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 Large Single Crystal
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
Unable to display preview. Download preview PDF.
© Elsevier Science Publishers Ltd 1989