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Multi-Phase Hydrothermal Fluid Events in the Giant Lannigou Gold Deposit, SW China: Insights from Calcite Sm-Nd Age, Trace Elements, and C-O-Sr Isotopes
Piyou Li; Yuzhao Hu; Zhendong Tian; Shenjin Guan; Huijun Fan
2023
Source PublicationMinerals
Volume13Issue:11
DOI10.3390/min13111420
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Indexed BySCI
Language英语
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Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/14461
Collection矿床地球化学国家重点实验室
Affiliation1.Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China
2.South-West Institute of Geological Survey, Geological Survey Center for Nonferrous Metals Resources, Kunming 650093, China
3.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
4.The First Gas Production Plant, PetroChina Changqing Oilfield Company, Jingbian 718500, China
Recommended Citation
GB/T 7714
Piyou Li,Yuzhao Hu,Zhendong Tian,et al. Multi-Phase Hydrothermal Fluid Events in the Giant Lannigou Gold Deposit, SW China: Insights from Calcite Sm-Nd Age, Trace Elements, and C-O-Sr Isotopes[J]. Minerals,2023,13(11).
APA Piyou Li,Yuzhao Hu,Zhendong Tian,Shenjin Guan,&Huijun Fan.(2023).Multi-Phase Hydrothermal Fluid Events in the Giant Lannigou Gold Deposit, SW China: Insights from Calcite Sm-Nd Age, Trace Elements, and C-O-Sr Isotopes.Minerals,13(11).
MLA Piyou Li,et al."Multi-Phase Hydrothermal Fluid Events in the Giant Lannigou Gold Deposit, SW China: Insights from Calcite Sm-Nd Age, Trace Elements, and C-O-Sr Isotopes".Minerals 13.11(2023).
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