Fluvial-aeolian interactions in northern China (Upper Yellow River): Implications for provenance and paleoenvironmental interpretations
CATENA(2023)
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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