Three-dimensional magnetotelluric axial anisotropic forward modeling and inversion

被引:21
|
作者
Cao, Hui [1 ,2 ,3 ]
Wang, Kunpeng [1 ,2 ,3 ]
Wang, Tao [4 ]
Hua, Boguang [2 ]
机构
[1] Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Sichuan, Peoples R China
[2] Chengdu Univ Technol, Coll Geophys, Chengdu 610059, Sichuan, Peoples R China
[3] Chengdu Univ Technol, Minist Educ, Key Lab Earth Explorat & Informat Technol, Chengdu 610059, Sichuan, Peoples R China
[4] Chinese Acad Sci, Key Lab Electromagnet Radiat & Sensing Technol, Beijing 100190, Peoples R China
基金
中国国家自然科学基金;
关键词
Magnetotellurics; Impedance tensor; Axial anisotropy; Staggered-grid finite difference; Broyden-Fletcher-Goldfarb-Shanno method; RESISTIVITY ANISOTROPY; AZIMUTHAL ANISOTROPY; LAYERED EARTH; MEDIA; TENSOR; INDUCTION; RESPONSES; FIELDS;
D O I
10.1016/j.jappgeo.2018.04.015
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Magnetotelluric (MT) data has been widely used to image underground electrical structural. However, when the significant axial resistivity anisotropy presents, how this influences three-dimensional MT data has not been resolved clearly yet. We here propose a scheme for three-dimensional modeling of MT data in presence of axial anisotropic resistivity, where the electromagnetic fields are decomposed into primary and secondary components. A 3D staggered-grid finite difference method is then used to resolve the resulting 3D governing equations. Numerical tests have completed to validate the correctness and accuracy of the present algorithm. A limited-memory Broyden-Fletcher-Goldfarb-Shanno method is then utilized to realize the 3D MT axial anisotropic inversion. The testing results show that, compared to the results of isotropic resistivity inversion, taking account the axial anisotropy can much improve the inverted results. (C) 2018 Elsevier B.V. All rights reserved.
引用
收藏
页码:75 / 89
页数:15
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