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- W2374483409 abstract "During earlier of this century,the geological brigade has found out the Shuicheng-Nayong manganese at vicinity of Shuicheng,which is attributed to the kind of superior oxidized manganese occurring within second member of Maokou Formation of the middle Permian.Oxidized manganese ores are just distributed at surface nearby,and 30~70m declined along the slope turn into primary manganese beds which contain manganese,minor manganese-bearing siliceous limestone,siliceous limestone,carbonaceous silicalite and limestone.The studies indicate that the original manganese protore strata is manganese-rich thermal sediments generating within platform-gully zone.Flow inclusion measured range between 105 and 178 celsius degrees.Manganese is source base in forming superior oxidized manganese,the manganese ore is infected by outer terms,especially by water actions,experienced the generation by leaching dirty out of protore beds and manganese concentration.It is a typical manganese-cap deposit in studing area.." @default.
- W2374483409 created "2016-06-24" @default.
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- W2374483409 date "2007-01-01" @default.
- W2374483409 modified "2023-09-23" @default.
- W2374483409 title "Geological Characteristics of the Shuicheng-Nayong Mangananese Deposit of Guizhou" @default.
- W2374483409 hasPublicationYear "2007" @default.
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