Electromagnetic Field Generated by an Earthquake Source Due to Motional Induction in 3D Stratified Media, and Application to 2008 M w 6.1 Qingchuan Earthquake-Reference-Cited by-同舟云学术

Electromagnetic Field Generated by an Earthquake Source Due to Motional Induction in 3D Stratified Media, and Application to 2008 M w 6.1 Qingchuan Earthquake

Published:2021-10 Issue:10 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Zhao Jie¹^ORCID,Gao Yongxin¹^ORCID,Tang Ji²,Klemperer Simon L.³^ORCID,Wen Jian⁴,Chen Chieh‐Hung⁵^ORCID,Chong Jiajun⁶⁷

Affiliation:

1. Institute of Applied Mechanics School of Civil Engineering Hefei University of Technology Hefei China

2. Institute of Geology China Earthquake Administration Beijing China

3. Department of Geophysics Stanford University Stanford CA USA

4. School of Earth and Space Sciences University of Science and Technology of China Hefei China

5. Institute of Geophysics and Geomatics China University of Geosciences Wuhan China

6. Innovation Academy for Precision Measurement Science and Technology Chinese Academy of Sciences Wuhan China

7. State Key Laboratory of Geodesy and Earth's Dynamics Wuhan China

Funder

National Natural Science Foundation of China

Youth Innovation Promotion Association

Fundamental Research Funds for the Central Universities of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB022102

Reference41 articles.

1. Co-seismic EM signals in magnetotelluric measurement—a case study during Bhuj earthquake (26th January 2001), India

2. Low-frequency, motionally induced electromagnetic fields in the ocean: 1. Theory

3. Co-seismic geomagnetic fluctuations and atmospheric disturbances during the 2018 M 6.2 Hualien Earthquake

4. Theory of electrokinetic-magnetic anomalies in a faulted half-space

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