徐桐, 周宝峰, 王晓敏, 任叶飞. 0: 2022年6.10四川马尔康震群特征初步分析. 地震学报. DOI: 10.11939/jass.20230072
引用本文: 徐桐, 周宝峰, 王晓敏, 任叶飞. 0: 2022年6.10四川马尔康震群特征初步分析. 地震学报. DOI: 10.11939/jass.20230072
Tong XU, BaoFeng ZHOU, XiaoMin WANG, YeFei REN. 0: Preliminary analysis of the characteristics of Sichuan Maerkang earthquake swarm on June 10, 2022. Acta Seismologica Sinica. DOI: 10.11939/jass.20230072
Citation: Tong XU, BaoFeng ZHOU, XiaoMin WANG, YeFei REN. 0: Preliminary analysis of the characteristics of Sichuan Maerkang earthquake swarm on June 10, 2022. Acta Seismologica Sinica. DOI: 10.11939/jass.20230072

2022年6.10四川马尔康震群特征初步分析

Preliminary analysis of the characteristics of Sichuan Maerkang earthquake swarm on June 10, 2022

  • 摘要: 2022年6月10日,四川省马尔康市先后发生MS5.8,MS4.1,MS4.4,MS6.0,MS5.2共计5次4.0级以上地震,系震群型地震。本文对强震动记录进行了滤波降噪处理,对比分析了不同震级地震的峰值加速度(PGA)、峰值速度(PGV) 和谱加速度值(Sa)的衰减关系;计算并对比了5次地震的加速度和速度反应谱,以及傅里叶幅值谱。结果表明: 5次地震的能量分布形式较为接近,可以推测这一系列地震具有相似的震源机制;由于台站分布位置的不均匀性,峰值加速度值高于衰减预测曲线;随着周期的增大,实际记录的加速度和速度反应谱值的衰减速率较衰减预测曲线更快;5次地震中同一强震动台站的加速度反应谱形状、峰值周期相同且谱值均未超过7度多遇地震的设计谱值;对于震级较高的地震,其0-30Hz频率范围内的傅里叶幅值谱幅值普遍高于低震级地震的幅值,且在某些频率区间更为显著;采用H/V谱比法与勘探得到的台站场地特征周期较为接近。

     

    Abstract: On June 10, 2022, a total of five earthquakes of magnitude 4.0 or above occurred in Maerkang City, Sichuan Province, with a total of MS5.8, MS4.1, MS4.4, MS6.0 and MS5.2. In this paper, the strong vibration records are filtered and noise reduction treatment, and the attenuation relationships of peak acceleration (PGA), peak velocity (PGV) and spectral acceleration value (Sa) of earthquakes of different magnitudes are compared and analyzed. The acceleration and velocity response spectra of five earthquakes, as well as the Fourier amplitude spectrum, were calculated and compared. The results show that the energy distribution patterns of the five earthquakes are relatively close, and it can be inferred that these series of earthquakes have similar source mechanisms. Due to the inhomogeneity of the station distribution position, the peak acceleration value is higher than the attenuation prediction curve. As the period increases, the decay rate of the actual recorded acceleration and velocity response spectra is faster than that of the attenuation prediction curve. The shape and peak period of the acceleration response spectrum of the same strong motion station in five earthquakes was same. The acceleration response spectrum of the five earthquakes did not exceed the design spectrum of the 7-degree frequently occured earthquake. For earthquakes with high magnitude, the Fourier amplitude spectrum in the frequency range of 0-30Hz is generally higher than that of earthquakes with low magnitude, and it is more significant in some frequency ranges. There is the same characteristic period of the station site by the H/V spectral ratio method and exploration.

     

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