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Fig. 12


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Interpreted view of the Soum de Ségu area, close to the Les Pernes lherzolite massif. Note that the Cenomanian carbonate flysch overlies unconformably the eroded Jurassic and Early Cretaceous limestones and marls without any internal deformation of this mesozoic cover during the mid-cretaceous crust extension and mantle exhumation stage.

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