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多年实践证明,对于普查被剥蚀的金属矿床,次生岩石晕具有重要找矿意义。根据次生岩石化学晕进行了普查隐伏矿化的工作。工作地区位于由下部构造岩石层组成的古老隆起的斜坡范围内,是铀-钼建造矿床的远景区。裂隙-脉型的内生矿化产于重叠式拗陷
Years of practice have proved that for census denuded metal deposits, secondary rock halo has an important prospecting significance. According to secondary rock chemical halo conducted a census of hidden mineralization work. The work area is located within the range of ancient uplifted slopes formed by the lower structural rock layers and is a vista of the uranium-molybdenum deposit. Fissure-vein-type endogenous mineralization occurs in overlying depressions