Thermomechanical model of the development of the West-Black Sea basin

On the base of variation finite element method it was carried out computer modeling of the slow sub horizontal movements of the West-Black Sea Basin (WBSB), and also evolution of its heat fields during a period of time from the moment of access to its lower boundaries of consolidated crust of а grou...

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Дата:2012
Автор: Lubkov, M. V.
Формат: Стаття
Мова:Російська
Опубліковано: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116598
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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author Lubkov, M. V.
author_facet Lubkov, M. V.
author_sort Lubkov, M. V.
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collection OJS
datestamp_date 2020-10-07T12:02:45Z
description On the base of variation finite element method it was carried out computer modeling of the slow sub horizontal movements of the West-Black Sea Basin (WBSB), and also evolution of its heat fields during a period of time from the moment of access to its lower boundaries of consolidated crust of а group of the most powerful asthenolithes (second quanta of tectonic action (QTA)), about 60 mln years ago to the modern geological period. On the base of general analysis of the obtained results of modeling it was shown that combined action of all considered factors of QTA mechanical and heat effects at the relevant stages of the WBSB of geological development could perfectly lead to the forming of its crust modern structure.
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spelling journalsuranua-geofizicheskiy-article-1165982020-10-07T12:02:45Z Thermomechanical model of the development of the West-Black Sea basin Lubkov, M. V. On the base of variation finite element method it was carried out computer modeling of the slow sub horizontal movements of the West-Black Sea Basin (WBSB), and also evolution of its heat fields during a period of time from the moment of access to its lower boundaries of consolidated crust of а group of the most powerful asthenolithes (second quanta of tectonic action (QTA)), about 60 mln years ago to the modern geological period. On the base of general analysis of the obtained results of modeling it was shown that combined action of all considered factors of QTA mechanical and heat effects at the relevant stages of the WBSB of geological development could perfectly lead to the forming of its crust modern structure. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-02-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116598 10.24028/gzh.0203-3100.v34i1.2012.116598 Geofizicheskiy Zhurnal; Vol. 34 No. 1 (2012); 190-198 Геофизический журнал; Том 34 № 1 (2012); 190-198 Геофізичний журнал; Том 34 № 1 (2012); 190-198 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116598/110624 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Lubkov, M. V.
Thermomechanical model of the development of the West-Black Sea basin
title Thermomechanical model of the development of the West-Black Sea basin
title_full Thermomechanical model of the development of the West-Black Sea basin
title_fullStr Thermomechanical model of the development of the West-Black Sea basin
title_full_unstemmed Thermomechanical model of the development of the West-Black Sea basin
title_short Thermomechanical model of the development of the West-Black Sea basin
title_sort thermomechanical model of the development of the west-black sea basin
url https://journals.uran.ua/geofizicheskiy/article/view/116598
work_keys_str_mv AT lubkovmv thermomechanicalmodelofthedevelopmentofthewestblackseabasin