Deformations due to the processes of compaction, decompaction and phase transitions in the internal structures of the Earth

Deformations due to the processes of compaction, decompaction and phase transitions in the internal structures of the Earth

Questions of dis tribution of medium depending on changes of deformation have been studied involving various elastic potentials using non-classical linearized approach within the limits of theory of small and large initial deformations and it has been shown that this dependence for various geologica...

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Видавець:Subbotin Institute of Geophysics of the NAS of Ukraine
Дата:2013
Автор: Kuliev, G. G.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2013
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116421
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Geofizicheskiy Zhurnal
id journalsuranua-geofizicheskiy-article-116421
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spelling journalsuranua-geofizicheskiy-article-1164212020-10-07T12:00:36Z Deformations due to the processes of compaction, decompaction and phase transitions in the internal structures of the Earth Kuliev, G. G. Questions of dis tribution of medium depending on changes of deformation have been studied involving various elastic potentials using non-classical linearized approach within the limits of theory of small and large initial deformations and it has been shown that this dependence for various geological media is instable. Given processes contribute to e mergence of structures of formation deconsolidation zones. In p resence of different kinds of inclusions, free and contacted surfaces and cavities the p rocess of de formation occurs differently than assumed in experiments. Comparing the received theoretical results with results o f known experimental studies, it has been shown that the processes of loss of stability of elastic state of equilibrium on geometric shape change and on "internal" instability precedes the p rocesses of phase transitions of various mineral systems. Subbotin Institute of Geophysics of the NAS of Ukraine 2013-04-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116421 10.24028/gzh.0203-3100.v35i3.2013.116421 Geofizicheskiy Zhurnal; Vol. 35 No. 3 (2013); 166-176 Геофизический журнал; Том 35 № 3 (2013); 166-176 Геофізичний журнал; Том 35 № 3 (2013); 166-176 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116421/110457 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Kuliev, G. G.
spellingShingle Kuliev, G. G.
Deformations due to the processes of compaction, decompaction and phase transitions in the internal structures of the Earth
author_facet Kuliev, G. G.
author_sort Kuliev, G. G.
title Deformations due to the processes of compaction, decompaction and phase transitions in the internal structures of the Earth
title_short Deformations due to the processes of compaction, decompaction and phase transitions in the internal structures of the Earth
title_full Deformations due to the processes of compaction, decompaction and phase transitions in the internal structures of the Earth
title_fullStr Deformations due to the processes of compaction, decompaction and phase transitions in the internal structures of the Earth
title_full_unstemmed Deformations due to the processes of compaction, decompaction and phase transitions in the internal structures of the Earth
title_sort deformations due to the processes of compaction, decompaction and phase transitions in the internal structures of the earth
description Questions of dis tribution of medium depending on changes of deformation have been studied involving various elastic potentials using non-classical linearized approach within the limits of theory of small and large initial deformations and it has been shown that this dependence for various geological media is instable. Given processes contribute to e mergence of structures of formation deconsolidation zones. In p resence of different kinds of inclusions, free and contacted surfaces and cavities the p rocess of de formation occurs differently than assumed in experiments. Comparing the received theoretical results with results o f known experimental studies, it has been shown that the processes of loss of stability of elastic state of equilibrium on geometric shape change and on "internal" instability precedes the p rocesses of phase transitions of various mineral systems.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2013
url https://journals.uran.ua/geofizicheskiy/article/view/116421
work_keys_str_mv AT kulievgg deformationsduetotheprocessesofcompactiondecompactionandphasetransitionsintheinternalstructuresoftheearth
first_indexed 2024-04-21T19:40:49Z
last_indexed 2024-04-21T19:40:49Z
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