PALEOSOLS AND THEIR ENVIRONMENTAL SIGNIFICANCE DURING HOLOCENE IN DAQINGSHAN MOUNTAIN REGION OF INNER MONGOLIA,NORTH CHINA | |
Wu Wanli | |
刊名 | The Journal of Hinese Geography
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1992 | |
关键词 | paleosols ~(14)C age climatic change Inner Mongolia |
英文摘要 | Studies on the paleosol and the environmental changes during the Holocene in the Daqingshan Mountain were carried out based on the analyses of strata section structure,morphological properties,~(14)C data,physico-chemical characteristics and soil micromorphology.The paleosol developed in five periods and are usually separated by horizons rich in gravels("stone line"layers).Fairly strong humus accumulation and weak carbonate eluviation processes are characteristic of the paleosol forming periods;and the"ston; 01; 72-83 |
语种 | 英语 |
内容类型 | 期刊论文 |
源URL | [http://ir.pku.edu.cn/handle/20.500.11897/479395] ![]() |
专题 | 城市与环境学院 |
推荐引用方式 GB/T 7714 | Wu Wanli. PALEOSOLS AND THEIR ENVIRONMENTAL SIGNIFICANCE DURING HOLOCENE IN DAQINGSHAN MOUNTAIN REGION OF INNER MONGOLIA,NORTH CHINA[J]. The Journal of Hinese Geography,1992. |
APA | Wu Wanli.(1992).PALEOSOLS AND THEIR ENVIRONMENTAL SIGNIFICANCE DURING HOLOCENE IN DAQINGSHAN MOUNTAIN REGION OF INNER MONGOLIA,NORTH CHINA.The Journal of Hinese Geography. |
MLA | Wu Wanli."PALEOSOLS AND THEIR ENVIRONMENTAL SIGNIFICANCE DURING HOLOCENE IN DAQINGSHAN MOUNTAIN REGION OF INNER MONGOLIA,NORTH CHINA".The Journal of Hinese Geography (1992). |
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