Migração 3D no tempo usando a teoria dos raios paraxiais
This presentation aims at the 3-D time migration of zero offset data, in true amplitude. This method is based on paraxial ray theory and uses a diffraction time function which is directly and correctly determined by the measurement of pre-stack seismic data. It is not necessary to know a macro veloc...
| Autor principal: | QUEIROZ, Norcirio Pantoja |
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| Grau: | Dissertação |
| Idioma: | por |
| Publicado em: |
Universidade Federal do Pará
2014
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| Assuntos: | |
| Acesso em linha: |
http://repositorio.ufpa.br/jspui/handle/2011/5920 |
| Resumo: |
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This presentation aims at the 3-D time migration of zero offset data, in true amplitude. This method is based on paraxial ray theory and uses a diffraction time function which is directly and correctly determined by the measurement of pre-stack seismic data. It is not necessary to know a macro velocity model in order to apply the time migration. In order to obtain a true amplitude time migration the migration result must be multiplied by a scaling factor and convolved with a known function. Together with a scaling factor, a filter was applied in order to recover the signal phase altered during the migration process. Due to the computational limitation synthetic dada in 2-D was used aims to test the program efficiency. The result was satisfactory, showing the efficiency and robustness of process. |