Analytical Data for a Suite 

of Granitoid Rocks from the 

Basin and Range Province 

By Donald E. lee 

U.S. GEOlOGICAl SURVEY BUllETIN 1602 
UNITED STATES DEPARTMENT OF THE INTERIOR 

WilliAM P. ClARK, Secretary 

U.S. GEOlOGICAl SURVEY 

Dallas l. Peck, Director 

UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1984 

For Sale by Distribution Branch 

Text Products Section 

U.S. Geological Survey 

604 South Pickett Street 

Alexandria, Virginia 22304 

Library of Congress Catalog Number 83-600631 
CONTENTS 

Abstract 1 

Introduction 1 

Methods of analysis 1 

Uses of data 3 

References cited 3 

FIGURE 

1. Outline map showing general distribution of samples included in tables 1-11 2 

TABlES 

1. Rapid-rock analyses of granitoid rocks from the Basin and Range province 6 

2. Rapid-rock analyses of replicate samples of granitoid rocks from the Basin and 

Range province 16 

3. Rapid-rock norms for granitoid rocks in table 1 18 

4. Rapid-rock norms for replicate samples of granitoid rocks in table 2 28 

5. Plate-reader semiquantitative emission spectrographic analyses of granitoid rocks 

from the Basin and Range province 30 

6. Plate-reader semiquantitative emission spectrographic analyses of replicate samples of granitoid rocks from the Basin and Range province 40 

7. Quantitative X-ray fluorescence values for barium, rubidium, and strontium in 

granitoid rocks from the Basin and Range province 42 

8. Quantitative neutron activation values for uranium and thorium in granitoid rocks 

from the Basin and Range province 45 

9. Quantitative neutron activation values for uranium and thorium in replicate samples of granitoid rocks from the Basin and Range province 48 

10. Quantitative emission spectrographic analyses of granitoid rocks from the Basin 

and Range province 49 

11. Quantitative emission spectrographic analyses of replicate samples of granitoid 

rocks from the Basin and Range province 54 

Contents Ill 

Analytical Data for a Suite of Granitoid Rocks 

from the Basin and Range Province 

By DONALD E. LEE 

Abstract 

This report presents the following data for a suite 

of 228 random samples of granitoid rocks from the Basin 

and Range province of Arizona, California, Nevada, and 

Utah: major-element analyses and rock norms, 

semiquantitative spectrographic analyses, and quantitative data for antimony, arsenic, barium, bismuth, cadmium, cesium, chlorine, fluorine, lithium, mercury, rubidium, strontium, thallium, and zinc. 

INTRODUCTION 

This report presents analytical data for a suite of 

granitoid rocks from the Basin and Range province of 

Arizona, California, Nevada, and Utah. Two random samples were collected from each of two randomly selected 

plutons within each 1 oX 1 o area shown on figure 1. A 

total of 230 samples was collected. However, sample GR128 was lost, and its odd-numbered counterpart (GR-127) 

also is excluded from this study. The general distribution 

of samples is shown on figure 1, where only odd-numbered samples are shown for the sake of simplicity. At 

the map scale of figure 1, the even-numbered samples 

would plot at or near the locations of their odd-numbered 

counterparts. Exact locations of all samples are listed in 

table 1. 

About 80 percent of the samples were collected by 

D. E. Lee, and about 20 percent were collected by D. 

E. Lee with the assistance of R. E. Van Loenen. Thus, 

for practical purposes, terrane not accessible to a single 

worker with a reasonable degree of safety was not amenable to sampling. In addition to being chosen at random, 

the samples were both fresh (zones of alteration, iron 

staining, and friable rock were avoided) and typical of 

the main intrusive phase in the area of the sample site 

(inclusions, dikes, and other minor variants were rejected). 

Usually a minimum of 4 hours was spent on the 

study of each pluton sampled. Samples that could not be 

broken out with a 5-kg sledge hammer were essentially 

inaccessible because no drilling or blasting was done. In 

the study area, many plutons display an erosion pattern 

of large rounded monoliths, impossible to break open with 

a sledge hammer. In such terrane, road cuts and rock 

falls often provided the only access to fresh material. 

Because we sampled only fresh material, the sample 

suite as a whole is no doubt biased in favor of those 

igneous materials that were originally relatively impermeable. Few of the plutons in the study area appear in outcrop as uniformly fresh and coherent rock. Commonly 

the area properly mapped as intrusive igneous rock contains monoliths ranging in size from a few meters to a 

few tens of meters across surrounded by igneous rubble; 

in other words, the monoliths appear as large raisins floating in a pudding of igneous rubble. In deep road cuts 

and in canyons exposing a vertical section, the same relationship between coherent rock and grus commonly was 

seen to persist for tens of meters below the surface. The 

different susceptibility to weathering from place to place 

within a pluton must result from original differences in 

permeability and acc~ss to surface waters. 

METHODS OF ANALYSIS 

Quantitative values for barium, rubidium, and strontium were obtained by analysis of samples submitted in 

order of consecutive field numbers (that is, GR-1, GR-2, 

GR-3, and so forth). For other analyses listed, the samples 

were submitted in a randomized sequence (R-1, R-2, R3, and so forth), and replicates were included in the suite 

analyzed. For example, samples GR--6 (table 1) and GR6a (table 2) are the same material. For most types of 

analyses, 50 replicates were included in the randomized 

sequence. However, only 30 replicates w,ere included in 

the suite analyzed for uranium and thorium (table 9). 

Major elements were determined by "rapid-rock" 

methods (Shapiro and Brannock, 1962; Shapiro, 1967). 

Totals determined by these methods would ordinarily be 

listed to the nearest whole percent. In this report, however, totals are recorded to two significant numbers 

Methods of Analysis 1 
0 75 0 89 

0 65 

Ogg 

0 79 

o77 

0 101 

0 

61 

c9103 0 85 

105 

NEVADA 0 95 o97 

0 37 

0 39 

o113 

0 33 

o35 

100 

I 0 21 

I 

I 

I WYOMING 

250 

lo23 l --- I 

I 

125o 0 I 

1231 

I 

o45 I 

200 

100 

0 93 

og1 017 

0 15 

... 201.6()203 

185... 183 

0 229 

0 161 

300 KILOMETERS 

200 MILES 

UTAH 

ARIZONA 

Figure 1. Outline map showing general distribution of samples included in tables 1-11. Solid triangle-Precambrian intrusion; open circle-post-Cambrian intrusion. 

2 Granitoid Rocks, Basin and Range Province 
beyond the decimal point, indicating more precision than 

is justified by the analytical methods used. Listed in this 

fashion, the totals provide the reader with somewhat more 

information, and they may be rounded at a glance. 

The plate-reader emission spectrographic analyses 

were obtained by methods described by Dorrzapf (1973). 

George A. Sellers and Robert G. Johnson determined the 

quantitative values for barium, rubidium, and strontium 

by X-ray fluorescence. Harriet G. Neiman determined the 

quantitative fluorine values by using an unpublished selective ion electrode method devised by Daniel R. Norton 

and Johnnie M. McDade. James S. Wahlberg obtained 

the quantitative values for chlorine by X-ray fluorescence 

(Wahlberg, 1976). Hugh T. Millard, Jr. used a neutron 

activation method (Millard, 1975) for determination of the 

quantitative uranium and thorium values. 

Other elements were determined by specially sensitive quantitative emission spectrographic methods (unpublished) devised by Robert E. Mays and Chris Heropoulos. 

Mays determined the lithium and cesium values· 

Heropoulos determined values for arsenic, bismuth, anti~ 

mony, cadmium, zinc, thallium, and mercury. All values 

for gold, tellurium, and selenium were below the limits 

of detection, which are 0.1, 1.0, and 10.0 ppm, respectively. 

USES OF DATA 

Little has been done to develop the usefulness of 

these data. McNeal and others ( 1981) carried out a statistical analysis of the uranium and thorium data, Lee and 

others (1980) discussed the barium analyses, and Lee and 

others (1981) presented oxygen-isotope data for the oddnumbered samples in the suite. In addition, Ronald W. 

Kistler of the U.S. Geological Survey is engaged in a 

study of the strontium-isotope compositions of all the samples in table 1. 

Each reader, depending on his special interests, will 

have his own list of additional uses to which these data 

might be put. Such a list might include: supplementing 

previous data on abundance figures and on the geochemical affinity of certain elements; study of the regional distribution of individual elements or groups of elements; investigation of possible correlations between certain elements 

and ore deposits associated with the intrusions; and study 

of possible correlations between the chemical nature of 

the country rock and the element content of the intrusion. 

In terms of scale, these data might be useful to those 

interested in the evolution of the Basin and Range province, or to others concerned primarily with a particular 

mining district. 

It will take a variety of interests and talents to make 

the most of these data. For this reason, and to prevent 

undue delay in release of this information, I have decided 

to make these data available now. 

In tables 3 and 4, Q, quartz; C, corundum; OR, 

orthoclase; AB, albite; AN, anorthosite; HL, halite; WO, 

wollastonite; EN, enstatite; FS, ferrosilite; MT, magnetite; 

HM, hematite; IL, ilmenite; TN, titanite; RU, rutile; AP, 

apatite; FR, fluorite; CC, calcite; MG, magnesite. 

REFERENCES CITED 

Dorrzapf, A. F., Jr., 1973, Spectrochemical computer analysisArgon- oxygen de-arc method for silicate rocks: U.S. 

Geological Survey Journal of Research, v. 1, no. 5, p. 

559-562. 

Lee, D. E., Friedman, Irving, and Gleason, J. D., 1981, Map 

showing oxygen isotope composition of granitoid rocks 

of the Basin-Range Province: U.S. Geological Survey 

Miscellaneous Field Studies Map MF-1305, scale 

1:3,168,000. 

Lee, D. E., Sellers, G. A., Johnson, R. G., and Rose, H. J., 

Jr., 1980, Barium in granitoid rocks of the Basin and 

Range Province of Nevada, Utah, California, and Arizona: 

U.S. Geological Survey Open-File Report 80-1085, p. 1-

6. 

McNeal, J. M., Lee, D. E., and Millard, H. T., Jr., 1981, 

The distribution of uranium and thorium in granitic rocks 

of the Basin and Range Province, Western United States: 

Journal of Geochemical Exploration, v. 14, p. 25-40. 

Millard, H. T., Jr., 1975, Determination of uranium and thorium 

in rocks and soils by the delayed neutron technique, in 

U.S. Geological Survey, Geochemical survey of the western coal regions, 2d annual progress report, July 1975: 

U.S. Geological Survey Open-File Report 75-436, p. 79-

81. 

Shapiro, Leonard, 1967, Rapid analysis of rocks and minerals 

by a single-solution method, in Geological Survey Research 1967: U.S. Geological Survey Professional Paper 

575-B, p. B187-B191. 

Shapiro, Leonard, and Brannock, W. W., 1962, Rapid analysis 

of silicate, carbonate, and phosphate rocks: U.S. Geological Survey Bulletin 1144A, 56 p. 

Wahlberg, J. S., 1976, Analysis of rocks and soils by X-ray 

fluorescence, in Miesch, A. T., Geochemical survey of 

Missouri-Methods of sampling, laboratory analysis and 

statistical reduction of data: U.S. Geological Survey Professional Paper 95~A. A11-A12. 

References 3 

TABLES 1-11 
Table 1. Rapid-rock analyses (in percent) of granitoid rocks from the Basin and Range province 

Sample Latitude Longitude Si02 Al203 Fe2o3 FeO MgO CaO Na2o K2o 

deg min s deg min s 

GR- 1 38 30 17 112 11 12 58.3 15.6 3.70 3.00 3.10 5.00 3.80 4.7 

GR- 2 38 30 08 112 11 48 59.9 15.8 3.40 2.20 2.30 3.60 4.20 5.1 

GR- 3 39 11 15 113 23 05 71.7 13.8 1.20 .64 .62 1.70 4.00 3.6 

GR- 4 39 11 05 113 26 10 72.1 14.0 .99 .72 .57 2.10 4.00 3.7 

GR- 5 38 21 30 113 04 40 64.2 14.9 2.70 2.50 3.00 4.10 3.60 3.3 

GR- 6 38 20 20 113 04 20 67.7 14.6 1.70 1. 80 1. 60 2.80 3.70 4.0 

GR- 7 38 27 50 113 17 35 60.2 15.0 3.60 2.80 3.00 5.00 3.60 3.4 

GR- 8 38 29 30 113 17 05 63.0 15.3 2.60 2.50 2.50 3.90 3.60 4.0 

GR- 9 37 34 00 113 21 15 63.5 15.0 2.80 2.00 2.60 4.00 3.30 3.6 

GR- 10 37 33 00 113 25 00 63.0 15.0 4.40 .48 2.60 4.20 3.20 3.7 

GR- 11 37 46 10 113 10 10 62.3 15.0 4.00 .88 2.10 3.80 3.30 3.8 

GR- 12 37 46 50 113 10 40 62.4 14.6 3.70 1.00 2.30 3.70 3.80 3.6 

GR- 13 38 26 00 112 33 00 57.4 15.7 2.90 3.60 3.30 5.20 3.50 4.0 

GR- 14 38 26 15 112 34 30 58.8 15.5 2.30 3.90 3.00 4.80 3.50 4.6 

GR- 15 39 43 00 112 35 35 69.8 14.7 1.10 .92 .57 2.30 3.80 4.3 

GR- 16 39 44 25 112 35 35 74.1 13.5 1. 20 .72 .38 1.70 3.50 4.0 

GR- 17 39 53 55 112 06 40 60.6 15.1 4.10 2.30 2.50 4.20 3.70 3.7 

GR- 18 39 54 30 112 07 45 61.3 15.3 3.50 2.40 2.50 4.00 3.70 3.8 

GR- 19 39 23 48 114 51 45 70.8 14.6 1.20 1.40 .83 2.80 3.20 3.9 

GR- 20 39 23 45 114 51 59 69.9 14.0 1.40 1.70 .83 2.90 3.10 4.0 

GR- 21 41 31 55 113 45 35 70.4 14.2 1.20 1.50 .61 2.10 3.90 3.5 

GR- 22 41 31 30 113 43 35 72.3 13.3 1. 40 .72 .54 2.00 3.70 3.6 

GR- 23 41 14 00 113 59 35 70.3 14.7 .89 1.00 .81 2.40 3.90 4.0 

GR- 24 41 12 00 113 59 55 73.1 13.3 .82 .68 .69 2.00 3.70 3.4 

GR- 25 41 00 20 114 17 40 74.0 14.1 .58 .16 .12 .89 4.00 4.2 

GR- 26 41 00 35 114 17 30 73.5 14.8 .55 .12 .05 .96 4.40 4.2 

GR- 27 41 47 47 115 38 04 68.1 15.4 1.70 1.40 .96 3.30 3.70 3.4 

GR- 28 41 48 15 115 38 58 70.0 15.2 1.40 1.20 .87 3.30 3.70 3.3 

GR- 29 41 49 16 115 55 37 68.5 14.9 1.90 1.90 1.30 3.40 3.30 3.6 

GR- 30 41 51 03 115 53 23 67.7 14.9 1.70 1. 80 1.30 3.10 3.40 3.6 

GR- 31 41 40 45 116 04 11 58.6 16.1 .41 4.80 5.00 5.90 3.90 1. 6 

GR- 32 41 40 57 116 04 39 61.6 15.9 1.10 4.00 3.50 5.60 3.90 2.1 

GR- 33 39 38 48 116 04 40 73.6 14.1 .55 .12 .10 .65 3.80 4.3 

GR- 34 39 39 52 116 06 07 74.8 14.9 .44 .36 .10 .83 3.90 4.2 

GR- 35 39 22 53 116 08 42 70.8 14.1 .94 1.60 .72 2.40 2.80 4.7 

GR- 36 39 22 38 116 09 06 71.1 13.6 1.00 1. 40 .62 2.10 2.90 4.9 

GR- 37 39 29 38 117 03 34 67.2 14.9 1.30 2.00 1.70 3.30 3.60 3.8 

GR- 38 39 28 46 117 02 15 66.0 15.5 1. 80 1.80 1.90 3.50 3.60 3.8 

GR- 39 39 08 09 117 07 54 68.3 15.6 1.90 1.40 .97 3.50 3.50 3.1 

GR- 40 39 07 16 117 09 28 71.2 15.0 1.10 .96 .66 2.70 3.50 3.9 

GR- 41 39 08 25 118 20 35 70.7 14.8 1.10 .88 .59 2.60 4.90 2.8 

GR- 42 39 09 40 118 21 15 73.2 14.4 .90 .44 .29 1.60 4.50 3.6 

GR- 43 39 39 44 118 12 40 64.0 15.2 2.50 2.00 1.90 4.00 3.60 3.8 

GR- 44 39 38 30 118 11 30 64.6 14.7 1.80 2.80 2.00 3.40 3.30 4.3 

GR- 45 39 37 55 114 54 20 76.4 12.4 .72 .28 .14 .80 3.80 4.5 

GR- 46 39 40 10 114 51 50 73.5 13 .. 3 .63 .52 .24 1.20 3.50 4.7 

GR- 47 38 51 28 114 12 24 74.1 13.0 .98 .20 .29 2.10 3.40 3.1 

GR- 48 38 50 57 114 11 04 71.7 14.3 1.10 .44 .44 2.10 3.70 3.2 

GR- 49 37 57 15 117 31 10 77.8 12.1 .48 .16 .06 .75 3.50 4.6 

GR- 50 37 57 35 117 32 00 74.5 13.2 .84 .36 .33 1.20 3.90 4.3 

6 Granitoid Rocks, Basin and Range Province 
Table 1. Rapid-rock analyses (in percent) of granitoid rocks-Continued 

Sample H o+ 2 H2

0- Ti02 P2os MnO co2 Cl F Total 

GR- 1 0.46 0.36 1.20 0.43 0.10 0.09 0.02 0.11 99.97 

GR- 2 .56 .34 1.10 .38 .08 .16 .03 .12 99.27 

GR- 3 .44 .23 .2S .11 .02 .26 (.01 .04 98.62 

GR- 4 .27 .10 .26 .16 .03 .15 (.01 .04 99.20 

GR- 5 .97 .17 .68 .17 .06 .03 .02 .06 100.46 

GR- 6 .88 .12 .48 .19 .06 .OS .03 .08 99.79 

GR- 7 .70 .19 .76 .31 .12 .06 .03 .08 98.85 

GR- 8 .58 .16 .66 .26 .08 .08 .02 .06 99.30 

GR- 9 .99 .79 .67 .28 .06 .20 .02 .06 99.87 

GR- 10 1.30 1.40 .64 .25 .06 .08 (.01 .04 100.36 

GR- 11 1.40 1.60 .67 .28 .06 .10 .01 .06 99.36 

GR- 12 1.70 1.40 .65 .28 .06 .02 .02 .04 99.27 

GR- 13 1.40 .so 1.10 .45 .11 .34 .01 .OS 99.56 

GR- 14 1.20 .18 1.10 .44 .10 .08 .04 .11 99.65 

GR- 15 .3 7 .10 .29 .15 .03 .20 <.01 .OS 98.69 

GR- 16 .58 .12 .21 .09 .03 .02 (.01 .03 100.19 

GR- 17 .98 .14 .83 .36 .09 .03 .02 .09 98.74 

GR- 18 1.00 .35 .81 .36 .08 .07 .03 .10 99.30 

GR- 19 .69 .07 .39 .14 .06 .02 .01 .07 100.18 

GR- 20 .46 .09 .44 .15 .OS .02 (.01 .06 99.11 

GR- 21 .39 .21 .31 .13 .07 .OS .01 .OS 98.63 

GR- 22 .35 .14 .26 .12 .OS .02 (.01 .OS 98.56 

GR- 23 .35 .10 .23 .14 .04 .04 (.01 .03 98.94 

GR- 24 .37 .06 .19 .08 .OS .07 (.01 .02 98.54 

GR- 25 .56 .06 .06 .12 .02 .02 (.01 .02 98.92 

GR- 26 .49 .08 .04 .14 .02 .06 (.01 .03 99.45 

GR- 27 .39 .16 .40 .23 .11 .04 (.01 .04 99.34 

GR- 28 .56 .10 .3S .15 .08 .01 (.01 .04 100.27 

GR- 29 .57 .15 .41 .19 .12 .06 (.01 .04 100.35 

GR- 30 .64 .18 .39 .17 .13 .06 .02 .03 99.12 

GR- 31 1.10 .13 .77 .21 .09 .25 .02 .03 98.91 

GR- 32 .82 .09 .87 .26 .08 .02 .03 .06 99.93 

GR- 33 .76 .28 .03 .15 .03 .02 (.01 .04 98.54 

GR- 34 .83 .14 .02 .09 .06 .06 (.01 .03 100.77 

GR- 35 .40 .30 .44 .12 .06 .06 (.01 .06 99.51 

GR- 36 .39 .11 .37 .12 .04 .02 .01 .07 98.75 

GR- 37 .73 .04 .49 .18 .02 .03 (.01 .OS 99.35 

GR- 38 1.10 .08 .56 .25 .08 .02 .01 .06 100.06 

GR- 39 .95 .12 .38 .20 .07 .OS .01 .04 100.09 

GR- 40 .2S .10 .26 .14 .08 .01 .01 .04 99.91 

GR- 41 .25 .08 .30 .17 .OS .03 (.01 .04 99.30 

GR- 42 .42 .22 .13 .06 .07 .02 (.01 .02 99.88 

GR- 43 .52 .01 .62 .27 .11 .01 .03 .06 98.63 

GR- 44 .73 .15 .64 .21 .10 .os .02 .08 98.88 

GR- 45 .28 .03 .08 .04 .04 .01 (.01 .03 99.56 

GR- 46 .48 .19 . .19 .04 .04 .10 .01 .10 98.74 

GR- 47 .53 .01 .11 .12 .OS .01 (.01 .03 98.64 

GR- 48 .95 .10 .21 .10 .03 .02 .02 .04 98.45 

GR- 49 .35 .07 .10 .03 (.01 .02 (.01 <.02 100.05 

GR- 50 .51 .01 .18 .06 .OS .01 (.01 .03 99.49 

Table 1 7 
Table 1. Rapid-rock analyses (in percent) of granitoid rocks-Continued 

Sample Latitude Longitude Si02 Al 2o3 Fe2o3 FeO MgO CaO Na 2o K20 

deg min s deg min s 

GR- 51 37 31 45 117 48 15 67.0 14.6 1.80 1.60 1.20 2.50 3.70 4.3 

GR- 52 37 27 35 117 46 00 66.0 15.0 2.00 1.60 I. 20 2.90 4.00 4.2 

GR- 53 38 24 04 118 14 00 74.6 13.0 .66 .12 .13 .17 3.60 5.4 

GR- 54 38 24 32 118 13 52 72.8 12.9 .62 .96 .30 .70 4.00 5.1 

GR- 55 38 26 45 118 45 25 72.8 13.4 .94 .60 .54 1.30 4.40 3.8 

GR- 56 38 25 15 118 46 15 67.9 15.6 1.60 1.60 1.10 3.40 3.80 3.5 

GR- 57 41 44 55 114 46 10 65.3 15.0 1.40 1.80 2.80 4.30 3.80 3.5 

GR- 58 41 43 25 114 43 20 66.1 15.3 I. 50 2.00 3.00 4.30 3.80 3.5 

GR- 59 41 42 06 116 09 00 65.5 15.8 .78 2.80 2.30 4.30 4.00 2.5 

GR- 60 41 42 30 116 09 57 66.2 15.4 .87 2.70 2.30 3.50 4.00 2.7 

GR- 61 40 45 26 117 36 56 69.4 14.1 .56 1.70 1.40 2.40 3.30 4.6 

GR- 62 40 45 26 117 37 40 65.0 14.5 .90 2.80 2.80 3.80 3.00 4.4 

GR- 63 39 47 35 119 40 20 62.2 16.1 2.70 2.60 2.40 5.10 3.90 2.5 

GR- 64 39 47 50 119 41 10 62.1 16.4 3.10 2.10 2.50 5.10 3.90 2.4 

GR- 65 40 26 05 119 15 45 61.0 16.7 2.20 2.80 2.50 5.60 3.80 2.3 

GR- 66 40 24 30 119 17 35 62.5 17.1 I. 40 3.00 2.40 5.10 3.80 2.3 

GR- 67 32 35 10 110 44 45 67.5 13.9 2.40 2.60 1.10 2.80 3.10 3.8 

GR- 68 32 35 40 110 45 00 68.1 14.0 2.80 2.40 I. 20 2.60 2.80 4.1 

GR- 69 32 26 45 110 46 10 71.9 14.9 1.30 .48 .30 1.20 4.30 3.8 

GR- 70 32 25 50 110 44 50 73.8 13.8 .86 .20 .14 1.30 3.90 4.1 

GR- 71 32 09 15 112 38 50 66.0 15.7 1.80 1.50 1.30 3.30 4.30 3.4 

GR- 72 32 09 30 112 38 25 66.3 15.9 2.10 1.40 1.70 3.40 4.20 3.5 

GR- 73 31 27 10 110 18 20 70.4 14.5 1.60 1.20 .75 .69 .41 5.6 

GR- 74 31 26 25 110 16 55 71.4 13.6 I. 30 1.40 .60 1.50 2.80 5.4 

GR- 75 40 40 35 119 23 05 66.1 15.9 1.80 1.80 1.60 3.90 4.40 2.6 

GR- 76 40 40 15 119 22 25 67.6 14.8 1.70 1.50 1.40 3.40 4.00 3.0 

GR- 77 41 10 19 117 44 28 65.7 15.8 2.20 2.00 1.70 4.60 3.90 2.6 

GR- 78 41 11 10 117 43 29 67.3 16.4 1.50 1.80 I. 50 3.90 3.80 3.0 

GR- 79 41 29 30 117 38 35 66.5 15.4 1.30 1.60 1.70 3.40 4.60 2.4 

GR- 80 41 33 13 117 35 56 66.8 15.9 .83 1.80 1.40 3.30 4.70 2.4 

GR- 81 38 50 46 115 28 52 69.5 14.7 1.40 2.00 1.00 3.60 3.00 3.6 

GR- 82 38 50 40 115 28 58 69.5 14.4 1.10 2.20 .91 3.10 2.90 3.8 

GR- 83 38 20 55 115 34 40 72.8 14.9 .73 .84 .39 2.20 3.70 3.1 

GR- 84 38 21 05 115 35 20 70.0 14.6 1.30 I. 00 .44 2.50 4.00 4.1 

GR- 85 40 19 34 115 30 30 69.8 14.6 .90 1.80 .82 3.00 3.20 3.5 

GR- 86 40 19 46 115 30 52 69.7 14.7 .96 2.10 .92 3.00 3.30 3.5 

GR- 87 41 55 45 118 12 00 65.1 16.1 2.60 1.60 1.50 3.80 4.60 2.6 

GR- 88 41 54 50 118 12 25 66.8 16.3 2.10 1.40 1.30 3.70 4.60 2.7 

GR- 89 40 41 48 118 14 46 67.0 15 .I 1.50 1.60 1.50 3.30 3.60 3.5 

GR- 90 40 42 12 118 14 10 66.7 16.0 1. 50 1.90 I. 80 4.00 3.60 3.0 

GR- 91 39 51 20 113 48 25 71.2 14.2 .69 1.50 .88 2.10 3.40 4.4 

GR- 92 39 47 40 113 53 15 72.3 13.7 .84 .96 .59 1.50 3.80 4.6 

GR- 93 40 08 45 113 45 12 61.0 14.7 2.10 2.80 3.40 5.00 3.40 3.9 

GR- 94 40 07 25 113 45 24 62.6 15.7 2.10 2.50 2.30 3.60 4.00 4.0 

GR- 95 39 55 12 116 33 20 66.8 15.2 1.60 2.00 1.40 3.20 3.20 3.9 

GR- 96 39 54 50 116 34 00 66.5 14.9 I. 60 2.00 1. 40 3.10 3.40 4.4 

GR- 97 40 00 50 115 50 15 67.5 15.8 1.00 2.30 1.10 3.50 3.60 3.2 

GR- 98 40 01 05 115 50 20 66.9 15.2 .71 2.30 1.10 3.70 3.40 3.5 

GR- 99 40 17 20 118 37 25 69.0 15.0 1.10 2.00 1.60 3.50 3.60 3.7 

GR-100 40 17 10 118 38 25 68.3 14.9 1.30 I. 60 1.40 3.30 3.60 3.4 

8 Granitoid Rocks, Basin and Range Province 
Table 1. Rapid-rock analyses (in percent) of granitoid rocks-Continued 

Sample H o+ 2 H2

0- Ti02 P2o5 MnO co2 Cl F Total 

GR- 51 0.87 0.15 0.53 0.29 0.03 0.02 0.01 0.07 98.67 

GR- 52 .69 .16 .60 .26 .03 .01 <.01 .08 98.74 

GR- 53 .67 .08 .08 .04 (.01 .01 .02 .05 98.64 

GR- 54 .63 .17 .09 .08 .02 .28 .02 .06 98.73 

GR- 55 .35 .01 .19 .12 .08 .03 <.01 .02 98.59 

GR- 56 .57 .22 .39 .17 .09 .08 <.01 .03 100.06 

GR- 57 .61 .14 .46 .30 .06 .09 .02 .07 99.65 

GR- 58 .70 .01 .51 .22 .07 (.01 .02 .07 101.11 

GR- 59 .94 .12 .58 .20 .06 .17 .02 .05 100.12 

GR- 60 .55 .04 .54 .20 .06 .20 <.01 .03 99.30 

GR- 61 .53 .07 .37 .16 .01 .02 .02 .06 98.70 

GR- 62 .88 .02 .68 .23 .02 .04 .01 .11 99.19 

GR- 63 .73 .10 .66 .18 .07 .05 .01 .04 99.34 

GR- 64 .44 .08 .66 .11 .10 (.01 .02 .03 99.05 

GR- 65 .58 .17 .61 .24 .08 .08 .01 .03 98.70 

GR- 66 .71 .24 .52 .17 .09 .06 .02 .03 99.44 

GR- 67 .59 .09 .92 .32 .10 .07 <.01 .09 99.39 

GR- 68 .53 .07 .80 .23 .ll .02 <.01 .09 99.86 

GR- 69 .60 .24 .18 .10 .06 .04 <.01 .07 99.48 

GR- 70 .38 .02 .08 .10 .05 .01 <.01 .04 98.79 

GR- 71 .47 .06 .49 .21 .06 .04 <.01 .04 98.68 

GR- 72 .60 .07 .65 .21 .08 .03 .01 .04 100.19 

GR- 73 1.90 .21 .70 .26 .03 .31 .01 .09 98.66 

GR- 74 .82 .ll .45 .15 .08 .02 <.01 .09 99.73 

GR- 75 .45 .09 .52 .20 .04 .08 <.01 .03 99.52 

GR- 76 .39 .01 .47 .16 .05 .08 <.01 .03 98.60 

GR- 77 .83 .07 .46 .23 .11 .02 <.01 .03 100.26 

GR- 78 .49 .19 .46 .16 .08 .01 .01 .03 100.63 

GR- 79 .so .31 .48 .21 .06 .03 <.01 .03 98.83 

GR- 80 .84 .23 .43 .24 .06 <.01 <.01 .04 98.98 

GR- 81 .77 .10 .62 .14 .07 .03 .02 .06 100.61 

GR- 82 .52 .11 .57 .16 .05 .04 <.01 .05 99.42 

GR- 83 .57 .18 .20 .10 .05 .02 (.01 .05 99.84 

GR- 84 .51 .07 .20 .08 .06 .08 .01 .03 98.98 

GR- 85 .54 .19 .47 .22 .02 .06 <.01 .05 99.18 

GR- 86 .51 .10 .so .19 .02 .06 (.01 .06 99.63 

GR- 87 .44 .15 .60 .29 .06 .07 .01 .04 99.56 

GR- 88 .79 .19 .so .18 .08 .02 <.01 .03 100.70 

GR- 89 .77 .10 .35 .16 .08 .01 <.01 .03 98.61 

GR- 90 .82 .18 .45 .17 .06 .02 .01 .04 100.25 

GR- 91 .48 .os .40 .10 .04 .02 <.01 .07 99.54 

GR- 92 .49 <.01 .26 .12 .05 .02 <.01 .08 99.32 

GR- 93 1.30 .04 .74 .42 .08 .34 .02 .13 99.37 

GR- 94 1.10 .27 .65 .46 .05 .08 .03 .10 99.54 

GR- 95 1.30 .23 .53 .19 .05 .01 .02 .06 99.69 

GR- 96 .39 .03 .60 .26 .01 .02 .03 .06 98.70 

GR- 97 .72 .19 .49 .18 .06 .01 .05 .08 99.78 

GR- 98 .85 .18 .53 .26 .01 .06 .os .08 98.83 

GR- 99 .56 .16 .43 .12 .05 .01 .02 .03 100.88 

GR-100 .58 .23 .36 .15 .03 .05 <.01 .03 99.24 

Table 1 9 
Table 1. Rapid-rock analyses (in percent) of granitoid rocks-Continued 

