Imaging with primaries and free-surface multiples by joint least-squares reverse time migration

Author:

Wong Mandy1,Biondi Biondo L.2,Ronen Shuki3

Affiliation:

1. Formerly Stanford Exploration Project, Stanford University, Stanford, California, USA; presently Shell Exploration and Production Company, Houston, Texas, USA..

2. Stanford Exploration Project, Stanford University, Stanford, California, USA..

3. Stanford University, Stanford, California, USA and Dolphin Geophysical, Houston, Texas, USA..

Abstract

We have used joint least-squares reverse time migration (LSRTM), also known as linearized waveform inversion, to jointly image primary and free-surface-multiples data. Although migration of free-surface multiples can provide the benefit of additional illumination, crosstalk artifacts that appear in images pose a challenge for migration-based approaches. Our method formulates the imaging problem as an inversion problem to attenuate these crosstalk noises in the image. We have developed a modified modeling operator that uses the data as an areal source. The modified operator is used in joint LSRTM to account for the free-surface multiples in the data. We have developed 3D synthetic and field data examples to reveal that our proposed method improves imaging in geologically complex areas and attenuated crosstalk artifacts in the image.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference48 articles.

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2. Barr, F. J., and J. I. Sanders, 1989, Attenuation of water-column reverberations using pressure and velocity detectors in a water-bottom cable: 59th Annual International Meeting, SEG, Expanded Abstracts, 653–655.

3. Subsalt 3D VSP imaging at Deimos Field in the deepwater Gulf of Mexico

4. Clapp, M., 2005, Imaging under salt: Illumination compensation by regularized inversion: Ph.D. thesis, Stanford University.

5. Clapp, R. G., 2014, Synthetic model building using a simplified basin modeling approach: Stanford Exploration Project, Report 155, 145–151.

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