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Soil CO2 emission and stable isotopes (δ13C, δ18O) of CO2 and calcites reveal the fluid origin and thermal energy in the supercritical geothermal system of Krafla, Iceland

by Bini, Giulio, Chiodini, Giovanni, Ricci, Tullio, Sciarra, Alessandra, Caliro, Stefano, Mortensen, Anette K, Martini, Marco, Mitchell, Andrew, Santi, Alessandro, Costa, Antonio
Published in Journal of Volcanology and Geothermal Research (2024)