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The “Urbasa” type flint. Main petrological and geochemical features of a litologhic marker in late Pleistocene and earliest Holocene archaeological sites

dc.contributor.authorTarriño, A.
dc.contributor.authorOlivares, M.
dc.contributor.authorEtxebarria, N.
dc.contributor.authorBaceta, Juan Ignacio
dc.contributor.authorLarrasoaña, J. C.
dc.contributor.authorYusta, Iñaki
dc.contributor.authorPizarro, José Luis
dc.contributor.authorCava, A.
dc.contributor.authorBarandiarán, I.
dc.contributor.authorMurelaga, Xabier
dc.date.accessioned2014-06-25T11:28:19Z
dc.date.available2014-06-25T11:28:19Z
dc.date.issued2007
dc.identifier.urihttp://hdl.handle.net/10272/8355
dc.description.abstractThe “Urbasa” flint, which occurs intercalated within shallow-water limestones of Thanetian (upper Paleocene) age was one of the best and most used flint sources during the Prehistoric times in the Basque-Cantabrian area. Two of the main outcrops/quarries where the “Urbasa” flint was exploited are located in the Urbasa ridge (W Navarra). The analysis of the compositional texture, mineralogy and geochemical features has revealed that the “Urbasa” flint is highly pure and of fine-grained texture, but with high contents of moganite, traces of organic matter and, less frequently, carbonates and clayen_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.otherFlinten_US
dc.subject.otherPaleoceneen_US
dc.subject.otherUrbasaen_US
dc.subject.otherArchaeological sitesen_US
dc.titleEl sílex de tipo “Urbasa”. Caracterización petrológica y geoquímica de un marcador litológico en yacimientos arqueológicos del Suroeste europeo durante el Pleistoceno superior y Holoceno inicialen_US
dc.titleThe “Urbasa” type flint. Main petrological and geochemical features of a litologhic marker in late Pleistocene and earliest Holocene archaeological siteseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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