The mineral assemblage of the ore deposit was formed by low to medium temperature hydrothermal fluids which, in turn, were low to medium temperature hot brines derived from the depth.

 
  • 礦床中發(fā)育一套典型的中低溫熱液成因的礦物組合,成礦流體性質(zhì)主要為來(lái)源于深部的中低溫熱鹵水。
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