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A stable and effective strategy for angle gather extraction from reverse time migration using traveltime gradient

机译:一种使用行进时间梯度从逆时偏移中提取角集的稳定有效策略

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The generation of angle-domain common imaging gathers (ADCIGs) from reverse time migration (RTM) is essential for velocity updates, migration quality control and amplitude variation with angle (AVA) inversion. However, computational stability and efficiency challenges remain with ADCIGs extracted from RTM. Here, we develop a stable and effective strategy to produce ADCIGs during RTM based on the traveltime gradient. The first arrival traveltime is calculated efficiently using the dynamic programming scheme, and the source-side propagating direction of the local plane-wave can be obtained using the traveltime field gradient. Compared with propagation directions calculated using the local slowness analysis method, the traveltime gradient can also provide stable and accurate source-side directions. Benefitting from the migrated images, we can collect normal direction information for the reflector from the stacked images effectively using the omnidirectional plane-wave destruction (OPWD) method. Construction of subsurface scattering angles is straightforward via combination of the source-side propagation and reflector normal directions. Subsequently, we apply an effective imaging condition based on the excitation criterion in the angle domain to generate ADCIGs. Thanks to conversion from a wavefield-based to a traveltime-based calculation, the proposed method provides more stable and reliable wave propagation directions in complicated areas compared with the Poynting vector (PV) method which is based on the full wavefield. Because traveltime can be calculated efficiently beforehand, the proposed method can be adapted economically to the conventional RTM imaging frame, which reveals significant implementation potential for practical seismic exploration. We demonstrate the stability and effectiveness of this approach for both synthetic and field data.
机译:从逆时偏移(RTM)生成角域通用成像道集(ADCIG)对于速度更新,偏移质量控制和振幅随角度(AVA)反演至关重要。但是,从RTM提取的ADCIG仍然存在计算稳定性和效率挑战。在这里,我们基于行进时间梯度,开发了一种稳定有效的策略,可以在RTM期间产生ADCIG。利用动态规划方案可以有效地计算出初次到达的传播时间,并可以利用传播时间场梯度来获得局部平面波的源侧传播方向。与使用局部慢度分析方法计算的传播方向相比,传播时间梯度还可以提供稳定且准确的源侧方向。受益于迁移的图像,我们可以使用全向平面波破坏(OPWD)方法从堆叠的图像中有效地收集反射器的法线方向信息。通过源侧传播方向和反射器法线方向的组合,可以简单地构造地下散射角。随后,我们基于角域中的激发准则应用有效的成像条件以生成ADCIG。由于从基于波场的计算转换为基于行程时间的计算,与基于全波场的Poynting矢量(PV)方法相比,该方法在复杂区域中提供了更稳定和可靠的波传播方向。由于可以预先有效地计算出行进时间,因此所提出的方法可以经济地适应传统的RTM成像框架,从而为实际地震勘探显示出巨大的实现潜力。我们证明了这种方法对于合成数据和现场数据的稳定性和有效性。

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