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Partial melting of spinel lherzolite in the system CaO�MgO�Al 2 O 3 �SiO 2 �K 2 O at 1.1 GPa

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Liu, Xi; O'Neill, Hugh

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The compositions of multiply saturated partial melts are valuable for the thermodynamic information that the contain, but are difficult to determine experimentally because they exist only over a narrow temperature range at a given pressure. Here we try a

dc.contributor.authorLiu, Xi
dc.contributor.authorO'Neill, Hugh
dc.date.accessioned2015-12-13T22:39:45Z
dc.date.available2015-12-13T22:39:45Z
dc.identifier.issn0022-3530
dc.identifier.urihttp://hdl.handle.net/1885/77913
dc.description.abstractThe compositions of multiply saturated partial melts are valuable for the thermodynamic information that the contain, but are difficult to determine experimentally because they exist only over a narrow temperature range at a given pressure. Here we try a
dc.publisherOxford University Press
dc.sourceJournal of Petrology
dc.subjectKeywords: chemical composition; igneous geochemistry; lherzolite; partial melting Feldspar solvus; Igneous sapphirine; Mantle solidus; Partial melting; Systems CMAS and CMAS-K2O
dc.titlePartial melting of spinel lherzolite in the system CaO�MgO�Al 2 O 3 �SiO 2 �K 2 O at 1.1 GPa
dc.typeJournal article
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.citationvolume45
dc.date.issued2004
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationMigratedxPub6647
local.type.statusPublished Version
local.contributor.affiliationLiu, Xi, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationO'Neill, Hugh, College of Physical and Mathematical Sciences, ANU
local.bibliographicCitation.issue7
local.bibliographicCitation.startpage1339
local.bibliographicCitation.lastpage1368
local.identifier.doi10.1093/petrology/egh021
dc.date.updated2015-12-11T09:52:00Z
local.identifier.scopusID2-s2.0-3242811907
CollectionsANU Research Publications

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