Evolución megasecuencial de los materiales oligo-miocenos del sector septentrional de la Cuenca del Ebro (provincia de Huesca)

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dc.contributor.authorLuzón, Aránzazu
dc.date.accessioned2015-04-10T10:09:30Z
dc.date.available2015-04-10T10:09:30Z
dc.date.issued1997
dc.description.abstractThe outcropping continental detrital formations in the northern margin of the Ebro Basin between the Sierras Exteriores Aragonesas and the Sierras Marginales Catalanas have been analyzed. These materials form part of the classic Peraltilla and Sarinena Formations. This study demonstrates the ambiguity which exists in delimiting of both formations. The study of the megasequential evolution of the materials may provide new criteria to precise the limit between themen_US
dc.identifier.urihttp://hdl.handle.net/10272/10309
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.otherMegasequential evolutionen_US
dc.subject.otherPeraltilla and Sarinena Formationsen_US
dc.subject.otherOligocene-Mioceneen_US
dc.subject.otherEbro Basinen_US
dc.titleEvolución megasecuencial de los materiales oligo-miocenos del sector septentrional de la Cuenca del Ebro (provincia de Huesca)en_US
dc.titleMegasequential evolution of Oligocene-Miocene materials of the northern sector of the Ebro Basin (Huesca to province)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 24, (1997)