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Metal Mine ›› 2008, Vol. 38 ›› Issue (03): 114-117.

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Geological Characteristics of Tianyu Cu-Ni Sulfide Deposit in East Tianshan, Xinjiang

Song Linshan1,Wang Lijin1,Deng Gang2,Li Jun2,Chai Fengmei1   

  1. 1.Xinjiang University; 2.No. 6 Exploration Brigade, Xinjiang Bureau of Geological and Mineral Resource Exploration & Development
  • Online:2008-03-15 Published:2011-07-21

Abstract: Tianyu Cu-Ni Sulfide Deposit in East Tianshan, Xinjiang is located in the middle of Weiya-Mazhuangshan Cu-Au-Wu-Mo-Fe mineralization belt in the middle of Central Tianshan poly-metallic mineralization belt, south of Shaquanzi fault at the north edge of the Central Tianshan Massif. In the recent years, several poly-metallic deposits have been found in this belt, including Jiyuan, Huanglongshan, Caixiashan and Baishiquan CU-Ni deposits, Tianyu nickel deposit, East Caixiashan, Shaquanzi and Baoyuan Ag-Pb-Zn deposits. A preliminary study was made on the geological characteristics of Tianyu Cu-Ni sulfide deposit in this area.

Key words: East Tianshan, Tianyu Cu-Ni sulfide deposit, Geological characteristics