Study of the seismicity temporal variation for the current seismic hazard evaluation in Val d'Agri, Italy

This study examines the temporal variation of the seismicity in the Val d'Agri (southern Italy) and adjacent areas, for the current seismic hazard evaluation. The temporal variation of the seismicity is expressed as time series of the number of earthquakes, <i>b</i> value of Gutenb...

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Main Authors: I. Baskoutas, A. D'Alessandro
Format: Article
Language:English
Published: Copernicus Publications 2014-12-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/14/3169/2014/nhess-14-3169-2014.pdf
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spelling doaj-a63e5f8b45414c91ba3475ce44d741bf2020-11-24T22:25:16ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812014-12-0114123169317410.5194/nhess-14-3169-2014Study of the seismicity temporal variation for the current seismic hazard evaluation in Val d'Agri, ItalyI. Baskoutas0A. D'Alessandro1Institute of Geodynamics, National Observatory of Athens, Athens, GreeceIstituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti, Rome, ItalyThis study examines the temporal variation of the seismicity in the Val d'Agri (southern Italy) and adjacent areas, for the current seismic hazard evaluation. The temporal variation of the seismicity is expressed as time series of the number of earthquakes, <i>b</i> value of Gutenberg–Richter relationship or <i>b</i> value of the frequency–magnitude distribution and the seismic energy released in the form of log<i>E</i><sup>2/3</sup>. The analysis was performed by means of a new research tool that includes visualizing techniques, which helps the interactive exploration and the interpretation of temporal variation changes. The obtained time series show a precursory seismicity pattern, characterized by low and high probability periods, which preceded earthquakes of magnitude <i>M</i> ≥ 4.0. The 75% of the examined cases were successfully correlated with a change in seismicity pattern. The average duration of the low and the high probability periods is 10.6 and 13.8 months respectively. These results indicate that the seismicity temporal variation monitoring in a given area and the recognition of the low and high probability periods can contribute to the evaluation, in regular monthly intervals, of current seismic hazard status.http://www.nat-hazards-earth-syst-sci.net/14/3169/2014/nhess-14-3169-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. Baskoutas
A. D'Alessandro
spellingShingle I. Baskoutas
A. D'Alessandro
Study of the seismicity temporal variation for the current seismic hazard evaluation in Val d'Agri, Italy
Natural Hazards and Earth System Sciences
author_facet I. Baskoutas
A. D'Alessandro
author_sort I. Baskoutas
title Study of the seismicity temporal variation for the current seismic hazard evaluation in Val d'Agri, Italy
title_short Study of the seismicity temporal variation for the current seismic hazard evaluation in Val d'Agri, Italy
title_full Study of the seismicity temporal variation for the current seismic hazard evaluation in Val d'Agri, Italy
title_fullStr Study of the seismicity temporal variation for the current seismic hazard evaluation in Val d'Agri, Italy
title_full_unstemmed Study of the seismicity temporal variation for the current seismic hazard evaluation in Val d'Agri, Italy
title_sort study of the seismicity temporal variation for the current seismic hazard evaluation in val d'agri, italy
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2014-12-01
description This study examines the temporal variation of the seismicity in the Val d'Agri (southern Italy) and adjacent areas, for the current seismic hazard evaluation. The temporal variation of the seismicity is expressed as time series of the number of earthquakes, <i>b</i> value of Gutenberg–Richter relationship or <i>b</i> value of the frequency–magnitude distribution and the seismic energy released in the form of log<i>E</i><sup>2/3</sup>. The analysis was performed by means of a new research tool that includes visualizing techniques, which helps the interactive exploration and the interpretation of temporal variation changes. The obtained time series show a precursory seismicity pattern, characterized by low and high probability periods, which preceded earthquakes of magnitude <i>M</i> ≥ 4.0. The 75% of the examined cases were successfully correlated with a change in seismicity pattern. The average duration of the low and the high probability periods is 10.6 and 13.8 months respectively. These results indicate that the seismicity temporal variation monitoring in a given area and the recognition of the low and high probability periods can contribute to the evaluation, in regular monthly intervals, of current seismic hazard status.
url http://www.nat-hazards-earth-syst-sci.net/14/3169/2014/nhess-14-3169-2014.pdf
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AT adalessandro studyoftheseismicitytemporalvariationforthecurrentseismichazardevaluationinvaldagriitaly
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