Trace elements in sulfide minerals from the Huangshaping copper-polymetallic deposit, Hunan, China: Ore genesis and element occurrence
文献类型：期刊论文
| 作者 | Chu, Xiangkai1,2,3; Li, Bo3,4; Shen, Ping1,2; Zha, Zhihui2,3; Lei, Zhen3; Wang, Xinfu3; Tao, Siyuan3; Hu, Qian2,3 |
| 刊名 | ORE GEOLOGY REVIEWS
 |
| 出版日期 | 2022-05-01 |
| 卷号 | 144页码:19 |
| ISSN号 | 0169-1368 |
| 关键词 | Pb-Zn mineralization Sulfide LA-ICP-MS Ore genesis Huangshaping copper-polymetallic deposit Southern Hunan |
| DOI | 10.1016/j.oregeorev.2022.104867 |
| 英文摘要 | & nbsp;The Huangshaping copper-polymetallic deposit, which is located in southern Hunan Province, China, is an important resource base for Pb-Zn minerals. This study used the major sulfides (sphalerite, pyrite, pyrrhotite), which formed during the Pb-Zn mineralization stage of the Huangshaping deposit, to determine the genesis of the Pb-Zn ore minerals and element occurrence. In-situ LA-ICP-MS analysis of minerals was conducted to determine their trace element concentrations and reveal the distribution and occurrence of trace elements in different sulfides. The formation temperature and genesis of the Pb-Zn ore minerals were also constrained based on the deposit geology and trace element data. Trace elements were significantly different among different sulfides in the Pb-Zn mineralization stage of the deposit. Sphalerite primarily enriches Mn, Cu, Ag, Sn, and Pb and is the main carrier mineral of Ga, In, and Cd. Pyrite relatively enriches Tl, Sb, W, and Se, and pyrrhotite primarily enriches Ge. In sphalerite, Fe, Mn, Cd, Ga, In, Cu, Sn, Ag, and Ge exist by substituting for other elements (such as Zn). The replacement method of Ge is Ge4++2Cu(+)?3Zn(2+), whereas that of In (Ga) is In3+(Ga3+) + Cu+?2Zn(2+). In pyrrhotite, Ge is incorporated through coupling substitution, and the abnormal concentrations of Pb, Ag, and Se are caused by galena that has replaced pyrrhotite. In pyrite, W occurs as a solid solution. When galena replaces pyrite, it causes abnormal concentrations of Pb, Tl, Sb, and Ag. The sphalerite is characterized by high concentrations of high-temperature ore-forming elements (e.g., Fe, Mn, In, and Sn) and relatively low concentrations of Cd, Ge, Ga, and other elements. Thus, the sphalerite was formed at a medium-high temperature (288-341 & nbsp;C). The trace element characteristics of sphalerite are consistent with those of high-temperature hydrothermal deposits. The deposit geology, pyrite Co/Ni ratio (averaging 0.13, n = 29), S/Se ratio (averaging 173,905, n = 19), pyrrhotite Co/Ni ratio (averaging 0.10, n = 26), and binary diagram of trace elements in sphalerite indicate that Pb-Zn mineralization is related to the late-stage hydrothermal activity of skarn mineralization. The Pb-Zn mineralization and W-Mo(Fe) mineralization together constitute a skarn-type mineralization system. |
| WOS关键词 | PB-ZN MINERALIZATION ; SOUTHERN HUNAN ; FLUID INCLUSIONS ; MINOR ELEMENTS ; PROVINCE ; SPHALERITE ; GEOCHEMISTRY ; CONSTRAINTS ; CU ; PYRITE |
| 资助项目 | National Key Research and Development Program of China[2018YFC0603903] ; National Natural Science Foundation of China[41862007] ; National Natural Science Foundation of China[41402072] ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project[YNWR-QNBJ-2018-093] |
| WOS研究方向 | Geology ; Mineralogy ; Mining & Mineral Processing |
| 语种 | 英语 |
| 出版者 | ELSEVIER |
| WOS记录号 | WOS:000799352400002 |
| 资助机构 | National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project ; Yunnan Ten Thousand Talents Plan Young & Elite Talents Project |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/105985]  |
| 专题 | 地质与地球物理研究所_中国科学院矿产资源研究重点实验室 |
| 通讯作者 | Li, Bo |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China 3.Kunming Univ Sci & Technol, Fac Land Resources Engn, Kunming 650093, Peoples R China 4.Kunming Univ Sci & Technol, Fac Land & Resource Engn, Kunming 650093, Peoples R China |
| 推荐引用方式 GB/T 7714 | Chu, Xiangkai,Li, Bo,Shen, Ping,et al. Trace elements in sulfide minerals from the Huangshaping copper-polymetallic deposit, Hunan, China: Ore genesis and element occurrence[J]. ORE GEOLOGY REVIEWS,2022,144:19. |
| APA | Chu, Xiangkai.,Li, Bo.,Shen, Ping.,Zha, Zhihui.,Lei, Zhen.,...&Hu, Qian.(2022).Trace elements in sulfide minerals from the Huangshaping copper-polymetallic deposit, Hunan, China: Ore genesis and element occurrence.ORE GEOLOGY REVIEWS,144,19. |
| MLA | Chu, Xiangkai,et al."Trace elements in sulfide minerals from the Huangshaping copper-polymetallic deposit, Hunan, China: Ore genesis and element occurrence".ORE GEOLOGY REVIEWS 144(2022):19. |
入库方式： OAI收割
来源：地质与地球物理研究所
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