CHARACTER OF SEDIMENTATION IN LAKE BAIKAL IN THE HOLOCENE

Простая страница элемента
dc.contributor.authorVologina E.G.
dc.contributor.authorSturm M.
dc.contributor.authorVorob'eva S.S.
dc.contributor.authorGranina L.Z.
dc.contributor.authorToshchakov S.Yu.
dc.date.accessioned2021-12-03T04:37:49Z
dc.date.available2021-12-03T04:37:49Z
dc.date.issued2003
dc.description.abstractThe bottom sediments of Lake Baikal were studied, with the emphasis placed upon the conditions of sedimentation in the Holocene and material composition of sediments. On the basis of study of spatial distribution of sediments in all parts of the lake, six characteristic zones of sedimentation have been recognized. Lithological types of sections of the modern bottom deposits of Baikal are described in detail. Much attention is given to the description of turbidite sedimentation as one of the main mechanisms of formation of bottom sediments in the Holocene. The features that distinguish turbidites from sediments accumulated under calm conditions are shown. It has been established that buried relics of oxidized Fe-Mn-formations occur not only in the northern basin of the lake but also in the southern basin.
dc.identifierhttps://www.elibrary.ru/item.asp?id=14997440
dc.identifier.citationGeologiya i geofizika, 2003, 44, 5, 407-421
dc.identifier.issn0016-7886
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/32675
dc.subjectBottom sediments
dc.subjectsedimentation conditions
dc.subjectturbidites
dc.subjectfrustules
dc.subjectoxidized layers
dc.subjectBaikal
dc.subject.ageCenozoic::Quaternary::Holocene
dc.subject.ageКайнозой::Четвертичная::Голоценru
dc.titleCHARACTER OF SEDIMENTATION IN LAKE BAIKAL IN THE HOLOCENE
dc.typeСтатья

Файлы

Коллекции

ELibrary