Fig. 9From: Banded amphibolites in the Alps: a new interpretation in relation to early Paleozoic peraluminous magmatismPercentages of mafic (indicated by numbers), intermediate and felsic intrusiva in batholiths of three different settings: (i) island arc, (ii) continental arc and (iii) subduction–accretion complex. Data are from Villaseca et al. (1998), Hauser and Zurbriggen (1994) for the Fusht Complex, and Zurbriggen (2015) for the Strona-Ceneri ZoneBack to article page