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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
2020
Source PublicationGondwana Research
Volume87Pages:248-262
DOI10.1016/j.gr.2020.06.019
Language英语
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Cited Times:26[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/11471
Collection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
Affiliation1.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, 99 West Lincheng Road, Guiyang 550081, China
2.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
Recommended Citation
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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