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《Chinese Journal of Geophysics》 2001-06
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RESISTIVITY TOMOGRAPHY IN EARTHQUAKE MONITORING

FENG RUI 1) \ HAO JIN QI 2) \ ZHOU JIAN GUO 2) 1) Center for Seismological Data and Information, China Seismological Bureau, Beijing 100045, China 2) Institute of Geophysics, Laboratory of Tectonophysics, China Seismological Bureau, Beiji  
Resistivity tomography was applied to earthquake monitoring in the present study. Through inversion for apparent resistivity, the image of true resistivity was reconstructed. This method well reveals the nature of the variation of the relevant physical parameters during seismogenic process. At two stations in North China, Baodi and Changli, obvious anomalous changes appeared in the tomograms 6 days before the occurrence of two earthquakes with M L5.0 and M L4.4, respectively, in Tangshan on 14 April 1998. The distribution of true resistivity in the images of Baodi station showed a new pattern, i.e. an ordered state, instead of an ordinarily stable pattern with an even background. The resistivity image of Changli station showed distinct high and low resistivity areas and an ordered pattern, too. After these earthquakes, the above mentioned phenomena all disappeared, while the basic image pattern relating to geological structure beneath the stations did not change much. As an indicator of the ordered state of an image, the entropy of tomograms at two stations all decreased distinctly before the earthquakes, which might be the precursors to these earthquakes. It is inferred that the present resistivity anomalies were mainly attributed to the changes of the electrical conducting structure and porosity in the soil layer under increasing tectonic stress before earthquakes. The present result shows that in a conventional apparent resistivity survey with one fixed electrode spacing the observational results are not sensitive to the change of true resistivity and have not basic spatial resolution. These shortcomings result from an essential property of apparent resistivity being both an integral value and potential function. Adopting resistivity tomography in the earthquake monitoring has become necessary to improve our present observational system.
【Fund】: 中国地震局地震科技攻关项目 ( 95 -0 4 -0 1 -0 3-0 3) ;; 中国地震局构造物理开放实验室资助课题
【CateGory Index】: P315.6
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