“…When RA, that is, the ratio of rise-time to the peak amplitude, is greater than the AF, that is, the average frequency given by the ratio of hit count by event duration, the AE event source is originated by a shear crack, and for the converse, it is a tensile crack [23,40]. Researchers have used the AF-RA crack classification concept for characterizing the AE source mechanism under different loading conditions on different types of rocks, such as sandstone, granite, diorite, and marble, as well as plain and reinforced concrete [5,23,27,30,40,41,42,49].…”