SEDIMENTS OF LAKES IN LENINGRAD REGION AS THE CHRONICLE OF BALTIC LEVEL FLUCTUATION

dc.contributor.author	Subetto D.A.
dc.contributor.author	Sevastyanov D.V.
dc.contributor.author	Savelyeva L.A.
dc.contributor.author	Arslanov H.A.
dc.date.accessioned	2021-06-19T08:13:25Z
dc.date.available	2021-06-19T08:13:25Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=15086333
dc.identifier.citation	Вестник Санкт-Петербургского университета. Серия 7. Геология. География, 2002, , 4, 75-85
dc.identifier.issn	1029-7456
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/29162
dc.description.abstract	The paper gives a comprehensive survey of the materials on sedimentation in the lakes of Leningrad region. On the strength of the new data on the structure of bottom sediments the authors conclude that sedimentation conditions had undergone a drastic change in late Pleistocene and Holocene. The chronological boundaries of the transgresses and regresses of the Baltic area and Ladoga Lake in Holocene have been defined more precisely.
dc.title	SEDIMENTS OF LAKES IN LENINGRAD REGION AS THE CHRONICLE OF BALTIC LEVEL FLUCTUATION
dc.type	Статья

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