skip to main content
DOE PAGES title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Azimuthally Anisotropic 3D Velocity Continuation

Abstract

We extend time-domain velocity continuation to the zero-offset 3D azimuthally anisotropic case. Velocity continuation describes how a seismic image changes given a change in migration velocity. This description turns out to be of a wave propagation process, in which images change along a velocity axis. In the anisotropic case, the velocity model is multiparameter. Therefore, anisotropic image propagation is multidimensional. We use a three-parameter slowness model, which is related to azimuthal variations in velocity, as well as their principal directions. This information is useful for fracture and reservoir characterization from seismic data. We provide synthetic diffraction imaging examples to illustrate the concept and potential applications of azimuthal velocity continuation and to analyze the impulse response of the 3D velocity continuation operator.

Authors:
 [1];  [1]
  1. The University of Texas at Austin, TX 78712, Austin, USA
Publication Date:
Sponsoring Org.:
USDOE
OSTI Identifier:
1198288
Resource Type:
Published Article
Journal Name:
International Journal of Geophysics
Additional Journal Information:
Journal Name: International Journal of Geophysics Journal Volume: 2011; Journal ID: ISSN 1687-885X
Publisher:
Hindawi Publishing Corporation
Country of Publication:
Country unknown/Code not available
Language:
English

Citation Formats

Burnett, William, and Fomel, Sergey. Azimuthally Anisotropic 3D Velocity Continuation. Country unknown/Code not available: N. p., 2011. Web. doi:10.1155/2011/484653.
Burnett, William, & Fomel, Sergey. Azimuthally Anisotropic 3D Velocity Continuation. Country unknown/Code not available. doi:10.1155/2011/484653.
Burnett, William, and Fomel, Sergey. Sat . "Azimuthally Anisotropic 3D Velocity Continuation". Country unknown/Code not available. doi:10.1155/2011/484653.
@article{osti_1198288,
title = {Azimuthally Anisotropic 3D Velocity Continuation},
author = {Burnett, William and Fomel, Sergey},
abstractNote = {We extend time-domain velocity continuation to the zero-offset 3D azimuthally anisotropic case. Velocity continuation describes how a seismic image changes given a change in migration velocity. This description turns out to be of a wave propagation process, in which images change along a velocity axis. In the anisotropic case, the velocity model is multiparameter. Therefore, anisotropic image propagation is multidimensional. We use a three-parameter slowness model, which is related to azimuthal variations in velocity, as well as their principal directions. This information is useful for fracture and reservoir characterization from seismic data. We provide synthetic diffraction imaging examples to illustrate the concept and potential applications of azimuthal velocity continuation and to analyze the impulse response of the 3D velocity continuation operator.},
doi = {10.1155/2011/484653},
journal = {International Journal of Geophysics},
number = ,
volume = 2011,
place = {Country unknown/Code not available},
year = {2011},
month = {1}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record
DOI: 10.1155/2011/484653

Save / Share: