摘要
Combining wavelet transforms with conventional log differential curves is used to identify fractured sections is a new idea.In this paper,we first compute the mother wavelet transform of conventional logs and the wavelet decomposed signals are compared with fractures identified from image logs to determine the fracture-matched mother wavelet.Then the mother wavelet-based decomposed signal combined with the differential curves of conventional well logs create a fracture indicator curve,identifying the fractured zone.Finally the fracture density can be precisely evaluated by the linear relationship of the indicator curve and image log fracture density.This method has been successfully used to evaluate igneous reservoir fractures in the southern Songnan basin and the calculated density from the indicator curve and density from image logs are both basically consistent.
通过常规测井曲线小波变换来评价裂缝参数是一个较新的研究课题。本文针对火山岩裂缝储层,对常规测井曲线做coif5、bior4.4和db5基小波的小波变换,通过变换后的分解信号与成像测井裂缝密度的对比研究,寻找出与裂缝密度相匹配的基小波,再将常规测井曲线在这个基小波下的分解信号与曲线变化率法相结合建立裂缝指示曲线来识别裂缝发育段,最后通过裂缝指示曲线与成像测井的裂缝密度之间的量化关系来比较准确的评价裂缝密度。将裂缝指示曲线法在松辽盆地南部进行了应用,通过裂缝指示曲线求取的裂缝密度与成像测井的裂缝密度之间的相对误差为0.53。
基金
sponsored by National Science and Technology Major Project of China (No. 2008 ZX 05009-001)
