Fig. 2From: Variscan granitoids of the East Serbian Carpatho-Balkanides: new insight inferred from U–Pb zircon ages and geochemical dataPetrographic characteristics in thin-section. a Brittlely deformed microcline with cracks filled with secondary recrystallized quartz and K-feldspar (NR-25). b Texture evidencing syn-kinematic crystallization with ductilely deformed feldspar and muscovite (ZI-3, inset ZI-5). c Syn-kinematically grown feldspar and mica surrounded by fine-grained aggregates of secondary recrystallized quartz (RD-35). d Equigranular syenodiorite from the Janja massif (JN-43) containing large (~ 0.5 mm) allanite with epidote overgrowths (arrow); the insets show similar allanite from Ravno Bučje (lower inset; RB-37) and allanite and apatite (arrows) crystals from Aldinac (upper inset; AL-7)Back to article page