 12 11 21211121222212121232121123212222222113

2

2122111211133222111111111101114111121111

34

3 4 43 3 4 2 23343223332322232323222222112233122112

3

]33242.1243300332442333330431330333424322

22

4 3 4 2 2 3 4 35342212233341213123323311433214244331

3

3514343334312243124543343022442033241514

14

2

332212222222213123323311433214244331

3

3413243233321243132243332132442023332414

14

i

252222222212222122322223112242231123

4

4512251335431323144543454043323122322513

33

20 40 50 40 30 30 40 50 20 10 20 50 45

10 50 20 40 50 40 50

50 60

90 70

50 5050 50 20 20 20 10 60 45 30

60 30 10 20 10 40 10 25 30 70

75 50 90 60 90 80 15 60

75 90 40 10 45

40 20 95

20

2060

5 30

15 4010 10 20

3020

15 40 75 90 70 90 90 90 70 95 50 50 60

50 95 80 50 80 70

100 50 90 60 90 40

100 90

40 100 95 90 90 20 40 607580

100100100100100100100100100100100

7090809570909580

65409030558075906045158040

40

80

8060

1007070954050509080807090501560

10010010090

1006070

30501040

100

8050102030403020

10025

1850

1005730

887117

80 60 50 60 70 70 60 50 80 90 80 50 45

80 50 80 60 50 60 50

25

10 26

50 50 5040 80 80 80 90 40 45 60

40 70 90 80 90 60 90 75 65 30

25 45 1040

5 20 80 40

25

60 90 50

60 80

95 80 9080 40 9020

70 40 90 90 80

70 80

80 60 25 10 30 10

30 5

50 50 35

50 5

20 30 20 30

50 1040 10 60

10 100

50

5 18 10 80 60 302520

301020

2010

20

5304020

540508020609535

20

2040

3028

5605050

520202510456040

10

4030

70508060

1002050906070307060

70

1575

1004827

718102

COUNT TOTAL GOLD GRAIN DESCRIPTION GOLD (.05 ram .05-. 1mm .1-.2 m . 2-. 3 mm .3-. 4 mm .4-. 5 m > .5 m Hgt.

Sed Other Shape GRAINS No. Shape No. Shape No. Shape No. Shape No. Shape No. Shape No. Shape (go.)

Qtz

5 Qtz

Qtz

50 15

Qtz

Qtz

10

Qtz Qtz

10 Qtz Qtz

Qtz Qtz

Qtz Qtz

Qtz

Qtz

iasp

Qtz

Qtz

Qtz Qtz

5

Qtz

QtzQtz Qtz

Qtz

Qtz

Qtz Qtz

Qtz

A A SA SA A SA A

10 SA A SA

Qtz A SA SA SA

10 SA

60

20

10

2

Qtz

5

5Qtz

100

10

30

20

210

1001524

56863

SASAAAAAAAAAASAA

A

A

A

A

AASASASAASASASRAAASRSRSAASAAAAAAAAA

AASASAASRAAASAAAAA

SRSA

4 2 SA 1 SA 1 SA 1 1 SA 0 5 2 SA 3 SA 2 2 SA/SR 4 1 SR 2 SA 1 SA 0 2 2 0 1 1 SA 0 1 1 SR 2 1 1

3 111 1 1 del 2 1 1 flakey 1 1 SA 1 1 del. 31 1 1 flake 5 3 SR 2 SA 1 1 1 1 0 6 4 SA 1 SA 1 A 2 2 SR/SA 2 1 1 1 1 4 3 SA 1 SA 3 2 SA 1 SA 7 1 SA 6 SA 0 2 2 SA 21 1 SA 2 1 SR 1 SA 2 1 SR 1 SA 7 5 SA 1 A 1 SA 0

12 6 SA 5 SA 1 A 5 4 1 6 1 SR 3 SA 2 A 3 1 1 1 SA 5 2 SR 2 SA 2 1 SA 1 SA 4 2 SA 2 SA 1 1 SR 2 2 SVSR 3 2 SA 1 SA 3 1 SA 2 SA 2 2 SR 2 1 R 1 R 1 1 42 1 SR 3 3 SA 6 1 R 4 2R/2A 3 1 2 1 1 A 3 3 R 8 2 del/R 4 3R/A 1 del

4 1 SA 3 SA 1 1 SA 6 2 SR 4 SR0 1 1

1 1 4 2 SA 2 SA 3 2 SA 1 SR 1 1 SA 0 2 1 SA 1 SA 2 2 SA 5 4 SA/R 1 SR 3 1 R 1 SR 1 3 1 A 2 A 0 3 1 A 2 SA

2 2 SA 3 2 SA 1 SA 1 1 A 5 3 R 2 R/del 3 3 A

5 2 R 2 del. 1 del. 1 1

1 1 A 3 1 SR 1 A 1 SA 3 1 A 1 R 1 del 1 1 SR 31 2 A/R 1 1 del 1 1 del 3 2 del/R 1 R 2 1 R 1 R 3 2 R 1 R 2 2 SA/R 1 1 del 2 1 A 1 R

2 1 1 2 2 SR,A 2 1 SA 1 SA 7 1 R 1 R 5 5A 1 1 A 2 1 1 1 1 SR

11 2 SR,SR 3 SR 5 SR 1 SR 10 2 SA,SR 1 SA 5 SA 1 SA

7 1 A 1 R 4 SA,Sr 1 SA 4 2 SA,SR 1 del

10 5 A 4 SA 1 SA 4 2 SR,SA 1 SR 1 A 5 2 SA 3 A,SA 6 3 A,SA 3 SA,SR

0 5 5 3A,SR,SA 7 6 3SA,2SR 1 SA 5 4 2del2SA 1 SA 32 1 SA 1 1 2 2 A,SR 2 1 del 1 A

11 2 A5 2 A,10111104 10007 20342 1043 12505 33 212 125 3

112 168 3

13 82 12 1

6

4000226 3200021003010001200003 1001010000001 101

199 710 0

13 83 23 17 28 4

2 A,SA 6 SR,A2SA 1 SASA 2 del, SA 1 del

1 SA

1 SR1 A

1 A1 SA

1 SA 2 A,SA

2 2 1

3 SA2 1 1

422 SA

3 2 SA

1 1 SA11 SA12 SA2 SA

7 SA-SR 3 SA-SR1 SA4 21 2 25

11

1 SR 3 dlSA,SA 2 del SA

2 A,SA 1 SA

1 SA 1 SR1 SA 1 A

3 A,SA,SA1 A 1 SA

1 A 1 A1 SA

1 SR 2 SA,SR

1 SR

1 SA1 SA 1 SR

1 SR 1 SA

1 SR

1 SA

iiiniiNiiiin5SFB4NE9650 63.6161 ADRIAN

1 SA

91 101 310 0 07 6 22 2 11 1 02 2 04 4 2

28.7 31.5

26.7 20.7 45.1 18.1 36.4 25.3 15.4 19.5 35.1 19.0

39.9 25.2 16.7 28.4 34.2 30.6 19.5 14.0 52.0 26.7 25.2 21.6 18.7 11.5 37.1 33.7 29.6 36.6 37.3 25.2 45.1 33.3 36.6 45.4 30.5 44.2 25.8

2 SA 25.7 15.7

1 SA 30.2 53.9 24.6 29.5 22.9 42.1 28.3 38.5 40.5 44.5

1 flat 32.9 42.4

1 SA 36.6 32.5 44.0 24.6

1 SR 25.2

55.4 22.2 60.7 34.3 12.4

15.2 40.6 22.9 18.4 29.5 40.7 30.8 46.5 35.7 16.9 25.8 54.9

39.020.1 U.I 16.2 39.8

37.1 34.5

32.1 17.7 33.4 26.5 28.3 41.1 32.5 27.3 34.0 37.2 47.0 38.8 18.2

59.1 52.5 63.3 63.0 46.3 44.9 13.2 41.1

1 SA 57.0 61.6

1 A 37.7 37.6 33.9 52.1 34.2

29.6 35.1 46.0 37.1 35.9 42.7 44.3 36.541.328.521.318.525.719.438.625.222.324.825.823.616.639.525.838.050.9

1 A 16.030.136.155.250.039.829.850.010.732.940.135.538.8

1 SA-SR 38.437.9

48.738.820.4

48.3

1 del 52.622.533.033.936.628.543.535.432.838.324.034.945.130.646.939.244.232.523.728.5

28.430.621.818.9

• 33.328.333.6

26.310.523.7

25.455.036.926.037.041.8

•44043.528.4

750 193000 0.01 2 0 63.31 1 0 33.20 1 0 11.60 1 0 134.52 2 0 56.4

Hag \

60

50

60 40 80 70 60 85 60

80

60

80

90 60

70 70 70

90 80 80 50

80 60 50

80 60 80

50

30 60 25 25 30 75

75 25 90 80

60

60

50

60

60

80

90 30

60 50 70 95 90

80 60

60

90

95 80 95 20 20 95 40

15 20 30 40 20 15

5 10 20 25

2525 35 30

35 15 25 30 30 25

20252510

55

151025

55020

10452025451530301035251010203030133080104040403735

25

2515253020

302510trtr6040

55

4520

1tr

1

151020tr10

010

107

15

220

55

3025

6530

1640

953728

77793

CONCENTRATE Ultraviolet py Gar Misc. lamp Rad \ \ Sen Zii

tr tr

tr 5

10 10 tr

5 30 tr

10

5

tr

tr 5

10 5

1020 10 tr

1010 10

tr tr 15

1010 tr

20 trtr

5 trtr tr tr

5tr trtr

10 5

10

5

5

tr

tr 10 tr trtr

tr8

trtr

tr

tr

tr

tr

trtr tr

5 tr

5 5 5

5

5

2 3 3 3

tr 5

tr2

tr3

tr02

tr5

tr2

tr

trtrtrtr

5557355

trtrtrtr

335

trtrtrtrtr10tr

tr

55

tr3

10

tr2

trtrtr

221222020

tr5

trtrtrtrtr

3tr

3

trtr

0trtr

1

02

1590

3034

2012

tr Y tr Y

Y

Y

tr Y tl Y

Y 15 Y

10 Y Y

tr Y

Y Y

Y

tr Y

Y 10 Y

Y

Ytr

Y Y

tr Y Y

5 Y Y

Y

tr Y tr Y tr Y tr Y

Y Y

5 Y

5 Y tr Y

tr Y

20 Y

Y

tr

Y Y Y

10 Y

Y Y Y

5 Y

Y 10 10 Y tr Cpy tr Y

tr Y Y

tr tr Y tr

tr

tr Y tr Cu Y

Y tr Y

5 1 tr 1

3 1 tr 1 tr 1

5 1 1

5 1 1

5 0 1

3 1 0

5 1 5 1

5 1 tr 0

4 0 3 1 3 0 2 0

0 tr 0trtr

00C2

tr0000

0trtrtrtrtr10tr

3tr10tr

313tr

tr13

10trtrtr

0

5trtr

35

tr4000

1050

tr50000

510

0trtr

0tr

204

053

trtr

0

00

ZZZZ33Z

1240

2024

1510

0011001001210

0

000000010101100101110200011

100

02011111

134020101

Y Y Y Y Y Y Y Y Y Y Y

Y

r

Y Y Y

Y Y

Y

Y Y Y

Y Y Y

Y Y Y Y Y

Y

Y Y

Y Y Y

YY

Y

Y Y Y Y

Y YY

Y Y

Y Y

Y Y Y Y Y

YY

1

1 1 1 1 1 1 1

2 0 2 1 0 2 1 11201222212112

2

12322222211322131000

2210001

212

031123

10

SS3SS

144031112

0 0 0 0

0 0

0 0 0 0 0 0 0 0

0 0

0 0 0 0 0

0 0 0 0

0

0

0 0

0

0

00 0 0 0

0 00 0 0

00

0 0

0 0 0 0 0 0

0

0

0 0 0 0 0 0 0 0 0 0 0 0 0 0 0

0 0 0 0 0 0 0 00000000000000

0

00000000000000000000

0000000

000

000000

00

ssss

134000000

NOTES NORMALIZED VALUES GOLD GOLD grains microgi

6 basal till 1 1 Au grain ?(.3 x.l) odd colour 0

6 3 5

clay in till 0 jasper, clay in till 2 clay 0 basal till 1 basal till 0 ablation till (boulders] 1 clay till 2

3 1 3 1 1

sandy, oxidized, basal till 4 6

ox basal/unox sandy till 1 coarse fraction 50% clay 1 unoxidized basal till 0 oxidized basal till 6 3rd Au grain 7 SA, proc. error 3 may/may not be gold 2 gold?, oxid & unoxid basal till 1 ox & unox basal till 4 ox & unox basal till 3 silty, ox basal till, no bdrk 11 sandy basal till 0

2 2

ox basal till 2 ox basal till above sand layer 2

8 oxidized basal till 0 oxidized basal till on bedrock 22

8 oxidized basal till 11 oxidized basal till 5 no bedrock 1

5 sand & boulders 2 very sandy, oxidized 4 sandy 1 clayey till 2 sandy 3

3 clayey, basal, vole, carb veins 2 silty basal till 2 Cpy in cone., boulder pile 1 basal till 4 basal till silty & stoney 3 sandy basal till 5 gravely basal till 5 sandy stoney basal till 1 bad sample, sandy 9 silty basal oxidized till 7

unoxidized basal till 6 oxidized till 1 oxidized till 5 oxidized 0 clay rich oxidized till 1

ox till 1 oxidized till, clay rich 3

3 oxid. /unoxid. sandy till 1 oxidized/unoxidized sandy till 0 oxidized/unoxidtzed sandy till 2 till on bedrock 2

5 2 3 0

grains on vole rk chip with qtz 3

oxidized/unoxidized sandy till 2 oxidized/unoxidized basal till 2 also 5% hble; unox basal till 1 unox, sandy till 5 oxid/unox till, tr. barite 4

unoxid. basal till, tr.raaq,bar 6 clay ox till/sandy unox till 1

ox. /unox. till 1 stoney ox., silty unox. basal 3 mag., epidote; loamy ox. till 3 silty or basal till 2 oxidized loamy till 3 oxid. loamy, cobbly till 2

1 cobbly 4 silty till/unox. clay till 2 silty till, iron formation frag 3 silty basal till 2 red clay in basal till 1 oxid. red clay 2

slty sdy bsl till 1 gravelly till 2 sandy gravelly till 2 silty, gravelly till (basal) 6 silty till; basal 1 clayey basal till 1 reddish till 1 reddish till 16 good till 11 clay-rich till 5 clay-rich till 4 clay and gravel 9 sandy till 4 till over clay-silt 3 poor (sandy) till 4

0 4 6 43 1

gravelly 22

basalbasal localsilty basalsilty basal

silty basalsilty basalsilty basal

siltysilty gravellysilty basal

basal

silty basalsilty basalsilty basalbasalbasalbasalsilty basalbasalbasalbasalbasalbasalbasalbasalbasalbasalsilty basalbasalbasalbasalbasalbasalsilty basalbasal

silty basalsandy

16B1011110500060332042240331224

1016

10921

5

4000236200021003020001300004001020000001

02

1990

2233

109

2.0 3.5 4.0 6.1 1.8 8.9 0.3 1.6 1.1 0.7 0.1 4.5

20.7

11.9 3.6 2.84.3 5.0 3.2 4.3 1.9 2.3

16.2 18.5 9.6 3.9

22.6 6.2 3.4 1.9 9.5 4.2 2.9 4.5 6.9

14.6 22.8 84.1 14.6 64.0

216.9 11.2 36.9 0.2

54.9 2.4 3.2 1.5 4.0 7.1

10.1 5.5

11.9 5.2

21.5 1.6

19.0 16.0 14.3

7.7 1.9 1.4 0.5 4.7

3.9 2.1 4.0 0.5 1.1 4,4 4.2 1.7 1.6 1.3 0.1 2.7

3.6 0.0 4.9 8.4 0.2

0.3 1.9

2.42.1

21.7 0.1 4.9

23.5 8.0 0.1 3.0 8.8 9.3 1.0 0.1

10.111.6

3.8 7.0

32.8 4.0 6.6

61.5 30.6 6.3

18.5 21.5

5.6 1.7 7.3

9.0 3.5

15.8 13.5

1.5 3.4 5.4

21.534.020.91.6

16.65.01.12.56.32.2

12.610.612.6

3.610.82.36.45.3

25.82.1

15.75.35.15.61.34.3

10.51.72.58.67.0

57.04.56.5

38.214.4

4.32.4

8.4

18.48.51.63.00.18.22.77.71.94.10.1

13.517.016.20.28.71.34.40.23.80.7

11.19.00.10.30.10.25.55.48.34.40.05.83.03.15.13.48.74.83.5

0.142.7

199.00.0

216.99.8

19.0361.2

47.8

Au ppb

det 5

4310572

19364

155154748373

125987

28513312717110184

17918437

701680347168

16301629639

2849811991210354410

1520213

137052506781380

32230

7815936

160224246158393108678158451216634

101812813

322

22859

1973942871183759733

53

973

243497

3

749

65124775

3173321281

3115217182233

32724668

1259D2133540

105049014145161112453

312

35213942847144

147114813570644327

11802156755

2538444435133822633599156145

15508644511913522949

1279426076

249237

1580164285990423134164

192

3812295691

321158

23544593

290470441

320425603

3616

361205

31333

139149196127

31638566

11579

17510984

3879

1993

5250288494

2443091277

Au rogn

1.23.33.05.11.37.00.31.71.20.60.14.4

18.7

11.33.32.14.83.42.63.52.61.9

18.617.17.53.1

18.66.03.21.1

10.33.63.04.16.9

12.918.545.89.4

35.2134.510.641.40.2

54.32.33.61.54.58.69.97.012.94.6

24.75.119.35.3

15.9

5.61.81.70.43.9

3.42.44.50.71.23.53.61.72.11.20.12.9

3.80.13.97.90.1

0,31.7

2.1-2.2

25.70.14.9

13.29.10.13.98.08.50.90.1

16.012.94.37.941.75.97.1

43.027.68.716.822.75.52.810.6

10.44.8

19.617.41.66.25.0

29.623.518.37.021.55.51.32.16.31.8

10.99.07.93.713.22.65.97.424.82.6

16.06.66.66.81.56.39.51.93.08.89.2

61.06.26.1

31.320.65.23.4

9.2

20.05.11.83.10.16.02.58.31.42.30.1

13.116.413.50.18.01.11.90.11.00.5

10.26.30.10.20.10.14.63.36.03.30.03.82.31.76.32.94.54.03.5

0.124.8

1990.0

134.58.713.4

178.935.4

Ag ppm

5

3333333333333

3333333333333333333333333333333333333333333333

33333

333333333333

33333

33

3333333333333

333333333333333

333333333333333333333333333333333333333333333

3

3333333333333333333333333333333333333333

33

199333003

Asppm

2

1512326111121

114131

28434111141631121111911111111112131323412

11135

313111311411

13131

11

3413121111114

131111153141111

332151152118211334611413143191141753135111111

3

11112411213111311

161

1015111451812111141411

11

1991

282378

BaPP»> 200

570230250100440100100270100390100250100

10010010026010010043010030010010045010010010010010010010010027028010010010010010010010036010010035010010029034010024010020010035010D100370

380100230420100

100520100640100210530360300500360240

100100100100400

650100

290340100370100380270100100100260210100

100100100100100100100100270100100220310100450

100100100100380370100100310100410300100100100100100100100240100100640100100100100100210100290100230100100100310100100100100100100400100

100

200100430360460100100340310100360100100300100290390100460100100100100590690100510440100100100100100100320100280100100100

100310

199100690198144

20677466

Br ppra

5

3333333333333

3333333333333333333333333333333333333333333333

33333

333333333333

33333

33

3333333333333

333333333333333

333333333333333333333333333333333333333333333

3

3333333333333333333333333333333333333333

33

199333003

Ca

1

1134121111111

2321213231112212112123321211211114111312313211

31146

545133531411

11221

11

3111133331211

213211211112212

112111111143435111611153634113144112111411255

1

315611111111113111651111

12111116111111111

31

1991

122225

Co ppm

5

35513756714079766496555372

637791865863879441865955961205765805243733662645068756986965734695465407857484170395054535883

5875372695

574066363051365325465727

5234657636

3741

44755036554962644317334886

695757638073

1205552516258415259

7255456947575460615550736760488582

110897073655456467563646560777043

1007764507198527090603463

42

298054493853404548413431275428353762

200537365819330487443

1006646847362483154585741

6067

19917

2006021

452103

Cr ppm 10

5306207208101200360500270400

11002000470810

7301400240014008205608008201704906606108801400390310460780390580250740840550690650

11001100210011002809508201200610560400300330640320490510550360640

1200420430200

2100

1000520

7900580370

1300440900490850660300

490250750670370

650500

8202100820480800510660

1200640270330280450

230071020001600160021004900710630530670

1100810810

1300

10006205709904209306704109506106201600350020001700300042005300280012001100660500670520

120077015001000560

3800120070013001200270014001400840730

26001400790970

1500

430

310660570570410400310440360260570660490650260740320370

3000400410990460460

5700280310620550460570680530600370300390460440600

300390

199170

7900959988

9764382935

CsPP"

2

1111111111113

1111311111112121211111111111111113111111111132

11331

411311111111

11111

11

1113111212111

111111111111111

111112111116131111111231111141111112111111113

1

1111111111111111111111111111111111111131

12

199161103

Fe

0.0

21.224.514.027.335.515.630.125.820.945.821.919.728.3

23.629.140.629.921.129.241.244.013.438.824.618.041.156.620.426.831.018.616.736.115.025.426.219.229.224.530.035.237.225.012.329.422.829.014.531.022.517.913.326.113.420.222.222.425.334.9

15.525.312.96.9

40.7

25.612.119.611.18.7

12.812.515.37.8

14.423.29.9

20.48.1

35.939.113.5

16.917.4

13.434.118.411.223.516.722.423.013.826.410.615.828.9

25.621.516.122.330.624.543.222.621.221.125.926.119.622.729.8

34.523.318.831.215.220.324.023.226.923.614.627.426.321.113.729.829.135.333.528.423.225.216.021.215.324.920.429.618.821.530.220.312.634.928.720.914.225.933.617.922.135.523.113.320.2

18.6

9.327.818.214.615.318.614.714.018.314.18.79.4

10.420.97.710.211.811.79.411.725.921.830.330.97.7

16.226.013.637.225.113.929.429.222.816.49.6

19.119.821.715.1

20.224.9

1996.956.622.48.7

75.039.7

HEppm

1

879

1314797

1632261419

13161918101232304

1112151843128

1389168

1196

10891140297

201221119767

1166776

17

41694

39

281143341810111025351911

53

12209

611

26199

101210161412569

13

118

11101819569898

15321922

161891521221111111321261840112021212416309

17112225211299

112015431513181711177714124153

8

20342936202913191115203740221236181436

3135282724171338201541562621161514251722

2115

1993

771811

12740

ppn 5

3333333333333

3333333333333333333333333333333333333333333333

33333

333333333333

33333

33

3333333333333

333333333333333

333333333333333333333333333333333333333333333

333333333333333333333333333333333333333333

33

200333003

Ir ppb 40

20202020202020202020202020

20202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020

2020202020

202020202020202020202020

2020202020

2020

20202020202020202020202020

202020202020202020202020202020

202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020

20

20202020202020202020202020202020202020202020202020202020202020202020202020202020

2020

19920202000

20

Ho ppn 20

10101010101010101010101010

10101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010

1010101010

101010101010101010101010

1010101010

1010

10101010101010101010101010

101010101010101010101010101010

101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010

10

10101010101010101010101010101010101010101010101010101010101010101010101010101010

1010

199101010Q0

10

Nappm 500

18700116001410011400940013000115007770109006040132001290010600

1030010800103007370

109001050072005710

126006050

1140013600664Q4620

112009010788014200164009580

198001260011200125001120094208360799076401100017500120001510012600166009700

1200012600153001100014000121001160011700123006340

120007910

14100235005141)

121001440012100191001910011300207001410019400232001400017500

137002120010500943017400

2030016000

17300120001340013200979012400100007640

140009800

14500126009240

64109080110009180496072903940

138001190010900117009930159001010011400

1040011700125008900

13700111001020011800123001130011000103001180011800133009400

115007990668012600107009980

125001060010600927091908430

111001030086308210

10500380091908440

104006870757012200700076808780

1850013500

11300

15400109001350013700118001250012600120001300010500120001410015300121001850016000131001360011800129006330

112007990953097301230071501410083909550

1470078608140

1180010100121001160011000927012400

1040010900

1993800

23500115803413

1164989518406

Ni ppm 200

100100100100100100100100100100100100100

240200100100100100100100100100100100100100100100100100100100100100100100100100100100580100100100100100100100100100100260100100100100100100

100100100100100

100100100100100300100100100100100100

100100100100100

100100

100100100100100100100100100100100100100

100100100100100100100100100100100100100100100

100100100100100100100100100100100100100100100100100390100100100100100100100100100100100100100100100100100150100100100100100100100100100

100

100100100100100100100100100100310340100100100100100100250100100100100100100100100280100100100100100100100100100100Vffm100100

19910058011152

2743216

Rb ppm 50

25252525252525252525252525

54252525662552252525252525252525252525255525252525252525255525252525252525252525252525252525

25252525

120

252525252525252525252525

2525252525

2525

67252525252525252525252525

252525252525622525252525252556

252525252525602525672525252525252525252525252525252525252525252525252525252525252525252525

25

252525252525252525252525252525252525252525252525256525252525252562252551252525M

2525

19925

1202811

11849

Sb ppn 0.2

0.116.00.10.10.10.10.11.10.10.10.10.10.1

0.10.10.10.10.10.10.10,10.10.10.10.50.10.10.10.10.10.10.10.10.30.10.10.18.30.10.10.10.10.10.10.50,10.10.10.10.10.10.10.10.10.10.10.30.40.1

0.10.10.10.10.1

0.10.10.10.10.10.30.30.10.10.10.10.1

0.10.10.10.50.1

0.10.1

0.50.10.20.30.10.10.10.10.10.20.10.30.1

0.40.10.10.10.10.10.10.10.10.20.10.10.10.10.1

0.10.10.1O.i0.10.10.10.10.30.10.10.40.10.10.10.10.10.10.10.10.10.40.40.10.30.10.10.10.10.10.10.10.10.10.10.10.10.10.10.30.10.50.10.10.1

0.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.30.10.50.10.10.10.10.10.10.10.10.10.30.10.10.10.10.1o.i0.10.10.10.1»rl

0.10.1

1990.1

16.00.31.31.62.8

Scppn

0

15172224201825262823242026

25262528252427242525283030262624292520231825222224222323362416242324212421191926201924222324

1632201925

261930272119181820292516

1826182118

1317

21252321212327402612202233

211924192427402019201922152119

222019242824182018233534333731333223302540203326263635242022213524192523302922265125221838

17

23342936202317251920253026242031233227282838292534212436312447532731312622292122

2823

1991253256

4037

Se ppn 20

10101010101010101010101010

10101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010

1010101010

101010101010101010101010

1010101010

1010

10101010101010101010101010

101010101010101010101010101010

101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010

10

10101010101010101010101010101010101010101010101010101010101010101010101010101010

1010

19910101000

10

Sr

0.2

0.10.10.10.10.10.10.10.10.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.1

0.10.10.10.10.1

0.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10,1

0.10.1

1990.10.10.10.00.00.1

Ta ppa

121112214111313335244111443624312341123114611311231513114311

11119

115111111111

11163

11

3131322111111

232345731323131

332111321111233227I51522311423111413134186311

1

152721132317711421221815221855

10752212252

43

1991

102236

Th

1

11131116241122141537122236

18352216172129255

37172240562527201014228

2525163811182486238

2523JO1236251916271121111975

120

1222165

92

189

29179656

14161810

225

182311

1011

10162211191619101388

2343

201913193525563216181522172825

30261524142121172315142218279

192031332424231616162520221318221416563217202438177928251240

15

17342840153014321714126691371151151114

2459423217162263384159524221122720313132

1523

1991

1202417

27957

I) ppn 0.5

0.31.81.72.61.60.32.00.30.33.81.92.43.4

1.40.30.30.32.30.33.34.50.30.32.40.33.54.72.23.43.50.30.32.60.34.52.31.43.50.30.35.25.23.20.35.32.50.30.33.53.12.00.30.30.30.31.92.55.48.5

2.63.20.30.35.6

3.30.34.63.91.52.01.80.31.70.30.31.3

0.32.22.10.31.6

0,30.3

2.80.30.31.40.30.33.00.31.70.31.12.25.0

0.32.21.31.83.80.36.13.51.62.21.81.42.82.41.9

2.92.81.51.82.02.72.02.83.33.04.03.21.71.92.04.30.73.81.03.01.30.31.70.33.15.40.32.40.32.51.62.60.36.20.30.33.03.33.42.7

11.03.32.72.55.2

2.4

2.51.45.62.51.54.02.53.03.11.43.46.34.83.92.84.03.40,70.30.31.53.94.21.71.01.03.11.71.63.55.69.61.01.00.71.02.03.13.53.2

0.72.9

1990.3

11.02.31.83.25.8

V ppai

4

20922222722222

22

122222

17293922222225252

112272222222222222222222

16

22222

2222272

222222

82

4522

22

2722222222222

222222262222222

2222422222222222222225222222

2213222222222222222

2

2222222222225222222822227222222222222222

22

1992

4535

2613

Zn

200

100100100330280100360280210500210100360

220340320340230280390530100450240200460470200310340100200320100300290100390240330320280220100300250260100420290100100370100210230200200410

100330100100480

230100100100100100100100100100220100

250100250420100

100240

100450100100270100220100100100100100300

290270240270300340660260220230220270100220250

280230100260100100280210240230200100350100100360410400470300280310200340220360210340240360410370100360430290320330340240220420300100310

100

100460200100100210100100250100100100100270100100100100330100370200410320320100250250480310100340370200200100100270350100

380320

199100660236120

14382 2475

Table 3

ATIKOKAN AREA

SAMPLE No.

A 1A 2A 3A 4A 5A 6A 7A BA 9A 10A 11A 12A 13A 14A 15A 16A 17A 18A 19A 20A 21A 22A 23A 24A 25A 26A 27A 28A 29A 30A 31A 32A 33A 34A 35A 36A 37A 38A 39A 40A 41A 42A 43A 44A 45A 46A 47A 48A 49A 50A 51A 52A 53A 54A 55A 56A 57A 58A 59A 60A 61A 62A 63A 64A 65A 66A 67A 68A 69A 70A 71A 72A 74A 75A 76A 77A 78A 79A 80A 81A 84A 85A 86A 87A 90A 93A 94A 100A 101A 102A 103A 104A 105A 106A 107A 108A 109A 110A 111A 112A 113A 114A 115A 116A 117A 118A 119A 137A 138A 139A 140A 141A 142A 143A 144A 145A 147A 150A 151A 152A 153A 154A 157A 158A 159A 160A 161A 162A 163A 164A 166A 167A 168A 169A 170A 171A 172A 173A 174A 175A 176A 177A 178A 179A 180A 181A 182A 184A 198A 199A 200A 201A 202A 203A 205A 206A 207A 208A 209A 210A 211A 212A 213A 214A 215A 216A 217A 218A 219A 220A 221A 222A 223A 224A 225A 232A 233A 234A 235A 236A 237 A 241 A 242A 243A 244A 245A 246A 247A 248A 249A 250A 251A 252A 253A 256A 257A 258A 259A 260A 262A 264A 265A 273A 274A 275A 276A 277A 278A 279A 281A 282A 283A 286A 287A 286A 289A 290A 291A 292A 293

ARE 1ARE 2ARE 3ARE 4ARE 5ARE 6ARE 7ARE 6ARE 9ARE 10ARE 11ARE 12ARE 19ARE 25ARE 27ARE 28ARE 29ARE 30ARE 31ARE 32ARE 33ARE 34ARE 35ARE 36ARE 37ARE 36

C 0 S

LOCATION BEDROCK WEIGHT (kg) N.T.S. *6mn

Total Frac.

52B/12 netaseds528/12 metaseds52B/12 aetaseds52B/12 metaseds52B/12 metaseds528/12 netaseds52B/12 metaseds52B/12 netaseds52B/12 netaseds52B/12 volcanic528/12 netaseds52B/12 metaseds528/12 metaseds52B/12 netaseds528/12528/12 netaseds52B/12 netaseds528/12 metaseds52B/12 netaseds528/12 metaseds52B/12 netaseds52B/12 metaseds528/12 netaseds52B/12 netaseds52B/12 metaseds52B/12 metaseds528/12 metaseds52B/12 netaseds52B/12 metaseds528/12 metaseds528/12 netaseds52B/12 metaseds52B/12 metaseds52B/12 netaseds52B/12 metaseds52B/12 metaseds52B/12 metaseds52B/11 netaseds52B/11 metaseds528/11 netaseds528/11 metaseds52B/11 seds/granite528/11 seds/granite526/11 metaseds52B/11 seds/granite52B/13 granite52B/13 granite52B/13 granite528/13 granite528/13 granite52B/13 granite52B/13 granite528/13 granite52B/13 granite52B/13 granite52B/13 granite528/13 granite528/11 metaseds52B/11 metaseds528/11 metaseds52B/11528/11 granite528/11 amphibolite528/11 migraatite52B/11 migmatite528/11 nignatite528/11 aaphibolite528/11528/1152B/11528/11 granite528/1152B/13 volcanic52B/13 volcanic52B/13 volcanic528/13 volcanic528/13 volcanic52B/13 volcanic528/13 volcanic52B/13 volcanic

, 528/13 volcanic528/13 volcanic528/13 volcanic52B/13 volcanic52B/1452B/1452B/14528/1452B/14 granite528/14 granite/seds52B/14 granite52B/14528/14 granite52B/13 granite526/13 granite52B/13 granite528/13 granite528/13 granite528/13 granite/seds52B/13 granite/seds52B/13 granite52B/15 metaseds528/15 gabbro52B/1552B/15 diorite52B/14 netaseds528/14 metaseds52B/14 granite52B/14 granite52B/14 granite528/14 granite52B/14 granite52B/14 granite52B/14 granite52B/14 granite52B/14 granite52B/14 granite52B/14 metaseds528/14 metaseds528/14 metaseds52B/14 metaseds52B/14 netaseds52B/15 granite52B/15 granite52B/15 granite52B/15 granite528/15 granite52B/15 metaseds52B/15 granite/seds528/15 granite528/10 granite52B/15 metaseds528/10 pegmatite528/10 netaseds52B/10 granite52B/10 granite528/10 granite52B/1052B/10 metaseds52B/10 granite528/1052B/1052B/10 granite52B/10 granite528/13 granite528/13528/13528/1352B/14 sheared vole52B/1452B/10 volcanic528/10 migmatite52B/1052B/10 granite52B/10 migmatite528/10 nigmatite52B/10 nigmatite52B/10 Migmatite528/10 granite52B/10 nigmatite52B/1B granite52B/1052B/15 netaseds528/10 metaseds52B/10 metaseds52B/10 metaseds528/10 nignatite52B/10 nigmatite52B/10 granite52B/10 granite52B/14 mafic vole528/14 sheared vole52B/14 sheared vole528/14528/1452B/14 sheared vole52B/1452B/1452B/13528/1352B/13 52B/15 sheared seds 52G/03 granite52G/03 intrusive52G/03 mafic vole52G/0352G/0352G/G3 migmatite52G/03 granite52G/03 granite520/03 granite52G/03 granite-52G/0352G/0352G/03 granite52G/0352G/0352G/03 mafic vole52G/03 mafic vole52G/03 granite52G/0352G/0352G/0352G/03 Mafic vole52G/0352G/03 metaseds52G/03 nafic vole52G/03 volcanic52G/0352G/03 sheared vole52G/03 sheared vole52G/03 sheared vole52G/03 sheared vole52G/03 volcanic52G/03 volcanic52G/0352G/03 iron fra52G/03 volcanic52G/0352G/03 metaseds

52B/1352B/13 volcanic52B/13 vole/granite528/1352B/12 metaseds52B/1252B/12 metaseds52B/12 metaseds52B/12 metaseds528/12 metaseds52B/10 granite52B/15 granite528/14 granite528/14 metaseds52B/10 granite528/10 granite528/10 granite52B/10 granite528/10 granite52B/10 granite52B/10 granite52B/1Q granite52B/10 granite528/10 granite528/10 granite528/10 granite

no. of samplesminimum valuemaxinuB valuenean valuestandard deviationvarianceanomalous threshold

28. 022.926.832.024.525.423.421.324.323.021.120.820.624,728.027.030.018.720.427.021.021.720.925.524.128.024.727.022.933.023.223.423.219.424.322.530.029.028.027.028.026.536.037.028.026.725.020.821.025.420.521.428.023.521.025.227.526.926.226.624.129.820.126.726.126.725.626.620.821.326.726.622.414.018.420.221.714.617.123.421.024.324.822.022.423.923.922.523.820.722.024.119.518.021.521.920.622.315.025,823.228.028.326.634.431.121.524.519.730.026.421.123.327.020.030.018.730.023.521.524.327.016.326.430.919.826.224.521.024.226.823.414.718.022.319.025.823.633.024.221.926.728. 021.726.722.035.028.026.526.824.823.020.824.227.026.425.920.430.430.830.020.425.027.022.417.522.123.621.123.621.019.517.227.025.516.619.221.727.324.127.3 22.9 23.827.026.327.528.031.020.823.932.118.921.423.530.018.521.429.027.527.427.227.030.017.226.017.015.519.019.030.016.829.017.519.530,018.919.325.116.223.1

25.329.329.033.224.630.328.232.032.331.025.724.726.3IB. 920.822.829.428.226.828.323.826.825.622.021.323.2

24614.037.024.44.2

18.032.9

7.67.3

9.07.4

11.110.39.48.72.87.94.55.04.03.4

12.42.50.84.92.41.15.46.2

10.15.08.51.83.67.31.95.60.610.43.43.43.43.48.68.44.33.04.912.415.27.6

15.35,39.34.63.49.8

13.5L2,06.09.27.89.4

14.48.22.40.60.94.68.82.29,90.88.61.02.3

10.49.46.31.94.09.36.50.03.99.75.84.57.24.53.94.53.2

11.67.4

12.610.211.86.47.17.85.13.65.57.0

11.17.20.95.74.76.25.22.36.65.07.74.39.48.89.06.5

10.76.4

22.36.89.03.9

12.01.35.5

10.82.27.63.93.86,36.27.02.52.42.43.32.62.66.42.54.99.82.01.37.83.64.35.210.812.94.33.67.41.90.85.65.46.28.3

24.09.93.69.22.91.21.23.17.31.93.4

15.09.810.111.94.86.93.84.6

11.32.47.1 8.9 4.82.74.27.4

14.22.42.43.7

10.04.63.92.9

10.92.08.45.53.74.1

12.93.34.24.03.03.83.12.22.8

12.02.67.94.74.07.72.63.55.14.35.5

3.710.49.23.92.51.83.99.96.22.72.1

11.08.08.25.33.44.17.24.06.73.50.95.52.01,30.4

2450.0

24.06.03.7

13.913.5

- compactness CS - clast size - oxidation CA - angularity - stoniness

TILL DESCRIPTION

C 0 S CS CA

3110211111111101122221111111134352333322322133423121332223221112121111112352243222322212243323333334422123111111112213211224343532333221243322421001121111212211111211112122222213232 3 32222232323233333322233434333333333323

11211121231132111111111111

2442555555555454545545535143421442432224322133123222313432334455553244212121021323223333433333333330433333244444555343322343343432254232322323123414214553444444344455555513422233222 4 33341434144332245223334444434432332235

33455453531334331233330333

55354555525332255152235453335222512322232334254222254443354211241515154532233034333342143334233213255L2222142413554444221423434442542322233234213124234452133442334311334443444245423 4 22334211.1I4241423243232333333333421223

45422234530333332323315320

34134555545433132142345334233333422322322232433432333232244313241323153541243i3432332344333533333334542222143424544443231244*55445554223332242224134223442233343434411443443434322322 3 22243132232232332233234343243432433433

34433234420532331332313340

2534445554554415545455545535445533443334322122133443232324442234241212321452452244431134342523433342443232353433334441333244343554254343434423443324224514444344445514445344512321232 3 53325444343334433213333434434544344324

44445455530535341323234320

PEBBLE

Vole Int

15

10

10

30

608050605010305

5

5809530

903090405030

10080808030

10

70

401580

35

40

301007580

100

1050

5050905080

25

25

5

40

2020

10

10

105

15

2570905060

405010

5030905020205010

100100100

40802550202

10

540

40S

10

101010405

3520

7030

90

570505070804020

60

50

5010

203080604050

7050

1020205

10

50

1270

1004229869101

7030

40

6030

1020305

10

30

401020

303080

20

9060

30

1050101530105

853095

10095

100100

20

10

10101010

30

2010153010905030

407015

10065

10060

10010030

100

10010

10020

20

20805080

10010010010010010010010010010050

209580100100957070

1001001001006060

10090859090909085

1001001001001001004030105020100100604585

10010010050TO105080605090

10060207550709060 20

1001001009560

100100100inn60IfiBO

10080909060956580

1003070

109590305050302060802040

50

508050

10050203010306050

1003050959080809$90

10010050

100

2050

1006234

1189131

COUNT

Sed Other Shape

1570

601004070

1001001008080709590

10010010010070

100100100608080

100707020

10010060

1001040

10070

10090509085409030 Qtz10 Qtz504050

Qtz30 Qtz

95

Qtz6090 Qtz

60

40 Qtz5030 Qtz

QtzQtz

4090

50

2015

Qtz

40

Qtz20

8040 Qtz

25 Qtz50

Qtz40 Qtz

10080202520

2510095

100405

20

53030

2020

15

10

5

30 Qtz

QtzQtz

108

30 Qtz 70

Qtz

10

100

5

80

100

1050

506030 Qtz1010

100

Qtz

1090

1005634

1163125

AA

SAAAAAAAAAAAAASAAAASAAAAASASRAASAAAASASAAAAAAAAAASASRSRSASRSRASRASAAASASASASRSRSRSASRSASRSRSRSASASRSRSRAAASA

SAAAASAASASASASAAAASASAASRSAAAASRSAAASASRSRSRAAASASAAAAASARAASRASRSRSASASRSASASASASASASASRASASRASASASRAASAASASASRSRSASRSRSRSRASRSRSRSRASRSRSR-SASASRASRSRSAAAASRSRASRSR-SAASRA A-SR A-SASA-SRSA-SRSA-SRASAA-SASAERSASARSASRASASASAA-SASA-SRSAAAAAAAASASAAASASAAAASA

SRSASARSASASASAASASRASAASRSASRASAASASAASR

A

SR - sub rounded SA - sub angular BULK TILL RECONNAISSANCE PROGRAM del - delicate

TOTAL GOLD GRAINS

01

00100131000501010130312420000010000011000010100020021020200000020100000000003101

110000213001000001200011000000020000000010000010000541425021130020272110000000100200001000001000101 10002100001000I020100010100000100000000

1000011000

1101220200

2460

111123

GOLD GRAIN DESCRIPTION <.05 mm .05-. Inn .1-.2 nun .2-. 3 mm .3-. 4 mm .4-. 5 ma >.5 mm tfgt. No. Shape No. Shape No. Shape No. Shape No. Shape No. Shape No. Shape (gn.)

