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SiO2 precipitation in olivine: ATEM Investigation of dunites annealed at 300 MPa in hydrous conditions.

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dc.contributor.authorRaterron, Paul
dc.contributor.authorChopra, Prame
dc.contributor.authorDoukhan, Jean-Claude
dc.date.accessioned2015-12-13T23:16:07Z
dc.date.issued2000
dc.date.updated2015-12-12T08:46:43Z
dc.description.abstractTwo natural dunites were annealed at pressure P = 300 MPa, temperature T = 1373, 1473 and 1573 K, and fO2 within the stability field of olivine. The starting materials contained small amounts of hydroxyls in the form of minor phases of hydrated minerals,
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/1885/89244
dc.publisherElsevier
dc.sourceEarth and Planetary Science Letters
dc.subjectKeywords: dunite; exsolution; metamorphism; olivine; precipitation (chemistry); silica Dunite; Exsolution; Olivine; Point defects; Precipitation; Silica; Transmission electron microscopy; Ultramafic composition; Xenoliths
dc.titleSiO2 precipitation in olivine: ATEM Investigation of dunites annealed at 300 MPa in hydrous conditions.
dc.typeJournal article
local.bibliographicCitation.lastpage423
local.bibliographicCitation.startpage415
local.contributor.affiliationRaterron, Paul, Universite Sciences et Technologies de Lille
local.contributor.affiliationChopra, Prame, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationDoukhan, Jean-Claude, Universite Sciences et Technologies de Lille
local.contributor.authoruidChopra, Prame, u9707732
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040202 - Inorganic Geochemistry
local.identifier.ariespublicationMigratedxPub19209
local.identifier.citationvolume180
local.identifier.doi10.1016/S0012-821X(00)00160-6
local.identifier.scopusID2-s2.0-0033843643
local.type.statusPublished Version

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