geothermal resource potential of the safford-san simon basin, arizona

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Table 2A. Analyses <strong>of</strong> Gila Valley-Indian Hot Springs ground waters Number 8amp1e Location Temperature TD8 pH Na K Ca Mg c1 8°4 HC0 3 +C0 3 810 2 Li B F Remarks Data Source Na+K 1 57 D-6-25-36CBBB 46 4431 6.8 1390 13.1 64 7.6 4011 672 64 55 2.3 0.6 6.7 W 1 2 53W86 D-5-24-17ADDCA 46 2967 7.5 670 13 39 7.2 1430 365 69 45 1.41 1.64 2.8 8 1 3 54W80 D-5-24-17ADDDB 45 2929 7.5 540 14 38 7.1 1414 348 98 48 1.42 0.94 5.2 8 1 4 55W80 D-5-24-17ADDBB 47 7.5 610 14 38 8.0 1257 325 120 49 1.25 1.64 4.0 8 1 5 1817 D-5-24-17AD 47.8 2570 - 879 78 9.6 1195 348 105 - - 2.0 3.9 8 3 6 1818 D-5-24-17AD 40 2970 - 1027 83 11 1400 395 106 - - 0.8 4.8 8 3 7 1822 D-5-24-17AD 47.8 2970 - 1023 81 14 1400 402 101 - - - 3.4 8 3 8 1823 D-5-24-17AD 47.8 2960 - 1026 80 12 1400 393 100 - - 0.8 4.6 8 3 9 2600 D-6-24-13AB 58.9 3530 - 1220 74 8.7 1660 416 101 - - 7.0 6.0 W 3 10 2683 D-7-24-17BD 30.0 2740 - 739 226 33 1250 426 116 - - 8.0 1.4 W 3 11 AZ10 D-5-24-17A 47 2672 7.9 837 13.6 80 9.0 1196 323 107 44 1.30 0.58 3.4 8 5 If) m 12 AZ11 D-5-24-17A 46.5 3004 7.9 10Z3 12.9 93 10.3 1382 361 101 44 - 0.70 3.8 8 5 13 AZ14 D-6-25-36C 43.5 8292 7.9 3027 10.9 135 7.9 4517 787 81 66 2.77 1.65 7.2 W 5 14 AZ21 D-5-24-17AD 33 3048 7.5 921 12.9 81 8.0 1412 338 109 57 - 0.84 3.9 8 5 15 AZ155 D-7-25-7CCC 29.5 9288 8.1 3072 14.5 133 28 3956 1455 46 27.5 4.05 2.33 6.27 W 5 16 AZ156 D-7-24-14DD 25.5 1804 8.3 709 2.7 9.2 0.7 688 452 107 27.0 - 1.62 7.8 W 5 . Ii,
Table 2B. Analyses <strong>of</strong> Buena Vista area ground waters Number Sample Location Temperature TDS pH Na K Ca Mg C1 S04 HC0 3 +C0 3 Si0 2 Li Na+K B F Remarks Data Source 3548 D-7-27-10AAD 792 7.7 163 69 15 218 70 244 1.0 W 4 1 58 D-7-27-11BBB 49 1094 7.5 333 3.9 1 0.1 212 272 205 62 0.4
Page 1:
GEOTHERMAL RESOURCE POTENTIAL OF TH
Page 5 and 6:
TABLE OF CONTENTS PAGE List Of Figu
Page 7 and 8:
FIGURES FIGURE 1 FIGURE 2 FIGURE 3
Page 9 and 10:
TABLES TABLE 1 TABLE 2 2A 2B 2C 2D
Page 11:
INTRODUCTION o In the Safford-San S
Page 14 and 15:
Land Status Figure 2 shows land own
Page 16 and 17:
asin are published in Andreasen and
Page 18 and 19:
114° 112° IIO O 108° 106° 104°
Page 20 and 21:
I.D ". ". '. ". ..... ",/" '. ~~~ ~
Page 22 and 23:
side of the mountains and coincide
Page 24 and 25:
stress fields may dilate some of th
Page 26 and 27:
I-' Ln !' .. "," "" ,,... P.c Tucso
Page 28 and 29:
The upper basaltic andesite, overly
Page 30 and 31:
over an inferred decollement in the
Page 32 and 33:
attitudes of the thrust faults, rev
Page 34 and 35:
gradation is observed only in certa
Page 36 and 37:
to depth of 555 meters (Knechtel, 1
Page 38 and 39:
asal conglomerate facies of the low
Page 40 and 41:
