Solving the dynamic rupture problem with different numerical approaches and constitutive laws

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Comparison of finite difference and boundary integral solutions to three‐dimensional spontaneous rupture (2005, methodology): “Bizzarri et al. [2001] made similar comparisons of finite difference and BI solutions to 2-D rupture problems.”
Earthquake ruptures with thermal weakening and the operation of major faults at low overall stress levels (2009, background): “Under such circumstances, ruptures that are nucleated in one of these regions can propagate into low-stressed regions [Perrin et al., 1995; Zheng and Rice, 1998; Bizzarri et al., 2001].”
Slip‐weakening behavior during the propagation of dynamic ruptures obeying rate‐ and state‐dependent friction laws (2003, methodology): “Bizzarri et al. [2001] discussed these relations in detail.”