GIG OpenIR
Cai, Keda; Sun, Min; Yuan, Chao; Xiao, Wenjiao; Zhao, Guochun; Long, Xiaoping; Wu, Fuyuan
Carboniferous mantle-derived felsic intrusion in the Chinese Altai, NW China: Implications for geodynamic change of the accretionary orogenic belt
Source PublicationGondwana Research
ISSN1342-937X
2012
Volume22Issue:2Pages:681-698
Language英语
WOS IDWOS:000307602000025
Indexed BySCI
Citation statistics
Cited Times:108[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/18101
Collection中国科学院广州地球化学研究所
Recommended Citation
GB/T 7714
Cai, Keda,Sun, Min,Yuan, Chao,et al. Carboniferous mantle-derived felsic intrusion in the Chinese Altai, NW China: Implications for geodynamic change of the accretionary orogenic belt[J]. Gondwana Research,2012,22(2):681-698.
APA Cai, Keda.,Sun, Min.,Yuan, Chao.,Xiao, Wenjiao.,Zhao, Guochun.,...&Wu, Fuyuan.(2012).Carboniferous mantle-derived felsic intrusion in the Chinese Altai, NW China: Implications for geodynamic change of the accretionary orogenic belt.Gondwana Research,22(2),681-698.
MLA Cai, Keda,et al."Carboniferous mantle-derived felsic intrusion in the Chinese Altai, NW China: Implications for geodynamic change of the accretionary orogenic belt".Gondwana Research 22.2(2012):681-698.
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