Oleki Fm
Type Locality and Naming
Mount Oleki at about 60 km NW of Séguédine (Type section stratigraphy in Fig. 2); named by Faure, 1966, p. 257, 258, 274, 285.
References: Faure, 1966; Fabre et al., 1983;
Synonym: Formation de l’Oleki
Equivalent(s): The combined Tiffa Fm, Cheffadène Fm, Arentigué Fm, Séguédine Fm and Emi-Bao Fm at the center of the Bilma Sub-Basin, as well as the combined Achegour Fm, Exerza Fm, Zoo Baba Fm, Kafra Fm and Bilma Fm in the south of the Bilma Sub-Basin (Fig. 1).
[Figure 1. Representative diagram of the facies variations towards the North of the Bilma basin (Faure, 1966, p. 281). The Oleki Fm would be to the right, where all the facies come together.]
Lithology and Thickness
Continental formation comprising coarse sandstones with conglomerate levels and kaolinitic siltstones with coarse quartz. The stratification is lenticular or cross-bedded. Thickness is 164 m at the type locality (Fig. 2)
[Figure 2. Lithological succession of the Oleki Fm at the type locality (Faure, 1966, p. 259).]
Relationships and Distribution
Lower contact
Precambrian is below
Upper contact
Overlain by Chad Fm
Regional extent
See Fig. 1
GeoJSON
Fossils
Age
Depositional setting
Continental
Additional Information