East Mountain Crimea strain fields of different age
Actual data of kinematic analysis have been given, reconstruction and discrimination of strain fields with respect to the stage of main folding within the limits of the East Mountain Crimea have been fulfilled. The field of sub-meridional—northwestern compression realized in connection with processe...
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| Дата: | 2017 |
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| Формат: | Стаття |
| Мова: | rus |
| Опубліковано: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2017
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| Назва журналу: | Geofizicheskiy Zhurnal |
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journalsuranua-geofizicheskiy-article-94011 |
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journalsuranua-geofizicheskiy-article-940112020-10-07T11:14:17Z East Mountain Crimea strain fields of different age East Mountain Crimea strain fields of different age Gonchar, V. V. East Mountain Crimea strain fields folding paleotectonic reconstructions East Mountain Crimea strain fields folding paleotectonic reconstructions Actual data of kinematic analysis have been given, reconstruction and discrimination of strain fields with respect to the stage of main folding within the limits of the East Mountain Crimea have been fulfilled. The field of sub-meridional—northwestern compression realized in connection with processes of Arabian collision is responsible for formation of final folding of the Sudak-Karadag zone and post-folding collision compression of the East Mountain Crimea. As pre-folding fields arc defined the following ones: the fields of thrust-displacement type with northeastern and west-north-west orientations of compression axes and thrust fields with northeastern and northwestern orientation of axes of tension. The last ones can most probably be related to manifestation of riftogenesis behind the arc in the Black Sea region during Middle Cretaceous—Paleocene. The field of northeastern compression might be related to regional compression in Late Eocene—Oligocene, stipulated the folding of the Great Caucasus. Actual data of kinematic analysis have been given, reconstruction and discrimination of strain fields with respect to the stage of main folding within the limits of the East Mountain Crimea have been fulfilled. The field of sub-meridional—northwestern compression realized in connection with processes of Arabian collision is responsible for formation of final folding of the Sudak-Karadag zone and post-folding collision compression of the East Mountain Crimea. As pre-folding fields arc defined the following ones: the fields of thrust-displacement type with northeastern and west-north-west orientations of compression axes and thrust fields with northeastern and northwestern orientation of axes of tension. The last ones can most probably be related to manifestation of riftogenesis behind the arc in the Black Sea region during Middle Cretaceous—Paleocene. The field of northeastern compression might be related to regional compression in Late Eocene—Oligocene, stipulated the folding of the Great Caucasus. Subbotin Institute of Geophysics of the NAS of Ukraine 2017-03-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/94011 10.24028/gzh.0203-3100.v39i1.2017.94011 Geofizicheskiy Zhurnal; Vol. 39 No. 1 (2017); 61-78 Геофизический журнал; Том 39 № 1 (2017); 61-78 Геофізичний журнал; Том 39 № 1 (2017); 61-78 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/94011/195717 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| institution |
Geofizicheskiy Zhurnal |
| collection |
OJS |
| language |
rus |
| topic |
East Mountain Crimea strain fields folding paleotectonic reconstructions East Mountain Crimea strain fields folding paleotectonic reconstructions |
| spellingShingle |
East Mountain Crimea strain fields folding paleotectonic reconstructions East Mountain Crimea strain fields folding paleotectonic reconstructions Gonchar, V. V. East Mountain Crimea strain fields of different age |
| topic_facet |
East Mountain Crimea strain fields folding paleotectonic reconstructions East Mountain Crimea strain fields folding paleotectonic reconstructions |
| format |
Article |
| author |
Gonchar, V. V. |
| author_facet |
Gonchar, V. V. |
| author_sort |
Gonchar, V. V. |
| title |
East Mountain Crimea strain fields of different age |
| title_short |
East Mountain Crimea strain fields of different age |
| title_full |
East Mountain Crimea strain fields of different age |
| title_fullStr |
East Mountain Crimea strain fields of different age |
| title_full_unstemmed |
East Mountain Crimea strain fields of different age |
| title_sort |
east mountain crimea strain fields of different age |
| title_alt |
East Mountain Crimea strain fields of different age |
| description |
Actual data of kinematic analysis have been given, reconstruction and discrimination of strain fields with respect to the stage of main folding within the limits of the East Mountain Crimea have been fulfilled. The field of sub-meridional—northwestern compression realized in connection with processes of Arabian collision is responsible for formation of final folding of the Sudak-Karadag zone and post-folding collision compression of the East Mountain Crimea. As pre-folding fields arc defined the following ones: the fields of thrust-displacement type with northeastern and west-north-west orientations of compression axes and thrust fields with northeastern and northwestern orientation of axes of tension. The last ones can most probably be related to manifestation of riftogenesis behind the arc in the Black Sea region during Middle Cretaceous—Paleocene. The field of northeastern compression might be related to regional compression in Late Eocene—Oligocene, stipulated the folding of the Great Caucasus. |
| publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
| publishDate |
2017 |
| url |
https://journals.uran.ua/geofizicheskiy/article/view/94011 |
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2024-04-21T19:39:48Z |
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2024-04-21T19:39:48Z |
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