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Seismic Hazar in the Guadix-Baza (S. Spain) Basin

dc.contributor.authorMartín Rojas, Iván
dc.contributor.authorDíaz Hernández, J. L.
dc.contributor.authorMartín Vallejo, M.
dc.contributor.authorJulià, Ramón
dc.date.accessioned2015-02-12T12:08:28Z
dc.date.available2015-02-12T12:08:28Z
dc.date.issued1999
dc.identifier.urihttp://hdl.handle.net/10272/9898
dc.description.abstractSinuosity, Facetation percentage, disectation percentage and width/high valley ratio geomorphic parameters are applied to the Alicun Spa resort mountain front. This front, defined by a normal fault, shows several springs originated during the Quaternary. Travertine deposits are related to the springs and the fault The travertine ages are correlated with the values from the geomorphic parameters, in order to obtain seismic risk informationen_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.otherTravertinesen_US
dc.subject.otherGeomorphic parametersen_US
dc.subject.otherActive tectonicsen_US
dc.subject.otherSouthern Spainen_US
dc.titleRiesgo Sísmico en La Depresión de Guadix-Baza (S España)en_US
dc.titleSeismic Hazar in the Guadix-Baza (S. Spain) Basineng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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