4.4 Article

Three-dimensional magnetotelluric modeling in anisotropic media using edge-based finite element method

期刊

JOURNAL OF APPLIED GEOPHYSICS
卷 149, 期 -, 页码 1-9

出版社

ELSEVIER SCIENCE BV
DOI: 10.1016/j.jappgeo.2017.12.009

关键词

Magnetotelluric; Anisotropy; Three-dimensional; Forward modeling; Edge-based finite element method; Vector finite element method

资金

  1. National Key Research and Development Project of China [2016YFC0600301]
  2. National Natural Science Foundation of China [41425017]
  3. National Key Research and Development Program of China [2016YFC0600505]

向作者/读者索取更多资源

It is important to understand how magnetotelluric (MT) modeling can most effectively be performed in general anisotropic media. However, previous studies in this area have mainly focused on the use of one-dimensional (1D) and two-dimensional (2D) algorithms. Thus, building on earlier work, it is important to study the performance of three-dimensional (3D) modeling in arbitrary conductivity media; therefore, an edge-based finite element (FE) method has been developed for 3D MT modeling in arbitrary conductivity media. This approach is based on the initial derivation of a series of equivalent variational equations that are based on Maxwell equations, generated using the weighted residual method. Specific values were then obtained for coefficient matrixes of this edge -based FE method using hexahedral meshes, and the algorithm was verified by comparing its results with finite difference (FD) solutions generated using a 2D anisotropic model. Finally, the results of a 3D anisotropic model were analyzed detailed for three conditions; another 3D anisotropic model was designed and its results were compared with two isotropic models'. (C) 2017 Elsevier B.V. All rights reserved.

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