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另外在大地电磁测勘上要特别注意的是接收能量上的选择。Another critical factor in a magnetotelluric survey is the selection of the energy passband.

海底大地电磁探测要解决的首要问题是海底信号采集。The main problem of marine magnetotelluric prospecting is the acquisition of marine sea bottom signal.

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这种方法还可推广到二维大地电磁测深和电测深资料的解释。This method can also be used to interpret the data of 2D magnetotelluric sounding and electric 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.

由于大地电磁测深法勘探的轻便和有效，其作为深层构造研究的重要手段越来越受到重视。For its effect and handiness magnetotelluric sounding is regarded as an important means to study deep structure.

感应磁力仪与前置放大器之间的匹配问题是大地电磁测深仪中最关键的一项技术。Matching a inductive magnetometer with its preamplifier is the keyest technique in magnetotelluric sounding system.

传统的测量电路无法解决诸如海底大地电磁场这样微弱地学信号的检测问题。Traditional measuring circuit can't be used to detect the faint geosciences signal such as seafloor magnetotelluric signal.

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这一结果与由大地电磁资料计算得到的二维模型剖面是一致的。Two-dimensional model by magnetotelluric data has been obtained and compared with the results by magnetic variation analysis.

本文阐述在大地电磁测深工作中，用有限单元法，模拟计算京津唐地区二维地质构造的大地电磁响应。The magnetotelluric response to the two dimension structures has been numerically modeled by use of the finite element method.

利用积分方程法实现了均匀导电半空间三维大地电磁响应的数值模拟。Using integral equation method, the numerical algorithm of 3D magnetotelluric responses in homogeneous half-space is realized.

本文可以分成两个部分，前半部分比较简要地介绍了大地电磁测深法的基本原理。The dissertation can be divided into two parts. The rationale of Magnetotelluric sounding will be briefly introduced in part one.

文章主要介绍了EH-4高频大地电磁方法的原理、特点和勘探效果。This paper mainly introduces the principle, characteristics and exploration effect of EH-4 high-frequency magnetotelluric method.

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由于常规的张量旋转分析方法的局限性，在处理三维阻抗问题时不能得到令人满意的结果。Because of the limitations of the ordinary analysis methods for magnetotelluric impedance tensor, we can't get satisfying results.

有源电磁测深数据在经过场源校正后可以利用现有的大地电磁反演技术进行反演。Active source electromagnetic sounding data can make use of existing magnetotelluric inversion technology after field source correction.

然而现行的大地电磁测深设备的检验办法既缺少整个系统的定量检测，也没有统一规范的技术标准。But nowadays tests for magnetotelluric surveying equipment can not quantitative detect overall system and there is no uniform technical standards.

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.

尖锐边界反演是大地电磁及其他地球物理反演中的一个较难解决的问题，目前有不少专家正对这方面进行研究。Sharp boundary inversion is a relatively difficult problem in magnetotelluric and other geophysical inversion , which has been studied by many researchers.

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结合区域地质资料和地球物理特征，对民和盆地的大地电磁测深资料进行了处理和解释。Combining with regional geologic data and geophysical characteristics, the data of magnetotelluric sounding in the Minhe Basin are processed and interpreted.

湖北襄樊—福建罗源一千多公里的剖面上作了23个大地电磁测深点。Magnetotelluric measurements were made at 23 sites along more than thousand kilometres long profile from Xiangfan, Hubei Province to Luoyuan, Fujian Province.

远参考法可以提高大地电磁测深方法的适应能力，有利于解释精度的改进和工效的提高。Remote reference method can be used to improve the applicability, the interpretation accuracy and the operation efficiency of magnetotelluric sounding method.