考虑地形影响和震源动力学过程的2021年漾濞MS6.4地震强地面运动数值模拟
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作者单位:

1.云南地震局, 云南 昆明 650041 ;2.中国科学院大学地球与行星科学学院, 北京 100049 ;3.地球系统数值模拟与应用国家重点实验室, 北京 100049 ;4.中国科学院计算地球动力学重点实验室, 北京 100049

作者简介:

王珏(1978-),女,硕士,工程师,主要从事地震危险性分析和地球动力学数值模拟研究。E-mail:wjnms@126.com。

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中图分类号:

P315

基金项目:

云南省地震局自立科研项目(漾濞地震专项)(2021YBZX16);国家自然科学基金面上项目(42374116);中央高校基本科研业务费专项资金(E2ET0413X2);云南省地震科技创新团队(CXTD202402)


Numerical simulation of strong ground motion for the 2021 Yangbi MS6.4 earthquake considering topographic effects and dynamic rupture process
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1.Yunnan Earthquake Agency, Kunming 650041 , Yunnan, China ; 2.College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049 , China ; 3.State Key Laboratory of Earth System Numerical Modeling and Application, Beijing 100049 , China ;4.Key Laboratory of Computational Geodynamics, CAS, Beijing 100049 , China

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    摘要:

    2021年云南漾濞MS6.4地震是云南省近年来发生的强度最大地震,引起较为强烈的强地面运动,造成了严重的生命和财产损失。为更深入地理解漾濞地震的强地面运动特征,采用数值模拟方法对此次地震的强地面运动过程进行模拟研究。建立三维地质模型时,考虑了实际地形,并采用断层弹性弱化模型来模拟震源动力学破裂过程。模拟结果显示,横断山区起伏的地形对漾濞地震的强地面运动分布具有较大的影响,在山脊、陡坡等高程陡起的区域地震动放大效应显著。此外,通过施加应力边界条件引入震前应力场,并考虑地震前后断层应力场强度的变化,使模拟的强地面运动的幅值大小、分布和衰减快慢等更为接近实际地震的情况。模拟得到的近场台站峰值加速度(PGA)、反应谱(ARS)与观测记录有较好的一致性,地表PGA等值线图与地震烈度图形态接近、分布范围相似。考虑实际地形起伏并采用动力学震源模型,能够增加强地面运动模拟的可靠性和有效性,在防震减灾和城镇规划中可发挥重要作用。

    Abstract:

    The 2021 Yangbi MS6.4 earthquake in Yunnan Province is the strongest seismic event in the region in recent years and has generated intense strong ground motions that caused significant casualties and property damage. Numerical simulations were conducted on the strong ground motion to deepen the understanding of its characteristics. A 3D geological model incorporating actual topography and a fault weakening model with elastic material properties were used to simulate dynamic rupture. Results demonstrate that the rugged topography of the Hengduan Mountains considerably influences the strong ground motion distribution of the Yangbi earthquake, with an amplification effect at the ridges and steep slopes where the elevation changes abruptly. When preseismic stress fields are introduced through boundary conditions and variations in fault material strength before and after the earthquake are considered, the simulated strong ground motion-including its magnitude, distribution, and attenuation rate-closely approximates the actual event. Simulated results of peak ground acceleration (PGA) and acceleration response spectrum at near-field stations align closely with the observational records. PGA contours correspond closely to the seismic intensity maps in spatial distribution. Integrating realistic topography with dynamic source modeling can enhance the simulation reliability for seismic hazard mitigation and resilient urban planning.

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王珏,胡才博,周元泽,等.考虑地形影响和震源动力学过程的2021年漾濞MS6.4地震强地面运动数值模拟[J].地震工程学报,2025,47(6):1457-1468. DOI:10.20000/j.1000-0844.20231012006

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  • 收稿日期:2023-10-12
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  • 在线发布日期: 2025-09-29
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