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Tavakoli F. B., Operto S., Ribodetti Alessandra, Virieux J. (2019). Matrix-free anisotropic slope tomography : theory and application. Geophysics, 84 (1), R21-R43. ISSN 0016-8033

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Lien direct chez l'éditeur doi:10.1190/geo2018-0112.1

Titre
Matrix-free anisotropic slope tomography : theory and application
Année de publication2019
Type de documentArticle référencé dans le Web of Science WOS:000457601800036
AuteursTavakoli F. B., Operto S., Ribodetti Alessandra, Virieux J.
SourceGeophysics, 2019, 84 (1), p. R21-R43. ISSN 0016-8033
RésuméSlope tomography uses traveltimes, source, and receiver slopes of locally coherent events to build subsurface velocity models. Locally coherent events by opposition to continuous reflections are suitable for semiautomatic and dense picking, which is conducive to better resolved tomographic models. These models can be further used as background/initial models for depth migration or full-waveform inversion. Slope tomography conventionally relies on ray tracing for traveltimes and slopes computation, where rays are traced from scatterers in depth to sources and receivers. The inverse problem relies on the explicit building of the sensitivity matrix to update the velocity model by local optimization. Alternatively, slope tomography can be implemented with eikonal solvers, which compute efficiently finely sampled traveltime maps from the sources and receivers, whereas slopes are estimated by finite differences of the traveltime maps. Moreover, a matrix-free inverse problem can be implemented with the adjoint-state method for the estimation of the data-misfit gradient. This new formulation of slope tomography is extended to tilted transverse isotropic (TTI) acoustic media, in which the model space is parameterized by four anisotropic parameters (e.g., vertical wave-speed, Thomson's parameter delta, is an element of,and tilt angle) and the coordinates of the scatterers. A toy synthetic example allows for a first assessment of the crosstalk between anisotropic parameters and scatterer coordinates. A more realistic synthetic example indicates the feasibility of the joint update of the vertical wavespeed and is an element of. The slope tomography is finally applied to real broadband towed-streamer data to build the vertical velocity and the scatterers, while anisotropic parameters is an element of and delta are used as background parameters. The velocity model quality is assessed through common-image gathers computed by TTI Kirchhoff prestack-depth migration.
Plan de classementGéologie et formations superficielles [064] ; Géophysique interne [066] ; Sciences fondamentales / Techniques d'analyse et de recherche [020]
LocalisationFonds IRD [F B010075164]
Identifiant IRDfdi:010075164
Lien permanenthttp://www.documentation.ird.fr/hor/fdi:010075164

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