Sep 2026· Journal of Seismic Exploration· 0 citations
Abstract
Conventional one-way wave-equation migration methods often suffer from phase errors, amplitude distortions, and low-amplitude artifacts in the presence of strong lateral velocity variations, complex structures, and noisy data. To address these problems, we propose a sparse-denoising-constrained least-squares one-way wave-equation migration method. A one-way propagation operator is first constructed in the space–frequency domain using matrix eigenvalue decomposition to improve the stability and phase accuracy of wavefield depth extrapolation in laterally heterogeneous media. Recursive primary wavefield modeling is then used to establish the forward relationship between the reflectivity model and surface primary reflection data, and the data-misfit gradient is computed through adjoint propagation. Furthermore, a curvelet-transform denoiser regularization term is introduced, so that the data-residual gradient and denoising-residual gradient jointly guide the reflectivity update. Numerical experiments on the Lens, Marmousi, and Overthrust models show that the proposed method produces clearer reflection interfaces, more continuous events, and more stable residual convergence than least-squares migration based on the generalized-screen propagation operator. Noisy-data tests further demonstrate that the proposed sparse denoising constraint improves peak signal-to-noise ratio (SNR) and structural similarity index under 5 dB, 1 dB, and −5 dB noise conditions, especially preserving structural similarity under strong noise. These results demonstrate the improved stability, resolution, and structural fidelity of the proposed method for complex synthetic models and low-SNR synthetic data.
Image-domain least-squares reverse time migration (ID-LSRTM) improves the resolution, illumination balance, and amplitude fidelity of reverse time migration (RTM) images by approximating the Hessian matrix with point-spread functions (PSFs) in the image domain. However, the conventional zero-lag cross correlation imagi...
Sumin Kim, Wookeen Chung· IEEE Geoscience and Remote S...· 0 citations
Marine seismic imaging is affected by limited acquisition aperture, nonuniform illumination, and complex features such as seafloor structures and low-velocity gas clouds. These factors can produce blurred reflectors, amplitude imbalance, and migration artifacts in conventional reverse-time migration (RTM). Point-spread...
Zi-Dong Zhao, Hao-Ran Ren, Yu-Xiang Wu et al.· Journal of Marine Science an...· 0 citations
Full Waveform Inversion (FWI) leverages the amplitude and phase of full wavefield seismic data to obtain high-resolution subsurface structures by minimizing an objective function. However, FWI encounters severe cycle-skipping issues when the seismic data lack low-frequency components or the initial velocity model is...
Conventional Kirchhoff migration is commonly affected by limited resolution, reflector broadening, and sidelobe contamination. Here, we propose DSVD-IHCM, a migration-imaging method that uses singular-value decomposition-based damped inverse Hessian compensation. The method first constructs local point-spread functions...
Li-Wei Song, Yi-Lin Bai, Ying Shi et al.· IEEE Transactions on Geoscie...· 0 citations
Accurate imaging of steeply dipping structures is critical for hydrocarbon reservoir identification and fault characterization in complex regions. However, conventional imaging methods based on primary reflections often fail to resolve near-vertical and overturned interfaces due to limited acquisition aperture and su...
Qi Zhang, Yingming Qu, Yixin Wang et al.· Journal of Geophysics and En...· 0 citations
Surface-wave tomography provides important constraints on the crust and upper mantle, but directly inverting millions of measurements for three-dimensional structure remains computationally demanding. We develop an efficient Gauss--Newton framework for one-step surface-wave tomography that jointly inverts multiperiod i...
Yiran Jiang, Ping Tong, Jian-Wei Ma· 0 citations
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