侯康明, 杜学彬. 偶极电测深法预报地震的试验研究[J]. 华北地震科学, 1993, 11(1): 74-83.
引用本文: 侯康明, 杜学彬. 偶极电测深法预报地震的试验研究[J]. 华北地震科学, 1993, 11(1): 74-83.
Hou Kangming, Du Xuebin. THE TEST RESEARCH ON APPLICATION OF ELECTRIC DIPOLE DEPTH-SOUNDING IN EARTHQUAKE PREDICTION[J]. North China Earthquake Sciences, 1993, 11(1): 74-83.
Citation: Hou Kangming, Du Xuebin. THE TEST RESEARCH ON APPLICATION OF ELECTRIC DIPOLE DEPTH-SOUNDING IN EARTHQUAKE PREDICTION[J]. North China Earthquake Sciences, 1993, 11(1): 74-83.

偶极电测深法预报地震的试验研究

THE TEST RESEARCH ON APPLICATION OF ELECTRIC DIPOLE DEPTH-SOUNDING IN EARTHQUAKE PREDICTION

  • 摘要: 本文依据现场仪器观测资料,总结了1982年以来,用偶极电测深法预报地震的试验研究,结果表明:震前测区内不同深度的岩石电阻率确有不同程度的异常反映,并具深部岩石电阻率异常幅度较其浅部岩石电阻率异常幅度大之特点,最大幅度可达24%。实验表明,利用偶极电测深法观测到的中等深度(2~6km)的电阻率(ρs)异常要比四极对称法测到的浅层(几百米)电阻率(ρs)异常幅度大。该深度与郭增建提出的地下前兆优显层的深度大体相等。

     

    Abstract: Based on the data of instrument observation, the test research results of the application of electric dipole depth-sounding in earthquake prediction, in the western part of China, have been summarized in this paper.
    The observation results have indicated that the resistivities observed at each test site showed obviously abnormal change before earthquakes and the abnormal change amplitude in depth is larger than that in shallow part.The maximum amplitude is as much as 24%.As a result, the resistivity abnormal change observed in mid depth (2-6Km) by using electric dipole depth-sounding method is more obvious than that in shallow part (several hundred meters) measured by four-pole symmetric method observation, being used by many seismic stations at the present time.This depth coincides with that of the precursor advantageous layer proposed by Mr Guo Zengjian.

     

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