Table 1 cant. Wells With Measured Temperatures >30 o C In The Safford-San Simon Basin Depth Temperature Location Temperature (oC) (Meters) Gradient (oC/km) Source D-13-30-14 DDD 32.2 284 50 5, 8, 9, 12, 13 D-13-30-15 DAA 35.0 397 43 5, 8, 12, 13 D-13-30-23 ACC 30.6 274 46 12, 13 D-13-30-23 B 33.3 274 56 4, 8 D-13-30-25 ACD 30.5 268 47 5, 12 D-13-30-27 AD 134.4 1952 60 4 D-13-30-30 B 40.6 284 80 8 D-13-30-30 BCB 40 293 75 5, 13 D-14-30-36 AA 75.6 2312 25 4 ('1") D-13-30-36 DDD 41. 7 610 39 3 m D-14-30-12 ADB 30.6 279 45 9, 12, 13 D-14-31-16 DCC 31.6 610 22 2, 9, 12, 13 D-14-31-21 BCC 32.2 217 65 9, 12, 13 D-16-31-10 AA 54.4 1657 22 1, 4 Sources (1) Conley, J.N., and Stacey, D.A., 1977 (10) Swanbere, C.A., and O<strong>the</strong>rs, 1977 (2) DeCook, K.J., 1952 (11) Harold Wardlaw, Pres. Carom. ( 3) Dut t, G. R. , and McCreary, T.W., 1970 (12) WATSTORE (4) Giardina, S, 1978 (13) White, N.D., 1965 (5) Hem, J. D. , 1950 (14) This Report (6) Knechtel, M.M., 1938 (15) Wilson, R.P., and White, N.D., 1976 (7) City <strong>of</strong> Safford (16) Witcher, 1979 (8) Schwennesen, 1918 (9) State Land Department
Table 2 Chemical analysis <strong>of</strong> ground waters in <strong>the</strong> Safford~SanSimon<strong>basin</strong> area Results in milligrams per liter except as noted (see data sources) Temperature in degrees celsius Remarks: S - spring W- well Data Sources: 1. Arizona Bureau <strong>of</strong> Geology and Mineral Technology 2. Dutt and McCreary, 1970 3. Hem, 1950 4. Muller and o<strong>the</strong>rs, 1973 5. Swanberg and o<strong>the</strong>rs, 1977 6. Files, U.S. Geological Survey Tucson, Arizona 7. White and Smith, 1965 Location Key: D-3-3l-3 ADCC Quadrant Township Range Section Quarter 94
- 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 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