In situ X ray observation of high-pressure phase transitions of MgSiO3and thermal expansion of MgSiO3perovskite at 25 GPa by double-stage multianvil system

Author:

Kato Takumi,Ohtani Eiji,Morishima Hideaki,Yamazaki Daisuke,Suzuki Akio,Suto Minoru,Kubo Tomoaki,Kikegawa Takumi,Shimomura Osamu

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference35 articles.

1. Heat capacity of MgSiO3 perovskite;Akaogi;Geophys. Res. Lett.,1993

2. High pressure transions of lower mantle materials;Akaogi;Cent. Core Earth,1993

3. Thermally induced phase changes, lateral heterogeneity of the mantle, continental roots, and deep slab anomalies;Anderson;J. Geophys. Res.,1987

4. Anharmonicity and the equation of state for gold;Anderson;J. Appl. Phys.,1989

5. Equation of state and thermodynamic parameters of NaCl to 300 kbar in the high-temperature domain;Birch;J. Geophys. Res.,1986

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