Simultaneous Inversion of cross-dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear waves

A method to jointly invert for azimuthal angle and dispersion relations from cross-dipole data is presented. Dispersion curves from the joint inversion are compared to both Prony’s method and a simple back propagation schema and an agrrement is found. The azimuthal angle estimate is shown to differ...

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Main Authors: Briggs, Victoria, Rao, Rama V. N., Burns, Daniel R.
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2011
Online Access:http://hdl.handle.net/1721.1/67859
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author Briggs, Victoria
Rao, Rama V. N.
Burns, Daniel R.
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Briggs, Victoria
Rao, Rama V. N.
Burns, Daniel R.
author_sort Briggs, Victoria
collection MIT
description A method to jointly invert for azimuthal angle and dispersion relations from cross-dipole data is presented. Dispersion curves from the joint inversion are compared to both Prony’s method and a simple back propagation schema and an agrrement is found. The azimuthal angle estimate is shown to differ from a frequency domain rotaion that takes no account of dispersion within the waveforms indicating the importance of joint inversion.
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spelling mit-1721.1/678592019-04-12T15:05:20Z Simultaneous Inversion of cross-dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear waves Briggs, Victoria Rao, Rama V. N. Burns, Daniel R. Massachusetts Institute of Technology. Earth Resources Laboratory Briggs, Victoria Rao, Rama V. N. Burns, Daniel R. A method to jointly invert for azimuthal angle and dispersion relations from cross-dipole data is presented. Dispersion curves from the joint inversion are compared to both Prony’s method and a simple back propagation schema and an agrrement is found. The azimuthal angle estimate is shown to differ from a frequency domain rotaion that takes no account of dispersion within the waveforms indicating the importance of joint inversion. Massachusetts Institute of Technology. Earth Resources Laboratory Massachusetts Institute of Technology. Borehole Acoustics and Logging Consortium 2011-12-21T21:38:56Z 2011-12-21T21:38:56Z 2003 Technical Report http://hdl.handle.net/1721.1/67859 Earth Resources Laboratory Industry Consortia Annual Report;2003-03 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Briggs, Victoria
Rao, Rama V. N.
Burns, Daniel R.
Simultaneous Inversion of cross-dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear waves
title Simultaneous Inversion of cross-dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear waves
title_full Simultaneous Inversion of cross-dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear waves
title_fullStr Simultaneous Inversion of cross-dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear waves
title_full_unstemmed Simultaneous Inversion of cross-dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear waves
title_short Simultaneous Inversion of cross-dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear waves
title_sort simultaneous inversion of cross dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear waves
url http://hdl.handle.net/1721.1/67859
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