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通过研究航磁异常与纬向构造的关系,了解到基底构造上存在纬向构造。它为岩浆侵入提供了通道。盖层上的新华夏构造带与北东向的正,负磁异常带吻合较好。矿床明显地受构造控制。通过研究负异常带切割正异常带,证实了本区的新构造运动。高空(飞行高度1600米)航磁异常对查明深部岩体的产状、形态、延深及岩体间的关系,提供了信息。
By studying the relationship between the aeromagnetic anomaly and the weft structure, we know that there is a zonal structure on the basement structure. It provides access to magma intrusion. The new Huaxia tectonic belt on the caprock is well matched with the positive and negative magnetic anomalies in the NE direction. The deposit is clearly structurally controlled. The neotectonic movement in this area was confirmed by studying the negative anomalous zone and cutting the positive anomalous zone. Altitude (altitude 1600 m) aeromagnetic anomalies provide insight into the occurrence, shape, depth of deep rock mass and the relationship between rock masses.