The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …

The Vrancea region of the south-eastern Carpathians is a remarkable site of intra-
continental intermediate-depth seismicity. A large set of geological, geophysical, and …

A correlation of tectonic units of the Alpine-Carpathian-Dinaridic system of orogens,
including the substrate of the Pannonian and Transylvanian basins, is presented in the form …

The architecture of sedimentary basins reflects the relationship between accommodation
space and sediment supply, their rates and localization being variable during basin …

The large number and distribution of rollback systems in Mediterranean orogens infer the
possibility of interacting extensional back‐arc deformation driven by different slabs. The …

The World Stress Map Project compiles a global database of contemporary tectonic stress
information of the Earth's crust. Early releases of the World Stress Map Project demonstrated …

This paper aims at summarizing the current extent and architecture of the former Mesozoic
passive margin of North Africa from North Algeria in the west up to the Ionian‐Calabrian arc …

We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30°
N–55° N, 5° W–40° E), extending in depth up to 700 km and constrained by inversion of data …

The idea that prominent geological phenomena observed in the crust and at the surface may
be caused by the detachment of subducting dense lithosphere has been anticipated by …

Mediterranean tectonics since the Lower Cretaceous has been characterized by a
multiphase subduction and collision history with temporally and spatially variable, small …