Rodés Bolumburu, ÁngelPallàs i Serra, RaimonOrtuño Candela, MariaGarcía Meléndez, EduardoMasana, Eulàlia2016-05-102016-05-102014-021871-1014https://hdl.handle.net/2445/98462Cosmogenic nuclide depth-profiles are used to calculate the age of landforms, the rates at which erosion has affected them since their formation and, in case of deposits, the paleo-erosion rate in the source area. However, two difficulties are typically encountered: 1) old deposits or strongly affected by cosmogenic nuclide inheritance often appear to be saturated, and 2) a full propagation of uncertainties often yields poorly constrained ages. Here we show how to combine surface-exposure-dating and burial-dating techniques in the same profile to get more accurate age results and to constrain the extent of pre-depositional burial periods. A 10Be-26Al depth-profile measured in an alluvial fan of SE Iberia is presented as a natural example.31 p.application/pdfeng(c) Elsevier B.V., 2014GeocronologiaPaleontologiaDatació arqueològicaQuaternariGeomorfologiaGeochronologyPaleontologyArchaeological datingQuaternaryGeomorphologyinfo:eu-repo/semantics/article6307632016-05-10info:eu-repo/semantics/openAccess