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The article focuses on a study of genesis regarding strong Kaolinization of Ore-bearing Sandstone in the uranium deposit of Mengqiguer in China. Topics discussed include Mengqiguer deposit suffering from clay alteration, the presence of crystal morphology in the kaolinite formed during burial process, and decarboxylation of the organic matter in rocks.

The article discusses a study on fluid of Mengqiguer uranium deposit in China. It mentions that fluid inclusions located in quartz fragment fracture contain liquid brine and hydrocarbon-containing aqueous solution. It states that vitrinite reflectance on organic matter in sand bodies is ranged from 0.40 percent to 0.74 percent. It also mentions that ore-forming fluid consists of mineral water containing oxygen and uranium and reducing hydrocarbon.