黄土高原河谷阶地黄土地层结构模式

雷祥义. 黄土高原河谷阶地黄土地层结构模式[J]. 海洋地质与第四纪地质, 2006, 26(2): 113-122.
引用本文: 雷祥义. 黄土高原河谷阶地黄土地层结构模式[J]. 海洋地质与第四纪地质, 2006, 26(2): 113-122.
LEI Xiang-yi. MODELS OF LOESS STRATIGRAPHICAL STRUCTURE ON THE TERRACES IN THE LOESS PLATEAU OF CHINA[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 113-122.
Citation: LEI Xiang-yi. MODELS OF LOESS STRATIGRAPHICAL STRUCTURE ON THE TERRACES IN THE LOESS PLATEAU OF CHINA[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 113-122.

黄土高原河谷阶地黄土地层结构模式

  • 基金项目:

    国家自然科学基金项目(49472132)

详细信息
    作者简介: 雷祥义(1942-),男,教授,博士生导师,主要从事第四纪地质与黄土、环境地质研究
  • 中图分类号: P539

MODELS OF LOESS STRATIGRAPHICAL STRUCTURE ON THE TERRACES IN THE LOESS PLATEAU OF CHINA

  • 流经黄土高原的黄河及其支流因受地壳不断间歇性隆升的影响而形成了5-6级阶地,这些阶地多系黄土覆盖阶地。以六盘山为界,河谷阶地黄土地层结构可分为东、西阶地地层区。六盘山以西河流阶地一般为6级。第6级阶地(T6)冲积黄土状土之上全系无层理黄土,厚310~505 m,含21-23层古土壤,是迄今世界上最厚的黄土剖面,黄土开始堆积的时间不早于1.43 MaBP。T5上的黄土厚200~400 m,含14-16层古土壤,黄土最早是在1.23 MaBP开始堆积的。T4上的黄土厚100~200 m,含5-6层古土壤,开始沉积时间为0.62 MaBP。T3上的黄土包括L1和S1,厚40~65 m,形成于0.12 MaBP。T2冲积黄土状土之上的风积黄土厚20~35 m,形成时间约为0.03 MaBP。T1冲积黄土状土之上为S0、L0及MS,厚1.5~2.5 m,形成时间不早于0.01 MaBP。六盘山以东的河谷阶地一般为5级。T5风积黄土厚70~90 m,含11-16层古土壤,黄土开始堆积时间不早于1.23 MaBP。T4黄土厚40~70 m,含8-9层古土壤,形成时间不晚于0.80 MaBP。T3的黄土包括L1-S6之间的土层,厚25~45 m,形成于0.62 MaBP。T2的黄土由L1和S1构成,厚10~17 m,形成于0.12 MaBP。T1冲积黄土状土之上为S0、L0及MS,厚1.5~2.5 m,形成时间不早于0.01 MaBP。
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出版历程
收稿日期:  2005-09-11
修回日期:  2005-12-21

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