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Figure 9
Results of the FPSM analysis for the sample containing nanocrystalline periclase and large grains of calcite and magnetite. The magnetite is less than 3 wt% and not identified owing to the poor statistics on its intensities in addition to the small amount of content. The magnetite peaks are better fitted by the similar qandilite structure. Also, a spurious diamond phase was erroneously found. Rwp: 0.151.

Journal logoJOURNAL OF
APPLIED
CRYSTALLOGRAPHY
ISSN: 1600-5767
Volume 52| Part 3| June 2019| Pages 587-598
https://doi.org/10.1107/S160057671900342X
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