Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1339
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dc.contributor.authorallKnapmeyer, M.; Institute of Geophysics, Ruhr University, Bochum, Germanyen
dc.date.accessioned2006-07-26T12:33:07Zen
dc.date.available2006-07-26T12:33:07Zen
dc.date.issued1999-02en
dc.identifier.urihttp://hdl.handle.net/2122/1339en
dc.description.abstractThe morphology of the Aegean Benioff zone was reconstructed using 1366 hypocentres from the PDE catalogue 1973-1997. Two such zones are identified under the Aegean area, a large one (Main Aegean Subduction, MAS) spanning the whole Hellenic arc and a smaller and younger one under the Western Peloponnesus. The geometry of the MAS suggests that it blocks its own subduction and, therefore, causes the development of the smaller western zone as a result of a step back process in the Pliocene.en
dc.format.extent3815964 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries1/42 (1999)en
dc.subjectAegeanen
dc.subjectsubductionen
dc.subjectWadati Benioff zonesen
dc.titleGeometry of the Aegean Benioff zonesen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.06. Subduction related processesen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorKnapmeyer, M.en
dc.contributor.departmentInstitute of Geophysics, Ruhr University, Bochum, Germanyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptInstitute of Geophysics, Ruhr University, Bochum, Germany-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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