The seismic signature of the Moho from which geologic and tectonic evolution hypotheses
are derived is to a large degree a result of the seismic methodology which has been used to …

The crustal structure and topography of the Moho boundary beneath the Atlas Mountains of
Morocco has been constrained by a controlled source, wide‐angle seismic reflection …

The crustal structure in Western Iberia, is the result of a complex geodynamic history. Most of
the surface is covered by rocks dating to the Variscan orogeny, the coastal ranges …

A crustal geotraverse through the Iberian Variscides is presented by integrating the
available geological and seismic profiling data. Different modes of orogenic shortening are …

This chapter summarizes the classical and recent ideas together with the geodynamic
hypotheses regarding the Variscan Cycle in Iberia, as an introduction to the more extensive …

Two wide‐angle seismic transects have been acquired across the SW Iberian Massif. They
crossed three major geological zones (South Portuguese Zone, Ossa‐Morena Zone, and …

Volcanoes represent one of the most critical geological settings for hazard modelling due to
their propensity to both unpredictably erupt and collapse, even in times of quiescence …

The Spanish Central System is an intraplate mountain range that divides the Iberian Inner
Plateau in two sectors–the northern Duero Basin and the Tajo Basin to the south. The …

The Iberian Central System, formed after the Alpine reactivation of the Variscan Iberian
Massif, features maximum altitudes of 2500 m. It is surrounded by two foreland basins with …

A multidisciplinary geophysical study along a large seismic transect in the SW-Iberian
Peninsula has been carried out. This study integrates the crustal structure, geometry and …