Fig. 5From: Dating emplacement and evolution of the orogenic magmatism in the internal Western Alps: 1. The Miagliano PlutonConcordia diagram showing the results of zircon U–Pb dating of the calc-alkaline rocks. Open ellipses denote zircons form the BVS (Kapferer et al. 2012b), filled ellipses denote zircon from the Miagliano tonalite (this study). The used most concordant grain (anal. 0637-6) is indicated. Apparent upper intercept of 4,129 ± 670 Ma is meaninglessBack to article page