THE MEZINO-LAPSHINOVKA REFERENCE SECTION OF THE UPPER CRETACEOUS AND PROBLEMS OF SANTONIAN-CAMPANIAN BOUNDARY IN SARATOV AREA NEAR THE VOLGA RIVER

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dc.contributor.author Olfer'ev A.G.
dc.contributor.author Alekseev A.S.
dc.contributor.author Beniamovskii V.N.
dc.contributor.author Shcherbinina E.A.
dc.contributor.author Vishnevskaya V.S.
dc.contributor.author Ivanov A.V.
dc.contributor.author Sel'tser V.B.
dc.contributor.author Kharitonov V.M.
dc.contributor.author Pervushov E.M.
dc.date.accessioned 2022-03-24T08:31:15Z
dc.date.available 2022-03-24T08:31:15Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=13453137
dc.identifier.citation Stratigraphy and Geological Correlation, 2004, 12, 6, 603-636
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/36657
dc.description.abstract Results of multidisciplinary study in the Upper Cretaceous reference section and characteristics of the Mezino-Lapshinovka Formation stratotype are presented. The late Santonian age of the formation is substantiated based on the analyzed organic remains. The formation is considered to be a stratigraphic equivalent of the Pteria Beds, the age of which was animatedly discussed during over a century. The age of the Mozhzhevelovyi Ovrag Formation that underlies the Mezino-Lapshinovka Formation and yields foraminifers, radiolarians, and calcareous nannoplankton is also discussed. The ammonite assemblage of the lower upper Campanian first discovered in the basal part of the Ardym Formation of the Volga region is characterized.
dc.subject Campanian
dc.subject Santonian
dc.title THE MEZINO-LAPSHINOVKA REFERENCE SECTION OF THE UPPER CRETACEOUS AND PROBLEMS OF SANTONIAN-CAMPANIAN BOUNDARY IN SARATOV AREA NEAR THE VOLGA RIVER
dc.type Статья
dc.subject.age Mesozoic::Cretaceous::Upper::Campanian
dc.subject.age Mesozoic::Cretaceous::Upper::Santonian
dc.subject.age Мезозой::Меловая::Верхний::Сантонский ru
dc.subject.age Мезозой::Меловая::Верхний::Кампанский ru


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