Argileux Fm
Type Locality and Naming
Named after the facies
Synonym: Claystone Fm (translation of the French)
References: Hallett, 2002; Bora and Dubey, 2015; Benvegnù, 2020
Lithology and Thickness
This succession is related to ice-sheet retreat and global sea-level rise and corresponds to a transgressive system tract during which a layer of graptolitic black shales was deposited. It is the lateral equivalent of the Tanezuft Fm. and consists of dark micaceous siltstone with interbedded sandstone. In the lowermost part, this formation is also made by radioactive shales due to the presence of uranium transported by wind as volcanic ash. The upper part is characterized by a thick siltstone member showing hummocky cross-stratification separated by hardgrounds, probably representing tempestite deposits (Hallett, 2002).
Relationships and Distribution
Lower contact
It conformably overlies the Gara Louki Fm.
Upper contact
It is conformably overlain by the F6 Fm.
Regional extent
[Just Illizi-Ghadames merger given in this GeoJSON pending making a larger one.]
GeoJSON
Fossils
Age
Depositional setting
Additional Information
T.R. Klett (2000): Province, Algeria, Tunisia, and Libya - The Tanezzuft-Oued Mya, Tanezzuft-Melrhir, and Tanezzuft-Ghadames. U.S. Geological Survey Bulletin, 2202-C.