摘要
本文将反斜率法推广应用于解释施伦贝尔热装置测得的电测深曲线,算法简便.将理论模拟计算所得的电阻率曲线(或数据),用反斜率法求得电性层参数,然后与模拟计算的电性层参数对比,两者有较明显的对应关系.最后以实例说明此法在定性一定量解释方面都有一定的优点.
The application scope of inverse slope method is expanded to interpretate resistivity sounding curves measured with a Schlumberger array. This method is a simple and fast-speed adculating method. A comparison of electric parameters of layers obtained by inverse slope method using apparent resistivity curves (or data) calculated by theoretical madellirg and thosc obtained by modelling calculation shows that both of them bear a good correspondence with each other. In order to illustrate some merits of the inverse slope method on qualitative-quantitative interpretation, practical examples are cited.
出处
《地质与勘探》
CAS
CSCD
北大核心
1991年第4期39-43,共5页
Geology and Exploration
