论文标题
通过扩展的图像空间重新设计,面向目标的弹性全波倒置
Target-oriented elastic full-waveform inversion through extended image-space redatuming
论文作者
论文摘要
弹性全波倒置(FWI)成功应用时可以提供准确且高分辨率的地下参数。但是,其高计算成本阻止了这种方法在大规模现场数据方案中的应用。为了减轻这一限制,我们根据依赖扩展最小二乘迁移过程的重新拟合步骤提出了面向目标的弹性FWI方法。在我们的方法中,当映射到图像空间时,表面反射数据可以归因于给定的地下部分。这个过程使我们能够重建由目标区域生成的反射数据,并以直接位于其上方的虚拟采集几何形状记录。 redatuming步骤仅在目标部分中应用弹性FWI方法。整个工作流程大大降低了表面数据反转的总成本,并允许检索目标领域的准确弹性参数。我们证明了基于众所周知的Marmousi2模型以及在墨西哥湾记录的3D海洋底 - 节点(OBN)压力数据上,我们的方法在合成案例上的有效性。我们首先讨论方法论的基本方面,并将提出的工作流程应用于合成测试案例。我们还采用了在现场数据方案上的方法,并在正确检索含有盐型侧面近距离的气体砂箱的弹性参数和岩石物理特性方面显示出其功效。
Elastic full-waveform inversion (FWI) when successfully applied can provide accurate and high-resolution subsurface parameters. However, its high computational cost prevents the application of this method to large-scale field-data scenarios. To mitigate this limitation, we propose a target-oriented elastic FWI methodology based on a redatuming step that relies upon an extended least-squared migration process. In our approach, the surface-reflection data can be attributed to a given subsurface portion when mapped into the image space. This process allows us to reconstruct reflection data generated by a target area and recorded with a virtual acquisition geometry positioned directly above it. The redatuming step enables the application of an elastic FWI method within the target portion only. The entire workflow drastically diminishes the overall cost of the surface-data inversion and allows the retrieval of accurate elastic parameters of the area of interest. We demonstrate the effectiveness of our approach on a synthetic case based on the well-known Marmousi2 model and on a 3D ocean-bottom-node (OBN) pressure data recorded in the Gulf of Mexico. We first discuss the fundamental aspects of the methodology and apply the proposed workflow to the synthetic test case. We also employ the methodology on the field-data scenario and show its efficacy at correctly retrieving the elastic parameters and rock-physical properties of a gas-bearing sand reservoir positioned in proximity of a salt-dome flank.