geological survey geochemical survey of the eastern ... · on a log scale, and is therefore useful...

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UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN SOLOMON AND SOUTHEASTERN BENDELEBEN QUADRANGLES, SEWARD PENINSULA, ALASKA by Thomas P. Miller and Donald G. Grybeck Open-file report 1973 73- This report is preliminary and has not been edited or reviewed for conformity with Geological Survey standards

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Page 1: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

UNITED STATES DEPARTMENT OF THE INTERIOR

GEOLOGICAL SURVEY

GEOCHEMICAL SURVEY OF THE EASTERN SOLOMON AND

SOUTHEASTERN BENDELEBEN QUADRANGLES, SEWARD PENINSULA, ALASKA

by

Thomas P. Miller and Donald G. Grybeck

Open-file report

197373-

This report is preliminary and has not been edited or reviewed for conformity with Geological Survey standards

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Introduction

A reconnaissance geochemical sampling program involving chiefly stream sediment sampling has recently been completed as part of a regional mapping project in the southeastern Seward Peninsula. A total of 422 stream sediment samples were collected over an area of about 1400 sq mi and rock samples from some of the mineralized localities encountered during the mapping were also analyzed. This program was designed to supplement geologic mapping by providing background geo­ chemical data and the purpose of this report is to present the results of this sampling program.

A geologic map which includes the survey area has recently been completed by Miller and others (1972) and should be consulted in inter­ preting the analytical results discussed in this report. Earlier geologic reports on parts of the area are contained in Smith and Eakin (1911) and Mendenhall (1901). The lead-silver deposits at the Omilak mine and the Foster prospect in the Darby Mountains (fig. 1) have been discussed by Herreid (1965) and Mulligan (1962) and a mineralized area in the northern Darby Mountains was reported in Miller and others (1971).

Sampling and Analytical Procedures

The analytical data for the stream and rock sediments are given in tables 1 and 2 respectively and the location of analyzed samples are shown in figure 1. Standard procedures were followed in the collection and preparation of the stream sediment samples. They were generally collected from the active stream channel; where this was not possible, the samples were collected from stream deposits adjacent to the active channel. The samples were dried, sieved, and the -80 mesh fraction was analyzed for 30 elements by the six-step semiquantitative spectrographic method and for gold by atomic absorption techniques. The spectrographic analyses were reported in percentage Cpct) or parts per million (ppm) as geo­ metric mid-points (i.e., 1.0, 0.7, 0.5, 0.3, 0.2, 0.15, 0.1, etc.) of geometric brackets having the boundaries 1.2, 0.83, 0.56, 0.38, 0.26, 0.18, 0.12, 0.083, etc. or some multiple thereof. The precision of semiquantitative spectrographic results is approximately plus 100 percent or minus 50 percent; analyses for gold by the atomic absorption method are accurate to +. 100 percent.

The geochemical results in tables 1 and 2 are reported as analytical values such as 7.000 ppm, 10.000 percent, etc. or as qualified values expressed by a letter symbol. These letter codes are N = not detected, L = present but less than value shown, G = greater than value shown, and B = no data. Note that the right-most zero digits for each analytical value may or may not be significant.

The specified lower limits of detection for each element are as follows:

Fe(iron) .05%

Mn(manganese) 10 ppm

Mg (magnesium)

Ag(silver) 0.5 ppm

Ca(calcium) .05%

As(arsenic) 200 ppm

Ti(titanium) .002%

Au(gold spec.) 10 ppm

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li (boron) 10 ppm

Cd (cadmium) 20 ppm

La(lanthanum) , 20 ppm

Pb(lead) 10 ppm

Sr(strontium) 100 ppm

Zn(zinc) 200 ppm

Ba(barium) 20 ppm

Co(cobalt) 5 ppm

Mo(molybdenum) 5 ppm

Sb(antimony) 100 ppm

V (vanadium) 10 ppm

Zr (zirconium) 10 ppm

Be (beryllium) 1 ppm

Cr( chromium) 10 ppm

Nb (niobium) 10 ppm

Sc(scandium) 5 ppm

W(tungsten) 50 ppm_ - r i -

Au(gold, atomic absorp.) .02 ppm

Bi(bismuth) 10 ppm

Cu(copper) 5 ppm

Ni (nickel) 5 ppm

Sn(tin) 10 ppm

Y(yttrium) 10 ppm

The semiquantitative spectrographic analyses were done by K. J. Curry and the atomic absorption analyses were done chiefly by R. L, Miller and D. G. Murrey.

Because the original computer print-out is used in tables 1, 2, 3 and 5, element symbols are in capital letters; for example, the symbol for iron, Fe, becomes FE, magnesium, Mg, becomes MG, and so on.

The results of the stream sediment analyses have been processed by means of a computer program known as GEOSUM and are presented in table 3. The GEOSUM program is designed primarily for summarizing and tabulating semiquantitative spectrographic analyses. The program output consists of: (a) a tabulation of the data, (b) histograms and cummulative frequency distributions, and (c) a statistical summary which includes geometric means and deviations. All 422 stream sediment analyses were run through this program and the histograms and other statistical para­ meters for the entire sample set are given in tables 1 and 3.

The frequency distributions and histograms are on logarithmic scales and are computed using these brackets as class intervals, for example:

Reported value (ppm)

1.01.5 ! 2.0 ! 3.0 5.0 7,0

10.0

Limits

.83 1.2 1.8 2.6 3.8 5.6 8.3

1.2 1.8 2.6 3.8 5.6 8.3 12.0

On the histograms decimal numbers are shown as powers of 10, for example:

i7.0E-01 means 7 7.0E 00 means 7 7.0E 01 means 7 7.0E 02 means 7 7.0E 03 means 7.0

0 x 100 x 10°0 x 1010 x 1020 x 103

or 0.7or 7.0or 70.0or 700.0or 7,000.0

Page 4: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

The histograms are constructed of X l s, each of which represents 1 percent of the total number of samples.

The histograms and the statistics given below them are derived only from data values within the ranges of analytical determination ("analytical values") and the statistics are biased if data values qualified with N, L, B, T, or H codes are present. Statistical estimates that are unbiased in this regard are given for all 422 samples at the end of table 3. The geometric mean is the antilogarithm of the arithmetic mean of the logs of the analyses and an estimate of "central tendency," or of a character­ istic value, of a frequency distribution that is approximately symmetrical on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an estimate of geo- chemical abundance. The geometric deviation is the antilogarithm of the standard deviation of the logs of the analyses. See U.S.G.S. Bulletin 1147-E, p. 20-23, for further discussion and explanation of geometric deviation.

Summary of Results

The stream sediment sampling program provided geochemical back­ ground information which will be useful in future exploration in this and nearby areas. As an aid in determining the geochemical background, statistical parameters for selected elements have been computed for each of six geologic units or combination of units that underlie most of the survey area (tables 4, 5). These parameters were determined by considering those samples from streams that drained only one particular geologic unit. In the interpretation of a geochemical result from any particular stream sediment sample, or group of samples, an examination of the geologic map in order to determine the geology of the drainage basin followed by inspection of tables 3, 4 and 5 is strongly recommended.

There is a wide range in background values depending on the bedrock of the drainage basin. Table 4 shows the geometric means of sediment analyses from the streams that drain a particular geologic unit or units. Copper, for example, shows a range in geometric mean from 5 ppm in streams draining only the Darby pluton to 55 ppm in streams draining the Devonian limestone and dolomite. The geometric mean of lead ranges from 16 ppm in the streams draining schistose marble to 72 ppm in streams draining the composite Kachauik pluton. Other elements show similar ranges and indicate the importance of considering the bedrock geology in interpreting the significance of any particular stream sediment analysis, or group of analyses.

Values were designated as anomalous in this report largely on the basis of the histograms in tables 3 and 5; it should be emphasized, however, that the stream sediment sampling was of a reconnaissance nature and the selection of anomalous values remains subjective and interpretive in our part.

The north end of the Darby Mountains is a strongly faulted area with numerous gossans and altered zones. Anomalous amounts of molybdenum, lead, zinc, and silver found in streams draining mineralized areas in and near Windy Creek and Granite Creek (samples 13-36, table 1) have already been reported in Miller and others (1971). Mapping in 1971 re­ sulted in the discovery of galena and sphalerite with minor chalcopyrite and rare fluorite in quartz-aplite breccia fillings in hornfelsed black slate northeast of the area at rock sample locality 1, fig. 1 and adjacent

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to the major fault bounding the south side of the Bendeleben Mountains. Although the examination was brief and much of the area is tundra- covered, mineralization was noted over an area of about 400 feet by 200 feet. Analyses of composite and selected grab samples from the area show anomalous lead, zinc, silver, and copper (samples 71 AGk282, table 2). Sediment samples (13 and 14) from streams draining the west side of the locality contain anomalous amounts of lead (150 ppm) and zinc (200 ppm).

Further east along the major fault mentioned above anomalous amounts of bismuth (more than 10,000 ppm) were reported in a small gossan in high grade metamorphic rocks (locality #2, fig. 1) and from a soil sample collected at a cold spring (locality#3, fig. 1). This general area at the north end of the Darby Mountains and near the range front fault appears to be a strongly mineralized area.

Numerous gossans and altered zones occur in the intrusive and metamorphic rocks of the eastern Bendeleben Mountains. They are generally narrow and of limited extent; analysis of grab samples (not shown in table 2) from some of these localities commonly showed weakly anomalous amounts of molybdenum (up to 100 ppm). Sainsbury and others (1969) reported a similar anomaly in the western Bendeleben Quadrangle and suggested the anomaly was related to either mineralization along faults or to a gneiss unit.

Sediment samples (50-87) from streams draining the Omilak mine and the Foster lead-silver prospect show expected high amounts of lead and zinc. Detailed discussions of the mine and prospect were contained in Herreid (1965) and Mulligan (1962) and they will not be discussed here. Numerous small gossans and altered zones occur in the area and many anomalous amounts of one or more of the following: lead, zinc, silver, copper, tin, arsenic, and antimony. Representative sampled localities are shown on fig. 1 and analyses are contained in table 2. Although these altered zones individually are of limited extent, they do indicate the area of mineralized rock surrounding the Omilak mine and Foster prospect.

Slightly anomalous amounts of tin and gold are reported from samples 48 and 49 from Otter Creek northeast of the Omilak-Foster area. Herreid (1965) reported tin anomalies in these and nearby streams and described an abandoned tin placer prospect on Otter Creek.

A small lead-zinc prospect occurs at the head of Dry Canyon Creek (fig. 1) near the contact between granite and feldspathic schist and marble. Sphalerite, galena, chalcopyrite, and pyrite were noted. A sediment sample (sample 121, table 1) from Dry Canyon Creek collected below the prospect contained expected anomalous amounts of lead and zinc. A sample (#130, fig. 1; table 1) from the head of the next creek to the south contains 150 ppm lead suggesting that the mineralized area may extend into the next drainage.

A placer gold mine (fig. 1) is located at Aggie Creek (mislabeled on published maps), a west-flowing tributary to Fish River. Lu and others (1968) report past production of $101,604, principally in the 1930 f s and 1940*s. Aggie Creek drains chiefly a schistose marble unit (labeled as p sm in Miller and others, 1972) cut locally by quartz latite porphyry. No obvious altered zones which might constitute a

Page 6: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

a bedrock source for the gold were noted in the schistose marble. East of Aggie Creek an altered quartz latite porphyry (loc. 14, fig. 1) contains anomalous amounts of gold and arsenic (sample 71 AGk266, table 2) and such altered intrusive rocks in the Aggie Creek might be the bedrock source. The Aggie Creek drainage also lies along the crest of a northwest-plunging anticline as shown by Miller and others (1972) and as indicated on aeromagnetic maps (State of Alaska, Div. of Geol. Survey, Aeromagnetic Survey maps, Solomon C-3, D-3) and mineralization may be related to this structure. A weak-to- moderate copper anomaly also occurs in this area as can be seen from histograms given for this unit in table 5. Histograms were computed for 62 samples collected from streams which drain only the schistose marble and the histogram for copper shows a distinct bi- modal distribution. When 22 samples from Aggie Creek and nearby drainages along the crest of the anticline were eliminated, most of the high copper values were eliminated as shown by a histogram of copper distribution without the Aggie Creek and nearby samples (table 5). The copper anomaly is distinct but not large as values are not over 100 ppm.

Anomalous amounts of niobium in the Clear Creek-Vulcan Creek area east of the Darby Mountains were noted by West (1953) who reported the occurrence of a uraniferous niobate mineral in heavy mineral fractions from pan concentrates. A moderate niobium anomaly also occurs in sediment samples from streams in this area as niobium values of 30- 70 ppm occur in several streams, particularly in the Clear Creek drainage. The 70 ppm values in samples 266 and 273 are the highest reported in approximately 2100 stream sediment samples collected from 6 different areas in western Alaska (this report; Miller, 1969; Elliott and Miller, 1969; Asher, 1969, 1970; Patton and Csejtey, 1970). The samples from the Clear Creek area also contain anomalous amounts of zirconium and lanthanum and weakly anomalous amounts of tin and molybdenum.

The bedrock source of the Clear Creek-Vulcan Creek anomaly is not known. The area is underlain by the Darby pluton, which is composed of coarse-grained leucocratic quartz monzonite. Semiquantitative spectrographic analyses of representative quartz monzonite samples show a niobium content of 10-30 ppm which is within the range shown by Parker and Fleischer (1968) for rocks of this composition. The distribution of anomalous niobium values in the Vulcan Creek area suggest possible mineralization along a faulted contact. In the Clear Creek area, however, the anomalous niobium occurs in streams that drain chiefly the interior of the pluton. West (1953) suggested that the association of topaz and a trace of cassiterite with the uraniferous niobate mineral in pan concentrates indicates a lode tin occurrence or pegmatitic phases in the granite. The recent regional geologic mapping in the area suggests several possibilities. Several distinct lineaments occur in the Clear Creek area and one or more of these may be mineralized. The association of anomalous elements found in the stream sediments is typical of late stage differentiates of granitic magma; pegmatites were not observed in the Darby pluton but

Page 7: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

aplite and alaskite dikes are common and may be the source of the anomalous elements. The Clear Creek area also marks the approximate contact between a hornblende-biotite quartz monzonite in the south and a hornblende-free biotite quartz monzonite in the north.

Although alkaline igneous rocks, commonly rich in niobium (Parker and Fleischer, 1968) occur in the southeastern Seward Peninsula (Miller, 1972; Miller and others, 1972), they are found west of the Darby Mountains and were not observed in any of the drainages discussed here. Also the alkaline rocks appear to be older than the quartz monzonite of the Darby pluton.

The Darby pluton also has high background values of uranium and thorium, which is particularly interesting in view of the uraniferous niobate minerals reported by West (1953). Three samples considered to be representative of the range in composition of the pluton showed a range of uranium content of 8.8 to 14.6 ppm and a 48.8 to 64.6 ppm range in thorium, according to gamma-ray spectrometric analysis (Carl M. Bunker, 1971, written com.). These values are similar to published averages of 15 ppm U and 56 ppm Th (Rodgers and Adams, 1969) for the thorium-and uranium-rich Conway granite of New Hampshire. The nearby Bendeleben pluton, in contrast, has a range of 1.8-4.4 ppm U and 16.9- 21.4 ppm Th which is similar to published values (Rodgers and Adams, 1969) of 4 ppm U and 18 ppm Th for average granite.

Relatively large amounts of Cu, Ni, Co, Cr, Mn, Fe, B, Sc, and V occur in sediments from streams that drain chiefly Devonian carbonate rocks east of the Darby Mountains as indicated by the high geometric means for these elements given in table 4. These elements are not typical of carbonate rocks and analyses of representative rock samples of limestone and dolomite from this unit show low values for all these elements. The high values of at least some of these elements may be due to the numerous dikes and plugs of diabase that intrude the strongly faulted carbonate rocks east of the Darby Mountains. Analyses of representative diabase show the expected high amounts of the above elements

Several minor prospects occur in the southeastern part of the survey area. A small copper prospect, first mentioned by Smith and Eakin (1911), occurs north of Carson Creek (loc. 15, fig. 1) northeast of Cape Darby where a malachite-stained area is exposed in the seacliff over an area of about 10 feet by 10 feet in quartz-biotite-feldspar schist. An analysis of a composite grab sample of mineralized schist is given in table 2 (sample 71 AMm609). Stibnite in quartz gangue was found in dump material around a small shaft north of Walla Walla Creek (loc. 16, fig. 1); this is probably the lode gold prospect mentioned in Smith and Eakin (1911, p. 129). An analysis of a composite grab sample of the richest material found (sample 71 AMm476, table 2) revealed the expected high antimony but no gold. The prospect is located in black siliceous-graphitic schist near the eastern border of the Darby pluton. A small gossan in limestone near the Kwiniuk River (loc.17, fig. 1) contains anomalous amounts of zinc, lead, copper, and barium (sample 70 AMml56, table 2).

Anomalous amounts of silver, arsenic, lead, and zinc were found in a highly altered 5-foot wide fault zone in granite on the west side of Cape Darby (loc. 18, fig. 1; sample 60 AMml35, table 2).

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References cited

Asher, R. R., 1969, Geological and geochemical study, SolomonC-5 quadrangle, Seward Peninsula, Alaska: Alaska Div. ofMines and Geology, Geologic Rept. No. 33, 65 p.

__________ 1970, Geology and geochemistry of the Belt Creek- Libby River area, Seward Peninsula, Alaska: Alaska Div. of Mines and Geology, Geochemical Rept. No. 22, 26 p.

Elliott, R. L., and Miller, T. P., 1969, Results of stream sediment sampling in the western Candle and southern Selawik quadrangles, Alaska: U.S. Geol. Survey open- file report, 61 p.

Herreid, G., 1965, Geology of the Omilak-Otter Creek area, Bendeleben quadrangle, Seward Peninsula, Alaska: Alaska Div. of Mines and Minerals, Geol. Rept., No. 11, 12 p.

Lu, F. C. J., Heiner, L. E., and Harris, D. P., 1968, Known and potential ore reserves, Seward Peninsula, Alaska: Univ. of Alaska, Mineral Ind. Res. Lab., Rept. 18, 107 p.

Mendenhall, W. C., 1901, A reconnaissance in the Norton Bay region, Alaska in 1900, pp. 181-222, in Brooks, A. H., Richardson, G. B., Collier, A. J., and Mendenhall, W. C., Reconnaissance in Cape Nome and Norton Bay regions, Alaska: Spec. Pub., U.S. Geol. Survey, 222 p.

Miller, T. P., 1969, Results of stream sediment sampling in thenorthern Melozitna, Hughes, and southern Shungnak quadrangles, west-central Alaska: U.S. Geol. Survey open-file report, 53 p.

