A Permian intermediate-sulfidation epithermal Pb-Zn-Ag deposit in the northern margin of North China Craton
文献类型:期刊论文
作者 | Wang, Yongbin1,4,5,6; Cai, Jiaqi5,6; Liu, Li3; Zhou, Jiaxi4,5; Feng, Peiling5,6; Guo, Yunkang5,6; Lin, Song5,6; Guo, Yunpeng2 |
刊名 | ORE GEOLOGY REVIEWS
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出版日期 | 2023-07-01 |
卷号 | 158页码:15 |
关键词 | Zhajiagou Pb Zn-Ag deposit Intermediate-sulfidation epithermal deposit Rb-Sr dating H-O-C-S-Pb isotope |
ISSN号 | 0169-1368 |
DOI | 10.1016/j.oregeorev.2023.105492 |
英文摘要 | Recent Pb-Zn-Ag exploration in the northern margin of North China Craton has made significant new discov-eries. Here we report one Pb-Zn-Ag deposit in the Shaolanghe orefield with typical signatures of intermediate-sulfidation epithermal deposits. Zhangjiagou Pb-Zn-Ag mineralization occurs within the Early Permian quartz diorite and Late Permian andesite. Three mineralization stages were identified: white quartz--rhodochrosite-sulfide Pb-Zn-mineralization stage (I), smoky quartz-sulfide Pb-Zn-Ag-mineralization stage (II), and calcite-quartz non-mineralization stage (III). Four sphalerite samples yield the Rb-Sr age of 265.3 Ma, indicating that Pb-Zn-Ag mineralization was associated with the Late Permian andesite. The liquid-rich fluid inclusions of Stage I show low-medium temperatures of 190-270 degrees C and low salinities (1-3 wt%), and those of Stage III are slightly lower (190-250 degrees C, 0.5-2 wt%), suggesting a low-salinity, low-temperature H2O-NaCl fluid system for the Zhangjiagou deposit. The H-O-C isotopic signatures indicate a mixed fluid of magmatic water with meteoric water. S and Pb isotopes suggest magmatic source for Zhangjiagou Pb-Zn-Ag mineralization, most likely shallow hydrous intermediate magma. Collectively, these geological, geochronological, and geochemical features indicate that Zhangjiagou is an intermediate-sulfidation epithermal Pb-Zn-Ag deposit. |
WOS研究方向 | Geology ; Mineralogy ; Mining & Mineral Processing |
语种 | 英语 |
WOS记录号 | WOS:001008565400001 |
源URL | [http://ir.gig.ac.cn/handle/344008/74353] ![]() |
专题 | 中国科学院广州地球化学研究所 |
通讯作者 | Guo, Yunpeng |
作者单位 | 1.Yunnan Key Lab Sanjiang Metallogeny & Resources Ex, Kunming 650051, Peoples R China 2.Capital Normal Univ, Beijing 100048, Peoples R China 3.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China 4.MNR, Key Lab Sanjiang Metallogeny & Resources Explorat, Kunming 650051, Peoples R China 5.Yunnan Univ, Key Lab Crit Minerals Metallogeny Univ Yunnan Prov, Kunming 650500, Peoples R China 6.Yunnan Univ, Yunnan Key Lab Earth Syst Sci, Kunming 650500, Peoples R China |
推荐引用方式 GB/T 7714 | Wang, Yongbin,Cai, Jiaqi,Liu, Li,et al. A Permian intermediate-sulfidation epithermal Pb-Zn-Ag deposit in the northern margin of North China Craton[J]. ORE GEOLOGY REVIEWS,2023,158:15. |
APA | Wang, Yongbin.,Cai, Jiaqi.,Liu, Li.,Zhou, Jiaxi.,Feng, Peiling.,...&Guo, Yunpeng.(2023).A Permian intermediate-sulfidation epithermal Pb-Zn-Ag deposit in the northern margin of North China Craton.ORE GEOLOGY REVIEWS,158,15. |
MLA | Wang, Yongbin,et al."A Permian intermediate-sulfidation epithermal Pb-Zn-Ag deposit in the northern margin of North China Craton".ORE GEOLOGY REVIEWS 158(2023):15. |
入库方式: OAI收割
来源:广州地球化学研究所
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