Quartzites de Hamra Fm
Type Locality and Naming
Synonym: Grès de Ouargla (Klett, 2000); Ouargla Fm
References: Klett, 2000.
Lithology and Thickness
The Quartzites de Hamra Fm. is made entirely of sandstones (Klett, 2000). Equivalent to the lower part of the Hamra Fm of the Illizi Basin and lower part of the Hawaz Fm (Haouaz Fm) of the Ghadames Basin (Klett, 2000).
Relationships and Distribution
Lower contact
It conformably overlies the Gres de’El Atchane Fm.
Upper contact
It is conformably overlain by the Gres de Ouargla 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