Model of localization of seismotectonic deformation of the Crimean orogen.
Discrimination of stress fields by age of folding processes is made for East Crimea Mountains. Stress fields of horizontal extension with north-east and north-west orientations of elongation axes are recognized as the most ancient. Stress fields of compression and strike-slip types with axes oriente...
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| Date: | 2013 |
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| Main Author: | |
| Format: | Article |
| Language: | Russian |
| Published: |
S. Subbotin Institute of Geophysics of the NAS of Ukraine
2013
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| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/111435 |
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| Journal Title: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| Summary: | Discrimination of stress fields by age of folding processes is made for East Crimea Mountains. Stress fields of horizontal extension with north-east and north-west orientations of elongation axes are recognized as the most ancient. Stress fields of compression and strike-slip types with axes oriented in north-east and west-north-west are most possibly considered as pre-folded ones. The youngest and responsible for the final folding of the Sudak- Kara-Dag zone and post-folding collision compression of East Crimea Mountains is a field of sub-longitudinal north-west compression realized in relation to processes of Arabian collision. |
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