The gradient of standard full-waveform inversion (FWI) attempts to map the residuals in the data to perturbations in the model. Such perturbations may include smooth background …
B Chi, L Dong, Y Liu - Geophysics, 2015 - library.seg.org
Because modeling for full-waveform inversion (FWI) cannot produce reflections unless the velocity model has the scattering potential (high wavenumbers), using a …
Full-waveform inversion (FWI) is a highly nonlinear problem due to the complex reflectivity of the earth, and this nonlinearity only increases under the more expensive elastic assumption …
Y Chen, H Chen, K Xiang, X Chen - … to the Monthly Notices of the …, 2016 - academic.oup.com
Full waveform inversion (FWI) is a promising technique for inverting a high-resolution subsurface velocity model. The success of FWI highly depends on a fairly well initial velocity …
T Alkhalifah, Z Wu - Geophysical Prospecting, 2015 - earthdoc.org
Integrating migration velocity analysis and full waveform inversion can help reduce the high non‐linearity of the classic full waveform inversion objective function. The combination of …
We investigate the feasibility of using the dynamic time warping (DTW) technique as an alternative to windowed cross correlation (WCC) for an indirect measure to quantify both the …
DJ Verschuur, XR Staal, AJ Berkhout - The Leading Edge, 2016 - library.seg.org
The future in seismic exploration and seismic monitoring is the inclusion of all orders of scattering in the imaging and inversion algorithms. Using the full wavefield in an inversion …
T Wang, J Cheng, J Geng - Journal of Geophysical Research …, 2021 - Wiley Online Library
In controlled‐source seismology, the standard full waveform inversion (FWI) can't reliably recover the macrovelocity structure in the deep part, if the surface seismic data lack of ultra …
Z Wu, T Alkhalifah - Geophysical Journal International, 2017 - academic.oup.com
Reflection-waveform inversion (RWI) can help us reduce the nonlinearity of the standard full- waveform inversion by inverting for the background velocity model using the wave path of a …