Sample Latitude Longitude Si02 Al203 Fe 2

o3 FeO MgO CaO Na 2o K2o 

deg min s deg min s 

GR-101 40 49 05 117 26 00 64.3 15!9 1.60 2.40 2.30 3.80 3.90 3.0 

GR-102 40 49 20 117 26 40 63.7 15.6 2.10 2.10 2.10 4.30 3.80 3.0 

GR-103 40 21 50 116 21 05 70.3 14.3 .90 1.40 .93 1.50 3.40 4.5 

GR-104 40 22 10 116 20 55 72.5 14.0 .47 .48 .62 .82 4.50 4.6 

GR-105 40 19 50 116 24 10 64.2 14.9 .94 1.70 3.00 5.10 4.10 4.0 

GR-106 40 20 10 116 23 20 62.0 15.2 .73 2.20 4.20 4.90 6.00 2.1 

GR-107 38 09 OS 117 12 10 62.8 15.9 2.30 2.20 1.60 4.70 3.30 3.7 

GR-108 38 09 OS 117 11 so 63.4 16.3 2.30 1.80 1.50 4.60 3.30 3.8 

GR-109 38 30 30 117 01 15 71.7 14.7 .71 .36 .29 1.40 4.70 4.4 

GR-110 38 30 00 117 01 OS 72.3 14.4 .67 .20 .15 1.30 4.60 4.0 

GR-111 38 34 24 116 53 05 71.5 15.3 .64 .92 .38 1.40 4.50 3.7 

GR-112 38 35 24 116 52 25 71.5 15.2 .71 .64 .35 1. 60 4.50 4.3 

GR-113 38 57 10 116 50 35 64.9 16.2 .70 2.70 2.20 4.00 4.20 2.2 

GR-114 38 57 10 116 so 35 66.0 16.1 .93 2.40 2.10 3.80 4.30 2.3 

GR-115 39 43 20 119 42 35 68.4 15.8 1.50 1.10 .84 2.70 4.20 3.6 

GR-116 39 43 55 119 42 25 63.4 16.1 2.70 1.90 1. 80 4.50 4.20 2.7 

GR-117 37 39 10 115 37 45 70.1 15.5 1.60 .60 .35 2.00 3.80 4.6 

GR-118 37 39 20 115 37 20 68.3 15.3 1.60 .96 .57 2.60 3.70 4.1 

GR-119 38 18 25 114 27 55 66.5 14.3 2.80 1.30 1.80 3.70 2.90 3.8 

GR-120 38 18 25 114 27 55 67.3 15.0 3.00 1. 30 1. 70 3.70 3.00 4.0 

GR-121 41 41 35 118 42 10 70.0 15.6 1.30 .76 .63 2.50 4.90 2.9 

GR-122 40 40 35 118 43 00 71.8 14.6 .81 .48 .34 1.80 4.90 3.0 

GR-123 40 15 55 114 17 10 70.1 14.0 1.10 1.20 1.10 2.30 3.70 4.0 

GR-124 40 15 15 114 18 00 69.7 14.3 1.50 1.10 1. 20 2.60 3.70 3.7 

GR-125 40 20 30 114 33 30 60.1 17.8 2.50 1.50 1.40 2.80 4.50 6.3 

GR-126 40 21 40 114 34 25 66.2 14.6 1. 70 1.60 1.40 3.70 3.60 4.1 

GR-129 36 20 15 117 28 30 53.4 17.9 3.90 3.90 3.30 7.20 3.70 3.0 

GR-130 36 20 25 117 28 so 55.7 16.7 3.30 4.00 3.50 6.40 3.50 3.2 

GR-131 36 19 25 117 41 10 72.1 13.9 1.40 .24 .31 1.20 3.60 5.1 

GR-132 36 19 00 117 40 35 72.4 13.1 1.10 .64 .52 1. 60 3.70 4.6 

GR-133 36 02 20 116 40 35 67.5 16.0 1.70 1.40 1.20 2.70 4.80 3.7 

GR-134 36 02 40 116 40 25 69.4 14.2 1. 20 1.30 .71 1. 80 3.60 5.0 

GR-135 36 06 55 116 32 30 69.1 14.6 1.60 .72 .82 1.40 4.90 4.0 

GR-136 36 06 10 116 33 30 69.8 14.6 1.30 .56 .71 1.40 5.10 3.8 

GR-137 35 47 25 116 20 00 72.2 14.3 1.50 .36 .42 .75 4.60 5.1 

GR-138 35 47 15 116 19 30 71.0 13.7 1.30 .52 .43 .79 4.40 5.1 

GR-139 35 27 45 114 54 50 65.3 14.9 2.20 1.10 1.70 2.70 4.20 4.4 

GR-140 35 27 20 114 54 50 64.2 15.0 2.60 1. 40 2.20 3.50 4.10 4.0 

GR-141 35 43 00 114 55 25 73.7 13.8 .91 .24 .14 .56 4.60 5.0 

GR-142 35 42 40 114 55 20 74.1 13.4 .81 .16 .17 .48 4.40 4.9 

GR-143 35 18 00 115 32 20 69.8 15.3 1.60 .72 .74 2.20 4.10 4.0 

GR-144 35 18 50 115 32 50 69.4 16.1 .75 1.00 .69 2.50 5.10 3.2 

GR-145 35 24 30 115 48 10 72.9 13.5 .71 .44 .40 1.00 4.00 4.4 

GR-146 35 24 40 115 47 20 73.3 13.4 .83 .48 .42 1.20 3.80 4.3 

GR-147 35 11 10 116 08 40 76.7 12.2 1.10 .16 .11 .37 4.30 4.4 

GR-148 35 11 45 116 09 00 76.5 11.8 .85 .16 .03 .16 4.40 4.5 

GR-149 35 32 30 117 41 35 68.7 14.8 1.80 1.40 1.10 2.60 3.00 4.6 

GR-150 35 31 15 117 40 20 69.1 14.0 1. 70 1.40 1.00 2.40 3.10 s.o 

GR-151 35 22 20 117 54 35 65.6 16.3 2.10 1. 70 1.40 5.00 4.10 1.8 

GR-152 35 22 05 117 55 20 57.9 18.0 2.60 3.40 3.50 8.10 3.60 1.3 

10 Granitoid Rocks, Basin and Range Province 
Table 1. Rapid-rock analyses (in percent) of granitoid rocks-Continued 

Sample H o+ 2 u2

o- Ti02 P2os MnO co2 Cl F Total 

GR-101 0.91 0.14 0.62 0.33 0.06 0.23 0.01 0.06 99.56 

GR-102 .76 .19 .67 .32 .09 .08 .02 .05 98.88 

GR-103 1.10 .39 .27 .12 .01 .34 .02 .04 99.52 

GR-104 .63 .12 .22 .14 .01 .15 .03 .03 99.32 

GR-105 .59 .32 .98 .32 .09 .08 .02 .09 100.43 

GR-106 .72 .28 1.00 .19 .os .17 .02 .09 99.85 

GR-107 .95 .21 .44 .30 .10 .55 .01 .04 99.10 

GR-108 .91 .11 .40 .22 .14 .10 <.01 .03 98.92 

GR-109 .22 .12 .21 .12 .o 1 .03 (.01 .05 99.03 

GR-110 .37 .30 .19 .14 <.01 .08 <.01 .03 98.74 

GR-111 .53 .15 .26 .09 .07 .02 (.01 .07 99.54 

GR-ll2 .45 .10 .25 .10 .04 .01 .01 .08 99.84 

GR-113 1.10 .14 .47 .23 .06 .28 .01 .03 99.42 

GR-114 .98 .19 .44 .23 .06 .18 .01 .03 100.05 

GR-115 .34 .26 .37 .16 .03 .08 <.01 .03 99.42 

GR-116 .so .31 .53 .20 .09 .09 .03 .03 99.08 

GR-117 .33 .15 .22 .17 .05 .04 <.01 .03 99.55 

GR-118 .63 .22 .33 .23 .08 .05 <.01 .07 98.75 

GR-119 .84 .76 .52 .19 .08 .13 .01 .07 99.70 

GR-120 .82 .68 .55 .17 .09 .01 .02 .07 101.41 

GR-121 .43 .28 .29 .11 .OS .01 (.01 .03 99.80 

GR-122 .29 .19 .19 .15 .01 .as <.01 .02 98.64 

GR-123 .89 .03 .41 .14 .03 .31 .01 .04 99.36 

GR-124 .46 .32 .42 .18 .os .06 .01 .07 99.37 

GR-125 .49 .27 .82 .28 .06 .02 .04 .16 99.04 

GR-126 .55 .20 .53 .32 <.01 .88 .02 .07 99.48 

GR-129 .78 .19 1.00 .52 .12 .25 .02 .12 99.30 

GR-130 1. 20 .15 .85 .45 .14 .10 .04 .07 99.30 

GR-131 .45 .16 .20 .13 .07 .10 .04 .02 99.02 

GR-132 .66 .06 .20 .12 .06 .14 .02 .04 98.96 

GR-133 .56 .08 .54 .20 .02 .08 .OS .04 100.57 

GR-134 .48 .09 .40 .14 .os .06 .02 .03 98.48 

GR-135 .40 .32 .37 .13 .06 .15 .04 .02 98.63 

GR-136 .40 .31 .34 .14 .05 .13 .04 .03 98.71 

GR-137 .30 .11 .38 .09 .03 .04 .04 .09 100.31 

GR-138 .43 .18 .34 .13 .11 .08 .04 .10 98.65 

GR-139 1.10 .22 .66 .23 .04 .11 .02 .08 98.96 

GR-140 .87 .44 .75 .29 .06 .28 .01 .09 99.79 

GR-141 .22 .04 .17 .02 .07 .02 .02 <.02 99.52 

GR-142 .30 .14 .12 .03 .08 .10 .01 .07 99.27 

GR-143 .20 .25 .39 .14 .04 <.01 .01 .OS 99.55 

GR-144 .48 .20 .28 .11 .06 <.01 <.01 .06 99.94 

GR-145 .68 .as .21 .07 .06 .16 <.01 .03 98.62 

GR-146 .42 .06 .19 .07 .01 .06 <.01 .02 98.57 

GR-147 .27 .03 .10 .01 .07 .04 <.01 .07 99.94 

GR-148 .06 .12 .10 .03 .05 .03 <.01 .12 98.92 

GR-149 .84 .17 .42 .14 .06 .08 .02 .06 99.79 

GR-150 .70 .11 .37 .17 .03 .07 .02 .06 99.23 

GR-151 .63 .10 .39 .15 .12 .02 <.01 .03 99.45 

GR-152 .83 .24 .57 .18 .12 .03 .01 .04 100.42 

Table 1 11 
Table 1. Rapid-rock analyses (in percent) of granitoid rocks-Continued 

Sample Latitude Longitude Si02 Al2o3 Fe 2

o3 FeO MgO CaO Na2o K20 

deg min s deg min s 

GR-153 34 27 30 117 03 35 61.4 19.0 1.90 1.30 0.63 4.20 4.70 4.9 

GR-154 34 28 05 117 04 55 60.0 19.2 2.40 1.40 .55 3.90 5.00 5.2 

GR-155 34 32 35 117 16 35 70.7 14.6 1.40 .92 .73 2.40 3.80 3.8 

GR-156 34 32 45 117 17 15 74.1 13.5 .74 .20 .20 1. so 3.50 4.7 

GR-157 34 33 25 116 54 30 74.2 13.7 .84 .56 .33 1.70 3.40 4.6 

GR-158 34 33 05 116 54 25 73.5 14.1 .78 .80 .33 1. 70 3.40 4.6 

GR-159 34 34 30 116 49 00 68.8 14.7 1.60 1.40 1.30 2.90 3.70 3.8 

GR-160 34 34 25 116 49 35 68.5 15.1 1.80 1.40 1. 30 3.10 3.70 3.7 

GR-161 33 44 20 113 40 15 66.7 15.5 1.70 1.90 1.90 3.50 3.70 3.5 

GR-162 33 44 40 113 40 10 66.4 15.6 1.80 2.10 2.00 3.90 3.80 3.3 

GR-163 33 44 35 114 30 45 74.0 12.5 1.50 .48 .37 .27 2.70 5.8 

GR-164 33 44 30 114 31 10 74.5 12.3 2 10 .28 .29 .43 2.70 5.7 

GR-165 33 39 40 114 19_25 68.0 15.1 2.00 1.40 1.20 3.10 3.30 4.4 

GR-166 33 39 00 114 22 45 68.0 14.5 2.00 1.10 1.00 2.70 3.40 4.5 

GR-167 33 27 20 115 08 00 62.0 16.1 2.00 2.90 2.30 4.70 3.70 3.0 

GR-168 33 28 35 115 07 15 67.6 15.2 1.50 1.80 1.60 3.20 3.80 3.8 

GR-169 33 42 40 115 48 20 64.6 16.0 2.10 2.40 1.30 2.40 4.50 5.2 

GR-170 33 43 40 115 49 25 73.7 13.4 .58 .36 .31 .85 3.90 4.5 

GR-171 34 03 55 114 39 15 65.0 15.6 1.90 2.10 1.30 4.50 3.50 2.9 

GR-172 34 04 45 114.40 00 66.1 15.8 1.80 2.20 1.50 4.40 3.50 3.0 

GR-173 34 04 so 115 11 05 73.2 14.5 .73 .56 .27 1.80 4.10 4.0 

GR-174 34 02 25 115 12 55 71.7 14.4 1.30 .68 .33 1.90 4.30 3.5 

GR-175 34 OS 40 115 24 35 74.3 14.3 .52 .28 .20 1.60 4.00 4.4 

GR-176 34 06 30 115 27 35 73.4 14.0 .92 .28 .14 1.50 4.00 4.0 

GR-177 34 40 20 114 41 40 64.4 13.5 2.50 3.90 .61 3.50 2.70 4.1 

GR-178 34 40 15 114 38 55 67.6 13.1 2.20 3.20 .76 2.80 2.80 5.4 

GR-179 35 25 20 113 39 00 70.6 14.9 .99 1.00 .73 2.30 4.90 3.2 

GR-180 35 24 OS 113 39 20 71.6 15.6 1.10 .44 .42 1.80 5.10 3.2 

GR-181 35 06 00 113 52 35 67.4 15.0 1.80 1.10 .66 1.50 3 .1,0 6.9 

GR-182 35 07 15 113 54 45 72.4 12.6 1.70 .60 .35 1.10 3.10 6.2 

GR-183 34 31 25 113 07 15 72.6 13.7 1.40 .64 .42 1.60 3.00 4.6 

GR-184 34 31 OS 113 OS 40 73.5 13.2 1.70 .12 .22 .80 3.00 4.9 

GR-185 34 28 15 113 19 OS 68.7 13.8 2.20 1.90 .91 2.40 3.10 4.8 

GR-186 34 28 55 113 22 00 72.1 13.4 1.10 1. 00 .31 1.10 3.20 5.4 

GR-187 36 16 25 114 11 35 68.2 13.1 2.50 1.80 .86 1.90 2.80 5.6 

GR-188 36 15 so 114 09 15 66.5 14.1 2.30 2.90 1.10 2.50 3.20 4.0 

GR-189 36 13 so 114 15 25 70.6 12.4 3.00 1.60 .32 1.60 2.30 5.1 

GR-190 36 12 00 114 15 10 70.1 13.3 1.70 2.30 .ss 2.20 2.80 5.1 

GR-191 31 45 20 109 52 25 76.1 12.8 .49 .04 .02 .25 3.70 4.6 

GR-192 31 45 00 109 51 55 72.8 13.3 1.30 .44 .so .15 4.20 4.3 

GR-193 31 55 15 109 57 55 75.4 12.9 .78 .48 .08 .43 3.90 s.o 

GR-194 31 55 so 109 57 55 74.4 12.9 1.10 .40 .14 .85 3.90 s.o 

GR-195 31 44 40 110 53 15 65.0 15.8 2.20 2.10 2.00 4.00 3.90 3.8 

GR-196 31 44 00 110 52 55 75.6 12.7 1.00 .60 .58 1.50 3.20 4.6 

GR-197 32 10 OS 109 35 15 68.2 14.3 1.80 2.70 .98 2.80 3.00 4.9 

GR-198 32 10 00 109 34 so 65.8 13.3 2.20 3.10 .99 2.90 3.00 4.4 

GR-199 32 14 00 109 29 45 71.6 14.8 .85 1.00 .61 2.30 4.10 3.4 

GR-200 32 14 30 109 30 30 70.9 14.6 .98 .88 .51 1.90 4.10 3.9 

GR-201 34 35 OS 112 34 00 68.1 13.9 2.10 1.80 1.00 2.20 3.20 4.2 

GR-202 34 34 55 112 33 20 68.6 13.6 1.90 1. 80 1.10 2.10 3.30 4.7 

12 Granitoid Rocks, Basin and Range Province 
Table 1. Rapid-rock analyses (in percent) of granitoid rocks-Continued 

Sample H o+ 2 H2

0- Ti02 P205 MnO C02 Cl F Total 

GR-153 0.39 0.14 0.42 0.12 0.10 0.08 <0.01 0.07 99.36 

GR-154 .31 .10 .46 .15 .10 .04 <.01 .04 98.86 

GR-155 .39 .09 .45 .23 .OS .01 <.01 .06 99.64 

GR-156 .24 .13 .19 .10 .01 <.01 <.01 .02 99.14 

GR-157 .48 .09 .18 .07 .03 .02 (.01 .05 100.26 

GR-158 .38 .03 .19 .07 .OS .01 (.01 .03 99.98 

GR-159 1.20 .26 .44 .15 .03 .11 (.01 .OS 100.45 

GR-160 .73 .19 .42 .15 .OS .08 <.01 .OS 100.28 

GR-161 .97 .32 .44 .15 .07 .08 .01 .04 100.48 

GR-162 .54 .14 .51 .16 .07 .08 .01 .04 100.45 

GR-163 .44 .16 .21 .09 .OS .11 (.01 .11 98.80 

GR-164 .42 .16 .18 .08 .04 .13 (.01 .11 99.43 

GR-165 .47 .11 .45 .15 .OS .02 .02 .os 99.82 

GR-166 .92 .03 .41 .13 .06 .02 .02 .08 98.87 

GR-167 .62 .28 .59 .22 .08 .06 .01 .os 98.61 

GR-168 .74 .06 .51 .14 .07 .03 (.01 .OS 100.11 

GR-169 .61 .08 .97 .30 .02 .01 .02 .07 100.58 

GR-170 .33 .24 .17 .09 .06 .07 <.01 .02 98.59 

GR-171 .78 .03 .46 .29 .10 .10 <.01 .03 98.60 

GR-172 1.20 .20 .47 .21 .11 .03 (.01 .03 100.56 

GR-173 .55 .14 .18 .07 .02 .02 (.01 .04 100.19 

GR-174 .28 .12 .24 .11 .os .15 (.01 .03 99.10 

GR-175 .64 .07 .11 .06 .02 .02 (.01 .02 100.55 

GR-176 .18 .23 .10 .08 .04 .OS <.01 .02 98.95 

GR-177 1.00 .26 .95 .34 .09 .65 <.01 .04 98.55 

GR-178 .89 .18 .73 .17 .10 .25 .02 .21 100.41 

GR-179 .35 .20 .35 .08 .06 .06 .02 .07 99.81 

GR-180 .51 .15 .18 .07 .02 .08 (.01 .04 100.32 

GR-181 .ss .03 .59 .13 .06 .02 (.01 .12 98.97 

GR-182 .21 .03 .40 .07 .OS .01 .02 .11 98.95 

GR-183 .59 .os .24 .14 (.01 .13 <.01 .OS 99.17 

GR-184 .53 .13 .18 .20 <.01 .05 <.01 .03 98.57 

GR-185 .65 .05 .69 .30 .09 .04 .01 .18 99.82 

GR-186 .39 .07 .23 .11 .01 .os .01 .16 98.64 

GR-187 .64 .11 .77 .24 .08 .01 .02 .35 98.98 

GR-188 .63 .14 1.00 .32 .09 .02 .02 .23 99.05 

GR-189 .97 .OS .68 .14 .06 <.01 (.01 .03 98.86 

GR-190 .61 .16 .61 .16 .06 .02 .02 .22 99.91 

GR-191 .46 .08 .08 .09 (.01 .06 (.01 <.02 98.80 

GR-192 .75 .23 .26 .12 .04 .06 <.01 <.02 98.47 

GR-193 .25 .13 .20 .07 .OS .OS (.01 .07 99.80 

GR-194 .19 .04 .19 .08 .04 .03 (.01 .12 99.39 

GR-195 .70 .03 .64 .18 .OS .01 .02 .04 100.47 

GR-196 .39 .11 .23 .07 .01 .02 (.01 <.02 100.63 

GR-197 .33 .16 .91 .30 .10 .02 .01 .13 100.64 

GR-198 .93 .06 .99 .37 .11 .45 <.01 .15 98.76 

GR-199 .51 .08 .24 .11 .OS .02 (.01 .os 99.73 

GR-200 .28 .OS .22 .20 .07 .04 <.01 .04 98.68 

GR-201 .59 .24 .68 .26 .10 .17 .01 .19 98.74 

GR-202 .35 .13 .74 .23 .07 .03 .01 .21 98.87 

Table 1 13 
Table 1. Rapid-rock analyses (in percent) of granitoid rocks-Continued 

Sample Latitude Longitude Si02 Al203 Fe 2o3 FeO MgO CaO Na 2o K2o 

deg min s deg min s 

GR-203 34 34 20 112 30 00 68.7 15.6 1.20 1.40 0.92 2.40 5.10 2.3 

GR-204 34 34 00 112 26 25 69.1 15.4 1.70 1.60 1.10 2.80 4.70 2.6 

GR-205 37 56 25 115 36 00 72.7 13.4 1.30 .24 .21 .97 3.60 4.9 

GR-206 37 56 15 115 36 15 75.1 13.2 .42 .32 .os .26 3.40 5.3 

GR-207 33 39 00 110 34 45 71.6 12.7 1.40 1.20 .79 1.30 2.80 5.2 

GR-208 33 39 00 110 34 15 71.7 13.3 1.80 1. 20 .85 1.50 2.90 5.2 

GR-209 33 21 so 110 58 10 70.0 15.3 1.10 .60 .39 2.20 4.60 3.6 

GR-210 33 22 10 110 56 45 71.0 15.5 1. 20 .56 .45 2.10 4.60 3.3 

GR-211 33 02 20 111 43 45 72.2 15.1 .86 .80 .58 2.80 4.30 2.8 

GR-212 30 02'20 111 43 25 72.4 15.1 1.10 .72 .62 2.50 4.00 3.5 

GR-213 33 01 so 111 46 20 69.3 15.5 1.90 1.20 1.10 3.30 3.60 3.2 

GR-214 33 01 35 111 46 35 66.5 15.9 2.10 1.60 1.30 3.90 3.70 3.0 

GR-215 32 25 55 111 32 55 72.8 13.7 .78 .60 .47 .96 3.70 4.5 

GR-216 32 25 55 Ill 33 35 74.0 13.8 .97 .60 .ss 1.70 3.70 4.7 

GR-217 32 17 30 111 09 45 56.9 16.2 3.50 3.60 3.60 5.80 3.80 3.0 

GR-218 32 17 00 111 10 20 59.3 15.9 2.80 3.20 3.20 5.20 3.90 3.3 

GR-219 31 59 10 111 36 00 63.2 16.7 1.80 2.60 1.60 4.10 4.20 3.3 

GR-220 31 58 15 111 37 10 76.2 12.5 .65 .56 .26 1.40 2.80 5.1 

GR-221 32 50 IS 112 08 so 74.1 12.6 .69 .64 .24 1.10 3.00 5.2 

GR-222 32 so 15 112 09 20 74.2 12.5 .87 .64 .32 1. 20 3.10 4.8 

GR-223 33 18 00 112 37 45 7 4.1 13.5 .63 .64 .40 1.20 3.50 4.5 

GR-224 33 18 45 112 37 15 70.2 14.5 1.10 1.10 .59 1. so 3.90 4.7 

GR-225 33 11 so 112 38 55 70.3 12.9 2.10 1.20 .65 1.90 3.20 5.1 

GR-226 33 11 35 112 38 55 71.2 13.4 1.40 1. 20 .67 1.60 3.30 4.7 

GR-227 34 15 00 111 16 15 75.4 11.9 .91 .24 .14 .45 3.10 5.4 

GR-228 34 15 so 111 14 45 75.1 12.5 1.10 .24 .10 .27 3.20 5.3 

GR-229 33 so 40 113 40 55 75.5 13.7 .57 .08 .os .85 4.70 4.0 

GR-230 33 51 20 113 41 35 75.3 13.5 .59 .08 <.01 .62 4.70 4.1 

14 Granitoid Rocks, Basin and Range Province 
Table 1. Rapid-rock analyses (in percent) of granitoid rocks-Continued 

Sample H o+ 2 H2

0- Ti02 P205 MnO co2 Cl F Total 

GR-203 0.59 0.14 0.37 0.11 0.07 0.08 (0.01 0.06 99.05 

GR-204 .70 .16 .35 .12 .02 .04 (.01 .05 100.45 

GR-205 .44 .36 .23 .09 .03 .08 .01 .04 98.60 

GR-206 .78 .19 .15 .06 .01 .02 <.01 <.02 99.28 

GR-207 .77 .24 .44 .15 .06 .06 .04 .09 98.84 

GR-208 .85 .13 .49 .12 .10 .04 .04 .12 100.34 

GR-209 .24 .10 .22 .16 .05 .09 <.01 .05 98.71 

GR-210 .41 .19 .23 .12 .02 .08 <.01 .06 99.83 

GR-211 .47 .07 .19 .08 .06 .02 <.01 .03 100.37 

GR-212 .25 .19 .23 .09 .05 .01 <.01 .03 100.80 

GR-213 .35 .19 .38 .13 .11 .04 <.01 03 100.34 

GR-214 .54 .30 .41 .16 .09 .02 <.01 .04 99.57 

GR-215 .79 .12 .19 .08 .04 .30 .01 .03 99.07 

GR-216 .65 .16 .20 .09 .05 .16 <.01 .04 101.38 

GR-217 .85 .24 1.00 .31 .09 .02 .04 .07 99.02 

GR-218 .68 .06 .86 .30 .03 .02 .03 .09 98.87 

GR-219 .55 .06 .62 .21 .13 .10 .01 .07 99.25 

GR-220 .49 .11 .16 .05 (.01 .06 .02 .04 100.41 

GR-221 .57 .04 .28 .16 .07 .01 (.01 .07 98.78 

GR-222 .44 .03 .25 .12 .09 .01 .01 .08 98.66 

GR-223 .24 .17 .24 .06 .04 .01 <.01 .07 99.31 

GR-224 .30 .07 .42 .17 .08 .03 <.01 .06 98.73 

GR-225 .48 .09 .49 .18 .07 .01 <.01 .13 98.81 

GR-226 .58 .13 .51 .15 .11 .04 <.01 .12 99.12 

GR-227 .60 .20 .13 .05 .01 .01 .01 <.02 98.56 

GR-228 .58 .21 .14 .07 .02 .05 .01 .02 98.91 

GR-229 .21 .19 .02 .02 .04 .01 <.01 (.02 99.96 

GR-230 .14 .06 .05 .05 .02 .05 (.01 <.02 99.29 

Table 1 15 
Table 2. Rapid-rock analyses (in percent) of replicate samples of granitoid rocks from the Basin and Range 

province 

Sample Latitude Longitude Si02 Al203 Fe2o3 FeO MgO CaO Na2o K2o 

deg min s deg min s 

GR- 6a 38 20 20 113 04 20 67.6 14.5 1.90 1.70 1.50 2.80 3.9 3.8 

GR- lOa 37 33 00 113 25 00 62.6 14.7 4.30 .52 2.60 4.40 3.1 3.6 

GR- lla 37 46 10 113 10 10 63.2 15.1 4.00 1.00 2.20 3.40 3.3 3.7 

GR- 18a 39 54 30 112 07 45 61.0 15.3 3.70 2.40 2.50 4.20 3.7 3.7 

GR- 2la 41 31 55 113 45 35 71.9 14.3 .98 1.50 .63 2.20 4.1 3.5 

GR- 29a 41 49 16 115 55 37 69.0 13.7 1.80 1.80 1. 40 3.10 3.6 3.7 

GR- 32a 41 40 57 116 04 39 61.5 15.9 1.10 4.10 3.40 5.60 3.9 2.0 

GR- 43a 39 39 44 118 12 40 65.1 16.2 2.00 2.20 2.10 4.10 3.9 3.7 

GR- 46a 39 40 10 114 51 50 74.6 13.7 .57 .72 .28 1.30 3.6 4.6 

GR- 55a 38 26 45 118 45 25 74.0 14.2 .91 .64 .45 1.30 4.4 3.7 

GR- 56a 38 25 15 118 46 15 66.4 15.7 1.80 1.60 1.20 3.70 3.7 3.5 

GR- 72a 32 09 30 112 38 25 66.9 15.7 2.10 1.40 1.60 3.20 4.0 3.6 

GR- 75a 40 40 35 119 23 OS 66.8 15.8 1.80 1.90 1.60 3.90 4.5 2.6 

GR- 79a 41 29 30 117 38 35 65.9 15.7 1.30 1.60 1. 70 3.50 4.7 2.4 

GR- 83a 38 20 55 115 34 40 71.9 14.6 .82 .92 .36 2.20 3.7 3.2 

GR- 85a 40 19 34 115 30 30 68.0 14.6 1.10 2.10 1.00 2.90 3.5 3.7 

GR- 87a 41 55 45 118 12 00 64.7 16.1 2.30 1.50 1.50 4.00 4.5 3.0 

GR- 95a 39 55 12 116 33 20 67.3 14.8 1. 50 2.00 1. 30 3.00 3.3 4.1 

GR- 96a 39 54 50 116 34 00 65.8 15.0 2.30 1.80 1.60 2.90 3.5 4.1 

GR-102a 40 49 20 117 26 40 64.7 15.9 1.70 2.10 2.10 4.00 3.7 3.0 

GR-103a 40 21 50 116 21 05 70.1 13.8 1.20 1.10 .91 1.30 3.6 4.8 

GR-105a 40 19 50 116 24 10 63.4 15.3 .80 1.70 2.90 5.00 4.0 3.8 

GR-107a 38 09 05 117 12 10 62.6 16.1 2.10 2.20 1.60 4.70 3.4 3.8 

GR-108a 38 09 05 117 11 50 63.7 16.3 2.70 1.80 1.60 s.oo 3.2 3.8 

GR-llla 38 34 24 116 53 OS 71.8 15.0 .57 1.00 .79 1.50 4.5 3.8 

GR-115a 39 43 20 119 42 35 69.4 15.5 1. 20 1.10 .82 2.40 4.1 3.4 

GR-124a 40 15 15 114 18 00 68.7 14.4 1.80 1.20 1.20 2.80 3.6 3.8 

GR-125a 40 20 30 114 33 30 60.8 16.9 2.60 1.50 1. 40 2.90 4.6 6.1 

GR-129a 36 20 15 117 28 30 53.7 18.5 4.00 3.90 3.50 7.70 3.9 3.1 

GR-133a 36 02 20 116 40 35 67.0 16.0 1.50 1. 30 1. 20 3.00 4.8 3.7 

GR-144a 35 18 50 115 32 50 69.7 16.4 1.10 .80 .78 2.60 4.9 3.3 

GR-156a 34 32 45 117 17 15 73.7 13.6 .88 .20 .22 1.30 3.6 4.6 

GR-166a 33 39 00 114 22 45 67.9 14.8 2.20 1.00 1.00 2.80 3.6 4.5 

GR-167a 33 27 20 115 08 00 62.0 15.8 3.20 2.20 2.40 4.60 3.6 3.0 

GR-178a 34 40 15 114 38 55 66.8 13.5 2.10 3.20 .54 2.70 2.9 5.3 

GR-185a 34 28 15 113 19 05 69.1 14.1 2.20 2.00 1.10 2.40 3.4 4.9 

GR-188a 36 15 50 114 09 15 66.9 14.0 4.20 1.40 1.10 2.80 3.1 4.0 

GR-195a 31 44 40 110 53 15 65.4 15.8 2.40 2.00 2.00 3.60 3.9 3.6 

GR-196a 31 44 00 110 52 55 75.0 11.9 1.10 .60 .61 1.30 3.0 4.7 

GR-203a 34 34 20 112 30 00 69.8 15.6 1. 20 1.50 .90 2.70 5.0 2.5 

GR-205a 37 56 25 115 36 00 72.8 13.3 1.30 .20 .22 1.00 3.6 5.0 

GR-206a 37 56 15 115 36 15 75.3 12.5 .87 .04 .11 .25 3.4 5.4 

GR-208a 33 39 00 110 34 15 70.9 13.1 1.80 1.20 .77 1.60 2.9 4.9 

GR-212a 33 02 20 111 43 25 71.5 14.9 .82 .76 .49 2.20 4.2 3.4 

GR-215a 32 25 55 111 32 55 73.3 13.0 .74 .64 .41 1.10 3.6 4.8 

GR-217a 32 17 30 111 09 45 58.1 16.2 2.90 3.70 3.50 5.90 3.8 2.8 

GR-218a 32 17 00 111 10 20 60.5 16.0 3.00 3.30 3.20 5.10 3.7 3.4 

GR-22la 32 50 15 112 08 50 74.1 12.8 .63 .64 .27 .95 3.1 5.0 

GR-224a 33 18 45 112 37 15 71.4 14.3 .92 1.10 .62 1.70 3.8 4.7 

GR-225a 33 11 50 112 38 55 70.2 13.3 1.70 1.40 .62 2.10 3.4 5.0 

16 Granitoid Rocks, Basin and Range Province 
Table 2. Rapid-rock analyses (in percent) of replicate samples of granitoid rocks 

from the Basin and Range province-Continued 

Sample H a+ 2 H

2

0- Ti02 P205 MnO co2 Cl F Total 

GR- 6a 0.62 0.24 0.43 0.17 o.os 0.13 0.03 0.08 99.45 

GR- lOa 1.60 1.20 .65 .27 .07 .08 <.01 .03 99.73 

GR- 11a 1.00 1.30 .65 .26 .07 .02 .01 .07 99.28 

GR- 18a 1.30 .25 .85 .34 .08 .01 .03 .10 99.46 

GR- 2la .53 .12 .30 .11 .OS .02 <.01 .05 100.30 

GR- 29a .73 .10 .38 .20 .10 .OS <.01 .04 99.71 

GR- 32a .72 .15 .86 .24 .08 .08 .04 .05 99.72 

GR- 43a .77 .07 .62 .22 .06 .01 .03 .OS 101.13 

GR- 46a .70 .10 .19 .06 .04 .02 .01 .1 0 100.59 

GR- 55a .45 .09 .18 .08 .09 .02 <.01 .02 100.54 

GR- 56a .62 .13 .42 .23 .05 .23 .01 .03 99.32 

GR- 72a .56 .21 .54 .19 .04 .08 <.01 .os 100.18 

GR- 75a .54 .OS .54 .16 .OS .04 <.01 .03 100.32 

GR- 79a 1.10 .21 .46 .17 .03 .06 <.01 .OS 98.89 

GR- 83a .77 .03 .22 .18 .03 .02 <.01 .04 99.00 

GR- 85a .82 .09 .47 .16 .03 .02 <.01 .06 98.56 

GR- 87a .45 .20 .60 .24 .04 .09 <.01 .03 99.26 

GR- 95a 1.20 .3_1 .53 .21 .os .os .02 .07 99.74 

GR- 96a .35 .15 .61 .20 .08 .04 .03 .07 98.53 

GR-102a .67 .29 .65 .28 .06 .08 .02 .07 99.32 

GR-103a 1.00 .28 .28 .11 <.01 .49 .02 .02 99.02 

GR-lOSa .55 .19 1.00 .28 .06 .03 .02 .08 99.11 

GR-107a 1.20 .05 .43 .21 .08 .20 .01 .04 98.72 

GR-108a .95 .13 .43 .23 .12 .11 <.01 .04 100.12 

GR-llla .43 .06 .29 .10 .OS .01 .02 .07 99.99 

GR-115a .62 .15 .34 .11 .08 .04 <.01 .03 99.30 

GR-124a .52 .28 .46 .20 .03 .12 .02 .OS 99.18 

GR-125a .45 .32 .81 .29 .06 .06 .04 .06 98.89 

GR-129a 1.20 .13 1.10 .52 .OS .05 .03 .12 101.50 

GR-133a .48 .09 .53 .19 .06 .08 .04 .04 100.01 

GR-144a .66 .14 .26 .08 .02 .02 .01 .05 100.82 

GR-156a .25 .26 .19 .08 <.01 .03 <.01 .04 98.96 

GR-166a <.01 .06 .43 .20 .06 .03 .02 .08 98.69 

GR-167a .64 .17 .62 .25 .10 .02 .02 .OS 98.67 

GR-178a .81 .23 .67 .20 .05 .60 .02 .28 99.90 

GR-185a .60 .06 .71 .27 .08 .01 <.Ol .16 101.10 

GR-188a .50 .27 1.00 .32 .06 .01 .02 .23 99.91 

GR-195a .58 .12 .61 .16 .09 <.01 .02 .04 100.33 

GR-196a .32 .09 .20 .08 .05 .02 .01 .02 99.00 

GR-203a .57 .12 .38 .15 .01 .08 <.01 .06 100.58 

GR-205a .47 .21 .25 .12 .02 .01 .01 .03 98.54 

GR-206a .68 .19 .13 .OS .01 .03 <.01 .03 99.00 

GR-208a .80 .17 .55 .16 .08 .06 .04 .12 99.15 

GR-212a .31 .10 .18 .13 .01 .04 <.01 .03 99.08 

GR-215a .66 .08 .22 .12 .04 .46 .01 .03 99.21 

GR-217a .87 .13 .96 .30 .07 .04 .04 .08 99.39 

GR-218a .67 .15 .94 .31 .04 .02 .03 .08 100.44 

GR-22la .72 .03 .25 .08 .03 <.Ol <.01 .08 98.69 

GR-224a .35 .04 .39 .10 .07 .01 <.01 .08 99.59 

GR-225a .44 (.01 .56 .24 .05 .03 <.01 .14 99.19 

Table 2 17 
Table 3. Rapid-rock norms for granitoid rocks in table 1 

[Norms could not be calculated for samples GR-148 and GR-192. Sample GR- 148 does not contain enough calcium 

to make the necessary fluorite, and sample GR-192 does not contain enough calcium to make the necessary apatite] 

