The Pyrenees is a collisional orogen built by inversion of an immature rift system during
convergence of the Iberian and European plates from Late Cretaceous to late Cenozoic. The …

This work aims to present the Les Avellanes diapir as a field analog to inquire how the
origin, advance, and emplacement of an allochthonous salt body in continental settings …

The present-day tectonic setting of the Western Mediterranean region, from the Pyrénées to
the Betics and from the Alps to the Atlas, results from a complex 3-D geodynamic evolution …

This contribution describes the influence of diapirism and compressional tectonics in the
sedimentary record of the Estopanyà and Boix synclines (salt-walled basins) in the South …

ABSTRACT A detailed geological map of the Les Avellanes salt Diapir (South-Central
Pyrenees, Spain) that includes both the diapir body and adjacent areas is presented to …

How to constrain the onset of continental subduction and prograde metamorphism in an
orogen remains a fundamental question. The widespread Triassic ultrahigh‐pressure (UHP) …

Rock slope failure (RSF) is now widely recognised as a significant contributor to the
denudation of mountain ranges. Its spatial incidence can consequently be a valuable …

The interplays between deep geodynamic processes and Earth-surface erosion processes
control the elevation and distribution of land masses, which in turn control environmental …

Abstract The Upper Garonne Basin included the longest glacier in the Pyrenees during the
Late Pleistocene. During major glacial advances, the Garonne palaeoglacier flowed …

Ambient seismic noise acquired in the Cerdanya Basin (eastern Pyrenees) is used to assess
the capability of different methodologies to map the geometry of a small-scale sedimentary …