二连盆地中部古河道砂岩型铀矿综合地球物理响应特征研究
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本文为中核集团集中研发项目“龙灿”示范工程科研项目(第二阶段)(中核科发〔2018〕111号)资助的成果。


Study of integrated geophysical characteristics of paleo- valley sandstone- type uranium deposits in the middle of the Erenhot basin
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    摘要:

    二连盆地是我国北方重要的产铀盆地,近年来盆地中部相继发现一批古河道型砂岩铀矿床,预示该区域具有明显的找铀前景。结合该区铀成矿与地层结构、断裂、砂体、氧化还原过渡带等因素密切相关的地质认识,利用多种地球物理方法对成矿地质环境进行综合探测试验研究,分析研究成矿有利区平面上的重力异常、磁异常、放射性异常特征,以及剖面上的地震响应特征,半定量地建立了成矿有利区的综合地球物理预测模型:平面上,矿(化)体主要位于剩余重力异常的梯度带及附近,异常范围主要于-1×10-5~1×10-5m/s2,位于“两高夹一低”“U”型和“高、低”半“U”型土壤氡浓度异常带上,位于“高、低”半“U”型剩余磁异常的过渡带部位。剖面上,矿区主要位于宽缓“U”型充填状河道地震相体内,“U”型河道的两侧及内部多出现弯曲、间断、陡立等类似断层的同相轴特征,“U”型河道内部矿(化)体多呈中弱振幅、中低频率、低连续性的杂乱状地震反射特征。利用该模型在二连盆地中部预测了1片铀成矿有利区,后期通过调研分析预测区内钻孔资料,验证了该预测结果是有效的。表明本文建立的“重力+地震+测氡+磁测”组合找矿方法和预测模型,可提升二连盆地砂岩型铀矿勘查预测效果,可为类似地区铀矿勘查工作提供有益参考。

    Abstract:

    The Erenhot basin is an important uranium- producing basin in northern China. In recent years, a number of paleo- valley sandstone- type uranium deposits have been discovered in the middle of the basin, indicating a high potential for uranium prospecting in this area. Based on the principle that the uranium mineralization is related to stratigraphic, faults, sands, redox transition zones and other factors, comprehensive exploration research has been carried out to survey the mineralization geological environment, characteristics of gravity anomalies, magnetic anomalies and radioactivity anomalies on the plane, and the seismic response characteristics on the profile. Finally, a comprehensive geophysical prediction model for favorable areas has been established. On the plane, the mineralized body is mainly located in the gradient zone of residual gravity anomaly, the value range is -1×10-5~1×10-5m/s2, and is mainly located in the “U” type and “high- low” half “U” type soil radon anomaly zone, and in the “high- low” half “U” shaped transition zone of residual magnetic anomaly. On the profile, the mining area is mainly located in the seismic facies of a wide and gentle “U” shaped infilled channel; the two sides and inside of the “U” shaped channel are mostly curved, discontinuous, steep and other similar characters of faults, and the mineralized bodies show the characteristics of chaotic seismic reflections with medium- weak amplitude, medium- low frequency and low continuity. Using this prospecting model, a prospecting target area was preliminarily predicted in the middle of the Erenhot Basin and verified by geological drilling data. It shows that an integrated prospecting method and prediction model of “gravity+seismic+radon+magnetic” established in this paper can effectively improve the exploration and efficiency of sandstone uranium deposit prospecting in the Erenhot Basin, and provide a useful reference for the exploration of uranium deposits in similar areas.

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吴曲波,陈聪,杨龙泉,喻翔,高玲举,周俊杰,李必红,汪硕,刘武生.2021.二连盆地中部古河道砂岩型铀矿综合地球物理响应特征研究[J].地质学报,95(8):2521-2536.
Wu Qubo, Chen Cong, Yang Longquan, Yu Xiang, Gao Lingju, Zhou Junjie, Li Bihong, Wang Shuo, Liu Wusheng.2021. Study of integrated geophysical characteristics of paleo- valley sandstone- type uranium deposits in the middle of the Erenhot basin[J]. Acta Geologica Sinica,95(8):2521-2536.

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  • 收稿日期:2020-11-10
  • 最后修改日期:2020-12-25
  • 录用日期:2021-03-09
  • 在线发布日期: 2021-03-24
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