1 SRsample lost in concentration

1 SR

1 SR1 2 SR

1 A

2 2 A 1 A

1 A

1 SR

1 SR3 SR,SA,A

1 A 1 SA 1 A1 SR

1 A 1 A2 2 SR

1 1 SA

1 SR

1 SR1 A

1

1

1 SR 1 A

1 SR 1 del1

1 SR 1 SA

2 SR

1 SA 1 SA

1

1 SR 1 SR1 SA

1 SA6 A 2 A 2 SA,del 1 A

1 SR1 SA1 1 SR 1 A

1 SA

1 A1 A

1 SR1 A

2

1 SR

1 A

4 2SA,2SR 1 A1 2 SA 1 A

1 SA2 SR,SA 2 SA,SA2 A4 2SA,2SR 1 A

2 SA,A1 SA

1 A3 2SA,A

1 SA 1 SR

1 1 SA5 2SA,3A 2 SR,del

1 SA 1 A1 A

1 SA

1

1 SA 1 R

^

1 SA

1 SA

1 SA

1 SA 1 SR

1 SR1 A

1 A

1 SA

1 A

1 SR

1 SA

1 A

1 A

1 A

1 SA

111 linn iiiiiiiiiiiiii mil ii iiiiiiiiiiiiii nilIll II III II III III II III II II III III III III III111 ii 111 ii in in ii linn ii iiiiiiiiiiiiii mi52F04NE965C 63.6161 ADRIAN ^50

1 SR1 A

1 SR2 SA A2 SA A

1 SA 1 SA

11 29 49 22 5010106452121111211002110053312

37.445.6

39.132,635.742.538.433. B21.943.338.544.136.440.943.939.426.940.427.939.230.347.446.747.631.743.842.431.248.126.835.646.944.235.433.040.649.445.445.337.946.235.142.847.744.540.140.028.138.326.930.044.837.832.935.541.542.237.439.944.237.531.130.233.748.130.838.430.327.532.232.641.831.142.835.741.231.637.3

1 A 31.132.438.037.946.445.438.627.933.9

1 SA 37.441.129.523.421.646.523.733.824.534.226.428.4

1 SA 39.$32.531.936.548.030.522.236.641.240.827.421.322.943.239.043.439.540.236.116.822.229.931.031.124.726.724.336.928.216.730.623.020.026.632.736.432.436.930.729.340.136.837.443.839.428.633.130.836.849.927.931.834.926.034.324.232.826.626.538.638.323.637.335.223.219.934.630.218.931.122.423.435.528.739.730.745.435.639.443.135.1 44,9 34.341.938.9

1 (.6x.3J 32.645.639.622.835.034.631.6«3.«21.836.825.547.7

1 1.5X.3) 43.335.333.932.733.733.244.546.132.339.343.330.845.045.439.842.552.143.951.233.235.9IB 1 JO. L

43.5

44.130.635.639.434.431.6

1 SA 41.121.139.929 3t, J . tf

37 1 *j t . x31.734.833.124.737.141.218.444.549.238.536.646.927.136.028.7

4 2 2451 1 16.71 1 52.11 1 35.50 0 7.50 0 56.71 1 50.5

CONCENTRATE

CONCENTRATE Ultraviolet NOTES FORMALIZED VALUES Hag Py Gar Misc. lanp Rad GOLD GOLD \ \ \ Sch Zir 9«ins microgra

1035

252040301015tr303530153515

1050252010151050101535172515301525105

153025503020201515205

1015153020105

4030

1510152515101015102020155

201525156010405

20

407025355550205

153015

5253055

155

253015153025255

15106015202050tr506010105

15201540201025256040

40102515151530202030203525252025151530254020151515401520252010201510201515401053

153025253035301535 15 302520304030tr20701560754520354015306050354020302020253030

2560355030153030

fin ou402550tr10onQV10153020101015201025101020203025153020

2390

BO241523255

3tr

552

trtrtrtr2

trtrtr55

0trtrtr5222

tr023

trtr00

tr02

tr2

tr25

tr000

trtrtr1

tr22220

tr

trtr0

tr00

trtr2

trtr0

trtrtr10tr101020205

trtr1033

trtrtrtr0

tr

trtr0

trtr024

tr0000003

tr3

tr00

tr0330

trtr0132

tr2

tr32

tr

tr0

tr22

trtrtrtr335552

trtrtrtrtr0

tr2

tr0200502

tr2

tr0522

tr100150

trtr000

trtr 5

15trtrtrtr6

trtrtrtr2

tr0

tr00333333

trtr2

trtr2

tr

52023

tr05

3trtrtr2

trtrtrtrtrtr3

tr3

tr2

trtr222

10

tr3

tr

2400

202397

1020

22

trtr5

tr00

tr00

trtr

tr0

tr00020

tr5555500

101005

20501555

tr0005050000

trtr

1010tr55

tr10505

tr050

tr10153533

15

trtrtrtr1000

205

tr0

055

tr105330050

tr50

tr500000000

tr00000

tr200

10tr50

00

trtr3

tr54

103

tr2055

tr55555

1045520255530

tt55

tr5

trtr0

trtrtr1055

tr05

155

10 5

trtr0

tr550205522

3010tr0

10100505

tr35505

0010

tr532

5050020

tr0252

tr5

tr03002355

3

2370

4535

3014

01

00111i00101100111100101000211121112211102110011011000022121111110110011101012011111021110101100011131120010110111011211100121112101I011

. 1110110100112012111111112111010110011000121 1 11102

Sph 1010101010000000

Sph 001i10100

5 01101100

11110111001001100210101110

245031102

13

0112120111220111121001221111102101120211101221121222212222212212021111220111212221121211112111121121111122211122111020122312121210212122221321211221111012122222312112011122110112 2 21221111211211211322221221220112121111

21220111222212313223232212

245031103

0 basal \0 basal

0 outvash0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal '0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 sandy basal0 silty basal0 sandy basal0 silty basal0 basal0 sandy basal0 sandy ablation0 ablation sandy0 loany basal0 gravelly basal0 gravelly basal0 sandy0 basal0 gandy0 basal0 gravelly0 nixed0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 ablation0 basal0 ablation0 basal0 silty clay basal0 clayey0 basal0 basal0 sandy clay0 sandy clay0 ablation0 basal0 sandy0 basal0 basal0 sandy0 silty basal0 silty0 ablation0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 silty basal0 silty basal0 basal0 silty basal0 silty basal0 silty basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 ablation0 silty basal0 silty basal0 basal0 stoney basal0 sandy0 good till0 basal0 basal0 sandy0 basal0 basal0 basal0 gravelly0 basal0 basal0 basal0 basal0 basal0 basal0 sandy0 basal0 silty basal0 basal/ablation0 sandy0 sandy clay0 sandy0 basal0 silty0 silty0 basal0 silty0 sandy till0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 silty basal0 silty basal0 basal?0 sandy till0 silty0 basal0 sandy basal0 sandy0 sandy0 silty clay0 sandy basal 0 basal 0 basal0 silty basal0 sandy basal0 basal0 sandy basal0 silty basal0 silty basal0 silty basal0 basal0 silty basal0 ablation sandy0 basal silty0 ?0 silty basal0 gravelly basal & ablation0 good silty basal0 basal0 silty, sandy basal0 silty ablation0 ablation0 silty basal0 basal0 silty basal0 basal0 basal0 silty basal0 basal0 basal0 basal0 basal0 basal0 basal0 sandy basal0 silty basal0 silty basal0 silty basal0 silty basal0 sandy basal

0 sandy basal0 basal0 basal0 silty basal0 basal0 silty basal0 silty basal0 basal0 basal0 basal0 silty basal0 loany basal0 basal0 basal0 basal0 silty basal0 silty basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 silty basal0 silty basal

::sss========;:=========;s=:===s:==S3B«e(

247000000

01000100132000401010140412320000010000011000020200050031030200000020100000000004101

1300002250020000013000110000000200000000100000100006413240211300103

102110000000100200001000001000101 100021000010001020i00020200000100000000

10000110001020001101210200

2460

131124

2.221.0

24.72.6

13.24.71.2

26.03.6

13.15.9

12.99.6

27.19.0

13.53.0

13.13.34.07.0

34.519.69.05.34.58.9

11.524.214.726. B5.4

10.96.92.78.018.69.48.97.6

15.814.12.0

30.10.20.10.20.10.10.20.82.20.1

12.90.11.862.215.23.8

17.71.19.31.31.20.23.62.61.82.52.00.10.23.36.64.04.80.10.976.123.529.77.5

15.76.85.79.85.0

148.15.7

79.863.34.911.45.29.75.04.7

13.310.762.00.50.11.34.14.10.114.24.2

11.040.81.2

17.122.6

125.710.665.71.72.62.00.11.1B.I0.46.71.51.00.15.83.26.60.45.229.810.13.43.01.9

20.30.5

15.13.02.25.10.38.61.41.21.521.41.90.90.60.11.70.71.11.51.05.30.60.21.93.32,20.21.10,10.90.6

12.525.81.1

24.812.11.10.20.50.92.71.3 1.91.50.11.9

44.02.40.10.76.61.0

16.00.10.12.26.70.236.91.03.5

52.35.21.01.10.80.10.20.23.24.60.20.11.51.12.60.21.61.03,61,2

25.06.63.93.60.8

12.9106.3

4.16.328.20.14.54.64.04.02.3

14.59.71.66.94.40.90.1

27. 71.12.7

2460.0

148.19.7

18.4340.346.6

Au ppb

det 5

59361

730692657318

60016620012522927481915147399

2521461021895373251811631192462907874858597419520679

26238520122325836947950

646333333

11393

2333

3892236711547343

23339443

1146160875033

6111261883

16168055077717429713814336577

325056

16001290147167143241171115202279

1250223

3B120176

334975300

165034

543471

2170236

10201660753

4419512

27449383

17817221516

15881731173

10956

86620

3206978

1207

276674433

300812B12

3652933414047158

401129910303

4619

17053711

660316IB3

12196838 30 403

521370

363

2119731

36533

56211

31000

34118

1140182411719333

859333

2317673

37285724

61619910713338

5713100211209

13804

9812265

12860

44655942

152115353

103032

108

2453

3250242427

1823501096

Au Agmgn ppn

5

2.216.4

28.52.29.53.10.7

20.33.68.64.8

10.19.9

33.36.6

18.62.7

10.14.04.05.7

25.415.18.65.15.210.49.0

37.612.930.63.58.77.32.6

10.619.09.210.19.817.016.72.1

30.70.10.10.10.10.10.10.31.70.17.60.11.638.813.74.6

20.81.67.21.21.50.14.42.31.82.41.60.10.12.04.B2.23.60.10.6

52.117.829.46.6

13.86.35.5

10.22.7

121.42.3

47.138.93.26.23.68.14.23.95.37.9

49.60.70.11,45.75.40.112.83.1

12.245.10.7

12.420.484.910.240.40.62.21.30.11.36.00.46.81.30.90.15.02.96.80.43.223.210. 12.63.52.0

27.00.6

12.82.52.95.20.37.92.21.41.2

14.91.90.90.40.12.20.71.11.11.11.80.60.21.53.92.30.21.00.10.90.63.8

12.50.418.812.50.60.10.40.72.91.3 1.31.40.12.144.21.60.10.66.91.1

11.40.10.12.15.5O.I43.41.24.1

37.16.21.40.80.90.10.10.12.64.20.10.11.00.92.90.21.21.02.21.0

27.06.23.95.20.918.4

129.24.68.2

39.90.13.14.22.13.12.2

18.310.21.97.54.41.30.1

27.71.13.1

2460.0

129.28.5

15.7247.940.0

33

3333373333333333333333333333333333333333333333333333333333333733333333333333333333333333333333333333333333333333333333333393333333333333333333333333333333333333333333333333333633 3 33333333333333333333333333333333333333

33333333333333333333333333

245393104

Asppn

2

711

236456

1214381591429252434635169

1606797234

947

191155353184316713101111111111115417111111311111184

76111

121873116415491931384422411112

26131241123414113111112131232111111111111531111511151241151441

2235

13033557324 3 11111I41111111115131111111311111111171

5533

1120

13013015

1101535121112111114

2451

1609

2250153

Ba Brppn ppn 200 5

100300

100350420100320100550330100590260100330350100100370230100310240270100100420590100480100250100100100100290310380100100100220350100340100450

, 100100100310390370390430520480380340250320540310100100360100100430100310100100100100100370250280100310240220340100100450100240210320100280470100360330100390290100100230100100290400100100550100230300300200360320100100300460350480400100100320100360460580460340100100480100100100460100100430100490490100270510240350590100100430100100100100450100100530100380100100260100310410100440100100320400350390100 100340100100210250610100330100100100250100220310390350320200100280260370240480100290320100400100440100100100100300

300460290400460100360100100310100310100100100100100100100100100100330100100100

245100610241148

21779536

33

3333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333353333333333333335333337333333333333333333333333333333333333333333333333363333333333 3 33333333333333333333333333333333333333

33335333333333333333335533

245373004

Ca \1

11

1321136114131111111111111311411514123331131111111111112111311113114411111141111111111111111121121131311311315711212111111131121331111311114111111231111511111114141114444311312143 3 11112111111111111111121111211111112111

13111111111131111111131131

245172114

Co ppn

5

1415

452521212624182520212162293627333132301731251629252519202429221824152523192125233020239

IB20162317121322221121192421202319271327292235242421258429351826282835302024172128321322221716342215192234153642513349272020233522452418202331352535372145282629283627303015764748483931295751242524252521232958414944293029224533422842293549374553412927483523272839382342 37 4633353436262635273228462933322137344936343521332525354422282519242121362524

2427293020452443323535463428564427513430462717722863

2459

843011

12953

Cr ppn 10

190390

400380310290320320170280300260540550370370340420550250250no2402902502502802303003102702902502302504003703702804604306005103103502301704403703602001401505102902003003905404604403803104401808205502704604204402703701904402202103007604104803003203601602403102801202802501602003702601402001603901905607207005509604703201903705202508603202103703304004502403204902203208BO200680230460440610360110500320400350340520250320270580310820360440270380560490310290440250260190190330290290280440530190450450580620350170210320

2000830440490680570180420 530 340280340470440340340440480490330620390330260250310340450480370340250360290180360340190250280160260iao180470250240

420310370350190670270370370350500770410610460340370940240300320340260480210490

2451102000373187

34936747

Cs ppn

2

11

11112511121111111114112113111121313131111111111111111111111131311123311111121111111112111111311111111111131111111111111111111121111111115111411111.11111111111131131131111111111131 111111111111111111113111311111111111311

11111111111331111111111111

245151103

Fe t0.0

7.315.5

16.420.324.816.57.8

12,16.8

16.512.78.012.926.613.616.114.121.520.914.229.415.219.315.86.9

19.717.010.913.67.58.8

16.59.69.49.37.817.715.010.710.715.713.416.410.515.46.3

10.914.07.2

19.014.66.46.0

15.615.710.011.711.613.114.38.1

14.012.814.7fl.O

10.316.99.816.614.114.413.513.712.39.6

16.26.3

15.420.526.234.520.519.716.710.314.710.919.85.5

15.918.110.310.616.812.15.7

10.67.720.09.211.014.820.716.923.29,811,410.814.531.513.329.814.36.7

11.413.512.314.710.011.316.310.221.015.814.011.811.218.612.313.519.65.732.818.520.621.013.012.114.223,721.611.29.2

19.621.629.214.812.813.925.316.718.913.610.413.114.612.323.714.317.010.015.410.39.618,116.421.721.818.320.27.19.819.415.39.5

13.218.322.98.0

22.9 15.5 21.820.827.929.322.717.313.415.518.218.719.731.624.317.416.215.319.225.227.628.226.820.312.720.718.611.223.127.412.419.014.410.519.512.824.814.613.114.2

21.317.820.219.77.1

24.526.828.217.726.111.619.414.915.426.718.19.820.613.812.720.99.65.7

31.410.526.1

2455.534.515.96.0

36.428.0

Hfppn

1

5150

1644323929443635402865272928503379221611U326513214050

130612335503983252927

1103763192122783190100893943

120656021204240517252473516

13019416130344961355832494364574851552559

11028533344834056784226492763466941342753616142946247

2105154575724676750555730

1505889505993604188322938285894683333

11064689454100533970382984684931355253264735

110645530499938131613

11040652924535062 26 392828231928685834311250403417155739486227303454242537111920162119IB20462841

5352605444362125462076382675594653

1002736205148444575

24511

2104827

712101

Hg ppn

5

33

3333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333 3 33333333333333333333333333333333333333

33333333333333333333333333

245333003

Ir ppb 40

2020

202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020 .20202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020 20 2020202020202020202020202020202020202020202020202020'

202020202020202020202020

2020202020202020202020202020202020202020202020202020

24520202000

20

No ppn 20

1010

10101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101067101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010 10 5510101010101010101010101010101010101010101010101010101010101010101010101010

1010101010101010101010101010101010101010101010101010

2451067105

2120

Nappm 500

1740012300

14100142001330011800155001540017400118001570017600137006970

1550015000141001250010600118007770

12600111001260015400106001490015700158001670016400123001400014100148001410012600 .14300 •1500014700155001570014200147001580016800161001590017900149001940020000181001440015200194001450015200149001390015500125001380015000157001390014500132001100014600136001560017400147001500015300184001390013600116009560

13500118001480017600157001550011500168001360014800155001590011600133001460016400145001500014400124001080010700125009970

141001450014800139009870

12500755012400169001560014700160001500017900171001560016800136001670019400218001890016300197001870021300176001120014900136001440015400183001480011000160001710017800166001700017000191001390014700136001420013600127001290016600150001770097301300013900170001480016100176001210014900131001130015500942020100135001150016500164001800017SOO172002060016400 9560 93901170086408790

11400133001410012800157001280013800105001010016100148001470013&00135001330012400107009970

1460012100108001480012600104001450013300124001380011600128009410119001240012700

124001560014000128001BOOO149001150013200129001130015600112001520014700823012000154001170012900127001120012900236008200

126007660

245755023600142412710

734415519661

ASSAYS

Hi ppm 200

100100

100100100100100100100100100100100100100220100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100230100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100310100360100240100100100100100220100100100100100100100100100200100100100100100100100100220100100100100100100100100100100 100 100100100100100100100100100100100100100100100100100100100100100100100230100100100100100100100LOO100100100100100100

100100100100100100100100100100100100210100100100100100100100100100100100100240

24510036010631

983169

Rb ppn 50

5425

25256725652525255664255255602525612525522525642525252525252525255625252525252525602550502525258025682525255825255925622525252525252525752525256225552525782525252525252525252561612555255925752525252525252525252525252525252525252525252525252525257225252551252525252525252525252525252525912568252525252525252569252525252525252525722525256087252525582525255525 25 255225252564255452252525552525706125

10078668125252552562525252525542525252525

2525602525252525257625252525252525252525252568252525

24525

100341728968

Sb ppm 0.2

0.40.8

3.10.60.30.10.10.11.02.20.80.31.22.11.92.62,23.52.93.76.24.25.11.6O.I4.90.51.20.50.10.50.30.10.10.40.10.30.40.10.10.50.10.60.10.10.10.10.10.10.10.10.30.10.10.10.10.10.10.10.10.10.10.10.10,10.10.10.10.10.10.10.10.30.10.40.10.10.40.10.50.10.3

12.00.40.10.40.10.40.10.10.30.60.10.40.30.10.10.50.60.50.10.40.90.30.10.10.10.10.10.10.50.10.10.10.10.30.10.50.60.10.10.10.30.10.10.10.10.30.10.30.10.30.10.10.10.10.10.40.10.10.10.10.10.10.10.10.10.10.10.40.60.10.10.10.10.10.10.10.10.10.30.10,10.30.10.10,10.10.14.30.61.6O.I0.10.20.11.10.30.10.3 0.4 0.10.30.10.10.10.10.40.10.10.10.30.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.60.10.10.1

8.20.10.10.10.61.86.17.50.95.60.10.40.10.70.10.30.10.90.10.10.10.10.10.10.10.1

2450.1

12.00.61.42.13.5

Sc ppm

0

2017

1118U172020171617161815181521163218111211132312U231332201624312737182117442133222820261822232016131917178

33251721274752IB19311520221312202916271726191913121413121417301812141717142717191321201335342617264018172314242915171418192427282316193018252116292515IB262321182426442123332216211021191531202540302125162321162026283743212636172722342814331818212521 21IB19151616172924131711221132169

23202017182115221920271413131814121314272014

1416171620161216171325202123242230391717183118262034

2458

52217

5335

Se ppm 20

1010

10101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010 101010101010101010101010101010101010101010101010101010101010101010101010101010

1010101010101010101010101010101010101010101010101010

2451010IP00

10

Sr Ta * ppm 0.2 1

0.10.1

0.10.1O.I0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10,10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1O.I0.10.10.10.10,10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1fl.l0.10.10.10.1fl.l0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1O.Ifl.l0.10.10.10.1 0.1 0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10,10,10.10.10.10.10.10,10,10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.30.10.10.10.10.10.10.10,1

2450.10.30.10.00.00.1

15

46

13443114333211321132211134734114134366

2031763177658744

1213

1767

11556534411531155725314111213341511111411235333751711234414331115I243124351466416156675444181145541224141252121

105333745 1 44665454454655233515631321112232431544

24332321122121112512211224

2451

203368

Th ppm

1

1526

U1521251118131418131923U181613289656

13157

1311193016139

14112213121019142598

17371730404336274342402579

111018162111103013153090933033162921252564142018161113231023122119121524221919113122141111101817221327331662202024166

141114121110

13040172019432713312716342948

1301206350

190160243625451412

1106150

11036777746916365308

20354416142913667

522915159352446 8

212029252117312915291945213716191929262939141516151023139

141114211312261414

2118232116289

111511

240141610

11053B8

2702935242625191521

2455

2702933

106994

U

0.5

5.35.4

4.73.34.65.03.85.24.94.33.73.65.04.93.23.24.61.07.43.31.81.11.13.53.70.71.03.42.87.95.31.42.24.03.13.93.12.12.55.12.95.42.82.94,56.33.86.77.06.24.24.17.24.95.72.61.75.33.02.75.02.92,62.83.07.61.13.25.66.26.73.94.04.14.13.74.63.39.23.13.94.53.02.42.95.13.65.12.54.15.33.23.45.63.83.74.83.38.34.74.22.81.00.73.54.94.62.55.95.04.9

11.02.63.43.63.91.95.93.54.53.02.82.9

12.05.66.34.54.98.53.82.3

36.03.82.63.33.05.1

11.09.05.54.6

17.018.04.39.06.19.23.72.9

12.07.76.6

12.06.0

14.014.08.511.06.15.63.02.5

11.07.85.22.13.57.75.41.71.71.05.73.43.13.63.77.B5.65.4 1.44.63.74.33.81.82.56.15.02.54.42.47.06.35.62.43.65.25.63.99.35.03.92.83.14.12.14.13.31.73.82.43.01.83.02.16.23.64.0

4.03.25.34.75.94.31.53.34.22.230.04.31.93.0

13.05.910.019.03.74.02.75.36.53.21.53.9

2450.7

36.04.93.814.512.5

Vppm

4

22

22822522227

172222

10222222222

1122

10222

15141527

5525132222222222222

19152

4022228222222292222

106122224222227

112222222222

18072

15222222222222

172

128222

212242522

452222

10119

1844222222222222

122

111622272222222292242225

382

15 12222

152222422222222222222222

242225222222

2222222222

13226222222222222

2452

1806

1419033

Zn ppM 200

100100

100100100100100100100100100100100230100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100230100100100100100100100100100100100100100100100100100100100200100100100100210260100100100100100100100100100100100100100100230100220100100100100100100100100100100100100100100200230100230100100100200100100100220100310240280210100100100320310200100100100100100100100300100230100100100100100100100250100240100100210100200100220100100100100100100100230100100100 100 330210100100210100100100100100100100100100100100210200200210220100100LOO100100220200100100100100100100210100100100

100100100100100100100100100100100260100100240100100100100100100100100340100230

24510034012354

2883231

1

1

1

22

1

1

1

3i:

1!

'

1.

1!4312:I-5(4!

i

U

2!11i:2<i;2!2'

3:1'23

E•

U

t

i1<'<

1'tti•'

(t

4c

5446736195

1034555573332212232342'

25l3i3!

5'11615:4'613(3'4(3:

6313t4<21

28C15C23(63C719fi64848!514255

24518

6307890

8022257

Table 5 MINE CENTRE AREA

SAMPLE No.

H 1H 2M 3 K 4 H 5 H 6 H 7 H 8 H 24H UL Zb

M 26 M 27H ID 10

M 29 H 30 M 31 H 32H 11n JoM 14n jiH 35H 36M 37H 38M 41H 42H 43H 44M 47H 48M 49M 50K 51M 52M 53M 54H 55K 56 H 57 H 58H 59H 60H 61M 62H 63M 64H 65M 66H 67M 68H &9M 70H 71M 72H 73H 74H 75H 78M 79H 80H 90H 91 H 92 H 93 M 94 H 95 H 96 M 97 M 98 H 99M 100M 101 M 102M 103H 104H 105M 106M 107

HCN 1HCN 2MCN 9MCN 10MCN 11HCN 12MCN 13MCN 14MCN 15HCN 16MCN HHCN IBMCN 19MCN 20HCN 21MCN 22HCN 23HCN 24MCN 25MCN 26MCN 27MCN 28MCN 29MCN 30HCN 31MCN 32HCN 33HCN 34MCN 35MCK 36MCN 37HCN 38MCN 39MCN 40MCN 41HCN MMCN 43HCN 44 HCN 45HCN 46MCN 47MCN 50MCN 51MCK 52HCN 53MCN 54MCN 55MCN 56MCN 57,HCN 58HCN 59MCN 60MCN 61HCN 62MCN 63HCN 64MCN 65

MRL 1MRL 2MRL 3MRL 4MRL 6MRL 7HRL 8MRL 9MRL 10MRL 12HRL 13MRL 15HRL UMRL 17MRL 19HRL 20MRL 21HRL 23HRL 24HRL 25HRL 26MRL 27HRL 28MRL 29 HRL 37 MRL 33 MRL 40 HRL 41 MRL 42 MRL 43HRL 44 HRL 46HRL 51HRL 52MRL 55MRL 62 MRL 63MRL 64HRL 65HRL 66 MRL 67

HRE IHRE 3UDP C HKCi 0

MRE 7 HRE 8 HRE 9HRE 10 MRE 11 MRE 12 MRE 15UDG1 1 £nKCi laMDC1 1 7nKii 1 /HRE 18 UDP i QflKfc L JMDC1 1 1nKfi i iMRE 22 MRE 23 MRE 24 MRE 25 MRE 26 HRE 28 HRE 29 MRE 43 MRE 45 HRE 46

Gfl 123A GB 124 GB 125GB 126 GB 127 GB 128 GB 129 GB 130 GB 131 GB 132 GB 133 GB 134 GB 135 GB 136

-

LOCATION BEDROCK H.T.S.

52C/09 fault brcc.52C/09 sheared vole52C/09 granitetvolc 52C/09 granite+volc 52C/09 52C/Q9 mafic rock 52C/09 mafic vole 52C/10 sheared vole 52C/09 sheared vole 52C/09 volcanic52C/09 sheared seds 52C/09 sheared seds 52C/09 metaseds52C/16 granite 52C/16 mafic vole 52C/16 mafic vole 52C/16 mafic vole 52C/16 volcanic52C/16 volcanic52C/09J L V / *J J

52C/09 metaseds52C/09 roetaseds52C/09 metaseds52C/OS metaseds52C/09 raetaseds52C/Q9 netaseds52C/09 raetaseds52C/09 metaseds52C/09 raetaseds52C/09 metaseds52C/16 metaseds52C/1652C/16 metaseds52C/16 metasedsB2C/09 metaseds52C/14 volcanic52C/14 volcanic 52C/14 volcanic 52C/14 volcanic52C/14 volcanic52C/1452C/1452C/14 intrusive52C/14 intrusive52C/14 granite52C/1452C/14 intrusive52C/14 granite52C/1452C/14 granite52C/14 granite52C/14 granite52C/14 granite52C/16 rhyolite52C/1652C/1652C/10 raetaseds52C/10 raetaseds52C/10 metaseds52C/10 metaseds52C/10 metaseds 52C/14 volcanic 52C/14 volcanic 52F/03 volcanic 52F/03 volcanic 52F/02 volcanic 52F/02 volcanic 52F/02 volcanic 52F/02 volcanic52F/02 volcanic52F/02 volcanic 52F/02 volcanic52F/02 volcanic52F/02 volcanic52F/07 granite52C/10 metaseds52C/10 raetaseds

52F/03 intrusive52F/03 intrusive52F/03 mafic vole52F/03 mafic vole52F/03 volcanic52F/03 mafic vole52F/03 sheared vole52F/03 mafic vole52F/03 mafic vole52F/03 metaseds52F/03 sheared ?52F/03 granite52F/0352F/03 metaseds52F/03 intrusive52F/03 metaseds52F/03 ultramafics52F/03 metaseds52F/03 metaseds52F/03 metaseds52F/03 volcanicS2F/03 mctaseds52F/0352F/03 metaseds52F/03 mafic vole52F/03 mafic vole52F/03 granite52F/03 granite52F/03 mafic vole52F/03 mafic vole52F/03 metaseds52F/Q3 seds/granite52F/03 vole granite52F/03 granite52F/03 mafic vole52F/03 mafic vole52F/03 mafic vole52F/03 52F/03 mafic vole52F/03 mafic vole52F/03 volc/seds52F/03 felsic vole52F/03 volcanic52F/03 volcanic52F/03 sheared vole52F/03 volcanic52F/03 mafic vole52F/Q3 sheared vole52F/0352F/0352F/03 volcanic52F/03 granite52F/0352F/03 sheared vole52F/0352F/0352F/03

52C/1552C/15 intrusive52C/1552C/15 granite52C/1552C/15 granite52C/15 granite52C/15 granite52C/15 migmatite52C/15 migmatite52C/15 intrusive52C/15 intrusive52C/15 granite52C/15 migmatite52C/15 raigraatite52C/1552C/15 granite52C/14 granite52C/14 granite52C/14 granite52C/U granite52C/14 granite52C/14 granite52C/14 52C/14 migmatite 52C/14 raigraatite 52C/14 migmatite 52C/14 migmatite 52C/14 migmatite 52C/14 migmatite52C/14 granite 52C/11 mafic vole52C/11 raetaseds52C/11 granite52C/11 granite52C/LO volcanic 52C/10 volcanic52C/10 volcanic52C/10 volcanic52C/10 sheared vole 52C/10 volcanic

52C/10 metaseds&2C/10 raetasecls52C/0952C/09 52C/09 tnetaseds 52C/16 migmatite52C/16 wlgiwUte 52C/16 migmatite 52C/16 migmatite 52C/15 raetasedsC Of / 1 Cb/C/1552C/14 52C/14 metaseds52C/1452C/10 52C/10 52C/10 52C/10 mafic vole 52C/10 volcanic 52C/10 sheared vole 52C/10 volcanic 52C/10 mafic vole 52C/14 52C/14 52C/14 raigmatite

52F/03 metaseds 52F/03 metaseds 52F/02 mafic vole52F/02 mafic vole 52F/02 mafic vole 52F/02 mafic vole 52F/02 mafic vole 52F/02 mafic vole 52F/02 mafic vole 52F/02 mafic vole 52F/02 granite 52F/02 granite 52F/02 granite 52F/02 granite

no. of samples minimum value maximum value mean value standard deviation variance anomalous threshold

WEIGHT

Total

25.0

C - compactness CS - clast size 0 - oxidation CA - angularity S - stoniness

(kg) +6mra Frac.

8.8

TILL DESCRIPTION

C 0 S CS CA

PEBBLE COUNT TOTAL GOLD

Vole Int Sed Other Shape GRAINS

65sample lost21.0 ' '

18.6 21.4 21.5 16.3 16.7 20.8 21.520.1 23.1 17.728.0 32.0 27.0 32.0 28.023.827.024.028.029.022.220.721.020.021.021.520.537.520.422.119.419.424.517.5 15.5 15.922.523.522.921.218.517.020.914.916.221.117.527.525.222.021.523.028.025.623.620.626.018.4 28.0 29.0 19.2 23.5 IS. 3 25.0 29.0 22.424.525.9 21.523.423.927.019.818.4

34.032.031.025.934.726.524.630.028.028.030.033.034.024.828.025.021.624.319.520.126.021.520.427.024.617.224.928.026.027.028.024.422.023.120.123.616.520.8 25.819.119.721.025.324.722.624.022.020.428.025.819.319.922,030.021.618.615.0

29.020.233.029.026.021.233.025.017.024.021.022.123.524.023.519.519.422.322.919.219.624.225.421.3 18.7 14.2 19.2 22.2 16.0 14.622.117.113.015.017.024.8 19.321.122.126.8 24.7

27.528. &24,826.0 2S.2 20.5 22.3 16.4 20.8 17.521.316.9 16.422.5U c

. D

17.9 17.1 22.8 26.4 16.8 21.6 22.1 22.2 22.7 14.8

32.7 33.8 31.232.4 38.4 34,0 35.2 36.8 35.0 40.3 35.2 35.9 34.3 33.8

214 0.0

40.3 23.5 5.6 30.8 34.6

4.6 3.9 4.4 3.8 6.9 5.6 9.2 5.47.6 5.3 5.06.5 5.2 5.4 8.5 6.55.08.38.03.05.34.74.55.33.06.05.54.8

10.42.33.33.86.06.48.0 3.7 2.9

11.010.02.96.45.26.45.03.84.33.54,^4.45.53.95.15.97.58.26.412.63.03.3 8.4

12. & 4.6 6.1 4.0 9.2

13.0 3,19.45.6

13.66.75,28.70.93.5

6.07.56.33.8

12.36.98.01.17.716.08.312.38.44.28.68.72.84.34.24.55.97. a5.66.59.25.46.67.04.67.27.06.64.46.57.04.02.03.69.15.0

12.04.68.54.74.49.69.210.815.612.75.18.96.54.78.07.84.6

8.15.14.4

12.815.13.4

13.43.90.52.62.51.42.37.35.65.93.92.66.02.36.31.811.27.3 4.8 4.5 8.5

11.4 6.4 3.76.4 4.88.43.06.13.6

10.75.84.0

16.3 9.2

6.714, 011.66,96.7 6.5 7.8 2.5 6.7 4.67.75.6 6.08.08.1 4.2 3.2 5.0 8.7 4.8 9.1 8.2

6.46.1

17.0 17.5 9.29.8 13.9 18.2 8.5

16.5 20.3 9.2

19.2 8.1 14.5 8.5

212 0.5

20.3 6.9 3.6 13.0 14.1

2 4 2 1 3 2 1 3 1 1 4 3 2 3 32 2 21 3 32 1 23 2 22 2 22 4 22 3 23 33 13 22 33 2 22 5 31 4 02 4 32 4 32 4 31 4 31 4 3 1 4 3 3 0 21 4 41 2 51 0 31 1 31 1 31 3 31 1 31 4 41 4 41 2 41 ) 11 1 4I 3 41 1 42 1 22 1 32 2 34 1 54 1 51 4 51 1 21 3 4 1 4 41 b 4 1 5 5 1 4 4 1 3 2 1 4 5 1 4 5 2 4 22 4 51 4 4 1554 2 51 4 41 4 44 1 43 1 3

3 1 22 0 23 2 13 3 33 4 54 3 31 3 32 1 10 3 22 2 52 0 22 1 34 2 34 2 24 1 44 2 32 4 33 2 32 3 23 3 33 4 32 4 34 2 42 3 23 3 32 3 43 3 32 3 34 2 53 2 23 4 43 4 32 4 21 3 24 3 43 3 23 4 34 2 4 4 3 43 4 32 3 42 3 11 2 21 3 21 3 12 3 32 3 22 4 42 2 32 3 22 3 21 3 32 2 13 4 22 1 32 2 23 3 2

1 4 51 2 31 4 21 0 31 1 31 1 32 1 41 1 31 3 01 2 31 1 23 1 21 2 22 3 23 3 32 3 23 2 23 3 13 3 23 3 31 3 41 0 12 2 31 0 3 1 5 31 5 4 1 3 5 1 1 5 1 2 5 6 2 11 1 52 1 31 3 32 4 22 2 22 3 1 2 2 41 2 32 1 22 2 41 2 2

2 3 24 1 43 3 32 2 2

1 2 3 4 4 3 3 3 3 1 2 3 2 4 33 2 42 3 2 3 4 43 1 41 2 3 2 1 2 2 2 2 5 1 3 2 3 3 4 0 2 2 1 2 2 3 2 2 2 3 2 1 2 2 2 2

4 4 4 4 4 4 2 4 41 5 42 5 4 2 5 4

2 b 41 5 5 1 5 3 3 5 4 4 5 2 2 5 2 3 5 3

2 3 2 2 2 2 4 2 3 33 33 23 12 33 35 22 32 31 13 32 33 42 11 12 23 22 22 32 4 3 4 3 32 42 23 33 43 32 42 34 33 43 4S hR R3 45 42 33 42 34 45 34 53 44 4 4 5 4 3 5 4 4 4 2 1 4 3 4 5 1 45 55 4 5 44 54 53 34 41 A

2 35 51 33 45 33 42 41 51 44 51 42 32 34 43 33 42 42 42 43 34 44 54 32 33 34 43 22 33 33 42 42 32 43 42 41 32 42 4 4 42 43 52 33 32 42 23 42 32 44 32 33 22 42 33 43 43 33 4

5 23 24 24 33 23 33 35 41 44 33 43 33 44 44 45 42 34 44 54 43 41 23 4

* 2 33 3 3 3 5 3 3 3 4 4 2 42 4 4 35 53 33 41 1 2 43 14 24 52 3

3 23 &4 23 3

4 2 3 3 3 3 4 3 3 44 34 43 53 34 4 3 3 3 42 3 2 2 1 2 4 5 4 4 3 2 3 2 2 4

4 5 4 32 23 2 4 44 3

4 3 4 53 3 4 3 2 3 3 2 4 2

30 5

100 504060

20

50

7010040 25

905040405

SO40152050

2030

70 90

100 80 70 50 60 307050 70707060

10

10010

20100

7050

5030

100905060

10090704070605060

60 40

4010020

10010050

1005095

1007040

20

35403020

40

20 30 20

20 80100204020 953070

100 10

5

20

10 6510

20 701030 503585

95 60 5 20 95 60 15

15

90100 5020 25 30 60 50 70 70 50 25 20 30

129 0

100 51 29 864 110

35

20 80 70 95 100

5 95

50 6040 60 40 50 5080100 100 100

10050 5030 7050 5020 805020 80

100100

10020 8050 5070 30

100100

40 6070 3030

60 75

100100105060609510010080 20SOf,0858050

10010060 2070

100100100

30 10

20 30 50 40 303050 30303040

10080 10

100100

10 8040 6050 30

10020 80

100100

10 9060 4020 8050 50

100100

3050

40 601001005070

105040

103020 4030405040

10040 6070 30

100100

20 40

40 40100100100

50

505

3060

10010010010010010010010010010080

100100100100100100656060 1080

10060

100 100 100 8070 80

10080 20

8050

80 5

7030

90

80 155 95

7565 35 60 30 3590

100 80 309060 10 5060 515

100

4095 80 5

30 85

100 85

10

5050 30 75 70 40 50 25 25 50 70 80 70

171 66 0 0

100 100 61 62 30 33

915 1112 122 128

A SA SA SA A A

A AASA SA SA

SAAAAASAAASAAASAASRAAASA-A

A A-SA SA-SRAASASASA-SRSASASASASRSR-ASA3ASAAAAAAAAAA SA SA SA A A A AAA AAAAASA

AAAAAASAAAAAAA

AASAAAAAAAASAAASAAAAASASA-A

AA AAAASAAAAAAASAAAAAASAA

SAASASAAAAAAA

SA-SRASASASASAASASASASASAAASA A SR SR SA ASA AASA

Qtz SR-SA

SAA

Qtz 3AA ASRR SR SR ASRSASASAA SR

Qtz A SA SA SR A

Qtz SR R SA

53F04NE3650 63

4

4 6 5 62 1 0 02 2 02 4 8 1 0144130?002127331333 0 3232&3•>

1014021020233030 2 2 0 1 0 1 1 020 120064

1i4824251127152

4344316640

1403734392533240206374

12152111

1026

106

542002160100202003322410 13 2 0 1 21 00211 0400 0

1I0b1 20 2 1 2001031 2 4 3 4 0 3 1 0 0

5 420 1 2 4 4 45 ^

III6161

213 0

43 3 5

21 12

SR - sub rounded SA - sub angular del - delicate

<.05 mm No. Shape

2 SA

2

1 1 1 1

2

1 SA

1

3

1 SA14

2

4 SR

2

2

37

2

J

3

51 A1

311

1

1 SR

3

1

5

32

2 A11

1 A

1

1 SA1 SR

1 SR

i

1

30 SA-SR

1

IIIIADR 1 AN

47 1

37 3 7

44 16

BULK TILL RECONNAISSANCE PROGRAM

GOLD GRAIN DESCRIPTION .05-. 1mm .1-.2 mm .2-. 3 mm .3- No. Shape No. Shape No. Shape No.

