Major and trace element variations of the sediments at ODP Site 1144, South China Sea, during the last 230 ka and their paleoclimate implications

GIG OpenIR > 中科院广州地化所(-2008)

	Wei GJ; Liu Y; Li XH; Shao L; Fang DY
	Major and trace element variations of the sediments at ODP Site 1144, South China Sea, during the last 230 ka and their paleoclimate implications
Source Publication	Palaeogeography Palaeoclimatology Palaeoecology
ISSN	0031-0182
	2004
Volume	212 Issue:3-4 Pages:331-342
Language	英语
WOS ID	WOS:000224215200009
Indexed By	sci
Citation statistics	Cited Times:101[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/12303
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	Wei GJ,Liu Y,Li XH,et al. Major and trace element variations of the sediments at ODP Site 1144, South China Sea, during the last 230 ka and their paleoclimate implications[J]. Palaeogeography Palaeoclimatology Palaeoecology,2004,212(3-4):331-342.
APA	Wei GJ,Liu Y,Li XH,Shao L,&Fang DY.(2004).Major and trace element variations of the sediments at ODP Site 1144, South China Sea, during the last 230 ka and their paleoclimate implications.Palaeogeography Palaeoclimatology Palaeoecology,212(3-4),331-342.
MLA	Wei GJ,et al."Major and trace element variations of the sediments at ODP Site 1144, South China Sea, during the last 230 ka and their paleoclimate implications".Palaeogeography Palaeoclimatology Palaeoecology 212.3-4(2004):331-342.

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