PALYNOSTRATIGRAPHY AND DINOCYST ZONATION OF THE MIDDLE EOCENE-LOWER MIOCENE DEPOSITS AT THE BELAYA RIVER (NORTHERN CAUCASUS)

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dc.contributor.author Zaporozhets N.I.
dc.date.accessioned 2021-01-11T07:47:36Z
dc.date.available 2021-01-11T07:47:36Z
dc.date.issued 1999
dc.identifier https://elibrary.ru/item.asp?id=13312743
dc.identifier.citation Stratigraphy and Geological Correlation, 1999, , 2, 161-178
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/22629
dc.description.abstract The detailed biostratigraphic subdivision of a complete and well-exposed Paleogene-Miocene section in the Ciscaucasia is substantiated on the basis of organic-walled phytoplankton, spores, and pollen. The distinguished regional dinocyst zonation for the second half of the Eocene and for the Oligocene and lower Miocene shows the direct interlinking of zonal units and is correlated with the West and Central European zonal scales with the help of indicated microphytofossils.
dc.subject Eocene en
dc.subject Miocene en
dc.title PALYNOSTRATIGRAPHY AND DINOCYST ZONATION OF THE MIDDLE EOCENE-LOWER MIOCENE DEPOSITS AT THE BELAYA RIVER (NORTHERN CAUCASUS)
dc.type Статья
dc.subject.age Cenozoic::Paleogene::Eocene en
dc.subject.age Cenozoic::Neogene::Miocene en
dc.subject.age Кайнозой::Палеоген::Эоцен ru
dc.subject.age Кайнозой::Неоген::Миоцен ru


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