Unsteady slip pulses under spatially-varying prestress

IF 4.8 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Earth and Planetary Science Letters Pub Date : 2024-11-06 DOI:10.1016/j.epsl.2024.119111
Anna Pomyalov, Eran Bouchbinder
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Abstract

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 Lc 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, demonstrates 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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空间变化预应力下的非稳定滑移脉冲
最近已经证实,在均匀背景/环境应力(预应力)τb条件下的自愈滑移脉冲是一种本质上不稳定的摩擦破裂模式,即它们要么随着时间t缓慢扩展,要么随着时间t缓慢衰减。此外,它们的时空动态已被证明遵循与特殊一维曲线L(c)相对应的降维描述,该曲线以τb为参数,位于由脉冲传播速度c(t)和大小L(t)定义的平面内。然而,在天然断层中,均匀预应力是例外而非规则。在此,我们研究了空间变化的预应力 τb(x)(在断层方向 x 上)对二维滑移脉冲的影响,这些滑移脉冲最初是在沿速率-状态摩擦断层的均匀 τb 条件下产生的。我们考虑了参考均匀τb周围的周期性和恒定梯度预应力分布τb(x)。对于周期性τb(x),脉冲要么持续并在 L-c 平面上形成准极限循环,要么主要沿 L(c) 曲线单调衰减,这取决于初始脉冲的不稳定指数和周期性τb(x) 的特性。对于恒定梯度的 τb(x),膨胀和衰减脉冲紧跟 L(c)曲线,由梯度的符号和大小决定小的系统偏移。我们还发现,空间变化的 τb(x) 可以恢复初始参考脉冲的膨胀/衰减性质。最后,我们表明,具有足够大小和特定符号的恒定梯度τb(x)可导致在初始脉冲的愈合尾部形成反向传播的断裂核,产生类似裂缝的双边断裂。这种脉冲到裂缝的转变以及上述效应表明,简单的空间变化预应力可以产生相当丰富的破裂动力学。此外,我们的结果表明,只要脉冲存在,它们的时空动力学就与特殊的 L(c) 曲线相关,从而为空间变化预应力下的非稳定滑移脉冲提供了有效的降维描述。
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来源期刊
Earth and Planetary Science Letters
Earth and Planetary Science Letters 地学-地球化学与地球物理
CiteScore
10.30
自引率
5.70%
发文量
475
审稿时长
2.8 months
期刊介绍: Earth and Planetary Science Letters (EPSL) is a leading journal for researchers across the entire Earth and planetary sciences community. It publishes concise, exciting, high-impact articles ("Letters") of broad interest. Its focus is on physical and chemical processes, the evolution and general properties of the Earth and planets - from their deep interiors to their atmospheres. EPSL also includes a Frontiers section, featuring invited high-profile synthesis articles by leading experts on timely topics to bring cutting-edge research to the wider community.
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