EOLIAN ORIGIN OF THE RED CLAY DEPOSITS IN THE LOESS PLATEAU AND IMPLICATIONS FOR PLIOCENE CLIMATIC CHANGES
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摘要: 本文通过对黄土高原第三纪红粘土的野外观察,以及沉积学和地球化学分析,得到能证明红粘土为风成沉积的新证据。另外,佳县红粘土沉积的土壤学特征表明,上新世时期的东亚夏季风强度总体强于第四纪。Abstract: In the Loess Plateau,most of the complete loess soil sequences are directly underlain by a set of reddish clay silt deposits named informally as the Red Clay formation.The contact between loess and the Red Clay has been paleomagnetically dated in several sections to be about 2 6 Ma B.P.(around the Matsuyama/Gauss reversal). Recently we have made careful field observations on several Red Clay sections in different parts of the Loess Platear,and analyzed 1 800 particle size and 30 geochemical samples taken from the Jiaxian section situated in the northern part of the Plateeau.Field and laboratory studies show the following interesting features
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Key words:
- Red Clay /
- East Asia summer monsoon /
- aridification
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