1 SA1 SA 1 SR

1 SR 1 SA

1 A

1 SA

11 A5 2SR2A,R2 SR1 A1 SA1 SR2 SA1 SA

2 SR,SA1 A

1 R3 SA2 SR,SA

1 SR

1 SA

1 1

2 5R,A

1 A2 SA,SR1 SA

1 SA

1

2 A1 SA3 A2 SA3 SR,2SA

1 SR1

5 SA

1 A

3 A

2 SA2 SR,SA1 A1 A

1

1 R

2 SR,SA3

51 A

1 SA11 A1 SA3 2SA,A2 SA

1 A1 del.1 SA

1 A1 SA2 SA

1 SA

2 SA

2 SA,A

1 1

1 1

1 A

1 SA

1 SR

2

2 SA,SR 11 2

1 A

1

4 SA-SR12 SA-SR

1 SA-SR

3 SA-SR 1 SA-SR2 SR-R111*

4 3A,SR

•) A 01 J & Gl L AfOn i i\(3n

2 SA 1 SA 3 2SA,A 1 SA 2 SA,SR 1 SA 2 A,SA 1 A

2 A,SR 2 A

1 A 2 A,SA 2 SA,A 3 A,2SA 1

1 SA2 A,SA 1 SA2 SA,SR

1 SA3 A,2SA

1 SA

1 A

1 A1 A 1 SA1 SA2 A,SR

1 A1 SA

1 SA 1 SA

1 SR1 A3 2SA,A1 A2 SR ( SA 1 SA1 SR

1 SR

1 A3 SR

1 SA 1 SA1 SR

1 SR 1 R

SR2 SR 1 del1 SR 1 SA

1 SA 2 SA

2 R,CA

1 SR

1 A 1 SA

i SR 1

1 SA2 .SA

3 SA,2A4 2SA,SRA

1 SA

2 SA,SR1 A 11 SA1 SR 1 A2 A

1 A

4 2A,SA,R 3 2A,SA1 A

1 A1 A2 SA 1 A2 A,SR1 A1 SR1 A5 2A,3SA 1 A1 SA 1 A3 SA

9 SA 1 A

2 SA 1 A2 SA,A1 SR3 A,delSA3 2A,SR3 A,2SA

1 SA1 SA 1 A1 SR2 SAi SR3 A

1 SA

3 2SR,SA 1 SA2 2SR

3 2SR,SA 1 SA1 SR 1 SR3 2A,SR 3 2SR,del1 SA

11 SR

4 A1 A2 A3 2SA,A 1 A2 A,SR 2 SA

2 SA2 SA

2 A 1 A

1 SA

I SA 1 del.

1 SA 1

1 R1 SA 1 SA1 SA1 SA

1 SR 1 CA 1 SR 1 sa

1 RSA

1 del

2 A1 SA

3 SR

1 SA1 SA

1 SR 2 del,SA1 SR

1 SA

1 A 1 R 1 SA

2 R,SA

1 SR

1 A 2 SA,SR 2 R 1 R 2 A,SA

2 A,SA 1

1 SA-SR

1 SA-SR 1 SA-SR 2 SA-SR 1

1 2 SA-SR 1 SA-SR 2 SR-R 1

460

86 122 53 8 1011

12 9 3 1 2211 1110 2100 5421

.4 mm .4-. 5 mm >.5 mm tfgt. Shape No. Shape No. Shape (gra.)

37.5

45.439.3 40.8 42.5 41.628.0 17.537.237.051.9 43.046.7 56.9

A 14.6 46.0

56.954.847.050.945.950.441.638.960.049.859.750.454.847.058.949.750.320.528.6 19.023.932.732.436.225.822.7

20.927.3

41.922.7?M17.029.721.320.627.524.9

1 SA 42.322.837.921.3 41.2 41.1 37.6 35.4 36.7 48.5 39.3 30.6

SR 26.840.4 25.940.141.919.335.923.3

50.357.057.9

A 52.039.654.847.661.6

50.2

34.778.6b4.b32.338.319.436.629.338.646.0bO.t41.530. B41.342.333.940.138.031.044.044.428.632.927.047.330.646.7 46.544.825.0

1 SA 49.950.5

2 SR,SA 1 l.6x.3) 31.246.644.840.736. B35.5

SA 42.942.841.640.143.244.141.637.0

40.041.027.945.136.430.541.037.748.418.416. B20.320.424.119.716.420.1

SR 1 R 23,916.727.427.239,316.326.521.0 13.4 24.5 25.4 17.6 17.024.934.025.927.018.921.9 21.030.543.128.0 45.7

4,i,i>39.339.357.3 39.5 41.2 33.1 37.8 30.3 29.644.338.3 45.534.639.625.0 30.2 38.5 31.3

1 (.&X.4) 36.9 19.1 30.1

SA 45.0 44.1 31.7

21.824.136.0 29.2 30.7 29.4

SA-SK 30.7 25.0

SR-H 23.9 1 SA-SR 39.9

29.6 33.6 34.6 30.8

4 3 209 1 1 0.0 2 1 61.6 1 1 35.7 1 0 11.2 0 0 125.6 2 1 58.1

CONCENTRATE Ultraviolet NOTES Mag Py Gar Misc. lamp Rad % \ \ Sen Zir

25

2520 10 25 20 10 10 3525 35 2530 30 25 35

1540n

352035203030304035402035202030b5

151020251530

1510152510K606020152520302

Ib2

25 3b 25 30 25 15 30 20204015352010tr20

35453510203510202525554020453 r;10tr30302030201060251525202520202b252510251530 30305

5070505010151060105

10tr5

1555

52055S

tr0

15201010105

2055

tr255

251010201510 10 15 40 tr 1520 15tr15tr15 5

156

20 15

4010202530 15 30 20 10 tr3010 5

1015 5

10 15 8

tr 2

10 5 0 5

20 5070 70 30 40 40 40 40 35 50 40 40 30

212 0

70 21 15

221 51

tr

trtr 0 5 0 5 fj

tr8 5

1015 0 00

50005550

10555055032

tr10 tr105

trtr5

trtrtrtr2t-r2

tr22

tr3

trtrUD 2 5 0

tr tr 5

tt 05

tr 1

tr1031

0b3

1010S35

2 rj

55505505

trtr00

1002

tt05000000020

tr0 0002222

trtrtr202

trtr5250

5525

trtr5050

trtrtr12

trtr15

tr5

trtr tr tr Lr tr tr trtr tr8

trtr2 2212 2

11tr

>tr0

trtr 0 2 223T

2trtr 1

tr tr tr tr 2 2 0 3

5 203 8 5

20 8 8 5

10 20 10 5

10

210 0

25 3 4

15 10

5

2010 60 20 15 20 tr 540 05 0 5 0

0001000

101510101055050

103

tr 2

trtr Cpytr050

tr50

tr255

tr105 Cpy

3020 Cpy15tr Cpy200 0 3 Cpy

tr 3

tr 5

10 52

tr 0

1051

tr15

10in100b500055

10101500505

10cj00b

tr0000000b5

tr5

tr0 000

105S55

101505

tr5050

trtr

10

20.

5

015005

905b

1055525

trtrb Cpy

60 10 b

15 10 J

2025 trtr Cub50 0050

tr

Ib10Ib5

15 5 2

15 tr 0b5 05

15 5

tr 15 1030 0 0 5 0 2

40108 8

10 10 tr tr 5

tr 10 20 5 5

209 0

90 6

10 105 27

2

11 1 0 1 0101 101 1 1 10000011011120111010 0010210

10

10100221110012 21 1 11 2 111 0101112211112101

112211011011112102120011121 0011121101' 1

00002010

1000000000001110121111111 1 12011 11111 1111 111011 1 11 10101113 1 2 2 0 2 0 010

1321 1 0 1 1 1 2 1 1 0 1

209 0 31 1 0 2

2

12 2 1 1 2 0 11 1 12 1 2 1

1122212222221111121 1 110202

02

2221110222011 2 21 1 1 2 2 222 111222

1?11i22211

1121131121211111

11221112211211221}1111201012111

2221112212122122132i2212 21 1 21 11 200211110 2

2211 22 2 2 2 012 022 3 0 2 3 3 2 1 1 3 1

1 11 1 2 0 2 1 2 2 2 0 01

209 0

11 1 1 1 3

0 basal

0 basal0 basal 0 basal 0 basal 0 basal 0 0 basal 0 basal0 basal 0 sandy 0 semi basal0 basal 0 basal 0 silty 0 basal

silty basal0 basal0 ablation0 basal00 basal00 bdLjdi000 silty0 silty0 silty0 basal0 basal0 basal0 basal0 basal0 silty basal0 basal ; 0 silty 0 clayey '•0 silty |0 gravelly •0 sandy0 silty0 siltysilty i

0 gravelly0 silty ;silty basal

0 sandy0 silty ]0 sandy basal0 sandy0 sandy basal '0 silty basal i0 basal j0 ablation0 sandy basal -0 basal i0 basal0 basal0 basal0 basal 0 basal 0 basal 0 basal 0 basal 0 basal ; 0 basal I 0 basal !0 basal j0 basal 0 basal0 basal0 basal !0 basal0 basal0 basal

0 sandy0 sandy0 sandy0 basal0 gravelly0 sandy0 basal0 sandy0 basal0 silty

sandy0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 sandy0 basalU basal0 silty0 silty0 clayey0 basal0 basal0 silty basal*0 basal0 sandy0 basal0 silty0 silty0 silty0 basal0 gravelly0 basal0 basal0 gravelly basal 0 basal0 silty0 silty0 sandy0 gritty basal0 silty ssndy0 silty basal0 silty0 silty0 silty0 silty sandy basal0 silty sandy basal0 silty0 silty0 silty0 silty0 sandy0 sandy silt basal0 silty basal

0 sandy0 sandy0 basal0 basal0 basal0 basal0 basal0 sandy clay0 silty0 silty0 basal0 basal0 silty0 basal0 basal0 semi basal0 basal0 basal0 semi basal0 sandy-basal0 silty basal0 basal0 basal0 basal 0 basal 0 basal 0 basal 0 outwash? 0 basal 0 basal0 sandy0 basal0 basal0 basal0 basal0 silty till 00000

0 sandy0 till s erosion product0 ablation0 ablation/basal 0 basal 0 sandy basal 0 clayey 0 basal 0 ablation 0 basal0 basal0 basal 0 basal0 basal0 silty 0 silty basal 0 basal 0 clayey 0 sandy 0 ablation 0 silty basal 0 silty basal 0 silty 0 silty 0 silty basal

000 0 0 0 0 0 0 0 0 0 0 0

CONCENTRATE ASSAYS

NORMALIZED VALUES Au GOLD GOLD ppb grains microgra det b

5 23.3

5 5.88 11.2 6 19.7 7 19. B 4 4.2 2 2.7 0 0.1 0 1.23 2.7 2 2.2 0 2.42 3.0 3 3.67 30J 1 18. b 0 1.21 5.64 2.35 38.01 2.73 2.50 18.72 7.50 2.80 0.23 8.11 5.53 3.3b 1.83 3.83 b.O1 21.34 43.63 20.46 4.2 0 15.5 5 20.93 1.84 6.82 2.78 18.05 15.90 0.53 13.70 3.72 45.55 13.20 52.42 2.71 2.50 59.12 2b.O0 292.32 11.73 15.93 126.30 5.23 13.90 0.8 2 16.6 2 4.1 0 3.6 1 10.8 0 0.8 1 104.0 1 lb.1 0 4.73 4.80 2.3 3 339.12 2.90 6.60 3.56 89.05 39.9

1 3.71 5.23 4.21 1 5.52 4.b4 9.92 3.63 8.31 7.32 4,22 4.77 14.41 4.15 3.42 13.0

53 585.44 1.74 49.74 18.31 9.26 6.99 9.45 21.70 11.6

18 26.90 3.03 13.37 10.73 3.74 11.13 10.6

10 13.32 3.76 10.05 14.93 12.63 5.05 3.1 0 5.83 8.40 1.07 117.24 97.77 KU4 30.0

17 86.92 24.5

10 13.23 36. b2 9.81 10.02 1.7

13 18.72 3.49 239.4

19 6.912 9.2

5 1.45 3.41 0.60 0.20 4.92 0.11 0.36 3.10 0.81 1.10 0.70 0.52 0.20 24.02 13.10 2.70 C.43 165.74 0.72 4.23 16.24 0.51 0.10 1.2 1 8.0 6 71.6 4 5.2 0 1.7 2 88.6 4 17.01 18.1 0 0.20 44.03 0.62 6.21 15.5 0 3.95 9b.30 23.50 7.2 0 1.1

1 19.23 2.70 1.2b 10.2 1 12.8 3 17.0 0 76. B 3 19.8 1 14.0 3 0.10 6.40 5.0 2 35.80 7.96 24.1 1 2.7 3 53.8 4 14.0 3 35.1 7 219.5 0 57.5 4 30.0 1 17.9 0 30.6 0 10.3

6 25.8 52 539.10 2.0 1 6.1 2 4.9 5 25.1 3 10.0 4 35.2 7 100.3 1 134.0 4 0.1 1 1.3 0 13.4 1 1.1

...,_,...__..._......-..._215 215

0 0.0 53 535.4 3 28.36 71.5

32 5118.1is in. 4

506

106209 412 413 48 54 3

264b 38 366986 747 47429

11939

6496665327146bl3

1727452447480

33658390770

48356831

1417b

b!7471

852375

824277

IbOO110144

1800962

12500438559

26109242529

396 82 70

267 17

1700 309 14813570

b!906114716823bO1250

10411290

: v';

12717863

19431750

12443018665

39112500

631360473184Ib2128337388502423602801053572b226711525236226111957

104134H

19301630

USOi.i588

140038617364115016622

363101

3690SO130

3663313

733

10861466402510

83559710217

6840}8

131WIb

j;3

2f.S 2560 11] 37

2430 547576

339212

117477 60

2400495136 19

460bO20

170 300 289

1700 366 325

3S974 410166319 71

12bO 327

1000 3600 1900 699 444 b70 142

924 18200

Bb 244 194 674 437

1420 3090 5220

3 b2

382 46

213 3

18200 730

2036 ****t*ft

4803

Au ragn

18.9

4.88.2

16,8 17.5 2.0 1.5 0.1 1.01.7 2.0 1.53.2 4.9

33.2 21.81.35.52.1

30.43.33.0

16.46.12.20,26.14.42.62.43,54.7

16.629.218. b2.0 9.2

13.61.04.62.7

13.310.60.3

10.92.0

27.111.634.03.22.4

53.420. b

249.912.013.6

110.42.116.00.6 16.3 3.4 2.6 9.4 0.6

82.2 12.1 4.53.62.8

134.02.46.23.284.129.8

5.26.45.2

17.15.09.73.0

11.9"'.4

2.55.2

14.95.33.512.6

477.11.6

49.714.07.27.06.5

16.011.920.71.8

12.211.24.0

11.011.111.93.38.39.7

12.43.62.7 4.95.90.4

96.182.1

)S4 J27.362. b15.76.322.66.47.10.9

14. b4.3

162.83.74.8

1.42.60.90.12.70.10.33.20.11.20.70.50.2

20.111.71.90.3

163.20.63.6

10.80.60.00.9 5.6

34.7 2.8 0.9

42. b 9.3

14.2 [1.1

1C.10.33.4

16.4 l.T72.321.33.8 0.9

20. 02.00.89.7 11.811.9 bb.7 13.8 9.9 0.14.42.8

18.65.7

12. b 1.8

37.4 12. b 31.0

131.7 36.0 20.9 19.8 24.9 4.5

20.3 439.3

2.2 6.9 6.0

19.8 13.3 3b.7 73.7 208.3 0.1 1.8

13,3 1.4

214 0.0

477.1 22.6 58.4

3411.3 139.5

Ag ppm

b

3

33 3 3 3 3 3 333 333 3 3 33333333333333333333 3 333333333333333333333333 3 3 3 3 3 3 333 33339

10

33333333333333333333333333333333333333 333334

3333333333333

33333333i333333333333333 3 33 3 j33 33333 3333 3

33333 3 3 3 3 333333 3 3 3 3 3 3 3 3 3 3

333 3 3 3 3 3 3 3 3 3 3 3

2133

10 3 1 1 5

AsPP»

2

1

11 I 1 I 1 5 41 I 12 1 11 1L199741318411416431 3 411141211111111111435131 1 3 3 1 3 4 333 4535

421

114822453

10115114b44b87101014126769855134171 2250396ub81715b24313312

111141614111141111113116 1 1 1 1 1 11 11311

1436561

1611 2 1 3 3 1 113113 1

27 6 3 1 1

10 1 1 3

1 87 1 1 8 4 5 7 3 6 3 3 5

213 1

50 4 6

41 17

Bappm 200

100

310100 100 290 100 570 390 310100 250 340100 100 240 270 270230100100340100100290100100300100220100230270310320100350 390 4002605304bO430100390100100340100100100570430100360410100bOO100100610 340 460 460 440 440 340 350 400330440 230340360330100390

3601001001004bO360320290100100100100420100blO1001001001003603602603101001004bO1003203301003bO2SO520460610420100380 1003303bO380100UKi100320430350100490400430320290210100270

100560520640100100100480450660100100100100100100670100370100340430100b90 100 100 100 100 670 100360 460420100950100 610100460460 310

100440300100 380 390 470 100 240 640blO170 440430350 100 660 100 3bO 400 100 410 270 100 490

690 100100 790 100 370 100 100 100 470 100 420 100 100

213 100 950 282 179

32072 640

Br ppro

5

3

33 3 3 3 3 3 33 3 33 3 3 3 33333333333333333333 3 33333383333333333333333 3 3 33 3 3 3 333 333333

3333333333333333333333333333333333333333333.i3333333333333

3333333l333333333333•j

333] 3 3 3 3 33 33333 3333 3

333•>

33 3 3 3 3J3 333 3 3 3 3 3 3 3 3 3 3

3 33 3 3 3 3 3 3 3 3 3 3 3

213 3 8 3 0 0 4

Ca \

• 1

1

21 1 1 2 3 1 13 2 31 2 1 1 11111121131212121314 3 31121111531111111113635 11 2 3 41 1111 111111

12331132543243146143143131323111131451 241121311311114151b

1414b586617b6111711111111 71 1 5 11 441111141T

i

1

1

1

1

1

1

3 1 3111113 21 3 1 8 1 1 4 1

8 51 13 1 31 1 41 1 1 1

213 1 8 2 2 3 5

Co ppra

b

14

131410 13 11 11 22 141812 1619 13 11 24 18121414111712152314161215Ib101216123224 20 2224231727291730U212423292328191717138

39Ib32 29 28 23 33 27 31 26 273027 352120268

' 12

17181813272926Ib

240252726151933b862242421212524292b2829262b24202b2521272319025 2726591223HIb19191445169

142023282724

1716162022132S1641282817222520161818241512141714 1923 15 26 17 2221 181216101370221637 12

13211412 Ib 9

20 11 12 7

1825 162710 1710 12 12 12 78 19 12 12 19

2858bl 40 41 48 42 48 b2 23 44 39 37 4b

213 7

240 24 22

450 68

Cr ppra 10

220

140200 150 190 120 270 200 230190 130 170140 180 120 310 210100170180180150IbO190640150410130190170IbO100140120950440490 360490620b20

100089025075012039053046068044063028064280240160230170210 680 890 800

1500 610 980 930 960

12001200 BOOb90770570140200

200190140140200IbO140110630no220230140220370240260370350240200210bbD70036029014002100310bbO40044068057015005906bO850

110088086

200140m17031013016018018017098190200180240280

25058024077

250290240230

16000760710290290390440210330450370320170250330280 350 410 260 710 290 330600 24012015018015010026016043

170

170530160150 220 100 220 150 IbO 260200JOO 220540i)b

170 160 150 230 150 310 310 250 260 260

320 370

2600 1400 1900 2300 2000 3000 1300 790

2400 2300 1400 890

213 43

16000 517

1169 1367126

2855

Cs ppm

2

1

11 1 1 1 1 1 11 1111 11 111111111111]1111113 4 13211111311111113113131 1 1 3 2 3 1 1 111 111111

1111111111i111311211111121111111111111 11b1211111111121112

1111111131111141511111111 1 1 1 1 11 13111 1111 1

1131 1 1 31 1 111 211 1 1 1 1 4 1 1 1 1 3

1 11 1 1 1 1 1 3 1 1 1 3 1

213 1 5 1 1 1 3

Fe \ 0.0

18.8

9.621.9 9.1 22.2 9.8 7.2

10.1 18.021.2 16.29.0

16.2 21.1 20.1 2b.O IB. 29.620.115.711.015. b16.718.519.111.77.1

11.623.718.720.914.918.913.923.69.5

13.1 12.014.614.112.924.629.713.029.09.7

16.725. S16,130.927.632.625.813.129.711.411.97.28.5

14.0 20.6 22.1 18.6 28.4 14.2 21.7 22.2 23.625.324.5 20.216.020.731.57.7

10.7

19.218.413.611.421.414.412.09.726.09.720.919.46.9

15.622.610.18.4

20.823. b14.815.79.4

12. b21.311.79.021.017.011.817.79.4

14. b17.615.317.413.816.818.6 23.916.17.8

10.417.214.J12.912.59.6

11.318. 08.35.16.08.19.06.9

11.09.8

11.920.89.96.9

13.35.28.09.2

10.919.916.412,59.420.211.69.1B.b27.915.016.16.49.0

12.713.2 12.5 19.611.9 42.1 12.6 14.528.1 7.86.47.2

10. &7.4

14.619.110.223.712.6

25.47.8

16. 914.021.7 14.5 28.1 16.9 21.8 17.710.521.6 11.715.64.98.6 8.0 7.1 15.9 8.0 9.9

19.7 10.7 7.6 11.3

12.7 15.044.4 31.5 35.3 42.4 35.7 47.4 29,0 15.3 37.0 35.5 26.6 24.4

213 4.9

47.4 16.5 7.9

62.0 32.2

Hf ppm

1

47

5346 74 39 37 65 49 352b 17 23

120 21 17 17 262516267436162031342032211615112327

16072 42 60305012080no3761

1304737

1609387b4140238085479

6248 4b 36 67 b8 70 45 47 81

10051 50blb37666

130

3b442329332716312510201521230216410193222202020342b133b212024182194703927bl73 38348

47239919412222221932152726122322

17022

1307897270700130

666

190130280190290310130230300160798b

230200 140 150 51 66

180 1909213012747872 84b52b

30

2b533838 37 4159 52 32 106639 303728 46 58 48 45 3b 22 37 29 81 39

462198 64 50 82 45 63 72 65 54 66 44 77

213 5

700 65 75

5652 216

Hg Ir ppa ppb

b 40

3

333 3 3 33 33 3 33 3 3 3 33333333333333333333 3 33333333333333333333J333 3 3 3 3 3 3 333 333333

33333333333333333333333333333333333333 3333333333333333333

33333333333i333333333333 3 3 3 3 3 33 33333 3333 3

3333 3 3 3 3 3 33j 333 3 3 3 J 3 3 3 3 3 3

3 33 3 3 3 3 3 3 3 3 3 3 3

213 3 '3

3 0 0 3

20

2020 20 20 2020 20 202020 2020 20 20 20 2020202020202020202020202020202020202020 20 2020202020202020202020202020202020202020202020 20 20 20 20 20 20 20 202020 202020202020

2920202020202020202020202020202020202020202020202020202020202020202020202020 20202020202020202020202020202020202020

20202020202021)20202020202Q2020202020202020202020 20 20 20 20 20 2020 2020202020 20202020 20

20202020 20 20 20 20 20 202020 202020 20 20 20 20 20 20 20 20 20 20

20 2020 20 20 20 20 20 20 20 20 20 20 20

213 20 20 20 0 0

20

Mo ppm 20

10

1010 10 10 10 10 10 1010 10 1010 10 10 10 101010101010101010101010101010101010101010 1010101010101010101010101010101010101010101010 10 10 10 10 10 10 10 101010101010201010

1010101010101010101010101010101010101010101010101010101010101010101010101010 10101010101010101010101010101010101010

101010101010101010101010101010101010101010101010 10 10 10 10 10 1010 1010101010 10101010 10

10101010 10 10 10 10 10 101010 10101010 10 10 10 10 10 10 10 10 10

101010 10 10 10 10 10 10 10 10 10 10 10

213 10 20 1010

11

Na ppra 500

12300

1320010600 13300 11200 16900 16200 19100 1450011900 12400 14400Ib400 10900 10900 93bO 12900139009960

138001390011800119001380C117001360015400128009b80

1250012bOO1130010300128001460016900 12000 HbOOIb30018600158001390012000IbbOO1660019300IGbOO142001690011300IbbOO12bOOlObOO978010301)1590015600109001610012600 18700 16800 HbOO 16900 17300 16600 14100 124001080012700 13900Ib7001170084605660

12600

14000139001410014100186001540014600IbbOO2140014300140001510024200141001580015100190001390013200Ib2001290U1410017800149001720017100131001510016100136001860014400126001420019100151002090016800 14000159001360016bOOHbOO114001730014500Ib60015200Ib9001840022200182001470013400180001530013000

14900191002410024200221002170018300212006B3021000174001250017800163002020019300209001190011300149002030016400IbOOOI2b0017300 1340020000 8600

16600 12bOO13100 165001310015900191001470013bOO12300IbbOO10400 18600

14100175001430013400 14600 15700 8170

13900 17100 5670

1820014000 145001900019700 18400 7010

15700 13100 15100 17800 11400 19400 18900 IbOOO

13700IbSOO8b80 10600 9970 8080

11400 5880

14900 17200 10100 9070

11400 9950

213 5660

24200 14688 3419

11690986 21527

Ni ppra 200

100

100100 100 100 100 100 100 100100 100 100100 100 100 100 100100100100100100100100100100100100100100100100100100100100 100 100100100100100100100100100100100100100220100100100100100100310100100 100 100 100 100 100 100 100 100100100 100100100100100100

10U100100100100100100100430100100100100100100100100100100210100100100100100100100100210100100100100100100100220100 100100100100100100100100100100100100100100100100100100100

10010010010010010010010010010010010010010(1100390100100100100100100100100100 100 100 100 100 100100 100100100100100100100100100 100

100100100100 100 100 100 100 100 100100100 100100100 100 100 100 100 100 100 230 100 100 100

100100100 100 100 100100 100 100 100 100 100 100 100

213 100 430 107 37

1403 182

Rb ppm 50

25

2525 25 2b b6 25 25 2525 502525 25 642b 2bb72b2b2b2b25252b60252525812553702b2b2bbO 255425252525252525252b252576252525252b642553252b 25 25 2b 25 25 25 852b2b 252525252b2b

25252525252b252b

1202b252bbO2b252b2b2b252b252b2525252b252b252b25252b252525252b2b252b2b2569252554252b2b2b25252b252b2b

2b2b252b2b2b25252b252b252b252525252b2b2b252b2b2525 2b 2b 25 25 252b 25252b11025 2b252b25 2b

2b612b2b 2b 252b 7b 2b 2b6125 942b25 25 bO 82 2b 64 72 2b 25 25 25

25 252b25 25 7225 59 2b 78 2b 2b 25 25

213 25

120 31 16

267 64

Sb ppm 0.2

0.1

0.10.1 0.10.1 0.1 0.1 0.10.10.10.1 0.30.3 0.1 0.1 0.2 0.10.10.10.30.1O.b0.40.50.20.1O.I0.10.10.10.10.30.10.10.30.1 0.1 0.10.12.30.10.10.40.10.10.10.10.10.40.10.10.10.10.1O.b0.1O.I0.10.10.5 0.1 0.30.1 0.1 0.4 0.1 0.1 0.10,10.1 0.10.10 , •}0,10.90.1

[j.l0.10.40.80.80.1O.I0.10.1O.b0.30.40.10.10.10.40.10.4O.bO.b0.70.80.31.30.90.60.50.70.50.60.40.30.40,10.10.20.50.1 0.10.13.60.60.81.10.60.71.61.30.10.1O.i0.10.10.30.10.50.1

0.10.10.10.10.10.10.10.10.10.10.10.10.60.10.10.10.60.10.10.40.10.10.10.10.1 0.1 0.1 O.i 0.1 O.b0.30.10.40.40.10.11.10 0 .0

0.10.70.1

0.10.20.10.1 0.1 0.10.1 0.1 0.1 0.10.10.10.10.10.1 0.1 0.9 0.3 0.1 0.1 1.6 0.1 0.1 0.3 0.1

0.1 0,50.1 0.6 0.1 0.10.5 0.1 fl.l 0.1 0.4 0.1 0.3 0.1

213 fl.l 3.6 0.3 0.4 0.1 1.1

Sc ppra

0.10

24

3128 4b 19 27 24 21 1415 12 1914 13 1212 1714915262012152020182015128

1117222530 35 3730IV2020272025602b15332130194029333721773454 18 1314 16 22 14 Ib 222011 2b1920.34203B

a171721272026163G251823232020263617262219222b292622192019222021232123182321 141429191947123125361314189

2627252631

49224b21322832493b2741b7bl3460383028b62217234bH 37 63 26 22 43 58242224274b2339octo2222 15

13222020 17 Ib33 26 10 262b23 23IbIB 29 21 28 28 20 38 21 14 33 20

49U16 23 17 22 20 15 29 23 17 17 2b 30

213 8

77 25 11

132 48

Se ppra 20

10

1010 10 10 10 10 10 10 .10 10 1010 10 10 10 10101010101C101010101010101010101010101010 1010101010101010101010101010101010101010101010 10 10 10 10 10 10 10 101010 101010101010

101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010

10101010101010101010101010101010101010101010101010 10 10 10 10 1010 1010101010 1010101010

101010101C 1010 10 10 101010 101010 10 1010 10 10 10 10 10 10 10

10 1010 10 10 101010 10 10 10 10 10 10

213 10 10 10 0 0

10

Sr\0.2

0.1

0.10.1 0.1 0.1 0.1 0.1 0.1 0.10.10.1 0.10.1 0.1fl.l0.1 0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1O.i0.10.10.1 0.1 0.10.10.1O.I0.10.10.10.10.10.10.10.10.10.1fl.l0.10.10.10.10.10.10.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.10.10.1 0.10.10.10.10.10.1

0,10.10.10.10.10.10.10.10.10.10.10.10.10.1O.L0.10.1U.I0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1O.i0.10.10.10.1fl.l0.10.10.10.10.1

0.1O.i0.1fl.l0.10.10.1O.I0.10.10.10.1O.I0.10.10.10.10.10.10.10.10.10.10.10.1 0.1 0.1 0.1 0.1 0.10.1 0.10.10.10.10,1 0.10,10.10.1 0.1

0.10.10.10.1 0.1 0.1 0.1 0.1 0.1 0.10.10.10.10.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1

0.1 0.10.1 0.1 0.1 0.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1

213 0.1 0.1 0.1 0.0 0.0 0.1

Ta ppm

16

612 14 8 6 7 3 4b 4 36 5 6143439456433196434511 1 124211b4

26134164

1018U51a

10i i i i i i i iii i21159

1411866612138b32111211211111114111131132 2114181111111111112

9192111

10118

1012?

214684413B57 7 4 8 1 57 116

1191411 1

976

10 8 8

22 9

10 241 1217 6 7 8 6 4 6 1 8 2

131 1 1 111 1 1 41 1 2

213 1

26 4 4

15 12

Th ppra

1

33

2340 3b 22 18 26 12 1816 14 9

17 28 24 22 231719163420213023241321251926Ib23233616 9

147

1226203411282616Ib33232020674

5930193

2526 19 14 21 24 22 IB 18 333519 24283h692338

333318221917922177

1714IB2023131424382620141837201133IB20391620332338262330 2013b

4918

120193612181614185

12186

149

3b4

419

102020234

163b234237

10020Ib3429201516b22624 36 13 25 35 4329 12B

2624252

14111

10

27232626 26 22 48 23 20 4

1410 101312 25 2b 25 24 18 10 20 13 27 17

31 1736 35 22 35 23 26 36 27 25 31 34 48

213 1

120 23 14

190 bl

U W ppm ppra O.b 4

6.2

5.510.0 12.0 11.0 b.O 7.8 4.1 5.34.2 3.43.48.5 3.6 4.7 3.2 3.02.63.02.67.44.23.53.33.43.93.64.64.64.72.92.83.75.64.53.50.3 2.03.53.73.83.56.24.34.B

26.04.52.76.03.65.34.9

15.03.b7.96.41.73.16.18.1 3.5 3.1 4.9 4.5 3.9 3.1 2.9 5.66.43.0 2.14.93.07.fi6.5tf.fl

3.66.21.93.60.32.81.93.15.60.32.62.00.32.64.63.27.52.35.94.02.71.52.34.33.32.16.23.12.53.13.01.95.74.44.22.95.64.53.12.21.53.83.2

10.02.84.62.61.91.82.31.92.91.53.12.52.10.3

11.02.36.24.24.15.4

18.08.80.32.811.08.815.09.6

23.013.08.59.613.05.63.43.712.07.26.59.9 1.5 5.9 9.2 9,8b.O 7.12.96.48.06.9 0.3t. tJ. D

3.00.3 2.9

6.56.55,27.6 5.6 6.5

18.0 9.0 5.6 O.b3.23.0 2.83.13.1 4.1 6.3 4.44.3 3.51.0 b.O 2.1 4.0 5.0

3.1 4.5b.7 4.9 4.2 5.2 3.4 4.1 5.8 3.8 2.9 5.5 b.l 6.8

213 0.3

26.0 5.0 3.5

12.5 12.1

10

22 2 22 22 222 22 2 2

152

IB2

3322222222222222

492 2 2227

4422726222662

1502

1222227 2 6 9 2 7

10 987

102L

3956

2422222

102

11222

122

8872

Ib10772

128622

Ib123626IB101218b

32IS 82

66182

30272222b222222

222222222222

142

1622

397b6322

12IS8 2 2

16 9 26

1092

2912 1033112 6

2222 2 2 9 2 2 222

1422 2

160 48 22

22 2 6 7

10202 2 2

16 9 2

21 2 2 6

22 9

213 2

160 10 19

3b7 47

Zn ppm 200

100

100100 100 100 100 100 100 200220 100 100100100 100 100 100100100100100100100100100100100100100100100100100100100100 100 100100100100100100100100100100100100100100200100100100210100280100100 100 100 100 230 210 100 100 100100100 1001001002301001UO

100100100100230100LOO100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100 100100100100100100100230100100100100100100100100100100100

100100100100100100100100

1100100100100100100100270100100100100100100100100100 100 100 230 100 100100100100100100100">} (1i.iO

100100100 100

100100100100 100 100 100 100 100 100100100 100100100 100 100 100 100 100 100 100 100 100 100

100 100100 100 100 100 100 100 210 100 100 100 100 100

213 100

1100 113 7b

5627 263

[ PI

C

i( 1

i 1 I

1

I

(

t

(

-I

-t

-I

C

4t

4I

E

fi1II

]i

(.1

(1

K

(

1i

I

1

I

1[

1

1

!ir

!

!

1,1

1

1

1

11

1

1

1

'

13

1

1

1

11211

1

1

1

1

1

2

3

11 1

Table 7

c -

0 -

EMO AREA

s -

compactness

CS -

clast s

ize

oxidation

CA -

angularity

stoniness

SR -

sub r

ounded

SA -

sub

angular

del

- delicate

~*\*y>

& LO

CATION

' BE

DROC

K WE

IGHT

(kg)

TILL D

ESCRIPTION

PEBBLE COUNT

TOTAL

•jo.

N.T.S.

HBB

Total

Frac.

? n

52C/12

granite

28.0

12.9

P J*

52C/12

granite

29.0

11.0

P n

52C/12

granite

29.0

9.8

p IZ

52

C/11

granite

27.0

7.0

F 2>

52C/11

granite

26.3

8.6

p 30

52C/11

23.2

4.8

•f'il

52C/

11

29-0

9.3

F ~'A

52

C/11

granite

23.4

4.

8F

'X

52C/14

granite

27.5

7.1

p ;<

52C/14

27.5

3.6

F i$

52C/

14

migmatite

21.2

5.1

f 36

52C/14

breccia

28.5

9.1

F 27

52C/14

granite

28.0

12.1

F 38

52C/14

gran

ite

28.5

10.1

p 39

52C/14

28.5

8.

2F

40

52C/14

granite

23.4

6.3

F 41

52C/13

granite

24.1

6.1

p 42

52C/

13

gran

ite

22.5

4.

8F

43

52C/13

24.3

10.1

F 44

52C/13

granite

26.2

5.7

F 45

52C/13

granite

26.3

12.3

F 47

52C/13

granite

26.0

8.0

F 49

52C/13

granite

27.0

6.5

F 51

52C/13

24.0

12.7

F 53

52

C/13

granite

28.0

8.

9F

56

52C/13

gran

ite

27.0

2.

3F

57

52C/

13

gran

ite

23.2

6.

5F

58

52C/13

granite

29.0

8.4

F 59

52C/13

volcanic

25.4

4.1

F 60

52C/13

granite

23-5

5.5

F 75

52C/

13

basalt

26.0

10.2

F 76

52C/13

volcanic

22.5

20.1

F 77

52C/13

ande

site

36.0

9.1

F 78

52C/

13

volc

anic

23.7

9.4

F 79

52C/13 g

abbro/volc

27.3

8.8

F 80

52C/13

23.0

4.6

F 81

52C/13

nafic

vole

25-8

4.0

F 82

52C/13

aafic

vole

32.1

10.2

F 83

52C/13

granite

25.7

8.5

F 84

52C/13

granite

26.5

4.4

F 85

52C/13

granite

22.0

5.5

F 86

52C/13

mafic

vole

29.0

6.0

F 87

52C/13

mafi

c vole

27.5

5.

