The Geological Feature of Dadi Hematite Deposit of Simao Port in Puer, Yunnan Province
详细信息   
摘要


     The hematite deposit is in the unconformity-fauh fractured zone between Manghuai Formation and Daxinshan Formation. The ore body is veined, in flaky aggregate and crustification. It belongs to the volcanic eruption intercalating sedimentation metamorphism type, which is formed by the active margin fissure eruption-sedimentation.

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