__________ 1972, Potassium-rich alkaline intrusive rocks ofwestern Alaska: Geol. Soc. America Bull. v. 83, p. 2111-2128.

Miller, T. P., Elliott, R. L., Grybeck, D., and Hudson, T., 1971,Results of geochemical sampling in the northern Darby Mountains, Seward Peninsula, Alaska: U.S. Geol. Survey open-file report, p. 12

Miller, T. P., Grybeck, D., Elliott, R. L., and Hudson, T., 1972,Preliminary geologic map of the eastern Solomon and southeastern Bendeleben quadrangles, Eastern Seward Peninsula, Alaska: U.S. Geol. Survey open-file report.

Mulligan, J. H., 1962, Lead-silver deposits in the Omilak area, Seward Peninsula, Alaska: U.S. Bureau of Mines Rept. of Inv. 6018, 44 p.

Parker, R. L., and Fleischer, M., 1968, Geochemistry of niobium and tantalum: U.S. Geol. Survey Prof. Paper 612, 43 p.

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Patton, W. W., Jr., and Csejtey, B., Jr., 1972, Analyses of stream- sediment and rock samples from St. Lawrence Island, Alaska: 1966-1971: U.S. Geol. Survey open-file report, 78 p.

Rodgers, J. J. W., and Adams, J. A. S., 1969, Handbook of geochemistry Vol. II, Chap. 90 and 92, K. H. Wedepohl, Editor, Springer- Verlag Berlin.

Sainsbury, C. L., Kachadoorian, R., Hudson, T., Smith, T. E., Richards, T. R., and Todd, W. E., 1969, Reconnaissance geologic maps and sample data, Teller A-l, A-2, A-3, B-l, B-2, B-3, C-l, and Bendeleben A-6, B-6, C-6, D-5, D-6 quadrangles, Seward Peninsula, Alaska: U.S. Geol. Survey open-file report, 49 p.

Smith, P. S., and Eakin, H. M., 1911, A geologic reconnaissance in southeastern Seward Peninsula and the Norton Bay-Nulato region, Alaska: U.S. Geol. Survey Bull. 449, 146 p.

West, W. S., 1953, Reconnaissance for radioactive deposits in the Darby Mountains, Seward Peninsula, Alaska, 1948: U.S. Geol. Survey Circular 300, 7 p.

Page 10: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

Table

1.

Anal

yses

of st

ream

se

dime

nt sa

mple

s fr

om southeastern Bendeleben and

east

ern

Solo

mon

quadrangles, Al

aska

.

SAMPLE

AGN251

AG^TOl

AGN250

AGM700

AGN702

AGN703

AGN704

AGN705

AGN253

AGN707

AGNZ5.2

AGN706

PAM162

B_AM

161

BAM164

BAM163

BAM166

BAM165

BAM167

BAM 168

BAM169

8AM160

JJAM

159

BAM063

BAM062

BAM065

BAM064

8AM066

BAM061

BAM060

BAM172

BAM173

BAM067

BAM066

BAM170

BAM171

BAM074

BAM075

BAM069

BAM070

BAM071

BAM072

BAM073

BAM076

BAM077

BAM078

BAM079

BAMOBC

BAM08I

BAM106

l.OOCO

2.0000

3.00CO

4.QOCG

5.0000

6.0000

7.000C

8.0000

9.0000

10.0000

11.0000

12.0000

13.0000

14.0000

15.0000

16.000C

17.0000

18.00CO

19.0000

20.0000

21.0000

22.0000

23.0000

24.0000

25.0000

26.0000

27.0000

28.0000

29.0000

30.0000

31.0000

32.0000

33.0000

34.0000

35.0000

36.0000

37.0005

38.0006

39.000C

40.0000

41.0000

42.0000

43.0000

44.0000

45.0000

46.0000

47.0000

48.0000

49.0000

50.0000

S-FE

(5.000C

5.0000

b.QOOO

3.GOCC

5.0000

15.00CO

15.UOOO

10.0000

5.0000

5.0000

3.0000

10.0000

7.0000

7.0000

3.000C

3.0000

3.0000

7.0000

3.000C

3.0000

10.0000

7.0000

3.0000

3.0000

10.0000

15.0000

3.000C

7.0000

7.0000

10.0000

10.0000

7.0000

15.0000

10.000C

7.0000

15.0000

10.0000

7.0000

15.0000

10.0000

15.0000

1G.OOOO

10.0000

7.0000

7.0000

7.0000

1C. 0000

10.0000

10.0000

15.0000

S-MG

(1.0000

1.5000

1.5000

2.0000

3.0000

3.0000

2.0000

2.00CO

1.5000

2.0000

1.5000

2.0000

1.5000

1.0000

0.7003

0.7000

0.5000

0.7000

0.7000

0.5000

1.5000

0.7000

0.7000

0.7000

1.0000

3.0000

0.7000

1.5000

l.OOOC

1.5000

2.0000

2.0000

1.5000

1.5000

1.5000

3.0000

3.0000

2.0000

5.0000

3.0000

5.0000

3.0000

3.0000

2.0000

3.0000

2.0000

1.5000

1.5000

2.0000

3.0000

S-CA

(0.7000

3.0000

1.5000

5.0000

10.0000

5.0000

2.0000

2.0000

2.0000

2.0000

3.0000

3.0000

1.5000

1.0000

0.7000

0.7000

0.5000

0.7000

0.5000

0.7000

1.0000

0.3000

0.5000

0.7000

1.0000

1.5000

0.7000

1.5000

0.7000

1.5000

1.5000

2.0000

1.0000

1.5000

2.0000

2.0000

3.0000

1.5000

3.0000

3.0000

5.0000

2.0000

1.5000

1.5000

3.0000

1.5000

1.5000

1.0000

1.5000

3.0000

S-TI

(0.3000

0.5000

0.2000

G.2000

0.3000

0.7000

0.7000

0.5000

0.3000

0.5000

0.2000

0.5000

0.5000

0.7000

0.3000

0.3000

0.3000

0.7000

0.3000

0.300Q

0.7000

0.3000

0.5000

0.3000

1.0000

I. 0000

0.3000

1.0000

0.7000

1.0000

1.0000

0.5000

1.0000

0.7000

0.7000

1.0000

1.0000

1.0000

l.OOOOG

1.0000

l.OOOOG

1.0003

1.0000

1.0000

1.0000

0.5000

l.OOOOG

1.0000

1.0000

1.0000

S-MN

500.0000

700.0000

500.0000

500.0000

700.0000

1000.0000

700.0000

1000.0000

1000.0000

700.0000

SCO. 0000

7CO.OOOO

150C.OOOO

2000.0000

700.0000

5000.0000G

700.0000

1000.0000

700.0000

700.0000

2000.0000

1500.0000

700.0000

700.0000

1500.0000

2000.0000

700.0000

1500.0000

700.0000

1500.0000

1000.0000

1000.0000

1500.0000

1500.0000

20CO.OOOO

1000. OCOO

1000.0000

700.0000

2000.0000

2000.0000

2000.0000

700.0000

700.0000

700.0000

700.0000

1500.0000

3000.0000

1500.0000

2000.0000

700.0000

S AG

0.5000N

0.5000N

0.5000N

0.50COL

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5COON

0.5000N

0.5000N

0.5000N

0.5000L

0.5000

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Page 20: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

Map

No.

101

102

103

104

105

106

107

108

109

110

111

112

113

114

115

116

117

118

119

120

121

122

123

124

125

126

127

128

129

130

131

132

133

134

135

136

137

138

139

140

141

142

143

144

145

146

147

148

149

150

S-NI

30.0000

70.0000

30.0000

30.0000

50.0000

70.0000

70.0000

70.0000

30.00CO

30.0000

70.0000

30.0000

30.0000

30.0000

30.0000

50.0000

30.0000

50.0000

30.0000

50.0000

50.0000

50.0000

50.0000

20.0000

50.0000

30.0000

30.0000

30.0000

50.0000

30.0000

50.0000

50.0000

70.0000

50.0000

50.0000

70.000D

50.0000

70.0000

7.0000

30.0000

10.0000

50.0000

50.0000

50.0000

20.0000

30.0000

30.0000

50.0000

30.0000

30.0000

S-PB

30.00CC

30.0000

20.0000

30.0000

20.0300

50.000C

30.0000

30.00CC

15.COOC

50.0000

30.00CC

30.0000

30.0000

30.0000

50.000C

70.000C

15.0000

70.0000

30.0000

50.0000

200.0000

70.0000

70.0000

20.0000

70.000C

50.0000

30.0000

70.0000

30.0000

150.0CCC

50.003C

30.0000

30.0000

70.0000

30.0000

70.0000

50.00CO

20.0000

70.0000

3C.OOOC

3C.OOOC

70. COCO

7C.OOOO

50.000C

20.0QOC

30.0000

7C.OOOO

7C.OOOC

70.003C

70.COOC

S-SB

100.

OOOON

100. OOOON

1CO.GOOCN

ICC. OOOON

ICO.

OOOON

130.0003N

100. OOOON

100. OOOON

100. OOOON

100. OOOON

100. OOOON

100. OOOON

100.

OOOON

100. OOOON

1CO.COOON

1GO.OOOCN

100. OOOON

100. OOOON

100.

OOOON

100. OOOON

100. OOOON

100. OOOON

100.

OOOON

100. OOOON

IOO.OOOCN

100. OOOON

1DO.OCOGN

1DC.OGOON

100.

OOOON

100. OOOON

100. OOOON

100.

OOOON

100. OOOON

100. OOOON

10G. OOOON

100. OOOON

100. OOOON

100. OOOON

100. OOOON

100.000DN

100.000CN

100. OOOON

100. 000 3N

100.300CN

100.

OOOON

100.0003N

100.COC2N

100. OOOON

100. OOCQN

100. OOOON

s-sc

30.0000

20.0000

20.0000

15.0000

15.0000

15.0000

15.0000

15.0000

70.0000

10.0000

15.0000

2C.OOOO

3C.CGOG

20.0000

15.0000

15.0000

20.0000

15.0000

50.0000

10.0000

15.0000

15.0000

15.0000

20.0000

30.0000

15.0000

15.0000

15.0000

10.0000

20.0000

20.0000

20.0000

20.0000

20.0000

20.0000

20. DODO

20.0000

2C.OOOO

10.0000

10.0000

7.0000

15.0000

10.0000

15.3000

15.0000

30.0000

15.0000

15.0000

15.0000

10.0000

S-SN

10. .O

OOON

10. OOOON

10. OOOON

10.0COON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

1C. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10.0000N

10.0000

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

15.0000

30.0000

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10.0000L

10.0000

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10.COOON

10.0000L

10. OOOON

10.COOON

10.0003

10. OOOON

10. OOOON

10.0003L

1C. OOOON

10. OOOON

15.0000

15.0000

10.0000L

S-SR

150.0000

150.0000

500.0000

300.COOO

500.0000

150.0000

700.0000

150.0000

500.0000

150.0000

300.0000

100.0000

150.0000

100.0000

300.0000

150.0000

150.0000

300.0000

200.0000

150.0000

200.0000

150.0000

150.0000

150.0000

150.0000

150.0000

100.0000

300.0000

200.0000

15C.OOOO

200.0000

500.0000

500.0000

300.0000

500.0000

300.0000

500.0000

500.0000

150.0000

150.0000

200.0COO

200.0000

3CO.OOOO

3CO.OOOO

200.0000

300.0000

300.0000

500.0000

500.0000

SCO. 0000

s-v

150.0000

150.0000

100.000C

150.0000

150.0000

150.0000

150.00CO

150.0000

100.0000

100.0000

150.0000

150.0000

100.0000

150.0000

150.0000

150.0000

150.0000

150.0000

100.0000

70.0000

150.0000

150.0000

150.0000

100.0000

150.0000

100.0000

100.0000

100.0000

100.0003

150.0000

150.0000

150.0000

150.0000

150.0000

150.0000

150.0COO

150.0000

150.0000

70.0000

100.0000

70.0000

150.0000

150.0000

100.0000

100.0000

150.0000

100.0000

150.0000

150.0000

100.0000

s-w

50. OOOON

50. OOOON

50. OOOON

50.000CN

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50.0003N

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50.0003N

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

50. OOOON

S-Y

70.0000

30.0000

30.0003

30.0000

33.0000

30.0000

30.0000

30.0000

30.0000

IS. 0000

30.0000

50.0000

70.0000

50.0000

50.0000

30.0000

50.0000

20.0000

33.0000

20.0000

30.0000

30.0000

30.0000

70.0000

50.0000

30.0000

30.0000

30.0000

20.0000

30.0000

30.0000

30.0000

30.0000

30.0000

30.0000

30.0000

30.0000

30.0000

15.0000

70.0000

20.0000

30.0003

15.0000

50.0000

20.0000

150.0000

20.0000

70.0000

100.0000

30.0000

S-ZN

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

203.0000L

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

300.0000

200. OOOON

200.0000L

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

203. OOOON

200. OOOON

200.

OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

200. OOOON

Page 21: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

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Page 22: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

SAMPLE

BAM494

BAM493

BAM491

BAM492

BAM489

BAM490

BAM486

BAM485

BAM488

BAM487

BAM378

BAM379

BAM380

BAM484

BAM483

BAM176

BAM270

BAM269

BAM267

BAM268

BAM265

BAM266

BAM253

BAM254

BAM252

BAM251

BAM255

BAM256

BAH258

BAM257

BAM259

BAM260

BAM261

BAM262

BAM263

BAM264

BAM370

BAM371

BAM373

BAM372

BAM374

BAM375

BAM376

BAM377

BAM364

BAM271

BAM366

BAM365

BAM367

BAM368

151.0000

152.0000

153.0000

154.0000

155.0000

156.0000

157.0000

158.0000

159.0000

160.0000

161.0000

162.0000

163.QCOO

164.0000

165.0000

166.0000

167.0000

168.0000

169.0000

170.0000

171.0000

172.0000

173.0000

174.0000

175.0000

176.0000

177.0000

178.0000

179.0000

180.0000

181.0000

182.0000

183.0000

184.0000

185.0000

186.0000

187.0000

188.0000

189.0000

190.0000

191.0000

192.0000

193.0000

194.0000

195.0000

196.0000

197.0000

198.0000

199.0000

200.0000

S-FE

(5.0000

7.000C

7. DODO

7.0000

7.0000

5.0000

3.0000

7.0000

7.0000

7.0000

10.0000

7.0000

7.00CC

5.0000

5.000C

10.0000

7.0000

10.0000

7.0COC

7.0000

10.0000

7.000C

5.0000

7.0000

5.0000

7.0000

5.0000

5.0000

3.0000

5.0000

3.0000

5.0000

7.0000

7.00CO

7.0000

7.000C

7.0000

7.0000

5.0000

7.00CG

5.000C

7.0000

1C. 0000

7.0000

5.0000

5.0000

5.0000

7.0000

7.0000

5.0000

S-MS

(2.0000

2.0000

1.5000

3.0000

2.000 >

2.0000

1.5000

2.0000

2.0000

2.0000

2.0000

1.5000

3.000C

3.0000

P.OOOO

3.0000

3.0000

2.000C

3.0000

3.0000

2.000C

3.0000

2.0000

3.0000

3.0000

2.0000

2.0000

3.0000

5.0000

3.0000

5.0000

5.0000

5.0000

5.0000

5.0000

3.0000

3.0000

3.0000

2.0000

3.0000

2.0000

3.0000

2.0000

2.0000

3.0000

3.0000

3.0000

1.5000

2.0000

2.0000

S-CA

(1.5000

2.0000

1.5000

3.0000

5.0COO

1.5000

1.0000

5.0000

3.0000

2.0000

3.0000

3.0000

2.0000

5.0000

1.5000

5.0000

3.0000

3.0000

3.0000

3.0000

3.0000

0.7000

1.0000

0.7000

1.0000

1.5000

1.5000

1.5000

2.0000

3.0000

5.0000

3.0000

5.0000

5.0000

7.0000

3.0000

0.2000

1.5000

1.0000

1.0000

l.COOO

1.5000

2.0000

7.0000

0.5000

2.0000

3.0000

1.0000

0.5000

7.0000

S-TI

(0.5003

0.70CO

0.7000

0.7000

0.7000

0.3000

0.3000

0.7000

0.7000

0.7000

0.7000

0.7000

0.7GDO

0.3000

0.3000

0.7000

0.7000

0.7000

0.7000

0.7000

0.7000

0.7000

0.7000

0.5000

0.5000

0.5000

0.3000

0.7000

0.5000

0.5000

0.3000

C.3000

0.7000

0.7000

0.7000

0.7000

0.7000

0.3000

0.5000

0.5000

0.3000

0.7000

0.5000

0.3000

0.7000

0.5000

0.3000

0.7000

0.7000

0.3000

S-MN

700.0000

10CO.OOOO

1000.0000

1000.0000

1000.0000

700.0000

500.0000

1000.0000

1000.0000

1000.0000

1500.0000

1000.0000

1500.0000

700.0000

1000.0000

1500.0000

1500.0000

2000.0000

3000.0000

15CO.OOOO

1500.0000

1500.0000

7CO.OOOO

700.0000

500.0000

700.0000

700.0000

700.0000

700.0000

700.0000

2000.0000

1000.0000

700.0000

1000.0000

1500.0000

700.0000

150.0000

1000.0000

700.0000

1000.0000

500.0000

1000.0000

700.0000

1500.0000

1500.0000

700.0000

700.0000

1500.0000

2000.0000

1000.0000

S-AG

0.5000N

0.5000N

0.5000N

G.5000N

0.500JN

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.50CON

0.5000N

0.5COON

0.5000N

0.5000N

0.50C3N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.50CON

0.500QN

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.50GON

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.5000N

0.500QN

0.5000N

0.5 00 OK

S-AS

200.0000N

?OO.OOODN

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

203.0000N

200.0000N

200.0000N

200.0000N

20C.OOOON

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

ZOO.OOOON

200.0000N

200.0000N

200.0000N

200.0000N

2Q0.0030N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

200.0000N

S-AU

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

10.0003N

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

iO.OOOON

iO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOQN

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

IO.OOOON

10.0003N

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IO.OOOON

13.0000N

10.0303N

IO.OOOON

IO.OOOON

10.0003N

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iO.OOOON

IO.OOOON

IO.OOOON

10.0003N

S-B

30.0000

20.0300

15.0000

20.0000

30.0000

15.0030

30.0000

70.0000

50.0000

50.0000

150.0000

100.0000

50.0000

100.0000

100.0003

70.0000

30.0000

150.0000

30.0000

30.0000

100.0000

70.0000

70.0000

100.0000

70.0000

50.0000

30.0033

70.0000

100.0000

30.0000

30.0000

100.0000

150.0000

100.0000

100.0000

103.0000

50.0000

50.0000

30.0030

70.0000

50.0000

100.0003

50.0000

30.0000

50.0000

30.0000

20.0000

70.0000

70.0000

100.0000

Page 23: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

Map

No.

