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Time-lapse slip variation associated with a medium-size earthquake revealed by 'repeating' micro-earthquakes: The 1999 Xiuyan, Liaoning, M _S = 5.4 earthquake

机译:通过“重复”微地震揭示的中级地震的时移滑移变化:1999年辽宁修岩,M _S = 5.4级地震

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摘要

We obtained the time-lapse cumulative slip before and after the 29 November 1999, Xiuyan, Liaoning, China, M_s = 5.4 earthquake by using "repeating events" defined by waveform cross-correlation. We used the seismic waveform data from the Liaoning Regional Seismograph Network from June 1999 to December 2006. Two "multiplets" located near the seismogenic fault of the 1999 Xiuyan earthquake and the 4 February 1975, Haicheng M _s = 7.3 earthquake, respectively, were investigated. For the "multiplet" that occurred before and after the 1999 Xiuyan earthquake, apparent pre-shock accelerating-like slip behavior, clear immediate-post- seismic change, and relaxation-like post-seismic change can be observed. As a comparison, for the "multiplet" near the 1975 Haicheng earthquake which occurred a quarter century ago, the cumulative slip appears linear with a much smaller slip rate.
机译:通过使用波形互相关定义的“重复事件”,我们获得了1999年11月29日中国辽宁修岩之前和之后的延时累积滑动。我们使用了辽宁地区地震台网1999年6月至2006年12月的地震波形数据。分别对位于1999年秀岩地震和1975年2月4日海城M s = 7.3级地震发震断层附近的两个“多重波”进行了研究。 。对于在1999年Xi岩地震前后发生的“多重”现象,可以观察到明显的震前类似加速的滑移行为,明显的震后即刻变化和震后的像松弛一样变化。相比之下,对于四分之一世纪前的1975年海城地震附近的“多重”,累积滑移呈线性,滑移率小得多。

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