Microquake seismic interferometry with SVD enhanced Green's function recovery
The conditions under which seismic interferometry (SI) leads to the exact Green’s function (GF) are rarely met in practice, resulting in errors in the recovered GF. To alleviate this problem, we employ additional information than what is typically used in SI. This information comes from the collecti...
| প্রধান লেখক: | , |
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| অন্যান্য লেখক: | |
| বিন্যাস: | Technical Report |
| ভাষা: | en_US |
| প্রকাশিত: |
Massachusetts Institute of Technology. Earth Resources Laboratory
2014
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| বিষয়গুলি: | |
| অনলাইন ব্যবহার করুন: | http://hdl.handle.net/1721.1/90452 |
| _version_ | 1826201236844576768 |
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| author | Melo, Gabriela Malcolm, Alison E. |
| author2 | Massachusetts Institute of Technology. Earth Resources Laboratory |
| author_facet | Massachusetts Institute of Technology. Earth Resources Laboratory Melo, Gabriela Malcolm, Alison E. |
| author_sort | Melo, Gabriela |
| collection | MIT |
| description | The conditions under which seismic interferometry (SI) leads to the exact Green’s function (GF) are rarely met in practice, resulting in errors in the recovered GF. To alleviate this problem, we employ additional information than what is typically used in SI. This information comes from the collection of crosscorrelated traces, one for each source for a pair of receivers, which we shall refer to as the crosscorrelogram. It is by stacking the crosscorrelogram in the source dimension that we obtain an interferometric GF. In general, this crosscorrelogram has both stationary energy that contributes to the estimated GF and non-stationary energy that does not. Stationary energy in the crosscorrelogram is characterized by linearity, coherency, low wavenumber, and thus nearly in-phase events along the source dimension. Non-stationary energy by contrast is characterized by non-linearity, incoherency, high wavenumber, and out-of-phase events along the source dimension. We exploit these differences to separate the two parts of the energy in the crosscorrelogram to obtain more accurate GF estimates for non-ideal cases.
In order to perform this separation and extract more information from the crosscorrelograms we use the singular value decomposition (SVD). We find that SVD is able to enhance physical arrivals that are not properly recovered using standard stacking in SI and inmany cases to recover arrivals that would otherwise be obscured by noise. Here, we filter the crosscorrelograms by using a lower-rank approximation, computed with SVD by keeping only the largest singular values, to enhance events that are coherent across multiple sources, thus isolating this stationary energy that gives the primary contribution to the GF. We illustrate this method with synthetic results for both homogeneous and scattering media simulating a possible application in microseismic monitoring with downhole receivers. |
| first_indexed | 2024-09-23T11:48:45Z |
| format | Technical Report |
| id | mit-1721.1/90452 |
| institution | Massachusetts Institute of Technology |
| language | en_US |
| last_indexed | 2024-09-23T11:48:45Z |
| publishDate | 2014 |
| publisher | Massachusetts Institute of Technology. Earth Resources Laboratory |
| record_format | dspace |
| spelling | mit-1721.1/904522019-04-12T22:09:13Z Microquake seismic interferometry with SVD enhanced Green's function recovery Melo, Gabriela Malcolm, Alison E. Massachusetts Institute of Technology. Earth Resources Laboratory Microseismic Interferometry The conditions under which seismic interferometry (SI) leads to the exact Green’s function (GF) are rarely met in practice, resulting in errors in the recovered GF. To alleviate this problem, we employ additional information than what is typically used in SI. This information comes from the collection of crosscorrelated traces, one for each source for a pair of receivers, which we shall refer to as the crosscorrelogram. It is by stacking the crosscorrelogram in the source dimension that we obtain an interferometric GF. In general, this crosscorrelogram has both stationary energy that contributes to the estimated GF and non-stationary energy that does not. Stationary energy in the crosscorrelogram is characterized by linearity, coherency, low wavenumber, and thus nearly in-phase events along the source dimension. Non-stationary energy by contrast is characterized by non-linearity, incoherency, high wavenumber, and out-of-phase events along the source dimension. We exploit these differences to separate the two parts of the energy in the crosscorrelogram to obtain more accurate GF estimates for non-ideal cases. In order to perform this separation and extract more information from the crosscorrelograms we use the singular value decomposition (SVD). We find that SVD is able to enhance physical arrivals that are not properly recovered using standard stacking in SI and inmany cases to recover arrivals that would otherwise be obscured by noise. Here, we filter the crosscorrelograms by using a lower-rank approximation, computed with SVD by keeping only the largest singular values, to enhance events that are coherent across multiple sources, thus isolating this stationary energy that gives the primary contribution to the GF. We illustrate this method with synthetic results for both homogeneous and scattering media simulating a possible application in microseismic monitoring with downhole receivers. United States. Dept. of Energy; Chevron Corporation; Massachusetts Institute of Technology. Earth Resources Laboratory 2014-09-30T12:14:47Z 2014-09-30T12:14:47Z 2011 Technical Report http://hdl.handle.net/1721.1/90452 en_US Earth Resources Laboratory Industry Consortia Annual Report;2011-12 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory |
| spellingShingle | Microseismic Interferometry Melo, Gabriela Malcolm, Alison E. Microquake seismic interferometry with SVD enhanced Green's function recovery |
| title | Microquake seismic interferometry with SVD enhanced Green's function recovery |
| title_full | Microquake seismic interferometry with SVD enhanced Green's function recovery |
| title_fullStr | Microquake seismic interferometry with SVD enhanced Green's function recovery |
| title_full_unstemmed | Microquake seismic interferometry with SVD enhanced Green's function recovery |
| title_short | Microquake seismic interferometry with SVD enhanced Green's function recovery |
| title_sort | microquake seismic interferometry with svd enhanced green s function recovery |
| topic | Microseismic Interferometry |
| url | http://hdl.handle.net/1721.1/90452 |
| work_keys_str_mv | AT melogabriela microquakeseismicinterferometrywithsvdenhancedgreensfunctionrecovery AT malcolmalisone microquakeseismicinterferometrywithsvdenhancedgreensfunctionrecovery |