
Zircon (Hf, O isotopes) as melt indicator: Melt infiltration and abundant new zircon growth within melt rich layers of granulite-facies lenses versus solid-state recrystallization in hosting amphibolite-facies gneisses (central Erzgebirge, Bohemian Massif
Keywords: UHP felsic granulites; Metamorphic zircon; Hf isotopes; O isotopes; Partial melting; Variscides;