Non-linear arrival time tomography
The use of 1D or pseudo- 3D ray tracing techniques in linearized tomographic problems leads to solutions for which it is difficult to assess the true resolution and error distribution. For this reason, we employ a revised 3D bending algorithm (Moser et al., 1992) and show that it can be used efficie...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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Istituto Nazionale di Geofisica e Vulcanologia (INGV)
1997-06-01
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| Series: | Annals of Geophysics |
| Subjects: | |
| Online Access: | http://www.annalsofgeophysics.eu/index.php/annals/article/view/3937 |
| _version_ | 1811313924743626752 |
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| author | G. Nolet C. B. Papazachos |
| author_facet | G. Nolet C. B. Papazachos |
| author_sort | G. Nolet |
| collection | DOAJ |
| description | The use of 1D or pseudo- 3D ray tracing techniques in linearized tomographic problems leads to solutions for which it is difficult to assess the true resolution and error distribution. For this reason, we employ a revised 3D bending algorithm (Moser et al., 1992) and show that it can be used efficiently for a non-linear inversion in a stepwise scheme. Initial paths are determined from graph theory in order to avoid local minima in bending. The importance of 3D ray tracing in inversion studies and the limitations of the standard 1D approach are demonstrated through synthetic examples. The speed of the ray tracing and the simple scaling scheme allow for an implementation in large-scale tomographic problems. |
| first_indexed | 2024-04-13T11:03:16Z |
| format | Article |
| id | doaj.art-537282205f5e4dcbbe9f2298f95e08c4 |
| institution | Directory Open Access Journal |
| issn | 1593-5213 2037-416X |
| language | English |
| last_indexed | 2024-04-13T11:03:16Z |
| publishDate | 1997-06-01 |
| publisher | Istituto Nazionale di Geofisica e Vulcanologia (INGV) |
| record_format | Article |
| series | Annals of Geophysics |
| spelling | doaj.art-537282205f5e4dcbbe9f2298f95e08c42022-12-22T02:49:21ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1997-06-0140110.4401/ag-3937Non-linear arrival time tomographyG. NoletC. B. PapazachosThe use of 1D or pseudo- 3D ray tracing techniques in linearized tomographic problems leads to solutions for which it is difficult to assess the true resolution and error distribution. For this reason, we employ a revised 3D bending algorithm (Moser et al., 1992) and show that it can be used efficiently for a non-linear inversion in a stepwise scheme. Initial paths are determined from graph theory in order to avoid local minima in bending. The importance of 3D ray tracing in inversion studies and the limitations of the standard 1D approach are demonstrated through synthetic examples. The speed of the ray tracing and the simple scaling scheme allow for an implementation in large-scale tomographic problems.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3937non-linear inversionarrival timesgraph theorybending3D ray tracing |
| spellingShingle | G. Nolet C. B. Papazachos Non-linear arrival time tomography Annals of Geophysics non-linear inversion arrival times graph theory bending 3D ray tracing |
| title | Non-linear arrival time tomography |
| title_full | Non-linear arrival time tomography |
| title_fullStr | Non-linear arrival time tomography |
| title_full_unstemmed | Non-linear arrival time tomography |
| title_short | Non-linear arrival time tomography |
| title_sort | non linear arrival time tomography |
| topic | non-linear inversion arrival times graph theory bending 3D ray tracing |
| url | http://www.annalsofgeophysics.eu/index.php/annals/article/view/3937 |
| work_keys_str_mv | AT gnolet nonlineararrivaltimetomography AT cbpapazachos nonlineararrivaltimetomography |