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以矿物学和矿床学为指导,从巴什布拉克铀矿床含矿层位下白垩统克孜勒苏群的人工重砂样品中分离和挑选矿物组分,经电子探针研究,首次在该矿床含矿层中发现胶硫钼矿、铀石和含钛铀矿物等新的矿物组分,丰富了本矿床的矿物组合。此外,对含矿层中有机质的含铀性进行分析,认为油气还原过程有2期,早期不含铀,晚期含铀,从而佐证了巴什布拉克铀矿床是红色杂岩系在油气还原退色过程中形成的砂岩型铀矿床。
Under the guidance of mineralogy and mineralogy, the mineral components were separated and selected from the artificial heavy sand samples from Cretaceous Kizilsu group in the ore-bearing layer of the Bashibulake uranium deposit. After the study of electron probe, The new mineral components such as glufosinate, uranium and titanium-bearing uranium minerals were found in the ore-bearing formations, enriching the mineral assemblage of this deposit. In addition, analyzing the uranium content of the organic matter in the ore-bearing layer, it is considered that there are two stages of the hydrocarbon reduction process, and the early uranium-free and late-stage uranium-bearing inclusions. This proves that the Bashibulake uranium deposit is a red complex in the process of hydrocarbon fading In the formation of sandstone-type uranium deposits.