SEG Technical Program Expanded Abstracts 2009 2009
DOI: 10.1190/1.3255050
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Image‐guided blended neighbor interpolation of scattered data

Abstract: Uniformly sampled images are often used to interpolate other data acquired more sparsely with an entirely different mode of measurement. For example, downhole tools enable geophysical properties to be measured with high precision near boreholes that are scattered spatially, and less precise seismic images acquired at the earth's surface are used to interpolate those properties at locations far away from the boreholes. Image-guided interpolation is designed specifically to enhance this process. Most existing me… Show more

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Cited by 64 publications
(55 citation statements)
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“…The biharmonic interpolant used for method 2 is very smooth compared to alternative interpolation methods, including polynomial interpolation, neighborhood-based methods, and harmonic interpolation. 31 The smoothness comes about because each dose point's force is determined in relation to radial basis functions defined for all other points, as shown in Appendix. Nonsmooth interpolants are not well suited for this application, where control points are sparse, given the size of the body phantom, since the interpolations respond to noisy dose point measurements with sudden bumps and overshoot characteristics which we do not see in our 2D dose profile.…”
Section: Discussionmentioning
confidence: 99%
“…The biharmonic interpolant used for method 2 is very smooth compared to alternative interpolation methods, including polynomial interpolation, neighborhood-based methods, and harmonic interpolation. 31 The smoothness comes about because each dose point's force is determined in relation to radial basis functions defined for all other points, as shown in Appendix. Nonsmooth interpolants are not well suited for this application, where control points are sparse, given the size of the body phantom, since the interpolations respond to noisy dose point measurements with sudden bumps and overshoot characteristics which we do not see in our 2D dose profile.…”
Section: Discussionmentioning
confidence: 99%
“…When solving the above anisotropic eikonal equation for the minimal-distance map tðxÞ, it is straightforward to simultaneously obtain the nearest neighbor interpolant (Hale, 2009). A known sample x k is nearest to a point x only if the non-Euclidean distance tðxÞ is less than that for any other known sample point.…”
Section: Dtwmentioning
confidence: 99%
“…One way to check for possible errors in wellseismic ties is to extend the well-log measurements along seismic reflectors to compute an image-guided nearest neighbor interpolation (Hale, 2010b) of the measurements. In this method, assuming that we have a set of k known well-log values V ¼ fv 1 ; v 2 ; : : : ; v k g (v k ∈ R) that are spatially scattered at corresponding k known locations X ¼ fx 1 ; x 2 ; : : : ; x k g, we then compute an image-guided nearest neighbor interpolation of the known values by solving the following anisotropic eikonal equation (Hale, 2009): ∇tðxÞ · DðxÞ∇tðxÞ ¼ 1; x ∈ = X ; tðxÞ ¼ 0;…”
Section: Dtwmentioning
confidence: 99%
“…where x ¼ ðx 1 ; x 2 ; x 3 Þ represent the 3D spatial coordinates within the 3D seismic image ( Figure 1a) and tðxÞ is a map of non-Euclidean distance (Hale, 2009) from x to the nearest known sample x k . When solving the above anisotropic eikonal equation for the minimal-distance map tðxÞ, it is straightforward to simultaneously obtain the nearest neighbor interpolant (Hale, 2009).…”
Section: Dtwmentioning
confidence: 99%