--> Abstract: Gaussian Beam De-Migration and Re-Migration, by Jianming Sheng and Chengbin Peng; #90105 (2010)
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AAPG GEO 2010 Middle East
Geoscience Conference & Exhibition
Innovative Geoscience Solutions – Meeting Hydrocarbon Demand in Changing Times
March 7-10, 2010 – Manama, Bahrain

Gaussian Previous HitBeamNext Hit De-Migration and Re-Migration

Jianming Sheng1; Chengbin Peng1

(1) Nexus Geosciences Inc., Sugar Land, TX.

In this abstract we will present a theoretical framework for demigration of seismic image data under the frame work of Gaussian Previous HitBeamNext Hit theory. The underlying methodology has no dip limitation and handles multi-valued arrivals well. The practical use of this technology is to perform prestack demigration of existing image volumes (CIG gathers) followed by prestack depth remigration using a replacement velocity and/or anisotropy model. The result is a fast, accurate, and cost effective way to improved seismic imaging as compared to proprietary reprocessing from field tapes.

Ross Hill published seminal works in common offset Gaussian Previous HitBeamNext Hit prestack depth migration (Hill, 1991 and 2001). Chevron has been largely the only beneficiary of the Gaussian Previous HitbeamNext Hit technology. To the best of our knowledge there have been no published work on Gaussian Previous HitbeamNext Hit prestack demigration.

For example, in prestack demigration, one can start with an individual common offset image volume (Kirchhoff migration volume, Gaussian Previous HitbeamNext Hit migration volume, or fast Previous HitbeamNext Hit migration volume). The single fold image is demigrated to reconstruct the corresponding input unmigrated seismic data. In Gaussian Previous HitBeamNext Hit prestack demigration, we actually reconstruct the individual beams used as input to the original Gaussian Previous HitBeamNext Hit migration. The individual beams are then synthesized to form an unmigrated seismic volume.

There are many uses of Gausian Previous HitBeamTop prestack demigration technology. For example, it can be used as a fast forward modeling tool to generate synthetic data for migration and inversion. Another use of this technology is to perform prestack demigration of existing image data, followed by prestack depth (re)migration with a replacement velocity and/or anisotropy model. This is a faster, more accurate and cost effective way of seismic imaging over proprietary reprocessing from field tapes. Both synthetic and field data examples of this will be shown.