Сравнение методов
Просматривайте выбранные методы рядом; строки с различиями подсвечены.
| Сейсмическая инверсия полных волновых форм× | Анализ функций приёмника× | |
|---|---|---|
| Область | Геофизика | Геофизика |
| Семейство | Process / pipeline | Process / pipeline |
| Год появления≠ | 1984 | 1979 |
| Автор метода≠ | Albert Tarantola | Charles Langston |
| Тип≠ | Seismic imaging and model parameterization technique | Teleseismic body wave analysis for subsurface imaging |
| Основополагающий источник≠ | Tarantola, A. (1984). Inversion of seismic reflection data in the acoustic approximation. Geophysics, 49(8), 1259-1266. DOI ↗ | Langston, C. A. (1979). Structure under Mount Rainier, Washington, inferred from teleseismic body waves. Journal of Geophysical Research, 84(B9), 4749-4762. DOI ↗ |
| Другие названия | FWI | RF |
| Связанные | 3 | 3 |
| Сводка≠ | 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. | Receiver Function (RF) analysis is a seismic method that isolates P-to-S wave conversions at crustal and mantle discontinuities using teleseismic records from distant earthquakes. Introduced by Langston in 1979, RF analysis provides a cost-effective way to determine crustal thickness, Poisson's ratio, and upper mantle structure without requiring active seismic sources, making it a workhorse technique in crustal and lithospheric studies. |
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