Divalent chromium in ferropericlase inclusions in lower-mantle diamonds revealed by micro-XANES measurements

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Abstract

Chromium. K-edge X-ray absorption near-edge structure (XANES) spectra of natural ferropericlase were measured using an X-ray microbeam from a synchrotron radiation source to estimate the valence state of Cr. Measured samples were inclusions collected from lower-mantle diamonds. The obtained results revealed that divalent chromium is present in the materials in the lower mantle and that the proportion of Cr2+ in the total Cr content varied among the samples. The valence state of chromium in the inclusions in diamonds is a potential indicator of the redox conditions in the lower mantle.

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Odake, S., Fukura, S., Arakawa, M., Ohta, A., Harte, B., & Kagi, H. (2008). Divalent chromium in ferropericlase inclusions in lower-mantle diamonds revealed by micro-XANES measurements. Journal of Mineralogical and Petrological Sciences, 103(5), 350–353. https://doi.org/10.2465/jmps.080620d

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