Oxygen fugacity and valence state of chromium in ferropericlase: Can Cr2+ be a redox indicator for the deep mantle?

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ژورنال

عنوان ژورنال: Journal of Mineralogical and Petrological Sciences

سال: 2013

ISSN: 1345-6296,1349-3825

DOI: 10.2465/jmps.121022f