“…Some traditional methods have been able to find faults by analyzing and calculating some attributes dependent on lateral discontinuities in 2D and 3D seismic images [10,11]. Many researchers have utilized different attributes for detecting faults such as the curvature [2,12], variance [13,14], semblance [4,15], coherency [10,[16][17][18], eigenstructure [17,19], fault likelihood [20], similarity [8,21,22], entropy [23], flexure [3,24,25], gradient magnitude [26], chaos [26,27] and derivatives [3,18,28,29]. In earlier research, Rijks et al presented how the azimuth and dip magnitude may reveal very tiny faults with movement substantially lower than that of a seismic wavelet [30].…”