STRATOTYPE OF THE FAMENNIAN VOLGOGRAD HORIZON IN THE RUSSIAN PLATFORM

dc.contributor.author	Mantsurova V.N.
dc.contributor.author	Tsygankova V.A.
dc.contributor.author	Smirnov V.E.
dc.date.accessioned	2021-11-23T00:58:45Z
dc.date.available	2021-11-23T00:58:45Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13441163
dc.identifier.citation	Stratigraphy and Geological Correlation, 2003, 11, 1, 1-17
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/32399
dc.description.abstract	Stratotype sections of the lower Famennian Volgograd Horizon, which are located in the Umet-Linevo paleodepression, the northeastern Volgograd area, are described. Lithological-geophysical characteristics of borehole sequences, correlation and paleogeological profile of the Frasnian-Famennian boundary beds of the Volgograd region are presented. Stratigraphic ranges of characteristic spore species of the Volgograd Horizon are defined. Palynological data elucidate correlation of the Frasnian-Famennian boundary beds in the Russian platform and the Urals. Distribution areas of the Volgograd Horizon deposits in the Russian platform are outlined.
dc.subject	Famennian
dc.title	STRATOTYPE OF THE FAMENNIAN VOLGOGRAD HORIZON IN THE RUSSIAN PLATFORM
dc.type	Статья
dc.subject.age	Paleozoic::Devonian::Upper::Famennian
dc.subject.age	Палеозой::Девонская::Верхний::Фаменский	ru

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