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Yuan, DX; Chen, J; Zhang, YC; Zheng, QF; Shen, SZ
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
Source PublicationGeological Journal
ISSN0072-1050
2015
Volume50Issue:2Pages:122-138
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/31662
Collection中国科学院广州地球化学研究所
Recommended Citation
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.(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.
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