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| Η Τεχνική InSAR (Interferometric Synthetic Aperture Radar)× | Σεισμική Αντιστροφή Πλήρους Κυματομορφής× | |
|---|---|---|
| Πεδίο | Γεωφυσική | Γεωφυσική |
| Οικογένεια | Process / pipeline | Process / pipeline |
| Έτος προέλευσης≠ | 1989 | 1984 |
| Δημιουργός≠ | Gabriel, Goldstein, and Zebker | Albert Tarantola |
| Τύπος≠ | Radar interferometry for millimeter-precision surface deformation | Seismic imaging and model parameterization technique |
| Θεμελιώδης πηγή≠ | Gabriel, A. K., Goldstein, R. M., & Zebker, H. A. (1989). Mapping small elevation changes over large areas: Differential radar interferometry. Journal of Geophysical Research, 94(B7), 9183-9191. DOI ↗ | Tarantola, A. (1984). Inversion of seismic reflection data in the acoustic approximation. Geophysics, 49(8), 1259-1266. DOI ↗ |
| Εναλλακτικές ονομασίες | InSAR | FWI |
| Συναφείς | 3 | 3 |
| Σύνοψη≠ | Interferometric Synthetic Aperture Radar (InSAR) is a radar remote sensing technique that measures millimeter-scale ground surface deformation by analyzing the phase difference between radar images acquired from slightly different orbital positions. Pioneered by Gabriel, Goldstein, and Zebker in 1989, InSAR has become essential for earthquake rupture characterization, volcanic monitoring, landslide detection, and subsidence quantification. | 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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