, Cette thèse analyse les effets de l'héritage d'un épisode tectonique sur la mise en place et l'évolution d'un bassin d'avant-pays, afin d'apporter des réponses aux questions suivantes : (1) Quel est le comportement flexural d'un rétro-bassin d'avant-pays qui se développe sur une marge hyperamincie ? (2) Comment les différentes sources de subsidence évoluent
, cette thèse s'est focalisée sur le Bassin Aquitain, qui est le rétro-bassin d'avant-pays pyrénéen qui s'est développé sur la plaque européenne du Campanien au Miocène. Celui-ci s'est initié alors que la lithosphère européenne n'avait pas retrouvé son état d'équilibre après un rift qui a duré de l'Aptien au Cénomanien. La démarche entreprise a été la suivante : une approche multi-échelle a été utilisée afin de caractériser les différents facteurs majeurs pouvant jouer un rôle dans l'évolution du bassin. Ceci a consisté en une combinaison de modélisation 3D, de modélisation flexurale, d'acquisition de données de terrain et de construction et restauration d, Quels sont les mécanismes d'inversion d'une marge hyper-amincie ? Pour répondre à ces problématiques
Ces résultats montrent que les structures du rift aptien-cénomanien sont préservées dans le rétro-bassin et que cet épisode a fortement influencé l'évolution du Bassin Aquitain, en créant une segmentation crustale qui a pour conséquence une variation est-ouest de l'amincissement de la croûte, qui augmente vers l'ouest. Cet héritage a influencé le comportement du bassin d'avant-pays : (1) en générant une subsidence thermique post-rift partiellement synchrone de la convergence pyrénéenne, Chapitre 4) a porté sur l'analyse de la flexure du Bassin Aquitain, grâce à une modélisation de la flexure et l'identification des différentes charges ,
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