杨苗,王宏伟,温瑞智,任叶飞. 2023. 2021年漾濞地震序列破裂方向性研究. 地震学报,45(5):836−848. doi: 10.11939/jass.20220227
引用本文: 杨苗,王宏伟,温瑞智,任叶飞. 2023. 2021年漾濞地震序列破裂方向性研究. 地震学报,45(5):836−848. doi: 10.11939/jass.20220227
Yang M,Wang H W,Wen R Z,Ren Y F. 2023. Study on the rupture directivity of the 2021 Yangbi earthquake sequence. Acta Seismologica Sinica45(5):836−848. doi: 10.11939/jass.20220227
Citation: Yang M,Wang H W,Wen R Z,Ren Y F. 2023. Study on the rupture directivity of the 2021 Yangbi earthquake sequence. Acta Seismologica Sinica45(5):836−848. doi: 10.11939/jass.20220227

2021年漾濞地震序列破裂方向性研究

Study on the rupture directivity of the 2021 Yangbi earthquake sequence

  • 摘要: 基于2021年云南漾濞MS6.4地震序列的强震动记录,建立了地震动参数预测方程,采用破裂方向性效应拟合方法估计了强震动记录丰富且空间分布均匀的九次地震的震源破裂方向性特征。结果表明:其中的四次地震(1号、4号、8号、9号)表现出破裂方向性效应,且均为不均匀双侧破裂,但优势破裂方向不同(4号和8号为东南向,1号西北向,9号西南向),说明2021年漾濞地震序列的地震破裂较为复杂;由于主震(4号地震)的破裂速度较慢(约为2.2 km/s),其破裂方向性效应较弱且主要对峰值速度有影响,其它三次地震破裂方向性效应十分显著,破裂速度大于主震;此外,四次地震的破裂方向性效应还存在一定的周期相关性。

     

    Abstract: This study used the strong-motion recordings of the MS6.4 Yangbi earthquake sequence in Yunnan Province to establish the prediction equations of ground motion parameters, and then estimated the focus rupture directivities characteristics for nine Yangbi earthquakes with abundant recordings in a good spatial station coverage based on the rupture directivity effect fitting method. The results indicated that the rupture directivity effects are observed in four of these earthquakes (i.e., the 1st, 4th, 8th, and 9th earthquakes). The four earthquakes are all characterized by the bilateral ruptures with various predominant rupture directions (i.e., southeast for the 4th and 8th events, northwest for the 1st event, and southwest for the 9th event), which illustrates the rupture complexities of the Yangbi earthquake sequence. Since the estimated rupture velocity (about 2.2 km) of the mainshock (the 4th event) is very slow, its rupture directivity effects are not strong and mainly affect the peak ground velocity. However, the rupture directivity effects for the other three earthquakes are very strong and the rupture velocities are faster than that of the mainshock. The dependency of the rupture directivity effects on the period was also observed in the four earthquakes.

     

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