3D time-domain airborne EM modeling for an arbitrarily anisotropic earth

被引:47
|
作者
Yin, Changchun [1 ]
Qi, Yanfu [1 ]
Liu, Yunhe [1 ]
机构
[1] Jilin Univ, Coll Geoexplorat Sci & Technol, Changchun 130021, Jilin, Peoples R China
基金
中国国家自然科学基金;
关键词
Airborne EM; Time-domain; Anisotropy; Unstructured grids; Edge finite-element method; ELECTROMAGNETIC INDUCTION; FINITE-ELEMENTS; ALGORITHM; INVERSION; RESPONSES; SYSTEMS;
D O I
10.1016/j.jappgeo.2016.05.013
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Time-domain airborne EM data is currently interpreted based on an isotropic model. Sometimes, it can be problematic when working in the region with distinct dipping stratifications. In this paper, we simulate the 3D time domain airborne EM responses over an arbitrarily anisotropic earth with topography by edge-based finite element method. Tetrahedral meshes are used to describe the abnormal bodies with complicated shapes. We further adopt the Backward Euler scheme to discretize the time-domain diffusion equation for electric field, obtaining an unconditionally stable linear equations system. We verify the accuracy of our 3D algorithm by comparing with 1D solutions for an anisotropic half-space. Then, we switch attentions to effects of anisotropic media on the strengths and the diffusion patterns of time-domain airborne EM responses. For numerical experiments, we adopt three typical anisotropic models: 1) an anisotropic anomalous body embedded in an isotropic half space; 2) an isotropic anomalous body embedded in an anisotropic half-space; 3) an anisotropic half-space with topography. The modeling results show that the electric anisotropy of the subsurface media has big effects on both the strengths and the distribution patterns of time-domain airborne EM responses; this effect needs to be taken into account when interpreting ATEM data in areas with distinct anisotropy. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:163 / 178
页数:16
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