1) microresistivity anomaly
微电阻率异常
3) apparent resistivity anomaly
视电阻率异常
1.
Based on the obtained simulation result of typical numerical value and with the help of information section of apparent resistivity anomaly,the anomalies are analyzed and studied,and the anomaly features and their variation regularity are summarized,and on this basis,the anomaly features of ot.
在跨孔条件下，利用积分方程法计算了孔区内外不同位置、不同产状的三维椭球体模型视电阻率异常。
2.
The characteristics of apparent resistivity anomaly and section with topographic correction in the landslide area clearly and intuitively show the vertical and lateral dist.
结果表明,对于沉积岩地区滑坡,滑坡体与滑床间存在明显的电性差异,根据经过地形改正的滑坡区视电阻率异常特征和断面,更清晰和直观显示了滑坡体的纵横向展布、主滑动面的位置与埋深,进而可圈定滑坡体的规模,从而为滑坡治理提供可靠的地球物理依据。
4) earth-resistivity anomaly
地电阻率异常
1.
The earth-resistivity anomaly characteristics analysis before the moderate earthquake in North China;
华北地区中强地震前的地电阻率异常特征分析
5) ρabnormal layer
电阻率异常层
6) microresistivity
微电阻率
1.
Estimating the optimum depth differences of microresistivity curves provided by six arm diplog;
求六臂地层倾角测井微电阻率曲线间的最优高程差
补充资料：电导率(见电阻率)
电导率(见电阻率)
conductivity
d!日nd日O}已电导率(eonduetivity)见电阻率。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条