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<dc:title xml:lang="fr">Déglaciation et dynamiques morpho-sédimentaires des systèmes juxtaglaciaires : exemple de la marge orientale de l'Inlandsis laurentidien depuis le dernier maximum glaciaire</dc:title>
<dcterms:alternative xml:lang="en">Deglaciation and morphosedimentary dynamics of ice-contact systems : example of the eastern margin of the Laurentide ice sheet since the last glacial maximum</dcterms:alternative>
<dc:subject xml:lang="fr">Inlandsis laurentidien</dc:subject>
<dc:subject xml:lang="fr">Déglaciation</dc:subject>
<dc:subject xml:lang="fr">Labrador</dc:subject>
<dc:subject xml:lang="fr">Ile de Baffin</dc:subject>
<dc:subject xml:lang="fr">Plate-forme de glace flottante</dc:subject>
<dc:subject xml:lang="fr">Système fjord-auge glaciaire</dc:subject>
<dc:subject xml:lang="fr">Datations cosmogéniques</dc:subject>
<dc:subject xml:lang="fr">Réajustement paraglaciaire</dc:subject>
<dc:subject xml:lang="en">Laurentide Ice Sheet</dc:subject>
<dc:subject xml:lang="en">Deglaciation</dc:subject>
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<dc:subject xml:lang="en">Fjord-cross-shelf through system</dc:subject>
<dc:subject xml:lang="en">Cosmogenic exposure dating</dc:subject>
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<dcterms:abstract xml:lang="fr">Cette thèse, combinant une double approche géomorphologique et sédimentologique couplée à différentes méthodes de datation, a permis de décrypter les séquences de déglaciation de la marge orientale de l’Inlandsis laurentidien depuis le Dernier maximum glaciaire, il y environ 21 000 ans. Deux systèmes présentant des caractéristiques différentes mais représentatives de leur région ont été analysés, soit : 1) le système fjord-auge glaciaire de Clyde et l’est de l’île de Baffin; et 2) la vallée de la rivière Churchill et l’est du Québec-Labrador. De manière générale, cette thèse permet de redéfinir la chronologie de déglaciation de ces deux secteurs clés et de préciser les principaux facteurs influençant le retrait de la marge glaciaire. De plus, l’ensemble des résultats présentés permet une couverture temporelle quasi intégrale de la dernière déglaciation pour la partie orientale de l’Inlandsis laurentidien, depuis sa couverture maximale et le retrait initial de la plate-forme de glace flottante au large de l’auge glaciaire de Clyde jusqu’à sa désintégration terrestre enregistrée par le système fluvio-deltaïque de la rivière Churchill à l’Holocène.</dcterms:abstract>
<dcterms:abstract xml:lang="en">His thesis, combining a dual geomorphological and sedimentological approach coupled with different dating methods, has deciphered the deglaciation sequences of the eastern margin of the Laurentide Ice Sheet since the Last Glacial Maximum, about 21,000 years ago. Two systems with different characteristics, but representative of their region, were investigated: 1) the Clyde fjord-cross-shelf trough system and eastern Baffin Island; and 2) the Churchill River valley and eastern Quebec-Labrador. Overall, this thesis allows redefining the deglaciation chronology of these two key areas and clarifies the main factors influencing the retreat of the ice margin. In addition, these results provide a near-complete temporal coverage of the last deglaciation for the eastern fringe of the Laurentide Ice Sheet, from its maximum extent and initial retreat of a floating ice shelf off Clyde Trough to its terrestrial disintegration recorded by the Churchill River fluvio-deltaic system during the Holocene.</dcterms:abstract>
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