Mineral-aqueous fluid partitioning of trace elements at 900-1200°C and 3.0-5.7 GPa: New experimental data for garnet, clinopyroxene, and rutile, and implications for mantle metasomatism

R. Stalder*, S. F. Foley, G. P. Drey, I. Horn

*Corresponding author for this work

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Earth and Planetary Sciences