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Uranium vein deposits are concentrations of uranium minerals, such as pitchblende, coffinite, and brannerite, in fractures, shear zones, and stockworks . The uranium minerals are commonly accompanied by quartz and/or carbonate gangue. The mineralization is, as a rule, lithologically and structurally controlled. The vein deposits occur either (a) in shear or mylonite zones in various geological environments (veins in shear zones), or (b) within granitic or syenitic plutons or in rocks mantling granitic batholiths

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