- Page 1: GEOTHERMAL RESOURCE POTENTIAL OF TH
- Page 6 and 7: Table of Contents (cont'd.) PAGE Sa
- Page 8 and 9: FIGURES PAGE FIGURE 19 FIGURE 20 FI
- Page 10 and 11: APPENDICES APPENDIX 1 APPENDIX 2 AP
- Page 13 and 14: usinesses such as food processing,
- Page 15 and 16: Previous Work Many studies are avai
- Page 17 and 18: Regional Setting The Safford-San Si
- Page 19 and 20: + 1.86 HFU - .33 HFU. The variation
- Page 21 and 22: tinuities appear to correlate with
- Page 23 and 24: Regional Stratigraphy and Structure
- Page 25 and 26: the uplift is approached. Late Cret
- Page 27 and 28: ase of the "Laramide" andesites (Du
- Page 29 and 30: (3) a metamorphic carapace displayi
- Page 31 and 32: noted that other explanations are p
- Page 33 and 34: "Basin and Range disturbance" is ch
- Page 35 and 36: Harbour (1966) further proposes tha
- Page 37 and 38: evaporite facies and green clay/red
- Page 39 and 40: The upper unit sediments overlie th
- Page 41 and 42: R27E T5S. T5S. T6S. T6S T7S. T7S. T
- Page 43 and 44: Graham Mineral Bath well, discharge
- Page 45 and 46: +N SCAL.E I o 15 Kilometers E3 F3 F
- Page 47 and 48: aquifers in these areas may have br
- Page 49 and 50: ~~/ ,~~/ -1/0'0 35 j>" / / "-"h.~"
- Page 51 and 52: hydraulic connection exists between
- Page 53 and 54: of the Buena Vista geothermal syste
- Page 55 and 56:
the area less than one mile north o
- Page 57 and 58:
sional origin. Geothermal systems a
- Page 59 and 60:
COMPLETE BOUGUER GRAVITY ANOMALY MA
- Page 61 and 62:
Cactus Flat-Artesia Area Geology Fi
- Page 63 and 64:
silt. These deposits become more co
- Page 65 and 66:
;"~,./(~'/' ·~sI:, .' ;~"' ~.'i"l'
- Page 67 and 68:
subsurface temperatures and depths
- Page 69 and 70:
, i. ,- " - , 35 • M53 'i'/ho EXP
- Page 71 and 72:
Figure 22. Map showing distribution
- Page 73 and 74:
tl 0 0 (f) u 1.5 1.0 + + rtl U 0 0.
- Page 75 and 76:
may be erroneous. However, silica c
- Page 77 and 78:
-2.0 / 15· / / -2.5 -3.5 -4.0 ·27
- Page 79 and 80:
sodium bicarbonate waters into sodi
- Page 81 and 82:
1000 AVERAGE TEMPERATURE GRADIENT O
- Page 83 and 84:
.- ... - - ~ 0 , ~ ." 17 to ~, '. .
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may displace the last remnants of t
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',~ ---...-..--_.- .- Figure 29. Es
- Page 89 and 90:
Bowie Area Introduction At least 20
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MAP SHOWING DISTRIBUTION OF Na-K-Ca
- Page 93 and 94:
(X) N BOUGUER GRAVITY MAP OF BOWIE'
- Page 95 and 96:
1975, GROUND-WATER TABLE MAP OF THE
- Page 97 and 98:
sidence that was created by ground
- Page 99 and 100:
Whitlock Mountains Area In 1927 and
- Page 101 and 102:
Table 1 cont. Wells With Measured T
- Page 103 and 104:
Table 1 cont. Wells With Measured T
- Page 105 and 106:
Table 2 Chemical analysis of ground
- Page 107 and 108:
Table 2B. Analyses of Buena Vista a
- Page 109 and 110:
Table 2C Analyses of Cactus Flat-Ar
- Page 111 and 112:
Table 2D. Analyses of SaIl Simon ar
- Page 113 and 114:
Table 2F. Analyses of Whitlock Moun
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Table 3B. Geotherrnometers for the
- Page 117 and 118:
Table 3D. Geothermometers for the S
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Table 3F. Geotherrnorneters for the
- Page 121 and 122:
APPENDIX 1 Selected Drillers Logs 1
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Driller's log Brown sand and dirt B
- Page 125 and 126:
D-7-27-2dbb Driller's log Thickness
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APPENDIX 2 .pH· Correction for··
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o Therefore, the ionization constan
- Page 131 and 132:
Memorandum to·· Dt"ljI Ohapman co
- Page 133 and 134:
-2- Clay, D. W., 1960, Late Cenozoi
- Page 135 and 136:
-4- Eaton, G. P., and Timmons, C. E
- Page 137 and 138:
-6- Heindl, L. A., and McCullough,
- Page 139 and 140:
-8- Pashley, E. F., 1966, Structure
- Page 141 and 142:
-10- Strangway, D. W., Holmer, R. C