Geology of Uranium Deposits

Jun 28th, 2015
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A silvery-white metallic chemical element in the actinide series of the periodic table with atomic number 92. It is assigned the chemical symbol U. The uranium establishing six isotopes, the most common of which are U-238 (146 neutrons) and U-235 (143 neutrons). Its density is about 70% higher than that of lead, but not as dense as gold or tungsten

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URANIUMA silvery-white metallic chemical element in the actinide series of the periodic table with atomic number 92. It is assigned the chemical symbol U. The uranium establishing six isotopes, the most common of which are U-238 (146 neutrons) and U-235 (143 neutrons). Its density is about 70% higher than that of lead, but not as dense as gold or tungsten. It occurs naturally in low concentrations in soil, rock and water, and is commercially extracted from uranium-bearing minerals such as uraninite.Geology of Uranium DepositsUranium occurs in a number of different igneous, hydrothermal and sedimentary geological environments.1. UNCONFIRMITY RELATED DEPOSITSUnconformity-related deposits arise from geological changes occurring close to major unconformities. Below the unconformity, the meta sedimentary rocks which host the mineralization are usually faulted and brecciated. Minerals are

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