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Phase relationships in metapelites were experimentally investigated in the model system CaO–K2O–FeO–MgO–Al2O3–SiO2–H2O on four synthetic compositions differing in their K2O content and K2O/Al2O3 ratio. Experiments were carried out at pressures ranging from 0·8 to 1·4 GPa and temperatures from 620 to 740°C under different fluid-buffered conditions. The stability of the assemblage garnet–biotite–sta...

An Experimental Determination of the Effect of Bulk Composition on Phase Relationships in Metasediments at Near-solidus Conditions