3D diffraction imaging of linear features and its application to seismic monitoring

Many subsurface features, such as faults, fractures, cracks, or fluid content terminations are defined by geological discontinuities. The seismic response from such features is encoded in diffractions. We develop an algorithm for imaging such discontinuities by detecting edge diffractions. The algor...

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Main Authors: Alonaizi, Faisal, Pevzner, Roman, Bona, Andrej, Shulakova, V., Gurevich, Boris
Format: Journal Article
Published: Wiley-Blackwell 2013
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/18098
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author Alonaizi, Faisal
Pevzner, Roman
Bona, Andrej
Shulakova, V.
Gurevich, Boris
author_facet Alonaizi, Faisal
Pevzner, Roman
Bona, Andrej
Shulakova, V.
Gurevich, Boris
author_sort Alonaizi, Faisal
building Curtin Institutional Repository
collection Online Access
description Many subsurface features, such as faults, fractures, cracks, or fluid content terminations are defined by geological discontinuities. The seismic response from such features is encoded in diffractions. We develop an algorithm for imaging such discontinuities by detecting edge diffractions. The algorithm exploits phase-reversal phenomena of edge diffractions and uses them as a criterion to separate these diffractions from specular reflections and diffractions produced by a leaner object. The performance of the method is demonstrated on both synthetic and real 3D seismic data. The output image focuses the diffracted energy back to its origin and shows high semblance values at the edge of the object. The method is applied on conventionally stacked data producing an image that contains only diffraction events called the D-volume. We also reveal the potential of diffractions to image and track the changes of a CO2 plume using time-lapse analysis and detect any possible CO2 seepage from its primary containment.
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institution Curtin University Malaysia
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publishDate 2013
publisher Wiley-Blackwell
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spelling curtin-20.500.11937-180982017-09-13T13:45:15Z 3D diffraction imaging of linear features and its application to seismic monitoring Alonaizi, Faisal Pevzner, Roman Bona, Andrej Shulakova, V. Gurevich, Boris edge diffraction D-volume semblance Many subsurface features, such as faults, fractures, cracks, or fluid content terminations are defined by geological discontinuities. The seismic response from such features is encoded in diffractions. We develop an algorithm for imaging such discontinuities by detecting edge diffractions. The algorithm exploits phase-reversal phenomena of edge diffractions and uses them as a criterion to separate these diffractions from specular reflections and diffractions produced by a leaner object. The performance of the method is demonstrated on both synthetic and real 3D seismic data. The output image focuses the diffracted energy back to its origin and shows high semblance values at the edge of the object. The method is applied on conventionally stacked data producing an image that contains only diffraction events called the D-volume. We also reveal the potential of diffractions to image and track the changes of a CO2 plume using time-lapse analysis and detect any possible CO2 seepage from its primary containment. 2013 Journal Article http://hdl.handle.net/20.500.11937/18098 10.1111/1365-2478.12063 Wiley-Blackwell restricted
spellingShingle edge diffraction
D-volume
semblance
Alonaizi, Faisal
Pevzner, Roman
Bona, Andrej
Shulakova, V.
Gurevich, Boris
3D diffraction imaging of linear features and its application to seismic monitoring
title 3D diffraction imaging of linear features and its application to seismic monitoring
title_full 3D diffraction imaging of linear features and its application to seismic monitoring
title_fullStr 3D diffraction imaging of linear features and its application to seismic monitoring
title_full_unstemmed 3D diffraction imaging of linear features and its application to seismic monitoring
title_short 3D diffraction imaging of linear features and its application to seismic monitoring
title_sort 3d diffraction imaging of linear features and its application to seismic monitoring
topic edge diffraction
D-volume
semblance
url http://hdl.handle.net/20.500.11937/18098