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Melting experiments were performed on a silica-rich peridotite composition at 10–17GPa to determine majoritic garnet–melt partition coefficients (D) for major and trace elements. Our results show that D for many elements, including Na, Sc, Y and rare earth elements (REE), varies significantly with increasing pressure or proportion of majorite component. Lu and Sc become incompatible at 17GPa, with...
Here we report the phase boundary of pyrope garnet (Mg 3 Al 2 Si 3 O 12 ) to Al-bearing silicate perovskite plus corundum, with the highest transition pressure determined by in situ measurements in a multi-anvil apparatus at high temperature. The consistency of the pressure scales by different standards of Au, NaCl, Pt, W, and Mo at high temperature was also evaluated...
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