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The 20 March 1992 South Aegean, Greece, earthquake (Ms= 5.3): possible anomalous effects

Identifieur interne : 000376 ( Main/Exploration ); précédent : 000375; suivant : 000377

The 20 March 1992 South Aegean, Greece, earthquake (Ms= 5.3): possible anomalous effects

Auteurs : Gerassimos A. Papadopoulos [Grèce]

Source :

RBID : ISTEX:E090F7CFFDCDE4B99D89653C42C91074CBD513AC

Descripteurs français

English descriptors

Abstract

The earthquake (Ms= 5.3) of 20 March 1992 and its aftershocks, which occurred near the volcanic island complex of Milos, South Aegean, Greece, are studied on the basis of filed observations and instrumental data. The mainshock caused some building damage, the maximum intensity of VI+ (MM) being assigned to Triovasalos, Milos. Ground cracks, liquefaction in soil, landslides and rockfalls were observed in Milos. Liquefaction took place at an apparently anomalously long epicentral distance (D= 12 km) and is associated with unusually small earthquake magnitude. Abnormal animal behaviour was reported no longer than twelve hours before the mainshock. The b‐value (= 1.02) of the G–R relation for the aftershock sequence, the exponentially decreasing number of aftershocks with time, and the difference (= 0.5) in magnitude between the mainshock and its largest aftershock imply that the origin of these earthquakes is tectonic and not associated with the volcanic field of Milos.

Url:
DOI: 10.1111/j.1365-3121.1993.tb00273.x


Affiliations:


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Le document en format XML

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<term>Instrumental period</term>
<term>Larger events</term>
<term>Largest aftershock</term>
<term>Liquefaction</term>
<term>Liquefaction occurrence</term>
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<term>Mainshock</term>
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<term>Precursor time</term>
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<term>Seismic events</term>
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<term>Small earthquake magnitude</term>
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<div type="abstract" xml:lang="en">The earthquake (Ms= 5.3) of 20 March 1992 and its aftershocks, which occurred near the volcanic island complex of Milos, South Aegean, Greece, are studied on the basis of filed observations and instrumental data. The mainshock caused some building damage, the maximum intensity of VI+ (MM) being assigned to Triovasalos, Milos. Ground cracks, liquefaction in soil, landslides and rockfalls were observed in Milos. Liquefaction took place at an apparently anomalously long epicentral distance (D= 12 km) and is associated with unusually small earthquake magnitude. Abnormal animal behaviour was reported no longer than twelve hours before the mainshock. The b‐value (= 1.02) of the G–R relation for the aftershock sequence, the exponentially decreasing number of aftershocks with time, and the difference (= 0.5) in magnitude between the mainshock and its largest aftershock imply that the origin of these earthquakes is tectonic and not associated with the volcanic field of Milos.</div>
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