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Transpresive neotectonics along South-lberián Atlantic shelf

dc.contributor.authorMaestro González, Adolfo
dc.contributor.authorSomoza, L.
dc.contributor.authorDíaz del Río, Víctor
dc.contributor.authorVázquez Garrido, Juan Tomás
dc.contributor.authorMartín Alfageme, S.
dc.contributor.authorAlveirinho, J. M.
dc.contributor.authorBarnolas, Antonio
dc.contributor.authorVegas, Ramón
dc.date.accessioned2015-04-13T11:01:45Z
dc.date.available2015-04-13T11:01:45Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10323
dc.description.abstractDetailed structural, interpretátioh of a network of high-resolution seismic lines runnig across, , and along the continental shelf of Faro (south-lberian Atlantic margin) provides evidences of recent deformation structures associated with the Africa-Eurasia plate boundary. In these seismic profiles, palm-tree type flower structures interpreted as strike-slip faults affect the non-consolidated Holocene muddy shelf deposits and the underlying semi-cemented sandy shelf-wedges of the Pleistocene units. These structures are lined up following a ENE-WSW. direction, associated with the existence of a deeper dextral transcurrent basement fault with recent active seismicity between the southern Coringe Bank, Horseshoe Plain, Faro continental shelf and northern of Guadalquivir basinen_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.otherIberian Atlantic marginen_US
dc.subject.otherRecent tectonic evolutionen_US
dc.subject.otherDextral transcurrent faultsen_US
dc.subject.otherPalm-tree structuresen_US
dc.titleNeotectómca transpresiva en la plataforma continental Suribérica Atlánticaen_US
dc.titleTranspresive neotectonics along South-lberián Atlantic shelfeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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