I use seismology as a tool to study the interior of the Earth, addressing geophysical issues as,
in particular, the amount of vertical downward (slabs) and upward (plumes) mass transport in a
convecting mantle.
Isolating different databases, I can
focus on specific regions of our planet's interior. I have started out looking at global body-wave
traveltimes, sensitive to the middle to lower mantle, and to the
core-mantle boundary region.
I have later moved on to teleseismic surface
waves, a powerful tool to constrain upper mantle structure and the lithosphere-asthenosphere
boundary. I am now trying to put it all together.
In the course of my studies, I have naturally become interested in the theory of seismic wave
propagation and its impact on tomographic resolution. My more theoretical works include applications
of the "banana-doughnut" theory to surface-wave tomography, with an
assessment of its resolution;
surface-wave ray-tracing in the presence of azimuthal anisotropy;
numerical modeling of surface-wave propagation in the
membrane-wave approach.
Outside of seismology, I have been interested in the
Earth's rheology and viscoelastic rebound, and
I am currently working on tomography of ionosphere electron density based on trans-horizon radar
observations.