dc.date.accessioned2020-03-11T20:27:00Z
dc.date.accessioned2022-10-18T22:42:07Z
dc.date.available2020-03-11T20:27:00Z
dc.date.available2022-10-18T22:42:07Z
dc.date.created2020-03-11T20:27:00Z
dc.date.issued2016
dc.identifierhttp://hdl.handle.net/10533/238176
dc.identifier15090013
dc.identifierWOS:000378205500013
dc.identifierno scielo
dc.identifiereid=2-s2.0-84960951951
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4469515
dc.description.abstractOver thousands to millions of years, the landscape evolution is predicted by models based on fluxes of eroded, transported and deposited material. The laws describing these fluxes, corresponding to averages over many years, are difficult to prove with the
dc.languageeng
dc.relationhttps://doi.org/10.5194/esurf-4-237-2016
dc.relation10.5194/esurf-4-237-2016
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.titleModelling sediment clasts transport during landscape evolution
dc.typeArticulo


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