Kirchhoff prestack depth migration in simple models of various anisotropy
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F10%3A10051726" target="_blank" >RIV/00216208:11320/10:10051726 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Kirchhoff prestack depth migration in simple models of various anisotropy
Original language description
We apply the Kirchhoff prestack depth migration to calculation of migrated sections in 2-D and 3-D simple anisotropic velocity models. Each velocity model is composed of two homogeneous layers separated by one curved interface. We use different types ofanisotropy in the upper layer: isotropy, transversely isotropic media with a horizontal symmetry axis, triclinic anisotropy and monoclinic anisotropy. We test Kirchhoff prestack depth migration in two ways: a) the anisotropy used for computation of the recorded wave field is the same as the anisotropy used for migration, b) the anisotropy used for computation of the recorded wave field differs from the anisotropy used for migration. In: Seismic Waves in Complex 3-D Structures, Report 20, pp. 35-52, Dep.Geophys., Charles Univ., Prague, 2010
Czech name
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Czech description
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Classification
Type
O - Miscellaneous
CEP classification
DC - Seismology, volcanology and Earth structure
OECD FORD branch
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Result continuities
Project
<a href="/en/project/GAP210%2F10%2F0736" target="_blank" >GAP210/10/0736: New trends in ray methods - part 4</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2010
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů