AGE OF UPPER PALEOZOIC DEPOSITS IN EASTERN MARGIN OF THE TUNGUSKA SYNECLISE: IMPLICATIONS FROM PALYNOLOGICAL DATA

dc.contributor.authorOshurkova M.V.
dc.date.accessioned2021-01-11T07:57:17Z
dc.date.available2021-01-11T07:57:17Z
dc.date.issued1999
dc.description.abstractSpore-and-pollen analysis of the Lapcha and Botuoba formations revealed four successive palynological assemblages. On the basis of the relative abundance of taxa and of the taxonomic composition of the assemblages, the Lapcha and Botuoba formations are attributed to the Upper Carboniferous and Lower Permian, respectively. The revealed palynofloras are correlated with the Upper Carboniferous and Lower Permian palynological zonation in the Kuznetsk coal basin.
dc.identifierhttps://elibrary.ru/item.asp?id=13316226
dc.identifier.citationStratigraphy and Geological Correlation, 1999, , 6, 594-605
dc.identifier.issn0869-5938
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/22663
dc.subjectPaleozoicen
dc.subject.agePaleozoicen
dc.titleAGE OF UPPER PALEOZOIC DEPOSITS IN EASTERN MARGIN OF THE TUNGUSKA SYNECLISE: IMPLICATIONS FROM PALYNOLOGICAL DATA
dc.typeСтатья

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