151

152

153

154

155

156

157

158

159

160

161

162

163

164

165

166

167

168

169

170

171

172

173

174

175

176

177

178

179

180

181

182

183

ISA

185

186

187

188

189

190

191

192

193

194

195

196

197

199

200

S-BA

700.0000

1500.0000

1000.0000

2000.0003

1000.0000

1500.0000

1000.0000

1000.0000

1500.0000

1503.0000

700.0000

1000.0000

700.000D

700.0000

700.0000

300.0000

700.0000

1000.0000

700.0000

700.0000

1000.0000

700.000C

730.0000

300.0000

3CO.OOOO

300.0000

700.0000

700.0000

700.0000

500.0000

700.0000

500.0000

500.0000

700.0000

700.0000

500.0000

150.0000

200.0000

150.0000

300.0000

150.0000

700.0000

700.0000

3CO.OOOO

150.0000

200.0000

150.0000

700.0000

700.0000

5.:-0.0003

S-BE

2.000C

2.0000

3.000C

3.0000

2.0000

2.0000

2.0000

3.0000

3.0000

2.0000

3.0000

3.0000

2.0000

1.5000

1.5000

3.0000

3.0000

3.0000

2.00CC

3.0000

3.0000

3.000C

1.5000

1.5000

1.5000

1.0000

1.5000

1.5000

2.0000

1.5000

1.5000

1.5000

1.0000

1.0000

1.0000

1.0000

1. OOOOL

1.0000

1.0000

1.0000

1.0000

1.5000

1.5000

1.0000

1.0000

1.0000

1.0000

2.0000

1.5000

1.5000

S-BI

10. OOOON

10. OOOON

10. OOOON

lO.OOOoN

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

1C. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

1C. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

10. OOOON

1C.OOOCN

10. OOOON

10. OOOON

1C. OOOON

10. OOOON

10. OOOON

S-CD

20.0COON

20. OOOON

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Page 42: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

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Page 43: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

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Page 44: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

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Page 45: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

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Page 46: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

Table

2.

Anal

yses

of ro

ck samples

from southeastern

Bend

eleb

en and

eastern

Solo

mon

Quad

rang

le,

Alaska.

(Gol

d an

alys

is by

at

omic

absorption;

all

othe

rs by

semiquantitative spectrographic analysis.)

Results

reported in pa

rts

per million

(ppm); lo

wer

limi

ts of de

tect

ion

for

each

el

emen

t gi

ven

in text.

Loca

lity

No

.

1 2 3 4 5 6 7 8 9

10 11 12 13 14 15 16 17 18

Samp

le

No.

71AG

k282

A

71AGk282B

71AG

k282

C

71AGk282D

68AMm293

68AMm292

70AH

202A

71AMm495

70AH208

70AG

k2

70AG

kl8

70AG

kl9

70AG

k26

70AG

k29

70AH

235

70AH

238

7lAGk266

71AMni609

71AM

m476

A

70AMml56

69AM

ml35

AK 0.5

3

30 50 N L 0.7

70 3 L 15

3 1.5

0.7

N N N 15

3 1

50

As N N N N L L N

2000

3000

7000 N N N N N

700

2000 N N N

30,000

Au .02

.04

0.1 N N N N

0.1 N N N N N N N N .35

.15 N N -

Bi N N 15 30

G(10,000)

G(10

,000

) N N N N N N N N N N 15 15 N N N

Cu 30

300 70

1500 10 100

150

200

200

700 50 150 5

10 10

7 L

20,0

00 15 500 7

Mo 15 15 N 10 7 L 70 15 70 70 L 5 N N N N N

700 N 5 N

Pb

300

3000

GC20.000)

G(20

,000

)

50 20 300

G(20,000)

1500

3000

3000

1000 700

7000 700

500 50 70 15 300

500

Sb N N N N N N N

700 N

10,000

7000 L N

200 N N N N

G (10, 000) N N

Sn N N N L N7 N N

500 N N N N N N N N L N N N 30

Zn 700

2000

G (10, 000

)

G(10

,000

) N N

300

7000

G(10,000)

10,0

00 L N N N L

200 N N N

G(10,000)

500

Rema

rks

Comp

osit

e gr

ab sa

mple

of

mineralized

brec

cia.

Composite

grab

sa

mple

of

mineralized

brec

cia.

Selected gr

ab sample of

aplitic

material wi

thap

prox

. 5% galena-

spha

leri

te.

Selected gr

ab sample of

aplitic

mate

rial

with

diss

emin

ated

ga

lena

.Grab sa

mple

fr

om go

ssan

in

schi

st.

Soil sa

mple

fr

om co

ld sp

ring

area.

Grab

sa

mple

fr

om a

lter

edbl

ack

slat

e.Co

mpos

ite

grab

sample from

small

iron

-sta

ined

carbonate

zone

.Grab sa

mple

of go

ssan

in

calcareous met

ased

imen

tary

rock

.Grab sample from g

ossan

atco

ntac

t between

schist and

marble .

Grab

sa

mple

from a

lter

edbi

otit

e-fe

ldsp

ar sc

hist

.Gr

ab sample from a

lter

edquartz-biotite sc

hist

.Gr

ab sa

mple

fr

om al

tere

dmarble.

Grab

sa

mple

from al

tere

dma

rble

.Grab sample from gossan in

marble.

Grab

sa

mple

from go

ssan

in

marble.

Grab

sa

nple

of altered

quar

tz la

tite

di

ke.

Grab

sa

mple

of copper-

stained

schi

st.

Grab

sa

mple

of

stibnite in

quar

tz .

Grab

sa

mple

fr

om small

goss

anin limestone; contains greater

than

5,000

ppm

Ba.

Grab

sa

mple

fr

om hi

ghly

alte

red

gran

ite;

abundant

arsenopyrite.

Page 47: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

Table

3.

FREQUENCY TABLE FOR COLUMN

Fre

quen

cy dis

trib

uti

on

s an

d his

togra

ms

of

all

an

alyse

s o

f st

ream

se

dim

ent

sam

ples

fr

om so

uth

east

ern

Ben

dele

ben

and

east

ern

So

lom

on

qu

adra

ng

les,

A

lask

a.

2 IS

-FE

()

LIMITS

FREQ

LOWER -

UPPER

3.8E-02 -

5.6E-02 -

8.3E-02 -

1.2E-01 -

1.8E-01 -

2.6E-01 -

3.8E-01 -

5.6E-01 -

8.3E-01 -

1.2E 00 -

1.8E 00 -

2.6E 00 -

3.8E 00

-

5.6E 00 -

8.3E 00 -

L.2E 01

-

U8E 01

-

5.6E-02

8.3E-02

1.2E-01

1.8E-01

2.6E-01

3.8E-01

5.6E-01

8.3E-M

1.2E 00

1.8E GO

2.6E 00

3.8E "3

5.6E 00

8.3E OG

1.2E Oi

1.8E 01

2.6E 01

0 I 0 0 0 0 0 0 0 6 6M

104

157

74

291

FREO

CUM 0 1 1 1 I 1 1 1 1 7

13 5716

131

8392

421

422

PERCENT

FREQ

0.0

0.24

0.0

0.0

0.0

0.0

0.0

0.0

0.0

1.4?

1.42

10.43

24.64

37.20

17.54

6.87

0.24

PERCENT

FREQ CUM

0.0

0.24

0.24

0.24

0.24

0.24

0.24

0.24

0.24

1.66

3.08

13.51

38.15

75.36

92.89

99.76

100.00

HISTOGRAM FOR COLUMN

2 (S-FE

1.5E 00 X

2.0E 00 X

3.0E 00 XXXXXXXXXX

5.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXX

7.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 01

XXXXXXXXXXXXXXXXXX

1.5E 01 XXXXXXX

2.0E 01

N 00.0

L 00.0

T 00.0

ANALYTICAL

G VALUES

0 422

0.0

MA

XIM

UM

=

2.0

0000E

0

1

MIN

IMU

M

= 7.0

0000E

-02

GE

OM

ET

RIC

M

EA

N

=

6.3

0489E

00

GE

OM

ET

RIC

D

EV

IAT

ION

=

1.6

71

45

E

00

Page 48: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

3 (S-MG

()

LIMITS

LOWER -

UPPER

1.8E-02 -

2.6E-02

2.6E-02 -

3.8E-02

3.8E-02 -

5.6E-A2

5.6E-02 -

8.3E-02

8.3E-02 -

1.2E-01

1.2E-01 -

1.8E-01

1.8E-01 -

2.6E-01

2.6E-01 -

3.8E-01

3.8E-01 -

5.6E-01

5.6E-01 -

8.3E-01

8.3E-01 -

i.2E 00

1.2E 00 -

1.8E 00

1.8E 00 -

2.6E 00

2.6E 00 -

3.8E 00

3.8E 00 -

5.6E 00

5.6E 00 -

8.3E 00

8.3E 00 -

1.2E 01

HISTOGRAM FOR COLUMN

2.0E-01 X

3.0E-01 X

5.0E-01 XX

7.0E-01 XXXXXX

l.OE 00

XXXX

FREQ

FREQ

PERCENT

CUM

0 0

0 0

0 C

0 C/

0 0

0 C

3 3

5 8

8 16

26

42

17

5991

151

118

268

98

366

23

389

26

415

5 420

3 (S-MG

()

FREQ

0.0

:.o

0.0

0.0

0.0

0.0

0.71

1.18

1.9C

6.16

4.03

21.56

27.96

23.22

5.45

6.16

1.18

PERCENT

FREQ CUM

0.0

0.0

0.0

0.0

0.0

0.0

0.71

1.90

3.79

9.95

13.98

35.55

63.51

86.73

92.18

98.34

99.53

1.5E 00 XXXXXXXXXXXXXXXXXXXXXX

2.0E 00

XXXXXXXXXXXXXXXXXXXXXXXXXXXX

3.0E 00 XXXXXXXXXXXXXXXXXXXXXXX

5.0E 00

XXXXX

7.0E 00 XXXXXX

i.CE 01 X

N 00.0

L 0 0.0

T 00.0

ANALYTICAL

G VALUES

2 420

0.47

MAXIMUM =

l.OOOOOE 01

MINIMUM =

2.00000E-01

GEOMETRIC MEAN =

2.04177E 00

GEOMETRIC DEVIATION =

1.93515E 00

Page 49: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

4 (S-CA

LIMITS

LOWER -

UPPER

3.8E-02 -

5.6E-02

5.6E-02 -

8.3E-02

8.3E-02 -

1.2E-G1

1.2E-01 -

1.8E-01

1.8E-01 -

2.6E-01

2.6E-01 -

3.8E-01

3.8E-01 -

5.6E-01

5.6E-01 -

8.3E-01

8. 1. 1. 2. 3. 5. 8. 1. L.

3E-01 -

2E 8E 6E 8E 6E 3E 2E 8E

00 -

00 -

00 -

00 -

00 -

00 -

01 -

01 -

HISTOGRAM FOR

N 00.

3 5 7 I 1 2 3 5 7 I I 2 0

.OE-01

.OE-01

.OE-01

.OE

.5E

.OE

.OE

.OE

.OE

.OE

.5E

.OE

00 00 00 00

00

00 01 01 01

1.2E

1.8E

2.6E

3.8E

5.6E

8.3E

1.2E

1.8E

2.6E

COLUMN

XX XXX

00 GO 00 00 00 00 01 01 01

FREQ

FREQ

PERCENT

PERCENT

CUM

FREQ

FREQ CUM

0 0

O.C

0.0

0 0

0.0

O.G

0 0

O.C

0.0

0 0

0.0

O.C

2 2

0.47

0.47

10

12

2.37

2.84

13

25

3.08

5.92

52

77

12.32

18.25

53

130

12.56

105

235

24.88

64

299

15.17

61

36C

14.45

19

379

4.50

9 38

8 2.13

7 395

1.66

5 4CO

1.18

5 405

1.18

4. (S-CA

()

30.81

55.69

70.85

85.31

89.81

91.94

93.60

94.79

95.97

XXXXXXXXXXXX

XXXXXXXXXXXXX

XXXXXXXXXXXXXXXXXXXXXXXXX

xxxxxxxxxxxxxxx

xxxxxxxxxxxxxx

xxxx

xXX XX X X

L 00.0

H B

T000

0.0

G17 4.03

ANALYTICAL

VALUES

405

MAXIMUM =

2.00000E 01

MINIMUM =

2.00000E-01

GEOMETRIC MEAN =

1.65426E 30

GEOMETRIC DEVIATION =

2.20808f 00

Page 50: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

(S-TI

LIMITS

LOWER

5.6E-03

8.3E-03

1.2E-02

1.8E-02

2.6E-02

3.8E-02

5.6E-02

8.3E-02

1.2E-01

1.8E-01

2.6E-01

3.8E-01

5.6E-01

8.3E-01

FREQ

- UPPER

- - - - - - - - - - - - - -

8.3E-03

1.2E-02

1.8E-02

2.6E-02

3.8E-02

5.6E-02

8.3E-02

1.2E-01

1.8E-01

2.6E-01

3.8E-01

5.6E-01

8.3E-01

1.2E 00

0 0 0 0 1 0 8 2 71278

97

15754

FREO

CUM c 0 0 G 1 1 9

11 18 30

108

205

362

416

PERCENT

FREQ

0.0

0.0

0.0

0.0

0.24

0.0

1.90

0.47

1.66

2.84

18.48

22.99

37.20

12.80

PERCENT

FREQ CUM

0.0

0.0

0.0

0.0

0.24

0.24

2.13

2.61

4.27

7.11

25.59

48.58

85.78

98.58

HISTOGRAM FOR COLUMN

5 (S-TI

7.0E-0? XX

l.OE-01

1.5E-01 XX

2.0E-01 XXX

3.0E-01 XXXXXXXXXXXXXXXXXX

5.0E-01 XXXXXXXXXXXXXXXXXXXXXXX

7.0E-C1 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 00 XXXXXXXXXXXXX

N 00.0

L 00.0

T 00.0

ANALYTICAL

G

VALUES

6 416

1.42

MAXIMUM =

l.OOOOOE OC

MINIMUM

= 3.oooooE-o2

GEOMETRIC MEAN =

5.11221E-01

GEOMETRIC DEVIATION =

1.74297E 00

Page 51: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

6 (S-MN

LIMITS

FREQ

LOWER -

UPPER

8 1 1 2 3 5 8 1 1 2 3 5 8 1 1 2 3

.3E

.2E

.8E

.6E

.8E

.6E

.3E

.2E

.8E

.6E

.8E

.6E

.3E

.2E

.8E

. 6E

.8E

00 -

01 -

01 -

01 -

01 -

01 -

01 -

02 -

02 -

02 -

02 -

02 -

02 -

03 -

03 -

03 -

03 -

1. 1. 2. 3. 5. 8. 1. 1. 2. 3. 5. 8. 1. 1. 2. 3. 5.

2E 8E 6E BE 6E 3E 2E 8E 6E 8E 6E 3E 2E 8E 6E 8E 6E

01 01 01 01 01 01 02 02

0202 02 02 03

03 0303

03

0 0 0 0 0 0 1 1 110 20

133

111

111 257 1

FREQ

CUM C 0 0 0 0 0 1 2 3

13 33166

277

388

413

420

421

PERCENT

FREQ

0. 0. 0. 0. 0. 0. 0. 0. 0. 2. 4.31

.26.

26. 5. 1. 0.

r* w 0 0 0 0 0 24

24 24 37 74 52 30 30 92

66 24

PERCENT

FREQ0 0 0 0 0 0 0 0 0 3 739 65

91 979999

CUM

.0 .0 .0 .0 .0 .0 .24

.47

.71

.08

.82

.34

.64

.94

.87

.53

.76

HISTOGRAM FOR COLUMN

6 (S-MN

3.0E 02 XX

5.0E 02 XXXXX

7.0E 02 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 03 XXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 03 XXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 03 XXXXXX

3.0E 03 XX

5.0E 03

N 00.0

L 00.0

T 00.0

ANALYTICAL

G

VALUES

1 421

C.24

MAXIMUM =

5.00000E 03

MINIMUM =

l.OOOOOE 02

GEOMETRIC MEAN =

9.82181E 02

GEOMETRIC DEVIATION =

1.60595E 00

Page 52: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

7 (S-AG

LIMITS

LOWER -

UPPER

3.8E-01 -

5.6E-01

5.6E-01 -

8.3E-01

8.3E-01 -

1.2E 00

1.2E 00 -

1.8E 00

EQ 4 3 0

FREQ

CUM

4 7 7

PERCENT

FREQ

0.95

3.71

0.0

PERCENT

FREQ CUM

0.95

1.66

1.66

0.24

1.90

HISTOGRAM FOR COLUMN

5.0E-01 X

7.CE-01 X

l.OE 00

1.5E 00

7 (S-AG

N403

95.50

L LI

2.61

T 00.0

ANALYTICAL

G

VALUES

0 8

0.0

MAXIMUM =

1.50000E 00

MINIMUM =

5.00000E-01

GEOMETRIC MEAN *

6.50742E-01

GEOMETRIC DEVIATION =

1.45686E 00

Page 53: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

1. (S-3

LIMITS

FRF'-J

LOWER -

JPPER

3. 1. 1. 2. 3. 5. 8. 1. 1. 2. 3. 5.

3E 2E8E6E 8E

6E 3E2E

8E6E

8E6E

OJ-

-01 -

01 -

01 -

01 -

01 -

01 -

02 -

02 -

02 -

02 -

02 -

1. 1. 2. 3. 5. 8. 1. 1. 2. 3. 5. 8.

2E

bE6E8E6£ 3E

2E

8E

6£8E

6E 3E

Cl 31 :i 01 Cl 01

02 C2C2

02

02 02

40

41 34

5744 55

55 48 18 2 0 1

FR6Q

CUM

4C ril

115

172

216

271

326

374

392

394

394

39 r>

PERCENT

FREO

9. 9. 3.13.

10.

13.

13.

11. 4. 0. C. Z- .48

72C6

5143

030337

27

47

0 24

PERCENT

FREQ CUM

9.19.

27.

40.

51.

64.

77.

88.

92.

93.

93.

93.

48 19

25 76 18 2225

6389 36

36

60

HISTOGRAM FOR COLUMN

1C (S-B

l.CL 01

XXXXXXXXX

1.5E Cl XXXXXXXXXX

2.3E 01 XXXXXXXX

3.0E 01 XXXXXXXXXXXXXX

5.0E 01 XXXXXXXXXX

7.0E 01

XXXXXXXXXXXXX

l.OE 02 XXXXXXXXXXXXX

1.5E 02

XXXXXXXXXXX

2.0E 02 XXXX

3.0E 02

5.0E 02

7.0E C2

N 40.95

L 235.45

T 00.0

ANALYTICAL

G VALUES

0 395

0.0

MAXIMUM =

7.QOOOCE 02

MINIMUM =

l.OOOOOE 01

GEOMETRIC MEAN =

4.59299E 01

GEOMETRIC DEVIATION =

2.54072E GO

Page 54: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

11 (S-8A

LIMITS

LOWER -

1. 2. 3. 5. 8. 1. 1. 2. 3. 5. B. 1. 1.

