Incongruent melting of Mg2SiO4 at 20 GPa-Reference-Cited by-同舟云学术

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Incongruent melting of Mg2SiO4 at 20 GPa

Published:1985-12 Issue:1 Volume:41 Page:1-5
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:

Kato Takumi,Kumazawa Mineo

Publisher

Elsevier BV

Subject

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

Reference11 articles.

1. High-pressure stability of dense hydrous magnesian silicate Mg23Si8O42H6 and some geophysical implications;Akaogi;J. Geophys. Res.,1980

2. The melting of forsterite up to 50 kilobars;Davies;J. Geophys. Res.,1964

3. Stability relations of silicate spinels, ilmenites, and perovskite;Ito,1982

4. Melting and phase relations in Mg2SiO4MgSiO3 system at 20 GPa under hydrous conditions;Kato;J. Geophys. Res.,1985

5. Stability of phase B, a hydrous magnesium silicate, to 2300°C at 20 GPa;Kato;Geophys. Res. Lett.,1985

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1. The Composition of Rocky Planets;Planetary Diversity;2020-12

2. The Principal Hugoniot of Forsterite to 950 GPa;Geophysical Research Letters;2018-05-12

3. The stability of anhydrous phase B, Mg14Si5O24, at mantle transition zone conditions;Physics and Chemistry of Minerals;2017-12-27

4. High Pressure Phase Transitions in a Homogeneous Model Martian Mantle;Evolution of the Earth and Planets;2013-03-18

5. Material transport in laser-heated diamond anvil cell melting experiments;Geophysical Research Letters;1992-05-22

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