Agadem Fm
Type Locality and Naming
Massif of Agadem. Seen by G. Rohlfs in 1868, found in 1941 by Chief Warrant Officer Gobin, studied by R. Furon (1942) and Ph. Renault in 1954. Furon (1942), emend. Faure (1954, 1966).
References: Furon, 1942; Faure, 1954, 1966; Faure et al., 1956; Fabre et al., 1983.
Synonym: Série d’Agadem; Formation d’Agadem; Equivalent(s): Kafra Fm.
Lithology and Thickness
At the top, gypsum clays and fine sandstone, sometimes with glauconite; at the base, fine red or white sandstone, with cross-bedded stratifications with marine lamellibranchs. 100 m thickness.
Relationships and Distribution
Lower contact
Underlying unit is the Zoo Baba Fm
Upper contact
Overlying unit is the Galhama Fm
Regional extent
In the Dibella, Agadem, Bilma Regions
GeoJSON
Fossils
Ammonites (Hoplitoides and Metengonoceras). Lamellibranchs such as Fragum subperobliquum ν. Koenen, Parmicorbula incurvata, etc. (Fig. 1)
[Figure 1: General disposition of the sedimentary formations in the Agadem Massif. Ŧ = Fossils. (Faure, 1966)]
Age
Depositional setting
Marine
Additional Information