The role of smectites in the electrical conductivity of active hydrothermal systems : Electrical properties of core samples from Krafla volcano, Iceland
The underground circulation of hot water, of interest for geothermal energy production, is often indirectly inferred from the presence of minerals formed by hydrothermal alteration at different temperatures. Clay minerals, such as smectite and chlorite, can be mapped from the surface using electrical soundings and give information about the structure of the geothermal system. Here, we investigate