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Faults and seismicity in the Northwest part of the Iberian Peninsula

dc.contributor.authorGonzález Casado, J. M.
dc.contributor.authorGiner Robles, J. L.
dc.date.accessioned2015-02-12T11:49:15Z
dc.date.available2015-02-12T11:49:15Z
dc.date.issued1999
dc.identifier.urihttp://hdl.handle.net/10272/9897
dc.description.abstractThe statistical study of the post-hercynian cartographic faults of the Northwest part of Spain (Galicia) allow to precise the existence of three main fault sets; NE-SW, NW-SE and N-S, which controlled the topograpic features in this area. The seismic epicentres in this region are related mainly with the NE-SW and N-S fault sets, which are, probably, the seismogenetic faults. The orientation of the stresses responsible for the seismic activity been deduced from the analyses of 76 earthquake focal mechanisms. The maximum horizontal compression direction is located NW-SE, then the NE-SW faults move as reverse faults, the NW-SE set as normal faults and the N-S as normal-oblique faults (sinistral)en_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.otherNorthwest Spainen_US
dc.subject.otherFaultsen_US
dc.subject.otherRecent stressesen_US
dc.subject.otherActive structuresen_US
dc.titleRelaciones entre fallas y sismicidad en el noroeste peninsularen_US
dc.titleFaults and seismicity in the Northwest part of the Iberian Peninsulaeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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