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The solubility of andradite garnet was determined at 800 °C and 10 kbar in a solution of 10 mol% NaCl and 90 mol% H 2 O. Experiments were syntheses carried out with high-purity natural wollastonite, reagent hematite or natural specular hematite containing ~1 wt% TiO 2 , and fluid. All experiments were performed with Mn 2 O 3 -Mn 3 O 4  or Fe 2 O 3 -Fe 3 O 4  oxygen buffers in a piston-cylinder apparatus with NaCl pressure media for 1-3 days. Andradite saturation was determined by the presence or absence of garnet in quenched charges.

american mineralogist

Solubility of andradite, Ca 3 Fe 2 Si 3 O 12 , in a 10 mol% NaCl solution at 800 °C and 10 kbar: Implications for the metasomatic origin of grandite garnet in calc-silicate granulites