摘要
本文结合标本测定和模拟实验结果,对不同条件下虚分量谱极值频率变化较大的原因进行了分析讨论.认为虚分量谱的“不稳定”实际上是极化体时间常数变化的客观反映.就反演频谱确定时间常数而言,相位谱并不比虚分量谱优越.
Based upon the results of sample measurements and model experiments, the cause for the large variation in the peak value of a imaginary part spectrum with frequency under different conditionsis analysed. It is believed that the 'unstability' of the imaginary part spectrum objectively reflects thechange of the time constant of a polarized body. So far as the determination of time constant by frequency spectrum inversion is concerned, the phase spectrum is not superior to the imaginary spectrum.
出处
《地质与勘探》
CAS
CSCD
北大核心
1989年第7期45-47,共3页
Geology and Exploration