THE QUASIPLATFORM SEDIMENTS OF THE EAST EUROPEAN PLATFORM

dc.contributor.author	Nagornyi M.A.
dc.contributor.author	Nikolaev V.G.
dc.date.accessioned	2023-01-20T06:52:43Z
dc.date.available	2023-01-20T06:52:43Z
dc.date.issued	2005
dc.identifier	https://www.elibrary.ru/item.asp?id=21531078
dc.identifier.citation	Russian Journal of Earth Sciences, 2005, 7, 5, ES5001
dc.identifier.issn	1681-1208
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/41485
dc.description.abstract	The subject of this paper is the structure of the peculiar rock complex of the East European Platform, composed of the rocks dated 1750 Ma to 1300 Ma and known as a quasiplatform rock cover. The western and eastern segments of the platform differ greatly in terms of the lithology and thickness of their rocks. The quasiplatform sediments have been subdivided into the lower and upper subtypes. The lower subtype is developed mainly in the west, and the formation of the structural features composed of these rocks is supposed to have been associated with the process that operated in the Ural Mountains.
dc.subject	SEDIMENTARY COVER
dc.subject	BASEMENT
dc.subject	MAGMATISM
dc.subject	TECTONICS
dc.subject	STRUCTURAL FEATURE
dc.title	THE QUASIPLATFORM SEDIMENTS OF THE EAST EUROPEAN PLATFORM
dc.type	Статья

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