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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