The collision model of the Crimean orogen - the experience of the finite element method

Finite elements method is attracted for numerical modeling of crust deformation of Crimea Mountains within hypothesis of its collisional formation. Elastic and elastoplastic (Coulomb) ap-proaches are used. As a result next basic positions of collisional model are proved: 1) localized indenter compre...

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Date:2013
Main Author: Gonchar, V. V.
Format: Article
Language:Russian
Published: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2013
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/116526
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Journal Title:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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author Gonchar, V. V.
author_facet Gonchar, V. V.
author_sort Gonchar, V. V.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:59:34Z
description Finite elements method is attracted for numerical modeling of crust deformation of Crimea Mountains within hypothesis of its collisional formation. Elastic and elastoplastic (Coulomb) ap-proaches are used. As a result next basic positions of collisional model are proved: 1) localized indenter compression of margin of Scythian plate from side of East Black Sea basin; 2) lateral extru-sion of south-west part of orogen; 3) ramp-obductional mechanism of interacting crust microplate with continental margin. Seismicity is explained as localization of plastic deformation in set of restricted subduction of mantle lithosphere and owerthrusting crust plate. Gravitational maximum within south-west margin of Crimea Mountains is connected to extensional zone of extrusive block, Alushta-Batun zone of magnetic anomalies is regarded as manifestation of crustal indenter moving responsible for collisional setting in Crimea.
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spelling journalsuranua-geofizicheskiy-article-1165262020-10-07T11:59:34Z The collision model of the Crimean orogen - the experience of the finite element method Gonchar, V. V. Finite elements method is attracted for numerical modeling of crust deformation of Crimea Mountains within hypothesis of its collisional formation. Elastic and elastoplastic (Coulomb) ap-proaches are used. As a result next basic positions of collisional model are proved: 1) localized indenter compression of margin of Scythian plate from side of East Black Sea basin; 2) lateral extru-sion of south-west part of orogen; 3) ramp-obductional mechanism of interacting crust microplate with continental margin. Seismicity is explained as localization of plastic deformation in set of restricted subduction of mantle lithosphere and owerthrusting crust plate. Gravitational maximum within south-west margin of Crimea Mountains is connected to extensional zone of extrusive block, Alushta-Batun zone of magnetic anomalies is regarded as manifestation of crustal indenter moving responsible for collisional setting in Crimea. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2013-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116526 10.24028/gzh.0203-3100.v35i6.2013.116526 Geofizicheskiy Zhurnal; Vol. 35 No. 6 (2013); 146-164 Геофизический журнал; Том 35 № 6 (2013); 146-164 Геофізичний журнал; Том 35 № 6 (2013); 146-164 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116526/110548 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Gonchar, V. V.
The collision model of the Crimean orogen - the experience of the finite element method
title The collision model of the Crimean orogen - the experience of the finite element method
title_full The collision model of the Crimean orogen - the experience of the finite element method
title_fullStr The collision model of the Crimean orogen - the experience of the finite element method
title_full_unstemmed The collision model of the Crimean orogen - the experience of the finite element method
title_short The collision model of the Crimean orogen - the experience of the finite element method
title_sort collision model of the crimean orogen - the experience of the finite element method
url https://journals.uran.ua/geofizicheskiy/article/view/116526
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AT goncharvv collisionmodelofthecrimeanorogentheexperienceofthefiniteelementmethod