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The Upper Ordovician sequence of Portilla de Luna (Canlabrian Tone, NW Spain)

dc.contributor.authorGutiérrez Marco, Juan Carlos
dc.contributor.authorAramburu, C.
dc.contributor.authorArbizu, M.
dc.contributor.authorMéndez Bedia, I.
dc.contributor.authorRábano, Isabel
dc.contributor.authorVillas, E.
dc.date.accessioned2015-11-24T12:59:16Z
dc.date.available2015-11-24T12:59:16Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/11425
dc.description.abstractUpper Ordovician rocks have been characterized for the first time in the Cantabrian Zone of the Hesperian Massif. The sequence consists of a lower siliciclastic unit of Caradoc-(‘basal Ashgill age developed as an alternation of shales, siltstones and sandstones, overlain by an upper unit of fossiliferous limestones with marly intercalations, of pre-Hirnantian (mainly Cautleyan-Rawtheyan) age. Ashgill fossils are fairly abundant in the limestone unit, and there have been identified brachiopods of the «Nicolella fauna», echinoderms of the «Heliocrinites fauna» and trilobites of the Qvalocephalus biofaciesen_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.otherOrdovicianen_US
dc.subject.otherLithostratigraphyen_US
dc.subject.otherBiostratigraphyen_US
dc.subject.otherCantabrian Zoneen_US
dc.subject.otherSpainen_US
dc.titleRasgos estratigráficos de la sucesión del Ordovícico Superior en Portilla de Luna (Zona Cantábrica, noroeste de España)en_US
dc.titleThe Upper Ordovician sequence of Portilla de Luna (Canlabrian Tone, NW Spain)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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