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Sedimentological characterization of Upper Miocene-Pliocene fluviolacustrine and tuffaceous systems of the Calatayud Basin (Zaragoza)

dc.contributor.authorSanz Rubio, E.
dc.contributor.authorHoyos, M.
dc.contributor.authorCañaveras, J.C.
dc.contributor.authorSánchez Moral, S.
dc.contributor.authorCalvo, J. Pedro
dc.date.accessioned2016-04-08T12:08:30Z
dc.date.available2016-04-08T12:08:30Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/11824
dc.description.abstractA complex fluviolacustrine calcareous system with associated autochtonous tufa deposits is recognized in the Upper Miocene-Pliocene of the Neogene Calatayud Basin. A detailed sedimentological analysis of the calcareous sediments reveals a wide spectrum óf facies associations mainly related to reworking of tufa deposits including products such as oncolithic tufas and less common phytoclastic and intraclastic tufasen_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.otherCalatayud Basinen_US
dc.subject.otherMiocene-Plioceneen_US
dc.subject.otherTufaen_US
dc.subject.otherOncoidsen_US
dc.titleCaracterización sedimentológica de los sistemas fluviolacustres y tobáceos del Mioceno Superior-Plioceno de la Cuenca de Calatayud (Zaragoza)en_US
dc.titleSedimentological characterization of Upper Miocene-Pliocene fluviolacustrine and tuffaceous systems of the Calatayud Basin (Zaragoza)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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