Abstract The European Variscan belt is a unique orogen that is covered by comprehensive
sets of seismic and potential field data from the Iberian Peninsula in the west to the Polish …

This paper provides a synthesis of current data and interpretations on the crustal structure of
the Pyrenean-Cantabrian orogenic belt, and presents new tectonic models for …

The Pyrenean Mountains represent the westernmost end of the long Alpine-Himalayan
collisional system. The excellent preservation of foreland basin deposits in conjunction with …

The Variscan metamorphic evolution of the autochthonous domain of NW and Central Iberia
is characterized by a Barrovian gradient followed by a high-temperature–low-pressure …

Seismic interpretation of the MARCONI deep seismic survey enables recognition of the
upper crustal structure of the eastern part of the Bay of Biscay and the main features of its …

The complex tectonic interaction processes between the European and African plates at the
Western Mediterranean have left marked imprints in the crustal architecture of this area …

Cretaceous rocks crop out extensively in the three main Alpine orogenic belts of Spain: the
Betic Cordillera, the Pyrenees and the Iberian Ranges. These rocks, deformed during …

The study of fluvial network rearrangement provides a key to understand past and future
landscape evolution. Large perturbations of hydrographic basins such as the change from …

The North Iberian or Cantabrian margin, located at the southern flank of the Bay of Biscay,
underwent successive tectonic regimes of rifting, passive margin, and compression from …

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 …