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References

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Vulkanologiya i seysmologiya (Volcanology and Seismology), 1980

Zemnoj teplovoj potok v Kurilo-Kamchatskoj i Aleutskoj provincijah (Terrestrial heat flow in the Kuril-Kamchatka and Aleutian provinces )

Ya.B. Smirnov, V.M. Sugrobov
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Okeanologiya (Oceanology), 1980

Issledovanija Teplovogo Potoka VRiftovoj Zone Krasnogo Morja (Heat Flow Studies in the Red Sea Rift Zone )

Evgeny V. Verzhbitsky, V.G. Zolotarev
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SECOND SERIES BULLETIN OF THE VOLCANOLOGICAL SOCIETY OF JAPAN, 1980

A discussion on “Heat Flow Measurements in the Submarine Calderas, Southern Kyushu, Japan-Preliminary Report-” by EHARA et al. (1980)

Osamu Matsubayashi
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Advances in European Geothermal Research: Proceedings of the Second, 1980

A Critical Study of Heat Flow Data in France

Guy Vasseur
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Izvestiya Akademii Nauk SSSR, Fizika Zemli (News of the USSR Academy of Sciences, Physics of the Earth), 1980

Raspredeleniye teplovogo potoka i priroda yego lokal'nykh anomaliy v rayone ozera Baykal (Heat flow distribution and the nature of its local anomalies in the area of Lake Baikal )

V.A. Golubev, S.V. Osokina
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AAPG Bulletin-American Association of Petroleum Geologists, 1980

Arc-continent collision in Banda Sea region

C. Bowin, G.M. Purdy, C. Johnston
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Tectonophysics, 1980

Terrestrial heat flow in the Tertiary basin of Central Sumatra

Humberto Da Silva Carvalho, Siswoyo Purwoko, Mochamad Thamrin, Victor Vacquier

Heat flow at 170 locations in the Central Tertiary basin of Sumatra was determined from thermal gradients obtained from the extrapolated oil well bottom hole formation temperature and the assumed temperature of 80°F at the surface. The effective thermal conductivity of the whole rock column, by which the gradient is multiplied to get the heat flow was calculated from measurements on 273 specimens of the geologic section and inspection of 92 well logs. For the whole basin the gradient averaged 3.71 ± 1.04°F/ 100 ft (67.6°C/km) the conductivity 4.83 ± 0.31 mcal °C−1 cm−1 sec−1, giving an average heat flow …

US Geological Survey Bulletin, 1980

Heat flow from the western arm of the Black Rock Desert, Nevada

John H. Sass, Charles W. Mase
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1980

Heat-flow measurements in the state of Arkansas

Robert F. Roy, Bruce Taylor, Arthur J. Pyron, James C. Maxwell
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Volcanology and Seismology (вулканология и сейсмология), 1980

Zemnoy teplovoy potok v kurilo-kamchatskoy i aleutskoy provintsiyakh ii karta izmerennogo i fonovogo teplovogo po- toka - vulkanologiya i seismologiya (Terrestrial heat flow in the Kuril-Kamchatka and Aleutian provinces II map of measured and background heat flow )

Ya.B. Smirnov, V.M. Sugrobov
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1980

Izmerenie teplovogo potoka Zemli u poverhnosti:(Metod redukcii temperatur voln) (Measurement of the Earth's heat flux at the surface: (Temperature wave reduction method) )

Vadim V. Gordienko, Olga V. Zavgorodnyaya
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Seismotectonics and seismicity of the BAM construction area. (Сейсмотектоника и сейсмичность района строительства БАМ.), 1980

Geotermicheskie issledovanija v Bajkalo-Angarakanskom rajone trassy BAM (Geothermal studies in the Baikal-Angarakan area of the BAM route )

S.T. Lysak, L.M. Platonov, R.P. Dorofeeva, V.U. Levitsky
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1980

Heat flow and geothermal assessment of the Escalante Desert : part of the Oligocene to Miocene volcanic belt in southwestern Utah

Monica D. Clement
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Journal of Geophysical Research, 1980

Preliminary heat flow and radioactivity studies in Wyoming

Edward R. Decker, Keith R. Baker, Gerald J. Bucher, Henry P. Heasler
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Izvestiya Akademii Nauk SSSR, Fizika Zemli (News of the USSR Academy of Sciences, Physics of the Earth), 1980

Geotermicheskiye Ussloviya Afrikansko Sicilianskogo Podnatiya (Geothermal Conditions of the African Sicilian Rise )

V.G. Zolotarev, V.V. Sochelnikov
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Canadian Journal of Earth Sciences, 1980

Geothermal measurements in Newfoundland

J.A. Wright, Alan M. Jessop, Alan S. Judge, Trevor J. Lewis

We report heat flow values for ten holes at five sites in Newfoundland. The average observed heat flow is 43 ± 4 mW m−2. Corrected for Pleistocene surface temperature variations, the average becomes 50 ± 4 mW m−2, with a range from 38–82 mW m−2. The Dunnage zone (a vestige of the Iapetus Ocean) exhibits a heat flow lower than normal for Paleozoic orogenic belts. The highest heat flow is associated with the Carboniferous St. Lawrence granite intrusion. Heat production measurements were made at three of the sites. Those in the Dunnage zone are low (< 0.8 μW m−3), as …

Earth and Planetary Science Letters, 1980

A geothermal study of the Jharia Gondwana basin (India) Heat flow results from several holes and heat production of basement rocks

G.Venkateshwar Rao, R.U.M. Rao
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Тбилиси,«Сабчота сакартвело, 1980

Geotermicheskie Usloviya I Termalnye Vody Gruzii (Geothermal Conditions and Thermal Waters of Georgia )

I.M. Buachidze, G.I. Buachidze, N.A. Goderzishvili, B.S. Mkheidze, M.P. Shaorshadze
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1980

Analysis of thermal data from drill holes UE25a-3 and UE25a-1, Calico Hills and Yucca Mountain, Nevada Test Site

John H. Sass, Arthur H. Lachenbruch, Charles W. Mase
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1980

Heat generation and terrestrial heat flow in northwestern Pennsylvania

Garry Maurath
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