PALEOSOLS AND THEIR ENVIRONMENTAL SIGNIFICANCE DURING HOLOCENE IN DAQINGSHAN MOUNTAIN REGION OF INNER MONGOLIA,NORTH CHINA

CORC > 北京大学 > 城市与环境学院

	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
	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).