Disproportionation of Fe2SiO4 to 2FeO+SiO2 at pressures up to 250kbar and temperatures up to 3000 °C
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics
Reference30 articles.
1. Equations of state and crystal structures of high-pressure phases of shocked silicates and oxides
2. High-pressure synthesis of a “modified” spinel and some geophysical implications
3. Effect of pressure on the melting of olivine and spinel polymorph of Fe2SiO4
4. Shock-wave equations of state for rocks and minerals
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