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http://hdl.handle.net/2122/6107| 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 | Journal: | Seismological Research Letter | Series/Report no.: | 6/81 (2010) | Publisher: | Seismological Society of America | Issue Date: | 2010 | Keywords: | Campi Flegrei volcanic activity seafloor monitoring |
Subject Classification: | 04. 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. |
| Appears in Collections: | Article published / in press |
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