SEG Technical Program Expanded Abstracts 2012 2012
DOI: 10.1190/segam2012-1535.1
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Improvements in time domain FWI and its applications

Abstract: In this abstract, we describe how to improve time domain full waveform inversion using source wavelet convolution, windowed back propagation and source side illumination. Instead of estimating the source wavelet from field data, a user defined source wavelet can be convolved to field data. This convolution makes waveform matching between modeled and field data easier. Increasing time window applied to residual enables top down velocity update and reduces the possibility of being stuck at a local minimum. The b… Show more

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Cited by 12 publications
(7 citation statements)
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“…The coarsely sampled active-source data (Mirandola example) and the recorded ambient-noise data (SW HUB example and USArray example) are inputs for the interferometric processing. We also convolve the interferometric Green's functions with a known source wavelet (Yoon et al, 2012) and do a 3D-to-2D phase correction (Pica et al, 1990) to avoid the source wavelet estimation and adopt a 2D rather than 3D inversion. After data preprocessing, we first transform the common-shot-gathers (t-x domain) to the frequency domain (f-x domain) and calculate their f-v spectra using the linear Radon transform (equation A-4).…”
Section: Methodsmentioning
confidence: 99%
“…The coarsely sampled active-source data (Mirandola example) and the recorded ambient-noise data (SW HUB example and USArray example) are inputs for the interferometric processing. We also convolve the interferometric Green's functions with a known source wavelet (Yoon et al, 2012) and do a 3D-to-2D phase correction (Pica et al, 1990) to avoid the source wavelet estimation and adopt a 2D rather than 3D inversion. After data preprocessing, we first transform the common-shot-gathers (t-x domain) to the frequency domain (f-x domain) and calculate their f-v spectra using the linear Radon transform (equation A-4).…”
Section: Methodsmentioning
confidence: 99%
“…A modified free-surface boundary condition, which can suppress strong surface waves, is used in the simulation (He et al, 2016). We convolve the observed data with the half-order differentiation of the known wavelet, and thus, we avoid source estimation, while correcting the phase discrepancy between the 3D acquisition and the 2D simulation (Pica et al, 1990;Yoon et al, 2012). The initial model is a 1D…”
Section: Numerical Examplementioning
confidence: 99%
“…It is known that field data contain quite high‐frequency components, and the source wavelet is important for imaging and inversion. Therefore, instead of estimating the source wavelet from the field data and to avoid numerical dispersion, a 15 Hz Ricker wavelet is convolved with the original observed data (Yoon et al, ). In addition to this, it is then used for inversion.…”
Section: Numerical Examplesmentioning
confidence: 99%