A. Geological cross-section oriented parallel to the Pyrenean shortening direction, in order to show the Pyrenean thrusting and folding in the upper crust. See location on Figure 2. B: Restored section in a late Cretaceous/pre-Pyrenean state, showing the localization of the EW oriented thrusts above structures inherited from the Durancian uplift event and/or Late Cretaceous differential subsidence.