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

• 摘要东帕米尔“层控碳酸岩型”铁铜金矿，形成于中元古代裂谷构造环境，产于中深变质相与中浅变质相转换部位，塔昔达阪群底部。