Formation of the Jurassic Changboshan-Xieniqishan highly fractionated I-type granites, northeastern China: implication for the partial melting of juvenile crust induced by asthenospheric mantle upwelling
文献类型:期刊论文
作者 | Yuan, DX; Chen, J; Zhang, YC; Zheng, QF; Shen, SZ; Chen, Huayong![]() |
刊名 | Geological Journal
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出版日期 | 2015 |
卷号 | 50期号:2页码:122-138 |
ISSN号 | 0072-1050 |
收录类别 | SCI |
语种 | 英语 |
源URL | [http://ir.gig.ac.cn:8080/handle/344008/31662] ![]() |
专题 | 中国科学院广州地球化学研究所 |
推荐引用方式 GB/T 7714 | Yuan, DX,Chen, J,Zhang, YC,et al. Formation of the Jurassic Changboshan-Xieniqishan highly fractionated I-type granites, northeastern China: implication for the partial melting of juvenile crust induced by asthenospheric mantle upwelling[J]. Geological Journal,2015,50(2):122-138. |
APA | Yuan, DX,Chen, J,Zhang, YC,Zheng, QF,Shen, SZ,&Chen, Huayong.(2015).Formation of the Jurassic Changboshan-Xieniqishan highly fractionated I-type granites, northeastern China: implication for the partial melting of juvenile crust induced by asthenospheric mantle upwelling.Geological Journal,50(2),122-138. |
MLA | Yuan, DX,et al."Formation of the Jurassic Changboshan-Xieniqishan highly fractionated I-type granites, northeastern China: implication for the partial melting of juvenile crust induced by asthenospheric mantle upwelling".Geological Journal 50.2(2015):122-138. |
入库方式: OAI收割
来源:广州地球化学研究所
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