GIVETIAN DEEPWATER SEDIMENTS IN THE WESTERN SLOPE OF THE SUBPOLAR URALS

dc.contributor.author	Tsyganko V.S.
dc.date.accessioned	2024-10-27T02:28:37Z
dc.date.available	2024-10-27T02:28:37Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13514683
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 8, 1218-1221
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46222
dc.description.abstract	In 1996, the author of the present paper first described and sampled macro- and microfossils in the Givetian section of deepwater sediments in the Subpolar Urals. The section outcrops in exposure 86 on the left bank of the Bol’shaya Nadota River near the western foothill of Mt. Olysya. The Givetian sediments are confined to the tectonically complicated area sandwiched between the Elets and Lemva facies that are characterized by wide development of reverse faults and thrusts.
dc.subject	Givetian
dc.title	GIVETIAN DEEPWATER SEDIMENTS IN THE WESTERN SLOPE OF THE SUBPOLAR URALS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06080125
dc.subject.age	Paleozoic::Devonian::Middle::Givetian
dc.subject.age	Палеозой::Девонская::Средний::Живетский

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