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本文首次提出剩余视极化率异常的概念和求 取公式。利用已知焦家式深部金矿床上所 测得大、 小两种极距激电中梯视极化率ηα,而求得的剩余视 极化率ηαsy,经与已知深部矿床对比,发现其ηαsy异 常具有单纯反映矿体的能力,而与破碎带内的强蚀 变岩石所形成的极化率异常无关。
This paper presents for the first time the concept of residual apparent polarizability anomaly and its formula. The apparent apparent polarizability ηαsy, obtained from the known polar polarizabilities ηα of the large and small polar gauge ladders in the deep gold deposits, is known to be comparable with the known deep deposits The ηαsy anomaly has the ability to reflect the orebody, but has nothing to do with the abnormal polarization rate formed by the strongly altered rocks in the crust.