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

GIG OpenIR

	Huang, Hui-Qing; Li, Xian-Hua; Li, Wu-Xian; Li, Zheng-Xiang
	Formation of high delta O-18 fayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks, southern China
Source Publication	Geology
ISSN	0091-7613
	2012
Volume	40 Issue:10 Pages:E278
Language	英语
WOS ID	WOS:000309986100026
Indexed By	SCI
Citation statistics	Cited Times:1[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/18256
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	Huang, Hui-Qing,Li, Xian-Hua,Li, Wu-Xian,et al. Formation of high delta O-18 fayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks, southern China[J]. Geology,2012,40(10):E278.
APA	Huang, Hui-Qing,Li, Xian-Hua,Li, Wu-Xian,&Li, Zheng-Xiang.(2012).Formation of high delta O-18 fayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks, southern China.Geology,40(10),E278.
MLA	Huang, Hui-Qing,et al."Formation of high delta O-18 fayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks, southern China".Geology 40.10(2012):E278.

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