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

Skelton, Richard; Walker, Andrew M


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

CollectionsANU Research Publications
Date published: 2015
Type: Journal article
Source: Physics and Chemistry of Minerals
DOI: 10.1007/s00269-015-0754-9


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