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Seismic‐electromagnetic signals from two monitoring stations in Southern Italy: Electromagnetic time series release

Urheber*innen

Ventola,  Ivana
External Organizations;

Balasco,  Marianna
External Organizations;

De Girolamo,  Michele
External Organizations;

Falco,  Luigi
External Organizations;

Filippucci,  Marilena
External Organizations;

/persons/resource/laura

Hillmann,  Laura
2.4 Seismology, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Romano,  Gerardo
External Organizations;

Serlenga,  Vincenzo
External Organizations;

Stabile,  Tony Alfredo
External Organizations;

/persons/resource/strollo

Strollo,  Angelo
2.4 Seismology, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Tallarico,  Andrea
External Organizations;

Tripaldi,  Simona
External Organizations;

/persons/resource/tzieke

Zieke,  Thomas
2.4 Seismology, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Siniscalchi,  Agata
External Organizations;

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Zitation

Ventola, I., Balasco, M., De Girolamo, M., Falco, L., Filippucci, M., Hillmann, L., Romano, G., Serlenga, V., Stabile, T. A., Strollo, A., Tallarico, A., Tripaldi, S., Zieke, T., Siniscalchi, A. (2024 online): Seismic‐electromagnetic signals from two monitoring stations in Southern Italy: Electromagnetic time series release. - Geoscience Data Journal.
https://doi.org/10.1002/gdj3.262


Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5027708
Zusammenfassung
The seismic-electromagnetic phenomenon entails the generation of transient electromagnetic signals, which can be observed both simultaneously (co-seismic) and preceding (pre-seismic) a seismic wave arrival. Following the most accredited hypothesis, these signals are mainly due to electrokinetic effects, generated on microscopic scale in porous media containing electrolytic fluids. Thus, the seismic-electromagnetic signals are expected to be suitable for the detection and tracking of crustal fluids. Despite the growing interest in this phenomenon, there is a lack of freely available observational database of earthquake-related electromagnetic signals recorded at co-located seismic and magnetotelluric stations. To fill this gap, we set up two multicomponent monitoring stations in two seismically active areas of Southern Italy: the Gargano Promontory and the High Agri Valley. This work is both aimed to systematically analyse earthquake-generated seismic-electromagnetic recordings and to make the collected database accessible to the scientific community.