Seismic imaging and inversion [electronic resource] : application of linear inverse theory / Robert H. Stol and, Arthur B. Weglein.
"Extracting information from seismic data requires knowledge of seismic wave propagation and reflection. The commonly used method involves solving linearly for a reflectivity at every point within the Earth, but this book follows an alternative approach which invokes inverse scattering theory....
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| Format: | Electronic eBook |
| Language: | English |
| Published: |
Cambridge ; New York :
Cambridge University Press,
2012.
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| Subjects: |
MARC
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| 100 | 1 | |a Stolt, Robert H. |0 http://id.loc.gov/authorities/names/nr87001031 |1 http://isni.org/isni/0000000080940780. | |
| 245 | 1 | 0 | |a Seismic imaging and inversion |h [electronic resource] : |b application of linear inverse theory / |c Robert H. Stol and, Arthur B. Weglein. |
| 260 | |a Cambridge ; |a New York : |b Cambridge University Press, |c 2012. | ||
| 300 | |a 1 online resource (404 pages) | ||
| 336 | |a text |b txt |2 rdacontent. | ||
| 337 | |a computer |b c |2 rdamedia. | ||
| 338 | |a online resource |b cr |2 rdacarrier. | ||
| 504 | |a Includes bibliographical references (pages 397-400) and index. | ||
| 505 | 0 | |a Modeling, migration, imaging, and inversion -- Basic migration concepts -- Prestack migration -- Migration limitations -- Models for wave propagation and reflection -- Green's functions -- The scattering potential -- Reflectivity -- Synthesizing reflection data -- Frequency-wavenumber migration -- Asymptotic modeling and migration -- Residual asymptotic migration -- Asymptotic data mapping and continuation -- Least-squares asymptotic migration. | |
| 520 | |a "Extracting information from seismic data requires knowledge of seismic wave propagation and reflection. The commonly used method involves solving linearly for a reflectivity at every point within the Earth, but this book follows an alternative approach which invokes inverse scattering theory. By developing the theory of seismic imaging from basic principles, the authors relate the different models of seismic propagation, reflection and imaging - thus providing links to reflectivity-based imaging on the one hand and to nonlinear seismic inversion on the other. The comprehensive and physically complete linear imaging foundation developed presents new results at the leading edge of seismic processing for target location and identification. This book serves as a fundamental guide to seismic imaging principles and algorithms and their foundation in inverse scattering theory and is a valuable resource for working geoscientists, scientific programmers and theoretical physicists"-- |c Provided by publisher. | ||
| 520 | |a "Extracting information from seismic data requires knowledge of seismic wave propagation and reflection. The commonly used method involves solving linearly for a reflectivity at every point within the Earth. The resulting reflectivity, however, is not an intrinsic Earth property, and cannot easily be extended to nonlinear processes which might provide a deeper understanding and a more accurate image of the subsurface"-- |c Provided by publisher. | ||
| 546 | |a English. | ||
| 588 | 0 | |a Print version record. | |
| 650 | 0 | |a Seismic reflection method. |0 http://id.loc.gov/authorities/subjects/sh85119625. | |
| 650 | 0 | |a Scattering (Mathematics) |0 http://id.loc.gov/authorities/subjects/sh85118046. | |
| 650 | 0 | |a Linear operators |x Generalized inverses. |0 http://id.loc.gov/authorities/subjects/sh85077179. | |
| 650 | 7 | |a Linear operators |x Generalized inverses. |2 fast |0 (OCoLC)fst00999088. | |
| 650 | 7 | |a Scattering (Mathematics) |2 fast |0 (OCoLC)fst01106580. | |
| 650 | 7 | |a Seismic reflection method. |2 fast |0 (OCoLC)fst01111272. | |
| 700 | 1 | |a Weglein, Arthur B. |0 http://id.loc.gov/authorities/names/n2006057868 |1 http://isni.org/isni/0000000036249546. | |
| 776 | 0 | 8 | |i Print version: |a Stolt, Robert H. |t Seismic imaging and inversion. |d Cambridge ; New York : Cambridge University Press, 2012 |z 9781107014909 |w (DLC) 2011041739 |w (OCoLC)758397288. |
| 856 | 4 | 0 | |u https://colorado.idm.oclc.org/login?url=https://app.knovel.com/hotlink/toc/id:kpSIIALITC/seismic-imaging-and?kpromoter=marc |z Full Text (via Knovel) |
| 880 | 8 | |6 505-00/(S |a 6.1 The general Green's function -- 6.2 The scalar Green's function -- 6.2.1 Constant velocity -- 6.2.2 Depth-variable velocity -- 6.2.3 Generally variable velocity -- 6.3 The acoustic Green's function -- 6.3.1 Constant velocity and density -- 6.3.2 Depth-variable velocity and density -- 6.3.3 Fully variable velocity and density -- 6.3.4 Constant velocity, variable density -- 6.4 The elastic Green's function -- 6.4.1 Constant α, β, ρ -- 6.4.2 Depth-variable α, β, ρ -- 6.4.3 Generally variable α, β, ρ -- 6.5 Local wavenumbers -- 6.6 Multipath Green's functions -- 6.7 Green's functions in a layered medium -- 6.7.1 Two-layer medium -- 6.7.2 Transmission through multiple layers -- 6.7.3 Transmission in 2.5 dimensions -- Exercises -- 7: The scattering potential -- 7.1 The scattering potential as a function of angle -- 7.2 The scalar scattering potential -- 7.3 The acoustic scattering potential -- 7.4 The elastic scattering potential -- 7.4.1 Diagonalization operators -- 7.4.2 Rotation into SV and SH components -- 7.4.3 The P-to-P scattering potential -- 7.4.4 The SH to SH scattering potential -- 7.4.5 The SV to SV scattering potential -- 7.4.6 The SH to SV or P, and SV or P to SH, scattering potentials -- 7.4.7 The P to SV and SV to P scattering potentials -- 7.5 Summary -- Exercises -- 8: Reflectivity -- 8.1 Point reflectivity -- 8.2 A scalar reflectivity function -- 8.3 An acoustic reflectivity function -- 8.4 Elastic reflectivity functions -- 8.4.1 P to P reflectivity -- 8.4.2 SV to SV reflectivity -- 8.4.3 SH to SH reflectivity -- 8.4.4 P to SV reflectivity -- 8.4.5 SV to P reflectivity -- 8.5 A general formula relating scattering potential and reflectivity -- 8.6 Summary of linearized reflectivity functions -- Exercises -- 9: Synthesizing reflection data -- 9.1 The Born model for seismic reflections -- 9.2 A constant background. | |
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