Zircon U-Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic

GIG OpenIR > 中科院广州地化所(-2008)

	Sun M; Yuan C; Xiao W; Long X; Xia X; Zhao G; Lin S; Wu F; Kroner A
	Zircon U-Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic
Source Publication	Chemical Geology
ISSN	0009-2541
	2008
Volume	247 Issue:3-4 Pages:352-383
Language	英语
WOS ID	WOS:000253178000003
Indexed By	sci
Citation statistics	Cited Times:322[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/13869
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	Sun M,Yuan C,Xiao W,et al. Zircon U-Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic[J]. Chemical Geology,2008,247(3-4):352-383.
APA	Sun M.,Yuan C.,Xiao W.,Long X.,Xia X.,...&Kroner A.(2008).Zircon U-Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic.Chemical Geology,247(3-4),352-383.
MLA	Sun M,et al."Zircon U-Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic".Chemical Geology 247.3-4(2008):352-383.

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