El Gassi Fm
Lithology and Thickness
The El Gassi Fm is mudstone. It overlies a transition (known as the “Zone des Alternances”) from the underlying sandstone (Klett, 2000).
Relationships and Distribution
Lower contact
It conformably overlies the Zone des Alternances Fm; which is a transition upward from the sands of the Massi Messaoud Fm into the overlying mudstone of the Argile d’El Gassi Fm
Upper contact
It is conformably overlain by the Argile d’El Gassi Fm.
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Additional Information
T.R. Klett (2000): Total Petroleum Systems of the Trias/Ghadames Province, Algeria, Tunisia, and Libya - The Tanezzuft-Oued Mya, Tanezzuft-Melrhir, and Tanezzuft-Ghadames. U.S. Geological Survey Bulletin, 2202-C.
Kraouia et al., (2023): Ordovician–Upper Silurian–Triassic Petroleum System Assessment in the Chotts Area. In S. Khomsi and F. Roure (eds.), Geology of North Africa and the Mediterranean: Sedimentary Basins and Georesources, Regional Geology Reviews, https://doi.org/10.1007/978-3-031-18747-6_7