Experimental determination of activities in Fe-Mg olivine at 1400 K
The exchage equilibrium {Mathematical expression} has been used to measure activity-composition relations along the olivine join FeSi0.5O2-MgSi0.5O2 at 1400 K and 1 atm pressure. Equilibrium Fe-Mg partitioning between the two phases was determined by reversing the compositions of olivine coexisting...
| المؤلفون الرئيسيون: | , |
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| التنسيق: | Journal article |
| اللغة: | English |
| منشور في: |
Springer-Verlag
1991
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