Por favor, use este identificador para citar o enlazar este ítem: https://cir.cenieh.es/handle/20.500.12136/972
Registro completo de metadatos
Campo DC Valor Lengua/Idioma
dc.contributor.authorTarriño Vinagre, Antonio-
dc.contributor.authorAguirre, Mikel-
dc.contributor.authorElorrieta Baigorri, Irantzu-
dc.contributor.authorJiménez Barredo, Fernando-
dc.contributor.authorOrúe Beltrán de Heredia, Íñigo-
dc.contributor.authorCava Almuzara, Ana Catalina-
dc.contributor.authorBarandiarán Maestu, Ignacio-
dc.date.accessioned2018-12-13T14:25:29Z-
dc.date.issued2016-
dc.identifier.citationRaw materials exploitation in Prehistory: sourcing, processing and distribution, 2016, p. 27es_ES
dc.identifier.isbn978-989-8472-79-3-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/972-
dc.descriptionPonencia presentada en: Raw materials exploitation in Prehistory: sourcing, processing and distribution, 10-12 de marzo 2016, Faroes_ES
dc.description.abstractNodular silicifications which were exploited during Prehistoric times can be found in Sierra de Urbasa plateau (Navarra). These flints, hosted in marls, marl-limestone and bioclastic calcarenites of the Thanetian (Paleocene, Cenozoic), contain benthonic foraminifera (Nummulites heberti and Discocyclina seunesi), pertaining to marine environments of shallow external platform. The outcrops are arranged along a 100-300 m thick and around 10 km long. The flints, which arise in discontinuous layers parallel to the stratification, present nodular morphologies in dark colours (usually 5-20 cm). They are fine grain flints composed of micro and cryptocrystalline quartz with carbonate relicts and a distinctive microdolomitization. Although the existence of flint outcrops has not been cited in the geological literature until present, the relation between archaeological sites and the outcrops has been described for us in recent investigations about Mugarduia. The prehistoric flint workshop is installed above the stratum itself or in its vicinity. We analyzed the lithic material that came from an intact archaeological deposit stratified discovered in the workshop, carried out in the fieldworks of the 80’s by I. Barandiaran and A. Cava. There were collected 995 retouched artefacts, around 400 cores and around 53,000 residues from the workshop. The analysis of the retouched artefacts of the mentioned collection allows the identification of seven flint types: Urbasa (local, mostly massive and showing a variable external aspect), Flysch, Trevino, Gaintxurizketa, Salies de Bearn, Urgonian, Loza (allochthonous all them). Allochthonous flint represents 7.8% of the retouched industry. This is a huge quantity taking into account the flint samples were collected from workshop context in the surroundings of Urbasa’s natural outcrops. We aim to study the nature and variability of the identified flints through geochemical and mineralogical methods and the management of the resources considering aspects of typology, typometry and technology.es_ES
dc.language.isoenes_ES
dc.publisherICArEHB ; Universidade do Algarve ; CSICes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.subjectRaw materialses_ES
dc.subjectUrbasa flintes_ES
dc.subjectGravettianes_ES
dc.subjectWorkshopes_ES
dc.subjectWestern Pyreneeses_ES
dc.titleFlints of the Gravettian Workshop of Mugarduia Sur (Sierra de Urbasa, Wester Pyrenees, Spain)es_ES
dc.typePresentationes_ES
dc.typeOtheres_ES
dc.date.available2018-12-13T14:25:29Z-
Aparece en las colecciones: Congresos, encuentros científicos y estancias de investigación

Ficheros en este ítem:
No hay ficheros asociados a este ítem.


Los ítems de DSpace están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.