“…Many researchers correlate AE counts to inelastic strain rates in rocks prior to failure [Boyce et al, 1981, Lockner et al, 1992. Other studies localize AE to demonstrate clustering, quantify material damage, and elucidate hysteresis [Berkovits and Fang, 1995, Godin et al, 2004, Iturrioz et al, 2019, Meng et al, 2016, Shah and Labuz, 1995, Sondergeld and Estey, 1981, and some even use AE to identify field scale fracture zones [Soma et al, 2002]. AE locations and magnitudes have shed light on heterogeneity controlled rock failures [Lei et al, 2004].…”