Tamamaït Fm
Type Locality and Naming
Group/Subgroup: Upper Izégouandane Gr
References: Faure, 1966; Valsardieu, 1971; Fabre et al., 1983; Fabre, 2005.
Synonym: Tamamait Fm
Lithology and Thickness
It includes several lower-order sequences made up of fine sandstones with calcareous cement and clays. The sandstone channels take an NW or NE direction. The Formation consists of two characteristic beds of medium to fine sandstone, pink in color, feldspathic, and numerous small pebbles of brown argillites. Limestone cement is very abundant. A layer of silty clay with fine sandstone lenses and clayey micro-conglomerates with clay pebbles is interposed between the two beds. The thickness of the layers is regular in the N-W of the flexure of Izeretagen, where the whole of the three levels reaches about forty meters of thickness. In the Aokaré region, the sand-argillite sequences proliferate. At the edge of the Aïr, to the S-E of the Madaouela flexure, the sandstone of the Tamamaït Fm is coarser, and the beds' regularity no longer exists. In all cases, the Tamamaït Fm is characterized by the abundance of fine to medium sandstone, with isogranular tendency, with calcareous cement, of gray or pink tint, with limestone slabs and oblique stratifications. 80 m thick.
Relationships and Distribution
Lower contact
Is either on the Téjia Fm or the Izégouande Fm
Upper contact
Overlain by the Moradi Fm
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Continental fluvio-lacustrine
Additional Information