Plate kinematic reconstructions available for the Late Jurassic-Early Cretaceous eastward
drift and counterclockwise rotation of the Iberian plate imply a major left-lateral motion of …

Trapping and binding of allochthonous grains by benthic microbial communities has been
considered a fundamental process of microbialite accretion since its discovery in popular …

Abstract The Bay of Biscay and the Pyrenees correspond to a Lower Cretaceous rift system
including both oceanic and hyperextended rift domains. The transition from preserved …

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 evolution of the Pyrenees, a mountain range between Iberia and Eurasia, has remained
the subject of many debates between geologists and geophysicists for a long time. By …

Three‐dimensional modeling that integrates fluvial sediment transport, crustal‐scale tectonic
deformation, and lithospheric flexural subsidence is carried out to simulate the landscape …

We focus on the Iberian-European plate boundary (IEPB), whose nature, age, and evolution
are strongly debated. In contrast to previous interpretations of the IEPB as a major …

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 …

Abstract The West European collisional Alpine belts are the result of the inversion, initiated
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …

Abstract During the Late Jurassic and Early Cretaceous, Iberia experienced extensional and
transtensional stresses leading to a complex rifting time interval. Africa–America–Europe …