VENDIAN STRATA IN THEIR TYPE AREA

dc.contributor.author	Yakobsan K.E.
dc.date.accessioned	2020-04-15T06:25:19Z
dc.date.available	2020-04-15T06:25:19Z
dc.date.issued	1987
dc.identifier	https://elibrary.ru/item.asp?id=30978669
dc.identifier.citation	GEOLOGICAL MAGAZINE, 1987, 124, 1, 73-78
dc.identifier.issn	0016-7568
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16760
dc.description.abstract	In the Eastern European region Vendian strata are divisible into two complexes: the lower one, only locally developed, is composed of alternating tillites, volcanics, sandy–clay rocks and dolomites; and the upper one, of alternating sandstone, siltstone, and mudstone strata with medusoid fauna, resting transgressively on the lower complex and older rocks. The lower complex is associated with sheet glaciation; the upper one was formed in a post-glacial isostatic basin. The name ‘Vendian’ should be applied only to the upper complex; the lower one should be called ‘Waranger’.
dc.subject	Vendian	en
dc.title	VENDIAN STRATA IN THEIR TYPE AREA
dc.type	Статья
dc.subject.age	Precambrian::Proterozoic::Neoproterozoic::Vendian	en
dc.subject.age	Докембрий::Протерозой::Неопротерозойская::Вендский	ru

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