Mangshan Loess in Central China and the Paleomonsoon Variations since the Last Interglaciation
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P642.131


Mangshan Loess in Central China and the Paleomonsoon Variationssince the Last Interglaciation
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    摘要:

    The Mangshan Yuan is a loess platform on the southern bank of the Yellow River, which is located in northwestern Zhengzhou of Henan Province, China. The typical Zhaoxiayu section of the Mangshan Yuan preserves stratigraphical loess units above S10 with a total thickness of 172.1 m, which includes 15.7 m of the last interglacial paleosol S1, 77.3 m of the last glacial loess L1 that consist of 41.6 m of the late stade L1LL1, 13.2 m of the interstade L1SS1 and 22.5 m of the early stade L1LL2. Based on the age marking points by correlating magnetic susceptibility of the section with the SPECMAP curve, the timescale of the section was constructed, and the average accumulation rate and the resolution of each loess strata over the S2 were subsequently calculated using the

    Abstract:

    The Mangshan Yuan is a loess platform on the southern bank of the Yellow River, which is located in northwestern Zhengzhou of Henan Province, China. The typical Zhaoxiayu section of the Mangshan Yuan preserves stratigraphical loess units above S10 with a total thickness of 172.1 m, which includes 15.7 m of the last interglacial paleosol S1, 77.3 m of the last glacial loess L1 that consist of 41.6 m of the late stade L1LL1, 13.2 m of the interstade L1SS1 and 22.5 m of the early stade L1LL2. Based on the age marking points by correlating magnetic susceptibility of the section with the SPECMAP curve, the timescale of the section was constructed, and the average accumulation rate and the resolution of each loess strata over the S2 were subsequently calculated using the

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JIANG Fuchu, WANG Shubing, ZHAO Zhizhong and FU Jianli Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing State Key Laboratory of Loess and Quaternary Geology, Chinese Academy of Sciences, Xi''''an, Shaanxi .2004. Mangshan Loess in Central China and the Paleomonsoon Variations since the Last Interglaciation[J]. ACTA GEOLOGICA SINICA(English edition),78(3):

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