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[an error occurred while processing this directive]Composition Typomorphic Characteristics of Pyrite and Its Genetic Implication for Gold Deposits in Tongdao County,Hunan Province
Received date: 2020-06-11
Revised date: 2020-08-18
Online published: 2020-11-05
Tongdao county is located in southwest of Xuefeng arc structure belt,there are some small and medium-sized gold deposit such as Jinkeng deposit,Huanggou deposit and Chaxi deposit.Few research have done in this area,in order to discuss the genesis of gold deposit,this paper focuses on the genetic mineralogy study about pyrites of different occurrence.The macroscopic geological characteristics of the three deposits show that the wall rocks of the ore body are all low-grade metamorphic sandstone slate.Strong silicification alteration and fading alteration occurred in the surrounding rocks near ore-bearing quartz veins in Jinkeng mining area.The dip angle of quartz vein is steep in Huanggou mining area,and the tendency is southeast or northwest,the fracture filled with quartz vein is shear fracture.The ore bearing quartz veins in Chaxi mining area are mainly NW steeply dipping veins and their branch gently dipping veins.The gold orebodies are mainly quartz vein type or altered rock type.The ore contains pyrite,arsenopyrite and other sulfides.Generally,the ore vein with more pyrite content has a relatively high gold grade,suggesting that pyrite is the main gold-carrying mineral.Rock-mineral determination show that pyrite is mainly cubic and pentagonal dodecahedron and other semi automorphic granular in three gold deposit.MLA(mineral liberation analyzer) scanning results show that gold was produced in pyrite farcture or pyrite intergranular in Huanggou gold deposit.Major element results analyzed by EPMA show that the pyrites in general are rich in iron and deficient in sulfur,containing a small amount of arsenic.The δFe-δS diagram shows that all points from three deposit concentrate in a narrow range,which is consistent with metamorphic hydrothermal gold deposit.Trace elements results analyzed by LA-ICPMS show that average Co/Ni value for Jinkeng pyrite samples is less than 1,which implies the fluid are from metamorphic water mainly.There are two kinds of pyrites in Huangou deposit,one produced in fine quartz vein,the Co/Ni value is near 0,the other zonal pyrite produced in wall rocks near ore,the Co/Ni value of core and edge are quite different,which implies the zonal pyrites have multi-stage growth history.As-Co-Ni diagram show that pyrites from Jinkeng and Huanggou deposit are mainly metamorphic hydrothermal type,and the metallogenic temperature should be medium low temperature.Compared with that of Huanggou gold deposit,pyrites collected from Jinkeng deposit has higher trace element content(e.g.,Au,Ag,Cu,Pb and Zn),which suggests that the Jinkeng area has more better prospecting potential.According to less private mining,we infer the gold body are eroded slightly,there is still great prospecting in deep part of the deposit.
Hua GAO , Yuhua XIE , Liang YANG , Zhe ZHANG , Xinxing KE , Xiaomin LIU , Jianbiao LUO , Qi LIU , Jishun LIU , Zhilin WANG , Hua KONG . Composition Typomorphic Characteristics of Pyrite and Its Genetic Implication for Gold Deposits in Tongdao County,Hunan Province[J]. Gold Science and Technology, 2020 , 28(5) : 712 -726 . DOI: 10.11872/j.issn.1005-2518.2020.05.105
http://www.goldsci.ac.cn/article/2020/1005-2518/1005-2518-2020-28-5-712.shtml
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