摘要
文中指出:单一沉积作用所导致的元素含量的概率分布服从正态分布;将柯尔莫各洛夫-斯米尔诺夫统计检验用于地层中元素含量背景值的研究有其独特优点.给出了实施此方法的微机程序.
In this paper the authors point out that the statistical distribution of element content resultedmerely from sedimentation will follow the normal distribution law. The Kolmogorov-Smirnov statistical test has a unique advantage for stydying the background level of elements in rock formations. A minicomputer program is also given for putting the method into effect.
出处
《地质与勘探》
CAS
CSCD
北大核心
1989年第2期45-48,共4页
Geology and Exploration
