The stratabound carbonate iron-copper-gold belt in the Eastern Pamir was formed in the Lower Taxidban group in a Mid Proterozoic rift.

 
  • 摘要東帕米爾“層控碳酸巖型”鐵銅金礦,形成于中元古代裂谷構造環(huán)境,產(chǎn)于中深變質(zhì)相與中淺變質(zhì)相轉換部位,塔昔達阪群底部。
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