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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| Date: | 2013 |
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Subbotin Institute of Geophysics of the NAS of Ukraine
2013
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| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/116421 |
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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 |
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Geofizicheskiy Zhurnal |
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| datestamp_date |
2020-10-07T12:00:36Z |
| 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 |
2025-07-17T11:06:51Z |
| last_indexed |
2025-07-17T11:06:51Z |
| _version_ |
1837892015929425920 |