MINERALOGICAL AND CRYSTALLOCHEMICAL INDICATORS OF ENVIRONMENTAL AND CLIMATIC CHANGES IN PLEISTOCENE-HOLOCENE SEDIMENTS OF LAKE KHUBSUGUL (MONGOLIA)
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dc.contributor.author | Solotchina E.P. | |
dc.contributor.author | Stolpovskaya V.N. | |
dc.contributor.author | Prokopenko A.A. | |
dc.contributor.author | Kuz'min M.I. | |
dc.contributor.author | Karabanov E.B. | |
dc.contributor.author | Tkachenko L.L. | |
dc.date.accessioned | 2022-01-15T07:43:08Z | |
dc.date.available | 2022-01-15T07:43:08Z | |
dc.date.issued | 2003 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13438811 | |
dc.identifier.citation | Doklady Earth Sciences, 2003, 391, 6, 866-870 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/34345 | |
dc.description.abstract | This paper presents the first data on mineral composition of Khubsugul sediments studied in core HSG-01-8. The core was taken by the Benthos gravity corer at the flattened floor in the central part of the lake during the cruise of the R/V Dybovsky. The water depth at the sampling site is 222 m; i.e., sedimentation was undisturbed by potential lake level fluctuations. The upper part of the 174-cm-long core is composed of greenish gray diatomaceous ooze grading downward into olive-gray silty clays. These sediment varieties are separated by a transitional light gray laminated layer. The reservoir-corrected 14C age obtained for the transitional layer base is 12.23 ka (14200 calendar years) [3], which corresponds to termination of the Late Pleistocene cooling and beginning of the Belling-Allerod warming. | |
dc.subject | Holocene | |
dc.subject | Pleistocene | |
dc.title | MINERALOGICAL AND CRYSTALLOCHEMICAL INDICATORS OF ENVIRONMENTAL AND CLIMATIC CHANGES IN PLEISTOCENE-HOLOCENE SEDIMENTS OF LAKE KHUBSUGUL (MONGOLIA) | |
dc.type | Статья | |
dc.subject.age | Cenozoic::Quaternary::Holocene | |
dc.subject.age | Кайнозой::Четвертичная::Голоцен | ru |
dc.subject.age | Cenozoic::Quaternary::Pleistocene | |
dc.subject.age | Кайнозой::Четвертичная::Плейстоцен | ru |
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