Estructuras post-sedimentarias en el margen noroccidental de la Cuenca del Guadalquivir (Niebla, Candón, Valverde del Camino), SO de España

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dc.contributor.authorAbad de los Santos, Manuel
dc.contributor.authorMantero Romero, Elena María
dc.contributor.authorCamacho Cerro, Manuel Alejandro
dc.contributor.authorMartín Banda, R.
dc.contributor.authorCantano Martín, Mercedes
dc.date.accessioned2014-09-19T11:41:54Z
dc.date.available2014-09-19T11:41:54Z
dc.date.issued2004
dc.description.abstractDescription of deformational structures in tertiary sediments, which have been interprerted as a result of a fluids migration process, along with the presence of preferential structural directions of fracture planes developed in the substratum. This fracture net could have been recently reactivated, so leading to the development of the described structuresen_US
dc.identifier.urihttp://hdl.handle.net/10272/8834
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherDeformational structuresen_US
dc.subject.otherFluid migrationen_US
dc.subject.otherFracture neten_US
dc.subject.otherSW Spainen_US
dc.titleEstructuras post-sedimentarias en el margen noroccidental de la Cuenca del Guadalquivir (Niebla, Candón, Valverde del Camino), SO de Españaen_US
dc.titlePost-sedimentary structures in the northwestern sector of the Guadalquivir foreland basin (Niebla, Candón, Valverde del Camino), SW Spaineng
dc.typejournal articleen_US
dspace.entity.typePublication
relation.isAuthorOfPublicationa35b0ebb-4ce5-449b-a1ff-dd14e4f5e4bd
relation.isAuthorOfPublicationc5f7096a-7d3a-462e-ac84-390f333d3015
relation.isAuthorOfPublication76a37e48-5f62-480a-af1f-d942b73829f8
relation.isAuthorOfPublication.latestForDiscoverya35b0ebb-4ce5-449b-a1ff-dd14e4f5e4bd

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Geogaceta -- Nº 37, (2004)