文摘
Groundwater circulation of a low-enthalpy geothermal system in Italy is studied. The major element chemistry and the δD, δ18O, 87Sr/86Sr and δ11B are analyzed. 87Sr/86Sr and δ11B behave as conservative tracers in low-enthalpy thermal systems. The results show a large energy potential of the Cimino-Vico Volcanic District.