Sample Q c OR AB AN HL wo EN FS MT 

GR- 1 6.41 o.o 28.03 32.30 11.81 0.03 3.87 7.79 0.66 5.41 

GR- 2 7.83 .o 30.65 35.92 9.47 .OS 1.88 5.83 .o 4.23 

GR- 3 31.92 1.22 21.72 34.49 5.97 .02 .o 1.58 .o 1.43 

GR- 4 30.62 .42 22.13 34.18 8.34 .02 .o 1.44 .13 1.45 

GR- 5 18.53 .o 19.64 30.53 14.93 .03 1.63 7.52 1.36 3.94 

GR- 6 23.32 .o 23.94 31.50 11.68 .05 .14 4.04 1.24 2.50 

GR- 7 13.74 .o 20.52 30.88 15.16 .05 3.06 7.63 1.16 5.33 

GR- 8 16.04 .o 23.99 30.77 14.06 .03 1.28 6.32 1.52 3.83 

GR- 9 20.05 .o 21.69 28.33 15.87 .03 .40 6.60 .37 4.14 

GR- 10 19.47 .o 22.39 27.66 16.06 .02 1.18 6.63 .o .o 

GR- 11 19.49 .o 23.31 28.91 15.50 .02 .52 5.43 .o 1.13 

GR- 12 17.72 .o 22.13 33.29 12.72 .03 1.76 5.96 .o 1.60 

GR- 13 8.10 .o 24.21 30.26 15.73 .02 2.26 8.42 2.67 4.31 

GR- 14 7.92 .o 27.68 29.85 13.39 .07 2.87 7.61 3.70 3.40 

GR- 15 26.92 .56 25.88 32.67 9.06 .02 .o 1. 45 .36 1.62 

GR- 16 34.82 .66 23.76 29.70 7.60 .02 .o .95 .04 1. 75 

GR- 17 14.83 .o 22.41 31.93 14.09 .03 1.77 6.38 .o 5.43 

GR- 18 15.23 .o 22.94 31.75 14.33 .OS 1.07 6.36 .33 5.18 

GR- 19 30.42 .58 23.19 27.17 12.51 .02 .o 2.08 1.05 1.75 

GR- 20 29.71 .o 23.99 26.55 12.70 .02 .18 2.10 1.35 2.06 

GR- 21 29.55 .74 21.10 33.60 9.15 .02 .o 1.55 1.41 1.78 

GR- 22 33.13 .14 21.70 31.86 8.90 .02 .o 1.37 .o 1.76 

GR- 23 26.61 .08 24.00 33.44 10.78 .02 .o 2.05 .81 1.31 

GR- 24 34.25 .31 20.48 31.84 9.03 .02 .o 1.75 .36 1.21 

GR- 25 33.62 1. 76 25.25 34.36 3.50 .02 .o .30 .o .41 

GR- 26 30.72 1.83 25.10 37.58 3.38 .02 .o .13 .o .34 

GR- 27 25.93 .35 20.34 31.62 14.65 .02 .o 2.42 .72 2.50 

GR- 28 27.90 .01 19.58 31.36 15.20 .02 .o 2.18 .62 2.04 

GR- 29 26.56 .06 21.36 27.96 15.14 .02 .o 3.25 1.47 2.77 

GR- 30 26.12 .40 21.64 29.12 14.02 .03 .o 3.29 1.52 2.51 

GR- 31 8.92 .o 9.68 33.64 22.30 .03 1.91 12.75 7.55 .61 

GR- 32 13.79 .o 12.54 33.11 20.00 .OS 2.49 8.81 5.20 1.61 

GR- 33 34.99 2.57 26.07 32.91 1.97 .02 .o .26 .o .41 

GR- 34 34.56 2.86 24.87 33.00 3.00 .02 .o .25 .38 .64 

GR- 35 30.69 .62 28.12 23.91 10.51 .02 .o 1.82 1.57 1.38 

GR- 36 30.68 .22 29.48 24.91 9.24 .02 .o 1.57 1.23 1.48 

GR- 37 22.67 .o 22.78 30.83 13.51 .02 .61 4.30 1.85 1.91 

GR- 38 20.96 .o 22.72 30.74 15.12 .02 .16 4.79 1.05 2.64 

GR- 39 28.00 .80 18.50 29.84 15.74 .02 .o 2.44 .51 2.78 

GR- 40 29.58 .56 23.15 29.68 12.27 .02 .o 1.65 .58 1.60 

GR- 41 26.13 .o 16.72 41.83 10.27 .02 .53 1. 49 .31 1.61 

GR- 42 29.94 .44 21.44 38.30 7.37 .02 .o .73 .o 1.28 

GR- 43 18.94 .o 22.90 30.84 14.49 .05 1. 51 4.83 .80 3.70 

GR- 44 19.28 .o 25.94 28.35 12.94 .03 .88 5.08 2.84 2.66 

GR- 45 35.70 .03 26.80 32.33 3.48 .02 .o .35 .o .81 

18 Granitoid Rocks, Basin and Range Province 
Table 3. Rapid-rock norms for granitoid rocks in table 1-:-Continued 

Sample HM IL TN RU AP FR cc MG 

GR- 1 o.o 2.30 o.o o.o 1.03 0.15 0.21 o.o 

GR- 2 .54 2.13 .o .o .92 .18 .37 .o 

GR- 3 .24 .48 .o .o .27 .06 .60 .o 

GR- 4 .o .so .o .o .38 .05 .35 .o 

GR- 5 .o 1.30 .o .o .41 .09 .07 .o 

GR- 6 .o .92 .o .o .46 .13 .12 .o 

GR- 7 .o 1.47 .o .o .75 .11 .14 .o 

GR- 8 .o 1.27 .o .o .63 .08 .18 .o 

GR- 9 .o 1. 30 .o .o .68 .07 .46 .o 

GR- 10 4.51 1.17 .10 .o .61 .04 .19 .o 

GR- 11 3.37 1.32 .o .o .69 .07 .24 .o 

GR- 12 2.75 1.28 .o .o .69 .03 .05 .o 

GR- 13 .o 2.14 .o .o 1.09 .02 .79 .o 

GR- 14 .o 2.13 .o .o 1.06 .15 .19 .o 

GR- 15 .o .56 .o .o .36 .08 .46 .o 

GR- 16 .o .40 .o .o .21 .05 .05 .o 

GR- 17 .46 1.62 .o .o .87 .12 .07 .o 

GR- 18 .o 1.57 .o .o .87 .14 .16 .o 

GR- 19 .o .75 .o .o .33 .12 .05 .o 

GR- 20 .o .85 .o .o .36 .10 .05 .o 

GR- 21 .o .60 .o .o .31 .08 .12 .o 

GR- 22 .21 .so .o .o .29 .08 .05 .o 

GR- 23 .o .44 .o .o .34 .04 .09 .o 

GR- 24 .o .37 .o .o .19 .03 .16 .o 

GR- 25 .30 .12 .o .o .29 .02 .05 .o 

GR- 26 .32 .08 .o .o .34 .04 .14 .o 

GR- 27 .o .77 .o .o .55 .04 .09 .o 

GR- 28 .o .67 .o .o .36 .OS .02 .o 

GR- 29 .o .78 .o .o .45 .05 .14 .o 

GR- 30 .o .75 .o .o .41 .03 .14 .o 

GR- 31 .o 1.50 .o .o .51 .02 .58 .o 

GR- 32 .o 1.67 .o .o .62 .08 .05 .o 

GR- 33 .28 .06 .o .o .36 .06 .05 .o 

GR- 34 .o .04 .o .o .21 .05 .14 .o 

GR- 35 .o .85 .o .o .29 .10 .14 .o 

GR- 36 .o .72 .o .o .29 .12 .05 .o 

GR- 37 .o .94 .o .o .43 .07 .07 .o 

GR- 38 .o 1.08 .o .o .60 .08 .05 .o 

GR- 39 .o .73 .o .o .48 .05 .11 .o 

GR- 40 .o .50 .o .o .33 .06 .02 .o 

GR- 41 .o .58 .o .o .41 .05 .07 .o 

GR- 42 .02 .25 .o .o .14 .03 .05 .o 

GR- 43 .o 1.20 .o .o .65 .08 .02 .o 

GR- 44 .o 1.24 .o .o .51 .13 .12 .o 

GR- 45 .17 .15 .o .o .10 .05 .02 .o 

Table 3 19 
Table 3. Rapid-rock norms for granitoid rocks in table 1-Continued 

Sample Q c OR AB AN HL wo EN FS MT 

GR- 46 33.54 0.89 28.33 30.14 4.44 0.02 o.o 0.61 0.20 0.93 

GR- 47 38.75 1.23 18.68 29.26 9.61 .02 .o .74 .o .50 

GR- 48 34.21 1. 3 7 19.42 32.00 9.66 .03 .o 1.13 .o .93 

GR- 49 38.53 .18 27.28 29.65 3.28 .02 .o .15 .o .26 

GR- 50 32.97 .20 25.68 33.27 5.37 .02 .o .83 .o .81 

GR- 51 23.21 .19 26.03 32.00 10.30 .02 .o 3.06 .65 2.67 

GR- 52 20.27 .o 25.36 34.51 10.84 .02 .68 3.05 .36 2.96 

GR- 53 33.54 1.22 32.61 30.98 .18 .03 .o .33 .o .19 

GR- 54 29.43 .55 30.78 34.42 .81 .03 .o .76 1.16 .92 

GR- 55 30.04 .08 22.86 37.83 5.51 .02 .o 1.37 .16 1.39 

GR- 56 23.93 .03 20.84 32.32 15.26 .02 .o 2.76 1.15 2.34 

GR- 57 18.32 .o 20.92 32.37 13.77 .03 2.06 7.05 1.52 2.05 

GR- 58 18.06 .o 20.61 31.89 14.38 .03 2.09 7.44 1.72 2.17 

GR- 59 19.97 .o 14.92 34.03 18.03 .03 .36 5.78 3.69 1.14 

GR- 60 21.58 .53 16.17 34.22 14.90 .02 .o 5.80 3.50 1. 28 

GR- 61 25.73 .o 27.72 28.32 10.35 .03 .10 3.56 2.11 .83 

GR- 62 19.03 .o 26.47 25.76 13.38 .02 1.40 7.10 3.37 1.33 

GR- 63 16.73 .o 15.00 33.43 19.37 .02 1.93 6.07 1.61 3.97 

GR- 64 17.05 .o 14.40 33.35 20.54 .03 1.75 6.32 .40 4.56 

GR- 65 15.38 .o 13.88 32.76 22.22 .02 1.66 6.36 2.52 3.26 

GR- 66 16.64 .o 13.80 32.50 23.24 .03 .35 6.07 3.72 2.06 

GR- 67 28.34 .71 22.76 26.51 11.05 .02 .o 2.78 1.48 3.53 

GR- 68 29.52 1.03 24.42 23.80 10.85 .02 .o 3.01 .99 4.09 

GR- 69 30.39 2.07 22.77 36.82 4.66 .02 .o .76 .o 1.24 

GR- 70 33.43 .96 24.63 33.47 5.60 .02 .o .35 .o .59 

GR- 71 20.13 .o 20.47 37.00 13.79 .02 .45 3.30 .58 2.66 

GR- 72 19.75 .o 20.79 35.64 14.31 .02 .38 4.26 .o 2.90 

GR- 73 47.33 8.06 34.29 3.52 .o .02 .o 1.66 .o 2.01 

GR- 74 31.08 1.06 32.31 23.92 5.85 .02 .o 1. 51 .91 1.91 

GR- 75 20.74 .o 15.52 37.55 16.16 .02 .61 4.03 1.04 2.64 

GR- 76 24.74 .o 18.06 34.40 13.86 .02 .68 3.55 .68 2.51 

GR- 77 21.69 .o 15.47 33.14 18.08 .02 1.33 4.26 1.31 3.21 

GR- 78 23.05 .27 17.74 32.10 18.14 .02 .o 3.74 1.46 2.18 

GR- 79 21.65 .o 14.52 39.76 14.66 .02 .38 4.33 1.21 1. 93 

GR- 80 21.46 .24 14.49 40.55 14.92 .02 .o 3.56 2.06 1.23 

GR- 81 29.21 .o 21.34 25.31 16.14 .03 .13 2.50 1.63 2.04 

GR- 82 30.15 .47 22.74 24.77 13.99 .02 .o 2.29 2.31 1. 61 

GR- 83 34.64 1.89 18.49 31.53 9.93 .02 .o .98 • 71 1.07 

GR- 84 26.07 .o 24.63 34.33 9.97 .02 .59 1.11 .55 1.92 

GR- 85 30.73 .87 21.01 27.44 13.05 .02 .o 2.07 1.85 1.33 

GR- 86 29.46 .76 20.89 28.13 13.08 .02 .o 2.31 2.30 1. 41 

GR- 87 19.49 .o 15.53 39.26 15.81 .02 .32 3.78 .o 3.65 

GR- 88 20.72 .o 16.00 38.96 15.94 .02 .44 3.25 .16 3.05 

GR- 89 23.99 .o 21.16 31.10 15.09 .02 .17 3.82 1.30 2.23 

GR- 90 23.13 .09 17.87 30.62 18.57 .02 .o 4.52 1.63 2.19 

20 Granitoid Rocks, Basin and Range Province 
Table 3. Rapid-rock norms for granitoid rocks in table 1-Continued 

Sample HM IL TN RU AP FR cc MG 

GR- 46 o.o 0.37 0.0 o.o 0.10 0.20 0.23 o.o 

GR- 47 .66 .21 .o .o .29 .04 .02 .o 

GR- 48 .49 .41 .o .o .24 .07 .OS .o 

GR- 49 .30 .19 .o .o .07 .04 .os .o 

GR- 50 .29 .35 .o .o .14 .OS .02 .o 

GR- 51 .o 1.03 .o .o .70 .09 .OS .o 

GR- 52 .o 1.16 .o .o .63 .12 .02 .o 

GR- 53 .54 .16 .o .o .10 .10 .02 .o 

GR- 54 .o .17 .o .o .19 .11 .65 .o 

GR- 55 .o .37 .o .o .29 .02 .07 .o 

GR- 56 .o .75 .o .o .41 .03 .18 .o 

GR- 57 .o .88 .o .o • 72 .09 .21 .o 

GR- 58 .o .97 .o .o .52 .1 0 .02 .o 

GR- 59 .o 1.11 .o .o .48 .07 .39 .o 

GR- 60 .o 1.04 .o .o .48 .03 .46 .o 

GR- 61 .o .72 .o .o .39 .10 .os .o 

GR- 62 .o 1. 31 .o .o .55 .19 .09 .o 

GR- 63 .o 1.27 .o .o .43 .OS .12 .o 

GR- 64 .o 1. 27 .o .o .26 .04 .02 .o 

GR- 65 .o 1.18 .o .o .58 .02 .19 .o 

GR- 66 .o 1.00 .o .o .41 .03 .14 .o 

GR- 67 .o 1.77 .o .o .77 .13 .16 .o 

GR- 68 .o 1.53 .o .o .ss .14 .OS .o 

GR- 69 .46 .35 .o .o .24 .13 .09 .o 

GR- 70 .47 .15 .o .o .24 .06 .02 .o 

GR- 71 .o .95 .o .o .51 .04 .09 .o 

GR- 72 .11 1. 24 .o .o .so .04 .07 .o 

GR- 73 .27 1.38 .o .o .64 .14 .46 .23 

GR- 74 .o .87 .o .o .36 .16 .OS .o 

GR- 75 .o 1.00 .o .o .48 .03 .18 .o 

GR- 76 .o .91 .o .o .39 .03 .19 .o 

GR- 77 .o .88 .o .o .ss .02 .OS .o 

GR- 78 .o .87 .o .o .38 .03 .02 .o 

GR- 79 .o .93 .o .o .51 .02 .07 .o 

GR- 80 .o .83 .o .o .58 .04 .02 .o 

GR- 81 .o 1.18 .o .o .33 .10 .07 .o 

GR- 82 .o 1.10 .o .o .38 .07 .09 .o 

GR- 83 .o .38 .o .o .24 .09 .OS .o 

GR- 84 .0 .39 .o .o .19 .OS .18 .o 

GR- 85 .o .91 .o .o .53 .06 .14 .o 

GR- 86 .0 .96 .o .o .45 .09 .14 .o 

GR- 87 .11 1.15 .o .o .69 .03 .16 .o 

GR- 88 .o .95 .o .o .43 .03 .OS .o 

GR- 89 .o .68 .o .o .39 .03 .02 .o 

GR- 90 .o .86 .o .o .41 .os .OS .o 

Table 3 21 
Table 3. Rapid-rock norms for granitoid rocks in table 1-Continued 

Sample Q c OR AB AN HL wo EN FS MT 

GR- 91 28.92 o.so 26.27 28.99 9.29 0.02 o.o 2.21 1.61 1. 01 

GR- 92 29.18 .28 27.51 32.47 6.10 .02 .o 1.49 .74 1.23 

GR- 93 13.49 .o 23.52 29.21 13.69 .03 2.48 8.64 2.38 3.11 

GR- 94 14.31 .o 24.09 34.27 13.44 .OS .31 5.84 1.91 3.10 

GR- 95 24.87 .53 23.49 27.44 14.53 .03 .o 3.55 1.60 2.36 

GR- 96 22.14 .o 26.46 29.06 12.74 .OS .33 3.55 1.40 2.36 

GR- 97 25.23 .76 19.13 30.45 15.84 .08 .o 2.77 2.73 1. 4 7 

GR- 98 24.78 .08 21.16 29.05 16.23 .08 .o 2.80 2.84 1.05 

GR- 99 24.06 .o 21.83 30.27 13.90 .03 1. 02 3.98 2.14 1.59 

GR-100 25.76 .o 20.42 30.88 14.73 .02 .19 3.54 1.35 1.92 

GR-101 19.58 .76 18.00 33.43 15.25 .02 .o 5.82 2.21 2.36 

GR-102 19.33 .o 18.11 32.69 17.09 .03 .79 5.34 1.21 3.11 

GR-103 30.13 2.34 27.13 29.20 4.38 .03 .o 2.36 1.43 1.33 

GR-104 27.38 .91 27.58 38.41 2.11 .os .o 1.57 .15 .69 

GR-105 13.26 .o 23.76 34.73 10.57 .03 4.93 7.51 .90 1. 37 

GR-106 5.66 .o 12.56 51.23 8.52 .03 5.51 10.59 1.90 1.07 

GR-107 19.12 .o 22.33 28.44 18.06 .02 .04 4.07 1.63 3.41 

GR-108 18.96 .o 22.94 28.45 18.88 .02 .94 3.82 1.03 3.41 

GR-109 25.02 .14 26.35 40.23 5.76 .02 .o .73 .o .59 

GR-110 28.50 .74 24.10 39.62 5.00 .02 .o .38 .o .13 

GR-111 28.09 1.81 22.12 38.45 5.85 .02 .o .96 .87 .94 

GR-112 25.58 .71 25.60 38.29 6.75 .02 .o .88 .25 1.04 

GR-113 20.38 .89 13.24 36.13 16.81 .02 .o 5.58 3.78 1.03 

GR-114 21.00 .64 13.75 36.73 16.33 .02 .o 5.29 3.06 1.36 

GR-115 24.11 .72 21.53 35.89 11.87 .02 .o 2.12 .23 2.20 

GR-116 18.06 .o 16.24 35.95 17.53 .OS 1.33 4.56 .56 3.98 

GR-117 26.52 1.20 27.44 32.39 8.53 .02 .o .88 .o 1.47 

GR-118 26.20 .88 24.76 31.91 10.95 .02 .o 1.45 .OS 2.37 

GR-119 26.33 .o 22.90 24.95 15.11 .02 .46 4.57 .o 3.00 

GR-120 25.12 .o 23.67 25.27 15.75 .03 .44 4.24 .o 2.89 

GR-121 24.79 .21 17.30 41.77 11.58 .02 .o 1.58 .o 1.79 

GR-122 28.62 .54 18.06 42.17 7.73 .02 .o .86 .o 1.05 

GR-123 28.22 .ss 24.02 31.74 8.47 .02 .o 2.78 .68 1.62 

GR-124 27.87 .21 22.18 31.69 11.11 .02 .o 3.03 .18 2.21 

GR-125 3.49 .o 37.91 38.47 10.10 .02 .44 3.55 .o 2.70 

GR-126 23.09 .46 24.55 30.71 10.54 .03 .o 3.53 .69 2.50 

GR-129 2.90 .o 18.04 31.71 23.86 .03 2.87 8.36 2.56 5.75 

GR-130 6.15 .o 19.31 29.95 21.00 .07 3.15 8.90 3.55 4.89 

GR-131 29.96 .91 30.63 30.66 4.48 .07 .o .78 .o .43 

GR-132 30.60 .o 27.68 31.73 5.73 .03 .18 1.32 .OS 1.62 

GR-133 18.84 .o 21.89 40.29 11.39 .08 .02 2.99 .31 2.47 

GR-134 25.28 .15 30.18 30.97 7.67 .Q3 .o 1.81 .85 1.78 

GR-135 22.55 .41 24.15 42.05 5.20 .07 .o 2.09 .o 1.48 

GR-136 23.01 .30 22.92 43.74 5.19 .07 .o 1.80 .o 1.00 

GR-137 24.55 .44 30.18 38.68 2.28 .07 .o 1.05 .o .16 

22 Granitoid Rocks, Basin and Range Province 
Table 3. Rapid-rock norms for granitoid rocks in table 1-Continued 

Sample HM IL TN RU AP FR cc MG 

GR- 91 o.o o. 77 0.0 0.0 0.24 0.13 0.05 o.o 

GR- 92 .o .so .o .o .29 .14 .OS .o 

GR- 93 .o 1.43 .o .0 1.02 .19 .79 .o 

GR- 94 .o 1.26 .o .o 1.11 .12 .19 .o 

GR- 95 .o 1.03 .o .o .46 .09 .02 .o 

GR- 96 .o 1.16 .o .o .63 .08 .05 .o 

GR- 97 .o .94 .o .o .43 .13 .02 .o 

GR- 98 .o 1.03 .o .o .63 .12 .14 .o 

GR- 99 .o .82 .o .o .28 .04 .02 .o 

GR-100 .o .69 .o .o .36 .03 .12 .o 

GR-101 .o 1. 20 .0 .o .79 .06 .53 .o 

GR-102 .o 1.30 .o .o .77 .05 .19 .o 

GR-103 .o .52 .o .o .29 .06 .79 .o 

GR-104 .o .42 .0 .o .34 .04 .35 .o 

GR-105 .o 1. 87 .o .o .76 .13 .18 .o 

GR-106 .o 1.92 .o .o .46 .15 .39 .o 

GR-107 .o .85 .o .o .73 .03 1. 28 .o 

GR-108 .o .78 .o .o .53 .02 .23 .o 

GR-109 .31 .40 .o .o • 29 .08 .07 .o 

GR-110 .59 .37 .o .o .34 .04 .19 .o 

GR-111 .o .so .o .o .22 .13 .OS .o 

GR-112 .o .48 .o .o .24 .15 .02 .o 

GR-113 .o .91 .o .o .56 .02 .65 .o 

GR-114 .o .85 .o .o .55 .02 .41 .o 

GR-115 .o .71 .o .o .38 .03 .18 .o 

GR-116 .o 1.02 .o .o .48 .03 .21 .o 

GR-117 .60 .42 .o .o .41 .03 .09 .o 

GR-118 .o .64 .o .o .56 .10 .12 .o 

GR-119 .78 1. 01 .o .o .46 .11 .30 .o 

GR-120 1.01 1.05 .o .o .40 .11 .02 .o 

GR-121 .08 .56 .o .o .26 .04 .02 .o 

GR-122 .10 .37 .o .o .36 .01 .12 .o 

GR-123 .o .79 .o .o .34 .06 .72 .o 

GR-124 .o .81 .o .o .43 .11 .14 .o 

GR-125 .68 1.59 .o .o .68 .28 .05 .o 

GR-126 .o 1.02 .o .o .77 .09 2.03 .o 

GR-129 .o 1.93 .o .o 1. 25 .15 .58 .o 

GR-130 .o 1.65 .o .o 1.09 .06 .23 .o 

GR-131 1.13 .39 .o .o .31 .02 .23 .o 

GR-132 .o .39 .o .o .29 .06 .32 .o 

GR-133 .o 1.03 .o .o .4 7 .05 .18 .o 

GR-134 .o .78 .o .o .34 .04 .14 .o 

GR-135 .62 .72 .o .o .31 .02 .35 .o 

GR-136 .64 .66 .o .o .34 .04 .30 .o 

GR-137 1. 39 .72 .0 .o .21 .17 .09 .o 

Table 3 23 
Table 3. Rapid-rock norms for granitoid rocks in table 1-Continued 

Sample Q c OR AB AN HL wo EN FS MT 

GR-138 25.13 0.30 30.76 37.69 1.96 0.07 o.o 1.09 o.o 1.07 

GR-139 17.78 .o 26.64 36.26 9.11 .03 .80 4.34 .o 1.81 

GR-140 16.90 .o 24.01 35.17 10.92 .02 1.05 5.57 .o 2.57 

GR-141 26.89 .o 29.77 39.07 2.34 .03 .03 .35 .o .51 

GR-142 29.45 .49 29.31 37.61 1.07 .02 .o .43 .o .43 

GR-143 25.66 .71 23.86 34.94 9.75 .02 .o 1.86 .o 1.33 

GR-144 21.42 .14 19.05 43.41 11.34 .02 .o 1.73 .87 1.10 

GR-145 31.49 .98 26.57 34.51 3.39 .02 .o 1.02 .o 1.03 

GR-146 32.63 .68 25.91 32.71 5.11 .02 .o 1.07 .o 1.05 

GR-147 34.43 .01 26.10 36.45 1.02 .02 .o .28 .o .46 

GR-149 27.41 .85 27.53 25.56 11.27 .03 .o 2.77 .51 2.64 

GR-150 26.45 .o 30.03 26.51 9.75 .03 .18 2.53 .62 2.51 

GR-151 23.10 .o 10.78 35.07 21.07 .02 1.18 3.53 .98 3.08 

GR-152 10.71 .o 7.73 30.59 29.35 .02 3.99 8.78 3.40 3.80 

GR-153 6.71 .o 29.31 40.18 16.51 .02 1.18 1.59 .31 2.79 

GR-154 3.26 .o 31.22 42.91 14.86 .02 1.40 1.39 .01 3.54 

GR-155 28.93 .57 22.65 32.36 10.14 .02 .o 1. 83 .o 1. 84 

GR-156 33.04 .24 28.12 29.91 6.73 .02 .o .so .o .13 

GR-157 33.19 .38 27.27 28.79 7.55 .02 .o .82 .09 1. 22 

GR-158 32.20 .71 27.30 28.82 7.77 .02 .o .83 .61 1.14 

GR-159 25.50 .o 22.69 31.56 12.45 .02 .OS 3.27 .58 2.34 

GR-160 24.99 .03 22.01 31.44 13.72 .02 .o 3.26 .49 2.63 

GR-161 21.80 .o 20.86 31.50 15.52 .02 .12 4.77 1.50 2.49 

GR-162 20.82 .o 19.55 32.16 15.84 .02 .76 4.99 1.66 2.62 

GR-163 36.42 1.83 34.92 23.20 .o .02 .o .69 .0 1.12 

GR-164 37.03 1.71 34.09 23.05 .04 .02 .o .73 .o .52 

GR-165 24.41 .o 26.21 28.00 13.58 .03 .22 3.01 .27 2.92 

GR-166 25.18 .o 27.17 29.24 11.33 .03 .35 2.54 .o 2.61 

GR-167 16.10 .o 18.15 31.97 18.94 .02 1.19 5.86 2.91 2.97 

GR-168 22.17 .o 22.62 32.31 13.33 .02 .53 4.01 1.36 2.19 

GR-169 12.37 .o 30.77 37.98 8.19 .03 .58 3.24 1.11 3.05 

GR-170 32.69 1.01 27.13 33.60 3.16 .02 .o .79 .01 .86 

GR-171 23.16 .o 17.53 30.21 18.75 .02 .61 3.31 1.75 2.82 

GR-172 23.00 .o 17.88 29.80 18.74 .02 .68 3. 77 2.00 2.63 

GR-173 30.28 .47 23.76 34.80 8.14 .02 .o .68 .17 1.06 

GR-174 29.96 .77 20.96 36.80 7. 71 .02 .o .83 .o 1.68 

GR-175 30.84 .29 26.05 33.83 7.32 .02 .o .so .o .65 

GR-176 32.33 .73 23.99 34.28 6.61 .02 .o .35 .o .75 

GR-177 26.45 .63 24.91 23.41 11.27 .02 .o 1. 56 3.80 3.73 

GR-178 24.73 .o 32.15 23.72 7.36 .03 1.04 1.91 3.06 3.21 

GR-179 24.63 .o 19.06 41.64 9.36 .03 .32 1. 83 .56 1.45 

GR-180 25.87 .94 18.98 43.24 7.75 .02 .o 1.05 .o .97 

