Deflected mode of the Western Mountain Crimea in Oligocene-Holocen according to tectonophysical data
Within the limits of western Crimean Mountains 2016 tectonic slickenside with kinematic indicators and 600 ruptures without visible signs of displacement have been studied. Stress fields were determined using structural-paragenetic and kinematic analyses. These fields were subdivided into three type...
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| Date: | 2012 |
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| Main Author: | |
| Format: | Article |
| Language: | Russian |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2012
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| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/116621 |
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| Journal Title: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543259887665152 |
|---|---|
| author | Murovskaya, A.V. |
| author_facet | Murovskaya, A.V. |
| author_sort | Murovskaya, A.V. |
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| collection | OJS |
| datestamp_date | 2020-10-07T12:21:24Z |
| description | Within the limits of western Crimean Mountains 2016 tectonic slickenside with kinematic indicators and 600 ruptures without visible signs of displacement have been studied. Stress fields were determined using structural-paragenetic and kinematic analyses. These fields were subdivided into three types: strike-slip, normal, and reverse that constitute 51, 30 и 19 % of the total fault planes. The principal axes trends for each field type were compared with the strike of the Main Ridge. Contemporary regional stress field was separated out by comparing inversed stress fields and 8 nearest earthquake source mechanisms. The results were interpreted in the context of regional tectonics of the Crimean-the Black Sea area. It was concluded that the Crimean Mountains were formed under the combined impact of the African-Arabic, Adriatic and Pannonien plates. |
| first_indexed | 2025-07-17T11:07:11Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-116621 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:07:11Z |
| publishDate | 2012 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1166212020-10-07T12:21:24Z Deflected mode of the Western Mountain Crimea in Oligocene-Holocen according to tectonophysical data Murovskaya, A.V. Within the limits of western Crimean Mountains 2016 tectonic slickenside with kinematic indicators and 600 ruptures without visible signs of displacement have been studied. Stress fields were determined using structural-paragenetic and kinematic analyses. These fields were subdivided into three types: strike-slip, normal, and reverse that constitute 51, 30 и 19 % of the total fault planes. The principal axes trends for each field type were compared with the strike of the Main Ridge. Contemporary regional stress field was separated out by comparing inversed stress fields and 8 nearest earthquake source mechanisms. The results were interpreted in the context of regional tectonics of the Crimean-the Black Sea area. It was concluded that the Crimean Mountains were formed under the combined impact of the African-Arabic, Adriatic and Pannonien plates. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-04-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116621 10.24028/gzh.0203-3100.v34i2.2012.116621 Geofizicheskiy Zhurnal; Vol. 34 No. 2 (2012); 109-119 Геофизический журнал; Том 34 № 2 (2012); 109-119 Геофізичний журнал; Том 34 № 2 (2012); 109-119 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116621/110655 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | Murovskaya, A.V. Deflected mode of the Western Mountain Crimea in Oligocene-Holocen according to tectonophysical data |
| title | Deflected mode of the Western Mountain Crimea in Oligocene-Holocen according to tectonophysical data |
| title_full | Deflected mode of the Western Mountain Crimea in Oligocene-Holocen according to tectonophysical data |
| title_fullStr | Deflected mode of the Western Mountain Crimea in Oligocene-Holocen according to tectonophysical data |
| title_full_unstemmed | Deflected mode of the Western Mountain Crimea in Oligocene-Holocen according to tectonophysical data |
| title_short | Deflected mode of the Western Mountain Crimea in Oligocene-Holocen according to tectonophysical data |
| title_sort | deflected mode of the western mountain crimea in oligocene-holocen according to tectonophysical data |
| url | https://journals.uran.ua/geofizicheskiy/article/view/116621 |
| work_keys_str_mv | AT murovskayaav deflectedmodeofthewesternmountaincrimeainoligoceneholocenaccordingtotectonophysicaldata |