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    3-D seismic discontinuity for faults and stratigraphic features: The coherence cube (1995)
    American Institute of Physics
    In:  The Leading Edge, 14 (10). pp. 1053-1058.
    Details
    Publication Date: 2016-07-26
    Description: Seismic data are usually acquired and processed for imaging reflections. This paper describes a method of processing seismic data for imaging discontinuities (e.g., faults and stratigraphic features). One application of this nontraditional process is a 3-D volume, or cube, of coherence coefficients within which faults are revealed as numerically separated surfaces. Figure 1 compares a traditional 3-D reflection amplitude time slice with the results of the new method. To our knowledge, this is the first published method of revealing fault surfaces within a 3-D volume for which no fault reflections have been recorded.
    Type: Article , PeerReviewed
    Format: text
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