Marchenko redatuming, imaging, and multiple elimination and their mutual relations

Author:

Wapenaar Kees1ORCID,Brackenhoff Joeri2ORCID,Dukalski Marcin3ORCID,Meles Giovanni4,Reinicke Christian5,Slob Evert1ORCID,Staring Myrna6,Thorbecke Jan1ORCID,van der Neut Joost1ORCID,Zhang Lele1ORCID

Affiliation:

1. Delft University of Technology, Department of Geoscience and Engineering, Stevinweg 1, Delft 2628 CN, The Netherlands.(corresponding author); .

2. Delft University of Technology, Department of Geoscience and Engineering, Stevinweg 1, Delft 2628 CN, The Netherlands and ETH Zürich, Department of Earth Sciences, Sonneggstrasse 5, Zürich 8092, Switzerland..

3. Aramco Overseas Company B.V., Informaticalaan 6-12, Delft 2628 ZD, The Netherlands..

4. Delft University of Technology, Department of Geoscience and Engineering, Stevinweg 1, Delft 2628 CN, The Netherlands and University of Lausanne, Institute of Earth Sciences, Lausanne 1015, Switzerland..

5. Delft University of Technology, Department of Geoscience and Engineering, Stevinweg 1, Delft 2628 CN, The Netherlands and Aramco Overseas Company B.V., Informaticalaan 6-12, Delft 2628 ZD, The Netherlands..

6. Delft University of Technology, Department of Geoscience and Engineering, Stevinweg 1, Delft 2628 CN, The Netherlands and Fugro Innovation and Technology, Prismastraat 4, Nootdorp 2631 RT, The Netherlands..

Abstract

With the Marchenko method, it is possible to retrieve Green’s functions between virtual sources in the subsurface and receivers at the surface from reflection data at the surface and focusing functions. A macro model of the subsurface is needed to estimate the first arrival; the internal multiples are retrieved entirely from the reflection data. The retrieved Green’s functions form the input for redatuming by multidimensional deconvolution (MDD). The redatumed reflection response is free of internal multiples related to the overburden. Alternatively, the redatumed response can be obtained by applying a second focusing function to the retrieved Green’s functions. This process is called Marchenko redatuming by double focusing. It is more stable and better suited for an adaptive implementation than Marchenko redatuming by MDD, but it does not eliminate the multiples between the target and the overburden. An attractive efficient alternative is plane-wave Marchenko redatuming, which retrieves the responses to a limited number of plane-wave sources at the redatuming level. In all cases, an image of the subsurface can be obtained from the redatumed data, free of the artifacts caused by internal multiples. Another class of Marchenko methods aims at eliminating the internal multiples from the reflection data, while keeping the sources and receivers at the surface. A specific characteristic of this form of multiple elimination is that it predicts and subtracts all orders of internal multiples with the correct amplitude, without needing a macro subsurface model. Like Marchenko redatuming, Marchenko multiple elimination can be implemented as an MDD process, a double dereverberation process, or an efficient plane-wave oriented process. We have systematically examined the different approaches to Marchenko redatuming, imaging, and multiple elimination using a common mathematical framework.

Funder

H2020 European Research Council

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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