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Sediment Melts at Sub-arc Depths: an Experimental Study

Hermann, Joerg; Spandler, Carl

Description

The phase and melting relations in subducted pelites have been investigated xperimentally at conditions relevant for slabs at sub-arc depths (T = 600-1050°C, P = 2·5-4 GPa). The fluid-present experiments produced a dominant paragenesis consisting of arn

dc.contributor.authorHermann, Joerg
dc.contributor.authorSpandler, Carl
dc.date.accessioned2015-12-10T22:15:36Z
dc.identifier.issn0022-3530
dc.identifier.urihttp://hdl.handle.net/1885/50754
dc.description.abstractThe phase and melting relations in subducted pelites have been investigated xperimentally at conditions relevant for slabs at sub-arc depths (T = 600-1050°C, P = 2·5-4 GPa). The fluid-present experiments produced a dominant paragenesis consisting of arn
dc.publisherOxford University Press
dc.sourceJournal of Petrology
dc.subjectKeywords: experimental study; garnet; magma; melt; paragenesis; pelite; phengite; sedimentary petrology; subduction zone; ultrahigh pressure metamorphism Experimental petrology; Fluid; LILE; Pelite; Subduction; UHP metamorphism
dc.titleSediment Melts at Sub-arc Depths: an Experimental Study
dc.typeJournal article
local.description.notesImported from ARIES
local.identifier.citationvolume49
dc.date.issued2008
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationu9503261xPUB209
local.type.statusPublished Version
local.contributor.affiliationHermann, Joerg, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationSpandler, Carl, University of Bern
local.description.embargo2037-12-31
local.bibliographicCitation.issue4
local.bibliographicCitation.startpage717
local.bibliographicCitation.lastpage740
local.identifier.doi10.1093/petrology/egm073
dc.date.updated2015-12-09T08:18:34Z
local.identifier.scopusID2-s2.0-41749113123
local.identifier.thomsonID000254472500007
CollectionsANU Research Publications

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