The goal of this work is to reveal factors which control Baoulé-Est gold occurrence. Gold traps which have been extracting from structural support have been tested by a variogram with the goal to find expect mineralized axis. Rocks with good grade and geochemistry anomalies have been inserted with the goal to find mineralized axis. Mineralized axis characteristics have led to elaborate mineralization hypothesis. Gold traps are plutonic nearbourgh quartz veins and N60°, N160°, NS faults zones junctions. N30° is the like trend of gold traps. Their geochemistry potential is setting in a triangle area draw by Dida-Kayabo, Dida-Moessou et Boorée-Ettienkro villages. Mineralization is setting by faults zones porosity. Second hypothesis gives a capital contribution to faults zones NS and N90° and N30° birimian trends. These hypotheses draw a prospect which represents 27.27% of Baoulé-Est gold occurrence.
