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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Format: | Technical Report |
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Massachusetts Institute of Technology. Earth Resources Laboratory
2012
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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. |
first_indexed | 2024-09-23T16:01:38Z |
format | Technical Report |
id | mit-1721.1/75181 |
institution | Massachusetts Institute of Technology |
last_indexed | 2024-09-23T16:01:38Z |
publishDate | 2012 |
publisher | Massachusetts Institute of Technology. Earth Resources Laboratory |
record_format | dspace |
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 |
work_keys_str_mv | AT chengch simulatedannealingdeterminationofshearwavetraveltime AT foleyjack simulatedannealingdeterminationofshearwavetraveltime |