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A Comparative Study of Geoelectric Signals Possibly Associated with the Occurrence of Two Ms > 7 EQs in the South Pacific Coast of Mexico
Author(s) -
Lev Guzmán-Vargas,
Carlos Carrizales-Velazquez,
Israel Reyes-Ramírez,
Jorge Fonseca-Campos,
Arturo de la Rosa-Galindo,
Víctor O. Quintana-Moreno,
José Antonio Peralta,
F. AnguloBrown
Publication year - 2019
Publication title -
entropy
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.468
H-Index - 74
ISSN - 1099-4300
DOI - 10.3390/e21121225
Subject(s) - detrended fluctuation analysis , magnitude (astronomy) , seismology , geology , range (aeronautics) , uncorrelated , series (stratigraphy) , exponent , shock (circulatory) , physics , scaling , statistics , paleontology , mathematics , astrophysics , medicine , geometry , materials science , composite material , linguistics , philosophy
During past decades, several studies have suggested the existence of possible seismic electric precursors associated with earthquakes of magnitudeM > 7. However, additional analyses are needed to have more reliable evidence of pattern behavior prior to the occurrence of a big event. In this article we report analyses of self-potentialΔ Vrecords during approximately two years in three electro-seismic stations in Mexico located at Acapulco, Guerrero; Petatlán, Guerrero and Pinotepa Nacional, Oaxaca. On 18 April 2014 anM s 7.2earthquake occurred near our Petatlán station. Our study shows two notable anomalies observed in the behavior of the Fourier power spectrum ofΔ Vfor ultra low frequency ULF-range, and the transition of theα l-exponent of the detrended fluctuation analysis of theΔ Vtime series from uncorrelated to correlated signals. These anomalies lasted approximately three and a half months before the main shock. We compare this electric pattern with another electric signal we reported associated with anM s 7.4that occurred on 14 September 1995 at Guerrero state, Mexico. Our characterization of the anomalies observed in both signals point out similar features that enrich our knowledge about precursory phenomena linked to the occurrence of earthquakes of magnitudeM > 7.

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