Heat flow map of the European part of the U.S.S.R.
Tóm tắt
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.
Tài liệu tham khảo
Kutas, R. I., Gordiyenko, V. V., Bevzyuk, M. I. andZavgorodnaya, O. V. (1975).Noviye opredelenya teplovogo potoka v Karpatskom regione, Geofiz. Sbornik, Kiev 63, 68–71.
Kutas, R. I., Lubimova, E. A. andSmirnov, Ya. B. Heat flow map of the European part of the U.S.S.R. and its geological and geophysical interpretation, inGeoelectric and geothermal studies (East-Central Europe, Soviet Asia) (ed. A. Ádám), KAPG Geophysical Monograph, 443–449 (Akadémiai Kiadó, Budapest, 1976).
Lubimova, E. A., Polyak, B. G., Smirnov, Ya. B., Kutas, R. I., Firsov, F. V., Sergienko, S. I. andLyusova, L. N. Katalog dannykh po teplovomu potoku na territorii S.S.S.R. Mat. Mir. Centra Dannykh — B, No. 3 (Moskva, 1973), 64 pp.
Subbotin, S. I. andKutas, R. I. Glubinniy teplovoy potok evropeyskoy chasti S.S.S.R. (Naukova Dumka, Kiev, 1974).