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The time-lapse seismic images show some dramatic changes in
amplitudes along baseline reflectors. Strong reflectivity changes
are visible in the monitor 2 survey, compared to the baseline survey,
along the reflector at the base of the P formation (200 ms).
In the monitor 2 images, at the west (left) side of the injector,
the baseline reflection has almost completely vanished out to the
survey edge. This feature is labeled ``Z'' in the stacked and migrated
images of Figures 6 and 7,
and indicates that an impedance match has occurred across the P/K
formation boundary, perhaps by differential heating from above and below,
or pressure changes in the P formation alone.
On the other side of injector, towards the east (right) the monitor 2
sections show what appears to be a polarity reversal along the P/K
formation boundary at 200 ms, labeled ``Pr''.
This feature is also clearly evident in both
the stacked and migrated and difference sections,
and suggests that the fluid-flow activity in the lower portion of the
P reservoir is different to the east from that to the west.
Next: Imaged steam zones
Up: IMAGES OF FLUID FLOW
Previous: Steam zone diffractions
Stanford Exploration Project
11/12/1997