In this framework, deformation due to strike-slip kinematics rather than to folding process may have focused hot fluids and driven localized thermal alteration of the cap-rock. Coupling these results together with the recently published geochemical, hydrogeological and audiomagnetotelluric data (Barcelona et al., 2013; Invernizzi et al., 2014; Chiodi et al., 2015) (CHAPTER 6), I suggest that the most favourable site for a potential future exploitation of the thermal fluids is located along the northern buried plunge of the Balboa anticline. The high temperatures reached by the thermal fluids in this area (~120°C) suggest that an undirect heat use for electric power generation could be feasible. Furthermore, the compartimentalization ruled by the NNW-SSE fault plane may guarantee, at the same time, the sustainability of the geothermal resource exploited at present by the Hotel Termas, in correspondence of the Termas anticline.
Exploration of medium - and low - enthalpy geothermal resources in the sub - Andean area for the sustainable development of the cities of Salta province (northwestern Argentina)
2015
Abstract
In this framework, deformation due to strike-slip kinematics rather than to folding process may have focused hot fluids and driven localized thermal alteration of the cap-rock. Coupling these results together with the recently published geochemical, hydrogeological and audiomagnetotelluric data (Barcelona et al., 2013; Invernizzi et al., 2014; Chiodi et al., 2015) (CHAPTER 6), I suggest that the most favourable site for a potential future exploitation of the thermal fluids is located along the northern buried plunge of the Balboa anticline. The high temperatures reached by the thermal fluids in this area (~120°C) suggest that an undirect heat use for electric power generation could be feasible. Furthermore, the compartimentalization ruled by the NNW-SSE fault plane may guarantee, at the same time, the sustainability of the geothermal resource exploited at present by the Hotel Termas, in correspondence of the Termas anticline.I documenti in UNITESI sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
https://hdl.handle.net/20.500.14242/273330
URN:NBN:IT:UNIROMA3-273330