基于模型的变周期预测反褶积
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摘要
地震资料中包含的多次波通常极其复杂,即使综合多种方法进行压制,仍然无法完全消除。由于残余多次波的分布规律已被打乱,特征愈加不明显,因而要对其识别与压制就更加困难。残余多次波的存在,不仅影响了地震资料的成像质量,还可能误导地质解释的结果。
     针对残余多次波的识别与压制问题,本项研究提出了一种新的基于模型的变周期预测反褶积方法。与传统的预测反褶积方法不同,基于模型的变周期预测反褶积首先根据所建立的强波阻抗界面的深度—速度模型,在地震偏移剖面上追踪识别出残余多次波并根据其传播时间确定出相应变化的多次波周期或预测步长,然后在成像道集上对含有残余多次波的成像道进行变周期预测反褶积压制处理,最后再将剔除残余多次波后的成像道集合成为新的地震偏移剖面。数值实验和实际资料处理的结果表明:基于模型的变周期预测反褶积方法不仅对微屈多次波有效,而且对残余的长周期鸣震多次波也可达到令人满意的压制效果,这是传统预测反褶积技术难以做到的。
     文中综合实验分析,总结了多种类型的鸣震等多次波特征,其结论对于实际地震资料的处理分析,特别是对于复杂多次波的识别和大倾角多次波的压制等,将具有很好的指导意义。
The multiples in the seismic records are usually very complicated. Even if attenuated by comprehending all kinds of the existing methods, there are still some residual multiples existing in the seismic data. Because that the attitude and feature of the residual multiples have been obscured, it is more difficult for them to be distinguished and attenuated afterwards. Not only their existence in the seismic data can affect the imaging quality but also they may lead to wrong geological interpretations as well.
     Aimed to distinguish and attenuate the residual multiples in the seismic data, a new method named Model-based Predictive Deconvolution with Varying Period is developed in this research. Not like as the conventional predictive deconvolution approach does, the method presented in this paper is firstly to distinguish the residual multiples on the migrated section by a ray-tracing manner based upon a built depth-velocity model of the stronger reflecting boundaries. The attenuation processing of the predictive deconvolution with variable periods or variable predictive steps, determined by the travel time(s) of the residual multiples on the section, is then applied to those traces which contain residual multiples in the corresponding imaging gathers. A new migrated section is finally synthesized by using the imaging gathers with the residual multiples eliminated. The experiment processing results of numerical and real data examples demonstrate that the method can not only sufficiently attenuate the peg-leg multiple but also can eliminate the long-period residual multiple to a satisfied result, which may be difficult to be attenuated by the conventional predictive deconvolution techniques.
     The characteristics of kinds of reverberations or multiples are presented in this paper based upon a comprehensive experiment analysis. The conclusions may have good instructive meanings for real seismic data processing and analysis, especially for the distinction of complex multiples and the attenuation of those with high dip angles.
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