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The importance of defining chemical potentials, substitution mechanisms and solubility in trace element diffusion studies: the case of Zr and Hf in olivine

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dc.contributor.authorJollands, Michael
dc.contributor.authorO'Neill, Hugh
dc.contributor.authorHermann, Joerg
dc.date.accessioned2015-12-07T22:21:26Z
dc.date.issued2014
dc.date.updated2015-12-07T08:57:41Z
dc.description.abstractThe diffusion, substitution mechanism and solubility limits of Zr and Hf in synthetic forsterite (Mg2SiO4) and San Carlos olivine (Mg0.9Fe0.1)2SiO4 have been investigated between 1,200 and 1,500 °C as a function of the chemical potentials of the componen
dc.identifier.issn0010-7999
dc.identifier.urihttp://hdl.handle.net/1885/20039
dc.publisherSpringer
dc.sourceContributions to Mineralogy and Petrology
dc.titleThe importance of defining chemical potentials, substitution mechanisms and solubility in trace element diffusion studies: the case of Zr and Hf in olivine
dc.typeJournal article
local.bibliographicCitation.lastpage19
local.bibliographicCitation.startpage1
local.contributor.affiliationJollands, Michael, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationO'Neill, Hugh, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationHermann, Joerg, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidJollands, Michael, u4707055
local.contributor.authoruidO'Neill, Hugh, u8101317
local.contributor.authoruidHermann, Joerg, u9907179
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationu8906087xPUB10
local.identifier.citationvolume168
local.identifier.doi10.1007/s00410-014-1055-x
local.identifier.scopusID2-s2.0-84906722413
local.identifier.thomsonID000341860900008
local.type.statusPublished Version

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