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对阿希金矿床高精度磁测结果分析，发现了环状磁异常，它是火山岩地区控矿构造—环状构造的反映。对该异常进行了延拓处理，得出其浅部为环状和放射状断裂，深部为南北向断裂。对该矿床又作了四道γ能谱测量，发现它可以清晰的划分矿化蚀变带与围岩的界线，其基本规律是：钾道和总道含量在矿化蚀变带上明显升高，而钍道则明显下降
Analysis of the high-precision magnetic measurement results of the Axi gold deposit revealed a ring-shaped magnetic anomaly, which is a reflection of the ore-controlling structure in the volcanic area - ring structure. The continuation of the anomaly, draw its shallow ring and radial fracture, deep north-south fracture. The deposit was made four gamma spectrometry and found that it can be clearly divided between mineralized alteration zone and the surrounding rock boundaries, the basic law is: potassium and total tract of mineralization in the alteration zone was significantly higher High, while thorium is significantly decreased