片语

array magnetotelluric阵列大地电磁

magnetotelluric prospecting磁気诱导地电流探查

magnetotelluric field[地物]

magnetotelluric surveying大地电磁测深

marine magnetotelluric海底大地电磁

3D Magnetotelluric三维大地电磁

d magnetotelluric二维大地电磁

magnetotelluric signal大地电磁信号

magnetotelluric data大地电磁资料

Magnetotelluric modeling大地电磁模拟

英汉例句

• This paper explains the special points in using this method by concrete examples, and Outlines the equipment requirement needed in making magnetotelluric sounding by the remote reference method.

  本文以实例介绍了此法使用上的特点，并指出利用远参考法进行大地电磁测深时对仪器设备的要求。

• Using integral equation method, the numerical algorithm of 3D magnetotelluric responses in homogeneous half-space is realized.

  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。

• Two-dimensional model by magnetotelluric data has been obtained and compared with the results by magnetic variation analysis.

  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。

• The authors present the achievements of 「863」 project for the research of the sea magnetotelluric data processing and explanation system.

  前言：作者在本文中详细地介绍了「863计划」项目「海底大地电磁数据处理和解释系统研究」所取得的成果。

• There are many difficulties in the marine magnetotelluric prospecting due to the cruel environment in the sea, the danger of working on the sea and the faint signal from the seabed.

  由于海洋环境的严酷、海上作业的风险和海底信号微弱，要实现海底大地电磁信号采集面临着重重困难。

• Based on the data of deep seismic sounding, gravity, magnetotelluric sounding and geotherm, two comprehensive geophysical sections are established in Tianshui earthquake area.

  根据人工地震、重力、大地电磁和地热资料，在天水地震区建立了二个综合地球物理剖面。

• Matching a inductive magnetometer with its preamplifier is the keyest technique in magnetotelluric sounding system.

  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。

• Recent marine experiments indicate that the seafloor magnetotelluric prospecting in China have achieved utility and can offer high technology support in marine prospecting.

  近期的海洋试验表明，中国的海底大地电磁探测技术已实现了实用化，可为海洋勘查提供高技术支撑。

• Two methods of the magnetotelluric impedance measurement are provided in this paper. That is, frequency conversion and DFT.

  介绍了两种大地电磁阻抗测量方法，即变频法与DFT分析法。

• Remote reference method can be used to improve the applicability, the interpretation accuracy and the operation efficiency of magnetotelluric sounding method.

  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。

• As to forward, emphasis is on analyzing basic equations, boundary conditions and finite-element solutions for magnetotelluric field in two dimension of finite-element forward method.

  在正演方面，着重分析了有限元正演方法的基本方程序，边界条件以及二维大地电磁场的有限元解法。

• Most magnetotelluric data processing methods make the Fourier transform of a segment record to get a power spectrum then to solve for tensor impedance element.

  大地电磁资料处理方法大多数都是对一段记录做傅氏变换，构成功率谱后再求张量阻抗元素。

• Active source electromagnetic sounding data can make use of existing magnetotelluric inversion technology after field source correction.

  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。

• For magnetotelluric (MT), its main research object is natural electromagnetic fields.

  在大地电磁测深法(MT)中，天然交变电磁场是其研究的主要对象。

• Controlled source acoustic magnetotelluric (CSAMT) is a new technique in electrical surveys, used in ore deposits exploration.

  可控源音频大地电磁法(CSAMT法)是一种直接探测地下巖性及矿产的电磁测深新技术。

• There are many great applications of the tensor analysis in survey with the magnetotelluric sounding method.

  张量分析在大地电磁测深法勘探中有许多重要的应用。

• The data acquisition of remote reference is used to suppress interference and acquire the high quality data due to the magnetotelluric regional noise.

  由于大地电磁场存在区域噪声，因而，为压制干扰并获得高质量的场源数据，就需进行带远参考方式的数据采集。

• In order to solve the problems above, the high-precision clock, detecting posture device and automatic measurement circuit are equipped in Marine magnetotelluric instrument.

  海底大地电磁仪为满足上述要求，其内部配备了高精度时钟源、姿态检测器件以及与海底电磁信息采集相关的自动信号测量与存储电路。

• The method is used for processing the apparent resistivity of magnetotelluric measured depth, and better result is achieved.

  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。

• Sharp boundary inversion is a relatively difficult problem in magnetotelluric and other geophysical inversion , which has been studied by many researchers.

  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。

• This method can also be used to interpret the data of 2d magnetotelluric sounding and electric sounding.

  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。

• The main problem of Marine magnetotelluric prospecting is the acquisition of Marine sea bottom signal.

  海底大地电磁探测要解决的首要问题是海底信号采集。

• The present paper describes in detail the basic train of thought, main functions and characteristics of the working station of magnetotelluric interpretation.

  本文详细介绍了大地电磁解释工作站的基本思路、主要功能和特点。