STRATOTYPE OF THE FAMENNIAN VOLGOGRAD HORIZON IN THE RUSSIAN PLATFORM

dc.contributor.authorMantsurova V.N.
dc.contributor.authorTsygankova V.A.
dc.contributor.authorSmirnov V.E.
dc.date.accessioned2021-11-23T00:58:45Z
dc.date.available2021-11-23T00:58:45Z
dc.date.issued2003
dc.description.abstractStratotype 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.identifierhttps://www.elibrary.ru/item.asp?id=13441163
dc.identifier.citationStratigraphy and Geological Correlation, 2003, 11, 1, 1-17
dc.identifier.issn0869-5938
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/32399
dc.subjectFamennian
dc.subject.agePaleozoic::Devonian::Upper::Famennian
dc.subject.ageПалеозой::Девонская::Верхний::Фаменскийru
dc.titleSTRATOTYPE OF THE FAMENNIAN VOLGOGRAD HORIZON IN THE RUSSIAN PLATFORM
dc.typeСтатья

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