Citation: K. Righter et al., PREDICTION OF SIDEROPHILE ELEMENT METAL-SILICATE PARTITION-COEFFICIENTS TO 20-GPA AND 2800-DEGREES-C - THE EFFECTS OF PRESSURE, TEMPERATURE, OXYGEN FUGACITY, AND SILICATE AND METALLIC MELT COMPOSITIONS, Physics of the earth and planetary interiors, 100(1-4), 1997, pp. 115-134