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dc.contributor.authorVidal Romaní, Juan Ramónes_ES
dc.contributor.authorFernández Mosquera D.es_ES
dc.contributor.authorMarti, Kurtes_ES
dc.date.accessioned2015-07-06T11:16:31Z
dc.date.available2015-07-06T11:16:31Z
dc.date.issued2015es_ES
dc.identifier.citationCadernos Laboratorio Xeolóxico de Laxe, 2015, 38: 27-45 ISSN:0213-4497es_ES
dc.identifier.issn0213-4497es_ES
dc.identifier.urihttp://hdl.handle.net/2183/14750
dc.description.abstract[Abstract]The Serras of Queixa-Invernadoiro and Gerês-Xurés in the NW of the Iberian Peninsula are two small mountain massifs located at low altitude that were glaciated in the Pleistocene. The prevailing granitic lithology was a problem for mapping glacial forms (in many cases interpreted as banal granite forms) and for the identification of the tills (misunderstood as remains of regolith). A combination of geomorphological techniques (genetic mapping of granite forms and deposits), the micromorphological study of till thin sections and the morphoscopy of quartz grains at the SEM enabled to establish a model of the geomorphological evolution complemented with the chronology by cosmogenic nuclides (21Ne and 10Be) of both glacial systems. The obtained results represent the glacial evolution of the area from circa 250 ka B.P.es_ES
dc.language.isoenges_ES
dc.publisherUniversidade da Coruñaes_ES
dc.subjectGlaciationes_ES
dc.subjectCosmogenic nuclides chronologyes_ES
dc.subjectNW Iberian Peninsulaes_ES
dc.subjectTilles_ES
dc.subjectMorainees_ES
dc.subjectPleistocenees_ES
dc.titleThe glaciation of Serra de Queixa-Invernadoiro and Serra do Gerês-Xurés, NW Iberia. A critical review and a cosmogenic nuclide (10Be and 21 Ne) chronology.es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccesses_ES


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