Abstract The Neo-Tethys Ocean was an eastward-gaping triangular oceanic embayment
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …

We propose a review to discuss the large number of studies dealing with the fluid history in
extensional and compressional sedimentary basins that evolved along the Iberian-Eurasian …

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 …

Estimating shortening in collision belts is critical to reconstruct past plate motions. Balanced
cross‐section techniques are efficient in external domains but lack resolution in the …

We focus on the southern North Atlantic rifted margins to investigate the partitioning and
propagation of deformation in hyperextended rift systems using plate kinematic modeling …

The existence of geological fluids rich in natural hydrogen (H 2) raises the question about
the energy potential of this carbon-free resource. However, to date there is no exploration …

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

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 …

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 …

Structural style of fold and thrust belts depends among many other factors on the mechanical
properties of the deformed sedimentary pile and the existence of weak horizons such as salt …