Normal faults are associated with rifts, where the full extension rate is typically in the range of 1-40 mm/yr (Tetreault & Buiter, 2018) and can accelerate up to 40-50 mm/yr before the breakup of the continental plate (Brune et al., 2016). The maximum slip of major continental normal fault earthquakes (CNFEs) does not exceed ∼6 m (Wells & Coppersmith, 1994) which together with slow loading produces centuries-long recurrence times for this kind of events. In this way, slow deformations and big recurrence time complicate the study of the dynamics of major CNFEs. Although normal faults have a low earthquake rate and rarely exceed the magnitude of Mw7.0 (Bignami et al., 2020;Wells & Coppersmith, 1994), they still pose a danger to highly populated areas.A few studies attempted to investigate the dynamics of CNFEs with numerical modeling (Albano