TY - GEN
T1 - Application of the unwrapped phase inversion to land field data with irregular topography
AU - Choi, Y.
AU - Devault, B.
AU - Alkhalifah, T.
PY - 2015
Y1 - 2015
N2 - Phase wrapping effect (or cycle skipping) is a big obstacle for the success of the full waveform inversion when low frequency information is not available. The phase unwrapping process recovers the missing cycles of the data, thus its inversion has a potential to generate an accurate and long wavelength structure model without low frequency information. Recently, the unwrapped phase inversion with an exponential damping was developed to generate a long wavelength structure with somewhat high frequency data. In this study, we apply the unwrapped phase inversion to land field data with a quite high minimum frequency. We also employ a finite-element-based modeling to take account of the irregular topography of the land data. Despite the elastic nature of the data, we use an acoustic-based inversion algorithm for the land data. In the pre-processing, we pick the first arrival traveltime and mute unwanted signals, like Rayleigh waves. We show that the unwrapped phase inversion provides a good convergent long wavelength velocity model. Numerical examples demonstrate that our unwrapped phase inversion result can be a good starting model for the subsequent conventional phase inversion and reverse-time migration on this high frequency, limited offset land data.
AB - Phase wrapping effect (or cycle skipping) is a big obstacle for the success of the full waveform inversion when low frequency information is not available. The phase unwrapping process recovers the missing cycles of the data, thus its inversion has a potential to generate an accurate and long wavelength structure model without low frequency information. Recently, the unwrapped phase inversion with an exponential damping was developed to generate a long wavelength structure with somewhat high frequency data. In this study, we apply the unwrapped phase inversion to land field data with a quite high minimum frequency. We also employ a finite-element-based modeling to take account of the irregular topography of the land data. Despite the elastic nature of the data, we use an acoustic-based inversion algorithm for the land data. In the pre-processing, we pick the first arrival traveltime and mute unwanted signals, like Rayleigh waves. We show that the unwrapped phase inversion provides a good convergent long wavelength velocity model. Numerical examples demonstrate that our unwrapped phase inversion result can be a good starting model for the subsequent conventional phase inversion and reverse-time migration on this high frequency, limited offset land data.
UR - http://www.scopus.com/inward/record.url?scp=85037524478&partnerID=8YFLogxK
U2 - 10.3997/2214-4609.201412910
DO - 10.3997/2214-4609.201412910
M3 - Conference contribution
AN - SCOPUS:85037524478
T3 - 77th EAGE Conference and Exhibition 2015: Earth Science for Energy and Environment
SP - 1811
EP - 1815
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 -