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Chevron Gulf of Mexico Salt Peircement Data

Figure [*] is a field 3D data cube from the Gulf of Mexico provided by Chevron. It consists of structurally simple horizons that have been warped up around a salt peircement. Numerous channels can be seen in time slices. In the time slice at the top of Figure [*], a channel can be seen snaking across the south side.

 
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Figure 4
Chevron Gulf of Mexico data. Notice the beds have been forced up to steep angles by the emplacement of a salt peircement. There is some evidence of channels in the time slice. (a) The time slice at time=$.51\ s$. (b) An in-line section at y=$11436.1\ m$. (c) A cross-line section at x=$12911\ m$.
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Figure [*] shows the flattened output of the data in Figure [*]. The seismic cube has been converted from a stack of time slices to a stack of horizon slices. Notice that the low frequency banding present in the unflattened data is no longer present in the flattened data. This is because horizons are no longer cutting across the image. Several channels are now easily viewed on the horizon slice. Also, notice the salt dome appears to be more localized in Figure [*].

 
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Figure 5
Result of flattening of Figure [*]. The top panel is now a horizon slice displaying several channels. The vertical sections illustrate that the cube is flat in both the x and y directions. (a) The horizon slice at time=$.51\ s$. (b) An in-line section at y=$11436.1\ m$. (c) A cross-line section at x=$12911\ m$.
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Figure [*] displays three horizons overlain on the original data in Figure [*]. The horizons track the reflectors on the flanks of the salt well as expected. Within the salt, the horizons gradually get off their respective reflector events as the estimated dip becomes very inaccurate. The time slice at the top displays the swath of a tracked horizon.

 
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Figure 6
Result of overlaying tracked horizons on the image in Figure [*]. It successfully tracks the horizons even to the considerably steep dips leading into the salt peircement. (a) The time slice at time=$.51\ s$. (b) An in-line section at y=$11436.1\ m$. (c) A cross-line section at x=$12911\ m$.
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next up previous print clean
Next: Elf North Sea Unconformity Up: examples of 3D flattening Previous: Synthetic Data
Stanford Exploration Project
5/3/2005