组合多分辨率地震速度模型的图学习方法

Zheng Zhou, Peter Gerstoft, K. Olsen
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引用次数: 1

摘要

层析成像法获得的速度模型的分辨率因多种因素和变量而异,如反演方法、射线覆盖范围、数据质量等。将不同分辨率的速度模型结合起来,可以实现更精确的地面运动模拟(如 Yeh 和 Olsen,2023 年)。为实现这一目标,我们提出了一种将多分辨率地震速度图与概率图形模型(PGMs)相结合的新方法。概率图形模型可在不同分辨率的地震速度模型中提供与各种速度区间相对应的分割结果。此外,通过考虑物理信息(如射线路径密度),我们引入了物理信息概率图形模型(PIPGMs)。这些模型提供了低分辨率(LR)和高分辨率(HR)子域之间的数据驱动关系。通过利用高分辨率模型的先验知识解决最大似然问题,从高分辨率区域转移(分割)分布信息,从而增强低分辨率区域的细节。在更新 HR 和 LR 区域的边界区域时,采用斑块扫描策略来考虑局部模式,避免出现尖锐的边界。为了评估所提出的 PGM 融合方法的有效性,我们在合成棋盘模型和 2019 年加利福尼亚州里奇克雷斯特地震序列中的断层带结构图像上测试了该融合方法。里奇克雷斯特断层带图像包括从环境噪声层析成像中获得的浅层(顶部 1 公里)高分辨率剪切波速度模型,该模型被嵌入到更粗糙的全州加利福尼亚地震中心社区速度模型 S4.26-M01 版本中。沿 HR 和 LR 区域边界的观测和计算行程时间之间的偏差比传统的高斯插值法少 38%,这凸显了模型的功效。所提出的 PGM 融合方法可以合并任何网格多分辨率速度模型,是计算地震学和地动估算的宝贵工具。
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Graph-learning approach to combine multiresolution seismic velocity models
The resolution of velocity models obtained by tomography varies due to multiple factors and variables, such as the inversion approach, ray coverage, data quality, etc. Combining velocity models with different resolutions can enable more accurate ground motion simulations (e.g., Yeh and Olsen, 2023). Toward this goal, we present a novel methodology to fuse multiresolution seismic velocity maps with probabilistic graphical models (PGMs). The PGMs provide segmentation results, corresponding to various velocity intervals, in seismic velocity models with different resolutions. Further, by considering physical information (such as ray-path density), we introduce physics-informed probabilistic graphical models (PIPGMs). These models provide data-driven relations between subdomains with low (LR) and high (HR) resolutions. Transferring (segmented) distribution information from the HR regions enhances the details in the LR regions by solving a maximum likelihood problem with prior knowledge from HR models. When updating areas bordering HR and LR regions, a patch-scanning policy is adopted to consider local patterns and avoid sharp boundaries. To evaluate the efficacy of the proposed PGM fusion method, we tested the fusion approach on both a synthetic checkerboard model and a fault zone structure imaged from the 2019 Ridgecrest, CA, earthquake sequence. The Ridgecrest fault zone image consists of a shallow (top 1 km) high-resolution shear-wave velocity model obtained from ambient noise tomography, which is embedded into the coarser Statewide California Earthquake Center Community Velocity Model version S4.26-M01. The model efficacy is underscored by the deviation between observed and calculated travel times along the boundaries between HR and LR regions, 38 per cent less than obtained by conventional Gaussian interpolation. The proposed PGM fusion method can merge any gridded multiresolution velocity model, a valuable tool for computational seismology and ground motion estimation.
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