Effects Of Layer Boundaries On Fwal And Dip Estimation (Oblique Events)
Data recorded by the full waveform acoustic logging tool EVA shows events generated at acoustic layer boundaries. These can be interpreted as reflections on and transmissions through interfaces. Ray modelling shows that these events are very sensitive to the dip. After processing of an iso-offset...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Technical Report |
| Published: |
Massachusetts Institute of Technology. Earth Resources Laboratory
2012
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| Online Access: | http://hdl.handle.net/1721.1/75065 |
| _version_ | 1826200298228547584 |
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| author | Paternoster, Benoit Larrere, Marc |
| author2 | Massachusetts Institute of Technology. Earth Resources Laboratory |
| author_facet | Massachusetts Institute of Technology. Earth Resources Laboratory Paternoster, Benoit Larrere, Marc |
| author_sort | Paternoster, Benoit |
| collection | MIT |
| description | Data recorded by the full waveform acoustic logging tool EVA shows events
generated at acoustic layer boundaries. These can be interpreted as reflections on
and transmissions through interfaces. Ray modelling shows that these events are
very sensitive to the dip. After processing of an iso-offset section designed to
enhance and separate such events, two sections are interpreted and the dip angles
of the interfaces are estimated. |
| first_indexed | 2024-09-23T11:34:20Z |
| format | Technical Report |
| id | mit-1721.1/75065 |
| institution | Massachusetts Institute of Technology |
| last_indexed | 2024-09-23T11:34:20Z |
| publishDate | 2012 |
| publisher | Massachusetts Institute of Technology. Earth Resources Laboratory |
| record_format | dspace |
| spelling | mit-1721.1/750652019-04-12T20:27:44Z Effects Of Layer Boundaries On Fwal And Dip Estimation (Oblique Events) Paternoster, Benoit Larrere, Marc Massachusetts Institute of Technology. Earth Resources Laboratory Paternoster, Benoit Larrere, Marc Data recorded by the full waveform acoustic logging tool EVA shows events generated at acoustic layer boundaries. These can be interpreted as reflections on and transmissions through interfaces. Ray modelling shows that these events are very sensitive to the dip. After processing of an iso-offset section designed to enhance and separate such events, two sections are interpreted and the dip angles of the interfaces are estimated. 2012-11-27T20:38:05Z 2012-11-27T20:38:05Z 1985 Technical Report http://hdl.handle.net/1721.1/75065 Earth Resources Laboratory Industry Consortia Annual Report;1985-07 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory |
| spellingShingle | Paternoster, Benoit Larrere, Marc Effects Of Layer Boundaries On Fwal And Dip Estimation (Oblique Events) |
| title | Effects Of Layer Boundaries On Fwal And Dip Estimation (Oblique Events) |
| title_full | Effects Of Layer Boundaries On Fwal And Dip Estimation (Oblique Events) |
| title_fullStr | Effects Of Layer Boundaries On Fwal And Dip Estimation (Oblique Events) |
| title_full_unstemmed | Effects Of Layer Boundaries On Fwal And Dip Estimation (Oblique Events) |
| title_short | Effects Of Layer Boundaries On Fwal And Dip Estimation (Oblique Events) |
| title_sort | effects of layer boundaries on fwal and dip estimation oblique events |
| url | http://hdl.handle.net/1721.1/75065 |
| work_keys_str_mv | AT paternosterbenoit effectsoflayerboundariesonfwalanddipestimationobliqueevents AT larreremarc effectsoflayerboundariesonfwalanddipestimationobliqueevents |