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A critical appraisal of asymptotic 3D-to-2D data transformation in full-waveform seismic crosshole tomography

机译:渐进式3D到2D数据转换在全波形地震井孔层析成像中的严格评估

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Seismic full-waveform inversion (FWI) is often based on forward modeling in the computationally attractive 2D domain. This implies the assumption of a line source extended in the out-of-plane medium invariant direction, with far-field amplitudes decaying inversely with the square root of distance. Realistic point sources, however, generate amplitudes that decay approximately with the inverse of distance. Conventionally, practitioners correct for this amplitude difference and the associated phase shift by transforming the recorded 3D field data to the approximate 2D equivalent by using simplistic asymptotic filter algorithms. Such filters assume straight raypaths, a constant velocity medium, and far-field recordings. We have assessed the validity of 3D-to-2D data transformation in the context of crosshole seismic full-waveform tomography by propagating 3D and 2D wavefields through 2D media and comparing 2D reference synthetics with their filtered 3D equivalent. The filter performs well in simple situations, which confirms the general applicability of the conventional asymptotic approach. However, we have observed substantial errors in more complex elastic models, associated with overlapping arrivals and strongly curved raypaths. To test if this error translates into deficient model reconstruction in FWI, we performed complementary inversion experiments using a frequency-domain algorithm. Purely acoustic waveform inversions of 3D-to-2D filtered data are only weakly affected, but in the case of elastic FWI, in which an S-wave influence is present, adverse effects increase substantially. Two-dimensional FWI in combination with filtering seems to be an acceptable strategy as long as the model is twodimensional, the recording geometry is straight and perpendicular to strike, and only slight S-wave energy is contained in the data. The latter two conditions are generally met in explorationtype marine seismic surveys at short offsets and in some crosswell applications using explosive sources and nondirectional pressure receivers.
机译:地震全波形反演(FWI)通常基于在计算上具有吸引力的2D域中的正向建模。这意味着假设线源在平面外介质不变方向上延伸,远场振幅与距离的平方根成反比。但是,现实的点源生成的幅度大约随着距离的倒数而衰减。传统上,从业者通过使用简单的渐近滤波器算法将记录的3D场数据转换为近似2D等效值来校正此幅度差和相关的相移。这种滤光片采用直线光线路径,等速介质和远场记录。我们通过在2D介质中传播3D和2D波场,并将2D参考合成物与经过过滤的3D等效物进行比较,评估了在井间地震全波形层析成像背景下3D到2D数据转换的有效性。该滤波器在简单的情况下表现良好,这证实了传统渐近方法的普遍适用性。但是,我们在更复杂的弹性模型中观察到了重大误差,这些误差与重叠的到达波和强烈弯曲的射线路径有关。为了测试此错误是否转化为FWI中的缺陷模型重构,我们使用频域算法进行了互补的反演实验。从3D到2D滤波数据的纯声波波形反演仅受到很小的影响,但是在存在S波影响的弹性FWI情况下,不利影响会大大增加。二维FWI与滤波相结合似乎是可以接受的策略,只要模型是二维的,记录的几何形状是笔直的并且垂直于走向,并且数据中仅包含很小的S波能量即可。在短距离偏移的勘探型海洋地震勘测中以及在使用炸药源和非定向压力接收器的某些井间应用中,通常满足后两个条件。

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