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Fig. 3 | Swiss Journal of Geosciences

Fig. 3

From: The Morcles microgranite (Aiguilles Rouges, Swiss Alps): geochronological and geochemical evidences for a common origin with the Vallorcine intrusion

Fig. 3

Harker 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)

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