Electrical resistivity tomography and time-domain induced polarization field investigations of geothermal areas at Krafla, Iceland : Comparison to borehole and laboratory frequency-domain electrical observations
Interaction of H2S and basaltic rocks in volcanic geothermal areas can originate from natural up-flow of magmatic fluids or H2S artificial re-injection in relation to geothermal exploitation, both causing pyrite mineralization. We study the possibility to track these processes with electrical impedance field measurements. Electrical Resistivity Tomography (ERT) and Time- Domain Induced Polarizatio
