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地震 ›› 2014, Vol. 34 ›› Issue (4): 152-157.

• • 上一篇    

东日本地震在北京GNSS连续观测站E分量的反应

吴培稚1, 孙建宝2, 徐平1, 邢成起1, 胡乐银1, 梁芳1, 黄雨蕊1, 施玉芳1, 季红1   

  1. 1.北京市地震局,北京 100038;
    2.中国地震局地质研究所,地震动力学重点实验室,北京 100029
  • 收稿日期:2013-10-10 修回日期:2013-12-15 发布日期:2020-09-11
  • 作者简介:李腊月（1986-)，女，黑龙江哈尔滨人，硕士研究生毕业，主要从事地壳形变与地震预测研究。

Responses of the East Component of Beijing GNSS Continuous Stations to the 2011 Japan Mw9.0 Earthquake

WU Pei-zhi1, SUN Jian-bao2, XU Ping1, XING Cheng-qi1, HU Le-yin1, LIANG Fang1, HUANG Yurrui1, SHI Yu-fang1, JI Hong1   

  1. 1. Earthquake Administration of Beiing, Beiing 100080, China;
    2. State Key Laboratory of Earthquake Dynamics, Institute of Geology, CEA, Bejing 100029, China
  • Received:2013-10-10 Revised:2013-12-15 Published:2020-09-11

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摘要： 北京GNSS连续观测台网孔径较小,不同的建设和管理单位执行着不同的规范,城市人 为活动强烈引起较多干扰,给观测数据的使用提出了新要求。本文对北京GNSS连续观测台网 数据做了一些必要的处理,如原始数据的高水平解算,设备、超差、迁址的改正,逐站消除E 分量线性趋势变化等。在全部可用1：个连续站E分量上,日本9. 0级地震前呈下锯齿波异常 (缓慢西移）、临震阶跃回升（快速东移）、震后n形恢复,构成了一个完整的地震过程,这个过 程在以往的GNSS观测中很少见到,为进一步研究提供了一个很好的实例。尤其是临震快速东 移,他不受人为设定的正常值大小影响,具有明显的预报和预警作用。

关键词: 东日本地震, GNSS# E分量, 地震过程, 临震阶跃

Abstract: While using the Beijing GNSS station network to monitor earthquake activity, some necessary processing must be carried out such as more accurate solution, corrections to the replacement of equipment, ultra poor and relocation, and elimination of the Ecomponent trends applying empirical algorithm. The E component of the 16 available stations showed a lower triangular w ave abnormality before the 2011 Tohoku Mw9.0 earthquake, a step change during the earthquake and a Q-shaped recovery after the earthquake. The whole steps constitute a complete seismic process that rarely seen in the past in the GNSS observations. It provided a perfect example for further study. Especially the step changes during the earthquake moves to the east rapidly, which will not be influenced by man- made normal values and may play a significant role in the earthquake forecasting and early warning.

Key words: Coulomb failure stress changes, Interactions between faults, The 2008 Wen-chuan 8.0 earthquake, The 2013 Lushan 7.0 eart hquake, The Longmenshan fault zone

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