地面地震和随钻地震数据集的联合最小二乘RTM

N. Kazemi, D. Trad, K. Innanen, R. Shor
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引用次数: 1

摘要

理论上,最小二乘偏移可以减少采集足迹并改善地下结构的照明。然而,在复杂的地下构造中,射线或波能在某些区域穿透性较差,例如盐下区域,该区域对于典型的地面地震采集来说将是一个阴影区。阴影区位于偏移算子的零空间,即使将成像作为逆问题也无法恢复该区域的地下信息。为了纠正这一点,我们使用了另一组数据,连同地面地震数据集,其射线路径与地面地震不同。随钻地震(SWD)数据集是对地面数据的补充,它通过在成像问题中添加新的测量值,为解决地震照明问题提供了机会。因此,在本研究中,我们制定了地面地震和SWD数据集的联合最小二乘逆时偏移,并探索了其在地面地震采集阴影区部分模型成像中的潜力。BP-Model94上的结果表明,联合最小二乘偏移在改善地下构造照明方面优于单一曲面和单一SWD最小二乘偏移。
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Joint Least-Squares RTM of Surface Seismic and Seismic-While-Drilling Datasets
Least-squares migration can, in theory, reduce the acquisition footprint and improve the illumination of the subsurface structures. However, in complex subsurface structures, rays or the wave energy will penetrate poorly in some regions, e.g., subsalt region, and that region will be a shadow zone to a typical surface seismic acquisition. The shadow zone is in the null space of the migration operator and the subsurface information in that region will not be recovered even by posing imaging as an inverse problem. To rectify this, we use another set of data, along with surface seismic dataset, whose ray paths are different from the surface seismic. Seismic-while-drilling (SWD) dataset are complementary to surface data, and it brings an opportunity to address seismic illumination issue by adding new measurements into the imaging problem. Accordingly, in this research, we formulate the joint least-squares reverse time migration of surface seismic and SWD datasets and explore its potential in imaging the parts of the model that is in the shadow zone of the surface seismic acquisition. Presented results on the BP-Model94 show that the joint least-squares migration outperforms the single surface and single SWD least-squares migrations in improving the illumination of subsurface structures.
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