Abstract
Fully recognize various problems in the observed magnetotelluric (MT) data is the precondition of inverse solutions. In the paper, according to the geomorphological conditions of the observational MT stations in the Guangxi area, we constructed several different kinds of models to conduct a three-dimensional forward simulation of the MT field using the vector finite element method (FEM). First, the variation rule and differences of apparent resistivity ρxy and ρyx in the xy and yx modes were studied and analyzed, and then the geoelectric information reflected by the change of apparent resistivity ρxx and ρyy were discussed. Final, the responses of typical geological structures that cause a static shift problem were presented. The synthetic examples showed that ρxy and ρyx were relevant to the layout of the survey line, for instance, ρxy had different values along the west-east profile compared with that of the south-north profile, Moreover, ρxx and ρyy could subtly show the abnormal body-host rock interface, which could be used to restrict the anomalous domain in the inversion process. In addition to the scale and depth of the top surface of the anomalous body, the widespread rivers and hills, can simulate static shift. Hence, to reduce the influence of static shift on MT data, a reasonable distance between a station and rivers or hills should be considered in accordance with the scale of rivers or hills.
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Acknowledgments
The authors would like to thank Prof. C. G. Fauquharson for his constructive comments and for providing mesh data and results for comparison. We would also like to thank the anonymous reviewers for their constructive criticism.
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This paper was partially supported by the National Natural Science Foundation of China (No. 41674075 and 41904123); the Natural Science Foundation of Guangxi Province (No. 2016GXNSFGA380004); and the High Level Innovative Team and Excellent Scholar Plan of Guangxi High Education Institution.
Xiong Bin, Professor, received his B.S. and Ph.D. degree from Jilin University in 1998, and China University of Geoscience (Wuhan) in 2004, respectively. From 2004 to 2006, he worked on post-doc at Central South University and became an Associate Professor in 2006. And now he works at Guilin University of Technology as Professor. His research interests are electromagnetic numerical modeling and inversion. Email: xiongbin@glut.edu.cn
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Bin, X., Tian-Ya, L., Long-Wei, C. et al. Influence of complex topography on magnetotelluric-observed data using three-dimensional numerical simulation: A case from Guangxi area, China. Appl. Geophys. 17, 601–615 (2020). https://doi.org/10.1007/s11770-020-0842-6
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DOI: https://doi.org/10.1007/s11770-020-0842-6