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
ISSN1000-0569
2006
Volume22Issue:6Pages:1665-1671
Indexed Bysci
Language中文
Document Type期刊论文
Identifierhttp://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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