ON AGE OF NAZIMOVSKAYA AND KHASAN FORMATIONS IN THE PALEOGENE SUCCESSION OF SOUTHWESTERN PRIMOR'E

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dc.contributor.author Pavlyutkin B.I.
dc.contributor.author Petrenko T.I.
dc.contributor.author Nevolina S.I.
dc.contributor.author Kutub-Zade T.K.
dc.date.accessioned 2024-07-20T12:13:54Z
dc.date.available 2024-07-20T12:13:54Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=13519984
dc.identifier.citation Stratigraphy and Geological Correlation, 2006, 14, 4, 444-457
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/44462
dc.description.abstract Materials of previous studies and new original geological and paleobotanic data are used to substantiate synchronism (late Eocene) of the Khasan and Nazimovskaya formations, the key stratigraphic units of the Paleogene in Primor'e. Coal-bearing sediments of the units rest upon early-middle Eocene volcanics (Kraskino rhyolite tuffs, Zaisanovka basaltic andesites) being overlain by the lower Fatash Subformation of the lower Oligocene with flora of the Kraskino type. The Ust'-Davydovskaya Formation of the Rechnoi Peninsula (outskirts of Vladivostok) is the most probable analogue of the Khasan (=Nazimovskaya) Formation. © MAIK "Nauka/Interperiodica" 2006.
dc.subject EOCENE
dc.subject FOSSIL FLORA ASSEMBLAGES
dc.subject OLIGOCENE
dc.subject PRIMOR'E REGION
dc.subject STRATIGRAPHY
dc.title ON AGE OF NAZIMOVSKAYA AND KHASAN FORMATIONS IN THE PALEOGENE SUCCESSION OF SOUTHWESTERN PRIMOR'E
dc.type Статья
dc.identifier.doi 10.1134/S0869593806040071
dc.subject.age Кайнозой::Палеоген::Эоцен
dc.subject.age Cenozoic::Paleogene::Eocene


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