摘要
深水地震资料处理中,水层多次波因深水水层为变速体的特性,无法应用浅水水层多次波压制技术(Shallow Water Multiple Attenuation,SWMA)进行压制,而传统的自由界面多次波压制技术(Surface-Related Multiple Elimination,SRME)压制水层多次波则不具有针对性。为此,开展了基于变水速模型驱动的深水水层多次波压制技术(Deepwater Water-layer Multiple Elimination,DWME)研究。该技术通过构建海底和变水速模型计算出水层多次波准确旅行时,在τ-p域根据水层多次波旅行时将地震数据进行延拓,得到水层多次波模型,然后应用自适应匹配相减方法完成水层多次波压制。理论模型验证及海外某工区实际地震资料应用结果表明,DWME对深水水层多次波压制效果较好,且针对性强。
It is difficult to attenuate deepwater water-layer multiple using the shallow water multiple attenuation(SWMA)method or the conventional surface-related multiple elimination(SRME)method,because the deepwater water-layer velocity is not constant.This paper proposes a deepwater water-layer multiple elimination(DWME)method driven by a variable water velocity model.The method first estimates the water-layer multiple travel-time by building the sea bottom model and variable water velocity model.Then,seismic data wave field extrapolation is performed according to the estimated travel-time in theτ-pdomain to predict water-layer multiple.Finally,the adaptive matching subtraction is applied to eliminate the multiples.Testing results on both synthetic data and field data show that the DWME can effectively suppress deepwater water-layer multiples.
引文
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