Fig. 3
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(A) WSW-ENE geological cross section of the Mouydir Basin showing typical arch and basin architecture defined as a syncline-shaped basin with boundary secondary arches. (B) NW-SE seismic profiles of the Ahnet Basin defined as a complex shaped basin with intra-basin arches. The specific zonation of the terranes age with the arches-basins architecture is observed (see also Perron et al., 2018).
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