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Tectosedìmentary evolution of the Blesa Fm. (Lower Cretaceous) around the La Cantalera fossil site (Josa, Teruel)

dc.contributor.authorBádenas, Beatriz
dc.contributor.authorCanudo, José Ignacio
dc.contributor.authorRuiz Omeñaca, José Ignacio
dc.date.accessioned2014-10-27T11:53:39Z
dc.date.available2014-10-27T11:53:39Z
dc.date.issued2003
dc.identifier.urihttp://hdl.handle.net/10272/8988
dc.description.abstractGeological mapping and fades analysis of the Jurassic-Lower Cretaceous units located around the La Cantalera fossil site (Josa locality, Teruel Province, NE Spain), has allowed a precise reconstruction of a continental sedimentary basin developed around the Hauterivian-Barremian turnover. The first stage of evolution of the basin was controlled by intense normal fault activity and resulted in the formation of an isolated basin, surrounded by limestone-marly relief. The existence of a non-permanent water marshy area, with an important vegetated area, explain the abundance and diversity of the fossil remains in the studied localityen_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.otherIberian Chainen_US
dc.subject.otherSynsedimentary tectonicsen_US
dc.subject.otherAlluvial fansen_US
dc.subject.otherVertebratesen_US
dc.titleEvolución tectosedimentaria de la Fm. Blesa (Cretàcico Inferior) en el entorno del yacimiento de vertebrados de La Cantalera (Josa, Teruel)en_US
dc.titleTectosedìmentary evolution of the Blesa Fm. (Lower Cretaceous) around the La Cantalera fossil site (Josa, Teruel)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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