首页|柴达木盆地北缘砂岩型铀矿目标层地球物理特征与找矿预测

柴达木盆地北缘砂岩型铀矿目标层地球物理特征与找矿预测

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柴达木盆地北缘地处柴北缘坳陷构造带,区内砂岩型铀矿成矿条件优越,具有较大的铀成矿潜力.文章基于铀矿地质条件,综合利用测井、能谱测量、活性炭、可控源音频大地电磁方法(Controlled Source Audio Magnetotelluric,CSAMT),总结目标层岩石物性、区内放射性特征,且选择典型剖面进行CSAMT实测,针对柴北缘铀成矿环境地球物理特征进行研究分析,并进行找矿预测.研究结果表明:区内目的层上干柴沟组骨架砂体发育较好,泥-砂-泥三元结构反映清晰,岩石物性变化明显,目的层灰色还原砂体(细砂岩、粗砂岩)中铀背景值高;典型剖面特征显示,区内呈现高铀、高钍、低钾的放射性特征,而铀矿化所赋存的目标砂体一般呈中高阻特征.文章根据地质-地球物理响应特征推断,区内电性剖面上中高阻电性层和地表目的层放射性异常之间、铀异常带局部膨大部位为找矿的有利部位,为柴北缘砂岩型铀矿勘查提供重要技术参考.
Geophysical Characteristics of the Target Layer and Exploration Prospects for Sandstone-type Uranium Deposits in Northern Qaidam Basin
Located in the northern margin of Qaidam uplift,the target layer in the northern Qaidam Basin is of favourable conditions for sand-type uranium mineralization.Based on uranium geological conditions,we analyzed the geophysical parameters of the target layer with multiple geophysical methods,such as geophysical logging,gamma ray spectrometry,activated carbon measurement and CSAMT method.The formation is of remarkable variation of geophysics parameters,the sanstone is with high uranium,high thorium and low potassium and uranium deposits in target sandstones are with high resistance.Sandstones are widely exist in the target layer Shangganchaigou Formation.The ternary structure of mud-sand-mud was quite well developed in the area,the grey reductant sandstones in the target layers,including fine sandstones and coarse sandstones,usually have high contents of uranium.According to geology-geophysics response characteristic,we concluded that radioactive anomaly is the direct clue to find out the location of uranium mineralization.Sector between two high radioactive areas,as well as inflated parts inside uranium anomaly area,are the potential positions for uranium deposits,which can be used as technical reference for uranium exploration in northern Qaidam Basin.

the northern Qaidam Basinsandstone-type uraniumgeophysical characteristicsradioactivity

赵旭、时志浩、郗昭、陈擎

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核工业二〇三研究所,陕西 西安 710086

柴达木盆地北缘 砂岩型铀矿 地球物理特征 找矿预测

中国铀业有限公司-东华理工大学核资源与环境国家重点实验室联合基金中国核工业地质局项目中国核工业地质局项目

2022NRE-LH-17202219-1202319-7

2024

铀矿地质
中国核学会铀矿地质学会

铀矿地质

CSTPCD
影响因子:0.714
ISSN:1000-0658
年,卷(期):2024.40(4)
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