Mineral equilibria calculations in the system K 2 O–FeO–MgO–Al 2 O 3 –SiO 2 –H 2 O–TiO 2 –Fe 2 O 3 (KFMASHTO) using thermocalc and its internally consistent thermodynamic dataset constrain the effect of TiO 2 and Fe 2 O 3 on greenschist and amphibolite facies mineral equilibria in metapelites. The e...
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