Fig. 21
From: The North Penninic Bündnerschiefer and Flysch of the Prättigau (Swiss Alps) revisited
Comparison of structural and metamorphic data for reconstructing the Cenozoic basin and tectonic deformation history of the North Penninic Tomül nappe in the Prättigau half-window. Exhumation/cooling rates in the relevant tectonic units according to Price et al. (2018): ZHe = (U-Th)/He; ZTF = zircon fission traces (Atemp. = approximate annealing temperatures). See text for further details