Tomographic analysis of self-potential data in a seismic area of Southern Italy

The time and space anomalous behaviour of the Self-Potential (SP) field recorded in a seismic area of Southern Apennines, Italy, is discussed. The SP data were collected in the period June 1992-November 1994 along a profile located north of the town of Potenza in the Basilicata region, Italy. The pr...

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Main Authors: S. Piscitelli, D. Patella, V. Lapenna
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2000-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3638
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spelling doaj-1c5b694fb1f141ee8d6dfe28d63362182020-11-24T23:02:55ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2000-06-0143210.4401/ag-3638Tomographic analysis of self-potential data in a seismic area of Southern ItalyS. PiscitelliD. PatellaV. LapennaThe time and space anomalous behaviour of the Self-Potential (SP) field recorded in a seismic area of Southern Apennines, Italy, is discussed. The SP data were collected in the period June 1992-November 1994 along a profile located north of the town of Potenza in the Basilicata region, Italy. The profile is perpendicular to an active fault system, where a W-E directed strike-slip structure has been identified from recent earthquakes. The SP data are modelled using a new tomographic method based on the search for similarities between the observed SP sequence and the surface signature of the electric field due to a scanning point source with unitary positive charge. The point scanner is ideally moved in a vertical cross-section through the profile and a regular 2D matrix of charge occurrence probability values is thus obtained. These values are used to image the state of electric polarization in the subsoil, compatible with the observed SP surface pattern. A selection of 2D tomographies across the profile is then discussed in order to outline the SP source geometry and dynamics within the faulted structure. Finally, the time pattern of the SP polarization state is compared with the local seismicity in the frame of the rock dilatancy-fluid diffusion theory. This comparison allows us to exclude a direct relationship of the SP time behaviour with the seismic sequences which occurred in the area during the SP monitoring period.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3638self-potentialtomographic techniquefault systemsouthern apennines
collection DOAJ
language English
format Article
sources DOAJ
author S. Piscitelli
D. Patella
V. Lapenna
spellingShingle S. Piscitelli
D. Patella
V. Lapenna
Tomographic analysis of self-potential data in a seismic area of Southern Italy
Annals of Geophysics
self-potential
tomographic technique
fault system
southern apennines
author_facet S. Piscitelli
D. Patella
V. Lapenna
author_sort S. Piscitelli
title Tomographic analysis of self-potential data in a seismic area of Southern Italy
title_short Tomographic analysis of self-potential data in a seismic area of Southern Italy
title_full Tomographic analysis of self-potential data in a seismic area of Southern Italy
title_fullStr Tomographic analysis of self-potential data in a seismic area of Southern Italy
title_full_unstemmed Tomographic analysis of self-potential data in a seismic area of Southern Italy
title_sort tomographic analysis of self-potential data in a seismic area of southern italy
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2000-06-01
description The time and space anomalous behaviour of the Self-Potential (SP) field recorded in a seismic area of Southern Apennines, Italy, is discussed. The SP data were collected in the period June 1992-November 1994 along a profile located north of the town of Potenza in the Basilicata region, Italy. The profile is perpendicular to an active fault system, where a W-E directed strike-slip structure has been identified from recent earthquakes. The SP data are modelled using a new tomographic method based on the search for similarities between the observed SP sequence and the surface signature of the electric field due to a scanning point source with unitary positive charge. The point scanner is ideally moved in a vertical cross-section through the profile and a regular 2D matrix of charge occurrence probability values is thus obtained. These values are used to image the state of electric polarization in the subsoil, compatible with the observed SP surface pattern. A selection of 2D tomographies across the profile is then discussed in order to outline the SP source geometry and dynamics within the faulted structure. Finally, the time pattern of the SP polarization state is compared with the local seismicity in the frame of the rock dilatancy-fluid diffusion theory. This comparison allows us to exclude a direct relationship of the SP time behaviour with the seismic sequences which occurred in the area during the SP monitoring period.
topic self-potential
tomographic technique
fault system
southern apennines
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3638
work_keys_str_mv AT spiscitelli tomographicanalysisofselfpotentialdatainaseismicareaofsouthernitaly
AT dpatella tomographicanalysisofselfpotentialdatainaseismicareaofsouthernitaly
AT vlapenna tomographicanalysisofselfpotentialdatainaseismicareaofsouthernitaly
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