The architecture and tectono-magmatic evolution of the lithosphere of Europe are the result
of a succession of subduction, rifting and inputs from plumes that have modified the …

The dimensions, the geographical position and the complex geological history of the Iberian
Peninsula makes it a unique and singular target to study its crustal and upper mantle …

Slab retreat, slab tearing and interactions of slabs are first-order drivers of the deformation of
the overriding lithosphere. An independent description of the tectonic evolution of the back …

The recent tectonic evolution of the western Mediterranean region is enigmatic. The causes
for the closure of the Moroccan marine gateway prior to the Messinian salinity crisis, for the …

The subsidence history of forearc and back‐arc basins reflects the relationship between
subduction kinematics, mantle dynamics, magmatism, crustal tectonics, and surface …

We compile an extensive catalog comprising geochemistry and ages of Cenozoic volcanic
provinces in the Mediterranean region, distinguishing between three groups according to …

Slab tearing induces localized deformations in the overriding plates of subduction zones
and transfer zones accommodating differential retreat in back-arc regions. Because the …

Upper-mantle upwellings are often invoked as the cause of Cenozoic volcanism in the Ibero-
western Maghreb region. However, their nature, geometry and origin are unclear. This study …

A global view of the Mesozoic-Cenozoic geodynamic evolution of the Iberian microplate is
necessary to determine the role of inherited Variscan structures in the configuration of the …

We investigate the global distribution of S-to-P scatterers in the shallow to mid-lower mantle
beneath subduction zones, where deep seismicity extends down to the bottom of the upper …