Here, global mantle flow is computed on the basis of recent, high-resolution seismic tomography, to investigate the role of buoyancy-driven and plate-motion-induced mantle circulation in the Mediterranean region. The findings show that mantle flow explains much of the observed dynamic topography and microplate motion in the region. Small-scale convection in the uppermost mantle may also hold the key to understanding complex mobile belts elsewhere.
- Claudio Faccenna
- Thorsten W. Becker