IMPROVED FULL-WAVEFORM INVERSION OF NORMALISED SEISMIC WAVEFIELD DATA
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dc.contributor.author | Kim H.J. | |
dc.contributor.author | Matsuoka T. | |
dc.date.accessioned | 2024-09-14T06:08:22Z | |
dc.date.available | 2024-09-14T06:08:22Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=29556906 | |
dc.identifier.citation | Exploration Geophysics, 2006, 37, 1, 86-92 | |
dc.identifier.issn | 0812-3985 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/45161 | |
dc.description.abstract | The full-waveform inversion algorithm using normalised seismic wavefields can avoid potential inversion errors due to source estimation required in conventional full-waveform inversion methods. In this paper, we have modified the inversion scheme to install a weighted smoothness constraint for better resolution, and to implement a staged approach using normalised wavefields in order of increasing frequency instead of inverting all frequency components simultaneously. The newly developed scheme is verified by using a simple two-dimensional fault model. One of the most significant improvements is based on introducing weights in model parameters, which can be derived from integrated sensitivities. The model-parameter weighting matrix is effective in selectively relaxing the smoothness constraint and in reducing artefacts in the reconstructed image. Simultaneous multiple-frequency inversion can almost be replicated by multiple single-frequency inversions. In particular, consecutively ordered single-frequency inversion, in which lower frequencies are used first, is useful for computation efficiency. © 2006, CSIRO. All rights reserved. | |
dc.subject | CROSS-HOLE | |
dc.subject | FULL WAVEFORM | |
dc.subject | NORMALISED WAVEFIELD | |
dc.subject | SENSITIVITIES | |
dc.subject | TOMOGRAPHY | |
dc.title | IMPROVED FULL-WAVEFORM INVERSION OF NORMALISED SEISMIC WAVEFIELD DATA | |
dc.type | Статья | |
dc.identifier.doi | 10.1071/EG06086 |
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