Thermophysical properties and phase diagrams in the system MgO–SiO2–FeO at upper mantle and transition zone conditions derived from a multiple-Einstein method-Reference-Cited by-同舟云学术

Thermophysical properties and phase diagrams in the system MgO–SiO2–FeO at upper mantle and transition zone conditions derived from a multiple-Einstein method

Published:2019-01-19 Issue:5 Volume:46 Page:513-534
ISSN:0342-1791
Container-title:Physics and Chemistry of Minerals
language:en
Short-container-title:Phys Chem Minerals

Author:

Jacobs Michael H. G.^ORCID,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/article/10.1007/s00269-018-01020-y/fulltext.html

Reference134 articles.

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

4. Akaogi M, Yusa H, Shiraishi K, Suzuki T (1995) Thermodynamic properties of α-quartz, coesite, and stishovite and equilibrium phase relations at high pressures and high temperatures. J Geophys Res B 100:22337–22347

5. Akimoto S, Syono Y (1969) Coesite–stishovite transition. J Geophys Res 74:1653–1659

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