Fig. 11

Simplified geological map of the Eastern Alps (east of Innsbruck) after Egger et al. (1999). Highlighted Austroalpine crystalline complexes are supposed to be the source area for Paleogene almandine-rich garnets of the Gosau Group in the study area (grey colored units include the Rhenodanubian Flysch Zone, the Greywacke Zone, the Graz Palaeozoic, the Drau Range and the Male Karpaty Mountains in Slovakia; see also Schmid et al. 2004)