Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022830153> ?p ?o ?g. }
Showing items 1 to 95 of
95
with 100 items per page.
- W2022830153 endingPage "903" @default.
- W2022830153 startingPage "897" @default.
- W2022830153 abstract "The main difficulties in anisotropic velocity analysis and inversion using surface seismic data are associated with the multiparameter nature of the problem and inherent trade‐offs between the model parameters. For the most common anisotropic model, transverse isotropy with a vertical symmetry axis (VTI media), P-wave kinematic signatures are controlled by the vertical velocity V 0 and the anisotropic parameters ε and δ. However, only two combinations of these parameters—NMO velocity from a horizontal reflector V nmo (0) and the anellipticity coefficient η—can be determined from P-wave reflection traveltimes if the medium above the reflector is laterally homogeneous. While V nmo (0) and η are sufficient for time‐domain imaging in VTI media, they cannot be used to resolve the vertical velocity and build velocity models needed for depth migration. Here, we demonstrate that P-wave reflection data can be inverted for all three relevant VTI parameters (V 0 , ε and δ) if the model contains nonhorizontal intermediate interfaces. Using anisotropic reflection tomography, we carry out parameter estimation for a two‐layer medium with a curved intermediate interface and reconstruct the correct anisotropic depth model. To explain the success of this inversion procedure, we present an analytic study of reflection traveltimes for this model and show that the information about the vertical velocity and reflector depth was contained in the reflected rays which crossed the dipping intermediate interface. The results of this work are especially encouraging because the need for depth imaging (such as prestack depth migration) arises mostly in laterally heterogeneous media. Still, we restricted this study to a relatively simple model and constrained the inversion by assuming that one of the layers is isotropic. In general, although lateral heterogeneity does create a dependence of P-wave reflection traveltimes on the vertical velocity, there is no guarantee that for more complicated models all anisotropic parameters can be resolved in a unique fashion." @default.
- W2022830153 created "2016-06-24" @default.
- W2022830153 creator A5003205059 @default.
- W2022830153 creator A5068635131 @default.
- W2022830153 creator A5074910484 @default.
- W2022830153 date "2001-05-01" @default.
- W2022830153 modified "2023-09-27" @default.
- W2022830153 title "Depth‐domain velocity analysis in VTI media using surfaceP-wave data: Is it feasible?" @default.
- W2022830153 cites W1987728976 @default.
- W2022830153 cites W1988125113 @default.
- W2022830153 cites W1988998716 @default.
- W2022830153 cites W2011903283 @default.
- W2022830153 cites W2028943300 @default.
- W2022830153 cites W2043934723 @default.
- W2022830153 cites W2047497200 @default.
- W2022830153 cites W2047784475 @default.
- W2022830153 cites W2082757142 @default.
- W2022830153 cites W2098274171 @default.
- W2022830153 cites W2115926364 @default.
- W2022830153 cites W2127165009 @default.
- W2022830153 cites W2136811094 @default.
- W2022830153 cites W2157879487 @default.
- W2022830153 cites W2161294688 @default.
- W2022830153 doi "https://doi.org/10.1190/1.1444979" @default.
- W2022830153 hasPublicationYear "2001" @default.
- W2022830153 type Work @default.
- W2022830153 sameAs 2022830153 @default.
- W2022830153 citedByCount "22" @default.
- W2022830153 countsByYear W20228301532012 @default.
- W2022830153 countsByYear W20228301532013 @default.
- W2022830153 countsByYear W20228301532014 @default.
- W2022830153 countsByYear W20228301532015 @default.
- W2022830153 countsByYear W20228301532016 @default.
- W2022830153 countsByYear W20228301532019 @default.
- W2022830153 crossrefType "journal-article" @default.
- W2022830153 hasAuthorship W2022830153A5003205059 @default.
- W2022830153 hasAuthorship W2022830153A5068635131 @default.
- W2022830153 hasAuthorship W2022830153A5074910484 @default.
- W2022830153 hasConcept C101842124 @default.
- W2022830153 hasConcept C109661024 @default.
- W2022830153 hasConcept C120665830 @default.
- W2022830153 hasConcept C121332964 @default.
- W2022830153 hasConcept C127313418 @default.
- W2022830153 hasConcept C165205528 @default.
- W2022830153 hasConcept C184050105 @default.
- W2022830153 hasConcept C1893757 @default.
- W2022830153 hasConcept C199360897 @default.
- W2022830153 hasConcept C2524010 @default.
- W2022830153 hasConcept C2778415886 @default.
- W2022830153 hasConcept C2982854487 @default.
- W2022830153 hasConcept C33923547 @default.
- W2022830153 hasConcept C41008148 @default.
- W2022830153 hasConcept C65682993 @default.
- W2022830153 hasConcept C76155785 @default.
- W2022830153 hasConcept C77928131 @default.
- W2022830153 hasConcept C85725439 @default.
- W2022830153 hasConceptScore W2022830153C101842124 @default.
- W2022830153 hasConceptScore W2022830153C109661024 @default.
- W2022830153 hasConceptScore W2022830153C120665830 @default.
- W2022830153 hasConceptScore W2022830153C121332964 @default.
- W2022830153 hasConceptScore W2022830153C127313418 @default.
- W2022830153 hasConceptScore W2022830153C165205528 @default.
- W2022830153 hasConceptScore W2022830153C184050105 @default.
- W2022830153 hasConceptScore W2022830153C1893757 @default.
- W2022830153 hasConceptScore W2022830153C199360897 @default.
- W2022830153 hasConceptScore W2022830153C2524010 @default.
- W2022830153 hasConceptScore W2022830153C2778415886 @default.
- W2022830153 hasConceptScore W2022830153C2982854487 @default.
- W2022830153 hasConceptScore W2022830153C33923547 @default.
- W2022830153 hasConceptScore W2022830153C41008148 @default.
- W2022830153 hasConceptScore W2022830153C65682993 @default.
- W2022830153 hasConceptScore W2022830153C76155785 @default.
- W2022830153 hasConceptScore W2022830153C77928131 @default.
- W2022830153 hasConceptScore W2022830153C85725439 @default.
- W2022830153 hasIssue "3" @default.
- W2022830153 hasLocation W20228301531 @default.
- W2022830153 hasOpenAccess W2022830153 @default.
- W2022830153 hasPrimaryLocation W20228301531 @default.
- W2022830153 hasRelatedWork W1996338263 @default.
- W2022830153 hasRelatedWork W2078831459 @default.
- W2022830153 hasRelatedWork W2104005719 @default.
- W2022830153 hasRelatedWork W2158787742 @default.
- W2022830153 hasRelatedWork W2162432441 @default.
- W2022830153 hasRelatedWork W2203836871 @default.
- W2022830153 hasRelatedWork W2314513269 @default.
- W2022830153 hasRelatedWork W2317008275 @default.
- W2022830153 hasRelatedWork W2329335609 @default.
- W2022830153 hasRelatedWork W2377225658 @default.
- W2022830153 hasVolume "66" @default.
- W2022830153 isParatext "false" @default.
- W2022830153 isRetracted "false" @default.
- W2022830153 magId "2022830153" @default.
- W2022830153 workType "article" @default.