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Geoscience ›› 2010, Vol. 24 ›› Issue (2): 237-244.

• Water Resource and Environment • Previous Articles     Next Articles

Metallogenic Characteristics of Barite and Witherite of the Barium Metallogenic Belt in Southern Qinling Mountains

 TUN  Qing-Hua 1, 2, LIU  Jia-Jun1, 2 , ZHANG  Nai3 , LIU  Zhen-Jiang1, 2   

  1. 1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing100083, China;
    2. School of Earth Sciences and Resources, China University of Geosciences, Beijing100083, China;
    3. Research Institute of Petroleum Exploration and Development, PetroChina, Beijing100083, China
  • Online:2010-04-20 Published:2010-05-10

Abstract:

More than 70 witherite and barite deposits  (or points) are located in Southern Qinling Mountains, which is a unique large Ba metallogenic belt in the world. By microthermometry analysis, the peak of fluid inclusions homogeneous temperature has a increasing trend from barite to witherite. The δ34S values of barite of the deposits are higher than those of the same period water of ocean basin (except one δ34S value of barite of Wenyu deposit, which is close to those of the same period water of ocean basin),which shows that the 34S enrichment in barite could be due to the reduction from germs to sulfate.Witherite deposits of Southern Qinling exist different ranges of δ13C and δ18O value, and C of witherite comes from reaction of organic matter.According to thermodynamics data, temperatue below 162.42 ℃ is favourable to forming barite ore;when temperature is over 162.42 ℃, and there is enough CO32-  (from reaction of organic matter), it is favourable to forming witherite in sea water.In the late period of forming barite deposits,if Ba2+ appears deficient in hydrotherm, and  CO32-  (from reaction of organic matter)is enough and temperature is over 16242 ℃ in sea water,CO32- will metasomate the SO42-  of barite to form metasomatic type witherite.

Key words: Southern Qinling, barite, witherite, fluid inclusion, S, C and O stable isotope

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