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

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Summary of description of Core Lithology by E.S. Davidson, U.S. Geological Survey, Tucson Test Hole 0-6-27-35cbb Thickness (feet) Depth (feet) No Record Conglomerate, "Dipping 30 0 from vertical," Red Granite Clasts "Tertiary" volcanic rock and volcanoclastic rock "Laramide" andesite, epidotised, mineralized with copper 560 129 3 308 560 689 692 1000 Driller's log Gravel Gravel and Caliche in alternating 3 foot layers 0-6-27-35dda Thickness 15 235 Depth 15 250 Driller's log Gravel Gravel and Caliche in alternating 3 feet beds 0-6-27-36ccc Thickness 15 235 Depth 15 250 Driller I slog Gravel Gravel and Caliche in alternating layers 3 feet apart 0-7-27-lbba Thickness 15 235 Depth 15 250 Driller's log 0-7-27-2aaa Thickness Depth Boulders Clay Sand-water Clay Clay Sandy clay Clay Sandy clay Clay Gravel Clay Gravel and warm water Clay Gravel and water raised to 18 feet of top Clay Gravel Clay Boulders and gravel Gravel Clay Gravel Clay Gravel and clay 18 27 7 13 7 13 12 8 12 8 20 12 8 12 23 6 6 20 11 4 101 9 43 18 45 52 65 72 85 97 105 117 125 145 157 165 177 200 206 212 232 243 247 348 357 400 111
Driller's log Brown sand and dirt Boulders Yellow clay Gravel Clay Gravel, conglomerate Yellow clay Conglomerate, last 10 feet hard D-7-27-2aab 2 Thickness 16 8 101 55 10 40 20 150 Depth 16 24 125 180 190 330 350 500 Driller's log D-7-27-2aca Thickness Depth Top soil 10' Boulders 15 OQ U Gravel 8 Clay 26 Fine sand 6 Clay 20 Fine sand 5 OQ 8 Fine sand 6 Clay and sand 37 Clay and gravel 8 Clay 20 Sand 6 Clay 4 Gravel 7 Sandy clay 5 OQ 6 Sand 6 Sand and gravel, water flowed 12 Clay and gravel 66 Sand 9 Gravel 11 Clay 4 Sand and gravel 8 OQ 6 Gravel and clay 7 Clay 15 Course sand 4 Boulders 12 Boulders and clay 21 Clay 3 Boulders 7 10 25 44 52 78 84 104 109 117 123 160 168 188 194 198 205 210 216 222 234 300 309 320 324 332 338 345 350 354 366 387 392 525 Driller's log Top soil Gravel Clay Sand clay and water Clay Gravel Clay Sand and gravel Clay Gravel Clay Gravel Clay Sand and gravel Clay Gravel and sand Clay Gravel Clay Sand and gravel Clay Sand anc.. gravel Clay Gravel and boulders D-i-27-2acd Thickness 8 7 10 13 7 7 25 11 7 15 3 7 9 11 6 20 13 16 17 10 12 13 10 38 Depth 8 15 25 38 45 52 77 88 95 110 118 125 134 145 151 171 184 200 217 227 239 252 262 400 112
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
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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
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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
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similar to the Precambrian granite
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100 + + + + 300 + 500 ~ + + + + + +
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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 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 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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