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 kinematic evolution of the Pyrenees was largely controlled by structural and thermal
heterogeneities inherited from a precursor rift system, resulting in complex along-strike …

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

Surface and subsurface data are combined to construct a crustal‐scale cross section of the
western central Pyrenees (France and Spain) at the boundary between the European and …

Native hydrogen (H2) may represent a new carbon free‐energy resource, but to date there is
no specific exploration guide to target H2‐fertile geological settings. Here, we present the …

Résumé New evolutionary models for the Pyrenean orogeny must consider feedbacks
between the Mid-Cretaceous hyperextension postulated recently and the Pyrenean …

Imaging the architecture of mountain roots is required to understand the support of
topography and for kinematic reconstructions at convergent plate boundaries, but is still …

We exploit the data from five seismic transects deployed across the Pyrenees to characterize
the deep architecture of this collisional orogen. We map the main seismic interfaces beneath …

Recent models support the view that the Pyrenees were formed after the inversion of a
previously highly extended continental crust that included exhumed upper mantle rocks …

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 …