Boulakoura Fm
Type Locality and Naming
Upper portion of the Koutous Plateau, Damergou
[Figure 1: The Boulakoura Formation on the upper portion of the Koutous Plateau, Damergou (Faure, 1966, page 350)]
References: Faure, 1966; Gavaud, 1975; Fabre et al., 1983.
Synonym: "Bella Kora" Fm; Boulakoura Fm. Equivalent(s): The oolite pebbles caught in a Quaternary ferruginous cuirass of the Zaouzaoua Fm (Damergou) and Boulakoura Fm (Koutous) are remnants of the erosion of the Ader Doutchi Fm (Ct1)
Lithology and Thickness
Pebbles and blocks of continental origin cemented by iron oxide. The blocks contain ferruginous oolites identical to the Dollé Fm and Homodji Fm. This leads Faure (1966) to think that the ferruginous oolitic formation extended above the Koutous before being dismantled and rearranged in the terraces of the Early Quaternary. Its thickness is about 2 to 4 m.
Relationships and Distribution
Lower contact
Underlying unit is the Koutous Gr
Upper contact
Overlain by Quaternary
Regional extent
Iullemmeden Basin - South Damergou and Koutous
GeoJSON
Fossils
None
Age
Depositional setting
Continental
Additional Information