Pattern of seismicity in the Lucanian Apennines and foredeep (Southern Italy) from recording by SAPTEX temporary array

The deployment of a temporary seismic network in Southern Italy during 2001-2004 (the SAPTEX array, Southern
 APennine Tomography EXperiment) allowed us to relocate the hypocenters of Southern Apennines earthquakes
 with low uncertainty among the location parameters. The best array d...

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Main Authors: P. De Gori, G. B. Cimini, L. Amicucci, F. R. Cinti, A. Frepoli, S. Pierdominici
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2005-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3252
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spelling doaj-c401170f4f7d47fcba3005f8c60a2fb22020-11-25T02:25:41ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2005-06-0148610.4401/ag-3252Pattern of seismicity in the Lucanian Apennines and foredeep (Southern Italy) from recording by SAPTEX temporary arrayP. De GoriG. B. CiminiL. AmicucciF. R. CintiA. FrepoliS. PierdominiciThe deployment of a temporary seismic network in Southern Italy during 2001-2004 (the SAPTEX array, Southern
 APennine Tomography EXperiment) allowed us to relocate the hypocenters of Southern Apennines earthquakes
 with low uncertainty among the location parameters. The best array distribution of the SAPTEX network
 for the analysis of seismicity in the Lucanian Apennines and foredeep was reached in the first two years of
 recording. The SAPTEX data were merged with those of the Italian National Seismic Network (RSNC) operated
 by the Istituto Nazionale di Geofisica e Vulcanologia (INGV). For the hypocenters computation of events in
 the upper Agri Valley we also included P- and S- waves arrivals from the local Eni-Agip network. The seismicity
 for the Lucanian Apennines and foredeep in the analyzed period has magnitudes ranging from 2.0 to 4.1. A
 major finding is the identification of two different crustal domains: the westernmost characterizing the chain,
 mostly with shallow earthquakes (within about 20 km of depth), and the easternmost one belonging to the outer
 margin of the chain and to the foredeep, with deeper seismicity (mostly between 20-40 km of depth). Thirty
 fault-plane solutions were computed and used for stress inversion; most of them are related to earthquakes within
 the chain sector and indicate a generalized NE-SW extension. Moreover, the dense network allowed us to improve
 the location of events relative to two low magnitude sequences which occurred in the study period.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3252seismicityseismic networkmotectonicsLucanian ApenninesLucanian foredeepSouthern Italy
collection DOAJ
language English
format Article
sources DOAJ
author P. De Gori
G. B. Cimini
L. Amicucci
F. R. Cinti
A. Frepoli
S. Pierdominici
spellingShingle P. De Gori
G. B. Cimini
L. Amicucci
F. R. Cinti
A. Frepoli
S. Pierdominici
Pattern of seismicity in the Lucanian Apennines and foredeep (Southern Italy) from recording by SAPTEX temporary array
Annals of Geophysics
seismicity
seismic network
motectonics
Lucanian Apennines
Lucanian foredeep
Southern Italy
author_facet P. De Gori
G. B. Cimini
L. Amicucci
F. R. Cinti
A. Frepoli
S. Pierdominici
author_sort P. De Gori
title Pattern of seismicity in the Lucanian Apennines and foredeep (Southern Italy) from recording by SAPTEX temporary array
title_short Pattern of seismicity in the Lucanian Apennines and foredeep (Southern Italy) from recording by SAPTEX temporary array
title_full Pattern of seismicity in the Lucanian Apennines and foredeep (Southern Italy) from recording by SAPTEX temporary array
title_fullStr Pattern of seismicity in the Lucanian Apennines and foredeep (Southern Italy) from recording by SAPTEX temporary array
title_full_unstemmed Pattern of seismicity in the Lucanian Apennines and foredeep (Southern Italy) from recording by SAPTEX temporary array
title_sort pattern of seismicity in the lucanian apennines and foredeep (southern italy) from recording by saptex temporary array
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2005-06-01
description The deployment of a temporary seismic network in Southern Italy during 2001-2004 (the SAPTEX array, Southern
 APennine Tomography EXperiment) allowed us to relocate the hypocenters of Southern Apennines earthquakes
 with low uncertainty among the location parameters. The best array distribution of the SAPTEX network
 for the analysis of seismicity in the Lucanian Apennines and foredeep was reached in the first two years of
 recording. The SAPTEX data were merged with those of the Italian National Seismic Network (RSNC) operated
 by the Istituto Nazionale di Geofisica e Vulcanologia (INGV). For the hypocenters computation of events in
 the upper Agri Valley we also included P- and S- waves arrivals from the local Eni-Agip network. The seismicity
 for the Lucanian Apennines and foredeep in the analyzed period has magnitudes ranging from 2.0 to 4.1. A
 major finding is the identification of two different crustal domains: the westernmost characterizing the chain,
 mostly with shallow earthquakes (within about 20 km of depth), and the easternmost one belonging to the outer
 margin of the chain and to the foredeep, with deeper seismicity (mostly between 20-40 km of depth). Thirty
 fault-plane solutions were computed and used for stress inversion; most of them are related to earthquakes within
 the chain sector and indicate a generalized NE-SW extension. Moreover, the dense network allowed us to improve
 the location of events relative to two low magnitude sequences which occurred in the study period.
topic seismicity
seismic network
motectonics
Lucanian Apennines
Lucanian foredeep
Southern Italy
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3252
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