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dc.contributor.authorArenas Abad, Concepción
dc.contributor.authorPardo, Gonzalo
dc.contributor.authorVillena, J.
dc.date.accessioned2020-06-08T08:42:57Z
dc.date.available2020-06-08T08:42:57Z
dc.date.issued1990
dc.identifier.urihttp://hdl.handle.net/10272/18191
dc.description.abstractAt the septentrional margin of the Ebro Basin, the conglomeratic facies of Uncastillo Formation correspond to two complex cyclic Tectosedimentary Units (TSU Ul and U). Towards the West, thesê TSU lie on Campodarbe Formation whose upper section is recognizable as another cyclic TSU (C), and towards the Fast lie on marine paleogene and mesozoic sediments of the Pyrenean Externa/ Sierras. The fining-up megasequences of the TSU C2, Ul and IJ2 represent the initial burial of the thrust units of the south Pyrenean frontal thrust complex, placed successively from West to East during the time of the coarsening-up megasequences of former TSUes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherSpaines_ES
dc.subject.otherAragónes_ES
dc.subject.otherSouth Pyrenean frontes_ES
dc.subject.otherTectosedimentary Unitses_ES
dc.subject.otherConglometatic facieses_ES
dc.subject.otherTertiaryes_ES
dc.subject.otherTectonic-sedimentation relationshipes_ES
dc.titleLas unidades tectosedimentarias del margen septentrional de la Depresión del Ebro en el sector Luesia-Riglos (provincias de Zaragoza y Huesca)es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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