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Extensional crustal-scale shear zones in the Western Cyclades (Kea, Greece)

dc.contributor.authorMüller, Monika
dc.contributor.authorGrasemann, Bernhard
dc.contributor.authorEdwards, Michael A.
dc.contributor.authorDraganits, Erich
dc.contributor.authorVoit, Klaus
dc.contributor.authorIglseder, Christoph
dc.contributor.authorZámolyi, András
dc.contributor.authorPetrakakis, Konstantin
dc.contributor.editorPhilipp, Sonja
dc.contributor.editorLeiss, Bernd
dc.contributor.editorVollbrecht, Axel
dc.contributor.editorTanner, David
dc.contributor.editorGudmundsson, Agust
dc.date.accessioned2010-11-26T13:21:35Z
dc.date.accessioned2013-01-28T10:20:11Z
dc.date.available2010-11-26T13:21:35Z
dc.date.available2013-01-28T10:20:11Z
dc.date.issued2006-03
dc.identifier.citationPhilipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds.): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, p. 143 - 145.
dc.identifier.isbn3-938616-40-7
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-3479-9
dc.description.abstractIntense seismicity and intensely developed active and ancient fault systems are common to the Aegean Region. Extending/ thinning crust involves a complex interplay of (1) Gulf of Corinth riftexpansion, (2) west- and south-ward retreat of the Hellenic Trench, (3) westward impingement of the Anatolian Platen, and/or (4) propagation of the Anatolian Fault system into the Aegean. New geological/structural investigations on Kea (also known as Tzia), in the Western Cyclades reveal a low angle crustal-scale, detachment-type ductile shear zone probably formed during Miocene extension and thinning of the continental crust...
dc.format.mimetypeapplication/pdf
dc.language.isodeu
dc.publisherUniversitätsverlag Göttingen
dc.relation.ispartof11. Symposium "Tektonik, Struktur- und Kristallingeologie"
dc.subject.ddc551
dc.subject.gokVEF 300
dc.subject.gokVAE 130
dc.subject.gokVKB 270
dc.subject.gokVAE 400
dc.titleExtensional crustal-scale shear zones in the Western Cyclades (Kea, Greece)
dc.typeanthologyArticle
dc.subject.gokverbalGriechenland und griechische Inseln {Geologie}
dc.subject.gokverbalGeomechanik
dc.subject.gokverbalProdukte mechanischer Deformation {Petrologie}
dc.subject.gokverbalTektogenese {Geologie}
dc.bibliographicCitation.firstPage143
dc.bibliographicCitation.lastPage145
dc.identifier.doi10.23689/fidgeo-1871
dc.type.versionpublishedVersion
dc.subject.freeKea
dc.subject.freeErdkruste
dc.subject.freeExtension <Geologie>
dc.subject.freeScherzone
dc.relation.collectionGeologische Wissenschaften
dc.description.typeconference


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