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

被引:43
|
作者
Xiao, Tiaojie [1 ,2 ]
Liu, Yun [1 ]
Wang, Yun [1 ]
Fu, Li-Yun [1 ]
机构
[1] Chinese Acad Sci, Inst Geochem, Guiyang 550002, Guizhou, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
Magnetotelluric; Anisotropy; Three-dimensional; Forward modeling; Edge-based finite element method; Vector finite element method; CONDUCTIVITY STRUCTURES; INHERENT NONUNIQUENESS; MANTLE ANISOTROPY; INVERSION; FIELDS; MT;
D O I
10.1016/j.jappgeo.2017.12.009
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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.
引用
收藏
页码:1 / 9
页数:9
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