摘要
主分量分析法(PCA)的数学原理是坐标转换,它将原变量变换成互不相关的变量。在实际应用中,它为综合解释法提供了一种变量组合的途径。从物理意义上来说,它可以求出各物理参数的权系数,从而判断出,在各个主分量中各个参数的贡献大小。这样,我们便可以有目的地选择各参数,利用主分量PCA曲线进行地质解释。本文概述了主分量分析法PCA的基本原理和自编的分析程序流程,并以新疆塔北地区为例,说明了分层、计算泥质含量及孔隙度的成果。应用实例表明,在测并解释工作中应用主分量PCA曲线可以取得更准确、更细致的效果。具体地说,在新疆塔北地区砂泥岩薄互层组上,可以用主分量PCA曲线进行薄互层组的地质解释。
The mathematic principle of principal component analysis method (PCA) lies in coordinate conversion.In practice,it provides a means of variable combination for integrated interpretation. The present paper has made a generalized description of basic principle of the principal component analysis method as well as analytical programscompiled by ourselves. Exemplified by northern Tarim area of Xinjiang,the paper has also illustrated the achievements gained in layering,calculation of argillaceous material content and porosity.
出处
《物探与化探》
CAS
CSCD
1996年第3期209-217,共9页
Geophysical and Geochemical Exploration
关键词
测井
解释法
主分量分析法
principal component analysis
log interpretation
layering
argillaceous material content
porosity