TY - GEN
T1 - An improved full waveform inversion procedure based on scattering angle enrichment
AU - Wu, Z.
AU - Alkhalifah, T.
PY - 2015
Y1 - 2015
N2 - The gradient of standard full waveform inversion (FWI) attempts to map the residuals in the data to perturbations in the model. Such perturbations include smooth background updates from the transmission components and high wavenumber updates from the reflection components. A new optimization approach is used to update the background and perturbed velocity, simultaneously. We also use a more efficient scattering angle filter to enhance the large scattering angle for the background velocity update and enhance the small scattering angle for the perturbed velocity update. This efficient implementation of the filter is fast and requires less memory. Thus, the new FWI procedure updates mainly along the wave-path for both diving and reflected waves in the initial stages. At the same time, it updates the perturbation with mainly reflections (filtering the diving waves). An application to Marmousi model shows that this method converges starting with a linearly increasing velocity, and with data free of frequencies below 4 Hz.
AB - The gradient of standard full waveform inversion (FWI) attempts to map the residuals in the data to perturbations in the model. Such perturbations include smooth background updates from the transmission components and high wavenumber updates from the reflection components. A new optimization approach is used to update the background and perturbed velocity, simultaneously. We also use a more efficient scattering angle filter to enhance the large scattering angle for the background velocity update and enhance the small scattering angle for the perturbed velocity update. This efficient implementation of the filter is fast and requires less memory. Thus, the new FWI procedure updates mainly along the wave-path for both diving and reflected waves in the initial stages. At the same time, it updates the perturbation with mainly reflections (filtering the diving waves). An application to Marmousi model shows that this method converges starting with a linearly increasing velocity, and with data free of frequencies below 4 Hz.
UR - http://www.scopus.com/inward/record.url?scp=85018965077&partnerID=8YFLogxK
U2 - 10.3997/2214-4609.201413211
DO - 10.3997/2214-4609.201413211
M3 - Conference contribution
AN - SCOPUS:85018965077
T3 - 77th EAGE Conference and Exhibition 2015: Earth Science for Energy and Environment
SP - 4082
EP - 4086
BT - 77th EAGE Conference and Exhibition 2015
PB - European Association of Geoscientists and Engineers, EAGE
T2 - 77th EAGE Conference and Exhibition 2015: Earth Science for Energy and Environment
Y2 - 1 June 2015 through 4 June 2015
ER -