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Shi Hongjun, Zhao Weixing, Zhang Kejia, Zhu Weinan, Li Ning. 2014: Characteristics of precursor anomalies of earth resistivity at Yushu and Siping seismic stations of Jilin Province. Acta Seismologica Sinica, 36(3): 452-463. DOI: 10.3969/j.issn.0253-3782.2014.03.011
Citation: Shi Hongjun, Zhao Weixing, Zhang Kejia, Zhu Weinan, Li Ning. 2014: Characteristics of precursor anomalies of earth resistivity at Yushu and Siping seismic stations of Jilin Province. Acta Seismologica Sinica, 36(3): 452-463. DOI: 10.3969/j.issn.0253-3782.2014.03.011
shu

Characteristics of precursor anomalies of earth resistivity at Yushu and Siping seismic stations of Jilin Province

  • 1.

    Yushu Seismic Station， Changchun 130400， China

  • 2.

    Earthquake Fast Determination and Report Center of Changchun City， Changchun 130012， China

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  • Received Date: December 02, 2012
  • Revised Date: March 09, 2013
  • Published Date: April 30, 2014
    Graphical Abstract
    • Abstract
  • This paper studies the anomalous changes of earth resistivity before 1999 Wangqing MS7.0 earthquake and 2006 Qian’an-Qianguo MS5.0 earthquake observed at Yushu and Siping stations of Jilin Province. The results show that, at the Yushu and Siping stations a long-trend decreasing or short-impending anomaly of earth resistivity appeared before the two earthquakes. Monthly mean curves of earth resistivity displayed two-year decrease anomalies at Yushu and Siping stations before the Wangqing earthquake. Before Wangqing and Qian’an-Qianguo earthquakes, normalized variation rates of earth resistivity are larger than anomaly index at Yushu and Siping stations. Before Qian’an-Qianguo earthquake, earth resistivity anisotropy degree showed obviously low value anomaly at Siping station, and at Yushu station it broke its annual variation value. Possible reasons for the anomalous changes maybe are related to the maximum principal compressive stress orientation’s (or close to the range) compressing NWwards in the source region and its vicinity resulting from NWwards extrusion of Pacific Plate, which makes the conductive fluid in the media quickly enter or redistribute, so that the earth resistivity shows a long-trend decrease and anisotropic variation.
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    • References (28)
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