We study the upper mantle P wave velocity structure below the Euro‐Mediterranean area,
down to 1000 km depth, by seismic travel time tomography. We invert summary residuals …

Post-collisional magmatism in the southern Iberian and northwestern African continental
margins contains important clues for the understanding of a possible causal connection …

Seismic data represent one of the most valuable resources for investigating the internal
structure and composition of the earth. One of the first people to deduce earth structure from …

Three cross sections of the Moroccan High Atlas illustrate the structural geometry and
relationship between tectonic shortening and topography in this Cenozoic intracontinental …

The study of the Gulf of Cadiz on the basis of multichannel seismic profiles and wells
illustrates the stratigraphy and tectonics. The evolution of the southern Iberian margins was …

Abstract The High Atlas intracontinental belt is an inverted rift formed along the Northwest
African Craton, between the Central Atlantic Ocean and the Africa-Eurasia plates' …

A number of different geodynamic models have been proposed to explain the extension that
occurred during the Miocene in the Alboran Sea region of the western Mediterranean …

A new model, partially based on the three most widely cited previous hypotheses, is
proposed to explain the genesis of the Canary Islands. From the hotspot hypothesis it retains …

We investigate the respective roles of crustal tectonic shortening and asthenospheric
processes on the topography of the High Atlas and surrounding areas (Morocco). The …

The Society makes every effort to ensure that the scientific and production quality of its
books matches that of its journals. Since 1997, all book proposals have been refereed by …