Introduction. This paper provides an analysis of lower Cretaceous (Aptian) strata in central Tunisia, using 2D seismic data and well logs. The study area (Fig. 1B) is characterized by east-, northwest- and northeast-trending fold belts verging to the south and bordered by strike-slip fault systems (e.g., Zargouni, 1985, Zouari et al., 1990, Boukadi, 1994, Bédir, 1995, Zitouni, 1997, …
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