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

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dc.contributor.authorSakhno V.G.
dc.contributor.authorBazanova L.I.
dc.contributor.authorMelekestsev I.V.
dc.contributor.authorGlushkova O.Yu.
dc.contributor.authorPonomareva V.V.
dc.contributor.authorSurnin A.A.
dc.contributor.authorOlaf J.
dc.date.accessioned2024-11-09T08:38:12Z
dc.date.available2024-11-09T08:38:12Z
dc.date.issued2006
dc.description.abstractWithin 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.identifierhttps://www.elibrary.ru/item.asp?id=13526364
dc.identifier.citationDoklady Earth Sciences, 2006, 411, 9, 1351-1356
dc.identifier.doi10.1134/S1028334X06090042
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46414
dc.subjectHolocene
dc.subjectPleistocene
dc.subject.ageCenozoic::Quaternary::Holocene
dc.subject.ageКайнозой::Четвертичная::Голоцен
dc.subject.ageCenozoic::Quaternary::Pleistocene
dc.subject.ageКайнозой::Четвертичная::Плейстоцен
dc.titleORIGIN OF PLEISTOCENE-HOLOCENE ASHES OF THE RUSSIAN NORTHEAST BASED ON TRACE AND RARE EARTH ELEMENT DATA
dc.typeСтатья

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