Fig. 4From: The Val Biandino Intrusive Suite (central Southern Alps, N Italy): new geochronological and geochemical data on the Early Permian magmatic activity in the Southalpine DomainField aspect of the VBQD intrusive rocks. a Leucocratic granitic dike intruding the Variscan basement just S of Rif. Grassi (Fig. 2); b The quartz-diorite of stock A (Fig. 2) as observable in the field; c Quartz-diorite of stock D (Fig. 2) intruding the basement paragneiss with apophyses of the main body that crosscut the regional foliation and sills of a few mm in thickness that expand along the foliation planes; d Basement xenoliths in the VBQD granodiorite (sample VBZ32, Fig. 2) that is in turn included in a granite dikeBack to article page