Articles | Volume 52
Adv. Geosci., 52, 75–85, 2020
Adv. Geosci., 52, 75–85, 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 et al.

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Cited articles

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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,, 2008. 
Short summary
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