Melting of enstatite (MgSiO_3) from 10 to 16.5 Gpa and the forsterite (Mg_2SiO_4)-Majorite (MgSiO_3) eutectic at 16.5 GPa: implications for the origin of the mantle

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  • J. Geophys. Res.

    J. Geophys. Res. 95, 15771-15777, 1990

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