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GIG OpenIR  > 中科院广州地化所(-2008)
资锋; 何光玉; 戴圣潜; 许卫
徐州利国早白垩世高镁埃达克质侵入岩的成因及其动力学、成矿意义
Source Publication岩石学报
ISSN1000-0569
2007
Volume23Issue:11Pages:2857-2868
Language中文
Indexed Bysci
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/13725
Collection中科院广州地化所(-2008)
Recommended Citation
GB/T 7714		 资锋,何光玉,戴圣潜,等. 徐州利国早白垩世高镁埃达克质侵入岩的成因及其动力学、成矿意义[J]. 岩石学报,2007,23(11):2857-2868.
APA 资锋,何光玉,戴圣潜,&许卫.(2007).徐州利国早白垩世高镁埃达克质侵入岩的成因及其动力学、成矿意义.岩石学报,23(11),2857-2868.
MLA 资锋,et al."徐州利国早白垩世高镁埃达克质侵入岩的成因及其动力学、成矿意义".岩石学报 23.11(2007):2857-2868.
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