Thermodynamic aspects of phase boundary among α-, β-, and γ-Mg2SiO4-Reference-Cited by-同舟云学术

Thermodynamic aspects of phase boundary among α-, β-, and γ-Mg2SiO4

Published:1987 Issue: Volume: Page:269-274
ISSN:0065-8448
Container-title:High‐Pressure Research in Mineral Physics: A Volume in Honor of Syun‐iti Akimoto
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Author:

Ashida Toshifumi,Kume Shoichi,Ito Eiji

Publisher

American Geophysical Union

Reference20 articles.

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

2. High pressure crystal chemistry in orthosilicates and formation of the mantle transition zone;Akimoto,1976

3. Heat capacity, compressibility and thermal expansion coefficient of ilmenite-type MgGeO3;Ashida;Phys. Chem. Minerals,1985

4. Elastic constants of single crystal forsterite as a function of temperature and pressure;Graham;J. Geophys. Res.,1969

5. Effect of temperature and pressure on the crystal structure of forsterite;Hazen;Am. Mineral.,1976

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