2. The highest grades of regional metamorphism of mica schists are commonly associated with abund...
2. The highest grades of regional metamorphism of mica schists are commonly associated with abundant granite. The accompanying map 2 illustrates the distribution of granite and some mineral assemblages common in pelitic schists: e: Qtz + Ms+ Pl+ Bt+ Grt+Sil f: Qtz +Pl + Kfs+ Grt+Sil g: Qtz+ Pl + Kfs +Grt + Ky a: Qtz+ Ms+PI+St+ Bt + And b: Qtz+ Ms+Pl+ St + Bt+ Grt c: Qtz + Ms +Pl+ Bt+Grt d: Qtz + Ms+Pl+St +Bt+ Sil The stability fields of these mineral assemblages are illustrated on the P-T diagram. The upper stability of Qtz + Ms +St extends through all three fields for aluminum silicate polymorphs. The upper stability of Qtz +Ms changes to a reaction limiting Qtz+ Ms + Pl. Assume that St is exhausted first at the low temperature rxn curve, and Ms is exhausted first at the high temperature rxn curve for the bulk composition represented by this phase diagram.