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Unipolar pre-seismic magnetic field pulses have been observed first by Bleieret al. (2009) and Villante et al. (2010) and Nenovski et al. (2013). In thepresent study a detailed analysis of the pulses is conducted looking forsignatures of transient signals similar to that recorded at the 2009 Aquilaearthquake main shock (Nenovski, 2015). Various magnetic field data around theAquila earthquake provide an instrumental basis for such an analysis. Inaddition to fluxgate magnetometer data (already examined in previous studies),overhauser magnetometer data are involved. The result is a detection anddiscrimination of transient signals of diffusive form that appear prior to theearthquake main shock.

Unipolar magnetic field pulses as transient signals prior to the 2009 Aquila earthquake shock