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Geochemical window into subduction and accretion processes: Raspas metamorphic complex, Ecuador.

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Arculus, Richard

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The high-pressure, low-temperature (P = 1.3-2 GPa; T ≤600 °C) Raspas metamorphic complex is an exhumed fragment of the partially accreted, partially subducted Amotape-Chaucha terrane in southwest Ecuador. Comparative analysis of major and trace element

dc.contributor.authorArculus, Richard
dc.date.accessioned2015-12-13T23:23:11Z
dc.date.available2015-12-13T23:23:11Z
dc.identifier.issn0091-7613
dc.identifier.urihttp://hdl.handle.net/1885/91802
dc.description.abstractThe high-pressure, low-temperature (P = 1.3-2 GPa; T ≤600 °C) Raspas metamorphic complex is an exhumed fragment of the partially accreted, partially subducted Amotape-Chaucha terrane in southwest Ecuador. Comparative analysis of major and trace element
dc.publisherGeological Society of America Inc
dc.sourceGeology
dc.subjectKeywords: accretion; geochemistry; metamorphism; oceanic lithosphere; subduction; terrane; Ecuador
dc.titleGeochemical window into subduction and accretion processes: Raspas metamorphic complex, Ecuador.
dc.typeJournal article
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.citationvolume27
dc.date.issued1999
local.identifier.absfor040313 - Tectonics
local.identifier.ariespublicationMigratedxPub22673
local.type.statusMetadata only
local.contributor.affiliationArculus, Richard, College of Physical and Mathematical Sciences, ANU
local.bibliographicCitation.startpage547
local.bibliographicCitation.lastpage550
local.identifier.doi10.1130/0091-7613(1999)027<0547:GWISAA>2.3.CO;2
dc.date.updated2016-02-24T09:48:27Z
local.identifier.scopusID2-s2.0-84879880514
CollectionsANU Research Publications

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