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

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

doi:https://doi.org/10.5194/nhess-20-1485-2020

Articles | Volume 20, issue 5

https://doi.org/10.5194/nhess-20-1485-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/nhess-20-1485-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 20, issue 5

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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Final revised paper (published on 27 May 2020)
Preprint (discussion started on 28 Nov 2019)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'The spatial-temporal total friction coefficient of the fault viewed from the seismo-electromagnetic theory. By Patricio Venegas-Aravena , Enrique G. Cordaro , David Laroze', Michael E. Contadakis, 19 Jan 2020
- AC1: 'Response R1', Patricio Venegas-Aravena, 26 Feb 2020
RC2: 'Comments to “The spatial-temporal total friction coefficient of the fault viewed from the seismo-electromagnetic theory” by Venegas-Aravena P. et al. submitted to NHESS', Angelo De Santis, 13 Feb 2020
- AC2: 'Response R2', Patricio Venegas-Aravena, 26 Feb 2020

Peer-review completion

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

AR by Patricio Venegas-Aravena on behalf of the Authors (28 Apr 2020) Manuscript

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.