Carboniferous mantle-derived felsic intrusion in the Chinese Altai, NW China: Implications for geodynamic change of the accretionary orogenic belt

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
刊名	Gondwana Research
ISSN号	1342-937X
	2012
卷号	22 期号:2 页码:681-698
语种	英语
WOS记录号	WOS:000307602000025
收录类别	SCI
引用统计	被引频次：108[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.gig.ac.cn/handle/344008/18101
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	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.