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The dynamic simulation of ground motion of Lushan earthquake by finite element method

机译:有限元法通过有限元方法动态仿真庐山地震地震

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In this paper, the finite element method with 6-node pentahedral elements will be applied to simulate the strong ground motion due to the Lushan earthquake fault dynamic rupture. In order to approximate the geophysics conditions in the region near the Lushan earthquake structure and the frictional fact along the Lushan earthquake fault plane, the layer model with different P and S wave velocities and the slip-weaken constitutive will be considered in the construction of finite element model corresponding to the Lushan earthquake fault. For validating the lastly computational result, the comparison between the calculation results and the stations records will be carried out. Basing on the above research achievements, the theoretical ground motion maps for the variation of east-west velocity component of ground motion in the earthquake process will be shown. Furthermore, for studying the correlations between the ground motion and the distribution of landslides brought by Lushan earthquake, we will simply analyze and summary the temporal and spatial distribution of ground motion caused by the Lushan earthquake. Just as the record data shown, the simulation result also shows the effect of hanging wall of fault is not so obvious, which maybe stems from the special characters of motion of blind-thrust fault during the earthquake rupture process.
机译:本文将应用具有6节 - 节点五光面元素的有限元方法来模拟由于庐山地震故障动态破裂而产生的强大的地面运动。为了近似庐山地震结构附近的地球物理条件和沿着庐山地震破坏平面的摩擦事实,在有限的构建中将考虑具有不同P和S波速度的层模型和滑动削弱的构成型。元素模型对应庐山地震故障。为了验证最后计算结果,将执行计算结果与站记录之间的比较。基于上述研究成果,将显示出地震过程中地区运动的东西速度分量变化的理论地面运动图。此外,为了研究地面运动和庐山地震所带来的滑坡之间的相关性,我们将简单地分析和概述由庐山地震引起的地面运动的时间和空间分布。正如所示的记录数据一样,仿真结果也显示了悬挂墙壁的效果并不是那么明显,这可能是在地震破裂过程中盲推扰故障运动的特殊特征。

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