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2016年7月19日新疆MS 4.5级地震乌什地震台形变异常
引用本文:赖爱京,张锦萍,蒋志英,黄帅堂.2016年7月19日新疆MS 4.5级地震乌什地震台形变异常[J].震灾防御技术,2017,12(2):433-440.
作者姓名:赖爱京  张锦萍  蒋志英  黄帅堂
作者单位:阿克苏中心地震台, 新疆维吾尔自治区阿克苏 843000
基金项目:新疆维吾尔自治区地震局科学基金(2015206),中国地震局监测、预测、科研三结合课题(163102)
摘    要:利用乌什台数字化前兆形变观测资料,分析乌什MS 4.5级地震前乌什台水管倾斜仪、洞体应变仪数据变化情况。通过对比分析发现:地震前,洞体应变仪北南分量数据曲线正常,东西分量数据曲线加速拉张,05:14-20:32拉张幅度达到7.40×10-7,7月19日5时至20日16时乌什洞体应变仪东西分量快速拉张了9.20×10-7;7月19日5-19时,水管倾斜仪北南分量数据曲线正常,东西分量数据曲线反向西倾7.13ms,且05:59-06:06、07:36-07:46、18:42-18:56数据掉格,水管倾斜仪异常结束后1小时,在洞体应变仪异常过程中发生了乌什MS 4.5级地震。水管仪东西分量震前反向西倾,洞体应变仪东西分量震前拉张加速,短临异常明显,且2套形变观测震前异常时间同步性较好。

关 键 词:乌什MS  4.5地震    水管仪    洞体应变仪    短临异常
收稿时间:2016/8/29 0:00:00

Analysis on Seismic Anomalous of Deformation Caused by the Wushi MS 4.5 Earthquake
Lai Aijing,Zhang Jinping,Jiang Zhiying and Huang Shuaitang.Analysis on Seismic Anomalous of Deformation Caused by the Wushi MS 4.5 Earthquake[J].Technology for Earthquake Disaster Prevention,2017,12(2):433-440.
Authors:Lai Aijing  Zhang Jinping  Jiang Zhiying and Huang Shuaitang
Institution:Aksu Central Seismic Station, Aksu 843000, Xinjiang Uyghur Autonomous Region, China
Abstract:We used Wushi digital precursory deformation observational data to analyze the water tube-tilt and cave strain changes before the Wushi MS 4.5 earthquake. Through comparative analysis we found that before the Wushi MS 4.5 earthquake, the north-south strain component recorded in the Wushi cave instrument is normal, but the east-west component value changes greatly. The amplitude of stretching is 7.40×10-7 from 05:14 to 20:32. From 05:00 to 19:00 on July 19, the east-west component records from the Wushi water-pipe tilt meter is normal and the east-west component value is reverse to westward inclination 7.13ms. Moreover, the recorded data drop out at 05:59 -06:06, 07:36-07:46, and 18:42-18:56. The water pipe inclinometer abnormal was observed after 1 hour, in the process of the body strain gauge anomaly Wushi MS 4.5 earthquake occurred. The EW component of water tube-tilt from Wushi station west-dipping reverse, cave stuff strain tensile EW component rapid tension before the earthquake, short-impending anomalies before the seismogenic, and the two sets of deformation observation of seismic anomalous have a good agreement to each other.
Keywords:Wushi MS 4  5 earthquake  Tube-tilt  Cave strain  Short-impending anomalies
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