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- W2388898089 abstract "Shuicheng-Nayong manganese deposits belong to manganese-capped deposits in type of superior oxidized manganese.Geochemical study indicates that constant elements,microelements and trace elements in manganese ores and protore wholly take on thermal sedimentary characteristics,the siliceous limestone,silica-bearing limestone and bioclastic limestone is predominant protore beds of manganese-capped ores.They are of middle-low-thermal sediments within platform-ditch-facies belt of upper Maokou Formaiton in middle of Guizhou, which manganese source mainly come from the basalt of the Maokou Phase.Pure silicalite only exposed at surface is silica-bearing rocks of protore beds experiencing extreme oxidation at surface as additional production while generating oxidized manganese ores" @default.
- W2388898089 created "2016-06-24" @default.
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- W2388898089 date "2007-01-01" @default.
- W2388898089 modified "2023-09-28" @default.
- W2388898089 title "Geochemical Characteristics of the Shuicheng-Nayong Manganese Deposits in Guizhou" @default.
- W2388898089 hasPublicationYear "2007" @default.
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