High-pressure decomposition of the system FeSiO3MgSiO3
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics
Reference11 articles.
1. Olivine-spinel solid solution equilibria in the system Mg2SiO4-Fe2SiO4
2. Effect of pressure on the melting of olivine and spinel polymorph of Fe2SiO4
3. Coesite-Stishovite transition
4. Pressure Calibration to 100 kbar Based on the Compression of NaCl
5. The pyroxene-garnet transformation in the earth's mantle
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2. Phase Transitions of Pyroxene and Garnet, and Post-spinel Transition Forming Perovskite;High-Pressure Silicates and Oxides;2022
3. Thermal expansivity, heat capacity and bulk modulus of the mantle;Geophysical Journal International;2021-09-25
4. Phase relations of MgSiO3-FeSiO3 system up to 64 GPa and 2300 K using multianvil apparatus with sintered diamond anvils;Physics of the Earth and Planetary Interiors;2019-10
5. Thermophysical properties and phase diagrams in the system MgO–SiO2–FeO at upper mantle and transition zone conditions derived from a multiple-Einstein method;Physics and Chemistry of Minerals;2019-01-19
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