Stratigraphic and tectonic studies in the central Aquitaine Basin, northern Pyrenees: Constraints on the subsidence and deformation history of a retro-foreland basin

The central North-Pyrenean retrowedge developed on a thinned lithosphere, rich in Keuper evaporites. The behavior of this retro-foreland system is studied using subsidence analyses and a sequentially restored cross-section (120km, Saint-Gaudens to Castelsarrasin) constrained by new chrono- and litho...

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Veröffentlicht in:Comptes Rendus Géoscience 2016-03, Vol.348 (3-4), p.224-235
Hauptverfasser: Rougier, Géraldine, Ford, Mary, Christophoul, Frédéric, Bader, Anne-Gaëlle
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Sprache:eng
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Zusammenfassung:The central North-Pyrenean retrowedge developed on a thinned lithosphere, rich in Keuper evaporites. The behavior of this retro-foreland system is studied using subsidence analyses and a sequentially restored cross-section (120km, Saint-Gaudens to Castelsarrasin) constrained by new chrono- and lithostratigraphy, surface and subsurface data. During the Late Cretaceous, a first episode of foreland subsidence (E1) produced a narrow marine depocenter (Comminges Basin, 30km wide), supplied from the east. A synchronous early deformation involved inversion of basement faults and gentle shortening (4.5km) of the Mesozoic strata above a Keuper decoupling layer. A tectonically quiet period (Q, Paleocene), characterized by a condensed succession (marine and continental), was followed by a second episode of subsidence (E2), basin migration and gentle thick- and thin-skinned shortening (8km). Continental sedimentation, supplied by the uplifting orogen, first filled a narrow flexural basin (E2, M-L Eocene), then expanded across the Aquitaine Platform (E3, Oligocene–Miocene).
ISSN:1631-0713
1778-7025
DOI:10.1016/j.crte.2015.12.005