SOME INDICATION FOR LATE QUATERNARY PECHORA RIVER DISCHARGE:RESULTS OF VIBROCORE STUDIES IN THE SOUTHEASTERN PECHORA SEA

dc.contributor.author	Levitan M.A.
dc.contributor.author	Kuptsov V.M.
dc.contributor.author	Romankevich E.A.
dc.contributor.author	Kondratenko A.V.
dc.date.accessioned	2021-01-28T11:15:51Z
dc.date.available	2021-01-28T11:15:51Z
dc.date.issued	2000
dc.identifier	https://elibrary.ru/item.asp?id=13349492
dc.identifier.citation	International Journal of Earth Sciences, 2000, 89, 3, 537-540
dc.identifier.issn	1437-3254
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/23903
dc.description.abstract	The study of Upper Quaternary sedimentary sequences in the Pechora Sea by means of vibrocoring revealed three sediment units. The (youngest) sandy unit accumulated in marine environments later than 5000 years B.P. The clayey unit belongs to a pro-deltaic facies, probably formed during Middle Holocene times. The diamict unit formed during Middle/Early Weichselian times, probably has a glacigenic origin and is separated from the clayey unit by a hiatus. The changes in lithology are partly related to changes in Pechora River discharge during late Weichselian/Holocene times.
dc.subject	Quaternary	en
dc.title	SOME INDICATION FOR LATE QUATERNARY PECHORA RIVER DISCHARGE:RESULTS OF VIBROCORE STUDIES IN THE SOUTHEASTERN PECHORA SEA
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary	en
dc.subject.age	Кайнозой::Четвертичная	ru

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