Fig. 2From: The relation between peak metamorphic temperatures and subsequent cooling during continent–continent collision (western Central Alps, Switzerland)Summary of the major tectonic events in the study area. Left column: the major events summarized in a given deformation phase; central column: selected literature names for the shown phases; right column: schematic sketch of the deformation; light gray: Doldenhorn Nappe, intermediate gray Upper Helvetic nappes, black: Gotthard Nappe, diagonal hatches: Penninic units. The deformation phases are sorted in relation to their structural overprint relationships, but the geodynamic processes are continuousBack to article page