Earthquake sources and seismic hazard in Southeastern Sicily

A study of some earthquakes (M > 5.3) affecting Southeastern Sicily was performed to define their seismic sources and to estimate seismic hazard in the region. An analysis of historical reports allowed us to reassess intensities of the 1542, 1693, 1818, 1848 and 1990 earthquakes by using the...

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Main Authors: R. Rigano, M. S. Barbano
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2001-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3570
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spelling doaj-2eb18a89e36a4a0ba6171a66462bafc32020-11-24T22:02:20ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2001-06-0144410.4401/ag-3570Earthquake sources and seismic hazard in Southeastern SicilyR. RiganoM. S. BarbanoA study of some earthquakes (M > 5.3) affecting Southeastern Sicily was performed to define their seismic sources and to estimate seismic hazard in the region. An analysis of historical reports allowed us to reassess intensities of the 1542, 1693, 1818, 1848 and 1990 earthquakes by using the new European Macroseismic Scale 98. The new intensity data were used to define parameters and the orientation of seismic sources. The sources obtained were compared with the ones computed using the MCS intensities retrieved from the Catalogue of Strong Italian Earthquakes. The adopted procedure gives results that are statistically significant, but both the epicentre location and source azimuth, in some cases, are strongly affected by the azimuthal gap in the intensity distribution. This is evident mainly for the 1693 January earthquakes. For these earthquakes the macroseismic data uncertainty gives significantly different solutions, and does not allow the events to be associated with known active faults. By handling the new estimated intensity data and using the site seismic histories, the seismic hazard for some localities was calculated. The highest probability of occurrence, for destructive events (I = 10), was obtained in the area between Catania, Lentini and Augusta, suggesting that the seismogenic sources are located near the Ionian coast.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3570Historical seismicitysource parametersseismic hazardSE Sicily
collection DOAJ
language English
format Article
sources DOAJ
author R. Rigano
M. S. Barbano
spellingShingle R. Rigano
M. S. Barbano
Earthquake sources and seismic hazard in Southeastern Sicily
Annals of Geophysics
Historical seismicity
source parameters
seismic hazard
SE Sicily
author_facet R. Rigano
M. S. Barbano
author_sort R. Rigano
title Earthquake sources and seismic hazard in Southeastern Sicily
title_short Earthquake sources and seismic hazard in Southeastern Sicily
title_full Earthquake sources and seismic hazard in Southeastern Sicily
title_fullStr Earthquake sources and seismic hazard in Southeastern Sicily
title_full_unstemmed Earthquake sources and seismic hazard in Southeastern Sicily
title_sort earthquake sources and seismic hazard in southeastern sicily
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2001-06-01
description A study of some earthquakes (M > 5.3) affecting Southeastern Sicily was performed to define their seismic sources and to estimate seismic hazard in the region. An analysis of historical reports allowed us to reassess intensities of the 1542, 1693, 1818, 1848 and 1990 earthquakes by using the new European Macroseismic Scale 98. The new intensity data were used to define parameters and the orientation of seismic sources. The sources obtained were compared with the ones computed using the MCS intensities retrieved from the Catalogue of Strong Italian Earthquakes. The adopted procedure gives results that are statistically significant, but both the epicentre location and source azimuth, in some cases, are strongly affected by the azimuthal gap in the intensity distribution. This is evident mainly for the 1693 January earthquakes. For these earthquakes the macroseismic data uncertainty gives significantly different solutions, and does not allow the events to be associated with known active faults. By handling the new estimated intensity data and using the site seismic histories, the seismic hazard for some localities was calculated. The highest probability of occurrence, for destructive events (I = 10), was obtained in the area between Catania, Lentini and Augusta, suggesting that the seismogenic sources are located near the Ionian coast.
topic Historical seismicity
source parameters
seismic hazard
SE Sicily
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3570
work_keys_str_mv AT rrigano earthquakesourcesandseismichazardinsoutheasternsicily
AT msbarbano earthquakesourcesandseismichazardinsoutheasternsicily
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