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- W2553483188 abstract "In the vicinity of the volcano Villarrica (South-Central Chile), geothermal manifestations at the surface are evident revealing lowenthalpy geothermal processes in the subsurface. The structural geology of the area, postulated by (Sanchez et al., 2013), set up a first draft of a structural model but also naming the complexity of the structural geology in the area generated by the interaction of two major fault systems and a change in the basement geology. In the first phase of the actual research project, geochemical methods are used to characterize the geothermal system. Besides standard geochemical techniques, clay mineralogy and δ 18 O[SO4]/δ 18 O[H2O] isotopes are used to determine the characteristics of the geothermal reservoir. The results of these techniques, pointing at a low-enthalpy reservoir in the vicinity of the active Villarrica volcano, are discussed in context of the special tectonic characteristics in the investigation area." @default.
- W2553483188 created "2016-11-30" @default.
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- W2553483188 date "2015-01-01" @default.
- W2553483188 modified "2023-09-23" @default.
- W2553483188 title "Geological and Tectonic Settings Preventing High-Temperature Geothermal Reservoir Development at Mt. Villarrica (Southern Volcanic Zone): Clay Mineralogy and Sulfate-Isotope Geothermometry" @default.
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