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Seismically active fracture zones related to the eastern segment of the Hellenic subduction

Identifieur interne : 000365 ( Main/Exploration ); précédent : 000364; suivant : 000366

Seismically active fracture zones related to the eastern segment of the Hellenic subduction

Auteurs : V. Hanuš [République tchèque] ; J. Van K [République tchèque]

Source :

RBID : ISTEX:1DD9A85D6F17D14AA9FFA03F1713C53095C1B1F4

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English descriptors

Abstract

Abstract: A system of eight seismically active fracture zones was delineated on the basis of the distribution of earthquake foci in the continental lithosphere in the eastern domain of the Hellenic area. The position and width of the outcrop, thickness, dip and maximum depth of the individual fracture zones were estimated and complemented by tectonic and geological evidence. The existence of the fracture zones was confirmed by the occurrence of historical diasastrous earthquakes.

Url:
DOI: 10.1016/0264-3707(93)90016-Y


Affiliations:


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Le document en format XML

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<div type="abstract" xml:lang="en">Abstract: A system of eight seismically active fracture zones was delineated on the basis of the distribution of earthquake foci in the continental lithosphere in the eastern domain of the Hellenic area. The position and width of the outcrop, thickness, dip and maximum depth of the individual fracture zones were estimated and complemented by tectonic and geological evidence. The existence of the fracture zones was confirmed by the occurrence of historical diasastrous earthquakes.</div>
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