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...
Main Authors: | Wiser, N, Wood, B |
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Format: | Journal article |
Language: | English |
Published: |
Springer-Verlag
1991
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