The structure and evolution of lithosphere of the central part of the northwestern shelf of the Black Sea
Density modeling has been conducted that made possible to specify the structure of lithosphere of the central part of northwestern shelf of the Black Sea.In the section of the profile the boundary between the East European platform and the Scythian plate has been identified, which is the fault incli...
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| Дата: | 2014 |
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| Автори: | , |
| Формат: | Стаття |
| Мова: | rus |
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Subbotin Institute of Geophysics of the NAS of Ukraine
2014
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| Назва журналу: | Geofizicheskiy Zhurnal |
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journalsuranua-geofizicheskiy-article-116025 |
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journalsuranua-geofizicheskiy-article-1160252020-10-07T11:57:02Z The structure and evolution of lithosphere of the central part of the northwestern shelf of the Black Sea Kozlenko, M.V. Kozlenko, Yu.V. density modeling northwestern sheff of the Black Sea paleoreconstruction Density modeling has been conducted that made possible to specify the structure of lithosphere of the central part of northwestern shelf of the Black Sea.In the section of the profile the boundary between the East European platform and the Scythian plate has been identified, which is the fault inclined southward and located in the upper part of the section about 30km northward of the Golitsyn fault. On the base of the plotted paleostructural section evolution of Scythian plate in the crossec-tion of the profile since Paleozoic has been traced. The basement of northwestern shelf of the Black Sea and its central part was broken by numerous disjunctives and fault zones, many of them can be traced within sedimentary cover and stretch to the lower levels of crystal crust. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116025 10.24028/gzh.0203-3100.v36i4.2014.116025 Geofizicheskiy Zhurnal; Vol. 36 No. 4 (2014); 65-74 Геофизический журнал; Том 36 № 4 (2014); 65-74 Геофізичний журнал; Том 36 № 4 (2014); 65-74 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116025/110146 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
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Geofizicheskiy Zhurnal |
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| datestamp_date |
2020-10-07T11:57:02Z |
| collection |
OJS |
| language |
rus |
| topic |
density modeling northwestern sheff of the Black Sea paleoreconstruction |
| spellingShingle |
density modeling northwestern sheff of the Black Sea paleoreconstruction Kozlenko, M.V. Kozlenko, Yu.V. The structure and evolution of lithosphere of the central part of the northwestern shelf of the Black Sea |
| topic_facet |
density modeling northwestern sheff of the Black Sea paleoreconstruction |
| format |
Article |
| author |
Kozlenko, M.V. Kozlenko, Yu.V. |
| author_facet |
Kozlenko, M.V. Kozlenko, Yu.V. |
| author_sort |
Kozlenko, M.V. |
| title |
The structure and evolution of lithosphere of the central part of the northwestern shelf of the Black Sea |
| title_short |
The structure and evolution of lithosphere of the central part of the northwestern shelf of the Black Sea |
| title_full |
The structure and evolution of lithosphere of the central part of the northwestern shelf of the Black Sea |
| title_fullStr |
The structure and evolution of lithosphere of the central part of the northwestern shelf of the Black Sea |
| title_full_unstemmed |
The structure and evolution of lithosphere of the central part of the northwestern shelf of the Black Sea |
| title_sort |
structure and evolution of lithosphere of the central part of the northwestern shelf of the black sea |
| description |
Density modeling has been conducted that made possible to specify the structure of lithosphere of the central part of northwestern shelf of the Black Sea.In the section of the profile the boundary between the East European platform and the Scythian plate has been identified, which is the fault inclined southward and located in the upper part of the section about 30km northward of the Golitsyn fault. On the base of the plotted paleostructural section evolution of Scythian plate in the crossec-tion of the profile since Paleozoic has been traced. The basement of northwestern shelf of the Black Sea and its central part was broken by numerous disjunctives and fault zones, many of them can be traced within sedimentary cover and stretch to the lower levels of crystal crust. |
| publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
| publishDate |
2014 |
| url |
https://journals.uran.ua/geofizicheskiy/article/view/116025 |
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