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layering of alpine-Type peridotite and the segregation of partial melt in the upper mantle

✍ Scribed by Obata, Masaaki; Nagahara, Nobuhiko


Book ID
118671524
Publisher
American Geophysical Union
Year
1987
Tongue
English
Weight
877 KB
Volume
92
Category
Article
ISSN
0148-0227

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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