Paleo- to Mesoproterozoic magmatic and tectonic evolution of the southwestern Yangtze Block, south China: New constraints from ca. 1.7–1.5 Ga mafic rocks in the Huili-Dongchuan area
Hong-Peng Fan; Wei-Guang Zhu; Zheng-Xiang Li
刊名Gondwana Research
2020
卷号87页码:248-262
DOI10.1016/j.gr.2020.06.019
语种英语
内容类型期刊论文
源URL[http://ir.gyig.ac.cn/handle/42920512-1/11471]  
专题地球化学研究所_矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
作者单位1.ARC Center of Excellence for Core to Crust Fluid Systems (CCFS) and The Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University, GPO Box U1987, Perth, Western Australia 6845, Australia
2.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, 99 West Lincheng Road, Guiyang 550081, China
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GB/T 7714
Hong-Peng Fan,Wei-Guang Zhu,Zheng-Xiang Li. Paleo- to Mesoproterozoic magmatic and tectonic evolution of the southwestern Yangtze Block, south China: New constraints from ca. 1.7–1.5 Ga mafic rocks in the Huili-Dongchuan area[J]. Gondwana Research,2020,87:248-262.
APA Hong-Peng Fan,Wei-Guang Zhu,&Zheng-Xiang Li.(2020).Paleo- to Mesoproterozoic magmatic and tectonic evolution of the southwestern Yangtze Block, south China: New constraints from ca. 1.7–1.5 Ga mafic rocks in the Huili-Dongchuan area.Gondwana Research,87,248-262.
MLA Hong-Peng Fan,et al."Paleo- to Mesoproterozoic magmatic and tectonic evolution of the southwestern Yangtze Block, south China: New constraints from ca. 1.7–1.5 Ga mafic rocks in the Huili-Dongchuan area".Gondwana Research 87(2020):248-262.
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