In Search of Correlations between Geoelectrical Signals and Earthquakes in a Seismic Active
Area of Southern Italy
HR: 0830h
AN: T51E-0203 [PDF]
TI: In Search of Correlations between Geoelectrical Signals and Earthquakes in a Seismic Active Area of
Southern Italy
AU: * Vincenzo, L
EM: lapenna@imaa.cnr.it
AF: Ist. di Metodologie per l'Analisi Ambientale, Zona Industriale
Tito Scalo, Tito, PZ I-85050
Italy
AU: Marianna, B
EM: balasco@imaa.cnr.it
AF: Ist. di Metodologie per l'Analisi Ambientale, Zona Industriale
Tito Scalo, Tito, PZ I-85050
Italy
AU: Gerardo, C
EM: colangelo@imaa.cnr.it
AF: Ist. di Metodologie per l'Analisi Ambientale, Zona Industriale
Tito Scalo, Tito, PZ I-85050
Italy
AU: Maria, M
EM: macchiato@na.infn.it
AF: Dip. di Scienze Fisiche, Univ. di Napoli
Via Cintia, Naples, NA I-80123
Italy
AU: Luciano, T
EM: ltelesca@imaa.cnr.it
AF: Ist. di Metodologie per l'Analisi Ambientale, Zona Industriale
Tito Scalo, Tito, PZ I-85050
Italy
AB:
The aim of this work is to investigate the possible correlation between electrical anomalous patterns and incoming
earthquakes in a seismic active area of Southern Apennine chain (Italy). In this research field, the greatest problem is the
sporadically monitoring activities in time and space. A very weak point is also the current approach to time series analysis
that makes no use of robust statistical methods to discriminate extreme events from random noise. Further, the lack of
objective criteria to assess the precursory character of the geophysical anomalous signals makes the short-term predictions
based on them poorly reliable. Altogether these shortages concur to explain the low scientific consensus placed so far on the
claimed correlation between the observed geophysical anomalies and the occurrence of earthquakes.
Taking into account these considerations, in this paper we analyse the self-potential time series coming from a new
geophysical monitoring network installed in a seismic active area of the Southern Apennine chain (Southern Italy). All the
remote stations (Tramutola, Tito, Giuliano, Marsico Nuovo and Laterza) are equipped with multi-electrode array able to
detect the time fluctuations of self-potential along two directions, N-S and E-W. The monitoring strategy combines new
technologies for data acquisition with advanced statistical packages for the identification of the extreme events in
geophysical time series. During the last years a very large data-base of self-potential time series has been organized and it
is actually available to assess robust statistical methodologies to identify extreme events.
Firstly, we have investigated the inner dynamical structure the self-potential time series and we have filtered the effects
induced by climatological parameters (temperature, rainfall, etc.). In a second step, we propose robust statistical methods
to pick out extreme events from background electrical noise. Finally, we compare the extreme events identified in the
self-potential time series and the earthquakes sequences recorded during the past 5 years (1997-2002) in the investigated
area. The results allow us to obtain only in few cases a significant correlation between sequence of extreme events in
electrical signals and incoming earthquakes, the measuring period is not sufficient to perform an high number of statistical
checks. However the time dynamics of self-potential signals seem to be correlate with the fluctuations of seismic cycle over
long time periods.
DE: 0619 Electromagnetic theory
DE: 0903 Computational methods, potential fields
DE: 0910 Data processing
DE: 1744 Tectonophysics
DE: 3250 Fractals and multifractals
SC: Tectonophysics [T]
MN: 2003 Fall Meeting