Formation of high delta(18)O fayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks, southern China

GIG OpenIR

	Huang, HQ; Li, XH; Li, WX; Li, ZX
	Formation of high delta(18)O fayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks, southern China
Source Publication	Geology
ISSN	0091-7613
	2011
Volume	39 Issue:10 Pages:903-906
Language	英语
Indexed By	SCI
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/17543
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	Huang, HQ,Li, XH,Li, WX,et al. Formation of high delta(18)O fayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks, southern China[J]. Geology,2011,39(10):903-906.
APA	Huang, HQ,Li, XH,Li, WX,&Li, ZX.(2011).Formation of high delta(18)O fayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks, southern China.Geology,39(10),903-906.
MLA	Huang, HQ,et al."Formation of high delta(18)O fayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks, southern China".Geology 39.10(2011):903-906.

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