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Locating and quantifying the seismic discontinuities in a complex medium through the migration and AVA analysis of reflected and converted waves: an application to the Mt Vesuvius volcano
No full textP-wave arrival time inversion by using the tau-p method: Application to the Mt Vesuvius volcano, southern Italy
No full textIn this paper we have applied a tau - p inversion method based on a non linear approach to a set of first P-arrival times from a 2-D active seismic experiment performed at Mt. Vesuvius in 1994. The initial seismic investigation is devoted to the study of the shallow structure and the tau - p method has been used for modelling velocity variations of a spherically concentric medium which is a better approximation than a flat layer of the Vesuvius geometry. We are able to obtain detailed 1-D velocity models along different specified sections of the recorded seismic line. These sections span different depth ranges and indicate strong lateral and vertical P-velocity variations in the first 1 km of the volcano structure with values ranging from about 1.5 km/s at the surface to 3.5-4.0 km/s at depth. The average 1-D concentric model obtained in this study call be used as a reasonable starting model for iterative high-resolution tomographies of Vesuvius velocity structures
Precise, absolute earthquake location under Somma-Vesuvius volcano using a new 3D velocity model
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Precise, absolute earthquake location under Somma-Vesuvius volcano using a new 3D velocity model
No full text
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