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The document presents preliminary results from high-resolution seismic investigations along the Charente shoreline, revealing significant geological features such as an erosion truncature and active sand waves indicative of Holocene sediment remobilization. The study highlights the impact of past sea level changes and current hydrodynamic processes on sediment distribution and coastal morphology. It emphasizes the necessity for further quantification of sediment transport to better understand coastline shif

Author
moab.gomes
Language
EN

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