PERMIAN-TRIASSIC BOUNDARY DEPOSITS IN FRAMING STRUCTURES OF THE EAST SIBERIAN PLATFORM

dc.contributor.author	Sadovnikov G.N.
dc.contributor.author	Orlova E.F.
dc.date.accessioned	2020-12-24T03:38:06Z
dc.date.available	2020-12-24T03:38:06Z
dc.date.issued	1997
dc.identifier	https://elibrary.ru/item.asp?id=13268095
dc.identifier.citation	Stratigraphy and Geological Correlation, 1997, , 1, 12-18
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/21223
dc.description.abstract	The first description of the stratotype of the Ust'-Kel'ter Horizon with its specific characteristics is given. A new stratigraphic unit, the Marininskii Horizon, is distinguished and substantiated, and its stratotype is described. The Marininskii and Ust'-Kel'ter horizons continue upward the succession of continental Permian-Triassic stratigraphic units of Siberia. Their recognition allows us to address the problem of age and correlation of the Permian-Triassic boundary deposits in the northern Siberian platform and its framing structures.
dc.subject	Permian	en
dc.subject	Triassic	en
dc.title	PERMIAN-TRIASSIC BOUNDARY DEPOSITS IN FRAMING STRUCTURES OF THE EAST SIBERIAN PLATFORM
dc.type	Статья
dc.subject.age	Paleozoic::Permian	en
dc.subject.age	Мезозой::Триасовая	ru
dc.subject.age	Палеозой::Пермская	ru
dc.subject.age	Mesozoic::Triassic	en

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