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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Wavelet-crosscorrelation-based interferometric redatuming in 4D seismic
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Wavelet-crosscorrelation-based interferometric redatuming in 4D seismic

机译:基于小波 - 横刷的干涉式减少4D地震的干涉

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Interferometric virtual source (VS) redatuming crosscorrelates downgoing waves with the corresponding upgoing waves to convert records from surface-source gathers to virtual gathers at the buried receiver locations. The assumption is that the VS records show the reduced effects of overburden complexity and therefore provide improved seismic repeatability and image quality. In practice, however, the repeatability and quality of the redatumed data can be degraded by one-sided illumination and inadequate preprocessing. In the presence of complex nearsurface structure for land redatuming, the intricate shallow structure and highly variable weathering layers introduce surface multiples, ground-roll/scattering noise, and interference among different wave modes that additionally contaminates the down-and upgoing wavefields. To address these issues, we have developed a new interferometric redatuming method based on crosscorrelation in the wavelet domain. Specifically, by transforming time-offset data into the local time-scale (TS) and local TS-wavenumber domains, we have designed and applied filters on the amplitude of the cross spectra in each domain to suppress the aforementioned artifacts and noise, while maintaining accurate kinematic information by retaining the original phase spectra. The new procedure involves forward wavelet transform of the source records, crosscorrelating the wavelet coefficients, filtering in the corresponding domains, and then inverse wavelet transformation to produce the VS records. Components associated with scattering noise and ground roll can be effectively suppressed because our designed filters tackle their features accurately in the local TS and local TS-wavenumber domains, respectively. We tested the method on data from 13 time-lapse surveys that included a significant repeatability problem across a 17-month survey gap, and we compared the results with results from the conventional VS methods. Our VS method produced the best improvement
机译:干涉测量虚拟源(VS)Redatuming与相应的上行波一起跨相关性,以将来自曲面源的记录转换为埋地接收器位置的虚拟收集。假设是VS记录显示覆盖复杂性的减少,因此提供了改善的地震重复性和图像质量。然而,在实践中,重复性和重新数据的重复性和质量可以通过单侧照射和预处理不足来降低。在存在复杂的近缝结构的土地重新制造的情况下,复杂的浅结构和高度可变的风化层引入了表面倍数,地面辊/散射噪声,以及不同波动模式之间的干扰,否则污染了下降的波场。为了解决这些问题,我们已经开发了一种基于小波域中的跨相关的新干涉重新制作方法。具体地,通过将​​时间偏移数据转换为局部时间尺度(TS)和本地TS-Wavenumber域,我们在每个域中的横频光谱的幅度上设计和应用了滤波器,以抑制上述伪像和噪声,同时保持通过保留原始相位光谱来准确的运动信息。新过程涉及源记录的向前小波变换,跨相关的小波系数,在相应的域中过滤,然后逆小波变换以产生VS记录。可以有效地抑制与散射噪声和地面辊相关的组件,因为我们的设计过滤器分别在本地TS和局部TS-Wavenumber域中精确地解决它们的特征。我们从13个延时调查中测试了数据的数据,该方法包括一个17个月的调查差距,并将结果与​​传统的VS方法的结果进行了比较。我们的VS方法产生了最佳改进

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