Estimating Azimuthal Stress-induced P-wave Anisotropy from S-wave Anisotropy Measured byVSP

Anisotropy is sometimes hard to characterize as it requires a number of parameters which are seldom measured on the field. In this study, we present a way to infer azimuthal P-wave anisotropy from measured S-wave anisotropy in areas where anisotropy is known to be caused by the presence of different...

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Main Authors: Collet, O., Gurevich, Boris
Other Authors: EAGE
Format: Conference Paper
Published: EAGE 2014
Online Access:http://hdl.handle.net/20.500.11937/16321
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author Collet, O.
Gurevich, Boris
author2 EAGE
author_facet EAGE
Collet, O.
Gurevich, Boris
author_sort Collet, O.
building Curtin Institutional Repository
collection Online Access
description Anisotropy is sometimes hard to characterize as it requires a number of parameters which are seldom measured on the field. In this study, we present a way to infer azimuthal P-wave anisotropy from measured S-wave anisotropy in areas where anisotropy is known to be caused by the presence of differential stresses acting on the rock. This methodology involves two key steps. In the first one, we estimate the P-wave anisotropy in the dry medium from S-wave anisotropy using a rock physics model which accounts for the stress dependency of seismic velocities in dry elastic isotropic media submitted to triaxial compression. The second major step then consists in calculating the P-wave anisotropy in the saturated medium using the anisotropic Gassmann equations. This workflow is applied to data acquired off North West Australia, in an area where anisotropy is likely to be stress-induced. Such analysis could help constraining orthorhombic tomography or azimuthal AVO analysis.
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institution Curtin University Malaysia
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publishDate 2014
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spelling curtin-20.500.11937-163212017-01-30T11:55:06Z Estimating Azimuthal Stress-induced P-wave Anisotropy from S-wave Anisotropy Measured byVSP Collet, O. Gurevich, Boris EAGE Anisotropy is sometimes hard to characterize as it requires a number of parameters which are seldom measured on the field. In this study, we present a way to infer azimuthal P-wave anisotropy from measured S-wave anisotropy in areas where anisotropy is known to be caused by the presence of differential stresses acting on the rock. This methodology involves two key steps. In the first one, we estimate the P-wave anisotropy in the dry medium from S-wave anisotropy using a rock physics model which accounts for the stress dependency of seismic velocities in dry elastic isotropic media submitted to triaxial compression. The second major step then consists in calculating the P-wave anisotropy in the saturated medium using the anisotropic Gassmann equations. This workflow is applied to data acquired off North West Australia, in an area where anisotropy is likely to be stress-induced. Such analysis could help constraining orthorhombic tomography or azimuthal AVO analysis. 2014 Conference Paper http://hdl.handle.net/20.500.11937/16321 EAGE restricted
spellingShingle Collet, O.
Gurevich, Boris
Estimating Azimuthal Stress-induced P-wave Anisotropy from S-wave Anisotropy Measured byVSP
title Estimating Azimuthal Stress-induced P-wave Anisotropy from S-wave Anisotropy Measured byVSP
title_full Estimating Azimuthal Stress-induced P-wave Anisotropy from S-wave Anisotropy Measured byVSP
title_fullStr Estimating Azimuthal Stress-induced P-wave Anisotropy from S-wave Anisotropy Measured byVSP
title_full_unstemmed Estimating Azimuthal Stress-induced P-wave Anisotropy from S-wave Anisotropy Measured byVSP
title_short Estimating Azimuthal Stress-induced P-wave Anisotropy from S-wave Anisotropy Measured byVSP
title_sort estimating azimuthal stress-induced p-wave anisotropy from s-wave anisotropy measured byvsp
url http://hdl.handle.net/20.500.11937/16321