IEECAS OpenIR  > 黄土与第四纪地质国家重点实验室(2005-2009)
Climate variability in the Salawusu River valley of the Ordos Plateau (Inner Mongolia, China) during Marine Isotope Stage 3
X.H. Wen; B.S. Li; Y.M. Zheng; D.D. Zhang; J.P. Ye
2009
Source PublicationJournal of Quaternary Science
Volume24Issue:1Pages:61-74
Cooperation Status其它
KeywordSalawusu River Valley Climate Variability Marine Isotope Stage 3 (Mis 3) East Asian Monsoon Chenchuan Formation
Subject Area地质学 ; 大气科学
Language中文
WOS IDWOS:000262615700006
Citation statistics
Cited Times:9[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/1866
Collection黄土与第四纪地质国家重点实验室(2005-2009)
Recommended Citation
GB/T 7714
X.H. Wen,B.S. Li,Y.M. Zheng,et al. Climate variability in the Salawusu River valley of the Ordos Plateau (Inner Mongolia, China) during Marine Isotope Stage 3[J]. Journal of Quaternary Science,2009,24(1):61-74.
APA X.H. Wen,B.S. Li,Y.M. Zheng,D.D. Zhang,&J.P. Ye.(2009).Climate variability in the Salawusu River valley of the Ordos Plateau (Inner Mongolia, China) during Marine Isotope Stage 3.Journal of Quaternary Science,24(1),61-74.
MLA X.H. Wen,et al."Climate variability in the Salawusu River valley of the Ordos Plateau (Inner Mongolia, China) during Marine Isotope Stage 3".Journal of Quaternary Science 24.1(2009):61-74.
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