Fig. 10From: Banded amphibolites in the Alps: a new interpretation in relation to early Paleozoic peraluminous magmatismA-B diagram (Debon and Le Fort 1988) with indicated sources of material and heat and magmatic processes (as listed with references in Table 3) for the genesis of peraluminous arc magmatism in subduction–accretion-complexes. For explanations see textBack to article page