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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Dynamic rupture on a material interface with spontaneous generation of plastic strain in the bulk
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Dynamic rupture on a material interface with spontaneous generation of plastic strain in the bulk

机译:材料界面上的动态破裂,自发产生塑性应变

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We discuss 2D simulations of in-plane ruptures on a fault between different solids in a model that includes dynamic generation of plastic strain off the fault. The fault is governed by a regularized friction with a gradual response to abrupt changes of normal stress, while plastic strain in the bulk is governed by a Coulomb yielding criterion. The occurrence of off-fault damage stabilizes the slip velocity on the fault. Stable self-sustaining ruptures propagate on the material interface as narrow unidirectional pulses in the direction of slip on the more compliant side of the fault. Plastic strain is generated only on the stiffer side of the fault (the tensional quadrant in the direction of rupture propagation) in a strip of approximately constant width that is correlated with the slip velocity on the fault. Simulations for various values of confining normal stress, material contrast and cohesion in the bulk suggest that significant generation of off-fault damage is limited to conditions that correspond to the top few kilometers of the crust. The results are compatible with field observations of shallow asymmetric damage patterns in the structure of several large faults. (c) 2005 Elsevier B.V. All rights reserved.
机译:我们在模型中讨论了不同实体之间的断层上平面破裂的二维模拟,该模型包括动态产生断层塑性应变。断层由规则的摩擦控制,并逐渐响应法向应力的突然变化,而大块中的塑性应变则由库仑屈服准则控制。断层损坏的发生稳定了断层上的滑动速度。稳定的自我维持断裂在材料界面上以窄单向脉冲的形式在断层较顺应侧的滑动方向上传播。塑性应变仅在断层较硬的一侧(断裂传播方向上的拉力象限)以近似恒定宽度的条带生成,该宽度与断层的滑动速度相关。对散装法向应力,材料对比度和内聚力的各种值的模拟表明,断层破坏的显着产生仅限于与地壳顶部几公里相对应的条件。该结果与几个大型断层结构中的浅层非对称破坏模式的现场观测结果相符。 (c)2005 Elsevier B.V.保留所有权利。

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