Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8553
AuthorsDel Pezzo, E.* 
Bianco, F.* 
Castellano, M.* 
Cusano, P.* 
Galluzzo, D.* 
La Rocca, M.* 
Petrosino, S.* 
TitleDetection of Seismic Signals from Background Noise in the Area of Campi Flegrei: Limits of the Present Seismic Monitoring
Issue DateMar-2013
Series/Report no./84 (2013)
DOI10.1785/0220120062
URIhttp://hdl.handle.net/2122/8553
Keywordsseismic noise
magnitude detection
Subject Classification04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoring 
04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology 
04. Solid Earth::04.06. Seismology::04.06.09. Waves and wave analysis 
AbstractIn the present paper, we will describe the field survey (Fig. 1) and the data analysis of an experiment carried out to put constraints on the magnitude detection threshold in the area of Campi Flegrei. Results show that seismic radiation emitted from VT seismic events at frequency lower than 2 Hz has a high detection threshold (minimum magnitude around 1.5). In the range between 2 and 20 Hz, VT events with magnitudes smaller than about 0.5 have a high probability to be undetected. This result indicates that noise reduction through borehole stations and/or small arrays is essential for an accurate seismic monitoring in the Campi Flegrei area.
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