GR-181 19.91 .37 41.46 26.60 5.77 .02 .o 1. 67 .o 2.07 

GR-182 29.23 .o 37.14 26.44 2.26 .03 .82 .88 .o .95 

GR-183 34.93 1.65 27.59 25.69 6.02 .02 .o 1.06 .o 1. 42 

24 Granitoid Rocks, Basin and Range Province 
Table 3. Rapid-rock norms for granitoid rocks in table 1-Continued 

Sample HM IL TN RU AP FR cc MG 

GR-138 0.59 0.66 0.0 0.0 0.31 0.19 0.19 0.0 

GR-139 1.01 1.28 .o .o .56 .13 .26 .o 

GR-140 .87 1.45 .o .o .70 .13 .65 .o 

GR-141 .56 .33 .o .o .05 .04 .05 .o 

GR-142 .52 .23 .o .o .07 .14 .23 .o 

GR-143 .70 .75 .o .o .33 .08 .02 .o 

GR-144 .o .54 .o .0 .26 .10 .02 .o 

GR-145 .02 .41 .o .o .17 .05 .37 .o 

GR-146 .12 .37 .o .o .17 .03 .14 .o 

GR-147 .79 .19 .o .o .02 .14 .09 .o 

GR-149 .o .81 .o .o .34 .10 .18 .o 

GR-150 .o .71 .o .o .41 .09 .16 .o 

GR-151 .o .75 .o .o .36 .03 .05 .o 

GR-152 .o 1.09 .o .o .43 .05 .07 .o 

GR-153 .o .81 .o .o .29 .12 .18 .o 

GR-154 .o .89 .o .o .36 .06 .09 .o 

GR-155 .14 .86 .o .o .55 .08 .02 .o 

GR-156 .66 .37 .o .o .24 .02 .02 .o 

GR-157 .o .34 .o .o .17 .09 .05 .o 

GR-158 .o .36 .o .o .17 .05 .02 .o 

GR-159 .o .84 .o .o .36 .08 .25 .o 

GR-160 .o .80 .o .o .36 .08 .18 .o 

GR-161 .o .84 .o .o .36 .06 .18 .o 

GR-162 .o .97 .o .o .38 .05 .18 .o 

GR-163 .75 .41 .o .o .22 .21 .oo .21 

GR-164 1.77 .35 .o .o .19 .21 .30 .o 

GR-165 .o .86 .o .o .36 .08 .05 .o 

GR-166 .24 .80 .o .o .31 .14 .05 .o 

GR-167 .o 1.15 .o .o .53 .06 .14 .o 

GR-168 .o .98 .o .o .33 .08 .07 .o 

GR-169 .0 1.84 .o .o .71 .09 .02 .o 

GR-170 .o .33 .o .o .22 .03 .16 .o 

GR-171 .o .89 .o .o .70 .01 .23 .o 

GR-172 .o .90 .o .o .so .02 .07 .o 

GR-173 .o .34 .o .o .17 .07 .05 .o 

GR-174 .16 .46 .o .o .26 .04 .35 .o 

GR-175 .07 .21 .o .o .14 .03 .05 .o 

GR-176 .41 .19 .o .o .19 .03 .12 .o 

GR-177 .o 1. 85 .o .o .83 .02 1.52 .o 

GR-178 .o 1.40 .o .o .41 .40 .57 .o 

GR-179 .o .67 .o .o .19 .13 .14 .o 

GR-180 .44 .34 .o .o .17 .07 .18 .o 

GR-181 .41 1.14 .o .o .31 .23 .05 .o 

GR-182 1. 07 .77 .o .o .17 .22 .02 .o 

GR-183 .44 .46 .o .o .34 .08 .30 .o 

Table 3 25 
Table 3. Rapid-rock norms for granitoid rocks in table 1-Continued 

Sample Q c OR AB AN HL wo EN FS MT 

GR-184 36.82 2.19 29.58 25.85 2.31 0.02 0.0 0.56 o.o o.o 

GR-185 27.23 .38 28.64 26.41 8.65 .02 .o 2.29 .71 3.22 

GR-186 31.31 1.11 32.52 27.52 3.39 .02 .o .79 .58 1.63 

GR-187 27.45 .so 33.74 24.01 5.49 .03 .o 2.18 .12 3.70 

GR-188 26.88 1.37 24.08 27.43 8.87 .03 .o 2.79 1.98 3.40 

GR-189 35.09 .62 30.80 19.82 6.98 .02 .o .81 .o 3.46 

GR-190 29.43 .19 30.43 23.77 8.32 .03 .o 1. 38 1. 94 2.49 

GR-191 37.57 1.71 27.66 31.79 .19 .02 .o .OS .o .o 

GR-193 33.33 .76 29.73 33.13 .90 .02 .o .20 .o 1.14 

GR-194 31.55 .11 29.81 33.22 2.70 .02 .o .35 .o .88 

GR-195 17.35 .o 22.52 32.95 14.50 .03 1. 66 5.00 1.08 3.20 

GR-196 35.61 .o 27.15 26.97 6.73 .02 .01 1.44 .o 1.30 

GR-197 24.81 .03 28.93 25.29 11.04 .02 .o 2.44 2.15 2.61 

GR-198 26.00 .60 26.61 25.91 8.46 .02 .o 2.52 2.50 3.26 

GR-199 29.33 .63 20.27 34.93 10.36 .02 .o 1.53 .84 1.24 

GR-200 28.30 .84 23.44 35.21 7.83 .02 .o 1.29 .58 1.45 

GR-201 29.33 1.60 25.37 27.60 7.07 .02 .o 2.55 .65 3.11 

GR-202 26.82 .42 28.25 28.33 7.47 .02 .o 2.79 .66 2.80 

GR-203 24.37 .97 13.83 43.83 10.49 .02 .o 2.33 1.12 1.77 

GR-204 24.45 .26 15.43 39.87 12.62 .02 .o 2.75 1.00 2.48 

GR-205 31.95 .93 29.61 31.08 3.56 .02 .o .53 .o .21 

GR-206 35.32 1.67 31.86 29.19 .68 .02 .o .13 .01 .62 

GR-207 33.02 .88 31.42 23.93 4.63 .07 .o 2.01 .44 2.08 

GR-208 31.63 .91 30.94 24.41 5.64 .07 .o 2.13 .09 2.63 

GR-209 25.45 .55 21.63 39.50 9.19 .02 .o .99 .o 1.48 

GR-210 27.43 1.17 19.66 39.16 8.84 .02 .o 1.13 .o 1.21 

GR-211 29.81 .22 16.58 36.38 13.10 .02 .o 1.45 .56 1.25 

GR-212 29.70 .so 20.61 33.66 11.55 .02 .o 1.54 .13 1.59 

GR-213 27.95 .58 18.95 30.45 15.17 .02 .o 2.75 .21 2.76 

GR-214 23.84 .o 17.96 31.64 18.19 .02 .01 3.28 .70 3.08 

GR-215 32.98 2.00 27.09 31.82 2.22 .02 .o 1.19 .22 1.15 

GR-216 30.67 .22 27.62 31.06 6.56 .02 .o 1.36 .06 1.40 

GR-217 7.63 .o 18.11 32.54 18.84 .07 3.36 9.16 2.28 5.18 

GR-218 10.03 .o 19.88 33.42 16.57 .os 2.98 8.13 2.24 4.14 

GR-219 15.33 .o 19.78 35.97 17.25 .02 .40 4.04 2.54 2.65 

GR-220 37.49 .21 30.20 23.59 5.99 .03 .o .65 .25 .94 

GR-221 35.27 .62 31.31 25.79 4.02 .02 .o .61 .28 1.02 

GR-222 35.95 .54 28.90 26.65 4.69 .02 .o .81 .22 1.29 

GR-223 34.04 1.06 26.90 29.88 5.08 .02 .o 1.01 .34 .92 

GR-224 26.37 .90 28.24 33.48 5.91 .02 .o 1.49 .58 1.62 

GR-225 28.93 .o 30.69 27.50 5.92 .02 .66 1. 65 .o 2.73 

GR-226 30.83 .74 28.24 28.31 6.02 .02 .o 1.70 .42 2.06 

GR-227 36.62 .34 32.64 26.76 1.77 .02 .o .36 .o .44 

GR-228 36.60 1.37 31.92 27.52 .47 .02 .o .25 .o .44 

GR-229 31.29 .23 23.74 39.87 3.91 .02 .o .13 .o .33 

GR-230 31.59 .so 24.45 40.06 2.34 .02 .o .03 .o .18 

26 Granitoid Rocks, Basin and Range Province 
Table 3. Rapid-rock norms for granitoid rocks in table 1-Continued 

Sample HM IL TN RU AP FR cc MG 

GR-184 1.74 0.28 o.o 0.04 0.48 0.03 0.12 o.o 

GR-185 .o 1.32 .o .o .72 .32 .09 .o 

GR-186 .o .45 .o .o .27 .31 .12 .o 

GR-187 .o 1.49 .o .o .58 .69 _.02 .o 

GR-188 .o 1. 93 .o .o .77 .42 .05 .o 

GR-189 .68 1.32 .o .o .34 .04 .02 .o 

GR-190 .o 1.17 .o .o .38 .43 .05 .o 

GR-191 .50 .11 .o .02 .22 .03 .14 .o 

GR-193 .o .38 .o .o .17 .13 .11 .o 

GR-194 .51 .36 .o .o .19 .23 .07 .o 

GR-195 .o 1.22 .o .o .43 .05 .02 .o 

GR-196 .10 .44 .o .o .17 .03 .05 .o 

GR-197 .o 1. 73 .0 .o .71 .21 .05 .o 

GR-198 .o 1.92 .o .o .90 .25 1.05 .o 

GR-199 .o .46 .o .o .26 .08 .05 .o 

GR-200 .o .42 .o .o .48 .05 .09 .o 

GR-201 .o 1. 32 .o .o .63 .35 .40 .o 

GR-202 .o 1.43 .o .o .55 .40 .07 .o 

GR-203 .o .71 .o .o .27 .10 .19 .o 

GR-204 .o .67 .o .o .29 .08 .09 .o 

GR-205 1.19 .45 .o .o .22 .07 .19 .o 

GR-206 .o .29 .o .o .14 .03 .05 .o 

GR-207 .o .85 .o .o .36 .16 .14 .o 

GR-208 .o .94 .o .o .29 .23 .09 .o 

GR-209 .10 .42 .o .o .39 .07 .21 .o 

GR-210 .37 .44 .o .o .29 .10 .18 .o 

GR-211 .o .36 .o .o .19 .05 .05 .o 

GR-212 .o .44 .o .o .21 .05 .02 .o 

GR-213 .o .72 .o .o .31 .04 .09 .o 

GR-214 .o .79 .o .o .38 .05 .05 .o 

GR-215 .o .37 .o .o .19 .05 .70 .o 

GR-216 .o .38 .o .o • 21 .07 .36 .o 

GR-217 .o 1. 94 .o .o .75 .09 .05 .o 

GR-218 .o 1.67 .o .o .72 .13 .05 .o 

GR-219 .o 1.19 .o .o .50 .11 .23 .o 

GR-220 .o .30 .o .o .12 .07 .14 .o 

GR-221 .o .54 .o .o .39 .12 .02 .o 

GR-222 .o .48 .o .o .29 .15 .02 .o 

GR-223 .o .46 .o .o .14 .13 .02 .o 

GR-224 .o .81 .o .o .41 .09 .07 .o 

GR-225 .26 .95 .o .o .43 .24 .02 .o 

GR-226 .o .98 .o .o .36 .22 .09 .o 

GR-227 .63 .25 .o .o .12 .03 .02 .o 

GR-228 .82 .27 .o .o .17 .03 .12 .o 

GR-229 .34 .04 .o .o .05 .04 .02 .o 

GR-230 .47 .10 .o .o .12 .03 .11 .o 

Table 3 27 
Table 4. Rapid-rock norms for replicate samples of granitoid rocks in table 2 

Sample Q c OR AB AN HL wo EN FS 

GR- 6a 23.36 o.o 22.79 33.26 11.11 0.05 0.22 3.79 0.95 

GR- lOa 20.00 .o 21.95 26.99 16.10 .02 1. 69 6.68 .o 

GR- 11a 20.91 .30 22.55 28.73 15.16 .02 .o 5.65 .o 

GR- 18a 15.03 .o 22.34 31.77 14.64 .05 1.58 6.36 .10 

GR- 2la 28.95 .20 20.76 34.75 9.81 .02 .o 1.57 1.55 

GR- 29a 26.37 .o 22.12 30.74 10.45 .02 1. 38 3.53 1.39 

GR- 32a 14.17 .o 11.96 33.10 20.37 .07 2.27 8.57 5.41 

GR- 43a 17.11 .o 21.81 32.69 15.85 .05 1.14 5.22 1. 47 

GR- 46a 33.23 .90 27.25 30.47 5.25 .02 .o .70 .61 

GR- 55a 31.03 .88 21.87 37.16 5. 71 .02 .o 1.12 .29 

GR- 56a 23.07 .22 20.99 31.69 15.55 .02 .o 3.03 .86 

GR- 72a 21.65 .15 21.40 33.98 13.97 .02 .o 4.01 .02 

GR- 75a 20.68 .o 15.41 38.11 15.32 .02 1.11 4.00 1.21 

GR- 79a 20.32 .o 14.54 40.69 15.06 .02 .40 4.34 1.19 

GR- 83a 33.87 1.64 19.26 31.81 9.61 .02 .o .91 .72 

GR- 85a 26.08 .13 22.40 30.26 13.19 .02 .o 2.55 2.28 

GR- 87a 18.08 .o 17.98 38.55 15.12 .02 1.16 3.79 .o 

GR- 95a 24.74 .27 24.67 28.29 13.06 .03 .o 3.30 1.68 

GR- 96a 22.34 .29 24.72 30.00 12.70 .05 .o 4.07 ;56 

GR-102a 20.92 .31 18.03 31.69 17.47 .03 .o 5.32 1.52 

GR-103a 28.82 1.81 29.02 31.02 2.62 .03 .o 2.32 .60 

GR-105a 13.61 .o 22.84 34.27 12.86 .03 4.13 7.35 .94 

GR-107a 17.39 .o 23.04 29.45 17.94 .02 1.30 4.09 1.79 

GR-108a 19.19 .o 22.68 27.27 19.12 .02 1.49 4.02 .59 

GR-11la 26.99 1.22 22.58 38.13 6.31 .03 .o 1.98 .98 

GR-115a 26.83 1.15 20.39 35.14 10.95 .02 .o 2.07 .63 

GR-124a 26.96 .15 22.83 30.82 11.78 .03 .o 3.04 .01 

GR-125a 4.70 .o 36.75 39.38 7.76 .07 1.81 3.55 .o 

GR-129a .61 .o 18.30 32.74 23.91 .05 4.18 8.71 2.13 

GR-133a 18.02 .o 21.99 40.56 11.41 .07 .68 3.01 .39 

GR-144a 22.23 .41 19.50 41.39 11.94 .02 .o 1.94 .17 

GR-156a 33.02 .71 27.61 30.87 5.58 .02 .o .56 .o 

GR-166a 23.73 .o 26.97 30.75 11.17 .03 .39 2.53 .o 

GR-167a 17.81 .o 18.12 30.98 18.57 .03 1.15 6.11 .57 

GR-178a 25.08 .69 31.72 24.70 6.46 .03 .o 1.36 3.17 

GR-185a 24.65 .o 28.85 28.59 8.75 .02 .13 2.73 .83 

GR-188a 27.86 .85 23.87 26.34 10.36 .03 .o 2.77 .o 

GR-195a 18.92 .o 21.36 32.98 15.11 .03 .63 5.00 .85 

GR-196a 36.88 .o 28.17 25.68 5.24 .02 .23 1.54 .o 

GR-203a 24.37 .44 14.79 42.29 11.58 .02 .o 2.24 1.16 

GR-205a 31.41 .54 30.20 31.06 4.06 .02 .o .56 .o 

GR-206a 35.18 .90 32.52 29.25 .55 .02 .o .28 .o 

GR-208a 32.47 1.00 29.51 24.71 5.85 .07 .o 1.95 .o 

GR-212a 29.39 .79 20.37 35.95 9.81 .02 .o 1. 24 .45 

GR-215a 33.12 1.32 28.81 30.86 1.65 .02 .o 1.04 .28 

GR-217a 9.21 .o 16.82 32.39 19.35 .07 3.24 8.86 2.99 

GR-218a 11.83 .o 20.18 31.22 17.20 .OS 2.37 8.00 2.11 

GR-221a 35.64 1.01 30.18 26.71 3.67 .02 .o .69 .30 

GR-224a 27.22 .34 28.01 32.35 7.26 .02 .o 1.56 .77 

GR-225a 27.58 .o 29.94 29.08 6.38 .02 .63 1. 56 .34 

28 Granitoid Rocks, Basin and Range Province 
Table 4. Rapid-rock norms for replicate samples of granitoid rocks-Continued 

Sample MT HM IL RU AP FR cc 

GR- 6a 2.80 o.o 0.83 o.o o. 41 0.14 0.30 

GR- lOa .02 4.42 1.27 .o .66 .01 .19 

GR- 11a 1.62 3.01 1.27 .o .64 .10 .OS 

GR- 18a 5.48 .o 1.65 .o .82 .15 .02 

GR- 2la 1.43 .o .57 .o .26 .08 .OS 

GR- 29a 2.64 .o .73 .o .48 .OS .12 

GR- 32a 1. 61 .o 1. 65 .o .58 .06 .18 

GR- 43a 2.89 .o 1.17 .o .52 .06 .02 

GR- 46a .83 .o .36 .o .14 .20 .OS 

GR- SSa 1.32 .o .34 .o .19 .03 .OS 

GR- 56a 2.65 .o .81 .o .ss .02 .53 

GR- 72a 3.06 .o 1.03 .o .45 .07 .18 

GR- 7Sa 2.62 .o 1. 03 .o .38 .03 .09 

GR- 79a 1. 93 .o .90 .o .41 .07 .14 

GR- 83a 1.21 .o .43 .o .43 .OS .05 

GR- 85a 1.63 .o .91 .o .39 .10 .OS 

GR- 87a 3. 27 .08 1.16 .o .58 .02 .21 

GR- 95a 2.21 .o 1.03 .o .51 .11 .12 

GR- 96a 3.40 .o 1.18 .o .48 .11 .09 

GR-102a 2.51 .o 1.26 .o .67 .09 .19 

GR-103a 1. 78 .o .54 .o .27 .02 1.14 

GR-lOSa 1.18 .o 1.93 .o .67 .12 .07 

GR-107a 3.12 .o .84 .o .51 .04 .47 

GR-108a 3.95 .o .82 .o .55 .04 .25 

GR-11la .83 .o .ss .o .24 .13 .02 

GR-115a 1. 77 .o .66 .o .26 .04 .09 

GR-124a 2.65 .o .89 .o .48 .07 .28 

GR-125a 2.73 .76 1.57 .o .70 .07 .14 

GR-129a 5.79 .o 2.09 .o 1.23 .15 .11 

GR-133a 2.19 .o 1.01 .o .45 .OS .18 

GR-144a 1. 59 .o .49 .o .19 .09 .OS 

GR-156a .13 .81 .37 .o .19 .07 .07 

GR-166a 2.20 .71 .83 .o .48 .13 .07 

GR-167a 4.74 .o 1.20 .o .61 .06 .05 

GR-178a 3.08 .o 1.29 .o .48 .ss 1.38 

GR-185a 3.18 .o 1.34 .o .64 .28 .02 

GR-188a 1. 83 2.98 1. 92 .o .77 .42 .02 

GR-195a 3.49 .o 1.16 .o .38 .OS .02 

GR-196a 1. 54 .as .39 .0 .19 .03 .OS 

GR-203a 1.74 .o .72 .o .36 .10 .18 

GR-205a .o 1.33 .48 .01 .29 .04 .02 

GR-206a .o .89 .11 .08 .12 .OS .07 

GR-208a 2.58 .05 1.06 .o .39 .22 .14 

GR-212a 1.21 .o .35 .o .31 .04 .09 

GR-215a 1.09 .o .42 .o .29 .04 1. 06 

GR-217a 4.28 .o 1.85 .o .72 .11 .09 

GR-218a 4.37 .o 1. 79 .o .74 .11 .OS 

GR-22la .93 .o .48 .o .19 .15 .02 

GR-224a 1. 35 .o .75 .o .24 .15 .02 

GR-225a 2.50 .o 1.08 .o .58 .25 .07 

Table 4 29 
Table 5. Plate-reader semiquantitative emiSSIOn spec- Table 5. Plate-reader semiquantitative emission spectrographic analyses (in parts per million) of granitoid trographic analyses (in parts per million) of granitoid 

rocks from the Basin and Range province rocks-Continued 

Sample Ag B Be Co Cr Cu La Sample Mo Nb Ni Pb Sc Sn v w 

GR- 1 (0.46 20.0 2.7 24.00 50.00 68.00 96.0 GR- 1 5.3 24.0 31.0 27.0 21.0 <4.6 150.0 <46 

GR- 2 <.46 49.0 2.8 16.00 38.00 70.00 120.0 GR- 2 4.1 37.0 24.0 23.0 17.0 <4.6 110.0 <46 

GR- 3 <.46 <S.O 2.3 s.so 10.00 2.30 53.0 GR- 3 1.5 43.0 5.4 26.0 4.5 <4.6 25.0 (46 

GR- 4 (.46 <S.O 2.3 4.70 9.20 .46 49.0 GR- 4 <1.0 43.0 4.8 21.0 4.0 <4.6 23.0 <46 

GR- 5 <.46 6.9 1.3 22.00 81.00 ss.oo so.o GR- 5 5.2 9.5 36.0 .o 19.0 <4.6 130.0 <46 

GR- 6 <.46 (5.0 1.6 13.00 23.00 11.00 65.0 GR- 6 2.5 13.0 12.0 17.0 13.0 s.o 86.0 <46 

GR- 7 <.46 8.1 (1.0 21.00 26.00 55.00 48.0 GR- 7 3.7 22.0 18.0 16.0 19.0 <4.6 160.0 <46 

GR- 8 .59 6.2 (1.0 22.00 33.00 51.00 74.0 GR- 8 5.3 15.0 23.0 31.0 14.0 <4.6 150.0 <46 

GR- 9 <.46 <S.O (1.0 19.00 46.00 30.00 72.0 GR- 9 2.4 12.0 26.0 18.0 17.0 <4.6 130.0 <46 

GR- 10 <.46 6.4 (1.0 18.00 39.00 34.00 71.0 GR- 10 2.1 18.0 26.0 20.0 16.0 <4.6 99.0 <46 

GR- 11 <.46 (5.0 (1.0 20.00 48.00 38.00 77.0 GR- 11 3.3 16.0 29.0 21.0 17.0 <4.6 120.0 <46 

GR- 12 <.46 <S.O (1.0 18.00 40.00 47.00 69.0 GR- 12 2.7 13.0 24.0 22.0 16.0 <4.6 110.0 <46 

GR- 13 <.46 32.0 2.2 24.00 48.00 56.00 80.0 GR- 13 3.9 26.0 30.0 25.0 17.0 <4.6 180.0 <46 

GR- 14 <.46 34.0 2.5 24.00 50.00 49.00 100.0 GR- 14 5.3 23.0 30.0 25.0 23.0 <4.6 160.0 <46 

GR- 15 <.46 <S.O 1.2 3.00 3.90 .70 50.0 GR- 15 <1.0 13.0 2.9 13.0 4.0 <4.6 17.0 <46 

GR- 16 <.46 <S.O 1.8 3.20 3.30 4.90 46.0 GR- 16 <1.0 29.0 2.5 24.0 2.5 <4.6 13.0 <46 

GR- 17 <.46 22.0 <1.0 18.00 17.00 26.00 62.0 GR- 17 2.4 11.0 12.0 14.0 16.0 <4.6 120.0 (46 

GR- 18 <.46 (5.0 (1.0 17,.00 20.00 3.20 71.0 GR- 18 3.1 15.0 11.0 14.0 16.0 <4.6 130.0 <46 

GR- 19 <.46 <S.O (1.0 4.30 4.60 .69 45.0 GR- 19 <1.0 15.0 2.0 13.0 4.2 <4.6 25.0 <46 

GR- 20 <.46 <S.O 1.6 6.10 7.50 .81 78.0 GR- 20 1.1 35.0 3.1 18.0 8.7 <4.6 39.0 <46 

GR- 21 <.46 <S.O 2.5 6.20 6.30 1.60 84.0 GR- 21 1.2 46.0 4.9 42.0 4.6 <4.6 22.0 <46 

GR- 22 <.46 <S.O 1. 7 4.30 3.90 16.00 51.0 GR- 22 1.0 53.0 3.9 37.0 3.1 <4.6 18.0 <46 

GR- 23 <.46 <S.O 1.2 5.70 10.00 1.20 37.0 GR- 23 1.0 18.0 9.3 16.0 4.7 <4.6 24.0 <46 

GR- 24 <.46 (5.0 1.4 4.60 8.90 2.20 29.0 GR- 24 <1.0 20.0 7.5 20.0 3.1 <4.6 20.0 <46 

GR- 25 <.46 <S.O 5.3 1.10 2.20 <.22 19.0 GR- 25 (1.0 37.0 2.5 31.0 2.2 <4.6 2.9 <46 

GR- 26 <.46 (5.0 74.0 <.46 2.00 .so 26.0 GR- 26 (1.0 45.0 2.8 27.0 2.5 5.2 2.4 <46 

GR- 27 <.46 (5.0 1.3 5.30 3.30 .67 44.0 GR- 27 1.7 33.0 3.5 9.0 5.9 <4.6 45.0 <46 

GR- 28 <.46 (5.0 (1.0 4.40 4.90 .25 36.0 GR- 28 1.1 16.0 3.3 9.1 4.8 <4.6 38.0 <46 

GR- 29 <.46 <S.O 1.9 8.10 7.90 s.oo 42.0 GR- 29 1.9 30.0 5.2 15.0 8.6 <4.6 65.0 <46 

GR- 30 <.46 (5.0 1.3 7.40 6.50 1.70 44.0 GR- 30 2.1 20.0 5.1 15.0 6.6 <4.6 75.0 <46 

GR- 31 <.46 17.0 <1.0 30.00 160.00 24.00 25.0 GR- 31 3.8 9.1 130.0 15.0 26.0 <4.6 180.0 <46 

GR- 32 <.46 24.0 (1.0 15 .• 00 32.00 20.00 29.0 GR- 32 3.3 17.0 18.0 13.0 16.0 <4.6 170.0 <46 

GR- 33 <.46 17.0 2.0 .80 1.90 (.22 18.0 GR- 33 <1.0 32.0 3.5 25.0 6.1 <4.6 1.6 <46 

GR- 34 <.46 <S.O 1.8 <.46 3.00 <.22 19.0 GR- 34 1.2 23.0 4.1 28.0 4.0 s.o 2.9 <46 

GR- 35 <.46 <S.O 1.4 6.50 5.30 .95 180.0 GR- 35 2.9 25.0 8.1 17.0 6.2 <4.6 33.0 <46 

GR- 36 <.46 <S.O 1.2 4.00 3.90 1.30 110.0 GR- 36 1.0 17.0 3.5 14.0 4.0 <4. 6 20.0 <46 

GR- 37 <.46 <S.O 2.2 9.90 17.00 39.00 52.0 GR- 37 1.7 24.0 12.0 21.0 10.0 <4.6 71.0 <46 

GR- 38 <.46 14.0 2.7 11.00 26.00 s.oo 54.0 GR- 38 1.8 24.0 13.0 16.0 12.0 <4.6 66.0 <46 

GR- 39 <.46 <S.O 1.4 5.70 3.50 5.10 36.0 GR- 39 1.2 13.0 3.4 14.0 4.7 <4.6 43.0 <46 

GR- 40 <.46 (5.0 1. 7 4.40 3.80 3.50 29.0 GR- 40 2.3 29.0 7.5 25.0 4.5 <4.6 32.0 <46 

GR- 41 <.46 (5.0 (1.0 4.50 2.80 4.90 19.0 GR- 41 1. 2 9.2 2.4 14.0 3.0 <4.6 26.0 <46 

GR- 42 <.46 (5.0 1.1 1.60 2.00 2.50 35.0 GR- 42 <1.0 5.6 2.3 19.0 1.9 <4.6 8.0 (46 

GR- 43 <.46 <S.O <1.0 8.80 9.40 3.90 43.0 GR- 43 1.8 7.5 4.6 14.0 7.6 (4.6 84.0 <46 

GR- 44 <.46 (5.0 <1.0 11.00 20.00 2.30 46.0 GR- 44 2.3 8.0 6.2 16.0 13.0 <4.6 95.0 <46 

GR- 45 <.46 (5.0 2.5 .96 1.50 .51 7.2 GR- 45 (1.0 80.0 2.0 42.0 3.7 5.9 3.4 <46 

GR- 46 <.46 <S.O 2.8 2.40 3.90 2.10 49.0 GR- 46 <1.0 54.0 3.0 31.0 4.2 s.s 9.5 <46 

GR- 47 (.46 <S.O 1.5 1.40 2.20 <.22 38.0 GR- 47 (1.0 7.3 2.4 17.0 1.8 <4.6 10.0 <46 

GR- 48 <.46 <S.O 2.1 1.70 3.20 .24 58.0 GR- 48 <1.0 13.0 2.4 20.0 2.6 <4.6 13.0 <46 

GR- 49 <.46 <S.O (1.0 .79 1.60 .64 20.0 GR- 49 (1.0 22.0 <1.0 7.5 1.5 <4.6 s.o <46 

