In situ observation of the olivine-spinel phase transformation in Fe2SiO4using synchrotron radiation-Reference-Cited by-同舟云学术

In situ observation of the olivine-spinel phase transformation in Fe2SiO4using synchrotron radiation

Published:1987 Issue:B7 Volume:92 Page:6207
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Yagi Takehiko,Akaogi Masaki,Shimomura Osamu,Suzuki Toshihiro,Akimoto Syun-Iti

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

Link

http://www.agu.org/journals/jb/v092/iB07/JB092iB07p06207/JB092iB07p06207.pdf

Reference24 articles.

1. The Mg2SiO4 polymorphs (olivine, modified spinel, and spinel)-Thermodynamic properties from oxide melt solution calorimetry, phase relations, and models of lattice vibrations;Akaogi;Am. Mineral,1984

2. The olivine-spinel transition in Fe2SiO4, and Ni2SiO4;Akimoto;J. Geophys. Res.,1965

3. Effect of pressure on the melting of olivine and spinel polymorph of Fe2SiO4;Akimoto;J. Geophys. Res.,1967

4. High-pressure equation of state for NaCl, KCl, and CsCl;Decker;J. Appl. Phys.,1971

5. Investigation of the mechanism of the olivine-spinel transition in fayalite by synchrotron radiation;Furnish;J. Geophys. Res.,1983

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