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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| Date: | 2014 |
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| Main Author: | |
| Format: | Article |
| Language: | Russian |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2014
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| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/111028 |
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| Journal Title: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543133056106496 |
|---|---|
| author | Vol'fman, Yu.M. |
| author_facet | Vol'fman, Yu.M. |
| author_sort | Vol'fman, Yu.M. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T11:45:12Z |
| 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. |
| first_indexed | 2025-07-17T11:05:08Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-111028 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:05:08Z |
| publishDate | 2014 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| 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. S. 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 ru https://journals.uran.ua/geofizicheskiy/article/view/111028/105951 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| 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 |
| title | 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_short | 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 |
| topic | tectonic faulting the stress fields deformation modes kinematic conditions stereographic models shifts upthrusts faults |
| topic_facet | tectonic faulting the stress fields deformation modes kinematic conditions stereographic models shifts upthrusts faults |
| url | https://journals.uran.ua/geofizicheskiy/article/view/111028 |
| work_keys_str_mv | AT volfmanyum deformationalregimesandkinematicenvironmentsofformationofuptodatetectonicdisruptionswithinthelimitsofthemountaincrimea |