Data-driven internal multiple elimination and its consequences for imaging : A comparison of strategies

We have compared three data-driven internal multiple reflection elimination schemes derived from the Marchenko equations and inverse scattering series (ISS). The two schemes derived from Marchenko equations are similar but use different truncation operators. The first scheme creates a new data set without internal multiple reflections. The second scheme does the same and compensates for transmission losses in the primary reflections. The scheme derived from ISS is equal to the result after the first iteration of the first Marchenko-based scheme. It can attenuate internal multiple reflections with residuals. We evaluate the success of these schemes with 2D numerical examples. It is shown that Marchenko-based data-driven schemes are relatively more robust for internal multiple reflection elimination at a higher computational cost.

[1]  R. Snieder,et al.  Connection of scattering principles: a visual and mathematical tour , 2012 .

[2]  Evert Slob,et al.  Accounting for free-surface multiples in Marchenko imaging , 2017 .

[3]  Kees Wapenaar,et al.  Reconstructing the primary reflections in seismic data by Marchenko redatuming and convolutional interferometry , 2016 .

[4]  Evert Slob,et al.  Transmission compensated primary reflection retrieval in the data domain and consequences for imaging , 2019, GEOPHYSICS.

[5]  Joost van der Neut,et al.  Adaptive overburden elimination with the multidimensional Marchenko equation , 2016 .

[6]  Evert Slob,et al.  Marchenko imaging: Imaging with primaries, internal multiples, and free-surface multiples , 2015 .

[7]  Jan Thorbecke,et al.  Finite‐difference modeling experiments for seismic interferometry , 2010 .

[8]  Arthur B. Weglein,et al.  An inverse-scattering series method for attenuating multiples in seismic reflection data , 1997 .

[9]  Fons ten Kroode,et al.  Prediction of internal multiples , 2002 .

[10]  Matteo Ravasi,et al.  Rayleigh-Marchenko redatuming for target-oriented, true-amplitude imaging , 2017 .

[11]  Helmut Jakubowicz Wave Equation Prediction And Removal of Interbed Multiples , 1998 .

[12]  D. J. Verschuur,et al.  Adaptive surface-related multiple elimination , 1992 .

[13]  Andrew Curtis,et al.  Relating source-receiver interferometry to an inverse-scattering series to derive a new method to estimate internal multiples , 2016 .

[14]  Evert Slob,et al.  Free-surface and internal multiple elimination in one step without adaptive subtraction , 2019, GEOPHYSICS.

[15]  D. J. Verschuur,et al.  Estimation of multiple scattering by iterative inversion, Part I: Theoretical considerations , 1997 .

[16]  Ken H. Matson,et al.  Inverse Scattering Internal Multiple Attenuation: Results From Complex Synthetic And Field Data Examples , 1999 .

[17]  Evert Slob,et al.  Artifact-free reverse time migration , 2018, GEOPHYSICS.

[18]  Evert Slob,et al.  Marchenko imagingMarchenko imaging , 2014 .

[19]  Yi Luo,et al.  Elimination of land internal multiples based on the inverse scattering series , 2011 .

[20]  Dan Hampson,et al.  Inverse Velocity Stacking For Multiple Elimination , 1986 .

[21]  Evert Slob,et al.  Seismic reflector imaging using internal multiples with Marchenko-type equations , 2014 .

[22]  Lele Zhang,et al.  Marchenko scheme based internal multiple reflection elimination in acoustic wavefield , 2018, Journal of Applied Geophysics.