Phase diagrams, thermodynamic properties and sound velocities derived from a multiple Einstein method using vibrational densities of states: an application to MgO

Phase diagrams, thermodynamic properties and sound velocities derived from a multiple Einstein method using vibrational densities of states: an application to MgO–SiO2

Published:2016-08-10 Issue:1 Volume:44 Page:43-62
ISSN:0342-1791
Container-title:Physics and Chemistry of Minerals
language:en
Short-container-title:Phys Chem Minerals

Author:

Jacobs Michael H. G.,Schmid-Fetzer Rainer,van den Berg Arie P.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,General Materials Science

Link

http://link.springer.com/content/pdf/10.1007/s00269-016-0835-4.pdf

Reference99 articles.

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2. Akaogi M, Ito E (1993b) Refinement of enthalpy measurement of MgSiO3 perovskite and negative pressure. temperature slopes for perovskite-forming reactions. Geophys Res Lett 20:1839–1842

3. Akaogi M, Ito E (1999) Calorimetric study on majorite-perovskite transition in the system Mg4Si4O12–Mg3Al2Si3O12: transition boundaries with positive pressure-temperature slopes. Phys Earth Plan Int 114:129–140

4. Akaogi M, Ito E, Navrotsky A (1989) Olivine-modified spinel-spinel transitions in the system Mg2SiO4–Fe2SiO4: calorimetric measurements, thermochemical calculation, and geophysical application. J Geophys Res 94:15671–15685

5. Akaogi M, Tanaka A, Ito E (2002) Garnet-ilmenite-perovskite transitions in the system Mg4Si4O12–Mg3Al2Si3O12 at high pressures and high temperatures: phase equilibria, calorimetry and implications for mantle structure. Phas Earth Plan Int 132:303–324

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