Fluvial-aeolian interactions in northern China (Upper Yellow River): Implications for provenance and paleoenvironmental interpretations

CATENA(2023)

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Abstract
•Aeolian sand deposited in riverbed rather than floodplain sedimentary environment.•Low weathering intensity during the late Holocene between 3.3 and 1.0 ka.•Rapid aeolian sand accumulation after climate-driven hydrological events.
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Key words
upper yellow river,northern china,provenance,fluvial-aeolian
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