Three-dimensional tensor controlled-source electromagnetic modeling based on the vector finite-element method

被引:26
|
作者
Hu Ying-Cai [1 ]
Li Tong-Lin [1 ]
Fan Cui-Song [2 ]
Wang Da-Yong [3 ]
Li Jian-Ping [4 ]
机构
[1] Jilin Univ, Coll Geoexplorat Sci & Technol, Changchun 130026, Peoples R China
[2] China Geol Survey, Tianjing Ctr, Tianjin 300170, Peoples R China
[3] Chinese Acad Geol Sci, Inst Geophys & Geochem Explorat, Langfang 065000, Peoples R China
[4] ShanDong Univ Sci & Technol, Coll Geosci & Technol, Qingdao 266590, Peoples R China
基金
中国国家自然科学基金;
关键词
CSAMT; model; impedance tensor; VFEM; SPRINGS THERMAL AREA; VALLES CALDERA; CSAMT SURVEY; NEW-MEXICO; USA;
D O I
10.1007/s11770-014-0469-1
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
Scalar CSAMT is only suitable for measurements in one and two dimensions perpendicular to geological structures. For complex 3D geoelectric structure, tensor CSAMT is more suitable. In this paper, we discuss 3D tensor CSAMT forward modeling using the vector finite-element method. To verify the feasibility of the algorithm, we calculate the electric field, magnetic field, and tensor impedance of the 3D CSAMT far-zone field in layered media and compare them with theoretical solutions. In addition, a three-dimensional anomaly in half-space is also simulated, and the response characteristics of the impedance tensor and the apparent resistivity and impedance phase are analyzed. The results suggest that the vector finite-element method produces high-precision electromagnetic field and impedance tensor data, satisfies the electric field discontinuity, and does not require divergence correction using the vector finite-element method.
引用
收藏
页码:35 / 46
页数:12
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