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.
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。
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