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preliminary studies on two kinds of aeolian dust accumulation in South China show thatthere are abrupt changes of magnetic susceptibility between the upper and lower parts of thetypical profiles. This stratigraphic boundary may indict change in East Asian monsoon circulationpattern, which is induced by the significant uplift of the Tibetan Plateau in 0.15 myr or so.
preliminary studies on two kinds of aeolian dust accumulation in South China show that are abrupt changes of magnetic susceptibility between the upper and lower parts of thetypical profiles. This stratigraphic boundary may indict change in East Asian monsoon circulationpattern, which is induced by the significant uplift of the Tibetan Plateau in 0.15 myr or so.