Deep structure and development of the Scythian plate in the Mezokainozoic in the section of the profile of MOV-OGT No. 598506

Deep structure and development of the Scythian plate in the Mezokainozoic in the section of the profile of MOV-OGT No. 598506

Gravity modeling has been conducted and paleostructural section along the profile MRW CMP № 598506 has been plotted. Results made possible to develop the concept on deep structure and evolution of the central part of the northwestern shelf of the Black Sea. Location of the boundary of the EastEurope...

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Бібліографічні деталі
Дата:2013
Автори: Kozlenko, M.V., Kozlenko, Yu.V.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2013
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/111344
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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spelling journalsuranua-geofizicheskiy-article-1113442020-10-07T10:46:54Z Deep structure and development of the Scythian plate in the Mezokainozoic in the section of the profile of MOV-OGT No. 598506 Kozlenko, M.V. Kozlenko, Yu.V. Gravity modeling has been conducted and paleostructural section along the profile MRW CMP № 598506 has been plotted. Results made possible to develop the concept on deep structure and evolution of the central part of the northwestern shelf of the Black Sea. Location of the boundary of the EastEuropean platform and the Scythian plate in the profile section has been delimited. Riftogenic origin of the Karkinite sag has been confirmed as well as the presence of the rock lens with the density value specific for Triassic deposits under Jurassic deposits of the Kalamite swell. According to velocity values of sediments accumulation calculated on the base of the data on thickness of sedimentary complexes the development of the structures of the region was produced by the sinking of the Karkinite sag during the Cretaceous — Maikopian and of the Edge footstep in the Upper Cretaceous. Currently the sinking within the limits of the West—Black Sea lobe occurred. The character of faults formation during the evolution of the Karkinite sag indicates the presence of the southward direction stretching regime in the Early Cretaceous, which changed by compression, produced probably by the pressure from the side of developed WestBlack Sea lobe. Subbotin Institute of Geophysics of the NAS of Ukraine 2013-03-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111344 10.24028/gzh.0203-3100.v35i2.2013.111344 Geofizicheskiy Zhurnal; Vol. 35 No. 2 (2013); 98-110 Геофизический журнал; Том 35 № 2 (2013); 98-110 Геофізичний журнал; Том 35 № 2 (2013); 98-110 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/111344/106345 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Kozlenko, M.V.
Kozlenko, Yu.V.
spellingShingle Kozlenko, M.V.
Kozlenko, Yu.V.
Deep structure and development of the Scythian plate in the Mezokainozoic in the section of the profile of MOV-OGT No. 598506
author_facet Kozlenko, M.V.
Kozlenko, Yu.V.
author_sort Kozlenko, M.V.
title Deep structure and development of the Scythian plate in the Mezokainozoic in the section of the profile of MOV-OGT No. 598506
title_short Deep structure and development of the Scythian plate in the Mezokainozoic in the section of the profile of MOV-OGT No. 598506
title_full Deep structure and development of the Scythian plate in the Mezokainozoic in the section of the profile of MOV-OGT No. 598506
title_fullStr Deep structure and development of the Scythian plate in the Mezokainozoic in the section of the profile of MOV-OGT No. 598506
title_full_unstemmed Deep structure and development of the Scythian plate in the Mezokainozoic in the section of the profile of MOV-OGT No. 598506
title_sort deep structure and development of the scythian plate in the mezokainozoic in the section of the profile of mov-ogt no. 598506
description Gravity modeling has been conducted and paleostructural section along the profile MRW CMP № 598506 has been plotted. Results made possible to develop the concept on deep structure and evolution of the central part of the northwestern shelf of the Black Sea. Location of the boundary of the EastEuropean platform and the Scythian plate in the profile section has been delimited. Riftogenic origin of the Karkinite sag has been confirmed as well as the presence of the rock lens with the density value specific for Triassic deposits under Jurassic deposits of the Kalamite swell. According to velocity values of sediments accumulation calculated on the base of the data on thickness of sedimentary complexes the development of the structures of the region was produced by the sinking of the Karkinite sag during the Cretaceous — Maikopian and of the Edge footstep in the Upper Cretaceous. Currently the sinking within the limits of the West—Black Sea lobe occurred. The character of faults formation during the evolution of the Karkinite sag indicates the presence of the southward direction stretching regime in the Early Cretaceous, which changed by compression, produced probably by the pressure from the side of developed WestBlack Sea lobe.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2013
url https://journals.uran.ua/geofizicheskiy/article/view/111344
work_keys_str_mv AT kozlenkomv deepstructureanddevelopmentofthescythianplateinthemezokainozoicinthesectionoftheprofileofmovogtno598506
AT kozlenkoyuv deepstructureanddevelopmentofthescythianplateinthemezokainozoicinthesectionoftheprofileofmovogtno598506
first_indexed 2024-04-21T19:40:17Z
last_indexed 2024-04-21T19:40:17Z
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