牛志仁, 陈党民. 1987: 含有单-粗糙面的走滑断层的滑动弱化不稳定性h. 地震学报, 9(3): 253-265.
引用本文: 牛志仁, 陈党民. 1987: 含有单-粗糙面的走滑断层的滑动弱化不稳定性h. 地震学报, 9(3): 253-265.
NIU ZHIREN, CHEN DANGMIN h. 1987: SLIP-WEAKENING INSTABILITY ON A STRIKE-SLIP FAULT WITH ASPERITY. Acta Seismologica Sinica, 9(3): 253-265.
Citation: NIU ZHIREN, CHEN DANGMIN h. 1987: SLIP-WEAKENING INSTABILITY ON A STRIKE-SLIP FAULT WITH ASPERITY. Acta Seismologica Sinica, 9(3): 253-265.

含有单-粗糙面的走滑断层的滑动弱化不稳定性h

SLIP-WEAKENING INSTABILITY ON A STRIKE-SLIP FAULT WITH ASPERITY

  • 摘要: 本文研究了有限长度含有单一粗糙面的垂直走滑断层的滑动弱化不稳定性.我们假定断层强度在其深度方向是均匀的,而在走滑方向是不均匀的,即存在一个高强度段.并假定断层上的粗糙段及断层上的其它部分具有相同类型的本构律,只是峰值应力不同.断层周围的地壳材料用上、下表面应力自由的弹性平板来模拟.我们用有限元方法研究了理论位移场、应力场和应变场随远场位移的演变情况.此时,断层位移和摩擦应力并不是预先给定的,而是在求解过程中同时确定的.根据计算结果,我们比较了理论位移场及断层上摩擦应力分布在稳定和不稳定滑动情况时的差别.并与内部含有低强度段的走滑断层的场合做了比较.

     

    Abstract: In this paper, we have studied the slip-weakening instability on a finite and vertical strike-slip fault with asperity. We assumed that the fault strength is uniform in depth, but the strength is non-uniform in the strike direction, i.e., there is asperity on the fault. The segments with and without asperity of the fault follow the same type of constitutive law, but have different peak stresses. The material surrounding the fault is represented by elastic plates whose upper-surface and bottom are stress-free. We use finite element method to study the evolution of theoretical displacement, stress and strain fields that vary with a remote displacement. When the displacement and frictional stress are not given in advance but are determined in the solving process. According to the results, we have compared the differences of theoretical displacement and the distribution of frictional stress on the fault between stable and unstable slip. In addition, we have compared the results in this paper with known results for the strike-slip fault with a segment of lower strength.

     

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