Research of a new algorithm on denoising frequency domain magnetotelluric data based on morphological clustering

被引:0
|
作者
Guo R. [1 ,2 ,3 ]
Tong W. [1 ,2 ]
Liu J. [1 ,2 ,3 ]
Wang Y. [1 ,2 ]
Yin Z. [1 ,2 ]
Chen H. [1 ,2 ]
机构
[1] Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Central South University, Ministry of Education, Changsha
[2] Hunan Key Laboratory of Nonferrous Resources and Geological Hazards Exploration, Central South University, Changsha
[3] School of Geosciences and Info-Physics, Central South University, Changsha
基金
中国国家自然科学基金;
关键词
clustering; Fourier transform; magnetotelluric method; signal processing;
D O I
10.11817/j.issn.1672-7207.2023.10.015
中图分类号
学科分类号
摘要
The magnetotelluric (MT) method is a geophysical method that uses natural electromagnetic sources for deep geoelectric structure exploration, but its signals are susceptible to various noise interferences. To better identify the MT signals and noise, a method for automatic clustering was proposed based on the MT signal patterns in the frequency domain, and the algorithm was used to calculate with synthetic and measured data. The results show that in the frequency domain, MT signal patterns have some similarities, and strong interference noise has specific characteristics different from the signal. Such characteristics can be distinguished using cosine similarity, and the signal can be separated from the noise using a clustering algorithm. The apparent resistivity and phase curves calculated by the new algorithm are smoother and more continuous, indicating a significant improvement in MT impedance estimation by using the improved method. © 2023 Central South University of Technology. All rights reserved.
引用
收藏
页码:3937 / 3948
页数:11
相关论文
共 51 条
  • [1] DONG Shuwen, LI Tingdong, SinoProbe: the exploration of the deep interior beneath the Chinese continent, Acta Geologica Sinica, 83, 7, pp. 895-909, (2009)
  • [2] YANG Bo, XU Yixian, HE Zhanxiang, Et al., 3D frequency-domain modeling of marine controlled source electromagnetic responses with topography using finite volume method, Chinese Journal of Geophysics, 55, 4, (2012)
  • [3] SU Meixia, YANG Bo, WU Yanjun, Et al., Deep mineralization processes in the central south Great Hinggan magmatic belt, Geological Review, 66, 5, (2020)
  • [4] DONG Hao, WEI Wenbo, YE Gaofeng, Et al., Study of two dimensional magnetotelluric inversions of complex three dimensional structures, Chinese Journal of Geophysics, 55, 12, pp. 4003-4014, (2012)
  • [5] ZHANG Kun, DONG Hao, YAN Jiayong, Et al., A NLCG inversion method of magnetotellurics with parallel structure, Chinese Journal of Geophysics, 56, 11, (2013)
  • [6] DONG Hao, Research on 3D terrain inversion of magnetotelluric sounding zone based on finite difference method, pp. 16-44, (2013)
  • [7] DONG Hao, WEI Wenbo, YE Gaofeng, Et al., Study of three-dimensional magnetotelluric inversion including surface topography based on finite-difference method, Chinese Journal of Geophysics, 57, 3, (2014)
  • [8] YAN Jiabin, Research on theory and method of magnetotelluric signal processing, pp. 49-72, (2003)
  • [9] YANG Wencai, ZHANG Luolei, XU Yixian, Et al., Three dimensional electrical resistivity structures of the Tarim Basin, Acta Geologica Sinica, 89, 12, (2015)
  • [10] ZHANG Letian, JIN Sheng, WEI Wenbo, Et al., Electrical structure of crust and upper mantle beneath the eastern margin of the Tibetan Plateau and the Sichuan Basin, Chinese Journal of Geophysics, 55, 12, pp. 4126-4137, (2012)