最后结合其它地质和地球物理资料的分析，对得到的地电模型进行了解释。
At last, the interpretation of the electrical model is performed considering the geology and other geophysical data.
针对复杂地电模型的井地电法三维反演方法研究一直是一个具有挑战性的课题。
Considering complex geoelectric model, the study of 3-d inversion approaches of borehole-to-surface electric data is always a challenge.
通过两种地电模型的计算结果表明，这一频段的电磁场是由传导电流和位移电流共同决定的。
After computing two models, the conclusion are reached that electromagnetic fields are determined by conduction currents and displacement currents.
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