Cronologia glaciar Pleistocena del NW de la Peninsula Iberica mediante 21 Ne cosmogenico en cuarzo

dc.contributor.author	Fernández Mosquera, D.
dc.contributor.author	Vidal Romani, J. R.
dc.contributor.author	Marti, K.
dc.date.accessioned	2015-02-10T11:56:12Z
dc.date.available	2015-02-10T11:56:12Z
dc.date.issued	1999
dc.description.abstract	Late 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.identifier.uri	http://hdl.handle.net/10272/9850
dc.language.iso	spa	en_US
dc.publisher	Sociedad Geológica de España	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.accessRights	open access	en_US
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Pleistocene glaciations	en_US
dc.subject.other	NW Iberian Peninsula	en_US
dc.subject.other	Cosmogenic 21 Ne	en_US
dc.title	Cronologia glaciar Pleistocena del NW de la Peninsula Iberica mediante 21 Ne cosmogenico en cuarzo	en_US
dc.title	Late Pleistocene deglaciation chronology in the NW of the Iberian Peninsula using cosmic-ray produced 27Ne in quartz	eng
dc.type	journal article	en_US
dspace.entity.type	Publication

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