“…1). The Birimian terranes, which make up the Baoulé-Mossi domain and the Kédougou inlier, consist of narrow sedimentary basins and linear to arcuate volcanic belts intruded by several generations of granitoids (Leube et al, 1990;Doumbia et al, 1998;Gasquet et al, 2003;Dioh et al, 2006). They correspond to a period of accretion during the Eburnean orogeny around 2.0 Ga (Abouchami et al, 1990;Boher et al, 1992;Taylor et al, 1992).…”