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

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Authors

Skelton, Richard
Walker, Andrew M

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Publisher

Springer

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

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Source

Physics and Chemistry of Minerals

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Restricted until

2037-12-31