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<dc:title xml:lang="fr">Signatures morphosédimentaires de la dynamique juxta-glaciaire à la transition de fronts glaciaires marins à terrestres : le cas de la Côte-Nord du Québec (estuaire et golfe du St Laurent)</dc:title>
<dcterms:alternative xml:lang="en">Morphostratigraphic signatures of margino-glacial dynamics at the transition from marine to continental ice-fronts : case studies along the Québec-North-Shore (St Lawrence estuary and gulf)</dcterms:alternative>
<dc:subject xml:lang="fr">Inlandsis Laurentidien</dc:subject>
<dc:subject xml:lang="fr">Délaciation</dc:subject>
<dc:subject xml:lang="fr">Transition marine à continentale</dc:subject>
<dc:subject xml:lang="fr">Géomorphologie</dc:subject>
<dc:subject xml:lang="fr">Sédimentologie</dc:subject>
<dc:subject xml:lang="fr">LiDAR</dc:subject>
<dc:subject xml:lang="fr">Photogrammétrie</dc:subject>
<dc:subject xml:lang="fr">Datations C14</dc:subject>
<dc:subject xml:lang="fr">Côte-Nord du Saint-Laurent</dc:subject>
<dc:subject xml:lang="fr">Québec</dc:subject>
<dc:subject xml:lang="en">Laurentide Ice Sheet</dc:subject>
<dc:subject xml:lang="en">Deglaciation</dc:subject>
<dc:subject xml:lang="en">Marine to continental transition</dc:subject>
<dc:subject xml:lang="en">Geomorphology</dc:subject>
<dc:subject xml:lang="en">Sedimentology</dc:subject>
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<dc:subject xml:lang="en">Photogrammetry</dc:subject>
<dc:subject xml:lang="en">C14 dating</dc:subject>
<dc:subject xml:lang="en">North Shore of the St. Lawrence</dc:subject>
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<tef:elementdEntree autoriteExterne="027330575" autoriteSource="Sudoc">Photogrammétrie</tef:elementdEntree>
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<tef:elementdEntree autoriteExterne="027569225" autoriteSource="Sudoc">Datation -- Méthode du carbone 14</tef:elementdEntree>
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<tef:elementdEntree autoriteExterne="034875328" autoriteSource="Sudoc">Côte-Nord (Canada)</tef:elementdEntree>
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<dcterms:abstract xml:lang="fr">Cette thèse combine une double approche géomorphologique et sédimentologique associée à l’utilisation de données LiDAR, bathymétriques, photogrammétrie drone et de datations radiocarbones. Elle a permis de reconstituer les paléos dynamiques glaciaires en contexte de déglaciation pour l’Inlandsis Laurentidien depuis le dernier maximum glaciaire, il y a environ 20 000 ans, et plus précisément au passage d’une marge glaciaire ancrée en mer à une marge glaciaire continentale Deux études ont été menées conjointement, soit : (1) la cartographie, la synthèse et la proposition d’un modèle concernant les mégacannelures de la Côte-Nord du Saint-Laurent, une première pour ces morphologies et (2) la reconstruction de l’enregistrement géomorphologique et morphosédimentaire du complexe sédimentaire de Pentecôte, mimant précisément cette transition. D’une manière générale, cette thèse démontre l’importance de l’héritage structural et de la physiographie du plancher au marge glaciaire dans la reconstruction de la dynamique glaciaire de retrait de la marge du LIS oriental.</dcterms:abstract>
<dcterms:abstract xml:lang="en">This thesis combines a dual geomorphological and sedimentological approach with the use of LiDAR data, bathymetry, drone photogrammetry and radiocarbon dating. It has enabled us to reconstruct the glacial paleodynamics in a deglaciation context for the Laurentide ice sheet since the last glacial maximum, around 20,000 years ago, and more specifically during the transition from an ice margin anchored at sea to a continental ice margin: (1) mapping, synthesising and proposing a model for the megagrooves of the North Shore of the St Lawrence, a first study for these morphologies, and (2) reconstructing the geomorphological and morphosedimentary record of the Pentecôte sedimentary complex, which precisely represents this transition. Overall, this thesis demonstrates the importance of the structural heritage and physiography of the floor at the glacial margin in the reconstruction of the glacial retreat dynamics of the eastern LIS margin.</dcterms:abstract>
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