Ca. 825 Ma komatiitic basalts in South China: First evidence for > 1500 degrees C mantle melts by a Rodinian mantle plume

GIG OpenIR > 中科院广州地化所(-2008)

	Wang XC; Li XH; Li WX; Li ZX
	Ca. 825 Ma komatiitic basalts in South China: First evidence for > 1500 degrees C mantle melts by a Rodinian mantle plume
Source Publication	Geology
ISSN	0091-7613
	2007
Volume	35 Issue:12 Pages:1103-1106
Indexed By	sci
Language	英语
WOS ID	WOS:000251597700012
Citation statistics	Cited Times:133[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/13685
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	Wang XC,Li XH,Li WX,et al. Ca. 825 Ma komatiitic basalts in South China: First evidence for > 1500 degrees C mantle melts by a Rodinian mantle plume[J]. Geology,2007,35(12):1103-1106.
APA	Wang XC,Li XH,Li WX,&Li ZX.(2007).Ca. 825 Ma komatiitic basalts in South China: First evidence for > 1500 degrees C mantle melts by a Rodinian mantle plume.Geology,35(12),1103-1106.
MLA	Wang XC,et al."Ca. 825 Ma komatiitic basalts in South China: First evidence for > 1500 degrees C mantle melts by a Rodinian mantle plume".Geology 35.12(2007):1103-1106.

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