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Hydrothermal Growth of Fayalite Crystals

  • S. Hirano
  • Y. Iwai
  • S. Sōmiya
  • S. Saito

Abstract

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.

Keywords

Growth 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.

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References

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Copyright information

© Elsevier Science Publishers Ltd 1989

Authors and Affiliations

  • S. Hirano
    • 1
  • Y. Iwai
    • 1
  • S. Sōmiya
    • 1
  • S. Saito
    • 1
  1. 1.Tokyo Institute of TechnologyTokyoJapan

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