2013
DOI: 10.1016/j.jappgeo.2013.06.010
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Fast seismic horizon reconstruction based on local dip transformation

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Cited by 22 publications
(8 citation statements)
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“…RGT estimation from a seismic image is a more challenging task than is fault detection. Several types of methods including phase unwrapping (Stark, 2003;Wu and Zhong, 2012) and slope-based methods (Lomask et al, 2006;Fomel, 2010;Parks, 2010;Wu andHale, 2013, 2015;Zinck et al, 2013) have been proposed to perform automatic RGT estimation. However, estimating geologically consistent RGT values across faults, especially the complicated crossing faults, remains a highly challenging problem for all of the methods.…”
Section: Train a Cnn For Rgt And Seismic Horizonsmentioning
confidence: 99%
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“…RGT estimation from a seismic image is a more challenging task than is fault detection. Several types of methods including phase unwrapping (Stark, 2003;Wu and Zhong, 2012) and slope-based methods (Lomask et al, 2006;Fomel, 2010;Parks, 2010;Wu andHale, 2013, 2015;Zinck et al, 2013) have been proposed to perform automatic RGT estimation. However, estimating geologically consistent RGT values across faults, especially the complicated crossing faults, remains a highly challenging problem for all of the methods.…”
Section: Train a Cnn For Rgt And Seismic Horizonsmentioning
confidence: 99%
“…To assist in seismic horizon interpretation, various methods such as phase-unwrapping (Stark, 2003;Wu and Zhong, 2012), waveform classification (Figueiredo et al, 2007(Figueiredo et al, , 2014(Figueiredo et al, , 2015, slope-based methods (Lomask et al, 2006;Fomel, 2010;Parks, 2010;Wu andHale, 2013, 2015;Zinck et al, 2013;Monniron et al, 2016), and multigrid correlation (Wu and Fomel, 2018b) have been proposed to automate the horizon mapping from a seismic image. These methods, however, face a common challenge of dealing with complex structures such as intensive crossing faults and complicated folding, which requires a globally optimal correlation of all the structure elements in a seismic image.…”
Section: Introductionmentioning
confidence: 99%
“…A more stable way of slope-based horizon picking is to compute a weighted least-squares fit of the horizon slopes with the preesti- (Lomask et al, 2006;Wu andHale, 2013, 2015;Zinck et al, 2013). In cases in which the estimated reflection slopes are highly noisy, we can further impose smooth regularizations on the horizon and build the following equations for the 2D slope-based horizon extraction:…”
Section: Least-squares Horizons With Local Slopesmentioning
confidence: 99%
“…A straightforward slope-based horizon extraction method is to pick horizons by starting from seed points and then recursively following the local slopes (Fomel, 2010). Most slope-based methods (e.g., Lomask et al, 2006;Parks, 2010;Wu andHale, 2013, 2015;Zinck et al, 2013;Monniron et al, 2016) compute horizons by fitting the slopes of horizons with the local reflection slopes in the least-squares sense. By recursively following local slopes or fitting local slopes in the least-squares sense, the computed horizons can correctly follow laterally continuous reflections but they often fail to track corresponding reflections across faults because the local slopes cannot correctly correlate reflections across faults.…”
Section: Introductionmentioning
confidence: 99%
“…Dip information can be computed everywhere in the seismic volume [3] and used for flattening the seismic image [4], for stratal slicing or for guiding automated interpretations by correlating neighboring seismic traces [5] [6]. Local correlation between traces can also be exploited for simultaneously tracking multiple horizon patches and identifying those that should be merged to form large scale horizon surfaces [7].…”
Section: Automated Seismic Interpretationmentioning
confidence: 99%