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- W2518225164 abstract "Dongsheng 沙岩类型铀矿床是在最近的年里在中国的 Ordos 盆的北部分发现的 large-sizedsandstone-type 铀矿床之一。Dongsheng 铀矿床的 Geochemical 特征与氧化沙岩类型铀矿在中间的亚洲的区域扔的典型 interlayered 的那些显著地不同。铀矿床的液包体研究证明形成 uraniumore 温度在 150-160 ℃的范围以内。他们的 ~3He/~ 4He 比率在 0.02-1.00 R/Ra 的范围以内，关于外壳的乘那些的 5-40。他们的 ~(40 )Ar/~(36 ) Ar 比率改变 from584 到 1243，比大气的氩的价值高得多。δ ~(18 )O_(H2O ) 和从铀矿床的液包体的δ D 价值是 -3.0per 千 -- 8.75per 千并且 -55.8perthousand--71.3per 千分别地，反映天落水和 magmatic 的混合液体的特征。δ ~(18 )O_(H2O ) 和在铀矿存款的底部的高岭石层的δ D 价值是 6.1per 千并且 -77per 千分别地，显示出 magmatic 的特征。δ ~(13 )C_(V-PDB ) 和 O_(H2O ) 在铀矿方解石静脉珍视的δ ~(18 ) 是 -8.0per 千并且 5.76per 千分别地，显示出披风来源的特征。液包体的 Geochemical 特征显示为 Dongsheng 铀矿床的 ore-formationfluid 从外壳是天落水的混合液体和深来源的液体。这被建议侏罗记白垩纪 U 富有的变质岩和在普遍的花岗石北高举 Ordos 盆的区域被捱过并且 denudated 和形成 theore 元素，主要铀，被天落水搬运到 Dongsheng 区域，在铀矿被形成的地方。在中生代在浅层次在深内部和油 / 气体使液体成为了起来的 Ordos Basinduring 的 Tectonothermal 事件和 magmatic 活动沿着断层带和激活的破裂变弯，充满进忍受 U 碎屑状的沙岩，因此为铀矿的形成提供必要精力。" @default.
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- W2518225164 date "2007-01-01" @default.
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- W2518225164 title "Isotope geochemistry of ore fluids for the Dongsheng sandstone-type uranium deposit, China" @default.
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