Conductivity distribution beneath Lascar volcano (Northern Chile) and the Puna, inferred from magnetotelluric data

Daniel DíazHeinrich BrasseFaustino Ticona2026-03-222026-03-22201110.1016/j.jvolgeores.2011.12.007https://doi.org/10.1016/j.jvolgeores.2011.12.007https://andeanlibrary.org/handle/123456789/44880Citaciones: 40enGeologyMagnetotelluricsVolcanoStratovolcanoSeismologyCrustHypocenterInversion (geology)SubductionGeomorphologyConductivity distribution beneath Lascar volcano (Northern Chile) and the Puna, inferred from magnetotelluric dataarticle