Stress-strain state of the Heraklei volcano-tectonic block of the Mountainous Crimea

This paper presents the paleostress results obtained for Heracleyskaya anticlinal (Western Crimea). On the basis of field tectonophysical study of brittle planes and 3D relief map deciphering the scheme of faults is made. Conjugate sets of fractures and fault-slip data are used to reconstruct orient...

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Бібліографічні деталі
Дата:2011
Автор: Murovskaya, A.V.
Формат: Стаття
Мова:Російська
Опубліковано: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2011
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/117293
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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author Murovskaya, A.V.
author_facet Murovskaya, A.V.
author_sort Murovskaya, A.V.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:00:55Z
description This paper presents the paleostress results obtained for Heracleyskaya anticlinal (Western Crimea). On the basis of field tectonophysical study of brittle planes and 3D relief map deciphering the scheme of faults is made. Conjugate sets of fractures and fault-slip data are used to reconstruct orientation of the principal stress and deformation regimes. It is shown that the Heracleyskiy peninsula has been exposed to the 10 compression and tension deformation phases from the Middle Jurassic period. Stress reconstruction results are compared with gravitational field data. In the Neogen-Quaternary time for lower lithosphere the compression stress is characteristic while for upper crust the tension stress is typical as well. It seems to be connected with the recent raising of the Crimean mountains.
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spelling journalsuranua-geofizicheskiy-article-1172932020-10-07T11:00:55Z Stress-strain state of the Heraklei volcano-tectonic block of the Mountainous Crimea Murovskaya, A.V. This paper presents the paleostress results obtained for Heracleyskaya anticlinal (Western Crimea). On the basis of field tectonophysical study of brittle planes and 3D relief map deciphering the scheme of faults is made. Conjugate sets of fractures and fault-slip data are used to reconstruct orientation of the principal stress and deformation regimes. It is shown that the Heracleyskiy peninsula has been exposed to the 10 compression and tension deformation phases from the Middle Jurassic period. Stress reconstruction results are compared with gravitational field data. In the Neogen-Quaternary time for lower lithosphere the compression stress is characteristic while for upper crust the tension stress is typical as well. It seems to be connected with the recent raising of the Crimean mountains. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2011-04-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/117293 10.24028/gzh.0203-3100.v33i2.2011.117293 Geofizicheskiy Zhurnal; Vol. 33 No. 2 (2011); 46-56 Геофизический журнал; Том 33 № 2 (2011); 46-56 Геофізичний журнал; Том 33 № 2 (2011); 46-56 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/117293/111380 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Murovskaya, A.V.
Stress-strain state of the Heraklei volcano-tectonic block of the Mountainous Crimea
title Stress-strain state of the Heraklei volcano-tectonic block of the Mountainous Crimea
title_full Stress-strain state of the Heraklei volcano-tectonic block of the Mountainous Crimea
title_fullStr Stress-strain state of the Heraklei volcano-tectonic block of the Mountainous Crimea
title_full_unstemmed Stress-strain state of the Heraklei volcano-tectonic block of the Mountainous Crimea
title_short Stress-strain state of the Heraklei volcano-tectonic block of the Mountainous Crimea
title_sort stress-strain state of the heraklei volcano-tectonic block of the mountainous crimea
url https://journals.uran.ua/geofizicheskiy/article/view/117293
work_keys_str_mv AT murovskayaav stressstrainstateoftheherakleivolcanotectonicblockofthemountainouscrimea