THE FAMENNIAN STAGE OF THE SOUTHERN TRANSCAUCASIA

dc.contributor.author	Mamedov A.B.
dc.date.accessioned	2021-06-24T08:05:47Z
dc.date.available	2021-06-24T08:05:47Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=27765536
dc.identifier.citation	Stratigraphy and Geological Correlation, 2002, 10, 1, 57-68
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/29305
dc.description.abstract	The Famennian sediments of the southern Transcaucasia are described. The Noravank and Ertich formations are referred to the lower substage of the Famennian, the Kadrli and Shamamidzor formations, to the middle one, and the Gortun and Arshakiakhbyur formations, to the upper substage. The Devonian-Carboniferous boundary was placed at the base of the Gerankalasy Formation in accord with resolution of the ISC Commission on the Devonian and Carboniferous (Minsk, 1986). All groups of organic remains encountered in the Famennian sediments of the Transcaucasia are analyzed.
dc.subject	Famennian
dc.title	THE FAMENNIAN STAGE OF THE SOUTHERN TRANSCAUCASIA
dc.type	Статья
dc.subject.age	Paleozoic::Devonian::Upper::Famennian
dc.subject.age	Палеозой::Девонская::Верхний::Фаменский	ru

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