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dc.contributor.authorMontes Santiago, M. J.
dc.contributor.authorAlonso Gavilán, G.
dc.contributor.authorDabrio, Cristino José
dc.date.accessioned2020-06-17T09:17:34Z
dc.date.available2020-06-17T09:17:34Z
dc.date.issued1989
dc.identifier.urihttp://hdl.handle.net/10272/18323
dc.description.abstractThe Villarcayo basin is situated at the NW of Duero Basin and it's incorporated into the Cantabric dominio. The ilerdien transgression is represented for Alveolina Limestone inconformity above transition marine-continental lower deposits Litoral detritic deposits are situated above this limestone unit and they constitue a new regresive episodees_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.otherTransgressiones_ES
dc.subject.otherAlveolina limestonees_ES
dc.subject.otherPaleogeographyes_ES
dc.subject.otherVillarcayo basines_ES
dc.subject.otherSpaines_ES
dc.titleLa transgresión Ilerdense (calizas de Alveolinas) en la Cuenca de Villarcayo (Burgos)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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