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Geology, mineral paragenesis and fluid inclusion studies of the Yueyang Ag-Au-Cu deposit, South China: implications for ore genesis and exploration

文献类型：期刊论文

作者Chi, Zhe1; Ni, Pei1; Pan, Jun-Yi1; Ding, Jun-Ying1; Wang, Yu-Quan2; Li, Su-Ning1; Bao, Tan1; Xue, Kai3; Wang, Wen-Bin4
刊名GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS
出版日期2018-11-01
卷号18期号:4页码:303-318
关键词intermediate-sulphidation fluid inclusion boiling the Yueyang Ag-Au-Cu deposit
ISSN号1467-7873
DOI10.1144/geochem2017-059
英文摘要The Yueyang epithermal Ag-Au-Cu deposit is located in the Zijinshan ore district in western Fujian Province, South China. Orebodies are predominately hosted by the Jurassic Zijinshan granite batholith and controlled by a group of NW-trending faults. Roughly all minerals were deposited in a single extended period, and three stages can be further defined: (1) the early sphalerite stage; (2) the base metal-silver stage; and (3) the post-mineralization stage. Microthermometric measurements on quartz- and sphalerite-hosted, liquid-rich fluid inclusions indicate that mixing and dilution of the ore forming fluids took place from early to late stages. However, fluid boiling may locally occur and lead to silver participation, as suggested by the presence of fluid inclusion assemblage consisting of coexisting liquid-rich and vapour-rich inclusions, and also indicated by adularia in Ag-bearing veins and the breccia type ore of bonanza grade. Compared with typical low-sulphidation epithermal deposits, the higher Ag/Au ratios and fluid salinities, Fe-poor sphalerite and large proportion of sulphide minerals suggest that the Yueyang deposit is best classified as an intermediate-sulphidation epithermal deposit. Since intermediate-sulphidation epithermal deposits favour a magmatic affinity and usually exhibit spatial and temporal association with high-sulphidation and porphyry deposits, mineral exploration at the adjacent area of the Yueyang deposit is promising.
WOS关键词GUANAJUATO MINING DISTRICT ; OHAAKI GEOTHERMAL SYSTEM ; FUJIAN PROVINCE ; NEW-ZEALAND ; EPITHERMAL ENVIRONMENTS ; HYDROTHERMAL SYSTEMS ; ZIJINSHAN OREFIELD ; STABLE-ISOTOPE ; VOLCANIC-ROCKS ; GOLD DEPOSITS
资助项目National Key R&D Program of China[2016YFC0600205] ; China Geological Survey[12120114028601]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000448970700004
出版者GEOLOGICAL SOC PUBL HOUSE
资助机构National Key R&D Program of China ; National Key R&D Program of China ; China Geological Survey ; China Geological Survey ; National Key R&D Program of China ; National Key R&D Program of China ; China Geological Survey ; China Geological Survey ; National Key R&D Program of China ; National Key R&D Program of China ; China Geological Survey ; China Geological Survey ; National Key R&D Program of China ; National Key R&D Program of China ; China Geological Survey ; China Geological Survey
源URL[http://ir.iggcas.ac.cn/handle/132A11/89141]  
专题地质与地球物理研究所_其他部门
通讯作者Ni, Pei; Pan, Jun-Yi
作者单位1.Nanjing Univ, Sch Earth Sci & Engn, Inst Geofluids, State Key Lab Mineral Deposits Res, Nanjing 210093, Jiangsu, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Zijin Min Grp Co Ltd, Shanghang 364200, Peoples R China
4.Fujian Inst Geol Survey, Fuzhou 350013, Fujian, Peoples R China
推荐引用方式
GB/T 7714		 Chi, Zhe,Ni, Pei,Pan, Jun-Yi,et al. Geology, mineral paragenesis and fluid inclusion studies of the Yueyang Ag-Au-Cu deposit, South China: implications for ore genesis and exploration[J]. GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS,2018,18(4):303-318.
APA Chi, Zhe.,Ni, Pei.,Pan, Jun-Yi.,Ding, Jun-Ying.,Wang, Yu-Quan.,...&Wang, Wen-Bin.(2018).Geology, mineral paragenesis and fluid inclusion studies of the Yueyang Ag-Au-Cu deposit, South China: implications for ore genesis and exploration.GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS,18(4),303-318.
MLA Chi, Zhe,et al."Geology, mineral paragenesis and fluid inclusion studies of the Yueyang Ag-Au-Cu deposit, South China: implications for ore genesis and exploration".GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS 18.4(2018):303-318.

入库方式： OAI收割

来源：地质与地球物理研究所

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