王宁,蔡璐,王莉婵, 等. 2016年8月20日唐山震群小震震源机制[J]. 华北地震科学,2020, 38(3):49-55. doi:10.3969/ j.issn.1003−1375.2020.03.009.
引用本文: 王宁,蔡璐,王莉婵, 等. 2016年8月20日唐山震群小震震源机制[J]. 华北地震科学,2020, 38(3):49-55. doi:10.3969/ j.issn.1003−1375.2020.03.009.
WANG Ning,CAI Lu,WANG Lichan, et al. Focal Mechanism of Small Earthquakes in Tangshan Earthquake Swarm on August 20, 2016[J]. North China Earthqauke Sciences,2020, 38(3):49-55. doi:10.3969/j.issn.1003−1375.2020.03.009.
Citation: WANG Ning,CAI Lu,WANG Lichan, et al. Focal Mechanism of Small Earthquakes in Tangshan Earthquake Swarm on August 20, 2016[J]. North China Earthqauke Sciences,2020, 38(3):49-55. doi:10.3969/j.issn.1003−1375.2020.03.009.

2016年8月20日唐山震群小震震源机制

Focal Mechanism of Small Earthquakes in Tangshan Earthquake Swarm on August 20, 2016

  • 摘要: 运用新近发展的适用于求解小震震源机制的广义极性振幅技术(GPAT),求解2016年8月20日唐山震群ML2.0以上地震事件的震源机制,结果显示:①震群的震源机制以正断型为主,占总数的69.5%;②对于震群中小于ML3.5的地震,GPAT得到的矩震级MW大于台网观测报告常用的ML震级,事件震级越小,差距越明显,最大震级偏差为1.0;③GPAT计算深度能够反映震源的真实深度。总之,GPAT方法在唐山震群震源机制反演中效果良好。

     

    Abstract: Measuring the source parameters of small earthquakes is a basic work to study the source and regional tectonic stress states. This study uses the recently developed Generalized Polarity and Amplitude Technique (GPAT) for solving the focal mechanism of small earthquakes above ML2.0 of Tangshan earthquake swarm on August 20, 2016. The results show that: ① The focal mechanism of the earthquake swarm is dominated by normal-fault types, accounting for 74.6% of the total. ② For earthquakes smaller than ML3.6 in the earthquake swarm, the moment magnitude MW obtained by GPAT is larger than the ML magnitude commonly used in the observation report of the network, the smaller the magnitude of the event, the more obvious the gap, the maximum magnitude deviation is 1.0. ③ The GPAT depth reflects the true depth of the source. In short, the GPAT method works well in the inversion of the focal mechanism of the Tangshan earthquake swarm.

     

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