Internally consistent thermodynamic data set for dense hydrous magnesium silicates up to 35GPa, 1600°C: Implications for water circulation in the Earth's deep mantle-Reference-Cited by-同舟云学术

Internally consistent thermodynamic data set for dense hydrous magnesium silicates up to 35GPa, 1600°C: Implications for water circulation in the Earth's deep mantle

Published:2006-06 Issue:1-2 Volume:156 Page:89-107
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Komabayashi Tetsuya,Omori Soichi

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

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3. Derivation of internally-consistent thermodynamic data by the technique of mathematical programming: a review with application to the system MgO–SiO2–H2O;Berman;J. Petrol.,1986

4. Water partitioning between nominally anhydrous minerals in the MgO–SiO2–H2O system up to 24GPa: implications for the distribution of water in the Earth's mantle;Bolfan-Casanova;Earth Planet. Sci. Lett.,2000

5. Hydroxyl in MgSiO3 akimotoite: a polarized and high-pressure IR study;Bolfan-Casanova;Am. Mineral.,2002

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