| Reference Type | Journal (article/letter/editorial) |
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| Title | Genesis of the Baiyun Gold Deposit in Northeast Hubei Province, China: Insights from In Situ Trace Elements and S-Fe Isotopes of Sulfide |
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| Journal | Minerals |
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| Authors | Song, Weifang | Author |
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| Liu, Jianzhong | Author |
| Zou, Yuanbing | Author |
| Liu, Xingping | Author |
| Long, Taocheng | Author |
| Zhu, Jiandong | Author |
| Fu, Shengbo | Author |
| Chen, Song | Author |
| Xiong, Yangfu | Author |
| Zhou, Runjie | Author |
| You, Jingjing | Author |
| Zhou, Xinqi | Author |
| Yang, Zaixi | Author |
| Fang, Jie | Author |
| Year | 2024 | Volume | < 14 > |
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| Issue | < 5 > |
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| URL | |
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| DOI | doi:10.3390/min14050517Search in ResearchGate |
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| Generate Citation Formats |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 17383549 | Long-form Identifier | mindat:1:5:17383549:6 |
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| GUID | 0 |
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| Full Reference | Song, Weifang, Liu, Jianzhong, Zou, Yuanbing, Liu, Xingping, Long, Taocheng, Zhu, Jiandong, Fu, Shengbo, Chen, Song, Xiong, Yangfu, Zhou, Runjie, You, Jingjing, Zhou, Xinqi, Yang, Zaixi, Fang, Jie (2024) Genesis of the Baiyun Gold Deposit in Northeast Hubei Province, China: Insights from In Situ Trace Elements and S-Fe Isotopes of Sulfide. Minerals, 14 (5) doi:10.3390/min14050517 |
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| Plain Text | Song, Weifang, Liu, Jianzhong, Zou, Yuanbing, Liu, Xingping, Long, Taocheng, Zhu, Jiandong, Fu, Shengbo, Chen, Song, Xiong, Yangfu, Zhou, Runjie, You, Jingjing, Zhou, Xinqi, Yang, Zaixi, Fang, Jie (2024) Genesis of the Baiyun Gold Deposit in Northeast Hubei Province, China: Insights from In Situ Trace Elements and S-Fe Isotopes of Sulfide. Minerals, 14 (5) doi:10.3390/min14050517 |
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| In | Link this record to the correct parent record (if possible) |
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| Abstract/Notes | The Baiyun gold deposit is a medium-sized deposit in northeastern Hubei around the southern margin of the Tongbai-Dabie metallogenic belt. However, its genesis has not been determined. The metallogenic process of the Baiyun gold deposit can be divided into three stages: quartz + feldspar, quartz + native gold + electrum + polymetallic sulfides, and quartz + pyrite + calcite + iron dolomite + illite. In this study, LA-ICP-MS was used for in situ trace element and isotope analyses in the main and late ore stage hydrothermal sulfides to evaluate the genesis and evolution of ore-forming fluids. Gold is positively correlated with Ag, Cu, Pb, Zn, and Te and the Co/Ni ratio is greater than 1. The S isotope values of Py1 and Py2 are β0.23β3.04β° and 1.27β6.09β°, respectively. As mineralization progressed, S isotope values increased. In situ S isotope values of the two types of galena symbiotic with pyrite in the main metallogenic stage are 2.97β3.47β°. In situ Fe isotopic values of pyrite are β0.05β0.82β°; values in the two stages are similar without significant fractionation. We inferred that the Baiyun gold deposit formed via magmatic mineralization related to the subduction of the Pacific Plate during the Yanshanian. |
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