3p

88

52C/13

basalt

29.0

5.6

p 89

52C/13

29.0

8.8

F 90

52C/13

basalt

25.0

7.9

F 91

52C/13

mafi

c vo

le

31,0

IB. 9

F 92

52C/13

volcanic

26.6

5.0

f 93

52C/13

volcanic

26.5

8.6

P 94

52C/13

basalt

28.0

10.7

F 101

52C/13

mafi

c vole

21.4

8.9

F 102

52C/13

volcanic

28.0

12.4

F 103

52C/13

32.7

16.3

F 104

52C/13

basalt

23.9

8.2

F 107

52C/13

28.5

6.6

F 10

8 52C/13

28.5

9.0

F 109

52C/13

mafic

vole

27.5

11.2

F 11

0 52C/13

29.5

5.6

F 111

52C/13 g

ranidiorite

16.2

3.2

S 1

52C/13

volcanic

24.8

2.8

S 2

52C/13

volcanic

32.0

10.9

S 3

52C/13

volcanic

23.5

2.0

S 4

52C/13

volcanic

26.0

15.3

S 5

52C/13

volc

anic

36.0

17.0

S 6

52C/13

volcanic

26.3

4.7

FR£

1 52C/13

24.6

6.5

FRE

2 52C/13

granite

30.2

10.5

FRE

3 52C/13

granite

25.0

6.4

FSB

4 52C/13

granite

26.5

9.3

- FR

E 5

52C/13

26.3

9.9

FRE

6 52

C/13

ma

fic

vote

26

-3

2.8

FtE

7 52C/13 sheared v

ole

22.7

5.6

PRE

8 52C/13

nafic

vole

20.1

5.8

FSE

9 52C/13

volc

anic

22.0

7.6

•FRE 1

0 52C/13

basa

lt

27.0

9.9

FRE

12

52C/13

volcanic

23.4

5.9

FRE

13

52C/13

23.7

2.6

FDER 1

52F/04

basalt

37.0

14.3

FDER

2

52F/04

mafi

c vole

29.0

11.1

FDER 3

52F/04

mafic

vole

32.3

9.0

FDER 4

52F/04

basalt

32.0

13.5

FDER 5

52F/04

basa

lt

27.3

10

.5FDER 6

52F/04

mafi

c vo

le

25.7

10.6

FDER 7

52F/04

mafi

c vo

le

28.0

6.1

FDER

8

52F/04

30.0

14.1

FDER

9

52F/04

26.1

4.6

FDER

10

52F/04

23.5

3.6

FDER

11

52F/04

30.0

5.4

FDER 1

2 52F/04

mafi

c vole

26.8

11.9

"FTRY

i 52F

/04

32.4

8.9FTRY 2

52F/04

mafi

c vole

26.4

6.1

FTRY 3

52F/04

Etaf

ic v

ole

28.5

8.1

FTRY 4

52F/04

mafi

c vole

26.4

7.

2PTRY 5

52F/04

basa

lt

29.0

14.4

FTRY

6

52F/04

basalt

33.7

15.0

FTRY 7

52F/04

basalt

27.0

9.2

FTRY 8

52F/04

mafi

c vo

le

28.0

10.3

FTRY 9

52F/04

mafi

c vole

29.5

9.0

FTRY 1

0 52F/04

mafi

c vole

37.9

13.8

FTRY 1

1 52F/04

mafic

vole

22.1

6.9

. FTRY 1

2 52F/04

mafi

c vole

28.0

10.5

FTRY 1

3 52F/04

28.0

8.

4FT

RY 1

4 52F/04

basalt

24.3

7.2

FTRY

15

52F/04

29.0

12.1

FTRY

16

52F/04

metaseds

25.8

5.7

FTRY 1

7 52

F/04

23.0

9.6

FTRY 1

8 52F/04

28.5

12.4

FTRY 1

9 52F/04 fe

lsic

vol

e 31

.6

9.8

FTRY 2

0 52F/04

21.2

6.

3FT

RY 2

1 52F/04

22.3

8.4

FTRY 2

2 52F/04

granite

21.9

8.5

FTRY

23

52F/04

raignatite

24.4

6.4

FTRY 2

4 52F/04

gabbro

27.0

6.

0

FPIP

1

52F/04 v

ole/granite

29.0

9.1

FPIP

2

52F/04

28.0

2.1

FPIP 3

52F/04

mafic

vole

26.5

5.0

FPIP

4

52F/04

mafi

c vo

le

19.2

7.9

FPIP

5

52F/04

mafi

c vo

le

25.5

4.4

FPIP 6

52F/04

27.2

5.7

FPIP

7

52F/04

granite

27.0

8.9

FPIP 8

52F/D4

mafi

c vo

le

26.2

5.6

FPIP 9

52F/04

25.0

6.6

FPIP 1

0 52F/04

28.0

3.2

FPIP

U

52F/04

mafi

c vo

le

26.4

5.9

FPIP 1

2 52F/04 v

olc/intrus

27.0

2.6

KPIP

13

52F/04

mafi

c vo

le

24.3

8.7

FPIP

14

52F/04

volc

anic

27.0

8.8

FPIF

15

52F/04

28.0

6.6

FPIP 1

6 52F/04 v

ole

breccia

31.7

8.0

FPIP 1

7 52F/04 s

heared v

ole

29.0

12.0

FPir I

B 52F/04

volc

anic

26.4

7.1

t'PIP

19

52F/04 s

heared v

ole

29.8

11.9

FPIP 7

0 52

F/04

sheared s

eds

20.9

9.5

FPIP

.!!

52F/04 t

uff, sh

ale

24.0

5.6

FPIP n

52F/04

30.0

8.5

FPIP

23

52F/04

35.7

5.3

*Ttt*

24

52F/04

volcanic

31.4

14.1

FPir

25

52F/04

mafi

c vo

le

29.0

13.9

KPir ;&

52F/04

mafi

c vole

29,1

15.3

FPIP

:i

52

F/04

mafic

vole

24.9

10.0

FPIP

28

52F/04

mafi

c vo

le

36.3

19.1

FTIP 79

52F/04

mafi

c vo

le

29.0

15.1

FPIP JO

52F/04

m.if

ic v

ole

24.7

12.5

FPir

?l

52F/04 s

heared v

ole

29.0

14.0

H'lr

32

52F/04

volc

anic

36.6

18.4

FPlt

4 -3

52F/04 s

heared v

ole

28.0

12.6

mi'

:«

52F/04

19.5

7.5

FTir

?5

52F/04

dior

ite

16.2

3.6

FP1?

?6

52F/04

15.3

11.3

*TIF

:7

52F/04

13.3

6.0

FFls"

:8

52F/04 s

heared v

ole

13.2

3.3

Ît

-9 52F/04

volcanic

19.6

3.6

*?lt

* <6

52F/04

19.9

8.0

H*'?

U

52F/04

21.2

5.3

CB 1U

52C/13

granite

28.0

6.5

°B U*

52C/13

30.0

8.2

SP 1

17

52C/

13

volc

anic

28

.0

6.3

°B l

lj

52C/13

27.0

5.2

SB 1

1*

52C/13

20.7

4.3

GB ll

'A

52C/13

rrafic v

ole

34.2

7.6

SBVfA

52C/13

mafi

c vole

35.0

14.5

GB -,-A

52C/13

mafic

vole

31.7

8.7

vS _

;;A

52C/13

intrusive

34.0

8.6

^ -~:K

52C/

13

intr

usiv

e 37.0

18.3

no.

of s

amples

164

164

mini

mum

valu

e 13.2

2.0

maximum

value

37.9

20.1

mean v

alue

26.8

8.5

standard d

evia

tion

4.3

3.7

variance

18.7

13.8

anomalous

threshold

35.5

15.9

C 0

S CS C

A Vole 50

60

60

20 20 10 20 40 10 40 50 45 20 25 40 55 40 35 15 30 70 40 30 5 10 20 10 10 100

100 80 100 90 90 90 80 50 50 50 50 60 60 70 70 60 60 60 60 70 80 60 60 50 80 70 40 50 50 30 10 50 50 50 70 30 40 50 40 20 55 100 70 45 20 60 40 35 70 80 35 eo 60 80 35 70 100 85 90 60 80 50 40 80 90 80 100 40 90 25 40 100

100 50 40 60 80 60 40 50 30 50 60 90 70 50 60 20 40 60 60 40 60 100

100 70 100

100 60 100 80 40 80 40 90 85 50 100 40 100

100

100

100 60 15 60 95 100 70 40 40 35

34314

5011412

5020234

1020244

3030323

30

23342

3534342

50141 12

100

14223

9014223

5

162 0

100 57 27 714

110

BULK

TILL R

ECONNAISSANCE

PROGRAM

CONC

ENTR

ATE ASSAYS

GOLD

GR

AIN

DESCRIPTION

GOLD

<.

05 m

m .05-. 1m

m In

t Se

d Ot

her

Shap

e GRAINS

No.

Shap

e No

. Sh

ape

50

40

40

80 80 90 75 100 60 90 60 50 50 80 75 60 45 60 60 80 70 30 55 70 95 90 100 80 90 85 20 10 10 10 20 50 50 50 50 40 30 30 30 40 40 40 40 JO 20 40 40 bO 15 30 bO 50 50 70 30 40 50 50 30 70 bO 50 60 80 45 30 55 80 40 60 30 10 65 20 40 20 65 30 15 10 40 20 40 10 20 10 20 20 20 25 20 50 50 40 20 40 60 50 70 50 40 10 30 50 40 80 60 40 40 60 40 30 40 10 60 20 60 10 15 50 60 40 85 40 5 30 60 60 65 65 50 10 70 145 0

100 46 24 570 54

5

Qtz

Qtz

5

5

Qtz

Qtz

Qtz

Qtz

Qtz

tr

Qtz

Qtz

Qtz

Qtz

35 10 50 40 50 40 10

Qtz

•111

52F04NE965a 63.6161

75

220

050

5

11

018

133

4 1

48

2

3 2 3 1 0 2 3 1 0 1 0 4 1 0 2 0 1 2 4 2 0 3 8 3 3 3 0 2 2 1 2 4 0 1 2 2 5 3 3 11 7 4 4 0 2 1 3 2 4 4 2 3 6 4 14 4 1 4 1 4 6 1 4 7 5 1 5 3 3 9 4 6 1 4 3 0 3 2 4 7 3 0 6 2 9 11 2 3 7 9 13 3 2 5 12 4 0 8 4 0 10 7 1 1 2 7 2 5 5 0 1 2 2 3 0 1 7 1 0 5 3 3 1 9 3 4 3 B 5 6 2 1 7 3 11 4 3 3 0 2 1 1 0 3 6 1 3 5 1 6 5 6 0 11 ADR 1 AN 1 1 5 7 0

163 0 14 3 3 8 9

1 SR

1 SR

2 SR

1 SR

1 SR

2 SR

2 A/

SA5

SR/S

A 3

SA2 SR

/SA

2 A/R

1 A

1 A

1 del

1 A

1 SR

1 R

1 1 2

SAx2

1 SA

1 SA

4 4 Ax4

1 2

SAx2

1 A

2 A,

A

1 del

I 1

1 1 A

1 SA

1 SA

11 SA

-SR

1 SR

1 del

1 2 A,A

2 A,

A

3 3A

1 2

A, A

2 1

A

1 2 2 1

A

1 3 SA

3 1 SR

1 SA

2 SR

,£A

1 SA

3

2 SR

2 SR

7 SR

,SA

1 A

4 A

1 R

1 R

1 R

2 3

SR1

SR

2 2

1 SA

1 SR

1 SA

1 SA

43

1 2

4 1

A

1 A

1 1 3 2 1

SA1 5

3 2

1

1 R

5 3 2

1

2 A

1 SA

3 1 SA

1 A

1 ill

•

1 SA

-SR

1 SA-A

4 PR

5 SA

-A

41

700

05

112

21

22

35

5

.1-.2

mm

.2-. 3

mm

.3-. 4

mm

.4-. 5

mm

No.

Shap

e No.

Shap

e No

. Shape

No.

Shap

e

1 SA

2

SA

2 1 SR

2 SR

1

SR

1 SR

2 SR

1 SA

1 SR

1 SR

1 SR

1 SA

1 SR

1 SA

1 SA

2 SR

1 SA

1 SA

1 A

1 SR

2 A/

del

1 A

1 A

1 A

1 1

2 Ax

2

1 SR

1 SR

1 A

2 SR,del

1 A

2 SA,A

2 SR,A

3 dl,A,SA

2 SA

x2

1 del

1 A

2 SA

VSR

1 A

1 A

1 A

1 1

A1 A

1 SF.

1

R 1

A1

A3

2A,

SR1

A 3

2A,

SA1 3

2A,

del

4 2A,SA,del

1 SA

1 SA

2 1

3 SR

1 3 2A

,del

1 A

1 A

4 4A

1 SR

1 A

3 A,A,SA

1 A

2 A,

SA

11 A

1 A

1 A

2 A

4 R,

R,A,

A 1

1 SR

4 A,

SR,S

R1

SA

4 A,

3S

A2 SR

,SA

1 SA

1 SA

2

A,SA

2 SA

1 SA

2 SA

2

R,SR

2 SA,del

1 SA

2 SR

2 SR

2 SA

3 A,

SA

4 SR

,SA,

A2

A,SA

2 del,SR

1 SA

1 SA

3 A,R,SA

6 SA

3 A

1 ER

12 R,

A1

A 2

SR1

SA

1 SA

2 A

1 SA

1 SA

6 3S

A/3SR

1 A

2 A,SA

3 3

SR

2 SA

1 3

SR

5 d,3A,SR

1 A

5 R,A,SA

1 A

1 SA

1 R

1 SA

3 A,SA,SR

2 SA

2 A,

SR

1 del

1 2 SR

,SA

1 SA

2 SR

2 SA,A

1 SR

2 A,SR

1 SR

3 2

SA,SR

1 SA

1 A

2 SA,A

2 1 SR

3 A,

A,SR

1

SA2 SA,SR

1 SA

2 SA

,SR

1 SR

2 SR

2 1

4 2S

A,R,

A 1 A

1 SR

1 A

1 SR

2 SR

2 SR

,SR

1 A

1 SR

3 £A

1 SR

2

SA1

SA

11

SA

1 A

3 A,

SA,S

A 1

A 1

SR1

2 A,SR

1 SA

2 SR

1 A

3 SA,2 S

R 2

A, SR

4 R,SR,SA

31

1 SR

1 SA

1 SA/SR

470 1 SA

2 SA-A

112

55

25

40011

12

4 3

12111

1100

2100

5321

>.5

mm

Wgt.

No

. Sh

ape

(gra.

)

28.3

33.7

44

.9

44.8

28.3

42.8

37.2

34.9

32.0

36.3

38.7

27.5

4S.8

23.3

5C.9

33.2

26.5

46.0

46.3

40.7

33.4

37.4

38.4

44.7

53.4

19.0

56.7

65.3

31.9

37.5

49.7

27.8

39.2

38.3

35.1

38.6

35.0

46.7

37.9

44.3

36.9

31.7

43.9

40.3

41.6

41.8

32,3

41.9

31.1

40.4

40.2

20.0

27.2

46.2

32.2

46.1

27.9

41.6

39.7

48.4

31.5

1 54

.4,-

39.6

48.7

32.1

41.6

36.8

48.0

38.8

22.5

34.6

27.0

15.5

18.1

46.1

16.7

36.7

33.0

23.0

28.4

32.8

16.3

36.4

24.4

33.3

46.0

29.7

26.2

16.7

39.1

21.4

42.2

38.9

39.1

20.9

37.3

1 R

.8x.3

22.2

44.0

32.1

31.6

27.8

28.1

42.2

34.3

27.3

34.4

27.7

40.1

34.2

28.9

45.5

30.7

27.5

45.2

30.5

31.1

33.4

24.8

34.6

14.9

21.5

19.3

30.4

25.6

34.9

25.2

32.4

38.8

40.9

32.1

39.5 8.4

36.3

39.0

29.6

19.6

19.1

32.8

20.0

1 (.

7x.3

) 24

.636

.137

.823

.926

.120

.429.0

22.3

22.4

21.3

45.4

28.4

31.4

40.5

19.3

28.2

24.3

28.0

27.0

25.4

25.4

28.7

21.0

2 16

33

0.0

1 65

.3]

33.4

0 9.8

0 96.0

1 13

.0

CONCENTRATE

Ultraviolet

Hag 30

70

80

10 10 30 20 10 5 5 25 5 30 25 30 tr 10 25 40 25 45 25 15 20 b JO Ib 50 10 10 Ib 10 tr 10 ID 2U JO 25 JU J5 15 Jb 30 30 10 35 20 20 10 15 5 20 20 15 10 20 IB 10 10 bO 5 15 25 5 15 20 b 85 30 40 2 15 15 15 10 41) 10 20 20 b 10 10 60 Ib /5 20 bb 'i 1(1 10 Ib 10 5 10 10 15 5 60 20 15 15 30 10 5 30 10 10 40 b 10 15 35 b 10 77 30 30 20 30 10 10 15 6 30tr

5 72 20 10 50 10 10 10 50 20 3 15 15 10 77 3 2 0 80 60 5 30 30 40 45 10 30 30 50 70 50 160 0 fib 23 19 378 61

Py

uar

nisc

.

10 5 5 tr tr tr tr 5 tr tr tr b tr 5 tr tr tr 5 b b tr tr tr tr tr tr tr tr tr 2 b tr tr tr tr tr tr tr tr tr tr tr tr tr 2 L tr 4 tr b b tr tr 5 5 5 tr tr 5 5 Ib tr tr tr tr tr b tr 3 tr tr tr tr 5 1 5 tr tr 1 J tr J tr tr tr tr 5 tr tr b tr tr tr tr 3 2 tr 5 tr tr tr tr 0 2 tr I tr 2 3

tr3

tr

3

tr tr3 3 tr 3 5 1 5 3 5 1 tr 3 tr tr 0 tr 2 5 10 5 tr 3 13 5 10 20 5 20 146 0 :o 2 1 12 9

60

20 10 5 5 10 5 tr 10 15 tr 5 tr 10 10 tr 15 5 tr 5 tr 5 5 tr tr 10 tr

Cpy

tr 5 5 5 15 tr tr 10 tr 5 2 tr 5 10 5 5 5 5 5 tr 5 5 5 15 5 5 10 5 tr tr 5 5 15 5 2 5 Cpy

Cpy

2 tr 3 Cpy

tr tr 10 7 4 5 5 tr tr 10 tr 10 5 5 10 5 40 2 tr 5 5 tr tr 5 5 tr 10 tr 5 tr 5 10 5 5 tr tr tr tr tr tr 3 10 2 5 10 10 5 10 5 5 5 5 5

Cu

5 5 Cp

ytr tr 5 2 5 10 tr 5 5 5 tr 0 tr 0

Cutr 10 5

Cpy

5 10 30 15 13 10 5 15 5 tr 151 0 60 5 7 ^.\ 20

lamp

Sch 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 2 1 1 1 0 1 1 1 1 1 1 0 1 1 1 1 1 1 1 1 1 1 1 1 i 1 2 1 1 2 1 1 0 1 1 1 1 0 0 0 1 1 1 1 1 1 1 1 0 1 1 2 0 1 2 1 1 1 1 1 1 1 2 1 1 2 1 1 0 0 1 1 1 0 0 0 1 1 1 1 1 1 1 0 2 1 0 1 0 1 1 0 0 1 1 1 0 1 1 1 0 1 0 0 2 1 2 0 1 1 1 1 0 1 1 2 0 0 0 1 1 1 2

IbO f) 2 1 1 L 2

Kaa

Zir 2

0 1

0 1

0 2

0 01

01

01

01

01

01

0 02

02

01

01

01

01

01

01

01

02

01

01

01

02

01

01

02

02

02

0 02

0 0 02

01

02

02

02

01

01

01

02

00

02

01

02

01

01

01

01

02

02

01

0 0 01

01

0

2 0

1 0 0

1 0

1 0

1 0

1 0

2 0

2 0

0 0

2 0

1 0

1 0

1 0

0 0

0 0

1 0

2 0

2 0

1 0

1 0

1 0

2 0

1 0

2 0

1 0

1 0

2 0

2 0

1 0

2 0

2 0

1 0

2 0

1 0

1 0

1 0

1 0

1 0

1 0

0 0

1 0

2 0

1 0

1 0

1 0

0 0

2 0

2 0

2 0

1 0

0 0

0 0

2 0

1 0

2 0

i o

1 0

2 0

1 0

2 0

2 0

2 0

1 0

2 0

1 0

2 0

1 0

1 0

1 0

1 0

1 0

2 0

2 0

1 0

1 0

1 0

0 0

1 0

0 0

0 0

1 0

2 0

3 0

0 0

0 0

1 0

2 0

1 0

0 0

1 0

1 0

2 0

1 0

0 0

0 0

1 0

2 0

1 0

1 0

155

160

0 0

3 0

1 0

1 0

0 0

3 0

NOTE

S NORMALIZED V

ALUE

SGOLD

grains

clay r

ich

basal

till

sandy/clay

sandy

basal

till

sandy, s

ilty b

asal t

ill

clayey,

cobb

ley

till

clayey,

cobbley

till

sandy/gravelly a

blation

till

org. ox.

basa

l till

silty

basal

till

ox.

sand

y till

basal

till

silty

basal

till

basal

till

silty, ox.

basal

till

sandy, bouldery t

ill

silty

basal

till

sandy, cbley

ox.

basal

till

silty/clay b

asal t

ill

till (abl

ation);

sheared

vole.

basal

till,

vole.

frag

.bo

uldery,

sandy

till

sand

y dark b

rn b

asal

till

dark

brn s

ilty

/clay

till

grav

el;

sand

ablation

till

ox. /

unox.

basa

l till

clay-rich

unox. b

asal t

ills s

and

sand

y ox.

till

sandy

gravel

ly t

ill

silty

red

brn

till o

n o/c

ox.

till

silty

basal? t

ill

silty

basal

till

basa

l till

silt o

x. basal

till

silty, ox

.bsal

till

clay,silty b

sl t

lclay,silty b

sl t

ill

silty, sa

ndy

basal

till

sand

y, g

ravelly

till

silt

y basal

till

silt

y basal

till

silt

y basal

till

silt

y, c

lay

ox.tl

silty,clay t

lsa

ndy

silty

tl;

abla

tion

till?

sandy/gravely

till

v. sd

y, gv

ly b

sl t

ill

sdy

bsl

tlsd

y, gvly t

ill

silt

y,gvly b

sl tl

boul

dery

bas

al t

ill

cobbly g

ravelly

basa

l ti

llwet

sandy

till

sdy, si

lty

bsl

tl m

af.

vol.

o/c

v. sandy

till

silty, c

layey

till

good b

asal t

ill

sand

y, g

ravell

y till

sdy

slty t

ill

clayey/sandy t

ill; v

ol.

o/c

sar.dy,

basal

till v

ole, o

/cox.

basal

till

; vole,

o/c

grav.

till;

sdy;

S OP V

ole,

o/c

sdy,

grav

. till N

of

vole,

o/c

clay

ey b

asal t

ill; v

ole, o

/c

sdy/

slty b

asal?

till u

nder t

ree

ox, s

lty

bsl

tlox.

silt

y basal

till

ox.

silty

basa

l till

good

basal t

ill

boul

dery s

ilty c

lay

rich

till

ox.

silty

basa

l till

cobb

ley

silty

basal

till

bouldery s

ilty

basal t

ill

gravelly b

asal

till

ox.

silt

y bouldery t

ill

sand

y silty

outwash? t

ill

ox. c

lay

rich t

lox

. /unox.

till

ox.

basal

till

ox. b

asal t

lox

. sd

y bs

l ti

llox.

sandy/clay b

asal t

ill

sandy/silty

basal

till

sandy/

gvly o

x. a

blation? t

ill

sand

y ox.

till

clay

-rich

ox.

till

clay-rich

ox.

till

sandy/clay o

x. t

ill

sandy, clay-rich

till

clay

-rich, unox-ox.

bsl

tlsandy, ox

. ba

sal

till

sand

y so

me c

lay, ba

sal

till

sdy

bsl

tlsdy, ox

. bsl t

lsdy, ox. bsl t

lsdy

gvly t

lsdy,

ox.

basal

till

sdy,

ox. b

asal t

ill

unox.

basal, s

dy t

ill

unox

. sandy

basal

till

clay r

ich, unox.

till

unox

. sdy

bsl

till

unox

. ti

lldrk

brn, un

ox. s

dy-cly b

sl t

lunox. s

dy t

ill

abov

e clay

unox.

sdy,gvly a

blat

ion

till

sdy,

gvly

cly

sandy, c

layey,

unox.

med.

ox. b

asal t

ill

silty, unox.

4 gv

lyme

d.ox

.bsl

silt

y ox.

basa

l

sandy, ox.

till

sandy-clay-rich

unox.

till

ox, ba

sal

till

sdy, ox. ba

sal

till

sdy, slty

, ox. u

nox.

basa

l till

sand

y, ox.

unox.

basa

l till

ox.

basal

till

ox.

sdy

bslt till

unox

, basal

till

sandy, si

lty

unox.

basa

l till

unox., ox.

sandy

basal

till

ox. s

andy,

ox.

basal

till

ox.

basa

l till

sand

y ox.

basal

till

unox

. sandy

till

ox.

unox.

sandy

basa

l till

unox.

till

ox,

unox.

basa

l till

ox.

basal

till

ox.

basa

l till

unox

. basal

till

ox.

basal

till

sandy

unox.

basal

till

unox.

basa

l till

ox,

basal

till

ox.

basal

till

ox.

basal

till

ox.

basa

l ti

llox.

basal

till

unox.

gravelly t

ill

ox.

basal

till

ox.

basa

l till

unox

. semi-till

unox.

slty b

sl t

lunox

. bsl

tlox.

basal

till

silt

y till

ox. s

erai-till

sdy/

gvly t

ill

ox.

with a

ngul

ar frags.

ox.

sandy

till

brow

n silty

grav

elly

till

light

brovn

sand

y

4 2 3 1 0 2 3 1 0 1 0 4 1 0 2 0 1 2 6 2 0 3 8 5 3 2 0 2 2 1 3 33 0 1 2 2 5 3 3 10 8 3 4 0 2 1 4 2 4 5 3 4 7 5 13 4 1 3 2 4 6 1 7 7 5 1 5 3 3 11 3 7 1 0 5 3 0 3 2 3 8 4 0 5 3 8 11 2 4 6 9 13 3 3 5 13 5 0 7 5 0 10 8 1 1 3 9 2 7 7 0 1 2 2 2 0 2 7 1 0 5 3 2 1 7 4 4 3 7 6 6 2 2 3 7 5 4 4 0 2 1 2 0 3 8 2 5 25 3 12 6 10 0 5 1 2 1 0 1 1 4 6 0

1G6 0 33 4 1 17 12

tiULU

microgm

38.8

5.1

18.9

4.5

0.4

1.5

4.0

3.4

24.7

13.6 2.6

26.9 5.5

2.7

4.0

1.0

7,7

4.9

6.6

4.0

2.4

12.4

47.5

25.6 3.9

43.0 4.7

20.2

15.2 0.1

7.7

0.7

4.9

5.6

29.7 2.6

26.9 9.6

34.9

12.6 7.5

26.7

22.2

10.3

23.4

10.2 2.2

5.7

10.6

57.9

29.4 4.6

1.9

32.1

25.0

14.9 2.7

4.5

5.5

4.0

12.4 2.9

9.9

13.8

12.4 8.2

27.5

19.9 9.1

25.5

20.4

14.6

187.

62.8

18.5

27.2

12.7

37.6

12.7

32.2

29.6

59.5 1.8

18.3 0.6

84.6

13.7

38.1

40.0 3.3

34.4 8.8

4.1

27.4

77.0

20.2

159.

810.8

83.5 2.1

3.6

33.3

24.3 8.5

5.3

27.7

40.4

82.3

17.8

21.8

22.7

18.2

54.9

20.8

10.9 9.9

52.6 4.6

8.1

59.2 5.1

4.6

5.8

20.6

34.9

10.0

39.5

14.8

32.9

17.2 6.5

0.9

0.2

21.7

21.1 9.6

42.5

11.2 1.7

1C8.

31.5

0.2

5.6

1.6

73.1 3.2

50.0

33.8

22.2

11.8

95.9

187.6

1.2

71.6 7.1

4.3

31.9 1.4

0.1

4.2

17.5

18.6

10.9 164

0.0

188.3

22. 6

21.8

I'll.

4?5

.2

Au ppb

det

5

1020

135

400

101 12 29 95 90 792

440 55 700 84 50 76 25 222 94 132

100 48 299

1270 324 90

2800 87 390

510 3

122 3

165

105

782 61 833

226

792

311

166

963

556

299

568

208 50 148

304

1450 458

119 58 547

842

315 79 129 90 92 419 58 135

271

423

179

737

386

201

934

696

465

8580 111

344

1430 355

1300 497

1330 835

3600 37 816 14

1980 457

17SO

2170 100

1640 215

102

513

3480 487

6530 252

3140 51 115

1170 493

210

195

541

1180

2240 389

524

334

532

2100 458

466

34$

892

194

349

3600 246

219

362

823

1220 310

1110 407

554

456

159 98 3

500

1090 425

1£90 236 62

5600 28 3159 57

2770 66

1420 302

377

129

2700

5210 24

4180 275

148

1240 43 317

0792

820

484

163 3

86SO 757

1247

tt**+tt

3250

Au mgn

29.3

4.6

18.1

4.5

0.3

1.3

3.9

3.1

25.2

16.2 2.1

26.1 4.4

2.5

4.0

0.8

7.0

4.3

6.1

4.1

1.7

11.1

48.6

14.5 3.7

53.1 3.9

20.8

15.2 0.1

6.1

0.1

6.5

4.0

27.4 2.4

29.3

10.5

30.0

13.9 6.2

30.7

24.6

12.0

23.7 8.7

1.6

6.2

9.5

58.8

18.4 3.6

1.6

25.2

2^.4

14.5 2.2

5.4

3.6

4.4

13.1 3.1

5.3

13.1

13.4 7.4

27.0

18.5 7.8

20.9

24.0

12.5

134.

12.

015.8

23.8

13.3

42.7

11.4

37.5

27.3

58.4 1.3

20.0 0.5

90.9

13.7

46.9

29.8 3.9

34.9 9.0

3.9

20.0

72.0

18.0

141.

411.1

100.

71.

63.2

32.6

20.8 7.2

5.3

18.5

32.5

89.7

13.2

15.1

15.2

16.4

57.6

20.7

14.2

10.7

29.7 4.9

8.7

53.5 5.3

4.2

11.0

21.1

42.5 7.8

35.0

15.8

39.0

14.6 6.3

0.8

0.1

23.4

32,0 8.3

32.1 7.7

: .2

151.9

1.0

0.1

4.2

1.5

56.3 1.9

31.5 6.8

8.1

5.9

76.7

111.7

1.0

77.0 7.7

4.6

34.8 1.2

0.1

4.3

20.1

23.6

10.2 163

0.1

161.9

20.5

?6.8

715.9

74. C

Ag ppm 5 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 j 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 j 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3

163 3 3 3 0 0 3

As Ppm 2 4 2 1 1 3 2 1 3 3 1 2 4 1 1 1 2 1 1 4 1 4 1 1 1 1 1 1 1 fc 1 9 1 1 6 10 7 7 13 10 5 8 8 6 11 14 10 10 1 8 8 1 3 3 5 10 10 10 11 7 3 12 1 8 6 1 9 7 7 5 8 .J 5 1 6 5 1 7 1 7 4 4 6 3 1 14 7 1 6 7 1 1 6 1 5 5 4 4 1 7 1 6 3 1 9 4 1 1 1 1 1 1 3 5 3 4 6 4 1 1 1 1 1 1 16 5 13 12 1 8 12 6 41 8 6 1 6 5 5 12 5 2 4 10 4 15 1 1 8 1 1 4 1 3 6 6 9 b 3 9 5 1 1 1

1C3 I 41 5 5 22 14

Ba ppm

200

560

100

400

350

450

360

380

650

460

500

590

100

420

530

430

- 100 42

032

042

0100

500

100

360

100

400

690

390

220

100

400

270

220

100

260

100

420

100

100

220

100

260

100

100

100

100

360

290

100

100

100

100

330

100

100

260

100

100

100

530

100

100

240

100

300

100

100

100

220

360

100

100

270

370

430

280

100

100

100

360

320

100

100

450

100

500

360

100

100

100

100

480

600

380

100

100

260

440

240

100

290

100

100

100

240

300

330

280

430

390

ICO

100

100

580

100

430

430

290

100

300

100

100

100

530

100

280

280

100

340

330

100

100

850

630

100

220

100

100

400

100

100

100

100

100

120

100

100

100

380

330

300

100

360

380

680

100

100

310

420

100

100

100

130

380

163

100

850

247

170

2902

5bS

8

Br ppm 5 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 j 3 3 3 3 j 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 j 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3

163 1 3 3 0 0 3

Ca X 1 1 3 2 3 5 1 3 6 1 1 6 1 1 4 1 1 5 1 1 2 1 3 1 3 2 7 2 1 1 j 1 1 4 3 2 1 2 2 2 1 2 3 3 4 1 1 2 1 1 I 4 3 5 2 1 4 2 1 3 1 3 2 1 1 5 2 1 2 3 1 1 1 5 7 3 1 1 1 1 1 1 1 1 1 6 1 1 1 1 1 1 1 1 4 1 1 1 1 4 5 1 1 1 4 4 4 1 1 3 3 1 1 1 1 1 3 2 5 1 6 1 1 1 1 1 1 3 1 1 1 1 1 1 1 1 1 1 4 3 1 1 3 1 2 3 4 1 3 6 4 1 1 2 5 4 1 4 5 1 6 1 5 7

iC3 1 7 2 2 3 5

Co ppm 5 14

28

18

15 21 17 17 86 18 21 23 26 28 19 22 36 19 17 23 19 29 23 21 31 12 n 19 35 23 20 78 180 22 20 56 19 22 24 31 22 22 24 21 21 31 24 35 23 29 78 18 17 16 25 35 26 27 29 19 11 24 120 25 21 26 19 18 18 20 27 17 19 22 23 24 35 23 19 22 25 20 34 21 26 30 21 15 35 30 6 16 27 16 20 31 23 29 21 26 22 32 18 23 31 24 25 27 23 16 22 20 29 28 22 15 29 31 24 38 32 12 12 25 27 26 30 20 16 21 31 19 100 39 15 22 47 25 18 70 35 43 24 58 43 30 18 24 19 31 9 22 27 10 32 27 27 25 21 39 45 25 78 15 163 f.

1^0 27 19 "j2 65

Cr ppm 10 210

660

300

300

320

3SO

470

1900 310

550

440

470

260

390

390

270

260

300

320

450

530

840

600

610

220

430

340

700

540

340

570 75 890

530

540

340

510

510

370

390

340

430

430

380

360

330

270

440

450

330

210

250

210

290

780

340

380

330

270

?40

520

2700 540

530

1700 350

540

310

230

620

640

280

240

240

220

850

470

230

460

360

310

540

200

670

210

450

350

750

730 no 410

300

310

300

1500 550

460

370

600

370

640

1200 410

370

560

€00

780

1400 550

490

530

720

540

230

290

480

380

4fiO

530

820

280

310

560

590

480

460

340

220

390

400

360

180

210

360

450

1500 470

360

480

350 43 180

170

210

1300 660

790 97 220 99 460

2200 77 980

830

560

600

450

590

480

450

240

190

163 43

"CO

494

362

H1C85

1218

Cs pptn

2 1 1 1 1 1 1 3 1 1 1 1 i 1 1 1 1 3 1 1 1 1 2 1 1 1 3 1 1 2 1 1 2 3 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 3 1 1 1 1 1 2 1 1 2 1 3 1 1 1 1 1 4 1 1 1 1 1 1 2 1 3 1 1 1 1 1 1 1 1 1 3 1 1 1 3 3 1 1 1 1 1 3 1 1 1 1 1 1 1 1 1 1 1 3 1 1 1 1 1 1 1 1 1 2 1 1 1 1 2 1 1 1 1 1 5 1 1 1 1 1 1 1 1 1

153 1 5 1 1 0 3

Fe 0.0

6.6

19.9

15.6

8.8

11.8

11.4

11.7 9.1

11.5

15.3

11.6

16.8

10.7

15.2

14.2

17.6

10.2

11.2

13.4

14.8

23.7

25.3

19.9

25.6 9.3

12.8

16.3

38.7

22.9

13.1

15.3

13.2 7.9

8.7

15.7 7.7

14.6

16.8

16.4

15.5

16.4

18.5

17.1

14.0

17.0

19.7

23.8

22.4

28.9

23.7

11.3

10.3 9.4

16.7

28.1

16.6

17.7

23.5

11.7 5.1

17.2

40.3

12.7

12.5

18.0

14.6

19.3

13.0

13.3

25.7

20.6

13.2 8.1

10.6

11.0

33.1

16.3

16.6

22.0

18.4

18.6

32.8

12.8

30.9

12.9

24.7

11.1

34.1

25.1 4.0

9.2

15.2

12.8

13.5

25.5

17.0

23.0

16.8

24.7

12.3

25.0 8.4

16.2

17.7

15.9

14.5

21.7

16.3 8.3

18.8

14.8

28.2

17.3

16.7

11.2

19.7

25.6

37.3

31.6

40.1

13.9

18.7

24.3

31.9

28.0

25.3

19.0

14.9

23.7

24.3

17.7

25.9 5.9

17.0

24.6

. 25.0

25.0

14.4

28.7

32.5

38.4

14.1

13.3

30.3

25.2

15.3

26.9 8.3

7.9

5.3

19.4

35.0 3.0

27.7

17.6

19.9

19.5

12.7

32.7

34.9

13.2

19.6

13.7 163

3.0

j r>

t•} U

. j

18.3 7.3

C1.8

34.0

Hf ppn 1 64

72

43

42 69 34 29 55 110 53 67 29 45 30 39 75 60 37 43 41 bl 84 230 33 74 480 50 58 140 56 25 5 63 23 33 24 28 36 27 43 35 35 51 77 33 27 30 80 67 29 29 50 42 28 76 31 39 32 22 29 44 2 19 21 71 23 34 32 21 63 63 36 42 26 11 80 41 37 44 17 25 55 34 89 19 26 120 71 200 37 120 23 33 22 51 26 21 35 27 28 32 65 15 11 35 15 34 50 47 25 20 28 63 18 50 29 25 60 55 60 37 28 86 76 34 46 26 15 27 35 36 17 5 36 56 36 32 40 93 20 1 12 16 7 35 48 78 13 9 14 41 45 3 78 34 50 54 72 45 43 77 100 83 H31

4oO 47 46

2123 ISO

Hg ppm 5 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 1 3 H 1 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 j 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 j 3 3 3 3 3 J 3 3 J 3 3 3

1G3 3 3 3 0 0 3

Ir ppb 40 20 20

20

20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 :o 20 20 20 20 20 :o 20 20 20 20 20 20 H: :o :o 20 0 0 :o

Mo ppm 20 10

10

10

10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 1C 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 :o 10 10 10 10 10 10 10 10 10 10 10 10 1C3 •f] :o 10 0 0

!(•'

1C

Na ppro

500

19100

14300

16000

1550

015400

15500

18500

1110

016200

15200

1530

012500

14300

13600

14300

1150

016

300

1510

015

400

14300

1530

014SOO

1250

014000

1970

022300

181C

O5910

1030

012900

1270

016

SOO

1810

018

2CO

13100

1980

015700

13600

1320

013200

1400

015

100

1340

017

500

15700

1440

015300

1260

011

800

1310

013

500

17600

1820

013100

10200

9140

12200

1300

013

000

1820

012

700

2880

16900

ISIO

O13

000

1320

012

400

13200

1380

010

800

1170

019

800

I420

C12300

1730

07670

1470

0

1170

010

700

1560

012200

6660

1580

09190

1540

09460

1090

07250

1050

0

7600

2050

036900

1640

016

500

1390

014

100

1740

015100

1400

016200

1250

019

900

1420

017

100

1440

016

400

1630

011

700

1770

014

500

1410

08770

132C

O

1330

019

200

1340

012

900

1110

097

8010

100

4170

4720

9880

9450

1100

012

800

15600

18200

122C

O13400

15000

1190

022

400

H200

12900

1360

017500

1C500

9590

1000

02240

14900

1340

0^40

1560

013900

8150

16200

1C4C

O16

^00

16700

7470

23400

15630

17SO

O12300

16200

2C300

11900

8510

1190

010

400

18100

163

7*1'!)

