摘要
论述了起因于EDA现象的地球介质电导率各向异性特征,分析研究了地球介质电导率各向异性变化引起的大地电磁响应函数变化形态特征,简述了大地电磁测深法对EDA电性变化前兆的可识别性及大地电磁资料解释中考虑电导率各向异性的必要性,研究了对称各向异性层状介质大地电磁资料的反演问题。
The characteristics of conductivity anisotropy of earth medium due to EDA phenomena were demonstrated,tha pattern and characteristics of MT response function variations caused by the cbanges of conductivityanisotropy were analysed and studied, the distinguishability of MTS to the earthquake precursor of EDA electricalchanges and the necessity of considering the anisotropy in the interpration of MT data were explained, and the.inverse problem of MT data for the symmetrically anisotropic layered medium was discussed.
出处
《西北地震学报》
CSCD
1995年第4期89-98,共10页
Northwestern Seismological Journal
关键词
地震前兆
大地电磁测深
电导率
各向异性
Earthquake precursor, Magnetotelluric sounding, Conductivity anisotropy, EDA