期刊:Geophysics [Society of Exploration Geophysicists] 日期:2025-01-06卷期号:: 1-93
标识
DOI:10.1190/geo2023-0493.1
摘要
Surface travel-time tomography is a widely-used method to characterize the structure of the underground. However, conventional seismic tomography techniques often require a high-fidelity numerical forward model, which leads to significant computational burden and time consumption. Additionally, the inverse problem in travel-time tomography is prone to ill-posedness and lacks uncertainty quantification for the inferred results.