36SJO

17° 8

ft<"71

5 7 tb

. '2

2:131

Ni ppn

200

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

ICO

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

200

100

100

100

100

100

100

100

100

100

100

100

100

100 inn 100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

ICO

100

100

100

100

100

100

120

100

100

100

100

100

100

100

130

ICO

100

100

100

100

100

100

100

100 mo 100

100

ICO

100

100

100

100

ICO

100

163 :oc 200

101 8 61 nc

Rb 50 78

25

25

25 25 25 25 25 25 93 25 25 25 25 25 25 25 25 25 25 89 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 51 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 70 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 60 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 62 65 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 60 25 25 25 25 25 25 25 25 25 25 25 75 25 25 25 25 25 25 25 1C w 25 25 25 r,7 163 it t. j 93 "'8 12 134 51

Sb ppia

0.2

0.1

0.3

0.2

0.1

0.3

0.3

0.2

0.4

0.1

0.1

0.1

0.3

0.3

0.3

0.5

0.1

0.1

0.1

0.7

0.1

0.1

0.6

0.1

0.4

0.1

0.1

0.1

0.1

0.5

0.1

0.1

0.5

0.3

0.4

0.3

0,4

0.1

0.8

0.1

0.1

0.4

0.5

0.1

0.1

0.5

0.1

0.1

C.I

0.4

0.4

0.3

0.3

0.4

0.3

0.4

0.3

0.4

0.3

0.5

0.6

0.6

0.5

0.1

0.3

0.1

0.5

0.3

0.3

0.4

0.7

0.1

0.1

0.1

0.1

0.3

0.8

0.4

0.1

0.1

0.4

0.1

0.1

0.4

0.1

0.9

0.5

0.6

0.7

0.1

0,1

0.5

0.6

0.1

0.6

0.1

0.1

0.1

0.1

0.5

0.1

0.6

0.1

0.3

0.3

0.4

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.3

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

1.7

0.1

0.8

0.6

0.1

0.1

1.1

0.1

0.1

0.1

0.1

0.5

0.6

0.1

0.6

0.1

0.1

0.4

0.5

0.8

0.3

0.1

0.1

0.1

0,3

0.6

0.1

0.1

0.1

0.3

0.7

0.1

0.1

0.1

0.1

G.7

C.6

P.I

0.5

0.1

163

0.1

1.7

0.3

0.?

0.1

0.8

Sc ppm 0 32 21

16

17 22 16 14 24 21 22 25 18 18 19 18 18 23 18 18 16 22 24 40 27 21 39 18 14 29 29 16 29 28 20 24 19 23 25 25 25 30 22 22 23 22 20 25 32 27 23 33 29 34 27 36 32 34 24 26 19 27 12 22 18 31 24 28 24 22 32 27 19 29 35 16 41 25 28 29 19 26 44 22 41 27 18 59 40 48 22 41 33 27 22 31 24 76 26 71 30 32 44 21 19 34 25 22 29 24 16 13 15 25 24 21 29 29 26 43 46 29 18 41 40 28 34 26 21 36 35 30 50 72 17 27 34 27 30 32 37 21 28 30 17 31 34 43 29 49 21 17 35 11 30 23 24 23 22 33 33 67 ?8 23 163 11 t7 77 9 78 45

Se ppia

20 10

10

10

10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 ' n 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 163 10 10 10 0 0 :o

Sr \ 0.2

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0,1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

C.I

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

Q.I

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0,1 fl.l 0.1

0.1

0.1

163

'J.I

0.1

0.1

0.0

fl.O

0.1

Ta ppn 1 1 1 1 2 1 1 1 1 1 4 1 1 1 1 1 3 3 1 2 4 1 4 5 1 4 10 3 6 4 3 2 1 3 2 2 2 3 17 9 5 6 6 5 4 3 4 j 6 4 6 4 8 5 4 8 3 4 5 3 3 4 1 3 3 6 3 8 5 1 8 6 6 1 1 2 9 6 4 6 4 7 7 3 10 2 9 12 12 23 4 11 1 3 1 5 4 6 3 8 3 3 7 2 2 4 3 3 5 1 3 1 2 5 4 5 5 10 9 9 9 6 21 11 9 9 5 8 4 6 8 1 1 1 6 11 6 4 4 3 70 1 1 2 1 22 8 13 1 1 3 6 78 1 6 3 1 1 2 4 6 12 1 4

163 1 :c •j 4 20 - 1

Th ppra 1 53

26 13

36 14 11 17 9 19 21 23 22 14 19 21 14 24 20 17 24 21 30 64 7 27 55 20 23 57 39 7 2 i j 7 7 5 15 20 17 21 20 18 22 20 15 12 10 26 23 18 1? 74 14 14 26 14 13 14 11 U 19 1 11 12 32 18 28 17 13 39 30 13 22 10 5 43 17 34 31 17 27 54 22 120 9 53 100 91 200 31 68 17 19 16 33 24 79 77 45 19 25 56 12 14 21 12 22 54 19 14 7 16 58 29 52 37 41 67 85 150 75 69 86 79 55 42 34 20 33 32 35 9 6 57 47 27 28 33 17 30 1 10 8 5 28 28 50 6 5 4 75 S3 2 44 11 :s 22 13 13 16 58 14 10 163 1

3CO 79 37 719 S3

U ppra

0.5 6 4 2 3 4 3 3 6 4 3 3 0 0 4 4 6 3 3 0 4 4

4.20

9.80

3.50

2.60

15.0

03.10

0.25

7.70

3.90

1.40

0.25

2.50

1.10

l.ftQ

1.80

2.20

3.80

4.10

0.25

3.50

0.25

0.25

3.20

3.30

2.50

1.90

4.90

3.70

2.70

2.40

4.30

2.50

3.10

4.00

2.10

2.00

2.10 1.7

0.3

4.3

0.3

0.3

2.8

7.4

2.4

3.8

2.4

2.9

7.5

3.4

0.3

4.5

0.3

0.3

6.4

3.3

3.4

3.7

4.1

0.3

6.8

3.3

11.0 0.3

4.3

10.0 8.9

20.0 0.3

9.3

2.7

0.3

0.3

4.4

3.1

2.7

3.4

3.9

0.3

3.4

6.7

0.3

0.3

2.4

0.3

3.4

5.1

3.6

2.4

1.8

3.0

6.6

2.9

7.5

3.3

5.7

7.9

7.4

13.0 8.1

5.6

9.6

10.0 4.9

5.5

3.1

1.5

5.2

5.2

3.1

0.4

0.3

0,3

5.8

0.3

4.6

3.7

4.2

4.5

0.3

0.3

0.3

0.3

4.0

4.7

5.3

1.7

1.9

0.3

3.7

8.9

0.3

5.3

1.5

2.5

5.5

3.3

3.8

3.6

6.7

2.8

3.0

1G3

n.3

70.0 3.6

3.0

B.1)

9.1,

V ppm 4 2 8 14

14 18 7 12 2 2 2 1 2 5 2 5 2 2 2 9 2 11 2 2 2 2 2 2 2 2 8 2 2 2 2 8 2 2 9 2 2 2 2 2 2 2 2 9 2 7 2 19 7 11 10 5 2 55 2 2 14 2 2 10 2 39 13 6 17 130 2 2 2 2 8 23 2 11 2 10 2 2 2 23 2 2 32 24 16 2 52 2 2 4 8 2 19 7 4? 24 11 24 2 2 2 2 2 9 6 2 2 2 2 41 2 12 47 2 20 23 13 25 2 2 15 2 2 2 2 2 2 2 2 2 2 2 2 2 2 18 2 12 2 2 45 18 38 2 2 2 12 5b 2 25 9 2 2 15 6 :o 25 2 2 ;(,3 2

uc ;o i r

j .1

10 S 40

Zn ppro

200

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

ICO

100

100

100

100

100

100

100

100

100

100

100

100

100 :oo 100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

320

ICO

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

1GO

100

100

100

100

100

100

100

100

100

100

100

240

100

100

100

100

100

100

100

100 :oo 100

100

100

ICO

100

100 ino 100

ICO

100

100

100

100

100

100

100

100

ICO

220

230

100

100

163 : oo 370

JtM 74 rng

153

La ppm 1

130 75

43

28 34 30 40 23 50 46 68 52 64 50 59 45 80 61 53 63 57 75 170 28 65 150 56 58 140

110 28 10 49 28 32 23 4.3 67 55 68 58 58 73 72 51 42 31 89 66 51 39 72 45 47 85 42 45 43 33 37 58 8 38 39 95 55 81 56 40 120 90 44 67 37 20 120 55 79 80 46 65 130 61 300 29 120

280

220

490 62 190 49 56 48 95 64 77 75 120 57 76 150 33 36 67 38 67 150 59 41 23 45 160 73 150 95 100

190

230

400

200

170

240

210

140

120 87 51 88 91 100 37 76 180

120 75 72 95 55 72 7 28 30 19 92 94 150 34 16 17 60 170 10 120 38 79 74 49 $4 58 170 86 51 163 7

490 !!2 C7

4461

. 215

Ce ppm 3

200

120 70

40 55 40 54 44 78 68 93 74 no 73 82 79 140 87 86 91 94 120

240 47 93 250 88 82 210

160 42 19 73 43 49 38 54 90 50 100 94 85 100

110 75 72 60 140

110 B4 7? 110 79 76 130 61 75 65 47 51 88 15 60 58 HO 31 120 82 58 180

130 75 110 71 36 190 86 120

140 76 100

200 90 420 54 170

410

320

740

120

290 79 85 78 150 91 120 no 180 92 120

230 56 54 100 62 100

190 98 62 39 71 220

100

210

140

140

270

340

500

280

240

340

320

210

180

130 78 120

140

140 84 120

240

180

120

120

140

120

170 16 43 59 32 140

ISO

270 C4 78 34 170

2'-0 17 180 60 120

110 73 R9 30 240

190

100

163 15 710

KM 97

'C'!

9

318

Nd ppm 10 83

47

25 19 26 10 34 40 42 40 67 36 63 38 27 43 100 51 51 40 49 41 94 25 41 130 40 24 73 58 24 25 47 24 27 17 42 40 56 53 43 45 63 55 58 39 28 50 45 32 39 49 50 29 47 28 33 28 36 45 44 5 5 35 86 49 58 48 33 no 62 44 60 63 28 100 50 63 67 34 60 130 53 230 15 87 220

160

370 39 no 30 32 22 50 30 49 34 67 37 38 78 16 22 34 23 47 93 67 44 26 34 120 48 120 72 71 no 120

220

100

100

120

130 71 67 43 36 48 49 54 39 58 93 73 57 46 54 45 44 5 18 45 18 70 93 no 53 33 24 63 100 5 84 30 58 47 32 46 16 81 110 52 153 5

37C '.'8 44

]UC

147

5m ppm

0.1

13.0

8.9

6.0

4.7

5.8

4.1

5.1

9.8

7.2

5.7

7.7

5.8

11.0 6.1

6.7

7.5

13.0 7.4

8.0

7.1

7.6

8.6

18.0 4.5

7.2

20.0 7.2

4.9

13.0 9.8

4.1

3.5

6.7

4.2

5.3

3.7

6.0

8.2

7.5

8.4

8.3

7.6

9.2

9.8

6.8

7.2

6.0

11.0 8.6

6.2

7.6

8.7

8.6

6.3

9.6

5.5

6.6

5.6

5.1

4.8

7.4

2.9

5.7

4.9

13.0 7.3

9.3

7.4

5.7

15.0

10.0 6.8

10.0

10.0 4.2

17.0 8.0

9.4

9.6

5.7

7.3

15.0 7.9

29.0 6.1

11.0

29.0

23.0

52.0 1.2

18.0 5.5

5.6

4.9

8.9

5.7

7.8

6.7

9.9

6.0

7.7

14.0 3.6

3.9

5.7

4.3

6.6

14.0 9.5

6.1

3.7

6.4

17.0 8.0

16.0

11.0

11.0

16.0

21.0

35.0

15.0

14.0

19.0

19.0

11.0

12.0 8.6

5.1

7.0

8.9

8.9

9.5

7.0

14.0

17.0 8.6

7.9

9.2

12.0 8.7

2.6

4.4

6.7

3.7

12.0

17.0

18.0

12.0 3.9

4.7

9.4

19.0 2.2

13.0 5.2

8.5

8.2

6.6

8.2

6.1

17.0

19.0 9.8

IG3

2.2

'.0.0

9.S

f.l

37.

f,71.8

EuTb

ppm

ppm

0.2

2

2.2

2.2

1.7

1.4

2.0

1.2

1.3

3.3

1.9

1.0

1.7

1.2

2.8

1.3

0.1

2.2

3.0

1.5

1.8

1.5

1.7

1.9

3.8

1.4

1.9

6.0

1.9

1.2

2.2

1.6

1.3

1.2

1.8

1.1

!.6

1.2

1.4

1.5

1.3

1.4

1.8

1.2

1.5

2.0

1.4

1.3

1.4

2.3

1.8

1.0

1.7

1.5

2.0

1.3

2.2

1.3

1.5

1.3

1.1

1.1

1.4

1.3

1.0

1.1

2.5

1.3

1.4

1.3

0.7

2.3

1.5

1.5

2.0

2.3

1.0

2.8

1.8

1.3

1.4

1.2

1.1

2.0

1.2

2.2

1.4

1.0

2.8

2.5

4.5

1.1

3.0

1.3

1.1

1.1

1.7

1.0

1.4

1.4

1.4

1.2

1.7

2.4

0.9

0.7

1.3

0.9

1.6

1.5

2.0

1.6

1.0

1.3

2.0

0.9

2.1

1.4

1.0

1.9

1.8

2.5

1.2

1.0

2,9

2.0

0.9

1.8

1.3

0.8

1.0

1.8

1.5

3.1

2.0

1.5

1.7

2.1

1.4

l.s

3.6

1.3

1.0

1.1

2.0

1.0

1.7

3.0

2.1

4.2

1.5

1.4

1.5

1.0

0.7

1.8

1.3

1.7

1.9

2.0

2.2

2.0

2.6

3.9

2.3 :u

:•0.

16.0

1.7

0.8

0.6

3.2

1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 3 1 1 3 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 X 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 2 1 1 1 1 2 1 1 1 i 1 1 1 1 1 1 1 3 1 5 1 1 1 1 5 1 1 3 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 2 1 1 1 1 1 1 1 2 T C J 1 1 2 1 1 1 1 1 3 1 T J 1 1 1 7 • 1 ; -. i 7 4 i I * - - 1 • j. '- • • -, - :: :

Yb ppm

0.2

7.4

4.3

3.0

4.1

6.1

3.6

2.8

3.8

6.4

6.4

5.4

3.7

4.1

3.4

3.8

4.9

4.7

3.3

3.6

3.3

4.5

5.7

11.4 4.1

4.8

17.4 3.6

4.0

9.3

7.6

3.4

5.3

6.1

3.1

4.7

3,2

4.3

6.4

5.8

5.6

7.5

5.6

6.3

8.2

5.3

5.0

6.0

8.6

8.3

4.9

5.9

6.0

6.3

5.4

8.5

5.2

5.7

4.7

4.7

3.2

6.5

2.1

4.8

3.0

7.5

5.3

6.9

5.4

4.3

8.9

7.8

4.0

5.8

5.5

2.7

12.6 5.5

7.1

6.9

3.7

6.1

13.0 4.3

11.5 4.9

4.3

15.9

10.0

15.5 5.5

12.0 5.1

5.3

3.7

6.1

4.8

5.4

4.6

3.9

5.1

6.5

3.7

3.1

2.7

7.0

3.6

4.5

6.7

5.6

3.8

2.6

2.5

5.6

5.1

4.3

6.1

7.3

5.9

10.0

10.5 6.5

4.6

10.5

10.1 6.8

7.9

5.5

4.3

8.3

8.3

5.1

13.3 2.8

4.0

8.7

7.2

6.1

6.1

6.8

8.5

3.2

5.3

5.1

3.5

8.5

9.4

12.7 4.8

4.3

2.9

4.0

:o.8

1.1

9.2

5.7

6.6

6.1

4.3

7.5

7.9

19-0 9.5

5.8

163

i i

15.0 6.2

2-9

8.6

12.0

Lu ppm

0.1

1.5

1.0

0.6

0.9

1.1

0.8

0.6

0.8

1.4

i i

1.1

0.8

0.8

0.7

0.8

0.9

1.0

0.7

0.7

0.7

0.3

1.2

2.3

0.7

1.0

3.6

0.8

C.8

1.9

1.5

G.6

0.9

1.1

0.6

0.8

0.6

C.9

1.2

1.1

1.1

1.3

1.1

1.3

1.5

1.0

1.0

1.2

1.7

1.5

1.0

1,1

1.1

1.7

1.0

1.6

1.0

1.1

0.9

0.9

0.7

i.l

C.3

C.9

0.6

1.4

1.0

1.3

1.0

0.8

1.7

1.4

0.9

1.1

1.0

0.5

2.6

1.0

1.4

1.5

0.7

1.1

2.2

0.9

2.2

C.9

D.7

3.2

2.2

3.3

1.2

2.4

0.9

1.2

0.8

1.4

1.0

1.0

1.0

0.8

1.1

1.4

1.9

0.6

0.6

1.1

0.6

C.9

1.3

1.2

0.8

0.5

0.6

1.2

1.0

1.0

1.1

1.3

1.2

2.0

2.5

1.4

1.0

2.0

2.1

1.4

1.4

1,0

0.8

1.6

1.5

1.2

2.4

0.4

0.8

1.5 1.4 1.2

1.2

1.4 :.i 0.5

1.0

C.8

0.6

1.6

1.5

7.4

0.8

G.7

0.5

C.8

7.3

0.2

1.6

1.0

1.1

0.6

0.9

1 Cf

1.4

3.1

1 R

1.0

-.53

- i £

i ?

' C

" 7

.- . j

Mass gm

28.7

3 34

.07

45.2

8 44

.70

28.1

346.07

41.04

34.69

31.63

36.5

638

.67

37.24

52.1

327.59

53.11

33.9

731.33

45.9

245

.00

40.58

34.49

37.23

38.30

44.70

41.2

718

.98

45.00

53.20

31.7

537,

;:249.71

2'7.7

7

33.54

38.3

.235.09

38. 5

535.23

46.51

37.^

244

. C3

37.23

31.84

44.23

40.23

41.67

41.9

132

.57

41.32

31.30

40.52

40.15

29.91

27.2

545.36

32.50

46.09

27.5

841.58

39.57

48.32

31.17

53.99

39.34

48.33

31.72

41.5

536.70

47.39

38.7

322

.42

34.44

26.3

915

.45

17.6

845.93

16.5

535.57

32.83

22.32

28.1

732.74

16.2

136.74

24.5

033

.15

45.9

229

-88

75.18

13.7

4

3S.9

521.28

41.98

38.7

139

.00

20.6

937.00

21.66

43.94

32.06

31.4

227.54

27.90

42.1

434.20

27.17

34.2

527.54

40.0

334

.05

28.89

45.51

30.74

27.44

45.1

030

.42

30.99

33.32

25.1

824

.83

14.8

721.47

19.1

930.28

25.6

234.86

25.1

432.39

38.78

4C.8

431.99

39.39

8.26

36.0

5

38.96

29.3

819

.55

18.98

32.73

19.84

24.5

335.11

37.60

24.9

475.79

20.33

28.8

072.17

72.40

21.47

45.37

28.40

71.4

340.40

18.41

•? 07

31.3

376.05

27.03

24.47

75.34

25.39

28.76

21.0

8

163

8.26

53.99

33.40

9.16

83.86

51.7

2

CHAKAC

As ppm

1.0

3.1

1.9

3.0

2.2

1.2

1.3

3.1

3.4

2.1

i.l

2.1

6.0

3.3

4.7

1.9

4.5

3.6

3.4

3.1

3.3

4.3

1.6

2.5

3.2

1.7

1.3

1.6

3.7

3.4

5.0

3.8

2.5

3.6

6.6

4.4

3.8

4.8

5.7

3.1

4.5

4.2

5.0

4.1

2.7

5.7

4.2

4.2

2.4

3.7

3.6

2.6

10.0 1.9

1.9

1.9

3.4

3.4

3.7

8.1

4.4

1.4

3.1

4.6

1.5

3.5

5.5

6.0

5.5

2.7

2.6

2.4

2.4

6.3

3.0

2.1

2.3

2.1

5.5

13.0 4.6

4.3

4.6

3.7

8.4

4.9

2.7

3.7

3.2

1.4

3.5

4.0

3.3

4.5

5.2

3.4

11.0 2.9

6.0

4.0

7.9

2.2

6.7

5.6

2.3

3.9

3.2

1.5

5.5

3.5

1.9

4.5

2.6

3.2

1.1

4.5

2.1

1.9

1.7

2.2

2.3

1.1

1.0

3.1

10.0

26.0

10.0 6.3

8.3

7.1

3.5

8.8

3.8

2.3

0.5

1.6

11.0 7.5

3.5

10.0 1.5

5.8

3.0

4.2

5.2

2.8

3.3

9.0

12.0 3.0

1.8

3.6

3.4

2.3

5,2

5.1

4.2

5.5

157

C.5

25.0 4.2

2.9

8.5

10.0

Sb

ppm

0.2

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.5

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

D.I

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.5

0.5

0.1

0.6

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.6

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

O.I

0.1

0.1

0.5 2.1 0.1

0.1

0.1

0.4

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

'0.1 0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

1.0

0.5

0.1

0.1

0.4

0.1

0.1

0.1

0.1

0.1

0.1

0.7

0.1

0.1

0.1

0.1

0.1

0.5

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.7

0.1

0.1

0.6

0.6

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.7

0.1

0.1

0.1

0.1

0.7

0.1

0.1

0.1

0.8

0.7

0.1

0.1

0.1

0.1

0.2

0.1

0.1

0.1

0.1

;57

0.1

1.0

0.2

0-2 c.o O.S

Cu ?Pi 1 13 10 16 14 9 5 9 14 24 3 17 55 25 1C 15 :o ^0 18 31 19 11 11 5, 65 8 12 6 15 14 10 32 53 58 25 51 16 25 41 19 33 22 33 23 25 30 31 44 27 36 20 22 75 37 25 26 23 52 30 17 17 75 22 57 6 21 43 30 46 16 14 75 37 44 33 10 35 14 86 64 89 55 45 31 57 21 9 17 57 S 55 24 30 36

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35 196 54 39 53 147 73 35 81 31 53 30 31 53 39 23 49 44 23 15 39 41 21 14 19 25 13 11 18 25 62 71 71 bl 37 30 84 9 10 12 32 59 88 49 es 135 54 99 131 60 13 13 27 LI 14 47 16 30 10 28 12

11 13 !f,e 0:% 36 29 tb7 I*,

TER

£.'/

.?LE

S

Zrs

pprc 1 39 30 42 G8 •10 31 12

5126 56 49 46 60 56 79 32 95 52 25 34 1 1 Li, 27 93 5.8 79 72 55 66 121

ICO 0 1

-' A

119 74 no 83 76 68 62 47 65 36 59 42 34 52 57 65 85 35 57 77 58 43 58 47 30 48 49 38 20 70 70 95 84 35 43 50 37 58 55 47 24 56 58 51 91 39 40 62 65 44 46 72 24 136 31 19 37 64 TO

L. U 52 44 34 44

48

40 62 31 32 49 62 47 54 67 46 50 33 28 56 135

114 96 36 31 35 51 66 27 57 35 34 39 25 32 67 53 51 45 43 24 £4 HO 34 43 10 46 55 57 116

1C4

1:3 £6 ?4 122 SI 58 44 ;C4 137 , i 43 51 42 69 ^6 £6 60 t\ " ~ i . j

* -

"!*

.. V

= 0 c? ?;: Ila

Ag ppm

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.2

0.1

0.1

0.2

0.3

0.1

0.1

G.I

0.1

0.1

C.I

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

C.I

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.2

0.1

0.1

0.2

0.3

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.5

0.2

0.2

0.1

0.1

0.1

0.1

0.1

0.3

0.3

0.2

0.1

0.2

0.2

3.1

0.1

0.6

0.1

0.1

0.1

0.1

0.1

0.2

0.1

C.I

0.2

0.1

0.1

0.1

0.2

0.1

0.1

0.8

0.1

0.1

0.1

0.2

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.2

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.4

C.I

0.2

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.4

0.1

0.1

0.4

0.2

0.1

0.1

157

0.1

0.8

0.1

0.1

O.C

0.3

Pb

ppm 2 9 3 3 7 3 3 4 11 4 4 5 4 4 8 1 5 i 3 1 1 4 5 1 5 3 1 4 5 7 9 6 1 4 3 5 1 1 1 1 3 3 1 3 1 3 4 6 T X 4 6 4 5 4 i 1 1 i 1 i j. 3 1 6 I 1 1 6 5 7 6 5 4 13 13 11 7 4 6 7 5 6 4 6 3 6 4 5 3 5 3 7 7 5 8 8 6 8 4 4 6 10 5 7 10 9 9 5 4 11 12 15 7 5 6 2 8 4 3 4 5 7 3 2 4 5 12 6 3 6 5 10 8 1 3 1 3 4 7 9 13 4 6 6 10 11 6 6 9 11 6 4 8 5 11 4 6 4 4

158 0 15 5 3 Q

11

Aa

p?b 5 3 3 3 3 3 3 55 3 3 3 3 3 •> j 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 •> 3 3 8 3 3 3 3 3 3 3 3 3 3 3 3 3 3 i 3 3 3 3 3 3 38 12 77 3 •> 3 3

219 3 3 3 3 3 6 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 71 3 3 3 3 3 3 3 3 3 3 3 3 11 3 3 3 65 3 3 3 12 3 10 3 3 3 3 9 3 3 3 3 3 -> 3 3 3 3 3 3 3 3 3 3 8 3 3 3 6 3 8 5 6 3 3 3 3 3 3 3 3 11 28 £ 3 3 3 5 7 5 6 6

1:8 n 0

219 7 23 1 n t

-. . j 47

NORMALIZED V

ALUE

no

rmal

ized

to

20

of -6

aim

nateria

GOLD

GOLD

grains

micr

ogr

4 2 3 1 0 2 3 1 0 1 0 4 1 0 2 0 1 2 6 2 0 3 8 5 3 2 0 2 2 1 3 33 0 1 2 2 5 3 3 10 8 3 4 0 2 1 4 2 4 5 3 4 7 5 13 4 1 3 2 4 6 ^ 7 7 5 1 5 3 3 11 3 7 1 0 5 3 0 3 2 3 8 4 0 5 3 8 11 2 4 6 9 13 3 3 5 13 5 0 7 5 0 10 8 1 1 3 9 2 7 7 0 1 2 2 2 0 2 7 1 0 5 3 2 1 7 4 4 3 7 6 6 2 2 3 7 5 4 4 0 2 1 2 0 3 8 2 5 25 3 12 6 10 0 5 1 2 1 0 1 1 4 6 0

153 0 33 4 4 17 12

39 5 19 5 0 1 4 3 25 14 3 27 6 3 4 1 8 5 9 T 2 12 47 26 4 43 5 20 15 0 8 1 5 5 30 3 27 10 35 13 7 27 22 10 23 10 2 6 11 68 29 5 2 32 25 15 3 4 5 i 12 3 10 14 12 8 27 20 9 26 20 15 188 3 18 27 13 38 13 32 30 69 2 18 1 85 14 38 40 3 34 9 4 27

77

20 160 11 84 2 4 33 24 8 5 28 40 82 18 22 23 18 55 21 11 10 53 5 8 59 5 5 9 21 35 10 40 15 33 17 6 1 0 22 21 10 42 11 2

1S8 1 0 6 2 73 3 50 34 22 12 96 188 1 72 7 4 32 1 0 4 17 19 11 163 0 :es 23 32

:ci4 86

c kg.

====

====

i GO

LD

RATI

NG

au

13 3 9 2 0 2 5 2 5 7 1 11 2 1 2 0 2 4 5 4 1 5 13 8 2 15 1 6 5 1 5 3 1 2 12 1 10 5 10 9 11 13 7 2 17 3 16 3 6 28 7 4 5 12 18 7 4 4 2 3 8 2 11 9 6 2 11 8 7 13 6 8 39 1 12 10 3 17 5 10 13 22 0 11 2 31 12 11 11 7 14 14 6 9 |

24

14 57 2 34 8 1 15 14 3 2 7 16 23 6 8 5 6 19 6 4 2 15 5 3 12 10 3 4 5 14 B 12 8 13 6 11 3 0 7 20 9 14 4 1 65 1 0 1 2 24 3 14 11 7 10 24 53 0

I 22 3

1 11 0

' 1 1 6 7 2

i

164 0 65 9 10 94 28

t FKUbKAfl

( nun .4-. 5 mm >.5 nm Wgt. Shape No. Shape No. Shape (gm.)

28.7 31.5

26.7 20.745.118.136.425.315.419.535.119.0

39.925.216.728. 434.230.619.514.052.026.725.2n c . t>18.711.537.133.729.636.637.3

45.133.3

45.430.544.225.8

2 SA 25.715.7

1 SA 30.253.924.629.522.942.128.338.540.544.5

it 32.942.4

\ 36.632.544.024.6

: 25.2

55.422.260.734.312.4

15.240.622.918.429.540.730.846.535.716.925.854.9

39.020.116.116.239.8

37.134.5

32.117.733.426.528.341.132.527.334.037.247.038.818.2

59.152.563.363.046.344.913.241.157.061.6

1 A 37.737.633.952.134.2

29.635.146.037.135.942.744.336.541.328.521.318.525.719.438.625.222.324.825.823.616.639.525.838.050.916.030.136.155.250.039.829.850,010.732.940.135.538.8

1 SA-SR 38.437.9

4B.738.8Tfl J20.4

43.3

52.622.533.033.936,628.543.535.432.83B.324,034.945.130.646.939.244.232.523.728.5

28.430.821.818.933.328.333.6

26.310.523.7

25.455.036.926.037.041.8

D 43.5 26.4

5 0 1930 0 0.02 0 63.31 0 33.21 0 11.61 0 134.52 0 56.4

Hag \

60

50

60408070608560

80

60

80

9060

707070

9080onOU50

806050

806080

50

306025253075

75259080

60

60

50

60

60

80

9030

6050709590

8060

60

90

95809520209540

1520304020155

102025

25253530

351525303025

20252510

55

1510255

5020

10452025451530301035251010203030133080104040403735

25

2515253020

302510trtr604055

45201

tr1

151020tr100

10

107

15

22055

3025

65 30

1640953726

77793

:=*===

CONCH Py

tr tr

tr5

1010tr5

30tr

10

5

tr

tr5

105

102010tr

101010

trtr15

1010tr

20trtr5

trtrtrtr

5trtrtr

105

10

5

5

tr

tr10trtrtr

tra

trtltr

tr

tr

tr

trtrtr

5tr555

5

5

2333

tr5

tr2

tr3

tr02

tr5

tr2

tr

trtrtrtr5557355

trtrtrtr335

trtrtrtrtr10tr

tr

55

tr3

10

tr2

trtrtr222222020

tr5

trtrtrtrtr

3tr3

trtr0

trtr1

0 2

1590

3034

2012

IMTRATEGar disc

tr tr

trtr

15

10

tr

tr

10

tr

tr

5

trtrtrtr

5

5tr

tr

20

tr

10

5

1010tr Cpytr

tr

trtrtr

tr

trtr Cu

tr

5tr3

trtr5

5

5

3

55

5tr4332

trtrtr00C2

tr0000

0trtrtrtrtr10tr3

tr10tr

313tr

tr13

10trtitr

0

5trtr35

tr4000

1050

tr50000

5100

trtr0

tr

204

053

trtr0

00

1240

2024

1510

Ultraviolet NOTES NORMALIZED VALUES Au , lamp Rad GOLD GOLD ppb Sch Zlr grains microgn det 5

Y Y Y

Y

YYYY

YY

Y

YY

Y

Y

YYY

Y

Y

YY

Y

YYYY

Y

YYYYYYY

YY

Y

Y

Y

YYYY

YYYY

Y

Y

Y

YY

Y

YY

YYY

111111111011011100100000011001001210

0

000000010101100101110200011

100

0201111 1

134020101

Y Y YYYYYYYYY

Y

t

YYY

YY

Y

YYY

YYY

YYYYY

Y

YY

YYY

YYYY

YYYY

YYY

YY

YY

YYYYY

YY

1

1111111

202102111201222212112

2

12322222211322131000

2210001

212

031123

10

144031112

0000

00

00000000

00

00000

0000

0

0

00

0

0

00000

00000

00

00

000000

0

0

000000000000000

000000000000000000000

0

00000000000000000000

0000000

000

000Q00

00

134000000

basal till 1 Au grain ?(.3 x.l) odd colour

clay in tilljasper, clay in tillclaybasal tillbasal tillablation till (boulders)clay till

sandy, oxidized, basal till

ox basal/unox sandy tillcoarse fraction 50* clayunoxidized basal tilloxidized basal till3rd Au grain ? SA, proc. errormay/may not be goldgold?, oxid t u nox id basal tillox 4 unox basal tillox & unox basal tillsilty, ox basal till, no bdrksandy basal till

ox basal tillox basal till above sand layer

oxidized basal tilloxidized basal till on bedrock

oxidized basal tilloxidized basal tillno bedrock

sand A bouldersvery sandy, oxidizedsandyclayey tillsandy

clayey, basal, vole, carb veinssilty basal tillCpy in cone,, boulder pilebasal tillbasal till silty & stoneysandy basal tillgravely basal tillsandy stoney basal tillbad sample, sandysilty basal oxidized till

unoxidized basal tilloxidized tilloxidized tilloxidizedclay rich oxidized till

ox tilloxidized till, clay rich

oxid./unoxid. sandy tilloxidized/unoxidized sandy tilloxidized/unoxidized sandy tilltill on bedrock

grains on vole rk chip with qtz

oxidized/unoxidized sandy tilloxidized/unoxidized basal tillalso 51 hble; unox basal tillunox, sandy tilloxid/unox till, tr. barite

unoxid. basal till, tr. nag, barclay ox till/sandy unox till

ox. /unox. tillstoney ox., silty unox. basalmag., epidote; loamy ox. tillsilty or basal tilloxidized loamy tilloxid. loamy, cobbly till

cobblysilty tni/unox. clay tillsilty till, iron formation fragsilty basal tillred clay in basal tilloxid. red clay

slty sdy bsl tillgravelly tillsandy gravelly tillsilty, gravelly till (basal)silty till; basalclayey basal tillreddish tillreddish tillgood tillclay-rich tillclay-rich tillclay and gravelsandy tilltill over clay-siltpoor (sandy) till

gravelly

basalbasal localsilty basal3llty basal

silty basalsilty basalsilty basal

siltysilty gravellysilty basal

basal

silty basalsilty basalsilty basalbasalbasalbasalsilty basalbasalbasalbasalbasalbasalbasalbasalbasalbasalsilty basalbasalbasalbasalbasalbasalsilty basalbasal

silty basal sandy

,_________---. -_.---.--z-----------

6 1 0 6 350201012

3131146110632143

110222280

22B

115152412332214355197

61501

133102252303

22154

61

1332321423212

1226111

1611549434

04643122

1661011110500060332042240331224

1016

10921

5

40002362000210030200013000040010200000010 2

1990

2233

109

2.0 3.5 4.0 6.1 1.88,90.31.61.10.70.14.5

20.7

11.93.62.84.35.03.24.31.92.316.218.59.63.9

22.66.23.41.99.54.22.94.56.9

14.622.884.114.664.0

216.911.238.90.254.92,43.21.54.07.1

10.15.511.95.2

21.57.8

19.016.014.3

7.71.91.40.54.7

3.92.14.00.51.14.44.21.71.61.30.12.7

3.60.04.98.40.2

0,31.9

2.42.1

21.70.14.9

23.58.00.13.08.69.31.00.1

10.111.63.87.0

32.84.06.6

61.530.66.3

18.521.55.61.77.3

9.03.5

15.813.51.53.45.427.534.020.97.6

18.65.01.12.56.32.212.610.612.63.6

10.82.36.45.325.82.1

15.75.35.15.61.34.3

10.51.72.58.67.0

57.04.56.538.214.44.32.4

8.4

18.48.51.63.00.18.22.77.71.94.10.1

13.517.016.20.28.71.34.40.23.80.7

11.19.00.10.30.10.25.55.48.34.40.05.83.03.15.13.48.74.83.5

0.1 42.7

199.00.0

216.99.619.0

361.247.8

43 105 72

193 64

155154748373

125987

28513312717110184

17918437

701680347168

16301629639

26498

11991

210354410

1520213

13705250678

13803

223078

15936

16022424615839310867815B451216634

101812813

322

22859

197394287

118375973

353

973

243497

3

149

65124775

3173321281

3115217182233

32724668

125902133540

105049014145161112453

312

35213942847144

147114813570644327

11802156755

2538444435133822633599

156145

15508644511913522949

1279426076

249237

1580164285990423134164

192

3812295&913

21158

23544593

290470441

320425603

3618

361205

31333

139149196127

316385661157917510984

3 879

1993

5250288494

2443091277

Au ntgn

1.2 3.3 3.0 5.1 1.37.00.31.71.20.60.14.4

16.7

11.33.32.1U3.42.63.52.61.918.617.17.53.1

18.66.03.21.1

10.33.63.04.16.9

12.918.545.89.4

35.2134.510.641.40.254.32.33.61.54.58.69.97.012.94.624.75.1

19.35.3

15.9

5.61.81.70.43.9

3.42.44.50.71.23.53.61.72.11.20.12.9

3.80.13.97.90.1

0.31.7

2.1•2.2

25.70.14.9

13.29.10.13.98.08.50,90.1

16.012.94.37.9

41.75.97.1

43.027.88.7

16.822.75.52.810.6

10.44.8

19.617.41.66.25.0

29.623.518.37.021.55.51.32.16.31.810.99.07.93.7

13.22.65.97.424.82.6

16.06.66.66.81.56.39.51.93.08.89.2

61.06.26.131.320.65.23.4

9.2

20.05.11.83,10.16.02.58.31.42.30.113.116.413.50.18.01.11.90.11.00.5

10.26.30.10.20.10.14.63.36.03.30.03.82.31.76.32.94.54.03.5

0.1 24.8

1990.0

134.58.713.4

178.935.4

Agppm

5

3 3 3 3 333333333

3333333333333333333333333333333333333333333333

33333

333333333333

33333

33

3333333333333

333333333333333

333333333333333333333333333333333333333333333

3

3333333333333333333333333333333333333333

3 3

199333003

Asppra

2

15 1 2 326111121

114131

28434111141631121111911111111112131323412

11135

313111311411

13131

11

3413121111114

131111153141111

332151152118211334611413143191141753135111111

3

11112411213111311161

1015111451812111141411

1 1

1991

282378

Ba ppn 200

570 230 250 100 440100100270100390100250100

100100100260100100430100300100100450100100100100100100100100270280100100100100100100100360100100350100100290340100240100200100350100100370

380100230420100

100520100640100210530360300500360240

100100100100400

650100

290340100370100380270100100100260210100

100100100100100100100100270100100220310100450

100100100100380370100100310100410300100100100100100100100240100100640100100100100100210100290100230100100100310100100100100100100400100

100

200100430380460100100340310100360100100300100290390100460100100100100590690100510440100100100100100100320100280100100100

100 310

199100690198144

20677466

Br ppn

5

3 3 3 3 333333333

3333333333333333333333333333333333333333333333

33333

333333333333

33333

33

3333333333333

333333333333333

333333333333333333333333333333333333333333333

3

3333333333333333333333333333333333333333

3 3

199333003

Ca \1

1 1 3 4 121111111

2321213231112212112123321211211114111312313211

31146

545133531411

11221

11

3111133331211

213211211112212

112111111143435111611153634113144112111411255

1

315611111111113111651111

12111116111111111

3 1

1991

122225

Co ppm

5

35 51 37 56 714079766496555372

63779186586387944186595596

1205765805243733662645068756986965734695465407857484170395054535883

5875372695

574066363051365325465727

5234657836

3741

44755036554962644317334886

6957576380731205552516258415259

7255456947575460615550736760486582110897073655456467563646560777043

1007764507198527090603463

42

298054493853404548413431275428353762

200537365819330487443

1006646847362483154585741

60 67

19917

2006021

452103

Cl Ppn 10

530 620 720 870

1200360500270400

11002000470810

730140024001400820560800820170490660610860

1400390310460780390580250740840550690650

11001100210011002809508201200610560400300330640320490510550360640

1200420430200

2100

10005207900580370

1300440900490850660300

490250750670370

650500

8202100620480800510860

1200640270330280450

230071020001600160021004900710630530670

11008108101300

10006205709904209306704109506106201600350020001700300042005300280012001100660500670520120077015001000560

