Madama Fm
Type Locality and Naming
Subsurface in Termit Sub-Basin
References: Lai et al., 2018; Lai et al., 2019; Ahmed et al., 2020;
Synonym: Madama reservoir; Madama sandstone. Not to confuse with the Carboniferous “Grès/Série de Madama” described below.
Equivalent(s): This sub-surface Formation correlates with surface formations of the lower part of the Termit Fm, the lower part of the Galhama Fm, the lower part of the Bilma Fm, and the lower part of the Emi-Bao Fm.
Lithology and Thickness
Massive sandstones with a thin layer of muddy sandstones and coal seam. Well data revealed that it has top reservoir quality with 25%-35% porosity and suitable reservoir property in its upper 100-200 m thick sandstone. Its lower sequence of alternating sandstone and shale has some oil shows. The Madama Formation only has one third-order sequence, namely, MSQ1 (Figure). Thickness: Exceeds 300 m in the Termit Sub-Basin and can reach 1500 m in the Ténéré Sub-Basin.
[Figure. Generalized stratigraphic column and sequence division of the Madama Formation of the Termit Sub-Basin (Source: Lai et al., 2018).]
Relationships and Distribution
Lower contact
Underlying unit is the Yogou Fm
Upper contact
Overlying unit is the Sokor 1 Fm
Regional extent
Seen only in the subsurface of Termit and Ténéré Sub-basins
GeoJSON
Fossils
Age
Depositional setting
The facies is a stack of braided delta channels associated with a continental fluvial/alluvial deposit.
Additional Information