Fig. 2From: Geology and stratigraphy of the Neogene section along the Oued Beth between Dar bel Hamri and El Kansera (Rharb Basin, northwestern Morocco) and its otolith-based fish fauna: a faunal inventory for the Early Pliocene remigration into the MediterraneanGeological map of the studied area from Dar bel Hamri to El Kansera resulting from a review of my master thesis (1977), and highlighting sections sampled. The location of the subsurface Sidi Fili fault and Nappe Prérifaine front are extrapolated from Tilloy (1952) and the postulated extension of the Kenitra-Sidi Slimane fault is from Zouhri et al. (2002)Back to article page