Geological characteristics of Tianshengtang Copper Deposit in the Dongchuan area, central Yunnan
  
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DOI:10.3969/j.issn.1671-4172.2016.06.008
KeyWord:Heishan formation; geological characteristics; genesis of deposit; central Yunnan
              
AuthorInstitution
ZHANG Shaoyun 江苏省有色金属华东地质勘查局,南京
XIAO Xiaoniu 江苏省有色金属华东地质勘查局,南京
CHENG Zengtao 江苏省有色金属华东地质勘查局,南京
LIU Dunhua 江苏省有色金属华东地质勘查局,南京
YI Fei 江苏省有色金属华东地质勘查局,南京
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Abstract:
      The Tianshengtang Copper Deposit lies in the Luoyin metallogenic belt of copper-polymetallic mineralization area in the Dongchuan area, central Yunnan. This paper mainly reports geological features of ore district, petrological and mineralogical characteristics of ore body, texture and structure of copper ores etc. Based on the above observation and analysis in combination with general comparative study with other famous deposits in this metallogenic belt, the genesis of the Tianshengtang Copper Deposit has been discussed. The study result shows that the genesis of the Tianshengtang Copper Deposit can be attributed to sedimentary-metamorphic superimposed by hydrothermal alteration type deposit.
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