Phase relations in the system MgSiO 3 –Al 2 O 3 up to 52 GPa and 2000 K-Reference-Cited by-同舟云学术

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Phase relations in the system MgSiO 3 –Al 2 O 3 up to 52 GPa and 2000 K

Published:2016-08 Issue: Volume:257 Page:18-27
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Liu Zhaodong,Irifune Tetsuo,Nishi Masayuki,Tange Yoshinori,Arimoto Takeshi,Shinmei Toru

Funder

JSPS

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference55 articles.

1. Electron microscopy of high pressure phases synthesized from natural garnets in a diamond anvil cell: implications for the mineralogy of the lower mantle;Ahmed-Zaïd;Earth Planet. Sci. Lett.,1995

2. Garnet–ilmenite–perovskite transitions in the system Mg4Si4O12-Mg3Al2Si3O12 at high pressures and high temperatures: phase equilibria, calorimetry and implications for mantle structure;Akaogi;Phys. Earth Planet. Inter.,2002

3. Thermodynamic parameters in the Earth as determined from seismic profiles;Brown;Geophys. J. R. Astron. Soc.,1981

4. Pressure-induced changes in the compression mechanism of aluminous perovskite in the Earth’s mantle;Brodholt;Nature,2000

5. High-pressure single-crystal structure determinations for ruby up to 90 kbar using an automatic diffractometer P=0kbar;D’Amour;J. Appl. Phys.,1978

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