Sr- and Nd- isotope variations along the Pleistocene San Pedro – Linzor volcanic chain, N. Chile: Tracking the influence of the upper crustal Altiplano-Puna Magma Body

dc.date.accessioned2020-03-11T20:27:02Z
dc.date.accessioned2022-10-18T22:42:13Z
dc.date.available2020-03-11T20:27:02Z
dc.date.available2022-10-18T22:42:13Z
dc.date.created2020-03-11T20:27:02Z
dc.date.issued2017
dc.identifierhttp://hdl.handle.net/10533/238190
dc.identifier15090013
dc.identifierWOS:000406728200015
dc.identifierno scielo
dc.identifiereid=2-s2.0-85020110858
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4469529
dc.description.abstractSubduction-related magmas that erupted in the Central Andes during the past 10 Ma are strongly affected by crustal assimilation as revealed by an increase in 87Sr/86Sr isotope ratios with time that in turn are correlated with increased crustal thickening 
dc.languageeng
dc.relationhttps://doi.org/10.1016/j.jvolgeores.2017.05.030
dc.relation10.1016/j.jvolgeores.2017.05.030
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.titleSr- and Nd- isotope variations along the Pleistocene San Pedro – Linzor volcanic chain, N. Chile: Tracking the influence of the upper crustal Altiplano-Puna Magma Body
dc.typeArticulo


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