在多数赤铁矿矿床上都有激电异常显示。
Over most hematite ore deposits induced polarization (IP) anomalies are observed.
本文用该法计算了二维极化体上近场源法的激电异常。
Using this method, the IP anomalies of NSI-PM on 2-d polarization body are calculated.
最后，通过分析激电异常，给出在该地区找水的几点建议。
At last, it gives some advice in searching of groundwater in this area by analyzing the DC IP abnormity.
在野外激电异常上，测定区分的视参数，无需反演求解真参数，可直接对异常源进行评价。
Apparent parameter determined in the field can be used directly to evaluate anomalous source without inversion of true parameter.
激电异常表现出高极化率低电阻率的电性特征，与矿区铜矿（体）石具有相同的电性特征。
The induced polarization anomaly is character of high in chargeability and low in electrical resistivity which is consistent with the electrical property of copper ore-body.
沿走向，激电异常在北东、南西两端有大幅度向外延伸趋势，可能是深部硫化物矿层向外延伸的反映。
The IP anomaly tends to extend considerably at the northeast and southwest ends, which might reflect outward extension of the deep sulfide ore bed.
沿走向，激电异常在北东、南西两端有大幅度向外延伸趋势，可能是深部硫化物矿层向外延伸的反映。
The IP anomaly tends to extend considerably at the northeast and southwest ends, which might reflect outward extension of the deep sulfide ore bed.
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