2.5D forward modeling and inversion of frequency-domain airborne electromagnetic data

被引:17
|
作者
Li Wen-Ben [1 ]
Zeng Zhao-Fa [1 ]
Li Jing [1 ]
Chen Xiong [1 ]
Wang Kun [1 ]
Xia Zhao [1 ]
机构
[1] Jilin Univ, Coll Geoexplorat Sci & Technol, Changchun 130026, Peoples R China
基金
中国国家自然科学基金;
关键词
Frequency-domain airborne electromagnetic; finite element method; 2.5D geoelectric model; damped least-squares method; LATERALLY-CONSTRAINED INVERSION; 3D INVERSION; RESISTIVITY; 2-D; REGION;
D O I
10.1007/s11770-016-0548-y
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Frequency-domain airborne electromagnetics is a proven geophysical exploration method. Presently, the interpretation is mainly based on resistivity-depth imaging and one-dimensional layered inversion; nevertheless, it is difficult to obtain satisfactory results for two-or three-dimensional complex earth structures using 1D methods. 3D forward modeling and inversion can be used but are hampered by computational limitations because of the large number of data. Thus, we developed a 2.5D frequency-domain airborne electromagnetic forward modeling and inversion algorithm. To eliminate the source singularities in the numerical simulations, we split the fields into primary and secondary fields. The primary fields are calculated using homogeneous or layered models with analytical solutions, and the secondary (scattered) fields are solved by the finite-element method. The linear system of equations is solved by using the large-scale sparse matrix parallel direct solver, which greatly improves the computational efficiency. The inversion algorithm was based on damping least-squares and singular value decomposition and combined the pseudo forward modeling and reciprocity principle to compute the Jacobian matrix. Synthetic and field data were used to test the effectiveness of the proposed method.
引用
收藏
页码:37 / 47
页数:11
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