P-wave velocity and density structure beneath Mt. Vesuvius: a magma body in the upper edifice?

<p>A high-resolution image of the compressional wave velocity and density structure in the shallow edifice of Mount Vesuvius has been derived from simultaneous inversion of travel times and hypocentral parameters of local earthquakes and from gravity inversion. The robustness of the tomography...

Full description

Bibliographic Details
Main Authors: Paolo Capuano, Guido Russo, Roberto Scarpa
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2013-11-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/6443