title: Subduction and slab detachment in the Mediterranean-Carpathian region.
abstract: Seismic tomography models of the three-dimensional upper mantle velocity structure of the Mediterranean-Carpathian region provide a better understanding of the lithospheric processes governing its geodynamical evolution. Slab detachment, in particular lateral migration of this process along the plate boundary, is a key element in the lithospheric dynamics of the region during the last 20 to 30 million years. It strongly affects arc and trench migration, and causes along-strike variations in vertical motions, stress fields, and magmatism. In a terminal-stage subduction zone, involving collision and suturing, slab detachment is the natural last stage in the gravitational settling of subducted lithosphere.
authors: Vening Meinesz Research School of Geodynamics, Faculty of Earth Sciences, Utrecht University, Budapestlaan 4, 3584CD, Utrecht, Netherlands.
authors: M J
authors: MJ
authors: Wortel
authors: W
authors: W
authors: Spakman