LATE DEVONIAN MAGMATISM IN THE PRIPYAT PALAEORIFT: A GEODYNAMIC MODEL

dc.contributor.author	Aizberg R.Y.
dc.contributor.author	Starchik T.A.
dc.contributor.author	Beskopylny V.N.
dc.contributor.author	Tsekoyeva T.K.
dc.date.accessioned	2021-03-02T07:46:16Z
dc.date.available	2021-03-02T07:46:16Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=27777637
dc.identifier.citation	Geological Quarterly, 2001, 45, 4, 349-358
dc.identifier.issn	1641-7291
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/26050
dc.description.abstract	Late Devonian magmatism in the Pripyat Trough, Belarus was associated with the development of the intraplate Pripyat-Donets Palaeorift. Magmatic rocks belong to an alkali-ultrabasic-alkali-basaltoid suite. These are represented by explosive, effusive, subvolcanic and volcanic facies. The magmatic activity and rock composition changes from the periphery to the axial part of the Pripyat Trough, corresponding to the general trend of destructive processes in the rifting zone. Geodynamically, the Pripyat alkali-ultrabasic rocks represent a series of magmatic suites of the Pripyat-Donets palaeovolcanic region coinciding with a zone of disappearance of Late Devonian divergence processes in the south-west of the East European Craton.
dc.subject	Devonian
dc.subject	magmatism
dc.subject	Pripyat Trough
dc.subject	geodynamic model
dc.title	LATE DEVONIAN MAGMATISM IN THE PRIPYAT PALAEORIFT: A GEODYNAMIC MODEL
dc.type	Статья
dc.subject.age	Paleozoic::Devonian	en
dc.subject.age	Палеозой::Девонская	ru

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