During the last decade, seismicity in the central USA, and particularly in Oklahoma and Kansas, drastically increased due to the rapid development of unconventional oil and gas fields (Ellsworth, 2013;Ellsworth et al., 2015;Rubinstein et al., 2018). The primary cause of the elevated seismicity rates is the underground injection of large volumes of wastewater that are a byproduct of the oil and gas production (Ellsworth et al., 2015;Walsh & Zoback, 2015;Weingarten et al., 2015). The injection of large volumes of wastewater results in perturbations of the pore fluid pressure and changes in local stress conditions in the vicinity of the wells and beyond. Over time and due to extremely large volumes injected, this led to downward migration of fluids, partly along preexisting fractures, and ultimately to the reactivation of critically stressed faults deeper in the crystalline basement (e.g., McNamara et al., 2015;Rubinstein & Mahani, 2015). As seismicity occurred at larger (>10 km) distances from the main wastewater disposal area, stress transfer