Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years

IEECAS OpenIR > 黄土与第四纪地质国家重点实验室(2005-2009)

	Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years
	An Z.S.; George J. Kukla; Stephen C; Xiao J.L.
	1991
发表期刊	Quaternary Research
卷号	36 期号:1 页码:29-36
合作性质	国际
摘要	The magnetic susceptibility of loess and paleosols in central China represents a proxy climate index closely related to past changes of precipitation and vegetation, and thus to summer monsoon intensity. Time series of magnetic susceptibility constructed for three loess-paleosol sequences in the southern part of the Chinese Loess Plateau document the history of summer monsoon variation during the last 130,000 yr. They correlate closely with the oxygen isotope record of stages 1 to 5 in deep-sea sediments. Soils were forming during intervals of strong summer monsoon, whereas loess units were deposited at times of reduced monsoon intensity. The Chinese loess-paleosol sequence can thus be viewed as a proxy record of Asian monsoon variability extending over the last 2.5 myr.
学科领域	地质学 ; 地球化学
收录类别	SCI
语种	英语
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/2584
专题	黄土与第四纪地质国家重点实验室(2005-2009)
推荐引用方式 GB/T 7714	An Z.S.,George J. Kukla,Stephen C,et al. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years[J]. Quaternary Research,1991,36(1):29-36.
APA	An Z.S.,George J. Kukla,Stephen C,&Xiao J.L..(1991).Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years.Quaternary Research,36(1),29-36.
MLA	An Z.S.,et al."Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years".Quaternary Research 36.1(1991):29-36.

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