宋文杰, 吴子泉, 姜早峰, 杜历英. 岩石裂隙电阻率特征研究[J]. 华北地震科学, 2010, 28(4): 24-26.
引用本文: 宋文杰, 吴子泉, 姜早峰, 杜历英. 岩石裂隙电阻率特征研究[J]. 华北地震科学, 2010, 28(4): 24-26.
SONG Wen-jie, WU Zi-quan, JIANG Zao-feng, DU Li-ying. STUDY ON RESISTIVITY CHARACTERISTIC OF ROCK FRACTURE[J]. North China Earthquake Sciences, 2010, 28(4): 24-26.
Citation: SONG Wen-jie, WU Zi-quan, JIANG Zao-feng, DU Li-ying. STUDY ON RESISTIVITY CHARACTERISTIC OF ROCK FRACTURE[J]. North China Earthquake Sciences, 2010, 28(4): 24-26.

岩石裂隙电阻率特征研究

STUDY ON RESISTIVITY CHARACTERISTIC OF ROCK FRACTURE

  • 摘要: 岩石的电阻率差是电阻率法的物理前提,利用电阻率法研究断层是比较有效的方法。利用断层破碎带与周围岩石的电阻率差异,跨断层做了大量的实验数据,通过对比和分析,得出了研究破碎带与周围岩石的电性差异,寻找变化规律,研究其变化特征。对今后断层探测具有重要价值,对防震减灾具有重要意义。

     

    Abstract: Resistivity difference of rock is the physical basis of resistivity method, which is a more efficient method.On basis of mass data obtained from cross fault experiment according to resistivity difference of rock between fault fracture zone and its surroundings.The electrical property difference between fault fracture zone and its surroundings is determined through contrasting analysis, which has active significance for future fault exploration and earthquake prevention and disaster alleviation.

     

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