THE LOWER AND UPPER BOUNDARIES OF THE LOWER CAMBRIAN ON THE SIBERIAN PLATFORM

dc.contributor.author	Luchinina V.A.
dc.contributor.author	Sipin D.P.
dc.contributor.author	Korovnikov I.V.
dc.contributor.author	Fedoseev A.V.
dc.date.accessioned	2021-01-31T12:47:15Z
dc.date.available	2021-01-31T12:47:15Z
dc.date.issued	2000
dc.identifier	https://elibrary.ru/item.asp?id=14995331
dc.identifier.citation	Geologiya i geofizika, 2000, 41, 9, 1233-1243
dc.identifier.issn	0016-7886
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/24124
dc.description.abstract	The Siberian Platform is well characterized paleontologically, sedimentologically, and geochemically. This makes it a suitable region for choosing the stratotypes of the lower and upper boundaries of the Lower Cambrian. However, the correlation of these boundaries both within the region and outside it is still disputable. The article considers one of the possible reasons for this disagreement, which rests upon the fact that the boundaries are drawn in most sections by organic fossils among bioherms and are correlated with boundaries in facies-different sections.
dc.subject	Cambrian	en
dc.title	THE LOWER AND UPPER BOUNDARIES OF THE LOWER CAMBRIAN ON THE SIBERIAN PLATFORM
dc.type	Статья
dc.subject.age	Paleozoic::Cambrian	en
dc.subject.age	Палеозой::Кембрийская	ru

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