tensor impedance

In this paper, we wil discuss how to use the the maximum entropy method theory to estimates the the tensor impedance of magnetotelluric ( MT) sounding data, and use the model to calculate the measured signal and model signal.

本文将从由最大熵方法出发，研究最大熵谱法估计大地电磁测深资料的张量阻抗，并利用模型信号与实测信号对此方法进行验证。

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For this reason, the paper theoretically and systematically deduced the general calculation formula of tensor impedance that is suitable for complex telluric model and gave the method for impedance elements calculated from the discrete electrical and magnetic fields that are resulted from numerical modeling.

为此，本文从理论上系统地推导了适用于复杂地电模型的张量阻抗通用计算公式，给出了由数值模拟得到的离散电场、磁场值计算阻抗元素的方法。

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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。

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The Expressions of Higher-Order Tensor Impedance Boundary Conditions in Longitudinal Components of Electromagnetic Fields

高阶张量阻抗边界条件的纵向电磁场分量表达式

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Higher-order tensor impedance boundary condition for multilayer complex material

多层介质涂覆结构的高阶张量阻抗边界条件

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Using reference station technique for computing MT tensor impedance

用参考台技术计算大地电磁张量阻抗

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A canonical decomposition method for impedance tensor analysis in 3 D medium is put forward to cope with the problems in ordinary analysis of 3 D magnetotelluric impedance tensor.

本文针对大地电磁三维阻抗张量常规分析处理中存在的问题，提出了一种用于三维介质阻抗张量分析的正则分解方法。

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Through deep analysis, we also got direct expression of calculation formula for each general tensor impedance element, showing a clear physical meaning.

通过深入分析，还得到了每个通用张量阻抗元素计算公式的直观表达式，显示出明确的物理意义。

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After processed by narrow band com-plex filtering or narrow band recurrence filtering and Hilbert trans-formation, real signal is transformed into narrow band complex sig-nal, whose instantaneous spectrum is then used to solve for tensor impedance element.

本文通过对记录上的实信号做窄带复数滤波或窄带递归滤波和希尔伯特变换，转换成窄带复信号，再由复信号的瞬时谱求出张量阻抗元素。

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