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- W2376039092 abstract "Genduo mineralized area is discovered lately by our institute in Tibet.The ore bed is Jiapila group in upper Triassic that sediment alternately by recede sedimentary tidal-flat facies,seashore facies and seashore outside shelf facies.The whole ore bed spreaded northwest,4000m length,0.4~13m large(thick),average 3m thick.The mineralization spreaded as floor and lens body,the ore bed(body) transition with wall rock gradully.There is 0.003%~0.855% uranium in the ore,average 0.02%~0.30%.We elementary think the mineralization are sediment cause and hydrothermal cause.The type maybe is granite outside touch belt type or sediment alteration type." @default.
- W2376039092 created "2016-06-24" @default.
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- W2376039092 date "2012-01-01" @default.
- W2376039092 modified "2023-09-27" @default.
- W2376039092 title "The uranium mineralization character of Genduo area Zuogong county in Tibet" @default.
- W2376039092 hasPublicationYear "2012" @default.
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