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

dc.contributor.author	Oshurkova M.V.
dc.date.accessioned	2021-01-11T07:57:17Z
dc.date.available	2021-01-11T07:57:17Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=13316226
dc.identifier.citation	Stratigraphy and Geological Correlation, 1999, , 6, 594-605
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22663
dc.description.abstract	Spore-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.subject	Paleozoic	en
dc.title	AGE OF UPPER PALEOZOIC DEPOSITS IN EASTERN MARGIN OF THE TUNGUSKA SYNECLISE: IMPLICATIONS FROM PALYNOLOGICAL DATA
dc.type	Статья
dc.subject.age	Paleozoic	en
dc.subject.age	Палеозой	ru

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