The Mid-Albian unconformity, a key to understand the geodynamics of the North Pyrenean Trough

Open Access

Fig. 2

N–S cross-section of the Mauléon basin at the beginning of the Late Cretaceous. The model, taken from Lavier and Manatschal (2006) deals with a 30-km thick crust and a ductile decoupling middle crust. The upper crust includes the pre-rift Fms (after Masini, 2011).

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