Partitioning of iron and magnesium betwe
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BjΓΈrn Mysen
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Article
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1975
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Springer
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English
β 503 KB
The iron-magnesium distribution coefficient, K, (v /v "~olivine [~,.-/y "~liquid D = ~,ZXZFeO/ZXMgO] ~/XMgO/~'~EFeO/ , has frequently been used as a means of testing whether experimental and natural silicate liquids could have been in equilibrium with olivine of mantle composition. It is shown here