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Experimental constraints on high pressure melting in subducted crust

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Hermann, Joerg; Green, David

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Synthesis piston-cylinder experiments were carried out from 2.0 to 4.5 GPa and 850 to 1150°C in order to determine phase and melting relations in a model composition for subducted crust in H2O and large ion lithophile elements (LILE), this study concentr

dc.contributor.authorHermann, Joerg
dc.contributor.authorGreen, David
dc.date.accessioned2015-12-13T23:22:27Z
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/1885/91458
dc.description.abstractSynthesis piston-cylinder experiments were carried out from 2.0 to 4.5 GPa and 850 to 1150°C in order to determine phase and melting relations in a model composition for subducted crust in H2O and large ion lithophile elements (LILE), this study concentr
dc.publisherElsevier
dc.sourceEarth and Planetary Science Letters
dc.subjectKeywords: high pressure; mineralogy; P-T conditions; partial melting; petrology; phengite; subduction Crust; Experimental studies; Partial melting; Phengite; Subduction; Trace elements
dc.titleExperimental constraints on high pressure melting in subducted crust
dc.typeJournal article
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.citationvolume188
dc.date.issued2001
local.identifier.absfor040313 - Tectonics
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationMigratedxPub22215
local.type.statusPublished Version
local.contributor.affiliationHermann, Joerg, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationGreen, David, College of Physical and Mathematical Sciences, ANU
local.description.embargo2037-12-31
local.bibliographicCitation.issue1-2
local.bibliographicCitation.startpage149
local.bibliographicCitation.lastpage168
local.identifier.doi10.1016/S0012-821X(01)00321-1
dc.date.updated2015-12-12T09:11:09Z
local.identifier.scopusID2-s2.0-0035005167
CollectionsANU Research Publications

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