连续小波变换在面波压制中的应用
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摘要
由于原始地震反射数据含有大量噪声,因此地震数据的降噪处理是十分重要的,而面波的压制是陆上地震资料降噪处理的主要问题之一。这里根据共炮点记录中面波与反射波主要能量在时间~尺度域的分布不同,以及面波的频率特性等特点,提出了一种基于时间~尺度域的面波衰减方法。将该方法用于实际炮集资料的处理,并与常用的F-K滤波方法进行对比,结果表明,该方法在衰减面波干扰的同时,能更好地保护反射波,并且对于信噪比较低的浅层反射信号能够取得较好的效果。
The original seismic signal contains a lot of noise,so surface wave attenuation is one of the im-portant problems in land seismic data processing.According to the distribution characteristics of surface wave and reflection signal in time-scale domain and the frequency characteristics of surface wave,attenuation of surface wave via continuous wavelet transform is presented.The method has been applied to the real data,and compared with F-K filtering method.The result shows that the proposed method is effective which can well preserve reflection wave and get better result for low SNR of shallow seismic reflection signals.
引文
[1]熊章强,周竹生,张大洲,等.地震勘探[M].长沙:中南大学出版社,2010.
    [2]GALBRAITH J N,WIGGINS R A.Characteristics ofoptimum multi-channel stacking filters[J].Geophys-ics,1968,33(1):36.
    [3]张雅纯,唐文榜.τ-p变换压制线性干扰的应用[J].石油物探,1994,33(2):102.
    [4]闫立志,景新义,李刚.F-K滤波在噪音减去法中的作用[J].海洋地质动态,2006,22(10):28.
    [5]刘洪林,张春堂,朱秋影,等.K-L变换在地震资料去噪声的应用[J].大庆石油学院学报,2007,31(4):19.
    [6]钟凌云.小波变换方法在地震资料噪声消除中的应用[J].物探与化探,2001,31(3):245.
    [7]刘财,王典,杨宝俊,等.二维小波变换在地震勘探面波消除中的应用[J].地球物理学进展,2003,18(4):711.
    [8]陈玉东.地球物理信息处理基础[M].北京:地质出版社,2006
    [9]CHRISTOPHER TORRENCE,GILBERT P.Compo.APractical Guide to Wavelet Analysis[J].Bulletin of theAmerican Meteorological Society,1998,79(1):61.
    [10]CORSO G,KUHN P S,LUCENA L S.Seismic groundroll time-frequency filtering using the gaussian wavelettransform[J].Physica A,2001,318(2003):551.
    [11]F.E.A.LEITE.Optimal wavelet filter for suppressionof coherent noise with an application to seismic data[J].Physica A 2007,387(2008):1439.

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