Fig. 12From: The Val Biandino Intrusive Suite (central Southern Alps, N Italy): new geochronological and geochemical data on the Early Permian magmatic activity in the Southalpine DomainChondrite normalized (McDonough and Sun, 1995) REE pattern of Early Permian intrusive rocks from the western (WSA), central (CSA) and eastern Southern Alps (ESA). Intrusive rocks in the central Southern Alps are basically represented by the Val Biandino Intrusive Complex and the Val Navazze Complex: their REE patterns (in colour) are compared in the diagrams with both the WSA and ESA intrusives having the same SiO2 contentBack to article page