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

dc.contributor.author	Skelton, Richard
dc.contributor.author	Walker, Andrew M
dc.date.accessioned	2015-12-10T23:36:20Z
dc.date.issued	2015
dc.date.updated	2015-12-10T11:53:10Z
dc.description.abstract	Omphacite, 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.issn	0342-1791
dc.identifier.uri	http://hdl.handle.net/1885/70089
dc.publisher	Springer
dc.source	Physics and Chemistry of Minerals
dc.title	The effect of cation order on the elasticity of omphacite from atomistic calculations
dc.type	Journal article
local.bibliographicCitation.lastpage	15
local.bibliographicCitation.startpage	1
local.contributor.affiliation	Skelton, Richard, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliation	Walker, Andrew M, University of Bristol
local.contributor.authoruid	Skelton, Richard, u4868117
local.description.embargo	2037-12-31
local.description.notes	Imported from ARIES
local.identifier.absfor	040402 - Geodynamics
local.identifier.ariespublication	a383154xPUB2217
local.identifier.doi	10.1007/s00269-015-0754-9
local.identifier.scopusID	2-s2.0-84929682839
local.type.status	Published Version

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