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Cenozoic Magmatism of the North-Eastern Eurasian Margin: The Role of Lithosphere Versus Asthenosphere

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dc.contributor.authorOkamura, Satoshi
dc.contributor.authorArculus, Richard
dc.contributor.authorMartynov, Yuri
dc.date.accessioned2015-12-13T22:54:04Z
dc.date.issued2005
dc.date.updated2015-12-11T11:01:33Z
dc.description.abstractSikhote-Alin and Sakhalin are located in the Russian Far East-flank of the northernmost part of the Sea of Japan. Magmatism in this region preceded, was concurrent with, and continued after the extension and sea-floor spreading (25-18 Ma) that formed the
dc.identifier.issn0022-3530
dc.identifier.urihttp://hdl.handle.net/1885/82076
dc.publisherOxford University Press
dc.sourceJournal of Petrology
dc.subjectKeywords: asthenosphere; Cenozoic; continental margin; igneous geochemistry; lithosphere; magmatism; Eastern Hemisphere; Eurasia; World Asthenosphere; Japan Sea opening; North-eastern Eurasian margin; Sikhote-Alin-Sakhalin; Subcontinental lithosphere
dc.titleCenozoic Magmatism of the North-Eastern Eurasian Margin: The Role of Lithosphere Versus Asthenosphere
dc.typeJournal article
local.bibliographicCitation.issue2
local.bibliographicCitation.lastpage253
local.bibliographicCitation.startpage221
local.contributor.affiliationOkamura, Satoshi, Hokkaido University
local.contributor.affiliationArculus, Richard, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationMartynov, Yuri, Far East Geological Institute
local.contributor.authoruidArculus, Richard, u9401389
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationMigratedxPub10373
local.identifier.citationvolume46
local.identifier.doi10.1093/petrology/egh065
local.identifier.scopusID2-s2.0-13344268976
local.type.statusPublished Version

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