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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 …
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 …
Crustal-scale balanced cross-section and restorations of the Central Pyrenean belt (Nestes-Cinca transect): Highlighting the structural control of Variscan belt and …
In this paper, we combined new field geological, structural, paleo-temperature and
subsurface data together with deep geophysical data to build a new 210 km-long crustal …
subsurface data together with deep geophysical data to build a new 210 km-long crustal …
Permian-Triassic rifting stage
Abstract The Permian-Triassic rifting represents the first of the two Mesozoic rifting stages
recorded in the Iberian Peninsula. Its first phases of development started during the Early …
recorded in the Iberian Peninsula. Its first phases of development started during the Early …
Role of rift-inheritance and segmentation for orogenic evolution: example from the Pyrenean-Cantabrian system
The Basque-Cantabrian junction corresponds to an inverted rift accommodation zone at the
limit between the former hyperextended Pyrenean and Cantabrian rift segments. The …
limit between the former hyperextended Pyrenean and Cantabrian rift segments. The …
Deformable plate tectonic models of the southern North Atlantic
Significant, poly-phase deformation occurred prior to, simultaneous with, and after the
opening of the North Atlantic Ocean. Understanding this deformation history is essential for …
opening of the North Atlantic Ocean. Understanding this deformation history is essential for …
Middle Jurassic–Early Cretaceous tectono-sedimentary evolution of the southwestern Iberian Basin (central Spain): Major palaeogeographical changes in the …
Abstract The Middle Jurassic-Early Cretaceous tectono-sedimentary evolution of the
southwestern part of the intraplate Iberian Basin (Spain) was mostly controlled by the Alto …
southwestern part of the intraplate Iberian Basin (Spain) was mostly controlled by the Alto …
New lithostratigraphy for the Cantabrian Mountains: A common tectono-stratigraphic evolution for the onset of the Alpine cycle in the W Pyrenean realm, N Spain
Abstract The Pyrenean-Cantabrian Orogen arose through the collision of the Iberian and
Eurasian plates, mostly in Cenozoic times. This orogen comprises two main mountain …
Eurasian plates, mostly in Cenozoic times. This orogen comprises two main mountain …
[HTML][HTML] Late Triassic to present-day tectono-thermal history of the coastal part of the Asturian basin: Implications for hydrocarbon exploration and for the North-Iberian …
Abstract The Asturian Basin, situated on the North Iberian margin, is a Permian-Mesozoic
extensional basin developed over a Variscan Palaeozoic basement, subsequently inverted …
extensional basin developed over a Variscan Palaeozoic basement, subsequently inverted …
Role of inheritance during tectonic inversion of a rift system in basement-involved to salt-decoupled transition: analogue modelling and application to the Pyrenean …
The reactivation of former rift systems and passive margins during tectonic inversion and
their incorporation into fold-and-thrust belts result in significant structural differences not only …
their incorporation into fold-and-thrust belts result in significant structural differences not only …