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Closed-system geochemical recycling of crustal materials in alpine-type peridotite

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dc.contributor.authorMorishita, Tomoaki
dc.contributor.authorArai, Shoji
dc.contributor.authorGeddes, Robert Stanley
dc.contributor.authorGreen, David
dc.date.accessioned2015-12-13T23:05:49Z
dc.date.available2015-12-13T23:05:49Z
dc.date.issued2003
dc.date.updated2015-12-12T08:02:28Z
dc.description.abstractWe examined aluminous mafic rock (with or without corundum or sapphirine) alternating with peridotite from the Ronda peridotite massif, southern Spain. On the basis of petrographic characteristics, these mafic rocks show a decompression history from high
dc.identifier.issn1872-9533
dc.identifier.urihttp://hdl.handle.net/1885/85725
dc.publisherPergamon-Elsevier Ltd
dc.sourceGeochimica et Cosmochimica Acta
dc.subjectKeywords: crustal recycling; geochemistry; high pressure; mafic rock; peridotite; petrography; Spain
dc.titleClosed-system geochemical recycling of crustal materials in alpine-type peridotite
dc.typeJournal article
local.bibliographicCitation.issue2
local.bibliographicCitation.lastpage310
local.bibliographicCitation.startpage303
local.contributor.affiliationMorishita, Tomoaki, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationArai, Shoji, Kanazawa University
local.contributor.affiliationGeddes, Robert Stanley, University of New England
local.contributor.affiliationGreen, David, College of Physical and Mathematical Sciences, ANU
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.absfor040313 - Tectonics
local.identifier.ariespublicationMigratedxPub14347
local.identifier.citationvolume67
local.identifier.doi10.1016/S0016-7037(02)01079-7
local.identifier.scopusID2-s2.0-0037438931
local.type.statusPublished Version

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