铀矿床

yóu kuàng chuáng
  • Uranium deposit;uranium ore deposit
铀矿床铀矿床
铀矿床[yóu kuàng chuáng]
  1. 铀矿床三下开采模拟试验

    Simulated mining test of uranium ore deposit under river and buildings

  2. 新疆511铀矿床微量元素富集特征研究

    Trace element geochemistry of No. 511 uranium ore deposit in Xinjiang

  3. 新疆某铀矿床CO2地浸采铀试验研究

    A experiment of in-situ leaching of uranium with co_2 at a uranium deposit

  4. Q铀矿床四种基本岩性矿样的浸出研究

    Study on leaching of four fundamental lithological ore samples of q-uranium deposit

  5. 土壤热释CO2测量法在碳硅泥岩型铀矿床上的试验效果

    The effectiveness of applying soil thermal co_2 - releasing method to carbonaceous - siliceous - argillaceous rock type uranium deposits

  6. 622铀矿床岩矿石的REE地球化学特征

    REE geochemistry of rocks and ores in uranium deposit 622

  7. 铀矿床样品中~(239)Pu的测定及应用

    Determination and application of  ̄( 239 ) pu in the samples from the uranium deposit

  8. 西秦岭铀矿床热液石英Pb同位素组成及其应用

    Pb isotope compositions of quartz forming in U-bearing hydrothermal solution and their application to uranium deposits in the western Qinling

  9. 建立了DS铀矿床的多源信息描述模型,从中归纳总结出DS式铀矿田和铀矿床的综合找矿模型,并应用该模型完成了东胜&榆林地区砂岩型铀矿成矿潜力综合评价。

    Finally , the integrated evaluation of sandstone-hosted uranium metallogenic potentials is performed by using established models in Dongsheng-Yulin district .

  10. 加拿大McArthurRiver铀矿床成矿特点及在我国寻找相同类型铀矿床的几点认识

    Metallogenic character of McArthur River uranium deposit in Canada and some ideas for searching similar deposit in China

  11. 以TM假彩色合成图像的解译为依据,研究认为,此铀矿床受线、环、弧构造控制,分布范围不超出矿床所处火山塌陷盆地的边界。

    It is considered that the mineral deposit was controlled by the line , ring and arc through the interpretation of color-composite images .

  12. 文章还对砂岩铀矿床Ra-Rn平衡系数的确定方法进行了讨论,认为目前工作中采用矿心Ra分析结果与伽马测井Ra解释结果对比计算Ra-Rn平衡系数的方法,不够科学,也不尽合理。

    Determination methods of Ra-Rn equilibrium coefficient for sandstone-type uranium ore deposits are also discussed .

  13. 在白垩-第三纪的干旱、炎热古气候条件下,U经过强风化和热水浸出,在断陷带内富集成铀矿床&岩源活化型铀矿床。

    Under the dry and hot paleoclimate condition in the Cretaceous-Tertiary period , strong weathering and hot water leaching forced uranium to be concentrated into the " rock origin activation " type uranium deposits in the fault depressed zone .

  14. 研究证实,石油的氧化物&地沥青及部分油浸砂岩对U、Mo、Se、V、Re等元素具有较强的还原沉淀能力,从而构成了砂岩型铀矿床成矿作用的重要环节。

    It is founded that land bitumen , the oxides of petroleum and oil soaked sandstone are of high reduction and precipitation ability to U , Mo , Se , V and Re , and fairly important to uranium metallogeny .

  15. 按金铀矿床的成因类型可划分为:1.变质砾岩型Au-U矿床,2.沉积角砾岩型Cu-U-Au矿床;

    According to their genesis , Au-U ore deposits may be divided into six types : ( 1 ) metamorphic conglomerate Au-U type ore deposits ; ( 2 ) sedimentary breccia Cu-U-Au type ;

  16. XW铀矿床为产于花岗岩断裂破碎带中的大型热液铀矿床。

    XW uranium deposit is a large hydrothermal uranium deposit localized in fault zones within granites .

  17. 本文对赣杭构造带几个有代表性的火山岩型铀矿床进行了U-Pb同位素体系研究,证明铀源主要来自富铀的火山岩系。

    The study of U-Pb isotopic systems with representative volcanite type uranium deposits in Gan-Hang tectonic belts indicates that the uranium source was mainly derived from the rich uranium volcanic rock series .

  18. 山地铀矿床预测铀资源总量为25000t。

    The total uranium predicted resources of Shandi uranium deposit are up to 25 000 t.

  19. QJD铀矿床为一具有特殊形式的层间氧化带砂岩型铀矿床。

    QJD uranium deposit is a sandstone-type uranium deposit with the special shape of the interlayer oxidation zone .

  20. 对该走滑断裂系统的构造解析及铀矿床成矿地质特征的综合分析表明,NNE向走滑断裂直接控制了区域大规模热液铀成矿作用的发生。

    Analyses of structural pattern of this regional fault system and mineralization features of uranium ore deposits hosted in the strike slip faults of various scales indicate that Mesozoic Cenozoic hydrothermal uranium mineralization was directly controlled by NNE trending strike slip faulting .

  21. 文章研究了ZG复式花岗岩体东南部铀矿床的时、空分布规律与构造活动之间的关系,以及361铀矿床各种构造的控矿、赋矿特征。

    In this paper , the relationships between the distribution of uranium deposits located in the southeast of ZG granitic complex in time and space with the tectonic movements are studied . Meanwhile , the ore-controlling and ore-bearing features of various structures in uranium 361 are illustrated .

  22. 碎屑沉积岩沉积作用的高精度定年&自生磷钇矿离子探针UPb年龄测定钱家店砂岩型铀矿床UPb等时线年龄为53±3Ma和7±0Ma。

    HIGH PRECISION DATING OF DEPOSITION OF CLASTIC SEDIMENTARY ROCKS & U-Pb SHRIMP DATING ON AUTHIGENIC XENOTIME The U-Pb isochron ages of uranium ore-formation have been obtained as 53 ± 3 Ma and 7 ± 0 Ma .

  23. 砂岩型铀矿床成矿过程中腐殖酸作用机理探索

    Role of humic acids in the formation of sandstone-type uranium deposits

  24. 3701铀矿床成因的同位素地球化学研究

    Study on isotopic geochemistry of origin of the 3701 uranium deposit

  25. 土壤天然热释光法在相山火山岩型铀矿床中的应用研究

    The application research of Soil Thermoluminescence in Xiangshan VOLCANICS-HOSTED URANIUM DEPOSIT

  26. 302铀矿床是一个大型的隐伏花岗岩型铀矿床。

    Uranium deposit No. 302 is s large blind granitic one .

  27. 湘东地区某些典型铀矿床的成矿流体特征

    Characteristics of metallogenic fluids of typical uranium deposits in eastern Hunan

  28. 犬牙状微斜长石&钾交代型铀矿床中的标型矿物

    Hackly microcline & a typomorphic mineral in potash metasomatic uranium deposits

  29. 361铀矿床花岗岩特征和铀源

    Characteristics of granites and sources of uranium in No.316 uranium deposit

  30. 460铀矿床主要矿化期的同位素年龄

    Isotope age of principal mineralization period in uranium deposit No. 460