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Structural and morphological indicators of postmiocene deformations in the western Crevillente Fault (Betic Cordillera)

dc.contributor.authorCanora Catalán, C.
dc.contributor.authorMartínez Díaz, J. J.
dc.date.accessioned2014-07-31T09:15:56Z
dc.date.available2014-07-31T09:15:56Z
dc.date.issued2005
dc.identifier.urihttp://hdl.handle.net/10272/8668
dc.description.abstractAccording to the NNW-SSE regional shortening direction active in the Eastern Betic Cordillera since the Upper Miocene, the ENE-WSW Crevillente Fault should be either blocked or locally reverse. However, dextral, sinestral or reverse movements have been reported along the fault zone. In this work, new observations on the post-Miocene deformations of the Crevillente Fault are described. A block-tectonics model active on different scales is proposed to explain the kinematics variability of the faulten_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherCrevillente Faulten_US
dc.subject.otherStress fielden_US
dc.subject.otherNeotectonic perioden_US
dc.titleIndicadores estructurales y morfológicos de deformaciones postmiocenas en el sector occidental de la Falla de Crevillente (Cordillera Bética)en_US
dc.titleStructural and morphological indicators of postmiocene deformations in the western Crevillente Fault (Betic Cordillera)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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