P-Wave Train Synthetic Seismograms Calculated by Quantized Ray Theory
The quantized ray theory formulation is used to construct synthetic body wave seismograms from a ray parameter-distance curve. The synthetic seismograms calculated by this new technique compare favourably with the exact Cagniard-de Hoop solutions, but require far less time to produce. The ease and r...
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1974
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fthighwire:oai:open-archive.highwire.org:gji:37/3/407 2023-05-15T15:07:26+02:00 P-Wave Train Synthetic Seismograms Calculated by Quantized Ray Theory McMechan, George A. 1974-06-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/37/3/407 https://doi.org/10.1111/j.1365-246X.1974.tb04093.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/37/3/407 http://dx.doi.org/10.1111/j.1365-246X.1974.tb04093.x Copyright (C) 1974, Oxford University Press Articles TEXT 1974 fthighwire https://doi.org/10.1111/j.1365-246X.1974.tb04093.x 2013-05-28T06:06:24Z The quantized ray theory formulation is used to construct synthetic body wave seismograms from a ray parameter-distance curve. The synthetic seismograms calculated by this new technique compare favourably with the exact Cagniard-de Hoop solutions, but require far less time to produce. The ease and rapidity with which the calculations can be done allow the routine use of synthetic seismograms in body wave inversions. Inclusion of amplitude constraints greatly reduces the range of valid Earth models. As an example, a P -wave velocity-depth model is found for the upper mantle beneath the Canadian Arctic. The model is constrained by ray parameter and travel time data as well as the observed amplitude behaviour in the first 10-15 s of real vertical component seismograms recorded between 10 and 40 degrees. As each arrival observed on each record provides a number of constraints for the ray parameter curve, a relatively few wave trains provide a great amount of information on the velocity structure. Even when individual arrivals cannot be separated on a record, because of interference with each other, synthetic seismograms can be used. The interference pattern itself can be reproduced, and by tracing back through the calculations, one can define the number, amplitudes and travel times of the interfering arrivals. Text Arctic HighWire Press (Stanford University) Arctic Geophysical Journal International 37 3 407 421 |
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English |
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Articles McMechan, George A. P-Wave Train Synthetic Seismograms Calculated by Quantized Ray Theory |
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The quantized ray theory formulation is used to construct synthetic body wave seismograms from a ray parameter-distance curve. The synthetic seismograms calculated by this new technique compare favourably with the exact Cagniard-de Hoop solutions, but require far less time to produce. The ease and rapidity with which the calculations can be done allow the routine use of synthetic seismograms in body wave inversions. Inclusion of amplitude constraints greatly reduces the range of valid Earth models. As an example, a P -wave velocity-depth model is found for the upper mantle beneath the Canadian Arctic. The model is constrained by ray parameter and travel time data as well as the observed amplitude behaviour in the first 10-15 s of real vertical component seismograms recorded between 10 and 40 degrees. As each arrival observed on each record provides a number of constraints for the ray parameter curve, a relatively few wave trains provide a great amount of information on the velocity structure. Even when individual arrivals cannot be separated on a record, because of interference with each other, synthetic seismograms can be used. The interference pattern itself can be reproduced, and by tracing back through the calculations, one can define the number, amplitudes and travel times of the interfering arrivals. |
format |
Text |
author |
McMechan, George A. |
author_facet |
McMechan, George A. |
author_sort |
McMechan, George A. |
title |
P-Wave Train Synthetic Seismograms Calculated by Quantized Ray Theory |
title_short |
P-Wave Train Synthetic Seismograms Calculated by Quantized Ray Theory |
title_full |
P-Wave Train Synthetic Seismograms Calculated by Quantized Ray Theory |
title_fullStr |
P-Wave Train Synthetic Seismograms Calculated by Quantized Ray Theory |
title_full_unstemmed |
P-Wave Train Synthetic Seismograms Calculated by Quantized Ray Theory |
title_sort |
p-wave train synthetic seismograms calculated by quantized ray theory |
publisher |
Oxford University Press |
publishDate |
1974 |
url |
http://gji.oxfordjournals.org/cgi/content/short/37/3/407 https://doi.org/10.1111/j.1365-246X.1974.tb04093.x |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/37/3/407 http://dx.doi.org/10.1111/j.1365-246X.1974.tb04093.x |
op_rights |
Copyright (C) 1974, Oxford University Press |
op_doi |
https://doi.org/10.1111/j.1365-246X.1974.tb04093.x |
container_title |
Geophysical Journal International |
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37 |
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3 |
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407 |
op_container_end_page |
421 |
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1766338941948002304 |