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

dc.contributor.authorSubetto D.A.
dc.contributor.authorSevastyanov D.V.
dc.contributor.authorSavelyeva L.A.
dc.contributor.authorArslanov H.A.
dc.date.accessioned2021-06-19T08:13:25Z
dc.date.available2021-06-19T08:13:25Z
dc.date.issued2002
dc.description.abstractThe 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.identifierhttps://elibrary.ru/item.asp?id=15086333
dc.identifier.citationВестник Санкт-Петербургского университета. Серия 7. Геология. География, 2002, , 4, 75-85
dc.identifier.issn1029-7456
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/29162
dc.titleSEDIMENTS OF LAKES IN LENINGRAD REGION AS THE CHRONICLE OF BALTIC LEVEL FLUCTUATION
dc.typeСтатья

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