Tracking Magmatic Hydrogen Sulfur Circulations Using Electrical Impedance : Complex Electrical Properties of Core Samples at the Krafla Volcano, Iceland
Interaction of H2S escaping from magma and basaltic rocks leads to pyrite mineralization, witnessing active hydrothermal circulation. We study the possibility to track this process using geoelectrical methods. Complex conductivity spectra of 30 core samples from the Krafla volcano, Iceland, measured in the laboratory, indicate that pyrite can be discriminated from other minerals present in volcani
