可提供视电阻率、阻抗相位、异常相位等地电学参数。
Parameters of apparent resistivity, impedance phase, and anomaly phase can be acquired.
大地电磁测深结果受表层构造横向不均匀性的影响，其视电阻率曲线会发生畸变。
The curves of apparent resistivity obtained from Magnetotelluric Sounding are greatly distorted by the lateral inhomogeneity of surficial structures.
使用该方法对大地电磁测深视电阻率进行了处理，应用效果良好。
The method is used for processing the apparent resistivity of magnetotelluric measured depth, and better result is achieved.
大地电磁测深研究中，长期以来使用视电阻率和相位作为解释参数，但视电阻率和相位均存在一定的局限性。
In MT, apparent resistivity and phase have been used as interpretative parameter for a long time. However, apparent resistivity and phase have some limitations.
大地电磁测深研究中，长期以来使用视电阻率和相位作为解释参数，但视电阻率和相位均存在一定的局限性。
In MT, apparent resistivity and phase have been used as interpretative parameter for a long time. However, apparent resistivity and phase have some limitations.
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