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Reflection seismic waveform tomography of physical modelling data

机译:物理模型数据的反射地震波层析成像

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摘要

Waveform tomography is commonly tested using numerically generated synthetic seismic data, before the method is applied to field seismic data. However, there are often noticeable differences between idealized synthetic data and real field data, and many factors in the field data, such as noise, irregular source/receiver geometry, affect the inversion solutions. For exploring the potential of reflection seismic waveform tomography, we presented a more realistic test than the synthetic data test, by applying it to physical modelling data, to reconstruct a laboratorial model with complex velocity variation. First, we provided a formulation of the perfectly matched layer absorbing boundary condition, associated with the second-order acoustic wave equation, in order to suppress artificial reflections from subsurface model boundaries in seismic waveform simulation and tomography. Then, we demonstrated the successful implementation of a layer-striping inversion scheme applicable to reflection seismic waveform tomography. Finally, we confirmed the effectiveness of frequency grouping, rather than a single frequency at each iteration, a strategy specifically for the frequency-domain waveform tomography.
机译:在将该方法应用于现场地震数据之前,通常使用数值生成的合成地震数据对波形层析成像进行测试。但是,理想的合成数据与真实现场数据之间通常存在明显的差异,并且现场数据中的许多因素(例如噪声,不规则的源/接收器几何形状)都会影响反演结果。为了探索反射地震波形层析成像的潜力,我们提出了比合成数据测试更现实的测试,方法是将其应用于物理建模数据,以重建具有复杂速度变化的实验室模型。首先,我们提供了与二阶声波方程关联的完全匹配层吸收边界条件的公式,以抑制地震波形模拟和层析成像中来自地下模型边界的人工反射。然后,我们演示了适用于反射地震波形层析成像的分层分层反演方案的成功实现。最后,我们确认了频率分组的有效性,而不是每次迭代都使用单个频率,这是一种专门针对频域波形层析成像的策略。

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