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Analytical investigations of the magnetotelluric directionality estimation in 1-D anisotropic layered media

机译:一维各向异性层状介质中大地电磁方向性估计的分析研究

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摘要

Inferring geoelectric dimensionality (1D, 2D or 3D) and directionality (strike directions) from the impedance tensor is a basic procedure in magnetotelluric data processing. Given that electrical anisotropy is increasingly recognized in observations, it is valuable to understand the imprint of anisotropy in these analyses. In this paper, we analytically investigate the estimation of strike directions based on rotational invariants in 1D anisotropic layered media. We first show that if anisotropy axes are identical in all anisotropic layers, the estimated strike coincides with that direction. We then derive an analytical formula of the strike angle at long periods for general anisotropic layers with an isotropic basement. This formula shows a clear physical interpretation that the strike angle points where the conductance integrated along depth takes a maximum value. (C) 2016 Elsevier B.V. All rights reserved.
机译:从阻抗张量推断地电维数(1D,2D或3D)和方向性(走向)是大地电磁数据处理的基本过程。鉴于观测中越来越认识到电各向异性,因此了解这些分析中各向异性的烙印非常有价值。在本文中,我们基于一维各向异性层状介质中的旋转不变性,分析性地研究了走向走向的估计。我们首先表明,如果各向异性轴在所有各向异性层中都相同,则估计走向与该方向一致。然后,我们得出具有各向同性基底的一般各向异性层长时的走向角的解析公式。该公式显示出清晰的物理解释,即触击角指向沿深度积分的电导取最大值的位置。 (C)2016 Elsevier B.V.保留所有权利。

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