Preservation of beach ridges due to pedogenic calcrete development in the Tongoy palaeobay, north-central Chile.

Geomorphology

dc.creatorPfeiffer, M.
dc.creatorLe Roux, J. P.
dc.creatorSolleiro-Rebolledo, E.
dc.creatorKemnitz, H.
dc.creatorSedov, S.
dc.creatorSeguel, O.
dc.date2020-03-11T20:26:28Z
dc.date2022-07-07T23:44:01Z
dc.date2020-03-11T20:26:28Z
dc.date2022-07-07T23:44:01Z
dc.date2011
dc.date.accessioned2023-08-22T03:54:42Z
dc.date.available2023-08-22T03:54:42Z
dc.identifier15090013
dc.identifier15090013
dc.identifierhttps://hdl.handle.net/10533/238020
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8317204
dc.descriptionAt the Tongoy palaeobay in north-central Chile, a series of beach ridges developed during seaward progradation that took place after the MIS 11 sea-level highstand (412 ka). The microrelief left by this succession of beach ridges has been well preserved f
dc.descriptionFONDAP
dc.descriptionFONDAP
dc.languageeng
dc.relationhttps://doi.org/10.1016/j.geomorph.2011.05.012
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titlePreservation of beach ridges due to pedogenic calcrete development in the Tongoy palaeobay, north-central Chile.
dc.titleGeomorphology
dc.typeArticulo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


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