Fig. 17
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Superimposed unconformities in the Babors massif (location: Fig. 11). A: Present cross-section presented by Obert (1974) as a proof of Early and Late Cretaceous folding events, involving overturned pre-Cenomanian folding. B: Restoration of two stages of the structural evolution of the area, suggesting progressive ascent of a diapir of Triassic evaporitic formations.
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