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黄土粒度组成的古环境意义研究进展
引用本文:马万栋,孙国芳.黄土粒度组成的古环境意义研究进展[J].河南气象,2007(1).
作者姓名:马万栋  孙国芳
作者单位:河南大学资源与环境研究所 河南开封475004
基金项目:河南大学科研基金项目(05YBZR006)
摘    要:中国黄土高原的黄土与古土壤序列完好地记录了250万年以来的全球气候变化情况,被认为是反映第四纪古气候和古环境的重要载体。阐述了黄土粒度研究现状与进展,黄土的粒度组成、磁化率、粒度分形等及其所反映的古环境意义。

关 键 词:黄土粒度  古环境  研究进展

Progress of Paleoenvironment Study on Loess Grain Size
MA Wan-dong,SUN Guo-fang.Progress of Paleoenvironment Study on Loess Grain Size[J].Meteorology Journal of Henan,2007(1).
Authors:MA Wan-dong  SUN Guo-fang
Abstract:The global climatic variations during the past 2.5 million years were perfectly recorded by the sequence of loess paleosoil developed loess plateau in China.Chinese loess is regarded as one of the best archives of climate and environment changes during the Quaternary.The current state and progress of loess grain size were expounded.The paper summarized the grain size,magnetic susceptibility and so on,further investigated the loess deposit and its record of climate and environmental changes.
Keywords:Loess grain size  Paleoenvironment  Research progress
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