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Neoproterozoic W-Sn Polymetallic Mineralization in the Western Jiangnan Orogen, South China: Insights from the Fanjingshan S-Type Granites  ( EI收录)  

文献类型:期刊文献

英文题名:Neoproterozoic W-Sn Polymetallic Mineralization in the Western Jiangnan Orogen, South China: Insights from the Fanjingshan S-Type Granites

作者:Luo, Jin-Cheng Zhang, Jiawei Shu, Xujie Tang, Yanwen Dai, Yaran Chen, Xiaocui Liu, Weipeng

第一作者:Luo, Jin-Cheng

机构:[1] State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550081, China; [2] Guizhou Geological Survey, Bureau of Geology and Mineral Exploration and Development of Guizhou Province, Guiyang, 550081, China; [3] School of Geographic Science, Nantong University, Nantong, 226019, China; [4] School of Resources and Environmental Engineering, Guizhou Institute of Technology, Guiyang, 550003, China

第一机构:State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550081, China

年份:2024

外文期刊名:SSRN

收录:EI(收录号:20240270095)

语种:英文

外文关键词:Alumina - Aluminum oxide - Apatite - Binary alloys - Geochronology - Granite - Gravel - Lead alloys - Mica - Mineralogy - Rare earth elements - Rare earths - Sedimentary rocks - Silica - Sodium compounds - Tin alloys - Zircon

摘要:The Jiangnan Orogen boasts abundant Neoproterozoic granitoids alongside locally significant W-Sn polymetallic mineralization in South China. However, the factors governing the relationships between granites and the W-Sn polymetallic mineralization remain elusive. Notably, Neoproterozoic W-Sn polymetallic mineralization locally occurred within the western margin of the Jiangnan Orogen, encompassing key deposits like the Jiumao, Huashadong, and Taoshulin deposits. The W-Sn-bearing Taoshulin muscovite granite intruded into Neoproterozoic Fanjingshan Group, comprising of low-degree metamorphosed sedimentary rocks that locally contain granitic gravel. These granites in this study have high SiO2 (73.6–77.4 wt.%), Al2O3 (12.8–15.1 wt.%), Na2O (3.16–5.25 wt.%) and high A/CNK values (1.28–1.47), which display co-variation trends. They have extremely low rare earth element (REE) concentrations ( ? 2024, The Authors. All rights reserved.

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