水平地层电阻率测深量板广泛用来快速推断解释电测深曲线.现有构制量板的方法都是利用合适的求积法对斯忒藩斯库积分求数值解.随着快速数字计算机的发展,这种方法获得了更大的成效.最近戈什利用线性滤波方法研究成一种迥然不同的计算电阻率测深量板的方法.本文介绍一种基于斯忒藩斯库方程,计算施伦贝尔热和温纳电极排列的水平层状地层测深量板的快速方法.在斯忒藩斯库方程中有贝塞尔函数,由于J_j(x)收敛慢,而且具有振 Horizontal formation resistivity depth gauges are widely used to quickly infer the interpretation of electrical sounding curves. The existing methods of constructing a volumetric plate use the appropriate quadrature method to solve the Stephanski points integral. With the rapid number The development of computers has achieved even greater success, and recently Ghosh used linear filtering methods to study a very different method of calculating resistivity depth gauges.This paper presents a method based on the Stein-Paussian equation Schlumberger and Wynner electrodes, a Bessel function in the Stein-Paussian equation, due to the slow convergence of J_j (x) and the fact that it has vibration