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Authors: Iannaccone, G.* 
Vassallo, M.* 
Elia, L.* 
Guardato, S.* 
Stabile, T. A.* 
Satriano, C.* 
Beranzoli, L.* 
Title: Long-term seafloor experiment with the CUMAS module: performance, noise analysis of geophysical signals, and hints towards the design of a permanent network
Issue Date: 2010
Series/Report no.: 6/81 (2010)
Keywords: Campi Flegrei
volcanic activity
seafloor monitoring
Subject Classification04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous 
04. Solid Earth::04.06. Seismology::04.06.10. Instruments and techniques 
04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous 
04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques 
Abstract: The Campi Flegrei caldera (southern Italy) is one of the most hazardous areas in the World as several hundred thousand people live there and where important socio-economic activities have developed. The caldera includes the western-most part of the city of Naples and extends into the Gulf of Pozzuoli (eastern Tyrrhenian basin; Fig. 1). The main feature of the present volcanic activity of the caldera is the episodic slow and high-amplitude soil movement (bradyseism) accompanied by intense and shallow seismic activity that only occurs during the uplift phase.
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