Shallow structure of Mt. Vesuvius volcano, Italy, from seismic array analysis
Data from a portable dense seismic array deployed on Mt. Vesuvius in May 1994, during a 2D seismic tomography experiment, are analyzed in the present paper. The array consisted of two groups of short period geophones, 4.5 hz natural frequency, formed by 16 and 25 vertical components (plus two horizontal components), distributed along an arc like
De Luca, G. et al.
Fecha de publicación:
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1997