TY - GEN
T1 - A two-stage elastic FWI strategy for 2D VTI elastic media to improve c13 structure
AU - Oh, J. W.
AU - Min, D. J.
PY - 2015
Y1 - 2015
N2 - To enhance the feasibility of the multi-parameter full waveform inversion (FWI) for field data, including various types of seismic waves, we introduce a new 2-stage elastic VTI FWI strategy. Because the influence of S-waves on FWI is dominant due to its strong amplitudes in partial derivative wavefields, some parameters may not be recovered well. In the elastic VTI FWI, c13 is a parameter that reverses direction in early stage of inversion due to reversed motions of S-S waves with strong amplitudes. To solve this problem, instead of the virtual source for c13, we use the virtual source for λ in isotropic parameterisation, which includes the Lamé constants and density. This approach is based on the fact that radiation patterns of P-P scattered waves for λ and c13 are similar to each other and that the virtual source for λ generates P-P dominant scattered waves. This approach allows us to enable the inversion process for c13 to behave as if we only use P-P scattered waves to invert c13. Next, we perform the multi-parametric elastic FWI again with original virtual source to compensate for the errors caused in the 1st stage and to conduct the FWI for c13 with full wavefields.
AB - To enhance the feasibility of the multi-parameter full waveform inversion (FWI) for field data, including various types of seismic waves, we introduce a new 2-stage elastic VTI FWI strategy. Because the influence of S-waves on FWI is dominant due to its strong amplitudes in partial derivative wavefields, some parameters may not be recovered well. In the elastic VTI FWI, c13 is a parameter that reverses direction in early stage of inversion due to reversed motions of S-S waves with strong amplitudes. To solve this problem, instead of the virtual source for c13, we use the virtual source for λ in isotropic parameterisation, which includes the Lamé constants and density. This approach is based on the fact that radiation patterns of P-P scattered waves for λ and c13 are similar to each other and that the virtual source for λ generates P-P dominant scattered waves. This approach allows us to enable the inversion process for c13 to behave as if we only use P-P scattered waves to invert c13. Next, we perform the multi-parametric elastic FWI again with original virtual source to compensate for the errors caused in the 1st stage and to conduct the FWI for c13 with full wavefields.
UR - https://www.scopus.com/pages/publications/85019003413
U2 - 10.3997/2214-4609.201413408
DO - 10.3997/2214-4609.201413408
M3 - Conference paper
AN - SCOPUS:85019003413
T3 - 77th EAGE Conference and Exhibition 2015: Earth Science for Energy and Environment
SP - 4097
EP - 4101
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 -