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      Mineralogy of the Martian interior up to core-mantle boundary pressures

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      Journal of Geophysical Research: Solid Earth
      American Geophysical Union (AGU)

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          Postspinel transformations in the system Mg2SiO4-Fe2SiO4and some geophysical implications

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            Melting of a dry peridotite KLB-1 up to 14 GPa: Implications on the Origin of peridotitic upper mantle

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              Magnetism and thermal evolution of the terrestrial planets

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                Author and article information

                Journal
                Journal of Geophysical Research: Solid Earth
                J. Geophys. Res.
                American Geophysical Union (AGU)
                01480227
                March 10 1997
                March 10 1997
                : 102
                : B3
                : 5251-5264
                Article
                10.1029/96JB03270
                26d787bf-a327-40d6-ac2b-f9087bb16d57
                © 1997

                http://doi.wiley.com/10.1002/tdm_license_1.1

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