NEW DATA ON UPPER CRETACEOUS DEPOSITS IN THE NORTH OF MOSCOW REGION

dc.contributor.author	Olfer'ev A.G.
dc.contributor.author	Vishnevskaya V.S.
dc.contributor.author	Kazintsova L.I.
dc.contributor.author	Kopaevich L.F.
dc.contributor.author	Osipova L.M.
dc.date.accessioned	2021-01-28T11:15:50Z
dc.date.available	2021-01-28T11:15:50Z
dc.date.issued	2000
dc.identifier	https://elibrary.ru/item.asp?id=13348279
dc.identifier.citation	Stratigraphy and Geological Correlation, 2000, 8, 3, 270-288
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/23894
dc.description.abstract	New data on Upper Cretaceous deposits exposed to the north of Yaroslavl and to the southwest of Vladimir are considered in order to show that the Khot'kovo Opokas, dated back to the Turonian by some researchers, are actually younger and correspond to the Coniacian-Santonian level. The Turonian age is identified for underlying beds of carbonate clay, because they yielded cephalopods and radiolarians typical of this stage, and also an assemblage of early Turonian foraminifers. The beds are attributed to the Chernevo Formation. Holo- and parastratotype of this formation are described, and its stratigraphic range is outlined. New data suggest connections between the Turonian sea basins of the East European and West Siberian paleobiogeographic provinces.
dc.subject	Cretaceous	en
dc.title	NEW DATA ON UPPER CRETACEOUS DEPOSITS IN THE NORTH OF MOSCOW REGION
dc.type	Статья
dc.subject.age	Мезозой::Меловая	ru
dc.subject.age	Mesozoic::Cretaceous	en

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