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Metal Mine ›› 2015, Vol. 44 ›› Issue (09): 100-104.

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S,Pb Isotope Geochemical Characteristics of the Gaerqiong-Galale Gold-Copper Ore-concentrated Area

Bai Yun1,2,Zhang Zhi1,Chen Yuchuan3,Tang Juxing3,He Lin4,Yang Yi1   

  1. 1.College of Earth Science,Chengdu University of Technology,Chengdu 610059,China;2.The 605 Brigade of Geological Exploration and Resources Development,Meishan 620860,China;3.Institute of Mineral Resources,Chinese Academy of Geological Sciences, Beijing 100037,China; 4.No.2 Geological Party,Tibet Bureau of Geology and Mineral Resources Exploration,Lhasa 850000,China
  • Online:2015-09-15 Published:2015-11-20

Abstract: Taking the Gaerqiong-Glalae Cu-Au ore-concentrated area as the research object,the S and Pb isotope compositions characteristics of sulfide ore and the metallogenic material sources are analyzed.The results show that:①the δ34S value of the ore metal sulfides vary from -4.4‰ to 6.2‰,with the average δ34S value of 0.13‰,mainly between -2 ‰ and 1.5 ‰,and with the characteristics of tower distribution,it overall reflects the characteristics of mantle magma sulfur,but has been contaminated by a few of crustal sulfur;②the composition range of Pb isotope of the ore is large,showing the characteristics of mixed source of lead,the characteristics of μ value and tectonic environment discrimination diagram indicate that lead of the research region is originated in the mantle source region,mainly the upper crust and mantle mixed orogenic belt lead;③comparing with the Buza and Naruo deposit in Duolong ore-concentrated area and the Gaerqiong-Glalae Cu-Au ore-concentrated area,it is considered that the source of sulfur of the above ore-concentrated areas are both magmatic sulfur,and the ore-forming materials of Duolong ore-concentrated area is relatively deep with the environment of subduction,and the ore-forming materials of Gaerqiong-Galale ore-concentrated area is relatively shallow with the environment of collision.The above analysis results have a certain reference for the prospecting work in the research area.

Key words: S isotope, Pb isotope, Geochemical characteristics, Crust mantle mixed sources, Sources of ore-forming materials