This chapter deals with the two Alpine Foreland Basins of the Iberian Peninsula. The first part of the chapter refers to the South Pyrenean Foreland Basin and its westward prolongation, the Basque–Cantabrian Paleogene Basin. It includes: (1) the introductory concepts about the basin extend, margins, sedimentary systems, basin evolution and segmentation, and terminology; (2) the impact of PETM; (3) the stratigraphy and geometry of foreland carbonate margin with special emphasis on the recent advances in its chronology and evolution, (4) the stratigraphy and geometry of the siliciclastic basin fill reflecting the recent advances in chronology and provenance; (5) and finally, discusses on the sedimentary imprints of the orogenic evolution. The...
International audienceThe relationship between tectonics and sedimentary fill has been studied in tw...
International audienceThe Aquitaine basin located in south western Europe, is a Pyrenean retro-forel...
International audienceThe Mesozoic Aquitaine Basin (alternations through time of rifts and intracrat...
This chapter deals with the two Alpine Foreland Basins of the Iberian Peninsula. The first part of t...
During the Paleogene and Neogene the NE Iberian plate underwent significant paleogeographic changes ...
The Iberian microcontinent stands out because of its intense Alpine intraplate deformation. This is ...
Abstract: The Iberian Peninsula, at the western end of the Alpine–Himalayan Belt, displays a complex...
23 pagesInternational audienceThe Pyrenean-Cantabrian Orogen arose through the collision of the Iber...
International audienceThe Aquitaine basin is the retro-foreland basin associated with the Pyrenean o...
Foreland systems are regions where the complex interplay between deep and surface processes causes t...
The Iberian Peninsula, at the western end of the Alpine - Himalayan Belt, displays a complex structu...
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...
The geometry and the infill of the south Pyrenean foreland basin mainly depend on the tectonic subsi...
The Pyrenean-Cantabrian Orogen arose through the collision of the Iberian and Eurasian plates, mostl...
International audienceThe relationship between tectonics and sedimentary fill has been studied in tw...
International audienceThe Aquitaine basin located in south western Europe, is a Pyrenean retro-forel...
International audienceThe Mesozoic Aquitaine Basin (alternations through time of rifts and intracrat...
This chapter deals with the two Alpine Foreland Basins of the Iberian Peninsula. The first part of t...
During the Paleogene and Neogene the NE Iberian plate underwent significant paleogeographic changes ...
The Iberian microcontinent stands out because of its intense Alpine intraplate deformation. This is ...
Abstract: The Iberian Peninsula, at the western end of the Alpine–Himalayan Belt, displays a complex...
23 pagesInternational audienceThe Pyrenean-Cantabrian Orogen arose through the collision of the Iber...
International audienceThe Aquitaine basin is the retro-foreland basin associated with the Pyrenean o...
Foreland systems are regions where the complex interplay between deep and surface processes causes t...
The Iberian Peninsula, at the western end of the Alpine - Himalayan Belt, displays a complex structu...
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...
The geometry and the infill of the south Pyrenean foreland basin mainly depend on the tectonic subsi...
The Pyrenean-Cantabrian Orogen arose through the collision of the Iberian and Eurasian plates, mostl...
International audienceThe relationship between tectonics and sedimentary fill has been studied in tw...
International audienceThe Aquitaine basin located in south western Europe, is a Pyrenean retro-forel...
International audienceThe Mesozoic Aquitaine Basin (alternations through time of rifts and intracrat...