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Characterization of the Neogen stress regime in Mallorca based on fault population analysis

dc.contributor.authorCéspedes, A.
dc.contributor.authorGiménez, J.
dc.contributor.authorSäbat, F.
dc.date.accessioned2014-12-11T12:27:27Z
dc.date.available2014-12-11T12:27:27Z
dc.date.issued2001
dc.identifier.urihttp://hdl.handle.net/10272/9514
dc.description.abstractThe analysis of neoformed faults in Miocene to Plio-Quaternary sediments of Mallorca Island has been used to characterize the paleostress regime. 1 7 sites are located at.the western part cf Palma Basin, and 7 at the Sta. Margalida-Muro area. The paleostress regime has been established using Anderson (1951) method if a monoclinic symmetry of faults is observed. Reches (1983) and Krantz (1988) method has been applied where faults show an orthorhombic symmetry. Results indicate tectonic regime during Upper Miocene was extensional, close to radial, and during Plio-Quaternary was extensional too but with NW-SE direction of maximum extensionen_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.otherMallorcaen_US
dc.subject.otherNeogene and Quaternaryen_US
dc.subject.otherFault population analysisen_US
dc.titleCaracterización del campo de esfuerzos neógenos en Mallorca mediante el análisis de poblaciones de fallasen_US
dc.titleCharacterization of the Neogen stress regime in Mallorca based on fault population analysiseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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