Spectral and multifractal study of electroseismic time series associated to the <i>M<sub>w</sub></i>=6.5 earthquake of 24 October 1993 in Mexico

In this work we present a spectral and multifractal study of the electric self-potential fluctuations registered in an electroseismic station located at 100km from the epicenter of an earthquake (EQ) with <i>M<sub>w</sub></i>=6.5 in the Pacific coast of Mexico. Our study sugg...

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Main Authors: A. Ramírez-Rojas, A. Muñoz-Diosdado, C. G. Pavía-Miller, F. Angulo-Brown
Format: Article
Language:English
Published: Copernicus Publications 2004-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/4/703/2004/nhess-4-703-2004.pdf
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spelling doaj-c471e53b45734653b39d27aa7e4e64ca2020-11-25T01:08:48ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812004-01-0145/6703709Spectral and multifractal study of electroseismic time series associated to the <i>M<sub>w</sub></i>=6.5 earthquake of 24 October 1993 in MexicoA. Ramírez-RojasA. Muñoz-DiosdadoC. G. Pavía-MillerC. G. Pavía-MillerF. Angulo-BrownIn this work we present a spectral and multifractal study of the electric self-potential fluctuations registered in an electroseismic station located at 100km from the epicenter of an earthquake (EQ) with <i>M<sub>w</sub></i>=6.5 in the Pacific coast of Mexico. Our study suggests that in general the time series analyzed displays a persistent behavior. Our results show an anticorrelation between the spectral exponent &beta; and the width of the multifractal spectrum &Delta;&alpha;, when they are calculated during a time interval of five months (four months before the EQ and one month after the EQ). In addition, we also calculate the time evolution of the correlation coefficient finding that it has a very similar behavior that the time evolution of &Delta;&alpha;.http://www.nat-hazards-earth-syst-sci.net/4/703/2004/nhess-4-703-2004.pdf
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language English
format Article
sources DOAJ
author A. Ramírez-Rojas
A. Muñoz-Diosdado
C. G. Pavía-Miller
C. G. Pavía-Miller
F. Angulo-Brown
spellingShingle A. Ramírez-Rojas
A. Muñoz-Diosdado
C. G. Pavía-Miller
C. G. Pavía-Miller
F. Angulo-Brown
Spectral and multifractal study of electroseismic time series associated to the <i>M<sub>w</sub></i>=6.5 earthquake of 24 October 1993 in Mexico
Natural Hazards and Earth System Sciences
author_facet A. Ramírez-Rojas
A. Muñoz-Diosdado
C. G. Pavía-Miller
C. G. Pavía-Miller
F. Angulo-Brown
author_sort A. Ramírez-Rojas
title Spectral and multifractal study of electroseismic time series associated to the <i>M<sub>w</sub></i>=6.5 earthquake of 24 October 1993 in Mexico
title_short Spectral and multifractal study of electroseismic time series associated to the <i>M<sub>w</sub></i>=6.5 earthquake of 24 October 1993 in Mexico
title_full Spectral and multifractal study of electroseismic time series associated to the <i>M<sub>w</sub></i>=6.5 earthquake of 24 October 1993 in Mexico
title_fullStr Spectral and multifractal study of electroseismic time series associated to the <i>M<sub>w</sub></i>=6.5 earthquake of 24 October 1993 in Mexico
title_full_unstemmed Spectral and multifractal study of electroseismic time series associated to the <i>M<sub>w</sub></i>=6.5 earthquake of 24 October 1993 in Mexico
title_sort spectral and multifractal study of electroseismic time series associated to the <i>m<sub>w</sub></i>=6.5 earthquake of 24 october 1993 in mexico
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2004-01-01
description In this work we present a spectral and multifractal study of the electric self-potential fluctuations registered in an electroseismic station located at 100km from the epicenter of an earthquake (EQ) with <i>M<sub>w</sub></i>=6.5 in the Pacific coast of Mexico. Our study suggests that in general the time series analyzed displays a persistent behavior. Our results show an anticorrelation between the spectral exponent &beta; and the width of the multifractal spectrum &Delta;&alpha;, when they are calculated during a time interval of five months (four months before the EQ and one month after the EQ). In addition, we also calculate the time evolution of the correlation coefficient finding that it has a very similar behavior that the time evolution of &Delta;&alpha;.
url http://www.nat-hazards-earth-syst-sci.net/4/703/2004/nhess-4-703-2004.pdf
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