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Modeling and inversion of PS-wave moveout asymmetry for tilted TI media: Part 1 - Horizontal TTI layer

DRS at CSIR-National Institute of Oceanography

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Title Modeling and inversion of PS-wave moveout asymmetry for tilted TI media: Part 1 - Horizontal TTI layer
 
Creator Dewangan, P.
Tsvankin, I.
 
Subject Mode-converted waves
Anisotropic velocity
 
Description One of the distinctive features of mode-converted waves is their asymmetric moveout (i.e., the PS-wave traveltime in general is different if the source and receiver are interchanged) caused by lateral heterogeneity or elastic anisotropy. If the medium is anisotropic, the PS-wave moveout asymmetry contains valuable information for parameter estimation that cannot be obtained from pure reflection modes. The so-called PP + PS = SS method is generalized, which is designed to replace reflected PS modes in velocity analysis with pure (unconverted) SS-waves, by supplementing the output SS traces with the moveout-asymmetry attributes of PS-waves. The time-asymmetry attribute delta tPS is computed in the slowness domain as the difference between the paired traveltimes of the PS arrivals corresponding to ray parameters (horizontal slownesses) of equal magnitude but opposite sign. Another useful asymmetry attribute is the offset X sub(min) of the PS-wave traveltime minimum on a common-midpoint (CMP) gather. The effectiveness of the developed algorithm and the importance of including the asymmetry attributes of PS-waves in anisotropic velocity analysis for a horizontal transversely isotropic layer with a tilted symmetry axis (or TTI) medium are demonstrated. Simple analytic expressions for the moveout asymmetry PSV-waves, derived in the weak-anisotropy approximation, verified by anisotropic ray tracing. The attribute delta tPS is proportional to the anellipticity parameter eta and reaches its maximum when the symmetry axis deviates by 20 degrees-30 degrees from the vertical horizontal direction. All relevant parameters of a TTI layer can be estimated by nonlinear inversion of the NMO velocities and zero-offset traveltimes of PP- and SS-(SVSV) waves combined with the moveout-asymmetry attributes of the PSV-wave. The inversion of puremode (PP and SS) moveouts alone is nonunique, while the addition of the attributes delta tPS and X min yields stable parameter estimates from 2D data acquired in the vertical symmetry-axis plane. If the TTI model is formed by obliquely dipping fractures, the anisotropic parameters can be inverted further for the fracture orientation and compliances
 
Date 2007-04-13T07:19:42Z
2007-04-13T07:19:42Z
2006
 
Type Journal Article
 
Identifier Geophysics, vol.71(4), D107-D121pp.
http://drs.nio.org/drs/handle/2264/579
 
Language en
 
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Publisher Society of Exploration Geophysicists