FLUCTUATIONS OF DEVONIAN SEA LEVEL IN THE MOSCOW BASIN

dc.contributor.author	Rodionova G.D.
dc.contributor.author	Umnova V.T.
dc.date.accessioned	2020-12-24T07:23:01Z
dc.date.available	2020-12-24T07:23:01Z
dc.date.issued	1997
dc.identifier	https://elibrary.ru/item.asp?id=13272392
dc.identifier.citation	Stratigraphy and Geological Correlation, 1997, , 2, 118-125
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/21308
dc.description.abstract	A representative data base is used to elucidate the history of Devonian sedimentation in the Moscow basin of the Russian platform. The Devonian section includes six rhythms of sedimentation and seven principal geological boundaries, whose levels are identified on the basis of miospore, brachiopod, and conodont zonation. The inferred curve of secular variations in the basin salinity is plotted versus palynological and standard conodont zones and correlated with the main stages of sedimentation and sporgenous plant evolution. There is also a positive correlation between the salinity variation in the Devonian Moscow basin and global eustatic events detected by Johnson and Sandberg.
dc.subject	Devonian	en
dc.title	FLUCTUATIONS OF DEVONIAN SEA LEVEL IN THE MOSCOW BASIN
dc.type	Статья
dc.subject.age	Paleozoic::Devonian	en
dc.subject.age	Палеозой::Девонская	ru

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