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Estimation and Application of Full Waveform Redatuming Operators

机译:全波形重氮算子的估计与应用

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Seismic data quality can be severely affected by near-surface anomalies. The imprint of a complex near-surface can be removed by redatuming the data to a level below which the subsurface is assumed to be relatively simple. It has been shown that this can be achieved by using focusing operators that are estimated along a user-defined horizon below the near surface complexities. In the current implementation of the CFP-technology, the estimation of the focusing operators is done in terms of traveltimes only, based on a high-frequency approximation. The accompanying amplitudes are usually derived from a local homogeneous medium, which is obviously a simplification of reality. The parameterization of focusing operators in terms of traveltimes and simple amplitudes has produced encouraging results in the past, but cannot remove the near-surface complexities completely, leaving artifacts in the redatumed results. In this paper we propose a method that estimates the focusing operators in a full waveform manner, such that detailed amplitude and phase variations are included. Based on 2D synthetic data it is demonstrated that the resulting redatuming quality is improved and artifacts are reduced.
机译:近表面异常可能会严重影响地震数据质量。通过将数据重新到下面的水平,可以将复杂的近表面的压印缩写到下面的水平被假设是相对简单的。已经表明,这可以通过使用沿着近近表面复杂性低于近方的用户定义的地平线估计的聚焦操作者来实现。在目前的CFP-Technology的实施中,基于高频近似,仅在旅行时间方面进行聚焦运营商的估计。伴随的幅度通常来自局部均匀介质,这显然是一种简化现实。在旅行时间和简单幅度方面的聚焦运营商的参数化已经产生了令人鼓舞的结果,但不能完全去除近表面复杂性,使伪像在减少的结果中留下。在本文中,我们提出了一种方法,其以完全波形方式估计聚焦运营商,使得包括详细的幅度和相位变化。基于2D合成数据,证明所得到的重新制质量得到改善,减少了伪影。

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