Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6349947 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2014 | 23 Pages |
Abstract
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.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Sami Riahi, Alfred Uchman, Dorrik Stow, Mohamed Soussi, Kmar Ben Ismail Lattrache,