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<dc:title xml:lang="fr">Loess, alluvions et dépôts de pente du Fossé rhénan en Alsace de l’Eemien à l’Anthropocène : approche pédosédimentaire, géomorphologie et chronostratigraphie</dc:title>
<dcterms:alternative xml:lang="en">Loess, alluvium and slope deposits of the Rhine graben in Alsace from the Eemien to the Anthropocene : pedosedimentary approach, geomorphology and chronostratigraphy</dcterms:alternative>
<dc:subject xml:lang="fr">Rhin</dc:subject>
<dc:subject xml:lang="fr">Graben</dc:subject>
<dc:subject xml:lang="fr">Loess</dc:subject>
<dc:subject xml:lang="fr">Paléosols</dc:subject>
<dc:subject xml:lang="fr">Cônes alluviaux</dc:subject>
<dc:subject xml:lang="fr">Colluvions</dc:subject>
<dc:subject xml:lang="fr">Chronostratigraphie</dc:subject>
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<dcterms:abstract xml:lang="fr">Un cadre chronostratigraphique des dépôts sédimentaires des derniers 130 000 ans a été élaboré pour la partie alsacienne du Fossé rhénan supérieur à partir d’une soixantaine de profils issus principalement de l’archéologie préventive. Il est fondé sur des analyses pédosédimentaires et micromorphologiques, accompagnées de datations numériques (radiocarbone et luminescence optiquement stimulée). Le climat et les formes du relief sont les principaux facteurs de contrôle de l’évolution du Fossé rhénan depuis 130 000 ans, jusqu’à ce que les activités anthropiques prévalent à l’Holocène récent. La part de la néotectonique demande toutefois à être réévaluée à partir de profils complémentaires visant à apprécier les épaisseurs des alluvions weichseliennes et à disposer d’une meilleure résolution spatiale.</dcterms:abstract>
<dcterms:abstract xml:lang="en">A chronostratigraphic framework of sedimentary deposits of the last 130 000 years is proposed for the Alsatian part of the Upper Rhine Graben based on about sixty profiles, most of them examined during operations of rescue archeology. It is based on pedo-sedimentary archives and micromorphological data and completed with numerical datings (radiocarbon and OSL). Climate, relief and inherited landforms have been the main factors controlling the graben’s evolution for the last 130 000 years, until the historical periods during which human earthworks have prevailed. However, the role of neotectonics must be re-evaluated on the basis of complementary profiles to assess the thickness of the Weichselian alluvium while a better spatial resolution is needed as well.</dcterms:abstract>
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