Seismically active fracture zones related to the eastern segment of the Hellenic subduction
Identifieur interne : 000365 ( Main/Exploration ); précédent : 000364; suivant : 000366Seismically active fracture zones related to the eastern segment of the Hellenic subduction
Auteurs : V. Hanuš [République tchèque] ; J. Van K [République tchèque]Source :
- Journal of Geodynamics [ 0264-3707 ] ; 1993.
Descripteurs français
English descriptors
- KwdEn :
- Agio, Agios fracture zone, Chios, Crete, Earthquake, Eastern domain, Eastern segment, Fracture, Fracture zone, Fracture zones, Hanu, Hellenic area, Hellenic subduction, Heraklion, Historical earthquakes, Individual fracture zones, Lesbos, Longitudinal, Longitudinal section, Maximum depth, Nisyros, Oros, Outcrop, Papazachos, Psara, Rhodos, Seismically, Smyrni, Subduction, Transverse section, Van6k, Vertical fault, Viii, Zone.
- Teeft :
- Agio, Agios fracture zone, Chios, Crete, Earthquake, Eastern domain, Eastern segment, Fracture, Fracture zone, Fracture zones, Hanu, Hellenic area, Hellenic subduction, Heraklion, Historical earthquakes, Individual fracture zones, Lesbos, Longitudinal, Longitudinal section, Maximum depth, Nisyros, Oros, Outcrop, Papazachos, Psara, Rhodos, Seismically, Smyrni, Subduction, Transverse section, Van6k, Vertical fault, Viii, Zone.
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:
Links toward previous steps (curation, corpus...)
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- to stream Main, to step Curation: 000365
Le document en format XML
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Agio</term>
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<term>Chios</term>
<term>Crete</term>
<term>Earthquake</term>
<term>Eastern domain</term>
<term>Eastern segment</term>
<term>Fracture</term>
<term>Fracture zone</term>
<term>Fracture zones</term>
<term>Hanu</term>
<term>Hellenic area</term>
<term>Hellenic subduction</term>
<term>Heraklion</term>
<term>Historical earthquakes</term>
<term>Individual fracture zones</term>
<term>Lesbos</term>
<term>Longitudinal</term>
<term>Longitudinal section</term>
<term>Maximum depth</term>
<term>Nisyros</term>
<term>Oros</term>
<term>Outcrop</term>
<term>Papazachos</term>
<term>Psara</term>
<term>Rhodos</term>
<term>Seismically</term>
<term>Smyrni</term>
<term>Subduction</term>
<term>Transverse section</term>
<term>Van6k</term>
<term>Vertical fault</term>
<term>Viii</term>
<term>Zone</term>
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<keywords scheme="Teeft" xml:lang="en"><term>Agio</term>
<term>Agios fracture zone</term>
<term>Chios</term>
<term>Crete</term>
<term>Earthquake</term>
<term>Eastern domain</term>
<term>Eastern segment</term>
<term>Fracture</term>
<term>Fracture zone</term>
<term>Fracture zones</term>
<term>Hanu</term>
<term>Hellenic area</term>
<term>Hellenic subduction</term>
<term>Heraklion</term>
<term>Historical earthquakes</term>
<term>Individual fracture zones</term>
<term>Lesbos</term>
<term>Longitudinal</term>
<term>Longitudinal section</term>
<term>Maximum depth</term>
<term>Nisyros</term>
<term>Oros</term>
<term>Outcrop</term>
<term>Papazachos</term>
<term>Psara</term>
<term>Rhodos</term>
<term>Seismically</term>
<term>Smyrni</term>
<term>Subduction</term>
<term>Transverse section</term>
<term>Van6k</term>
<term>Vertical fault</term>
<term>Viii</term>
<term>Zone</term>
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<keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Crète</term>
<term>Séisme</term>
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<front><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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<name sortKey="Van K, J" sort="Van K, J" uniqKey="Van K J" first="J" last="Van K">J. Van K</name>
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