This study was carried out with the aim of clarifying the lithostratigraphy of the Dougbafla –Bandama area located in the southern part of the Birimian belt of Fettékro, in the center-West of Côte d’Ivoire. The vertical succession of these formations can be summarized at the base by volcanic rocks (basaltic and andesitic) mainly basalts, with in intermediate positions several successive volcaniclastic flows of autobrechic type and at the top by Various sedimentary lithologies usually composed of black schists or a more modest volume of sericite or chlorite schists capped with quartzites. These various shales sometimes play an important role of transition between lithologies. This complex is intersected by intrusions (granites, granophyres, granodiorites, tonalites, epidiorites, microgranodiorites, microdiorites, lamprophyres) and several generations of veins and quartz veinlets.
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