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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.

1968

Oceanic vertical temperature measurements across the water-sediment interface at selected stations west of Oregon

Roderick S. Mesecar
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Journal of Geophysical Research, 1968

Heat flow and water temperature fluctuations in the Denmark Strait

Arthur H. Lachenbruch, B.Vaughn Marshall
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Dopovidni An USSR, 1968

Teplovoe pole radyanskikh karpat i su- sidnikh teritorii - dopovidni an ursr (Thermal field of the Radianski Carpathians and Sids territories - dopovidny an ursr )

Vadim V. Gordienko, R.I. Kutas
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Earth and Planetary Science Letters, 1968

Experimental determination of the coefficient of heat transfer during hole boring and the re-establishment of the temperature field equilibrium

Vladimir Cermak, Milan Kresl, Ivan Veselý
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1968

The measurement of terrestrial heat flow at Budapest and Recsk: Unpublished paper

P. Salat
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National Geophysical Research Institute Bulletin India, 1968

Heat flow and crustal structure near Cambay, Gujarat, India

R.K. Verma, Mohan L. Gupta, Valiya M. Hamza, G.Venkateshwar Rao, R.U.M. Rao
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1968

Annual Report

R. K. Verma, M. L. Gupta, G.Venkateshwar Rao, Valiya M. Hamza, B. Panda, U.V. Rao
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Journal of Geophysical Research, 1968

Heat flow in the United States

Robert F. Roy, Edward R. Decker, David D. Blackwell, Francis S. Birch

New measurements of heat flow are reported for one hundred thirty-eight sites in the United States. The tabulation includes mean gradients, mean resistivities, and uncorrected and topographically corrected heat flow. Methods and calibrations are briefly described. In several areas, station density is adequte for preliminary contouring and for correlation with basement geology and radioactivity.


Novye Dannye Po Neftyanoi Geologii, Gidrogeolo-Gii, Geotermii I Geofizike Tsentralnogo I Vostochnogo Kavkaza (New data on oil geology, hydrogeology, geothermia and geophysics of the Central and Eastern Caucasus), 1968

O Velichine Poverh-Nostnoj Plotnosti Teplovogo Potoka Po Skv (About the value of the surface density of the heat flux along the borehole )

G.M. Sukharev, S.P. Vlasova, Yu.K. Taranukha
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The Crust and Upper Mantle of the Pacific Area, 1968

Terrestrial Heat Flow in India

R. K. Verma, Hari Narain

Summary A program of terrestrial heat flow measurements in different parts of India was begun in 1963. As a first step, calibrated thermistor thermometers are being used to measure geothermal gradients up to the maximum depths available in mines, oil wells, and bore holes. Tentative values of heat flow have been obtained in four areas of the Precambrian shield and in the Gondwana coal deposits of Godavari valley. Geothermal gradients have been measured in the Tertiary basins of Assam and of Gujarat. In the Kolar gold fields in Mysore state and in the Agnigundala copper belt of Andhra Pradesh, heat …


The crust and upper mantle of the Pacific area, 1968

Statistical Analysis of terrestrial Heat Flow and Seismicity of the Pacific Ocean

R. W. Girdler

The history and evolution of the Red Sea are considered in the light of the continental movement of Africa and Arabia. The relevant palaeomagnetic data pertaining to the latter are summarized. The Red Sea developed in phases, and it is likely that these correspond in time to phases of continental drift. The geophysical data for the Red Sea are summarized in a general résumé and in more detail by considering the Red Sea in three parts, viz. the northern Red Sea (north of 25°N), the central Red Sea (17° to 25°N) and southern Red Sea (south of 17°N). Structural differences …


Pure and Applied Geophysics, 1968

Heat flow in the upper Silesian coal basin

Vladimir Cermak

The paper presents results of heat flow measurements made in 6 deep bores in the Czechoslovakian part of the Upper Silesian coal basin. The heat flow measured was in the range from 1.74 to 1.87 μcal/cm2s. The undisturbed period before the temperature measurement in the bore is discussed and results of repeated temperature measurements carried out 0.1, 1,5 and 36 days after cessation of drilling in one of the bores NP-522, are also given. Although the temperature in the bore still differs considerably from equilibrium, it is possible to determine the temperature gradient with an accuracy better than 5% as …


Oceanography Magazine Tokyo, 1968

Terrestrial heat flow in the Okhotsk Sea, 2

Masashi Yasui, Koichi Nagasaka, Toshio Kishii, A.John Halunen Jr
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1968

Heat flow near major strike-slip faults in central and southern California

Thomas L. Henyey
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Yearbook Carnegie Institution for Science, 1968

Heat Flow

Stanley R. Hart, John S. Steinhart, T.J. Smith
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Journal of Geophysical Research, 1968

Terrestrial heat flow in the Alpine-Carpathian foredeep in South Moravia

Vladimir Cermak

The heat flow was determined in four deep boreholes drilled while making the basic geological investigations of the basement of the Carpathian foredeep and Flysch zone in South Moravia. The coordinates and the depth of the boreholes together with the value of the heat flow determined are given in Table 1. For this purpose the results of temperature measurements provided by the Czechoslovak Oil Mines, Hodonin, were elaborated; the course of the temperature gradient in the boreholes and the average temperature gradient for the individual lithostratigraphic units were determined (Figure 1). The measuring element used was a temperature-dependent resistor (a …


International Geological Congress. Report of the 23. Session Czechoslovakia 1968, 1968

Terrestrial heat flow in Czechoslovakia and its relation to some geological features

Vladimir Cermak
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Zeitschrift für Angewandte Geologie, 1968

Der Wärmefluß zwischen Harz und Prignitz

D. Becher, W. Meincke
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Bollettino di geofisica teorica ed applicata, 1967

Geotermal'nye issledovanija v juzhnyh i jugo-zapadnyh regionah Ukrainskoj SSR (Krym i Sovetskie Vostochnye Karpaty) (Geothermal InvestigationsIn The Southern And Southwestern Areas Of The Ukrainian Ssr (TheCrimea And Soviet Eastern Carpathians) )

T.S. Lebedev, R.I. Kutas, Vadim V. Gordienko
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Journal of Geophysical Research, 1967

Heat flow, Hawaiian area

John G. Sclater, Charles E. Corry

Fifty-three measurements of the outward flow of heat through the ocean floor have been made around the Hawaiian Islands. The heat flow values ranged from a low of 0.71 to a high of 1.9 ?cal/cm2/sec. The mean value for all the measurements (this includes ten previous measurements) north and east of the islands of Oahu, Maui, and Hawaii is 1.38 ?cal/cm²/sec. A statistical analysis on these values indicates that the mean outward flow of heat through the area southeast of Hawaii, 1.60 ?cal/cm²/sec, is significantly greater than the mean flow, 1.30 ?cal/cm²/sec, through the Hawaiian arch. The similarity of all …