Heat flow map of the European part of the U.S.S.R. |
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Authors: | R. I. Kutas E. A. Lubimova Ya. B. Smirnov |
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Affiliation: | (1) Geophysical Institute, Acad. Sci. Ukrainian SSR, Kiev;(2) Institute of Physics of the Earth, USSR Acad. Sci., Moscow;(3) Geological Institute, USSR Acad. Sci., Moscow |
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Abstract: | A heat flow isoline map is presented. Low and relatively constant heat flow has been observed in the old shield areas of the East European Platform (25–40 mW/m2). Increased heat flow (>50 mW/m2) has been found in the Dniepr-Donetz depression. The area south of the East European Platform is characterized by highly variable heat flow (55–100 mW/m2). Some geophysical implications are discussed. |
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Keywords: | Heat flow map U.S.S.R. East European Platform Dniepr-Donetz depression Carpathians Crimea peninsula Heat generation |
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