Pleistocene magnetic susceptibility and paleomagnetism of the Tibetan loess and its implications on large climatic change events

doi:10.1007/BF02911991

IEECAS OpenIR > 黄土与第四纪地质国家重点实验室（1985-2004）

	Pleistocene magnetic susceptibility and paleomagnetism of the Tibetan loess and its implications on large climatic change events
	Yan, MD; Fang, XM; Chen, SY; Yang, SL; Lu, LQ; Li, JJ; An, ZS
	2001-10
发表期刊	SCIENCE IN CHINA SERIES D-EARTH SCIENCES
卷号	44 页码:227-232
文章类型	Article
摘要	Ganzi loess represents the oldest Tibetan loess, its formation is the key to determining the readjustment of Tibetan atmospheric circulation and the relationship between Tibetan uplift and global climatic change. Detailed magnetostratigraphic study shows that the Ganzi loess was formed at about 1.13 MaBP. It also reveals that there are two notable climatic events occurring in 0.95-0.92 Ma and 0.65-0.5 Ma respectively. They both demonstrate that the Tibetan atmospheric circulation was readjusted and the Tibetan Plateau entered the cryosphere at 21.13 Ma, and the Tibetan glaciation might reach its maximum at similar to0.65-0.5 Ma.
关键词	Tibetan Plateau loess uplift atmospheric circulation climatic change
学科领域	Geology
DOI	10.1007/BF02911991
收录类别	SCI ; SCIE
语种	英语
WOS研究方向	Geosciences, Multidisciplinary
WOS记录号	WOS:000175181800027
出版者	SCIENCE CHINA PRESS
引用统计	被引频次：22[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/12024
专题	黄土与第四纪地质国家重点实验室（1985-2004）
推荐引用方式 GB/T 7714	Yan, MD,Fang, XM,Chen, SY,et al. Pleistocene magnetic susceptibility and paleomagnetism of the Tibetan loess and its implications on large climatic change events[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2001,44:227-232.
APA	Yan, MD.,Fang, XM.,Chen, SY.,Yang, SL.,Lu, LQ.,...&An, ZS.(2001).Pleistocene magnetic susceptibility and paleomagnetism of the Tibetan loess and its implications on large climatic change events.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,44,227-232.
MLA	Yan, MD,et al."Pleistocene magnetic susceptibility and paleomagnetism of the Tibetan loess and its implications on large climatic change events".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 44(2001):227-232.