Indian Hot Springs-Gila Valley Intr
Page 42 and 43:
flow. A fault zone(s) is inferred t
Page 44 and 45:
DWG. NO.-R.-IJ.-~ CALCULATED THICKN
Page 46 and 47:
Geophysics, 1979). Nearby at Saffor
Page 48 and 49:
Buena Vista Area Introduction More
Page 50 and 51:
/ I / / / / / / / / / / I / / / / /
Page 52 and 53:
33 34 31 T6S T7S
Page 54 and 55:
GElEIEEOl'3,53IEEa3lljO Mile E] B R
Page 56 and 57: similar to the Precambrian granite
Page 58 and 59: 100 + + + + 300 + 500 ~ + + + + + +
Page 60 and 61: 500 m interval, while 1.2 HFU is re
Page 62 and 63: tN I \ 5 IOMiles \ ""1. EXPLANATION
Page 64 and 65: are interpreted as evidence of a ma
Page 66 and 67: LINE 7 RESISTIVITY N =2000 FEET, DI
Page 68 and 69: 100 200 0...---..."...-------------
Page 70 and 71: Artesia in D-8-26-32 and 33 have es
Page 72 and 73: trending 1.5 km 2 closures with soi
Page 74 and 75: waters occur in confined or artesia
Page 76 and 77: Equation (1) Alumino-silicate + H 2
Page 78 and 79: Silica concentration in Figure 24 i
Page 80 and 81: San Simon Introduction The San Simo
Page 82 and 83: Geology Subsurface geology controls
Page 84 and 85: " " '"",.- ~--- ,....~, ~. 7 '1.v-~
Page 86 and 87: o 1 Mile '2, WATER LEVEL OF WELLS I
Page 88 and 89: Conclusion Geothermal potential at
Page 90 and 91: geothermometry for waters containin
Page 92 and 93: GRAVITY MODEL OF THE BOWIE AREA Mod
Page 94 and 95: TRANSVERSE TOPOGRAPHIC PROALES ACRO
Page 96 and 97: probably correlative with the "blue
Page 98 and 99: excellent chemical quality suitable
Page 100 and 101: Table 1 Wells With Measured Tempera
Page 102 and 103: Table 1 cont. Wells With Measured T
Page 104 and 105: Table 1 cant. Wells With Measured T
Page 108 and 109: Table 2B. Analyses of Buena Vista a
Page 110 and 111: Table 2C. Analyses of Cactus Flat-A
Page 112 and 113: Tabl~ 2E. Analyses of Bowie area gr
Page 114 and 115: Table 3A Geothermometers for the Gi
Page 116 and 117: Table 3C. Geothermorneters for the
Page 118 and 119: Table 3E. Geothermometers for the B
Page 120 and 121: Table 4. Summary table showing aqui
Page 122 and 123: Summary of description of Core Lith
Page 124 and 125: D-7-27-2cdb Driller's log Surface s
Page 126 and 127: APPENDIX 2 pH Correction for the Si
Page 128 and 129: By converting milligrams per liter
Page 130 and 131: APPENDIX 3 Arizona Bureau of Mines
Page 132 and 133: BIBLIOGRAPHY Aiken~ C. L. V., 1978,
Page 134 and 135: -3- Davidson, E. S., and Cooley, M.
Page 136 and 137: -5- Fournier, R. O. and Truesdell,
Page 138 and 139: 7 Marjaniemi, ,D. K., 1968, Geologi
Page 140 and 141: -9- Scarborough, R. B., 1975, Chemi
Page 142: Van Horn, W. L., 1958, Late Cenozoi
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geothermal resource potential of the safford-san simon basin, arizona

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