GR- 50 <.46 <S.O 1. 9 2.20 3.70 (.22 31.0 GR- 50 <1.0 37.0 2.8 17.0 2.1 <4.6 12.0 <46 

30 Granitoid Rocks, Basin and Range Province 
Table 5. Plate-reader semiquantitative emiSSIOn spec- Table 5. Plate-reader semiquantitative emission spectrographic analyses (in parts per million) of granitoid trographic analyses (in parts per million) of granitoid 

rocks-Continued rocks-Continued 

Sample y Zr Ce Ga Ge Yb Pr Nd Sample Sm Eu Gd Tb Dy Ho Er Tm 

GR- 1 37.0 590 220 13.0 <0.46 2.30 <68 130 GR- 1 <46 7.1 6.0 <22 <10 <10 <4.6 <2.2 

GR- 2 50.0 640 230 12.0 1.60 2.30 <68 110 GR- 2 <46 3.7 <2.2 <22 <10 <10 <4.6 <2.2 

GR- 3 14.0 160 130 9.5 1.80 1.20 <68 93 GR- 3 <46 3.5 14.0 <22 <10 <10 <4.6 3.4 

GR- 4 12.0 98 100 8.9 <.46 1.10 <68 <46 GR- 4 <46 (1.0 17.0 <22 <10 <10 <4.6 <2.2 

GR- 5 28.0 240 130 12.0 <.46 2.00 <68 <46 GR- 5 <46 5.3 <2.2 <22 (10 <10 <4.6 <2.2 

GR- 6 25.0 140 140 11.0 <.46 1.90 <6•8 110 GR- 6 <46 3.0 7.7 <22 <10 <10 <4.6 <Z.2 

GR- 7 25.0 210 130 11.0 .78 1. 70 <68 120 GR- 7 <46 3.3 20.0 <22 <10 <10 <4.6 (2.2 

GR- 8 31.0 320 180 15.0 <.46 2.20 <68 150 GR- 8 <46 4.3 13.0 <22 <10 <10 <4.6 <2.2 

GR- 9 25.0 260 160 11.0 .82 1.60 <68 <46 GR- 9 <46 2.7 <2.2 <22 <10 <10 <4.6 <2.2 

GR- 10 23.0 250 150 12.0 1.80 1.60 <68 180 GR- 10 <46 4.6 4.1 <22 <10 <10 <4.6 <2.2 

GR- 11 24.0 180 170 11.0 .78 1.50 <68 56 GR- 11 <46 3.5 4.3 <22 <10 <10 <4.6 <2.2 

GR- 12 24.0 210 150 12.0 .80 1.70 <68 71 GR- 12 <46 4.3 4.0 <22 <10 <10 <4.6 <2.2 

GR- 13 36.0 290 180 12.0 1.30 2.50 <68 51 GR- 13 <46 5.2 4.0 <22 <10 <10 <4.6 <2.2 

GR- 14 39.0 370 230 12.0 1.10 2.10 <68 68 GR- 14 <46 6.0 14.0 <22 <10 <10 <4.6 <2.2 

GR- 15 10.0 190 83 4.7 <.46 .79 <68 68 GR- 15 <46 2.9 7.0 <22 <10 <10 <4.6 <2.2 

GR- 16 11.0 91 85 8.0 1.40 1.00 <68 <46 GR- 16 <46 2.6 8.7 <22 <10 <10 <4. 6 <2.2 

GR- 17 24.0 210 140 11.0 <.46 1.60 <68 68 GR- 17 <46 4.0 3.2 <22 <10 <10 <4.6 <2.2 

GR- 18 26.0 310 150 11.0 <.46 1.70 <68 <46 GR- 18 47 3.1 13.0 <22 <10 <10 <4.6 <2.2 

GR- 19 14.0 86 75 s.o <.46 1.20 <68 <46 GR- 19 <46 2.7 6.7 <22 <10 <10 <4.6 <2.2 

GR- 20 33.0 250 140 8.7 1.30 1.80 <68 65 GR- 20 <46 2.7 18.0 <22 <10 <10 <4.6 <2.2 

GR- 21 37.0 120 150 13.0 <.46 1.80 <68 97 GR- 21 <46 2.9 13.0 <22 <10 <10 <4.6 <2.2 

GR- 22 20.0 120 96 9.1 1.90 1. 30 <68 50 GR- 22 <46 2.8 14.0 <22 <10 <10 <4.6 <2.2 

GR- 23 10.0 72 67 5.9 <.46 .96 <68 75 GR- 23 <46 <1.0 4.8 <22 15 <10 <4.6 <2.2 

GR- 24 15.0 83 58 7.7 2.20 1.20 <68 59 GR- 24 <46 2.5 7.3 <22 <10 <10 <4.6 2.8 

GR- 25 16.0 57 51 15.0 1.00 1.20 <68 53 GR- 25 <46 <1.0 8.6 <22 14 <10 <4.6 <2.2 

GR- 26 18.0 43 67 14.0 <.46 1.10 <68 46 GR- 26 48 2.8 11.0 <22 <10 <10 <4.6 2.2 

GR- 27 22.0 130 120 9.9 <.46 1.80 <68 110 GR- 27 <46 4.4 9.9 <22 <10 <10 <4.6 <2.2 

GR- 28 15.0 130 67 10.0 1. 20 1. 20 <68 90 GR- 28 <46 3.3 22.0 <22 <10 <10 <4.6 <2.2 

GR- 29 23.0 150 110 11.0 2.60 1.80 <68 70 GR- 29 <46 3.8 <2.2 <22 <10 <10 <4.6 <2.2 

GR- 30 19.0 120 110 8.7 <.46 1.60 <68 <46 GR- 30 <46 1.8 6.1 <22 <10 <10 <4.6 <2.2 

GR- 31 21.0 160 110 10.0 <.46 1.50 <68 160 GR- 31 <46 2.6 22.0 <22 <10 (10 <4.6 <2.2 

GR- 32 21.0 140 94 9.4 .72 1. 50 <68 47 GR- 32 <46 2.6 12.0 <22 <10 <10 <4. 6 <2.2 

GR- 33 17.0 42 <46 11.0 <.46 1. 20 <68 <46 GR- 33 <46 2.1 <2.2 <22 12 <10 <4.6 3.1 

GR- 34 22.0 43 64 11.0 2.60 1. 50 <68 <46 GR- 34 <46 <1.0 6.0 <22 11 <10 <4.6 3.1 

GR- 35 16.0 400 300 10.0 <.46 1.20 <68 140 GR- 35 <46 6.1 5.7 <22 <10 <10 <4.6 <2.2 

GR- 36 13.0 200 190 7.3 <.46 1. 30 <68 <46 GR- 36 <46 3.1 18.0 <22 <10 <10 <4.6 <2.2 

GR- 37 22.0 110 120 13.0 1.50 1.50 <68 92 GR- 37 <46 3.4 (2.2 <22 <10 <10 <4.6 <2.2 

GR- 38 27.0 150 120 8.5 <.46 1. 70 <68 <46 GR- 38 <46 2.5 14.0 <22 <10 <10 <4.6 <2.2 

GR- 39 15.0 88 59 7.6 1.30 1.20 <68 58 GR- 39 <46 (1.0 13.0 <22 <10 <10 <4.6 <2.2 

GR- 40 14.0 92 70 9.0 <.46 1. 20 <68 <46 GR- 40 <46 3.2 2.6 <22 <10 <10 <4.6 <2.2 

GR- 41 5.8 69 57 12.0 <.4 6.59 <68 72 GR- 41 <46 3.3 5.2 <22 <10 <10 <4.6 3.2 

GR- 42 6.0 91 54 9.7 2.00 .61 <68 53 GR- 42 <46 <1.0 19.0 <22 <10 <10 <4.6 <2.2 

GR- 43 16.0 180 85 8.6 <.46 1.30 <68 49 GR- 43 <46 3.2 <2.2 (22 <10 <10 <4.6 <2.2 

GR- 44 20.0 180 130 9.3 <.46 1. so <68 <46 GR- 44 <46 <1.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR- 45 52.0 52 47 12.0 <.46 3.10 <68 <46 GR- 45 <46 1.7 4.2 <22 <10 <10 <4.6 <2.2 

GR- 46 33.0 77 130 14.0 1. 70 2.10 <68 <46 GR- 46 <46 <1.0 <2. 2 <22 <10 <10 <4.6 <2.2 

GR- 47 7.0 120 69 10.0 <.46 .59 <68 <46 GR- 47 <46 (1.0 7.1 <22 <10 <10 <4.6 2.4 

GR- 48 11.0 130 89 15.0 2.00 76 <68 52 GR- 48 <46 2.5 <2.2 <22 <10 <10 <4.6 <2.2 

GR- 49 4.9 26 52 4.6 <.46 .48 <68 <46 GR- 49 <46 <1.0 <2.2 <22 <10 (10 <4.6 <2.2 

GR- 50 8.6 71 <46 8.8 <.46 1.10 <68 <46 GR- 50 <46 1.8 18.0 <22 <10 <10 <4.6 2.7 

Table 5 31 
Table 5. Plate-reader semiquantitative emiSSIOn spec- Table 5. Plate-reader semiquantitative emission spectrographic analyses (in parts per million) of granitoid trographic analyses (in parts per million) of granitoid 

rocks-Continued rocks-Continued 

Sample Ag B Be Co Cr Cu La Sample Mo Nb Ni Pb Sc Sn v w 

GR- 51 (0.46 (5.0 1.8 11.00 8.30 38.00 88.0 GR- 51 2.3 24.0 12.0 14.0 5.2 <4.6 70.0 (46 

GR- 52 (.46 (5.0 1.7 9.70 7.90 21.00 75.0 GR- 52 1.9 18.0 11.0 15.0 4.6 (4.6 62.0 (46 

GR- 53 <.46 8.7 (1.0 (.46 2.00 .48 52.0 GR- 53 (1.0 24.0 1.3 3.5 2.0 (4.6 2.6 <46 

GR- 54 <.46 (5.0 2.0 2.10 4.00 .83 110.0 GR- 54 (1.0 35.0 2.4 4.9 2.5 (4.6 5.8 (46 

GR- 55 (.46 (5.0 (1.0 2.60 2.70 .27 32.0 GR- 55 (1.0 23.0 2.3 8.9 2.5 (4.6 12.0 <46 

GR- 56 <.46 (5.0 (1.0 6.80 4.30 21.00 29.0 GR- 56 1.7 6.6 3.6 9.0 4.4 (4.6 56.0 <46 

GR- 57 <.46 (5.0 1.4 13.00 67.00 2.30 96.0 GR- 57 1.3 37.0 49.0 11.0 11.0 <4.6 62.0 <46 

GR- 58 (.46 (5.0 1.7 15.00 78.00 .90 81.0 GR- 58 1.7 27.0 62.0 12.0 13.0 (4.6 69.0 (46 

GR- 59 (.46 5.3 (1.0 12.00 38.00 10.00 41.0 GR- 59 1.7 23.0 23.0 18.0 9.7 (4.6 66.0 <46 

GR- 60 (.46 (5.0 (1.0 10.00 39.00 5.30 62.0 GR- 60 1.4 14.0 22.0 11.0 8.1 <4.6 56.0 <46 

GR- 61 <.46 10.0 2.4 8.80 51.00 1.00 70.0 GR- 61 1.8 38.0 19.0 21.0 7.1 (4.6 48.0 (46 

GR- 62 (.46 15.0 3.2 15.00 120.00 8.00 75.0 GR- 62 2.3 36.0 38.0 19.0 14.0 (4.6 90.0 <46 

GR- 63 <.46 (5.0 (1.0 18.00 15.00 32.00 34.0 GR- 63 3.1 13.0 11.0 9.9 17.0 <4.6 150.0 <46 

GR- 64 (.46 8.3 (1.0 16.00 18.00 39.00 31.0 GR- 64 3.2 5.5 15.0 10.0 20.0 <4. 6 150.0 (46 

GR- 65 (.46 16.0 (1.0 18.00 16.00 45.00 24.0 GR- 65 3.4 13.0 14.0 13.0 19.0 (4.6 150.0 <46 

GR- 66 .70 23.0 (1.0 15.00 15.00 16.00 31.0 GR- 66 3.5 19.0 13.0 16.0 16.0 (4.6 150.0 <46 

GR- 67 <.46 9.5 1.9 11.00 12.00 19.00 76.0 GR- 67 2.3 28.0 11.0 21.0 18.0 (4.6 66.0 <46 

GR- 68 <.46 7.1 1.9 11.00 12.00 15.00 48.0 GR- 68 2.3 23.0 12.0 21.0 19.0 (4.6 59.0 <46 

GR- 69 (.46 (5.0 2.4 3.10 4.90 6.50 32.0 GR- 69 1.2 27.0 3.1 16.0 4.1 (4.6 13.0 <46 

GR- 70 (.46 (5.0 (1.0 1.20 1.60 2.60 11.0 GR- 70 (1.0 30.0 (1.0 13.0 2.5 (4.6 3.8 <46 

GR- 71 (.46 (5.0 1.2 11.00 10.00 3.60 43.0 GR- 71 2.2 3.2 12.0 11.0 8.5 (4.6 62.0 (46 

GR- 72 <.46 (5.0 (1.0 13.00 17.00 26.00 42.0 GR- 72 2.0 14.0 15.0 13.0 8.1 <4.6 92.0 (46 

GR- 73 (.46 67.0 4.0 6.20 6.10 37.00 83.0 GR- 73 (1.0 27.0 7.0 24.0 13.0 (4.6 30.0 (46 

GR- 74 (.46 6.1 2.4 7.10 7.60 9.70 66.0 GR- 74 1.6 22.0 5.9 35.0 13.0 (4.6 21.0 (46 

GR- 75 <.46 (5.0 1.1 8.50 9.00 7.70 35.0 GR- 75 1.8 9.6 5.9 13.0 6.6 <4.6 75.0 <46 

GR- 76 (.46 (5.0 (1. 0 8.60 7.90 3.60 28.0 GR- 76 2.1 14.0 5.8 12.0 5.2 (4.6 66.0 <46 

GR- 77 <.46 (5.0 1.3 9.10 9.10 5.60 42.0 GR- 77 1.8 15.0 7.0 14.0 10.0 <4.6 82.0 (46 

GR- 78 (.46 (5.0 1.5 8.80 8.00 2.80 37.0 GR- 78 2.2 14.0 10.0 19.0 11.0 (4.6 64.0 <46 

GR- 79 (.46 (5.0 1.2 8.30 16.00 6.80 44.0 GR- 79 1.8 6.3 11.0 14.0 8.5 (4.6 72.0 (46 

GR- 80 (.46 (5.0 (1.0 9.90 14.00 11.00 49.0 GR- 80 1.5 17.0 9.8 16.0 10.0 (4.6 66.0 <46 

GR- 81 (.46 (5.0 1.4 8.00 8.90 1.20 64.0 GR- 81 1.8 18.0 5.3 19.0 6.8 (4.6 58.0 (46 

GR- 82 <.46 (5.0 1.6 6.90 7.80 1.20 65.0 GR- 82 1. 8 34.0 4.3 19.0 7.4 (4.6 44.0 (46 

GR- 83 (.46 (5.0 1.5 2.00 2.40 (.22 42.0 GR- 83 (1.0 10.0 2.5 12.0 2.9 (4.6 10.0 <46 

GR- 84 <.46 (5.0 1.5 2.20 2.00 .31 65.0 GR- 84 1.3 22.0 3.5 21.0 3.4 (4.6 11.0 (46 

GR- 85 (.46 (5.0 1.9 6.50 5.90 .32 81.0 GR- 85 1.8 27.0 5.4 18.0 6.1 (4.6 31.0 <46 

GR- 86 <.46 (5.0 1.5 5.50 5.10 .67 67.0 GR- 86 1.5 33.0 4.1 17.0 4.2 (4.6 30.0 <46 

GR- 87 (.46 (5.0 (1.0 11.00 11.00 6.50 33.0 GR- 87 1.8 6.1 8.6 8.7 7.1 (4.6 87.0 <46 

GR- 88 (.46 8.3 (1.0 11.00 11.00 5.00 29.0 GR- 88 2.0 12.0 9.2 12.0 6.5 (4.6 100.0 <46 

GR- 89 <.46 (5.0 1.3 7.30 8.20 28.00 40.0 GR- 89 1.6 16.0 7.5 14.0 9.7 (4.6 69.0 <46 

GR- 90 (.46 (5.0 1.4 9.70 12.00 4.60 39.0 GR- 90 1.8 30.0 9.4 16.0 13.0 (4. 6 83.0 <46 

GR- 91 (.46 (5.0 1.7 5.80 12.00 1.20 110.0 GR- 91 1.9 35.0 8.9 19.0 5.4 <4.6 44.0 <46 

GR- 92 (.46 (5.0 2.5 3.90 5.60 .45 64.0 GR- 92 (1.0 52.0 5.7 28.0 4.6 (4. 6 20.0 <46 

GR- 93 (.46 41.0 2.6 22.00 82.00 30.00 170.0 GR- 93 4.3 56.0 51.0 34.0 19.0 (4.6 140.0 (46 

GR- 94 <.46 32.0 2.7 14.00 29.00 51.00 130.0 GR- 94 3.2 94.0 21.0 15.0 10.0 (4.6 89.0 <46 

GR- 95 (.46 (5.0 2.2 11.00 15.00 36.00 80.0 GR- 95 4.6 22.0 17.0 18.0 10.0 (4.6 69.0 120 

GR- 96 (.46 (5.0 2.1 12.00 23.00 2.40 79.0 GR- 96 2.9 34.0 14.0 17.0 11.0 (4.6 83.0 <46 

GR- 97 (.46 (5.0 1.4 5.80 5.30 25.00 73.0 GR- 97 2.7 35.0 9.4 11.0 5.7 (4.6 29.0 (46 

GR- 98 (.46 (5.0 1.5 6.50 5.20 3.40 88.0 GR- 98 1.6 23.0 4.0 9.9 4.7 (4.6 29.0 <46 

GR- 99 (.46 8.9 2.1 11.00 25.00 4.70 47.0 GR- 99 3.0 30.0 14.0 18.0 12.0 <4.6 80.0 (46 

GR-100 (.46 11.0 1.8 7.90 19.00 5.00 42.0 GR-100 1.1 26.0 11.0 16.0 7.7 (4.6 67.0 <46 

32 Granitoid Rocks, Basin and Range Province 
Table 5. Plate-reader semiquantitative emiSSIOn spec- Table 5. Plate-reader semiquantitative emiSSIOn spectrographic analyses (in parts per million) of granitoid trographic analyses (in parts per million) of granitoid 

rocks-Continued rocks-Continued 

Sample y Zr Ce Ga Ge Yb Pr Nd Sample Sm Eu Gd Tb Dy Ho Er Tm 

GR- 51 13.0 180 170 13.0 1.70 1.00 <68 110 GR- 51 <46 3.2 7.3 <22 (10 (10 <4.6 <2.2 

GR- 52 12.0 200 150 13.0 1.10 1.00 <68 140 GR- 52 <46 4.4 5.1 (22 <10 <10 <4.6 <2.2 

GR- 53 35.0 94 73 6.5 <.46 1.60 <68 67 GR- 53 <46 <1.0 <2.2 (22 <10 <10 <4.6 <2.2 

GR- 54 47.0 210 200 8.2 1.90 3.00 <68 69 GR- 54 <46 2.1 9.1 <22 <10 <10 <4.6 <2.2 

GR- 55 11.0 99 60 6.6 1.50 1.10 (68 <46 GR- 55 <46 <1.0 12.0 (22 <10 <10 <4.6 <2.2 

GR- 56 11.0 96 65 6.3 <.46 .98 <68 75 GR- 56 <46 2.0 12.0 <22 <10 <10 <4.6 <2.2 

GR- 57 15.0 150 170 7.9 99 1.10 <68 100 GR- 57 <46 4.1 4.5 <22 <10 <10 <4.6 <2.2 

GR- 58 16.0 140 170 8.7 <.46 1.20 <68 56 GR- 58 <46 3.5 12.0 30 <10 <10 <4.6 <2.2 

GR- 59 17.0 200 110 8.8 .88 1.50 (68 60 GR- 59 <46 4.2 8.7 <22 <10 <10 <4.6 <2.2 

GR- 60 16.0 120 120 7.6 <.46 1.30 <68 <46 GR- 60 <46 (1.0 4.9 <22 <10 <10 <4.6 <2.2 

GR- 61 26.0 210 160 11.0 1.40 1.60 (68 69 GR- 61 <46 3.6 16.0 <22 <10 <10 <4.6 <2.2 

GR- 62 27.0 240 150 11.0 1.60 1. 80 <68 61 GR- 62 48 3.8 <2.2 <22 <10 <10 <4.6 <2. 2 

GR- 63 21.0 150 92 11.0 <.46 1.50 (68 94 GR- 63 <46 3.1 8.4 <22 <10 <10 <4.6 <2.2 

GR- 64 20.0 130 110 10.0 <.46 1.50 <68 64 GR- 64 <46 3.0 6.6 <22 <10 <10 <4.6 <2.2 

GR- 65 20.0 120 100 9.5 1.30 1.40 <68 120 GR- 65 <46 2.5 10.0 <22 <10 <10 <4.6 (2.2 

GR- 66 15.0 100 110 11.0 2.00 1.30 <68 100 GR- 66 <46 3.0 14.0 <22 <10 <10 <4.6 <2.2 

GR- 67 69.0 250 170 10.0 1.50 5.20 (68 <46 GR- 67 <46 3.4 <2.2 <22 (10 (10 <4.6 <2.2 

GR- 68 52.0 180 130 8.8 2.00 4.30 <68 47 GR- 68 <46 5.3 15.0 <22 <10 <10 <4.6 <2.2 

GR- 69 19.0 89 65 10.0 <.46 1.30 (68 81 GR- 69 <46 1.9 (2.2 <22 (10 <10 <4.6 <2.2 

GR- 70 15.0 65 <46 6.9 <.46 1.40 (68 <46 GR- 70 <46 2.6 3.5 (22 <10 <10 <4.6 2.6 

GR- 71 13.0 110 120 9.4 <.46 1.10 (68 80 GR- 71 <46 1.4 6.4 <22 <10 (10 <4.6 <2.2 

GR- 72 13.0 73 110 14.0 <.46 1.20 <68 <46 GR- 72 <46 3.0 (2.2 <22 <10 <10 <4. 6 <2.2 

GR- 73 63.0 260 180 10.0 <.46 6.30 <68 59 GR- 73 <46 3.9 (2.2 <22 <10 <10 <4.6 <2.2 

GR- 74 56.0 190 150 9.6 2.00 5.40 <68 110 GR- 74 <46 4.6 5.4 36 <10 <10 <4.6 <2.2 

GR- 75 13.0 90 68 13.0 .55 1.10 <68 <46 GR- 75 (46 4.5 4.5 <22 (10 <10 <4.6 (2.2 

GR- 76 13.0 100 62 9.8 <.46 1.30 <68 62 GR- 76 <46 3.5 16.0 <22 <10 <10 <4.6 (2.2 

GR- 77 15.0 90 86 10.0 .97 1.20 (68 <46 GR- 77 <46 2.7 (2.2 <22 <10 <10 <4.6 <2.2 

GR- 78 14.0 120 120 11.0 1.10 1.40 <68 53 GR- 78 (46 2.8 14.0 <22 <10 <10 (4.6 <2.2 

GR- 79 14.0 140 110 11.0 <.46 1.10 (68 58 GR- 79 <46 2.7 8 9 <22 <10 <10 (4.6 <2.2 

GR- 80 15.0 120 110 16.0 <.46 1.40 <68 92 GR- 80 <46 3.7 <2.2 (22 <10 <10 <4.6 <2.2 

GR- 81 20.0 180 150 11.0 <.46 1.50 <68 52 GR- 81 <46 3.9 7.8 <22 <10 <10 <4.6 (2.2 

GR- 82 21.0 200 140 11.0 .75 1.60 <68 67 GR- 82 <46 3.7 18.0 <22 <10 <10 <4.6 (2.2 

GR- 83 6.6 150 63 9.0 <.46 .61 <68 77 GR- 83 <46 1.9 3.7 <22 <10 <10 <4.6 <2.2 

GR- 84 8.8 170 140 11.0 1.30 .72 <68 50 GR- 84 <46 <1.0 12.0 <22 <10 <10 <4.6 <2.2 

GR- 85 20.0 120 140 12.0 2.30 1.20 (68 120 GR- 85 <46 2.7 11.0 <22 (10 <10 <4.6 <2.2 

GR- 86 20.0 140 130 9.3 <.46 1.20 <68 62 GR- 86 <46 4.1 4.0 (22 <10 <10 (4.6 <2.2 

GR- 87 14.0 110 83 9.7 <.46 1.10 <68 64 GR- 87 <46 (1.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR- 88 11.0 73 94 13.0 <.46 .99 (68 75 GR- 88 (46 2.4 12.0 (22 (10 <10 <4.6 <2.2 

GR- 89 17.0 84 100 11.0 1.70 1.20 (68 63 GR- 89 <46 2.7 12.0 <22 <10 <10 <4.6 <2.2 

GR- 90 18.0 130 98 10.0 <.46 1.40 <68 50 GR- 90 <46 3.5 9.7 (22 (10 <10 (4.6 <2.2 

GR- 91 24.0 140 180 10.0 <.46 1.60 (68 <46 GR- 91 <46 3.6 11.0 25 <10 <10 <4.6 <2.2 

GR- 92 21.0 180 110 14.0 <.46 1.60 (68 <46 GR- 92 <46 2.6 14.0 (22 <10 <10 <4.6 (2.2 

GR- 93 43.0 410 300 11.0 <.46 2.50 <68 160 GR- 93 48 7.5 <2.2 <22 (10 <10 <4.6 <2.2 

GR- 94 21.0 240 220 11.0 <.46 1.60 (68 130 GR- 94 <46 5.6 6 5 <22 <10 <10 <4.6 <2.2 

GR- 95 23.0 230 170 11.0 1.90 1.60 (68 110 GR- 95 <46 4.5 3.5 36 <10 <10 <4.6 <2.2 

GR- 96 24.0 280 160 12.0 <.46 1.60 <68 96 GR- 96 <46 4.5 8.0 <22 <10 <10 <4.6 <2.2 

GR- 97 16.0 360 160 15.0 <.46 1.10 <68 92 GR- 97 (46 (1.0 7.4 <22 <10 <10 <4.6 <2.2 

GR- 98 17.0 230 150 11.0 .95 1.10 <68 140 GR- 98 <46 4.2 <2.2 <22 <10 <10 <4.6 <2.2 

GR- 99 20.0 85 110 10.0 2.40 1.50 <68 58 GR- 99 <46 3.1 5.5 <22 <10 <10 <4.6 (2.2 

GR-100 17.0 97 110 8.3 1. 20 1.40 <68 <46 GR-100 (46 3.2 6.0 <22 <10 (10 <4.6 (2.2 

Table 5 33 
Table 5. Plate-reader semiquantitative emiSSIOn spec- Table 5. Plate-reader semiquantitative emiSSIOn spectrographic analyses (in parts per million) of granitoid trographic analyses (in parts per million) of granitoid 

rocks-Continued rocks-Continued 

Sample Ag B Be Co Cr Cu La Sample Mo Nb Ni Pb Sc Sn v w 

GR-101 (0.46 <5.0 1.3 11.00 36.00 84.00 60.0 GR-101 3.4 19.0 19.0 11.0 12.0 (4.6 79.0 <46 

GR-102 <.46 (5.0 1.5 9.20 26.00 3.40 50.0 GR-102 1.5 24.0 13.0 6.8 9.9 (4.6 89.0 <46 

GR-103 <.46 (5.0 1.9 4.60 18.00 .80 49.0 GR-103 1.3 42.0 12.0 12.0 6.7 (4.6 53.0 <46 

GR-104 <.46 (5.0 3.0 3.80 7.60 .76 18.0 GR-104 <1.0 35.0 7.4 8.6 6.0 5.0 11.0 <46 

GR-105 <.46 <5.0 1.6 7.70 64.00 1.50 53.0 GR-105 1.4 24.0 22.0 4.9 17.0 (4.6 100.0 <46 

GR-106 <.46 18.0 1.5 7.90 160.00 1.30 35.0 GR-106 2.6 19.0 25.0 9.5 23.0 <4.6 150.0 (46 

GR-107 <.46 6.2 1.1 12.00 9.00 8.00 78.0 GR-107 2.8 31.0 6.6 10.0 13.0 <4.6 96.0 <46 

GR-108 <.46 8.8 2.0 11.00 8.10 2.10 81.0 GR-108 3.0 33.0 6.2 11.0 12.0 (4.6 130.0 <46 

GR-109 <.46 <5.0 1.6 2.20 2.30 1.80 49.0 GR-109 <1.0 9.2 3.6 18.0 2.2 (4.6 15.0 <46 

GR-110 <.46 <5.0 1.3 1.40 2.40 .54 50.0 GR-110 (1.0 13.0 2.9 17.0 2.3 <4.6 16.0 <46 

GR-111 <.46 <5.0 2.7 2.90 3.00 36.00 43.0 GR-111 1.8 19.0 5.1 17.0 3.3 <4.6 19.0 <46 

GR-112 <.46 <5.0 2.0 2.60 3.20 8.40 45.0 GR-112 1. 7 24.0 5.4 20.0 3.1 <4.6 22.0 <46 

GR-113 <.46 <5.0 <1.0 11.00 40.00 4.30 34.0 GR-113 8.6 15.0 24.0 6.6 10.0 <4.6 67.0 (46 

GR-114 <.46 <5.0 1.2 10.00 38.00 3.80 40.0 GR-114 1.9 18.0 23.0 6.0 8.6 <4.6 67.0 <46 

GR-115 <.46 (5.0 1.2 6.30 5.00 14.00 38.0 GR-115 1.3 7.3 7.4 20.0 4.8 (4.6 38.0 <46 

GR-116 (.46 (5.0 (1.0 17.00 17.00 5.70 32.0 GR-116 3.0 7.6 14.0 10.0 15.0 <4.6 120.0 <46 

GR-117 <.46 (5.0 3.1 2.50 3.60 2.30 54.0 GR-117 <1.0 41.0 2.8 21.0 2.4 <4.6 15.0 <46 

GR-118 (.46 <5.0 2.6 3.90 4.10 60.00 68.0 GR-118 1.5 27.0 3.8 12.0 4.1 <4.6 28.0 <46 

GR-119 <.46 7.1 1.6 11.00 13.00 10.00 69.0 GR-119 3.0 30.0 10.0 21.0 13.0 <4.6 94.0 (46 

GR-120 <.46 <5.0 1.7 12.00 16.00 15.00 78.0 GR-120 3.7 23.0 12.0 23.0 13.0 <4.6 74.0 <46 

GR-121 <.46 (5.0 (1.0 4.50 3.90 .95 32.0 GR-121 1.3 3.2 3.8 11.0 3.2 (4.6 33.0 <46 

GR-122 <.46 <5.0 1.1 2.50 3.50 1.40 22.0 GR-122 (1.0 14.0 2.6 11.0 3.2 <4.6 15.0 (46 

GR-123 <.46 <5.0 2.6 8.00 21.00 6.40 77 .o GR-123 1.4 59.0 16.0 16.0 6.2 <4.6 36.0 (46 

GR-124 <.46 <5.0 1.5 6.60 15.00 .98 56.0 GR-124 (1.0 53.0 12.0 9.5 4.0 (4.6 41.0 <46 

GR-125 <.46 8.5 3.1 6.50 6.60 9.40 59.0 GR-125 1.5 39.0 6.0 34.0 12.0 (4.6 23.0 <46 

GR-126 <.46 (5.0 1. 8 8.90 24.00 14.00 140.0 GR-126 2.2 85.0 13.0 14.0 9.1 <4.6 78.0 <46 

GR-129 (.46 15.0 (1.0 24.00 22.00 54.00 69.0 GR-129 4.4 16.0 15.0 13.0 18.0 <4.6 180.0 <46 

GR-130 .54 37.0 <1.0 25.00 26.00 57.00 62.0 GR-130 5.8 20.0 20.0 22.0 19.0 <4.6 170.0 <46 

GR-131 <.46 <5.0 (1.0 2.30 2.40 .25 54.0 GR-131 <1.0 14.0 2.7 12.0 2.6 (4.6 11.0 <46 

GR-132 <.46 <5.0 1.4 4.00 3.10 .69 68.0 GR-132 (1.0 20.0 3.5 12.0 3.4 (4.6 20.0 <46 

GR-133 <.46 22.0 1.5 6.80 12.00 2.40 66.0 GR-133 2.2 23.0 16.0 13.0 6.2 <4.6 56.0 (46 

GR-134 <.46 7.9 1.1 4.70 5.10 2.00 140.0 GR-134 (1.0 15.0 4.8 17.0 2.7 (4.6 18.0 <46 

GR-135 <.46 18.0 1.2 4.60 6.70 .36 41.0 GR-135 1.4 23.0 8.0 9.1 4.0 <4.6 27.0 (46 

GR-136 <.46 18 0 1.2 4.80 5.50 3.60 60.0 GR-136 1.3 25.0 7.2 9.0 4.7 <4.6 24.0 <46 

GR-137 (.46 <5.0 2.5 2.00 2.50 .78 86.0 GR-137 3.6 48.0 7.3 18.0 5.0 <4.6 14.0 <46 

GR-138 <.46 (5.0 2.7 2.60 3.10 1.20 110.0 GR-138 2.1 42.0 2.6 27.0 5.8 (4.6 15.0 <46 

GR-139 (.46 30.0 1.6 13.00 35.00 67.00 97.0 GR-139 2.4 20.0 36.0 21.0 10.0 <4.6 71.0 <46 

GR-140 <.46 <5.0 1.5 12.00 30.00 19.00 84.0 GR-140 4.3 37.0 29.0 21.0 9.7 <4.6 82.0 <46 

GR-141 <.46 (5.0 3.0 1.10 3.80 1.60 62.0 GR-141 1.5 63.0 4.0 30.0 2.4 4.8 4.6 <46 

GR-142 <.46 (5.0 2.5 <.46 1. 90 .87 51.0 GR-142 1.4 74.0 7.8 23.0 1.8 <4.6 5.0 <46 

GR-143 (.46 (5.0 1.3 5.80 5.20 3.20 58.0 GR-143 1. 9 9.2 9.0 16.0 4.2 <4.6 41.0 <46 

GR-144 <.46 (5.0 1.7 5.90 6.50 42.00 39.0 GR-144 2.1 12.0 8.5 16.0 5.7 <4.6 28.0 (46 

GR-145 (.46 (5.0 1.0 3.50 8.90 .32 36.0 GR-145 (1.0 34.0 4.1 20.0 3.8 <4.6 17 .o (46 

GR-146 <.46 (5.0 <1.0 2.70 6.20 1.40 51.0 GR-146 1.0 19.0 3.3 16.0 2.9 <4. 6 16.0 <46 

GR-147 <.46 (5.0 3.6 .92 2.40 .40 31.0 GR-147 (1.0 51.0 2.3 10.0 2.7 5.0 2.9 (46 

GR-148 <.46 (5.0 2.2 .64 (.46 <.22 38.0 GR-148 (1.0 47.0 1.7 11.0 2.9 (4.6 3.4 (46 

GR-149 <.46 <5.0 (1.0 8.20 7.00 23.00 76.0 GR-149 1.6 15.0 5.0 9.6 9.4 <4.6 51.0 <46 

GR-150 (.46 <5.0 (1.0 7.30 5.70 9.20 71.0 GR-150 1. 8 26.0 6.1 12.0 6.1 <4.6 48.0 (46 

GR-151 <.46 <5.0 <1.0 8.20 2.60 49.00 24.0 GR-151 1.7 6.8 3.8 11.0 6.7 <4.6 80.0 <46 

GR-152 (.46 6.9 <1.0 26.00 22.00 50.00 25.0 GR-152 5.0 2.6 13.0 7.7 30.0 (4.6 240.0 <46 

Granitoid Rocks, Basin and Range Province 
Table 5. Plate-reader semiquantitative emiSSIOn spec- I Table 5. Plate-reader semiquantitative emission spectrographic analyses (in parts per million) of granitoid trographic analyses (in parts per million) of granitoid 

rocks-Continued rocks-Continued 

Sample y Zr Ce Ga Ge Yb Pr Nd Sample Sm Eu Gd Tb Dy Ho Er Tm 

GR-101 19.0 230 130 11.0 1.80 1.30 <68 110 GR-101 <46 2.9 4.7 <22 <10 <10 <4.6 <2.2 

GR-102 19.0 170 120 9.7 <.46 1.40 <68 52 GR-102 46 3.3 <2. 2 <22 <10 <10 <4.6 <2.2 

GR-103 18.0 220 100 10.0 <.46 1.50 <68 <46 GR-103 <46 4.1 15.0 <22 <10 <10 <4.6 <2.2 

GR-104 15.0 130 <46 14.0 <.46 1.10 <68 <46 GR-104 <46 4.0 19.0 <22 <10 <10 <4. 6 <2.2 

GR-105 30.0 200 130 13.0 1.60 1.90 <68 100 GR-105 <46 5.7 <2.2 <22 <10 <10 <4.6 <2.2 

GR-106 26.0 140 120 16.0 <.46 l. 80 <68 58 GR-106 <46 4.6 11.0 <22 <10 <10 <4.6 <2. 2 

