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Creators/Authors contains: "Fan, Niannian"

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  1. ; ; ; ; ; ; ; ; ; (, Geophysical Research Letters)
    Key Points Provenance changes at the outlet of the Hetao Basin indicate the desiccation and re‐integration of the upper Yellow River over the last ∼40 ka Paleo‐lake shorelines and geochemical proxies confirm that the west Hetao Basin contained the terminal lake for the desiccated Yellow River Climate‐river feedbacks across glacial‐interglacial cycles have implications for constraining terrestrial‐marine source‐to‐sink processes 
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