随着找矿方向和目标类型从硬岩转移到可地浸砂岩型铀矿，如何改进数据处理方法和异常分析方法就日益紧迫起来。
With the change of prediction type from harder rock to in-situ leachable sandstone-type uranium deposits, it is urgent to improve the data processing method and abnormal analysis method.
地浸法开采砂岩型铀矿床具有与常规开采无法比拟的优势，因此成为当前找矿的主攻类型。
With the comparative advantage, the in-situ uranium mining of sandstone-hosted uranium deposit becomes the most popular style of currently mining technology.
铀矿类型为层间氧化带砂岩型铀矿床。
The uranium deposits fall into the category of sandy deposits in interlayer oxidization zones.
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