小波分析在砂砾岩层序地层划分中的应用

Jinliang Zhang, A. Song
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引用次数: 3

摘要

层序地层划分与对比是砂砾岩储层研究的关键。由于砂砾岩沉积物中缺乏页岩标志层位和古生物化石,常规的测井地层划界处理难度大,效率低。针对东营凹陷大厚砾岩,提出了一种基于DB5连续小波变换的小波分析新方法,进行层序地层划分对比。小波变换是一种很好的多尺度分析工具,它可以通过研究GR或AC测井曲线CWT在最佳尺度下小波系数的循环规律来进行地层划分。研究表明,小波分析方法对砂砾岩沉积物的分界是非常适用和有效的,并取得了较好的效果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Application of Wavelet Analysis in Sequence Stratigraphic Division of Glutenite Sediments
The sequence stratigraphic division and correlation are the key of the research for glutenite reservoir. For the reasons that lacking shale marker horizons and paleaobiological fossils in glutenite sediments, the conventional treatments of strata demarcation based on well logging are difficult and inefficient. Aimed to the great thick glutenite in Dongying Depression, this paper presents a new method of wavelet analysis based on DB5 continuous wavelet transform to make sequence stratigraphic division and correlation. The wavelet transform is an excellent tool of multi-scale analysis, it can make strata demarcation by studying the cycle regulation of the wavelet coefficients in the best scales resulted from the CWT of the GR or AC well logs. The research shows that the method of wavelet analysis is quite suitable and effective for the demarcation of glutenite sediments and gets quite good results.
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