Estudio preliminar sobre la tectónica sinsedimentaria del Cretácico inferior en el borde septentrional de la Cubeta de Aliaga (Cordillera Ibérica)

dc.contributor.authorLiesa, Carlos L.
dc.contributor.authorSoria, Ana Rosa
dc.contributor.authorMeléndez Hevia, Alfonso
dc.date.accessioned2017-01-26T12:57:04Z
dc.date.available2017-01-26T12:57:04Z
dc.date.issued1996
dc.description.abstractThe Aliaga sub-basin was developed during the Early Cretaceous in an extensional context. Structures near the northern border of this sub-basin (normal faults, syntectonic unconformities and facies and thickness changes in the basin infill) are related to this extensional tectonics. The graben and semigraben system determines the syntectonic infill thickness. In the footwall of the main faults the pre-rift sequence is erodeden_US
dc.identifier.urihttp://hdl.handle.net/10272/13201
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.otherSynsedimentary tectonicen_US
dc.subject.otherLower Cretaceousen_US
dc.subject.otherAliaga sub-basinen_US
dc.titleEstudio preliminar sobre la tectónica sinsedimentaria del Cretácico inferior en el borde septentrional de la Cubeta de Aliaga (Cordillera Ibérica)en_US
dc.titlePreliminary study of the Lower Cretaceous synsedimentary tectonics in the northern border of Aliaga sub-basin (Iberian Chain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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