Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (5): 1365-1382.doi: 10.13278/j.cnki.jjuese.201705104

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Origin and Evolution of Ore-Forming Fluids of Duhuangling and Jiusangou High-Sulfidation Gold Deposit in Yanbian

Men Lanjing1, Sun Jinggui2, Wang Haojun1, Chai Peng2, Zhao Keqiang2, Gu Alei2, Liu Chengxian1   

  1. 1. School of Prospecting and Surveying Engineering, Changchun Institute of Technology, Changchun 130021, China;
    2. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2016-12-12 Online:2017-09-26 Published:2017-09-26
  • Supported by:
    Supported by Science Research Foundation of Jilin Province (120160038,120140075), National Natural Science Foundation of China (40472050, 40772052 ) and Science and Technology Research Project of Education Department, Jilin Province from the 13th National Five-Year Plan (120160014)

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Abstract: Less than 10 km away from each other,Duhuangling and Jiusangou deposits are two typical high-sulfidation gold deposits in Yanbian. The fluid inclusions in quartz from alteration rocks and ores were analyzed by using micro thermometry, Raman microprobe,and noble gas isotope to reveal the origin and evolution of the ore-forming fluids. The fluid inclusions in the alteration stage and the early mineralization stage are mainly gas-liquid two-phase inclusions with major gases of CO2 and N2. The occurrence of a few high-salinity (33.4%-48.1%), high-temperature (410-460℃) fluid inclusions represent the mixing of a epithermal mineralization fluids with the porphyry system at depth. The fluid inclusions indicate that the homogenization temperature of the main mineralization stage is from 90℃ to 330℃, the salinity is 0.4%-44.9%,and the composition is dominated by H2O and a small amount of CO2. The coexistence of liquid-,vapor-rich inclusions and halite-bearing multiphase inclusions suggests a boiling event. These inclusions were trapped at depth between 100 and 500 m, representing the fluids related to the epithermal mineralization at Duhuangling and Jiusangou. The fluid inclusions in pyrite are characterized by the 3He/4He ratio of 0.009 6-0.020 6 Ra, 20Ne/22Ne ratio of 9.734-9.987, 21Ne/22Ne ratio of 0.030 9-0.040 6, and 40Ar/36Ar ratio of 1 302.4-4 433.6. Combined with the stable isotope data,these ratios suggest that the early ore-forming fluid was of high temperature and high oxidized magmatic gas carrying Au, Ag, Cu and other ore-forming elements,the mixing of the fluid in the crust led to the boiling process during the main ore-forming stage, and the liquid was dominated later by low temperature and low salinity atmospheric water.

Key words: fluid inclusion, noble gas isotope, Duhuangling gold deposit, Jiusangou gold deposit, Yanbian

CLC Number: 

  • P618.51
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