Porphyry Mo and epithermal Au-Ag-Pb-Zn mineralization in the Zhilingtou polymetallic deposit, South China
文献类型:期刊论文
作者 | Wang, Yongbin1,4; Zeng, Qingdong1,2,4; Liu, Jianming1,2,4; Wu, Lin1,3; Qin, Kezhang1,2,4 |
刊名 | MINERALIUM DEPOSITA
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出版日期 | 2020-10-01 |
卷号 | 55期号:7页码:1385-1406 |
关键词 | Porphyry Mo mineralization Epithermal Au-Ag-Pb-Zn mineralization Zhilingtou South China |
ISSN号 | 0026-4598 |
DOI | 10.1007/s00126-019-00942-z |
英文摘要 | The Zhilingtou polymetallic deposit, South China, provides an excellent opportunity to investigate the magmatic-hydrothermal evolution of the porphyry Mo to epithermal Au-Ag-Pb-Zn ore spectrum. New zircon U-Pb, sphalerite(40)Ar/Ar-39, and pyrite Rb-Sr ages, together with previous molybdenite Re-Os ages, indicate that the granitic magmatism and Mo-Au-Ag-Pb-Zn mineralization were coeval and cogenetic in the Early Cretaceous (~ 113 Ma). Fluid inclusions and H-O isotope results have established the evolution from an early high-temperature H2O-NaCl magmatic fluid system (Mo mineralization), to a medium-temperature mixed fluid system of magmatic and meteoric water (Au-Ag mineralization), to a peripheral late-stage low-temperature H2O-NaCl meteoric water fluid system (epithermal Au-Ag-Pb-Zn mineralization). Moreover, the sulfur isotopic compositions (delta S-34 = 2.1-7.8 parts per thousand) of the sulfide minerals confirm a genetic link to the granitic magma. Lead isotope data from pyrite and the granite-rhyolite porphyries are similar, indicating that they share a common Pb source. The geochronological, geochemical, and isotopic lines of evidences consistently suggest that the porphyry Mo and epithermal Au-Ag-Pb-Zn mineralization formed in one magmatic-hydrothermal system. The porphyry-epithermal mineralization model for Zhilingtou has significant importance for prospecting work in South China, where Mo and associated Pb-Zn-Ag resources are abundant. |
WOS关键词 | TIME-SPACE DISTRIBUTION ; RE-OS GEOCHRONOLOGY ; U-PB ; RB-SR ; ISOTOPIC GEOCHEMISTRY ; ZHEJIANG PROVINCE ; FLUID INCLUSIONS ; INNER-MONGOLIA ; ORE-DEPOSITS ; NEW-MEXICO |
WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
语种 | 英语 |
WOS记录号 | WOS:000563170900011 |
出版者 | SPRINGER |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/97651] ![]() |
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 地质与地球物理研究所_岩石圈演化国家重点实验室 |
通讯作者 | Wang, Yongbin |
作者单位 | 1.Chinese Acad Sci, Inst Earth Sci, Beijing, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth Sci, Beijing, Peoples R China 3.Chinese Acad Sci, Inst Geol & GeophysW, State Key Lab Lithospher Evolut, Beijing, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Wang, Yongbin,Zeng, Qingdong,Liu, Jianming,et al. Porphyry Mo and epithermal Au-Ag-Pb-Zn mineralization in the Zhilingtou polymetallic deposit, South China[J]. MINERALIUM DEPOSITA,2020,55(7):1385-1406. |
APA | Wang, Yongbin,Zeng, Qingdong,Liu, Jianming,Wu, Lin,&Qin, Kezhang.(2020).Porphyry Mo and epithermal Au-Ag-Pb-Zn mineralization in the Zhilingtou polymetallic deposit, South China.MINERALIUM DEPOSITA,55(7),1385-1406. |
MLA | Wang, Yongbin,et al."Porphyry Mo and epithermal Au-Ag-Pb-Zn mineralization in the Zhilingtou polymetallic deposit, South China".MINERALIUM DEPOSITA 55.7(2020):1385-1406. |
入库方式: OAI收割
来源:地质与地球物理研究所
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