Palaeosol development in the Chinese Loess Plateau as an indicator of the strength of the East Asian summer monsoon: Evidence for a mid-Holocene maximum

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	Palaeosol development in the Chinese Loess Plateau as an indicator of the strength of the East Asian summer monsoon: Evidence for a mid-Holocene maximum
	Wang, HP; Chen, JH; Zhang, XJ; Chen, FH
刊名	QUATERNARY INTERNATIONAL
	2014-06-17
卷号	334 页码:155-164
关键词	Holocene Palaeosol development Aeolian activity Chinese Loess Plateau East Asian summer monsoon
ISSN号	1040-6182
通讯作者	Chen, JH (reprint author), Lanzhou Univ, Collaborat Innovat Ctr Arid Environm & Climate Ch, MOE Key Lab Western Chinas Environm Syst, 222 South Tianshui Rd, Lanzhou 730000, Gansu, Peoples R China.
学科主题	Physical Geography; Geology
出版地	OXFORD
语种	英语
WOS记录号	WOS:000338817800016
内容类型	期刊论文
源URL	[http://ir.lzu.edu.cn/handle/262010/120470]
专题	资源环境学院_期刊论文
推荐引用方式 GB/T 7714	Wang, HP,Chen, JH,Zhang, XJ,et al. Palaeosol development in the Chinese Loess Plateau as an indicator of the strength of the East Asian summer monsoon: Evidence for a mid-Holocene maximum[J]. QUATERNARY INTERNATIONAL,2014,334:155-164.
APA	Wang, HP,Chen, JH,Zhang, XJ,&Chen, FH.(2014).Palaeosol development in the Chinese Loess Plateau as an indicator of the strength of the East Asian summer monsoon: Evidence for a mid-Holocene maximum.QUATERNARY INTERNATIONAL,334,155-164.
MLA	Wang, HP,et al."Palaeosol development in the Chinese Loess Plateau as an indicator of the strength of the East Asian summer monsoon: Evidence for a mid-Holocene maximum".QUATERNARY INTERNATIONAL 334(2014):155-164.