Evolution of low-Al orthopyroxene in the Horoman peridotite, Japan: an unusual indicator of metasomatizing fluids

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dc.contributor.authorMorishita, Tomoaki
dc.contributor.authorArai, Shoji
dc.contributor.authorGreen, David
dc.date.accessioned2015-12-13T23:35:48Z
dc.date.available2015-12-13T23:35:48Z
dc.date.issued2003
dc.date.updated2015-12-12T09:41:17Z
dc.description.abstractUnusually alumina-poor orthopyroxene is found in a spinel peridolite from the Horoman Peridotite Complex, Japan. Al2O3, Cr2O3 and CaO contents in the low-Al orthopyroxene (named Low-Al OPX hereafter) are <0·25 wt%, <0·04 wt% and <0·3 wt%, respectively,
dc.identifier.issn0022-3530
dc.identifier.urihttp://hdl.handle.net/1885/94085
dc.publisherOxford University Press
dc.sourceJournal of Petrology
dc.subjectKeywords: chemical composition; mantle; metasomatism; orthopyroxene; peridotite; petrography; Japan Horoman Peridotite Complex; Low-Al orthopyroxene; Mantle wedge; Metasomatism
dc.titleEvolution of low-Al orthopyroxene in the Horoman peridotite, Japan: an unusual indicator of metasomatizing fluids
dc.typeJournal article
local.bibliographicCitation.issue7
local.bibliographicCitation.lastpage1246
local.bibliographicCitation.startpage1237
local.contributor.affiliationMorishita, Tomoaki, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationArai, Shoji, Kanazawa University
local.contributor.affiliationGreen, David, College of Physical and Mathematical Sciences, ANU
local.contributor.authoremailrepository.admin@anu.edu.au
local.contributor.authoruidMorishita, Tomoaki, v002660
local.contributor.authoruidGreen, David, u9400843
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationMigratedxPub25574
local.identifier.citationvolume44
local.identifier.scopusID2-s2.0-0038450895
local.identifier.uidSubmittedByMigrated
local.type.statusPublished Version

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