Postorogenic planar paleosurfaces of the central Pyrenees: weathering and neotectonic records - Université Toulouse III - Paul Sabatier - Toulouse INP Accéder directement au contenu
Article Dans Une Revue Comptes Rendus Géoscience Année : 2016

Postorogenic planar paleosurfaces of the central Pyrenees: weathering and neotectonic records

Résumé

Flat high-elevation surfaces in the Pyrenees are defined by thick weathered horizons that were developed from granitic lithology. We analysed such horizons in detail within two areas: the Bordères-Louron granite and the Aston massif. They are characterized by a lower fissured zone overlain by unconsolidated saprolite. Mapping these horizons allows a 3D reconstruction of the ancient paleosurface with an elevation uncertainty of 50 m. We discuss the age of weathering by means of stratigraphy and low-temperature thermochronology. The surfaces are clearly postorogenic, postdating Eocene-Oligocene denudation. Their incision and the fact they are stepped suggest (1) an increase of the local relief and (2) recent normal faulting.
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Dates et versions

hal-01212752 , version 1 (07-10-2015)

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Bernard Monod, Vincent Regard, Julie Carcone, Robert Wyns, Frédéric Christophoul. Postorogenic planar paleosurfaces of the central Pyrenees: weathering and neotectonic records. Comptes Rendus Géoscience, 2016, 348 (3-4), pp.184-193. ⟨10.1016/j.crte.2015.09.005⟩. ⟨hal-01212752⟩
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