LATE PRECAMBRIAN GEOCHRONOLOGY OF THE EUROPEAN U.S.S.R

dc.contributor.author	Krasnobaev A.A.
dc.contributor.author	Keller B.M.
dc.date.accessioned	2020-02-13T07:43:59Z
dc.date.available	2020-02-13T07:43:59Z
dc.date.issued	1983
dc.identifier	https://elibrary.ru/item.asp?id=30930312
dc.identifier.citation	GEOLOGICAL MAGAZINE, 1983, 120, 4, 381-389
dc.identifier.issn	0016-7568
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/15749
dc.description.abstract	The available data on radiometric dating of Riphean and Vendian deposits in the European part of the U.S.S.R. enabled us to establish the age of geochronological boundaries. The Riphean lower boundary was adopted as 1650 ± 50 Ma, the Vendian lower boundary as 650 ± 10 Ma, and the Cambrian lower boundary as 590 ± 10 Ma, making the total length of the Riphean about 1000 Ma and that of the Vendian about 60 Ma. This paper suggests a draft of the geochronological scale of the Late Precambrian.
dc.subject	Precambrian	en
dc.title	LATE PRECAMBRIAN GEOCHRONOLOGY OF THE EUROPEAN U.S.S.R
dc.type	Статья
dc.subject.age	Докембрий	ru
dc.subject.age	Precambrian	en

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