Potential fields study of Marsili basin and Palinuro volcanic complex
Muccini, Filippo <1978>
Subject
GEO/11 Geofisica applicata
Description
In this thesis Marsili back-arc basin and Palinuro Volcanic Complex (Southern
Tyrrhenian Sea) have been investigated by using magnetic, bathymetric and
gravimetric data. A new velocity model of opening of the Marsili basin has
been proposed, highlighting the transition from the horizontal spreading of the
back-arc to the vertical accretion of the Marsili seamount. Introducing gravity
data, Marsili's internal structure has been modeled and a huge portion of the
volcano with low density and vanishing magnetization has been detected.
Forward modeling of Palinuro Volcanic Complex showed as Palinuro
represents the shallowest evidence of a deep tectonic discontinuity and the
possible transition domain between the oceanic crust of Marsili Basin and the
continental crust related to the Appenninic chain.
Muccini, Filippo (2011) Potential fields study of Marsili basin and Palinuro volcanic complex, [Dissertation thesis], Alma Mater Studiorum Università di Bologna. Dottorato di ricerca in Scienze della terra , 23 Ciclo.