8E 6E 8E 6E 3E 2E 8E 6E 8E 6E 3E 2E

8E

01 -

01 -

01

-01

-

01 -

02 -

02 -

02 -

02 -

02 -

02 -

03 -

03 -

FRFQ

UPPER

HISTOGRAM FOR

2 3 5 7 1 1 2 3 5 7 1 1 2

.OE

.OE

.OE

.OE

.OE

.5E

.OE

.OE

.OE

.OE

.OE

.5E

.OE

01 01 01 01 02 02 02

02 02 02 03

03 03

2.6E

3.8E

5.6E

8.3E

1.2E

1.8E

2.6E

3.8E

5.6E

8.3E

1.2E

1.8E

2.6E

COLUMN

X X X X

01 01 Cl 01 02 02 02 02 02 02 03 03

03

11

3 0 3 5 332 23

108

42 117

35 355 (S-BA

FREQ

PERCENT

CUM 3 3 6

11 14 46 69

177

219

336

371

406

411

)

FREQ

0. j

0 » 1. 0. 7. 5.

25. 9.

27. 8. 8. 1.

71 0 71 18 71 58 4559 95 73 29 29 18

PERCENT

FREQ CUM

0. 0. 1. 2. 3.10

.16

.41

.51

.79

.87

.96.

97.

71 71 42 61 32 90 35 94

90 62 91 21 39

xxxxxxxx

xxxx

xxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxxxxxxxxxxxxxxxxxxxxxxxxxxxxx

xxxxxxxx

xxxx

xxxx

X

N 00.0

L11

2.61

T 00.0

ANALYTICAL

G VALUES

0 41

10.0

MAXIMUM =

2.00000E 03

MINIMUM =

2.00000E 01

GEOMETRIC MEAN =

4.56895E 02

GEOMETRIC DEVIATION =

2.17387E 00

Page 55: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

12 (S-BE

LIMITS

LOWER

8, 1. 1, 2. 3, 5.

FREQ

- UPPER

.3E-01 -

.2E

,8E

,6E

,8E

. 6E

OC 00 00 00 00

- - - - -

1. 1. 2. 3. 5. 8.

2E BE 6E 8E 6E 3E

00 00 00 00

00 00

5510

9 84109 123

FREQ

CUM

5516

4248

357

369

372

PERCENT

FREQ

13.03

25.83

19.91

25.83

2.84

0.71

PERCENT

FREQ 13 38 58 84

87

88

CUM

.03

.86

.77

.60

.44

.15

HISTOGRAM FOR COLUMN

12 (S-BE

l.CE 00 XXXXXXXXXXXXX

1.5E 00 XXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 00 XXXXXXXXXXXXXXXXXXXX

3.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXX

5.0E 00 XXX

7.0t 00

X

N 16

3.79

8.06

T 00.0

ANALYTICAL

G VALUES

0 372

0.0

MAXIMUM -

7.00000E 00

MINIMUM =

l.QOOOOE 00

GEOMETRIC MEAN *

1.94415E 00

GEOMETRIC DEVIATION =

1.53364E 00

Page 56: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

15 (S-CO

LIMITS

LOWER

3. 5. 8. 1. 1. 2.

8E 6E 3E 2E 8E 6E

00 00 00 01 01 01

FREQ

- UPPER

- - - - - -

5.6E

8.3E

1.2E

1.8E

2.6E

3.8E

00 00

01 01 01 01

13 18 5417

8 81 53

FREQ

CUM

13 31 85263

344

397

PERCENT

FREQ

3.08

4.27

12.80

42.18

19.19

12.56

PERCENT

FREQ CUM

3.08

7.35

20.14

62.32

81.52

94. C8

HISTOGRAM FOR COLUMN

15 (S-CO

5.0E 00 XXX

7.0E 00

XXXX

l.OE 01

XXXXXXXXXXXXX

1.5E 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 01

XXXXXXXXXXXXXXXXXXX

3.0E 01

XXXXXXXXXXXXX

N 14

3.32

L II

2.61

T 00.0

ANALYTICAL

G VALUES

0 397

0.0

MAXIMUM =

3.0000CE 01

MINIMUM =

5.00000E 00

GEOMETRIC MEAN =

1.53866E 01

GEOMETRIC DEVIATION =

1.50887E 00

Page 57: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

16 (S-CR

LIMITS

FREQ

LOWER -

UPPER

8. 1. I. 2. 3. 5. 8. 1* 1.

3E2E8E

6E 8E

6E

3E2E

8E

OD -

01 -

01 -

Oi -

01 -

01 -

01 -

02 -

02 -

HISTOGRAM FOR

l.OE 01

1.5E 01

1. 1. 2. 3. 5. 8. 1. 1. 2.

2E 8E 6E

BE 6E 3E 2E 8E 6E

01 01 01 01 01 01 02 02 02

COLUMN

X XX

3 9 11 2643

152 71 93 7

16 (S-CR

FREQ

CUM 3

12 23

49

92244

315

408

415

,

PERCENT

FREQ

0. 2. 2. 6.10

.36.

16.

22. 1.

71 13 61 16 19 02 82 0466

PERCENT

FREQ CUM

0.71

2.B4

5.45

11.61

21.83

57.82

74.64

96.68

98.34

2.0E 01 XXX

3.0E 01 XXXXXX

5.0E 01 XXXXXXXXXX

7.0E 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

I.OE 02 XXXXXXXXXXXXXXXXX

1.5E 02 XXXXXXXXXXXXXXXXXXXXXX

2.0E 02 XX

N 00.0

L 7 1.66

T 00.0

ANALYTICAL

G

VALUES

0 415

0.0

MAXIMUM =

2.00000E 02

MINIMUM =

l.OOOOOE 01

GEOMETRIC MEAN =

7.58856E 01

GEOMETRIC DEVIATION =

1.79634E 00

Page 58: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

17 (S-CU

LIMITS

LOWER

3. 5. 8. 1. 1. 2. 3. 5, 8. 1.

BE 6E 3E 2E 8E 6E 8E 6E 3E

2E

00

00 00 01 01 01 01 01 01 02

FREO

- UPPER

- - - - - - - - - -

5. 8. 1. 1. 2. 3. 5. 8, 1. 1.

6E 3E 2E

8E 6E BE

6E

3E 2E BE

00 00 01 01 01 01 01 01 02

02

57 38 29

2423 37 33

102 26 2

FREQ

CUM

57 95

124

148

171

208

241

343

369

371

PERCENT

FREQ

13.51

9.00

6.87

5.69

5.45

8.77

7.82

24.17

6.16

0.47

PERCENT

FREQ 13 22 29 35 40 49 57 81 87 87

CUM

.51

.51

.38

.07

.52

.29

.11

.28

.44

.91

HISTOGRAM FOR COLUMN

17 (S-CU

5.0E 00 XXXXXXXXXXXXXX

7.0E 00 XXXXXXXXX

l.OE 01

XXXXXXX

1.5E 01 XXXXXX

2.0E 01

XXXXX

3.0E 01

XXXXXXXXX

5.0E 01 XXXXXXXX

7.0E 01 XXXXXXXXXXXXXXXXXXXXXXXX

l.OE 02 XXXXXX

1.5E 02

N 0 0.0

L51

12.09

T 0 o.o

ANALYTICAL

G VALUES

0 37

10.0

MAXIMUM =

1.5000CE 02

MINIMUM =

5.00000E 00

GEOMETRIC MEAN =

2.43434E 01

GEOMETRIC DEVIATION =

2.91180E 00

Page 59: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

18

CS

-LA

LIMITS

LOWER -

1 2 3 5 8 1 1 2 3 5

.8E

. 6E

.8E

. 6E

. 3E

. 2E

.8E

.6E

.BE

.6E

Oi -

01 -

01 -

01 -

01 -

02 -

02 -

02 -

02 -

02 -

FREQ

UPPER

HISTOGRAM FOR

N79

18.

2.0E

3.0E

5.0E

7.0E

l.OE

1.5E

2.0E

3.0E

5.0E

7.0E

72

01 01 01 01 02 02 02 02

02 02

2.6E 01

3. BE

015.6E 01

8.3E 01

1.2E 02

1.8E 02

2.6E 02

3. BE

025.6E 02

8.3E 02

COLUMN

18

XXXXXXXXXXX

XXXXXXXXXXX

XXXXXXXXXX

xxxxxxxxxx

xxxx

xxXXXXXXXXXXX

XXX

X

L7317.30

4748 42 42 24

45 14 6 1 1

(S-LA

H 0

FREQ

CUM

47 95

137

179

203

248

262

268

269

270

) B n

PERCENT

PERCENT

FREQ

FREQ

11.

11. 9. 9. 5.

10. 3. I. 0. 0.

14 37 959569

66 32

42 2424

T 00.0

11 22 32 42 48 58 62 63 63 63

CUM

.14

.51

.46

.42

.10

.77

.09

.51

.74

.98 G 00.0

ANALYTICAL

VALUES

270

MA

XIM

UM

*

7.0

00

OT

TE

02

MIN

IMU

M

= 2

.00

00

0E

01

GE

OM

ET

RIC

M

EA

N *

5.9

66

07

E

01

G

EO

ME

TR

IC

DE

VIA

TIO

N

=

2.2

2852E

00

Page 60: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

19 (S-MO

LIMITS

LOWER -

UPPER

3.8E 00

-

5.6E

5.6E 00 -

8.3E

8.3E 00 -

1.2E

1.2E 01 -

1.8E

1.8E 01

-

2.6E

2.6E 01 -

3.8E

3.8E 01 -

5.6E

5.6E 01

-

8.3E

HISTOGRAM FOR COLUMN

5.0E 00 XXX

7.0E 00

l.OE 01

1.5E 01

2.0E 01

3.0E 01

5.0E 01

7.0E 01

N L

164

242

38.86

57.35

00

00

01

01

01

01

01

01

FREQ

11 2 0 0 0 1 1 1

19 (S-MO

H 0

FREO

CUM

11

13

13

13

13

14

15

16

» B 0

PERCENT

FREO

2.61

0.47

0.0

0.0

0.0

0.24

0.24

0.24

T 0 0.0

PERCENT

FREQ CUM

2.61

3.08

3.08

3.08

3.08

3.32

3.55

3.79 G 0 0.0

ANALYTICAL

VALUES

16

MAXIMUM =

7.00000E 01

MINIMUM =

5.00000E 00

GEOMETRIC MEAN =

7.94334E 00

GEOMETRIC DEVIATION =

2.47098E 00

Page 61: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

20 (S-NB

LIMITS

LOWER

8. 1. I. 2. 3. 5.

3E 2E 8E 6E 8E

6E

00 01 01 01 01 01

FREQ

- UPPER

- - - - - -

1. 1. 2. 3. 5. 8.

2E 8E 6E 8E 6E 3E

01 01 01 01 01 01

180

51 138 4 2

FREQ

CUM

180

231

244

252

256

258

PERCENT

FREQ

42.65

12.09

3.08

1.90

0.95

0.47

PERCENT

FREQ 42 54

5759

60 61

CUM

.65

.74

.62

.72

.66

.14

HISTOGRAM FOR COLUMN

20 (S-NB

l.OE 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 01 XXXXXXXXXXXX

2.0E 01 XXX

3.0E 01 XX

5.0E 01 X

7.0E 01

N 2

0.47

L162

38.39

ANALYTICAL

T G

VALUES

0 0

258

0.0

0.0

MAXIMUM =

7.00000E 01

MINIMUM =

l.OOOOOE 01

GEOMETRIC MEAN -

1.20818E 01

GEOMETRIC DEVIATION -

1.43090E 00

Page 62: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

21 CS-NI

LIMITS

LOWER

3 5 8 1 1 2 3 5 8 1

. 8E

.6E

.3E

.2E

BE

.6E

.BE

6E

.3E

.2E

00 00 00 01 01 01 01 01 01 02

FREQ

- UPPER

- - - - - - - - - -

5. 8. 1. 1. 2. 3. 5. 8. 1. I.

6h 3E 2E BE 6E 8E

6E 3E 2E

BE

00 00

01 01 01 01 01 01 02

02

622a

30 19 71 79

144

29 7

FREQ

CUM 6

28 36 66 85

156

235

379

408

415

PERCENT

FREQ

1.42

5.21

1.90

7.11

4.50

16.82

18.72

34.12

6.87

1.66

PERCENT

FREQ

1 6 815 20 36

5589

9698

CUM

.42

.64

.53

.64

.14

.97

.69

.81

.68

.34

HISTOGRAM FOR COLUMN

21 (S-NI

5.0E

7.0E

l.OE

1.5E

2.0E

3.0E

5.0E

7.0E

l.OE

1.5E

N 20.47

00 00 01 01 01 01 01 01 02 02

X XXXXX

XX xxxx

xxx

XXXXX

xxxx

xxxx

xxxx

xxxx

xxx

xxxx

xxxx

xxxx

xxxx

xxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxx

XX L 51.18

H B

0 0

T 00.0

ANALYTICAL

G

VALUES

0 415

0.0

MAXIMUM -

1.50000E 02

MINIMUM =

5.00000E 00

GEOMETRIC MEAN »

4.08792E 01

GEOMETRIC DEVIATION =

2.13419E 00

Page 63: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

22 (S-PB

LIMITS

FREQ

LOWER -

UPPER

8. 1. 1. 2. 3. 5. 8. 1. 1. 2. 3. 5. 8. 1. 1. 2. 3. 5.

3E 2E 8E 6E 8E 6E 3E 2E 8E

6E 8E 6E 3E 2E 8E 6E 8E 6E

03 -

01 -

01 -

01 -

01 -

01 -

01 -

02 -

02 -

02 -

02 -

02 -

02 -

03 -

03 -

03 -

03 -

03 -

1. 1. 2. 3. 5. 8. I. 1. 2. 3. 5. 3. 1. I. 2. 3. 5. 8.

2E 8E 6E8E 6E 3E 2E 8E 6 8E

6E 3E 2E 8E 6E

8E 6E 3E

01 01 01 01 01 01

02 02 02 22 02 02 D3 0303

03 03

03

12 19

25 87 80

131

28 182 1 1 3 0 1 0 0 0 I

FREQ

CUM

12 31 56

143

223

354

382

400

402

403

404

407

407

408

408

408

408

409

PERCENT

FREQ

2. 4. 5.20.

18.

31. 6. 4. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0.

84

50 92

62 9604

64

2747 24

24 71 0 24

0 0 0 24

PERCENT

FREQ CUM

2. 7. 13.

33.

52.

63.

90.

94.

95.

95.

95.

96.

96.

96.

96.

96.

96.

96.

84

3527 89

84 69

52 7926 50 73

45 4568

68

68 68 92

HISTOGRAM FOR COLUMN

22 IS-PB

l.Ot

1.5E

2.0E

3.0E

5.0E

7.0E

l.OE

1.5E

2.0E

3.0E

5.0E

7.0E

l.OE

1.5E

2.0E

3.0E

5.0E

7.0E

N 51.18

01 01 01 01 01 01 02 02 0202

02 02 03 03

03 03 03 03

XXX

xxxx;

xxxx;

xxxx;

xxxx:

xxxx:

xxxx:

xxxx

X

L 81.90

XXXXXXXXXXXXXXXXXXXXX

xxxx

xxxx

xxxx

xxxx

xxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxxx

xxx

T 00.0

ANALYTICAL

G VALUES

0 409

0.0

MA

XIM

UM

=

7.0

0000E

0

3

MIN

IMU

M

= l.O

OO

OO

E

01

G

EO

ME

TR

IC

ME

AN

=

4.9

6064E

01

GEO

MET

RIC

D

EV

IAT

ION

=

2.0

9126E

00

Page 64: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

24 (S-SC

LIMITS

LOWER

3. 5. a. i. i. 2. 3.

8E 6E 3E 2E 8E

6E 8E

00 00 03 01 01

01 01

FREQ

- UPPER

- - - - - - -

5. 8. 1. I. 2. 3. 5.

6E 3E 2E 8E 6E 8E 6E

00 00 31 01 01 01 01

14 45

53

177 84

32 1

FREQ

CUM

14 59

112

289

373

405

406

PERCENT

FREQ

3.32

13.66

12.56

41.94

19.91

7.58

0.24

PERCENT

FREQ3

13 26

68 889596

CUM

.32

.98

.54

.48

.39

.97

.21

HISTOGRAM FOR COLUMN

24 (S-SC

)

5.0E 00 XXX

7.0E 00 XXXXXXXXXXX

l.OC 01 XXXXXXXXXXXXX

1.5E 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

2.OF 01 XXXXXXXXXXXXXXXXXXXX

3.3E 31 XXXXXXXX

5.0E 01

ANALYTICAL

N

L

H

B T

6 V

AL

UE

S

88

00

00

4

06

1

.90

1

.90

0

.0

0.0

MAXIMUM =

5.000JOE 01

MINIMUM *

5.00000E 00

GEOMETRIC MEAN -

U41509E 01

GEOMETRIC DEVIATION =

1.53426E 00

Page 65: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

25 (S-SN

LIMITS

LOWER -

UPPER

8.3E 00 -

1.2E 01

i.2E 01 -

1.8E 01

1.8E 01

-

2.6E Cl

2.6E 01 -

3.8E 01

FREO

32 215 6

FREQ

CUM

32 53 58 64

PERCENT

FREO

7.58

4.98

1.18

1.42

PERCENT

FREQ CUM

7.58

12.56

13.74

15.17

HISTOGRAM FOR COLUMN

l.OE 01

XXXXXXXX

1.5E 01 XXXXX

2.0E 01 X

3.0E 01 X

25 (S-SN

M305

72.27

L53

12.56

T 00.0

ANALYTICAL

G VALUES

0 64

0.0

MAXIMUM «

3.00000E 01

£ MINIMUM *

l.OOOOOE 01

GEOMETRIC MEAN =

1.33665E 01

GEOMETRIC DEVIATION =

1.41882E 00

Page 66: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

26 (S-SR

LIMITS

LOWER

8. 1. 1. 2. 3. 5. 8. 1.

3E 2E 8E 6E BE6E 3E 2E

01 02

02 02 02 02 02 03

FREQ

- UPPER

- - - - - - - -

1. 1. 2. 3. 5. 8. 1. 1.

2t 8E6E8c

6E 3E

2E 8E

02 02 02 02 02

02 03 03

37 68 46 11470

48 9 1

FREO

CUM

37105

151

265

335

383

392

393

FREQ

3.77

16.11

10.90

27.01

16.59

11.37

2.13

0.24

FREQ CUM

8.77

24.88

35.78

62.80

79.38

90.76

92.89

93.13

HISTOGRAM FOR COLUMN

26 (S-SR

I.OB 02 XXXXXXXXX

1.5E 02 XXXXXXXXXXXXXXXX

2.0E 02

XXXXXXXXXXX

3.0E 32 XXXXXXXXXXXXXXXXXXXXXXXXXXX

S.J'

I 02 XXXXXXXXXXXXXXXXX

7.3E 02 XXXXXXXXXXX

l.OE 03 XX

1.5E 03

N 10.24

L28

6.64

T 00.0

ANALYTICAL

G VALUES

0 393

0.0

MAXIMUM =

1.50000E 03

MINIMUM -

l.OOOOOE 02

GEOMETRIC MEAN =

2.86842E 02

GEOMETRIC DEVIATION =

1.86804E

Page 67: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

27 (S-V

LIMITS

FREQ

LOWER -

UPPER

8. 1. 1. 2. 3. 5. 8. 1. 1. 2. 3.

