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The Characteristics of Magnetotelluric Responses for anisotropic conductivity

机译:各向异性电导率的磁仪反应的特性

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In this paper, we assume a 2D earth structure with anisotropic conductivity. One of the principal anisotropy axes is parallel to the striking direction and another axes is perpendicular to the surface of structure layer. By solving the variational problem with assigned boundary condition, we can compute the apparent resistivity for magnetotelluric (MT). Based on the forward modeling of MT field, we will analysis the difference of EM field for isotropic and anisotropic medium for TE_(Z )polarization model. Our study shows that the MT field can be significantly affected by anisotropic medium and should be taken into consideration in many geophysical applications. We also analyzed the effect of anisotropic parameter (ration of horizontal conductivity to vertical conductivity) and dipping layer on MT field.
机译:在本文中,我们假设具有各向异性电导率的2D地球结构。其中一个主各向异性轴线平行于撞击方向,另一个轴垂直于结构层的表面。通过求解分配边界条件的变分问题,我们可以计算磁通科(MT)的表观电阻率。基于MT场的前向建模,我们将分析TE_(Z)极化模型的各向同性和各向异性介质的EM场差异。我们的研究表明,MT场可以受到各向异性介质的显着影响,并且应该在许多地球物理应用中考虑。我们还分析了各向异性参数(水平电导率对垂直电导率的比率)和MT场浸渍层的影响。

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