The thorough interpretation of the South Atlantic long offset seismic lines provides a new
view of the magmatic and crustal architecture and of the evolution of the conjugate volcanic …

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 …

Rifted margins are the result of the successful process of thinning and breakup of the
continental lithosphere leading to the formation of new oceanic lithosphere. Observations on …

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 …

Rifted margins are commonly defined as magma-poor or magma-rich archetypes based on
their morphology. We re-examine the prevailing model inferred from this classification that …

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 …

Our understanding of continent-ocean transition structures and magmatism in the absence
of excessive magmatic additions has been guided by the observations and models …

In natural doubly vergent orogens, the relationship between the pro‐and retro‐wedges is, as
yet, poorly constrained. We present a detailed tectonostratigraphic study of the retro‐wedge …

Accurate reconstructions of the dispersal of supercontinent blocks are essential for testing
continental breakup models. Here, we provide a new plate tectonic reconstruction of the …

We summarize here observations from the South Atlantic Angola–Gabon rifted margin. Our
study was based on the interpretation of a selection of deep penetration depth-migrated …