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:130[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.

Related Services

Bookmark

Google Scholar

Similar articles in Bing Scholar

Terms of Use

No data!

Social Bookmark/Share

All comments (0)

No comment.

The comment function is only available to registered usersLog In

If you have any objections to this item, please fill out the form below and the administrator will contact you as soon as possible.
Content:
Email：	*
Institution:
Verification Code:	Refresh

Any comments and suggestions are welcomed.
Title:	*
Content:
Email：	*
Verification Code:	Refresh

中国科学院广州地球化学研究所机构知识库