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The authors have pointed out certain discovered facts related to statistical analysis of near fault earthquakes. Directivity effect occurs when the harmonic mean of the velocity of the fault rupture propagation towards a site varies from that of the shear velocity of the rock near the source by a constant factor. The geometric mean of the combined fling effects bears a relation among the individual geometric mean of strike-slip and dip-slip faults, the individual and total number of observeddoi:10.5120/ijca2017915190 fatcat:xfnhndkgkvcnplv6272e2t74zu