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

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GRAVITY MODEL OF THE BOWIE AREA Modified from Eaton, 1972. Location of Gravity Profile Shown in Figure 32 o A A' LITHOLOGY DENSITY c:=J f=2.259/cm 3 ~ 500 ~ Q) ~ 1000 .s= a. ~ 1500- 2000 -15LI-__- West OBSERVED GRAVITY~ MODEL ~GRAVITY East ++++++++++\\ + + + + + + + + + +.v + + + + + + + + + +\ ++++++++++\ ++++++++++ +++++++++++ +++++++++++++ ~~~++++++++++++++ +++++++++++++ I +++ ++++++++++++++ +++++++++++++++++++ ++ +++++++++++++++++++ ++++++++++++++++++++++ + + VERTICAL EXAGGERATION 5.28 + + + LATE TERIARY- QUATE RNARY BASIN FILL SEDI MENT [=2.70 9/cm3 PRE-TERTIARY BASEMENT FAULT ARROW ON DOWN DROPPED SIDE o o ! 5 Mil•• I 5 Kilom.t... , Figure 31. A gravity subsurface model of the Bowie area. 81
(X) N BOUGUER GRAVITY MAP OF BOWIE' AREA WITH WATER FALLS AND PROFILE USED TO MODEL 'I I ,/:~----7~\-~;iR ... ~«-- .I _t\/\>~ . / ):fte1lC1-~ • r~~I l~,~':J , -,,,. fi~~?\:- -~-J , 1\ C' . -:?'~4 ./1 .; ';' '.ii.,~'b \" { - ' j 1,\ \1 ,I "'/,\ \ -"r I, ' ",,' J ,~..~. II _ .. " ~.l'~ , .~. t--"-'--t-' 1 \ I~I W~-ldl'ljI: \ I t~v> Center LOCATIONS OF GROUND SUBSURFACE STRUCTURE GA of Bouguer Gravity Anomaly East of BOWIe Bouguer Gravity contour Contour interval is 5 mi lIigals 1975, Ground-water fall (See Figure 34, Ground-water Table Map of the.Bowie area,) A AI Gravity profile used to model subsurface geology, (See Figure 31 Gravity DATA Model of Bowie Area.) SOURCES: (I) 'GRAVITY-Wynn and Dansereau, 1979. (2) PROFI LE - Eaton t 1972. (3}GROUND-WATER TABLE -Information for 1975 j Wilson and White, 1976. BASE: N --160- -r- US, Geological Survey 1:25Q!000, Silver City, 1970, SCALE: 1:250,000 0 6 Miles I I I « , I I Figure 32. Bouguer gravity map of Bowie area compared to' locations of ground-water falls.
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 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 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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