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Data from
three seismic lines posted on top of a four-layer model.
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This particular view shows the completed horizons; however, typically users would first look at the data in relationship to just the fault surfaces.
In the first step of horizon gridding, the data are labeled based on which fault block they lie in. In this particular data set, some problems appear in the line farthest from our eye. The figure below shows the same seismic data color-coded based on which fault block it was used in horizon gridding. (For information on how to create the labeled data set in the WorkFlow Manager and/or the Geologic Structure Builder, refer to Labeling Horizon Data in the WorkFlow Manager and Labeling Horizon Data in the Geologic Structure Builder, respectively, below).
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Seismic
data color-coded based on for which fault block each data point
was used in horizon gridding. The marked point is being used
for the wrong fault block.
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The point at the 3D Cursor location is colored in yellow, indicating that it is associated with the fault block on the foot wall of this large reverse fault (the data point is being used to model the horizon in the foot wall because of its lateral position relative to the fault). Clearly, based on its elevation, it should be associated with the fault block of the hanging wall. If modeling proceeded with the data being used as labeled, the horizon in the foot wall would be pulled upward to try to honor the mislabeled point.
Clearly, an acceptable horizon will not be calculated with this data set in its current form since several of the points are labeled in the wrong fault block. There are two solutions to this problem. The best solution is to correct the fault surface so that all the points that should be used in the hanging-wall fault block would be physically within that block (the fault-surface location should be changed usually because typically the accuracy of the fault location is less than the accuracy of the data location).
A second solution, shown here for illustration purposes, is to increase the "fault tolerance" value. The fault tolerance is used to filter out points within a certain distance of a fault surface. These filtered points appear as white in this following illustration.
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Seismic data
color-coded based on for which for which fault block each data
point was used in horizon gridding. The white/gray points are
ones not used in the horizon gridding calculations due to an
increased fault tolerance value.
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This image shows exactly which points are not used in the horizon gridding process when a fault tolerance is applied.
A more extensive discussion of horizon gridding techniques in EarthVision 5 is found in the FAQ section of this web site and, of course, in the EarthVision User's Guide.
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Last updated: March 22, 2007