华北克拉通中、新生代典型火山岩的岩石成因：Hf同位素新证据

GIG OpenIR > 中科院广州地化所(-2008)

	杨岳衡; 张宏福; 谢烈文; 刘颖; 祁昌实; 涂湘林
	华北克拉通中、新生代典型火山岩的岩石成因：Hf同位素新证据
Source Publication	岩石学报
ISSN	1000-0569
	2006
Volume	22 Issue:6 Pages:1665-1671
Language	中文
Indexed By	sci
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/13255
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	杨岳衡,张宏福,谢烈文,等. 华北克拉通中、新生代典型火山岩的岩石成因：Hf同位素新证据[J]. 岩石学报,2006,22(6):1665-1671.
APA	杨岳衡,张宏福,谢烈文,刘颖,祁昌实,&涂湘林.(2006).华北克拉通中、新生代典型火山岩的岩石成因：Hf同位素新证据.岩石学报,22(6),1665-1671.
MLA	杨岳衡,et al."华北克拉通中、新生代典型火山岩的岩石成因：Hf同位素新证据".岩石学报 22.6(2006):1665-1671.

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