A map of the study
area is shown below
in Figure
1. The solid
dots show production wells, many drilled at 40-acre spacing. The circled
dots locate wells where geologic and engineering control was acquired
in the form of modern logs, cores, or pressure tests. The 3-D seismic
area is approximately 7.6-mi2. VSP
control data
were recorded in two closely spaced wells, 175 and 202, inside the triangle
near the center of the 3-D seismic grid. The pressure
interference test
data that
will be analyzed were recorded between these same two wells.

Figure
1. Map of the study area. The solid dots show production wells, many
drilled at 40-acre spacing. The circled dots locate wells where additional
geologic and engineering control was acquired in the form of modern
logs, cores, or pressure tests. The 3-D seismic area is approximately
7.6-mi2. VSP control data were recorded in two closely spaced
wells, 175 and 202, inside the triangle near the center of the 3-D seismic
grid. The pressure interference test was done between these same two
wells.
Figure
2 (below) is
a horizon
slice through
the 3-D seismic data volume that cuts through a targeted thin-bed reservoir
system.
Figure
2. Static reservoir pressures measured during a 1-month period in
the four wells shown in Figure 5. The bottom-hole pressure in well
75 was 300 psi at abandonment. The different reservoir pressure at
these four well locations suggests that each well may be in a different
reservoir compartment.
Figure
3 (below) is
an enlarged view of the reflection
amplitude
behavior on this horizon slice in an area of four critical control wells,
75, 175, 197, and 202. The problem that is to be addressed is to determine
if these four wells penetrate the same reservoir compartment, or are in
different compartments and have no fluid-flow
connection
between them.
Figure
3. Stratigraphic cross section of the reservoir along the 4-well profile
showing the depositional environments interpreted from log shapes and
the initial bottom-hole pressure (BHP) observed in each well. The date
when each well was drilled is shown above the BHP value. The log depths
are measured from KB and the curves are shifted to align on a stratigraphic
datum. The log curves infer that the reservoir in each well was deposited
in a channel environment that shows some evidence of splay deposition.
These log data, by themselves, do not provide enough information to
define where compartment boundaries may exist.
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