38001200700

13001200270014001400640730

26001400790970

1500

430

310660570570410400310440360260570660490650260740320370

3000400410990480460

5700280310620550480570660530600370300390460440600

300 390

1991707900959968

9764382935

Cs ppm

2

11 11 111111113

1111311111112121211111111111111113111111111132

11331

411311111111

11111

11

1113111212111

111111111111111

111112111116131111111231111141111112111111113

1

1111111111111111111111111111111111111131

1 2

199161103

Fe \0.0

21.2 24.5 14.0 27.3 35.515.630.125.820.945.821.919.728.3

23.629.140,629.921.129.241.244.013.438.824.618.041.156.620.426.831.018.616.736.115.025.426.219,229.224.530,035.237.225.012.329.422.629.014.531.022.517.913.326.113.420.222.222.425.334.9

15.525.312.96.9

40.7

25.612.119.611.18.7

12.812.515.37.8

14.423.29.9

20.48.135.939.113.5

16.917.4

13.434.118.411.223.516.722.423.013.828.410.615.828.9

25.621.518.122.330.624.543.222.621.221.125.926.119.622.729.6

34.523.318.831.215.220.324.023.226,923.614.627.426.321.113.729.829.135.333.528.423.225.216.021.215.324.920.429.818.821.530.220.312.634.928.720.914.225.933.617.922.135.523.113.320.2

18.6

9.327.818.214.615.318.614.714.018.314.18.79.4

10.420.97.7

10.211.811.79.411.725.921.830.330.97.716.226.013.637.225.113.929.429.222.816.49.6

19.119.821.715.1

20.2 24.9

1996.956.622.48.7

75.039.7

Hf ppro

1

8 7 9

13 14797

1632261419

13161918101232304

1112151843128

13B9

168

1196

1089

1140297

201221n9767

1166776

17

41694

39

281143341810111025351911

53

12209

6n28199

101210161412569

13

118

11101819569898

15321922

161891521221111111321261840112021212416309

17112225211299

1120154315131817n177714124153

8

20342936202913191115203740221236181436

3135282724171338201541562627161514251722

21 15

1993

771811

12740

Kg ppn

5

3 3 3 3 333333333

3333333333333333333333333333333333333333333333

33333

333333333333

33333

33

3333333333333

333333333333333

333333333333333333333333333333333333333333333

33 3333333333333333333333333333333333333333

3 3

200333003

Ir ppb 40

20 20 20 20 202020202020202020

20202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020

2020202020

202020202020202020202020

2020202020

2020

20202020202020202020202020

202020202020202020202020202020

202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020

20

20202020202020202020202020202020202020202020202020202020202020202020202020202020

20 20

1992020200020

Ho ppa 20

10 10 10 10 101010101010101010

10101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010

1010101010

101010101010101010101010

1010101010

1010

10101010101010101010101010

101010101010101010101010101010

101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010

10

10101010101010101010101010101010101010101010101010101010101010101010101010101010

10 10

1991010100

CONCENTRATE ASSAYS

Happn 500

18700 11600 14100 11400 9400

13000115007770109006040132001290010600

1030010800103007370

109001050072005710

126006050

114001360066404620

1120090107880

14200164009580

19800126001120012500112009420836079907640

1100017500120001510012600166009700

1200012600153001100014000121001160011700123006340

120007910

14100235005140

121001440012100191001910011300207001410019400232001400017500

1370021200105009430

17400

2030016000

17300120001340013200979012400100007640

1400098DO

14500126009240

64109080110009180496072903940

138001190010900117009930

159001010011400

1040011700125008900

13700111001020011800123001130011000103001180011800133009400

1150079906680

12600107009980

125001060010600927091908430

111001030086308210

10500380091906440

1040068707570

122007000768087801850013500

11300

15400109001350013700118001250012600120001300010500120001410015300121001850016000131001360011800129008330

11200799095309730123007150

1410083909550

14700786081401180010100121001160011000927012400

10400 10900

1993800

23500115803413

0 1164989510 18406

Ni ppm 200

100 100 100 100 100100100100100100100100100

240200100100100100100100100100100100100100100100100100100100100100100100100100100100580100100100100100100100100100100260100100100100100100

100100100100100

100100100100100300100100100100100100

100100100100100

100100

100100100100100100100100100100100100100

100100100100100100100100100100100100100100100

1001001001001001001001001001001001001001001001001003901001001001001001001001001001001001001001001001001001JO100100100100100100100100100

100

1001001001001001001001001001003103401001001001001001002501001001001001001001001002801001001001001001001001001001001QQw100 100

19910056011152

2743216

Rb ppm 50

25 25 25 25 252525252525252525

54252525662552252525252525252525252525255525252525252525255525252525252525252525252525252525

25252525

120

252525252525252525252525

2525252525

2525

67252525252525252525252525

252525252525622525252525252556

252525252525602525672525252525252525252525252525252525252525252525252525252525252525252525

25

2525252525252525252525252525252525252525252525252565252525252525622525512525

J

25 25

19925

1202611

11849

Sb Ppn 0.2

0.1 16.0 0.1 0.1 0.10.10.11.10.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.50.10.10.10.10.10.10.10.10.30.10.10.18.30.10.10.10.10.10.10.50.10.10.10.10.10,10.10.10.10.10.10.30.40.1

0.10.10.10.10.1

0.10.10.10.10.10.30.30.10.10.10.10.1

0.10,10.10,50.1

0.10.1

0.50.10.20.30.10.10.10.10.10.20.10.30.1

0,40.10.10.10.10.10.10.10.10.20.10.10.10.10.1

0.10.10.10.10.10.10.10.10.30.10.10.40.10.10.10.10.10.10.10.10.10.40.40.10.30.10.10.10.10,10.10.10.10.10.10.10.10.10.10.30.10.50.10.10.1

0.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.30.10.50.10.10.10.10.10.10.10.10.10.30.10.10.10,10.10.10.10.10.10.10,1

0.1 0.1

1990.1

16.00.31.31.62.8

ScPpn

0

15 17 22 24 201825262823242026

25262528252427242525283030262624292520231825222224222323362416242324212421191926201924222324

1632201925

261930272119181820292516

1826182118

1317

21252321212327402612202233

211924192427402019201922152119

222019242824182018233534333731333223302540203326263635242022213524192523302922265125221838

17

233429362023172519202530262420312332272828382925342724363124475327313126222921n28 23

1991253256

4037

Se ppa 20

10 10 10 10 101010101010101010

10101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010

1010101010

101010101010101010101010

1010101010

1010

10101010101010101010101010

101010101010101010101010101010

101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010

10

101010101010101010101010101010101010101010101010101010101010101010101010101010It)10 10

19910101000

10

Sr

0.2

0.1 0.1 0.1 0.1 0.10.10.10.10.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.1

0.10.10.10.10.1

0.10.1

0.10.10.10.10.10.10.10.10.10.10,10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10,10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.1

0.10.10.10.10.10.10.10,10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10,1o.t0.10.10.10.10.10.10.10,1

0.1 0.1

1990.10.10.10.00.00.1

Ta

121 1 12214111313335244111443624312341123114611311231513114311

111I9

115111111111

11163

11

3131322111111

232345731323131

3321113211112332221515223114231114131341a6311

1

152721132317711421221815221855

10752212252

4 3

1991

102236

Th ppm

1

11 1311 16 241122141537122236

18352216172129255

37172240562527201014228

2525163811182486238

2523301236251916271121111975

120

1222165

92

189

29179656

14161810

225

1823n10n10162211191619101368

2343

201913193525563216181522172825

30261524142121172315142218279

19203133242423161616252022131822141656321720243617792825

, 1240

15

17342840153014321714126691371151151114

2459423217162263384159524221122720313132

15 23

1991

1202417

27957

U ppn 0.5

0.3 1.8 1.7 2.6 1.60.32.00.30.33.81.92.43.4

1.40.30.30.32.30.33.34.50.30.32.40.33.54.72.23.43.50.30.32.80.34.52.31.43.50.30.35.25.23.20.35.32.50.30.33.53.12.00.30.30.30.31.92.55.48.5

2.63.20.30.35.6

3.30.34.63.91.52.01.80.31.70.30.31.3

0.32.22.10.31.6

0.30.3

2.80.30.31.40.30.33.00.31.70.31.12.25.0

0.32.21.3l.B3.80.36.13.51.62.21.81.42.82.41.9

2.92.81.51.82.02,72.02.83.33.04.03.21.71.92.04.30.73.81.03.01.30.31.70.33.15.40.32.40.32.51.62.60.36.20.30.33.03.33.42.7

11.03.32.72.55.2

2.4

2.51.45.62.51.54.02.53.03.11.43.46.34.83.92.84.03.40.70.30.31.53.94.21.71.01.03.11.71.63.55.69.61,01.00.71.02.03.13.53.2

0.7 2.9

1990.3

11.02.31.83.25.8

V ppn

4

20 9 2 2 222722222

22

122222

1729

3922222225252

112272222222222222222222

16

22222

2222272

222222

82

4522

22

2722222222222

222222262222222

2222422222222222222225222222

2213222222222222222

2

2222222222225222222822227222222222222222

2 2

1992

4535

2613

Zn ppi 200

100 100 100 330 280100360280210500210100360

220340320340230280390530100450240200460470200310340100200320100300290100390240330320280220100300250260100420290100100370100210230200200410

100330100100480

230100100100100100100100100100220100

250100250420100

100240

100450100100270100220100100100100100300

290270240270300340660260220230220270100220250

280230100260100100280210240230200100350100100360410400470300280310200340220380210340240360410370100360430290320330340240220420300100310

100

100460200100100210100100250100100100100270100100100100330100370200410320320100250250460310100340370200200100100270350100

380 320

199100660236120

14382475

La ppa

1

31 40 36 49 653356374687386194

518157804657806622985263no1607471623441683073684497375263230762980688644946853477136593452180310

34615020

230

646692613835282250596437

5420516639

3540

405367325547583143262568110

59574361

10080

1709644514160547168

756940624560524662424160517731636692957772644944507061594148574350

1406045596710053

240847068120

41

6610092

13053974497554343

22028011040

16053377

1677

180120953105458

190110130170170130724238619192110

60 67

1997

3107349

2366170

Ce ppra

3

53 57 52 79

10048895574

1306887

140

7012089

1207084120no30

14079

1001602401301109145679345

11010064

1405480

10034012046

13011014074

140997270

10056885477270440

48916635

350

120100160997073633992

10010056

793469

11061

6059

718594537866894861363996170

61805981

1401102601306668648695

110110

130no709076938174937675

10087

13055nono15015012012095826675no93926075967371

2201207087951508738013097

150210

62

9616014019080

15065

140866473

29040016061

23076561124

120260180160560B286

27017018026025018011071

12086

140130150

87 100

19911

56011174

5424259

Nd ppn 10

37 50 25 37 412339255970515872

27463850263438431247322863804330311823261727281843202722120582245445557744436394830463435120220

27324029

170

757084595461522364573927

295

587236

2945

4754453949375530345

164575

321526255248935223192130454744

4149183528333028302529472754193337385849593228222734313415253925318840n45355232

13048368879

16

3145498519632070222129no120595

723434101050815146

2802840935557

100no5751224628584660

31 30

1995

2804632

1026110

Sffl ppm 0.1

4.44.8 4.9 6.7 7.44.36.84.45.69.46.66.49.8

5.08.66.16.04.85.97.67.22.78.65.16.610.015.06.96.65.93.54.66.23.16.35.84.08.63.55.56.420.09.23.88.47.19.16.69.46.85.45.27.64.46.24.35.517.029.0

3.46.95.33.5

23.0

12.08.9

13.09.47.38.97.04.08.28.97.14.0

5.63.77.28.84.9

4.15.2

7.27.36.94.55.85.36.55.05.33.23.27,412.0

4.44.43.74.37.16.1

15.07.34.14.44.26.17.87.58.0

7.16.64.06.05.36.04.64.65.64.55.56.95.98.53.56.07.07.88.47.18.25.66.04.55.18.06.85.84.14.96.15.35.2

11.07.84.56.56.88.16.223.07.56.3

16.014.0

3.9

6.09.77.9

11.04.98.43.98.15.04.35.0

16.022.09.24.2

13.04.94.81.82.67.2

15,010.08.5

51.05.55.4

15.09.19.616.016.010.06.54.66.75.48.57.18.9

5.6 6.4

1991.8

51.07.54.9

24.517.4

Eu Tb ppm ppm 0.2 2

0.1 0.6 1.1 1.0 0.90.10.80.10.91.21.31.11.1

0.81.01.11.10.11.01.01.10.80.80.91.00.82,00.80.60.60.70.60.70.70.70.80.50.70.60.10.11.81.50.91.31.01.41.20.80.70.70.90.70.90.90.10.10.81.4

0.60.10.90.82.0

2.12.12.51.81.62.21.70.71.71.81.10.9

0.51.00.11.10.9

0.71.1

1.70.10.10.90.70.11.01.11.00.80.60.90.1

0,60.60.70,80.71.12.20.80.80.50.80.51.51.11.3

1.01.00.70.81.00.90.60.70.60,61.41.21.11.40.81.01.70.81.00.80.80.71.20.81.01.41.20.70.70.80.70.90.91.31.00.51.01.10.91.13.40.90.63.82.1

1.0

1.01.41.11.30.81.30.81.00.70.81.11.71.81.10.91.60.91.00.60.51.31.81.02.3

15.61,01.01.20.61.22.12.91.01.11.00.90.70.81.01.1

1.01.1

1990.1

15.61.11.21.43.4

11 1 1 111111111

1111111111111111111111111111111111111111111114

11111

111111111111

11111

11

1111111111111

111111211111111

111111111111111111111111111111111111111111121

1

11111111111311111I1111111111111111111111

1 1

199141002

Ybppra 0.2

2.1 2.0 2.3 2.5 2.61.92.91.92.83.23.12.43.5

2.43.32.52.42.32.33.62.22.32.63.53.84.13.02.73.33.32.11.72.51.82.41.72.02.02.02.71.94.62.31.63.03.03.52.62.62.01.41.62,81.91.62.61.92.84.0

1,23.42.31.74.3

4.72,24.74.02.72.42.42.53.13.74.12.1

1.62.53.03.22.0

1.31.8

3.63.72.12.42.62,32.84.52.41.41.82.54.3

1,91.82.01.52.02.85.01.71.91.51.61.82.22.31.9

2.32.31.62.33.02.61.82.21.62.33.43.12.73.62.72.93.51.73.22.53.92.33.22.73.14.24.02.82.32.22.73.92.83.33.02.73.63.01.53.09.72.32,54.15.8

1.5

2.64.13.94.22.62.91.93.01.92.22.86.04.73.02.34.92.22.41.82.23.65.43.72.53.73.62.64.93.73.06.17.23.44.03.43.02.04.22.83.0

2.7 2.6

1991.29.72.81.11.25.0

Lu ppra 0.1

0.4 0.3 0.5 0.6 0.50.30.60.40.60.70.60.40.7

0.50.60.60.50.40.50.70.60.40.50.60.60.90.60.50.50.50.40.30.50.30.60.40.40.50.50.40.41.00.40.30.50.60.70.40.40.40.30.30.40,40.30.50.40.40.6

0.20.60.40.30.7

0.90.41.00.80.60.30.40.40.60.70.70.4

0.30.40.40.60.3

0.20.4

0.70.70.40.50.50.40.50.80.50.30.30.50.8

0.40.40.40.40.50.51.40.40.30.30.30.40.50.50.5

0.40.50.30.50.60.50.30.40.30.50.60.80.60.90.40.40.90.50.70.60.80.40.80.50.71.00.80.60.60.50.50.80.50.70.60.60.70.70.50.61.90.50.40.71.2

0.3

0.60.90.80.90.60.70.40.70.50,50.61.11.10.70.51.10.50.50.30.40.81.20.80.60.70.80.51.10.80.61.31.70.90.90.70.50.50.70.60.6

0.6 0.4

1990.21.90.60.20.11.1

Mass gm

28.60 31.51 41.96 26.64 20.6844.9917.9436.2725.0515.2419.2834.9318.90

39.8025.1016.5528.2234.0330.4719.4513.9451.7026.5725.1121.5218.6611.4336.9133.6129.4436.3437.1525.1744.9932.9736.3045.2430.1644.0725.7025.6215.6430.0253.4424.3625.3822.8841.9528.1438.3440.3944.4232.7242.2536.3832.2342.7724.4825.01

55.1522.1360.6334.1712.26

15.0940.5722.7916.2529.2940.5030.7546.3035.6416.6825.7354.74

38.8419.9215.9615.9539.62

36.9034.23

31.9717.5133.2026.3328.1741.0032.3327.1633.8836.9446.7938.6318.06

48.9452.3463.1262.8946.2244,6913.1040.9956.7961.4437.3437.0944.7552.0133.83

29.5534.8445.8736.8635.7542.4744.1036.4241.1528.4021.3618.2425.4119.1838.3524.9022.0024.5025.5023.4016.2639.5325.7837.9150.8016.0130.1835.9855.1048.6529.8529.7349.8110.1031.8740.1035.3138.8138.5937.8121.3431.6148.5938.7020.44

48.10

52.4322.3632.7533.8436.4128.3043.3935.3132.9138.1523.7245.1134.8230.5846.8439.1743.8232.2623.3328.3127.1828.1330.5222.5118.5933.0528.0133.3822.1730.8126.1810.2123.5127.4425.2054.6236.6125.7636.6641.62

43.30 28.19

19910.1063.1232.9911.18

124.9855.35

CHARACTER SAMPLES

As ppra 1.0

2.5 4.2 3.3 2.5 2.23.1

11.02.72.42.02.31.32.6

2.42.30.51.72.31.11.62.07.22.25.62.84.54.34.04.35.01.33.70.53.33.46.95.86.45.67.38.11.60.51.71.91.60.50.52.42.03.42,42.13.04.07.08.73.92.7

2.93.12.12.83.4

1.60.50.51.20.50.51.20.50.52. 30.50.5

5.84.01.40.52.2

0.51.4

2.42.01,64.02.93.13.04.72.13.52.05.14.9

2.03.04.03.03.03.02.05.04.06.04.03.66.90.52.32.22.26.78.44.93.94.11.83.33.03.82.64.95.63.15.32.61.82.45.43.11.71.71.31.91.66.02.10.50.5

4.0

1.05.02.03.02.05.02.01.02.12.33.92.51.42.42.81.42.0

10.01.74.72.21.21.71.31.30.54.60.53.51.51.32.00.52.54.20.52.02.70.51.6

1.0 3.0

1850

113247

Sb ppm 0.2

0.1 0.6 0.1 0.10.10.10.10.40.10.10.10.10.1

0.10.10.10.10.10.10.10.10.40.10.10.30.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.1

0.10.10.10.10.1

0.10.1

0.10.10.10.40.10.30.10.10.30.10.10.30.5

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.80.10.10.10.10.10.10.10.10.50.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.1

0.10.10.10.10.10.10,10.10.10.10.10.10.10.1D.I0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.10.1

184010000

Cu ppn

115 57 26 23 131732182015242421

16352516171929399330611437321737311321231827263087666666142722128

12102240371931442953516714

1832321220

1114139

109

201915111415

4459172945

1912

11302331362937

1032324207073

411954324215344659729543391417161619735640241738142224771926343713155820691319122080261711

50

28510628

1241425383069735419202924241470213027362318482121266719no2511302316173413

130

41 27

1660

2853430

89794

ZnPPJn

1

32 71 53 30 413872655268333944

443326263523293590384859395838294435614943605665835862

10033253525182718724350524137546948

11757

3227304025

423032231531313621402524

7453343766

4351

60394762466532543825428378

1

416842373347396147398164376032333931385228484732367535444840513145454931874144202593281621

37

743827

13521

10725253028172122393027282839323422212895374216482544351628331529372529

27 71

18415

1354320

40483

Agppm 0.1

0.1 0.1 0.0 0.0 0.00.00.10.00.00.10.00.10.0

0.10.10.00.00,10.20.00.10.30.10.10.10.00.10.20.00.20.10.10.20.00.00.00.00.00.00.20.00.20.00.20.10.00.00.00.20.10.10.10.00.00.00.10.10.10.0

0.20.00.00.30.0

0.00.20.00.40.00.00.00.00.00.00.00.0

0.20.00.00.00.0

0.00.0

0.00.00.10.00.40.00.20.00.40.00.90.00.7

0.10.10.60.20.1 '0.40.10.40.10.10.10.20.10.10.10.10.10.2

, 0.20.10.10.10.10.10.10.10.20.20.10.20.20.10.10.10.10.10.10.30.10.10.10.10.10.10.2

0.1

0.10.10.10.10.20.10.10.10.10.10.10.10.30.50.10.10.20.10.10.10.10.30.10.10.20.10.10.10.10.10.10.10.10.10.10.10.10.20.10.1

0.2 0.4

184010000

Pb ppm

2

419 1 3 144354433

33331144813314115453355674773113111575534543

143

13331

331111111511

73546

63

7115383111168

5744

- 6'3

5573B64676533665555555

136657753

355746

12534

5

36128

2010683697645785

105

105376

116

104

1174856847

1027

5 10

1841

3654

2014

Au ppb

5

3 3 6 3 363373333

63

883333373336

1173333733

10507487

596

36113736373

1955

123710138

33333

53333

17553639

33333

33

3335337637636

333333

223333373666B6

106863576687677333333333333

3

3333333333363333333333333333333333333333

3 3

1843

686

1010827

NORMALIZED VALUES normalized to 20 kg. ««=«« of -6 tea wterial GOLD

GOLD GOLD RATINGgrains aicrograms

6 1 0 6 350201012

3131146110632143

110222280

228

115152412332214355197

61501

133102252303

22154

61

1332321423212

122G111

1611549434

04643122

1661011110500060332042240331224

1016

10921

5

40002362000210030200013000040010200000010 2

2000

2233

109

2 4 46 29021105

21

1243453422

1618104

23632943471523841564

21711390

5523247

106

125

228

191614

82115

424114422103

40580

02

22

2205

248039910

101247

3347

61316

1921627

94

1614135

2834218

1951262

1311134n265

262

1655614

1123975747

381442

B

189230838240

1317160914041

11900005584063353953

0 43

2000

2171019

36046

4 2 1 5 160101026

63522J312376263242222366

245

17663

222

14112264394

13555

14

31302

132103234303

22252

31

1281263124322

3427822

21188

1713346

26

1192129

179342222162312111513111012012111118311

9

10201245301044304020104300003121021111211

011

2000

6646

3616

HCE PROGRAM

4 nun .4-. 5 mn >.5 ma Shape No. Shape No. Shape

CONCENTRATE Ultraviolet Vgt. Hag Py Gar Misc. lamp Rad

(gn.) \ \ \ S ch Zir

NOTES NORMALIZED VALUES GOLD GOLD grains microgra

37.445.6

39.132.635.742.538.433.821.943.338.544.136.440.943.9

A 39.426.940.427.939.230.347.446.747.631.743.842.431.248.126.635.846.944.235.433.040.649.445.445.337.946.235.142.847.744.540.140.028.138.326.930.044.837.8

del 32.935.541.542.237,439,944.237.531.130.233.748.130.838.430.327.532.232.641.831.142.835.741.231.637.3

1 A 31.132.438.037.946.445.438.627.933.9

1 SA 37.441.1

A 29.523.421.846.523.733.824.534.226.428.4

1 SA 39.632.531.936.548.030.522.236.641.240.827.421,322.943,239.043,439,540.236,116.822.229.931.031.124.726.724.336.928.216.730.623.020.028.632.736.432.436.930.729.340.136.837.443.839.428.833.130.836.849.927.931.834.926.034.324.232.826.626.538.638.323.637.335.223.219.934.630.218.931.122.423.435.528.739,730.745.435.639.443.135.144.934.341.936.9

1 (.6x.3) 32.645.639.622.835.034.631.643,621.836.825.547.7

1 (,5x.3J 43.335.333.932.733.733.244.546.132.339.343.330.845.045.439.842.552.143.951.233.235.938.243.5

44.130.635.639.434.431.6

1 SA 41.121.139.929.337.131.734.833.1

50 24.737.141.218.444.549,238.536.646.927.136.026.7

4 2 2451 1 16.71 1 52.11 1 35.50 0 7.50 0 56.71 1 50.5

1035

252040301015tr303530153515

105025201015105010153517251530152510

515302550302020151520

5101515302010

54030

151015251510101510202015

520152515601040

520

40702535555020

5153015

52530

55

155

25301515302525

515106015202050tr50601010

515201540201025258040

401025151515302020302035252520251515302540201515154015202520102015102015154010

53

15302525303530153515302520304030tr20701560754520354015306050354020302020253030

2560355030153030

80402550tr108010153020101015201025101020203025153020

2390

802415

23255

3tr

552

trtrtrtr

2trtrtr

55

0trtrtr

5222

tr023

trtr

00

tr02

tr2

tr25

tr000

trtrtr

1tr

22220

tr

trtr

Dtr

00

trtr

2trtr

0trtrtr10tr10102020

5

trtr10

33

trtrtrtr

0tr

trtr

0trtr

024

tr0000003

tr3

tr00

tr0330

trtr

0132

tr2

tr32

tr

tr0

tr22

trtrtrtr

335552

trtrtrtrtr

0tr

2tr

0200502

tr2

tr0522

tr10

015

0trtr

000

trtr

515trtrtrtr

6trtrtrtr

2tr

0tr

00333333

trtr

2trtr

2tr

52023

tr05

3trtrtr

2trtrtrtrtrtr

3tr

3tr

2trtr

222

10

tr3

tr

2400

202397

1020

22

trtr

5tr

00

tr00

trtr

tr0

tr00020

tr5555500

1010

05

2050

1555

tr0005050000

trtr

1010tr

55

tr10

505

tr050

tr1015

3533

15

trtrtrtr10

00

205

tr0

055

tr10

5330050

tr50

tr500000000

tr00000

tr20

010tr

50

00

trtr

3tr

54

103

tr20

55

tr55555

1045

520

255530

tr55

tr5

trtr

0trtrtr10

55

tr05

155

105

trtr

0tr

55 Sph0205522

3010tr

01010

050 Sph5

tr35505

0 5010

tr532

5050020

trfl252

tr5

tr03002355

3

2370

4535

3014

01

001111001011001111001010002111211122111021100110110000221211111101100111010220111110211101011000111311200101101110112111001211121011011

. 11I0110100112012111111112111010110011000121111102101010101000000000111010001101100

11110111001001100210101110

245031102

13

0112120111220111121001221111102101120211101221121222212222212212021111220111212221121211112111121121111122211122111020122312121210212122221321211221111012122222312112011122110112221221111211211211322221221220112121111

21220111222212313223232212

245031103

0 basal0 basal

0 autvash0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 sandy basal0 silty basal0 sandy basalfl silty basal0 basal0 sandy basal0 sandy ablation0 ablation sandy0 loamy basal0 gravelly basal0 gravelly basal0 sandy0 basal0 sandy0 basal0 gravelly0 mixed0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 ablation0 basal0 ablation0 basal0 silty clay basal0 clayey0 basal0 basal0 sandy clay0 sandy clay0 ablation0 basal0 sandy0 basal0 basal0 sandy0 silty basal0 silty0 ablation0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 silty basal0 silty basal0 basal0 silty basal0 silty basal0 silty basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 ablation0 silty basal0 silty basal0 basal0 stoney basal0 sandy0 good till0 basal0 basal0 sandy0 basal0 basal0 basal0 gravelly0 basal0 basal0 basal0 basal0 basal0 basal0 sandy0 basal0 silty basal0 basal/ablation0 sandy0 sandy clay0 sandy0 basal0 silty0 silty0 basal0 silty0 sandy till0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 silty basal0 silty basal0 basal?0 sandy till0 silty0 basal0 sandy basal0 gandy0 sandy0 silty clay0 sandy basal0 basal0 basal0 silty basal0 sandy basal0 basal0 sandy basal0 silty basal0 silty basalfl silty basal0 basal0 silty basal0 ablation sandy0 basal silty0 ?0 silty basal0 gravelly basal 4 ablation0 good silty basal0 basal0 silty, sandy basal0 silty ablation0 ablation0 silty basal0 basal0 silty basal0 basal0 basal0 silty basal0 basal0 basal0 basal0 basal0 basal0 basal0 sandy basal0 silty basal0 silty basal0 silty basal0 silty basal0 sandy basal

0 sandy basal0 basal0 basal0 silty basal0 basal0 silty basal0 silty basal0 basalfl basal0 basal0 silty basal0 loamy basal0 basal0 basal0 basal0 silty basal0 silty basal0 basal0 basal0 basal0 basal0 basal0 basal0 basal0 silty basal0 silty basal

247000000

010001001320004010101404123200000100000110fl0020200050031030200000020100000000004101

1300002250020000013000110000000200000000100000100006413240211300103

102110000fl001002000010000010001011000210000100010201000202000fl01000000 00

1000011000102000110121020

. 0

'!=s=a = s = s=3BXS*

2460

131124

2.221.0

24.72.6

13.24.71.2

26.03.6

13.15.9

12.99.6

27.19.0

13.53.0

13.13.34.07.0

34.519.69.05.34.58.9

11.524.214.726.85.4

10.96.92.78.0

16.69.48.97.8

15.814.12.0

30.10.20.10.20.10.10.20.82.20.1

12.90.11.8

62.215.2

3.817.7

1.19.31.31.20.23.62,61.82.52.00.10.23.36.64.04.80.10.9

76.123.529.77.5

15.76.85.79.85.0

148.15.7

79.863.34.9

11.45.29.75.04.7

13.310.762.0

0.50.11.34.14.10.1

14.24.2

11.040.81.2

17.122.6

125.710.665.7

1.72.62.00.11.78.10.46.71.51.00.15.83.26.60.45.2

29.810.1

3.43.01.9

20.30.5

15.13.02.25.10.36.61.41.21.5

21.41.90.90.60.11.70.71.11.51.05.30.60.21.93.32.20.21.10.10.90.6

12.525.81.1

24.812.11.10.20,50.92.71.31.91.50.11.9

44.02.40.10.76.81.0

16.00.10.12.26.70.2

36.91.03.5

52.35.21.01.10.80.10.20.23.24.60.20.11.51.12.60.21.61.0 3.61.2

25.0 6.63,93.6n dU .0

12.9106.3

4.16.3

28.20.14.54.64.04.02.3

14.59.71.66.94.40.90.1

27.71,12.7

2460.0

148.19.7

16.4340.346.6

CONCENTRATE ASSAYS

Au ppb

det 5

59361

73069

2657318

60016620012522927481915147399

25214610218953732518116311924629078748585974

19520679

26238520122325836947950

646333333

11393

2333

3892236711547343

23339443

1446160875033

6411261883

16168055077717429713814336577

325056

16001290147167143241171115202279

125022338

120176

334975300

165034

543471

2170236

10201660753

4419512

27449383

17817221516

15881731173

10956

88620

3206978

1207

276674433

3008126123

65293341404715a

401129910303

4619

17053711

660316183

1219693830403

521370

363

2119731365

33

56211

31000

34118

1140182411719333

859333

2317673

37285724

61619910713338

5713100211209

13804

9812265

12860

44655942

152115353

103032

108

Au mgn

2.216.4

28.52.29.53.10.7

20.33.68.64.8

10.19.9

33.36.6

18.62.7

10. 14.04.05.7

25.415.18.65.15.210.49.037.612.930.63.56.77.32.6

10.619.09.210.19.817.016.72.1

30.70.10.10.10.10.10.10.31.70.17.60.11.6

38.813.74.6

20.61.67.21.21.50.14.42.31.82.41,60.10.12.04.82.23.60.10,652.117.829.46.6

13.86.35.5

10.22.7

121.42.3

47.138.93.26.23.68.14.23.95.37.9

49.60.70.11.45.75.40.1

12.83.1

12.245.10.7

12.420.484.910.240.40.62.21.30.11.36.00.46.81.30.90.15.02.96.80.43.223.210. 12.63.52.0

27.00.6

12.82.52.95.20.37.92.21.41.214.91.90.90.40.12.20.71.11.11.11.80.60.21.53.92.30.21.00.10.90.63.8

12.50.418.812.50.60.10.40.72.91.31.31.40.12.1

44.21.60.10.66.91.111.40.10.12.15.50.143.41.24.1

37.46.21.40.80.90.10.10.12.64.20.10.11.00.92.90.21.21.02.21.0

27.06.23.95.20.918.4

129.24.66.239.90.13.14.22.13.12.2

18.310.21.97.54.41.30.127.71.13.1

Ag ppn

5

33

3333373333333333333333333333333333333333333333333333333333333733333333333333333333333333333333333333333333333333333333333393333333333333333333333333333333333333333333333333333633333333333333333333333333333333333333333

33333333333333333333333333

As ppra

2

711

236456

121438159

1429252434635169

1606797234

947

1911553531843167

13101111111111115417111111311111164

76111

12187311641549193138442241111226131241123414113111112131232111111111111531111511151241151441

2235

13033557324311111141111111115131111111311111111171

5533

1120

13013015

1101535121112111114

fiappm 200

100300

100350420100320100550330100590280100330350100100370230100310240270100100420590100480100250100100100100290310380100100100220350100340100450

. 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

300460290400480100360100100310100310100100100100100100100100100100330100100100

Br ppm

5

33

3333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333353333333333333335333337333333333333333333333333333333333333333333333333363333333333333333333333333333333333333333333333333

33335333333333333333335533

Ca \1

11

1321136114131111111111111311411514123331131111111111112111311113114411111141111111111111111121121131311311315711212111111131121331111311114111111231111511111114141114444311312143311112111111111111111121111211111112111

13111111111131111111131131

Co ppm

5

1415

452521212624182520212162293627333132301731251629252519202429221824152523192125233020239

1820162317121322221121192421202319271327292235242421256429351826282835302024172128321322221716342215192234153642513349272020233522452418202331352535372145282629283627303015764748483931295751242524252521232958414944293029224533422842293549374553412927463523272839382342374633353436262635273228462933322137344936343521332525354422282519242121362524

2427293020452443323535463428564427513430462717722863

Cr

10

190390

4003803102903203201702803002605405503703703404205502502501602402902502502802303003102702902502302504003703702804604306005103103502301704403703802001401505102902003003905404604403803104401808205502704604204402703701904402202103007604104803003203601602403102801202802501602003702601402001603901905607207005509604703201903705202508603202103703304004502403204902203208802006802304604406103601105003204003503405202503202705803108203604402703805604903102904402502601901903302902902804405301904504505806203501702103202000830440490680570180420530340280340470440340340440460490330620390330260250310340450480370340250360290180360340190250280180260180180470250240

420310370350190670270370370350500770410610480340370940240300320340260480210490

Cs ppm

2

11

11112511121111111114112113111121313131111111111111111111111131311123311111121111111112111111311111111111131111111111111111111121111111115111411111.11111111111131131131111111111131111111111111111111113111311111111111311

11111111111331111111111111

Fe \0.0

7.315.5

16.420.324.816.57.8

12.16.6

16.512.78.0

12.926.613.616.114.121.520.914.229.415.219.315.86,9

19.717.010.913.67.58.8

16.59.69.49.37.817.715.010.710.715.713.416.410.515.46.3

10.914.07.2

19.014.66.46.0

15.615.710.011.711.613.114.38.1

14.012.814.78.0

10.316.99.816.614.114.413.513.712.39.8

16.26.3

15.420.526.234.520.519.716.710.314.710.919.85.5

15.918.110.310.616.812.15.7

10.67.7

20.09.211.014.820.716.923.29.811.410.814.531.513.329.814.36.7

11.413.512.314.710.011.316.310.221.015.814.014.811.218.612.313.519.65.7

32.818.520.621.013.012.114.223.721.611.29.2

19.621.629.214.812.813.925.316.718.913.610.413.114.612.323.714.317.010.015.410.39.618.116.421.721.818.320.27.19.819.415.39.5

13.216.322.96.0

22.915.521.820.827.929.322.717.313.415.518.218.719.731.624.317.416.215.319.225.227.828.226.820,312.720.718.611.223,127.412.419.014.410.519.512.824.814.613.114.2

21.317.820.219.77.124.526.828.217.726.111.619.414.915.426.718.19.820.613.812.720.99.65.731.410.526.1

Hf

1

5150

164432392944363540286527292850337922161111326513214050

130612335503983252927

1103763192122783190100893943

120656021204240517252473516

13019416130344961355832494364574851552559

11028533344834056784226492763466941342753618142946247

2105154575724676750555730

1505889505993604186322938265894683333no64689454

100533970362984684931355253264735

110645530499938131613

11040652924535062263928282319286858343112504034171557394862273034542425371119201621191820462841

53526054443621254620763826755946531002738205148444575

Hg ppm

5

33

3333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333333

33333333333333333333333333

irppb 40

2020

20202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020'

202020202020202020202020

2020202020202020202020202020202020202020202020202020

Ho ppm 20

1010

10101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101067101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010105510101010101010101010101010101010101010101010101010101010101010101010101010

1010101010101010101010101010101010101010101010101010

fia

500

1740012300

141001420013300118001550015400174001180015700176001370089701550015000141001250010600118007770

12600111001260015400106001490015700158001670016400123001400014100148001410012600 .14300 •1500014700155001570014200147001580018600161001590017900149001940020000181001440015200194001450015200149001390015500125001360015000157001390014500132001100014600136001560017400147001500015300184001390013600116009580

13500118001480017800157001550011500168001360014800155001590011600133001460016400145001500014400124001080010700125009970

1410014500148001390098701250075501240016900156001470016000150001790017100156001680013600167001940021800189001630019700167002130017600112001490013600144001540018300148001100016000171001780016600170001700019100139001470013600142001360012700129001660015000177009730130001390017000148001610017600121001490013100113001550094202010013500115001650016400180001750017200206001640095609390

1170086408790

1140013300141001280015700128001380010500101001610014800147001360013500133001240010700S970

1460012100108001460012600104001450013300124001380011600128009410119001240012700

12400156001400012800180001490011500132001290011300156001120015200147008230

12000154001170012900127001120012900236008200

126007660

Ni ppm 200

100100

100100100100100100100100100100100100100220100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100230100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100310100360100240100100100100100220100100100100100100100100100200100100100100100100100100220100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100230100100100100100100100100100100100100100100

100100100100100100100100100100100100210100100100100100100100100100100100100240

Rb ppm 50

5425

2525672565252525566425525560252561252552252564252525252525252525562525252525252560255050252525802568252525582525592562252525252525252575252525622555252576252525252525252525256161255525592575252525252525252525252525252525252525252525252525252525722525255125252525252525252525252525252591256825252525252525256925252525252525252572252525608725252558252525552525255225252564255452252525552525706125

10078666125252552562525252525542525252525

2525602525252525257625252525252525252525252566252525

Sb ppm 0.2

0.40.8

3.10.60.30.10.10.11.02.20,60.31.22.11.92.6'

2.23.52.93.78.24.25.11.60.14.90.51.20.50.10.50.30.10.10.40.10.30.40.10.10.50.10.60.10.10.10.10.10.10.10.10.30.10.10.10.10,10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.30.10.40.10.10.40.10.50.10.3

12.00.40.10.4fl.l0.40.10.10.30.60.10.40.30.10.10.50.60.50.10.40.90.30.10.10.10.10.10.10.50.10.10.10.10.30.10.50.60.10.10.10.30.10.10.10.10.30.10.30.10.30.10.10.10.10.10.40.10.10.10.10.10.10.10.10.10.10.10.40.60.10.10.10.10.10.10.10.10.10.30.10.10.30.10.10.10.10.14.30.61.60.10.10.20.11.10.30.10.30.40.10.30.10.10.10.10.40.10.10.10.30.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.60.10.10.1

8.20.10.10,10.61.86.17.50.95.6fl.l0.40.10.70.10.30.10.90.10.10.10.10.1fl.l0.10.1

ScPpn

0

2017

11181117202017161716181518152116321811121113231211231332201624312737182117442133222820261822232016131917176

33251721274752IB193115202213122029182717261919131214131214173018121417171427171913212013-353426172640181723142429151714181924272823161930182521182925151826232118242644212333221621102119153120254030212516232116202628374321263617272234281433181821252121IB19151616172924131711221132169

23202017182115221920271413131814121314272014

14161716201612161713252021232422303917171631IB262034

Seppra 20

1010

1010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010101010Ifl10101010101010ID1010101010101010101010

