小波包变换叠前地震信号研究  

Study on Pre-Stacking Seismic Signals for Wavelet Packet

作　　者：王振国[1] 周熙襄[1] 钟本善[1] 

机构地区：[1]成都理工大学信息工程学院,四川成都610059

出　　处：《新疆石油地质》2002年第6期513-515,446,共3页Xinjiang Petroleum Geology

摘　　要：叠前地震资料是多种波的复合体,为了提取有效波,必需消除主要的干扰波,如面波、高频随机干扰波。一般的去噪方法有:一维滤波、滤波、变换、f—x预测等,但它们都侧重于考虑某一方面的单一特性或某种条件假设,这些方法具有一定的局限性。小波包变换是一种时频分析的方法,它对地震资料进行时频精细划分优于小波变换,与传统的Fourier变换相比,它能刻画出具有相同频率的有效波与干扰波在时间-空间域的分布。经过小波包对叠前资料分解,可分离出面波、高频随机干扰等,然后再经过小波包重构,可有效地剔除干扰,且对有效波的伤害较少。经实际资料验证,小波包变换,确实是一个十分有效的去噪方法。There are usually different noises in seismic data before stacking.In order to pick-up effectual wave,we must remove noise waves such as surface wave and random noise with high frequency.The normal methods include:1D filter,f-x filter,t-p transform,f-x prediction,etc.However,these methods have limitations that they only particular emphasis on a single characteristic of surface wave or are based on some hypothesis.Wavelet packet is a time-frequency analytical method,and can be better of dividing the seismic data in detail than wavelet transform.It can describe the distribution of effectual wave and noise wave in time-space field at same frequency,comparing with traditional Fourier transform.By decomposing seismic data before stacking with wavelet packet,separate surface-wave and random noise of high frequency from seismic data.After processing wavelet packet reconstruction,we can eliminate noise-wave and al-low fewer damage of effectual wave.Through validating real data,wavelet packet is good for removing noise.

关 键 词：小波包变换 地震信号 叠前分析 去噪方法 面波 地震资料 时频分析 

分 类 号：P631.443[天文地球—地质矿产勘探]