dc.date.accessioned2020-03-11T20:27:06Z
dc.date.accessioned2022-10-18T22:42:20Z
dc.date.available2020-03-11T20:27:06Z
dc.date.available2022-10-18T22:42:20Z
dc.date.created2020-03-11T20:27:06Z
dc.date.issued2016
dc.identifierhttp://hdl.handle.net/10533/238206
dc.identifier15090013
dc.identifierWOS:000390969700006
dc.identifierno scielo
dc.identifiereid=2-s2.0-85027930464
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4469545
dc.description.abstractWe measured noble gas and stable isotopes of the geothermal and hydrothermal fluids of the Caviahue-Copahue Volcanic Complex (CCVC), one of the most important geothermal systems in Argentina/Chile, in order to provide new insights into fluid circulation a
dc.languageeng
dc.relationhttps://doi.org/10.1016/j.jvolgeores.2016.10.007
dc.relation10.1016/j.jvolgeores.2016.10.007
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.titleNew insight from noble gas and stable isotopes of geothermal/ hydrothermal fluids at Caviahue-Copahue Volcanic Complex: Boiling steam separation and water-rock interaction at shallow depth
dc.typeArticulo


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