The possibility of obtaining nearby 3D resistivity structure from magnetotelluric 2D profile data using 3D inversion

被引:11
作者
Lin Chang-Hong [1 ,2 ,3 ]
Tan Han-Dong [1 ,2 ,3 ]
Tong Tuo [1 ,2 ,3 ]
机构
[1] China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China
[2] China Univ Geosci, Minist Educ, Key Lab Geodetect, Beijing 100083, Peoples R China
[3] China Univ Geosci, Sch Geophys & Informat Technol, Beijing 100083, Peoples R China
来源
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION | 2011年 / 54卷 / 01期
关键词
Magnetotelluric inversion; 2D; 3D; Tensor elements; NONLINEAR CONJUGATE GRADIENTS; RAPID RELAXATION INVERSION;
D O I
10.3969/j.issn.0001-5733.2011.01.026
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
Currently, most of MT(magnetotelluric) data are still collected on 2D profiles. The issue that most MT researchers concern is how to invert these 2D profile data to get better results, which are closer to the real structure. Based on the analysis of 3D tensor impedance response generated from the test models and on the study of the inversion results of synthetic data and field data, we discuss the possibility of obtaining nearby 3D resistivity structure from magnetotelluric 2D profile data using 3D inversion. The results show that it is possible to interpret 2D profile data using 3D inversion method. Not only a reasonable image beneath the profile but also reasonable pictures of nearby 3D structure which can not be got by 2D inversion can be obtained using all tensor elements of the 2D profile data in the 3D inversion. The synthetic examples show that the on-diagonal elements have special effect on recovering the distribution of 3D abnormity near the profile. Therefore, all the tensor elements are suggested to be used in 3D inversion to interpret the profile data.
引用
收藏
页码:245 / 256
页数:12
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