1010101010101010101010101010101010101010101010101010

Sr

0.2

0,10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10,1fl.l0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10,10.10.10.10.10.10.10.10.10.1fl.l0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1fl.l0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10,10.10.10.10.10.10.10.10.10.10.10.10.10.1fl.l0.10.10.10.10.10.10.10.10.10.1fl.l0.10.10.10.10,10.10.30.10.10.10.10.10.1Q.I0.1

Ta ppm

115

46

13443114333211321132211134734114134366

2031763177656744

1213

1767

115565344115311557253141112133415111114112353337517112344143311151243124351466416156675444181145541224141252121

105333745144665454454655233515631321112232431544

24332321122121112512211224

Th ppm

1

1526

1115212511181314181319231118161328965613157

1311193016139

14112213121019142598

17371730404336274342402579

111018162111103013153090933033162921252564142018161113231023122119121524221919113122141111101817221327331662202024166

141114121110

13040172019432713312716342948

1301206350

1901602436254514121106150

11036777746916365306

20354416142913667

522915159

3524488

212029252117312915291945213716191929262939141516151023139

141114211312261414

2116232116289

111511

240141610

1105388

2702935242625191521

U ppn 0.5

5.35.4

4.73.34.65.03.65.24.94.33.73.65.04.93.23.24.61.07.43.31.81.11.13.53.70.71.03.42.87.95.31.42.24.03.13.93.12.12.55.12.95.42.82.94.56.33.86.77.06.24.24.17.24.95.72.61.75.33.02.75.02.92.62.83.07.61.13.25.66.26.73.94.04.14.13.74,63.39.23.13.94.53.02.42.95.13.65.12.54.15.33.23.45.63.83.74.83.36.34.74.22.81.00.73.54.94.82.55.95.04.9

11.02.63.43.63.91.95.93.54.53.02.82,9

12.05.66.34.54.98.53.82.336.03.82.63.33.05,111.09.05.54.6

17.016.04.39.06.19.23.72.9

12.07.76.6

12.06.014.014.08.5

11.06.15.63.02.5

11.07.85.22.13.57.75.41.71.71.05.73.43.13.63.77.85.65.41.44.63.74.33.81.82.56.15.02.54.42.47.06.35.62.43.65.25.63.99.35.03.92.83.14.12.14.13.31.73.82.43.01.83.02.16.23.64.0

4.03.25.34.75.94.31.53.34.22.230.04.31.93.0

13.05.9

10.019.03.74.02.75.36.53.21.53.9

V ppra

4

22

22822522227

172222

10222222222

1122

10222

15141527

5525132222222222222

19152

4022228222222292222

106122224222227

112222222222

16072

15222222222222

172128222

212242522

452222

10U9

1844222222222222

122

111622272222222292242225

382

1512222

152222422222222222222222

242225222222

2222222222

13226222222222222

Zn

200

100100

10010010010010010010010010010010023010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010010023010010010010010010010010010010010010010010010010010010010020010010010010021026010010010010010010010010010010010010010010023010022010010010010010010010010010010010010010010020023010023010010010020010010010022010031024028021010010010032031020010010010010010010010030010023010010010010010010010025010024010010021010020010022010010010010010010010023010010010010033D2101001002101001001001001001001001001001001002102002002102201001001001001002202001001001001001001002:0100100100

100100100100100100100100100100100260100100240100100100100100100100100340100230

La

1

3950

27344750284434323634515329494438613019192133422239355982523532393070353633614070302835824068

100907967

10093866322343644564355302984274171210no6679406143575412037505442304164335529110744142595051504180634032313149506436767548

1705767684618443749493731310120587556

1506641578151

11080

150no380230140590490557654

1103841290180130290120250240150310140210832863no1404451

10042222729no925447307860912456475451494284743769409451

100394452575253703232382927472825312431442728583035

544666534461 ,30314633

630364927

2801502306307798648482514255

Ce ppra

3

6773

435364714967654860587371457467559049302930507134556484

1408771547765

12055575510064120534369

13064

12016014014010015014014093435763658975975354

1404271

11033035087

1206187669083

16055768160456793558045

16011064639177757068

120875948514980829856

11011083

2508198996637626083695243

44017087

11086

2501306311011071

15012020054052028020071063078

11083

1505757

4402501904301803703502204602103001304188

150190677716078364743

220120796443

11069

13036627261787869

13011057

11062

13072

1605769798666851105453634246734343554551654451924660

73759880829148616846

880557246

45022033094012014098

130120917597

NdPpn 10

4443

292737302848472335323828293520' 28

4735241455

305

25383743291319302245121619492342231721562941513640355051612720173719361844161957163243

12012024442125233930622128311814224325432363644536405144253954333940312135413125434231762938272517342524222717

160753945339554244942256131852301705464

250230253523613738

19013095

2301101901601102301201307825376283223553172039237250352017514466273428393829234957174032644899323429394426461928361934312721202335381524402927

31265436495923203230

420234820

15083

1103304244395343293752

SB

fl.l

7.06.0

4.35.35.46.04.45.35.34.24.84.56.35.44.25.36.65.18.34.52.62.72.63.86.22.94.75.55.09.35.73.53.44.13.76.83.03.23.26.43.87.03.22.74.38.14.16.68.57.96.15.28.37.47.04.72.54.23.85.05.95.37.13.83.79.73.35.87.8

20.021.06.08.85.06.74.57,25.610.03.84.56.54.03.24.96.54.36.14.0

10.08.66.25,37.86.96.65.55.59.46.35.94.74.44.06.07.66.54.06.76.65.5

16.04.96.76.04.72.64.84.85.44.34.03.7

35.012.06.07.76.0

17.09.34.7

12.07.75.29.57.5

13.036.033.016.013.046.040.06.27.45.69.85.64.632.019.015. 1)33.014.027.025.016.030.019.019.011.03.36.4

13.013.04.75.111.04.73.55.04.0

14.07.66.54.23.08.67.89.63.86.14,95.64.95.04.9

11.09.04.37.94.39.55.2

13.04.54.05.56.66.66.37.54.64.05.23.74.25.93.33.73.73.73.74.63.23.87.54.14.5

5.65.77.36.06.66.74.04.95.54.0

67.04.86.03.6

29.015.022.062.07.79.26.49.38.65.85.77.0

Eu ppm 0.2

1.81.3

0.91.31.11.21.21.61.41.21.31.11.50.91.41.30.71.22.21.30.90.80.71.11.70.81.01.61.32.61.40.9l.l1.41.21.50.80.90.81.71.21.41.01.00.91.61.02.11.51.71.41.31.31.51.51.01.01.41.11.31,61.11.41.40.62.10.60.51.41.21.11.31.71.21.71.02.41.51.81.01.21.81.10.91.42.01.21.11.42.42.01.81.31.71.41.31.21.61.51.21.51.21.00.81.41.71.71.21.31.31.62.31.11.41.10.90.91.41.51.51.10.90.92.41.61.41.61.12.31.31.22.00,91.01.10.91.52.72.01.31.43.12.51.31.71.41.91.31.02.71.51.62.81.82.92.51.72.31.91.11.61.21.42.21.81.11.32.51.01.11.41.01.31.41.40.91.01.41.71.51.01.20.90.80.80.81.01.91.31,10.80.61.60.81,20.70.61.30.41.01.21.11.00.91,20.71.11.10.51.00.80.80.90.40.60.81.50.90.9

1.01.31.60.71.81.21.11.51.31.03.71.00.60.71.91.52.13.30.91.00.81.01.00.71.21.5

Tb ppm

2

11

1111111111131111111111111111111111111311111111121111111111111111111111111111211111111111111111111111111111112211111111111111111114111111131561111111111113111111131113111121111131111111111111311111111111111111111111111

1111111111

10111111911111111

Yb ppm 0.2

7.06.9

3.57.54.96.84.36.14.35.06.23.66.55.44.74.35.14.59.43.01.91.91.93.57.11.82.45.53.4

13.45.64.08.121.69.617.46.48.24.5

16.66.013.67.08.15.2

10.65.17.88.67.44.73.99.06.57.22.1

13.59.34.26.88.116.619.94.36.79.42.74.04.53.83.95.96.93.96.84.76.65.67.34.12.73.93.82.43.66.58.15.23.15.17.64.34.58.35.34.14.84.08.14.16.26.95.72.65.4

14.36.03.86.64.25.112.74.54.04.35.63.35.47.75.25.13.52.8

11.04.56.74.33.28.56.63.022.13.22.93.42.35.27.9

12.43.54.1

11.58.35.48.63.38.76.04.07.34.16.1

10.68.19.915.67.6

10.74.73.04.04.28.2

15.69.34.25.17.73.13.93.34.19.03.68.03.93.57.26.29.33.46.45.34.74.94.64.38.35.53.94.42.77.63.55.73.72.05.77.46.27.84.84.73.55.04.33.46.42.42.72.53.33.02.63.23.37.24.14.0

4.84.56.15.14.75.11.82.94.62.3

11.03.54.25.85.53.56.111.02.42.92.04.53.53.12.84.6

Lu ppra 0.1

1.41.4

0.71.41.01.21.01.20.81.01.20.71.31.00.80.71.00.91.90.50.40.30.40.71.40.30.51.00.72.61.10.81.54.01.93.41.31.60.93.21.22.61.31.61.02.11.01.61.71.60.90.81.91.31.40.42.41.70.91.41.53.23.50.81.21.90.60.91.00.70.81.41.40.91.50.91.30.91.40.80.60.80.80.50.81.31.31.10.60.91.50.90.91.60.90.71.00.71.40.91.11.11.00.51.22.41.30.91.50.91.12.61.00.80,81.20.61.11.50.70.80.60.52,20.81.30.90.81.51.30.73.90.60.50.70.40.81.52.10.80.91.81.11.01.80.71.61.20.71.41.01.11.81.51.92.71.42.30.90.60.80.81.62.71.70.80.80.50.60.60.50.71.70.71.50.60.51.31.21.80.71.31.01.01.00,90.71.81.10.81.00.61.50.71.10.70.41.21.31.11.41.00.90.71.00.90.61.20.50.50.50.80.70.50.70.71.30.80.9

1.00.91.21.01.01.10.50.60.90.41.90.80.81.31.10.71.52.70.50.60.40.80.70.60.61.0

Massgm

37.3245.43

38.9832.4835.6642.4436.1433.8021.8343.1238.4443.9936.0840.6543.6739.2826.8840.2427.7339.4430.1847.2846.5247.6131.4543.6542.3231.0347.7226.6535.6146.6644.5935.2432.9040.4949.3445.6845.2237.8446.1034.8242.7247.5844.4440.1140.0228.0338.1326.8629.9244.6237.6432.7535.4741.9542.1337.2639.6344.0637.3631.0430.1533.5947.9230.7238.4430.1927.3732.1432.5642.0731.1342.7235.7141.2731.5237.3031.0432.4137.8237.8046.3045.4938.5027.9135.5737.3641.2129.4430.1621.7037.2224.9633.7424.6634.1026.4128.3039.6532.4431.7836.3847.9030.5222.1336.5441.2240.8127.3121.4922.8643.2439.1143.4339.6240.1735.9816.6822.0429.7530.9931.1124.6726.6424.1936.7728.0716.5931.5422.9019.9628.4332.4536.1732.1736.5230.4829.1640.0136.6237.2043.5439.2028.6732.9930.7236.6349.6623.7631.6034.7325.8934.2223.9632.6526.4426.4438.4138.0823.5837.1735.0723.1319.7834.4730.1118.8530.9322.1223.2635.2828.4139.5030.6045.3335.4639.1842.9134.9344.5434.7841.6639.5332.2545.1839.3423.2735.0335.0231.2943.4922.5236.8326.0747.3843.3635.3434.4932.8333.8132.9444.1945.7431.9839.0143.0130.5644.6845.1039.5242.2151.8243.8250.8633.6235.8337.8043.15

43.6831.3036.2339.2523.3732.2141.6721.7039.4128.9337.0231.4334.4632.8824.4636.9740.9918.2244.3749.0238.4636.4346.6526.8735.7526.61

As

1.0

2.88.2 3.7

71.03.54.33.94.25.58.77.44.66.03.95.7

23.048.03.9

13.06.5

15.018.06.559.08.04.0

47.07.34.82.92.32.56.43.02.82.92.6

16.04.64.81.18.8

13.011.010.02.11.22.30.51.82.60.50.50.51.40.50.526.08.02.24.91.42.52.41.92.23.14.92.42.40.50.52.51.91.83,94.70.50.54.06. a2.12.75.36.13.03.16.26.55.6

10.04.94.03.8

15.04.12.21.7

10.01.44.01.62.72.62.42.22.72.82.8

55.01.74.82.74.88.65.64.38.44.92.52.35.52.20.52.12.01.40.51.62.32.40.52.82.32.01.61.50.50.50.50.58.52.31.51.72.00.51,73.03.02.02.00.50.51.01.02.04.02.00,52.02.04.01.02.04.02.03.02.02.0

21.033.0

219.04.05.0

12.018.018.04.01.02.07.02.01.00.50.53.01.00.52.00.52.00.51.01.01.01.02.02.00.51.01.00.52.01.02.02.00.52.00.50.51.00.51.00.51.0

13.00.53.00.5

3.04.02.03.07.010.024.052.05.0

36.00.57.02.08.03.01.02.02.01.02.01.0

0.52.00.51.0

CHARACTER SAMPLES

Sb ppra 0.2

0.10.6 0.110.00.10.10.10.10.10.10,10.10.10.10.71.03.80.10.10.61.00.70.13.00.10.13.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.50.10.10.10.10.10.60.10.60.10.10.10.10.10.10.10.10.10.10.10.10.1O.I0.10.10.10.10.10.10.10.10.10.10.10.10.10,10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10,10.10.10.10.6fl.l0.10.10.10.10.10.10.10.10.10.10.10.50.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1O.I0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.11.00.12.00.10.10.10.10.10.10.10.10.10.10.10.10.10,10.10.10.10.10.11.00.10.10.10.10.10.10.10.10.10.50.10.10.10.10.10.10.10.10.10.10.10.10.12.00.10.10.1

0.10.10.10.10.11.01.03.00.12.00.10.10.10.1C.I0.10.10.10.10.10.1

0.10.10.10.1

Cu ppra

11625 9

96101010352626271219311653

177137728322317

1142313

104261713231734271720192825241718776720308

1587

112966

18107

74297

221010129

30114979

165

22142535662130261111326

10105

234625137

146

107

149

191516212017242015147

1210138

1123101566251322315

132

1287

1111

110119

14161511103010137447

15667

117

1115121412131423136

159

22181710121515205123

19212141351

111353927307479

48113314117

24567887

1010144

2668

18146

191818141534

131311510

9251610344047

12731871217153313161320118

12

11171112

Zn ppiB

1

2940 206427355681515446566743566587536845557650

1554436

1073644333829464130373035394428324863375618211914232618162018185137192328293515342150583139163025394547422416322451342739476150695563

104585781672545362932395321323752361921452031292645757251295518251132132621366227193527222221324335631420272316242218364434281924294034303224383839322633399247336036393687794233384234211619273122352725641823221819171434231929162142211733211631221416

273202020

39445731394655

1403291234935792?272630262523

102263027

Ag ppra0.1

0.60.7 0.20.60.20.50.30.30.30.30.30.20.50.30.40.40.60.40.30.30.30.40.50.30.30.40.60.50.40.10.20.10.50.10.30.40.10.30.10.10,40.50.30.10.20.10.10.30.30.10.10.10.10.10.10.20.40.10.10.20.10.20.10.10.10.10.10.10.10.10.10.10.10.10.10.20.10.10.10.10.10.30.20.10.10.10.10.10.10.10.1D.I0.40.60.90.10.20.60.10.30.30.30.10.10.10.30.20.10.10.10.10.10.10.10.20.10.10.10.20.10.10.10.2fl.l0.10.10.10.10.10.10.10.10.10.10.20.10.10.20,10.10.10.10.10.10.30.10.10.10.30.10.20.10.10.10.10.10.10.10.10.10.10.20.10.10.10.20.20.10.10.30.20.30.30.10.10.10.20.10.30.20.30.10.70.30.10.20.10.20.10.10.10.10.10.30.20.10.10.30.20.10.40.30.30.10.10.10.10.10.20.10.40.20.10.10.10.30.50.10.10.1

0.10.10.10.10.20.10.10,10.10.20.30.10.10.4A 1

0.10.10.10.10.10.3

0.10.10.10.1

Pb Ppn

2

710 3

1145694996

1255

1623131146

11773353418314141313

12156

1916416875555673135116476483655965375375155786

118

129

119

10596845645777761155856

11984

128446876

11141014106547

12167

1699

10768624987265

1193

10689786

108786

119599

128595

14741453452

18563452761235482654473537752

59

124847

11878638

1?547753

4434

Au ppb

5

33 3

843333333833339333333

1133833

1733333533367733333533333333333333333333333

123333333356533333677336753653

2233339533

11335353

19333353333333333733333333333333333333333333633373333333

19375333333a333333333333333333333333

10333333333

81333

9333338

1337

12333?333333

3333

NORMALIZED VALUES normalized to 20 kg. of -6 mm material

GOLD GOLD grains micrograms

01 0001001320004010101404123200000100000110fl0D20200050031030200000020100000000004101

1300002250020000013000110000000200000000100000100006413240211300103

102110000000I00200001000001000101100021000010001020100020200000100000000

10000110001020n

01101210200

221

253

1351

264

136

1310279

143

13347

35209559

122415275

11738

19998

16142

30000000120

1302

62154

18191104323200314501

7623307

1676

105

1486

60635

115

1055

131162101440

144

11411

1723

12611662320280711063705

3010332

201

1532509112

2121102112151fl23201011,

13261

25121001312102

4420171

1600270

3713

525111000350021302141

257441

13106

46

28fl454t2

141027410

2813

GOLD RATING

16 071510733132

1027141147

434425351311242333306101000310810

16324020002111fl00111100

2876',!1121

412

221314121133

25000230313a045

252

140100030100021101

10414180511402202

132120000fl0110fl4100010360550001112000292001040

! 01302502

111010000110100103010

511103

211160111-13201100601

2460

131124

2460.0

148.19.716.4

340.346.6

2453

3250242427

1823501096

2460.0

129.28.515.7

247.940.0

245393104

2451

1609

2250153

245100610241148

21779536

245373004

245172114

2459

643011

12953

2451102000373187

34936747

245151103

2455.5

34.515.96.0

36.428.0

24511

2104827

712101

245333003

2452020200020

2451067105

2120

245755023600142412710

734415519661

24510036010631

983169

24525

1003417

28968

2450.1

12.00.61.42.13.5

2456

52217

5335

24510101000

10

====*=== 2450.10.30.10.00.00.1

2451

203368

2455

2702933

106994

2450.7

36.04.93.8

14.512.5

2452

1806

1419033

24510034012354

2883231

24518

6307890

8022257

24529

940116123

15189363

2455

4204950

2520149

2452.5

67.08.28.4

70.225.0

2450.43.71.30.50.32.4

2451

101113

2451.8

22.15.93.3

11.212.6

2450.34.01.10.60.42.4

24516.5951.8235.347.48

55.9550.30

2460.0

219.05.116.6

275.339.3

2470.0

10.00.30.80.61.8

2450

1922226

66574

2460

2733926

65890

2470.00.90.20.10.00.5

m0

23I;3

1213

2410

845a

5720

013

1124

Wl 0

148 10 18

339 47

W0

41

52813

CE PROGRAM

.4 mm .4-. 5 mm ).5 im tfgt. Shape No. Shape No. Shape |gn.)

37.5

45.4 39.340.842.541.628.017.537.237.051.943.046.756.9

A 11.646.0

56.954.847.050.945.950.441.638.960.049.859.750.454.847.058.949.750.320.528.619.023.932.732,4 36.225,822.7

20.9 27.3

41.9 22.7

17.029.1 21.320.6 27.524.9

1 SA 42.3 22.8 37.9 21.341.241.137.635.4 36.7 48.5 39.330.6

SR 26.8 40.425.940.1 41.919.3 35.9 23.3

50.3 57.057.9

A 52.0 39.6 54.847.661.6

50.2

34.72G.654.532.338.319.436.629.338.64b.O50.641.530.841.342.333.940.1 38.0 31.0 44.0 44.4 28.6 32.9 27.0 47.3 30.6 46.746.5 44.8 25.0

1 SA 49.9 50.5

2 SR,SA 1 {.6x.3J 31.2 46.6 44.8 40.7 36.8 35.5

; SA 42,9

41.640.1 43.2 44.1 41.6 37.0

40.0 41.0 27.9 45.136.430.5 41.0 37.7 48.4 18.4 lfi.820.320.4 24.1 19.7 18.4 20.1

£R 1 ft 23.9 16.7 27.4 27.2 39.3 16.3 26.5 21.0

; 13.424.5 25.4 17.6 17.0 24.9 34,0 25.9 27.0 18.9 21.9 21.0 30.5 43.1 28.0

: 45.7

4 j , (i39.3 39.3 57.3 39.5 41.2 33.1 37.3 30.329.6 44.338.3 45.5 34.6 39.6 25.0 30.2 38.5 31.3

i (.6x.4J 36.9 19.1 30.1

SA 45.0 44.131.7

21.824.136.0 29.2 30.7 29.4

SA-SR 30.7 25.0

3R-R 23.9 1 SA-SR 39.9

29.633.6 34.630.8

4 3 209 1 1 0.0 2 1 61.6i 1 35.71 0 11.20 0 125.62 1 58.1

CONCENTRATE====;-__• = ----------

CONCENTRATE Mag Py Gar Misc.\ \ \

25

25 2010252010103525352530302535

1540n

35203520303030403540203520203055

151020 251530

1510 15 25 10

60 60 20152520 30 2

15 2

25352530 25 15 302020 401535 2010 tr 20

35

35 10 20 351020252555402045Vj10tr30302030201060251525 20 25 20 20 25 25 25 10 25 15 3030 30 5

50 70 50 50 10 15 10 60 105

10tr 5

15 5 5

5 20 55

tr 0

15 20 10 1010 5

20

5 tr 25 5

25 10 1020 1510 1015 40tr 15 20 15 tr 15 tr 15 5

15 6

20 15

40 10 20 25 30 15 30 20 10tr 30 10 5

10 15 5

10 15 3

tr 2

10 5 05

205070 70 30 40 40 4040 355040 4030

212 0

702115

22151

tr

tr tr05055

tr85

1015000

50005550

10555055032

tr10tr105

trtr5

tr trtr tr 2

tr2

tr 22

tr3

tr tr tr025U

tr tr 5

tt0 5

tr1

tr 10 31

0

j 10 10 535

255550$505

trtr00

1002

tr05 0 0 0 0 0 0 0 2 0

tr 00 0 fl 2 2 2 2

tr tr tr 2 02

trtr 5 2 5 0

5 5 2 5

trtr 5 0 5 0

Li tr tr

1 2

tr tr 2 b

tr 5

tr tr tr trtr tr tr tr tr tr 8

tr tr 22 i1 2 2

i) tr j

tr 0

tr tr 0 22 2 3 2 2

tr tr 1

tr tr tr tr 2 2 0J

5203 8 5

208 85

1020105

10

210 0

2534

1510

5

20 1060201520tr54005050

000

1000

101510101055050

103

tr2

trtr Cpytr 050

tr 5 0

tr 2 5 5

tr 105 Cpy

3020 Cpy 15 tr Cpy 20 0 03 Cyy

tr3

tr5

10 52

tr0

1051

tr 15

10

10 0 5 500055

10101500505

10

005

tr00 0 0 0 0 0 5 5

tr 5

tr 00 0 0

10 5 5 5 5

10 15 0 5

tr50 5 0

tr tr

10

20

5

0 15 0 0

905 5

10 5

5 2 5

tr tr 5 Cpy

60 10 5

15 10 3

20 25 ti tr Cu 5 5 0 0 0 5 0

tr

15 10 15 5

15 5 2

15 tr0 5

0 5

15 5

tr 15 10 30 0 0 5 02

4010

o0

8 1010 tr tr5

tr1020 55

2090

90610

10527

Ultraviolet lamp Rad

Sch Zir

2

1 1101010110111100000i10111201110100010 210

10

1010 0 22 11 1 0 01221i1 1 2 11 1 0101 11_21 1 1 12101

1122110110111121 0 2 1 2 0 fl 1 1 1 2 1 00 11 1 2 i 1 0 1 1 0000 2 010

10 0 000 0 0 0 0 0011101211 1 1 1 1 1 11201 11 1 11 1 1 1 1 1 11 101 1 1 1 1 10101 1 13 1 2 2 0 2 0 010

1321 1 0 1 11211 fli

209 0 31102

2

1 22112011112121

11222122222211111211110 202

0 2

22 2 1 1 1022 2 0 1 1 221112 2222 11122 2

1 111 i 22211

1121131121211111

11 2 2 1 1 1 2 2 1 1 2 112 2 1

1 1 1 1 2 0101 21 1 1

2 2 2111 2 2 1 2 12 2 1 2 2 1 3 2 1 2 2 1 2 2 11 2 1 1 1 2 0 0 2 1 1 1 1 0 2

22 1 1 2 2 2 2 20 1 2 0 2 2 3 0 2 3 3 2 1 1 31

1111 2 02 12 220 01

209 0

111113

NOTES NORHALIZED VALUES GOLD GOLD grains microgm

0 basal

0 basal0 basal0 basal0 basal0 basal00 basal0 basal0 basal0 sandy0 semi basal0 basal0 basal0 silty0 basal

silty basal0 basal0 ablation0 basal00 basal00 basal000 silty0 silty0 silty0 basal0 basal0 basal0 basal0 basal0 silty basal0 basal ;0 silty0 clayey0 silty ;0 gravelly ; 0 sandy0 silty0 siltysilty ;

0 gravelly 0 silty

silty basal j 0 sandy 0 silty i 0 sandy basal 0 sandy 0 sandy basal \ 0 silty basal0 basal i0 ablation ;0 sandy basal - 0 basal 0 basal 0 basal 0 basal ; 0 basal0 basal0 basal0 basal !0 basal 0 basal ; 0 basal j 0 basal j0 basal j 0 basal j 0 basal0 basal '0 basal :0 basal 0 basal 0 basal

0 sandy ;0 sandy 0 sandy 0 basal 0 gravelly 0 sandy :0 basal0 sandy0 basal0 silty

sandy0 basal0 basal0 basal0 basal .0 basal0 basal0 basal0 sandy ;0 basal(] basal0 silty i0 silty0 clayey i0 basal <0 basal ;0 silty basal 0 basal 0 sandy 0 basal 1 0 silty I 0 silty 0 silty i 0 basal ' 0 gravelly ! 0 basal i 0 basal : 0 gravelly basal •O K-lf T 1oasai : 0 silty ' 0 silty j 0 sandy 0 gritty basal ! 0 silty 5-3iidy ' 0 3ilty basal 0 silty 0 silty fl silty 0 silty sandy basal 0 silty sandy basal0 silty0 silty0 silty 0 silty 0 sandy 0 sandy silt basal 0 silty basal

0 sandy 0 sandy 0 basal 0 basal0 basal0 basal 0 basal 0 sandy clay 0 silty 0 silty 0 basal0 basal 0 silty 0 basal 0 basal 0 semi basal 0 basal 0 basal 0 semi basal 0 sandy-basal 0 silty basal 0 basal 0 basal 0 basal 0 basal 0 basal0 basal0 outwash? 0 basal 0 basal 0 sandy 0 basal 0 basal 0 basal 0 basal 0 silty till 0 0 0 0 0

0 sandy 0 till 4 erosion product 0 ablation 0 ablation/basal 0 basal fl sandy basal 0 clayey 0 basal 0 ablation0 basal 0 basal 0 basal 0 basal 0 basal 0 silty 0 silty basal 0 basal 0 clayey 0 sandy 0 ablation 0 silty basal 0 silty basal 0 silty 0 silty0 silty basal

0fl0 0 0 0 0 00 000 00

5 23.3

5 5.88 11,26 19.77 19.84 4.22 2.70 0.10 1.23 2.72 2.20 2.42 3.03 3.67 30.71 18.50 1.21 5.84 2.35 36.01 2.73 2.5fl 18.72 7.50 2.B0 0.23 8.11 5.53 3.35 1.83 3.83 5.01 21.34 43.63 20.46 4.20 15.55 20.93 1.84 6.32 2.78 18.05 15.90 0.53 13.7 0 3.7 2 45.5 5 13.2 0 52.4 2 2.7 1 2.5 0 59.1 2 25.00 292,3 2 11.73 15.93 128,3 0 5,2 3 13.9 0 0.8 2 16.62 4.10 3.61 10.30 0.8 1 104.0 1 15.1 0 4.73 4.8 0 2.8 3 339.12 2.9C 6.60 3.5 6 89.0 5 39.9

1 3.7 1 5.23 4.2 7 15.5 2 4.5 4 9.92 3.63 8.31 7.32 4.22 4.17 14.41 4.15 3.42 13.0

53 585.44 1.74 49.74 18.31 9.26 6.99 9.45 21.70 11.6

IB 26.90 3.03 13.3 7 10.7 3 3.7 4 11.1 3 10.6

10 13.3 2 3.7 6 10.0 5 14.9 3 12,6 3 5.0 5 3.1 0 5.83 8.40 1.0 7 117.2 4 97.1

4 30.0 17 86.9 2 24.5

10 13.2 3 36.5 2 9.8 1 10.02 1.7

13 13.72 3.49 239.4

19 6.9 12 9.2

5 1.4 5 3.41 0.6 0 0.20 4.92 0.1 1 0.3 6 3.1 0 0.8 1 1.1 0 0.70 0.52 0.2 0 24.0 2 13.1 0 2.7 0 0 . 4 3 165,7 4 0.7 2 4.2 3 16.2 4 0.5 1 0.1 0 1.2 1 8.0 6 71.64 5.2 0 1.7 2 68.6 4 17.0 1 18.1 0 0.2 0 44.0 3 0.6 2 6.2 1 15.5 0 3.9 5 95.3 0 23.5 0 7.2 0 1.1

1 19.2 3 2.1 0 1.2 5 10.2 1 12.8 3 17.0 0 16.8 j 19.8 1 14.0 3 0.10 6.4 0 5.0 2 35.8 0 7.9 6 24.1 1 2.7 3 53.8 4 14.0 3 35.1 7 219.5

; 0 57.5; 4 30.0

1 17.90 30.6 0 10.3

6 25.8 : 52 539.1

0 2.0• 1 6.1 i 2 4 .9

5 25.1 3 10.0 4 35.2 7 100.31 134.0 4 0.11 1.30 13.4 1 1.1

iL____________---______---_.-

1 215 215 0 0.0

53 585.4 3 26.3

i 6 71.532 5118.115 171.4

Au ppb

det 5

506

106 20941241348543

264538366986

74747429

11939

6496665321146573

1727452447480

33658390770

48356331

141 75

517471

852375

824 277

1500 110 144

1800 962

12500 438559

2610 92 425 29 3968270

26717

1700 309 148135 70

519061

147168

2350 1250

104 11290

127 17863

19431750

12443018665391

1250083

136047816415212838733850242

360 280 105 357 252 267 115 252 362 261 119 57

104134 16

1930 1630

llSflfl 586

1400 386 173 641 150 16622363101

3690 90 130

36 63 31

3733

10 86 14 66 4025 10

B35 597 102 17

6840 38

131 35S 15

2580113 37

2430 547 576

3 392 12

117 477 80

2400 495 136 19

460 50 20

170 300 289

1700 366 325

399 74

410 166J19 71

1250 327

1000 3600 1900 699 444 570 142

924 18200

85244 194 674 437

1420 30905220

352

382 46

213 3

18200 730

2036*******

4803

Au ragn

18.9

4.8 8.2

16.817.52.01.50.11.01.72.01.53.24.9

33.221.81.35.52.1

30.43.33.0

16.46.12.20.26.14.42.62.43.54.7

16.629.218.52.09.2

13.61,04,62.7

13.310.60.3

10.9 2,0 27.1 11.6 34.0 3.2 2.4

53,4 20.5

249.912.013.8

110.4 2.1 16.0 0.6 16.33.42.69.40.6

82.2 12.14.53.62.8

134.02.46.23.2 84.129.8

5.26.45.2

17.1 5.0 9.13.0

11.97.42.55.2

14.95.33.5

12.6477.1

1.649.714.07.27.06.5

16.011.920.71.8

12.2 11.2 4.0

11.0 11.1 11.9 3.3 8.3 9.7

12.4 3.6 2.7 4.95.90.4

96.1 82.1 JSM 27.3 62.5 15.7 6.3

22.6 6.4 7.10.914.54.3

162.6 3.7 4.8

1.4 2.60.90.12.70.1 0.3 3.2 0.7 1.2 0.70.5 0.2

20.1 11.7 1.9 0.3

163.2 0.6 3.6

10.8 0.6 0.0 0.9 5.6 34.72.8 0.9

4?. 5 9. 3

14.2 0.1

10.1 0.3 3.4

16.4 1.7

72.9 21.3

0.9

20.0 2.0 0,8 9.7 11.8 11.9 55.7 13.8 9.9 0.14.4 2.3 18.6 5.7

12.5 1.6

37.4 12.5 31.0

131.7 36.0 20.9 19.8 24.9 4.5

20.3 439.3

2.26.9 6.0

19.8 13.3 35.7 73.7

208.3 0.11.8

13.3 1.4

214 0.0

477.1 22.658.4

3411.3139.5

Agppra

5

3

33333333333333'3

333333333333333333333333 333333 3 3 3 3 3 3 33 33 3 3 3 3 33333 3 3 333 33339

10

3 33 33 3333333333333333333333 3 3 3 3 3 3 3 3 3 3 3 333 3 3

3 3 3 3 3 3 3333 3 33

3 3 3 3333 3

3 333 3 3 3 3 3 3 3 3 3 3 3 3 33 3 33 3 3 3 3 3 3 3 3 3 3 3

3 3 3 3 3 3 3 3 3 33

33 3 3 3 3 3 3 3 3 3 3 3

3 3333 3 33 333333

2133

10 3115

As ppn

2

1

1 11111541I12i1111199741318411416431341i 141211 1 1 1 1 1 1 1i 14 3 51 311331 3 433 3 4535

421

1 14 8

22 453

10115114544587

1010141267 8 9 8 5 5 1 3 4 1 7 1 2250 39 6 li 5 8 17 15 5 2 4313 31 2

11 11416 1 4 1 11 1 4 1 1 1 1 1 1 3 1 1 6 1 11 1 1 1 1 1 1 3 1 1

14 36 5 6 1

1 8 1 1 2 1 3 3 i 11 3 1 1 3 i

27 6 3 1 1

10 1 1 3

1 871 1 8 4 5 73 6335

213 1

50 46

4117

Ba ppra 200

100

310 100100290100570390310100250340100100240270270230100100340100100290100100300100220100230270310320100350390400260530 450430100390100 100340 100 100 100 570 430 100360410100 500 100 100 610 340460460440440 340 350 400330 440230340360330100 390

360 100100 100 450 360320290100100100100420100510100100100100360360260310100100450100 320 330 100 350 290 520 460 610 420 100 380 100330350 380 100 10(t 100 320 430 350 100 490 400430320290 210 100 270

100 560 520 640100100100 480 490 660 100100 100 100 100 100 670 100 370 100 340 430 100 590 100 100100 100 670 100 360 460 420 100 950 100 610 100 460 460 310

100 440 300 100 380 390 470 100 240 640510470 440 430350 100 660 100 350 400 100 410 270 100 490

690100100790100 370 100 100 100470 100420100100

213 100 950 282179

32072640

Br ppra

5

3

3 33333333333333333333333333333333333333 33383 3 3 3 3 3 3 3 33 333 3 33 33333 3 3 33 3 333333

3 33 3 33333333333333333333333 3 3 3 3 3 3 3 3 3 3 3 33 3 33

3 3 3 3 3 3 3333 3 3 3

3 3 3 333313 3 33 3 3 3 3 3 3 3 3 3 3 3 3 3 33 3 3 3 3 3 3 3 3 3 3 3 3 3 3

3 3 3 3 3 3 3 3 3 33 3 3 3 3 3 3 3 3 3 3 3 3 3 3

3 333 3 3 3 3 33333 3

213 3 8 3004

Ca \1

1

21112311323121111111121131212121314331i 211115 3 1 11 1 1 11 11 3 8 3 5 11234 1111 1 1111 11

123 31 1325432431461431431313 2 3 1 1 i 1 3 1 4 5 1 24 i 1 2 1 3 1 1 3 1 1 1141 5 1 5

1 41 455 8 6 6 1 756 i 1 1 71i1 1 1 1 1 1 71 1 5 1 1 4 4 I 1 1 1 1 4 1L

I

1

1

1

1

1

3 3 1 311 1 1 1 3 2 1 3 1 8 1 1 4 1

8 5113 1 3 114111 1

213 1 8 2235

Co ppm

5

14

13 1410131111221418121619131124181214141117121523141612151510121612322420222423 1721291730 11 21 24 23 29 23 23 1917 17138

3915 32 2928233327 3126 2730 27 35212026 8

12

11 1818 13 27 292615

240252726151933586224242121252429252329 26 25 24 20 25 25 21 27 23

190 25 2726 59 12 23

15 19 19 14 45 16 9

1420232B 27 24

17 1616 202213 29 16 41 28 2817 22 25 20 U 18 18 24 15 12 14 17 14 19 2315 25 17 22 21 18 12 16 10 13 70 22 16 37 12

13 2114 12 15 9

20 11 12 7

18 25 16 27 10 17 10 12 12 12 78 19 12 12 19

28 585140 41 48 42 48 5223 443937 45

213 7

240 2422

48066

Cr ppra 10

220

140 200150190120270200230190130170140180120310210100170180180150150190640150410130190170150100140120950440400360490620 520

1000890250750 120 390 530 460 680 440 630 28064280240160 230 110 210 680890300

1500610 980930 9601200 1200 600590770570 140 200

200 190140 140 200 1501401406301102202301402203702402603703502402002105507003602901400 2100 310 550 400 440 680 570 1500 5SO 650 850 1100880 86

200 140

170 310 130 160180 180 17098190200 180240 280

250 580 24077

250290 240 230

16000 760 710290 290 390 440 210 330 450 370 320 170 250 330 260 350 410260 710 290 330 600 240 120 150 180 150 100 260 160 43

170

170 530 160 150 220 100 220 150 150 260200 300 220 540 95

170 160 150 230 150 310 310 250 260 260

320 370

26001400 1900 2300 2000 3000 1300790

240023001400 890

213 43

16000517

11691367126

2855

Cs ppm

2

1

1 11111111111i1111111111111111111113413211111 3 1 1 1 1 1 1 1311 3 1 3 1 113231 1 11 1 1111 1 1

111 1 1 1i111111131i2111111211 11 1 1 1 1 1 1 1 1 1 11 5 1 2 1 1 1 1 1 1 1 1121 11 2

1 11 111 1 1 3 1 11 1 1 4 1 5 1 i 1 1 1 1 1 1 111 1 1 1 1 3 1 1 1 1 1 1 1 1

1 1 3 1 1 1 3 1 1 11 1 2 1 1 1 1 1 1 4 1 1 1 i 3

1 111 1 1 1 1 3i113 1

213 1 51113

Fe

0.0

18.8

9.6 21.99.122.29.87.2

10.118.021.216.29.0

16.221.120.125.018.29.620.115.711.015.516.718.519.111.77.1

11,623.718.720.914.918.913.923.69.5

13.112.014.614.112.924.629.713.029.0 9.7 16.7 25.9 16.1 30.9 27.6 32.6 25.813.1 29.711.4 11.97.2 8.5

14.0 20.622.118.628.414.2 21.7 22.2 23.625.3 24.5 20.216.020.731.57.7

10.7

19.218.413.6 11.4 21.4 14.412.09.7

26.09.7

20.919.46.9

15.622.610.18.4

20.823.514.815.79.4

12.521.311.79.021.0 17.0 11.8 17.7 9.4

14.5 17.6 15.3 17.4 13.8 16.8 16.6 23.916.1 7.8

10.4 17.2 14.J 12.9 12.5 9.6

11.3 16.0 8.3 5.16,08.19.0 6,9

11.0 9.8

11.920,8 9.9 6.9

13.35.2 8.0 9.2

10.9 19.9 16.412.5 9.4 20.2 11.6 9.1 8.5

27.9 15.0 16.1 6.4 9.0

12.7 13.2 12.5 19.611.9 42.1 12.6 14.5 28. 1 7.8 6.4 7.2

10.6 7.4

14.6 19.1 10.2 23.7 12.6

25.4 7.8 16.9 14.021.7 14.5 28.1 16.9 21.8 17.710.5 21.6 11.7 15.6 4.9 8.6 8,0 7.1