3E 2E BE

6E BE 6E 3E 2E BE 6E 8E

o: -

01 -

01 -

01 -

01 -

31 -

01 -

02 -

02 -

02 -

02 -

1. 1. 2. 3. 5. 8. 1. 1. 2. 3. 5.

2E 8E faE

8E 6E 3E 2E 8E 6E 8E 6E

31 31 31 31 01 01 02 32 02 02 32

0 1 1163

26 76

182 61 551

FREQ

CUM 0 1 2

18 21 47

123

305

366

421

422

PERCENT

FREQ

j.C

3.24

C.24

3.79

C.71

6.16

18.01

43.13

14.45

13.03

C.24

PERCENT

FREQ0 0 0 4 4

11 29

72 86 9910

0

CUM

.

.24

.47

.27

.98

.14

.15

.27

.73

.76

.00

HISTOGRAM FOR COLUMN

27 (S-V

3.0E 01 XXXX

5.0E 01

X

7.0E 01 XXXXXX

l.OE 02 XXXXXXXXXXXXXXXXXX

1.5E 02 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 02 XXXXXXXXXXXXXX

3.0E 02 XXXXXXXXXXXXX

5.CE 02

N 00.0

L 0 O.C

T 0O.C

ANALYTICAL

G VALUES

0 422

,.0

MAXIMUM -

5.00000E 02

MINIMUM =

1.50000E 01

GEOMETRIC MEAN =

1.40652E 02

GEOMETRIC DEVIATION =

1.68058E 00

Page 68: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

29 (S-Y

LIMITS

LOWER

8. 1. 1. 2. 3. 5. 8. 1. 1.

3E 2E 8E6E 8E 6E 3E 2E 8E

00 01 01 01 01 01 01 02 0?

FREQ

- UPPER

- - - - - - - - -

1. 1. 2. 3. 5. 8. 1. 1. 2.

2E 8E

6E 8E6E 3E 2E 8E 6E

01 01 01 01 01 01 02 02 02

1658 77

15260

42 4 4 1

FREQ

CUM

16 74 151

303

363

405

409

413

414

PERCENT

FREQ

3.79

13.74

18.25

36.02

14.22

9.95

i.95

0.95

0.24

PERCENT

FREQ3

17 35 71 86

95 96

97

98

CUM

.79

.54

.78

.80

.02

.97

.92

.87

.10

HISTOGRAM FOR COLUMN

29 IS-Y

l.CE 01 XXXX

1.5E 01 XXXXXXXXXXXXXX

2.0E 01

XXXXXXXXXXXXXXXXXX

3.0E 01

XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

5.0E 01

XXXXXXXXXXXXXX

7.0E 01

XXXXXXXXXX

l.OE 02

X

1.5E 02

X

2.0E 02

N 20.47

L 61.42

T 00.0

ANALYTICAL

G VALUES

0 414

0.0

MAXIMUM =

2.00000E 02

MINIMUM =

l.OOOOOE 01

GEOMETRIC MEAN =

2.93077E 01

GEOMETRIC DEVIATION =

1.73515E 00

Page 69: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

30 (S-ZN

LIMITS

LOWER -

UPPER

1.8E 02 -

2.66 02

2.6E 02 -

3.86 02

3.BE 02 -

5.6E 02

5.6E 02 -

3.3E 32

8.3E 02 -

1.2E

1.2

E

33

-03

1.8

E

03

EQ

4 5 0 0 0

FKEQ

CUM

4 9 9 9 9

PERCENT

FREQ

0.95

1.18

0.0

0.0

0.0

PERCENT

FREQ CUM

0.95

2.13

2.13

2.13

2.13

100.

2<»

2.3

7

HIS

TO

GR

AM

F

IR

CO

LUM

N

2.D

E

02

X

3.3

E

32

X 5.3

E

02

7.D

E

02

l.O

fc

03

l.b

F

03

30 (S-ZN

N393

93.13

L 19

T 0 0.0

ANALYTICAL

G VALUES

0 10

0.0

MAXIMUM =

1.5COOOE 03

MINIMUM =

2.00000E 02

GEOMETRIC MEAN =

2.99625E 02

GEOMETRIC DEVIATION =

1.82357E 00

Page 70: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

FREQUENCY TABLE FOR COLUMN

31 (S-ZR

LIMITS

LOWER

1. 2. 3. 5. 8. 1. 1. 2. 3. 5. 8.

8E

6E

8E6E 3E 2E

BE 6E 8E

6E3E

01 01 01 01 01 02

02020202

02

- UPPER 2. 3. 5. 8. 1. 1. 2. 3. 5. 8. 1.

6E

8E

6E 3E 2E 8E 6E

8E6E 3E 2E

01 01 01 01 02

02

02

02

02 02

03

FREQ

6 5 126

49

10570

106

24 21 5

FREQ

CUM

6 11 12 38

87

192

26?

368

392

413

418

PERCENT

FREQ

1.42

1.18

0.2t

6. 16

11.61

24.88

16.59

25.12

5.69

4.98

1.18

PERCENT

FREQ

i 2 2 92045

6287

929799

CUM

.42

.61

.84

.00

.62

.50

.09

.20

.89

.87

.05

HISTOGRAM FOR COLUMN

31 (S-ZR

2.0E 01

X

3.JE 01 X

5.06 01

7.0E 01

XXXXXX

1.3E 02 XXXXXXXXXXXX

1.5E 02 XXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 02 XXXXXXXXXXXXXXXXX

3.0E 02 XXXXXXXXXXXXXXXXXXXXXXXXX

5.0E 02 XXXXXX

7.0E 02 XXXXX

l.JE 03 X

N 0 0.0

L 40.95

T 00.0

G 00.0

ANALYTICAL

VALUES

MAXIMUM =

l.OOOOOE 03

MINIMUM =

2.00000E 01

GEOMETRIC MEAN =

1.92085E 02

GEOMETRIC DEVIATION =

1.98431E 00

Page 71: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

IN THE COMPUTATIONS PERFORMED TO PRODUCE THE FOLLOWING TABLE OF

GEOMETRIC MEANS AND DEVIATIONS, ALL ELEMENTS ARE IGNORED WHERE

ONE OR MORE OF THE UNQUALIFIED DATA VALUES IS

LESS THAN THE ANALYTICAL LIMIT OF DETECTION SPECIFIED ON INPUT OR WHERE ANY DATA

VALUES ARE QUALIFIED WITH TH

E G

(GREATER THAN) CODE.

DATA VALUES QUALIFIED WITH B

OR H

ARE NO

T USED IN TH

E COMPUTATIONS.

WHERE

NONE OF THE DATA VALUES FOR AN ELEMENT AR

E QUALIFIED TH

E MEAN AND DEVIATION SHOULD BE

THE SAKE AS

THOSE GIVEN IN TH

E PRECEDING

SECTION.

WHERE DATA ARE QUALIFIED WITH THE CODES N,

L» OR

T,

TH

E ESTIMATES OF GEOMETRIC MEAN AND DEVIATION ARE BASED ON A

METHOD

BY A.

J.

COHEN FOR TREATING CENSORED DISTRIBUTIONS.

THE

APPLICATION OF THIS METHOD TO GEOCHEMICAL PROBLEMS IS

DESCRIBED IN

USGS PROFESSIONAL PAPER 574-B.

THE ESTIMATES ARE UNBIASED IN

A

STRICT SENSE ONLY WHERE THE DATA ARE DERIVED FROM A

LOGNORMAL

PARENT POPULATION, BUT EXPERIMENTS HAVE SHOWN THAT LARGE DEPARTURES FROM THIS REQUIREMENT MAY NOT GREATLY INVALIDATE THE RESULTS

ACCEPTANCE AND USE OF THE ESTIMATES, HOWEVER, IS

THE RESPONSIBILITY OF THE INDIVIDUAL.

ELEMENT

S-FE

(S-MG

(S-CA

(S-TI

(S-MN

S-AG

S-B

S-BA

^ S-BE

0 S-CO

S-CR

S-CU

S-LA

S-MO

S-NB

S-NI

S-PB

S-SC

S-SN

S-SR

S-V

S-Y

S-ZN

S-ZR

AA-AU-P

ELEMENT

S-FE

(S-MG

(S-CA

(S-TI

<S-MN

S-AG

S-B

S-BA

0 C 0 0 0 0403 4 0 16 14 0 079

164 2 2 5 8

305 I 0 2

393 0 0

GEOMETRIC

MEAN

156.672287

6.304686

********

********

********

********

********

39.952332

417.097656

0 0 0 0 0 0 11 23 11 34 117

51 73242

162 5 8 853 28 0 6194

406

GEOMETRIC

DEVIATION

2.65

1.67

******

******

******

******

******

2.87

2.58

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 11

G 0 0 217 6 1 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0

ANALYTICAL

VALUES

422

422

420

405

416

421 8

395

411

372

397

415

371

270 16

258

415

409

406

64

393

422

414 10

418 5

REMARKS

422 SAMPLES AND

422 ANALYTICAL VALUES.

422 SAMPLES AND

422 ANALYTICAL VALUES.

2 GREATER THAN VALUES. NO COMPUTATIONS.

17 GREATER THAN VALUES. NO COMPUTATIONS.

6 GREATER THAN VALUES. NO COMPUTATIONS.

1 GREATER THAN VALUES. NO COMPUTATIONS.

COHEN'S TABLE EXCEEDED. H(

1.0) OR GAMMA(

27 NUT DETECTED, LESS THAN, OR TRACE VALUES.

11 NOT DETECTED, LESS THAN, OR TRACE VALUES.

0.5) GTR THAN ALLOW.

395 REPORTED VALUES.

411 REPORTED VALUES.

NO COMPUTATIONS.

Page 72: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

S-BE

S-CD

S-CR

S-CU

S-LA

S-MO

S-NB

S-NI

S-P8

S-SC

S-SN

S-SR

S-V

S-Y

S-ZM

S-ZR

AA-AU-P

1.703786

14.017659

72.933136

18.002045

28.536636

********

9.067518

39.144516

46.520554

13.38299?

3.160229

257.762695

140.651367

28.498642

********

187.455856

********

1.72

1.73

1.93

3.68

3.45

******

1.63

2.28

2.25

1.66

2.47

2.06

1.68

1.79

******

2.07

******

50 NOT DETECTED,

25 NOT DETECTED,

7 NOT DETECTED,

51 NOT DETECTED,

152 NOT DETECTED,

COHEN'S TABLE

164 NOT DETECTED,

7 NOT DETECTED,

13 NOT DETECTED,

16 NOT DETECTED,

358 NOT DETECTED,

29 NOT DETECTED,

422 SAMPLES AND

8 N

OT

DE

TE

CT

ED

, C

OH

EN

'S

TA

BLE

4 NOT DETECTED,

COHEN'S TABLE

LESS THAN, OR TRACE VALUES.

LESS THAN, OR TRACE VALUES.

LESS THAN, OR TRACE VALUES.

LESS THAN, OR TRACE VALUES.

LESS THAN, OR TRACE VALUES.

EXCEEDED. H(

1.0) OR GAMMA(

LESS THAN, OR TRACE VALUES.

LESS THAN, OR TRACE VALUES.

LESS THAN, OR TRACE VALUES.

LESS THAN, OR TRACE VALUES.

LESS THAN, OR TRACE VALUES.

LESS THAN, OR TRACE VALUES.

422 ANALYTICAL VALUES.

LESS THAN, OR TRACE VALUES.

EXCEEDED. HI

1.0) OR GAMMA I

LESS THAN, OR TRACE VALUES.

EXCEEDED. H<

1.0) OR GAMMA*

372 REPORTED VALUES.

397 REPORTED VALUES.

415 REPORTED VALUES.

371 REPORTED VALUES.

270 REPORTED VALUES.

1.5) GTP THAN ALLOW. NO COMPUTATIONS,

258 REPORTED VALUES.

415 REPORTED VALUES.

409 REPORTED VALUES.

406 REPORTED VALUES.

64 REPORTED VALUES.

393 REPORTED VALUES.

414 REPORTED VALUES.

1.3) STR THAN ALLOW. NO COMPUTATIONS,

418 REPORTED VALUES.

0.2) GTR THAN ALLOW. NO COMPUTATIONS,

Page 73: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

N>

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Page 74: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

DE

VO

NIA

N

LS

-

Dl

FR

EQ

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NC

Y

TA

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LIM

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d T

ab

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R

CO

LUM

N

FR

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LOW

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PE

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2.6

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8.3

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1.2

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1.8

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5.6

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8.3

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1.2

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01

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5.6

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28

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1.2

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11

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2.6

E-0

13.8

E-0

15.6

E-0

18.3

E-0

11

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C

O1.8

E

00

2.6

E

00

3.8

6

00

5.6

E

00

8.3

E

00

1.2

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01

1.8

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01

0 0 0 0 0 0 0 0 0 0 0 2 512 8 1

Fre

quency

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dis

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ns

and hi:

t)

FR

EO

P

ER

CE

NT

CU

M 0 0 0 0 0 0 0 0 0 0 0 2 719

27

28

FR

EQ

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

7.1

417.8

642.8

62

8.5

73

.57

PE

RC

EN

TF

RE

Q

CU

M0

.00.0

0.0

0.0

0.0

0.0

0.0

0.0 o.c

0.0

0.0

7.1

425.0

067.8

69

6.4

31

00

.00

HISTOGRAM FOR COLUMN

4 IS-FE

3.0E 00 XXXXXXX

5.0E 00 XXXXXXXXXXXXXXXXXX

7.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 01

XXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 01 XXXX

N 00.0

L 0 n.c

T 0 0.0

ANALYTICAL

G VALUES

0 28

0.0

MAXIMUM =

1.50000E 01

MINIMUM =

3.00000E 00

GEOMETRIC MEAN =

7.05984E 00

GEOMETRIC DEVIATION =

1.44066E 00

Page 75: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

S

ch

isto

se m

arb

le

(pS

sra)

FR

EQ

UE

NC

Y

TA

BLE

F

OR

C

OLU

MN

(S-FE

LIMITS

LOWER -

UPP

3.8E-02 -

5.6E-02 -

8.3E-02 -

1.2E-01 -

1.8E-01 -

2.6E-01 -

3.8E-01 -

5.6E-01 -

8.3E-01 -

1.2E 00 -

1.8E 00 -

2.6E 00 -

3.8E 00 -

5.6E 00 -

E*5.6E-02

8.3E-02

1.2E-01

1.8E-01

2.6E-01

3.8E-01

5.6E-01

8.3E-01

1.2E 00

1.8E 00

2.6E 00

3.8E 00

5.6F 00

8.3C 00

FREQ 0 0 0 0 0 0 0 0 0 0 1

10

33 18

FREQ

CUM

0 0 0 0 0 0 0 0 0 0 1 11 44

62

PERCENT

FREQ

0.0

0.0

0.0

0.0

0.0

0.0

o.o

0.0

0.0

0.0

1.61

16.13

53.23

29.03

PERC

ENT

FREQ CUM

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

o.o

0.0

1.61

17.74

70.97

100.00

HISTOGRAM FOR COLUMN

2.0E

(S-Ft

00 XX

3.0E 00 XXXXXXXXXXXXXXXX

5.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX<XXXXXXXXXXXXXXXX

7.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXX

N 00.0

L 0 ,.0

T 00.0

ANALYTICAL

G

VALUES

0 62

0.0

MAXIMUM =

7.COGOOE CO

MINIMUM =

2.00000E 00

GEOMETRIC MEAM =

5.00251t 00

GEOMETRIC DEVIATION =

1.34980E 00

Page 76: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

S

chis

tose

mar

ble

min

us

Agg

ie

Cre

ek

sam

ple

s

FR

EQ

UE

NC

Y

TA

BLE

F

OR

C

OLU

MN

4

(5-F

E

LIMITS

LOWE* -

3.8E-02 -

5.6E-02 -

8.3E-02 -

1.2E-01 -

1.8E-01 -

2.6E-01 -

3.8E-01 -

5.6E-01 -

8.3E-01 -

1.2E 00 -

1.8E 00 -

2.6E 00 -

3.8E 00 -

5.6E 00 -

UPPEK 5.66-C2

8.3&-02

1.2E-01

1.3E-01

2.6F-01

3.8E-01

5.6E-01

8.3E-C1

1.2E 00

1.8E 00

2.6E CO

3.8F 00

5.6E 00

8.3E 00

FREQ

0 0 0 0 0 0 0 0 0 0 1 819 12

FREQ

CUM

0 0 0 0 0 0 0 0 0 0 1 92840

PERCENT

FREQ

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

2.5'

J20.00

47.50

30.00

PERCENT

FREQ CUM

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

2.50

22.50

70.00

100.00

HIS

TO

GR

AM

F

OR

C

OLU

MM

4

(S-F

E

*)

2.0

E

00

X

XX

3.0E 00 XXXXXXXXXXXXXXXXXXXX

5.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

7.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

ANALYTICAL

N L

H

B T

G

VALUES

0 0

0 0

0 0

40

0.0

0.0

0.0

0.0

MA

XIM

UM

=

7.0

00

00

E

00

MIN

IMU

M

=

2.0

00

00

E

00

G

EO

ME

TR

IC

ME

AN

=

4.6

80

74

E

00

GE

OM

ET

RIC

D

EV

IAT

ION

=

1

.39

18

3E

00

Page 77: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DARBY PLUTON

FREQUENCY TABLE

LIMITS

FOR COLUMN

FREQ

LOWER -

UPPER

3.8E-02 -

5.6E-02 -

8.3E-02 -

1.2E-01 -

1.8E-01 -

2.6E-01 -

3.8E-01 -

5.6E-01 -

8.3E-01 -

1.2E 00 -

1.8E 00 -

2.6E 00 -

3.8E 00 -

5.6E 00 -

8.3E 00 -

1.2E 01 -

5.6E-02

8.3E-02

1.2E-01

1.8E-01

2.6E-01

3.8E-CI

5.6E-01

8.3E-01

1.2E 00

1.8E 00

2.6E 00

3.8E 00

5.6E 00

8.3E 00

1.2E 01

1.8E 01

0 0 0 0 0 0 0 0 0 2 0 416 8 6 2

4 (S-FE

FREQ

CUM 0 0 0 0 0 0 0 0 0 2 2 6

22

3036

38

«)

