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Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians

Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians

Within the limits of the Ukrainian sector of the East Carpathians and adjacent edge of the East European platform thermal flows vary from 35 to 130 mVt/m2. It has been shown on the base of geological-geophysical analysis and mathematical modeling of the heat flow that the principal regularities in d...

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Main Author: Kutas, R.I.
Format: Article
Language:rus
Published: Subbotin Institute of Geophysics of the NAS of Ukraine 2014
Subjects:
Carpathians
temperature
thermal flow
geothermic model
the earth’s crust
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/111016
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spelling journalsuranua-geofizicheskiy-article-1110162020-10-07T11:45:12Z Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians Kutas, R.I. Carpathians temperature thermal flow geothermic model the earth’s crust Within the limits of the Ukrainian sector of the East Carpathians and adjacent edge of the East European platform thermal flows vary from 35 to 130 mVt/m2. It has been shown on the base of geological-geophysical analysis and mathematical modeling of the heat flow that the principal regularities in distribution of thermal flow are controlled by regional tectonic zoning, which was formed by the process of geological development of the region. Low values of heat flow correspond to the structures with earth’s crust produced in Precambrian and Early Paleozoic (the slope of Precambrian platform and considerable parts of Pre-Carpathian flexure and external flysh Carpathians). Variations of thermal flow within the Folded Carpathians are possibly stipulated by lateral changes of heat generation or heat conductivity within sedimentary layer. High thermal flows in the Pannonian basin are associated with special features of tectonic evolution of lithosphere and earth’s crust during the Alpine stage and with magmatic activity. The increase of thermal flow is conditioned by stretching of the earth’s crust and lifting of asthenosphere. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111016 10.24028/gzh.0203-3100.v36i6.2014.111016 Geofizicheskiy Zhurnal; Vol. 36 No. 6 (2014); 3-27 Геофизический журнал; Том 36 № 6 (2014); 3-27 Геофізичний журнал; Том 36 № 6 (2014); 3-27 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/111016/105943 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
topic Carpathians
temperature
thermal flow
geothermic model
the earth’s crust
spellingShingle Carpathians
temperature
thermal flow
geothermic model
the earth’s crust
Kutas, R.I.
Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians
topic_facet Carpathians
temperature
thermal flow
geothermic model
the earth’s crust
format Article
author Kutas, R.I.
author_facet Kutas, R.I.
author_sort Kutas, R.I.
title Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians
title_short Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians
title_full Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians
title_fullStr Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians
title_full_unstemmed Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians
title_sort thermal flow and geothermic models of the earth’s crust of the ukrainian carpathians
description Within the limits of the Ukrainian sector of the East Carpathians and adjacent edge of the East European platform thermal flows vary from 35 to 130 mVt/m2. It has been shown on the base of geological-geophysical analysis and mathematical modeling of the heat flow that the principal regularities in distribution of thermal flow are controlled by regional tectonic zoning, which was formed by the process of geological development of the region. Low values of heat flow correspond to the structures with earth’s crust produced in Precambrian and Early Paleozoic (the slope of Precambrian platform and considerable parts of Pre-Carpathian flexure and external flysh Carpathians). Variations of thermal flow within the Folded Carpathians are possibly stipulated by lateral changes of heat generation or heat conductivity within sedimentary layer. High thermal flows in the Pannonian basin are associated with special features of tectonic evolution of lithosphere and earth’s crust during the Alpine stage and with magmatic activity. The increase of thermal flow is conditioned by stretching of the earth’s crust and lifting of asthenosphere.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2014
url https://journals.uran.ua/geofizicheskiy/article/view/111016
work_keys_str_mv AT kutasri thermalflowandgeothermicmodelsoftheearthscrustoftheukrainiancarpathians
first_indexed 2024-04-21T19:39:55Z
last_indexed 2024-04-21T19:39:55Z
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