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Late Pleistocene deglaciation chronology in the NW of the Iberian Peninsula using cosmic-ray produced 27Ne in quartz

dc.contributor.authorFernández Mosquera, D.
dc.contributor.authorVidal Romani, J. R.
dc.contributor.authorMarti, K.
dc.date.accessioned2015-02-10T11:56:12Z
dc.date.available2015-02-10T11:56:12Z
dc.date.issued1999
dc.identifier.urihttp://hdl.handle.net/10272/9850
dc.description.abstractLate Pleistocene glaciations in the NW Iberian Peninsula over Serra de Queixa and Serra de Xurés, all with granite substrata, were studied by mass spectrometry using cosmogenic 21 Ne. Rock cores were drilled in glacial polished surfaces and push moraine boulders, and were analyzed to determine their integral exposure time to cosmic rays. First results, which are consistent with the relative géomorphologie model estimates, allow the identification of at least three different glacial stages, with the latest one terminating about 75 Ka B.P.en_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.otherPleistocene glaciationsen_US
dc.subject.otherNW Iberian Peninsulaen_US
dc.subject.otherCosmogenic 21 Neen_US
dc.titleCronologia glaciar Pleistocena del NW de la Peninsula Iberica mediante 21 Ne cosmogenico en cuarzoen_US
dc.titleLate Pleistocene deglaciation chronology in the NW of the Iberian Peninsula using cosmic-ray produced 27Ne in quartzeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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