Inversion gradients for acoustic VTI wavefield tomography
dc.contributor.author | Li, V. | |
dc.contributor.author | Wang, Hui | |
dc.contributor.author | Tsvankin, Ilya | |
dc.contributor.author | Díaz, E. | |
dc.contributor.author | Alkhalifah, T. | |
dc.date.accessioned | 2018-12-13T09:10:23Z | |
dc.date.available | 2018-12-13T09:10:23Z | |
dc.date.created | 2018-12-12T02:46:56Z | |
dc.date.issued | 2017 | |
dc.identifier.citation | Li, V. and Wang, H. and Tsvankin, I. and Díaz, E. and Alkhalifah, T. 2017. Inversion gradients for acoustic VTI wavefield tomography. Geophysics. 82 (4): pp. WA55-WA65. | |
dc.identifier.uri | http://hdl.handle.net/20.500.11937/71525 | |
dc.identifier.doi | 10.1190/GEO2016-0624.1 | |
dc.description.abstract |
© 2017 Society of Exploration Geophysicists. All rights reserved. Wavefield tomography can handle complex subsurface geology better than ray-based techniques and, ultimately, provide a higher resolution. Here, we implement forward and adjoint wavefield extrapolation for VTI (transversely isotropic with a vertical symmetry axis) media using a generalized pseudospectral operator based on a separable approximation for the P-wave dispersion relation. This operator is employed to derive the gradients of the differential semblance optimization (DSO) and modified image-power objective functions. We also obtain the gradient expressions for a data-domain objective function that can more easily incorporate borehole information necessary for stable VTI velocity analysis. These gradients are similar to the ones obtained with a space-time finite-difference (FD) scheme for a system of coupled wave equations but the pseudospectral method is not hampered by the imprint of the shear-wave artifact. Numerical examples also show the potential advantages of the modified image-power objective function in estimating the anellipticity parameter ?. | |
dc.publisher | Society of Exploration Geophysics | |
dc.title | Inversion gradients for acoustic VTI wavefield tomography | |
dc.type | Journal Article | |
dcterms.source.volume | 82 | |
dcterms.source.number | 4 | |
dcterms.source.startPage | WA55 | |
dcterms.source.endPage | WA65 | |
dcterms.source.issn | 0016-8033 | |
dcterms.source.title | Geophysics | |
curtin.accessStatus | Fulltext not available |
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