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The occurrence of a Cretaceous succession in the Ubiñas Massif (Cantabrian Mountains). Tectonic and geomorphologic implications

dc.contributor.authorAlonso, J. L.
dc.contributor.authorMartínez Abad, I.
dc.contributor.authorGarcía Ramos, José Carlos
dc.date.accessioned2014-06-26T11:44:17Z
dc.date.available2014-06-26T11:44:17Z
dc.date.issued2007
dc.identifier.urihttp://hdl.handle.net/10272/8372
dc.description.abstractThis paper describes the stratigraphy and structural setting of a new outcrop of Cretaceous sands and clays located in the center of the exposure of Palaeozoic rocks in the Cantabrian Zone. This isolated outcrop of Cretaceous rocks provides information on the uplift and structural imprint of the Variscan basement during the Alpine times. Thus, the uplift of the Ubiñas Massif, 400m above the regional level of summits, is the result of a reverse fault, which overrides the Cretaceous successionen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherCantabrian Mountainsen_US
dc.subject.otherCretaceousen_US
dc.subject.otherUtrillas faciesen_US
dc.titleNota sobre la presencia de una sucesión cretácica en el Macizo de Las Ubiñas (Cordillera Cantábrica). Implicaciones tectónicas y geomorfológicasen_US
dc.titleThe occurrence of a Cretaceous succession in the Ubiñas Massif (Cantabrian Mountains). Tectonic and geomorphologic implicationseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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