KFU. Card publication. Early Cretaceous Sea Level Fluctuations in the Eastern Part of the East European Platform

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EARLY CRETACEOUS SEA LEVEL FLUCTUATIONS IN THE EASTERN PART OF THE EAST EUROPEAN PLATFORM

Form of presentation

Articles in international journals and collections

Year of publication

2016

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Authors, employees of KFU

Zorina Svetlana Olegovna, author

Bibliographic description in the original language

Zorina S.O. Early Cretaceous Sea Level Fluctuations in the Eastern Part of the East European Platform. Doklady Earth Sciences, 2016, Vol. 470, Part 2, pp. 1002–1005. DOI: 10.1134/S1028334X16100081

Annotation

The quantitative sea-level curve in the eastern part of the East European Platform during the Early Cretaceous first compiled for this region is based on the results of analysis of the corresponding deposits and the bathymetric distribution of benthic foraminifers in their sections. This quantitative curve is correlated with the sea-level curve constructed for central areas of the East European Platform [9]. According to [9], the basin in the central part of the platform was as deep as 110 m, while in its eastern areas the depth amounted to 350 m. It is revealed that tectono-eustatic cycles defined previously in the central part of the platform and cycles (megasequences) in its eastern areas are asynchronous and are characterized by different orders. Such asynchrony is determined by the different tectonic trends in these regions during the Early Cretaceous.

Keywords

sea level changes, Early Cretaceous, East European Platform

The name of the journal

DOKL EARTH SCI

URL

http://link.springer.com/article/10.1134/S1028334X16100081

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=141465&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Zorina Svetlana Olegovna	ru_RU
dc.date.accessioned	2016-01-01T00:00:00Z	ru_RU
dc.date.available	2016-01-01T00:00:00Z	ru_RU
dc.date.issued	2016	ru_RU
dc.identifier.citation	Zorina S.O. Early Cretaceous Sea Level Fluctuations in the Eastern Part of the East European Platform. Doklady Earth Sciences, 2016, Vol. 470, Part 2, pp. 1002–1005. DOI: 10.1134/S1028334X16100081	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=141465&p_lang=2	ru_RU
dc.description.abstract	DOKL EARTH SCI	ru_RU
dc.description.abstract	The quantitative sea-level curve in the eastern part of the East European Platform during the Early Cretaceous first compiled for this region is based on the results of analysis of the corresponding deposits and the bathymetric distribution of benthic foraminifers in their sections. This quantitative curve is correlated with the sea-level curve constructed for central areas of the East European Platform [9]. According to [9], the basin in the central part of the platform was as deep as 110 m, while in its eastern areas the depth amounted to 350 m. It is revealed that tectono-eustatic cycles defined previously in the central part of the platform and cycles (megasequences) in its eastern areas are asynchronous and are characterized by different orders. Such asynchrony is determined by the different tectonic trends in these regions during the Early Cretaceous.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	sea level changes	ru_RU
dc.subject	Early Cretaceous	ru_RU
dc.subject	East European Platform	ru_RU
dc.title	Early Cretaceous Sea Level Fluctuations in the Eastern Part of the East European Platform	ru_RU
dc.type	Articles in international journals and collections	ru_RU