1991
DOI: 10.1190/1.1443080
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Tomographic traveltime inversion using natural pixels

Abstract: The problem consists of determining the unknown coefficients an from the measured traveltimes. Once these coefficients have been calculated, the computation of the sum (1) is straightforward.The representation (1) has two important degrees of freedom that influence decisively the kind of results obtained. These are the number (M) and kind of functions I3n(r) to be used. The most common choice for the functions f3n(r) is orthogonal cells (square or cubic pixels), and in that case the coefficients an represent t… Show more

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Cited by 39 publications
(23 citation statements)
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“…Traveltime inversion algorithms yield good results in some cases, e.g. cross-hole tomography (McMechan 1983;Wong, Hurley & West 1983;Ivansson 1985;Michelena & Harris 1991), even though only a small part of the information contained in the waveform is used. Information about velocity anomalies in an inhomogeneous medium is concealed in the waveform data but is not used in standard traveltime tomographic techniques.…”
Section: Introductionmentioning
confidence: 99%
“…Traveltime inversion algorithms yield good results in some cases, e.g. cross-hole tomography (McMechan 1983;Wong, Hurley & West 1983;Ivansson 1985;Michelena & Harris 1991), even though only a small part of the information contained in the waveform is used. Information about velocity anomalies in an inhomogeneous medium is concealed in the waveform data but is not used in standard traveltime tomographic techniques.…”
Section: Introductionmentioning
confidence: 99%
“…The bias matrix in Trampert & Snieder (1996) shows that spectral leakage is highest for degrees closest to the truncation level. The most common are integral quelling (Chou & Booker 1979), a priori model covariance functions (Tarantola & Nercessian 1984) and finite ray widths (Michelena & Harris 1991). This has been used in the synthetic experiment of Trampert & Snieder (1996).…”
Section: O R R E C T I N G F O R S P E C T R a L L E A K A G Ementioning
confidence: 99%
“…With Tikhonov regularization, the solution will be at most a flattened and/or smoothed model of the earth's subsurface. Nevertheless, the smooth model is not always the best model for geologic structures that are commonly characterized by sharp boundaries and comprise distinct geologic bodies, for example, the sharp petrophysical boundaries between the host rocks and the hydrocarbon reservoir zones (Michelena and Harris, 1991; boundary-preserving regularizations have been developed in image reconstruction to restore sharp edges and high-contrast images (Charbonnier et al, 1997). Some schemes have been applied to geophysical data, for example, the compactness body constraint (Last and Kubik, 1983;Ajo-Franklin et al, 2007), the L p -norm (Claerbout and Muir, 1973;Bube and Langan, 1997;Farquharson, 2008;Zhang and Castagna, 2011;Li et al, 2012;Zhang et al, 2013), total variation regularization (e.g., Farquharson and Oldenburg, 1998), the minimum gradient constraint (Portniaguine and Zhdanov, 1999;Abubakar et al, 2008), and the level-set method (Lelièvre et al, 2012;Li and Leung, 2013;Zheglova et al, 2013;Li et al, 2014).…”
Section: Introductionmentioning
confidence: 99%