Abstract
Full-waveform inversion (FWI) suffers from the cycle-skipping problem when the available frequency-band of data is not low enough. We have applied an exponential damping to the data to generate artificial low frequencies, which helps FWI to avoid cycle skipping. In this case, the least-squares misfit function does not properly deal with the exponentially damped wavefield in FWI because the amplitude of traces decays almost exponentially with increasing offset in a damped wavefield. Thus, we use a deconvolution-based objective function for FWI of the exponentially damped wavefield. The deconvolution filter includes inherently a normalization between the modeled and observed data; thus, it can address the unbalanced amplitude of a damped wavefield. We specifically normalize the modeled data with the observed data in the frequency-domain to estimate the deconvolution filter and selectively choose a frequency-band for normalization that mainly includes the artificial low frequencies. We calculate the gradient of the objective function using the adjoint-state method. The synthetic and benchmark data examples indicate that our FWI algorithm generates a convergent long-wavelength structure without low-frequency information in the recorded data.
Original language | English (US) |
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Pages (from-to) | R77-R88 |
Journal | Geophysics |
Volume | 83 |
Issue number | 2 |
DOIs | |
State | Published - Mar 1 2018 |
Bibliographical note
Publisher Copyright:© 2018 Society of Exploration Geophysicists.
Keywords
- Amplitude
- Deconvolution
- Full-waveform inversion
- Low frequency
- Time-domain
ASJC Scopus subject areas
- Geochemistry and Petrology