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The effect of cation order on the elasticity of omphacite from atomistic calculations

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dc.contributor.authorSkelton, Richard
dc.contributor.authorWalker, Andrew M
dc.date.accessioned2015-12-10T23:36:20Z
dc.date.issued2015
dc.date.updated2015-12-10T11:53:10Z
dc.description.abstractOmphacite, a clinopyroxene mineral with two distinct crystallographic sites, M1 and M2, and composition intermediate between diopside and jadeite, is abundant throughout the Earth’s upper mantle and is the dominant mineral in subducted oceanic crust. Un
dc.identifier.issn0342-1791
dc.identifier.urihttp://hdl.handle.net/1885/70089
dc.publisherSpringer
dc.sourcePhysics and Chemistry of Minerals
dc.titleThe effect of cation order on the elasticity of omphacite from atomistic calculations
dc.typeJournal article
local.bibliographicCitation.lastpage15
local.bibliographicCitation.startpage1
local.contributor.affiliationSkelton, Richard, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationWalker, Andrew M, University of Bristol
local.contributor.authoruidSkelton, Richard, u4868117
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040402 - Geodynamics
local.identifier.ariespublicationa383154xPUB2217
local.identifier.doi10.1007/s00269-015-0754-9
local.identifier.scopusID2-s2.0-84929682839
local.type.statusPublished Version

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