PERCENT

FREQ

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

5.26

0.0

10.53

42.11

21.05

15.79

5.26

PERCENT

FREQ CUM

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

5.26

5.26

15.79

57.89

78.95

94.7*

100.00

HISTOGRAM FOR COLUMN

(S-FE

1.5E 00 XXXXX

2.QE 00

3.0E 00 XXXXXXXXXXX

5.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

7.0E 00 XXXXXXXXXXXXXXXXXXXXX

l.OE 01

XXXXXXXXXXXXXXXX

1.5E 01 XXXXX

N 00.0

L 0 o.c

T 00.0

ANALYTICAL

G VALUES

0 38

0.0

MAXIMUM =

1.50000E 01

MINIMUM =

1.50000E 00

GEOMETRIC MEAN =

5.64285E 00

GEOMETRIC DEVIATION =

1.66381E 00

Page 78: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

KACHAUIK PLUTOM

FREQUENCY TABLE FUR COLUMN

4 (S-FE

LIMITS

LOWEK -

3.8E-02 -

5.6E-02 -

8.3E-02 -

1.2E-01 -

1.8E-01 -

2.6E-01 -

3.8E-OL -

5.6E-01 -

8.3E-01 -

1.2E 00 -

1.8E 00 -

2.6E 00 -

3.8E 00 -

5.6E 00 -

8.3E 00 -

1.2E 01

-

1.8E 01 -

UPPER 5.65-02

8.3E-02

1.2E-01

1.8E-01

2.6E-01

3.8E-01

5.6E-01

8.3JE-01

1.2E 00

1.8E 00

2.6E 00

3.86 00

5.6E 00

8.3E 00

1.2E 01

1.8E 01

2.6E 01

FREQ

0 0 0 0 0 0 0 0 0 0 0 0 11 25 17 111

FREQ

CUM 0 0 0 0 0 0 0 0 0 0 0 0

11 36

5364

65

PERCENT

FREQ

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

16.92

38.46

26.15

16.92

1.54

PERCENT

FREQ CUM

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

16.92

55.38

81.54

98.46

100.00

HISTOGRAM FOR COLUMN

4 (S-FE

5.0E 00 KXXXXXXXXXXXXXXXX

7.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 01 XXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 01

XXXXXXXXXXXXXXXXX

2.0E 01

XX

N 00.0

L 00.0

T 00.0

ANALYTICAL

G VALUES

0 65

0.0

MAXIMUM =

2.00000E 01

MINIMUM =

5.00000E 00

GEOMETRIC MEAN =

8.39273E 00

GEOMETRIC DEVIATION =

1.44772E 00

Page 79: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

ME

TA

MO

RPH

IC

CO

MPL

EX

-

pGm

c

FR

EQ

UE

NC

Y

TA

BL

E

FOR

C

OLU

MN

4 (S-FE

LIMITS

LOWFK -

UP*

3.8E-02 -

5.6E-02 -

8.3E-02 -

1.2E-01 -

1.8E-01 -

2.6E-01 -

3.8E-01 -

5.6E-01 -

8.3E-01 -

1.2E 00 -

1.8E 00 -

2.6E 00 -

3.8E 00 -

5.6E 00 -

8.3E 00 -

1.2E 01 -

>PR

5.6E-02

8.3E-02

1.2E-OL

1.86-01

2.66-01

3.8E-01

5.6E-01

8.3E-01

1.2E 00

1.8E 00

2.6E 00

3.86 00

5.6E 00

8.3E 00

1.2E 01

1.8E 01

FREQ 0 0 0 0 0 0 0 0 0 0 0 3

17 35 131

FREQ

CUM 0 0 0 0 0 0 0 0 0 0 0 3

20 55 6869

PERCENT

FREQ

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

4.35

24.64

50.72

18.84

1.45

PERCENT

FREQ CUM

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

0.0

4.35

28.99

79.71

98.55

100.00

HISTOGRAM FOR COLUMN

4 (S-FE

3.0E 00 XXXX

5.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXX

7.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 01 XXXXXXXXXXXXXXXXXXX

1.5E 01 X

N 00.0

L 00.0

T 00.0

ANALYTICAL

G

VALUES

0

69

0.0

MAXIMUM =

1.50000E 01

MINIMUM =

3.00000E 00

GEOMETRIC MEAN =

6.71538E 00

GEOMETRIC DEVIATION =

1.35239F.

00

Page 80: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

OcVONIAN LS -Di

d

FREQUENCY TABLE FOR COLUMN

8 (S-MN

LIMITS

FREQ

LOWER -

UPPER

8. I. 1. 2. 3. 5. 8. 1. I. 2. 3. 5. 8. 1. 1.

3E 2E

8E 6E8E

6E

3E

2E8E

6E

8E6E

3E2E8E

00 -

01 -

01 -

01 -

01 -

01 -

01 -

02 -

02 -

02 -

02 -

02 -

02 -

03 -

03 -

I. 1. 2. 3. 5. 8. I. I. 2. 3. 5. 8. 1. I. 2.

2E 8E 6E

8E 6E

3E

2E

8E 6E

8E

6E 3E 2E

8E

6E

01

01

01 01 01 01 02

02 02

02 0202

03 03

03

0 0 0 0 0 0 0 0 0 0 0 12 6 7 3

FREQ

CUM 0 0 0 0 0 0 0 0 0 0 0

12 18 2528

PERCENT

FREQ

0, 0, 0. 0. 0. 0. 0. 0. 0, 0. 0,42,

21,

25,

10..0 .0 .0 ,0 ,0 ,0 ,0 ,0 ,0 .0 .0 .8

6,43

,00

.71

PERCENT

FREQ CUM

0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0.42.

64.

89.

100.

0 0 0 0 0 0 0 0 0 0 0 8629

29 00

HISTOGRAM FOR COLUMN

8 (S-MN

7.0E 02 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 03 XXXXXXXXXXXXXXXXXXXXX

USE 03 XXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 03 XXXXXXXXXXX

N 00.0

L 00.0

T 00.0

ANALYTICAL

G

VALUES

0

28

0.0

MAXIMUM =

2.00000E 03

MINIMUM =

7.00000E 02

GEOMETRIC MEAN =

1.02302E 03

GEOMETRIC DEVIATION =

1.47697E 00

Page 81: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

Sch

isto

se m

arb

le

(pG

sm)

FR

EQ

UE

NC

Y

TA

BLE

FO

R

CO

LUM

N8

(S-MN

LIMITS

LOWER -

UPPER

8. I. 1. 2. 3. 5. 8. 1. 1. 2. 3. 5. 8. 1. 1.

3E 2E 8E 6E

3E 6E 3E

2E

8E6E

8E

6E 3E 2E 8E

00 -

01 -

01 -

01 -

01 -

01 -

01 -

02 -

02 -

02 -

02 -

02 -

02 -

03 -

03 -

1. 1. 2. 3. 5. 8. 1. 1. 2. 3. 5. 8. 1. 1. 2.

2E 8E 6E

8E 6E 3E 2E

8E 6E 8E

6E 3E 2E BE

6E

01 01

01

01 01 0102

02 02

02 02

020303

03

FREQ

0 0 0 0 0 0 0 1 0 1 927 185 1

FREQ

CUM 0 0 0 0 0 0 0 1 1 2

11 38 56

6162

PERCENT

FREQ

0.0

0.0

0.0

0.0

0.0

0.0

o.o

1.61

0.0

1.61

14.52

43.55

29.03

8.06

1.61

PERCENT

FREQ CUM

0.0

0.0

0.0

0.0

0.0

0.0

0.0

1.61

1.61

3.23

17.74

61.29

90.32

98.39

100.00

HISTOGRAM FOR COLUMN

8 (S-MN

1.5E 02 XX

2.0E 02

3.0E 02 XX

5.0E 02

XXXXXXXXXXXXXXX

7.0E 02 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 03 XXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.56 03 XXXXXXXX

2.0E 03 XX

N 00.0

L 00.0

T 0 0.0

ANALYTICAL

G VALUES

0 62

0.0

MAXIMUM =

2.00000E 03

MINIMUM =

1.50000E 02

GEOM

ETRI

C MEAN =

7.

6943

8E 02

GEOMETRIC DEVIATION =

1.49444E OC

Page 82: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

Schis

tose

mar

ble

m

inus

A

ggie

C

reek

sa

mp

les

FR

EQ

UE

NC

Y

TA

BL

E

FO

R

CO

LUM

N(S-MN

LIMITS

F^EO

LOWER -

UPPER

8. I. 1. 2. 3. 5. 8. 1. 1. 2. 3. 5. 8. 1. 1.

3E 2E 8E 6E 8E 6E 3E

2E 8E 6E 8E

6E 3E

2E 8E

00 -

Oi -

01 -

01 -

01 -

01 -

01 -

02 -

02 -

02 -

02 -

02 -

02 -

03 -

03 -

1 I 2 3 5 8 1 I 2 3 5 8 1 1 2

.2E

.8E

.6E

.8E

.6F

.3E

.2E

.8E

.6E

.8E

.6E

.3E

.2E

.8E

.6E

01 01

01 01 01

01 02 02 02 02

02 02

03

0303

0 0 0 0 0 0 0 1 0 0 815 1?3 1

F*EQ

PERCENT

CUM 0 0 0 0 0 0 0 1 1 1 9

2436

39

40

FREQ

0, 0. 0, 0. 0. 0. 0. 2, 0, 0.20,

37,

30, 7. 2.

,0 .0 .0 .0 .0 .0 ,0 ,50

,0 .0 ,00

,50

,00

,50

.50

PERCENT

FREQ CUM

0. 0. 0. 0. 0. 0. 0. 2. 2. 2.22.

60.

90.

97.

100.

0 0 0 0 0 0 0 50

50

50

50

0000

5000

HISTOGRAM FOR COLUMN

8 (S-MM

1.5E 02 XXX

2.0E 02

3.0E 02

5.0E 02 XXXXXXXXXXXXXXXXXXXX

7.0E 02 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 03 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 03 XXXXXXXX

2.0E 03

XXX

N 00.0

L 00.0

T 00.0

G 00.0

ANALYTICAL

VALUES

MAXIMUM =

2.0000GE 03

MINIMUM =

1.50000E 02

i^tOMtTRIC MEAN =

7.617JOE 02

GEOMETRIC DEVIATION =

U54423E CO

Page 83: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DARBY PLUTDN

FREQUENCY TABLE FOR COLUMN

LIMITS

FREQ

LOWER -

UPPER

8 1 1 2 3 5 8 1 1 2 3 5 8 1 1 2

.3E

.2E

.8E

.6E

.8E

.6E

.3E

.2E

.8E

.6E

.BE

.6E

.3E

.2E

.8E

.6E

00 -

01 -

01 -

01 -

01 -

01 -

01 -

02 -

02 -

02 -

02 -

02 -

02 -

03 -

03 -

03 -

1. 1. 2. 3. 5. 8. I. 1. 2. 3. 5. 8. I. I. 2. 3.

2E 8E 6E

8E

6E 3E 2E

8E

6E 8E 6E 3E 2E 8E

6E 8E

01 01

01

01 01

01 020202

02

02 0203

03

03 03

0 0 0 0 0 0 I 0 0 0 113 10

12 0 I

8 (S-MN

FREQ

CUM 0 0 0 0 0 0 1 I I I 2

15 2537

37 38

)

PERCENT

FREQ

0. 0. 0. 0. 0. 0. 2. 0. 0. 0. 2.34.

26.

31. 0. 2.

0 0 0 0 0 0 63

0 0 0 63

2132

58

0 63

PERCENT

FREO CUM

0. 0. 0. 0. 0. 0. 2. 2. 2. 2. 5.

39.

65.

97.

97.

100.

0 0 0 0 0 0 6363

6363

2647

79

37 3700

HISTOGRAM FOR COLUMN

8 <S-MN

l.OE 02 XXX

1.5E 02

2.0E 02

3.0E 02

5.0E 02 XXX

7.0E 02 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 03 XXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 03 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 03

3.0E 03 XXX

N 00.0

L 00.0

T 00.0

ANALYTICAL

G

VALUES

0 38

0.0

MAXIMUM =

3.00000E 03

MINIMUM =

l.OOOOOE 02

GEOMETRIC MEAN =

9.57037E 02

GEOMETRIC DEVIATION =

1.70535E 00

Page 84: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

KACHAUIK PLUTON

FREQUENCY TABLE FOR COLUMN

8 (S-MN

LIMITS

FREQ

LOWER -

UPPER

8. 1. 1. 2.

3. 5. 8. I. 1. 2. 3. 5. 8. 1. 1. 2.

3E 2E8E6E

8E 6E3E

2E

8E 6E8E

6E

3E 2E8E

6E

00 -

01 -

01 -

01 -

01 -

01 -

01 -

02 -

02 -

02 -

02 -

02 -

02 -

03 -

03 -

03 -

1. I, 2. 3. 5, 8, 1, 1, 2. 3. 5. 8, 1. 1. 2, 3,

,2E

.BE

.6E

.8E

,6E

,3E

,2E

.8E

,6E

.BE

,6E

,3E

,2F.

.86

,6E

.BE

01

01 01

01

01

010202

0202

02

02 03

03

0303

0 0 0 0 0 0 0 0 0 0 0 422 34 4 1

FREQ

CUM 0 0 0 0 0 0 0 0 0 0 0 4

2660

6465

PERCENT

FREQ

0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 6.33

.52

. 6. I.

0 0 0 0 0 0 0 0 0 0 0 15 85

31 15 54

PERCENT

FREQ0 0 0 0 0 0 0 0 0 0 0 6

40

9298

100

CUM

.0 .0 .0 .0

.0 .0 .0 .0 .0 .0 .0 .15

.00

.31

.46

.00

HISTOGRAM FOR COLUMN

8 (S-MN

7.0E 02

XXXXXX

l.OE 03

XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 03 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 03 XXXXXX

3.0E 03 XX

N 00.0

L 00.0

T 00.0

ANALYTICAL

G VALUES

0 65

0.0

MAXIMUM =

3.00000E 03

MINIMUM »

7.00000E 02

GEOMETRIC MEAN =

1.28362E 03

GEOMETRIC DEVIATION =

1.32850E 00

Page 85: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

METAMORPHIC COMPLEX -

p6mc

FREQUENCY TABLE FOR COLUMN

8 (S-MN

LIMITS

FREQ

LOWER -

UPPER

8. 1. 1. 2. 3. 5. 8. 1. I. 2. 3. 5. 8. 1. 1. 2. 3.

3E2E8E

6E

8E 6E 3E 2E 8E 6E 8E 6E

3E2E8E

6E 8E

00 -

01 -

01 -

01 -

01 -

01 -

01 -

02 -

02 -

02 -

02 -

02 -

02 -

03 -

03 -

03 -

03 -

1. 1. 2, 3. 5. 8, I, 1. 2. 3, 5. 8. 1, 1. 2. 3. 5.

,2E

.8E

,6E

.8E

.6E

,3E

,2E

.8E

.6E

.BE

.6E

.3E

,2E

,8E

,6E

,8E

>6E

01

01 0101

01 0102

02 02

0202

02

0303

0303

03

0 0 0 0 0 0 0 0 0 0 018 2124 4 1 1

FREQ

CUM 0 0 0 0 0 0 0 0 0 0 0

18

39

63

6768

69

PERCENT

FREQ

0. 0. 0. 0. 0. 0. 0. O. 0. 0. 0.

26.

30.

34. 5. 1. 1.

0 0 0 0 0 0 0 0 0 0 0 09

43

78 80

45

45

PERCENT

FREQ CUM

0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0.26

.56.

91.

97.

98.

100.

0 0 0 0 0 0 0 0 0 0 0 09

52 30 10

55 00

HISTOGRAM FOR COLUMN

8 (S-MN

7.0E 02

XXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 03 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 03 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 03 XXXXXX

3.0E 03 X

5.0E 03 X

N 00.0

L 00.0

T 00.0

ANALYTICAL

G VALUES

0 69

0.0

MAXIMUM =

5.00000E 03

MINIMUM =

7.00000E 02

GEOMETRIC MEAN =

1.13588E 03

GEOMETRIC DEVIATION, -

1.49026E 00

Page 86: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DEVONIAN LS -Did

FREQUENCY TABLE FOR COLUMN

LIMITS

LOWER

8.3E 00

1.2E 01

1.8E 01

2.6E 01

3.8E 01

5.6E 01

8.3C 01

1.2E 02

1.8E 02

1.2E 01

1.85 01

2.6E 01

3.8E 01

5.6b 01

8.3E 01

1.2R 02

1.8E 02

2.6E 02

1? (S-B

CUM

0 1 2 2 7 916

24

28

RCENT

FREQ

0.0

3.57

3.57

0.0

17.86

7.14

25.00

28.57

14.29

PERCENT

FREO CUM

0.0

3.57

7.14

7.14

25.00

32.14

57.14

85.71

100.00

HISTOGRAM FUR COLUMN

12 <S-B

1.5E 01 XXXX

2.0E 01 XXXX

3.0E 01

5.0E 01 XXXXXXXXXXXXXXXXXX

7.0E 01 XXXXXXX

l.OE 02 XXXXXXXKXXXXXXXXXXXXXXXXX

1.5E 02 XXXXXXXXXXXXXXXXXXXXXXXXXXXXX

?.OE 02 XXXXXXXXXXXXXX

N 00.0

L 00.0

T 00.0

ANALYTICAL

6

VALUES

0

28

0.0

MAXIMUM =

2.00000E 02

MINIMUM -

1.50000E 01

GEOMETRIC MEAN »

9.42114E 01

GEOMETRIC DEVIATION -

1.94690E 00

Page 87: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

Sch

isto

se m

arb

le

(pG

sm)

FR

EQ

UE

NC

Y

TA

BLE

F

OR

C

OLU

MN

12

(S-!

LIMITS

FREQ

LOWER -

UPPER

8 1 1 2 3 5 8 1

.3E

.2E

.8E

.6E

.8E

.6E

.3E

.2£

00 -

01 -

01 -

01 -

01 -

01 -

01 -

02 -

1. 1. 2. 3. 5. 8. 1. 1.

2t 8E 66 86 66 3E 2E 8£

01

01 01

01 01 01 02

02

1 6 816 10 145 2

FREQ

CUM 1 7

15 31 41 5560

62

FR

tQ1

.61

9.6

81

2.9

025.8

11

6.1

32

2.5

88

.06

3.2

3

PE

RC

EN

TF

RE

Q

CU

M1.6

11

1.2

924.1

950.0

06

6.1

388.7

196.7

7100.0

0

HIS

TO

GR

AM

F

QR

C

OLU

MN

12 (S-B

l.OE 01 XX

1.5E 01

XXXXXXXXXX

2.0E 01 XXXXXXXXXXXXX

3.0E 01 XXXXXXXXXXXXXXXXXXXXXXXXXX

5.0E 01

XXXXXXXXXXXXXXXX

7.0E 01 XXXXXXXXXXXXXXXXXXXXXXX

l.OE 02 XXXXXXXX

1.5E 02 XXX

N 0O.G

T 0 o.c

ANALYTICAL

G

VALUES

0

62

0.0

MAXIMUM =

1.50000E 02

MINIMUM =

l.OOOOOE OL

GEOMETRIC MEAN =

3.99167E 01

GtOMETRIC DEVIATION =

1.90748E 00

Page 88: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

Schis

tose

mar

ble

min

us

Agg

ie

Cre

ek

sam

ple

s

FR

EQ

UE

NC

Y

TA

BLE

F

UR

C

OLJ

MN

12 (S-B

LIMITS

LOWER

8 1 I 2 3 5 8 I

.3E

.2E

. 8E

.66

.8E

.6E

.3E

,2b

00

01 01 01 01 01 01 02

FREQ

- UPPER

- - - - - - - -

1. 1. 2. 3. 5. 8. 1. 1.

