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The Cap-Ferret Canyon (CFC), a major morphologic feature of the eastern margin of the Bay of Biscay, occupies a deep structural depression that opens about 60km southwest of the Gironde Estuary. Detailed depth profiles of the particle-reactive radionuclides 234 Th and 210 Pb in interface sediments were used to characterise the present sedimentation (bioturbation, sediment mass accumulation,...
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