首页> 外文期刊>Natural Hazards and Earth System Sciences Discussions >Time-lapse slip variation associated with a medium-size earthquake revealed by 'repeating' micro-earthquakes: the 1999 Xiuyan, Liaoning, MS = 5.4 earthquake
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Time-lapse slip variation associated with a medium-size earthquake revealed by 'repeating' micro-earthquakes: the 1999 Xiuyan, Liaoning, MS = 5.4 earthquake

机译:与中等地震相关的延时滑移变异,透露的“重复”微地震:1999年秀妍,辽宁,MS = 5.4地震

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We obtained the time-lapse cumulative slip before and after the 29 November 1999, Xiuyan, Liaoning, China, Ms = 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 Ms = 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:我们在1999年11月29日之前和之后获得了延期累积单据,夏燕,辽宁,中国,MS = 5.4地震,采用波形交叉相关定义的“重复事件”。我们从1999年6月到2006年6月辽宁区域地震仪网络中的地震波形数据。靠近1999年秀岩地震和1975年2月4日,海城MS = 7.3地震附近的两个“乘积”分别进行了调查。对于1999年秀艳地震前后发生的“多重”,可以观察到明显的预震动加速滑动行为,清晰立即发生地震变化,并且可以观察到放松的后地震变化。作为一个比较,对于1975年海城地震附近发生的“乘积”发生四分之一世纪前的,累积滑动显得较小的滑动速率。

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