TO THE LOWER DEVONIAN BIOSTRATIGRAPHY IN THE RUSSIAN FAR EAST AND MONGOLIA

dc.contributor.author	Alekseeva R.E.
dc.contributor.author	Shishkina G.R.
dc.date.accessioned	2021-06-10T12:09:36Z
dc.date.available	2021-06-10T12:09:36Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=13408644
dc.identifier.citation	Stratigraphy and Geological Correlation, 2002, 10, 6, 565-574
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/28983
dc.description.abstract	Recent data on the Lower Devonian biostratigraphy in the studied regions are generalized. The described terrigenous and carbonate reference sections yield sharply different faunal assemblages. Carbonate sections of Mongolia, which yield conodont index species of the standard zonation, are correlated with the general stratigraphic scheme of the Devonian. Terrigenous sequences of the Far East and Mongolia are subdivided into regional brachiopod zones of identical stratigraphic succession. The regional zones are calibrated versus the standard Devonian zonations based on their correlation with the carbonate sections.
dc.subject	Devonian
dc.title	TO THE LOWER DEVONIAN BIOSTRATIGRAPHY IN THE RUSSIAN FAR EAST AND MONGOLIA
dc.type	Статья
dc.subject.age	Paleozoic::Devonian
dc.subject.age	Палеозой::Девонская	ru

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