Identifying the occurrence time of an impending mainshock: A very recent case

Fuente: arXiv
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Main Authors: Varotsos, P. A., Sarlis, N. V., Skordas, E. S., Lazaridou-Varotsos, M. S.
Format: Preprint
Published: 2019
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_version_ 1866910106030964736
author Varotsos, P. A.
Sarlis, N. V.
Skordas, E. S.
Lazaridou-Varotsos, M. S.
author_facet Varotsos, P. A.
Sarlis, N. V.
Skordas, E. S.
Lazaridou-Varotsos, M. S.
contents The procedure by means of which the occurrence time of an impending mainshock can be identified by analyzing in natural time the seismicity in the candidate area subsequent to the recording of a precursory Seismic Electric Signals (SES) activity is reviewed. Here, we report the application of this procedure to an Mw5.4 mainshock that occurred in Greece on 17 November 2014 and was strongly felt in Athens. This mainshock (which is pretty rare since it is the strongest in that area for more than half a century) was preceded by an SES activity recorded on 27 July 2014 and the results of the natural time analysis reveal that the system approached the critical point (mainshock occurrence) early in the morning on 15 November 2014. SES activities that have been recently recorded are also presented. Furthermore, in a Note we discuss the case of the Mw5.3 earthquake that was also strongly felt in Athens on 19 July 2019 (Parnitha fault).
format Preprint
id arxiv_https___arxiv_org_abs_1908_00279
institution arXiv
publishDate 2019
record_format arxiv
spellingShingle Identifying the occurrence time of an impending mainshock: A very recent case
Varotsos, P. A.
Sarlis, N. V.
Skordas, E. S.
Lazaridou-Varotsos, M. S.
Geophysics
Statistical Mechanics
The procedure by means of which the occurrence time of an impending mainshock can be identified by analyzing in natural time the seismicity in the candidate area subsequent to the recording of a precursory Seismic Electric Signals (SES) activity is reviewed. Here, we report the application of this procedure to an Mw5.4 mainshock that occurred in Greece on 17 November 2014 and was strongly felt in Athens. This mainshock (which is pretty rare since it is the strongest in that area for more than half a century) was preceded by an SES activity recorded on 27 July 2014 and the results of the natural time analysis reveal that the system approached the critical point (mainshock occurrence) early in the morning on 15 November 2014. SES activities that have been recently recorded are also presented. Furthermore, in a Note we discuss the case of the Mw5.3 earthquake that was also strongly felt in Athens on 19 July 2019 (Parnitha fault).
title Identifying the occurrence time of an impending mainshock: A very recent case
topic Geophysics
Statistical Mechanics
url https://arxiv.org/abs/1908.00279