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Geochemical and Sr–Nd–Pb isotopic compositions of the detrital sediments from ODP Hole 1202B and Taiwan rivers were measured in this study, aiming to reveal changes in sediment provenance in the southern Okinawa Trough (SOT) since 28ka, and to examine the weathering and sediment transport processes in response to monsoon climate variability. Large variations in Sr–Nd–Pb isotopic ratios at 11–9ka suggest...
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