Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/1269
Full metadata record
DC FieldValueLanguage
dc.contributor.authorRixhon, Gilles-
dc.contributor.authorBriant, Rebecca M.-
dc.contributor.authorCordier, Stéphane-
dc.contributor.authorDuval, Mathieu-
dc.contributor.authorJones, Anna F.-
dc.contributor.authorScholz, Denis-
dc.date.accessioned2019-06-03T13:17:44Z-
dc.date.issued2017-06-
dc.identifier.citationQuaternary Science Reviews, 2017, 166, 91-113es_ES
dc.identifier.issn0277-3791-
dc.identifier.issn1873-457X-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/1269-
dc.description.abstractDuring the last twenty years, several technical developments have considerably intensified the use of numerical dating methods for the Quaternary. The study of fluvial archives has greatly benefited from these enhancements, opening new dating horizons for a range of archives at distinct time scales and thereby providing new insights into previously unanswered questions. In this contribution, we separately present the state of the art of five numerical dating methods that are frequently used in the fluvial context: radiocarbon, Luminescence, Electron Spin Resonance (ESR), 230Th/U and terrestrial cosmogenic nuclides (TCN) dating. We focus on the major recent developments for each technique that are most relevant for new dating applications in diverse fluvial environments and on explaining these for non-specialists. Therefore, essential information and precautions about sampling strategies in the field and/or laboratory procedures are provided. For each method, new and important implications for chronological reconstructions of Quaternary fluvial landscapes are discussed and, where necessary, exemplified by key case studies. A clear statement of the current technical limitations of these methods is included and forthcoming developments, which might possibly open new horizons for dating fluvial archives in the near future, are summarised.es_ES
dc.description.sponsorshipM. Duval's research was funded by a Marie Curie International Outgoing Fellowship of the EU’s Seventh Framework Programme (FP7/2007-2013), awarded under REA Grant Agreement No. PIOF-GA-2013-626474. D. Scholz acknowledges funding of the DFG (SCHO 1274/9-1).es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectNumerical dating methodes_ES
dc.subjectFluvial archiveses_ES
dc.subjectQuaternaryes_ES
dc.subject14C datinges_ES
dc.subjectLuminescence datinges_ES
dc.subjectESR datinges_ES
dc.subject230Th/U datinges_ES
dc.subjectTerrestrial cosmogenic nuclides datinges_ES
dc.titleRevealing the pace of river landscape evolution during the Quaternary: recent developments in numerical dating methodses_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.quascirev.2016.08.016-
dc.relation.publisherversionhttps://doi.org/10.1016/j.quascirev.2016.08.016es_ES
dc.date.available2019-06-03T13:17:44Z-
Appears in Collections:Geocronología y Geología



This item is licensed under a Creative Commons License Creative Commons