КФУ. Карточка публикации. 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

Форма представления

Статьи в зарубежных журналах и сборниках

Год публикации

2016

Язык

английский

Авторы, сотрудники КФУ

Зорина Светлана Олеговна, автор

Библиографическое описание на языке оригинала

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

Аннотация

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.

Ключевые слова

sea level changes, Early Cretaceous, East European Platform

Название журнала

DOKL EARTH SCI

URL

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

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https://repository.kpfu.ru/?p_id=141465

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Зорина Светлана Олеговна	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/?p_id=141465	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	Статьи в зарубежных журналах и сборниках	ru_RU