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Late Pleistocene evolution of the Rhine-Meuse system in the southern North Sea basin: imprints of climate change, sea-level oscillation and glacio-isostacy
handle: 1871/29827
High-resolution continuous core material, geophysical measurements, and hundreds of archived core descriptions enabled to identify 13 Late Pleistocene Rhine-Meuse sedimentary units in the infill of the southern part of the North Sea basin (the Netherlands, northwestern Europe). This sediment record and a large set of Optical Stimulated Luminescence dates,
- Utrecht University Netherlands
- Geological Survey of the Netherlands Netherlands
- Netherlands Organisation for Applied Scientific Research Netherlands
- Vrije Universiteit Amsterdam Netherlands
- Delft University of Technology Netherlands
glacioeustacy, Luminescence, Climate control, cooling, paleogeography, periglacial environment, SDG 13 - Climate Action, SDG 14 - Life Below Water, Atlantic Ocean, Glacio isostacy, Sea level oscillation, basin evolution, subsidence, Climatology, Holocene, Last Glacial, Southern North Sea basins, drainage basin, coastal sediment, Pleistocene evolution, Geophysics, climate change, Saalian, uplift, late glacial, luminescence dating, Catchments, biomarker, biostratigraphy, North Sea, avulsion, sedimentation, Sedimentation, bedload, Biomarkers, aggradation
glacioeustacy, Luminescence, Climate control, cooling, paleogeography, periglacial environment, SDG 13 - Climate Action, SDG 14 - Life Below Water, Atlantic Ocean, Glacio isostacy, Sea level oscillation, basin evolution, subsidence, Climatology, Holocene, Last Glacial, Southern North Sea basins, drainage basin, coastal sediment, Pleistocene evolution, Geophysics, climate change, Saalian, uplift, late glacial, luminescence dating, Catchments, biomarker, biostratigraphy, North Sea, avulsion, sedimentation, Sedimentation, bedload, Biomarkers, aggradation
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