The magnesiowustite: iron equilibrium and its implications for the activity-composition relations of (Mg,Fe) 2 SiO 4 olivine solid solutions
The chemical potential of oxygen (μO2) in equilibrium with magnesiowüstite solid solution (Mg, Fe)O and metallic Fe has been determined by gas-mixing experiments at 1,473 K supplemented by solid-cell EMF experiments at lower temperatures. The results gi
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|Source:||Contributions to Mineralogy and Petrology|
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