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In Northern China, sandstone‐type uranium (U) deposits are mostly developed in Mesozoic‐Cenozoic basins. These U deposits are usually hosted in unvarying horizons within the basins and exhibit typical U‐forming sedimentary associations, which is referred to as U‐bearing rock series. This study describes the structural features of U‐bearing rock series within the main Mesozoic‐Cenozoic U‐producing...
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