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The Medjez-el-Bab (MEB) box anticline, northern Tunisia, gives new evidence allowing us to precise the tectonic agenda of the North African paleo-margin inversion. On the one hand, the examination of this structure permits us to show that the inversion began approximately by the transition between the Lower and Upper Senonian. On the other hand, it highlights the occurrence of a Middle-to-Late Eocene...
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