“…The orientations frequency and cumulative lengths are in the case of the visible fracture map, respectively, 16.4% for 1426.7 km, 14.6% for 1276.8 km and 8.8% for 773.9 km, in the case of the infrared fracture map respectively 16.2% for 1928.5 km, 6.8% for 805.6 km and 8.1% for 967.8 km and finally in the case of the PALSAR fracture map respectively 18.2% for 6024.9 km, 11.8% for 3916.4 km and 15.7% for 5216.5 km. The N10-N20 and N180 represent a significant orientation in the central area of Benin republic especially the Kandi Shear Zone (KSZ) related to the pan-African orogenic cycle as recognized by many authors (Breda, 1985, Adissin Glodji, 2012and Alhassane & al., 2018. Further, it characterizes the crystallophyllian orientation of schistose green rocks, gneisses (NS to NNE-SSW, NNW-SSE), migmatites, and the extension of granite and spilite-keratophyre massifs (Boukari, 1982, Breda, 1989, Akokponhoué & al., 2019and Oussou & al., 2019.…”