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Published byAbel Charles Modified over 9 years ago
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Uranium Deposits
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Geography of U Deposits – USA States with mineable resources States currently producing U 3 O 8
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Geography of major U Deposits – USA
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North Dakota’s Uranium Deposits
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Sedimentary Host Rocks Sandstones and Arkoses –Porous –Permeable –Lower pH than incoming water Coal and lignite beds –Also have low pH compared to inflowing water
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Sedimentary-hosted Uranium Deposits Very high tonnage but lower grade (compared to unconformity type) U transported by ground water U deposited as water encounters a reducing environment (organic matter or gas, sulfide minerals) Drop in pH results in precipitation of U minerals in pore spaces.
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Prerequisites for a Sedimentary- hosted Uranium deposit 1)Source of U 2)Coarse sands with good porosity and permeability 3)Ground water flow (naturally oxygenated) – ideally channelized, high rate of flow 4)Reduction zone – heavy minerals, decaying organic matter
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Uranium Deposit host Rocks Wasatch Formation - PRB
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Fort Union Formation - PRB
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Wind River Formation, Puddle Springs Member – Gas Hills
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Wind River Formation Shirley Basin
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Battle Spring Formation Great Divide Basin
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