2D joint inversion of CSAMT and magnetic data based on cross-gradient theory

被引:16
|
作者
Wang, Kun-Peng [1 ]
Tan, Han-Dong [1 ,2 ]
Wang, Tao [3 ]
机构
[1] China Univ Geosci Beijing, Sch Geophys & informat Technol, Beijing 100083, Peoples R China
[2] China Univ Geosci, Key Lab Geodetect, Minist Educ, Beijing 100083, Peoples R China
[3] 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
CSAMT; magnetic method; data space inversion; cross-gradient; joint inversion; MAGNETOTELLURIC DATA; RESISTIVITY; ALGORITHM; GRAVITY; SMOOTH; MODELS;
D O I
10.1007/s11770-017-0615-z
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
A two-dimensional forward and backward algorithm for the controlled-source audio-frequency magnetotelluric (CSAMT) method is developed to invert data in the entire region (near, transition, and far) and deal with the effects of artificial sources. First, a regularization factor is introduced in the 2D magnetic inversion, and the magnetic susceptibility is updated in logarithmic form so that the inversion magnetic susceptibility is always positive. Second, the joint inversion of the CSAMT and magnetic methods is completed with the introduction of the cross gradient. By searching for the weight of the cross-gradient term in the objective function, the mutual influence between two different physical properties at different locations are avoided. Model tests show that the joint inversion based on cross-gradient theory offers better results than the single-method inversion. The 2D forward and inverse algorithm for CSAMT with source can effectively deal with artificial sources and ensures the reliability of the final joint inversion algorithm.
引用
收藏
页码:279 / 290
页数:12
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