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Episodic aseismic slip in a two-degree-of-freedom block-spring model - art. no. 1681

机译:两自由度块簧模型中的偶发性抗震滑动-艺术。没有。 1681

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1] We consider a two-degree-of-freedom block-spring model, in which two blocks (Block 1 and Block 2) are connected by a spring and driven by a slowly moving driver. Assuming a rate- and state-dependent friction law, we set the friction parameters such that dynamic instability occurs at Block 1. Episodic aseismic slip occurs at Block 2 when its frictional parameters are near the stability transition. When the stress has accumulated to approximately a steady state level during an interseismic period, Block 2 starts a slow slip. Quasi-static oscillation in the stress and slip velocity occurs with decaying fluctuation amplitudes leading to the steady state values. The decaying oscillation could be a plausible generation mechanism of the episodic aseismic slip observed in the Tokai district, Japan, since 2001. We also consider various slip modes on a plate boundary based on this two-block model associated with the interaction between different frictional properties. [References: 17
机译:1]我们考虑一个两自由度的块簧模型,其中两个块(块1和块2)通过弹簧连接,并由一个缓慢移动的驱动器驱动。假设速率和状态相关的摩擦定律,我们设置摩擦参数,以便在块1处发生动态不稳定性。当块的摩擦参数接近稳定过渡时,则在块2上发生偶发抗震滑动。在间震期间,当应力累积到大约稳态水平时,块2开始缓慢滑动。应力和滑移速度的准静态振荡会随着波动幅度的衰减而产生,从而导致达到稳态值。自2001年以来,衰减振荡可能是在日本东海地区观测到的偶发性抗震滑动的可能机理。我们还基于与不同摩擦特性之间相互作用相关的这种两块模型,考虑了板块边界上的各种滑动模式。 。 [参考:17

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