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Volume 24 Issue 2
Apr 2013
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Article Contents
Igor'V Kemkin, Raisa A. Kemkina. Microheterogeneity of the Koupol Deposit Fahlores as a Reflection of Changing of Physicochemical Parameters of the Ore-forming Solution. Journal of Earth Science, 2013, 24(2): 179-187. doi: 10.1007/s12583-013-0321-6
Citation: Igor'V Kemkin, Raisa A. Kemkina. Microheterogeneity of the Koupol Deposit Fahlores as a Reflection of Changing of Physicochemical Parameters of the Ore-forming Solution. Journal of Earth Science, 2013, 24(2): 179-187. doi: 10.1007/s12583-013-0321-6

Microheterogeneity of the Koupol Deposit Fahlores as a Reflection of Changing of Physicochemical Parameters of the Ore-forming Solution

doi: 10.1007/s12583-013-0321-6
Funds:

the President of the Russian Federation 5162.2010.5

the Federal Program of Russia 02.740.11.0723

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  • Corresponding author: Kemkin Igor'V, kemkin@fegi.ru
  • Received Date: 23 Mar 2012
  • Accepted Date: 21 May 2012
  • Publish Date: 01 Apr 2013
  • New data on a zonal structure of the Koupol deposit fahlores grains are given, and features of their chemism are shown. The fahlores chemical composition within the zones evolves from essentially arsenious (Fe-tennantite and Zn-tennantite), through mixed fahlores (Zn-tennantite-tetrahedrite arsenious and Zn-tennantite-tetrahedrite antimonous), to essential antimonous (Ag-bearing Zn-tetrahedrite). Varying chemical composition manifested as mineralogical-geochemical zonation of the fahlores grains is caused by changes of physicochemical conditions of the ore forming process during the time.

     

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