Solubility of hydrogen and ferric iron in rutile and TiO2(II): Implications for phase assemblages during ultrahigh-pressure metamorphism and for the stability of silica polymorphs in the lower mantle-Reference-Cited by-同舟云学术

Solubility of hydrogen and ferric iron in rutile and TiO2(II): Implications for phase assemblages during ultrahigh-pressure metamorphism and for the stability of silica polymorphs in the lower mantle

Published:2004 Issue:4 Volume:31 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Bromiley Geoffrey

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference27 articles.

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4. High concentration of water in stishovite in the MORB system;Chung;Geophys. Res. Lett.,2002

5. Crystal growth and defect structure of Al3+-doped rutile;Gesenhues;J. Solid State Chem.,1999

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