2001
DOI: 10.1007/978-1-4613-0001-4_1
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Multidimensional Seismic Inversion

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Cited by 29 publications
(49 citation statements)
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“…Depending on the disorder, the renormalization group (RG) flows exhibit a transition to localized regime in any dimension. We have numerically checked the RG results using the transfer-matrix method and direct numerical simulations for one-and two-dimensional systems, respectively.Understanding how waves propagate in heterogeneous media is fundamental to such important problems as earthquakes, underground nuclear explosions, the morphology of oil and gas reservoirs, oceanography, and medical and materials sciences [1]. For example, seismic wave propagation and reflection are used to not only estimate the hydrocarbon content of a potential oil or gas field, but also to image structures located over a wide area, ranging from the Earth's near surface to the deeper crust and upper mantle.…”
mentioning
confidence: 99%
See 1 more Smart Citation
“…Depending on the disorder, the renormalization group (RG) flows exhibit a transition to localized regime in any dimension. We have numerically checked the RG results using the transfer-matrix method and direct numerical simulations for one-and two-dimensional systems, respectively.Understanding how waves propagate in heterogeneous media is fundamental to such important problems as earthquakes, underground nuclear explosions, the morphology of oil and gas reservoirs, oceanography, and medical and materials sciences [1]. For example, seismic wave propagation and reflection are used to not only estimate the hydrocarbon content of a potential oil or gas field, but also to image structures located over a wide area, ranging from the Earth's near surface to the deeper crust and upper mantle.…”
mentioning
confidence: 99%
“…Understanding how waves propagate in heterogeneous media is fundamental to such important problems as earthquakes, underground nuclear explosions, the morphology of oil and gas reservoirs, oceanography, and medical and materials sciences [1]. For example, seismic wave propagation and reflection are used to not only estimate the hydrocarbon content of a potential oil or gas field, but also to image structures located over a wide area, ranging from the Earth's near surface to the deeper crust and upper mantle.…”
mentioning
confidence: 99%
“…The usual travel time migration imaging with the active array is done with the Kirchhoff Migration imaging function [2,3] …”
Section: Formulation Of the Imaging Problemmentioning
confidence: 99%
“…Another linearizing approximation that can be used for re ection from smooth surfaces is the Kirchhoff approximation, in which the scattered eld is replaced by its geometrical optics approximation [8] [25]. Here, however, we consider only the Born approximation.…”
Section: The Model For Scattering From the Targetmentioning
confidence: 99%