A horizontal crack in a layered structure satisfies deformation for the 2004-2006 uplift of Campi Flegrei
Sources responsible for volcanic unrest produce characteristic surface deformation. Given a sufficient number of distributed observation points, inversion is the preferred procedure for retrieving the source parameters of location and volume or pressure change. Most often the solutions have been for point sources embedded in a homogeneous half
Amoruso, A. et al.
Fecha de publicación:
11
2007