摘要
激发极化法是根据岩石、矿石的激发极化效应来寻找金属矿的一种物探方法。通过对该工区进行中梯扫面及激电测深,大致圈出了矿化异常体规模,而且物探测试中的几处低阻高极化异常体都在构造带中并受构造带的控制,与矿化体有密切的关系。
Induced polarization method is a geophysical prospecting method for metal deposits based on the induced polarization effect of rocks and ores. The scale of mineralization anomaly body is roughly delineated by means of mid-ladder sweep and IP sounding in this area. Several low resistivity and high polarization anomaly bodies in geophysical prospecting test are in the structural zone and controlled by the structural zone, which is closely related to the mineralization body.
引文
[1]刘国兴.电法勘探原理与方法.北京:地质出版社,2008.
[2]傅良魁.激发极化法[M].北京:地质出版社,1982.
[3]《时间域激发极化法技术规程》(DZ/T 0070-93).