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In the migrated difference section, and to a lesser extent in
the stacked difference section, some seismic features are visible that
correlate with the known intervals of steam injection.
In the migration difference section, a crisp image of a steam zone
reflection is visible at about 165 ms depth (labeled ``S1''),
which is near the top of the upper steam zone in the P formation.
A fairly strong steam zone reflection (S2) is imaged at the base of
the P formation (210 ms), and a much weaker response (S3) correlates
with the base of the K formation (245 ms). These steam zone reflections
are obtained by migrating the diffraction responses D1-D3, and are
likely to be direct evidence of steam accumulation.
Next: Time pull-up and delay
Up: IMAGES OF FLUID FLOW
Previous: Polarity changes and vanishing
Stanford Exploration Project
11/12/1997