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

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Table 3E. Geothermometers for the Bowie area G E 0 THE RHO H E T ~ R VAL'JES NUHB E R SA t'PLE LOCATION TEI·PERATU'lE NA-K-CA CHALCEDONY OUARTIICONOUCTIVEI ALPHA-CRISTORALITE I CI I C 1 I CI I CI I CI 1 '10 DIU83~CCC 17.00 9~.~7 19.54 71.29 21.BO 2 '11 DllZ827CCC 25.00 51.91 19.53 71.28 21.79 1 'l? 01ll Rl7B!\q 21,.00 ~7. 7~ ~1. 31 72.93 21.42 ~ 93 DIU~10CCC J5.00 ------- 51.22 8l.~O 32.51 5 linno D1128109CC 37.00 101.15 ------- ------- ------- 6 2 1 ~ HO OlllP,I?OCC 15.00 124.17 b?04 95.42 45.10 7 .lZk~1l 0IllRl?AOO 14. 00 122.67 69.40 99.?0 49.1? 8 21HiW {)U~815RDC 15.00 124.19 70.58 100. "0 50.23 ~ 24kAO 01178'JBCCC 33.00 54.62 57.10 87.97 J7.91 10 2?HEO o 122326CCD 37.00 45.49 4B .16 79.50 29.71 11 2&"RO D122834BCB 31.00 82.42 41.7\> 73.~ 1 23.84 12 l7Wfi0 0122827ABB 14.'10 41.68 52.15 83.2~ 33.37 lJ lOW'tO D_H925COO 37.00 43.85 57.12 B3.2b B.H 14 29H'!'l o 13l925COO )~.IjO 97.28 52.70 83.81 33.87 15 ~lQtl OlJ2927ACC D.30 76.01 36.01 67.91 18.56 1" (] III 94DOB J7.20 ------- 50.8il 82.09 32.21 17 01llBncc 11.70 ------- 00.41 91.08 40.91 1,1 01379240CC 41.70 ------- ------- ------- ------ 19 ADa DllZd34ec 31.00 41.53 4R.54 79.67 30.00 20 A711 01U834RA 2'1.00 H.29 54.42 35.44 35.~5 21 Al37 0122 R34AA 36. ao 76.10 44.11 75.65 26.00 22 AI J:\ 01il~10Cq 36.00 47.79 ~0.72 72.41 22.88 2J AI14 ill77810CC )5.~0 66.66 46.77 78.17 2 8. ~4 l~ H3'J 01l29369R 30."0 90.06 61.41 92.02 ~1.85 r--- l~ Alk fJn3030B 21.00 58.22 81.36 110.00 60.0b 0 2b AZ 17 .--l DLB015 27.')0 78.04 20.46 52.89 4.25
Table 3F. Geotherrnorneters for the Whitlock Mountains area G E 0 THE RHO h f T E R ~ A L U E S .... Uh--2 (R SH;PLF LflCATION T3 35.6" 3 !J~Z;D6H.C 41. GO 4 330, 0IfJZ'HISB "1.10 5 Alb? DI')?~)6AO 41. 10 'J7.23 77 .65 107.17 56.6e 6 A71,) OIoznOAC 34.10 13Z.80 4".~b 76.3b l6.be 7 Al!>" DB2"Z2CAA )o.~o 67.51 64.58 '14.99 4".7't 8 Al ~}'J Dolo2lAB 32.1'0 11'1.78 76.60 IOb.lO 55.73 co o ,.--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 114 and 115: Table 3A Geothermometers for the Gi
Page 116 and 117: Table 3C. Geothermorneters for the
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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