Fig. 9From: Late Palaeozoic tectonics in Central Mediterranean: a reappraisala Calabria upper crust phyllites and metasandstones of the low grade unit of Stilo-Bivongi (Fiumara di Stilaro); b microscopic fabric of phyllite samples collected close to Bivongi village. S1 foliation in phyllite is parallel to axial plane of folds affecting S0 layering; c decimetre-thick granodioritic dyke within the low-grade host rock close to the margin of the Serre batholith near Stilo; d spotted schist in the aureola of Serre batholith near Stilo (see details Festa et al. 2013)Back to article page