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Fig. 14


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Alternative models (A/B) accounting for the occurrence of the BBMs between the Filali and Beni Bousera units. A: Triassic unconformable sedimentation onto the exhumed kinzigites (lower crust). B: Triassic-Early Jurassic extensional allochthons (rafts) emplaced onto the exhumed kinzigites.

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