To date, research on neotectonics and related continental topography development has
mostly focused on active plate boundaries characterized by generally high deformation …

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 …

We examine the role of lithosphere folding in the large‐scale evolution of the continental
lithosphere. Analysis of the record of recent vertical motions and the geometry of basin …

A general synthesis of the recent and present stress situation and evolution in the Iberian
Peninsula was obtained from microstructural and seismological analysis. The stress …

Integration of stress indicator data, gravity data, crustal kinematics data, and analysis of
topography and recent vertical motions demonstrates the occurrence of consistently oriented …

The Iberian microcontinent and its connected oceanic crust are affected by deformations
related to the Eurasian‐African plate boundary. Active stress inversions from populations of …

The distribution of active faults in the Iberian Peninsula is not homogeneous, being mainly
present, but not only, in areas affected by the Alpine Orogeny. They are located in several …

Abstract The Permian-Triassic rifting represents the first of the two Mesozoic rifting stages
recorded in the Iberian Peninsula. Its first phases of development started during the Early …

In the interior of the Iberian Peninsula, the main geomorphic features, mountain ranges and
basins, seems to be arranged in several directions whose origin can be related to the N–S …

The Spanish Central System is a Cenozoic pop-up with an E–W to NE–SW orientation that
affects all the crust (thick-skinned tectonics). It shows antiform geometry in the upper crust …