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Karstic geomorphological evolution and Quaternary palaeoenvironments in Patones-Cerro de la Oliva massif (Madrid)

dc.contributor.authorBarea, José
dc.contributor.authorLópez Martínez, Jerónimo
dc.contributor.authorDurán Valsero, Juan José
dc.contributor.authorArribas, A.
dc.contributor.authorJulià, Ramón
dc.date.accessioned2014-12-09T13:45:32Z
dc.date.available2014-12-09T13:45:32Z
dc.date.issued2001
dc.identifier.urihttp://hdl.handle.net/10272/9487
dc.description.abstractGeomorphological, sedimentological and palaeontological evidences allowed to identify several phases in the evolution of the Patones-Cerro c/e la Oliva karstic massif. The studied speleothems, jointly with data of previous works indicate the presence of at least five episodes of chemical precipitation under favorable climatic conditions during isotopic stages 9-11?, 7, 5, 4-3 and 7, respectivelyen_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.otherKarsten_US
dc.subject.otherEvolución paleoambientalen_US
dc.subject.otherCuaternarioen_US
dc.subject.otherSistema Centralen_US
dc.titleEvolución geomorfológica del karst y paleoambientes cuaternarios en el macizo de Patones-Cerro de la Oliva (Madrid)en_US
dc.titleKarstic geomorphological evolution and Quaternary palaeoenvironments in Patones-Cerro de la Oliva massif (Madrid)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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