Automated salt model building: From compaction trend to final velocity model using waveform inversion

Q2 Earth and Planetary Sciences Leading Edge Pub Date : 2023-03-01 DOI:10.1190/tle42030196.1
M. Warner, T. Nangoo, A. Umpleby, N. Shah, C. Manuel, D. Bevc, M. Merino
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Abstract

Conventional seismic velocity model building in complicated salt-affected areas requires the explicit identification of salt boundaries in migrated images and typically involves testing of possible subsurface scenarios through multiple generations. The resulting velocity models are slow to generate and may contain interpreter-driven features that are difficult to verify. We show that it is possible to build a full final velocity model using advanced forms of full-waveform inversion applied directly to raw field data, starting from a model that contains only a simple 1D compaction trend. This approach rapidly generates the final velocity model and migrates processed reflection data at least as accurately as conventionally generated models. We demonstrate this methodology using an ocean-bottom-node data set acquired in deep water over Walker Ridge in the Gulf of Mexico. Our approach does not require exceptionally long offsets or the deployment of special low-frequency sources. We restrict the inversion so it does not use significant energy below 3 Hz or offsets longer than 14 km. We use three advanced forms of waveform inversion to recover the final model. The first is adaptive waveform inversion to proceed from models that begin far from the true model. The second is nonlinear reflection waveform inversion to recover subsalt velocity structure from reflections and their long-period multiples. The third is constrained waveform inversion to produce salt- and sediment-like velocity floods without explicitly identifying salt boundaries or velocities. In combination, these three algorithms successively improve the velocity model so it fully predicts the raw field data and accurately migrates primary reflections, though explicit migration forms no part of the workflow. Thus, model building via waveform inversion is able to proceed from field data to the final model in just a few weeks. It entirely avoids the many cycles of model rebuilding that may otherwise be required.
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自动盐模型建立:从压实趋势到最终速度模型,使用波形反演
在复杂的受盐影响地区建立传统的地震速度模型需要在偏移图像中明确识别盐边界,并且通常涉及通过多代测试可能的地下场景。生成的速度模型生成速度较慢,并且可能包含难以验证的解释器驱动特征。我们表明,使用直接应用于原始现场数据的高级全波形反演形式,从只包含简单1D压实趋势的模型开始,可以建立完整的最终速度模型。这种方法快速生成最终速度模型,并至少与传统生成的模型一样准确地迁移处理后的反射数据。我们使用在墨西哥湾沃克岭深水中获得的海底节点数据集演示了这种方法。我们的方法不需要超长的偏移或部署特殊的低频源。我们限制反演,使其不使用低于3赫兹的显著能量或超过14公里的偏移。我们使用三种高级形式的波形反演来恢复最终模型。第一种是从远离真实模型的模型开始进行自适应波形反演。二是非线性反射波形反演,从反射及其长周期多次波中恢复盐下速度结构。第三种是约束波形反演,在没有明确确定盐边界或速度的情况下产生类似盐和沉积物的速度洪水。结合起来,这三种算法相继改进了速度模型,使其能够充分预测原始现场数据并准确地迁移主反射,尽管显式迁移不构成工作流程的一部分。因此,通过波形反演的模型构建能够在短短几周内从现场数据进行到最终模型。它完全避免了可能需要的许多模型重建周期。
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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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