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Holocene relative sea-level change, isostatic subsidence and the radial viscosity structure of the mantle of northwest Europe (Belgium, the Netherlands, Germany, southern North Sea)

GeophysicsRadial Viscosity StructureMarine GeologyPlate TectonicsEngineeringMantle DynamicGeologyLithosphereGeochronologyIsostatic SubsidenceSea-level HistoryEarth ScienceNorthwest EuropeMantle GeochemistryTectonics