Geoscience Reference
In-Depth Information
Fig. 3.21
Vertical section through coherency lineation shown in fig. 3.20 .
(Hesthammer & Fossen, 1997 ) . Careful study of seismic sections and comparison with
well data are needed to avoid this pitfall.
3.2.5
Viewing data in 3-D
All the interpretation technology we have discussed so far works by presenting to the
interpreter a 2-D section through the 3-D data cube. This may be a vertical section
or a map view; as we have seen, the high density of trace data can be very helpful,
particularly when making attribute maps. There is another possibility, however, which
is to present the data to the interpreter as genuinely 3-D images. This is a rapidly
 
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