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Accumulation and erosion of aeolian sediments in the northeastern Qinghai-Tibetan Plateau and implications for provenance to the Chinese Loess Plateau
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文摘
Northeastern Qinghai-Tibetan Plateau (NEQTP) suffered severe erosion during cold stages in glaciation. Fine sediments conveyed from NEQTP to Chinese Loess Plateau (CLP) mainly occurred at cold stages and by westerly wind. Material transport pattern from NEQTP to CLP is different between cold and warm stages.

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