विधियों की तुलना करें

	भूकंपीय पूर्ण-तरंगरूप व्युत्क्रमण	रिसीवर फ़ंक्शन विश्लेषण
क्षेत्र	भूभौतिकी	भूभौतिकी
परिवार	Process / pipeline	Process / pipeline
उद्भव वर्ष	1984	1979
प्रवर्तक	Albert Tarantola	Charles Langston
प्रकार	Seismic imaging and model parameterization technique	Teleseismic body wave analysis for subsurface imaging
मौलिक स्रोत	Tarantola, A. (1984). Inversion of seismic reflection data in the acoustic approximation. Geophysics, 49(8), 1259-1266.	Langston, C. A. (1979). Structure under Mount Rainier, Washington, inferred from teleseismic body waves. Journal of Geophysical Research, 84(B9), 4749-4762.
उपनाम	FWI	RF
संबंधित	3	3
सारांश	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.