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

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Table 1 Wells With Measured Temperatures >30 o C In The Safford-San Simon Basin Depth Temperature Location Temperature (oC) (Meters) Gradient (oCjkm) Source D-5-24-16 CB 4803 183 166 1,4 D-5-24-17 AD 48 03 183 166 4, 12 D-6-24-4 CBB 47.8 18 1655 4, 12 D-6-24-13 AB 58.9 1148 36 4, 5, 6 D-6-25-36 CBB 46.0 660 42 4, 9, 10, 12 D-7-24-17 BD 30 0 6 11 1145 4 D-7-25-22 DDD 43.3 416 61 7 D-7-27-1 BBA 37.8 76 260 9 D-7-27-2 AAA 37.2 122 157 9 D-7-27-2 ACD 38 0 0 122 164 8, 10 0'1 D-7-27-2 ADD 41.0 122 188 9, 12 co D-7-27-2 CC 35.6 91 193 5, 9 D-7-27-11 BBB 43.5 122 209 10 D-7-27-11 BBB 49.0 133 233 14 D-8-25-1 DDD 36.0 213 85 5, 6 D-8-25-12 AA 30.6 305 41 6 D-8-25-12 AA 36 07 320 58 4, 5 D-8-25-12 AAA 39.0 366 57 9, 10, 14 D-8-25-12 ABA 30.0 180 67 7 D-8-25-12 AC 34.4 320 51 4 D-8-25-12 AD 32.2 244 58 6 D-8-25-12 AD 32.2 274 52 6 D-8-25-12 AD 34.4 122 134 5,9
Table 1 cont. Wells With Measured Temperatures >30 o C In The Safford-San Simon Basin Depth Temperature Location Temperature (oC) (Meters) Gradient (oC/km) Source D-8-26-7 DA 41.5 488 48 9, 10 D-8-26-7 DDA 39.0 421 50 9, 14 D-8-26-7 DDB 35 0 0 381 45 9, 14 D-8-26-7 DDB 38.0 387 52 9, 14 D-8-26-8 BDC 39 0 4 195 110 10, 16 D-8-26-18 AC 33.9 274 58 6 D-8-26-18 DDA 42.0 463 52 9, 10 D-8-26-20 AB 30.6 213 59 6 D-8-26-20 DBC 45 0 0 390 69 10, 6 D-8-26-28 ABC 31 244 53 7 D-8-26-32 CB 32 0 2 110 129 6 D-8-26-32 DB 32 0 2 122 116 6 D-8-26-32 DC 32.8 122 121 6 D-8-26-33 AC 32.8 226 65 6 D-8-26-33 CA 32.8 122 121 6 D-8-26-33 CA 33.3 152 100 6 D-8-26-33 CCC 31.0 132 99 9, 14 D-8-26-6 CCB 31.0 227 57 9 D-9-30-11 DD 72.2 98 553 4 D-10-28-25 DD 36 0 0 474 38 4, 6, 12 D-10-28-36 AAC 41.1 587 39 1, 4, 5, 6, 10, 12, 13 D-10-29-20 AC 34.1 160 101 10, 15 ........ D-11-29-36 CBB 32.2 207 69 2, 10, 13 0 0"\
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
Page 16 and 17:
asin are published in Andreasen and
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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 102 and 103: Table 1 cont. Wells With Measured T
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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