SEG Technical Program Expanded Abstracts 2006 2006
DOI: 10.1190/1.2369825
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Extracting horizon patches and geo‐bodies from 3D seismic waveform sequences

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Cited by 6 publications
(3 citation statements)
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“…Even though these tools become better and faster there are situations where the information a geologist uses is nonlocal -a certain feature cannot be selected based on one (or more) attributes at a certain seismic reflector. To overcome these difficulties methods like sequence classification, Borgos (2006) and textures identification Carrillat (2002) have been used for non-local feature identification. In the case of features only detectable through the combination of different attributes volume co-rendering and sculpting can be used with success.…”
Section: Introductionmentioning
confidence: 99%
“…Even though these tools become better and faster there are situations where the information a geologist uses is nonlocal -a certain feature cannot be selected based on one (or more) attributes at a certain seismic reflector. To overcome these difficulties methods like sequence classification, Borgos (2006) and textures identification Carrillat (2002) have been used for non-local feature identification. In the case of features only detectable through the combination of different attributes volume co-rendering and sculpting can be used with success.…”
Section: Introductionmentioning
confidence: 99%
“…Horizon identification methods that do not rely on growing, such as performing clustering of the voxels based on their local neighborhood [4], result in segmentation masks that are not directly transferable to polygonal surfaces. Incremental growing methods are better suited as they can be made topology aware.…”
Section: Horizon Extraction and Representationmentioning
confidence: 99%
“…There are completely automatic approaches for horizon interpretation [4]. In their work, voxels are mapped to points in an ndimensional space based on their local waveforms.…”
Section: Related Workmentioning
confidence: 99%