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Quaternary tectonic activity in the Huércal-Overa Basin (Almería, Southeast Spain): deformations associated with the Albox fault

dc.contributor.authorGarcía Meléndez, E.
dc.contributor.authorGoy, José L.
dc.contributor.authorZazo, C.
dc.date.accessioned2014-10-21T08:32:51Z
dc.date.available2014-10-21T08:32:51Z
dc.date.issued2004
dc.identifier.urihttp://hdl.handle.net/10272/8909
dc.description.abstractThe main Quaternary tectonic ativity in the Huercal-Overa Basin is related to the Albox fault, which extends from Tijola in the Almanzora Corridor (SSW) to the eastern Huercal-Overa Basin (NNE). In this work an example of the effects of the fault movement both in the sediments and in the relief is presented linked to a fault segment in the Alto de Ruchete area. Analysis of deformation structures related to the main fault present in the Quaternary sediments, such as small and medium reverse faults, monoclinal folds, drag-folds and scarps, allow the establishment of an evolution model during the Quaternary for the tectonic and sedimentary activity and their effects in the relief genesis.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.otherNeotectonicsen_US
dc.subject.otherCeomorphologyen_US
dc.subject.otherQuaternaryen_US
dc.subject.otherBetic Cordilleraen_US
dc.titleActividad tectónica cuaternaria en la Cuenca de Huércal-Overa (Almería, Sureste de España): deformaciones asociadas a la falla de Alboxen_US
dc.titleQuaternary tectonic activity in the Huércal-Overa Basin (Almería, Southeast Spain): deformations associated with the Albox faulteng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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