THE ERDENETUIN-OBO PORPHYRY CU-MO MAGMA CHAMBER (MONGOLIA) AS A REFLECTION OF THE PERMIAN-TRIASSIC SUPERPLUME

dc.contributor.author	Berzina A.P.
dc.contributor.author	Dobretsov N.L.
dc.contributor.author	Sotnikov V.I.
dc.contributor.author	Ponomarchuk V.A.
dc.date.accessioned	2022-07-18T00:49:00Z
dc.date.available	2022-07-18T00:49:00Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13448665
dc.identifier.citation	Doklady Earth Sciences, 2004, 399, 9, 1311-1314
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38191
dc.description.abstract	Large-scale Permian-Triassic magmatism of northern and central Asia has been recently proved to be of plume origin. Based on these concepts, the present paper considers a possible relationship between the evolution of the Erdenetuin-Obo porphyry Cu-Mo magma chamber and the Siberian superplume.
dc.subject	Triassic
dc.subject	Permian
dc.title	THE ERDENETUIN-OBO PORPHYRY CU-MO MAGMA CHAMBER (MONGOLIA) AS A REFLECTION OF THE PERMIAN-TRIASSIC SUPERPLUME
dc.type	Статья
dc.subject.age	Mesozoic::Triassic
dc.subject.age	Paleozoic::Permian
dc.subject.age	Мезозой::Триасовая	ru
dc.subject.age	Палеозой::Пермская	ru

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