Chinese Loess Paleosol sediments were just controlled by both the factors of glacial interglacial and paleomonsoon climate.
中国黄土—古土壤堆积是全球冰期—间冰期气候变化与东亚古季风气候变化共同作用的结果。
The intact stratigraphic profile at the Dali Man site consists of the upper Loess-Paleosol series and the lower sandy soil series.
完整的陕西大荔人遗址剖面由上部黄土—古土壤序列和下部砂土地层两部分组成。
A holocene paleosol-loess sediment profile and lacustrine sediment profile were found in Mengjin, Henan province.
在河南孟津地区发现全新世古土壤-黄土沉积剖面和湖沼相沉积剖面。
In UCC and CL normalized maps, the variation trend of loess is basically consistent with that of paleosol in Dadunling section.
在UCC标准化图与CL标准化图中，大墩岭黄土与古土壤变化趋势基本一致。
The last interglacial paleosol and last glacial loess units overlie the top of this section.
其顶部覆盖了末次间冰期古土壤与末次冰期黄土。
The focus issue of pole-climatic and paleosol study is to extract factor which affects environment change from loess- paleosol.
从黄土-古土壤中提取影响环境变化的因子并对未来全球变化的预测是目前古土壤与环境变化研究中的热点。
The focus issue of pole-climatic and paleosol study is to extract factor which affects environment change from loess- paleosol.
从黄土-古土壤中提取影响环境变化的因子并对未来全球变化的预测是目前古土壤与环境变化研究中的热点。
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