摘要
谱分解理论是把单道地震记录分解为连续的时频谱平面,是地震资料处理和解释的重要技术之一.由于谱分解方法的多解性,所以同一道地震记录因为分解方法不同,得到的时频谱是不一样的.短时傅里叶变换,小波变换,S变换和匹配追踪算法都是对信号开窗分析,这些方法都受到不确定性原理的限制.Wigner-Ville变换避开了不确定性原理的限制,但是交叉项的存在限制了本方法的使用.本文利用谱图重排的时频分析方法(RSPWV)对合成的单道地震记录和实际的地震资料进行了分析.与短时傅里叶变换和匹配追踪算法的比较得出:此方法具有较高的时频分辨率,能够很好地识别气层.
Spectral decomposition refers to any method that produces a continuous time-frequency spectrum of a seismic trace.Time frequency analysis is an important technology in seismic data processing and interpretation.Since spectral decomposition is a non-unique process,thus a single seismic trace can produce various time-frequency spectra.The short time Fourier transform(STFT),wavelet transform(WT),S-transform and matching pursuit(MP) method are all using windows,thus under the control of uncertainty principle.The Wigner-Ville distribution(WVD) avoids the windows.However,WVD is quadratic that produces cross-terms for multi-components signal that restricts its applications.In this paper,we analyze the time-frequency properties of a synthetic trace by using the reassigned smooth pseudo Wigner-Ville distribution(RSPWV) method,experiments and field data show that the method is superior to the STFT and MP methods,and can delineate the gas reservoir.
出处
《地球物理学进展》
CSCD
北大核心
2012年第2期596-602,共7页
Progress in Geophysics
基金
中国石油大学(北京)基础学科基金:储层预测中新的谱分解方法研究(JCXK-2011-12)
国家自然科学基金项目:基于孔隙弹性介质波动理论的AVF规律研究(41140033)项目联合资助
关键词
短时傅里叶变换
小波变换
Wigner-Ville变换
谱图重排
short time Fourier transform
wavelet transform
Wigner-Ville transform
resigned smooth pseudo Wigner-Ville distribution