方法对比
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| 环境噪声层析成像× | 地震全波形反演× | |
|---|---|---|
| 领域 | 地球物理学 | 地球物理学 |
| 方法族 | Process / pipeline | Process / pipeline |
| 起源年份≠ | 2005 | 1984 |
| 提出者≠ | Shapiro, Campillo, Stehly, and Ritzwoller | Albert Tarantola |
| 类型≠ | Passive seismic imaging via correlation of ambient noise | Seismic imaging and model parameterization technique |
| 开创性文献≠ | Shapiro, N. M., Campillo, M., Stehly, L., & Ritzwoller, M. H. (2005). High-resolution surface-wave tomography from ambient seismic noise. Science, 307(5715), 1615-1618. DOI ↗ | Tarantola, A. (1984). Inversion of seismic reflection data in the acoustic approximation. Geophysics, 49(8), 1259-1266. DOI ↗ |
| 别名 | ANT | FWI |
| 相关 | 3 | 3 |
| 摘要≠ | Ambient Noise Tomography (ANT) is a seismic imaging method that extracts surface wave information from long-term records of seismic background noise, enabling high-resolution imaging of crustal and upper mantle structure. Developed by Shapiro, Campillo, and colleagues in 2005, ANT has revolutionized seismic imaging by enabling detailed crustal velocity maps at minimal cost without requiring earthquakes or active sources. | Seismic Full-Waveform Inversion (FWI) is a computational technique that reconstructs detailed subsurface velocity and impedance models by iteratively fitting synthetic seismic waveforms to observed data. Introduced by Albert Tarantola in 1984, FWI has become the leading method for high-resolution imaging in exploration geophysics, engineering seismology, and subsurface characterization. |
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