Regularized inversion of controlled source audio-frequency magnetotelluric data in horizontally layered transversely isotropic media

被引:10
|
作者
Zhou, Jianmei [1 ]
Wang, Jianxun [2 ]
Shang, Qinglong [1 ]
Wang, Hongnian [1 ]
Yin, Changchun [3 ]
机构
[1] Jilin Univ, Coll Phys, Changchun 130012, Peoples R China
[2] Jilin Univ, Coll Elect Sci & Engn, Changchun 130012, Peoples R China
[3] Jilin Univ, Coll Geoexplorat Sci & Technol, Changchun 130013, Peoples R China
关键词
CSAMT; transversely isotropic; regularized inversion; ELECTROMAGNETIC-FIELDS; ELECTRIC-DIPOLE; INDUCTION; ANISOTROPY; EARTH; SENSITIVITIES; RESPONSES; MODELS; WELL;
D O I
10.1088/1742-2132/11/2/025003
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
We present an algorithm for inverting controlled source audio-frequency magnetotelluric (CSAMT) data in horizontally layered transversely isotropic (TI) media. The popular inversion method parameterizes the media into a large number of layers which have fixed thickness and only reconstruct the conductivities (e. g. Occam's inversion), which does not enable the recovery of the sharp interfaces between layers. In this paper, we simultaneously reconstruct all the model parameters, including both the horizontal and vertical conductivities and layer depths. Applying the perturbation principle and the dyadic Green's function in TI media, we derive the analytic expression of Frechet derivatives of CSAMT responses with respect to all the model parameters in the form of Sommerfeld integrals. A regularized iterative inversion method is established to simultaneously reconstruct all the model parameters. Numerical results show that the inverse algorithm, including the depths of the layer interfaces, can significantly improve the inverse results. It can not only reconstruct the sharp interfaces between layers, but also can obtain conductivities close to the true value.
引用
收藏
页数:12
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