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GeoRef Categories
Era and Period
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Availability
Log-validated waveform inversion of reflection seismic data with wavelet phase and amplitude updating Available to Purchase
Estimation of elastic constants for HTI media using Gauss-Newton and full-Newton multiparameter full-waveform inversion Available to Purchase
Efficient pseudo-Gauss-Newton full-waveform inversion in the τ - p domain Available to Purchase
Azimuthal amplitude variation with offset analysis of physical modeling data acquired over an azimuthally anisotropic medium Available to Purchase
Fractured shale description using isotropic seismic analysis Available to Purchase
Surface-consistent matching filters for time-lapse seismic processing Available to Purchase
Gabor deconvolution: Estimating reflectivity by nonstationary deconvolution of seismic data Available to Purchase
The wedge model revisited: A physical modeling experiment Available to Purchase
Direct downward continuation from topography using explicit wavefield extrapolation Available to Purchase
Seismic depth imaging with the Gabor transform Available to Purchase
The equivalent offset method of prestack time migration Available to Purchase
Abstract A prestack time migration is presented that is simple, efficient, and provides detailed velocity information. It is based on Kirchhoff prestack time migration and can be applied to both 2-D and 3-D data. The method is divided into two steps: the first is a gathering process that forms common scatterpoint (CSP) gathers; the second is a focusing process that applies a simplified Kirchhoff migration on the CSP gathers, and consists of scaling filtering, normal moveout (NMO) correction, and stacking. A key concept of the method is a reformulation of the double square-root equation (of source-scatterpoint-receiver traveltimes) into a single square root. The single square root uses an equivalent offset that is the surface distance from the scatterpoint to a educated source and receiver. Input samples are mapped into offset bins of a CSP gather, without time shifting, to an offset defined by the equivalent offset. The single square-root reformulation gathers scattered energy to hyperbolic paths on the appropriate CSP gathers.