Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis

GIG OpenIR > 中科院广州地化所(-2008)

	Xiong XL; Adam J; Green TH
	Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis
Source Publication	Chemical Geology
ISSN	0009-2541
	2005
Volume	218 Issue:3-4 Pages:339-359
Language	英语
WOS ID	WOS:000229691700008
Indexed By	sci
Citation statistics	Cited Times:567[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/12673
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	Xiong XL,Adam J,Green TH. Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis[J]. Chemical Geology,2005,218(3-4):339-359.
APA	Xiong XL,Adam J,&Green TH.(2005).Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis.Chemical Geology,218(3-4),339-359.
MLA	Xiong XL,et al."Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis".Chemical Geology 218.3-4(2005):339-359.

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中国科学院广州地球化学研究所机构知识库