Articles | Volume 52
https://doi.org/10.5194/adgeo-52-75-2020
https://doi.org/10.5194/adgeo-52-75-2020
28 Oct 2020
 | 28 Oct 2020

Array and spectral ratio techniques applied to seismic noise to investigate the Campi Flegrei (Italy) subsoil structure at different scales

Lucia Nardone, Roberta Esposito, Danilo Galluzzo, Simona Petrosino, Paola Cusano, Mario La Rocca, Mauro Antonio Di Vito, and Francesca Bianco

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Cited articles

AGIP: Geologia e geofisica del sistema geotermico dei Campi Flegrea, Internal Report, 17 pp., 1987. 
Aki, K.: Space and time of stationary stochastic wave, with special reference to microtremors, Bull. Earthq. Res. Ins., XXXV, 415–457, 1957. 
Aki, K.: A note on the use of microseisms in determining the shallow structure of the Earth's crust, Geophysics, 30, 665–666, 1965. 
Battaglia, J., Zollo, A., Virieux, J., and Dello Iacono, D.: Merging active and passive data sets in traveltime tomography: The case study of Campi Flegrei caldera (Southern Italy), Geophys. Prospect., 56, 555–573, 2008. 
Bean, C., Lokmer, I., and O'Brien, G.: Influence of near-surface volcanic structure on long-period seismic signals and on moment tensor inversions: simulated examples from Mount Etna, J. Geophys. Res., 113, B08308, https://doi.org/10.1029/2007JB005468, 2008. 
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We studied the subsoil structure of the Campi Flegrei area using both spectral ratios and array techniques (f-k and MSPAC) applied to seismic noise recorded by three different array. By means of joint inversion of dispersion curve and spectral ratio we obtained a Vs model, that is in a good agreement with the stratigraphic information available in the area. In areas such as Campi Flegrei the definition of the velocity model is a crucial issue to characterize the physical parameters of the medium