LATE PALEOZOIC RADIOLARIANS FROM THE POLYFACIES FORMATIONS OF THE URALIAN FOREDEEP

dc.contributor.author	Chuvashov B.I.
dc.contributor.author	Amon E.O.
dc.contributor.author	Caridroit M.
dc.contributor.author	Proust J.N.
dc.date.accessioned	2021-01-11T07:52:42Z
dc.date.available	2021-01-11T07:52:42Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=13314494
dc.identifier.citation	Stratigraphy and Geological Correlation, 1999, , 1, 35-48
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22643
dc.description.abstract	Stratigraphic and facies distribution of radiolarians within the interval from the Gzhelian Stage of the Upper Carboniferous to the Kungurian Stage of the Lower Permian in the Cis-Ural foredeep are considered. The interrelation between facies and specific features of radiolarian fauna is analyzed. In the longitudinal direction, the area of radiolarian distribution is limited by the foredeep boundaries. Its latitudinal interval coincides with the southern part of the foredeep below 57° N in the north. It is supposed that this latitude bordered the northern thermocline, which served as a paleoclimatic barrier to the dispersal of radiolarian biota northward.
dc.subject	Paleozoic	en
dc.title	LATE PALEOZOIC RADIOLARIANS FROM THE POLYFACIES FORMATIONS OF THE URALIAN FOREDEEP
dc.type	Статья
dc.subject.age	Палеозой	ru
dc.subject.age	Paleozoic	en

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