| 云南会泽铅锌矿地质特征及研究现状 |
| |
| 引用本文： | 王忠伟.云南会泽铅锌矿地质特征及研究现状[J].世界有色金属,2020(3):260-260,262. |
| |
| 作者姓名： | 王忠伟 |
| |
| 作者单位： | 广西壮族自治区区域地质调查研究院 |
| |
| 摘 要： | 会泽铅锌矿为川-滇-黔成矿省中一大型矿床,具有负责的矿床成因特征。矿区出露地层主要为前寒武纪基底及沉积盖层;构造特征以断裂为主,呈NW向;出露岩浆岩为峨眉山玄武岩;Pb-Zn矿体主要受NW向断裂控制。同位素特征显示,矿床形成于晚三叠,成矿物质主要来自于沉积盖层,成矿流体主要为变质流体。
|
| 关 键 词： | 会泽铅锌矿 地质特征 研究现状 |
Geological characteristics and research status of Huize Lead zinc mine,Yunnan Province |
| |
| WANG Zhong-wei.Geological characteristics and research status of Huize Lead zinc mine,Yunnan Province[J].World Nonferrous Metals,2020(3):260-260,262. |
| |
| Authors: | WANG Zhong-wei |
| |
| Affiliation: | (Regional geological survey and Research Institute of Guangxi Zhuang Autonomous Region,Guilin 541003,China) |
| |
| Abstract: | Located in the SYG(Sichuan-Yunnan-Guizhou)metallogenic province,the Huize is a large Pb-Zn deposit with complex mineralization process.Precambrian basement and sedimentary rocks are occurred at this deposit,and the main structures are the NW-trending faults.The Emeishan basalt is the only discovered magmatic rocks of the deposit.Isotopic data reveal that mineralization materials came from the sedimentary rocks and the ore-forming fluids were originated from the metamorphism.The deposition of the Pb-Zn elements was likely occurred at late Triassic. |
| |
| Keywords: | Huize Lead zinc mine geological characteristics research status |
| 本文献已被 CNKI 维普 等数据库收录！ |
|
