刘奕君,李小军,赵晓芬,徐超,温增平. 2023. 2014年云南鲁甸MW6.1地震强地面运动模拟. 地震学报,45(0):1−18. doi: 10.11939/jass.20220216
引用本文: 刘奕君,李小军,赵晓芬,徐超,温增平. 2023. 2014年云南鲁甸MW6.1地震强地面运动模拟. 地震学报,45(0):1−18. doi: 10.11939/jass.20220216
Liu Y J,Li X J,Zhao X F,Xu C,Wen Z P. 2023. Strong ground motion simulation for the 2014 MW6.1 Ludian,Yunnan earthquake. Acta Seismologica Sinica45(0):1−18. doi: 10.11939/jass.20220216
Citation: Liu Y J,Li X J,Zhao X F,Xu C,Wen Z P. 2023. Strong ground motion simulation for the 2014 MW6.1 Ludian,Yunnan earthquake. Acta Seismologica Sinica45(0):1−18. doi: 10.11939/jass.20220216

2014年云南鲁甸MW6.1地震强地面运动模拟

Strong ground motion simulation for the 2014 MW6.1 Ludian,Yunnan earthquake

  • 摘要: 基于震源运动学模型,采用宽频带混合模拟方法,对鲁甸地震开展了考虑复杂震源破裂过程的地震动模拟,将代表性场点的模拟结果与实际观测的强震记录进行对比研究,分析了不同震源模型对场点强地面运动特征影响的差异。研究表明:就震源尺度有限的中等地震而言,地震矩相近的不同震源破裂模型对震中距稍远场点的地震动影响差异相对较小,而对近震源区场点的地震动特征影响差异较为明显。另外,得出的不同震源模型模拟的地震动参数空间分布结果显示,不同震源模型对地震动空间分布形态有显著影响。因此,精细的震源模型对合理估计近震源区地震动特征及近震源区地震危险性具有重要价值。

     

    Abstract: Considering the complex source rupture process from Zhang Yong (2015), the hybrid broadband simulation method was applied to synthesize the ground motions for the Ludian earthquake based on kinematic source model. The simulation results of representative sites were compared with the observed strong motion recordings, and impacts from three different source rupture models on strong ground motions were analyzed. The results show that for moderate earthquakes with limited fault dimension, the differences of strong ground motion characteristics among different source rupture models with the similar seismic moment are not obvious in the far fields, but are distinct in the near-fields. In addition, the distributions of intensity measurements of ground motions are given, and it is found that source rupture model plays an important role in the spatial distribution pattern of strong ground motions and strong ground motion characteristics. Therefore, the elaborate source rupture models are very important to estimate the strong ground motion characteristics and seismic hazard analysis in the near field.

     

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