2E BE 6E 8E 6E 3E 2E 8E

01

01 01 01 01 01

02 02

1 5 7 8 8 8 2 1

FREQ

CUM 1 6 13 21 2

93739

40

PERCENT

FREQ

2.50

12.50

17.50

20.00

20.00

20.00

5.00

2.50

PERCENT

FREQ2

15 32 52 72 92

97

100

CUM

.50

.00

.50

.50

.50

.50

.50

.00

HISTOGRAM FJR COLUMN

12 (S-B

l.OE 01 XXX

1.5E 01 XXXXXXXXXXXXX

2.0E 01 XXXXXXXXXXXXXXXXXX

3.0fc

01 XXXXXXXXXXXXXXXXXXXX

5.0E 01

XXXXXXXXXXXXXXXXXXXX

7.0E 01 XXXXXXXXXXXXXXXXXXXX

l.OE 02

XXXXX

1.5E 02

XXX

N 00.0

L 0 O.L

T 00.0

ANALYTICAL

G VALUES

0 40

0.0

MAXIMUM =

1.50000E 02

MINIMUM =

l.OOOOOE 01

GEOMETRIC MEAN =

3.61681E 01

GEOMETRIC DEVIATION =

1.92333E 00

Page 89: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DARBY PLUTON

FREQUENCY TABLE

LIMITS

FOR

COLUMN

FREQ

LOWER -

UPPER

8.3E 00 -

1.2E 01

-

1.8E 01 -

2.6E 01 -

3.8E 01

-

5.6E 01

-

8.3E 01 -

1.2E 02

-

1.2E

1.8E

2.6E

3.8£

5.6E

8.3E

1.2E

1.8E

01 01 01 01 01 01 02 02

11 6 2 3 I 2 0 2

12 (S-B

FREQ

CUM

11 17 19 22 23 25 2527

)

PERCENT

FREQ

28.95

15.79

5.26

7.89

2.63

5.26

0.0

5.26

PERCENT

FREQ CUM

28.95

44.74

50.00

57.89

60.53

65.79

65.79

71.05

HISTOGRAM FOR COLUMN

12 (S-B

00 00

l.OE 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 01 XXXXXXXXXXXXXXXX

2.0E 01 XXXXX

3.0E 01

XXXXXXXX

5.0E 01 XXX

7.0E 01 XXXXX

l.OE 02

1.5C 02 XXXXX

N 00.0

L11

28.95

T 00.0

ANALYTICAL

G

VALUES

0 27

0.0

MAXIMUM «

1.50000E 02

MINIMUM *

l.OOOOOE 01

GEOMETRIC MEAN -

1.95004E 01

GEOMETRIC DEVIATION =

2.31693E 00

Page 90: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

KACHAUIK PLUTON

FREQUENCY TABLE FOR COLUMN

12 (S-B

LIMITS

LOWER

8 1 1 2 3 5 8 1

.3E

.2E

.8E

.6E

.86

.6E

.3E

.2E

00

01 01 01 01 01 01 02

FREO

- UPPER

- - - - - - - -

1. I. 2. 3. 5. 8. 1. 1.

2E 8E

6E 8E 66

3E 2E BE

01

01

01

01

01

01 02

02

157 6

115 5 3 5

FREQ

CUM

15 2228 39

44

49

52 57

FREQ

23.08

10.77

9.23

16.92

7.69

7.69

4.62

7.69

PERCENT

FREQ CUM

23.08

33.85

A3.08

60.00

67.69

75.38

80.00

87.69

HISTOGRAM FOR COLUMN

12 (S-B

l.OE 01 XXXXXXXXXXXXXXXXXXXXXXX

1.5E 01

XXXXXXXXXXX

2.0E 01

XXXXXXXXX

3.0E 01 XXXXXXXXXXXXXXXXX

5.0E 01

XXXXXXXX

7.0E 01

XXXXXXXX

l.OE 02 XXXXX

1.5E 02 XXXXXXXX

N 00.0

L 812.31

T 0 0.0

ANALYTICAL

G VALUES

0 57

0.0

MAXIMUM =

1.50000E 02

MINIMUM *

1.000006 01

GEOMETRIC MEAN =

2.73289E 01

GEOMETRIC DEVIATION =

2.43023E 00

Page 91: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

METAHORPHIC COMPLEX

- p

mc

FREQUENCY TABLE FOR COLUMN

12 CS-B

LIMITS

LOWER -

8. I. I. 2. 3. 5. 8. 1. 1. 2.

3E 2E 8E 6E 8E 6E

3E 2E 8E 6E

00 01 01 01 01 01 01 02 02 02

- - - - - - - - - -

UPPER 1. 1. 2. 3. 5. 8. 1. I. 2. 3.

2E 8E 6E 8E 6E 3E 2E 8E 6E8E

01 01 01 01 01 01 02 02

02 02

FREQ

4 4 2 4 8 S 12 14 9 1

FREQ

CUM 4 8

10 14 22 30

42 56

65 66

PERCENT

FREQ

5.80

5.80

2.90

5.80

11.59

11*59

17.39

20.29

13.04

1.45

PERCENT

FREQ5

11 14 20 31 43 60 81 94 95

CUM

.80

.59

.49

.29

.88

.48

.87

.16

.20

.65

HISTOGRAM FOR COLUMN

12 CS-B

l.OE 01 XXXXXX

1.5E 01 XXXXXX

2.0E 01 XXX

3.0E 01 XXXXXX

5.0E 01

XXXXXXXXXXXX

7.0E 01 XXXXXXXXXXXX

l.OE 02 XXXXXXXXXXXXXXXXX

1.5E 02 XXXXXXXXXXXXXXXXXXXX

2.0E 02 XXXXXXXXXXXXX

3.0E 02 X

N 00.0

L 34.35

T 00.0

ANALYTICAL

G

VALUES

0 66

0.0

MAXIMUM *

3.00000E 02

MINIMUM -

l.OOOOOE 01

GEOMETRIC MEAN =

7.36123E 01

GEOMETRIC DEVIATION *

2.46878E 00

Page 92: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DEVONIAN LS -Did

FREQUENCY TABLE FOR COLUMN

LIMITS

LOWER - UPPER

8.3E-01 -

1.2E 00

1.2E 00 -

1.8E 00

1.8E 00 -

2.6E 00

2.6E 00 -

3.BE 00

14 (S-BE

FREQ

13 8 1 1

FREQ

CUM

13 21 22 23

PERCENT

FREQ

46.43

28.57

3.57

3.57

PERCENT

FREQ CUM

46.43

75.00

78.57

82.14

HISTOGRAM FOR COLUMN

14 (S-BE

l.OE 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 00 XXXX

3.0E OO XXXX

N 00.0

L 517.86

0.0

ANALYTICAL

G VALUES

0 23

0.0

MAXIMUM =

3.00000E 00

MINIMUM *

L.OOOOOE 00

GEOMETRIC MEAN =

1.24475E 00

GfcOMETRIC DEVIATION >

1.14164E 00

Page 93: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

S

chis

tose

mar

ble

(p

6sm

)

FR

EQ

UE

NC

Y

TA

BL

E

FOR

C

OLU

MN

14

(S-B

E

)

LIMITS

LOWER -

UPPER

8.36-01 -

1.2E 00 -

00 -

1.8E

2.6E 00

1.2E 00

1.8E 00

2.6E 00

3.8E 00

FREQ

20 193 1

FREQ

CUM

20 39 4243

PERCENT

FREO

32.26

30.65

4.84

1.61

PERCENT

FREQ CUM

32.26

62.90

67.74

69.35

HISTOGRAM FOR COLUMN

tS-BE

i.OE 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 00 XXXXX

3.0E 00 XX

N 00.0

L19

30.65

0.0

ANALYTICAL

G VALUES

0 43

0.0

MAXIMUM *

3.00000E 00

MINIMUM *

l.OOOOOE 00

GEOMETRIC MEAN *

1.28797E 00

GEOMETRIC DEVIATION *

1.30743E 00

Page 94: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

Sch

isto

se m

arbl

e m

inus

A

ggie

C

reek

sam

ples

FR

EQ

UE

NC

Y

TA

BL

E

FOR

C

OLU

MN

14

(S

-8F

)

LIM

ITS

FR

EO

FR

EQ

P

ER

CE

NT

P

ER

CE

NT

LOW

ER

-

UP

PE

R

CU

M

FR

EQ

FR

EQ

C

UM

8.3

E-0

1

- 1.2

E

00

13

13

32.5

0

32.5

01

.2E

00

-

1.8

E

00

14

27

35

.00

6

7.5

01

.8E

00

-

2.6

£

00

3 30

7.5

0

75

.00

HISTOGRAM FOR COLUMN

14 (S-8F

)

l.OE 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 00 XXXXXXXX

ANALYTICAL

N

L H

B T

G

VALUES

0 10

0 0

0 0

30

0.0

25.00

0.0

0.0

MAXIMUM «

2.00000E 00

MINIMUM *

l.OOOOOE 00

GEOMETRIC MEAN =

1.29503E 00

GEOMETRIC DEVIATION =

1.27736E 00

Page 95: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DARBY

PLUTON

FREQ

UENC

Y TABLE

LIMITS

FOR

COLUMN

1

FREQ

LOWE

R -

UPPER

8.3E-01

-1.

2E 00 -

1.8E

00 -

2.6E 00 -

3.8E 00 -

5.6E 00 -

1.2E

1.8E

2.6E

3.8E

5.6E

8.3E

00 00 00 00 00 00

0 0 10 16 9 3

4 (S-BE

FREQ CUM 0 0 10 26 35 38

>

PERCENT

FREQ

0.0

0.0

26.3

242.11

23.68

7.89

PERCENT

FREQ

CUM

0.0

0.0

26.3

268.42

92.11

100.00

HISTOGRAM FOR COLUMN

14 (S-BE

2.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXX

3.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

5.0E 00 XXXXXXXXXXXXXXXXXXXXXXXX

7.0E 00 XXXXXXXX

N 00.0

L 00.0

ANALYTICAL

T G

VALUES

0 0

38

0.0

0.0

MAXIMUM =

7.00000E 00

MINIMUM =

2.00000E 00

GEOMETRIC MEAN =

3.25367E 00

GEOMETRIC DEVIATION *

1.49062E 00

Page 96: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

KACHAUIK PLUTON

FREQUENCY TABLE FOR COLUMN

LIMITS

LOWER -

UPPER

8.3E-01 -

1.2E 00

1.2E 00 -

1.8E 00

1.8E 00 -

2.6E 00

2.6E 00 -

3.8E 00

3.8E 00 -

5.6E 00

(S-BE

FREQ

0 817

39 1

FREQ

CUM 0 8

2564

65

PERCENT

FREQ

0.0

12.31

26.15

60.00

1.54

PERCENT

FREQ CUM

0.0

12.31

38.46

98.46

100.00

HISTOGRAM FOR COLUMN

14 (S-BE

1.5E 00 XXXXXXXXXXXX

2.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXX

3.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

5.0E 00 XX

N 00.0

L 00.0

T 00.0

ANALYTICAL

G

VALUES

0

65

0.0

MAXIMUM =

5.00000E 00

MINIMUM =

1.500006 00

GEOMETRIC MEAN =

2.49704E 00

GfOMETRIC DEVIATION =

1.31170E 00

Page 97: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

METAMORPHIC COMPLEX -

p6mc

FKEQUENCY TABLE FOR COLUMN

LIMITS

LOWER -

UPPER

8.3E-01 -

1.2E 00

L.2E 00 -

1.8E 00

L.8E 00 -

2.6E 00

2.6E 00 -

3.8E 00

14 (S-BE

)

FREQ

FREQ

PERCENT

PERCENT

52223 17

CUM 5

2750

67

FREQ

7.25

31.88

33.33

24.64

FREQ CUM

7.25

39.13

72. 46

97.10

HISTOGRAM FOR COLUMN

(S-BE

l.OE 00 XXXXXXX

1.5E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

2.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

3.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXX

N 00.0

L 22.90

T 00.0

ANALYTICAL

G

VALUES

0 67

0.0

MAXIMUM «

3.00000E 00

MINIMUM =

l.OOOOOE 00

GEOMETRIC MEAN =

1.91522E 00

GEOMETRIC DEVIATION *

1.38148E 00

Page 98: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DEVONIAN LS -

Did

FREQUENCY TABLE FOR COLUMN

LIMITS

LOWER -

UPPER

8.3E 00 -

1.2E 01

1.2E 01

-

1.8E 01

1.8E 01 -

2.6E 01

22 (S-NB

FREQ

12 0 1

FREQ

CUM

12 12 13

PERCENT

FREQ

42.86

0.0

3.57

PERCENT

FREQ CU

M42.86

42.86

46.43

HISTOGRAM FOR COLUMN

22 (S-N8

l.OE 01

XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 01

2.0E 01 XXXX

N 00.0

L 15

53.57

T 00.0

ANALYTICAL

6 VALUES

0

13

0.0

MAXIMUM *

2.00000E 01

MINIMUM *

l.OOOOOE 01

GEOMETRIC MEAN =

1.05476E 01

GEOMETRIC DEVIATION *

1.21198E 00

Page 99: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

D

AR

BY

P

LU

TU

N

FR

EQ

UE

NC

Y

TA

BL

E

FO

R

CO

LUM

N22 (S-NB

LIMITS

FREQ

FREQ

PERCENT

LOWER -

UPPER

8.3E 00 -

1.26 01

-

1.8E 01 -

2.6E 01 -

3.86 01

-

5.66 01

-

HISTOGRAM FOR

l.OE 01

1.5E 01

1.2E 01

1.8E 01

?.6E 01

3.8E 01

5.6E 01

8.3E 01

COLUMN

22

CUM

FREQ

11

11

28.95

10

21

26.32

4 25

10.53

6 31

15.79

2 33

5.26

1 34

2.63

(S-NB

)

PERCENT

FREQ CUM

28.95

55.26

65.79

81.58

86.84

89.47

XXXXXXXXXXXXXXXXXXXXXXXXXXXXX

xxxx

xxxx

xxxx

xxxx

xxxx

xxxx

xx2.0E 01 XXXXXXXXXXX

3.0E 01 XXXXXXXXXXXXXXXX

5.0E 01 XXXXX

7.06 01 XXX

N 00.0

L 410.53

T 00.0

ANALYTICAL

G

VALUES

0

34

0.0

MAXIMUM =

7.00000E 01

MINIMUM ~

l.OOOOOE 01

GEOMETRIC MtAN =

1.72731E 01

GEOMETRIC DEVIATION =

1.71580E 00

Page 100: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

KACHAUIK PLUTON

FREQUENCY TABLE FOR COLUMN

LIMITS

LOWER -

UPPER

8.3E 00 -

1.2E 01

1.2E 01 -

1.8E 01

1.8E 01

-

2.6E 01

22 (S-NB

FREQ

36 7 2

FREQ

CUM

36

43

45

PERCENT

FREQ

55.38

10.77

3.08

PERCENT

FREQ CUM

55.38

66.15

69.23

HISTOGRAM FOR COLUMN

22 CS-NB

l.OE 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 01 XXXXXXXXXXX

2.0E 01

XXX

N 00.0

L20

30.77

T 00.0

ANALYTICAL

G

VALUES

0

45

0.0

MAXIMUM *

2.00000E 01

MINIMUM *

l.OOOOOE 01

GEOMETRIC MEAN =

1.09840E 01

GEOMETRIC DEVIATION »

1.21845E 00

Page 101: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

METAMORPHIC COMPLEX -

p mc

FREQUENCY TABLE FOR COLUMN

22 (S-NB

)

LIMITS

FREQ

FREQ

PERCENT

PERCENT

LOWER -

UPPER

CUM

FREQ

FREQ CUM

8.3E 00 -

1.2E 01

37

37

53.62

53.62

1.2E 01 -

1.8E 01

3 40

4.35

57.97

HISTOGRAM FOR COLUMN

22

t S-NB

)

l.OE 01

XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.5E 01 XXXX

ANALYTICAL

N L

H

B T

G

VALUES

0 29

0 0

O

0 40

0.0

42.03

0.0

0.0

MAXIMUM *

1.50000E 01

MINIMUM *

l.OOOOOE 01

GEOMETRIC MEAN *

1.03085E 01

GEOMETRIC DEVIATION *

I.U445E 00

Page 102: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DEVONIAN LS

- Did

FREQUENCY TABLE FUR COLUMN

24 (S-PB

LIMITS

FREO

FREQ

LOWER -

UPPER

8.3E 00 -

1.2E 01 -

1.8E 01 -

2.6E 01 -

3.8E 01 -

5.66 Oi -

HISTOGRAM FOR

1.5E 01

2.0E 01

1.2E 01

1.8E 01

2.6E 01

3. 8t 01

5.6E 01

8.3E 01

COLUMN

XXXXXXX

0 2 4117 2

24 (S-PB

CUM 0 2 6

17 24

26

)

PERCENT

FREQ

0.0

7.14

14.29

39.29

25.00

7.14

PERCENT

FREQ CUM

0.0

7.14

21.43

60.71

85.71

92.86

xxxx

xxxx

xxxx

xx3.0E 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

5.0E 01 XXXXXXXXXXXXXXXXXXXXXXXXX

7.0E 01 XXXXXXX

N 00.0

1 27.14

T 0 0.0

ANALYTICAL

G

VALUES

0

26

0.0

MAXIMUM =

7.00000E 01

MINIMUM =

1.50000E 01

GEOMETRIC MEAN *

3.27267E 01

GEOMETRIC DEVIATJON =

1.54175E 00

Page 103: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

Sch

isto

se m

arble

(p

sm

)

FR

EQ

UE

NC

Y

FA

BLE

FO

R

CO

LUM

N2

4

(S-P

B

LIMITS

LOWER -

8 I 1 2 ^ 5

.36

.2c

.86

.6E

.85

.6E

00

01 Oi 01 01 01

- - - - - -

FREQ

UPPER I 1 2 3 5 8

* * . . . *

2E 8E 6E 8E 6£ 3F

01

0101

01

0101

11 116

138 3

FREQ

CUM

11 22 28 4149 52

FRE

Q17.7

417.7

49

.68

20.9

7

12.9

04.8

4

FRE

Q

CUM

17.7

4

35

.48

4

5.1

6

66

.13

7

9.0

3

83*87

HIS

TO

GR

AM

FO

R

CO

LUM

N24 IS-P8

l.OE 01

XXXXXXXXXXXXXXXXXX

1.5E 01 XXXXXXXXXXXXXXXXXX

2.0E 01

XXXXXXXXXX

3.0E 01 XXXXXXXXXXXXXXXXXXXXX

5.0E 01 XXXXXXXXXXXXX

7.0E 01 XXXXX

N 5

8.06

L 58.06

T 00.0

ANALYTICAL

G

VALUES

0 52

0.0

MAXI

MUM

« 7.oooooe 0

1MINIMUM *

l.GuOOOC 01

GEOM

ETRI

C MEAT*

- 2.2251 it

01

GcOMETRIC DEVIATION *

1.84595E 00

Page 104: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

S

chis

tose

mar

ble

min

us A

ggie

Cre

ek

sam

ples

FK

EQ

UE

NC

Y

TA

BLF

F

UR

C

OLU

MN

24

(S

-PB

LIMITS

FP.E

!LOWFR -

JPPEK

8. 1, 1, 2, 3, 5.

