Articulo
Structural 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
Journal of Volcanology and Geothermal Research
Registro en:
15090013
15090013
Autor
Roulleau, 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.
Institución
Resumen
Natural 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 FONDAP FONDAP