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磁异常是地表及其深部岩石磁性差异的信息,是各种磁性地质体的综合反映。航空磁测不仅能反映地表的地质特征,而且能探测隐伏深部的磁性体,从而为寻找与磁性体有关的铀矿床提供了可能性。
Magnetic anomaly is the magnetic difference between the surface and its deep rock. It is a comprehensive reflection of various magnetic geologic bodies. Aeromagnetic surveying not only reflects the geologic features of the earth’s surface, but also can detect buried deep magnetic bodies, thus providing the possibility of searching for magnetic-related uranium deposits.