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Hydrothermal Growth of Fayalite Crystals

  • S. Hirano
  • Y. Iwai
  • S. Somiya
  • 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 Mossbauer Spectrum 
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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    S. Hirano and S. Somiya, J. Crystal Growth 35, 273 (1976).CrossRefGoogle Scholar

Copyright information

© Springer Science+Business Media New York 1979

Authors and Affiliations

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

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