THE MANZURKA ALLUVIUM OF THE BAIKAL REGION: PALYNOLOGY, STRATIGRAPHY, ACCUMULATION STAGES

dc.contributor.author	Trofimov A.G.
dc.contributor.author	Popova S.M.
dc.contributor.author	Kulagina N.V.
dc.contributor.author	Shibanova I.V.
dc.contributor.author	Ufimtsev G.F.
dc.contributor.author	Malaeva E.M.
dc.date.accessioned	2021-01-11T07:43:32Z
dc.date.available	2021-01-11T07:43:32Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=13307555
dc.identifier.citation	Stratigraphy and Geological Correlation, 1999, , 4, 396-409
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22604
dc.description.abstract	The Manzurka Alluvium fills ancient valleys of the Baikal-Lena watershed. Previously, the sequence of the constrative alluvium was considered to be of the Eopleistocene age. Latest investigations showed that despite the lithological uniformity, the sequence includes several stratigraphic units ranging in age from the Pliocene to late Pleistocene. The Manzurka Alluvium is a typical example of the polychronous sedimentary complex of the intracontinental frost-free areas that were formed under gradual environmental changes.
dc.subject	Pleistocene	en
dc.subject	Pliocene	en
dc.title	THE MANZURKA ALLUVIUM OF THE BAIKAL REGION: PALYNOLOGY, STRATIGRAPHY, ACCUMULATION STAGES
dc.type	Статья
dc.subject.age	Cenozoic::Neogene::Pliocene	en
dc.subject.age	Cenozoic::Quaternary::Pleistocene	en
dc.subject.age	Кайнозой::Четвертичная::Плейстоцен	ru
dc.subject.age	Кайнозой::Неоген::Плиоцен	ru

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