Can towed-streamer seismic data be used for elastic wave imaging? Synthetic and field data examples

GEOPHYSICS Pub Date : 2024-01-25 DOI:10.1190/geo2022-0534.1
Rui Gong, Jianhua Geng, P. Yu, Xueying Hu
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Abstract

In marine seismic exploration, towed-streamer seismic data acquisition stands out as a prevalent and economical approach. This data records scalar pressure and captures P waves including those that are converted from sub-seabed S waves. Theoretically, towed-streamer seismic data can be used to reconstruct S-wave fields for elastic wave imaging via backward extrapolation. Our research applies an acoustic-elastic coupled equation that includes a pressure term to perform elastic reverse time migration, using the pressure seismic data as the boundary condition for backward extrapolation. The feasibility of employing towed-streamer seismic data for elastic wave imaging of complex subsurface structures is confirmed through synthetic and field data examples. The investigation demonstrates how the smoothness of velocity and density models impacts the quality of elastic reverse time migration using towed-streamer seismic data. We find that using smooth velocity and density models for elastic wave imaging can enhance imaging quality by utilizing transmitted S waves. Furthermore, certain nonphysical S waves generated during backward extrapolation can contribute to PS images, as evidenced by a synthetic data example. Overall, the results indicate that the towed-streamer seismic data for elastic wave imaging has potential in marine seismic exploration. Moving forward, it is crucial to focus on refining the quality of PS images and reducing artifacts caused by the backward extrapolated nonphysical waves.
拖曳流地震数据可用于弹性波成像吗?合成数据和现场数据示例
在海洋地震勘探中,拖曳流地震数据采集是一种普遍而经济的方法。这种数据记录标量压力并捕捉 P 波,包括从海底下 S 波转换而来的 P 波。从理论上讲,拖曳流地震数据可通过反推法重建 S 波场,用于弹性波成像。我们的研究应用了包含压力项的声弹耦合方程,利用压力地震数据作为反推的边界条件,进行弹性反向时间迁移。通过合成和现场数据实例,证实了利用拖曳流地震数据对复杂地下结构进行弹性波成像的可行性。研究证明了速度和密度模型的平滑度如何影响使用拖曳流地震数据进行弹性反向时间迁移的质量。我们发现,使用平滑的速度和密度模型进行弹性波成像,可以利用透射 S 波提高成像质量。此外,在反向外推过程中产生的某些非物理 S 波也有助于 PS 成像,一个合成数据实例就证明了这一点。总之,研究结果表明,用于弹性波成像的拖曳流地震数据在海洋地震勘探中具有潜力。展望未来,关键是要提高 PS 成像的质量,减少后推非物理波造成的伪影。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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