Journal of Volcanology and Geothermal Research

dc.creatorRoulleau, E.3; Bravo, F.; Pinti, D.L.; Barde-Cabusson, S.; Pizarro, M.; Tardani, D.; Muñoz, C.; Sánchez, J.; Sano, Y.; Takahata, N.; de la Cal, F.; Esteban, C; Morata, D.
dc.date2020-03-11T20:27:24Z
dc.date2022-07-07T23:46:55Z
dc.date2020-03-11T20:27:24Z
dc.date2022-07-07T23:46:55Z
dc.date2017
dc.date.accessioned2023-08-22T23:38:38Z
dc.date.available2023-08-22T23:38:38Z
dc.identifier15090013
dc.identifier15090013
dc.identifierhttps://hdl.handle.net/10533/238281
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8351964
dc.descriptionNatural geothermal systems are limited areas characterized by anomalously high heat flow caused by recent tectonic or magmatic activity. The heat source at depth is the result of the emplacement of magma bodies, controlled by the regional volcano-tectonic
dc.descriptionFONDAP
dc.descriptionFONDAP
dc.languageeng
dc.relationhttps://doi.org/10.1016/j.jvolgeores.2017.05.010
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.titleStructural controls on fluid circulation at the Caviahue-Copahue Volcanic Complex (CCVC) geothermal area (Chile-Argentina), revealed by soil CO2 and temperature, self-potential, and helium isotopes
dc.titleJournal of Volcanology and Geothermal Research
dc.typeArticulo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


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