The effect of cation order on the elasticity of omphacite from atomistic calculations
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Skelton, Richard
Walker, Andrew M
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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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Physics and Chemistry of Minerals
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2037-12-31
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