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Diffusion and partition coefficients of minor and trace elements in San Carlos olivine at 1300 degrees C with some geochemical implications

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dc.contributor.authorSpandler, Carl
dc.contributor.authorO'Neill, Hugh
dc.date.accessioned2015-12-10T22:38:46Z
dc.date.issued2010
dc.date.updated2016-02-24T12:02:29Z
dc.description.abstractLattice diffusion coefficients have been determined for 19 elements (Li, Be, Na, Ca, Sc, Ti, V, Cr, Mn, Fe, Co, Ni, Zn, Y, Zr, Eu, Gd, Lu and Hf) in a single crystal of San Carlos olivine as a function of crystallographic orientation, at 1,300°C, 1 bar a
dc.identifier.issn0010-7999
dc.identifier.urihttp://hdl.handle.net/1885/56877
dc.publisherSpringer
dc.sourceContributions to Mineralogy and Petrology
dc.subjectKeywords: basalt; crystal chemistry; crystallography; diffusion; geochemistry; lattice dynamics; mantle source; olivine; partition coefficient; trace element Basalt; Crystal chemistry; Diffusion; Mantle; Olivine; Trace elements
dc.titleDiffusion and partition coefficients of minor and trace elements in San Carlos olivine at 1300 degrees C with some geochemical implications
dc.typeJournal article
local.bibliographicCitation.issue6
local.bibliographicCitation.lastpage818
local.bibliographicCitation.startpage791
local.contributor.affiliationSpandler, Carl, James Cook University
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.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationu9503261xPUB378
local.identifier.citationvolume159
local.identifier.doi10.1007/s00410-009-0456-8
local.identifier.scopusID2-s2.0-77952243222
local.type.statusPublished Version

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