GENERATION OF THE MAGMAS OF THE DNIEPER-DONETS PALEORIFT VOLCANICS

dc.contributor.author	Lyashkevich Z.M.
dc.contributor.author	Malyuk B.I.
dc.date.accessioned	2020-10-31T02:50:04Z
dc.date.available	2020-10-31T02:50:04Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=27814763
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 5, 116-120
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18248
dc.description.abstract	The Dnieper-Donets paleorift (DDR) of Late Devonian age is a typical province of continental, subalkalic and alkalic volcanism that was similar in its principal parameters to the volcanism of classical Cenozoic rift zones. The general trend of variation in chemical composition of the experimentally obtained residual liquids does not quite agree with that for volcanics of the DDR. Views can be supplemented by modeling the fractional crystallization of melts of several different compositions. For modeling, we selected three presumed parent magma compositions: Olivine melilitite, picritic basalt and meymechite.
dc.subject	Cenozoic	en
dc.subject	Devonian	en
dc.title	GENERATION OF THE MAGMAS OF THE DNIEPER-DONETS PALEORIFT VOLCANICS
dc.type	Статья
dc.subject.age	Cenozoic	en
dc.subject.age	Paleozoic::Devonian	en
dc.subject.age	Палеозой::Девонская	ru
dc.subject.age	Кайнозой	ru

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