Dipping planes

The 3D synthetic data set in Figure consists of a single synthetic seismic trace that is replicated and delayed so that the dip in both the x and y directions is unity. Running a dip estimator as in equation () will ideally result in dips of one in each direction.

The results of the flattening method of the data in Figure are shown in Figure . Notice that the dipping planes are now flat and that the time slice on top is all one gray tone, indicating that it is flat.

 

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Figure 3 Test case 2. Curved horizons.

 

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Figure 4 Result of flattening data in Figure .

 

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Figure 5 Test case 3. Chevron Gulf of Mexico data.

 

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Figure 6 Result of flattening data in Figure .

 

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Figure 7 Time slice from Unflattened Chevron Gulf of Mexico data.

 

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Figure 8 Time slice from Flattened Chevron Gulf of Mexico data.