Precursory accelerated Benioff strain in the Aegean area

Accelerating seismic crustal deformation due to the occurrence of intermediate magnitude earthquakes leading to the generation of a mainshock has recently been considered a critical phenomenon. This hypothesis is tested by the use of a large data sample concerning the Aegean area. Elliptical critica...

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Main Authors: B. Papazachos, C. Papazachos
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/3597
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author B. Papazachos
C. Papazachos
author_facet B. Papazachos
C. Papazachos
author_sort B. Papazachos
collection DOAJ
description Accelerating seismic crustal deformation due to the occurrence of intermediate magnitude earthquakes leading to the generation of a mainshock has recently been considered a critical phenomenon. This hypothesis is tested by the use of a large data sample concerning the Aegean area. Elliptical critical regions for fifty-two strong mainshocks, which have occurred in the Aegean area since 1930, have been identified by applying a power-law relation between the cumulative Benioff strain and the time to the main rupture. Empirical relations between the parameters of this model have been further improved by the use of a large data sample. The spatial distribution of preshocks with respect to the mainshock is examined and its tectonic significance is pointed out. The possibility of using the results of this work to predict the epicentre, magnitude and time of ensuing mainshocks are discussed and further work towards this goal is suggested.
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spelling doaj.art-b97b609e4fbf403884d21a8d236f4e2c2022-12-22T00:44:29ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2001-06-0144210.4401/ag-3597Precursory accelerated Benioff strain in the Aegean areaB. PapazachosC. PapazachosAccelerating seismic crustal deformation due to the occurrence of intermediate magnitude earthquakes leading to the generation of a mainshock has recently been considered a critical phenomenon. This hypothesis is tested by the use of a large data sample concerning the Aegean area. Elliptical critical regions for fifty-two strong mainshocks, which have occurred in the Aegean area since 1930, have been identified by applying a power-law relation between the cumulative Benioff strain and the time to the main rupture. Empirical relations between the parameters of this model have been further improved by the use of a large data sample. The spatial distribution of preshocks with respect to the mainshock is examined and its tectonic significance is pointed out. The possibility of using the results of this work to predict the epicentre, magnitude and time of ensuing mainshocks are discussed and further work towards this goal is suggested.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3597Benioff straincritical pointAegean area
spellingShingle B. Papazachos
C. Papazachos
Precursory accelerated Benioff strain in the Aegean area
Annals of Geophysics
Benioff strain
critical point
Aegean area
title Precursory accelerated Benioff strain in the Aegean area
title_full Precursory accelerated Benioff strain in the Aegean area
title_fullStr Precursory accelerated Benioff strain in the Aegean area
title_full_unstemmed Precursory accelerated Benioff strain in the Aegean area
title_short Precursory accelerated Benioff strain in the Aegean area
title_sort precursory accelerated benioff strain in the aegean area
topic Benioff strain
critical point
Aegean area
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3597
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