Fault plane solutions of crustal earthquakes in Southern Italy (1988-1995): seismotectonic implications

The Southern Apennines and the Sicilian-Calabrian regions belong to the complex geodynamic Central Mediterranean area, which is dominated by the NNW-SSE convergence of the European and African plates and is strongly affected by the presence of Neogene-Quaternary subduction/collision arcs and related...

Full description

Bibliographic Details
Main Authors: A. Amato, A. Frepoli
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/3651
id doaj-c87d8604704246ab902252398fc67783
record_format Article
spelling doaj-c87d8604704246ab902252398fc677832020-11-24T23:46:06ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2000-06-0143310.4401/ag-3651Fault plane solutions of crustal earthquakes in Southern Italy (1988-1995): seismotectonic implicationsA. AmatoA. FrepoliThe Southern Apennines and the Sicilian-Calabrian regions belong to the complex geodynamic Central Mediterranean area, which is dominated by the NNW-SSE convergence of the European and African plates and is strongly affected by the presence of Neogene-Quaternary subduction/collision arcs and related back-arc basins In order to obtain a more detailed picture of the processes active in these two regions, we calculated 173 new fault plane solutions of crustal events with 2.5 < M < 4.4 recorded by the national seismic network of the Istituto Nazionale di Geofisica in the period 1988-1995. Normal and strike-slip solutions are largely prevalent in the Southern Apennines, with tensional (T) axes mostly oriented NE-SW, perpendicular to the belt, in agreement with active stress directions from breakouts. In the Sicilian region the seismicity is concentrated in the eastern portion of the island. Different focal mechanism categories are present in the Nebrodi and Etna sector indicating a complex strain release in these two regions. Thrust and strike-slip solutions prevail in the Aeolian Islands associated with ~ N-S compression, whereas in Western Sicily the prevailing orientation of P-axes is around WNW-ESE. Although not well constrained due to only a few data in the region, there is a hint of active compression at the outer front of the Calabrian arc, in the Ionian Sea. The observed pattern of fault plane solutions suggests that the transition between oceanic subduction beneath Calabria and continental subduction in Sicily and in Southern Apennines controls the active tectonics of Southern Italy.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3651southern Italyfocal mechanismsseismicitystress distribution
collection DOAJ
language English
format Article
sources DOAJ
author A. Amato
A. Frepoli
spellingShingle A. Amato
A. Frepoli
Fault plane solutions of crustal earthquakes in Southern Italy (1988-1995): seismotectonic implications
Annals of Geophysics
southern Italy
focal mechanisms
seismicity
stress distribution
author_facet A. Amato
A. Frepoli
author_sort A. Amato
title Fault plane solutions of crustal earthquakes in Southern Italy (1988-1995): seismotectonic implications
title_short Fault plane solutions of crustal earthquakes in Southern Italy (1988-1995): seismotectonic implications
title_full Fault plane solutions of crustal earthquakes in Southern Italy (1988-1995): seismotectonic implications
title_fullStr Fault plane solutions of crustal earthquakes in Southern Italy (1988-1995): seismotectonic implications
title_full_unstemmed Fault plane solutions of crustal earthquakes in Southern Italy (1988-1995): seismotectonic implications
title_sort fault plane solutions of crustal earthquakes in southern italy (1988-1995): seismotectonic implications
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2000-06-01
description The Southern Apennines and the Sicilian-Calabrian regions belong to the complex geodynamic Central Mediterranean area, which is dominated by the NNW-SSE convergence of the European and African plates and is strongly affected by the presence of Neogene-Quaternary subduction/collision arcs and related back-arc basins In order to obtain a more detailed picture of the processes active in these two regions, we calculated 173 new fault plane solutions of crustal events with 2.5 < M < 4.4 recorded by the national seismic network of the Istituto Nazionale di Geofisica in the period 1988-1995. Normal and strike-slip solutions are largely prevalent in the Southern Apennines, with tensional (T) axes mostly oriented NE-SW, perpendicular to the belt, in agreement with active stress directions from breakouts. In the Sicilian region the seismicity is concentrated in the eastern portion of the island. Different focal mechanism categories are present in the Nebrodi and Etna sector indicating a complex strain release in these two regions. Thrust and strike-slip solutions prevail in the Aeolian Islands associated with ~ N-S compression, whereas in Western Sicily the prevailing orientation of P-axes is around WNW-ESE. Although not well constrained due to only a few data in the region, there is a hint of active compression at the outer front of the Calabrian arc, in the Ionian Sea. The observed pattern of fault plane solutions suggests that the transition between oceanic subduction beneath Calabria and continental subduction in Sicily and in Southern Apennines controls the active tectonics of Southern Italy.
topic southern Italy
focal mechanisms
seismicity
stress distribution
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3651
work_keys_str_mv AT aamato faultplanesolutionsofcrustalearthquakesinsouthernitaly19881995seismotectonicimplications
AT afrepoli faultplanesolutionsofcrustalearthquakesinsouthernitaly19881995seismotectonicimplications
_version_ 1725494523024375808