Fig. 12From: Formation of an intra-orogenic transtensional basin: the Neogene Wagrain basin in the Eastern AlpsModel of potential provenance in the eastern Niedere Tauern and Bösenstein areas for the Wagrain basin fill. Average K–Ar and Ar–Ar white mica ages are from Hejl (1984), Hejl et al. (1987), Abart and Martinelli (1988) and references in Pfingstl et al. (2015). Apatite fission track ages are compiled from Hejl (1997, 1998) and Reinecker (2000)Back to article page