A 14C-DATING AND OXYGEN-ISOTOPE DIAGRAM OF A HOLOCENE-REFORMED ICE WEDGE ON THE CHARA RIVER (TRANSBAIKAL REGION)

dc.contributor.author	Vasil'chuk Yu.K.
dc.contributor.author	Zaitsev V.N.
dc.contributor.author	Vasil'chuk A.C.
dc.date.accessioned	2024-11-02T11:07:48Z
dc.date.available	2024-11-02T11:07:48Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13522506
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 2, 265-270
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46349
dc.description.abstract	The purpose of our work is to refine the age of the Holocene polygonal ice wedge complex in Terrace 1 of the Chara River, plot an isotope diagram, which allows one to reconstruct winter temperatures of the period of ice-wedge formation, and prove the possibility of active formation of ice wedges in the Holocene Optimum in even the southern regions of Siberia.
dc.subject	Chara river
dc.subject	Holocene
dc.title	A 14C-DATING AND OXYGEN-ISOTOPE DIAGRAM OF A HOLOCENE-REFORMED ICE WEDGE ON THE CHARA RIVER (TRANSBAIKAL REGION)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06020267
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен

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