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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
I
I
I
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 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
I I I I I I I I I I I I I I I I I I I
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 I I I I I I I I I I I I I I I I I I
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.
I I I I I I I I I I I I I I I I I I I
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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.
I I I I I I I I I I I I I I I I I I I
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.
I I I I I I I I I I I I I I I I I I I
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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.
I I I I I I I I I I I I I I I I I I I
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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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MINGOLD RESOURCES INC.
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QUETICO PROJECT
Shebandowan Area
I I I I I I I I I I I I I I I I I I I
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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.
I I I I I I I I I I I I I I I I I I I
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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)
I I I I I I I I I I I I I I I I I I I
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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.
I I I I I I I I I I I I I I I I I I I
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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
I I I I I I I I I I I I I I I I I I I
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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 ' ' *^i 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'
- 16 -
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
I I I I I I I I I I I I I I I I I I I
- 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.
I I I I I I I I I I I I I I I I I I I
- 19 -
(c) Results (Table 3)
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
Normalized ValuesSampleNo.
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
CharacterSampleAu ppb
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
I I I I I I I I I I I I I I I I I I I
- 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.
(c) Results (Table 5)
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
Normalized ValuesSampleNo.
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
CharacterSampleAu ppb
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
I I I I I I I I I I I I I I I I I I I
- 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.
I I I I I I I I I I I I I I I I I I I
- 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 ppb^u. 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 sedi^e^ts clastic sedinients
4 clsstic ssdi'snts
2 felsic volcanics
MINGOLDEASTERN DISTRICT
RESOURCESTHUNDER BAY OFFICE
Ql'ETICO PROJECT
Emo Area
I I I I I I I I I I I I I I I I I I I
- 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.
(c) Results (Table 7)
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
Normalized ValuesSampleNo.
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
CharacterSampleAu ppb
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
I I I I I I I I I I I I I I I I I I I
- 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
I I I I I I I I I I I I I I I I I I I
- 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
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I
I
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(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
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I
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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.
I
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NORMAL::3D V
ALUES
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39
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CHARACTER
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APS
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TEM
SY
MB
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A
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A 76
A 77
A 78
A 73
A 80
A
81
A 84
A
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6A
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8 A
109
A 11
0 A
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2 A
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A 180
A 181
A 182
A 184
A 235
A 236
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7 ARE
1 ARE
2 AR
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4
4 1 0 1 13 2 0 0 0 0 0 1 3 0 0 1
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idge
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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
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perty descriptions)
(7)
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(8)
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ay C
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r(3
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Thom
pson
(31)
Ano
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4U
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etal
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Bar
ber
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Au
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tt Is
land
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nel
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(37}
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m O
GS P
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GS P
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15
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2279
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GS H
ap P
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77.
Publ
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1979
P
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n pa
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s (I
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fouf
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(2)
Trav
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Inl
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H
upch
uck
(4)
Miro
nsky
(5)
Redg
ut B
ay(6
) Be
lacoin
a(7
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cket
Pond
(8)
Horan
da P
ocke
t(9
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Tavi
sh(1
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aram
aque
(11)
Dal
ey-G
albr
aith
(12)
Nick
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3) W
allac
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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
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geol
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GN
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GS P
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SHEBANDOWAN AREA s - stoniness del - delicateBULK TILL. RECONNAISSANCE PROGRAM
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
52A/05 52A/05 52A/Q5 52A/05 52A/05 52A/05 52A/05 52A/05 52B/09 52B/09 52B/09 52B/09 52B/09
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
^It
-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
95
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
. 10010010031039037039043052048038034025032054031010010036010010043010031010010010010010037025028010031024022034010010D45010024021032010028047010036033010039029010010023010010029040010010055010023030030020036032010010030046035048040010010032010036046058046034010010048010010010046010010043010049049010027051024035059010010043010010010010045G100100530100380100100280100310410100440100100320400350390100100340100100210250610100330100100100250100220310390350320200100280260370240480100290320100400100440100100100100300
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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