Reevaluating the necessity of static shift correction in magnetotelluric inversion

Magnetotelluric (MT) is a significant electromagnetic exploration method. However, due to uneven distribution of surface charges and other factors, static shift often affects observed data, reducing the accuracy of inversion and interpretation. Correcting static shift through data processing remains...

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Main Authors: Jingzhong Zeng, Xiaobin Chen, Peijie Wang, Zhongyin Liu, Juntao Cai
Format: Article
Language:English
Published: Frontiers Media S.A. 2025-02-01
Series:Frontiers in Earth Science
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Online Access:https://www.frontiersin.org/articles/10.3389/feart.2025.1527004/full
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author Jingzhong Zeng
Jingzhong Zeng
Xiaobin Chen
Xiaobin Chen
Peijie Wang
Zhongyin Liu
Zhongyin Liu
Juntao Cai
Juntao Cai
author_facet Jingzhong Zeng
Jingzhong Zeng
Xiaobin Chen
Xiaobin Chen
Peijie Wang
Zhongyin Liu
Zhongyin Liu
Juntao Cai
Juntao Cai
author_sort Jingzhong Zeng
collection DOAJ
description Magnetotelluric (MT) is a significant electromagnetic exploration method. However, due to uneven distribution of surface charges and other factors, static shift often affects observed data, reducing the accuracy of inversion and interpretation. Correcting static shift through data processing remains a challenging task. Based on the characteristic that static shift affects only apparent resistivity data without impacting phase data, this paper proposes an inversion strategy that avoids static shift correction. At sites affected by static shift, apparent resistivity data are excluded, and only phase data are used in the inversion. Synthetic and field data tests indicate that the reduced inclusion of apparent resistivity data has minimal impact on inversion results, and due to the exclusion of data influenced by static shift, the inversion accurately reflects deep anomalous structures. This demonstrates that by excluding apparent resistivity data and relying solely on phase data at static-shifted sites, accurate inversion results can be achieved without additional static shift correction.
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issn 2296-6463
language English
publishDate 2025-02-01
publisher Frontiers Media S.A.
record_format Article
series Frontiers in Earth Science
spelling doaj-art-22d955d031004fb6a715040e9108c9aa2025-02-10T06:49:08ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632025-02-011310.3389/feart.2025.15270041527004Reevaluating the necessity of static shift correction in magnetotelluric inversionJingzhong Zeng0Jingzhong Zeng1Xiaobin Chen2Xiaobin Chen3Peijie Wang4Zhongyin Liu5Zhongyin Liu6Juntao Cai7Juntao Cai8National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing, ChinaKey Laboratory of Compound and Chained Natural Hazards Dynamics, Ministry of Emergency Management of China, Beijing, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing, ChinaKey Laboratory of Compound and Chained Natural Hazards Dynamics, Ministry of Emergency Management of China, Beijing, ChinaDepartment of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing, ChinaKey Laboratory of Compound and Chained Natural Hazards Dynamics, Ministry of Emergency Management of China, Beijing, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing, ChinaKey Laboratory of Compound and Chained Natural Hazards Dynamics, Ministry of Emergency Management of China, Beijing, ChinaMagnetotelluric (MT) is a significant electromagnetic exploration method. However, due to uneven distribution of surface charges and other factors, static shift often affects observed data, reducing the accuracy of inversion and interpretation. Correcting static shift through data processing remains a challenging task. Based on the characteristic that static shift affects only apparent resistivity data without impacting phase data, this paper proposes an inversion strategy that avoids static shift correction. At sites affected by static shift, apparent resistivity data are excluded, and only phase data are used in the inversion. Synthetic and field data tests indicate that the reduced inclusion of apparent resistivity data has minimal impact on inversion results, and due to the exclusion of data influenced by static shift, the inversion accurately reflects deep anomalous structures. This demonstrates that by excluding apparent resistivity data and relying solely on phase data at static-shifted sites, accurate inversion results can be achieved without additional static shift correction.https://www.frontiersin.org/articles/10.3389/feart.2025.1527004/fullmagnetotelluricsinversionapparent resistivityimpedance phasestatic shift
spellingShingle Jingzhong Zeng
Jingzhong Zeng
Xiaobin Chen
Xiaobin Chen
Peijie Wang
Zhongyin Liu
Zhongyin Liu
Juntao Cai
Juntao Cai
Reevaluating the necessity of static shift correction in magnetotelluric inversion
Frontiers in Earth Science
magnetotellurics
inversion
apparent resistivity
impedance phase
static shift
title Reevaluating the necessity of static shift correction in magnetotelluric inversion
title_full Reevaluating the necessity of static shift correction in magnetotelluric inversion
title_fullStr Reevaluating the necessity of static shift correction in magnetotelluric inversion
title_full_unstemmed Reevaluating the necessity of static shift correction in magnetotelluric inversion
title_short Reevaluating the necessity of static shift correction in magnetotelluric inversion
title_sort reevaluating the necessity of static shift correction in magnetotelluric inversion
topic magnetotellurics
inversion
apparent resistivity
impedance phase
static shift
url https://www.frontiersin.org/articles/10.3389/feart.2025.1527004/full
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