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Origin of mantle peridotite and komatiite by partial melting

✍ Scribed by Herzberg, C. T.; O'Hara, M. J.


Book ID
119707271
Publisher
American Geophysical Union
Year
1985
Tongue
English
Weight
383 KB
Volume
12
Category
Article
ISSN
1944-8007

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πŸ“œ SIMILAR VOLUMES


Partitioning of iron and magnesium betwe
✍ BjΓΈrn Mysen πŸ“‚ Article πŸ“… 1975 πŸ› Springer 🌐 English βš– 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