GR-107 26.0 170 150 9.8 <.46 1.80 <68 <46 GR-107 <46 2.6 <2.2 <22 <10 <10 <4.6 <2.2 

GR-108 21.0 180 170 10.0 l. 50 1.60 <68 57 GR-108 48 3.5 20.0 37 <10 <10 <4.6 <2.2 

GR-109 7.2 120 98 13.0 1.20 .59 <68 <46 GR-109 <46 4.5 11.0 <22 <10 <10 <4.6 <2.2 

GR-110 7.9 120 66 12.0 <.46 .67 <68 64 GR-110 <46 2.9 16.0 <22 <10 <10 <4.6 2.2 

GR-111 5.3 120 100 l7 .o 1.70 .62 <68 54 GR-111 <46 2.7 <2.2 <22 <10 <10 <4.6 <2.2 

GR-112 4.9 89 76 15.0 1.40 .58 <68 <46 GR-112 <46 1.2 13.0 <22 <10 <10 <4.6 <2.2 

GR-113 15.0 82 86 8.5 1.40 1.20 <68 100 GR-113 <46 <1.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR-114 15.0 92 110 7.8 <.46 1.20 <68 130 GR-114 <46 2.7 20.0 <22 <10 <10 <4.6 <2.2 

GR-llS 11.0 130 95 11.0 .74 .91 <68 82 GR-115 <46 1.4 <2.2 <22 <10 <10 <4.6 <2.2 

GR-116 15.0 78 100 12.0 2.10 1. 20 <68 <46 GR-116 <46 2.7 15.0 <22 <10 <10 <4.6 <2.2 

GR-117 16.0 240 120 14.0 2.00 1.10 <68 78 GR-117 <46 2.1 <2.2 <22 <10 <10 <4.6 <2.2 

GR-118 19.0 200 130 11.0 <.46 l. 20 <68 98 GR-118 <46 4.3 9.8 <22 <10 <10 <4.6 <2.2 

GR-ll9 26.0 170 160 9.1 1.80 1.60 <68 110 GR-119 51 2.0 6.3 <22 <10 <10 <4.6 <2.2 

GR-120 23.0 190 180 14.0 1.70 1.70 <68 <46 GR-120 <46 3.4 12.0 <22 <10 <10 <4.6 <2.2 

GR-121 8.2 96 77 12.0 1.20 .74 <68 110 GR-121 <46 1.7 5.3 <22 <10 <10 <4.6 <2.2 

GR-122 8.5 100 62 12.0 1.40 .85 <68 69 GR-122 <46 2.2 8.0 <22 <10 <10 <4.6 <2. 2 

GR-123 18.0 260 150 9.4 1.10 1.40 <68 79 GR-123 <46 2.6 19.0 <22 <10 <10 <4.6 <2.2 

GR-124 16.0 160 97 6.2 <.46 l. 30 <68 <46 GR-124 <46 2.3 17.0 <22 <10 <10 <4.6 <2.2 

GR-125 59.0 420 140 11.0 1.80 5.40 <68 68 GR-125 <46 4.3 9.1 35 <10 <10 <4.6 <2.2 

GR-126 28.0 250 260 8.9 .65 1.70 85 98 GR-126 <46 4.5 <2.2 <22 <10 <10 <4.6 <2.2 

GR-129 27.0 170 180 14.0 1.30 1.60 <68 61 GR-129 <46 <1.0 19.0 <22 <10 <10 <4.6 <2.2 

GR-130 26.0 200 180 14.0 <.46 1.60 <68 48 GR-130 <46 5.0 16.0 <22 <10 <10 <4.6 <2.2 

GR-131 15.0 93 100 6.1 <.46 1.20 <68 76 GR-131 <46 <1.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR-132 18.0 110 130 9.8 2.20 1. 30 <68 59 GR-132 <46 (1.0 14.0 <22 13 <10 <4.6 <2.2 

GR-133 15.0 360 140 14.0 1.40 1.20 <68 <46 GR-133 <46 3.5 <2.2 <22 <10 <10 <4.6 <2.2 

GR-134 10.0 320 200 9.0 1. 90 .91 <68 78 GR-134 <46 2.8 <2. 2 <22 <10 <10 <4.6 <2.2 

GR-135 14.0 240 82 10.0 <.46 1.20 <68 130 GR-135 <46 2.3 13.0 <22 <10 <10 <4.6 <2.2 

GR-136 14.0 200 120 8.6 1.00 1.30 <68 130 GR-136 <46 2.4 10.0 <22 <10 <10 <4.6 <2.2 

GR-137 34.0 320 170 13.0 <.46 2.60 74 <46 GR-137 <46 3.9 3.5 <22 <10 <10 <4.6 <2.2 

GR-138 45.0 330 230 16.0 <.46 3.00 <68 130 GR-138 <46 3.3 8.3 <22 <10 <10 <4.6 <2. 2 

GR-139 26.0 310 190 17.0 <.46 1.90 <68 120 GR-139 <46 4.8 6.7 <22 <10 <10 <4.6 <2.2 

GR-140 24.0 360 170 9.7 1.10 2.20 <68 53 GR-140 <46 4.6 11.0 <22 <10 <10 <4.6 <2.2 

GR-141 11.0 150 130 10.0 <.46 1.30 <68 <46 GR-141 <46 2.7 14.0 <22 <10 <10 <4.6 <2.2 

GR-142 7.7 120 76 9.6 .85 1. 00 <68 <46 GR-142 <46 1.1 9.3 (22 <10 <10 <4.6 <2.2 

GR-143 9.4 230 130 14.0 <.46 .94 <68 98 GR-143 <46 3.3 15.0 <22 <10 <10 <4.6 <2.2 

GR-144 8.2 77 96 15.0 1.50 .94 <68 57 GR-144 <46 3.4 5.8 <22 <10 <10 <4.6 <2.2 

GR-145 14.0 56 84 12.0 1.00 1.00 <68 <46 GR-145 <46 <1.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR-146 8.6 91 110 8.1 1.60 .89 <68 49 GR-146 <46 2.6 13.0 <22 <10 <10 <4.6 <2.2 

GR-147 41.0 120 86 11.0 <.46 3.80 <68 <46 GR-147 48 2.6 16.0 <22 13 <10 <4.6 <2.2 

GR-148 39.0 97 99 11.0 2.00 3.60 <68 67 GR-148 so 1.7 5.4 <22 10 <10 <4.6 <2.2 

GR-149 29.0 160 140 7.1 <.46 2.40 <68 110 GR-149 <46 2.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR-150 38.0 140 150 7.6 1. 20 2.70 <68 100 GR-150 <46 3.9 <2.2 <22 <10 <10 <4.6 <2.2 

GR-151 16.0 78 70 9.7 1.90 1.40 <68 62 GR-151 <46 <1.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR-152 15.0 75 95 10.0 1.10 1. 50 <68 <46 GR-152 <46 <1.0 8.6 <22 <10 <10 <4.6 <2.2 

Table 5 35 
Table 5. Plate-reader semiquantitative emiSSIOn spec- Table 5. Plate-reader semiquantitative emiSSIOn spectrographic analyses (in parts per million) of granitoid trographic analyses (in parts per million) of granitoid 

rocks-Continued rocks-Continued 

Sample Ag B Be Co Cr Cu La Sample Mo Nb Ni Pb Sc Sn v w 

GR-153 (0.46 (5.0 1.3 5.20 6.40 3.20 79.0 GR-153 2.1 11.0 9.9 29.0 5.6 <4.6 69.0 <46 

GR-154 .48 (5.0 1.4 7.10 2.30 12.00 58.0 GR-154 3.1 13.0 8.0 27.0 5.8 <4.6 110.0 (46 

GR-155 <.46 (5.0 1.3 5.20 3.50 1.00 54.0 GR-155 1.1 14.0 3.5 16.0 3.7 (4.6 35.0 <46 

GR-156 <.46 (5.0 1.4 1.90 2.00 .89 48.0 GR-156 (1.0 18.0 2.4 21.0 2.8 (4.6 14.0 (46 

GR-157 <.46 (5 0 1.5 2.70 5.10 6.30 68.0 GR-157 (1.0 21.0 3.2 26.0 4.8 4.7 14.0 (46 

GR-158 <.46 (5.0 1.4 2.70 3.80 2.30 52.0 GR-158 1.4 22.0 5.6 23.0 3.8 <4.6 11.0 <46 

GR-159 <.46 (5.0 1.1 8.30 8.70 7.00 47.0 GR-159 (1.0 15.0 8.0 15.0 5.2 <4.6 55.0 <46 

GR-160 <.46 6.2 1. 9 12.00 15.00 7.50 74.0 GR-160 1.8 26.0 11.0 24.0 11.0 <4.6 76.0 <46 

GR-161 <.46 9.8 (1.0 12.00 18.00 38.00 39.0 GR-161 1.7 20.0 16.0 23.0 7.3 (4.6 87.0 (46 

GR-162 (.46 (5.0 1.5 14.00 22.00 38.00 35.0 GR-162 2.4 20.0 18.0 22.0 8.7 (4.6 91.0 <46 

GR-163 <.46 <5.0 1.3 3.20 4.10 1.10 180.0 GR-163 1.1 46.0 2.3 24.0 4.2 <4.6 5.6 <46 

GR-164 <.46 (5.0 2.3 2.60 3.40 3.90 270.0 GR-164 1.1 52.0 2.4 23.0 5.2 <4.6 6.0 <46 

GR-165 <.46 7.5 1.3 8.30 7.10 45.00 55.0 GR-165 1.6 26.0 7.3 20.0 9.0 (4.6 65.0 <46 

GR-166 <.46 5.0 1.9 7.10 6.50 4.10 82.0 GR-166 2.4 35.0 8.2 22.0 14.0 <4.6 54.0 <46 

GR-167 <.46 (5.0 1.3 19.00 16.00 33.00 50.0 GR-167 3.1 18.0 14.0 18.0 16.0 <4.6 120.0 <46 

GR-168 <.46 (5.0 1.2 11.00 16.00 11.00 77.0 GR-168 2.1 9.3 13.0 16.0 7.6 <4.6 64.0 <46 

GR-169 <.46 (5.0 (1.0 6.40 7.40 3.30 97.0 GR-169 2.7 18.0 5.8 17.0 16.0 <4.6 34.0 (46 

GR-170 <.46 (5.0 (1.0 2.30 5.10 .83 70.0 GR-170 (1.0 59.0 3.7 27.0 4.6 <4.6 6.2 <46 

GR-171 (.46 9.3 (1.0 9.10 8.70 3.80 37.0 GR-171 2.8 20.0 6.6 12.0 12.0 <4.6 68.0 <46 

GR-172 <.46 5.8 (1.0 9.90 11.00 4.30 41.0 GR-172 2.6 24.0 9.7 9.2 10.0 <4.6 80.0 <46 

GR-173 <.46 <5.0 (1.0 1.80 2.30 .40 37.0 GR-173 <1.0 21.0 8.4 20.0 3.2 <4.6 9.5 <46 

GR-174 <.46 (5.0 (1.0 2.00 2.10 1.20 33.0 GR-174 (1.0 9.7 3.1 15.0 3.0 (4.6 11.0 <46 

GR-175 (.46 (5.0 1.0 1.70 2.20 1.80 16.0 GR-175 (1.0 22.0 3.9 25.0 2.3 (4.6 6.6 (46 

GR-176 <.46 (5.0 1.0 1. 80 2.60 1.00 14.0 GR-176 (1.0 20.0 2.0 23.0 3.2 (4.6 8.1 <46 

GR-177 <.46 (5.0 (10 9.20 4.10 6.40 120.0 GR-177 3.2 22.0 3.9 19.0 26.0 <4.6 24.0 (46 

GR-178 <.46 (5.0 2.0 7.40 12.00 8.00 210.0 GR-178 4.5 50.0 9.4 22.0 28.0 <4.6 21.0 <46 

GR-179 <.46 (5.0 1.1 7.50 9.10 1.30 40.0 GR-179 1.4 15.0 8.2 15.0 5.5 <4.6 28.0 <46 

GR-180 <.46 (5.0 1.5 5.10 9.70 .47 23.0 GR-180 1.2 6.1 8.7 25.0 3.6 <4.6 18.0 <46 

GR-181 (.46 (5.0 1.2 4.80 6.40 8.00 250.0 GR-181 1.9 41.0 4.7 48.0 5.7 <4.6 26.0 <46 

GR-182 <.46 (5.0 1.3 4.50 3.20 3.20 150.0 GR-182 (1.0 46.0 3.4 37.0 5.3 <4.6 17.0 <46 

GR-183 <.46 (5.0 1.3 4.20 5.30 25.00 80.0 GR-183 (1.0 34.0 3.2 19.0 5.6 <4.6 17.0 <46 

GR-184 (.46 (5.0 (1.0 2.30 3.40 9.40 54.0 GR-184 (1.0 16.0 3.0 24.0 6.4 (4.6 10.0 <46 

GR-185 <.46 (5.0 1.8 7.00 4.60 8.40 100.0 GR-185 1.7 45.0 3.9 19.0 8.4 <4.6 33.0 (46 

GR-186 <.46 (5.0 3.4 3.40 3.50 .71 180.0 GR-186 1.0 66.0 3.0 33.0 4.0 (4.6 11.0 <46 

GR-187 <.46 (5.0 2.8 7.50 6.10 4.00 150.0 GR-187 3.0 80.0 5.0 26.0 19.0 5.9 48.0 (46 

GR-188 <.46 8.6 2.5 11.00 4.20 10.00 170.0 GR-188 4.0 24.0 9.4 28.0 21.0 <4.6 50.0 (46 

GR-189 (.46 (5.0 (1.0 4.60 2.30 8.30 150.0 GR-189 3.9 34.0 3.2 21.0 26.0 4.6 9.3 (46 

GR-190 <.46 (5.0 (1.0 5.40 2.60 4.00 180.0 GR-190 1. 8 28.0 2.8 22.0 14.0 <4.6 13.0 (46 

GR-191 (.46 (5.0 (1.0 .79 2.20 1.60 8.9 GR-191 (1.0 38.0 1. 7 12.0 3.5 <4.6 2.2 (46 

GR-192 .62 (5.0 1.4 3.10 3.80 2.90 55.0 GR-192 <1.0 14.0 3.0 19.0 3.7 (4.6 15.0 <46 

GR-193 <.46 <S.O 2.4 (.46 1.20 .62 70.0 GR-193 1.0 68.0 2.7 19.0 5.1 <4.6 3.8 <46 

GR-194 <.46 (5.0 3.5 1.80 2.30 .42 130.0 GR-194 1.4 55.0 2.7 24.0 6.3 5.9 4.9 <46 

GR-195 <.46 <5.0 1.5 18.00 18.00 250.00 47 .o GR-195 4.3 18.0 21.0 10.0 9.5 <4.6 120.0 (46 

GR-196 <.46 (5.0 1.1 4.50 6.50 23.00 39.0 GR-196 4.5 22.0 6.2 13.0 3.6 <4.6 27.0 (46 

GR-197 <.46 (5.0 1.8 11.00 7.90 6.80 94.0 GR-197 3.6 19.0 13.0 26.0 13.0 <4.6 57.0 (46 

GR-198 <.46 5.7 3.3 14.00 9.80 8.70 120.0 GR-198 4.5 19.0 8.7 34.0 21.0 <4.6 69.0 <46 

GR-199 (.46 <5.0 1.3 4.60 3.40 4.10 28.0 GR-199 (1.0 20.0 3.4 18.0 2.7 <4.6 18.0 <46 

GR-200 <.46 <5.0 1.1 3.00 2.20 4.70 29.0 GR-200 (1.0 15.0 2.6 17.0 2.3 <4.6 12.0 <46 

GR-201 (.46 6.6 2.2 8.40 13.00 7.10 160.0 GR-201 2.2 27.0 7.8 23.0 18.0 <4.6 38.0 <46 

GR-202 <.46 6.1 1.7 7.80 12.00 5.70 120.0 GR-202 2.5 28.0 9.8 24.0 15.0 <4.6 46.0 <46 

36 Granitoid Rocks, Basin and Range Province 
Table 5. Plate-reader semiquantitative emiSSIOn spec- Table 5. Plate-reader semiquantitative emission spectrographic analyses (in parts per million) of granitoid trographic analyses (in parts per million) of granitoid 

rocks-Continued rocks-Continued 

Sample y Zr Ce Ga Ge Yb Pr Nd Sample Sm Eu Gd Tb Dy Ho Er Tm 

GR-153 33.0 340 180 18.0 <0.46 2.20 <68 <46 GR-153 <46 4.2 9.7 <22 <10 <10 <4.6 <2.2 

GR-154 26.0 130 150 18.0 <.46 1.90 <68 110 GR-154 <46 5.5 13.0 <22 <10 <10 <4.6 <2.2 

GR-155 11.0 140 120 12.0 1.80 .86 <68 <46 GR-155 <46 4.4 11.0 <22 <10 <10 <4.6 <2.2 

GR-156 8.8 170 100 13.0 1. 70 .65 <68 93 GR-156 <46 3.0 9.2 <22 <10 <10 <4.6 2.6 

GR-157 41.0 120 140 9.4 <.46 2.90 <68 82 GR-157 <46 3.1 9.2 <22 15 <10 <4.6 <2.2 

GR-158 54.0 120 130 7.7 1.90 3.70 <68 71 GR-158 <46 <1.0 11.0 <22 <10 <10 <4.6 <2.2 

GR-159 11.0 160 87 11.0 <.46 1.10 <68 53 GR-159 <46 3.3 15.0 <22 <10 <10 <4.6 <2.2 

GR-160 20.0 200 160 18.0 1.60 1.50 <68 75 GR-160 <46 4.9 2.5 <22 <10 <10 <4.6 <2.2 

GR-161 16.0 140 97 13.0 1.20 1.20 <68 99 GR-161 <46 2.9 6.5 <22 <10 <10 <4.6 <2.2 

GR-162 16.0 110 110 13.0 .64 1.40 <68 <46 GR-162 <46 2.4 13.0 <22 <10 <10 <4.6 <2.2 

GR-163 50.0 140 300 8.3 <.46 3.30 <68 160 GR-163 47 3.6 <2.2 <22 <10 <10 <4.6 <2.2 

GR-164 69.0 270 410 8.4 <.46 3.70 96 210 GR-164 53 2.2 5.9 <22 20 <10 <4.6 <2.2 

GR-165 29.0 140 130 8.6 <.46 2.70 <68 74 GR-165 <46 3.0 9.5 <22 <10 <10 <4.6 <2.2 

GR-166 53.0 360 170 11.0 1. 20 4.30 <68 130 GR-166 <46 3.7 12.0 <22 <10 <10 <4.6 <2.2 

GR-167 22.0 130 140 12.0 2.70 1.50 <68 54 GR-167 47 3.1 8.7 <22 <10 <10 <4.6 <2.2 

GR-168 15.0 160 140 10.0 <.46 1.30 <68 86 GR-168 <46 3.6 4.9 <22 <10 <10 <4.6 <2.2 

GR-169 50.0 480 200 12.0 <.46 4.10 <68 76 GR-169 <46 5.7 5.5 <22 <10 <10 <4.6 <2.2 

GR-170 72.0 78 130 6.8 1.30 5.70 <68 97 GR-170 <46 <1.0 7.9 <22 15 <10 <4.6 <2. 2 

GR-171 33.0 150 110 12.0 <.46 2.60 <68 130 GR-171 <46 <1.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR-172 23.0 180 120 9.8 1.70 1. 90 <68 54 GR-172 <46 4.2 11.0 <22 <10 <10 <4.6 <2.2 

GR-173 12.0 80 100 8.1 1.20 .90 <68 79 GR-173 <46 2.9 <2.2 <22 <10 <10 <4.6 <2.2 

GR-174 6.5 170 56 10.0 <.46 .64 <68 <46 GR-174 <46 2.1 7.7 <22 <10 <10 <4.6 2.3 

GR-175 9.5 90 68 7.8 <.46 .79 <68 57 GR-175 <46 <1.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR-176 19.0 140 62 11.0 <.46 1.40 <68 <46 GR-176 <46 1.8 5.8 <22 <10 <10 <4.6 <2.2 

GR-177 88.0 750 230 14.0 <.46 6.00 <68 77 GR-177 <46 8.2 11.0 <22 <10 <10 5.2 <2.2 

GR-178 140.0 600 470 13.0 <.46 23.00 110 130 GR-178 57 7.3 <2.2 <22 77 14 7.8 <2. 2 

GR-179 7.5 130 98 12.0 <.46 .77 <68 <46 GR-179 <46 <1.0 5.7 <22 <10 <10 <4.6 <2.2 

GR-180 6.3 160 60 15.0 <.46 .55 <68 96 GR-180 <46 2.2 12.0 <22 <10 <10 <4.6 <2.2 

GR-181 65.0 560 470 12.0 1.20 4.00 100 220 GR-181 62 10.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR-182 50.0 530 320 8.1 1.80 2. 70 91 170 GR-182 <46 <1.0 <2.2 <22 <10 <10 <4.6 <2.2 

GR-183 26.0 360 160 7.6 <.46 1. 70 <68 62 GR-183 <46 2.4 14.0 <22 <10 <10 <4.6 <2.2 

GR-184 41.0 130 96 6.6 <.46 2.80 <68 77 GR-184 <46 2.0 20.0 <22 <10 <10 <4.6 <2. 2 

GR-185 61.0 210 190 6.6 <.46 3.90 <68 110 GR-185 <46 2.2 9.5 <22 <10 <10 <4.6 <2.2 

GR-186 66.0 370 290 9.5 <.46 4.60 <68 <46 GR-186 <46 2.8 <2.2 <22 <10 <10 <4.6 <2. 2 

GR-187 100.0 770 330 11.0 <.46 9.60 100 180 GR-187 49 7.8 9.0 <22 <10 <10 4.8 <2.2 

GR-188 76.0 590 320 13.0 1. 80 5.00 73 160 GR-188 <46 9.3 <2. 2 <22 <10 <10 <4.6 <2.2 

GR-189 110.0 1,000 320 12.0 1.50 6.70 95 190 GR-189 50 11.0 <2.2 <22 <10 <10 5.2 <2.2 

GR-190 65.0 530 300 12.0 <.46 6.00 87 150 GR-190 50 9.3 <2.2 <22 <10 <10 <4.6 <2.2 

GR-191 13.0 30 <46 5.3 1.10 1.20 <68 <46 GR-191 <46 <1.0 6.1 <22 <10 <10 <4.6 3.8 

GR-192 13.0 100 100 7.1 1.60 1.20 <68 61 GR-192 <46 1.6 8.0 <22 <10 <10 <4.6 <2.2 

GR-193 53.0 270 150 9.0 <.46 4.50 <68 <46 GR-193 <46 3.0 13.0 <22 16 <10 <4.6 <2.2 

GR-194 63.0 250 250 12.0 1.30 4.70 <68 130 GR-194 <46 5.2 10.0 <22 19 <10 <4.6 <2.2 

GR-195 15.0 110 120 12.0 <.46 1.40 <68 <46 GR-195 <46 3.3 8.4 <22 <10 <10 <4.6 <2.2 

GR-196 11.0 64 68 6.1 1.80 1.20 <68 69 GR-196 <46 1.7 4.8 <22 <10 <10 <4.6 <2.2 

GR-197 79.0 300 200 9.7 2.60 6.80 <68 64 GR-197 <46 6.5 <2.2 <22 <10 <10 <4.6 <2.2 

GR-198 110.0 650 250 14.0 2.00 12.00 78 170 GR-198 53 6.1 15.0 <22 <10 <10 5.4 <2.2 

GR-199 16.0 130 54 8.1 1.70 1.60 <68 <46 GR-199 <46 3.3 14.0 <22 <10 <10 <4.6 <2.2 

GR-200 18.0 180 55 9.5 <.46 1.70 <68 <46 GR-200 <46 <1.0 19.0 <22 <10 <10 <4.6 <2.2 

GR-201 58.0 380 300 11.0 <.46 4.20 <68 120 GR-201 <46 6.2 6.2 <22 <10 <10 <4.6 <2.2 

GR-202 48.0 180 230 9.0 <.46 3.50 <68 <46 GR-202 <46 5.7 <2.2 <22 <10 <10 <4.6 <2.2 

Table 5 37 
Table 5. Plate-reader semiquantitative emiSSIOn spec- Table 5. Plate-reader semiquantitative emission spectrographic analyses (in parts per million) of granitoid trographic analyses (in parts per million) of granitoid 

rocks-Continued rocks-Continued 

Sample Ag B Be Co Cr Cu La Sample Mo Nb Ni Pb Sc Sn v w 

GR-203 <0.46 (5.0 1.6 4.00 8.20 0.88 49.0 GR-203 1.9 33.0 12.0 13.0 3.3 <4.6 16.0 <46 

GR-204 <.46 <5.0 (1.0 11.00 16.00 40.00 34.0 GR-204 1.9 11.0 13.0 17.0 7.7 4.7 42.0 <46 

GR-205 <.A6 <5.0 1.2 2.10 8.50 1.70 54.0 GR-205 1.2 26.0 2.6 15.0 4.7 <4.6 12.0 <46 

GR-206 <.46 <5.0 (1.0 <.46 1.80 <.22 78.0 GR-206 1.0 40.0 1. 7 18.0 3.0 <4.6 2.5 <46 

GR-207 <.46 12.0 1.8 7.40 6.60 13.00 100.0 GR-207 1.4 22.0 5.0 40.0 13.0 <4.6 25.0 <46 

GR-208 <.46 20.0 2.8 7.10 6.70 14.00 89.0 GR-208 2.2 26.0 11.0 34.0 12.0 <4.6 34.0 <46 

GR-209 <.46 <5.0 1.6 4.60 4.30 2.60 40.0 GR-209 1.7 24.0 4.8 17.0 4.0 <4.6 23.0 <46 

GR-210 <.46 <5.0 1.4 4.30 4.80 .78 44.0 GR-210 1.0 15.0 4.5 16.0 3.8 <4.6 22.0 <46 

GR-211 <.46 (5.0 (1.0 4.90 4.30 2.60 26.0 GR-2"11 1.3 11.0 4.5 14.0 3.7 <4.6 24.0 <46 

GR-212 <.46 <5.0 1.5 5.50 5.40 2.60 11.0 GR-212 1.2 27.0 11.0 19.0 4.5 <4.6 25.0 <46 

GR-213 <.46 <5.0 1.2 9.00 7.80 6.20 34.0 GR-213 2.1 11.0 7.3 14.0 9.4 <4.6 53.0 <46 

GR-214 <.46 (5.0 (1.0 8.40 5.60 4.20 32.0 GR-214 1.4 24.0 5.6 11.0 7.7 <4.6 59.0 <46 

GR-215 <.46 (5.0 1.7 4.00 8.30 .87 49.0 GR-215 2.0 33.0 12.0 13.0 3.3 <4.6 17.0 <46 

GR-216 <.46 (5.0 2.4 3.90 5.10 .78 60.0 GR-216 1.4 33.0 11.0 16.0 4.8 <4.6 17.0 <46 

GR-217 <.46 7.0 <1.0 25.00 43.00 74.00 59.0 GR-217 3.3 11.0 57.0 11.0 18.0 <4.6 190.0 <46 

GR-218 <.46 9.7 (1.0 31.00 49.00 160.00 61.0 GR-218 4.1 4.6 69.0 15.0 22.0 <4.6 210.0 <46 

GR-219 <.46 <5.0 1.6 12.00 7.70 12.00 63.0 GR-219 2.5 23.0 7.4 12.0 16.0 <4.6 79.0 <46 

GR-220 <.46 <5.0 1.1 3.00 1.80 1.80 57.0 GR-220 (1.0 11.0 2.5 11.0 2.5 <4.6 15.0 <46 

GR-221 <.46 (5.0 3.0 3.70 4.70 4.40 49.0 GR-221 1.1 37.0 4.4 28.0 12.0 4.7 14.0 <46 

GR-222 <.46 <5.0 2.6 3.80 4.30 4.00 38.0 GR-222 1.1 37.0 3.5 22.0 8.3 4.5 11.0 <46 

GR-223 <.46 <5.0 3.6 3.10 3.20 9.20 58.0 GR-223 <I.O 37.0 3.7 18.0 4.0 <4.6 14.0 <46 

GR-224 <.46 (5.0 1.3 3.10 4.80 4.20 85.0 GR-224 1.2 26.0 3.3 26.0 4.2 <4.6 27.0 <46 

GR-225 <.46 <5.0 2.6 6.40 5.20 7.60 130.0 GR-225 2.6 40.0 5.3 24.0 11.0 <4.6 34.0 <46 

GR-226 <.46 (5.0 2.5 6.20 5.50 5.10 78.0 GR-226 2.0 22.0 5.5 23.0 11.0 <4.6 29.0 <46 

GR-227 <.46 (5.0 <I.O 1.40 2.00 .45 90.0 GR-227 (1.0 19.0 2.1 17.0 2.4 <4.6 4.3 <46 

GR-228 <.46 <5.0 1.1 <.46 2.30 .48 63.0 GR-228 (1.0 29.0 2.1 16.0 2.6 <4.6 4.4 <46 

GR-229 <.46 <5.0 (1.0 .76 1.60 3.60 <4.6 GR-229 <I.O 16.0 1.6 31.0 1.4 <4.6 2.9 <46 

GR-230 <.46 (5.0 (1.0 <.46 2.10 2.50 5.0 GR-230 (1.0 12.0 1.5 22.0 1. 7 <4.6 2.4 <46 

38 Granitoid Rocks, Basin and Range Province 
Table 5. Plate-reader semiquantitative emiSSIOn spec- Table 5. Plate-reader semiquantitative emission spectrographic analyses (in parts per million) of granitoid trographic analyses (in parts per million) of granitoid 

rocks-Continued rocks-Continued 

Sample y Zr Ce Ga Ge Yb Pr Nd Sample Sm Eu Gd Tb Dy Ho Er Tm 

GR-203 16.0 83 110 9.4 1.90 1.30 (68 48 GR-203 46 (1.0 4.3 (22 <10 <10 <4.6 <2.2 

GR-204 12.0 200 100 14.0 1.90 1.10 (68 <46 GR-204 <46 3.5 16.0 <22 (10 (10 <4.6 <2.2 

GR-205 40.0 210 120 6.9 <.46 2.30 (68 60 GR-205 <46 (1.0 <2.2 <22 16 <10 <4.6 (2.2 

GR-206 27.0 150 120 8.0 1.80 2.00 <68 83 GR-206 51 (1.0 2.9 (22 (10 (10 <4. 6 <2.2 

GR-207 71.0 180 210 8.9 1.60 5.20 <68 65 GR-207 <46 5.1 12.0 (22 (10 (10 <4.6 (2.2 

GR-208 77.0 200 200 8.8 l. 80 11.00 <68 120 GR-208 48 5.4 7.7 <22 <10 <10 <4.6 (2.2 

GR-209 20.0 220 86 15.0 <.46 1.50 <68 72 GR-209 <46 (1.0 12.0 (22 <10 (10 (4.6 <2.2 

GR-210 11.0 270 94 13.0 <.46 1.10 (68 69 GR-210 <46 2.6 8.3 <22 (10 (10 <4.6 <2.2 

GR-211 11.0 110 59 14.0 1.10 .94 <68 53 GR-211 <46 2.7 12.0 <22 (10 (10 (4.6 <2.2 

GR-212 9.8 100 73 14.0 1.60 1.10 <68 <46 GR-212 (46 3.5 25.0 <22 <10 <10 <4.6 (2.2 

GR-213 25.0 86 110 11.0 1.30 2.10 (68 <46 GR-213 <46 4.0 22.0 <22 (10 (10 <4.6 <2.2 

GR-214 28.0 170 85 9.0 l. 90 2.40 <68 91 GR-214 <46 3.9 11.0 <22 (10 <10 <4.6 <2.2 

GR-215 15.0 84 110 9.4 <.46 1.30 <68 49 GR-215 <46 <1.0 3.8 26 (10 (10 <4.6 (2.2 

GR-216 20.0 150 120 10.0 <.46 1.70 (68 74 GR-216 <46 (1.0 19.0 <22 (10 <10 <4.6 2.4 

GR-217 25.0 130 140 11.0 .66 1.50 <68 72 GR-217 <46 2.8 13.0 <22 <10 (10 <4.6 <2.2 

GR-218 28.0 220 170 13.0 1.10 1.80 (68 47 GR-218 <46 3.8 13.0 <22 (10 (10 <4.6 <2.2 

GR-219 39.0 200 150 9.4 1.00 2.30 <68 180 GR-219 <46 3.7 9.9 <22 (10 (10 <4.6 (2.2 

GR-220 19.0 43 99 5.4 .60 1.50 (68 <46 GR-220 <46 (1.0 7.7 <22 <10 <10 <4.6 <2.2 

GR-221 84.0 64 120 10.0 2.00 8.70 <68 110 GR-221 <46 2.8 12.0 <22 24 (10 <4.6 <2.2 

GR-222 87.0 98 100 7.2 2.40 9.10 (68 <46 GR-222 <46 2.1 16.0 <22 18 <10 <4.6 3.2 

GR-223 27.0 130 120 6.5 <.46 1.70 <68 <46 GR-223 <46 2.1 13.0 <22 11 <10 <4.6 <2.2 

GR-224 31.0 230 170 8.1 .99 2.00 <68 <46 GR-224 (46 3.5 9.5 <22 (10 <10 <4.6 <2.2 

GR-225 65.0 350 210 9.3 2.20 5.10 <68 130 GR-225 (46 4.8 11.0 <22 <10 <10 <4.6 <2.2 

GR-226 62.0 380 170 8.7 <.46 5.50 (68 76 GR-226 <46 6.1 11.0 <22 <10 <10 (4.6 <2.2 

GR-227 27.0 140 170 5.3 .85 1.40 (68 63 GR-227 <46 <1.0 7.9 <22 <10 (10 <4.6 (2.2 

GR-228 26.0 210 140 5.7 <.46 1. 90 <68 50 GR-228 (46 3.1 7.1 <22 <10 <10 <4.6 <2.2 

GR-229 3.1 27 <46 14.0 .91 <.46 (68 <46 GR-229 <46 (1.0 8.9 (22 (10 <10 <4.6 2.4 

GR-230 2.9 17 47 12.0 <.46 <.46 (68 <46 GR-230 <46 2.2 9.9 <22 (10 <10 <4.6 <2.2 

Table 5 39 
Table 6. Plate-reader semiquantitative emiSSIOn spec- Table 6. Plate-reader semiquantitative emiSSIOn spectrographic analyses (in parts per million) of replicate sam- trographic analyses (in parts per million) of replicate sampies of granitoid rocks from the Basin and Range pro- pies of granitoid rocks-Continued 

vince 

Sample Ag B Be Co Cr Cu La Sample Mo Nb Ni Pb Sc Sn v w 

GR- 6a <0.46 <5.0 (1.0 12.00 21.0 11.00 61 GR- 6a 1.8 19.0 12.0 16.0 11.0 <4.6 75.0 <46 

