Stability of spinelloid phases in the system Mg2SiO4–Fe2SiO4–Fe3O4 at 1100 °C and up to 10.5 GPa
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics
Reference24 articles.
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2. Crystal structure of spinelloid II in the system Fe3O4–Fe2SiO4;Angel;Eur. J. Mineral.,1998
3. The olivine-spinel transition: experimental and thermodynamic constraints and implications for the nature of the 400-km discontinuity;Bina;J. Geophys. Res.,1987
4. Calibration of a belt apparatus to 1800°C and 6GPa;Brey;J. Geophys. Res.,1990
5. A preliminary look at phase relations in the system γ-Fe2SiO4–Fe3O4 at 7GPa;Canil;Terra Abstr.,1991
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