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<dc:title xml:lang="fr">Unravelling the impact of inheritance on the Wilson cycle : a combined mapping and numerical modelling approach applied to the North Atlantic rift system</dc:title>
<dcterms:alternative xml:lang="en">Impact de l'héritage sur le Cycle de Wilson : approche cartographique et modélisation numérique appliquées à l'étude du système de rift de l'Atlantique Nord</dcterms:alternative>
<dc:subject xml:lang="fr">Cycle de Wilson</dc:subject>
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<dc:subject xml:lang="fr">Système de rift hyper-étendu</dc:subject>
<dc:subject xml:lang="fr">Atlantique Nord</dc:subject>
<dc:subject xml:lang="fr">Orogenèses calédonienne et varisque</dc:subject>
<dc:subject xml:lang="en">Wilson cycle</dc:subject>
<dc:subject xml:lang="en">Inheritance</dc:subject>
<dc:subject xml:lang="en">Hyperextended rift system</dc:subject>
<dc:subject xml:lang="en">North Atlantic</dc:subject>
<dc:subject xml:lang="en">Caledonian and Variscan orogens</dc:subject>
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<dcterms:abstract xml:lang="fr">Cette thèse analyse l’impact de l’héritage sur le Cycle de Wilson de l'Atlantique Nord via (1) la cartographie des structures orogéniques, et de l’architecture et l'évolution temporelle des rifts ; (2) une synthèse de l'architecture des systèmes de rift hyper-étendus ; (3) la modélisation numérique de l'effet d'un sous-plaquage magmatique sur un épisode de rift subséquent. Conclusions : (1) Les caractéristiques du rift Nord Atlantique diffèrent significativement entre les lithosphères Calédonienne et Varisque; (2) Deux types extrêmes de systèmes de rift : (a) étroits et immatures, dont la fermeture mène à une orogenèse contrôlée par des processus mécaniques ; et (b) larges et matures, dont les orogenèses sont affectées par des processus magmatiques; (3) Le sous-plaquage mafique de la croûte continentale et/ou l'existence de manteau appauvri à l'aplomb d'une ancienne zone orogénique peut empêcher la réactivation des faiblesses héritées et entraîner le boudinage de la croûte continentale.</dcterms:abstract>
<dcterms:abstract xml:lang="en">In this thesis, I analyse the impact of inheritance on the Wilson Cycle in the North Atlantic: (1) I map the main orogenic structures, the first-order architecture of rift systems and the timing of major rifting events; (2) I synthesise the first-order architecture of rift systems; (3) I study, via numerical modelling, the impact of underplating on subsequent rifting. Conclusions: (1) The characteristics of the North Atlantic rift system vary significantly depending on whether it affects the Caledonian or Variscan orogenic lithosphere; (2) Two end-members for rift systems can be defined : (a) narrow and immature, whose closure results in orogenesis essentially controlled by mechanical processes; (b) wide and mature, whose closure and subsequent orogenesis is largely affected by magmatic processes; (3) Mafic underplating and/or mantle depletion beneath a former orogenic area may prevent the reactivation of the inherited weaknesses and may trigger the boudinage of the continental crust.</dcterms:abstract>
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