ORIGIN OF PLEISTOCENE-HOLOCENE ASHES OF THE RUSSIAN NORTHEAST BASED ON TRACE AND RARE EARTH ELEMENT DATA

Sakhno V.G.; Bazanova L.I.; Melekestsev I.V.; Glushkova O.Yu.; Ponomareva V.V.; Surnin A.A.; Olaf J.

dc.contributor.author	Sakhno V.G.
dc.contributor.author	Bazanova L.I.
dc.contributor.author	Melekestsev I.V.
dc.contributor.author	Glushkova O.Yu.
dc.contributor.author	Ponomareva V.V.
dc.contributor.author	Surnin A.A.
dc.contributor.author	Olaf J.
dc.date.accessioned	2024-11-09T08:38:12Z
dc.date.available	2024-11-09T08:38:12Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13526364
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 9, 1351-1356
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46414
dc.description.abstract	Within the framework of a Joint Russian–German project, sediments of Lake El’gygytgyn were studied to determine paleoclimatic changes in the Pleistocene and Holocene. A 13-m-thick upper section of the bottom sediments was recovered. The thickness of bottom sediments in the lake caldera is 350–400 m. Ashes found in the borehole at depths of 2–3 and 7–8m were referred to the upper Pleistocene based on the composition of diatomaceous algae. The upper and lower horizons correspond to intervals of 40–60 and 160–180 ka ago.
dc.subject	Holocene
dc.subject	Pleistocene
dc.title	ORIGIN OF PLEISTOCENE-HOLOCENE ASHES OF THE RUSSIAN NORTHEAST BASED ON TRACE AND RARE EARTH ELEMENT DATA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06090042
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен
dc.subject.age	Cenozoic::Quaternary::Pleistocene
dc.subject.age	Кайнозой::Четвертичная::Плейстоцен