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The Mesozoic Iberia-Eurasia diffuse plate boundary: A wide domain of distributed transtensional deformation progressively focusing along the North Pyrenean Zone
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 …
drift and counterclockwise rotation of the Iberian plate imply a major left-lateral motion of …
[HTML][HTML] Salt production by ignition during the prehistory in the Iberian Peninsula with special focus on the archaeological site of Espartinas (Ciempozuelos, Spain)
One of the prehistoric techniques of salt production consisted of using ceramic vessels,
known as briquetage, for the artificial evaporation of salt water. This paper summarizes all …
known as briquetage, for the artificial evaporation of salt water. This paper summarizes all …
Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinematics of the Europe-Africa diffuse plate boundary
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 …
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …
[HTML][HTML] A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic
The western European kinematic evolution results from the opening of the western
Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological …
Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological …
Evolution of a low convergence collisional orogen: a review of Pyrenean orogenesis
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 …
convergence of the Iberian and European plates from Late Cretaceous to late Cenozoic. The …
Evolution of a salt-rich transtensional rifted margin, eastern North Pyrenees, France
M Ford, J Vergés - Journal of the Geological Society, 2021 - pubs.geoscienceworld.org
In this field study we reinterpret the narrow eastern North Pyrenean Zone, France, as an
inverted salt-rich transtensional rift system based on identification of halokinetic depositional …
inverted salt-rich transtensional rift system based on identification of halokinetic depositional …
[HTML][HTML] Eustasy in the Aptian world: A vision from the eastern margin of the Iberian Plate
Abstract Eustatic controls on Early Cretaceous (Aptian) sedimentation in the western Tethys
are discerned in outcrops of carbonate platforms that developed in the Maestrat rift basin …
are discerned in outcrops of carbonate platforms that developed in the Maestrat rift basin …
[HTML][HTML] Extension and inversion of salt-bearing rift systems
We used physical models to investigate the structural evolution of segmented extensional
rifts containing syn-rift evaporites and their subsequent inversion. An early stage of …
rifts containing syn-rift evaporites and their subsequent inversion. An early stage of …
Reconstructing the Iberian salt‐bearing rifted margin of the Southern Pyrenees: Insights from the Organyà Basin
Reinterpretation of the Organyà Basin, based on new detailed field observations and
subsurface data, emphasizes the key contribution of Upper Triassic evaporites in the tectono …
subsurface data, emphasizes the key contribution of Upper Triassic evaporites in the tectono …
Salt tectonics along the High Zagros Fault in Iran, faulting through welded salt walls
In salt-bearing foreland fold-thrust belts, precursor salt structures affect deformation and
accommodate fault zones during orogenic shortening. The complex structure and the …
accommodate fault zones during orogenic shortening. The complex structure and the …