Chemical and isotopic features of cold and thermal fluids discharged in the Southern Volcanic Zone between 32.5°S and 36°S: Insights into the physical and chemical processes controlling fluid geochemistry in geothermal systems of Central Chile

Author:

Benavente O.,Tassi F.,Reich M.,Aguilera F.,Capecchiacci F.,Gutiérrez F.,Vaselli O.,Rizzo A.

Funder

FONDAP

MECESUP

CONICYT (Chilean National Commission for Science and Technology)

FONDECYT

Fluid Geochemistry and Stable Isotopes of the Department of Earth Sciences of the University of Florence

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference89 articles.

1. Gas geochemistry of the magmatic-hydrothermal fluid reservoir in the Copahue–Caviahue Volcanic Complex (Argentina);Agusto;J. Volcanol. Geotherm. Res.,2013

2. The Maipo Orocline: a first scale structural feature in the Miocene to Recent geodynamic evolution in the central Chilean Andes;Arriagada;AndGeo,2013

3. Spatial distribution of earthquakes and subduction of the Nazca plate beneath South America;Barazangi;Geology,1976

4. Geothermal projects in South America of hot rock limited;Barnett,2012

5. Origin of fumarolic fluids from Tupungatito Volcano (Central Chile): interplay between magmatic, hydrothermal, and shallow meteoric sources;Benavente;Bull. Volcanol.,2013

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