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Pseudomorphs of melt-filled pores, recognized by their generally cuspate shape, are used as diagnostic for the former presence of partial melt. They are commonly observed in migmatites from the mid- to deep crust although they occur in the smaller pores in migmatites from shallower levels (1–2 kbar). The pseudomorphing of melt-filled pores is controlled by the kinetics of nucleation and is a conse...

On the Pseudomorphing of Melt-filled Pores During the Crystallization of Migmatites