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Literature Review

The Global Heat Flow Database (GHFDB) is committed to maintaining the highest standards of data quality. To achieve this, we have implemented a rigorous literature review process that ensures all datasets are thoroughly vetted before being made publicly available. To learn more about the review process and how you can contribute, please click the button below.

Izv. Academy of Sciences of the USSR. Physics of the Earth, 1983

Informativnost' geotermii pri izuchenii zemnoj kory Ural'skoj evgeosinklinali (Informative value of geothermy in the study of the earth's crust of the Ural eugeosyncline )

Yu P. Bulashevich
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Tectonophysics, 1983

Heat flow in Indian Gondwana basins and heat production in basement rocks

G.Venkateshwar Rao, R.U.M. Rao
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Comptes Rendus Geoscience, 1983

Premières déterminations du flux de chaleur et de la production de chaleur en Corse

Alain Lesquer, Maurice Pagel, Jean-Baptiste Orsini, Bernard Bonin
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Zentralblatt für Geologie und Palaontologie, 1983

Assessment of geothermal resources of Brazil — 1981

Valiya M. Hamza, S.M. Eston
No preview available

1983

Thermal ground water flow systems in the thrust zone in southeastern Idaho

D.R. Ralston, John L. Arrigo, Joseph V. Baglio, Leonard M. Coleman, Joel M. Hubbell, Karl Souder, Alan L. Mayo
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Geophysical Prospecting, 1983

Regional Geothermal Exploration in Egypt

Paul Morgan, Fouad K. Boulos, Chandler A. Swanberg

Abstract Although Egypt is not characterized by abundant Cenozoic igneous activity, its location in the northeastern corner of the African plate suggests that it may possess geothermal resources, especially along its eastern margin. Regional geothermal exploration has been carried out in Egypt using the thermal gradient/heat flow technique and groundwater temperature/chemistry technique. In the thermal gradient/heat flow study, existing oil-well bottom-hole temperature data as well as subsurface temperature measurements in existing boreholes were utilized before special thermal gradient holes were drilled. Groundwater temperature and chemistry data were used to extend the geographic range of the direct subsurface thermal measurements. On …


1983

Geothermal low-temperature reservoir assessment in Dona Ana County, New Mexico. Final report

L Icerman, RL Lohse
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Journal of Geophysical Research, 1983

Heat flow on the western flank of the East Pacific Rise at 21°N

Keir Becker, Richard P. Von Herzen
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Geothermy application in regional and prospecting and exploration studies, 1983

Metodika i rezul'taty opredeleniya teplovogo potoka v zone sochleneniya dokembrijskoj Vostochno-Evropejskoj i paleozojskoj Zapadno-Sibirskoj platform (The methods and results of a heat flow determination in the junction zone of the Precambrian East European and Paleozoic West Siberian Platforms )

V.E. Salnikov, S.I. Sergienko, Ya.B. Smirnov
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Initial Reports of the Deep Sea Drilling Project, 1983

Initial Reports of the Deep Sea Drilling Project

David K. Watkins, Margaret M. Testarmata, Isabella Premoli Silva, Kenneth A. Pisciotto, J.W. Patton, Hajimu Kinoshita, Roberet B. Halley, Pierre Cotillon, Jay L. Bowdler, Peter Rothe, Alastair H.F. Robertson, James Ogg, Michel Moullade, Keith A. Kvenvolden, J. Kostecki, Everly Keenan, Hideo Kagami, Peter D. Jenden, Daniel Habib, D.M. Bliefnick, Leo A. Barnard, Thomas H. Shipley, Robert E. Sheridan, Felix M. Gradstein
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Journal of Geophysical Research, 1983

Heat transfer through the sediments of the Mounds Hydrothermal Area, Galapagos Spreading Center at 86°W

Keir Becker, Richard P. Herzen
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Bulletin of NAS RA. Earth Sciences, 1983

Geotermicheskie Usloviya Uchastka Shakhty Arpa-Sevan (Geothermal conditions of the Arpa-Sevan mine site )

R.T. Miridzhanyan
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Journal of Geophysical Research, 1983

On the terrestrial heat flow and physical limnology of Crater Lake, Oregon

David L. Williams, Richard P. Von Herzen

The heat flow into 7000-year-old Crater Lake caldera is dominated by hydrothermal processes. The average of the conducted heat flow value is 138±121 mW/m2 (3.3±2.9 HFU). The total heat flow is estimated to be between 669 and 1381 mW/m2 (16 and 33 HFU). Hydrothermal fluids penetrate into the lake floor to a depth of at least 1.5 to 2.0 km and possibly much deeper. Two thermal spring areas were discovered on the deep lake floor. These springs, and probably other as yet undiscovered ones, have a dramatic effect on the water temperature, circulation, and stratification of the lake. Dense thermal …


Antarctic Geoscience, 1983

Geothermal studies in the Ross Island-Dry Valley region

Edward R. Decker, Gerald J. Bucher
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1983

Karten der Temperatur-Tiefenverteilung für das Territorium der DDR als Grundlage für die Höffigkeitseinschätzung "Geothermische Energie"

Siegmar Gläser
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Metodicheskie i Eksperimentalnye Osnovy Geotermii (Методические и экспериментальные основы геотермии / Methodical and Experimental Basics of Geothermy), 1983

Uzhno-Kitayskoe (South-China Sea)

V. M. Sugrobov, A.P. Gorshkov, V.N. Merkushov, L.V. Smirnov
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Okeanologiya (Oceanology), 1983

Geotermicheskii Potok V Zapadnoi Chasti Chernogo Morya (Geothermal Stream in the Western and Parts of the Black Sea )

A.V. Kondyurin, V.V. Sochelnikov
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Geothermy application in regional and prospecting and exploration studies, 1983

Metodika opredeleniya teplovyh potokov i teploprovodnosti gornyh porod v skvazhinah na osnove teplometricheskih datchikov (teplomerov) (The method for determination of heat flows and rock’s thermal conductivity in boreholes based on heat-measuring sensors (heat meters) )

R.I. Kutas, M.I. Bevzyuk, S.F. Mikhailyuk
No preview available

1983

Geothermal exploration in Trans-Pecos, Texas/New Mexico. Final report

Robert F. Roy, Bruce Taylor, Michael P. Miklas Jr
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1983

Dati di flusso di calore nei mari italiani

Bruno Della Vedova, Giulio Pellis
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