ON THE MARINE GENESIS AND PONTIAN AGE OF DEPOSITS FROM THE LYUBIMOVKA REFERENCE SECTION IN THE CRIMEA

dc.contributor.author	Pevzner M.A.
dc.contributor.author	Vangengeim E.A.
dc.contributor.author	Sadchikova T.A.
dc.contributor.author	Semenenko V.N.
dc.contributor.author	Kovalenko V.A.
dc.contributor.author	Lyul'eva S.A.
dc.date.accessioned	2022-03-24T08:31:18Z
dc.date.available	2022-03-24T08:31:18Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13457131
dc.identifier.citation	Stratigraphy and Geological Correlation, 2004, 12, 5, 523-533
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/36674
dc.description.abstract	A comprehensive study of the Lyubimovka section (western coast of the Crimea Peninsula, in the vicinity of Sevastopol) is carried out. The section is adopted as stratotype of six and as hypostratotype of three lower and basal middle Pliocene horizons in the stratigraphic scheme of continental deposits in the Ukraine. The late Miocene (early Pontian) age and the lagoonal-marine genesis of most deposits, which represent a typical molasse at the foot of the Crimean Mountains, is substantiated based on paleomagnetic, lithologic, biostratigraphic, and geological data. The results obtained imply that horizons of the lower and basal middle Pliocene continental deposits, which are distinguished in the Ukrainian stratigraphic scheme, are invalid.
dc.title	ON THE MARINE GENESIS AND PONTIAN AGE OF DEPOSITS FROM THE LYUBIMOVKA REFERENCE SECTION IN THE CRIMEA
dc.type	Статья

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