Equal Spaced Contouring Methods
One of the first Quick Look Techniques to apply when evaluating
a prospect is the method used to contour the map (mechanical, equal-spaced,
parallel or interpretive). Many prospect maps are prepared using
an equal-spaced contouring method. Of all the contouring methods
available (Bishop 1960; Tearpock and Bischke 1991), the equal-spaced
method results in the most optimistic structural interpretation.
This method assumes a slope of uniform dip over a general area mapped.
The use of the equal-spaced method often results in unrealistic
structure maps (Figure 1)
Fig. 1 with highs looking like bubble shaped structures and lows portrayed
as having sharp cusps. Compare the maps shown in Figures 2a and 2b.
Figure 2a

Fig. 2a
is a prospect map showing three proposed locations updip of existing
wells. Notice that the map has been prepared using the equal-spaced
contouring method which shows untested highs adjacent to existing wells
(the elusive high that always escapes penetration
of the drillbit).
Are the three prospective highs shown in Figure 2a real or the result
of the mapping technique? Figure 2b

Fig. 2b
is an alternate interpretation using the same well data, but an interpretive
contouring method which allows the mapper to incorporate his or her
experience, understanding of the structural and depositional geology
of the area, three dimensional geometry, imagination and skill to prepare
a geologically reasonable interpretation. Notice that in Figure 2b,
there is 1, not 3 prospective locations.
No one can really develop a correct interpretation of the subsurface
with the same accuracy as a topographic map. What is more important
is to develop the most reasonable and realistic interpretation of
the subsurface with the available data.
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