Deep-sea trace fossils of the Oligocene-Miocene Numidian Formation, northern Tunisia

The second domain includes the NE part of Mogod Mountain (e.g. the Ras El Korane, Jebel Gattous-Zoukar), which exhibit more proximal characteristics compatible with a probable slope canyon interpretation. The southern margin of the Kroumirie (Balta and Zouza areas) and Sejnene area shows a distal setting compared with the Ras El Korane and Jebel Gattous-Zoukar areas. It is ascribed to a mid- to upper slope depositional environment during the Oligocene to early Miocene.