Influence of protons on Fe-Mg interdiffusion in olivine

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Influence of protons on Fe-Mg interdiffusion in olivine

[1] We report the experimental measurement of Fe-Mg interdiffusivity in olivine along the [001] crystallographic direction in a water-saturated environment at pressures of 0.1 to 6 GPa and temperatures between 1373 and 1450 K. The concentration of water-derived protons in olivine was controlled by varying the water fugacity. The oxygen fugacity was set by the Ni-NiO solid state reaction, while ...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research: Solid Earth

سال: 2005

ISSN: 0148-0227

DOI: 10.1029/2004jb003292