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Deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the Mountain Crimea

It has been shown on the base of considerable tectonophysical material that producing of up-to-date tectonic disruptions within the limits of the Mountain Crimea is specified by broad spectrum of deformational regimes and kinematic environments. The technique of plotting is methodologically substant...

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Main Author: Vol'fman, Yu.M.
Format: Article
Language:rus
Published: Subbotin Institute of Geophysics of the NAS of Ukraine 2014
Subjects:
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/111028
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spelling journalsuranua-geofizicheskiy-article-1110282020-10-07T11:45:12Z Deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the Mountain Crimea Vol'fman, Yu.M. tectonic faulting the stress fields deformation modes kinematic conditions stereographic models shifts upthrusts faults It has been shown on the base of considerable tectonophysical material that producing of up-to-date tectonic disruptions within the limits of the Mountain Crimea is specified by broad spectrum of deformational regimes and kinematic environments. The technique of plotting is methodologically substantiated for stereographical models of deformational regimes by averaging the parameters of structural-kinematic parageneses of tectonic disruptions and displacements produced in similar conditions. These models reflect adequately regional environments of producing tectonic disruptions. Quantitative ratio of slickensides in parageneses, which make up the basis of corresponding models specify the measure of effects of these or other deformational regimes on the processes of tectogenesis in  the region. The models and examples of shearing, upthrust- and upthrust-displacement deformational regimes are presented and their description is given. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111028 10.24028/gzh.0203-3100.v36i6.2014.111028 Geofizicheskiy Zhurnal; Vol. 36 No. 6 (2014); 93-112 Геофизический журнал; Том 36 № 6 (2014); 93-112 Геофізичний журнал; Том 36 № 6 (2014); 93-112 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/111028/105951 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
topic tectonic faulting
the stress fields
deformation modes
kinematic conditions
stereographic models
shifts
upthrusts
faults
spellingShingle tectonic faulting
the stress fields
deformation modes
kinematic conditions
stereographic models
shifts
upthrusts
faults
Vol'fman, Yu.M.
Deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the Mountain Crimea
topic_facet tectonic faulting
the stress fields
deformation modes
kinematic conditions
stereographic models
shifts
upthrusts
faults
format Article
author Vol'fman, Yu.M.
author_facet Vol'fman, Yu.M.
author_sort Vol'fman, Yu.M.
title Deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the Mountain Crimea
title_short Deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the Mountain Crimea
title_full Deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the Mountain Crimea
title_fullStr Deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the Mountain Crimea
title_full_unstemmed Deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the Mountain Crimea
title_sort deformational regimes and kinematic environments of formation of up-to-date tectonic disruptions within the limits of the mountain crimea
description It has been shown on the base of considerable tectonophysical material that producing of up-to-date tectonic disruptions within the limits of the Mountain Crimea is specified by broad spectrum of deformational regimes and kinematic environments. The technique of plotting is methodologically substantiated for stereographical models of deformational regimes by averaging the parameters of structural-kinematic parageneses of tectonic disruptions and displacements produced in similar conditions. These models reflect adequately regional environments of producing tectonic disruptions. Quantitative ratio of slickensides in parageneses, which make up the basis of corresponding models specify the measure of effects of these or other deformational regimes on the processes of tectogenesis in  the region. The models and examples of shearing, upthrust- and upthrust-displacement deformational regimes are presented and their description is given.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2014
url https://journals.uran.ua/geofizicheskiy/article/view/111028
work_keys_str_mv AT volfmanyum deformationalregimesandkinematicenvironmentsofformationofuptodatetectonicdisruptionswithinthelimitsofthemountaincrimea
first_indexed 2024-04-21T19:39:56Z
last_indexed 2024-04-21T19:39:56Z
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