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Metal Mine ›› 2014, Vol. 43 ›› Issue (08): 95-98.

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Geochemical Characteristics of Sulfur and Lead Isotopes of the Polymetallic Deposit in Mabugang

Sun Ning1,2,Luo Wei2,Kong Fanqian1,Wei Longming1,Wei Hongjun3   

  1. 1.College of Earth Science,Guilin University Of Technology,Guilin 541006 China;2.South Geology Investigation Institute of China non-ferrous Metals Resource Geological Survey,Changsha 410001 China;3.China Non-ferrous Metals Resource Exploration Co.,Ltd.,Changsha 410001,China
  • Online:2014-08-15 Published:2015-03-31

Abstract: According to the S,Pb isotope survey results of the six pieces of ore samples from the polymetallic deposit in Mabugang,the parameters and graphic of S,Pb isotopes were calculated by Geokit software,to discuss the source of ore-forming materials.Results showed that: the δ34S of sulfide mainly varies from -4.6‰ to +3.2‰,which reflects the composition characteristics of magmatic sulfur.δ206Pb/δ204Pb of Pb isotope among minerals is from 18.6 to 18.8,δ207Pb/δ204Pb is from 15.7 to 5.8,and δ208Pb/δ204Pb is from 39.07 to 39.25.All these display a normal lead character,which are similar to the lead isotopic composition at the upper crust of orogenic belt.In summary,the analysis indicated that the metallogenic sources of Mabugang polymetallic deposit mainly come from the upper crust.Its tectonic background is under cratonization action,and is basically consistent with the actual tectonic environment of mine field at active continental margin.

Key words: Sulfur isotope, Lead isotope, Polymetallic deposit