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

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Table 3A Geothermometers for the Gila Valley-Indian Hot Springs area G E a THE ~ H n H E T E R V A L U E S NUN9fR S AI-lf'l 1. UV;,\ TION IE HP < RATIP E NA-1(-CA CHALCEDONY aUARTllCONOUCTIVEI ALPHA-CRISIOBALITE ( CI l CI l CI I C I I Cl 1 57 1)',2, 36C81"- 'tf.,.OO 99.09 76.',3 10&.23 55.75 2 5 3H ~') D52~1 Honr. 4b.no 82.'n 66.26 96.5& 4&.28 3 51,''; -:() O')2',17AOOD 45.~0 82.18 "9.42 99.52 49.) 7 4 55"'(1 ~72(, 171\DD9 47.no 7b.05 70.43 100.4& ')0.09 5 lei 7 051Q 7AD 47.PO b IHH 0>;2417AO 40.~0 7 1 i'l.? ll'iU+l7AG 47.flO "- Inll 052417AO 47. PO '! 2~) (}O D/,24 11 Art 58.'10 10 2~" I D7,?411Bfj 10.1)0 It AIt:l f)52417A 47.f)0 101.35 64.51 ')4.92 44.68 12 AlII ')52417A 41>.50 99.82 &4.51 '}4.93 44.68 13 All4 'O/,253bC 43.>;0 70.29 85.22 114.1& 63.58 14 AllI il>;?417AD B.OO 101.93 7"-.21 107.69 57.19 t', A71. ~'J 07/57CCC 29.50 79.16 41.20 74.78 25.16 16 All,!> 07241400 2'i. 5 0 70.90 4 L. 89 73.53 23.9b ('f) o r-l
Table 3B. Geotherrnometers for the Buena Vista area G EaT HER ~ n H E T E R v A l U E S NUHIl"R SAI"tPlf U)C~TlllN Tri'1pr.~f\TlJ?E NA-K-CA CHAlCEOONY ~UARTl(CllNOUCTIVEI ALPHA-CRISTOAALIIE ( C 1 ( CI ( CI ( C 1 ( CI I ~p. DU7IIAAH 49.no 152.61 82.51 111.67 61.12 2 ~Q 0717nco ]~.OO ·8R .19 81.118 111.08 60.?4 3 74 Dh772':>00DO ·27.00 BO.43 73.60 103.41 52. 'I'i 4 17 WI\D ll7?7ZAAOC 3h.()O 66.18 40.97 72 .66 23.12 5 1 ?,'-iriC n7Z711~1l~~ '.. *).00 96.P2 48.52 79.84 3C.04 b l'h,;'1() D7272A:JeB ltD.DO 82.81 43.12 74.71 25.0·. 7 30W'\0 !)7Z7ZADDCA J9.00 127.36 AI.11l nO.43 59.90 8 811) 7 D7277 4 ~J. 1 0 67.56 7'1.32 108.71 58.20 .~ QZ7 07272CC 35.hO ------- ------- ------- ------- 10 ·fJ I ~ 1)7?7I1RBB 41. ~O 90.11 H2.4b 111.&2 bl.!)? 11 All (l lJ 7.7 7Z ACA 37. '0 94.52 83.B3 112.88 02.11 -.::1 o r-l
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 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 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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