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Annals of Geophysics
Geodetic and magnetic investigations have been playing an increasingly important role in studies on Mt. Etna eruptive processes. During ascent, magma interacts with surrounding rocks and fluids, and inevitably crustal deformation and disturbances in the local magnetic field are produced. These effects are generally interpreted separately from each other and consistency of interpretations obtained from different methods is qualitatively checked only a posteriori. In order to make the estimationdoi:10.4401/ag-3082 doaj:157273aea0624f41be28e217c1f39dac fatcat:sbioamm3ljasbbprh6elll76bu