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Asian Gold reserves DB
Rodnikova Gold Mine (Russia)
      paishanlou gold mine (china)
      gaolong gold mine (china)
      ..................
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اولينقبليبعديآخرين
   Geology
   The geology at Rodnikova is similar in nature to that at Asacha. The deposit consists of a number of north-south trending veins hosted by a brittle dolerite intrusion, which is emplaced into a suite of volcanic rocks. Other volcanic rocks in the surrounding area have been interpreted to post-date the diorite but pre-date the veins. As at Asacha, it is postulated that the deposit is contained within a collapsed or eroded volcanic edifice.
   The veins occupy a north-south structural trend and occur as a number of parallel veins the principal of which are steeply dipping, while further to the west the veins display moderate dips to the east.

Geological map of Rodnikova Gold mine
    It is postulated that these veins may converge at depth to form a single vein. Post-mineralisation landslides have obscured the southern continuation of the veins although their presence has been confirmed by drilling.
   As at Asacha, Rodnikova is classed as a low sulphidation adularia-sericite epithermal type vein deposit with the gold being predominantly associated with dark sulphidic bands within the quartz veins.
  
 
 
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