During the Paleogene and Neogene the NE Iberian plate underwent significant paleogeographic changes driven by the Iberian and European plate collision and the resulting formation of the Pyrenean orogen and its corresponding foreland basin. Shortening resulted in the advance of the orogenic wedge, emplacement of allochthonous units, and progressive basin partitioning. Sediment transfer systems reacted to the evolving paleogeographic scenario, shifting from forebulge to foredeep and wedge-top settings. Critical reorganizations included successive shifts from open to close drainage conditions, which had an strong impact on accommodation, and the stratigraphic architecture of the basin infill, overfill and later erosion. The aim of this w...
International audienceThe relationship between tectonics and sedimentary fill has been studied in tw...
This project has focused on the Early and Middle Eocene sediments of the Pamplona Basin, an area whi...
A basin analysis of the Eocene South-Eastern Pyrenean Foreland Basin shows a backstepped geometry of...
Foreland systems are regions where the complex interplay between deep and surface processes causes t...
International audienceThe southern foreland (proforeland) of the pyrenean orogeny is one of the most...
International audienceThe North Pyrenean retroforeland (Aquitaine basin) display a quite different t...
This chapter deals with the two Alpine Foreland Basins of the Iberian Peninsula. The first part of t...
The geometry and the infill of the south Pyrenean foreland basin mainly depend on the tectonic subsi...
International audienceThe southern foreland (proforeland) of the Pyrenean orogeny is one of the most...
International audienceThe Aquitaine basin located in south western Europe, is a Pyrenean retro-forel...
International audienceThe Aquitaine basin is the retro-foreland basin associated with the Pyrenean o...
International audienceThe Aquitaine basin located in south western Europe, is a Pyrenean retro-forel...
Late Paleocene to Middle Eocene strata in the easternmost part of the Southern Pyrenees, up to 4 km ...
The Paleogene Alicante Trough of the South-Iberian Margin (External Betic Zone) consists of a narrow...
International audienceThe relationship between tectonics and sedimentary fill has been studied in tw...
This project has focused on the Early and Middle Eocene sediments of the Pamplona Basin, an area whi...
A basin analysis of the Eocene South-Eastern Pyrenean Foreland Basin shows a backstepped geometry of...
Foreland systems are regions where the complex interplay between deep and surface processes causes t...
International audienceThe southern foreland (proforeland) of the pyrenean orogeny is one of the most...
International audienceThe North Pyrenean retroforeland (Aquitaine basin) display a quite different t...
This chapter deals with the two Alpine Foreland Basins of the Iberian Peninsula. The first part of t...
The geometry and the infill of the south Pyrenean foreland basin mainly depend on the tectonic subsi...
International audienceThe southern foreland (proforeland) of the Pyrenean orogeny is one of the most...
International audienceThe Aquitaine basin located in south western Europe, is a Pyrenean retro-forel...
International audienceThe Aquitaine basin is the retro-foreland basin associated with the Pyrenean o...
International audienceThe Aquitaine basin located in south western Europe, is a Pyrenean retro-forel...
Late Paleocene to Middle Eocene strata in the easternmost part of the Southern Pyrenees, up to 4 km ...
The Paleogene Alicante Trough of the South-Iberian Margin (External Betic Zone) consists of a narrow...
International audienceThe relationship between tectonics and sedimentary fill has been studied in tw...
This project has focused on the Early and Middle Eocene sediments of the Pamplona Basin, an area whi...
A basin analysis of the Eocene South-Eastern Pyrenean Foreland Basin shows a backstepped geometry of...