Comparison of stable maximum likelihood estimator with traditional robust estimator in magnetotelluric impedance estimation

被引:3
作者
Chen, Hang [1 ,2 ,3 ]
Guo, Rongwen [1 ,2 ,3 ]
Dong, Hao [4 ]
Wang, Yongfei [1 ,2 ,3 ]
Li, Jian [1 ,2 ,3 ]
机构
[1] Cent South Univ, Sch Geosci & Infophys, Changsha 410083, Hunan, Peoples R China
[2] Cent South Univ, Sch Geosci & Infophys, Hunan Key Lab Nonferrous Resources & Geol Hazards, Changsha 410083, Peoples R China
[3] Cent South Univ, Sch Geosci & Infophys, Key Lab Metallogen Predict Nonferrous Met & Geol, Minist Educ, Changsha 410083, Peoples R China
[4] China Univ Geosci, Sch Geophys & Informat Technol, Beijing 100083, Peoples R China
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
Magnetotelluric; Stable distribution; Maximum likelihood estimator; Robust estimator; Leverage points; INVERSION; BASIN;
D O I
10.1016/j.jappgeo.2020.104046
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The newly developed stable maximum likelihood estimator (MLE) has been considered to be superior to the traditional robust estimation for Magnetotelluric (MT) transfer functions, based on the examination of field data. However, due to the unknown MT response function for real data, it is difficult to judge the validity of any comparisons between the performance of the two estimators. This can be realized by comparing the performances on synthetic data, as different ideal error distributions can be modeled (e.g., noise contaminated magnetic fields can be simulated by adding desired noise into the assumed clean version). In this paper, we generate synthetic MT data with desired error distributions (e.g. Gaussian and Cauchy distributions) based on the estimated MT impedance and Fourier transformed measured magnetic data (as the input) from one MT site located in southeast part of Tibet Plateau collected under the SinoProbe project. The comparison is demonstrated in terms of the apparent resistivity and phase, and their estimated standard deviations. The performance of the two methods and their variants are tested based on generated synthetic data with various noise patterns. Synthetic tests indicate that their performance in terms of handling noisy data is generally comparable. The bias in the estimation is more sensitive to noise in the input. Then they are applied to process real data from two MT sites in the same region, indicating their solutions are generally similar. (C) 2020 Published by Elsevier B.V.
引用
收藏
页数:11
相关论文
共 30 条
  • [1] [Anonymous], 2003, ROBUST REGRESSION OU
  • [2] [Anonymous], [No title captured]
  • [3] [Anonymous], [No title captured]
  • [4] Understanding hydrothermal circulation patterns at a low-enthalpy thermal spring using audio-magnetotelluric data: A case study from Ireland
    Blake, Sarah
    Henry, Tiernan
    Muller, Mark R.
    Jones, Alan G.
    Moore, John Paul
    Murray, John
    Campanya, Joan
    Vozar, Jan
    Walsh, John
    Rath, Volker
    [J]. JOURNAL OF APPLIED GEOPHYSICS, 2016, 132 : 1 - 16
  • [5] Chave A.D., 2012, The Magnetotelluric Method: Theory and Practice, P165, DOI [10.1017/CBO9781139020138.007, DOI 10.1017/CBO9781139020138.007]
  • [6] Bounded influence magnetotelluric response function estimation
    Chave, AD
    Thomson, DJ
    [J]. GEOPHYSICAL JOURNAL INTERNATIONAL, 2004, 157 (03) : 988 - 1006
  • [7] SOME COMMENTS ON MAGNETOTELLURIC RESPONSE FUNCTION ESTIMATION
    CHAVE, AD
    THOMSON, DJ
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1989, 94 (B10): : 14215 - 14225
  • [8] ON THE ROBUST ESTIMATION OF POWER SPECTRA, COHERENCES, AND TRANSFER-FUNCTIONS
    CHAVE, AD
    THOMSON, DJ
    ANDER, ME
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1987, 92 (B1): : 633 - 648
  • [9] Estimation of the Magnetotelluric Response Function: The Path from Robust Estimation to a Stable Maximum Likelihood Estimator
    Chave, Alan D.
    [J]. SURVEYS IN GEOPHYSICS, 2017, 38 (05) : 837 - 867
  • [10] Magnetotelluric data, stable distributions and impropriety: an existential combination
    Chave, Alan D.
    [J]. GEOPHYSICAL JOURNAL INTERNATIONAL, 2014, 198 (01) : 622 - 636