大地电磁测深是通过改变电磁场频率进行测深的一类电法分支方法，它利用电磁感应的趋肤效应，即高频电磁场穿透浅，低频电磁场穿透深，在场源和接收点间距不变的条件下，改变电磁场的频率来达到测深的目的。
数字大地电磁测深仪 digital magnetic telluro sounding instrument ; magnetic telluro sounding instrument
大地电磁测深法 [地物] magnetotelluric sounding method
音频大地电磁测深 audio magnetotelluric sounding
大地电磁测深剖面 DPEM
大地电磁测深MT Magnetotelluric sounding MT
海洋大地电磁测深 marine magnetotelluric sounding
二维大地电磁测深 d mt
大地电磁测深仪器 Magnetotelluric sounding
超宽频带大地电磁测深 super wide band MT sounding
张量分析在大地电磁测深法勘探中有许多重要的应用。
There are many great applications of the tensor analysis in survey with the magnetotelluric sounding method.
在大地电磁测深法中，曲线类型的分析划分是资料解释流程中相当重要的一环。
In magnetotelluric sounding method, the analysis and partition of curve types is a very important step in the data processing.
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.
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