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Uraninite: a 2 Ga spent nuclear fuel from the natural fission reactor at bangombe in gabon, west africa

机译:铀铁矿:来自西非加蓬bangombe的自然裂变反应堆的2 Ga乏核燃料

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Uraninites from the Bangombe natural fission reactor (RZB) and 'normal' uranium -ore occur as fine veins in the sandstone host-rock as well as altered, broken, and slightly dispolaced grains in an illitic matrix, and in nodules and veins of solid bitumen. Inclusions of galena, (Y.Gd)-rich phosphates, a Pb-oxide and a Ti-oxide? were observed. Uraninites just below RZB were partially altered to a uranyl-sulfate. Three generations of uraninite were identified based on their PbO-contents of 8-11.06 wt
机译:Bangombe自然裂变反应堆(RZB)和“正常”铀矿中的铀铀矿以细砂岩出现在砂岩宿主岩中,并在坚硬的基质中以及在固体的结核和矿脉中发生改变,破碎和略微脱落的晶粒沥青。方铅矿,富含(Y.Gd)的磷酸盐,Pb氧化物和Ti氧化物的夹杂物?被观察。低于RZB的铀铀矿被部分改变为硫酸铀酰。根据PbO含量为8-11.06 wt

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