Simulated Annealing Determination Of Shear Wave Travel Time

The method of simulated annealing is introduced to obtain relative moveouts between different depths from an iso-offset section. This method has been shown to be more consistent than conventional picks based on peaks, troughs, or zero crossings especially in situations where the signal-to-noise r...

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Main Authors: Cheng, C. H., Foley, Jack
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2012
Online Access:http://hdl.handle.net/1721.1/75181
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author Cheng, C. H.
Foley, Jack
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Cheng, C. H.
Foley, Jack
author_sort Cheng, C. H.
collection MIT
description The method of simulated annealing is introduced to obtain relative moveouts between different depths from an iso-offset section. This method has been shown to be more consistent than conventional picks based on peaks, troughs, or zero crossings especially in situations where the signal-to-noise ratio is low or the wavelet is emergent. This method also provides a means of quantifying the relative confidence in each pick over the entire depth of the well. The method has been applied to the data obtained by the ARCO shear wave logging tool and compared favorably with more conventional estimates of shear wave slowness and was shown to be robust, even in areas of weak arrivals.
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spelling mit-1721.1/751812019-04-12T20:30:54Z Simulated Annealing Determination Of Shear Wave Travel Time Cheng, C. H. Foley, Jack Massachusetts Institute of Technology. Earth Resources Laboratory Cheng, C. H. The method of simulated annealing is introduced to obtain relative moveouts between different depths from an iso-offset section. This method has been shown to be more consistent than conventional picks based on peaks, troughs, or zero crossings especially in situations where the signal-to-noise ratio is low or the wavelet is emergent. This method also provides a means of quantifying the relative confidence in each pick over the entire depth of the well. The method has been applied to the data obtained by the ARCO shear wave logging tool and compared favorably with more conventional estimates of shear wave slowness and was shown to be robust, even in areas of weak arrivals. Massachusetts Institute of Technology. Full Waveform Acoustic Logging Consortium 2012-12-03T21:10:51Z 2012-12-03T21:10:51Z 1991 Technical Report http://hdl.handle.net/1721.1/75181 Earth Resources Laboratory Industry Consortia Annual Report;1991-10 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Cheng, C. H.
Foley, Jack
Simulated Annealing Determination Of Shear Wave Travel Time
title Simulated Annealing Determination Of Shear Wave Travel Time
title_full Simulated Annealing Determination Of Shear Wave Travel Time
title_fullStr Simulated Annealing Determination Of Shear Wave Travel Time
title_full_unstemmed Simulated Annealing Determination Of Shear Wave Travel Time
title_short Simulated Annealing Determination Of Shear Wave Travel Time
title_sort simulated annealing determination of shear wave travel time
url http://hdl.handle.net/1721.1/75181
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