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辉绿岩中氟的可淋失比例与原岩中氟含量存在正相关关系。The leachable fluorine in diabase is in direct proportion to its fluorine concentration.
按照该理论，我们发现了我国第一个万吨级可地浸砂岩型铀矿床。According to the theory, we found a ton of first-situ leachable sandstone-type uranium deposit.
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伊犁盆地是我国可地浸砂岩铀矿床的主要产出区。Yili basin is the main occurrence region of in-situ leachable sandstone-type uranium deposits in China.
对密封垫片中的可溶性氯离子加以检测和控制是防止垫片导致密封件腐蚀的重要措施。The testing and control of leachable chloride in seal gaskets can prevent seal faces from corrosion caused by gaskets.
舍伯吐地区位于松辽盆地西南部，主要找矿目的层为第三系。Tertiary is the target layer for exploring in-situ leachable uranium deposit in Shebotu area, southwest Songliao Basin.
经在二连盆地可地浸砂岩型铀矿床上的试验，表明其对深部铀成矿沉积地质环境的研究和铀矿定位具有实用价值。The authors also enumerate several examples in Kp survey at in situ leachable sandstone type uranium deposit in Erlian basin.
近期，在不断的对该盆地进行考察之后发现，其蕴藏着大量可地浸砂岩型铀矿。Recently, after the ongoing visit to the basin, it found that it contained a large number of leachable sandstone-type uranium deposits.
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其中511、513、512等矿床为可地浸砂岩型铀矿床，受层间氧化带控制非常明显。The uranium deposits 511, 513 and 512 belong to in-situ leachable sandstone-type uranium, strictly controlled by interlayer oxidization zones.
伊犁盆地南缘中、下侏罗统水西沟群产有数个可地浸的砂岩型铀矿床。Several in-situ leachable sandstone-type uranium deposits are hosted in the Shuixigou Group, Middle-Lower Jurassic in the southern margin area of Yili basin.
理论和实践表明，在可地浸层间氧化带型砂岩型矿床上可观察到明显的自然电位异常。Theory and practice indicates that an evident spontaneous potential abnormity can be observed in sandstone uranium deposits in situ leachable inter layered oxidation zone.
伊犁盆地南缘是典型的可地浸层间氧化带砂岩型铀矿产出区，近年来诸多单位对其控矿因素、成矿环境与成矿远景进行了研究。At present, the southern flank of the Yili basin is a typical area for the occurrence of in situ leachable interlayer oxidation zone type sandstone hosted uranium deposits in China.
结合砂岩型铀成矿理论，探讨了砂岩型铀成矿与沈积相的关系。Further, the relationships between the sedimentary facies and the sandstone-type uranium mineralization are discussed according to the theory about leachable uranium mineralization.
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在可地浸砂岩型铀矿床的找矿中，由于水位资料匮乏，水动力场研究受到很大的限制。A large restriction exists in acquiring hydrodynamic field due to the insufficient data of water level in the course of exploration of in-situ leachable sandstone-type uranium deposit.
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.