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中国北方砂岩型铀矿中铀的储集空间类型探讨
引用本文:陈路路,聂逢君,严兆彬,殷栋法,杨冰彬,李晓东,李剑琦,刘杰.中国北方砂岩型铀矿中铀的储集空间类型探讨[J].沉积与特提斯地质,2013(4):80-85.
作者姓名:陈路路  聂逢君  严兆彬  殷栋法  杨冰彬  李晓东  李剑琦  刘杰
作者单位:[1]东华理工大学核资源与环境国家重点实验室培育基地,江西南昌,330013 [2]核工业270研究所,江西南昌,330000 [3]湖南核工业地质调查院,湖南长沙,410000 [4]甘肃省地矿局第二地质矿产勘察院,甘肃兰州,730020
基金项目:国家自然科学基金资助项目(编号:40972067)
摘    要:在中国北方的大多数沉积盆地里均发现有砂岩型铀矿床或铀矿化现象。通过样品薄片电子探针背散射图像分析,结合前人对各盆地砂岩型铀矿中铀矿物的赋存状态及近年来铀储层的研究成果,认为中国北方砂岩型铀矿中铀矿物的主要储集空间类型可分为原生孔隙(主要是炭屑)、缩小(残留)粒间孔隙、次生溶蚀孔隙、晶间孔隙及微裂缝。通过对铀储层孔隙类型的分析讨论,有利于进一步从微观了解砂岩铀储层内部结构的不均一性及铀矿物的成因。

关 键 词:砂岩型铀矿  铀储层  储集空间
收稿时间:2013/3/28 0:00:00
修稿时间:2013/4/10 0:00:00

An approach to the uranium reservoir space types in the sandstone-type uranium deposits in northern China
CHEN Lu-lu,NIE Feng-jun,YAN Zhao-bin,YIN Dong-f,YANG Bing-bin,LI Xiao-dong,LI Jian-qi,LIU Jie.An approach to the uranium reservoir space types in the sandstone-type uranium deposits in northern China[J].Sedimentary Geology and Tethyan Geology,2013(4):80-85.
Authors:CHEN Lu-lu  NIE Feng-jun  YAN Zhao-bin  YIN Dong-f  YANG Bing-bin  LI Xiao-dong  LI Jian-qi  LIU Jie
Institution:1. Key Laboratory of Nuclear Resources and Environments, East China Institute of Technology, Nanchang 330013, Jiangxi , China; 2. No. 270 Institute, China National Nuclear Corporation, Nanchang 330000, Jiangxi , China; 3. Hunan Institute of Geological Survey, Hunan Bureau of Nuclear Geology, Changsha 410000, Hunan , China; 4. No. 2 Institute of Geology and Mineral Exploration, Gansu Bureau of Geology and Mineral Resources, Lanzhou 730020, Gansu, China)
Abstract:The sandstone-type uranium deposits or uranium mineralization were discovered in most of sedimentary basins in northern China. The authors propose,in terms of backscattered electron images analysis in this study and previous results of research concerning the uranium occurrence and uranium reservoirs in the sandstone-type uranium deposits in some sedimentary basins in northern China that the main reservoir space types in the sandstonetype uranium deposits in northern China include the primary pores( dominatedly charcoal debris),narrow or residual intergranular pores,secondary dissolution pores,intercrystal pores and microfissures. The diagenesis and postdiagenetic alteration may change the pore structures and types,and facilitate the reduction and precipitation of uranium.
Keywords:sandstone-type uranium deposit  uranium reservoir  reservoir space
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