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dc.contributor.authorAlonso Diago, María A.
dc.date.accessioned2020-07-10T09:51:01Z
dc.date.available2020-07-10T09:51:01Z
dc.date.issued1986
dc.identifier.urihttp://hdl.handle.net/10272/18505
dc.description.abstractThe use of paleontologic and sedimentologic-morfologic arguments has allow us to identify four groups of sediments with diverse chronology: —Lower Unit (Upper Ruscinian, Ruscinian-VilIafranchian limit).—Upper Unit (Villafranchian).—lncrust Glacis Sistem (Upper Pleistocene).—Watershed deposits (Upper Pleistocene, Holocene). Their geometric distribution, litology, lateral changes and relations between them give information about some aspects of the Plio-Pleistocene history in the West edge of the Guadix-Baza Depressiones_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherPliocenees_ES
dc.subject.otherPleistocenees_ES
dc.subject.otherGuadix-Baza Depresiones_ES
dc.titleSituación estratigráfica de los yacimientos de vertebrados del borde oeste de la depresión de Guadix-Baza (zona de Huélago y Fonelas)es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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