Fig. 6From: The Val Biandino Intrusive Suite (central Southern Alps, N Italy): new geochronological and geochemical data on the Early Permian magmatic activity in the Southalpine Domaina The typical porphyric texture of the VSBG granite as it appears in outcrops; b) The VSBG intruding Variscan basement NW of the SRNF (Fig. 2); c Myrmekites developed at the contacts between K-feldspar and plagioclase crystals; d detail of figure cBack to article page