THE UPPER CRETACEOUS RADIOLARIANS, FORAMINIFERS, AND STRATIGRAPHY OF THE SOUTHEASTERN RUSSIAN PLATE, THE RIGHT-BANK VOLGA REGION NEAR VOLGOGRAD

dc.contributor.author	Bragina L.G.
dc.contributor.author	Ben'yamovskii V.N.
dc.contributor.author	Zastrozhnov A.S.
dc.date.accessioned	2021-01-11T07:57:18Z
dc.date.available	2021-01-11T07:57:18Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=13319979
dc.identifier.citation	Stratigraphy and Geological Correlation, 1999, , 5, 492-500
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22676
dc.description.abstract	Paleontological study of the Upper Cretaceous sediments from wells 502 and 28 in the Volgograd region revealed distinct radiolarian and foraminiferal assemblages. Two stratigraphic levels, Coniacian-Santonian and upper Campanian, are recognized on the basis of radiolarians. Foraminiferal and radiolarian zones of the same section are first correlated to each other in the Volgograd region, and coeval assemblages from the Moscow syneclise and Volgograd region are compared.
dc.subject	Cretaceous	en
dc.title	THE UPPER CRETACEOUS RADIOLARIANS, FORAMINIFERS, AND STRATIGRAPHY OF THE SOUTHEASTERN RUSSIAN PLATE, THE RIGHT-BANK VOLGA REGION NEAR VOLGOGRAD
dc.type	Статья
dc.subject.age	Мезозой::Меловая	ru
dc.subject.age	Mesozoic::Cretaceous	en

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