利用重复地震观测重庆武隆地区地壳介质变化 |
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作者姓名: | 汪建 杨亚运 马伟 |
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作者单位: | 重庆市地震局,重庆401147 |
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基金项目: | 中国地震局监测、预报、科研三结合项目(3JH-2021040)与重庆市地震局科研项目联合资助。 |
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摘 要: | 选取重庆数字地震台网记录的武隆地区107次ML≥1.5地震波形和观测报告资料,采用波形互相关技术进行相关计算,识别出12组同时被3个地震台站记录且各台波形互相关系数不小于0.8的重复地震。利用射线追踪方法,对武隆地区重复地震位置做归一化处理,得到所选台站记录地震P波走时差变化,结果显示:在2017年武隆MS5.0地震前4年,武隆、仙女山、涪陵地震台记录到P波走时差均存在长期的负异常变化,持续时间长达339天,共出现18次负值,表明该时段地壳介质速度有明显升高现象。
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关 键 词: | 重复地震 射线追踪 P波走时差 武隆地区 |
收稿时间: | 2021-10-16 |
Monitoring variation of crustal media in Wulong area of Chongqing Municipality by using repeating earthquakes |
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Institution: | Chongqing Earthquake Agency, Chongqing 401147, China |
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Abstract: | The waveform and observation report data of 107 earthquakes with ML≥1.5 recorded by Chongqing Digital Seismic Network in Wulong area were selected. The waveform cross-correlation technology was used for correlation calculation. 12 groups of repeating earthquakes with waveform correlation coefficient larger than 0.8 and recorded by 3 seismic stations at the same time were identified. The position of repeating earthquakes in Wulong area was normalized by ray tracing method, and the change of P-wave travel-time difference of the selected stations was obtained. The results show that four years before the 2017 Wulong MS5.0 earthquake, there are long-term negative abnormal changes in P-wave travel-time difference recorded by Wulong, Xiannushan and Fuling seismic stations, lasting for 339 days, with a total of 18 negative values. It shows that the crustal medium velocity increases obviously in this period. |
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