CAJ | 학술논문

地电阻率各向异性参量计算方法是由钱复业,赵玉林等研究出来的方法.我们试用该方法编制相应的计算机程序,对蒙城地震台1978～2008年地电阻率的数据进行处理;并结合震例进行对比分析,发现对于震中距300 km内的中强震,与地电阻率各向异性参数的趋势性变化存在密切的关系;地电阻率各向异性参量特征可以反映孕震区地下介质的孕震信息,对未来地震的预测将起到一定作用.
지전조솔각향이성삼량계산방법시유전복업,조옥림등연구출래적방법.아문시용해방법편제상응적계산궤정서,대몽성지진태1978～2008년지전조솔적수거진행처리;병결합진례진행대비분석,발현대우진중거300 km내적중강진,여지전조솔각향이성삼수적추세성변화존재밀절적관계;지전조솔각향이성삼량특정가이반영잉진구지하개질적잉진신식,대미래지진적예측장기도일정작용.
Resistivity anisotropy parameter is calculated with the method presented by Qian Fuye and Zhao Yulin et al. A computer program is developed base on this method and used to process the resistivity data recorded at Mengcheng Seismic Station from 1978 to 2008, comparing with the earthquakes, the analyzed results show that there is a close relationship between the medium and strong earthquake with epicentral distance no more then 300 km and trend variation of the resistivity anisotropy parameters. The characteristic of resistivity anisotropy parameters can reflect the seismogenic information come from the underground medium of seismogenic zone. This result is useful for the earthquake forecasting in the further.