4.6 Article

Subsurface wavefields based on the generalized internal multiple imaging

Journal

GEOPHYSICAL JOURNAL INTERNATIONAL
Volume 219, Issue 2, Pages 1212-1224

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/gji/ggz340

Keywords

Image processing; Numerical modelling; Numerical solutions; Waveform inversion; Seismic interferometry; Wave scattering and diffraction

Funding

  1. KAUST

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Full Green's functions between image points and the recording surface are crucial to constructing accurate subsurface wavefields and images beyond the single-scattering assumption. A direct approach to do so is offered by utilizing the recorded data combined with a background imaging velocity. The process includes extrapolating the recorded data back in time followed by a simple interferometric cross-correlation of the back-propagated wavefield with the recorded data. This interferometric step offers the opportunity to extract subsurface Green's functions with first-order scattering forming the transmission component, and the second-order scattering becoming the leading scattering term. A cross-correlation of the resulting, assumed upgoing, wavefield with a forward modelled down going wavefield highlights the double-scattered reflectivity in a process referred to as the generalized internal multiple imaging (GIMI). The resulting image is vulnerable to cross-talk between different order multiples interacting with each other. Thus, we develop the adjoint GIMI operation that takes us from the image to the data, and use it to formulate a least-squares optimization problem to fit the image to the data. The result is reduced cross-talk and cleaner higher resolution multiscattered images. We also extract space extensions of the image, which offers the opportunity to evaluate the focusing capability of the velocity model, and formulate updates for that model based on double scattering. We show the features of this approach on the modified Marmousi model.

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