NEW DATA ON CRETACEOUS VOLCANIC ARCS OF THE NORTHEASTERN ASIAN MARGIN

dc.contributor.author	Chekhovich V.D.
dc.contributor.author	Sukhov A.N.
dc.contributor.author	Filatova N.I.
dc.contributor.author	Vishnevskaya V.S.
dc.contributor.author	Basov I.A.
dc.date.accessioned	2024-10-23T07:16:02Z
dc.date.available	2024-10-23T07:16:02Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13512598
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 381-384
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46165
dc.description.abstract	Various models of evolution of the northwestern Pacific folded fringing during the Cretaceous were proposed in recent decades. Almost all of them consider the Late Cretaceous geodynamic evolution of the region as spatiotemporal succession of suprasubduction structures near the eastern margin of Asia that resulted from the subduction of the oceanic crust of the spreading Pacific.
dc.subject	Cretaceous
dc.title	NEW DATA ON CRETACEOUS VOLCANIC ARCS OF THE NORTHEASTERN ASIAN MARGIN
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06030081
dc.subject.age	Mesozoic::Cretaceous
dc.subject.age	Мезозой::Меловая

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