Figure I Generalized map of the Wilbur Mining ... - University of Utah

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Ceothermal Resources • GEOCHEHISTRY OF ACTIVE GEOTHERMAL SYSTEMS IN THE NORTHERN BASIN AND RANGE PROVINCE ABSTOACT Numerous thermal springs occur in the northern Basin and Range Province due primarily to the structure and high regional heat flow. Dilute to slightly saline (200 to 3,000 mg/L TDS) Ca and/or Na-UCO, type waters, many associated with travertine, are dominant in eastern and northeastern Nevada. CO.-charged Na-HCO waters are particularly common along the eastern side of the Sierra Nevada from Long Valley north to Bridgeport. Moderately to very saline (3,000 to 35,000 mg/L TDS) Na-Cl type waters predominate near major topographic lows, Na-SO. type waters are common in western Nevada and in northeastern California. Na-mixed anion waters are common along the north side of the Black Rock Desert in northwestern Nevada and the Alvord Desert in southeastern Oregon, Measured temperatures in deep geothermal wells in the northern Basin and Range Province are about 14 C cooler than the average temperature calculated using two chemical and one isotope geothermometer on waters discharged by nearby thermal springs and shallow wells (
Page 1 and 2: Geol^ertnal Resources Council, TRAN
Page 3 and 4: silica concentration in a water sam
Page 5 and 6: Morgan, et at. holes over the anoma
Page 7 and 8: Morgan, et al. point the gradient b
Page 9 and 10: Olson, et al of a theoretically gen
Page 11 and 12: Olson, et al Isherwood, W. F., 1977
Page 13 and 14: Sun and Ershaghi history matching p
Page 15 and 16: Sun and Ershaghi eg S o "^ lii z >o
Page 17 and 18: « •'t Lund. et. al. In general,
Page 19 and 20: Lund. et. al. FIGURE 3 Production F
Page 21 and 22: W.:-- Lund, et. al. Since the heat
Page 23 and 24: Lund, et. al, and temperature in th
Page 25 and 26: Lund. et. al. of the well with cont
Page 27 and 28: Lund, et, al. special heat resistan
Page 29 and 30: Lund, et. al. Ste«) in {«) Tunne\
Page 31 and 32: Lund, et al. 3. 4. References TABLE
Page 33 and 34: •Edmis-tjon period of time buried
Page 35 and 36: Edmiston VININI FM (SILICEOUS ASSEM
Page 37 and 38: Table I. Chemical analyses and calc
Page 39 and 40: Satkln et al. GEOTHERMOMETRY The te
Page 41 and 42: Denlinger We modeled the gravity da
Page 43 and 44: TABLE 3. RESULTS OF MODELING RESERV
Page 45 and 46: Knirsch Table 1. Continued Location
Page 47: Knirsch Spring/Well Edgemont Burlin
Page 52: out. The dilute Na-UCO, waters deve
Page 55: Naae/Uictt Ion Tablf I. Clioalt-al
Page 58: '' I riRure 3. Distribution of Sa-H
Page 61: ''Fumaroles'* occur along the west
Page 64: Table 3. (^othermometer temperature
Page 67: Table 3. (feotherraometer teraperat
Page 70: thermal water discharging at Leach
Page 73: • Table 6. Isotopic data for ther
Page 76: 5 - 4- ^^- >> S2 ^ 3 • • ••
Page 79 and 80: ulfate—water isotope geothermomet
Page 81 and 82: Dansgaard, W., Johnson, S. J., Moll
Page 83 and 84: S. Geological Survey and Oregon Dep
Page 85 and 86: w- \''" • ' '' .,si"hgle borehole
Page 87 and 88: I CD 1.6 FIGURE 3b Surface resistiv
Page 89 and 90: *>. • . fc*iS£-*-i.A-"ASSe: HORt
Page 91 and 92: .• Halfman, S. E., Lippmann, M. J
Page 93 and 94: Trexler et al. PRELIMINARY SURVEY E
Page 95 and 96: Trexler et aL •^s^:^ Tortoise hig
Page 97 and 98: Trexler et al. Environmental Issue
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Trexler et al. ACKNOWLEDGEMENTS Man
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.Vlurray, et al. 38-30' Figure 1. H
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Murray, et al. EMfiU a uvllm •UMt
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Murray, et al. Fournier, R.O., and
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flurray and Jonas Figure 1. Map sho
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Murray and Jonas ComposfTe ProfTIo
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Murray and Jonas ACKNOWLEDGEMENTS T
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ilackwell, Kelley and Edmiston ther
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ilackwell, Kelley and Edriiiston ap
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Blackwell, Kelley and Edmiston assu
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temperatures of fluid inclusions ar
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ABSTRACT Caldera environments are y
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'Spu4 lf.i1* CCnplilioJt tit* TJrtl
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ohm-m. The logs- probably to not re
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CcoiheiJ-iaf RosouTces Council APPL
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General Discussion. There is no who
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Wright et al. Hoover, 0. 6., Long.
