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The partitioning of Cl between apatite, felsic melts, and aqueous fluids (vapor±brine), and the partitioning of F between apatite and felsic melt were investigated experimentally at 50–58MPa and 850–950°C. Chlorine partitioning between apatite, melt, and fluid(s) is a function of the Cl content of the system, melt composition, Cl solubility in the melt, and pressure. For most of the 23 equilibrium...
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