Hydrothermal Growth of Fayalite Crystals
Fayalite, Fe2SiO4, is the iron-rich end member of the olivine series, which constitutes most of the upper mantle of the earth. It is thus a most important mineral with respect to geophysical science.
KeywordsGrowth Temperature Oxygen Fugacity Supercritical Water Silicon Powder Mossbauer Spectrum
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