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730 BAiCALQWICZ AND OTHERS I one wa
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732 BAKALOWICZ AND OTHERS rise thro
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734 BAKALOWICZ AND OTHERS Rahn and
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736 BAKALOWICZ AND OTHERS .^mple De
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738 BAKALOWICZ AND OTHERS There wer
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GUTIERREZ-NEGRIN be enlarged to an
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Figure 6.- Map showing high Radon c
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GEOTHERMAL RESOURCES IN THE WILLIST
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Mesozoic rocks due to the high cond
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Resources This assessraent of geoth
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'•- '.*' i: ABSTRACT Ttie Desert
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Table 1. Concentrations in ppn of s
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Ceothermal Resources Council TRANSA
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water as indicated by relatively lo
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' Satnp I e 3 5 45 Z15 27i 272 272
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.3 I D a o
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ACKNOWLEDGMENTS The project descrip
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Session Description: Agenda: Paneli
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Special Session/Agenda (continued)
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DOE PROJECT OFFICES Three Departmen
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Industrial Process Sites 1 ORE-IDA
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District Heating Systems 1 Monroe C
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Project Title: Commercial Culture o
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Project Title: Boise City - A Field
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Project Title: Diamond Ring Ranch G
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City of El Centro Project Page 2 Sy
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Project Title: Field Experiments fo
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Project Title: Direct Utilization o
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Philip School Project Page 3 Status
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Sugar Beet Processing Project Page
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o 5/5ic jo-r 651 1891 92 33 J'.'-i
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o t Figure 2. HOLLY SUGAR PLANT Wit
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Project Title: Kelley Hot Springs A
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Kelley Hot Springs Agricultural Cen
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Klamath County YMCA Project Page 2
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Klamath Falls Project Page 2 Geothe
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Project Title: Madison County Geoth
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Project Title: Location: Principal
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Project Title: Water and Space Heat
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Project Title: Pagosa Springs Geoth
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Project Title: Multiple Use of Geot
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Moana KGRA Project Page 3 Status: I
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St. Mary's Hospital Project Page 2
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-LPS" •LP/f—O e-HW/i^ L_ 1 ^ ST
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Susanville Energy Project Page 2 Sy
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Susanville Energy Project Page 4 St
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a Project Title: Direct Utilization
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Project Title: Location: Floral Gre
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V Project Title: Location: Geotherm
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Group 10 Appendix 1 Industrial Proc
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® 16. 17. 18. 19. 20. 21. Appendix
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Appendix 1 (continued) industrial P
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( ^ Appendix 1 (continued) Industri
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FEDERAL ASSISTANCE PROGRAM PROJECT
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. c. d. Name Date Nature Darrel Sev
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Name Date Nature d. Jack McNamara 6
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2.3 Presentations and Tours. 2.3.1
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3.3 Carson City Elementary School t
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4.2 Schedule of Delivery Dates: 4.2
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Figure I Generalized map of the Wilbur Mining ... - University of Utah

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