Schematic south-north crustal profiles along the ECORS (“Étude Continentale et Océanique par Réflexion et Réfraction Sismique”) section showing the geodynamic evolution of the eastern Pyrenees from the Cenomanian to the early Campanian (modified from Mouthereau et al., 2014). No vertical exaggeration. Decompacted sedimentation rates and accommodation rates are calculated from sources listed in Table 2 for paleogeographic domains defined in this study.