Free energy of formation of zircon and hafnon

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dc.contributor.authorO'Neill, Hugh
dc.date.accessioned2015-12-07T22:43:04Z
dc.date.issued2006
dc.date.updated2015-12-07T11:15:23Z
dc.description.abstractThe free energy of formation of zircon (ZrSiO4) from its oxides was determined between 1100 and 1300 K by an electrochemical method, in which values of μ02 defined by the two assemblages Fe2SiO4-Fe-SiO2 (fayalite-iron-quartz) and Fe2SiO4- Fe-ZrO2-ZrSiO4
dc.identifier.issn0003-004X
dc.identifier.urihttp://hdl.handle.net/1885/24846
dc.publisherMineralogical Society of America
dc.sourceAmerican Mineralogist
dc.subjectKeywords: baddeleyite; cristobalite; electrochemical method; enthalpy; entropy; fayalite; phase transition; zircon Fayalite; Free energy of formation; Hafnon; Thermodynamic data; Zircon
dc.titleFree energy of formation of zircon and hafnon
dc.typeJournal article
local.bibliographicCitation.lastpage1141
local.bibliographicCitation.startpage1134
local.contributor.affiliationO'Neill, Hugh, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidO'Neill, Hugh, u8101317
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationu9503261xPUB34
local.identifier.citationvolume91
local.identifier.doi10.2138/am.2006.2071
local.identifier.scopusID2-s2.0-33746996454
local.type.statusPublished Version

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