NissirosV1, Main, Exploration, bibRecord, 000471

Source and short-distance propagation of the July 9, 1956 southern Aegean tsunami

Identifieur interne : 000471 ( Main/Exploration ); précédent : 000470; suivant : 000472

Source and short-distance propagation of the July 9, 1956 southern Aegean tsunami

Auteurs : B. C. Papazachos [Grèce] ; Ch. Koutitas [Grèce] ; P. M. Hatzidimitriou [Grèce] ; B. G. Karacostas [Grèce] ; Ch. A. Papaioannou [Grèce]

Source :

Marine Geology [ 0025-3227 ] ; 1985.

RBID : ISTEX:2273A8DB18B1D1A341DC51D11DDD62CAC5333616

Descripteurs français

Wicri :
- topic : Crète, Répartition géographique.

English descriptors

Abstract

Abstract: Properties of the tsunamigenic source as well as the attenuation of the tsunami intensities of the large tsunami of July 9, 1956 in the southern Aegean are investigated. This tsunami was generated by a shallow earthquake with a surface wave magnitude of 7.5 which was caused by a normal fault.Fault-plane solution, isoseismal lines and bathymetric information indicate that the tsunamigenic source had an elliptical shape with the large axis equal to 110 km and oriented in an ENE—WSW direction. This is also the strike of the normal fault which produced the earthquake and it is probable that the southern block was downthrown.Linear relations between: (a) the tsunami intensity and the epicentral distance for distances up to 330 km; (b) the observed tsunami height and the epicentral distance; and (c) the tsunami height and intensity, have been determined.This information, concerning the source parameters of tsunamis and the attenuation of the tsunami intensity and tsunami height with distance, are of great importance for determining the tsunami hazard in this area.

Url:

https://api.istex.fr/document/2273A8DB18B1D1A341DC51D11DDD62CAC5333616/fulltext/pdf

DOI: 10.1016/0025-3227(85)90064-7

Affiliations:

Grèce

Links toward previous steps (curation, corpus...)

to stream Istex, to step Corpus: 000012
to stream Istex, to step Curation: 000012
to stream Istex, to step Checkpoint: 000396
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to stream Main, to step Curation: 000471

Le document en format XML

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<front><div type="abstract" xml:lang="en">Abstract: Properties of the tsunamigenic source as well as the attenuation of the tsunami intensities of the large tsunami of July 9, 1956 in the southern Aegean are investigated. This tsunami was generated by a shallow earthquake with a surface wave magnitude of 7.5 which was caused by a normal fault.Fault-plane solution, isoseismal lines and bathymetric information indicate that the tsunamigenic source had an elliptical shape with the large axis equal to 110 km and oriented in an ENE—WSW direction. This is also the strike of the normal fault which produced the earthquake and it is probable that the southern block was downthrown.Linear relations between: (a) the tsunami intensity and the epicentral distance for distances up to 330 km; (b) the observed tsunami height and the epicentral distance; and (c) the tsunami height and intensity, have been determined.This information, concerning the source parameters of tsunamis and the attenuation of the tsunami intensity and tsunami height with distance, are of great importance for determining the tsunami hazard in this area.</div>
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Source and short-distance propagation of the July 9, 1956 southern Aegean tsunami

Source and short-distance propagation of the July 9, 1956 southern Aegean tsunami

Source :

Descripteurs français

English descriptors

Abstract

Links toward previous steps (curation, corpus...)

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri