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

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Table 1 cont. Wells With Measured Temperatures >30 o C In The Safford-San Simon Basin Location Temperature (oC) Depth Temperature (Meters) Gradient (oC/km) Source D-8-25-12 DA 31.4 161 83 6, 9 D-8-25-12 DBD 30 213 56 7 D-8-26-7 ABA 42.0 467 51 7 D-8-26-7 AB 30.0 253 47 6 D-8-26-7 ACC 30.0 274 44 7 D-8-26-7 AC 35.0 329 52 6 D-8-26-7 AC 30.0 213 56 6 D-8-26-7 ADD 34 305 52 7 D-8-26-7 AD 30 0 6 274 46 6 D-8-26-7 ADC 32.0 243 58 9, 10, 14 .-l D-8-26-7 BAA 41.5 463 51 9, 10 D-8-26-7 BA 35.6 344 51 6 D-8-26-7 BBB 34 262 61 6, 10 D-8-26-7 BB 35.8 320 56 6 D-8-26-7 BDB 32.0 335 42 7 D-8-26-7 BDB 38.0 476 55 7 D-8-26-7 BDB 34.4 464 35 9 D-8-26-7 BDB 32.0 415 34 7 D-8-26-7 BD 33.3 396 39 6 D-8-26-7 BD 35 366 46 6 D-8-26-7 BD 33.9 299 53 6 D-8-26-7 CA 37 0 0 244 78 6, 10 D-8-26-7 CD 33.9 290 55 6 '"
Table 1 cont. Wells With Measured Temperatures >30 o C In The Safford-San Simon Basin Depth Temperature Location Temperature ( C) (Meters) Gradient (oC/km) Source ° D-12-28-10 CCC 35.5 305 58 10, 14, 15 D-12-28-22 CDC 31. 5 200 68 2, 4, 12 D-12-28-23 CCC 32.2 305 47 9 D-13-28-1 BB 30.0 218 55 12 D-13-28-3 C 37.2 244 79 2, 4 D-13-28-4 DDB 37.2 253 76 12, 13 D-13-28-9 BCC 31.0 213 61 12, 13 D-13-28-10 BC 36.0 305 59 9, 10 D-13-28-15 CCC 31.7 139 99 9 N Cl'\ D-13-29-6 CCC 31.1 255 51 12 D-13-29-6 CC 31.1 214 61 4 D-13-29-24 CD 40.6 293 77 5 D-13-29-24 DCC 40.6 293 77 2, 8, 12, 13 D-'13-29-27 ACC 33.3 311 49 3 D-13-29-36 AD 43.3 305 83 11 D-13-29-36 ACC 35.6 305 58 11 D-13-29-36 ADC 36.7 229 82 11 D-13-30-3 B 42.8 262 95 8 D-13-30-3 BeC 33.5 262 59 12 D-13-30-3 BDe 33.3 262 58 13 D-13-30-9 ACD 34.0 274 58 5, 8, 9, 12 D-13-30-11 BCC 32.2 290 49 5, 8, 12, 13 D-13-30-13 A 31.1 232 56 8
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
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Land Status Figure 2 shows land own
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asin are published in Andreasen and
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114° 112° IIO O 108° 106° 104°
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I.D ". ". '. ". ..... ",/" '. ~~~ ~
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side of the mountains and coincide
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stress fields may dilate some of th
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I-' Ln !' .. "," "" ,,... P.c Tucso
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The upper basaltic andesite, overly
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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
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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
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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 104 and 105: Table 1 cant. Wells With Measured T
Page 106 and 107: Table 2A. Analyses of Gila Valley-I
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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