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微航磁异常与可地浸砂岩型铀矿床

Weak-aeromagnetic anomaly and in-situ leachable sandstone-type uranium deposit

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【作者】 江民忠李名松王怀武谢迎春张积运石岩

【Author】 JIANG Min-zhong,LI Ming-song,WANG Huai-wu,XIE Ying-chun,ZHANG Ji-yun,SHI Yan (Airborne Survey and Remote Sensing Center,CNNC,Shijiazhuang of Hebei Prov.050002,China)

【机构】 核工业航测遥感中心

【摘要】 可地浸砂岩型铀矿床由于其上覆盖层较厚,地表异常信息十分微弱,找矿难度相当大。该论文的目的就是探索与可地浸砂岩型铀矿床有关的航空物探信息,为此类矿床成矿预测提供依据。通过研究新疆伊犁盆地510、511、512等3个已知可地浸砂岩型铀矿床的航磁资料,发现这些矿床上方均存在5nT~20nT微航磁异常。根据可地浸砂岩型铀矿的成矿地球化学机制,探讨了微航磁异常的形成机理,结合试验区的实际预测成果,指出与氧化-还原过渡带有关的可地浸砂岩型铀矿床上方存在微磁异常,高精度航磁完全能探测到。微航磁异常是此类矿床的特征异常之一,可以作为一种重要标志信息运用于前期成矿预测。

【Abstract】 Anomaly the information over in-situ leachable sandstone type uranium deposit appears rather weak due to the thick cover,therefore,prospecting in this area is extremely difficult.The purpose of this paper is to search the aerogeophysical prospecting information relative to the formation of in-situ leachable sandstone-type uranium deposit.After careful study of aeromagnetic data of three known deposits No.510,511 and 512 in the southern rim of Yili Basin,this paper discovers that there are weak-aeromagnetic anomalies over this deposits,and makes further discussion on the forming mechanism of weak-aeromagnetic anomaly according to the metallogenetic geochemical mechanism of this type uranium deposit.Combining with the practical predictions,it concludes that there are weak-micromagnetic anomalies over in-situ leachable sandstone type uranium deposits related to redox transitional zone,and high precision aeromagnetic survey can detect these anomalies,so weak-aeromagnetic anomaly can be regarded as one of characteristic anomalies for this type deposit and can act as a kind of direct guiding information in the pre-phase metallogenetic prediction.

  • 【会议录名称】 中国核科学技术进展报告——中国核学会2009年学术年会论文集(第一卷·第1册)
  • 【会议名称】“创新——核科学技术发展的不竭源泉”——中国核学会2009年学术年会
  • 【会议时间】2009-11-18
  • 【会议地点】中国北京
  • 【分类号】P619.14
  • 【主办单位】中国核学会
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