The stable isotope altimeter: Do Quaternary pedogenic carbonates predict modern elevations?

dc.date.accessioned2020-03-11T20:37:30Z
dc.date.accessioned2022-10-18T23:06:15Z
dc.date.available2020-03-11T20:37:30Z
dc.date.available2022-10-18T23:06:15Z
dc.date.created2020-03-11T20:37:30Z
dc.date.issued2009
dc.identifierhttp://hdl.handle.net/10533/241328
dc.identifier15010001
dc.identifierWOS:000271215600014
dc.identifierno scielo
dc.identifiereid=2-s2.0-70450214724
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4472667
dc.description.abstractStable isotope altimetry is a useful tool for estimating paleoelevation in sedimentary records. Yet questions remain regarding how source moisture, climate, and local topography can influence these estimates. Here we present stable isotope altimetry resul
dc.languageeng
dc.relationhttps://doi.org/10.1130/G30308A.1
dc.relation10.1130/G30308A.1
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.titleThe stable isotope altimeter: Do Quaternary pedogenic carbonates predict modern elevations?
dc.typeArticulo


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