GR- lOa .48 18.0 1.4 20.00 49.0 37.00 77 GR- lOa .2 18.0 30.0 24.0 18.0 <4.6 130.0 <46 

GR- 11a <.46 11.0 <1.0 22.00 53.0 61.00 69 GR- lla 3.7 7.3 31.0 25.0 18.0 <4.6 120.0 <46 

GR- 18a <.46 8.2 <1.0 22.00 24.0 3.30 74 GR- 18a 4.2 10.0 17.0 18.0 17.0 <4.6 160.0 <46 

GR- 2la <.46 <S.O 2.0 5.50 5.2 1.40 67 GR- 2la 1.1 45.0 3.9 41.0 3.5 (4.6 19.0 <46 

GR- 29a <.46 (5.0 1.3 7.20 6.5 3.90 30 GR- 29a 1.3 12.0 4.4 15.0 6.6 <4.6 58.0 <46 

GR- 32a <.46 12.0 (1.0 18.00 26.0 16.00 42 GR- 32a 2.1 8.8 17 .o 12.0 18.0 <4.6 150.0 <46 

GR- 43a <.46 (5.0 1.4 11.00 12.0 3.60 43 GR- 43a 4.1 16.0 8.7 16.0 12.0 <4.6 99.0 <46 

GR- 46a <.46 <S.O 2.3 2.30 3.9 1.60 33 GR- 46a <1.0 <2.2 3.0 24.0 3.4 <4.6 9.7 <46 

GR- 55a <.46 (5.0 1.4 2.80 2.7 .46 41 GR- 55a 1.2 23.0 4.4 13.0 2.7 <4.6 13.0 <46 

GR- 56a <.46 <5.0 <1.0 7.50 3.7 34.00 40 GR- 56a 2.4 13.0 4.8 11.0 6.0 <4.6 61.0 <46 

GR- 72a <.46 <5.0 (1.0 11.00 11.0 20.00 41 GR- 72a 1.4 12.0 12.0 12.0 4.8 <4.6 73.0 <46 

GR- 75a <.46 <5.0 1.2 11.00 11.0 7.80 39 GR- 75a 2.8 9.6 11.0 14.0 11.0 <4.6 90.0 <46 

GR- 79a <.46 (5.0 (1.0 9.20 17.0 6.70 56 GR- 79a 1.6 12.0 13.0 16.0 7.7 <4.6 78.0 <46 

GR- 83a <.46 <5.0 2.1 2.10 3.1 <.22 74 GR- 83a <1.0 10.0 3.5 18.0 3.8 <4. 6 13.0 <46 

GR- 85a <.46 <5.0 1.7 6.40 8.0 .26 69 GR- 85a 1.7 32.0 4.9 21.0 5.7 <4.6 31.0 <46 

GR- 87a <.46 <5.0 <1.0 13.00 14.0 6.80 39 GR- 87a 2.8 8.6 10.0 12.0 10.0 <4.6 100.0 <46 

GR- 95a <.46 <5.0 1.7 11.00 15.0 38.00 73 GR- 95a 2.0 27 .o 8.5 15.0 10.0 <4.6 65.0 <46 

GR- 96a <.46 <S.O 1.4 10.00 22.0 2.00 86 GR- 96a 2.6 24.0 11.0 14.0 10.0 <4.6 63.0 <46 

GR-102a <.46 9.9 1.7 11.00 26.0 21.00 86 GR-102a 1.9 44.0 15.0 9.6 9.6 <4.6 85.0 <46 

GR-103a <.46 <S.O 1.8 3.90 14.0 .92 31 GR-103a <1.0 29.0 10.0 8.9 7.2 <4.6 39.0 <46 

GR-105a <.46 <5.0 1.7 6.80 66.0 1.40 43 GR-105a 1.6 15.0 23.0 6.5 13.0 <4.6 110.0 <46 

GR-107a <.46 9.7 1.4 11.00 8.8 8.50 62 GR-107a 2.7 21.0 7.0 11.0 11.0 <4.6 120.0 <46 

GR-108a <.46 8.5 2.0 12.00 8.2 2.30 89 GR-108a 3.7 35.0 9.1 11.0 13.0 <4.6 110.0 <46 

GR-111a <.46 <S.O 1.8 2.90 2.4 18.00 37 GR-111a 1.8 19.0 11.0 15.0 2.9 <4.6 21.0 <46 

GR-llSa <.46 <S.O 1.3 6.20 5.5 14.00 37 GR-115a 2.5 5.5 6.1 18.0 5.6 <4.6 46.0 <46 

GR-124a <.46 <5.0 1.9 7.50 18.0 1.30 68 GR-124a 1.4 62.0 15.0 13.0 5.8 <4.6 46.0 <46 

GR-125a <.46 16.0 2.8 14.00 11.0 55.00 270 GR-125a 3.6 130.0 7.3 26.0 7.0 <4.6 85.0 <46 

GR-129a <.46 15.0 (1.0 25.00 25.0 44.00 61 GR-129a 6.6 20.0 19.0 13.0 16.0 <4.6 190.0 <46 

GR-133a <.46 19.0 1.3 7.20 10.0 2.60 73 GR-133a 1.5 12.0 11.0 12.0 6.3 <4.6 51.0 <46 

GR-144a <.46 (5.0 1.4 5.30 5.5 44.00 33 GR-144a <1.0 5.3 4.2 16.0 4.1 <4.6 23.0 <46 

GR-156a <.46 <5.0 <1.0 1.90 3.2 .71 48 GR-156a 1.0 25.0 2.4 20.0 2.9 <4.6 13.0 <46 

GR-166a <.46 <S.O 1. 5 6.40 4.6 4.40 84 GR-166a 2.2 32.0 6.7 17.0 10.0 <4.6 59.0 <46 

GR-167a <.46 (5.0 (1.0 18.00 15.0 39.00 45 GR-167a 2.9 14.0 12.0 18.0 14.0 <4.6 110.0 <46 

GR-178a <.46 <S.O 1.7 6.10 9.1 6.50 220 GR-178a 2.3 70.0 4.1 19.0 23.0 <4.6 20.0 <46 

GR-185a <.46 <5.0 3.0 10.00 7.9 13.00 130 GR-185a 3.4 32.0 5.9 32.0 15.0 <4.6 42.0 <46 

GR-188a <.46 <5.0 1.8 9.50 4.4 11.00 210 GR-188a 2.9 24.0 5.9 21.0 18.0 <4.6 44.0 <46 

GR-195a .48 <5.0 1.3 14.00 14.0 230.00 49 GR-195a 4.2 15.0 21.0 12.0 8.6 <4.6 94.0 68 

GR-196a <.46 <5.0 <1.0 4.60 5.2 43.00 42 GR-196a 1.0 10.0 5.7 11.0 2.4 <4.6 26.0 <46 

GR-203a <.46 <5.0 <1.0 8.20 7.1 22.00 41 GR-203a 1.1 6.6 7.4 12.0 4.2 <4.6 39.0 <46 

GR-205a <.46 <5.0 1.4 2.10 6.2 2.30 83 GR-205a 1.7 43.0 3.6 18.0 5.7 4.9 14.0 <46 

GR-206a <.46 <5.0 1.4 .92 1.9 .31 120 GR-206a (1.0 43.0 1.9 19.0 3.8 <4.6 2.2 <46 

GR-208a <.46 14.0 2.9 7.10 5.4 6.90 81 GR-208a 1.6 36.0 6.8 30.0 13.0 <4.6 32.0 <46 

GR-212a <.46 <5.0 1.0 5.00 4.0 2.40 19 GR-212a 1.0 20.0 5.2 17.0 4.2 <4.6 21.0 <46 

GR-215a <.46 <S.O 1.6 4.20 8.3 .91 70 GR-215a 1.0 17.0 5.8 14.0 4.0 <4.6 17.0 <46 

GR-217a <.46 6.3 (1.0 24.00 40.0 71.00 46 GR-217a 3.5 2.4 52.0 13.0 15.0 <4.6 170.0 <46 

GR-218a <.46 6.7 (1.0 28.00 48.0 120.00 61 GR-218a 3.7 13.0 64.0 16.0 19.0 <4.6 190.0 <46 

GR-221a <.46 (5.0 2.9 3.60 3.9 3.80 45 GR-221a 1.0 44.0 3.9 26.0 8.7 <4.6 12.0 <46 

GR-224a <.46 <5.0 1.7 4.50 6.1 3.70 88 GR-224a 1.3 34.0 3.7 29.0 5.9 <4.6 31.0 <46 

GR-225a <.46 <5.0 2.5 6.50 5.4 7.90 120 GR-225a 2.5 18.0 5.4 25.0 10.0 <4.6 32.0 <46 

40 Granitoid Rocks, Basin and Range Province 
Table 6. Plate-reader semiquantitative emission spec- Table 6. Plate-reader semiquantitative emiSSIOn spectrographic analyses (in parts per million) of replicate sam- trographic analyses (in parts per million) of replicate sampies of granitoid rocks-Continued pies of granitoid rocks-Continued 

Sample y Zr Ce Ga Ge Yb Pr Nd Sample Sm Eu Gd Tb Dy Ho Er Tm 

GR- 6a 29.0 290 130 12.0 <0.46 2.10 <68 76 GR- 6a <46 1.6 4.1 <22 <10 <10 <4.6 <2.2 

GR- lOa 27.0 350 170 13.0 2.10 1.70 (68 140 GR- lOa <46 (1.0 24.0 <22 <10 <10 <4.6 (2.2 

GR- 1la 21.0 170 170 15.0 <.46 1.70 <68 130 GR- lla <46 4.8 (2.2 <22 (10 <10 <4.6 (2.2 

GR- 18a 26.0 130 170 13.0 1.40 2.30 (68 98 GR- 18a <46 4.4 (2.2 (22 <10 <10 <4.6 (2.2 

GR- 2la 31.0 120 130 11.0 1.20 1. 60 <68 59 GR- 2la <46 2.4 5.7 <22 <10 <10 (4.6 (2.2 

GR- 29a 17.0 91 75 9.6 1.30 1.40 (68 <46 GR- 29a <46 3.6 9.1 (22 <10 <10 <4.6 (2.2 

GR- 32a 22.0 120 91 7.6 .63 1.50 (68 85 GR- 32a <46 3.3 (2.2 (22 <10 <10 (4.6 (2.2 

GR- 43a 16.0 200 110 10.0 <.46 1.50 (68 79 GR- 43a <46 2.9 16.0 <22 <10 <10 <4.6 (2.2 

GR- 46a 32.0 60 94 9.3 1. so 2.80 <68 63 GR- 46a <46 3.1 11.0 36 <10 <10 <4.6 (2.2 

GR- SSa 12.0 130 96 7.5 <.46 1.20 <68 (46 GR- SSa <46 1.7 14.0 33 (10 <10 (4.6 <2.2 

GR- 56a 12.0 91 120 8.0 <.46 1.20 <68 110 GR- 56a <46 2.9 2.6 (22 (10 <10 <4.6 <2.2 

GR- 72a 11.0 78 90 9.5 .56 1.00 <68 <46 GR- 72a <46 3.7 17.0 (22 <10 (10 <4.6 (2.2 

GR- 75a 13.0 83 100 16.0 .57 1.30 (68 <46 GR- 75a <46 3.1 25.0 (22 <10 <10 <4. 6 (2.2 

GR- 79a 14.0 180 99 13.0 <.46 1.10 (68 49 GR- 79a (46 (1.0 8.2 <22 <10 (10 <4.6 (2.2 

GR- 83a 7.9 160 120 14.0 <.46 .76 <68 110 GR- 83a <46 3.2 5.7 (22 <10 (10 <4. 6 (2.2 

GR- 85a 22.0 200 150 12.0 1.10 1.40 (68 59 GR- 85a (46 3.0 12.0 (22 (10 <10 (4.6 (2.2 

GR- 87a 14.0 78 110 14.0 .64 1.20 <68 160 GR- 87a <46 5.1 (2.2 (22 (10 <10 (4.6 (2.2 

GR- 95a 22.0 120 160 10.0 1.50 1.60 (68 91 GR- 95a <46 (1.0 9.9 (22 (10 (10 <4.6 (2.2 

GR- 96a 22.0 250 170 11.0 1.00 1.50 <68 70 GR- 96a <46 (1.0 (2.2 (22 (10 (10 <4.6 (2.2 

GR-102a 20.0 170 180 8.8 .98 1.20 (68 84 GR-102a <46 3.3 (2.2 (22 (10 (10 (4.6 (2.2 

GR-103a 17.0 160 83 10.0 2.40 1. 30 (68 70 GR-103a (46 s.o 11.0 (22 (10 (10 <4.6 <2.2 

GR-lOSa 25.0 190 120 12.0 1.40 1.90 (68 51 GR-105a <46 4.4 12.0 (22 <10 (10 <4.6 <2.2 

GR-107a 21.0 71 130 9.6 <.46 1.60 <68 87 GR-107a (46 4.0 14.0 (22 (10 (10 <4.6 (2.2 

GR-108a 24.0 130 170 12.0 2.10 1.70 <68 59 GR-108a <46 6.2 18.0 (22 (10 (10 (4.6 (2.2 

GR-11la 5.2 68 81 14.0 1.40 .62 (68 (46 GR-11la (46 (1.0 14.0 <22 (10 <10 (4.6 <2.2 

GR-llSa 11.0 140 100 12.0 <.46 .98 <68 82 GR-115a <46 3.2 7.7 (22 (10 (10 <4.6 (2.2 

GR-124a 20.0 240 160 7.4 (.46 1. 20 <68 <46 GR-124a <46 3.3 8.5 (22 <10 <10 <4.6 (2.2 

GR-125a 34.0 750 420 13.0 .99 1.90 81 160 GR-125a <46 7.6 (2.2 (22 (10 (10 <4.6 (2.2 

GR-129a 21.0 140 190 14.0 .69 1.80 (68 <46 GR-129a <46 s.o 29.0 (22 (10 (10 <4.6 (2.2 

GR-133a 15.0 220 150 13.0 1.70 1.30 <68 63 GR-133a <46 4.1 (2.2 (22 (10 (10 <4.6 (2.2 

GR-144a 6.5 100 59 15.0 .81 .77 <68 77 GR-144a (46 (1.0 8.2 (22 (10 (10 <4.6 (2.2 

GR-156a 8.3 130 110 9.8 (.46 .67 (68 76 GR-156a <46 3.2 14.0 (22 <10 (10 <4.6 (2.2 

GR-166a 45.0 220 160 8.5 1.90 3.30 <68 79 GR-166a (46 3.0 (2.2 (22 <10 <10 <4.6 <2.2 

GR-167a 19.0 93 100 14.0 <.46 1.40 (68 57 GR-167a <46 4.2 (2.2 (22 (10 <10 (4.6 (2.2 

GR-178a 150.0 770 430 11.0 <.46 17.00 110 130 GR-178a 64 5.3 31.0 (22 67 12 7.2 (2.2 

GR-185a 66.0 330 270 12.0 <.46 7.00 <68 69 GR-185a <46 5.2 10.0 (22 (10 (10 <4.6 (2.2 

GR-188a 69.0 730 360 12.0 1.40 4.40 <68 150 GR-188a <46 8.5 6.8 <22 (10 <10 <4.6 (2.2 

GR-195a 15.0 130 120 11.0 <.46 1.30 <68 90 GR-195a <46 2.1 (2.2 <22 (10 <10 (4.6 (2.2 

GR-196a 9.8 77 79 6.4 1.90 1.00 (68 73 GR-196a <46 2.5 14.0 (22 (10 (10 <4.6 <2.2 

GR-203a 9.7 230 99 13.0 .90 .77 <68 60 GR-203a <46 <1.0 6.3 (22 (10 (10 <4.6 (2.2 

GR-205a 45.0 410 150 9.4 3.20 3.10 (68 81 GR-20Sa <46 2.9 15.0 (22 <10 (10 <4.6 2.5 

GR-206a 41.0 290 170 8.9 <.46 2.60 <68 94 GR-206a (46 2.4 7.0 (22 (10 (10 <4.6 (2.2 

GR-208a 94.0 220 200 8.0 <.46 9.90 (68 140 GR-208a <46 4.1 (2.2 (22 (10 <10 <4.6 (2.2 

GR-212a 11.0 110 <46 12.0 <.46 .99 <68 <46 GR-212a (46 3.1 11.0 (22 (10 (10 <4.6 (2.2 

GR-215a 20.0 87 120 10.0 1.80 1.50 (68 110 GR-215a <46 2.4 12.0 (22 (10 <10 <4.6 (2.2 

GR-217a 23.0 140 110 11.0 <.46 1.40 (68 55 GR-217a <46 2.3 7.2 (22 (10 (10 <4.6 (2.2 

GR-218a 27.0 150 160 14.0 1.20 2.00 (68 90 GR-218a <46 4.7 16.0 (22 <10 <10 (4.6 <2.2 

GR-221a 83.0 92 97 7.9 1.90 8.00 <68 75 GR-221a <46 (1.0 22.0 (22 23 (10 (4.6 2.5 

GR-224a 39.0 300 190 ll.O 1.80 2.40 <68 120 GR-224a <46 4.0 4.7 (22 <10 <10 <4.6 <2.2 

GR-225a 62.0 350 230 10.0 <.46 5.60 (68 82 GR-22Sa 47 4.7 (2.2 <22 (10 (10 <4.6 (2.2 

Table 6 41 
Table 7. Quantitative X-ray fluorescence Table 7. Quantitative X-ray fluorescence 

values (in parts per million) for barium, values (in parts per million) for barium, 

rubidium, and strontium in granitoid rubidium, and strontium in granitoid 

rocks from the Basin and Range province rocks-Continued 

Sample Ba Rb Sr Sample Ba Rb Sr 

GR- 1 826 216 706 GR- 51 1,305 139 748 

GR- 2 709 277 549 GR- 52 1,341 122 800 

GR- 3 545 171 387 GR- 53 75 279 26 

GR- 4 598 180 391 GR- 54 153 230 34 

GR- 5 717 112 537 GR- 55 1,218 100 218 

GR- 6 759 150 482 GR- 56 1,120 134 607 

GR- 7 831 105 670 GR- 57 1,272 117 807 

GR- 8 810 139 587 GR- 58 1,330 112 836 

GR- 9 1,012 112 664 GR- 59 1,450 71 592 

GR- 10 1,068 118 657 GR- 60 1,473 74 580 

GR- 11 1,058 116 677 GR- 61 961 220 370 

GR- 12 994 112 639 GR- 62 1,142 231 439 

GR- 13 823 179 753 GR- 63 768 69 452 

GR- 14 797 187 680 GR- 64 798 61 473 

GR- 15 790 183 453 GR- 65 912 67 620 

GR- 16 445 179 348 GR- 66 883 82 600 

GR- 17 1,094 125 624 GR- 67 671 182 166 

GR- 18 948 141 622 GR- 68 699 188 174 

GR- 19 680 174 282 GR- 69 787 204 342 

GR- 20 739 159 302 GR- 70 916 157 284 

GR- 21 827 138 217 GR- 71 942 104 667 

GR- 22 567 123 202 GR- 72 979 100 684 

GR- 23 1,169 116 328 GR- 73 738 411 26 

GR- 24 694 112 264 GR- 74 709 307 134 

GR- 25 852 174 204 GR- 75 923 73 533 

GR- 26 598 190 155 GR- 76 929 71 464 

GR- 27 1 '112 107 731 GR- 77 1,001 82 585 

GR- 28 1,200 91 684 GR- 78 1,081 92 553 

GR- 29 1,182 124 462 GR- 79 1,298 53 594 

GR- 30 1,238 124 463 GR- 80 1,461 52 590 

GR- 31 1,168 39 642 GR- 81 905 128 449 

GR- 32 1,266 50 811 GR- 82 917 135 429 

GR- 33 1,478 152 212 GR- 83 1' 118 107 795 

GR- 34 1,548 145 226 GR- 84 1,286 116 785 

GR- 35 2,574 113 513 GR- 85 986 130 432 

GR- 36 2,209 124 453 GR- 86 1,004 135 439 

GR- 37 1,181 131 438 GR- 87 1,016 50 777 

GR- 38 1,512 141 502 GR- 88 978 60 745 

GR- 39 1,127 89 714 GR- 89 1,003 108 471 

GR- 40 1,018 137 588 GR- 90 1,001 91 499 

GR- 41 801 92 639 GR- 91 1,042 163 308 

GR- 42 995 158 343 GR- 92 639 256 203 

GR- 43 1,491 114 704 GR- 93 1,388 122 724 

GR- 44 1,171 146 545 GR- 94 1,529 156 888 

GR- 45 39 393 19 GR- 95 1,007 139 478 

GR- 46 499 236 188 GR- 96 1,125 164 479 

GR- 47 662 101 610 GR- 97 1,319 87 717 

GR- 48 724 113 671 GR- 98 1,445 87 761 

GR- 49 143 151 88 GR- 99 872 117 333 

GR- 50 571 173 234 GR-100 880 122 338 

42 Granitoid Rocks, Basin and Range Province 
Table 7. Quantitative X-ray fluorescence Table 7. Quantitative X-ray fluorescence 

values (in parts per million) for barium, values (in parts per million) for barium, 

rubidium, and strontium in granitoid rubidium, and strontium in granitoid 

rocks-Continued rocks-Continued 

Sample Ba Rb Sr Sample Ba Rb Sr 

GR-101 895 87 552 GR-153 1,590 118 1,283 

GR-102 1,059 84 681 GR-154 1,944 134 1,606 

GR-103 1,051 121 390 GR-155 1,091 118 559 

GR-104 1,116 115 323 GR-156 831 147 315 

GR-105 1,008 79 613 GR-157 844 185 201 

GR-106 650 47 530 GR-158 834 173 201 

GR-107 1,418 118 722 GR-159 915 131 617 

GR-108 1,421 122 854 GR-160 735 133 507 

GR-109 1,800 117 779 GR-161 787 102 646 

GR-110 1,577 117 711 GR-162 786 107 653 

GR-111 1,168 165 832 GR-163 316 336 44 

GR-112 1,512 151 829 GR-164 295 289 48 

GR-113 1,078 70 584 GR-165 741 162 305 

GR-114 1,021 71 565 GR-166 679 186 281 

GR-115 988 112 472 GR-167 925 94 581 

GR-116 970 58 676 GR-168 882 99 488 

GR-117 1,041 167 768 GR-169 1,275 100 206 

GR-118 1,100 181 966 GR-170 321 119 148 

GR-119 917 142 463 GR-171 910 80 643 

GR-120 965 140 468 GR-172 931 96 646 

GR-121 1,104 so 643 GR-173 915 90 653 

GR-122 922 81 490 GR-174 1,178 92 595 

GR-123 763 153 415 GR-175 940 150 323 

GR-124 790 138 482 GR-176 1,038 129 396 

GR-125 1,694 198 924 GR-177 1,626 94 224 

GR-126 1,144 140 625 GR-178 1,115 181 158 

GR-129 1,163 81 1,357 GR-179 651 lOS 520 

GR-130 860 79 1,073 GR-180 812 103 837 

GR-131 728 133 220 GR-181 1,580 190 568 

GR-132 732 141 274 GR-182 989 160 585 

GR-133 1,438 72 502 GR-183 1,550 188 556 

GR-134 1,643 103 436 GR-184 555 238 106 

GR-135 1,092 81 312 GR-185 896 234 269 

GR-136 1,109 69 309 GR-186 513 344 120 

GR-137 576 176 178 GR-187 1,435 234 204 

GR-138 624 194 274 GR-188 2,233 116 335 

GR-139 1,073 113 566 GR-189 2,382 91 265 

GR-140 1,155 104 667 GR-190 2,279 144 258 

GR-141 39 206 20 GR-191 91 302 22 

GR-142 38 215 27 GR-192 666 231 162 

GR-143 1,260 108 709 GR-193 198 305 35 

GR-144 380 123 625 GR-194 238 306 47 

GR-145 402 163 167 GR-195 827 160 541 

GR-146 750 100 224 GR-196 717 181 157 

GR-147 23 192 3 GR-197 932 219 164 

GR-148 20 196 4 GR-198 642 205 172 

GR-149 829 165 327 GR-199 658 146 300 

GR-150 769 193 281 GR-200 818 149 304 

GR-151 651 42 604 GR-201 1,538 120 498 

GR-152 496 26 574 GR-202 1,692 138 506 

Table 7 43 
Table 7. Quantitative X-ray fluorescence 

values (in parts per million) for barium, 

rubidium, and strontium in granitoid 

rocks-Continued 

Sample Ba Rb Sr 

GR-203 1,127 57 746 

GR-204 795 72 470 

GR-205 1,027 221 256 

GR-206 671 217 83 

GR-207 566 277 144 

GR-208 525 267 152 

GR-209 971 104 674 

GR-210 985 98 788 

GR-211 665 77 574 

GR-212 961 103 552 

GR-213 686 116 502 

GR-214 742 98 545 

GR-215 597 220 174 

GR-216 643 219 206 

GR-217 895 96 794 

GR-218 879 115 749 

GR-219 1,123 102 469 

GR-220 412 175 155 

GR-221 216 329 55 

GR-222 183 330 55 

GR-223 688 340 194 

GR-224 1,208 179 343 

GR-225 867 236 166 

GR-226 801 212 173 

GR-227 490 158 112 

GR-228 489 153 114 

GR-229 16 135 21 

GR-230 17 137 22 

44 Granitoid Rocks, Basin and Range Province 
Table 8. Quantitative neutron activa- Table 8. Quantitative neutron activation values for uranium and thorium in tion values for uranium and thorium in 

granitoid rocks from the Basin and granitoid rocks-Conitnued 

Range province 

u Th u Th 

Sample ppm ppm Th/U Sample ppm ppm Th/U 

GR- 1 14.38 46.97 3.27 GR- 51 1.89 13.01 6.88 

GR- 2 14.90 64.31 4.32 GR- 52 1. 73 10.11 5.84 

GR- 3 4.88 24.14 4.95 GR- 53 5.26 30.60 5.82 

GR- 4 5.74 25.76 4.49 GR- 54 5.63 36.85 6.55 

GR- 5 5.09 15.93 3.13 GR- 55 2.03 12.63 6.22 

GR- 6 7.77 20.99 2.70 GR- 56 5.86 14.49 2.47 

GR- 7 5.23 13.49 2.58 GR- 57 4.70 22.63 4.81 

GR- 8 5.00 26.90 5.38 GR- 58 3.08 15.17 4.93 

GR- 9 4.17 17.22 4.13 GR- 59 2.56 10.78 4.21 

GR- 10 3.90 21.10 5.41 GR- 60 3.04 14.27 4.69 

GR- 11 2.06 19.97 9.69 GR- 61 5.80 25.28 4.36 

GR- 12 2.35 16.51 7.03 GR- 62 6.49 26.14 4.03 

GR- 13 11.99 35.94 3.00 GR- 63 2.73 6.17 2.26 

GR- 14 14.71 39.09 2.66 GR- 64 2.48 6.77 2. 73 

GR- 15 4.69 23.28 4.96 GR- 65 3.35 7.19 2.15 

GR- 16 9.29 26.49 2.85 GR- 66 3.84 24.64 6.42 

GR- 17 4.71 16.82 3.57 GR- 67 2.03 16.52 8.14 

GR- 18 3.57 22.05 6.18 GR- 68 2.22 16.16 7.28 

GR- 19 4.72 19.17 4.06 GR- 69 2.65 5.84 2.20 

GR- 20 8.29 35.43 4.27 GR- 70 .95 4.54 4.78 

GR- 21 6.98 20.49 2.94 GR- 71 2.72 9.22 3.39 

GR- 22 3.46 16.96 4.90 GR- 72 2.81 6.72 2.39 

GR- 23 2.89 13.17 4.56 GR- 73 9.46 29.88 3.16 

GR- 24 2.20 11.52 5.24 GR- 74 6. 71 27.97 4.17 

GR- 25 2.63 7.80 2.97 GR- 75 2.53 5.31 2.10 

GR- 26 2.26 5.46 2.42 GR- 76 2.30 7.99 3.47 

GR- 27 3.09 10.64 3.44 GR- 77 2.08 6.50 3.13 

GR- 28 3.28 7.56 2.30 GR- 78 2.87 8.85 3.08 

GR- 29 7.80 10.76 1.38 GR- 79 2.39 6.25 2.62 

GR- 30 6.01 10.67 1.78 GR- 80 2.10 6.72 3.20 

GR- 31 3.53 5.67 1.61 GR- 81 2.77 16.74 6.04 

GR- 32 3.57 6.33 1.77 GR- 82 4.11 17.40 4.23 

GR- 33 2.56 4.94 1.93 GR- 83 1.19 8.97 7.54 

GR- 34 2.25 4.01 1.78 GR- 84 .95 8.82 9.28 

GR- 35 1. 75 23.09 13.19 GR- 85 3.57 20.95 5.87 

GR- 36 1.16 20.28 17.48 GR- 86 6.43 18.25 2.84 

GR- 37 4.69 13.36 2.85 GR- 87 2.17 2.93 1. 35 

GR- 38 3.87 14.62 3.78 GR- 88 1.87 5.26 2.81 

GR- 39 2.48 8.18 3.30 GR- 89 2.54 12.13 4.78 

GR- 40 3.54 5.08 1.44 GR- 90 2.42 9.47 3.91 

GR- 41 1.90 6.07 3.19 GR- 91 3.47 30.31 8.73 

GR- 42 2.09 10.52 5.03 GR- 92 5.28 31.46 5.96 

GR- 43 3.97 17.36 4.37 GR- 93 10.91 10.90 1.00 

GR- 44 4.80 17.01 3.54 GR- 94 6.76 20.35 3.01 

GR- 45 10.56 27.65 2.62 GR- 95 4.29 26.23 6.11 

GR- 46 13.31 17.49 1.31 GR- 96 4.72 27.13 5.75 

GR- 47 1.29 9.25 7.17 GR- 97 2.08 15.49 7.45 

GR- 48 2.10 10.81 5.15 GR- 98 2.13 13.53 6.35 

GR- 49 5. 29 24.54 4.64 GR- 99 2.60 16.47 6.33 

GR- 50 4.29 22.90 5.34 GR-100 2.28 14.12 6.19 

Table 8 45 
Table 8. Quantitative neutron activa- Table 8. Quantitative neutron activation values for uranium and thorium in tion values for uranium and thorium in 

