INDICATION OF CLIMATE HUMIDITY IN CENTRAL ASIA: EVIDENCE FROM THE GRANULOMETRIC RECORD OF BOTTOM SEDIMENTS IN LAKE KHUBSUGUL (MONGOLIA) FOR THE LAST 450 KA

dc.contributor.author	Fedotov A.P.
dc.contributor.author	Ziborova G.A.
dc.contributor.author	Khabuev A.V.
dc.contributor.author	Otinova E.L.
dc.contributor.author	Kugakolov S.A.
dc.contributor.author	Rodyakin S.V.
dc.date.accessioned	2024-10-19T07:54:48Z
dc.date.available	2024-10-19T07:54:48Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13505443
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 686-688
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46071
dc.description.abstract	One of the methods used for recording environmental variations in the past is the reconstruction of sedimentation facies conditions based on distribution of the terrigenous component and mineral associations. This kind of work was previously carried out successfully to study bottom sediments in Lake Baikal. The present paper is devoted to the results of grain size analysis of a part of the drill core (KDP-01) taken from bottom sediments accumulated in Lake Khubsugul over the last 450 ka.
dc.title	INDICATION OF CLIMATE HUMIDITY IN CENTRAL ASIA: EVIDENCE FROM THE GRANULOMETRIC RECORD OF BOTTOM SEDIMENTS IN LAKE KHUBSUGUL (MONGOLIA) FOR THE LAST 450 KA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040404

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