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

dc.contributor.authorTrofimov A.G.
dc.contributor.authorPopova S.M.
dc.contributor.authorKulagina N.V.
dc.contributor.authorShibanova I.V.
dc.contributor.authorUfimtsev G.F.
dc.contributor.authorMalaeva E.M.
dc.date.accessioned2021-01-11T07:43:32Z
dc.date.available2021-01-11T07:43:32Z
dc.date.issued1999
dc.description.abstractThe 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.identifierhttps://elibrary.ru/item.asp?id=13307555
dc.identifier.citationStratigraphy and Geological Correlation, 1999, , 4, 396-409
dc.identifier.issn0869-5938
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/22604
dc.subjectPleistoceneen
dc.subject.ageCenozoic::Quaternary::Pleistoceneen
dc.titleTHE MANZURKA ALLUVIUM OF THE BAIKAL REGION: PALYNOLOGY, STRATIGRAPHY, ACCUMULATION STAGES
dc.typeСтатья

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