Articles | Volume 20, issue 5
https://doi.org/10.5194/nhess-20-1485-2020
https://doi.org/10.5194/nhess-20-1485-2020
Research article
 | 
27 May 2020
Research article |  | 27 May 2020

The spatial–temporal total friction coefficient of the fault viewed from the perspective of seismo-electromagnetic theory

Patricio Venegas-Aravena, Enrique G. Cordaro, and David Laroze

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (14 Mar 2020) by Heidi Kreibich
AR by Patricio Venegas-Aravena on behalf of the Authors (08 Apr 2020)  Author's response    Manuscript
ED: Publish as is (26 Apr 2020) by Filippos Vallianatos
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Short summary
Over the past few years, a number of data have emerged on predicting large earthquakes using the magnetic field. These measurements are becoming strongly supported by rock electrification mechanisms experimentally and theoretically in seismo-electromagnetic theory. However, the processes that occur within the faults have yet to be elucidated. That is why this work theoretically links the friction changes of the faults with the lithospheric magnetic anomalies that surround the faults.
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