CAJ | 학술논문

在实验室对人工合成的岩、矿石标本进行了复电阻率特性测量，利用标本的复电阻率振幅频谱曲线反演求得其Cole—Cole模型参数，讨论了各标本的Cole—Cole模型参数的异同，得出了可以通过标本的4个模型参数（ρ0、m、τ、C）区分良导电、高极化率岩、矿石，达到区分矿与非矿的目的的结论，为在有干扰地层（黄铁矿、炭质层等）的地区开展物探电法找矿工作提供了试验依据。
재실험실대인공합성적암、광석표본진행료복전조솔특성측량，이용표본적복전조솔진폭빈보곡선반연구득기Cole—Cole모형삼수，토론료각표본적Cole—Cole모형삼수적이동，득출료가이통과표본적4개모형삼수（ρ0、m、τ、C）구분량도전、고겁화솔암、광석，체도구분광여비광적목적적결론，위재유간우지층（황철광、탄질층등）적지구개전물탐전법조광공작제공료시험의거。
Synthetic rocks and ore samples＇ complex resistivity were measured in this experiment,used Cole-Cole model to fit the complex resistivity spectrum curve follow the system theory, obtained four Cole-Cole model parameters,discussed the similarities and differences of Cole-Cole model parameters between various samples,obtained the conclusion that can distinguish good conductivity and high susceptibility rock or ore by the four model parameters （ρ0、m、τ、C） and distinguish mine and non-mine, provide the experimental basis that can carry out geophysical electrical prospecting in interference formation （pyrite, carbonaceous layer, etc.） areas.