15.9 8.0 9.9

19.7 10.7 7.6

11.3

12.7 15.044.431.5 35.342.4 35.7 47.4 29.015.3 37.035.526.6 24.4

213 4.9

47.4 16.57.9

62.032.2

ppm 1

47

53 48743937654935251723

120211717262516267436162031342032211615U2327

160724260305012080

1103761

130 41 37

160 93 67 54

14023 8085 47

6248 4536675870 45 47 81

100 51 50515376 66

130

35 4423 29 33 2716312510201521238216

41019322220202034251335 21 20 24 18 21 94 70 39 27 51 73 3834 8

47 23 99 19 41 22 22 22 19 32152726 12 23 22

170 22

130 7897270 700 130

6 66

190130 280 190 290 310 130 230 300 160 79 85

230 200 140 15051 66

180 19092

130 12 74 78 72 8

45 52 5

30

2553 38 38 37 41 59 52 32 1066

30 37 28 46 58 48 45 35 22 37 29 81 39

46 21986450 82 45 637265 546644 77

213 5

700 6575

5652216

Hg ppra

5

3

3 333333333333333333J333333333333333333333333 3 3 3 3 3 3 3 33333 3 3 3 33333 33 33 3 3333 3 3

3 33 33 3333333333333333333333 3 3 3 3 3 3 3 3 3 3 3 33 3 3 3 3 3 3 3 3 3 3 3333 3 33

3 3 3333 3 33 3 33 3 3 3 3 3 3 3 3 3 3 3 3 3 333 3 3 3 3 3 3 3 3 3 3 3 3 3

3 3 3 3 3 3 J 3 3 33

33 3 3 3 3 3 3 3 3 3 3 3

33333 3 3 333 333 3

213 3'3

3003

Ir ppb 40

20

20 2020202020202020202020202020202020202020202020202020202020202020202020202020 2020202020 20 20 20 20 20 20 20 2020 2020 20 20 20 20 2020202020 20 20 2020 20 20202020 20 20

20 2020 20 20 20202020202020202020202020202020202020202020 20 20 20 20 20 20 20 20 20 20 20 2020 20 20 20 20 20 20 20 20 20 20 20202020 20 20 20

20 20 20 202020 20 20 20 20 2020 20 20 20 20 20 20 20 20 20 20 20 20 20 2020 20 20 20 20 20 20 20 20 20 20 20 20 20 20

20 20 20 20 20 20 20 20 20 2020 20 20 20 20 20 20 20 20 20 20 20 20 20 20

20 202020 20 20 20 20 2020 202020 20

213 2020 200020

Mo ppm 20

10

10 1010101010101010101010101010101010101010101010101010101010101010101010101010 101010101010 10 10 10 10 10 10 1010 1010 10 10 1010 1010101010 10 101010 10 10101020 10 10

10 1010 10 1010101010101010101010101010101010101010101010 10 10 10 10 10 10 10 10 10 10 10 1010 10 10 ID 10 10 10 10 10 10 10 10101010 1010 10

1010 10 10101010 10 1010 1010 10 10 10 10 10 10 10 10 10 10 10 10 10 1010 10 10 10 10 10 10 10 10 10 10 10 10 10 10

10 1010 10 10 10 10 10 10 1010 10 10 10 10 10 10 10 10 10 10 1C 10 10 10

10 101010 10 10 10 10 1010 101010 10

213 10 20 1010

11

Nappra 500

12300

13200 10600133001120016900162001910014500119001240014400154001090010900935012900139009960

1380013900118001190013800117001360015400128009580

1250012500113001030012800146001690012000145001530018600 158001390012000155001660019300 16500 14200 16900 11300 15500 12500 105009760 1030U15900 15600 10900 16100 12600 1870016800165001690017300 1660014100 1240010800 12700 1390015700117008460 5660

12600

14000 1390014100 14100 18600 1540014600155002140014300140001510024200141001580015100190001390013200152001290U141001780014900172001710013100 15100 16100 13600 18600 14400 12600 14200 19100 15100 20900 16800 1400015900 13600 16500 14500 11400 17300 14500 15600 15200 15900 18400 2220018200147001340018000 16300 13000

14900 19100 24100 242002210021700 18300 21200 6830 21000 1740012500 17800 16300 20200 1S300 20900 11900 11300 14900 20300 16400 15000 12500 17300 134UO20000 6600

16600 12500 13100 16500 13100 15900 19100 14700 13500 12300 15500 10400 18600

1410017500 14300 13400 14600 15100 8170

13900 17100 567018200 14000 14500 19000 19700 18400 7010

15700 13100 15100 17800 11400 19400 18900 15000

1370015800858010600 9370 8080

11400 5880

1490017200 101009070

11400 9950

213 5660

24200 146883419

1169098621527

ASSAYS

Ni ppm 200

100

100 100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100100 100100 100 100 100220 100 100100 100100100 310 100 100 100100100100100 100 100 100100 100 100100100100 100 100

IDU 100100 100 100 100100100430100100100100100100100100100100210100100100100100100100 100 210 100 100 100 100 100 100 100 220 100 100100 100 100 100 100 100 100 100 100 100 100 100100100100 100 100 100

100 100 100 100100100 100 100 100 100 100100 100 100 100 390 100 100 100 100 100 100 100 100 100 100100 100 100 100 100 100 100 100 100 100 100 100 100 100 100

100 100 100 100 100 100 100 100 100 100100100 100 100 100 100 100 100 100 100 100 230 100 100 100

100100100100 100 100 100 100 100100100100100100

213 100 430 10737

1403182

CHARACTER SAMPLES— _^ — — — .. — — — — _ — — -. — - — — — — — — — — — = = •" = =. = '" = = •• — — — — — — —- = """" = = = *" = =; = =;;= = = = — — = """' = = — — — — — — — — -- — — — *- — — — — — —

Rb ppm 50

25

25 2525255625252525502525256425255725252525252525602525258125537025252550255425 2525252525 25 2525 25 25 76 25 2525 2525 64 25 53 25 2525252525 25 25 8525 25 25252525 25 25

2525 2525 252525

120252525502525252525252525252525252525 25 25 25 25 25 25 25 25 25 25 25 2525 25 25 25 69 25 25 54 25 25 25 25252525 25 25 25

25 25 25 252525 25 25 25 25 252525 25 25 25 25 25 25 25 25 25 25 25 25 2525 25 25 25 25 25 25 25

110 25 25 25 25 25 25

25 6125 25 2525 25 75 25 256125 94 25 25 25 50 82 25 64 72 25 25 25 25

25 252525 25 7225 59 2578 252525 25

213 25

120 3116

26764

Sb ppra 0.2 0

0.1

0.1 0.10.10.10.10.10.10.10.1O.i0.30.30.10,10.20.10.10,10.30.10.50.40.50.20.10.10.10.10.10.10.30.10.10.30.10.10.10.12.30.10.10.40.10.10.1 0.1 0.1 0.4 0.1 0.1 0.1 0.10.1 0.50.10.1 0.1 0.1 0.5 0.10.30.10.10.4 0.1 O.i 0.10.1 0.1 0.10.1(UO.i 0.9 0.1

0.1 0.10.40.8 0.8 0.10.10.10.10.50.30.40.10.10.10.40.10.40.50.50.70.30.91.30.90.60.5 0.7 0.5 0.6 0.4 0.3 0.4 0.1 0.1 0.2 0.5 0.1 0.10.1 3.6 O.S 0.8 1.1 0.6 0.7 1.6 1.3 0.1 0.1 0.10.10.10.3 0.1 0.5 0.1

0.1 0.10.1 0.10.10.1 0.1 0.1 0.1 0.1 0.10.1 0.6 O.i O.i 0.1 0.6 0.1 0.1 0.4 0.1 0.1 0.1 0.1 0.1 0,10.1 0,1 0.1 0.5 0.3 0.1 0.4 0.4 0.1 0.11.10.8 0.10.7 0.1

0.1 0.2 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.10.1 O.i 0.1 0.1 0.1 0.1 0.9 0.3 0.1 0.1 1.6 0.1 O.i 0.3 0.1

0.1 0.5O.i0.6 0.1 0.1 0.5 0.1 0.10.1 0.40.10.3 0.1

213 0.1 3.6 0.30.40.11.1

Sc ppm .10

24

31 284519272421141512191413121217149

15262012152020182015128

1117222530353730172020272025 6025 15 33 21 30 19 4029 3337 21 77 34 54 1813141622 14 152220 11 25192034 2038

21 1717 21 27 20261636251823232020263617262219222529262219 20 19 22 20 21 23 21 23 18 23 21 1414 29 19 19 47 12 31 25 36 13 14 189

2627 25 26 31

49 22 45213228 32 49 35 27 4157 51 34 60 38 30 26 56 22 17 23 45 66 37 6326 22 43 58 24 22 24 27 45 23 39 26 22 22 15

1322 20 20 17 15 33 26 10 2625 2323 15 18 29 21 28 28 20 36 21 14 33 20

49411623 17 2220 152923 17172530

213 6

77 2511

13248

Se ppra 20

10

10 10101010101010 ,101010101010101010101010101010101010101010101010101010101010101010101010 10 10 10 10 10 10 10 1010 1010 10 10 10 10 1010101010 10 10 1010 10 101010iO 10 10

10 1010 10 1010101010101010101010101010101010101010101010 10 10 10 10 10 10 10 10 10 10 10 1010 10 10 10 10 10 10 10 10 10 10 10101010 10 10 10

10 1010 101010 10 10 10 10 1010 1010 10 10 10 10 10 10 10 10 10 10 10 1010 10 10 10 10 10 10 10 10 10 10 10 10 10 10

10 1010 1010 1010 10 10 101010 10 10 10 10 10 10 10 10 10 10 10 10 10

10 101010 10 1010 10 1010 10101010

213 10 10 1000

10

Sr Ta % ppm 0.2 1

0.1

0.1 0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10,10.10.1O.i0.10.10.10.10.10.10.10.10.10.10.10.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.10.1 0.10.10.1 0.1 O.i 0.1 0.10.10.10.1O.I 0.1 0.1 0.10.1 0.1 0.10.10.10.10.1o.i0.1 0.10.1 0.1 0.1 0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.10.1 0.1 0.1 0.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.10.10.10.1 O.i 0.1 0.1

0.1 0.1 0.1 0.10.10.1 0.1 0.10.1 0.1 0.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 O.i 0.1 0.1 0.1

0.10.1 0.1 0,1 0.1 0.1 0.1 0.1 0,1 0.10.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1

0.1 O.i0.10.1 0,1 0.1 0.1 0.1 0.10.1 0.10.10.10.1

213 0.1 0.1 0.10.00.00.1

6

6121486734543656143439456433496434511i12421154

26 1 3 4 1 6 4

101 8

11 5 1 8

10 11111 i 1 111 1211 5 9

14 118 8 6 6121385321112112111111 1 4 1 1 1 1 3 1 1 3 2 211 4 1 8 1 1 1 1 1 1 1111 1 1 2

91 9 211 1

10 ii 8

10 12

214 6B

4 1 3 8 5 7 7

8 1 5 7 1 1 6

11 9 1 4 1 1 1

9 7 6 10 8 8

22 9

10 24 11 2 1 7 6 1 8 6 4 6 1 8 2

1 311 1 11 111 411 2

213 1

26 441512

Th U tf Zn La Ce Nd Sm Eu Tb Yb ppm ppm ppm ppm ppra ppm ppm ppm ppra ppm ppra

1 0.5 4 200 1 3 10 0.1 0.2 2 0.2 __ —— __ — -- — — -_, — „____-----_- ———— —— ____- — — — ———33 6.2 10 100 53 81 36 5.4 0.9 1 9.1

23 5.5 2 100 42 71 22 5.4 1.2 1 13.1 40 10.0 2 100 53 89 30 6.2 1.1 2 15,435 12,0 2 100 50 86 31 6.3 1.2 3 25.522 11.0 2 100 40 60 25 4.1 1.0 1 9.418 5.0 2 100 41 73 29 5.3 1.4 1 11.326 7.8 2 100 56 91 32 6.7 1.5 1 11.512 4.1 2 100 31 57 33 5.2 1.8 1 5.218 5.3 2 200 36 62 15 3.8 1.0 1 4.516 4.2 2 220 26 46 15 2.9 0.6 1 3.814 3.4 2 100 21 38 19 2.4 0.6 1 3.89 3.4 2 100 19 35 19 3.4 1.2 1 3.5

17 8.5 2 100 23 46 5 4.1 1.6 2 16.328 3.8 2 100 16 71 19 4.1 OJ 1 4.224 4.7 2 100 32 53 14 3.0 0.8 1 4.022 3.2 15 100 33 61 14 3.2 0.7 1 3.723 3.0 2 100 34 59 25 3.7 1.1 1 4.617 2.6 18 100 24 38 18 2.8 0.8 1 3.819 3.0 2 100 28 46 18 2.8 0.6 1 2.816 2.8 33 100 30 53 21 3.5 0.9 i 5.134 7.4 2 100 60 95 26 6.5 1.0 1 11.120 4.2 2 100 30 54 21 3.7 1.1 1 6.021 3.5 2 100 32 55 16 3.3 0.7 1 4.030 3.3 2 100 41 65 24 4.5 0.0 1 4.923 3.4 2 100 34 60 20 4.4 0.9 1 6.424 3.9 2 100 40 68 22 5.1 1.4 1 6.313 3.6 2 100 34 54 28 4.3 1.3 1 4.221 4.6 2 100 46 65 21 4.3 0.8 1 5.925 4.6 2 100 50 63 21 4.4 0.8 1 5.619 4.7 2 100 33 67 33 3.2 0.6 1 4.626 2. 9 2 100 45 60 18 3.7 0.5 1 2.615 2.8 2 100 28 39 20 2.6 0.5 1 2.923 3.7 2 100 41 58 21 3.9 0.8 1 4.723 5.6 2 100 45 56 20 4.2 0.6 1 7.936 4.5 49 100 67 120 40 8.4 2.4 1 7.116 3.5 2 100 33 60 21 5.4 2.0 1 6.79 OJ 2 100 29 56 30 4.7 1.6 1 6.9

14 2.0 2 100 34 59 32 6.1 2.0 1 6.47 3.5 2 100 31 62 31 6.5 2.1 1 4.9

12 3.7 2 100 32 66 21 5.1 0.9 1 5.2 26 3.S 7 100 61 110 41 7.6 2.0 1 5.720 3.5 44 100 46 79 22 6.0 1.6 1 4.634 6.2 2 100 77 120 36 9.3 2.4 1 8.311 4.3 2 100 25 44 12 3.7 1.2 1 8.928 4.8 7 100 58 100 42 7.2 1.1 1 10.5 26 26.0 2 100 19 45 23 6.6 2.5 3 26.1 16 4.5 6 100 40 69 31 5.7 1.3 1 7.5 15 2.7 2 100 39 64 30 4.0 1.1 1 5.7 33 6.0 2 100 92 150 51 10.0 2.4 1 12.4 23 3.6 2 100 59 100 29 6.2 1.7 1 8.8 20 5.3 6 100 63 130 62 12.0 3.1 1 8.9 20 4.9 6 200 45 85 31 5.5 1.5 1 7.0 67 15.0 2 100 100 160 65 11.0 0.8 4 18.04 3.5 150 100 18 33 10 3.3 1.4 1 12.5

59 7.9 2 100 92 140 49 9.6 1.6 1 13.430 6.4 12 210 62 100 27 8.0 1.8 1 21.2 19 4.7 2 100 41 59 22 5.0 0.5 1 13.7

3 3.1 2 280 17 34 20 4.9 2.1 1 5.4 25 6.1 2 100 55 34 36 7.4 1.7 1 12.4 26 8.1 2 100 43 75 26 8.8 2.6 2 14.0 19 3.5 7 100 49 72 33 5.0 1.4 1 2.614 3.1 2 100 41 64 30 4.0 1.2 1 2.221 4.9 6 100 50 76 27 5.1 1.3 1 3.324 4.5 9 230 63 98 34 6.4 1.6 1 3.722 3.9 2 210 55 79 33 6.4 1.6 1 4.3 18 3.1 7 100 50 69 28 4.7 1.2 1 3.0 18 2.9 10 100 42 70 33 5.0 1.5 1 2.9 33 5.6 9 100 69 110 45 8.0 1.7 1 4.735 6.4 8 100 69 120 52 8.8 2.1 1 5.0 19 3.0 7 100 48 82 27 5.1 1.4 2 2.4 24 2.1 10 100 57 110 54 8.9 2.1 1 4.928 4.9 2 100 67 98 32 7.0 1.4 1 3.73(5 3.0 2 100 32 120 44 3,0 1,6 1 4.5W 7 .6 39 230 130 200 72 12.0 2.2 1 9.8 23 6.5 5 100 36 63 25 5.1 1.3 1 10.3 36 M fc 100 65 160 bb 12.0 2,5 3 24.7

33 J.6 24 100 'J5 120 4S fl.6 1.1 1 5,4 33 6.2 2 100 94 130 45 6.4 1,2 1 5.518 1.9 2 100 55 35 33 6.0 1.0 1 4.6 22 3.6 2 100 67 93 30 6.3 1.1 1 5.0 19 0.3 2 230 69 100 51 8.0 1.5 1 5.9 17 2.8 2 100 56 79 31 5.3 1.4 1 3.79 1.9 10 100 31 48 20 3.6 0.9 1 3.222 3.1 2 100 65 90 32 5.9 0.9 1 3.017 5.6 11 100 50 91 36 7.1 1.8 1 4.77 0.3 2 100 21 38 13 3.3 0.8 1 2.7

17 2.6 2 100 52 81 30 5.5 0.9 1 3.814 2.0 2 100 39 59 22 4.5 1.1 1 3.718 0.3 12 100 51 78 37 6.2 i.O 1 5.220 2.6 2 100 54 69 28 5.0 1.0 1 3.923 4.6 88 100 65 110 58 7.6 1.6 1 5.713 3.2 7 100 33 50 35 5.3 1.1 1 3.614 7.5 2 100 55 110 76 13.0 3.8 1 8.424 2.3 15 100 60 95 44 6.6 0.9 1 3.938 5.9 10 100 97 140 76 10.0 1.5 1 6.126 4.0 7 100 73 110 55 8.6 1.4 1 4.220 2.7 7 100 61 85 35 6.4 1.1 1 3.514 1.5 2 100 43 63 38 5.4 1.1 1 3.318 2,3 12 100 55 78 44 6.6 1.4 1 4.737 4.3 6 100 93 130 80 9.9 1.4 1 6.320 3.3 6 100 62 88 57 7.5 1.8 1 4.211 2.1 2 100 43 81 54 8.2 2.0 1 3.733 6.2 2 100 70 110 55 7.8 1.8 1 3.2 18 3.1 15 100 54 81 34 6.4 1.0 1 3.0 20 2.5 12 100 56 87 52 6.9 1.1 1 3.8 39 3.1 36 100 97 140 78 9.8 1.7 1 4.1 16 3.0 26 100 45 74 39 5.5 1.0 1 3.6 20 1.9 16 100 56 84 38 6.1 1.1 1 4.3 33 5.7 10 100 84 120 66 9.0 1.6 1 5.7 23 4.4 12 100 60 89 39 6.6 1.3 1 5.1 38 4.2 18 100 90 130 76 10.0 1.7 1 5.6 26 2.9 5 100 72 100 46 7.8 1.5 1 3.8 23 5.6 32 100 69 95 44 7.7 1.9 1 4.3 30 4.5 19 100 85 120 52 9.1 2.2 1 4.7 20 3.1 8 100 55 76 33 5.2 1.2 1 2.713 2.2 2 100 39 64 26 4.3 1.3 1 2.7 5 1.5 66 100 23 42 19 3.6 1.0 1 2.7

49 3.8 18 100 140 170 68 11.0 1.1 1 4.7 18 3.2 2 100 52 69 30 5.3 1.0 1 4.3

120 10.0 30 100 330 430 240 26.0 2.4 1 12.8 19 2.8 2 100 55 75 28 4.9 0.8 1 2.3 38 4.6 7 230 110 170 61 11.0 1.9 1 7.3 12 2.6 2 100 43 66 37 5.8 1.5 1 5.4 18 1.9 2 100 72 110 37 8.3 1.0 1 5.5 16 1.3 2 100 41 66 26 4.1 1.1 1 2.3 14 2.3 2 100 44 67 24 4.7 1.1 1 2.2 18 1.9 5 100 55 88 33 5.4 1.1 1 3.35 2.9 2 100 20 26 14 2.2 0.7 1 1.5

12 1.5 2 100 36 55 24 4.3 1.0 1 3.518 3.1 2 100 52 78 20 5.3 1.2 1 3.3 6 2.5 2 100 21 35 20 3.4 1.0 1 2.5

14 2.1 2 100 33 74 30 5.3 U 1 3.6 9 0.3 2 100 29 49 32 4.5 1.4 1 3.3

35 11.0 2 100 88 140 52 11.0 2.7 1 16.5 4 2.3 2 100 17 35 5 4.1 0.7 i 3.0

41 6.2 2 100 110 170 75 12.0 2.2 3 14.3 9 4.2 2 100 71 200 130 23.0 7.4 1 6.6

10 4.1 2 100 32 67 41 7.6 3.0 1 8.720 5.4 2 100 41 84 40 10.0 3.4 3 16.4 20 18.0 2 100 140 350 200 34.0 10. B 1 19.6 23 8.8 2 100 54 93 49 8.6 2.3 1 22.8 4 0.3 2 1100 15 22 5 1.8 0.9 1 1.6

18 2.6 2 100 52 92 5 7.2 1.9 4 5.0 35 11.0 2 100 84 150 79 13.0 3.8 1 10. B23 8.8 2 100 57 110 50 9.5 3.1 4 20.9 42 15.0 14 100 130 210 120 22.0 5.9 1 18.5 37 9.6 2 100 100 160 67 13.0 3.5 1 13.4

100 23.0 16 100 230 350 140 25.0 4.0 1 27.1 20 13.0 2 270 110 230 130 25.0 8.0 1 15.8 lb 8.5 2 100 130 240 140 21.0 7.2 1 7.9 34 9.6 39 100 80 140 60 11.0 2.3 1 11. 7 29 13,0 75 100 76 140 43 15.0 4.8 4 18.9 20 5.6 63 100 53 96 35 8.1 2.7 1 8.2 15 3.4 2 100 41 66 27 4.9 1.5 1 5.1 H 3.7 2 100 49 78 35 6.8 2.2 1 5.9 52 12,0 12 100 130 220 100 16.0 3.6 4 18.1 26 7.2 15 100 69 110 48 9.1 2.4 3 18.1 24 6.5 8 100 65 100 40 7.9 1.0 1 17.8 36 9.9 2 100 90 160 63 13.0 3.7 4 24.513 1.5 2 100 39 68 33 5.3 1.7 1 8.0 25 5.9 16 230 58 93 31 5.8 1.0 3 9.5 35 9.2 9 100 78 140 54 11.0 3.2 1 19.7 43 9.8 2 100 110 170 68 13.0 3.8 1 224 29 5.0 6 100 70 100 36 6.6 1.0 1 8.7 12 7.1 10 100 49 94 70 11.0 3.1 1 7.8 8 2.9 9 100 35 63 35 5.5 1.1 1 15.5

26 6.4 2 100 87 140 79 13.0 2,4 1 12.3 24 8.0 29 100 58 99 54 11.0 2.3 4 29.2 25 6.9 12 100 61 92 49 7.3 1.0 2 12.5 2 0.3 10 210 20 41 34 5.9 2.4 1 3.9

14 5.6 33 100 32 43 20 4.7 1.0 1 6.8 11 3.0 11 100 47 75 35 6.3 2.0 1 6.8 1 0.3 2 100 10 24 5 3.5 1.1 1 5.4

10 2.9 6 100 29 47 26 4.3 1.1 1 5.7

27 6.5 2 100 46 68 22 5.6 0.9 1 7.4 23 6.5 2 100 50 78 34 7.0 1.5 1 11.4 26 5.2 2 100 39 62 42 5.7 1.3 1 9.4 26 7.6 2 100 43 62 31 5.4 0.9 1 10.4 26 5.6 2 100 43 70 36 5.5 1.1 1 6.5 22 6.5 2 100 48 77 25 5.7 1.0 1 12.0 48 18.0 9 100 100 150 50 12.0 1.4 3 25.9 23 9.0 2 100 50 73 20 6.0 1.2 1 15.6 20 5.6 2 100 49 72 19 6.3 1.2 1 8.4

4 0.5 2 1 00 13 21 5 2.1 0.7 1 4.614 3.2 2 100 43 61 15 5.0 1.4 1 5.7 10 3.0 2 100 32 45 23 3.6 0.9 1 4.9 10 2.8 14 100 34 45 23 3.5 1.1 i 3.5 13 3.1 2 100 36 53 24 4.3 1.2 1 3.5 12 3.1 2 100 23 38 22 2.9 0.8 1 6.8 25 4.1 2 100 47 85 60 8.0 1.9 2 12.5 25 6.3 160 100 43 72 40 6,7 1.4 1 12.0 25 4.4 4 100 53 83 41 7,9 1.1 1 12.7 24 4.3 8 100 52 84 48 7.4 0.7 3 16.4 18 3.5 2 100 38 64 28 6.0 1.4 i B.I 10 1.0 2 100 44 74 51 9.2 2.8 1 5.4 20 5.0 22 100 45 69 29 6.2 1.3 1 6.8 13 2.1 2 100 35 51 26 4.1 0.9 i 6.7 27 4.0 6 100 69 100 32 7.6 1.5 1 13.8 17 5.0 7 100 36 58 38 6.6 1.0 1 6.9

31 3.1 10 100 84 140 51 9.8 1.9 1 8.511 4.5 _b 100 4l> 85 20 6.6 1.7 1 4.836 5.7 2 100 79 120 26 7.1 1.9 1 5.035 4.9 2 100 94 160 55 9.7 2.0 1 5.3 22 4.2 2 100 52 81 25 5.1 1.4 1 3.7 35 5.2 16 100 87 120 45 7.5 0.6 1 5.8 23 3.4 9 100 59 95 33 6.0 1.6 1 4.6 26 4.1 2 100 60 90 30 5.2 1.6 1 4.1 36 5.6 21 210 100 160 71 12.0 2.6 1 6.327 3.8 2 100 77 110 33 7.6 1.7 1 4.4 25 2.9 2 100 66 110 34 6.7 1.7 1 3.931 5.5 6 100 85 120 44 7.6 1.5 2 4.334 5.1 22 100 78 120 41 7.8 1.4 1 5.2 48 6.8 9 100 130 180 59 12.0 2.2 1 7.7

____--.-_ — ------------••-- ^ = ===== = = ±=. = zs = =;= = = = = = = = = ==- =— — — — ——— -— ===-=======

213 213 213 213 213 213 213 213 213 213 213 1 0.3 2 100 10 21 5 1.8 0.5 1 1.5

120 26.0 160 1100 330 430 240 34.0 10.8 4 29.2 23 5.0 10 113 58 93 40 7.2 1.7 1 7.914 3.5 19 75 34 53 28 4,3 1.2 1 5.7

190 12.5 357 5627 1166 2782 811 18.6 1.5 0 32.751 12.1 47 263 126 198 97 15,9 4,2 3 19.3

Lu ppm 0.1

1.9

2.32.84.51.92.12.11.00.90.90.70.73.2n au . o n nU.o0.70.9n flU . 0

0.61.12.01.10 0

. 0

1.01.31.20.71.11.10 0.0

0.60.60.51.51.51.41.41.21.01.0 1.11.01.31.22.23.6 1.4 1.1 2.3 1.9 1.7 1.3 3.42.3 2.53.92.4 0.92.2 2.3 0.60.40.70.80.8 0.6 0.7 1.01.2 0.6 0.90.80.92.0 2.0 4.8

1.0 1.10.8 1.0 1.20.70.60.60.80.50.70.61.00.61.10.61.80.71.2o.e0.60.7o.e1.20.90.70.7 0.5 0.7 D.9 0.8 0.7 1.3 1.1 1.1 0.6 0.8 0.9 0.60.4 0.4 0.9 0.7 2.5 0.4 1.4 0.9 1.0 0.4 0.5 0.70.30.80.8 0.50.8 0.7

3.2 0.5 2.8 1.51.6

4.3 4.3 0.4 1.0 2.41.1 3.8 2.6 5,2 3.2 1.6 2.8 3.5 1.7 0.9 1.2 3.8 3.5 3.5 4.91.5 2.0 3.9 4.5 1.7 1.5 2.7 1.9 4.9 2.1 0.9 1.3 1.1 0.8 1.0

1.1 2.1 1.6 1.9 1.3 2.0 4.6 2.7 1.6 0.81.1 0.9 0.7 0.6 1.3 2.3 2.1 2.4 3.1 1.5 1.1 1.2 1.2 2.7 1.3

1.7 1.01.11.3 0.8 1.3 0.9 0.9 1.21.00.81.00.9 1.5

213 0.3 5.2 1.51.01.13.6

Mass gra

37.27

45.22 39.24 40.7242.3741.5127.8417.3937.0836.89M titJj. . 00

42.9846.5756.7444.4545.9145.6445.9054.6546.8950.6745.7250.1641.5338.7559.8649.7259.5950.2654.6546.8558.7649.4550.1220.35

i a a*.ia ,3 j11 00L J . OJ T) (, 1j_ . bi ) "> ifSt. io36.06

22.46U » T. 4.20.86 27.23 32.87 41.81 22.69 28.70 16.97 29.69 21.2919.99 27.36T » 1 f24.76 42.2822.64 37.72 21.11 41.0641.0737.4735.2936.57 48.35 39.17 30.4226.66 40.35 25.8140.0141.8413.1935.80 23.80

50.26 56.3157.93 51.86 39.53 54.6247.4961.46 23 374- J . J i

50.0341.54J4.5tf28.4954.2732.25 la i TJO . i '

19.43

29.23 39.0645.8450.4941.4130.7241.314 "I 1 9W. . i o11 0 1JJ .OJ

40.10 37.80 30.91 44.00 44.39 28.62 32.80 26.87 47.32 30.60 46.54 46.6544.0224. V9 49.79 50.37 30.85 46.50 44.67 40.67 36.61 35.32 42.86 42.7541.5940.0142.94 44.11 41.5336.84

40.03 40.99 27.80 45.00 36.3430,4329.7937.63 48.2318.29 16.7420.2620.5224.03 19.65 18.20 20.03 23.66 16.63 27.12 27.02 39.25 16.11 26.37 21.05 13.46 24.4125.24 17.51 16.98 24.73 33.55 25.84 27.97 18.95 34.47 20.93 30.39 42.93 21.79 45.56

43.5139.26 39.18 57.09 39.39 41.20 32.76 37.57 30.34 29.4044.15 38.20 45.41 34.4339.29 25.57 29.89 38.22 31.03 36.59 18.93 29.85 44.69 43.77 31.44

21.94 24.1426.30 TQ in/o , JU

30.90 29.41 30.50 25.15 23.8539.91 29.73Tl (.7 JJ . t> 1

34.69 30,84

.= == ======213

13.46 61.46 35.70 10.77

116.0257.24

As ppm

1

3.11.91.4 1.30.51.12.82.57.63.44.02.37.74.00.51.60.51.92.31.9

10.037.09.57.67.32.7

11.012.02.46.41.52.51.912.02.63.33.24.01.90.50.52.11.61.63. 30.5 4,3 1.5 1.4 2.3 0.5 0.5 1.4 2,5

0.59.4 5.0 3.6 1.7

10.0 2.13.24.40.50.5 3.8 3.8 3.01.6 0.5 5.53.94.25.6

66.0 5.1

1.71.12.4

23.0 56.0 6.17.35.3 6.24.13.35.11.52.84.31.53.2f 1ij . L5 10 . '

14.016.0i a n io .U14.015.015.04.8

12.010.0 10.0 18.0 8.0 8.2 4.2 3.6 4.2 2.9 2.7 3.3 3.83.5

18.0 108.0 10.0 12.0 8.5

18.0 32.0 31.0 3.4 3.6 2.72.20.53.2

1.7 3.1

3.1 3.0 1.9 1.9 0.54.30.5 1.81.72.1 1.8 3.10.5 0.5 2.2 1.4 1.6 0.5 3.2 1.5 2.0 0.5 3.3 0.5 2.0 4,2 1.80.5 2.8 2.1 0.5 2.2 4.5 0.5 2.6 1.8

10.0 171.0 18.0 5.1 2.6

0.5 3.0 2.0 0.5 2.0 1.9 1.7 0.5 1.2 2.50.5 2.7 2.4 0.5 10.0 2.5 57.0 6.9 4.3 2.3 6.5

32.0 2.1 2.1 5.5

3.0

====-======1990.5

171.0 7.0 16.4

268.039.7•i j • .

Sb ppm

0

0.1 0.10.1 0.1 0.10.10.50.40.10.10.10.10.50.10.10.10.10.10.10.10.10.10.50.40.10.50.50.10.10.10.10.10.10.10.40.10.1O.iO.I0.10.10.10.10.10.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1

0.10.1 0.1 0.1 0.1 0.8 0.10.10.10.10.1 0.1 0.1 0.10.1 0.1 0.10.10.10.11.2 0.1

0.1 0.1G.I 0.1 1.6 0.10.10.1 O.iO.i0.1O.i0.10.10.1 0.10.11.10.10.71.20.50 0. o

1.20.10.11.10.1 0.1 0.9 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.10.1 2.5 0.9 0.8 1.5 0.1 2.0 4.3 2.6 0.1 0.1 0.10.10.10.1

0.1 0.1

0.1 0.4 0.1 0.1 0.1LI. 50.3 0.1 0.10.1 0.1 0.10.1 0.1 0.1 0.1 0.1 O.i 0.1 0.1 C.I 0.1 O.i 0.1 0.1 0.1 0.10.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.6 1.0 0.1 0.1 0.7

0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.50.1 0.1 0.1 0.1 0.1 0.1 1.3 0.1 0.1 0.4 0.4 0.4 0.1 0.1 0.1

0.3

======1990.1 4.3 0.3 0.50.21.2

Cu ppra

1

5 1719 939

17131816131313975

22226

202018237

133220251012101914228

tiD 1

59

17606

12t 74 /

1719 11 10 17 8

19 34 21 8

92911 28 45 63 624712278

28 64 1527 30 83773353 13 13

11 1713 47

127 508530 08

5675201858 45353039

Tfl'0

4473

7144T jl/441 73

127 74 65 63 84 87 28 28 42 4527 49 18 19 16 23 76 25 40 5

13 155

1331

20 19

8 29 17 8 7

1014 8

22 1626 2010 23 12

3 8 7

10 2

17 6

14 3

14 29 859

1633 19 12 43 6

13 27 28 35 18 42 34

613 18 11 14 6

33 8 0

16533U 71 27 51 26 10 14

fl 18 65 21 9

10 10

138

5=====

199 2

16530 27

71683

Zn ppra

1

30 2130 26 192052284229662151281031623837385518362460J823712123205840

12349

46104

641122

5211025 62 64 15 29 20 46 15 37

541227 77 55

144 202427212625 46216232 603130

18 16

28 1918 53 94 415016 606611n28

404583214B40,n4 /

4546426056C QJO

44 110 57 66 40 38 19 64 25 70 36 2531 98 24 54 29 28

626 43 63 20 36 47354558

4060

16

36 57 313U

128 15 8639 512127 22 45 18 28 19 22 7

22 IB 26 10 10 47 6574 45

29 45

132 26 29 13 87 168 43

199 60

17 35 63 29 31 2S 50 13 21 6923 42

109 26 89 57 21 29 22 23

128 107 17 16 44

77

=======199

7 62647 51

2565148

Ag ppra

0

0.1 0.10.10.1 0.10.10.10.10,10.10,10,10.10.10.20.10.10.20.10.30.10.10.10.30.10.10.10.20.30.10.10.10.10.10.10.20.10.10.10.10.10.1 0.10.10.10.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1

0.10.1 0.1 0.1 0.1 0.1 0.10.10.10.10.1 0.1 0.1 0.10.1 0.1 0.1O-.l0.10.1 0.1 0.1

0.1 0.10.1 0.1 0.1 0.10.10.1 0.10.10.2O.i0.10.10.1 0.20.20.10.10.10.10.10.10.20.10.10.1O.i 0.1 0.1 0.1 0.1 0.1 0.2 0.1 0.1 0.1 0.1 0.10.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.10.10.10.3

0.1 0.1

0.1 0.1 0.1 0.1 0.3O.i0.1 0.1 0.10.1 0.3 0.10.2 0.1 0.2 0.5 0.3 0.4 0.3 0,1 0.3 0.2 1.0 0.1 0.1 0.1 0.10.1 0.1 0.10.1 0.1 0.2 0.1 0.1 0.1 0.1 0.5 0.1 0.2 0.2

0.3 0.1 0.1 0.3 0.2 0.1 0.1 D.I 0.1 0.10.1 0.1 0.1 0.1 0.1 0.1 0.2 0.1 0.1 0.1 0.1 0.1 0.1 0.1 0.1

0.1

======199 0.1 1.0 0.1 0.10.00.3

Pbppra

2

44 4 41

129

148

11101415693111213211098

117S

12631

128796

10i a io4

12

3 5

1017

4 21

585 42 1 63 7

52 1

12 4

18 448433 9 49 i

14529 8 2

111 5 4 175

1212

75

7 87466675599

6 22 12 11 7 8 6

13 8 8 7 87

10 2 7

11 3

10 4 7

5 7

1155

36

7 17 6

10 5

1615 1 8 9

14 96 4

11 7 5 6 6 6 4 4 7 2 6

17 114

12 11 7 5

21 4 9 7 4

15 2 1 B

2 3 6 3 6 3

10 2 5 95 483 a

12 7 4 4 6 1

11 2 6

15

6

= === =199

1 585 10 41

169433

Au ppb

5

3 33 3 J33333333336336373333333333333333333333335 3 3 3 3 3 3 3 3

3 3 3 3 3 33333 3 333 3

12333

19 3

7 3333 333 333j333

503383j3-*

33333 333 3 3 3 3 3 3 3 33 3 3 J J 3 3 3 3 3 3 3333

3 3

33 3 3 333 J3 3 3 33 3 3 3 3

3 3 3 3 5 3 3 3 33 35 3 3 3 3 3 3 3 7 3 3 3

33 3 3 3 3 3

432 3 333 3 3 3 3

15 3

11 6 3

15 3

17 3

8

— - =====202

0 432

630

92467

NORMALIZED VALUES normalized to 20 kg, ========of -6 mm

GOLDgrains

5

5 8 67420032023710145130200313533143605342 85030 2 5 0 2 1 0 2 023 3 0 3 0 22010 1 1 03 0 320 06 5

1 13 7 2 4231227

52

5344416950

18037 3 4 3

10 2 6 5 3 3 5 03 0 7 4 7 4

17 2

10 3 2 1L

132 9

19 12

5 5 1 0 0* 2

1 If0

0 02 0 2 0 0 3 4 2 3 4 1 0 1 6 402 4 i 0 0 3 2 1 0 5 0 0 0

13 0 51 3 0 3 1 j0 0 2 0 6 1 34i7 0 4 1 0 0

6 52 012 5 3 4 7

J01

=============215

0 533

3215

material GOLD micrograms

23

611 2020430132234

3119162

3833

1973flB63245

2144204

1621273

1816014 4

46 13 52 3 2

59 25

29212 16

128 5

14 1

1744

111

104 15 55 3

339374

89 40

4 54

15

104n0

745

144 3

5852

50189792212273

1311 4

11 11 13 4

10 15 13 5 3 68 1

117 98

355 30 87 25 13 37 10 102

193

239 . 7 9

1 3 1 0 500J 11 100 24 13 3 0

166 1 4

16 1 0 1 8

72 52

89 17 18 0

44 1 6

16 4

95 23 7 1

19 3 1

10 13 17 77 20 14 065

36 8

24 3

54 14 35

220 58 30 18 31 10

26 539

265

25 10 35

100

0 1

131

==========215

0 56528 '12

5119171

GOLDRATING

9

7 7

109320033134

194025

103443103226345

121436242 9

0

10 6

11 4 3

12 8

t BJO

37

52 18 0 52130

22 4 16 1

69i--1 1

22 12

314

11 2 6 34312

13334

1363

13633682

201763 6 5 8 3 6 5 5 3 4 13 0

39 24

116 10 29 6 5 8 6 41

, 102

5111 9

4 4 1 0111

0 10 02 5 6 1 0 49 2

: 21 6

31 0 4

18 30

20 4 5 0 9 2 2 4 1

26 5 2 0

52 0 8 5 5 15 19 5 21 1 8 2 6 1

13 6 11 80 12 9 8 7 2

8 124

022 9 7 12 27 n1 131

===========215

0 136

9id

31644

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BULK TILL SAMPLING PROGRAM - Geology Ontario