Protracted late magmatic stage of the Caleu Pluton: Insights from zircon data and thermal modeling.

dc.date.accessioned2020-03-11T20:26:57Z
dc.date.accessioned2022-10-18T22:41:58Z
dc.date.available2020-03-11T20:26:57Z
dc.date.available2022-10-18T22:41:58Z
dc.date.created2020-03-11T20:26:57Z
dc.date.issued2015
dc.identifierhttp://hdl.handle.net/10533/238157
dc.identifier15090013
dc.identifierWOS:000356115800017
dc.identifierno scielo
dc.identifiereid=2-s2.0-84929658980
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4469496
dc.description.abstractZircon U-Pb geochronology and geochemistry are combined with whole-rock composition and thermal modeling to decipher the late magmatic stage of the composite Cretaceous Caleu pluton, which consists of four lithological zones: Gabbro-Diorite Zone (GDZ), Qu
dc.languageeng
dc.relationhttps://doi.org/10.1016/j.lithos.2015.04.008
dc.relation10.1016/j.lithos.2015.04.008
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.titleProtracted late magmatic stage of the Caleu Pluton: Insights from zircon data and thermal modeling.
dc.typeArticulo


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