Enhancing salt model resolution and subsalt imaging with elastic FWI

Q2 Earth and Planetary Sciences Leading Edge Pub Date : 2023-03-01 DOI:10.1190/tle42030207.1
Zhigang Zhang, Zedong Wu, Zhiyuan Wei, J. Mei, Rongxin Huang, Ping Wang
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引用次数: 1

Abstract

Full-waveform inversion (FWI) has become the centerpiece of velocity model building (VMB) in seismic data processing in recent years. It has proven capable of significantly improving the velocity model and, thus, the migration image for different acquisition types and geologic settings, including complex environments such as salt. With the advent of FWI imaging, the scope of FWI applications has extended further from VMB into the imaging landscape. However, current FWI applications in the industry prevalently employ the acoustic approximation. One common problem of acoustic FWI (A-FWI) is the apparent salt halos at the salt-sediment interface in the resulting FWI velocity and FWI image, the presence of which hinders direct interpretation and imaging focusing around salt bodies. With synthetic and field data examples, we demonstrate that this salt halo is caused mainly by the large mismatch between the elastic recorded data and the acoustic modeled data, particularly at middle to long offsets. To overcome limitations imposed by acoustic assumptions, we developed an elastic FWI (E-FWI) algorithm that combines an elastic modeling engine with the time-lag cost function, which we call elastic time-lag FWI (E-TLFWI). With a more accurate modeling engine, E-TLFWI significantly reduces the salt halo observed in its acoustic counterpart. However, we also observe that the images migrated using the A-FWI and E-FWI velocity models remain similar overall, with some slight improvements around and beneath salt boundaries, particularly near steep salt flanks, as a result of the reduced salt halo. By contrast, FWI images derived from E-TLFWI show considerable benefits over those from acoustic time-lag FWI, such as improved event focusing, better structural continuity, and higher signal-to-noise ratio. The sharpened salt boundaries and enhanced quality of the FWI images reveal the significant value of E-FWI and provide the justification for its greatly increased cost.
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利用弹性FWI提高盐模型分辨率和盐下成像
近年来,全波形反演(FWI)已成为地震数据处理中速度模型建立的核心。事实证明,它能够显著改善速度模型,从而改善不同采集类型和地质环境(包括盐等复杂环境)的迁移图像。随着FWI成像技术的出现,FWI的应用范围已经从VMB进一步扩展到成像领域。然而,目前行业中的FWI应用普遍采用声学近似。声波FWI (A-FWI)的一个常见问题是,在产生的FWI速度和FWI图像中,盐-沉积物界面存在明显的盐晕,这阻碍了盐体周围的直接解释和成像聚焦。通过综合和现场数据实例,我们证明了这种盐晕主要是由弹性记录数据和声学模型数据之间的巨大不匹配造成的,特别是在中长偏移。为了克服声学假设的限制,我们开发了一种弹性FWI (E-FWI)算法,该算法将弹性建模引擎与时滞成本函数相结合,我们称之为弹性时滞FWI (E-TLFWI)。通过更精确的建模引擎,E-TLFWI显著减少了在声学模拟中观察到的盐晕。然而,我们也观察到,使用a - fwi和E-FWI速度模型迁移的图像总体上保持相似,由于盐晕减少,盐边界周围和盐边界下方有一些轻微的改善,特别是在陡峭的盐翼附近。相比之下,通过E-TLFWI获得的FWI图像比声波时滞FWI具有更大的优势,例如改进的事件聚焦、更好的结构连续性和更高的信噪比。盐边界的锐化和FWI图像质量的提高显示了E-FWI的巨大价值,也为其大幅增加的成本提供了理由。
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来源期刊
Leading Edge
Leading Edge Earth and Planetary Sciences-Geology
CiteScore
3.10
自引率
0.00%
发文量
180
期刊介绍: THE LEADING EDGE complements GEOPHYSICS, SEG"s peer-reviewed publication long unrivalled as the world"s most respected vehicle for dissemination of developments in exploration and development geophysics. TLE is a gateway publication, introducing new geophysical theory, instrumentation, and established practices to scientists in a wide range of geoscience disciplines. Most material is presented in a semitechnical manner that minimizes mathematical theory and emphasizes practical applications. TLE also serves as SEG"s publication venue for official society business.
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