It has been recently established that self-healing slip pulses under uniform background/ambient stress (prestress) τb are intrinsically unstable frictional rupture modes, i.e., they either slowly expand or decay with time t. Furthermore, their spatiotemporal dynamics have been shown to follow a reduced-dimensionality description corresponding to a special one-dimensional curve L(c), parameterized by τb, in a plane defined by the pulse propagation velocity c(t) and size L(t). Yet, uniform prestress is rather the exception than the rule in natural faults. Here, we study the effects of a spatially-varying prestress τb(x) (in the fault direction x) on 2D slip pulses, initially generated under a uniform τb along a rate-and-state friction fault. We consider both periodic and constant-gradient prestress distributions τb(x) around the reference uniform τb. For a periodic τb(x), pulses either sustain and form quasi-limit cycles in the L−c plane or decay predominantly monotonically along the L(c) curve depending on the instability index of the initial pulse and the properties of the periodic τb(x). For a constant-gradient τb(x), expanding and decaying pulses closely follow the L(c) curve, with small systematic shifts determined by the sign and magnitude of the gradient. We also find that a spatially-varying τb(x) can revert the expanding/decaying nature of the initial reference pulse. Finally, we show that a constant-gradient τb(x), of sufficient magnitude and specific sign, can lead to the nucleation of a back-propagating rupture at the healing tail of the initial pulse, generating a bilateral crack-like rupture. This pulse-to-crack transition, along with the above-described effects, demonstrate that rather rich rupture dynamics can emerge from a simple, spatially-varying prestress. Furthermore, our results show that as long as pulses exist, their spatiotemporal dynamics are related to the special L(c) curve, providing an effective, reduced-dimensionality description of unsteady slip pulses under spatially-varying prestress.
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