“…The resulting complex mechanical response can be captured by empirical friction laws that employ a state variable to represent structural evolution within the fault zone (Chester, 1994; Dieterich, 1979, 1981; Ruina, 1983). The rate‐ and state‐dependent friction formulations are key to representing all stages of the seismic cycle with different rupture styles (Barbot et al., 2012, 2018, 2020, 2021; Lapusta & Barbot, 2012; Lapusta & Rice, 2003; Liu & Rice, 2005; Mei, Barbot, & Wu, 2021; Nie & Barbot, 2021; Sathiakumar & Barbot, 2021; Shi et al., 2020; Veedu & Barbot, 2016) and recurrence patterns (Cattania, 2019; Nie & Barbot, 2022).…”