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Grain misorientations in partially molten olivine aggregates: an electron backscatter diffraction study

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dc.contributor.authorFaul, Ulrich
dc.contributor.authorFitz Gerald, John
dc.date.accessioned2015-12-13T23:35:27Z
dc.date.issued1999
dc.date.updated2015-12-12T09:39:57Z
dc.description.abstractIn polycrystalline aggregates of olivine with mean grain sizes above 35 μm plus a low basaltic melt fraction, both wetted and melt-free grain boundaries are observed after equilibration times at high pressures and temperatures of between 15 and 25 days.
dc.identifier.issn0342-1791
dc.identifier.urihttp://hdl.handle.net/1885/93913
dc.publisherSpringer
dc.sourcePhysics and Chemistry of Minerals
dc.subjectKeywords: grain boundary; melt; olivine; partial melting Electron backscatter diffraction; Grain boundary; Misorientation; Olivine; Partial melt
dc.titleGrain misorientations in partially molten olivine aggregates: an electron backscatter diffraction study
dc.typeJournal article
local.bibliographicCitation.lastpage197
local.bibliographicCitation.startpage187
local.contributor.affiliationFaul, Ulrich, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationFitz Gerald, John, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidFaul, Ulrich, u9501887
local.contributor.authoruidFitz Gerald, John, u8001315
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040312 - Structural Geology
local.identifier.ariespublicationMigratedxPub25348
local.identifier.citationvolume26
local.identifier.doi10.1007/s002690050176
local.identifier.scopusID2-s2.0-0032945834
local.type.statusPublished Version

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