granitoid rocks-Conitnued granitoid rocks-Conitnued 

u Th u Th 

Sample ppm ppm Th/U Sample ppm ppm Th/U 

GR-101 3.64 7.09 1.95 GR-151 1.15 3.64 3.17 

GR-102 2.76 7.62 2.76 GR-152 .86 2.12 2.47 

GR-103 3.75 14.80 3.95 GR-153 2.45 11.71 4.78 

GR-104 2.35 15.65 6.66 GR-154 2.91 15.74 5.41 

GR-105 3.00 10.76 3.59 GR-155 1.29 7.50 5.81 

GR-106 1.88 13.23 7.04 GR-156 2.47 12.06 4.88 

GR-107 3.90 11.77 3.02 GR-157 2.63 19.19 7.30 

GR-108 3.70 13.70 3.70 GR-158 3. 77 19.20 5.09 

GR-109 1. 77 13.63 7.70 GR-159 2.26 11.63 5.15 

GR-110 1.74 10.44 6.00 GR-160 2.95 22.19 7.52 

GR-111 7.32 12.54 1.71 GR-161 3.61 8.09 2.24 

GR-112 2.85 7.54 2.65 GR-162 5.01 13.13 2.62 

GR-113 2.31 6.65 2.88 GR-163 15.68 131.70 8.40 

GR-114 2.26 7.49 3.31 GR-164 13.92 124.70 8.96 

GR-115 3.27 12.74 3.90 GR-165 6.93 29.31 4.23 

GR-116 3.11 5.25 1.69 GR-166 7.76 26.25 3.38 

GR-117 2.76 12.60 4.57 GR-167 2.30 8.21 3.57 

GR-118 2.08 7.28 3.50 GR-168 2.04 12.12 5.94 

GR-119 4.32 22.48 5.20 GR-169 2.27 15.66 6.90 

GR-120 4.63 21.84 4.72 GR-170 3.36 46.77 13.92 

GR-121 .72 3.06 4.25 GR-171 1.51 5.05 3.34 

GR-122 1.34 10.03 7.49 GR-172 1.24 7.43 5.99 

GR-123 3.35 21.06 6.29 GR-173 1. 26 17.21 13.66 

GR-124 2.25 15.69 6.97 GR-174 .99 5.94 6.00 

GR-125 14.91 63.78 4.28 GR-175 1.48 7.94 5.36 

GR-126 6.74 30.45 4.52 GR-176 2.83 5.56 1. 96 

GR-129 2.49 6.85 2.75 GR-177 .81 4.84 5.98 

GR-130 2.89 7.49 2.59 GR-178 1.41 6.09 4.32 

GR-131 .93 8.26 8.88 GR-179 2.65 8.05 3.04 

GR-132 1.84 13.45 7.31 GR-180 1.·25 7.39 5.91 

GR-133 1. 84 7.97 4.33 GR-181 3.07 19.86 6.47 

GR-134 1.50 15.52 10.35 GR-182 2.68 16.12 6.01 

GR-135 2.39 12.14 5.08 GR-183 3.30 18.39 5.57 

GR-136 2.44 7.05 2.89 GR-184 3.46 14.21 4.11 

GR-137 6.15 18.63 3.03 GR-185 6.27 34.02 5.43 

GR-138 6.19 25.29 4.09 GR-186 14.09 82.46 5.85 

GR-139 2.98 17.97 6.03 GR-187 3.74 22.19 5.93 

GR-140 3.11 17.34 5.58 GR-188 1.40 12.59 8.99 

GR-141 5.50 34.74 6.32 GR-189 .67 3.52 5.26 

GR-142 5.41 39.58 7.32 GR-190 1.00 11.87 11.87 

GR-143 1.70 10.01 5.89 GR-191 4.02 12.83 3.19 

GR-144 2.12 10.87 5.13 GR-192 4.96 18.54 3.74 

GR-145 2.02 16.19 8.01 GR-193 9.43 36.23 3.84 

GR-146 1.75 12.94 7.39 GR-194 6.07 36.73 6.05 

GR-147 2.46 16.55 6.73 GR-195 9.38 29.72 3.17 

GR-148 3.71 18.60 5.01 GR-196 6.87 27.15 3.95 

GR-149 8.37 45.16 5.40 GR-197 4.41 26.86 6.09 

GR-150 11.82 43.41 3.67 GR-198 4.17 26.16 6.27 

GR-199 4.33 14.23 3.29 

GR-200 2.44 11.87 4.86 

46 Granitoid Rocks, Basin and Range Province 
Table 8. Quantitative neutron activation values for uranium and thorium in 

granitoid rocks--Conitnued 

u Th 

Sample ppm ppm Th/U 

GR-201 3.97 13.14 3.31 

GR-202 4.15 12.37 2.98 

GR-203 1.66 3.85 2.32 

GR-204 1.98 6.19 3.13 

GR-205 5.78 32.81 5.68 

GR-206 6.87 26.92 3.92 

GR-207 6.51 26.18 4.02 

GR-208 8.62 31.87 3.70 

GR-209 1. 21 5. 71 4.72 

GR-210 .97 6.63 6.84 

GR-211 .58 4.02 6.93 

GR-212 .58 3.02 5.21 

GR-213 2.16 6.15 2.85 

GR-214 2.10 8.71 4.15 

GR-215 5.25 22.92 4.37 

GR-216 6.22 19.24 3.09 

GR-217 3.19 9.56 3.00 

GR-218 3.47 10.84 3.12 

GR-219 3.81 11.36 2.98 

GR-220 6.78 42.75 6.31 

GR-221 5.62 27.85 4.96 

GR-222 5.94 22.32 3.76 

GR-223 4.58 19.03 4.16 

GR-224 3.14 23.16 7.38 

GR-225 6.61 29.43 4.45 

GR-226 4.58 22.12 4.83 

GR-227 7.14 22.69 3.18 

GR-228 6.83 17.88 2.62 

GR-229 3.64 5.02 1.38 

GR-230 3.34 3.75 1.12 

Table 8 47 
Table 9. Quantitative neutron activation 

values for uranium and thorium in replicate samples of granitoid rocks from the 

Basin and Range province 

u Th 

Sample ppm ppm Th/U 

GR- 3a 4.98 24.38 4.90 

GR- 6a 8.05 21.18 2.63 

GR- 9a 3.89 19.21 4.94 

GR- 12a 2.45 17.84 7.28 

GR- 14a 14.16 36.95 2.61 

GR- 16a 8.76 20.55 2.35 

GR- 36a 1.41 22.99 16.31 

GR- 49a 4.96 23.56 4.75 

GR- 58a 2.73 19.01 6.96 

GR- 64a 2.55 7.54 2.96 

GR- 71a 2.79 7.12 2.55 

GR-104a 2.45 12.41 5.07 

GR-109a 1. 92 11.76 6.13 

GR-122a 1.72 8.05 4.68 

GR-123a 3.58 19.41 5.42 

GR-137a 5.51 24.29 4.41 

GR-138a 6.47 23.95 3.70 

GR-139a 3.14 17.17 5.47 

GR-147a 2.39 18.26 7.64 

GR-148a 3.73 19.08 5.12 

GR-163a 14.78 129.40 8.76 

GR-177a .60 4.43 7.38 

GR-178a 1.33 5.94 4.47 

GR-179a 2.70 8.55 3.17 

GR-205a 5.49 30.32 5.52 

GR-206a 6.49 26.54 4.09 

GR-211a .71 3.96 5.56 

GR-212a .55 3.00 5.45 

GR-214a 2.18 8.86 4.06 

GR-223a 4.11 26.57 6.46 

48 Granitoid Rocks, Basin and Range Province 
Table 10. Quantitative emission spectrographic analyses (in parts per million) 

of granitoid rocks from the Basin and Range province 

Sample As Bi Cd Sb Zn Tl Cs Hg Li 

GR- 1 24.0 (0.20 0.120 <1.0 60.0 (1.0 8 (0.5 20 

GR- 2 18.0 (.20 .080 <1.0 49.0 (1.0 12 <.5 30 

GR- 3 7.0 1.30 <.010 (1.0 39.0 1.5 8 <.5 57 

GR- 4 8.0 (.20 .020 <1.0 36.0 1.4 5 (.5 37 

GR- 5 3.0 <.20 .055 <1.0 96.0 (1.0 (5 <.5 20 

GR- 6 3.0 .36 .040 1. 0 46.0 1.2 (5 <.5 27 

GR- 7 4.0 .60 .020 3.0 23.0 (1.0 6 (.5 20 

GR- 8 11.0 (.20 .080 (1.0 73.0 <1.0 (5 <.5 9 

GR- 9 6.0 <.20 .190 (1.0 23.0 1.4 <5 <.5 28 

GR- 10 3.0 (.20 .280 (1.0 41.0 <1.0 <5 (.5 23 

GR- 11 5.0 <.20 .045 <1.0 64.0 <1.0 8 <.5 40 

GR- 12 3.0 <.20 <.010 1. 8 22.0 (1.0 6 (.5 13 

GR- 13 7.0 <.20 .180 1.5 100.0 (1.0 14 <.5 11 

GR- 14 6.0 <.20 .210 <1.0 110.0 (1.0 6 (.5 16 

GR- 15 1.7 <.20 <.010 <1.0 34.0 2.1 5 <.5 38 

GR- 16 3.0 .70 <.010 1.4 8.0 2.0 <5 (.5 20 

GR- 17 23.0 .25 .230 <1.0 82.0 1.0 (5 <.5 11 

GR- 18 3.9 .83 .070 <1.0 43.0 (1.0 6 (.5 32 

GR- 19 11.0 <.20 .350 3.0 37.0 1.6 5 <.5 18 

GR- 20 2.2 <.20 .040 (1.0 57.0 2.0 (5 (.5 30 

GR- 21 5.0 <.20 .063 (1.0 64.0 (1.0 (5 <.5 42 

GR- 22 (1.0 <.20 .020 1.0 21.0 1.5 (5 (.5 46 

GR- 23 7.0 <.20 .015 <1.0 39.0 1.4 (5 <.5 40 

GR- 24 1. 3 <.20 <.010 1. 0 16.0 (1.0 (5 <.5 20 

GR- 25 2.4 .65 (1.000 (1.0 71.0 1.0 5 <.5 53 

GR- 26 3.3 .60 .070 (1.0 21.0 1. 0 5 <.5 55 

GR- 27 14.0 <.20 (.010 (1.0 40.0 (1.0 (5 (.5 30 

GR- 28 7.0 (.20 .100 1.0 38.0 (1.0 (5 <.5 24 

GR- 29 15.0 <.20 <.010 (1.0 55.0 (1.0 (5 <.5 50 

GR- 30 9.0 <.20 .020 <1.0 42.0 (1.0 5 <.5 39 

GR- 31 5.2 <.20 .100 1.0 84.0 (1.0 (5 <.5 18 

GR- 32 3.0 <.20 .470 <1.0 79.0 <1.0 (5 <.5 30 

GR- 33 (1.0 .26 .060 <1.0 76.0 (1.0 6 <.5 50 

GR- 34 7.0 <.20 .080 <1.0 50.0 2.0 (5 <.5 50 

GR- 35 11.0 <.20 .040 (1.0 68.0 1.6 (5 <.5 24 

GR- 36 1. 0 <.20 <.010 1.5 22.0 <1.0 (5 (.5 28 

GR- 37 2.9 .35 .028 <1.0 32.0 1.4 10 <.5 75 

GR- 38 8.0 <.20 .280 (1.0 54.0 1.0 7 <.5 33 

GR- 39 1.6 <.20 .040 (1.0 55.0 (1.0 <5 <.5 36 

GR- 40 <1.0 <.20 .023 (1. 0 67.0 (1.0 <5 (.5 26 

GR- 41 8.0 <.20 .032 (1.0 69.0 (1.0 5 <.5 50 

GR- 42 6.0 .70 .250 (1.0 32.0 1.7 5 <.5 38 

GR- 43 12.0 (.20 .310 (1.0 39.0 1.8 <5 <.5 34 

GR- 44 5.0 <.20 .060 (1.0 42.0 <1.0 5 <.5 20 

GR- 45 2.9 <.20 .090 1.0 23.0 7.0 (5 <.5 33 

GR- 46 8.0 <.20 (.010 (1. 0 31.0 2.0 5 <.5 29 

GR- 47 1.7 <.20 (.010 1.1 18.0 2.0 <5 (.5 41 

GR- 48 3.0 <.20 (.010 1. 0 21.0 1.4 <5 (.5 55 

GR- 49 2.0 .20 <.010 (1.0 2.0 1.0 <5 (.5 15 

GR- 50 <1.0 <.20 <.010 1.0 48.0 1.1 (5 (.5 41 

Table 10 49 
50 

Table 10. Quantitative emission spectrographic analyses (in parts per million) 

of granitoid rocks from the Basin and Range province 

Sample As Bi Cd Sb Zn Tl Cs Hg Li 

GR- 51 2.8 <0.20 <0.010 <1.0 50.0 1.2 <5 <0.5 15 

GR- 52 2.3 <.20 <.010 1. 0 99.0 1.1 <5 <.5 25 

GR- 53 3.0 <.20 <.010 2.7 4.8 3.2 <5 <.5 2 

GR- 54 3.0 <.20 <.010 2.1 6.0 1.4 <5 <.5 3 

GR- 55 2.2 <.20 .035 <1.0 26.0 (1.0 <5 <.5 16 

GR- 56 4.0 <.20 .100 <1.0 17.0 1.3 5 <.5 10 

GR- 57 10.0 <.20 .050 <1.0 47.0 <1.0 <5 <.5 39 

GR- 58 16.0 <.20 .023 <1.0 29.0 <1.0 <5 <.5 17 

GR- 59 6.0 <.20 .260 <1.0 100.0 <1.0 <5 <.5 18 

GR- 60 4.3 <.20 .050 1.8 41.0 <1.0 <5 <.5 16 

GR- 61 2.5 <.20 .040 <1.0 65.0 1. 6 9 <.5 79 

GR- 62 4.6 <.20 .090 1.8 48.0 2.2 6 <.5 44 

GR- 63 12.0 <.20 .230 <1.0 54.0 <1.0 <5 <.5 33 

GR- 64 14.0 <.20 .035 <1.0 42.0 <1.0 <5 <.5 10 

GR- 65 8.0 <.20 .022 <1.0 70.0 <1.0 6 <.5 39 

GR- 66 15.0 .70 .100 1.5 92.0 <1.0 <5 <.5 21 

GR- 67 1.7 1.00 .350 <1.0 57.0 <1.0 19 <.5 75 

GR- 68 3.0 <.20 .020 <1.0 39.0 <1.0 7 <.5 38 

GR- 69 9.0 .60 .014 <1.0 42.0 1.7 8 <.5 45 

GR- 70 1.0 <.20 <.010 1.0 17.0 2.5 <5 <.5 18 

GR- 71 10.0 <.20 .035 <1.0 48.0 <1.0 <5 <.5 40 

GR- 72 <1.0 <.20 .010 <1.0 78.0 <1.0 <5 <.5 22 

GR- 73 3.4 1.60 .250 3.8 60.0 3.1 41 <.5 175 

GR- 74 14.0 <.20 .050 <1.0 55.0 3.0 15 <.5 38 

GR- 75 1.8 <.20 .060 <1.0 61.0 <1.0 <5 <.5 30 

GR- 76 8.1 <.20 .050 2.0 32.0 1. 0 <5 <.5 35 

GR- 77 <1.0 <.20 .030 <1.0 30.0 <1.0 5 <.5 30 

GR- 78 <1.0 <.20 .012 <1.0 64.0 <1.0 <5 <.5 36 

GR- 79 3.3 <.20 .030 1.0 29.0 (1.0 <5 <.5 35 

GR- 80 4.1 <.20 .060 <1.0 62.0 <1.0 <5 <.5 49 

GR- 81 <1.0 <.20 .018 <1.0 80.0 (1.0 <5 <.5 25 

GR- 82 12.0 <.20 .080 <1.0 45.0 1.5 <5 <.5 28 

GR- 83 <1.0 <.20 <.010 <1.0 25.0 2.0 6 <.5 50 

GR- 84 12.0 <.20 .038 <1.0 84.0 1.0 <5 <.5 40 

GR- 85 11.0 <.20 .030 <1.0 49.0 1.4 <5 <.5 28 

GR- 86 <1.0 <.20 <.010 <1.0 60.0 2.0 5 <.5 41 

GR- 87 1.7 <.20 .020 <1.0 48.0 (1.0 <5 <.5 16 

GR- 88 9.0 <.20 .020 <1.0 58.0 <1.0 <5 <.5 26 

GR- 89 9.0 1.20 .030 1.0 24.0 (1.0 5 <.5 26 

GR- 90 8.0 <.20 .290 4.8 12.0 1.7 <5 <.5 34 

GR- 91 10.0 <.20 .031 <1.0 35.0 1.4 (5 .9 34 

GR- 92 5.6 1.00 .010 1. 0 24.0 1. 8 8 <.5 55 

GR- 93 11.0 <.20 .050 4.6 62.0 (1.0 6 <.5 29 

GR- 94 7.0 <.20 .300 (1.0 19.0 1.0 28 <.5 50 

GR- 95 12.0 1.50 .100 <1.0 48.0 1.0 (5 <.5 36 

GR- 96 1. 8 <.20 .060 <1.0 84.0 1.2 (5 (.5 31 

GR- 97 14.0 <.20 .200 (1.0 38.0 <1.0 <5 <.5 22 

GR- 98 15.0 <.20 1.000 (1.0 62.0 1. 3 <5 <.5 16 

GR- 99 18.0 .67 .210 <1.0 93.0 <1.0 <5 <.5 50 

GR-100 2.3 <.20 .050 <1.0 38.0 (1.0 7 (.5 50 

Granitoid Rocks, Basin and Range Province 
Table 10. Quantitative emission spectrographic analyses (in parts per million) 

of granitoid rocks from the Basin and Range province 

Sample As Bi Cd Sb Zn Tl Cs Hg Li 

GR-101 2.2 (0.20 0.060 1. 8 31.0 (1.0 (5 (0.5 23 

GR-102 5.5 <.20 .020 (1.0 42.0 (1.0 7 <.5 20 

GR-103 13.0 .60 .080 2.0 14.0 (1.0 (5 <.5 20 

GR-104 (1.0 <.20 (1.000 (1.0 26.0 (1.0 (5 <.5 15 

GR-105 (1.0 <.20 .100 (1.0 15.0 <1.0 8 <.5 6 

GR-106 (1.0 (.20 .040 (1.0 41.0 (1.0 6 <.5 24 

GR-107 (1.0 .78 .150 <1.0 42.0 <1.0 7 <.5 22 

GR-108 18.0 .80 .080 2.0 44.0 <1.0 (5 <.5 24 

GR-109 2.3 <.20 <.010 <1.0 20.0 (1.0 (5 (.5 42 

GR-110 6.5 1. 70 (.010 (1.0 23.0 1.2 <5 <.5 33 

GR-111 16.0 <.20 (.010 (1.0 64.0 2.0 (5 <.5 56 

GR-112 11.0 <.20 .060 (1.0 100.0 2.0 <5 (.5 47 

GR-113 3.0 <.20 .069 (1.0 34.0 (1.0 <5 <.5 29 

GR-114 7.0 <.20 .037 (1.0 26.0 (1.0 (5 <.5 19 

GR-115 2.6 <.20 .056 <1.0 56.0 (1.0 6 (.5 50 

GR-116 7.0 <.20 .014 <1.0 46.0 (1.0 <5 <.5 10 

GR-117 <1.0 <.20 .094 <1.0 24.0 <1.0 (5 <.5 64 

GR-118 13.0 .40 .048 (1.0 54.0 1.7 6 <.5 53 

GR-119 6.0 .80 .025 <1.0 50.0 (1.0 5 <.5 43 

GR-120 13.0 1.40 .170 (1.0 82.0 1. 0 (5 (.5 38 

GR-121 8.0 <.20 .160 1.0 41.0 (1.0 (5 <.5 30 

GR-122 6.0 2.50 <.010 (1.0 36.0 <1.0 (5 <.5 38 

GR-123 1.5 <.20 <.010 (1.0 55.0 (1.0 5 <.5 35 

GR-124 3.0 <.20 .070 <1.0 19.0 (1.0 5 <.5 51 

GR-125 23.0 <.20 .100 <1.0 74.0 1.0 (5 (.5 32 

GR-126 3.6 .90 .120 2.4 22.0 2.2 8 <.5 27 

GR-129 7.0 .50 .260 (1.0 100.0 <1.0 <5 <.5 59 

GR-130 5.0 .80 .200 (1.0 110.0 <1. 0 <5 <.5 49 

GR-131 8.0 <.20 .017 <1.0 27.0 1.2 (5 <.5 13 

GR-132 3.0 <.20 <.010 (1.0 20.0 (1.0 (5 (.5 13 

GR-133 4.0 <.20 .080 <1.0 30.0 <1.0 <5 (.5 8 

GR-134 6.2 (.20 .020 1. 0 20.0 (1.0 <5 <.5 18 

GR-135 3.0 <.20 .020 <1.0 25.0 <1.0 (5 <.5 6 

GR-136 4.0 <.20 .010 <1.0 29.0 (1.0 <5 <.5 6 

GR-137 11.0 <.20 .012 <1.0 60.0 1.3 <5 <.5 28 

GR-138 1.5 .28 .080 <1.0 44.0 2.0 5 (.5 20 

GR-139 12.0 .30 .070 1. 0 80.0 1. 2 (5 (.5 20 

GR-140 2.9 <.20 .094 (1.0 45.0 (1.0 <5 <.5 16 

GR-141 17.0 <.20 .073 (1.0 60.0 2.0 (5 (.5 13 

GR-142 8.0 <.20 .020 (1.0 18.0 2.0 (5 (.5 10 

GR-143 22.0 1.20 <.010 <1.0 63.0 (1.0 (5 <.5 6 

GR-144 24.0 <.20 (.010 <1. 0 56.0 <1.0 <5 <.5 25 

GR-145 1.0 <.20 <.010 (1.0 46.0 1.0 (5 <.5 28 

GR-146 1. 4 <.20 (.010 <1.0 19.0 1. 0 (5 <.5 14 

GR-147 6.0 <.20 .400 <1.0 40.0 1.0 <5 <.5 13 

GR-148 4.0 <.20 (.010 <1.0 36.0 1.0 (5 <.5 13 

GR-149 2.0 <.20 .070 (1.0 21.0 1. 3 5 <.5 5 

GR-150 3.9 <.20 .030 (1.0 34.0 1. 0 (5 (.5 4 

GR-151 2.0 <.20 .260 1.0 72.0 (1.0 (5 <.5 4 

GR-152 (1.0 <.20 .014 <1.0 48.0 <1.0 (5 <.5 5 

Table 10 51 
52 

Table 10. Quantitative emission spectrographic analyses (in parts per million) 

of granitoid rocks from the Basin and Range province 

Sample As Bi Cd Sb Zn Tl Cs Hg Li 

GR-153 6.0 (0.20 0.600 (1.0 43.0 (1.0 <S (0.5 9 

GR-154 12.0 <.20 .oso (1.0 72.0 (1.0 <S (.5 9 

GR-155 16.0 (.20 .450 1.2 38.0 (1.0 (5 .8 38 

GR-156 (1.0 (.20 <.010 (1.0 56.0 (1.0 <S (.5 27 

GR-157 10.0 <.20 .200 (1.0 18.0 1.0 <S (.5 13 

GR-158 14.0 <.20 (.010 (1.0 50.0 1.2 <S (.5 14 

GR-159 7.0 (.20 .090 1.6 20.0 1.2 <S <.S 16 

GR-160 16.0 <.20 .130 (1. 0 69.0 2.0 (5 (.5 11 

GR-161 7.0 <.20 .300 1.0 100.0 1.0 <S (.5 14 

GR-162 <1.0 <.20 .020 (1.0 96.0 <1.0 <S (.5 15 

GR-163 14.0 .40 .oss (1.0 22.0 1.9 <S (.5 13 

GR-164 3.0 (.20 <.010 (1.0 19.0 1.7 <S (.5 6 

GR-165 24.0 1.00 .100 (1.0 75.0 1.4 <S (.5 10 

GR-166 4.6 4.40 .390 1. 0 80.0 1.5 6 <.S 14 

GR-167 9.0 (.20 .060 (1.0 64.0 (1.0 <S (.5 22 

GR-168 16.0 (.20 .oss (1.0 86.0 (1.0 <S (.5 10 

GR-169 16.0 .80 .130 (1.0 110.0 (1.0 <S <.5 8 

GR-170 4.0 <.20 .200 (1.0 27.0 (1.0 <S (.5 6 

GR-171 4.1 <.20 .030 (1.0 88.0 (1.0 5 <.S 18 

GR-172 (1.0 (.20 .013 (1.0 74.0 (1.0 <S <.5 14 

GR-173 20.0 <.20 <.010 (1.0 90.0 1.3 <S (.5 20 

GR-174 <1.0 <.20 .040 (1.0 36.0 (1.0 (5 (.5 21 

GR-175 <1.0 (.20 .016 (1.0 42.0 (1.0 <S (.5 23 

GR-176 14.0 <.20 .065 (1.0 44.0 1.1 <S <.5 10 

GR-177 4.3 .91 .370 1.8 72.0 (1.0 (5 <.S 7 

GR-178 10.0 .80 .170 (1.0 180.0 1. 0 (5 (.5 6 

GR-179 20.0 .69 (.010 (1.0 77.0 1.5 '(5 (.5 36 

GR-180 10.0 <.20 (.010 (1.0 40.0 2.0 <S (.5 so 

GR-181 1.8 <.20 .020 (1.0 86.0 1.5 <S <.S 39 

GR-182 6.3 (.20 (.010 (1.0 29.0 1.8 <S (.5 10 

GR-183 6.0 .90 .044 1.0 26.0 3.9 8 (.5 34 

GR-184 2.0 <.20 .030 (1.0 20.0 2.0 11 (.5 18 

GR-185 3.0 .30 .400 (1.0 93.0 1.2 11 <.S 51 

GR-186 2.9 <.20 .340 (1. 0 36.0 2.4 20 (.5 65 

GR-187 1.3 <.20 .015 (1.0 48.0 1.5 6 <.S 39 

GR-188 6.0 1.00 .070 (1.0 54.0 (1.0 (5 (.5 44 

GR-189 s.s <.20 .300 (1.0 69.0 (1.0 (5 <.S 9 

GR-190 (1.0 (.20 .170 (1.0 36.0 2.6 <S (.5 14 

GR-191 4.0 .40 .oss (1.0 28.0 1.5 7 (.5 10 

GR-192 2.4 1.10 .040 (1. 0 28.0 (1.0 6 (.5 16 

GR-193 1.7 (.20 (.010 (1.0 26.0 1.4 6 <.S 37 

GR-194 1.2 <.20 (.010 (1.0 64.0 1. 5 (5 (.5 22 

GR-195 27.0 1.10 .053 (1.0 68.0 1.0 <S .s 23 

GR-196 10.0 <.20 .140 (1.0 16.0 (1.0 6 (.5 9 

GR-197 20.0 1.20 .110 <I .o 72.0 1.0 <S (.5 14 

GR-198 9.0 .20 .670 (1.0 150.0 1.4 8 (.5 29 

GR-199 3.0 <.20 .090 (1.0 20.0 (1.0 <S (.5 36 

GR-200 <1.0 (.20 (.010 (1.0 34.0 1.5 5 (.5 31 

GR-201 s.o (.20 .010 (1.0 55.0 (1.0 6 (.5 54 

GR-202 9.0 <.20 .011 (1.0 49.0 (1.0 (5 (.5 47 

Granitoid Rocks, Basin and Range Province 
Table 10. Quantitative emission spectrographic analyses (in parts per million) 

of granitoid rocks from the Basin and Range province 

Sample As Bi Cd Sb Zn Tl Cs Hg Li 

GR-203 5.0 0.50 0.040 <1.0 52.0 <1.0 <S <0.5 40 

GR-204 8.0 <.20 .040 <1.0 70.0 (1.0 <S <.5 32 

GR-205 9.0 <.20 .094 <1.0 52.0 1.2 5 <.5 40 

GR-206 1.6 <.20 .030 <1.0 33.0 <1.0 <5 <.5 20 

GR-207 5.0 1.60 .055 (1.0 46.0 2.1 8 <.5 39 

GR-208 14.0 .so .050 <1.0 38.0 2.0 7 <.5 30 

GR-209 3.6 <.20 .020 <1.0 80.0 1.0 <S <.5 36 

GR-210 5.0 <.20 .030 (1.0 35.0 <1.0 <S <.5 50 

GR-211 14.0 <.20 .300 <1.0 42.0 1.0 <S <.5 37 

GR-212 24.0 .80 .058 <1.0 75.0 <1.0 <5 .6 37 

GR-213 28.0 1.30 <.010 <1.0 100.0 <1.0 <S <.5 32 

GR-214 6.0 <.20 .220 1.8 68.0 <1.0 18 <.5 46 

GR-215 14.0 <.20 <.010 <1.0 10.0 2.0 <S <.5 12 

GR-216 5.0 <.20 <.010 <1.0 40.0 1.0 6 <.5 12 

GR-217 5.0 <.20 .480 1.0 69.0 <1.0 <5 <.5 15 

GR-218 7.0 <.20 .050 <1.0 95.0 (1.0 5 <.5 27 

GR-219 11.0 <.20 .046 (1.0 56.0 <1.0 6 <.5 38 

GR-220 2.0 <.20 .080 1. 3 9.0 1. 9 <5 <.5 15 

GR-221 1.4 .61 .040 <1.0 64.0 1.8 30 <.5 55 

GR-222 <1 0 .48 (.010 <1.0 30.0 1.7 49 <.5 65 

GR-223 (1.0 3.00 .100 <1.0 18.0 3.8 21 <.5 38 

GR-224 2.6 .65 .070 <1.0 43.0 2.0 12 <.5 49 

GR-225 2.6 .so .010 1.0 24.0 1.7 9 <.5 42 

GR-226 17.0 <.20 .040 1.0 64.0 2.0 7 <.S 40 

GR-227 2.6 <.20 .100 <1.0 11.0 1.0 <S <.5 4 

GR-228 3.1 <.20 <.010 <1.0 19.0 1. 3 <S <.5 4 

GR-229 (1.0 <.20 .060 <1.0 16.0 1.6 <S <.5 5 

GR-230 <1.0 <.20 .030 <1.0 22.0 1.0 <5 <.5 6 

Table 10 53 
54 

Table 11. Quantitative emission spectrographic analyses (in parts per million) 

of replicate samples of granitoid rocks from the Basin and Range province 

Sample As Bi Cd Sb Zn Tl Cs Hg Li 

GR- 6a 1.8 (0.20 0.044 <1.0 32 1.1 6 (0.5 28 

GR- lOa 20.0 2.00 .800 9.0 so (1.0 <5 <.5 26 

GR- 11a 18.0 .90 .100 (1.0 60 (1.0 6 <.S so 

GR- 18a 15.0 .27 .280 (1.0 71 1. 0 6 <.5 32 

GR- 2la 8.0 <.20 .430 2.0 75 2.6 <S <.S so 

GR- 29a 3.8 <.20 .020 1. 0 22 (1.0 6 (.5 60 

GR- 32a (1.0 <.20 .200 <1.0 34 (1.0 (5 <.S 22 

GR- 43a 20.0 .90 .110 (1.0 71 1. 0 <S <.S 15 

GR- 46a 16.0 (.20 .027 <1.0 24 1.5 (5 .7 27 

GR- SSa 10.0 <.20 .020 <1.0 26 (1.0 (5 <.S 11 

GR- 56a 13.0 <.20 .054 <1.0 51 1.0 5 <.5 13 

GR- 72a (1.0 <.20 <.010 (1.0 24 (1.0 12 <.S 27 

GR- 75a 14.0 <.20 .100 (1.0 120 (1.0 <S <.5 38 

GR- 79a 13.0 <.20 .110 <1.0 110 (1.0 <S (.5 32 

GR- 83a 2.6 <.20 (.010 <1.0 23 (1.0 5 (.5 55 

GR- 85a 5.3 <.20 .020 (1.0 120 1.5 <S <.S 44 

GR- 87a 7.0 <.20 .010 (1.0 66 (1.0 <S <.5 22 

GR- 95a 12.0 <.20 .091 (1.0 32 1.2 <S (.5 16 

GR- 96a s.o <.20 .020 (1.0 33 1.5 (5 <.S 28 

GR-102a 1.2 <.20 .230 <1.0 56 1. 0 <S <.S 54 

GR-103a 1.7 <.20 .015 <1.0 6 (1.0 <S <.S 15 

GR-lOSa 16.0 <.20 .069 <1.0 20 (1.0 <S (.5 8 

GR-107a 5.8 <.20 .030 <1.0 59 (1.0 7 <.S 25 

GR-108a 12.0 <.20 .040 (1.0 52 <1.0 (5 <.S 20 

GR-11la 26.0 <.20 <.010 <1.0 94 1.5 5 <.S 24 

GR-115a 18.0 <.20 <.010 1.0 66 (1.0 6 <.S 40 

GR-124a 3.6 <.20 (.010 (1.0 33 (1.0 5 <.5 47 

GR-125a 3.5 .so .020 1.5 23 (1.0 5 (.5 28 

GR-129a <1.0 <.20 .026 <1.0 120 (1.0 (5 <.S 28 

GR-133a 9.0 <.20 <.010 (1.0 18 (1.0 <S <.5 6 

GR-144a s.o <.20 (.010 2.5 20 1.0 <S <.S 21 

GR-156a (1.0 <.20 <.010 (1.0 21 1. 0 (5 (.5 24 

GR-166a 3.3 .65 .270 <1.0 50 2.0 6 (.5 16 

GR-167a 4.1 <.20 .020 2.5 24 (1.0 (5 <.S 18 

GR-178a 2.6 <.20 .140 <1.0 72 (1.0 <S (.5 7 

GR-185a 22.0 .88 .081 (1.0 150 1.8 7 <.5 so 

GR-188a <1.0 <.20 .130 <1.0 28 (1.0 12 <.S 28 

GR-195a 11.0 .80 .030 (1.0 31 <1.0 6 (.5 31 

GR-196a 2.0 <.20 (.010 1.4 12 1. 8 6 <.S 10 

GR-203a 6.0 <.20 130 1.0 22 (1.0 (5 (.5 40 

GR-205a 1.0 <.20 .060 <1.0 68 1.0 6 <.S 41 

GR-206a 2.3 <.20 .030 (1.0 9 1. 0 5 (.5 20 

GR-208a 12.0 .so .078 <1.0 33 2.0 7 (.5 29 

GR-212a 2.0 <.20 <.010 <1.0 35 (1.0 <S (.5 39 

GR-215a 1.2 <.20 <1.000 <1.0 20 1.0 <5 <.S 12 

GR-217a 4.8 <.20 .oso <1.0 52 (1.0 6 <.S 29 

GR-218a 6.0 <.20 .220 (1.0 10 (1.0 <S <.S 12 

GR-22la 1.3 .44 <.010 (1.0 48 1.5 23 (.5 70 

GR-224a 1.0 .62 .060 <1.0 120 1.5 13 <.5 98 

GR-225a 2.4 <.20 .110 <1.0 60 1.6 13 (.5 59 

Granitoid Rocks, Basin and Range Province *U.S OOVERIIMENT PRINTINGOFRCE: 198~776-041/4006 FEGION NO.8