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Fig. 7


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 Wedge-top Neogene basins of the Mesorif. (A) Geological map of the Abra Taourirt-Taounate basins area. Location of the seismic cross-sections (B) and (D) is given on (A). (B, D) Two seismic cross-sections from the Taounate Basin, from Samaka (1999). The sections are roughly perpendicular to illustrate the bias that can exist if one only looks at the NNE-SSW to NE-SW sections. (C, E) Neogene interpretation of the two seismic cross-sections (B) and (D), respectively. This is mostly based on the interpretations by Samaka et al. (1997) and Capella et al. (2017) given they propose a similar subdivision for the Neogene infill, divided into two main sequences. Blue faults show the first normal motion along the faults, whereas black lines show the inverse posterior motion.

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