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Identification of ca. 850 Ma high-temperature strongly peraluminous granitoids in southeastern Guizhou Province, South China: A result of early extension along the southern margin of the Yangtze Block
Tao Wu; Jia-Xi Zhou; Xuan-Ce Wang; Wu-Xian Li; Simon A. Wilde; Hai-Rui Sun; Jing-Song Wang; Zhen Li
2018
发表期刊Precambrian Research
卷号308页码:18-34
DOI10.1016/j.precamres.2018.02.007
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收录类别SCI
语种英语
WOS记录号WOS:000430775800002
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被引频次:20[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.gyig.ac.cn/handle/42920512-1/14061
专题矿床地球化学国家重点实验室
作者单位1.School of Earth Sciences, Zhejiang University, Hangzhou 310027, China
2.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
3.The Institute for Geoscience Research, Department of Applied Geology, Curtin University, GPO Box U1987, Perth, WA 6845, Australia
4.School of Earth Science and Resources, Chang’an University, Shaanxi, Xi’an 710054, China
5.State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Science, Guangzhou 510640, China
6.Development Research Center of China Geological Survey, Beijing 100037, China
7.The 102 Geological Team, Guizhou Bureau of Exploration and Development of Geology and Mineral Resources, Zunyi 563003, China
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Tao Wu,Jia-Xi Zhou,Xuan-Ce Wang,et al. Identification of ca. 850 Ma high-temperature strongly peraluminous granitoids in southeastern Guizhou Province, South China: A result of early extension along the southern margin of the Yangtze Block[J]. Precambrian Research,2018,308:18-34.
APA Tao Wu.,Jia-Xi Zhou.,Xuan-Ce Wang.,Wu-Xian Li.,Simon A. Wilde.,...&Zhen Li.(2018).Identification of ca. 850 Ma high-temperature strongly peraluminous granitoids in southeastern Guizhou Province, South China: A result of early extension along the southern margin of the Yangtze Block.Precambrian Research,308,18-34.
MLA Tao Wu,et al."Identification of ca. 850 Ma high-temperature strongly peraluminous granitoids in southeastern Guizhou Province, South China: A result of early extension along the southern margin of the Yangtze Block".Precambrian Research 308(2018):18-34.
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