Thermodynamic mixing properties of olivine derived from lattice vibrations-Reference-Cited by-同舟云学术

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Thermodynamic mixing properties of olivine derived from lattice vibrations

Published:2009-01-08 Issue:7 Volume:36 Page:365-389
ISSN:0342-1791
Container-title:Physics and Chemistry of Minerals
language:en
Short-container-title:Phys Chem Minerals

Author:

Jacobs Michel Henricus Gerardus,de Jong Bernard H. W. S.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,General Materials Science

Link

http://link.springer.com/content/pdf/10.1007/s00269-008-0284-9

Reference84 articles.

1. Abramson EH, Brown JM, Slutsky LJ, Zaug J (1997) The elastic constants of San Carlos olivine to 17 GPa. J Geophys Res 102:12253–12263. doi: 10.1029/97JB00682

2. Akimoto S (1972) The system MgO–FeO–SiO2 at high pressures an temperatures-phase equilibria and elastic properties. Tectonophysics 13:161–187. doi: 10.1016/0040-1951(72)90019-4

3. Andrault D, Bouhifd MA, Itié JP, Richet P (1995) Compression and amorphization of (Mg, Fe)2SiO4 olivines: an X-ray diffraction study up to 70 GPa. Phys Chem Miner 22:99–107. doi: 10.1007/BF00202469

4. Aronson MC, Stixrude L, Davis MK, Gannon W, Ahilan K (2007) Magnetic excitations and heat capacity of fayalite, Fe2SiO4. Am Mineral 92:481–490. doi: 10.2138/am.2007.2305

5. Barin I (1989) Thermochemical data of pure substances, part II. VCH Verlags-gesellschaft mbH, Weinheim

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