Fig. 10From: Provenance of the Upper Cretaceous to Eocene Gosau Group around and beneath the Vienna Basin (Austria and Slovakia)Plate tectonic model for the Eastern Alps and Western Carpathians during the deposition of the Gosau Group with associated souce areas of detritus. Types of detrital garnets and chrome spinels are marked from various provenances: Grt LM low-grade metamorphosed garnets, Grt HM high-grade metamorphosed garnets, Chr H chrome spinels of mainly harzburgite-provenance, Chr L chrome spinels of mainly lherzolite-provenanceBack to article page