Fig. 3From: The Morcles microgranite (Aiguilles Rouges, Swiss Alps): geochronological and geochemical evidences for a common origin with the Vallorcine intrusionHarker diagrams of selected chemical elements for the Morcles microgranite (this study and Meisser 2003) compared to literature data for other contemporaneous intrusive bodies: the Dorénaz basal dacite (Pilloud 1991; Capuzzo and Bussy 2000; Mollex 2003), the Aiguilles Rouges rhyolites (Capuzzo and Bussy 2000; Meisser 2003), the Fully granodiorite (Mollex 2003), and the Vallorcine “D” and “H” granites (Brändlein 1991; Brändlein et al. 1994; Meisser 2003)Back to article page