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The imbricate fan of Valverde del Camino (southern part of the South Portuguese Zone, Huelva)

dc.contributor.authorMantero Cuajares, Macarena
dc.contributor.authorAlonso Chaves, Francisco Manuel 
dc.contributor.authorAzor, A.
dc.date.accessioned2014-10-30T12:12:41Z
dc.date.available2014-10-30T12:12:41Z
dc.date.issued2003
dc.identifier.urihttp://hdl.handle.net/10272/9039
dc.description.abstractThe South Portuguese Zone is a foreland affected by a thin-skinned tectonics characterized by SSW-vergent thrust-and-folds developed in Carboniferous times as a consequence of the Variscan collision. In the Valverde del Camino area, detailed mapping and structural analysis show the existence of a fault-propagation antiform related to an imbricate fan with SSW sense of movement. The thrusts of this imbricate fan merge at depth with a detachment located in the middle crust. The total displacement produced by the imbricate fan is very scarce, most of the shortening being probably accommodated by folding and cleavage developmenten_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.otherThrust systemen_US
dc.subject.otherImbricate fanen_US
dc.subject.otherInclined foldsen_US
dc.subject.otherSouth Portuguese Zoneen_US
dc.titleEl abanico imbricado de Valverde del Camino (parte meridional de la Zona Sudportuguesa, Huelva)en_US
dc.titleThe imbricate fan of Valverde del Camino (southern part of the South Portuguese Zone, Huelva)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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