Crustal origin for coupled ultra-depleted and plagioclase signatures in MORB olivine-josted melt inclusions: evidence from the Siqueiros Transform Fault, East Pacific Rise

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dc.contributor.authorDanyushevsky, Leonid V.
dc.contributor.authorPerfit, Michael
dc.contributor.authorEggins, Stephen
dc.contributor.authorFalloon, Trevor
dc.date.accessioned2015-12-13T22:35:15Z
dc.date.available2015-12-13T22:35:15Z
dc.date.issued2003
dc.date.updated2015-12-11T09:26:54Z
dc.description.abstractGeochemical data from melt inclusions in olivine phenocrysts in a picritic basalt from the Siqueiros Transform Fault on the northern East Pacific Rise provide insights into the petrogenesis of mid-ocean ridge basalts (MORB). The fresh lava contains ∼ 10
dc.identifier.issn0010-7999
dc.identifier.urihttp://hdl.handle.net/1885/76506
dc.publisherSpringer
dc.sourceContributions to Mineralogy and Petrology
dc.subjectKeywords: crustal contamination; magma; melt inclusion; mid-ocean ridge basalt; olivine; petrogenesis; phenocryst; plagioclase; Pacific Ocean
dc.titleCrustal origin for coupled ultra-depleted and plagioclase signatures in MORB olivine-josted melt inclusions: evidence from the Siqueiros Transform Fault, East Pacific Rise
dc.typeJournal article
local.bibliographicCitation.lastpage637
local.bibliographicCitation.startpage619
local.contributor.affiliationDanyushevsky, Leonid V., University of Tasmania
local.contributor.affiliationPerfit, Michael, University of Florida
local.contributor.affiliationEggins, Stephen, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationFalloon, Trevor, University of Tasmania
local.contributor.authoruidEggins, Stephen, u9109238
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationMigratedxPub5319
local.identifier.citationvolume144
local.identifier.scopusID2-s2.0-0037330821
local.type.statusPublished Version

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