, 3£

,2E

,8E

,6E

,8E

,6E

00 01 01 01 01 01

- - - - - -

1. 1. 2, 3. 5. 8.

,?tr

,8.=

,6F

,ae

>6E

, 3c

01 01 01 01 01 01

7 7 4 103 1

FP

.EO

F.

RE

O

PE

RC

EN

T

PE

RC

EN

TC

UM

F

^EQ

F

RE

Q

CU

M7

17

.50

1

7.5

014

17

.50

35.0

018

10.0

0

45

.00

28

25.0

0

70.0

031

7.5

0

77

.50

32

2.5

0

80

.00

HIS

TO

GR

AM

F

UR

C

OLU

MN

24 <S-P«

l.Ot 01 XXXXXXXXXXXXXXXXXX

1.5E 01

XXXXXXXXXXXXXXXXXX

2.0E 01

XXXXXXXXXX

3.0E 01

XXXXXXXXXXXXXXXXXXXXXXXXX

5.0E 01 XXXXXXXX

7.0E 01

XXX

N 512.50

L 37.50

T 00.0

ANALYTICAL

G

VALUES

0

32

0.0

MA

XIM

UM

*

7.0

00

00

E

01

MINIMUM

* i.

oooooe 0

1G

EO

ME

TR

IC

ME

M

*

2.0

75786

01

G

EO

ME

TR

IC

OE

VIA

TIU

N

=

1.7

46

15

E

00

Page 105: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DARBY PLUTON

FREQUENCY TABLE FOR COLUMN

LIMITS

LOWER -

8. 1. 1. 2. 3. 5. 8.

3E 2E

8E

6E 8E6E

3E

00 01

01 01 01

01 01

- - - - - - -

UPPER I. 1. 2. 3. 5. 8. 1.

2E 8E 6E8E

6E 3E

2E

01 01 01 01

01

01

02

24 (S-PB

)

FREO

FREQ

PERCENT

0 0 0 519 131

CUM 0 0 0 5

2437

38

FREO

0.0

0.0

0.0

13.16

50.00

34.21

2.63

PERCENT

FREC CUM

0.0

0.0

0.0

13.16

63.16

97.37

100.00

HISTOGRAM FUR COLUMN

24 (S-PB

3.0E 01 XXXXXXXXXXXXX

5.06 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

7.0E 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

1.06 02 XXX

N 00.0

L 00.0

ANALYTICAL

T G

VALUES

0 0

38

0.0

0.0

MAXIMUM *

l.OOOOOE 02

MINIMUM *

3.00000E 01

GEOMETRIC MEAN *

S.34177E 01

GEOMETRIC DEVIATION =

1.33S26E 00

Page 106: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

KACHAUIK PLUTON

FREQUENCY TABLE FOR COLUMN

LIMITS

LOWER

8, I, 1. 2, 3. 5. 8.

,3E

,2E

,8E

,6E

,8E

,6E

,3E

00

01 01 01 01 01 01

- UPPER

- - - - - - -

I. I. 2. 3. 5. 8. 1.

2E 8E

6E 8E 6E

3E 2E

01 01

01

01

01 01 02

(S-PB

FREO 0 0 0 I 6

45 13

FREQ

CUM 0 0 0 I 7

52

65

PERCENT

FREQ

0.0

0.0

0.0

1.54

9.23

69.23

20.00

PERCENT

FREO CUM

0.0

0.0

0.0

1.54

10.77

80.00

100.00

HISTOGRAM FUR COLUMN

24 (S-P8

3.0E 01 XX

5.0E 01 XXXXXXXXX

7.0E 01

XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 02 XXXXXXXXXXXXXXXXXXXX

N 00.0

L 00.0

T 00.0

ANALYTICAL

G

VALUES

0 65

0.0

MAXIMUM *

l.OOOOOE 02

MINIMUM *

3.00000E 01

GEOMETRIC MEAN =

7.19322E 01

GEOMETRIC DEVIATION *

1.24195E 00

Page 107: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

METAMORPHIC COMPLEX -

pCmc

FREQUENCY TABLE FOR COLUMN

24 (S-PB

LIMITS

LOWER -

8. 1. 1. 2. 3. 5. 8. 1. 1.

3E 2E8E

6E

8E

6E3E2E

8E

00

01 01 01 01 01 01 02

02

- - - - - - - - -

UPPER 1. 1. 2. 3. 5. 8. 1. 1. 2.

2E 8E

6E 8E

6E

3E 2E

8E

6E

01

01

010101

010202

02

FREQ 0 2 4

24 13

24 0 1 I

FREQ

CUM 0 2 6

30

4367

67

6869

PERCENT

FREQ

0.0

2.90

5.80

34.78

18.84

34.78

0.0

1.45

1.45

PERCENT

FREQ0 2 8

43

62

9797

98

100

CUM

.0 .90

.70

.48

.32

.10

.10

.55

.00

HISTOGRAM FOR COLUMN

24 (S-PB

1.5E 01 XXX

2.0E 01

XXXXXX

3.0E 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

5.0E 01

XXXXXXXXXXXXXXXXXXX

7.0E 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

l.OE 02

1.5E 02 X

2.0E 02 X

N 00.0

L 00.0

T 00.0

ANALYTICAL

6

VALUES

0

69

0.0

MAXIMUM *

2.00000E 02

MINIMUM *

1.50000E 01

GEOMETRIC MEAN =

4.46725E 01

GEOMETRIC DEVIATION =

1.66069E 00

Page 108: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DARBY PLUTON

FREQUENCY TABLE FOR COLUMN

LIMITS

LOWER -

UPPER

6.3E 00 -

1.2E 01

1.2E 01

-

1.8E 01

1.8E 01

-

2.6E 01

2.6E 01 -

3.8E 01

27 (S-SN

)

FREQ

FREQ

PERCENT

PERCENT

8 7 1 1

CUM 8

15 16 17

FREO

21.05

18.42

2.63

2.63

FREQ CUM

21.05

39.47

42.11

44.74

HISTOGRAM FUR COLUMN

27 (S-SN

l.OE 01

XXXXXXXXXXXXXXXXXXXXX

1.5E 01 XXXXXXXXXXXXXXXXXX

2.0E 01

XXX

3.0E 01 XXX

N 71

8.4

2

L14

36.8

4

T 00.0

AN

AL

YT

ICA

L

G

VA

LU

ES

0

17

0.0

MAXIMUM *

3.00000E 01

MINIMUM =

l.OOOOOE 01

GEOMETRIC MEAN *

1.31304E 01

GEOMETRIC DEVIATION »

1.36886E 00

Page 109: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

KACHAUIK PLUTON

FKEQUENCY TABLE FUR COLUMN

LIMITS

F LOWER -

UPPER

8.3E 00 -

1.2E 01

1.2E 01

-

1.8E 01

27 (S-SM

1.8E 01 -

2.6E 01

EQ 8 7 1

FREQ

CUM 8

15 16

PERCENT

FREQ

12.31

10.77

1.54

PERCENT

FREQ CUM

12.31

23.08

24.62

HISTOGRAM FOR COLUMN

27 (S-SN

l.OE 01 XXXXXXXXXXXX

1.5E 01 XXXXXXXXXXX

2.0E 01

XX

N31

47.69

L18

27.69

T 00.0

ANALYTICAL

G VALUES

0 16

0.0

MAXIMUM =

2.00000E 01

MINIMUM

l.OOOOOE 01

GEOMETRIC MEAN =

1.24696E 01

GEOMETRIC DEVIATION =

1.26909E 00

Page 110: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLL

METAMORPHIC COMPLEX- p mc

FREQUENCY TABLE FUR COLUMN

LIMITS

LOWER -

UPPER

8.3E 00 -

1.2E 01

1.2E 01

-

1.8E 01

1.8E 01

-

2.6E 01

2.6E 01 -

3.8E 01

27 (S-SN

)

FREQ

F'*EQ

PERCENT

PERCENT

7 3 0 2

CUK 7

10 10 12

FREQ

10.14

4.35

0.0

2.90

FREQ CUM

10.14

14.49

14.49

17.39

HISTOGRAM FOR COLUMN

27 (S-SN

l.OE 01 XXXXXXXXXX

1.5E 01 XXXX

2.0E 01

3.0E 01 XXX

N49

71.01

L 811.59

T 00.0

ANALYTICAL

G

VALUES

0

12

0.0

MAXIMUM =

3.00000E 01

MINIMUM =

l.OOOOOE 01

GEOMETRIC MEAN =

1.32905E 01

GEOMETRIC DEVIATION =

1.52125E 00

Page 111: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DEVONIAN LS

- Did

FREQUENCY TABLE FOR COLUMN

(S-CU

LIMITS

LOWER -

3. 5. 8. 1. 1. 2. 3. 5. 8. 1.

8E

6E

3E 2E

8E

6E 8E 6E 3E 2E

00 -

00 -

00 -

01 -

01 -

01 -

01 -

01 -

Oi -

02 -

UPPER 5. 8. 1. 1. 2. 3. 5. 8. 1. 1.

6E

36

2F.

BE 6E

8E

6E3E

2E 8E

00

00

01 01

01 01 01 01 02 02

FREQ 0 1 2 0 1 0 3

173 1

FREQ

CUM 0 1 3 3 4 4 7

24 27

28

PERCENT

FREQ

0.0

3.57

7.14

0.0

3.57

0.0

10.71

60.71

10.71

3.57

PERCENT

FREQ CUM

0.0

3.57

10.71

10.71

14.29

14.29

25,00

85.71

96.43

100.00

HISTOGRAM FOR COLUMN

19 (S-CU

5

7.0E 00 XXXX

l.OE 01

XXXXXXX

1.5E 01

2.0E 01

XXXX

3.0E 01

5.0E 01 XXXXXXXXXXX

7.0E 01 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

i.OE 02

XXXXXXXXXXX

1.5E 02 XXXX

N 00.0

L 00.0

T 00.0

ANALYTICAL

G

VALUES

0 28

0.0

MAXIMUM =

1.50000E 02

MINIMUM =

7.00000E 00

GEOMETRIC MEAN =

5.52515E 01

GEOMETRIC DEVIATION =

2.06413E 00

Page 112: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

Schis

tose

mar

ble

(p

sm

)

FR

EQ

UE

NC

Y

TA

BL

E

FU

R

CO

LUM

N19 (S-CU

LIMITS

FREQ

LOWER -

UPPE*

3 5 8 1 1 2 3 5 8

.8E

.6E

.3E

.2E

.8E

.6E

.8E

.6E

.3E

00 -

00 -

00 -

01 -

01 -

01 -

01 -

Cl -

01 -

5. 8. I. I. 2. 3. 5. 8. 1.

6E 3F 2E 8E 6E 8E 6E 3E 2E

00

00

01 01 01 01 01 01 02

117 3 4 4 5 2

137

F3EQ

CUM

11 18 21 25

2934

36

49 56

PERCENT

FKEQ

17.74

11-29

4.84

6.45

6.45

8.06

3.23

20-97

11.29

PERCENT

FREQ 17 29 33 4046 54 58 79 90

CUM

.74

.03

.87

.32

.77

.84

.06

.03

.32

HISTOGRAM FOR COLUMN

19 (S-CU

5.0E 00 XXXXXXXXXXXXXXXJCXX

7.0E 00 XXXXXXXXXXX

l.OE 01 XXXXX

1.5E 01

XXXXXX

2.0E 01 XXXXXX

3.0E 01 XXXXXXXX

5.0E 01 XXX

7.0E 01 XXXXXXXXXXXXXXXXXXXXX

l.OE 02 XXXXXXXXXXX

N 00.0

L 69.68

T 00.0

ANALYTICAL

G VALUES

0 56

0.0

MAXIMUM =

l.OOOOOE 02

MINIMUM =

5.00000E 00

GEOMETRIC MEAN =

2.20967E 01

GEOMETRIC DEVIATION =

3.11756E 00

Page 113: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TIT

LE

Schis

tose

m

arb

le

min

us

Aggie

C

reek

sa

mple

s

FR

EQ

UE

NC

Y

TA

BL

F

FO

R

CO

LUM

N19

(S-CU

LIMITS

LOWER -

3. 5. 8. I. 1. 2. 3.

8E

6E

3E

2E8E

6E8E

00 -

00 -

00 -

01 -

01 -

01 -

01 -

F2EQ

JPPEK 5 8 I 1 2 3 5

. . . . . .

kt 3fc

2t 8 =

6F.

8E

6t

uo CO

01

0101

01

01

117 3 4 3 4 2

PR eg CUM

1 1

18

21

25283234

PERCENT

FREQ

27.50

17.50

7.50

10.00

7.50

10.00

5.00

PERCENT

FREQ 27

4552

627080

85

CUM

.50

.00

.50

.50

.00

.00

.00

HISTOGRAM FUR COLUMM

5.0E

(S-CU

00 XXXXXXXXXXXXXXXXXXXXXXXXXXXX

7.0E 00 XXXXXXXXXXXXXXXXXX

l.OE 01 XXXXXXXX

1.5E 01 XXXXXXXXXX

2.0E 01

XXXXXXXX

3.0E 01 XXXXXXXXXX

5.0E 01 XXXXX

N 00.0

L 615.00

T 0 O.G

ANALYTICAL

G

VALUES

0

34

O.G

MAXIMUM =

5.00000E 01

MINIMUM =

5.00000E 00

GEOMETRIC MEAN =

L.03571F 01

GEOMETRIC DEVIATION =

2.10327E 00

Page 114: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

DARBY PLUTON

FREQUENCY TABLE FOR

LIMITS

LOWER -

UPPER

3.8E 00 -

5.6E

5.6E 00 -

B.3E

8.3E 00 -

1.2E

1.2E 01 -

1.8E

1.8E 01

-

2.6E

2.6E OL -

3.8E

3.8E 01 -

5.6E

COLUMN

00

00

01

01

01

01

01

FREQ

12 2 0 0 3 2 A

19 (S-CU

FREQ

CUM

12

14

14

14

17

19

23

)

PERCENT

FREQ

31.58

5.26

0.0

0.0

7.89

5.26

10.53

PERCENT

FREQ CUM

31.58

36.84

36.84

36.84

44.74

50.00

60.53

HISTOGRAM FOR COLUMN

19 (S-CU

5.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

7.0E 00 XXXXX

l.OE 01

1.5E 01

2.0E 01 XXXXXXXX

3.0E 01 XXXXX

5.0E 01 XXXXXXXXXXX

N 00.0

L15

39.47

T 00.0

ANALYTICAL

G VALUES

0 23

0.0

MAXIMUM =

5.00000E 01

MINIMUM =

5.00000E 00

GEOMETRIC MEAN =

1.07592E 01

GEOMETRIC DEVIATION =

2.60168E 00

Page 115: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

KACHAUIK PLUTON

FREQUENCY TABLE FOR COLUMN

19 (S-CU

LIMITS

FREQ

LOWER -

UPPER

3.8E

5.6E

8.3E

1.2E

1.8E

2.6E

3.8E

5.6E

8.3E

00 -

00 -

00 -

01 -

01 -

01 -

01 -

01 -

01 -

5. 8. 1. I. 2. 3. 5. 8. 1.

6E 3E 2E 8E 6E

8E 6F 3E 2E

00

00

01 01

01

01 01 01 02

810 7 5 2 8 6 9 1

FREQ

CUM 8

18 25 30 32 4046 55 56

FREQ

12.31

15.38

10.77

7.69

3.08

12.31

9.23

13.85

1.54

PERCENT

FREQ CUM

12.31

27.69

38.46

46.15

49.23

61.54

70.77

84.62

86.15

HISTOGRAM FOR COLUMN

19 (S-CU

5.0E 00 XXXXXXXXXXXX

7.0E 00 XXXXXXXXXXXXXXX

l.OE 01 XXXXXXXXXXX

1.5E 01 XXXXXXXX

2.0E 01 XXX

3.0E 01 XXXXXXXXXXXX

5.0E 01 XXXXXXXXX

7.0E 01 XXXXXXXXXXXXXX

l.OE 02

XX

N 00.0

L 913.85

T 00.0

ANALYTICAL

G VALUES

0 56

0.0

MAXIMUM =

l.OOOOOE 02

MINIMUM =

5.00000E 00

GEOMETRIC MEAN =

1.78866E 01

GEOMETRIC DEVIATION =

2.65762E 00

Page 116: GEOLOGICAL SURVEY GEOCHEMICAL SURVEY OF THE EASTERN ... · on a log scale, and is therefore useful for characterizing many geo- chemical distributions. The geometric mean is not an

TITLE

METAMORPHIC COMPLEX -

p mc

FREQUENCY TABLE FOR COLUMN

19 (S-CU

LIMITS

LOWER

3 5 8 1 1 2 3 5 8

.8E

.6E

.3E

.2E

.8E

.6E

.8E

.6E

.3E

00

00

00 01

01

01 01 01

01

FRF'

Q-

UPPER

- - - - - - - - -

5. 8. 1. 1. 2. 3. 5. 8. 1.

6E3E

2E 8E

6E 8E

6E

3E2E

00

00

01 01

01

01 01 0102

17 9, 106 1

100 7 1

FREQ

CUM

17 26

36

4243

53

53

60

61

PERCENT

FREQ

24.64

13.04

14.49

8.70

1.45

14.49

0.0

10.14

1.45

PERCENT

FREQ 2437

52 60 62 76

7686

88

CUM

.64

.68

.17

.87

.32

.81

.81

.96

.41

HISTOGRAM FOR COLUMN

19 (S-CU

5.0E 00 XXXXXXXXXXXXXXXXXXXXXXXXX

7.0E 00 XXXXXXXXXXXXX

l.OE 01 XXXXXXXXXXXXXX

1.5E 01 XXXXXXXXX

2.0E 01 X

3.0E 01 XXXXXXXXXXXXXX

5.0E 01

7.0E 01 XXXXXXXXXX

l.OE 02 X

N 00.0

L 811.59

T 00.0

ANALYTICAL

G

VALUES

0

61

0.0

MAXIMUM =

l.OOOOOE 02

MINIMUM *

5.00000E 00

GEOMETRIC MEAN =

1.27964E 01

GEOMETRIC DEVIATION -

2.51309E 00