MAGMATISM OF THE KAROO-MAUD SUPERPLUME IN THE SCHIRMACHER OASIS, EAST ANTARCTICA

dc.contributor.author	Belyatskii B.V.
dc.contributor.author	Sushchevskaya N.M.
dc.contributor.author	Leichenkov G.L.
dc.contributor.author	Mikhal'skii E.M.
dc.contributor.author	Laiba A.A.
dc.date.accessioned	2024-10-19T07:54:43Z
dc.date.available	2024-10-19T07:54:43Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13503738
dc.identifier.citation	Doklady Earth Sciences, 2006, 406, 1, 128-131
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46047
dc.description.abstract	The origination of large plateau basalt provinces in the Earth’s geological history has traditionally been referred to the deep thermal convection caused by plume geodynamics. The emplacement of a large plume into the lithosphere of central Gondwana in the Early–Middle Jurassic (180–173 Ma ago) resulted in the formation of a vast igneous province 2000 km across [2, 3] and probably predetermined the subsequent breakup of the supercontinent and opening of the Southern Ocean.
dc.title	MAGMATISM OF THE KAROO-MAUD SUPERPLUME IN THE SCHIRMACHER OASIS, EAST ANTARCTICA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06010314
dc.subject.age	Мезозой::Юрская

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