arXiv:2506.13529cs.LGcs.AI2025-06被引 1

用潜空间扩散模型快速高精度反演地震阻抗,适合地质解释场景。

Seismic Acoustic Impedance Inversion Framework Based on Conditional Latent Generative Diffusion Model

  • 在潜空间进行条件生成扩散反演,减少迭代步骤
  • 仅需少数扩散步数即达高精度,合成与实测数据均验证有效
  • 轻量小波模块嵌入条件输入,适合实际地震数据应用

地震声学阻抗在岩性识别和地下结构解释中至关重要。然而,由于反演问题本质上不适定,直接从叠后地震数据估计阻抗仍极具挑战。近年来,扩散模型因其强大的先验学习和生成能力,在解决此类逆问题方面展现出巨大潜力。但现有方法多在像素域操作,需多次迭代,限制了其在野外数据中的应用。为此,本文提出一种基于条件潜空间生成扩散模型的地震声学阻抗反演框架,将反演过程置于潜空间中。为避免引入额外训练开销,在框架中设计轻量级小波模块,用于投影地震数据,并复用预训练的阻抗编码器将低频阻抗嵌入潜空间。此外,提出一种模型驱动的采样策略,提升反演精度并减少所需扩散步数。合成模型上的数值实验表明,该方法在仅少数扩散步数下即可实现高精度和强泛化能力。对实测数据的应用显示,地质细节更清晰,且与井数据一致性更高,验证了方法的有效性与实用性。

原文摘要 · Abstract (English)

Seismic acoustic impedance plays a crucial role in lithological identification and subsurface structure interpretation. However, due to the inherently ill-posed nature of the inversion problem, directly estimating impedance from post-stack seismic data remains highly challenging. Recently, diffusion models have shown great potential in addressing such inverse problems due to their strong prior learning and generative capabilities. Nevertheless, most existing methods operate in the pixel domain and require multiple iterations, limiting their applicability to field data. To alleviate these limitations, we propose a novel seismic acoustic impedance inversion framework based on a conditional latent generative diffusion model, where the inversion process is made in latent space. To avoid introducing additional training overhead when embedding conditional inputs, we design a lightweight wavelet-based module into the framework to project seismic data and reuse an encoder trained on impedance to embed low-frequency impedance into the latent space. Furthermore, we propose a model-driven sampling strategy during the inversion process of this framework to enhance accuracy and reduce the number of required diffusion steps. Numerical experiments on a synthetic model demonstrate that the proposed method achieves high inversion accuracy and strong generalization capability within only a few diffusion steps. Moreover, application to field data reveals enhanced geological detail and higher consistency with well-log measurements, validating the effectiveness and practicality of the proposed approach.

地震反演扩散模型潜空间地质解释

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