IEECAS OpenIR  > 黄土与第四纪地质国家重点实验室(2005-2009)
Grain size of loess, palaeosol and Red Clay deposits on the Chinese Loess Plateau: Significance for understanding pedogenic alteration and palaeomonsoon evolution
Y.B. Sun; H.Y. Lu; Z.S. An
2006
Source PublicationPalaeogeography, Palaeoclimatology, Palaeoecology
Volume241Issue:1Pages:129-138
KeywordChinese Loess Plateau Loess–palaeosol Sequence Red Clay Sequence Grain Size Pedogenic Alteration Palaeomonsoon Evolution
WOS IDWOS:000242001100011
Citation statistics
Cited Times:75[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/2446
Collection黄土与第四纪地质国家重点实验室(2005-2009)
Recommended Citation
GB/T 7714
Y.B. Sun,H.Y. Lu,Z.S. An. Grain size of loess, palaeosol and Red Clay deposits on the Chinese Loess Plateau: Significance for understanding pedogenic alteration and palaeomonsoon evolution[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2006,241(1):129-138.
APA Y.B. Sun,H.Y. Lu,&Z.S. An.(2006).Grain size of loess, palaeosol and Red Clay deposits on the Chinese Loess Plateau: Significance for understanding pedogenic alteration and palaeomonsoon evolution.Palaeogeography, Palaeoclimatology, Palaeoecology,241(1),129-138.
MLA Y.B. Sun,et al."Grain size of loess, palaeosol and Red Clay deposits on the Chinese Loess Plateau: Significance for understanding pedogenic alteration and palaeomonsoon evolution".Palaeogeography, Palaeoclimatology, Palaeoecology 241.1(2006):129-138.
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