Obduction-type granites within the NE Jiangxi Ophiolite: Implications for the final amalgamation between the Yangtze and Cathaysia Blocks

GIG OpenIR > 中科院广州地化所(-2008)

	Li WX; Li XH; Li ZX; Lou FS
	Obduction-type granites within the NE Jiangxi Ophiolite: Implications for the final amalgamation between the Yangtze and Cathaysia Blocks
Source Publication	Gondwana Research
ISSN	1342-937X
	2008
Volume	13 Issue:3 Pages:288-301
Language	英语
WOS ID	WOS:000254659200002
Indexed By	sci
Citation statistics	Cited Times:213[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/13789
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	Li WX,Li XH,Li ZX,et al. Obduction-type granites within the NE Jiangxi Ophiolite: Implications for the final amalgamation between the Yangtze and Cathaysia Blocks[J]. Gondwana Research,2008,13(3):288-301.
APA	Li WX,Li XH,Li ZX,&Lou FS.(2008).Obduction-type granites within the NE Jiangxi Ophiolite: Implications for the final amalgamation between the Yangtze and Cathaysia Blocks.Gondwana Research,13(3),288-301.
MLA	Li WX,et al."Obduction-type granites within the NE Jiangxi Ophiolite: Implications for the final amalgamation between the Yangtze and Cathaysia Blocks".Gondwana Research 13.3(2008):288-301.

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